Dunne et al. edited dataset containing only occurrences determinate at species level,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,
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,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,,
occurrence_no,record_type,reid_no,flags,collection_no,permissions,identified_name,identified_rank,identified_no,difference,accepted_name,accepted_attr,accepted_rank,accepted_no,ref_author,ref_pubyr,phylum,phylum_no,class,class_no,order,order_no,family,family_no,genus_no,subgenus_no,plant_organ,plant_organ2,abund_unit,lng,lat,collection_name,collection_subset,collection_aka,cc,state,county,latlng_basis,latlng_precision,geogscale,geogcomments,paleomodel,paleolng,paleolat,geoplate,cc.1,protected,formation,stratgroup,member,stratscale,zone,localsection,localbed,localorder,regionalsection,regionalbed,regionalorder,stratcomments,lithdescript,lithology1,lithadj1,lithification1,minor_lithology1,fossilsfrom1,lithology2,lithadj2,lithification2,minor_lithology2,fossilsfrom2,environment,tectonic_setting,geology_comments,assembl_comps,articulated_parts,associated_parts,common_body_parts,rare_body_parts,feed_pred_traces,artifacts,component_comments,pres_mode,preservation_quality,spatial_resolution,temporal_resolution,lagerstatten,concentration,orientation,abund_in_sediment,sorting,fragmentation,bioerosion,encrustation,preservation_comments,collection_type,collection_methods,museum,collection_coverage,collection_size,rock_censused,collectors,collection_dates,collection_comments,taxonomy_comments,taxon_environment,environment_basis,motility,life_habit,vision,diet,reproduction,ontogeny,composition,architecture,thickness,reinforcement,primary_name,primary_reso,subgenus_name,subgenus_reso,research_group,primary_reference,authorizer_no,enterer_no,modifier_no,authorizer,enterer,modifier,created,modified,collection.reference_no,occurrence.species_name,occurrence.genus_name,occurrence.reference_no,occurrence.species_reso,ma_max,ma_min,max_interval,min_interval,occurrence.abund_value,country,occurrence.binomial
146665,occ,NA,,12943,,n. gen. Anconastes n. sp. vesperus,species,136412,,Anconastes vesperus,NA,species,136412,Berman et al.,1987,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,136411,NA,NA,NA,specimens,-106.347778,36.304443,El Cobre Canyon,34761,(Cutler Formation) type horizon of Anconastes vesperus,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"lower portion of exposed section of Cutler Formation, El Cobre Canyon, 11 km northwest of Abiquiu, specimens collected from the floor of the canyon",gp_mid,-34.93,2.53,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"""lower portion of exposed section of the Cutler Formation, [...] approx. 200 and 170 m stratigraphically lower than the Virgilian to Wolfcampian age fossil localities of the Rio Puerco valley and San Diego Canyon""\r\nVirgilian = aka Noginskian","""The dark brown siltstone matrix in which the type specimens described here were preserved indicates deposition in an overbank facies. However, the original bed has been lost to erosion""",siltstone,brown,,,,,,,,,dry floodplain,,"""Cutler Formation redbeds at the horizon of the type locality were deposited in a fluvial system dominated by low sinuosity, multichanneled, mixed load rivers on a narrow braid plain. Numerous small ponds formed adjacent to the braid belts where they were frequently inundated by flood waters and periodically became desiccated.""\r\n",macrofossils,,,,,,NA,,body,good,parautochthonous,,,dispersed,random,,,,NA,,specimens in isolated blocks on canyon floor,taxonomic,"surface (float),field collection",,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Anconastes,n. gen.,NA,NA,vertebrate,"D. S. Berman, R. R. Reisz, and D. A. Eberth. 1987. A new genus and species of trematopid amphibian from the Late Pennsylvanian of north-central New Mexico. Journal of Vertebrate Paleontology 7(3):252-269",4,76,697,J. Alroy,R. Whatley,E. Dunne,11/01/2002 17:57,18/07/2016 08:26,4336,vesperus,Anconastes,4336,n. sp.,305.9,298.9,Missourian,Gzhelian,2,US,Anconastes vesperus
147523,occ,NA,R,13044,,Bolosaurus striatus,species,138029,,Bolosaurus striatus,NA,species,138029,Case,1907,Chordata,33815,Reptilia,36322,,NA,Bolosauridae,37510,37511,NA,NA,NA,individuals,-98.933609,33.611668,Mouth of Godwin Creek,NA,"""Godlin Creek"", Locality XI of Case, 1907",US,Texas,Archer,based on nearby landmark,seconds,small collection,"Near mouth of Godwin Creek, northern portion of Archer County (Vaughn, 1955; for further details see discussion therein). Lat long is for junction of Godwin Creek and North Fork of Little Wichita River.\r\n",gp_mid,-30.27,-1.15,101,US,,Nocona,Wichita,,bed,,,,,,,NA,"Specimens come from a single conglomerate bed sandwiched between a sandstone above and claystone below. ""Case's specimens of A. casei may be assigned then, to the upper Admiral of the Wichita group, Lower Permian of Texas."" (Vaughn, 1955 p. 309).\r\nLower Permian stratigraphy for Texas was modified by Hentz (1988)\r\nthe Admiral Formation is early Artinskian according to Wardlaw 2005, Permophiles (JA)\r\n","Specimens come from a fossiliferous conglomerate bed sandwiched between a sandstone above and a claystone below (see discussion in Vaughn, 1955 pp. 308/309).",conglomerate,red or brown,lithified,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,"selective quarrying,surface (float),surface (in situ),mechanical,field collection,survey of museum collection",AMNH,,,,E. C. Case,1906,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Bolosaurus,,NA,NA,vertebrate,E. C. Case. 1907. Description of the Skull of Bolosaurus striatus Cope. Bulletin of the American Museum of Natural History 23:653-658,21,21,334,C. Sidor,C. Sidor,T. Liebrecht,17/01/2002 11:47,02/04/2009 13:35,5938,striatus,Bolosaurus,5938,,290.1,279.3,Artinskian,,2,US,Bolosaurus striatus
147523,occ,21597,,13044,,n. gen. Ophiodeirus n. sp. casei,species,138981,recombined as,Araeoscelis casei,NA,species,138981,Broom,1913,Chordata,33815,Reptilia,36322,Araeoscelidia,37769,Araeoscelidae,37772,37773,NA,NA,NA,individuals,-98.933609,33.611668,Mouth of Godwin Creek,NA,"""Godlin Creek"", Locality XI of Case, 1907",US,Texas,Archer,based on nearby landmark,seconds,small collection,"Near mouth of Godwin Creek, northern portion of Archer County (Vaughn, 1955; for further details see discussion therein). Lat long is for junction of Godwin Creek and North Fork of Little Wichita River.\r\n",gp_mid,-30.27,-1.15,101,US,,Nocona,Wichita,,bed,,,,,,,NA,"Specimens come from a single conglomerate bed sandwiched between a sandstone above and claystone below. ""Case's specimens of A. casei may be assigned then, to the upper Admiral of the Wichita group, Lower Permian of Texas."" (Vaughn, 1955 p. 309).\r\nLower Permian stratigraphy for Texas was modified by Hentz (1988)\r\nthe Admiral Formation is early Artinskian according to Wardlaw 2005, Permophiles (JA)\r\n","Specimens come from a fossiliferous conglomerate bed sandwiched between a sandstone above and a claystone below (see discussion in Vaughn, 1955 pp. 308/309).",conglomerate,red or brown,lithified,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,"selective quarrying,surface (float),surface (in situ),mechanical,field collection,survey of museum collection",AMNH,,,,E. C. Case,1906,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiodeirus,n. gen.,NA,NA,vertebrate,R. Broom. 1913. On the Structure and Affinities of Bolosaurus. Bulletin of the American Museum of Natural History 32:509-516,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,02/04/2009 11:33,02/04/2009 13:35,5938,casei,Araeoscelis,28940,n. sp.,290.1,279.3,Artinskian,,2,US,Araeoscelis casei
147563,occ,NA,,13046,,Broiliellus n. sp. arroyoensis,species,136989,,Broiliellus arroyoensis,NA,species,136989,DeMar,1967,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37024,NA,NA,NA,specimens,-99.199997,33.809723,Broiliellus pocket,28256,East Coffee Creek,US,Texas,Baylor,based on nearby landmark,seconds,small collection,DMS coordinates are for mouth of East Coffee Creek into Lake Kemp.,gp_mid,-28.89,1.8,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,medium,,snapshot,,,,,,,NA,,,taxonomic,"mechanical,survey of museum collection",,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Broiliellus,,NA,NA,vertebrate,R. E. DeMar. 1967. Two new species of Broiliellus (amphibians) from the Permian of Texas. Fieldiana Geology 16(5):117-129,21,21,697,C. Sidor,C. Sidor,E. Dunne,17/01/2002 12:16,04/07/2016 06:41,4333,arroyoensis,Broiliellus,4333,n. sp.,279.3,272.3,Kungurian,,6,US,Broiliellus arroyoensis
147564,occ,NA,,13048,,Broiliellus n. sp. olsoni,species,136990,,Broiliellus olsoni,NA,species,136990,DeMar,1967,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37024,NA,NA,NA,specimens,-98.147781,33.826389,Thaxton Ranch,NA,Texas Ranch,US,Texas,Clay,estimated from map,seconds,small collection,"Thaxton Ranch (more commonly known as Texas Ranch) is about 2 mi ENE of Henrietta, Clay Co.",gp_mid,-29.58,-1.28,101,US,,,Wichita,,,,,,,,,NA,possibly from the Admiral Fm. (p. 127),,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,medium,,,,,,,,,NA,,,taxonomic,mechanical,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Broiliellus,,NA,NA,vertebrate,R. E. DeMar. 1967. Two new species of Broiliellus (amphibians) from the Permian of Texas. Fieldiana Geology 16(5):117-129,21,21,0,C. Sidor,C. Sidor,,17/01/2002 12:31,17/01/2002 14:31,4333,olsoni,Broiliellus,4333,n. sp.,296.4,268,Wolfcamp,,2,US,Broiliellus olsoni
147591,occ,NA,,13049,,Edaphosaurus n. sp. colohistion,species,122353,,Edaphosaurus colohistion,NA,species,122353,Berman,1979,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,specimens,-80.62722,40.044167,I-70 Roadcut half mile East of Elm Grove,NA,,US,West Virginia,Ohio,estimated from map,seconds,small collection,"Road cut on Interstate highway 70, about 1/2 mile east of Elm Grove, West Virginia (p. 187)",gp_mid,-15.2,-3.5,101,US,,Pittsburgh,Monongahela,Limestone B,bed,,,,,,,NA,"Stratigraphy update (2012-02-20): The Pittsburgh Fm. is the lower unit of the Monongahela Group and is entirely within the Virgilian (see, e.g. Eble et al., 2006, pp. 197-222 in GSA Spec. Pap. 399) [TL]",,not reported,,,,,,,,,,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,"""The deposit from which the holotype was collected has been described by Lund (1972:51) as a meander cutoff channel that filled slowly."" p. 187",taxonomic,"selective quarrying,surface (in situ),mechanical,field collection,survey of museum collection",,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,"D. S. Berman. 1979. Edaphosaurus (Reptilia, Pelycosauria) from the Lower Permian of Northeastern United States, with description of a new species. Annals of the Carnegie Museum 48(11):185-202",21,21,0,C. Sidor,C. Sidor,,17/01/2002 12:52,17/01/2002 14:52,4337,colohistion,Edaphosaurus,4337,n. sp.,303.4,298.9,Virgilian,,1,US,Edaphosaurus colohistion
148242,occ,NA,,13080,,Cricotus sp.,genus,37197,,Cricotus,NA,genus,37197,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37197,NA,NA,NA,specimens,-98.856941,33.622501,Briar Creek,NA,"(Admiral Formation) Locality 13 (Romer 1928), Locality IVd (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds; Brier Creek",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""the collecting ground being mainly on the east side a few miles from the mouth, near and in the bone bed discovered by Case."" Lat long is for Dundee, approx. 9 mi south of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""; DMS coordinates are for the mouth of Briar Creek into Lake Kickapoo",gp_mid,-30.21,-1.18,101,US,,Admiral,Wichita,,bed,,,,,,,NA,"""about 190 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Admiral Formation and middle Wichita Group are both Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones."" ",claystone,red,,,,sandstone,red,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cricotus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,18/01/2002 14:08,16/08/2016 05:30,7693,sp.,Cricotus,7693,,290.1,279.3,Artinskian,,39,US,Cricotus sp.
148243,occ,NA,,13080,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.856941,33.622501,Briar Creek,NA,"(Admiral Formation) Locality 13 (Romer 1928), Locality IVd (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds; Brier Creek",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""the collecting ground being mainly on the east side a few miles from the mouth, near and in the bone bed discovered by Case."" Lat long is for Dundee, approx. 9 mi south of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""; DMS coordinates are for the mouth of Briar Creek into Lake Kickapoo",gp_mid,-30.21,-1.18,101,US,,Admiral,Wichita,,bed,,,,,,,NA,"""about 190 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Admiral Formation and middle Wichita Group are both Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones."" ",claystone,red,,,,sandstone,red,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,18/01/2002 14:08,16/08/2016 05:30,7693,sp.,Eryops,7693,,290.1,279.3,Artinskian,,56,US,Eryops sp.
148244,occ,NA,,13080,,Aspidosaurus sp.,genus,37021,,Aspidosaurus,NA,genus,37021,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37021,NA,NA,NA,specimens,-98.856941,33.622501,Briar Creek,NA,"(Admiral Formation) Locality 13 (Romer 1928), Locality IVd (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds; Brier Creek",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""the collecting ground being mainly on the east side a few miles from the mouth, near and in the bone bed discovered by Case."" Lat long is for Dundee, approx. 9 mi south of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""; DMS coordinates are for the mouth of Briar Creek into Lake Kickapoo",gp_mid,-30.21,-1.18,101,US,,Admiral,Wichita,,bed,,,,,,,NA,"""about 190 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Admiral Formation and middle Wichita Group are both Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones."" ",claystone,red,,,,sandstone,red,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Aspidosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,18/01/2002 14:08,16/08/2016 05:30,7693,sp.,Aspidosaurus,7693,,290.1,279.3,Artinskian,,2,US,Aspidosaurus sp.
148245,occ,NA,,13080,,Zatrachys serratus,species,255221,,Zatrachys serratus,NA,species,255221,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,specimens,-98.856941,33.622501,Briar Creek,NA,"(Admiral Formation) Locality 13 (Romer 1928), Locality IVd (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds; Brier Creek",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""the collecting ground being mainly on the east side a few miles from the mouth, near and in the bone bed discovered by Case."" Lat long is for Dundee, approx. 9 mi south of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""; DMS coordinates are for the mouth of Briar Creek into Lake Kickapoo",gp_mid,-30.21,-1.18,101,US,,Admiral,Wichita,,bed,,,,,,,NA,"""about 190 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Admiral Formation and middle Wichita Group are both Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones."" ",claystone,red,,,,sandstone,red,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,18/01/2002 14:08,16/08/2016 05:30,7693,serratus,Zatrachys,7693,,290.1,279.3,Artinskian,,1,US,Zatrachys serratus
148246,occ,NA,,13080,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-98.856941,33.622501,Briar Creek,NA,"(Admiral Formation) Locality 13 (Romer 1928), Locality IVd (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds; Brier Creek",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""the collecting ground being mainly on the east side a few miles from the mouth, near and in the bone bed discovered by Case."" Lat long is for Dundee, approx. 9 mi south of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""; DMS coordinates are for the mouth of Briar Creek into Lake Kickapoo",gp_mid,-30.21,-1.18,101,US,,Admiral,Wichita,,bed,,,,,,,NA,"""about 190 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Admiral Formation and middle Wichita Group are both Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones."" ",claystone,red,,,,sandstone,red,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,18/01/2002 14:08,16/08/2016 05:30,7693,sp.,Trimerorhachis,7693,,290.1,279.3,Artinskian,,3,US,Trimerorhachis sp.
148247,occ,NA,,13080,,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,specimens,-98.856941,33.622501,Briar Creek,NA,"(Admiral Formation) Locality 13 (Romer 1928), Locality IVd (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds; Brier Creek",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""the collecting ground being mainly on the east side a few miles from the mouth, near and in the bone bed discovered by Case."" Lat long is for Dundee, approx. 9 mi south of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""; DMS coordinates are for the mouth of Briar Creek into Lake Kickapoo",gp_mid,-30.21,-1.18,101,US,,Admiral,Wichita,,bed,,,,,,,NA,"""about 190 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Admiral Formation and middle Wichita Group are both Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones."" ",claystone,red,,,,sandstone,red,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,18/01/2002 14:08,16/08/2016 05:30,7693,sp.,Diplocaulus,7693,,290.1,279.3,Artinskian,,1,US,Diplocaulus sp.
148248,occ,NA,,13080,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-98.856941,33.622501,Briar Creek,NA,"(Admiral Formation) Locality 13 (Romer 1928), Locality IVd (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds; Brier Creek",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""the collecting ground being mainly on the east side a few miles from the mouth, near and in the bone bed discovered by Case."" Lat long is for Dundee, approx. 9 mi south of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""; DMS coordinates are for the mouth of Briar Creek into Lake Kickapoo",gp_mid,-30.21,-1.18,101,US,,Admiral,Wichita,,bed,,,,,,,NA,"""about 190 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Admiral Formation and middle Wichita Group are both Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones."" ",claystone,red,,,,sandstone,red,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,18/01/2002 14:08,16/08/2016 05:30,7693,sp.,Diadectes,7693,,290.1,279.3,Artinskian,,3,US,Diadectes sp.
148249,occ,NA,,13080,,n. gen. Archeria n. sp. robinsoni,species,345354,subjective synonym of,Archeria crassidisca,NA,species,229309,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,specimens,-98.856941,33.622501,Briar Creek,NA,"(Admiral Formation) Locality 13 (Romer 1928), Locality IVd (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds; Brier Creek",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""the collecting ground being mainly on the east side a few miles from the mouth, near and in the bone bed discovered by Case."" Lat long is for Dundee, approx. 9 mi south of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""; DMS coordinates are for the mouth of Briar Creek into Lake Kickapoo",gp_mid,-30.21,-1.18,101,US,,Admiral,Wichita,,bed,,,,,,,NA,"""about 190 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Admiral Formation and middle Wichita Group are both Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones."" ",claystone,red,,,,sandstone,red,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,n. gen.,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,18/01/2002 14:08,16/08/2016 05:30,7693,robinsoni,Archeria,7693,n. sp.,290.1,279.3,Artinskian,,4,US,Archeria robinsoni
148250,occ,NA,,13080,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-98.856941,33.622501,Briar Creek,NA,"(Admiral Formation) Locality 13 (Romer 1928), Locality IVd (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds; Brier Creek",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""the collecting ground being mainly on the east side a few miles from the mouth, near and in the bone bed discovered by Case."" Lat long is for Dundee, approx. 9 mi south of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""; DMS coordinates are for the mouth of Briar Creek into Lake Kickapoo",gp_mid,-30.21,-1.18,101,US,,Admiral,Wichita,,bed,,,,,,,NA,"""about 190 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Admiral Formation and middle Wichita Group are both Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones."" ",claystone,red,,,,sandstone,red,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,18/01/2002 14:08,16/08/2016 05:30,7693,sp.,Ophiacodon,7693,,290.1,279.3,Artinskian,,11,US,Ophiacodon sp.
148257,occ,NA,,13083,,n. gen. Noteosaurus n. sp. africanus,species,138739,nomen dubium,Mesosauridae,NA,family,37578,Modesto,1996,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Mesosauridae,37578,NA,NA,NA,NA,individuals,23.116667,-31.4,Victoria West District,NA," (""Dwyka Formation"") Karoo, Karroo",ZA,Northern Cape,Victoria West (Ubuntu),based on nearby landmark,minutes,small collection,"""Reported by Broom (1913) to have been collected from the Dwyka Formation in the Victoria West District, South Africa."" (Modesto, 1996).\r\nDMS coordinates are for town of Victoria West.",gp_mid,-47.63,-62.51,701,ZA,,Whitehill,Ecca,,bed,,,,,,,NA,"Stratigraphic range originally entered as >>Rotliegend<<.\r\nThe name ""Dwyka"", formerly applied to the Permo-Carboniferous glacial deposits als well as to the shales directly overlying them (""Upper Shales"" = Prince Albert and Whitehill Formations; cf., e. g., Chapter VII ""The Karroo System"" in Rogers & Du Toit, 1909, An Introduction to the Geology of Cape Colony, 2nd ed.; Catuneanu et al., 2005, J. Afr. Earth Sci. 43), now is exclusively restricted to the glacial deposits and all the overlying shales are entirely included in the Ecca Group (Catuneanu et al., 2005 fig. 2). Also, Broom (1909 in Rogers & Du Toit) and later Oelofsen & Araujo (1987, S. Afr. J. Sci. 83) say that the occurrence of mesosaurs in South Africa is exclusively restricted to the Whitehill Formation (""the White Band"") of the Ecca Group. Thus, the type locality of Noteosaururus africanus is tentatively assigned to the Whitehill Formation in the present collection record.\r\nRadiometric ages of the Collinson Fm. (overlying the Whitehill Fm.) vary between 270 and 275 Ma (Turner, 1999, J. Afr. Earth Sci. 28(1); Fildani et al., 2007 J. Sedim. Res. 77), and radiometric ages of the basal beds of the Prince Albert Fm. (underlying the Whitehill Fm.) vary between 293 and 285 Ma (Bangert et al., 1999, J. Afr. Earth Sci. 29(1)), implying an Artinskian age for the Whitehill Fm. (see time scales of Gradstein et al. (2004) and Ogg et al. (2008)). Radiometric dating within the Whitehill Fm. of southern Namibia (Werner, 2006, PhD thesis, http://www.opus-bayern.de/uni-wuerzburg/volltexte/2007/2175/pdf/00-Complete_thesis-STD.pdf) corroborates an assigment to the Artinskian. ","not reported but probably a dark, whitish weathering shale",not reported,,,,,,,,,,marine indet.,foreland basin,There is no consensus about the true nature (lacustrine/brackish/fully marine) of the water body in which the mesosaurs lived. The environment is tentatively chosen to have been marine. ,macrofossils,,,,,,NA,,mold/impression,variable,autochthonous,time-averaged,,,,,,,NA,,"Articulated partial skeleton in a single block.\r\n""SAM 2358, like all specimens referrable to Mesosaurus and some Stereosternum material, is an impression of the original skeleton [...]"" (Modesto, 1996).",taxonomic,survey of museum collection,,,,,,,"SAM = South African Museum, Cape Town","Two other mesosaurid taxa are present in the ""Dwyka Formation"", Mesosaurus tenuidens, and Stereosternum tumidum (otherwise known from South America). Specific localities are not indicated. ","coastal,marine,brackish",NA,actively mobile,amphibious,NA,piscivore,dispersal=direct/internal,"addition of parts,modification of parts",hydroxyapatite,,NA,,Noteosaurus,n. gen.,NA,NA,vertebrate,S. P. Modesto. 1996. Noteosaurus africanus Broom is a nomen dubium. Journal of Vertebrate Paleontology 16(1):172-174,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,18/01/2002 16:12,05/01/2009 17:21,4307,africanus,,4307,n. sp.,290.1,279.3,Artinskian,,1,ZA, africanus
149618,occ,NA,,13219,,Dendrerpeton sp.,genus,36995,,Dendrerpeton,NA,genus,36995,Milner,1982,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dendrerpetonidae,36994,36995,NA,NA,NA,individuals,-64.316666,45.400002,Main Bluff at West Bay,NA,(Parrsboro Formation) West Bay southwest of Parrsboro,CA,Nova Scotia,Cumberland,based on nearby landmark,minutes,outcrop,"Lat long is for Parrsboro. See Carroll, R. L., E. S. Belt, D. L. Dineley, D. Baird and D. C. McGregor. 1972. Excursion A59, Vertebrate paleontology of eastern Canada. Guidebook, 24th Int. Geol. Cong. 1-113. (fig. 10) for specific locality. Specimen was found ""in the upright core of a lycopod stump at the talus of the main bluff near the midpoint of West Bay.""",gp_mid,-10.26,-13.62,108,CA,,Parrsboro,Mabou,,group of beds,,,,,,,NA,"The lycopod stump containing the specimen was in the grey upper facies of the Parrsboro Formation. ""horizon appears to be of late Early Pennsylvanian (=late Westphalian A) age (Carroll et al. 1972).""",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,snapshot,,,,,,,NA,,"Specimen was found ""in the upright core of a lycopod stump at the talus of the main bluff near the midpoint of West Bay.""",taxonomic,survey of museum collection,,,,,,,"This specimen first mentioned in Romer 1966, p. 362, as ""Eugyrinus ?NA"", and is referred to in Carroll, Belt, Dineley, Baird, and McGregor 1972, p. 63 (a guidebook) as a ""Eugyrinus-like skull"".",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Dendrerpeton,,NA,NA,vertebrate,A. R. Milner. 1982. A small Temnospondyl Amphibian from the Lower Pennsylvanian of Nova Scotia. Journal of Paleontology 56(5):1302-1305,4,76,76,J. Alroy,R. Whatley,R. Whatley,29/01/2002 13:51,05/12/2002 17:45,4391,sp.,Dendrerpeton,4391,,318.1,314.6,Westphalian A,,1,CA,Dendrerpeton sp.
149740,occ,NA,,13257,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Vaughn,1962,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-109.848053,37.174168,Platyhystrix pocket Locality,NA,(Cutler Formation) Halgaito Tongue,US,Utah,San Juan,based on nearby landmark,seconds,,"NW 1/4 Sec. 21, T. 42S, R. 19 E. Lime Creek Valley\r\nLat.Long. based on Mexican Hat Rock",gp_mid,-35.77,6.4,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"""The known fossils from the Halgaito tongue of the Cutler Formation, with rare exceptions, were found in lenses of channel conglomerates or in cross-bedded sandstones immediately above, below, or at the lateral edges of such conglomerates.""",Finely laminated red sandstone and conglomerates.,sandstone,"""cross stratification"",red",,,Y,conglomerate,"pebbly,gray,red or brown",,calcareous,,"""channel""",,,macrofossils,,,,,,NA,,"body,cast",,,,,,,,,frequent,NA,,,taxonomic,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"P. P. Vaughn. 1962. Vertebrates from the Halgaito Tongue of the Cutler Formation, Permian of San Juan County, Utah. Journal of Paleontology 36(3):529-539",4,76,0,J. Alroy,R. Whatley,,02/02/2002 19:23,02/02/2002 21:23,4394,sp.,Eryops,4394,,298.9,290.1,Asselian,Sakmarian,NA,US,Eryops sp.
149741,occ,NA,,13257,,cf. Platyhystrix rugosus,species,345923,,Platyhystrix rugosus,NA,species,194929,Vaughn,1962,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37034,NA,NA,NA,,-109.848053,37.174168,Platyhystrix pocket Locality,NA,(Cutler Formation) Halgaito Tongue,US,Utah,San Juan,based on nearby landmark,seconds,,"NW 1/4 Sec. 21, T. 42S, R. 19 E. Lime Creek Valley\r\nLat.Long. based on Mexican Hat Rock",gp_mid,-35.77,6.4,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"""The known fossils from the Halgaito tongue of the Cutler Formation, with rare exceptions, were found in lenses of channel conglomerates or in cross-bedded sandstones immediately above, below, or at the lateral edges of such conglomerates.""",Finely laminated red sandstone and conglomerates.,sandstone,"""cross stratification"",red",,,Y,conglomerate,"pebbly,gray,red or brown",,calcareous,,"""channel""",,,macrofossils,,,,,,NA,,"body,cast",,,,,,,,,frequent,NA,,,taxonomic,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Platyhystrix,cf.,NA,NA,vertebrate,"P. P. Vaughn. 1962. Vertebrates from the Halgaito Tongue of the Cutler Formation, Permian of San Juan County, Utah. Journal of Paleontology 36(3):529-539",4,76,0,J. Alroy,R. Whatley,,02/02/2002 19:23,02/02/2002 21:23,4394,rugosus,Platyhystrix,4394,,298.9,290.1,Asselian,Sakmarian,NA,US,Platyhystrix rugosus
149742,occ,NA,,13257,,Nectridea ? indet.,unranked clade,37260,,Nectridea,NA,unranked clade,37260,Vaughn,1962,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,individuals,-109.848053,37.174168,Platyhystrix pocket Locality,NA,(Cutler Formation) Halgaito Tongue,US,Utah,San Juan,based on nearby landmark,seconds,,"NW 1/4 Sec. 21, T. 42S, R. 19 E. Lime Creek Valley\r\nLat.Long. based on Mexican Hat Rock",gp_mid,-35.77,6.4,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"""The known fossils from the Halgaito tongue of the Cutler Formation, with rare exceptions, were found in lenses of channel conglomerates or in cross-bedded sandstones immediately above, below, or at the lateral edges of such conglomerates.""",Finely laminated red sandstone and conglomerates.,sandstone,"""cross stratification"",red",,,Y,conglomerate,"pebbly,gray,red or brown",,calcareous,,"""channel""",,,macrofossils,,,,,,NA,,"body,cast",,,,,,,,,frequent,NA,,,taxonomic,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Nectridea,?,NA,NA,vertebrate,"P. P. Vaughn. 1962. Vertebrates from the Halgaito Tongue of the Cutler Formation, Permian of San Juan County, Utah. Journal of Paleontology 36(3):529-539",4,76,0,J. Alroy,R. Whatley,,02/02/2002 19:23,02/02/2002 21:23,4394,indet.,,4394,,298.9,290.1,Asselian,Sakmarian,2,US, indet.
149743,occ,NA,,13257,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Vaughn,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-109.848053,37.174168,Platyhystrix pocket Locality,NA,(Cutler Formation) Halgaito Tongue,US,Utah,San Juan,based on nearby landmark,seconds,,"NW 1/4 Sec. 21, T. 42S, R. 19 E. Lime Creek Valley\r\nLat.Long. based on Mexican Hat Rock",gp_mid,-35.77,6.4,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"""The known fossils from the Halgaito tongue of the Cutler Formation, with rare exceptions, were found in lenses of channel conglomerates or in cross-bedded sandstones immediately above, below, or at the lateral edges of such conglomerates.""",Finely laminated red sandstone and conglomerates.,sandstone,"""cross stratification"",red",,,Y,conglomerate,"pebbly,gray,red or brown",,calcareous,,"""channel""",,,macrofossils,,,,,,NA,,"body,cast",,,,,,,,,frequent,NA,,,taxonomic,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"P. P. Vaughn. 1962. Vertebrates from the Halgaito Tongue of the Cutler Formation, Permian of San Juan County, Utah. Journal of Paleontology 36(3):529-539",4,76,0,J. Alroy,R. Whatley,,02/02/2002 19:23,02/02/2002 21:23,4394,sp.,Diadectes,4394,,298.9,290.1,Asselian,Sakmarian,1,US,Diadectes sp.
149744,occ,NA,,13257,,Limnoscelidae indet.,family,37231,,Limnoscelidae,NA,family,37231,Vaughn,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Limnoscelidae,37231,NA,NA,NA,NA,specimens,-109.848053,37.174168,Platyhystrix pocket Locality,NA,(Cutler Formation) Halgaito Tongue,US,Utah,San Juan,based on nearby landmark,seconds,,"NW 1/4 Sec. 21, T. 42S, R. 19 E. Lime Creek Valley\r\nLat.Long. based on Mexican Hat Rock",gp_mid,-35.77,6.4,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"""The known fossils from the Halgaito tongue of the Cutler Formation, with rare exceptions, were found in lenses of channel conglomerates or in cross-bedded sandstones immediately above, below, or at the lateral edges of such conglomerates.""",Finely laminated red sandstone and conglomerates.,sandstone,"""cross stratification"",red",,,Y,conglomerate,"pebbly,gray,red or brown",,calcareous,,"""channel""",,,macrofossils,,,,,,NA,,"body,cast",,,,,,,,,frequent,NA,,,taxonomic,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Limnoscelidae,,NA,NA,vertebrate,"P. P. Vaughn. 1962. Vertebrates from the Halgaito Tongue of the Cutler Formation, Permian of San Juan County, Utah. Journal of Paleontology 36(3):529-539",4,76,0,J. Alroy,R. Whatley,,02/02/2002 19:23,02/02/2002 21:23,4394,indet.,,4394,,298.9,290.1,Asselian,Sakmarian,1,US, indet.
149745,occ,NA,,13257,,cf. Ophiacodon navajovicus,species,122334,,Ophiacodon navajovicus,NA,species,54987,Vaughn,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-109.848053,37.174168,Platyhystrix pocket Locality,NA,(Cutler Formation) Halgaito Tongue,US,Utah,San Juan,based on nearby landmark,seconds,,"NW 1/4 Sec. 21, T. 42S, R. 19 E. Lime Creek Valley\r\nLat.Long. based on Mexican Hat Rock",gp_mid,-35.77,6.4,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"""The known fossils from the Halgaito tongue of the Cutler Formation, with rare exceptions, were found in lenses of channel conglomerates or in cross-bedded sandstones immediately above, below, or at the lateral edges of such conglomerates.""",Finely laminated red sandstone and conglomerates.,sandstone,"""cross stratification"",red",,,Y,conglomerate,"pebbly,gray,red or brown",,calcareous,,"""channel""",,,macrofossils,,,,,,NA,,"body,cast",,,,,,,,,frequent,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,cf.,NA,NA,vertebrate,"P. P. Vaughn. 1962. Vertebrates from the Halgaito Tongue of the Cutler Formation, Permian of San Juan County, Utah. Journal of Paleontology 36(3):529-539",4,76,0,J. Alroy,R. Whatley,,02/02/2002 19:23,02/02/2002 21:23,4394,navajovicus,Ophiacodon,4394,,298.9,290.1,Asselian,Sakmarian,NA,US,Ophiacodon navajovicus
149746,occ,NA,,13257,,Sphenacodontidae indet.,family,38901,,Sphenacodontidae,NA,family,38901,Vaughn,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,NA,NA,NA,NA,individuals,-109.848053,37.174168,Platyhystrix pocket Locality,NA,(Cutler Formation) Halgaito Tongue,US,Utah,San Juan,based on nearby landmark,seconds,,"NW 1/4 Sec. 21, T. 42S, R. 19 E. Lime Creek Valley\r\nLat.Long. based on Mexican Hat Rock",gp_mid,-35.77,6.4,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"""The known fossils from the Halgaito tongue of the Cutler Formation, with rare exceptions, were found in lenses of channel conglomerates or in cross-bedded sandstones immediately above, below, or at the lateral edges of such conglomerates.""",Finely laminated red sandstone and conglomerates.,sandstone,"""cross stratification"",red",,,Y,conglomerate,"pebbly,gray,red or brown",,calcareous,,"""channel""",,,macrofossils,,,,,,NA,,"body,cast",,,,,,,,,frequent,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodontidae,,NA,NA,vertebrate,"P. P. Vaughn. 1962. Vertebrates from the Halgaito Tongue of the Cutler Formation, Permian of San Juan County, Utah. Journal of Paleontology 36(3):529-539",4,76,0,J. Alroy,R. Whatley,,02/02/2002 19:23,02/02/2002 21:23,4394,indet.,,4394,,298.9,290.1,Asselian,Sakmarian,1,US, indet.
157307,occ,NA,,13947,,Eryops ? sp.,genus,37011,,Eryops,NA,genus,37011,Kissel and Lehman,2002,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-96.699997,34.933334,OMNH V1005,NA,,US,Oklahoma,Seminole,based on nearby landmark,minutes,small collection,"""just north of the Canadian River""; shown on map as due north of Ada, in the southermost part of Seminole County; this is just north of the town of Tyrola",gp_mid,-28.89,-2.47,101,US,,Ada,,,bed,,,,,,,NA,"from a ""single stratigraphic horizon... 22.4 m above the contact"" with the ""underlying Vamoosa Formation""",,mudstone,gray,,,,,,,,,coarse channel fill,,"bone horizon is from ""tributary channel fill deposits"" immediately below a layer of ""pedogenic carbonate nodules""",macrofossils,,,,,,NA,,body,,allochthonous,time-averaged,,,preferred,,,occasional,NA,,,taxonomic,"selective quarrying,surface (float),sieve,field collection",,,250 specimens,,,,"All of the in situ specimens recovered from the locality were found within a single stratigraphic horizon stretching approximately 11 m along the face of the outcrop. Screenwashing of 40 kg of sediment recovered ""very little additional material""","authors report minimum number of individuals, but material is transported and allochthonous, so specimen counts are recorded instead","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,?,NA,NA,vertebrate,"R. A. Kissel and T. M. Lehman. 2002. Upper Pennsylvanian tetrapods from the Ada Formation of Seminole County, Oklahoma. Journal of Paleontology 76(3):529-545",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,05/05/2002 16:35,10/11/2009 10:12,6174,sp.,Eryops,6174,,303.4,298.9,Virgilian,,3,US,Eryops sp.
157308,occ,NA,,13947,,Diasparactus zenos,species,157286,recombined as,Diadectes zenos,NA,species,157286,Kissel and Lehman,2002,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-96.699997,34.933334,OMNH V1005,NA,,US,Oklahoma,Seminole,based on nearby landmark,minutes,small collection,"""just north of the Canadian River""; shown on map as due north of Ada, in the southermost part of Seminole County; this is just north of the town of Tyrola",gp_mid,-28.89,-2.47,101,US,,Ada,,,bed,,,,,,,NA,"from a ""single stratigraphic horizon... 22.4 m above the contact"" with the ""underlying Vamoosa Formation""",,mudstone,gray,,,,,,,,,coarse channel fill,,"bone horizon is from ""tributary channel fill deposits"" immediately below a layer of ""pedogenic carbonate nodules""",macrofossils,,,,,,NA,,body,,allochthonous,time-averaged,,,preferred,,,occasional,NA,,,taxonomic,"selective quarrying,surface (float),sieve,field collection",,,250 specimens,,,,"All of the in situ specimens recovered from the locality were found within a single stratigraphic horizon stretching approximately 11 m along the face of the outcrop. Screenwashing of 40 kg of sediment recovered ""very little additional material""","authors report minimum number of individuals, but material is transported and allochthonous, so specimen counts are recorded instead","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diasparactus,,NA,NA,vertebrate,"R. A. Kissel and T. M. Lehman. 2002. Upper Pennsylvanian tetrapods from the Ada Formation of Seminole County, Oklahoma. Journal of Paleontology 76(3):529-545",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,05/05/2002 16:35,10/11/2009 10:12,6174,zenos,Diadectes,6174,,303.4,298.9,Virgilian,,3,US,Diadectes zenos
157309,occ,NA,,13947,,Ophiacodon cf. mirus,species,123418,,Ophiacodon mirus,NA,species,123418,Kissel and Lehman,2002,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-96.699997,34.933334,OMNH V1005,NA,,US,Oklahoma,Seminole,based on nearby landmark,minutes,small collection,"""just north of the Canadian River""; shown on map as due north of Ada, in the southermost part of Seminole County; this is just north of the town of Tyrola",gp_mid,-28.89,-2.47,101,US,,Ada,,,bed,,,,,,,NA,"from a ""single stratigraphic horizon... 22.4 m above the contact"" with the ""underlying Vamoosa Formation""",,mudstone,gray,,,,,,,,,coarse channel fill,,"bone horizon is from ""tributary channel fill deposits"" immediately below a layer of ""pedogenic carbonate nodules""",macrofossils,,,,,,NA,,body,,allochthonous,time-averaged,,,preferred,,,occasional,NA,,,taxonomic,"selective quarrying,surface (float),sieve,field collection",,,250 specimens,,,,"All of the in situ specimens recovered from the locality were found within a single stratigraphic horizon stretching approximately 11 m along the face of the outcrop. Screenwashing of 40 kg of sediment recovered ""very little additional material""","authors report minimum number of individuals, but material is transported and allochthonous, so specimen counts are recorded instead",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,"R. A. Kissel and T. M. Lehman. 2002. Upper Pennsylvanian tetrapods from the Ada Formation of Seminole County, Oklahoma. Journal of Paleontology 76(3):529-545",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,05/05/2002 16:35,10/11/2009 10:12,6174,mirus,Ophiacodon,6174,cf.,303.4,298.9,Virgilian,,30,US,Ophiacodon mirus
157310,occ,NA,,13947,,Sphenacodontia indet.,suborder,95328,,Sphenacodontia,NA,suborder,95328,Kissel and Lehman,2002,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,NA,NA,NA,NA,specimens,-96.699997,34.933334,OMNH V1005,NA,,US,Oklahoma,Seminole,based on nearby landmark,minutes,small collection,"""just north of the Canadian River""; shown on map as due north of Ada, in the southermost part of Seminole County; this is just north of the town of Tyrola",gp_mid,-28.89,-2.47,101,US,,Ada,,,bed,,,,,,,NA,"from a ""single stratigraphic horizon... 22.4 m above the contact"" with the ""underlying Vamoosa Formation""",,mudstone,gray,,,,,,,,,coarse channel fill,,"bone horizon is from ""tributary channel fill deposits"" immediately below a layer of ""pedogenic carbonate nodules""",macrofossils,,,,,,NA,,body,,allochthonous,time-averaged,,,preferred,,,occasional,NA,,,taxonomic,"selective quarrying,surface (float),sieve,field collection",,,250 specimens,,,,"All of the in situ specimens recovered from the locality were found within a single stratigraphic horizon stretching approximately 11 m along the face of the outcrop. Screenwashing of 40 kg of sediment recovered ""very little additional material""","authors report minimum number of individuals, but material is transported and allochthonous, so specimen counts are recorded instead",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodontia,,NA,NA,vertebrate,"R. A. Kissel and T. M. Lehman. 2002. Upper Pennsylvanian tetrapods from the Ada Formation of Seminole County, Oklahoma. Journal of Paleontology 76(3):529-545",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,05/05/2002 16:35,10/11/2009 10:12,6174,indet.,,6174,,303.4,298.9,Virgilian,,2,US, indet.
157311,occ,NA,,13947,,Tetrapoda informal indet. 1,species,137279,species not entered,Tetrapoda,NA,unranked clade,53190,Kissel and Lehman,2002,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,specimens,-96.699997,34.933334,OMNH V1005,NA,,US,Oklahoma,Seminole,based on nearby landmark,minutes,small collection,"""just north of the Canadian River""; shown on map as due north of Ada, in the southermost part of Seminole County; this is just north of the town of Tyrola",gp_mid,-28.89,-2.47,101,US,,Ada,,,bed,,,,,,,NA,"from a ""single stratigraphic horizon... 22.4 m above the contact"" with the ""underlying Vamoosa Formation""",,mudstone,gray,,,,,,,,,coarse channel fill,,"bone horizon is from ""tributary channel fill deposits"" immediately below a layer of ""pedogenic carbonate nodules""",macrofossils,,,,,,NA,,body,,allochthonous,time-averaged,,,preferred,,,occasional,NA,,,taxonomic,"selective quarrying,surface (float),sieve,field collection",,,250 specimens,,,,"All of the in situ specimens recovered from the locality were found within a single stratigraphic horizon stretching approximately 11 m along the face of the outcrop. Screenwashing of 40 kg of sediment recovered ""very little additional material""","authors report minimum number of individuals, but material is transported and allochthonous, so specimen counts are recorded instead","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tetrapoda,,NA,NA,vertebrate,"R. A. Kissel and T. M. Lehman. 2002. Upper Pennsylvanian tetrapods from the Ada Formation of Seminole County, Oklahoma. Journal of Paleontology 76(3):529-545",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,05/05/2002 16:35,10/11/2009 10:15,6174,indet. 1,,6174,informal,303.4,298.9,Virgilian,,1,US, indet. 1
157312,occ,NA,,13947,,Tetrapoda informal indet. 2,species,137279,species not entered,Tetrapoda,NA,unranked clade,53190,Kissel and Lehman,2002,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,specimens,-96.699997,34.933334,OMNH V1005,NA,,US,Oklahoma,Seminole,based on nearby landmark,minutes,small collection,"""just north of the Canadian River""; shown on map as due north of Ada, in the southermost part of Seminole County; this is just north of the town of Tyrola",gp_mid,-28.89,-2.47,101,US,,Ada,,,bed,,,,,,,NA,"from a ""single stratigraphic horizon... 22.4 m above the contact"" with the ""underlying Vamoosa Formation""",,mudstone,gray,,,,,,,,,coarse channel fill,,"bone horizon is from ""tributary channel fill deposits"" immediately below a layer of ""pedogenic carbonate nodules""",macrofossils,,,,,,NA,,body,,allochthonous,time-averaged,,,preferred,,,occasional,NA,,,taxonomic,"selective quarrying,surface (float),sieve,field collection",,,250 specimens,,,,"All of the in situ specimens recovered from the locality were found within a single stratigraphic horizon stretching approximately 11 m along the face of the outcrop. Screenwashing of 40 kg of sediment recovered ""very little additional material""","authors report minimum number of individuals, but material is transported and allochthonous, so specimen counts are recorded instead","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tetrapoda,,NA,NA,vertebrate,"R. A. Kissel and T. M. Lehman. 2002. Upper Pennsylvanian tetrapods from the Ada Formation of Seminole County, Oklahoma. Journal of Paleontology 76(3):529-545",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,05/05/2002 16:35,10/11/2009 10:15,6174,indet. 2,,6174,informal,303.4,298.9,Virgilian,,1,US, indet. 2
219910,occ,NA,,22635,,Eryops megacephalus,species,70397,,Eryops megacephalus,NA,species,70397,Sander,1989,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-98.389999,33.34,Archer City Bonebed 3,NA,"ETE Locality 1509, Archer City Bonebed 3, ",US,Texas,,,4,basin,,gp_mid,-30.01,-1.59,101,US,,Archer City,Wichita,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\noriginally entered as Asselian to Olenekian","ETE rock type adj: ""gray,blocky"", ETE lithology comments: .",mudstone,gray,,,,,,,,,"""channel""",,"ETE sed env 1: fluvial, ETE sed env 2: ab_chan_fill ETE event: ., ETE env comment: .",,,,,,,NA,,,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: attritional, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",paleoecologic,,,,1 specimens,,,,"ETE Size: .; ETE reference list: 478, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,,"P. M. Sander. 1989. Early Permian Depositional Environments of Pond Bonebeds in Central Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 69:1-21",24,24,697,A. Behrensmeyer,A. Behrensmeyer,E. Dunne,10/07/2002 20:49,18/07/2016 10:34,5743,megacephalus,Eryops,5743,,296.4,268,Wolfcamp,,NA,US,Eryops megacephalus
219911,occ,NA,,22635,,Archeria crassidisca,species,345353,,Archeria crassidisca,NA,species,229309,Sander,1989,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,,-98.389999,33.34,Archer City Bonebed 3,NA,"ETE Locality 1509, Archer City Bonebed 3, ",US,Texas,,,4,basin,,gp_mid,-30.01,-1.59,101,US,,Archer City,Wichita,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\noriginally entered as Asselian to Olenekian","ETE rock type adj: ""gray,blocky"", ETE lithology comments: .",mudstone,gray,,,,,,,,,"""channel""",,"ETE sed env 1: fluvial, ETE sed env 2: ab_chan_fill ETE event: ., ETE env comment: .",,,,,,,NA,,,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: attritional, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",paleoecologic,,,,1 specimens,,,,"ETE Size: .; ETE reference list: 478, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,,NA,NA,,"P. M. Sander. 1989. Early Permian Depositional Environments of Pond Bonebeds in Central Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 69:1-21",24,24,697,A. Behrensmeyer,A. Behrensmeyer,E. Dunne,10/07/2002 20:49,18/07/2016 10:34,5743,crassidisca,Archeria,5743,,296.4,268,Wolfcamp,,NA,US,Archeria crassidisca
219912,occ,NA,,22635,,Edaphosaurus boanerges,species,122352,,Edaphosaurus boanerges,NA,species,122352,Sander,1989,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,,-98.389999,33.34,Archer City Bonebed 3,NA,"ETE Locality 1509, Archer City Bonebed 3, ",US,Texas,,,4,basin,,gp_mid,-30.01,-1.59,101,US,,Archer City,Wichita,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\noriginally entered as Asselian to Olenekian","ETE rock type adj: ""gray,blocky"", ETE lithology comments: .",mudstone,gray,,,,,,,,,"""channel""",,"ETE sed env 1: fluvial, ETE sed env 2: ab_chan_fill ETE event: ., ETE env comment: .",,,,,,,NA,,,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: attritional, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",paleoecologic,,,,1 specimens,,,,"ETE Size: .; ETE reference list: 478, ; ETE museum list: ",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,,"P. M. Sander. 1989. Early Permian Depositional Environments of Pond Bonebeds in Central Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 69:1-21",24,24,697,A. Behrensmeyer,A. Behrensmeyer,E. Dunne,10/07/2002 20:49,18/07/2016 10:34,5743,boanerges,Edaphosaurus,5743,,296.4,268,Wolfcamp,,NA,US,Edaphosaurus boanerges
220192,occ,NA,,22714,,Trimerorhachis insignis,species,90711,,Trimerorhachis insignis,NA,species,90711,Parrish,1978,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-98.621597,34.125999,Thrift Bone Bed,NA,"ETE Locality 1589, Thrift Bone Bed, ",US,Texas,Wichita,,4,,,gp_mid,-29.78,-0.85,101,US,,Bead Mountain,,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\nentered as Asselian - Olenekian, but the Bead Mountain Formation is Artinskian (see Wardlaw 2005, Permophiles)","ETE rock type adj: 0, ETE lithology comments: 0",,,,,,,,,,,terrestrial indet.,,"ETE sed env 1: ., ETE sed env 2: . ETE event: storm, ETE env comment: tidal flat",,,,,,,NA,,,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: mass_death, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",paleoecologic,,,,300 specimens,,,,"ETE Size: .; ETE reference list: 478, 121, 456, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,,"W. C. Parrish. 1978. Paleoenvironmental analysis of a Lower Permian bonebed and adjacent sediments, Wichita County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 24:209-237",24,24,8,A. Behrensmeyer,A. Behrensmeyer,M. Kosnik,10/07/2002 20:49,10/07/2002 22:49,5693,insignis,Trimerorhachis,5693,,290.1,279.3,Artinskian,,NA,US,Trimerorhachis insignis
220193,occ,NA,,22714,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Parrish,1978,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-98.621597,34.125999,Thrift Bone Bed,NA,"ETE Locality 1589, Thrift Bone Bed, ",US,Texas,Wichita,,4,,,gp_mid,-29.78,-0.85,101,US,,Bead Mountain,,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\nentered as Asselian - Olenekian, but the Bead Mountain Formation is Artinskian (see Wardlaw 2005, Permophiles)","ETE rock type adj: 0, ETE lithology comments: 0",,,,,,,,,,,terrestrial indet.,,"ETE sed env 1: ., ETE sed env 2: . ETE event: storm, ETE env comment: tidal flat",,,,,,,NA,,,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: mass_death, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",paleoecologic,,,,300 specimens,,,,"ETE Size: .; ETE reference list: 478, 121, 456, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,,"W. C. Parrish. 1978. Paleoenvironmental analysis of a Lower Permian bonebed and adjacent sediments, Wichita County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 24:209-237",24,24,8,A. Behrensmeyer,A. Behrensmeyer,M. Kosnik,10/07/2002 20:49,10/07/2002 22:49,5693,sp.,Eryops,5693,,290.1,279.3,Artinskian,,NA,US,Eryops sp.
220194,occ,NA,,22714,,Archeria sp.,genus,37196,,Archeria,NA,genus,37196,Parrish,1978,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,,-98.621597,34.125999,Thrift Bone Bed,NA,"ETE Locality 1589, Thrift Bone Bed, ",US,Texas,Wichita,,4,,,gp_mid,-29.78,-0.85,101,US,,Bead Mountain,,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\nentered as Asselian - Olenekian, but the Bead Mountain Formation is Artinskian (see Wardlaw 2005, Permophiles)","ETE rock type adj: 0, ETE lithology comments: 0",,,,,,,,,,,terrestrial indet.,,"ETE sed env 1: ., ETE sed env 2: . ETE event: storm, ETE env comment: tidal flat",,,,,,,NA,,,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: mass_death, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",paleoecologic,,,,300 specimens,,,,"ETE Size: .; ETE reference list: 478, 121, 456, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,,NA,NA,,"W. C. Parrish. 1978. Paleoenvironmental analysis of a Lower Permian bonebed and adjacent sediments, Wichita County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 24:209-237",24,24,8,A. Behrensmeyer,A. Behrensmeyer,M. Kosnik,10/07/2002 20:49,10/07/2002 22:49,5693,sp.,Archeria,5693,,290.1,279.3,Artinskian,,NA,US,Archeria sp.
220195,occ,NA,,22714,,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Parrish,1978,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-98.621597,34.125999,Thrift Bone Bed,NA,"ETE Locality 1589, Thrift Bone Bed, ",US,Texas,Wichita,,4,,,gp_mid,-29.78,-0.85,101,US,,Bead Mountain,,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\nentered as Asselian - Olenekian, but the Bead Mountain Formation is Artinskian (see Wardlaw 2005, Permophiles)","ETE rock type adj: 0, ETE lithology comments: 0",,,,,,,,,,,terrestrial indet.,,"ETE sed env 1: ., ETE sed env 2: . ETE event: storm, ETE env comment: tidal flat",,,,,,,NA,,,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: mass_death, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",paleoecologic,,,,300 specimens,,,,"ETE Size: .; ETE reference list: 478, 121, 456, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,,"W. C. Parrish. 1978. Paleoenvironmental analysis of a Lower Permian bonebed and adjacent sediments, Wichita County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 24:209-237",24,24,8,A. Behrensmeyer,A. Behrensmeyer,M. Kosnik,10/07/2002 20:49,10/07/2002 22:49,5693,sp.,Diplocaulus,5693,,290.1,279.3,Artinskian,,NA,US,Diplocaulus sp.
220196,occ,NA,,22714,,Ophiacodon sp.,genus,38888,,Ophiacodon,NA,genus,38888,Parrish,1978,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-98.621597,34.125999,Thrift Bone Bed,NA,"ETE Locality 1589, Thrift Bone Bed, ",US,Texas,Wichita,,4,,,gp_mid,-29.78,-0.85,101,US,,Bead Mountain,,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\nentered as Asselian - Olenekian, but the Bead Mountain Formation is Artinskian (see Wardlaw 2005, Permophiles)","ETE rock type adj: 0, ETE lithology comments: 0",,,,,,,,,,,terrestrial indet.,,"ETE sed env 1: ., ETE sed env 2: . ETE event: storm, ETE env comment: tidal flat",,,,,,,NA,,,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: mass_death, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",paleoecologic,,,,300 specimens,,,,"ETE Size: .; ETE reference list: 478, 121, 456, ; ETE museum list: ",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,,"W. C. Parrish. 1978. Paleoenvironmental analysis of a Lower Permian bonebed and adjacent sediments, Wichita County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 24:209-237",24,24,8,A. Behrensmeyer,A. Behrensmeyer,M. Kosnik,10/07/2002 20:49,10/07/2002 22:49,5693,sp.,Ophiacodon,5693,,290.1,279.3,Artinskian,,NA,US,Ophiacodon sp.
220197,occ,NA,,22714,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Parrish,1978,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-98.621597,34.125999,Thrift Bone Bed,NA,"ETE Locality 1589, Thrift Bone Bed, ",US,Texas,Wichita,,4,,,gp_mid,-29.78,-0.85,101,US,,Bead Mountain,,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\nentered as Asselian - Olenekian, but the Bead Mountain Formation is Artinskian (see Wardlaw 2005, Permophiles)","ETE rock type adj: 0, ETE lithology comments: 0",,,,,,,,,,,terrestrial indet.,,"ETE sed env 1: ., ETE sed env 2: . ETE event: storm, ETE env comment: tidal flat",,,,,,,NA,,,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: mass_death, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",paleoecologic,,,,300 specimens,,,,"ETE Size: .; ETE reference list: 478, 121, 456, ; ETE museum list: ",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,,"W. C. Parrish. 1978. Paleoenvironmental analysis of a Lower Permian bonebed and adjacent sediments, Wichita County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 24:209-237",24,24,8,A. Behrensmeyer,A. Behrensmeyer,M. Kosnik,10/07/2002 20:49,10/07/2002 22:49,5693,sp.,Dimetrodon,5693,,290.1,279.3,Artinskian,,NA,US,Dimetrodon sp.
220214,occ,NA,R,22725,,Reptilia indet.,class,36322,,Reptilia,NA,class,36322,Rolfe et al.,1990,Chordata,33815,Reptilia,36322,,NA,,NA,NA,NA,NA,NA,,-3.2,55.950001,East Kirkton site (Units 70-82: East Kirkton Limestone),NA,ETE Locality 1604,UK,Scotland,West Lothian,based on nearby landmark,4,basin,"East Kirkton quarry, near Bathgate, West Lothian, Scotland; ca. 27 km W of Edinburgh (Grid reference NS 991690).",gp_mid,-4.83,-20.31,313,UK,,East Kirkton Limestone,Upper Oil Shale,East Kirkton Limestone,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min. Bed 82 - bed ""b""; lower part of Brigantian","Many specimens are from Unit 82, 'the black shale member'. But others come from the range of units 70-82, including adjacent limestone units or spoil heaps at East Kirkton.","""shale""",black,,,Y,"""limestone""",,,,Y,spring,,"ETE sed env 1: volcanic, ETE sed env 2: spring ETE event: ., ETE env comment: toxic water poss.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: attritional, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",general faunal/floral,"selective quarrying,surface (in situ),mechanical,field collection",BMNH,,66 specimens,,S. P. Wood,1988,"ETE reference list: 478, 479, 483, 482\r\nNMS (National Museum of Scotland, Edinburgh), UMZC (University Museum of Zoology, Cambridge), and GLAHM (Hunerian Museum, Glasgow) collections",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Reptilia,,NA,NA,,"W. D. I. Rolfe, G. P. Durant, and A. E. Fallick, A. J. Hall, D. J. Large, A. C. Scott, T. R. Smithson, and G. M. Walkden. 1990. An early terrestrial biota preserved by Visean vulcanicity in Scotland. In M.G. Lockley and A. Rice (eds.), Volcanism and Fossil Biotas. Geological Society of America Special Paper 244:13-24",24,24,697,A. Behrensmeyer,A. Behrensmeyer,E. Dunne,10/07/2002 20:49,11/07/2016 11:08,4596,indet.,,4596,,336,326.4,Brigantian,,NA,UK, indet.
220214,occ,24373,,22725,,n. gen. Westlothiana n. sp. lizziae,species,179032,,Westlothiana lizziae,NA,species,179032,Smithson and Rolfe,1990,Chordata,33815,Osteichthyes,34881,,NA,,NA,179031,NA,NA,NA,,-3.2,55.950001,East Kirkton site (Units 70-82: East Kirkton Limestone),NA,ETE Locality 1604,UK,Scotland,West Lothian,based on nearby landmark,4,basin,"East Kirkton quarry, near Bathgate, West Lothian, Scotland; ca. 27 km W of Edinburgh (Grid reference NS 991690).",gp_mid,-4.83,-20.31,313,UK,,East Kirkton Limestone,Upper Oil Shale,East Kirkton Limestone,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min. Bed 82 - bed ""b""; lower part of Brigantian","Many specimens are from Unit 82, 'the black shale member'. But others come from the range of units 70-82, including adjacent limestone units or spoil heaps at East Kirkton.","""shale""",black,,,Y,"""limestone""",,,,Y,spring,,"ETE sed env 1: volcanic, ETE sed env 2: spring ETE event: ., ETE env comment: toxic water poss.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: attritional, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",general faunal/floral,"selective quarrying,surface (in situ),mechanical,field collection",BMNH,,66 specimens,,S. P. Wood,1988,"ETE reference list: 478, 479, 483, 482\r\nNMS (National Museum of Scotland, Edinburgh), UMZC (University Museum of Zoology, Cambridge), and GLAHM (Hunerian Museum, Glasgow) collections",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Westlothiana,n. gen.,NA,NA,,T. R. Smithson and W. D. I. Rolfe. 1990. Westlothiana gen. nov.: naming the earliest known reptile. Scottish Journal of Geology 26:137-138,14,14,14,M. Carrano,M. Carrano,M. Carrano,05/03/2011 01:52,04/03/2011 08:53,4596,lizziae,Westlothiana,35413,n. sp.,336,326.4,Brigantian,,NA,UK,Westlothiana lizziae
220215,occ,NA,R,22725,,Temnospondyli indet.,unranked clade,36320,,Temnospondyli,NA,unranked clade,36320,Rolfe et al.,1990,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,NA,NA,NA,NA,specimens,-3.2,55.950001,East Kirkton site (Units 70-82: East Kirkton Limestone),NA,ETE Locality 1604,UK,Scotland,West Lothian,based on nearby landmark,4,basin,"East Kirkton quarry, near Bathgate, West Lothian, Scotland; ca. 27 km W of Edinburgh (Grid reference NS 991690).",gp_mid,-4.83,-20.31,313,UK,,East Kirkton Limestone,Upper Oil Shale,East Kirkton Limestone,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min. Bed 82 - bed ""b""; lower part of Brigantian","Many specimens are from Unit 82, 'the black shale member'. But others come from the range of units 70-82, including adjacent limestone units or spoil heaps at East Kirkton.","""shale""",black,,,Y,"""limestone""",,,,Y,spring,,"ETE sed env 1: volcanic, ETE sed env 2: spring ETE event: ., ETE env comment: toxic water poss.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: attritional, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",general faunal/floral,"selective quarrying,surface (in situ),mechanical,field collection",BMNH,,66 specimens,,S. P. Wood,1988,"ETE reference list: 478, 479, 483, 482\r\nNMS (National Museum of Scotland, Edinburgh), UMZC (University Museum of Zoology, Cambridge), and GLAHM (Hunerian Museum, Glasgow) collections",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Temnospondyli,,NA,NA,,"W. D. I. Rolfe, G. P. Durant, and A. E. Fallick, A. J. Hall, D. J. Large, A. C. Scott, T. R. Smithson, and G. M. Walkden. 1990. An early terrestrial biota preserved by Visean vulcanicity in Scotland. In M.G. Lockley and A. Rice (eds.), Volcanism and Fossil Biotas. Geological Society of America Special Paper 244:13-24",24,24,697,A. Behrensmeyer,A. Behrensmeyer,E. Dunne,10/07/2002 20:49,11/07/2016 11:08,4596,indet.,,4596,,336,326.4,Brigantian,,27,UK, indet.
220215,occ,27216,,22725,,n. gen. Balanerpeton n. sp. woodi,species,227178,,Balanerpeton woodi,NA,species,227178,Milner and Sequeira,1994,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,227174,NA,NA,NA,specimens,-3.2,55.950001,East Kirkton site (Units 70-82: East Kirkton Limestone),NA,ETE Locality 1604,UK,Scotland,West Lothian,based on nearby landmark,4,basin,"East Kirkton quarry, near Bathgate, West Lothian, Scotland; ca. 27 km W of Edinburgh (Grid reference NS 991690).",gp_mid,-4.83,-20.31,313,UK,,East Kirkton Limestone,Upper Oil Shale,East Kirkton Limestone,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min. Bed 82 - bed ""b""; lower part of Brigantian","Many specimens are from Unit 82, 'the black shale member'. But others come from the range of units 70-82, including adjacent limestone units or spoil heaps at East Kirkton.","""shale""",black,,,Y,"""limestone""",,,,Y,spring,,"ETE sed env 1: volcanic, ETE sed env 2: spring ETE event: ., ETE env comment: toxic water poss.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: attritional, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",general faunal/floral,"selective quarrying,surface (in situ),mechanical,field collection",BMNH,,66 specimens,,S. P. Wood,1988,"ETE reference list: 478, 479, 483, 482\r\nNMS (National Museum of Scotland, Edinburgh), UMZC (University Museum of Zoology, Cambridge), and GLAHM (Hunerian Museum, Glasgow) collections",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Balanerpeton,n. gen.,NA,NA,,"A. R. Milner and S. E. K. Sequeira. 1994. The temnospondyl amphibians from the Vis̩an of East Kirkton, West Lothian, Scotland. Transactions of the Royal Society of Edinburgh: Earth Sciences 84:331-361",447,447,697,R. Benson,R. Benson,E. Dunne,27/07/2012 20:00,11/07/2016 11:08,4596,woodi,Balanerpeton,42475,n. sp.,336,326.4,Brigantian,,27,UK,Balanerpeton woodi
220216,occ,NA,R,22725,,Anthracosauridae indet.,family,37199,,Anthracosauridae,NA,family,37199,Rolfe et al.,1990,Chordata,33815,Osteichthyes,34881,,NA,Anthracosauridae,37199,NA,NA,NA,NA,specimens,-3.2,55.950001,East Kirkton site (Units 70-82: East Kirkton Limestone),NA,ETE Locality 1604,UK,Scotland,West Lothian,based on nearby landmark,4,basin,"East Kirkton quarry, near Bathgate, West Lothian, Scotland; ca. 27 km W of Edinburgh (Grid reference NS 991690).",gp_mid,-4.83,-20.31,313,UK,,East Kirkton Limestone,Upper Oil Shale,East Kirkton Limestone,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min. Bed 82 - bed ""b""; lower part of Brigantian","Many specimens are from Unit 82, 'the black shale member'. But others come from the range of units 70-82, including adjacent limestone units or spoil heaps at East Kirkton.","""shale""",black,,,Y,"""limestone""",,,,Y,spring,,"ETE sed env 1: volcanic, ETE sed env 2: spring ETE event: ., ETE env comment: toxic water poss.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: attritional, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",general faunal/floral,"selective quarrying,surface (in situ),mechanical,field collection",BMNH,,66 specimens,,S. P. Wood,1988,"ETE reference list: 478, 479, 483, 482\r\nNMS (National Museum of Scotland, Edinburgh), UMZC (University Museum of Zoology, Cambridge), and GLAHM (Hunerian Museum, Glasgow) collections",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Anthracosauridae,,NA,NA,,"W. D. I. Rolfe, G. P. Durant, and A. E. Fallick, A. J. Hall, D. J. Large, A. C. Scott, T. R. Smithson, and G. M. Walkden. 1990. An early terrestrial biota preserved by Visean vulcanicity in Scotland. In M.G. Lockley and A. Rice (eds.), Volcanism and Fossil Biotas. Geological Society of America Special Paper 244:13-24",24,24,697,A. Behrensmeyer,A. Behrensmeyer,E. Dunne,10/07/2002 20:49,11/07/2016 11:08,4596,indet.,,4596,,336,326.4,Brigantian,,1,UK, indet.
220216,occ,24374,,22725,,n. gen. Silvanerpeton n. sp. miripedes,species,243094,,Silvanerpeton miripedes,NA,species,243094,Clack,1994,Chordata,33815,Osteichthyes,34881,,NA,,NA,243093,NA,NA,NA,specimens,-3.2,55.950001,East Kirkton site (Units 70-82: East Kirkton Limestone),NA,ETE Locality 1604,UK,Scotland,West Lothian,based on nearby landmark,4,basin,"East Kirkton quarry, near Bathgate, West Lothian, Scotland; ca. 27 km W of Edinburgh (Grid reference NS 991690).",gp_mid,-4.83,-20.31,313,UK,,East Kirkton Limestone,Upper Oil Shale,East Kirkton Limestone,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min. Bed 82 - bed ""b""; lower part of Brigantian","Many specimens are from Unit 82, 'the black shale member'. But others come from the range of units 70-82, including adjacent limestone units or spoil heaps at East Kirkton.","""shale""",black,,,Y,"""limestone""",,,,Y,spring,,"ETE sed env 1: volcanic, ETE sed env 2: spring ETE event: ., ETE env comment: toxic water poss.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: attritional, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",general faunal/floral,"selective quarrying,surface (in situ),mechanical,field collection",BMNH,,66 specimens,,S. P. Wood,1988,"ETE reference list: 478, 479, 483, 482\r\nNMS (National Museum of Scotland, Edinburgh), UMZC (University Museum of Zoology, Cambridge), and GLAHM (Hunerian Museum, Glasgow) collections",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Silvanerpeton,n. gen.,NA,NA,,"J. A. Clack. 1994. Silvanerpeton miripedes, a new anthracosauroid from the Vis̩an of East Kirkton, West Lothian, Scotland. Transactions of the Royal Society of Edinburgh: Earth Sciences 84:369-376",14,14,447,M. Carrano,M. Carrano,R. Benson,05/03/2011 02:33,27/07/2012 04:38,4596,miripedes,Silvanerpeton,42473,n. sp.,336,326.4,Brigantian,,1,UK,Silvanerpeton miripedes
220217,occ,NA,,22725,,Loxommatidae indet.,family,36969,objective synonym of,Baphetidae,NA,family,227378,Rolfe et al.,1990,Chordata,33815,Osteichthyes,34881,,NA,Baphetidae,227378,NA,NA,NA,NA,,-3.2,55.950001,East Kirkton site (Units 70-82: East Kirkton Limestone),NA,ETE Locality 1604,UK,Scotland,West Lothian,based on nearby landmark,4,basin,"East Kirkton quarry, near Bathgate, West Lothian, Scotland; ca. 27 km W of Edinburgh (Grid reference NS 991690).",gp_mid,-4.83,-20.31,313,UK,,East Kirkton Limestone,Upper Oil Shale,East Kirkton Limestone,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min. Bed 82 - bed ""b""; lower part of Brigantian","Many specimens are from Unit 82, 'the black shale member'. But others come from the range of units 70-82, including adjacent limestone units or spoil heaps at East Kirkton.","""shale""",black,,,Y,"""limestone""",,,,Y,spring,,"ETE sed env 1: volcanic, ETE sed env 2: spring ETE event: ., ETE env comment: toxic water poss.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: attritional, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",general faunal/floral,"selective quarrying,surface (in situ),mechanical,field collection",BMNH,,66 specimens,,S. P. Wood,1988,"ETE reference list: 478, 479, 483, 482\r\nNMS (National Museum of Scotland, Edinburgh), UMZC (University Museum of Zoology, Cambridge), and GLAHM (Hunerian Museum, Glasgow) collections",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Loxommatidae,,NA,NA,,"W. D. I. Rolfe, G. P. Durant, and A. E. Fallick, A. J. Hall, D. J. Large, A. C. Scott, T. R. Smithson, and G. M. Walkden. 1990. An early terrestrial biota preserved by Visean vulcanicity in Scotland. In M.G. Lockley and A. Rice (eds.), Volcanism and Fossil Biotas. Geological Society of America Special Paper 244:13-24",24,24,14,A. Behrensmeyer,A. Behrensmeyer,M. Carrano,10/07/2002 20:49,04/03/2011 08:53,4596,indet.,,4596,,336,326.4,Brigantian,,NA,UK, indet.
220222,occ,NA,,22726,,Anthracosauria indet.,unranked clade,37177,,Anthracosauria,NA,unranked clade,37177,Andrews et al.,1977,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,,-3.35,56.1166,Cowdenbeath Amphibian Bonebed,NA,ETE Locality 1605; Dora Opencast Coal Site,UK,,,,4,outcrop,"""south-east of Cowdenbeath... a section 30 m long""",gp_mid,0.18,-9.49,313,UK,,,Limestone Coal,,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min\r\n""lower Namurian A... 62 m beneath the base of the Index Limestone [which is]... at the junction between the top of the Pendleian (E1) and the base of the Arnsbergian (E2) stages"": originally entered as Namurian to Bashkirian","ETE rock type adj: ""rooty,muddy"", ETE lithology comments: 0\r\n""a localised patch in a seatrock (rooty, muddy siltstone)""",siltstone,,,,,,,,,,terrestrial indet.,,,,,,,,,NA,,,,,,,,,,,,NA,,,general faunal/floral,,,,7 specimens,,,1974 and 1975,"ETE Size: .; ETE reference list: 478, 479, 483, 482, 485, 454, 81, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Anthracosauria,,NA,NA,,"S. M. Andrews, M.A.E. Browne, and AL Panchen, and SP Wood. 1977. Discovery of amphibians in the Namurian (Upper Carboniferous of Fife). Nature 265:529-532",24,24,697,A. Behrensmeyer,A. Behrensmeyer,E. Dunne,10/07/2002 20:49,01/12/2015 08:45,5931,indet.,,5931,,326.4,318.1,Pendleian,,NA,UK, indet.
220223,occ,NA,,22726,,Lepospondyli indet.,unranked clade,37250,,Lepospondyli,NA,unranked clade,37250,Andrews et al.,1977,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,,-3.35,56.1166,Cowdenbeath Amphibian Bonebed,NA,ETE Locality 1605; Dora Opencast Coal Site,UK,,,,4,outcrop,"""south-east of Cowdenbeath... a section 30 m long""",gp_mid,0.18,-9.49,313,UK,,,Limestone Coal,,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min\r\n""lower Namurian A... 62 m beneath the base of the Index Limestone [which is]... at the junction between the top of the Pendleian (E1) and the base of the Arnsbergian (E2) stages"": originally entered as Namurian to Bashkirian","ETE rock type adj: ""rooty,muddy"", ETE lithology comments: 0\r\n""a localised patch in a seatrock (rooty, muddy siltstone)""",siltstone,,,,,,,,,,terrestrial indet.,,,,,,,,,NA,,,,,,,,,,,,NA,,,general faunal/floral,,,,7 specimens,,,1974 and 1975,"ETE Size: .; ETE reference list: 478, 479, 483, 482, 485, 454, 81, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lepospondyli,,NA,NA,,"S. M. Andrews, M.A.E. Browne, and AL Panchen, and SP Wood. 1977. Discovery of amphibians in the Namurian (Upper Carboniferous of Fife). Nature 265:529-532",24,24,697,A. Behrensmeyer,A. Behrensmeyer,E. Dunne,10/07/2002 20:49,01/12/2015 08:45,5931,indet.,,5931,,326.4,318.1,Pendleian,,NA,UK, indet.
220224,occ,NA,,22726,,Spathicephalus mirus,species,332435,,Spathicephalus mirus,NA,species,332435,Andrews et al.,1977,Chordata,33815,Osteichthyes,34881,,NA,Spathicephalidae,332447,36973,NA,NA,NA,,-3.35,56.1166,Cowdenbeath Amphibian Bonebed,NA,ETE Locality 1605; Dora Opencast Coal Site,UK,,,,4,outcrop,"""south-east of Cowdenbeath... a section 30 m long""",gp_mid,0.18,-9.49,313,UK,,,Limestone Coal,,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min\r\n""lower Namurian A... 62 m beneath the base of the Index Limestone [which is]... at the junction between the top of the Pendleian (E1) and the base of the Arnsbergian (E2) stages"": originally entered as Namurian to Bashkirian","ETE rock type adj: ""rooty,muddy"", ETE lithology comments: 0\r\n""a localised patch in a seatrock (rooty, muddy siltstone)""",siltstone,,,,,,,,,,terrestrial indet.,,,,,,,,,NA,,,,,,,,,,,,NA,,,general faunal/floral,,,,7 specimens,,,1974 and 1975,"ETE Size: .; ETE reference list: 478, 479, 483, 482, 485, 454, 81, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Spathicephalus,,NA,NA,,"S. M. Andrews, M.A.E. Browne, and AL Panchen, and SP Wood. 1977. Discovery of amphibians in the Namurian (Upper Carboniferous of Fife). Nature 265:529-532",24,24,697,A. Behrensmeyer,A. Behrensmeyer,E. Dunne,10/07/2002 20:49,01/12/2015 08:45,5931,mirus,Spathicephalus,5931,,326.4,318.1,Pendleian,,NA,UK,Spathicephalus mirus
220225,occ,NA,,22726,,Eoherpeton watsoni,species,229321,,Eoherpeton watsoni,NA,species,229321,Andrews et al.,1977,Chordata,33815,Osteichthyes,34881,,NA,Eoherpetontidae,37179,37180,NA,NA,NA,,-3.35,56.1166,Cowdenbeath Amphibian Bonebed,NA,ETE Locality 1605; Dora Opencast Coal Site,UK,,,,4,outcrop,"""south-east of Cowdenbeath... a section 30 m long""",gp_mid,0.18,-9.49,313,UK,,,Limestone Coal,,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min\r\n""lower Namurian A... 62 m beneath the base of the Index Limestone [which is]... at the junction between the top of the Pendleian (E1) and the base of the Arnsbergian (E2) stages"": originally entered as Namurian to Bashkirian","ETE rock type adj: ""rooty,muddy"", ETE lithology comments: 0\r\n""a localised patch in a seatrock (rooty, muddy siltstone)""",siltstone,,,,,,,,,,terrestrial indet.,,,,,,,,,NA,,,,,,,,,,,,NA,,,general faunal/floral,,,,7 specimens,,,1974 and 1975,"ETE Size: .; ETE reference list: 478, 479, 483, 482, 485, 454, 81, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Eoherpeton,,NA,NA,,"S. M. Andrews, M.A.E. Browne, and AL Panchen, and SP Wood. 1977. Discovery of amphibians in the Namurian (Upper Carboniferous of Fife). Nature 265:529-532",24,24,697,A. Behrensmeyer,A. Behrensmeyer,E. Dunne,10/07/2002 20:49,01/12/2015 08:45,5931,watsoni,Eoherpeton,5931,,326.4,318.1,Pendleian,,NA,UK,Eoherpeton watsoni
221283,occ,NA,,22715,,Captorhinus sp.,genus,37497,,Captorhinus,NA,genus,37497,White,1939,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-99.2369,33.797699,West Coffee Creek,NA,"ETE Locality 1591, Reptile B, West Coffee Creek, ",US,Texas,Baylor,,4,,,gp_mid,-28.93,1.81,101,US,,Arroyo,Clear Fork,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\noriginally entered as Asselian to Olenekian\r\n","ETE rock type adj: 0, ETE lithology comments: 0",claystone,,,,,,,,,,terrestrial indet.,,"ETE sed env 1: fluvial, ETE sed env 2: floodplain ETE event: burrow, ETE env comment: collapse",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: mass_death, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",taxonomic,,,,11 specimens,,,,"ETE Size: .; ETE reference list: 478, 482, 485, 483, 81, ; ETE museum list: ",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,,T. E. White. 1939. Osteology of Seymouria baylorensis Broili. Bulletin of the Museum of Comparative Zoology 85(5):325-409,24,24,8,A. Behrensmeyer,A. Behrensmeyer,M. Kosnik,10/07/2002 20:49,10/07/2002 22:49,5719,sp.,Captorhinus,5719,,279.3,272.3,Kungurian,,2,US,Captorhinus sp.
221284,occ,NA,,22715,,Seymouria sp.,genus,37223,,Seymouria,NA,genus,37223,White,1939,Chordata,33815,Osteichthyes,34881,,NA,Seymouriidae,37219,37223,NA,NA,NA,individuals,-99.2369,33.797699,West Coffee Creek,NA,"ETE Locality 1591, Reptile B, West Coffee Creek, ",US,Texas,Baylor,,4,,,gp_mid,-28.93,1.81,101,US,,Arroyo,Clear Fork,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\noriginally entered as Asselian to Olenekian\r\n","ETE rock type adj: 0, ETE lithology comments: 0",claystone,,,,,,,,,,terrestrial indet.,,"ETE sed env 1: fluvial, ETE sed env 2: floodplain ETE event: burrow, ETE env comment: collapse",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: mass_death, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",taxonomic,,,,11 specimens,,,,"ETE Size: .; ETE reference list: 478, 482, 485, 483, 81, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Seymouria,,NA,NA,,T. E. White. 1939. Osteology of Seymouria baylorensis Broili. Bulletin of the Museum of Comparative Zoology 85(5):325-409,24,24,8,A. Behrensmeyer,A. Behrensmeyer,M. Kosnik,10/07/2002 20:49,10/07/2002 22:49,5719,sp.,Seymouria,5719,,279.3,272.3,Kungurian,,9,US,Seymouria sp.
221285,occ,NA,,22716,,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Dalquest and Mamay,1962,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,individuals,-99.771301,32.942402,Rowland Site,NA,"ETE Locality 1592, Rowland Site, ",US,Texas,Jones,,4,local area,,gp_mid,-29.75,1.3,101,US,,Vale,,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\noriginally entered as Asselian to Olenekian","ETE rock type adj: greenish, ETE lithology comments: 0",siltstone,green,,,,,,,,,"""channel""",,"ETE sed env 1: fluvial, ETE sed env 2: channel ETE event: ., ETE env comment: drought",,,,,,,NA,,,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: mass_death, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",general faunal/floral,,,,400 specimens,,,,"ETE Size: .; ETE reference list: 478, 482, 485, 454, 81, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,,"W. W. Dalquest and S.H. Mamay. 1962. A remarkable concentration of Permian amphibian remians in Haskell County, Texas. Journal of Geology 71:641-644",24,24,8,A. Behrensmeyer,A. Behrensmeyer,M. Kosnik,10/07/2002 20:49,10/07/2002 22:49,5665,sp.,Diplocaulus,5665,,279.3,272.3,Kungurian,,360,US,Diplocaulus sp.
221286,occ,NA,,22716,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Dalquest and Mamay,1962,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,individuals,-99.771301,32.942402,Rowland Site,NA,"ETE Locality 1592, Rowland Site, ",US,Texas,Jones,,4,local area,,gp_mid,-29.75,1.3,101,US,,Vale,,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\noriginally entered as Asselian to Olenekian","ETE rock type adj: greenish, ETE lithology comments: 0",siltstone,green,,,,,,,,,"""channel""",,"ETE sed env 1: fluvial, ETE sed env 2: channel ETE event: ., ETE env comment: drought",,,,,,,NA,,,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: mass_death, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",general faunal/floral,,,,400 specimens,,,,"ETE Size: .; ETE reference list: 478, 482, 485, 454, 81, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,,"W. W. Dalquest and S.H. Mamay. 1962. A remarkable concentration of Permian amphibian remians in Haskell County, Texas. Journal of Geology 71:641-644",24,24,8,A. Behrensmeyer,A. Behrensmeyer,M. Kosnik,10/07/2002 20:49,10/07/2002 22:49,5665,sp.,Trimerorhachis,5665,,279.3,272.3,Kungurian,,32,US,Trimerorhachis sp.
221287,occ,NA,,22716,,Eryopidae indet.,family,37007,,Eryopidae,NA,family,37007,Dalquest and Mamay,1962,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,NA,NA,NA,NA,individuals,-99.771301,32.942402,Rowland Site,NA,"ETE Locality 1592, Rowland Site, ",US,Texas,Jones,,4,local area,,gp_mid,-29.75,1.3,101,US,,Vale,,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\noriginally entered as Asselian to Olenekian","ETE rock type adj: greenish, ETE lithology comments: 0",siltstone,green,,,,,,,,,"""channel""",,"ETE sed env 1: fluvial, ETE sed env 2: channel ETE event: ., ETE env comment: drought",,,,,,,NA,,,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: mass_death, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",general faunal/floral,,,,400 specimens,,,,"ETE Size: .; ETE reference list: 478, 482, 485, 454, 81, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryopidae,,NA,NA,,"W. W. Dalquest and S.H. Mamay. 1962. A remarkable concentration of Permian amphibian remians in Haskell County, Texas. Journal of Geology 71:641-644",24,24,4,A. Behrensmeyer,A. Behrensmeyer,J. Alroy,10/07/2002 20:49,27/07/2006 16:51,5665,indet.,,5665,,279.3,272.3,Kungurian,,8,US, indet.
229269,occ,NA,,22667,,Parioxys ferricolus,species,345270,,Parioxys ferricolus,NA,species,345270,Moustafa,1952,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37052,NA,NA,NA,specimens,-98.540001,33.439999,Parioxys site,NA,"ETE Locality 1542, Parioxys site, near Dundee",US,Texas,Baylor,estimated from map,4,,,gp_mid,-30.38,-1.97,101,US,,Belle Plains,Wichita,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min","ETE rock type adj: 0, ETE lithology comments: .",not reported,,,,,,,,,,terrestrial indet.,,"ETE sed env 1: ., ETE sed env 2: . ETE event: ., ETE env comment: drought",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: mass_death, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",taxonomic,,,,8 specimens,,,,"ETE Size: .; ETE reference list: 478, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Parioxys,,NA,NA,vertebrate,Y. S. Moustafa. 1952. Amphibian mass death in the Permian. Institute d'Egypt Bulletin 33:301-304,24,24,697,A. Behrensmeyer,A. Behrensmeyer,E. Dunne,10/07/2002 20:49,15/07/2016 06:31,5689,ferricolus,Parioxys,5689,,298.9,290.1,Asselian,Sakmarian,8,US,Parioxys ferricolus
229270,occ,NA,,22668,,Trematops sp.,genus,37050,objective synonym of,Acheloma,NA,genus,37048,White,1939,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,37048,NA,NA,NA,specimens,-98.949997,33.633301,Williams Ranch 1,NA,"ETE Locality 1543, Williams Ranch 1, ",US,Texas,,,4,,,gp_mid,-30.27,-1.13,101,US,,,,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\noriginally entered as Asselian to Olenekian\r\n","ETE rock type adj: 0, ETE lithology comments: .",not reported,,,,,,,,,,terrestrial indet.,,"ETE sed env 1: ., ETE sed env 2: . ETE event: burrow, ETE env comment: burow collapse",,,,,,,NA,,,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: mass_death, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",taxonomic,,,,5 specimens,,,,"ETE Size: .; ETE reference list: 478, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Trematops,,NA,NA,,T. E. White. 1939. Osteology of Seymouria baylorensis Broili. Bulletin of the Museum of Comparative Zoology 85(5):325-409,24,24,8,A. Behrensmeyer,A. Behrensmeyer,M. Kosnik,10/07/2002 20:49,10/07/2002 22:49,5719,sp.,Acheloma,5719,,290.1,279.3,Artinskian,,5,US,Acheloma sp.
229271,occ,NA,,22669,,Parioxys sp.,genus,37052,,Parioxys,NA,genus,37052,White,1939,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37052,NA,NA,NA,specimens,-98.949997,33.633301,Williams Ranch 2,NA,ETE Locality 1544,US,Texas,,,4,,,gp_mid,-30.27,-1.13,101,US,,,,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\noriginally entered as Asselian to Olenekian\r\n","ETE rock type adj: 0, ETE lithology comments: .",not reported,,,,,,,,,,terrestrial indet.,,"ETE sed env 1: ., ETE sed env 2: . ETE event: burrow, ETE env comment: burow collapse",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: mass_death, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",taxonomic,,,,2 specimens,,,,"ETE Size: .; ETE reference list: 478, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Parioxys,,NA,NA,,T. E. White. 1939. Osteology of Seymouria baylorensis Broili. Bulletin of the Museum of Comparative Zoology 85(5):325-409,24,24,8,A. Behrensmeyer,A. Behrensmeyer,M. Kosnik,10/07/2002 20:49,10/07/2002 22:49,5719,sp.,Parioxys,5719,,290.1,279.3,Artinskian,,2,US,Parioxys sp.
229272,occ,NA,,22670,,Conodectes favosus,species,138237,subjective synonym of,Seymouria baylorensis,NA,species,137488,White,1939,Chordata,33815,Osteichthyes,34881,,NA,Seymouriidae,37219,37223,NA,NA,NA,specimens,-99.233299,33.783298,Gray Creek,NA,"ETE Locality 1545, Gray Creek, ",US,Texas,,,4,,,gp_mid,-28.93,1.79,101,US,,,,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\noriginally entered as Asselian to Olenekian\r\n","ETE rock type adj: 0, ETE lithology comments: .",not reported,,,,,,,,,,terrestrial indet.,,"ETE sed env 1: ., ETE sed env 2: . ETE event: burrow, ETE env comment: burow collapse",,,,,,,NA,,,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: mass_death, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",taxonomic,,,,4 specimens,,,,"ETE Size: .; ETE reference list: 478, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Conodectes,,NA,NA,,T. E. White. 1939. Osteology of Seymouria baylorensis Broili. Bulletin of the Museum of Comparative Zoology 85(5):325-409,24,24,697,A. Behrensmeyer,A. Behrensmeyer,E. Dunne,10/07/2002 20:49,18/08/2016 11:51,5719,favosus,Seymouria,5719,,279.3,272.3,Kungurian,,4,US,Seymouria favosus
229273,occ,NA,,22671,,Dissorophus multicinctus,species,255227,,Dissorophus multicinctus,NA,species,255227,White,1939,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37027,NA,NA,NA,specimens,-99.233299,33.783298,Indian Creek,NA,"ETE Locality 1546, Indian Creek, ",US,Texas,,,4,,,gp_mid,-28.93,1.79,101,US,,,,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\noriginally entered as Asselian to Olenekian\r\n","ETE rock type adj: 0, ETE lithology comments: .",not reported,,,,,,,,,,terrestrial indet.,,"ETE sed env 1: ., ETE sed env 2: . ETE event: burrow, ETE env comment: burow collapse",,,,,,,NA,,,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: mass_death, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",taxonomic,,,,6 specimens,,,,"ETE Size: .; ETE reference list: 478, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Dissorophus,,NA,NA,,T. E. White. 1939. Osteology of Seymouria baylorensis Broili. Bulletin of the Museum of Comparative Zoology 85(5):325-409,24,24,697,A. Behrensmeyer,A. Behrensmeyer,E. Dunne,10/07/2002 20:49,13/07/2016 06:38,5719,multicinctus,Dissorophus,5719,,279.3,272.3,Kungurian,,6,US,Dissorophus multicinctus
285528,occ,NA,,27133,,n. gen. Carrolla n. sp. craddocki,species,227004,,Carrolla craddocki,NA,species,227004,Langston,1986,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Brachystelechidae,37314,37316,NA,NA,NA,individuals,-98.901947,33.740276,South side of Tit Mountain butte,NA,TMM 40031 (Belle Plains Formation),US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Dissected flats about 100 feet above the base of the south side of a butte termed Tit Mountain, about three miles notheast of Dundee, in northwest Archer County, Texas.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,,,group of beds,,,,,,,NA,"entered as Wolfcamp and Asselian - Sakmarian\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)",redbeds,"""siliciclastic""",red,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,"""skull and jaw, firmly united""",taxonomic,"surface (float),field collection",TMM,,,,,,Not the same as Tit Mountain Locality 21 (Romer 1928).,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Carrolla,n. gen.,NA,NA,vertebrate,"W. Langston, Jr. 1986. Carrolla craddocki; a new genus and species of microsaur from the Lower Permian of Texas. The Pearce-Sellards series (43):1-20",4,76,0,J. Alroy,R. Whatley,,19/11/2002 18:12,19/11/2002 20:12,7510,craddocki,Carrolla,7510,n. sp.,290.1,279.3,Artinskian,,1,US,Carrolla craddocki
286238,occ,NA,,27263,,n. gen. Lysipterygium n. sp. deterrai,species,345841,species not entered,Lysipterygium,NA,genus,345841,Branson,1935,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Lysipterygiidae,345842,345841,NA,NA,NA,specimens,74.908333,34.041668,Risin Spur (Gangamopteris Shales),NA,Lower Gondwanan series,IN,Kashmir,,based on nearby landmark,seconds,,"specimens were collected ""..on Risin Spur near Zewan Village..""",gp_mid,61.41,-55.08,501,IN,,,,,,,,,,,,NA,"""collected from the Lower Permian Gangamopteris shales (glassy volcanic tuff) of the Lower Gondwana series"". Age previously given as Rotliegendes but Gangamopteris shales correlated with Eurydesma-bearing beds at Manendragarh and the Salt Range, suggesting an Asselian-Sakmarian age.","""shales (glassy volcanic tuff)""","""shale""",tuffaceous,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,mold/impression",medium,,,,,,,,,NA,,"Specimen is in a slab. Much of the specimen is preserved as an impression. Bones, where preserved, are of ""a reddish crumbly material, mixed with matrix.""",taxonomic,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Lysipterygium,n. gen.,NA,NA,vertebrate,C. C. Branson. 1935. A labyrinthodont from the lower Gondwana of Kashmir and a new edestid from the Permian of the Salt range. Memoirs of the Connecticut Academy of Arts & Sciences 9:19-26,4,76,697,J. Alroy,R. Whatley,E. Dunne,25/11/2002 18:07,04/08/2016 05:32,7535,deterrai,Lysipterygium,7535,n. sp.,298.9,290.1,Asselian,Sakmarian,1,IN,Lysipterygium deterrai
286240,occ,NA,,27263,,Archegosaurus ornatus,species,345879,recombined as,Kashmirosaurus ornatus,NA,species,345879,Branson,1935,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Archegosauridae,37057,345877,NA,NA,NA,,74.908333,34.041668,Risin Spur (Gangamopteris Shales),NA,Lower Gondwanan series,IN,Kashmir,,based on nearby landmark,seconds,,"specimens were collected ""..on Risin Spur near Zewan Village..""",gp_mid,61.41,-55.08,501,IN,,,,,,,,,,,,NA,"""collected from the Lower Permian Gangamopteris shales (glassy volcanic tuff) of the Lower Gondwana series"". Age previously given as Rotliegendes but Gangamopteris shales correlated with Eurydesma-bearing beds at Manendragarh and the Salt Range, suggesting an Asselian-Sakmarian age.","""shales (glassy volcanic tuff)""","""shale""",tuffaceous,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,mold/impression",medium,,,,,,,,,NA,,"Specimen is in a slab. Much of the specimen is preserved as an impression. Bones, where preserved, are of ""a reddish crumbly material, mixed with matrix.""",taxonomic,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Archegosaurus,,NA,NA,vertebrate,C. C. Branson. 1935. A labyrinthodont from the lower Gondwana of Kashmir and a new edestid from the Permian of the Salt range. Memoirs of the Connecticut Academy of Arts & Sciences 9:19-26,4,76,697,J. Alroy,R. Whatley,E. Dunne,25/11/2002 18:07,04/08/2016 05:32,7535,ornatus,Kashmirosaurus,7535,,298.9,290.1,Asselian,Sakmarian,NA,IN,Kashmirosaurus ornatus
289594,occ,NA,,27601,,Tetrapoda indet.,unranked clade,53190,,Tetrapoda,NA,unranked clade,53190,Olson,1965,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,specimens,-97.55722,34.978889,MC-1 (Duncan Formation),NA,,US,Oklahoma,McClain,based on political unit,seconds,small collection,"Sec. 19, T. 6 N., R. 3 W., 0.5 mile east of Criner. Lat long is for this Sec., T., R. Specimens are from a road cut.",gp_mid,-26.45,3.46,101,US,,Duncan,El Reno,,bed,,,,,,,NA,"""The beds lie only a few feet above the contact of the Hennessey and are Duncan rather than Chickasha."" beds are ""older than the Chickasha""\nThe El Reno Group is the stratigraphic equivalent of the Pease River Group of North Texas. The Duncan Sandstone is the lowermost Formation of the El Reno and hence is Kungurian, probably Roadian in age. (see e. g. Smith, 1974, Texas Bureau of Economic Geology, Report of Investigations 80; or Lucas, 2004, Stratigraphy 1(1))","""Bones were found in a very fine-grained sandstone.""",sandstone,,,,Y,,,,,,deltaic indet.,,"""The Chickasha Formation, along with the underlying Duncan Formation from which it is lithologically indistinguishable in many places, comprises an array of clastic sediments ranging through all gradations from shales to coarse conglomerates. The beds appear to have been deposited by waters of a major stream system which terminated in a large delta, the Tussey delta of Green (1937), marginal to a persistent evaporite basin.""",macrofossils,,,,,,NA,,body,,,snapshot,,,,,,occasional,NA,,,taxonomic,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tetrapoda,,NA,NA,vertebrate,E. C. Olson. 1965. New Permian vertebrates from the Chickasha Formation in Oklahoma. Circular Oklahoma Geological Survey 70:1-70,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,13/12/2002 14:52,20/08/2009 18:24,4327,indet.,,4327,,279.3,268.8,Kungurian,Roadian,1,US, indet.
290380,occ,NA,I,27703,,Matthewichnus sp.,genus,125551,,Matthewichnus,NA,genus,125551,Clark and Jewkes,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,125551,NA,NA,NA,individuals,-4.416667,55.599998,Redford Pit (GLAHM 0HF 3.28.2),NA,Broadhead Farm (GLAHM OHF 3.28.6); No.2 Candie Pit (GLAHM OHF 3.28.1); Lower Coal Measures; Colinburn and Armadale Main coals,UK,Scotland,,based on nearby landmark,seconds,small collection,"The sandstone block containing the trackways was collected from and ""old bing"", or heap, near Broadhead Farm (GLAHM OHF 3.28.6), 1.5 km south of Bowhouse, south east of Falkirk. The Redford Pit is the likely source. Lat long is for Bowhouse.",gp_mid,-4.5,-18.72,313,UK,,Coal Measures,,,formation,,,,,,,NA,"The exact stratigraphic position of the sandstone is unclear. It may have come from the lower half of the Coal measures between the Colinburn and Armadale Main coals, which consist mainly of sandstones, or from above the Armadale Main below the Mill Coal.",slab of Carboniferous sandstone,sandstone,,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"mold/impression,trace",,,snapshot,,,life position,,,,NA,,two tetrapod trackways on the upper surface of a sandstone slab,taxonomic,"salvage,survey of museum collection",,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Matthewichnus,,NA,NA,vertebrate,N. D. L. Clark and M. Jewkes. 2000. Tetrapod trackways (Matthewichnus sp. and ?Pseudobradypus sp.) from the Coal Measures (Carboniferous) of Central Scotland. Scottish Journal of Geology 36(1):87-90,4,76,0,J. Alroy,R. Whatley,,20/12/2002 11:43,20/12/2002 13:43,NA,sp.,Matthewichnus,7616,,358.9,298.9,Tournaisian,Gzhelian,1,UK,Matthewichnus sp.
290381,occ,NA,IF,27703,,Pseudobradypus ? sp.,genus,328598,,Pseudobradypus,NA,genus,328598,Clark and Jewkes,2000,Chordata,33815,Osteichthyes,34881,,NA,,NA,328598,NA,NA,NA,individuals,-4.416667,55.599998,Redford Pit (GLAHM 0HF 3.28.2),NA,Broadhead Farm (GLAHM OHF 3.28.6); No.2 Candie Pit (GLAHM OHF 3.28.1); Lower Coal Measures; Colinburn and Armadale Main coals,UK,Scotland,,based on nearby landmark,seconds,small collection,"The sandstone block containing the trackways was collected from and ""old bing"", or heap, near Broadhead Farm (GLAHM OHF 3.28.6), 1.5 km south of Bowhouse, south east of Falkirk. The Redford Pit is the likely source. Lat long is for Bowhouse.",gp_mid,-4.5,-18.72,313,UK,,Coal Measures,,,formation,,,,,,,NA,"The exact stratigraphic position of the sandstone is unclear. It may have come from the lower half of the Coal measures between the Colinburn and Armadale Main coals, which consist mainly of sandstones, or from above the Armadale Main below the Mill Coal.",slab of Carboniferous sandstone,sandstone,,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"mold/impression,trace",,,snapshot,,,life position,,,,NA,,two tetrapod trackways on the upper surface of a sandstone slab,taxonomic,"salvage,survey of museum collection",,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Pseudobradypus,?,NA,NA,vertebrate,N. D. L. Clark and M. Jewkes. 2000. Tetrapod trackways (Matthewichnus sp. and ?Pseudobradypus sp.) from the Coal Measures (Carboniferous) of Central Scotland. Scottish Journal of Geology 36(1):87-90,4,76,0,J. Alroy,R. Whatley,,20/12/2002 11:43,20/12/2002 13:43,NA,sp.,Pseudobradypus,7616,,358.9,298.9,Tournaisian,Gzhelian,1,UK,Pseudobradypus sp.
290382,occ,NA,,27704,,n. gen. Waggoneria n. sp. knoxensis,species,120859,,Waggoneria knoxensis,NA,species,120859,Olson,1951,Chordata,33815,Osteichthyes,34881,,NA,Waggoneriidae,120858,120857,NA,NA,NA,individuals,-99.557777,33.731667,Locality KF (Middle Vale Formation),NA,"three-channel hill, ""fish quarry""",US,Texas,Knox,estimated from map,seconds,small collection,"""approx. seven miles north of Vera, Knox County, Texas"" (Olson, 1951)\r\n""North wall of valley of South Wichita River, east of Vera-Gilliland road"" (Olson, 1948); for details see map on p. 188 in Olson (1948)",gp_mid,-29.19,1.89,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""The locality [...] KF, was assigned to the upper Vale in an earlier paper. More recent field work has shown that it comprises beds that must be assigned to the middle rather than the upper part of the Vale."" (Olson, 1954 p. 213)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191);\r\nspecimen ""was preserved in a nodule that had weathered from a conglomeratic deposit of channel origin."" (Olson, 1951 p. 89) other specimens are from a quarry in fine-grained, green channel deposits",conglomerate,"pebbly,green,red",,,Y,"""siliciclastic""","fine,green",,,Y,"""channel""",foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,,,,NA,,"""Fragmentation of the specimens occurred before and during deposition, probably as the materials were transported by the waters of the streams. This group of animals cannot be considered to represent a life assemblage."" (Olson, 1955 p. 258)",taxonomic,field collection,FMNH,,,,E. C. Olson,1946-1948,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Waggoneria,n. gen.,NA,NA,vertebrate,E. C. Olson. 1951. Fauna of upper Vale and Choza: 1-5. Fieldiana: Geology 10(11):89-128,4,76,697,J. Alroy,R. Whatley,E. Dunne,20/12/2002 17:49,15/03/2016 11:15,28928,knoxensis,Waggoneria,4326,n. sp.,279.3,272.3,Kungurian,,1,US,Waggoneria knoxensis
290383,occ,NA,,27704,,n. gen. Captorhinoides n. sp. valensis,species,120860,,Captorhinoides valensis,NA,species,120860,Olson,1951,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37498,NA,NA,NA,individuals,-99.557777,33.731667,Locality KF (Middle Vale Formation),NA,"three-channel hill, ""fish quarry""",US,Texas,Knox,estimated from map,seconds,small collection,"""approx. seven miles north of Vera, Knox County, Texas"" (Olson, 1951)\r\n""North wall of valley of South Wichita River, east of Vera-Gilliland road"" (Olson, 1948); for details see map on p. 188 in Olson (1948)",gp_mid,-29.19,1.89,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""The locality [...] KF, was assigned to the upper Vale in an earlier paper. More recent field work has shown that it comprises beds that must be assigned to the middle rather than the upper part of the Vale."" (Olson, 1954 p. 213)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191);\r\nspecimen ""was preserved in a nodule that had weathered from a conglomeratic deposit of channel origin."" (Olson, 1951 p. 89) other specimens are from a quarry in fine-grained, green channel deposits",conglomerate,"pebbly,green,red",,,Y,"""siliciclastic""","fine,green",,,Y,"""channel""",foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,,,,NA,,"""Fragmentation of the specimens occurred before and during deposition, probably as the materials were transported by the waters of the streams. This group of animals cannot be considered to represent a life assemblage."" (Olson, 1955 p. 258)",taxonomic,field collection,FMNH,,,,E. C. Olson,1946-1948,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinoides,n. gen.,NA,NA,vertebrate,E. C. Olson. 1951. Fauna of upper Vale and Choza: 1-5. Fieldiana: Geology 10(11):89-128,4,76,697,J. Alroy,R. Whatley,E. Dunne,20/12/2002 17:49,15/03/2016 11:15,28928,valensis,Captorhinoides,4326,n. sp.,279.3,272.3,Kungurian,,1,US,Captorhinoides valensis
294218,occ,NA,,28067,,Embolomeri indet.,suborder,37178,,Embolomeri,NA,suborder,37178,Langston,1952,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,individuals,-106.783333,35.716667,"UCMP 39179, Jemez Canyon (Abo Formation)",NA,"Harvard locality, Canyon de San Diego",US,New Mexico,Sandoval,stated in text,minutes,small collection,"4.5 mi south of Jemez Springs, Sandoval County, New Mexico. Western side of the Permian Basin. Lat long is for Jemez Springs.\n"" [...] on east side of Canyon de San Diego, east of State Highway 4, about 4 1/2 miles south of Jemez Springs, approximately lat 35 43' N.; long 106 47' W., Sandoval County, New Mexico"" (Berman, 1977)",gp_mid,-34.43,4.24,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)","""shale""",red,,,Y,sandstone,"coarse,micaceous,red",,,Y,fluvial indet.,non-subsiding area,"""relative abundance of micaceous and coarse arkosic detritus often associated with the bone-beds suggest that these Abo sediments were laid down nearer their source and under conditions of better regional drainage than contemporary ""deltaic"" Wichita rocks in Texas. The late Pennsylvanian and early Permian uplifts of the near-by ""Ancestral Rockies"" were evidently responsible for this early advent of red-bed deposition on the west side of the Permian Basin...""",macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,field collection,UCMP,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Embolomeri,,NA,NA,vertebrate,"W. Langston, Jr. 1952. The first embolomerous amphibians from New Mexico. Journal of Geology 61(1):68-71",4,76,14,J. Alroy,R. Whatley,M. Carrano,22/01/2003 15:07,10/12/2012 14:40,43845,indet.,,7686,,296.4,268,Wolfcamp,,1,US, indet.
294219,occ,NA,,28067,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Langston,1952,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-106.783333,35.716667,"UCMP 39179, Jemez Canyon (Abo Formation)",NA,"Harvard locality, Canyon de San Diego",US,New Mexico,Sandoval,stated in text,minutes,small collection,"4.5 mi south of Jemez Springs, Sandoval County, New Mexico. Western side of the Permian Basin. Lat long is for Jemez Springs.\n"" [...] on east side of Canyon de San Diego, east of State Highway 4, about 4 1/2 miles south of Jemez Springs, approximately lat 35 43' N.; long 106 47' W., Sandoval County, New Mexico"" (Berman, 1977)",gp_mid,-34.43,4.24,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)","""shale""",red,,,Y,sandstone,"coarse,micaceous,red",,,Y,fluvial indet.,non-subsiding area,"""relative abundance of micaceous and coarse arkosic detritus often associated with the bone-beds suggest that these Abo sediments were laid down nearer their source and under conditions of better regional drainage than contemporary ""deltaic"" Wichita rocks in Texas. The late Pennsylvanian and early Permian uplifts of the near-by ""Ancestral Rockies"" were evidently responsible for this early advent of red-bed deposition on the west side of the Permian Basin...""",macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,field collection,UCMP,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"W. Langston, Jr. 1952. The first embolomerous amphibians from New Mexico. Journal of Geology 61(1):68-71",4,76,14,J. Alroy,R. Whatley,M. Carrano,22/01/2003 15:07,10/12/2012 14:40,43845,sp.,Eryops,7686,,296.4,268,Wolfcamp,,NA,US,Eryops sp.
294220,occ,NA,,28067,,Diadectidae indet.,family,37246,,Diadectidae,NA,family,37246,Langston,1952,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,NA,NA,NA,NA,,-106.783333,35.716667,"UCMP 39179, Jemez Canyon (Abo Formation)",NA,"Harvard locality, Canyon de San Diego",US,New Mexico,Sandoval,stated in text,minutes,small collection,"4.5 mi south of Jemez Springs, Sandoval County, New Mexico. Western side of the Permian Basin. Lat long is for Jemez Springs.\n"" [...] on east side of Canyon de San Diego, east of State Highway 4, about 4 1/2 miles south of Jemez Springs, approximately lat 35 43' N.; long 106 47' W., Sandoval County, New Mexico"" (Berman, 1977)",gp_mid,-34.43,4.24,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)","""shale""",red,,,Y,sandstone,"coarse,micaceous,red",,,Y,fluvial indet.,non-subsiding area,"""relative abundance of micaceous and coarse arkosic detritus often associated with the bone-beds suggest that these Abo sediments were laid down nearer their source and under conditions of better regional drainage than contemporary ""deltaic"" Wichita rocks in Texas. The late Pennsylvanian and early Permian uplifts of the near-by ""Ancestral Rockies"" were evidently responsible for this early advent of red-bed deposition on the west side of the Permian Basin...""",macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,field collection,UCMP,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectidae,,NA,NA,vertebrate,"W. Langston, Jr. 1952. The first embolomerous amphibians from New Mexico. Journal of Geology 61(1):68-71",4,76,14,J. Alroy,R. Whatley,M. Carrano,22/01/2003 15:07,10/12/2012 14:40,43845,indet.,,7686,,296.4,268,Wolfcamp,,NA,US, indet.
294221,occ,NA,,28067,,Sphenacodontidae indet.,family,38901,,Sphenacodontidae,NA,family,38901,Langston,1952,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,NA,NA,NA,NA,,-106.783333,35.716667,"UCMP 39179, Jemez Canyon (Abo Formation)",NA,"Harvard locality, Canyon de San Diego",US,New Mexico,Sandoval,stated in text,minutes,small collection,"4.5 mi south of Jemez Springs, Sandoval County, New Mexico. Western side of the Permian Basin. Lat long is for Jemez Springs.\n"" [...] on east side of Canyon de San Diego, east of State Highway 4, about 4 1/2 miles south of Jemez Springs, approximately lat 35 43' N.; long 106 47' W., Sandoval County, New Mexico"" (Berman, 1977)",gp_mid,-34.43,4.24,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)","""shale""",red,,,Y,sandstone,"coarse,micaceous,red",,,Y,fluvial indet.,non-subsiding area,"""relative abundance of micaceous and coarse arkosic detritus often associated with the bone-beds suggest that these Abo sediments were laid down nearer their source and under conditions of better regional drainage than contemporary ""deltaic"" Wichita rocks in Texas. The late Pennsylvanian and early Permian uplifts of the near-by ""Ancestral Rockies"" were evidently responsible for this early advent of red-bed deposition on the west side of the Permian Basin...""",macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,field collection,UCMP,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodontidae,,NA,NA,vertebrate,"W. Langston, Jr. 1952. The first embolomerous amphibians from New Mexico. Journal of Geology 61(1):68-71",4,76,14,J. Alroy,R. Whatley,M. Carrano,22/01/2003 15:07,10/12/2012 14:40,43845,indet.,,7686,,296.4,268,Wolfcamp,,NA,US, indet.
294222,occ,NA,,28068,,Embolomeri indet.,suborder,37178,,Embolomeri,NA,suborder,37178,Langston,1952,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,specimens,-106.71833,35.730278,UCMP V-3440 (Abo Formation),NA,Johnson locality,US,New Mexico,Sandoval,based on nearby landmark,seconds,small collection,"""...locality lies about 100 yards north of the abandoned ""Spanish Queen"" copper mine (Burnett on some maps), on the east side of Canyon San Diego, 2.75 miles south of Jemez Springs.""",gp_mid,-33.06,6.75,101,US,FED,Abo,,,bed,,,,,Permian Basin,,NA,"""The fossil horizon is in the lower fourth of the Abo formation at this spot and stratigraphically below the Harvard locality to the south."" The ""Harvard"" locality is UCMP-39179.","""A number of reptile and amphibian bones were also collected here in a dark-gray mudstone that overlies a yellow plant-bearing sandstone, through which the main mine shaft enters the east wall of the canyon.""",mudstone,gray,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,UCMP,some macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Embolomeri,,NA,NA,vertebrate,"W. Langston, Jr. 1952. The first embolomerous amphibians from New Mexico. Journal of Geology 61(1):68-71",4,76,0,J. Alroy,R. Whatley,,22/01/2003 16:02,22/01/2003 18:02,7686,indet.,,7686,,298.9,254,Rotliegendes,,1,US, indet.
294223,occ,NA,,28068,,Amphibia indet.,unranked clade,36319,,Amphibia,NA,unranked clade,36319,Langston,1952,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,,-106.71833,35.730278,UCMP V-3440 (Abo Formation),NA,Johnson locality,US,New Mexico,Sandoval,based on nearby landmark,seconds,small collection,"""...locality lies about 100 yards north of the abandoned ""Spanish Queen"" copper mine (Burnett on some maps), on the east side of Canyon San Diego, 2.75 miles south of Jemez Springs.""",gp_mid,-33.06,6.75,101,US,FED,Abo,,,bed,,,,,Permian Basin,,NA,"""The fossil horizon is in the lower fourth of the Abo formation at this spot and stratigraphically below the Harvard locality to the south."" The ""Harvard"" locality is UCMP-39179.","""A number of reptile and amphibian bones were also collected here in a dark-gray mudstone that overlies a yellow plant-bearing sandstone, through which the main mine shaft enters the east wall of the canyon.""",mudstone,gray,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,UCMP,some macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Amphibia,,NA,NA,vertebrate,"W. Langston, Jr. 1952. The first embolomerous amphibians from New Mexico. Journal of Geology 61(1):68-71",4,76,0,J. Alroy,R. Whatley,,22/01/2003 16:02,22/01/2003 18:02,7686,indet.,,7686,,298.9,254,Rotliegendes,,NA,US, indet.
294225,occ,NA,R,28069,,Batrachia indet.,unranked clade,157518,,Batrachia,NA,unranked clade,67352,Wyman,1853,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,specimens,-64.451385,45.698612,"Coal Mine Point; Divison 4, Section XV, coal-group 15",NA,South Joggins; Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Cliffs called the South Joggins (coast), about half a mile eastward of the Coal Pier.",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XV",coal-group 15,,,,NA,"From Steen (1934): ""top of the Joggins formation...Division 4, Section XV., Coal-group 15 of the Joggins section given in Dawson's 'Acadian Geology,' 1868, pp. 156-178."" From Lyell (1853): The fossils are from Bed 5 of a 25 ft section, composed of 7 beds. Bed 5 is approximately 600 ft below the main coal, ""King's Vein"".\r\nOriginal entry for Local Section name was ""South Joggins""; for Bed/horizon ""bed 5"". In Steen (1934) a ""bed 5"" is not mentioned in any way. Also, in papers published before and after Lyell's ""On the Remains of a Reptile..."" (1953) a different numbering is applied to the Joggins Section. Thus, it is more appropriate to follow the stratigraphic terminology used in Dawson (1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173), Steen (1934, see description above) and Carroll (1964). Coal-group 15 consists of 3 beds with a total thickness of 10 ft 6 in. (Dawson, 1878) (TL) \r\nOriginal entry for chronostratigraphy was simply ""Westphalian"". Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","From Lyell (1853): 5. Grey sandstone, with three erect trees, one having Stigmarian roots; erect Calamites and stems of unknown plants. (One of the erect trees in this bed contained the bones, teeth, &c. and land-shell above-mentioned.) ...9 ft;\r\n",sandstone,gray,,,Y,coal,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",good,,snapshot,,,,,,occasional,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" ",taxonomic,"bulk,selective quarrying,field collection,survey of museum collection",BMNH,,,,"J. W. Dawson, C. Lyell, among others",,"RM = Redpath Museum of McGill Unversity, Montreal","Listed by Steen (1934) as Indeterminate species: Hylerpeton dawsoni Owen; Hylerpeton longidentatum Dawson; Hylerpeton intermedium Dawson; Hylonomus multidens Dawson; Hylonomus wymani Dawson; Smilerpeton aciedentatus Dawson; Amblyodon problematicum Dawson; Sparodus sp. Dawson; Baphetes minor Dawson.\r\n\r\nAll catalogue numbers are from Steen (1934) and/or from Carroll (1967).\r\n\r\nThe taxon ""Batrachoididae indet."", entered under the reference Lyell & Dawson (1853), has been removed from the taxonomic list for it is a family of teleost fish. It probably referred to the ""batrachian"" affinities of the tetrapod bones noticed by Wyman (1853) but all these bones finally were assigned to Dendrerpeton acadianum n. gen. et sp. (see pls. II and III in Lyell & Dawson/Wyman/Owen, 1853). Thus the originally enterd taxon ""Dendrerpeton acadianum"", reference: Lyell & Dawson, was replaced by ""Batrachia indet."", reference: Wyman (1853), and re-identification by Owen (1853) was added (TL).\r\nRe-identification of ""Dendrerpeton oweni n. sp."" as ""Dendrerpeton acadianum"" by by Steen was removed after opinons on synonymy of the the former with the latter species were entered into the database (TL).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Batrachia,,NA,NA,vertebrate,J. Wyman. 1853. Notes on the Reptilian Remains. Quarterly Journal of the Geological Society of London 9:64-66,4,76,697,J. Alroy,R. Whatley,E. Dunne,22/01/2003 17:47,20/01/2016 04:56,7856,indet.,,32314,,318.1,314.6,Westphalian A,,1,CA, indet.
294225,occ,23005,,28069,,n. gen. Dendrerpeton n. sp. acadianum,species,164775,,Dendrerpeton acadianum,NA,species,164775,Owen,1853,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dendrerpetonidae,36994,36995,NA,NA,NA,specimens,-64.451385,45.698612,"Coal Mine Point; Divison 4, Section XV, coal-group 15",NA,South Joggins; Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Cliffs called the South Joggins (coast), about half a mile eastward of the Coal Pier.",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XV",coal-group 15,,,,NA,"From Steen (1934): ""top of the Joggins formation...Division 4, Section XV., Coal-group 15 of the Joggins section given in Dawson's 'Acadian Geology,' 1868, pp. 156-178."" From Lyell (1853): The fossils are from Bed 5 of a 25 ft section, composed of 7 beds. Bed 5 is approximately 600 ft below the main coal, ""King's Vein"".\r\nOriginal entry for Local Section name was ""South Joggins""; for Bed/horizon ""bed 5"". In Steen (1934) a ""bed 5"" is not mentioned in any way. Also, in papers published before and after Lyell's ""On the Remains of a Reptile..."" (1953) a different numbering is applied to the Joggins Section. Thus, it is more appropriate to follow the stratigraphic terminology used in Dawson (1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173), Steen (1934, see description above) and Carroll (1964). Coal-group 15 consists of 3 beds with a total thickness of 10 ft 6 in. (Dawson, 1878) (TL) \r\nOriginal entry for chronostratigraphy was simply ""Westphalian"". Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","From Lyell (1853): 5. Grey sandstone, with three erect trees, one having Stigmarian roots; erect Calamites and stems of unknown plants. (One of the erect trees in this bed contained the bones, teeth, &c. and land-shell above-mentioned.) ...9 ft;\r\n",sandstone,gray,,,Y,coal,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",good,,snapshot,,,,,,occasional,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" ",taxonomic,"bulk,selective quarrying,field collection,survey of museum collection",BMNH,,,,"J. W. Dawson, C. Lyell, among others",,"RM = Redpath Museum of McGill Unversity, Montreal","Listed by Steen (1934) as Indeterminate species: Hylerpeton dawsoni Owen; Hylerpeton longidentatum Dawson; Hylerpeton intermedium Dawson; Hylonomus multidens Dawson; Hylonomus wymani Dawson; Smilerpeton aciedentatus Dawson; Amblyodon problematicum Dawson; Sparodus sp. Dawson; Baphetes minor Dawson.\r\n\r\nAll catalogue numbers are from Steen (1934) and/or from Carroll (1967).\r\n\r\nThe taxon ""Batrachoididae indet."", entered under the reference Lyell & Dawson (1853), has been removed from the taxonomic list for it is a family of teleost fish. It probably referred to the ""batrachian"" affinities of the tetrapod bones noticed by Wyman (1853) but all these bones finally were assigned to Dendrerpeton acadianum n. gen. et sp. (see pls. II and III in Lyell & Dawson/Wyman/Owen, 1853). Thus the originally enterd taxon ""Dendrerpeton acadianum"", reference: Lyell & Dawson, was replaced by ""Batrachia indet."", reference: Wyman (1853), and re-identification by Owen (1853) was added (TL).\r\nRe-identification of ""Dendrerpeton oweni n. sp."" as ""Dendrerpeton acadianum"" by by Steen was removed after opinons on synonymy of the the former with the latter species were entered into the database (TL).","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Dendrerpeton,n. gen.,NA,NA,vertebrate,R. Owen. 1853. Notes on the above-described fossil remains. Quarterly Journal of the Geological Society of London 9:66-67,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,15/03/2010 18:23,15/03/2010 21:03,7856,acadianum,Dendrerpeton,32300,n. sp.,318.1,314.6,Westphalian A,,1,CA,Dendrerpeton acadianum
295886,occ,NA,,28119,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.764725,33.473057,"Cottonwood Creek, 1 (Putnam Formation)",NA,"Locality 1 (Romer 1928), faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,estimated from map,seconds,outcrop,"Cottonwood Creek, a tributary of the south fork of the Little Wichita, 10 miles south of Archer City. See detailed locality map in Romer 1928.",gp_mid,-30.42,-1.67,101,US,,Archer City,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone. ""vertebrates are found in the upper 200 feet in Archer County."" Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles);\nThe former Putnam Formation comprises the upper part of the Archer City Formation (Hentz, 1988, The University of Texas at Austin, Bureau of Economic Geology, Report of Investigations, 170). ","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,327,J. Alroy,R. Whatley,R. Butler,07/02/2003 12:40,08/08/2016 09:51,7693,sp.,Eryops,7693,,295.5,290.1,Sakmarian,,1,US,Eryops sp.
295887,occ,NA,,28120,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.625275,33.595554,"Elm Creek, 2 (Putnam Formation)",NA,"Locality 2 (Romer 1928), Locality IIIa (Romer & Price (1940), faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Elm Creek, stated by Cummins to be 12 miles southwest of Archer City; its exact position is uncertain.."" Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group- boundary is at the top of the Coleman Junction Limestone. ""probably about 100 feet below the Coleman Junction."" Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984). \nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 12:43,07/02/2003 14:43,7693,sp.,Eryops,7693,,295.5,290.1,Sakmarian,,3,US,Eryops sp.
295888,occ,NA,,28120,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-98.625275,33.595554,"Elm Creek, 2 (Putnam Formation)",NA,"Locality 2 (Romer 1928), Locality IIIa (Romer & Price (1940), faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Elm Creek, stated by Cummins to be 12 miles southwest of Archer City; its exact position is uncertain.."" Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group- boundary is at the top of the Coleman Junction Limestone. ""probably about 100 feet below the Coleman Junction."" Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984). \nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 12:43,07/02/2003 14:43,7693,sp.,Dimetrodon,7693,,295.5,290.1,Sakmarian,,3,US,Dimetrodon sp.
295889,occ,NA,,28121,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-98.625275,33.595554,"Onion Creek, 3 (Putnam Formation)",NA,"Locality 3 (Romer 1928), mouth of Onion Creek, faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"The mouth of Onion Creek, northeast of Archer City. Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone. ""about 90 feet below the top of the Cisco."" Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 12:46,07/02/2003 14:46,7693,sp.,Ophiacodon,7693,,295.5,290.1,Sakmarian,,1,US,Ophiacodon sp.
295890,occ,NA,,28122,,Cricotus sp.,genus,37197,,Cricotus,NA,genus,37197,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37197,NA,NA,NA,specimens,-98.625275,33.595554,"Fireplace, 4 (Putnam Formation)",NA,"Locality 4 (Romer 1928), faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""The ""Fireplace,"" on the south fork, near the mouth of Cottonwood Creek."" Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone. ""not far below the Cisco-Wichita boundary."" Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\nterrestrial and near-shore deposition",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cricotus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 12:51,07/02/2003 14:51,7693,sp.,Cricotus,7693,,295.5,290.1,Sakmarian,,1,US,Cricotus sp.
295891,occ,NA,,28122,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.625275,33.595554,"Fireplace, 4 (Putnam Formation)",NA,"Locality 4 (Romer 1928), faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""The ""Fireplace,"" on the south fork, near the mouth of Cottonwood Creek."" Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone. ""not far below the Cisco-Wichita boundary."" Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\nterrestrial and near-shore deposition",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 12:51,07/02/2003 14:51,7693,sp.,Eryops,7693,,295.5,290.1,Sakmarian,,1,US,Eryops sp.
295892,occ,NA,,28123,,Cricotus sp.,genus,37197,,Cricotus,NA,genus,37197,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37197,NA,NA,NA,specimens,-98.625275,33.595554,"Three Forks of the Little Wichita, 5 (Putnam Formation)",NA,"Locality 5 (Romer 1928), Locality IVb (Romer & Price, 1940) faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Three Forks of the Little Wichita, northwest of Archer City."" Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone.""close to the line of the Coleman Junction."" Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cricotus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 12:53,07/02/2003 14:53,7693,sp.,Cricotus,7693,,295.5,290.1,Sakmarian,,1,US,Cricotus sp.
295893,occ,NA,,28123,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.625275,33.595554,"Three Forks of the Little Wichita, 5 (Putnam Formation)",NA,"Locality 5 (Romer 1928), Locality IVb (Romer & Price, 1940) faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Three Forks of the Little Wichita, northwest of Archer City."" Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone.""close to the line of the Coleman Junction."" Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 12:53,07/02/2003 14:53,7693,sp.,Eryops,7693,,295.5,290.1,Sakmarian,,2,US,Eryops sp.
295894,occ,NA,,28123,,Zatrachys sp.,genus,37056,,Zatrachys,NA,genus,37056,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,specimens,-98.625275,33.595554,"Three Forks of the Little Wichita, 5 (Putnam Formation)",NA,"Locality 5 (Romer 1928), Locality IVb (Romer & Price, 1940) faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Three Forks of the Little Wichita, northwest of Archer City."" Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone.""close to the line of the Coleman Junction."" Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 12:53,07/02/2003 14:53,7693,sp.,Zatrachys,7693,,295.5,290.1,Sakmarian,,1,US,Zatrachys sp.
295895,occ,NA,,28123,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-98.625275,33.595554,"Three Forks of the Little Wichita, 5 (Putnam Formation)",NA,"Locality 5 (Romer 1928), Locality IVb (Romer & Price, 1940) faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Three Forks of the Little Wichita, northwest of Archer City."" Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone.""close to the line of the Coleman Junction."" Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 12:53,07/02/2003 14:53,7693,sp.,Dimetrodon,7693,,295.5,290.1,Sakmarian,,2,US,Dimetrodon sp.
295896,occ,NA,,28124,,Cricotus sp.,genus,37197,,Cricotus,NA,genus,37197,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37197,NA,NA,NA,specimens,-98.625275,33.595554,"Shell Point, 6 (Putnam Formation)",NA,"Locality 6 (Romer 1928), ""Shell Point"", faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,""" ""Shell Point,"" a Boll locality whose exact position is unknown, but which was probably not far from the Three Forks [of the Little Wichita collection]."" Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone. Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cricotus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:02,07/02/2003 15:02,7693,sp.,Cricotus,7693,,295.5,290.1,Sakmarian,,1,US,Cricotus sp.
295897,occ,NA,,28124,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.625275,33.595554,"Shell Point, 6 (Putnam Formation)",NA,"Locality 6 (Romer 1928), ""Shell Point"", faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,""" ""Shell Point,"" a Boll locality whose exact position is unknown, but which was probably not far from the Three Forks [of the Little Wichita collection]."" Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone. Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:02,07/02/2003 15:02,7693,sp.,Eryops,7693,,295.5,290.1,Sakmarian,,1,US,Eryops sp.
295898,occ,NA,,28124,,Diadectes n. sp. latibuccatus,species,320987,subjective synonym of,Diadectes sideropelicus,NA,species,320982,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-98.625275,33.595554,"Shell Point, 6 (Putnam Formation)",NA,"Locality 6 (Romer 1928), ""Shell Point"", faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,""" ""Shell Point,"" a Boll locality whose exact position is unknown, but which was probably not far from the Three Forks [of the Little Wichita collection]."" Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone. Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:02,07/02/2003 15:02,7693,latibuccatus,Diadectes,7693,n. sp.,295.5,290.1,Sakmarian,,1,US,Diadectes latibuccatus
295899,occ,NA,,28124,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-98.625275,33.595554,"Shell Point, 6 (Putnam Formation)",NA,"Locality 6 (Romer 1928), ""Shell Point"", faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,""" ""Shell Point,"" a Boll locality whose exact position is unknown, but which was probably not far from the Three Forks [of the Little Wichita collection]."" Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone. Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:02,07/02/2003 15:02,7693,sp.,Ophiacodon,7693,,295.5,290.1,Sakmarian,,1,US,Ophiacodon sp.
295900,occ,NA,,28124,,n. gen. Dimetrodon n. sp. incisivus,species,54986,subjective synonym of,Dimetrodon limbatus,NA,species,70401,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-98.625275,33.595554,"Shell Point, 6 (Putnam Formation)",NA,"Locality 6 (Romer 1928), ""Shell Point"", faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,""" ""Shell Point,"" a Boll locality whose exact position is unknown, but which was probably not far from the Three Forks [of the Little Wichita collection]."" Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone. Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,n. gen.,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:02,07/02/2003 15:02,7693,incisivus,Dimetrodon,7693,n. sp.,295.5,290.1,Sakmarian,,3,US,Dimetrodon incisivus
295901,occ,NA,,28125,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.625275,33.595554,"Long Creek, 7 (Putnam Formation)",NA,"Locality 7 (Romer 1928), faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Long Creek, which empties into the north side of the Little Wichita due north of Archer City (not northwest of the copper mines, as stated by Cummins). ""Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,formation,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone. "" If the locality was near the mouth, as was probably the case, it would be just below the Wichita-Cisco boundary."" Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:05,07/02/2003 15:05,7693,sp.,Eryops,7693,,295.5,290.1,Sakmarian,,1,US,Eryops sp.
295902,occ,NA,,28125,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-98.625275,33.595554,"Long Creek, 7 (Putnam Formation)",NA,"Locality 7 (Romer 1928), faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Long Creek, which empties into the north side of the Little Wichita due north of Archer City (not northwest of the copper mines, as stated by Cummins). ""Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,formation,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone. "" If the locality was near the mouth, as was probably the case, it would be just below the Wichita-Cisco boundary."" Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:05,07/02/2003 15:05,7693,sp.,Diadectes,7693,,295.5,290.1,Sakmarian,,1,US,Diadectes sp.
295903,occ,NA,,28125,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-98.625275,33.595554,"Long Creek, 7 (Putnam Formation)",NA,"Locality 7 (Romer 1928), faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Long Creek, which empties into the north side of the Little Wichita due north of Archer City (not northwest of the copper mines, as stated by Cummins). ""Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,formation,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone. "" If the locality was near the mouth, as was probably the case, it would be just below the Wichita-Cisco boundary."" Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:05,07/02/2003 15:05,7693,sp.,Dimetrodon,7693,,295.5,290.1,Sakmarian,,1,US,Dimetrodon sp.
295904,occ,NA,,28125,,Edaphosaurus sp.,genus,38911,,Edaphosaurus,NA,genus,38911,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,specimens,-98.625275,33.595554,"Long Creek, 7 (Putnam Formation)",NA,"Locality 7 (Romer 1928), faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Long Creek, which empties into the north side of the Little Wichita due north of Archer City (not northwest of the copper mines, as stated by Cummins). ""Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,formation,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone. "" If the locality was near the mouth, as was probably the case, it would be just below the Wichita-Cisco boundary."" Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:05,07/02/2003 15:05,7693,sp.,Edaphosaurus,7693,,295.5,290.1,Sakmarian,,1,US,Edaphosaurus sp.
295905,occ,NA,,28141,,Cricotus sp.,genus,37197,,Cricotus,NA,genus,37197,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37197,NA,NA,NA,specimens,-98.625275,33.595554,"Middle Fork of the Little Wichita, 10 (Admiral Formation)",NA,"Locality 10 (Romer 1928), Locality Vg (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"This locality is ""...4 miles west of Archer City; on the east bank, near the old Archer-Seymour (now Archer-Megargel) road."" Lat long is for Archer City, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30.06,-1.3,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"This locality is ""about 50 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\nterrestrial and near-shore deposition","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cricotus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:15,07/02/2003 15:15,7693,sp.,Cricotus,7693,,290.1,279.3,Artinskian,,1,US,Cricotus sp.
295906,occ,NA,,28141,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.625275,33.595554,"Middle Fork of the Little Wichita, 10 (Admiral Formation)",NA,"Locality 10 (Romer 1928), Locality Vg (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"This locality is ""...4 miles west of Archer City; on the east bank, near the old Archer-Seymour (now Archer-Megargel) road."" Lat long is for Archer City, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30.06,-1.3,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"This locality is ""about 50 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\nterrestrial and near-shore deposition","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:15,07/02/2003 15:15,7693,sp.,Eryops,7693,,290.1,279.3,Artinskian,,2,US,Eryops sp.
295907,occ,NA,,28141,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-98.625275,33.595554,"Middle Fork of the Little Wichita, 10 (Admiral Formation)",NA,"Locality 10 (Romer 1928), Locality Vg (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"This locality is ""...4 miles west of Archer City; on the east bank, near the old Archer-Seymour (now Archer-Megargel) road."" Lat long is for Archer City, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30.06,-1.3,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"This locality is ""about 50 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\nterrestrial and near-shore deposition","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,4,J. Alroy,R. Whatley,J. Alroy,07/02/2003 13:15,17/12/2006 15:12,7693,sp.,Trimerorhachis,7693,,290.1,279.3,Artinskian,,1,US,Trimerorhachis sp.
295908,occ,NA,R,28141,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-98.625275,33.595554,"Middle Fork of the Little Wichita, 10 (Admiral Formation)",NA,"Locality 10 (Romer 1928), Locality Vg (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"This locality is ""...4 miles west of Archer City; on the east bank, near the old Archer-Seymour (now Archer-Megargel) road."" Lat long is for Archer City, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30.06,-1.3,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"This locality is ""about 50 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\nterrestrial and near-shore deposition","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:15,07/02/2003 15:15,7693,sp.,Ophiacodon,7693,,290.1,279.3,Artinskian,,1,US,Ophiacodon sp.
295908,occ,21225,,28141,,Ophiacodon retroversus,species,123420,,Ophiacodon retroversus,NA,species,138048,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-98.625275,33.595554,"Middle Fork of the Little Wichita, 10 (Admiral Formation)",NA,"Locality 10 (Romer 1928), Locality Vg (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"This locality is ""...4 miles west of Archer City; on the east bank, near the old Archer-Seymour (now Archer-Megargel) road."" Lat long is for Archer City, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30.06,-1.3,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"This locality is ""about 50 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\nterrestrial and near-shore deposition","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,0,J. Mueller,T. Liebrecht,,14/01/2009 00:34,14/01/2009 02:34,7693,retroversus,Ophiacodon,5692,,290.1,279.3,Artinskian,,1,US,Ophiacodon retroversus
295909,occ,NA,,28141,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-98.625275,33.595554,"Middle Fork of the Little Wichita, 10 (Admiral Formation)",NA,"Locality 10 (Romer 1928), Locality Vg (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"This locality is ""...4 miles west of Archer City; on the east bank, near the old Archer-Seymour (now Archer-Megargel) road."" Lat long is for Archer City, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30.06,-1.3,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"This locality is ""about 50 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\nterrestrial and near-shore deposition","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:15,07/02/2003 15:15,7693,sp.,Dimetrodon,7693,,290.1,279.3,Artinskian,,1,US,Dimetrodon sp.
295910,occ,NA,,28141,,Edaphosaurus sp.,genus,38911,,Edaphosaurus,NA,genus,38911,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,specimens,-98.625275,33.595554,"Middle Fork of the Little Wichita, 10 (Admiral Formation)",NA,"Locality 10 (Romer 1928), Locality Vg (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"This locality is ""...4 miles west of Archer City; on the east bank, near the old Archer-Seymour (now Archer-Megargel) road."" Lat long is for Archer City, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30.06,-1.3,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"This locality is ""about 50 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\nterrestrial and near-shore deposition","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:15,07/02/2003 15:15,7693,sp.,Edaphosaurus,7693,,290.1,279.3,Artinskian,,1,US,Edaphosaurus sp.
295911,occ,NA,,28239,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.694725,33.816113,"South of Holliday, 11 (Admiral Formation)",NA,"Locality 11 (Romer 1928), S. of Holliday, Head of Long Creek, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Case's notes for 1906 show that a number of specimens were collected south of Holliday and near the Little Wichita, but the exact location cannot now be ascertained."" That being said, the detailed locality map in Romer 1928 marks locality 11 at the head of Long Creek, ~7 mi due south of Holliday. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?"" Lat long is for Holliday.",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"""This region would be about 70 feet above the base of the Wichita."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n","""shale""",red,,"sandy,conglomeratic",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,76,J. Alroy,R. Whatley,R. Whatley,07/02/2003 13:16,07/02/2003 15:16,7693,sp.,Eryops,7693,,290.1,279.3,Artinskian,,3,US,Eryops sp.
295912,occ,NA,,28239,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-98.694725,33.816113,"South of Holliday, 11 (Admiral Formation)",NA,"Locality 11 (Romer 1928), S. of Holliday, Head of Long Creek, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Case's notes for 1906 show that a number of specimens were collected south of Holliday and near the Little Wichita, but the exact location cannot now be ascertained."" That being said, the detailed locality map in Romer 1928 marks locality 11 at the head of Long Creek, ~7 mi due south of Holliday. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?"" Lat long is for Holliday.",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"""This region would be about 70 feet above the base of the Wichita."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n","""shale""",red,,"sandy,conglomeratic",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:16,07/02/2003 15:16,7693,sp.,Ophiacodon,7693,,290.1,279.3,Artinskian,,1,US,Ophiacodon sp.
295913,occ,NA,,28239,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-98.694725,33.816113,"South of Holliday, 11 (Admiral Formation)",NA,"Locality 11 (Romer 1928), S. of Holliday, Head of Long Creek, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Case's notes for 1906 show that a number of specimens were collected south of Holliday and near the Little Wichita, but the exact location cannot now be ascertained."" That being said, the detailed locality map in Romer 1928 marks locality 11 at the head of Long Creek, ~7 mi due south of Holliday. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?"" Lat long is for Holliday.",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"""This region would be about 70 feet above the base of the Wichita."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n","""shale""",red,,"sandy,conglomeratic",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,76,J. Alroy,R. Whatley,R. Whatley,07/02/2003 13:16,07/02/2003 15:16,7693,sp.,Dimetrodon,7693,,290.1,279.3,Artinskian,,4,US,Dimetrodon sp.
295914,occ,NA,,28142,,Cricotus sp.,genus,37197,,Cricotus,NA,genus,37197,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37197,NA,NA,NA,specimens,-98.694725,33.816113,"Mount Barry, 12 (Admiral Formation)",NA,"Locality 12 (Romer 1928), Locality IVf (Romer & Price 1940), Mt. Barry, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""10 miles west of Wichita Falls."" Lat long is for Holliday, approx. 5 mi southeast of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,"""Many of Cope's types are from this region.""","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cricotus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:46,07/02/2003 15:46,7693,sp.,Cricotus,7693,,290.1,279.3,Artinskian,,1,US,Cricotus sp.
295915,occ,NA,,28142,,Eryops n. sp. anatinus,species,37011,species not entered,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.694725,33.816113,"Mount Barry, 12 (Admiral Formation)",NA,"Locality 12 (Romer 1928), Locality IVf (Romer & Price 1940), Mt. Barry, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""10 miles west of Wichita Falls."" Lat long is for Holliday, approx. 5 mi southeast of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,"""Many of Cope's types are from this region.""","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:46,07/02/2003 15:46,7693,anatinus,Eryops,7693,n. sp.,290.1,279.3,Artinskian,,7,US,Eryops anatinus
295916,occ,NA,,28142,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-98.694725,33.816113,"Mount Barry, 12 (Admiral Formation)",NA,"Locality 12 (Romer 1928), Locality IVf (Romer & Price 1940), Mt. Barry, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""10 miles west of Wichita Falls."" Lat long is for Holliday, approx. 5 mi southeast of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,"""Many of Cope's types are from this region.""","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,4,J. Alroy,R. Whatley,J. Alroy,07/02/2003 13:46,17/12/2006 15:12,7693,sp.,Trimerorhachis,7693,,290.1,279.3,Artinskian,,2,US,Trimerorhachis sp.
295917,occ,NA,,28142,,n. gen. Parioxys n. sp. ferricolus,species,345270,,Parioxys ferricolus,NA,species,345270,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37052,NA,NA,NA,specimens,-98.694725,33.816113,"Mount Barry, 12 (Admiral Formation)",NA,"Locality 12 (Romer 1928), Locality IVf (Romer & Price 1940), Mt. Barry, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""10 miles west of Wichita Falls."" Lat long is for Holliday, approx. 5 mi southeast of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,"""Many of Cope's types are from this region.""","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Parioxys,n. gen.,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,76,J. Alroy,R. Whatley,R. Whatley,07/02/2003 13:46,09/02/2003 16:35,7693,ferricolus,Parioxys,7693,n. sp.,290.1,279.3,Artinskian,,1,US,Parioxys ferricolus
295918,occ,NA,,28142,,n. gen. Diadectes n. sp. sideropelicus,species,320982,,Diadectes sideropelicus,NA,species,320982,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-98.694725,33.816113,"Mount Barry, 12 (Admiral Formation)",NA,"Locality 12 (Romer 1928), Locality IVf (Romer & Price 1940), Mt. Barry, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""10 miles west of Wichita Falls."" Lat long is for Holliday, approx. 5 mi southeast of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,"""Many of Cope's types are from this region.""","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,n. gen.,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:46,07/02/2003 15:46,7693,sideropelicus,Diadectes,7693,n. sp.,290.1,279.3,Artinskian,,NA,US,Diadectes sideropelicus
295919,occ,NA,,28142,,Diadectes n. sp. biculminatus,species,320986,subjective synonym of,Diadectes sideropelicus,NA,species,320982,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-98.694725,33.816113,"Mount Barry, 12 (Admiral Formation)",NA,"Locality 12 (Romer 1928), Locality IVf (Romer & Price 1940), Mt. Barry, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""10 miles west of Wichita Falls."" Lat long is for Holliday, approx. 5 mi southeast of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,"""Many of Cope's types are from this region.""","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:46,07/02/2003 15:46,7693,biculminatus,Diadectes,7693,n. sp.,290.1,279.3,Artinskian,,NA,US,Diadectes biculminatus
295920,occ,NA,,28142,,n. gen. Empedias n. sp. alatus,species,320991,subjective synonym of,Diadectes sideropelicus,NA,species,320982,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-98.694725,33.816113,"Mount Barry, 12 (Admiral Formation)",NA,"Locality 12 (Romer 1928), Locality IVf (Romer & Price 1940), Mt. Barry, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""10 miles west of Wichita Falls."" Lat long is for Holliday, approx. 5 mi southeast of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,"""Many of Cope's types are from this region.""","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Empedias,n. gen.,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 13:46,07/02/2003 15:46,7693,alatus,Diadectes,7693,n. sp.,290.1,279.3,Artinskian,,NA,US,Diadectes alatus
295921,occ,NA,,28142,,Theropleura n. sp. retroversa,species,138048,recombined as,Ophiacodon retroversus,NA,species,138048,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-98.694725,33.816113,"Mount Barry, 12 (Admiral Formation)",NA,"Locality 12 (Romer 1928), Locality IVf (Romer & Price 1940), Mt. Barry, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""10 miles west of Wichita Falls."" Lat long is for Holliday, approx. 5 mi southeast of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,"""Many of Cope's types are from this region.""",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 13:46,11/01/2009 21:39,7693,retroversa,Ophiacodon,7693,n. sp.,290.1,279.3,Artinskian,,6,US,Ophiacodon retroversa
295922,occ,NA,,28142,,Dimetrodon n. sp. rectiformis,species,138121,subjective synonym of,Dimetrodon limbatus,NA,species,70401,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-98.694725,33.816113,"Mount Barry, 12 (Admiral Formation)",NA,"Locality 12 (Romer 1928), Locality IVf (Romer & Price 1940), Mt. Barry, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""10 miles west of Wichita Falls."" Lat long is for Holliday, approx. 5 mi southeast of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,"""Many of Cope's types are from this region.""",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 13:46,09/01/2009 15:15,7693,rectiformis,Dimetrodon,7693,n. sp.,290.1,279.3,Artinskian,,8,US,Dimetrodon rectiformis
295923,occ,NA,,28142,,Clepsydrops n. sp. natalis,species,54971,recombined as,Dimetrodon natalis,NA,species,54971,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,individuals,-98.694725,33.816113,"Mount Barry, 12 (Admiral Formation)",NA,"Locality 12 (Romer 1928), Locality IVf (Romer & Price 1940), Mt. Barry, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""10 miles west of Wichita Falls."" Lat long is for Holliday, approx. 5 mi southeast of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,"""Many of Cope's types are from this region.""",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Clepsydrops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 13:46,09/01/2009 17:27,7693,natalis,Dimetrodon,7693,n. sp.,290.1,279.3,Artinskian,,1,US,Dimetrodon natalis
295924,occ,NA,,28142,,n. gen. Bolosaurus n. sp. striatus,species,138029,,Bolosaurus striatus,NA,species,138029,Romer,1928,Chordata,33815,Reptilia,36322,,NA,Bolosauridae,37510,37511,NA,NA,NA,individuals,-98.694725,33.816113,"Mount Barry, 12 (Admiral Formation)",NA,"Locality 12 (Romer 1928), Locality IVf (Romer & Price 1940), Mt. Barry, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""10 miles west of Wichita Falls."" Lat long is for Holliday, approx. 5 mi southeast of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,"""Many of Cope's types are from this region.""",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Bolosaurus,n. gen.,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 13:46,09/01/2009 15:13,7693,striatus,Bolosaurus,7693,n. sp.,290.1,279.3,Artinskian,,7,US,Bolosaurus striatus
295925,occ,NA,,28142,,Bolosaurus n. sp. major,species,138979,,Bolosaurus major,NA,species,138979,Romer,1928,Chordata,33815,Reptilia,36322,,NA,Bolosauridae,37510,37511,NA,NA,NA,individuals,-98.694725,33.816113,"Mount Barry, 12 (Admiral Formation)",NA,"Locality 12 (Romer 1928), Locality IVf (Romer & Price 1940), Mt. Barry, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""10 miles west of Wichita Falls."" Lat long is for Holliday, approx. 5 mi southeast of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,"""Many of Cope's types are from this region.""",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Bolosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 13:46,09/01/2009 15:13,7693,major,Bolosaurus,7693,n. sp.,290.1,279.3,Artinskian,,1,US,Bolosaurus major
295927,occ,NA,,13080,,Edaphosaurus sp.,genus,38911,,Edaphosaurus,NA,genus,38911,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,specimens,-98.856941,33.622501,Briar Creek,NA,"(Admiral Formation) Locality 13 (Romer 1928), Locality IVd (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds; Brier Creek",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""the collecting ground being mainly on the east side a few miles from the mouth, near and in the bone bed discovered by Case."" Lat long is for Dundee, approx. 9 mi south of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""; DMS coordinates are for the mouth of Briar Creek into Lake Kickapoo",gp_mid,-30.21,-1.18,101,US,,Admiral,Wichita,,bed,,,,,,,NA,"""about 190 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Admiral Formation and middle Wichita Group are both Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones."" ",claystone,red,,,,sandstone,red,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,07/02/2003 14:03,16/08/2016 05:30,7693,sp.,Edaphosaurus,7693,,290.1,279.3,Artinskian,,21,US,Edaphosaurus sp.
295928,occ,NA,,13080,,Bolosaurus sp.,genus,37511,,Bolosaurus,NA,genus,37511,Romer,1928,Chordata,33815,Reptilia,36322,,NA,Bolosauridae,37510,37511,NA,NA,NA,specimens,-98.856941,33.622501,Briar Creek,NA,"(Admiral Formation) Locality 13 (Romer 1928), Locality IVd (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds; Brier Creek",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""the collecting ground being mainly on the east side a few miles from the mouth, near and in the bone bed discovered by Case."" Lat long is for Dundee, approx. 9 mi south of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""; DMS coordinates are for the mouth of Briar Creek into Lake Kickapoo",gp_mid,-30.21,-1.18,101,US,,Admiral,Wichita,,bed,,,,,,,NA,"""about 190 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Admiral Formation and middle Wichita Group are both Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones."" ",claystone,red,,,,sandstone,red,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Bolosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,07/02/2003 14:03,16/08/2016 05:30,7693,sp.,Bolosaurus,7693,,290.1,279.3,Artinskian,,7,US,Bolosaurus sp.
295930,occ,NA,,28150,,Cricotus sp.,genus,37197,,Cricotus,NA,genus,37197,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37197,NA,NA,NA,specimens,-98.92083,33.601391,"Godwin Creek, 14 (Admiral Formation)",NA,"Locality 14 (Romer 1928), Locality IVe (Romer & Price 1940), Southeast side of Godwin creek, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""specimens appear to come from the southeast side of this creek."" See detailed locality map in Romer 1928. ""Zone 1. Lat long is for Godwin Creek, USGS Dundee SW, Archer County.",gp_mid,-30.27,-1.17,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"""The horizon is about 250-300 feet above the base of the formation."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,, terrestrial and near-shore deposition\n,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,"AMNH,FMNH,MCZ",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cricotus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,07/02/2003 14:12,18/07/2016 10:55,7693,sp.,Cricotus,7693,,290.1,279.3,Artinskian,,1,US,Cricotus sp.
295931,occ,NA,,28150,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.92083,33.601391,"Godwin Creek, 14 (Admiral Formation)",NA,"Locality 14 (Romer 1928), Locality IVe (Romer & Price 1940), Southeast side of Godwin creek, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""specimens appear to come from the southeast side of this creek."" See detailed locality map in Romer 1928. ""Zone 1. Lat long is for Godwin Creek, USGS Dundee SW, Archer County.",gp_mid,-30.27,-1.17,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"""The horizon is about 250-300 feet above the base of the formation."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,, terrestrial and near-shore deposition\n,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,"AMNH,FMNH,MCZ",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,07/02/2003 14:12,18/07/2016 10:55,7693,sp.,Eryops,7693,,290.1,279.3,Artinskian,,11,US,Eryops sp.
295932,occ,NA,,28150,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-98.92083,33.601391,"Godwin Creek, 14 (Admiral Formation)",NA,"Locality 14 (Romer 1928), Locality IVe (Romer & Price 1940), Southeast side of Godwin creek, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""specimens appear to come from the southeast side of this creek."" See detailed locality map in Romer 1928. ""Zone 1. Lat long is for Godwin Creek, USGS Dundee SW, Archer County.",gp_mid,-30.27,-1.17,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"""The horizon is about 250-300 feet above the base of the formation."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,, terrestrial and near-shore deposition\n,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,"AMNH,FMNH,MCZ",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,07/02/2003 14:12,18/07/2016 10:55,7693,sp.,Trimerorhachis,7693,,290.1,279.3,Artinskian,,5,US,Trimerorhachis sp.
295933,occ,NA,,28150,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-98.92083,33.601391,"Godwin Creek, 14 (Admiral Formation)",NA,"Locality 14 (Romer 1928), Locality IVe (Romer & Price 1940), Southeast side of Godwin creek, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""specimens appear to come from the southeast side of this creek."" See detailed locality map in Romer 1928. ""Zone 1. Lat long is for Godwin Creek, USGS Dundee SW, Archer County.",gp_mid,-30.27,-1.17,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"""The horizon is about 250-300 feet above the base of the formation."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,, terrestrial and near-shore deposition\n,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,"AMNH,FMNH,MCZ",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,07/02/2003 14:12,18/07/2016 10:55,7693,sp.,Diadectes,7693,,290.1,279.3,Artinskian,,7,US,Diadectes sp.
295934,occ,NA,,28150,,Empedias n. sp. fissus,species,309287,subjective synonym of,Diadectes sideropelicus,NA,species,320982,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-98.92083,33.601391,"Godwin Creek, 14 (Admiral Formation)",NA,"Locality 14 (Romer 1928), Locality IVe (Romer & Price 1940), Southeast side of Godwin creek, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""specimens appear to come from the southeast side of this creek."" See detailed locality map in Romer 1928. ""Zone 1. Lat long is for Godwin Creek, USGS Dundee SW, Archer County.",gp_mid,-30.27,-1.17,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"""The horizon is about 250-300 feet above the base of the formation."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,, terrestrial and near-shore deposition\n,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,"AMNH,FMNH,MCZ",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Empedias,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,07/02/2003 14:12,18/07/2016 10:55,7693,fissus,Diadectes,7693,n. sp.,290.1,279.3,Artinskian,,NA,US,Diadectes fissus
295935,occ,NA,R,28150,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-98.92083,33.601391,"Godwin Creek, 14 (Admiral Formation)",NA,"Locality 14 (Romer 1928), Locality IVe (Romer & Price 1940), Southeast side of Godwin creek, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""specimens appear to come from the southeast side of this creek."" See detailed locality map in Romer 1928. ""Zone 1. Lat long is for Godwin Creek, USGS Dundee SW, Archer County.",gp_mid,-30.27,-1.17,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"""The horizon is about 250-300 feet above the base of the formation."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,, terrestrial and near-shore deposition\n,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,"AMNH,FMNH,MCZ",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,07/02/2003 14:12,18/07/2016 10:55,7693,sp.,Ophiacodon,7693,,290.1,279.3,Artinskian,,1,US,Ophiacodon sp.
295935,occ,21219,,28150,,Ophiacodon uniformis,species,123419,,Ophiacodon uniformis,NA,species,138049,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-98.92083,33.601391,"Godwin Creek, 14 (Admiral Formation)",NA,"Locality 14 (Romer 1928), Locality IVe (Romer & Price 1940), Southeast side of Godwin creek, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""specimens appear to come from the southeast side of this creek."" See detailed locality map in Romer 1928. ""Zone 1. Lat long is for Godwin Creek, USGS Dundee SW, Archer County.",gp_mid,-30.27,-1.17,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"""The horizon is about 250-300 feet above the base of the formation."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,, terrestrial and near-shore deposition\n,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,"AMNH,FMNH,MCZ",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,0,J. Mueller,T. Liebrecht,,11/01/2009 16:25,11/01/2009 18:25,7693,uniformis,Ophiacodon,5692,,290.1,279.3,Artinskian,,1,US,Ophiacodon uniformis
295936,occ,NA,,28150,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-98.92083,33.601391,"Godwin Creek, 14 (Admiral Formation)",NA,"Locality 14 (Romer 1928), Locality IVe (Romer & Price 1940), Southeast side of Godwin creek, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""specimens appear to come from the southeast side of this creek."" See detailed locality map in Romer 1928. ""Zone 1. Lat long is for Godwin Creek, USGS Dundee SW, Archer County.",gp_mid,-30.27,-1.17,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"""The horizon is about 250-300 feet above the base of the formation."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,, terrestrial and near-shore deposition\n,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,"AMNH,FMNH,MCZ",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,07/02/2003 14:12,18/07/2016 10:55,7693,sp.,Dimetrodon,7693,,290.1,279.3,Artinskian,,24,US,Dimetrodon sp.
295937,occ,NA,,28240,,Cricotus sp.,genus,37197,,Cricotus,NA,genus,37197,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37197,NA,NA,NA,specimens,-98.901947,33.740276,"Scalen's, 16 (Belle Plains Formation)",NA,"Locality 16 (Romer 1928), Scalen's Ranch, Scalen's place S, Scalen's pasture, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Case recorded a number of specimens from Scalen's ranch. This was situated somewhere to the south (and probably to the east) of Dundee; its location is not known to me."" \nAMNH records for Case's 1908 Permian, Belle Plains Formation collections as Scalen's Ranch, Scalen's place S, and Scalen's pasture localities. \nSee detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,AMNH,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cricotus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 14:24,07/02/2003 16:24,7693,sp.,Cricotus,7693,,290.1,279.3,Artinskian,,1,US,Cricotus sp.
295938,occ,NA,,28240,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.901947,33.740276,"Scalen's, 16 (Belle Plains Formation)",NA,"Locality 16 (Romer 1928), Scalen's Ranch, Scalen's place S, Scalen's pasture, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Case recorded a number of specimens from Scalen's ranch. This was situated somewhere to the south (and probably to the east) of Dundee; its location is not known to me."" \nAMNH records for Case's 1908 Permian, Belle Plains Formation collections as Scalen's Ranch, Scalen's place S, and Scalen's pasture localities. \nSee detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,AMNH,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 14:24,07/02/2003 16:24,7693,sp.,Eryops,7693,,290.1,279.3,Artinskian,,2,US,Eryops sp.
295939,occ,NA,,28240,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-98.901947,33.740276,"Scalen's, 16 (Belle Plains Formation)",NA,"Locality 16 (Romer 1928), Scalen's Ranch, Scalen's place S, Scalen's pasture, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Case recorded a number of specimens from Scalen's ranch. This was situated somewhere to the south (and probably to the east) of Dundee; its location is not known to me."" \nAMNH records for Case's 1908 Permian, Belle Plains Formation collections as Scalen's Ranch, Scalen's place S, and Scalen's pasture localities. \nSee detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,AMNH,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,4,J. Alroy,R. Whatley,J. Alroy,07/02/2003 14:24,17/12/2006 15:12,7693,sp.,Trimerorhachis,7693,,290.1,279.3,Artinskian,,1,US,Trimerorhachis sp.
295940,occ,NA,,28240,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-98.901947,33.740276,"Scalen's, 16 (Belle Plains Formation)",NA,"Locality 16 (Romer 1928), Scalen's Ranch, Scalen's place S, Scalen's pasture, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Case recorded a number of specimens from Scalen's ranch. This was situated somewhere to the south (and probably to the east) of Dundee; its location is not known to me."" \nAMNH records for Case's 1908 Permian, Belle Plains Formation collections as Scalen's Ranch, Scalen's place S, and Scalen's pasture localities. \nSee detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,AMNH,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 14:24,07/02/2003 16:24,7693,sp.,Diadectes,7693,,290.1,279.3,Artinskian,,1,US,Diadectes sp.
295941,occ,NA,,28240,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-98.901947,33.740276,"Scalen's, 16 (Belle Plains Formation)",NA,"Locality 16 (Romer 1928), Scalen's Ranch, Scalen's place S, Scalen's pasture, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Case recorded a number of specimens from Scalen's ranch. This was situated somewhere to the south (and probably to the east) of Dundee; its location is not known to me."" \nAMNH records for Case's 1908 Permian, Belle Plains Formation collections as Scalen's Ranch, Scalen's place S, and Scalen's pasture localities. \nSee detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,AMNH,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 14:24,07/02/2003 16:24,7693,sp.,Dimetrodon,7693,,290.1,279.3,Artinskian,,5,US,Dimetrodon sp.
295942,occ,NA,,28143,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.901947,33.740276,"Cox's Camp, 17 (Belle Plains Formation)",NA,"Locality 17 (Romer 1928), Wooderum's pasture, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""Cox's Camp (Cummins); Wooderum's pasture (Case). Exposures on the north side of the Little Wichita about opposite the mouth of Goodwin Creek."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee, approx. 7 mi north of locality.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 350 beet above the base of the Wichita."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present."" \nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 14:29,09/08/2011 14:21,28729,sp.,Eryops,7693,,290.1,279.3,Artinskian,,14,US,Eryops sp.
295943,occ,NA,,28143,,Aspidosaurus n. sp. glascocki,species,194932,,Aspidosaurus glascocki,NA,species,194932,Case,1910,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37021,NA,NA,NA,specimens,-98.901947,33.740276,"Cox's Camp, 17 (Belle Plains Formation)",NA,"Locality 17 (Romer 1928), Wooderum's pasture, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""Cox's Camp (Cummins); Wooderum's pasture (Case). Exposures on the north side of the Little Wichita about opposite the mouth of Goodwin Creek."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee, approx. 7 mi north of locality.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 350 beet above the base of the Wichita."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present."" \nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Aspidosaurus,,NA,NA,vertebrate,E. C. Case. 1910. New or little known reptiles and amphibians from the Permian (?) of Texas. Bulletin of the American Museum of Natural History 28:163-181,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 14:29,09/08/2011 14:23,28729,glascocki,Aspidosaurus,28729,n. sp.,290.1,279.3,Artinskian,,1,US,Aspidosaurus glascocki
295944,occ,NA,,28143,,Trimerorhachis n. sp. alleni,species,194933,subjective synonym of,Trimerorhachis insignis,NA,species,90711,Case,1910,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-98.901947,33.740276,"Cox's Camp, 17 (Belle Plains Formation)",NA,"Locality 17 (Romer 1928), Wooderum's pasture, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""Cox's Camp (Cummins); Wooderum's pasture (Case). Exposures on the north side of the Little Wichita about opposite the mouth of Goodwin Creek."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee, approx. 7 mi north of locality.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 350 beet above the base of the Wichita."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present."" \nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,E. C. Case. 1910. New or little known reptiles and amphibians from the Permian (?) of Texas. Bulletin of the American Museum of Natural History 28:163-181,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 14:29,09/08/2011 14:23,28729,alleni,Trimerorhachis,28729,n. sp.,290.1,279.3,Artinskian,,1,US,Trimerorhachis alleni
295945,occ,NA,,28143,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-98.901947,33.740276,"Cox's Camp, 17 (Belle Plains Formation)",NA,"Locality 17 (Romer 1928), Wooderum's pasture, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""Cox's Camp (Cummins); Wooderum's pasture (Case). Exposures on the north side of the Little Wichita about opposite the mouth of Goodwin Creek."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee, approx. 7 mi north of locality.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 350 beet above the base of the Wichita."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present."" \nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 14:29,09/08/2011 14:21,28729,sp.,Diadectes,7693,,290.1,279.3,Artinskian,,5,US,Diadectes sp.
295946,occ,NA,,28143,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-98.901947,33.740276,"Cox's Camp, 17 (Belle Plains Formation)",NA,"Locality 17 (Romer 1928), Wooderum's pasture, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""Cox's Camp (Cummins); Wooderum's pasture (Case). Exposures on the north side of the Little Wichita about opposite the mouth of Goodwin Creek."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee, approx. 7 mi north of locality.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 350 beet above the base of the Wichita."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present."" \nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 14:29,09/08/2011 14:21,28729,sp.,Dimetrodon,7693,,290.1,279.3,Artinskian,,6,US,Dimetrodon sp.
295947,occ,NA,,28144,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-99.022781,33.687222,"Head of Godwin Creek, 18 (Belle Plains Formation)",NA,"Locality 18 (Romer 1928), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""Specimens so labeled are from the exposures below the Beaverburk on the west side of the Godwin Creek Valley, near Dagget Creek, etc."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 5 mi north of locality.",gp_mid,-30.3,-1.05,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 14:32,07/02/2003 16:32,7693,sp.,Eryops,7693,,290.1,279.3,Artinskian,,6,US,Eryops sp.
295948,occ,NA,,28144,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-99.022781,33.687222,"Head of Godwin Creek, 18 (Belle Plains Formation)",NA,"Locality 18 (Romer 1928), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""Specimens so labeled are from the exposures below the Beaverburk on the west side of the Godwin Creek Valley, near Dagget Creek, etc."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 5 mi north of locality.",gp_mid,-30.3,-1.05,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 14:32,07/02/2003 16:32,7693,sp.,Dimetrodon,7693,,290.1,279.3,Artinskian,,3,US,Dimetrodon sp.
295949,occ,NA,,28145,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-99.022781,33.687222,"South of Fulda, 19 (Belle Plains)",NA,"Locality 19 (Romer 1928), Locality Vb (Romer & Price 1940), S. of Fulda, Hackberry Creek, North Side Little Wichita, South Side Little Wichita, North Side of Godwin Creek, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""Numerous exposures occur in the valley of the Little Wichita south and southeast of Fulda."" Specimens are labeled with various locality names, see aka above. See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 2 mi north of locality.",gp_mid,-30.3,-1.05,101,US,,Petrolia,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,Cope,1908,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 14:50,09/08/2011 14:25,28729,sp.,Eryops,7693,,290.1,279.3,Artinskian,,37,US,Eryops sp.
295950,occ,NA,,28145,,Trimerorhachis n. sp. medius,species,345365,subjective synonym of,Trimerorhachis insignis,NA,species,90711,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-99.022781,33.687222,"South of Fulda, 19 (Belle Plains)",NA,"Locality 19 (Romer 1928), Locality Vb (Romer & Price 1940), S. of Fulda, Hackberry Creek, North Side Little Wichita, South Side Little Wichita, North Side of Godwin Creek, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""Numerous exposures occur in the valley of the Little Wichita south and southeast of Fulda."" Specimens are labeled with various locality names, see aka above. See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 2 mi north of locality.",gp_mid,-30.3,-1.05,101,US,,Petrolia,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,Cope,1908,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 14:50,09/08/2011 14:25,28729,medius,Trimerorhachis,7693,n. sp.,290.1,279.3,Artinskian,,30,US,Trimerorhachis medius
295951,occ,NA,,28145,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-99.022781,33.687222,"South of Fulda, 19 (Belle Plains)",NA,"Locality 19 (Romer 1928), Locality Vb (Romer & Price 1940), S. of Fulda, Hackberry Creek, North Side Little Wichita, South Side Little Wichita, North Side of Godwin Creek, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""Numerous exposures occur in the valley of the Little Wichita south and southeast of Fulda."" Specimens are labeled with various locality names, see aka above. See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 2 mi north of locality.",gp_mid,-30.3,-1.05,101,US,,Petrolia,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,Cope,1908,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 14:50,09/08/2011 14:25,28729,sp.,Diadectes,7693,,290.1,279.3,Artinskian,,18,US,Diadectes sp.
295954,occ,NA,R,28145,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-99.022781,33.687222,"South of Fulda, 19 (Belle Plains)",NA,"Locality 19 (Romer 1928), Locality Vb (Romer & Price 1940), S. of Fulda, Hackberry Creek, North Side Little Wichita, South Side Little Wichita, North Side of Godwin Creek, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""Numerous exposures occur in the valley of the Little Wichita south and southeast of Fulda."" Specimens are labeled with various locality names, see aka above. See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 2 mi north of locality.",gp_mid,-30.3,-1.05,101,US,,Petrolia,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,Cope,1908,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,07/02/2003 14:50,18/07/2016 10:56,28729,sp.,Dimetrodon,7693,,290.1,279.3,Artinskian,,38,US,Dimetrodon sp.
295954,occ,27876,,28145,,Dimetrodon n. sp. booneorum,species,122783,,Dimetrodon booneorum,NA,species,122783,Romer,1937,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-99.022781,33.687222,"South of Fulda, 19 (Belle Plains)",NA,"Locality 19 (Romer 1928), Locality Vb (Romer & Price 1940), S. of Fulda, Hackberry Creek, North Side Little Wichita, South Side Little Wichita, North Side of Godwin Creek, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""Numerous exposures occur in the valley of the Little Wichita south and southeast of Fulda."" Specimens are labeled with various locality names, see aka above. See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 2 mi north of locality.",gp_mid,-30.3,-1.05,101,US,,Petrolia,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,Cope,1908,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1937. New genera and species of pelycosaurian reptiles. Proceedings of the New England Zo̦logical Club 16:89-95,14,14,0,M. Carrano,M. Carrano,,11/12/2012 07:46,10/12/2012 14:46,28729,booneorum,Dimetrodon,43845,n. sp.,290.1,279.3,Artinskian,,38,US,Dimetrodon booneorum
295955,occ,NA,,28145,,Edaphosaurus sp.,genus,38911,,Edaphosaurus,NA,genus,38911,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,specimens,-99.022781,33.687222,"South of Fulda, 19 (Belle Plains)",NA,"Locality 19 (Romer 1928), Locality Vb (Romer & Price 1940), S. of Fulda, Hackberry Creek, North Side Little Wichita, South Side Little Wichita, North Side of Godwin Creek, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""Numerous exposures occur in the valley of the Little Wichita south and southeast of Fulda."" Specimens are labeled with various locality names, see aka above. See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 2 mi north of locality.",gp_mid,-30.3,-1.05,101,US,,Petrolia,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,Cope,1908,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 14:50,09/08/2011 14:25,28729,sp.,Edaphosaurus,7693,,290.1,279.3,Artinskian,,4,US,Edaphosaurus sp.
295956,occ,NA,,28145,,n. gen. Therosaurus n. sp. watsoni,species,66597,subjective synonym of,Ophiacodon retroversus,NA,species,138048,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-99.022781,33.687222,"South of Fulda, 19 (Belle Plains)",NA,"Locality 19 (Romer 1928), Locality Vb (Romer & Price 1940), S. of Fulda, Hackberry Creek, North Side Little Wichita, South Side Little Wichita, North Side of Godwin Creek, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""Numerous exposures occur in the valley of the Little Wichita south and southeast of Fulda."" Specimens are labeled with various locality names, see aka above. See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 2 mi north of locality.",gp_mid,-30.3,-1.05,101,US,,Petrolia,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,Cope,1908,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Therosaurus,n. gen.,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 14:50,09/08/2011 14:25,28729,watsoni,Ophiacodon,7693,n. sp.,290.1,279.3,Artinskian,,1,US,Ophiacodon watsoni
295957,occ,NA,,28145,,n. gen. Tersomius n. sp. texensis,species,90713,,Tersomius texensis,NA,species,90713,Case,1910,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,37035,NA,NA,NA,specimens,-99.022781,33.687222,"South of Fulda, 19 (Belle Plains)",NA,"Locality 19 (Romer 1928), Locality Vb (Romer & Price 1940), S. of Fulda, Hackberry Creek, North Side Little Wichita, South Side Little Wichita, North Side of Godwin Creek, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""Numerous exposures occur in the valley of the Little Wichita south and southeast of Fulda."" Specimens are labeled with various locality names, see aka above. See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 2 mi north of locality.",gp_mid,-30.3,-1.05,101,US,,Petrolia,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,Cope,1908,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Tersomius,n. gen.,NA,NA,vertebrate,E. C. Case. 1910. New or little known reptiles and amphibians from the Permian (?) of Texas. Bulletin of the American Museum of Natural History 28:163-181,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 14:50,09/08/2011 14:25,28729,texensis,Tersomius,28729,n. sp.,290.1,279.3,Artinskian,,1,US,Tersomius texensis
295958,occ,NA,,28145,,Gymnarthrus willoughbyi,species,137382,subjective synonym of,Cardiocephalus sternbergi,NA,species,90715,Romer,1928,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37294,NA,NA,NA,specimens,-99.022781,33.687222,"South of Fulda, 19 (Belle Plains)",NA,"Locality 19 (Romer 1928), Locality Vb (Romer & Price 1940), S. of Fulda, Hackberry Creek, North Side Little Wichita, South Side Little Wichita, North Side of Godwin Creek, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""Numerous exposures occur in the valley of the Little Wichita south and southeast of Fulda."" Specimens are labeled with various locality names, see aka above. See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 2 mi north of locality.",gp_mid,-30.3,-1.05,101,US,,Petrolia,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,Cope,1908,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Gymnarthrus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 14:50,09/08/2011 14:25,28729,willoughbyi,Cardiocephalus,7693,,290.1,279.3,Artinskian,,1,US,Cardiocephalus willoughbyi
295959,occ,NA,,28146,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.901947,33.740276,"Slippery Creek, 20 (Belle Plains Formation)",NA,"Locality 20 (Romer 1928), Locality Vc (Romer & Price 1940), Lyle locality, Pearce locality, Young locality, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Slippery Creek is a tributary of the Little Wichita on the north side. Along it's course, nearly due south of Dundee, is a series of breaks. Lyle's, Pearce's, and Young's localities of Case were in this neighborhood."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee, approx. 4 mi due north of locality.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 14:56,10/12/2012 13:54,7693,sp.,Eryops,7693,,290.1,279.3,Artinskian,,10,US,Eryops sp.
295960,occ,NA,,28146,,Zatrachys sp.,genus,37056,,Zatrachys,NA,genus,37056,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,specimens,-98.901947,33.740276,"Slippery Creek, 20 (Belle Plains Formation)",NA,"Locality 20 (Romer 1928), Locality Vc (Romer & Price 1940), Lyle locality, Pearce locality, Young locality, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Slippery Creek is a tributary of the Little Wichita on the north side. Along it's course, nearly due south of Dundee, is a series of breaks. Lyle's, Pearce's, and Young's localities of Case were in this neighborhood."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee, approx. 4 mi due north of locality.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 14:56,10/12/2012 13:54,7693,sp.,Zatrachys,7693,,290.1,279.3,Artinskian,,1,US,Zatrachys sp.
295961,occ,NA,,28146,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-98.901947,33.740276,"Slippery Creek, 20 (Belle Plains Formation)",NA,"Locality 20 (Romer 1928), Locality Vc (Romer & Price 1940), Lyle locality, Pearce locality, Young locality, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Slippery Creek is a tributary of the Little Wichita on the north side. Along it's course, nearly due south of Dundee, is a series of breaks. Lyle's, Pearce's, and Young's localities of Case were in this neighborhood."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee, approx. 4 mi due north of locality.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 14:56,10/12/2012 13:54,7693,sp.,Trimerorhachis,7693,,290.1,279.3,Artinskian,,1,US,Trimerorhachis sp.
295962,occ,NA,,28146,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-98.901947,33.740276,"Slippery Creek, 20 (Belle Plains Formation)",NA,"Locality 20 (Romer 1928), Locality Vc (Romer & Price 1940), Lyle locality, Pearce locality, Young locality, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Slippery Creek is a tributary of the Little Wichita on the north side. Along it's course, nearly due south of Dundee, is a series of breaks. Lyle's, Pearce's, and Young's localities of Case were in this neighborhood."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee, approx. 4 mi due north of locality.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 14:56,10/12/2012 13:54,7693,sp.,Diadectes,7693,,290.1,279.3,Artinskian,,5,US,Diadectes sp.
295963,occ,NA,,28146,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-98.901947,33.740276,"Slippery Creek, 20 (Belle Plains Formation)",NA,"Locality 20 (Romer 1928), Locality Vc (Romer & Price 1940), Lyle locality, Pearce locality, Young locality, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Slippery Creek is a tributary of the Little Wichita on the north side. Along it's course, nearly due south of Dundee, is a series of breaks. Lyle's, Pearce's, and Young's localities of Case were in this neighborhood."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee, approx. 4 mi due north of locality.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 14:56,10/12/2012 13:54,7693,sp.,Dimetrodon,7693,,290.1,279.3,Artinskian,,4,US,Dimetrodon sp.
295964,occ,NA,,28238,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.901947,33.740276,"Tit Mountain, 21 (Belle Plains Formation)",NA,"Locality 21 (Romer 1928), Locality Vd (Romer & Price 1940), Corn Mountain, Corn Hill, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Tit Mountain or Corn Hill, an elevation just northeast of Dundee"" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 500 feet above the Coleman Junction."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Not the same as ""South side of Tit Mountain butte, TMM 40031"" locality (Langston 1986); that collection was obviously made much later than the Tit Mountain collection of Romer (1928), which has less detailed locality data.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 15:00,10/12/2012 14:28,26948,sp.,Eryops,7693,,290.1,279.3,Artinskian,,12,US,Eryops sp.
295965,occ,NA,,28238,,Aspidosaurus sp.,genus,37021,,Aspidosaurus,NA,genus,37021,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37021,NA,NA,NA,specimens,-98.901947,33.740276,"Tit Mountain, 21 (Belle Plains Formation)",NA,"Locality 21 (Romer 1928), Locality Vd (Romer & Price 1940), Corn Mountain, Corn Hill, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Tit Mountain or Corn Hill, an elevation just northeast of Dundee"" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 500 feet above the Coleman Junction."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Not the same as ""South side of Tit Mountain butte, TMM 40031"" locality (Langston 1986); that collection was obviously made much later than the Tit Mountain collection of Romer (1928), which has less detailed locality data.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Aspidosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 15:00,10/12/2012 14:28,26948,sp.,Aspidosaurus,7693,,290.1,279.3,Artinskian,,1,US,Aspidosaurus sp.
295966,occ,NA,,28238,,Trimerorhachis n. sp. bilobatus,species,309285,subjective synonym of,Trimerorhachis insignis,NA,species,90711,Cope,1883,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-98.901947,33.740276,"Tit Mountain, 21 (Belle Plains Formation)",NA,"Locality 21 (Romer 1928), Locality Vd (Romer & Price 1940), Corn Mountain, Corn Hill, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Tit Mountain or Corn Hill, an elevation just northeast of Dundee"" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 500 feet above the Coleman Junction."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Not the same as ""South side of Tit Mountain butte, TMM 40031"" locality (Langston 1986); that collection was obviously made much later than the Tit Mountain collection of Romer (1928), which has less detailed locality data.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,E. D. Cope. 1883. Fourth contribution to the history of the Permian formation of Texas. Paleontological Bulletin 36:628-636,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 15:00,13/11/2014 14:50,26948,bilobatus,Trimerorhachis,26948,n. sp.,290.1,279.3,Artinskian,,12,US,Trimerorhachis bilobatus
295967,occ,NA,,28238,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-98.901947,33.740276,"Tit Mountain, 21 (Belle Plains Formation)",NA,"Locality 21 (Romer 1928), Locality Vd (Romer & Price 1940), Corn Mountain, Corn Hill, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Tit Mountain or Corn Hill, an elevation just northeast of Dundee"" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 500 feet above the Coleman Junction."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Not the same as ""South side of Tit Mountain butte, TMM 40031"" locality (Langston 1986); that collection was obviously made much later than the Tit Mountain collection of Romer (1928), which has less detailed locality data.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 15:00,10/12/2012 14:28,26948,sp.,Diadectes,7693,,290.1,279.3,Artinskian,,NA,US,Diadectes sp.
295968,occ,NA,,28238,,Dimetrodon n. sp. longiramus,species,123422,subjective synonym of,Secodontosaurus obtusidens,NA,species,138129,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38908,NA,NA,NA,,-98.901947,33.740276,"Tit Mountain, 21 (Belle Plains Formation)",NA,"Locality 21 (Romer 1928), Locality Vd (Romer & Price 1940), Corn Mountain, Corn Hill, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Tit Mountain or Corn Hill, an elevation just northeast of Dundee"" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 500 feet above the Coleman Junction."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Not the same as ""South side of Tit Mountain butte, TMM 40031"" locality (Langston 1986); that collection was obviously made much later than the Tit Mountain collection of Romer (1928), which has less detailed locality data.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 15:00,10/12/2012 14:28,26948,longiramus,Secodontosaurus,7693,n. sp.,290.1,279.3,Artinskian,,NA,US,Secodontosaurus longiramus
295969,occ,NA,,28147,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.843887,33.867222,"Camp Creek, 22 (Belle Plains Formation)",NA,"Locality 22 (Romer 1928), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Camp Creek, 4 miles west of Tit Mountain."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Camp Creek.",gp_mid,-30.07,-0.98,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:04,07/02/2003 17:04,7693,sp.,Eryops,7693,,290.1,279.3,Artinskian,,1,US,Eryops sp.
295970,occ,NA,,28147,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-98.843887,33.867222,"Camp Creek, 22 (Belle Plains Formation)",NA,"Locality 22 (Romer 1928), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Camp Creek, 4 miles west of Tit Mountain."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Camp Creek.",gp_mid,-30.07,-0.98,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,4,J. Alroy,R. Whatley,J. Alroy,07/02/2003 15:04,17/12/2006 15:12,7693,sp.,Trimerorhachis,7693,,290.1,279.3,Artinskian,,1,US,Trimerorhachis sp.
295971,occ,NA,,28147,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-98.843887,33.867222,"Camp Creek, 22 (Belle Plains Formation)",NA,"Locality 22 (Romer 1928), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Camp Creek, 4 miles west of Tit Mountain."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Camp Creek.",gp_mid,-30.07,-0.98,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:04,07/02/2003 17:04,7693,sp.,Diadectes,7693,,290.1,279.3,Artinskian,,1,US,Diadectes sp.
295972,occ,NA,,28147,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-98.843887,33.867222,"Camp Creek, 22 (Belle Plains Formation)",NA,"Locality 22 (Romer 1928), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Camp Creek, 4 miles west of Tit Mountain."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Camp Creek.",gp_mid,-30.07,-0.98,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:04,07/02/2003 17:04,7693,sp.,Dimetrodon,7693,,290.1,279.3,Artinskian,,1,US,Dimetrodon sp.
295973,occ,NA,,28147,,Edaphosaurus sp.,genus,38911,,Edaphosaurus,NA,genus,38911,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,specimens,-98.843887,33.867222,"Camp Creek, 22 (Belle Plains Formation)",NA,"Locality 22 (Romer 1928), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Camp Creek, 4 miles west of Tit Mountain."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Camp Creek.",gp_mid,-30.07,-0.98,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:04,07/02/2003 17:04,7693,sp.,Edaphosaurus,7693,,290.1,279.3,Artinskian,,1,US,Edaphosaurus sp.
295974,occ,NA,,28148,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-99.022781,33.687222,"Big Wichita, Cummins, 23 (Belle Plains Formation)",NA,"Locality 23 (Romer 1928), Locality Ve (Romer & Price 1940), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 6 mi southwest of locality.",gp_mid,-30.3,-1.05,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""Just below the Beaverburk limestone... probable elevation above the Coleman Junction of about 525 feet."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 15:10,24/11/2014 13:58,28847,sp.,Eryops,7693,,290.1,279.3,Artinskian,,3,US,Eryops sp.
295975,occ,NA,,28148,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-99.022781,33.687222,"Big Wichita, Cummins, 23 (Belle Plains Formation)",NA,"Locality 23 (Romer 1928), Locality Ve (Romer & Price 1940), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 6 mi southwest of locality.",gp_mid,-30.3,-1.05,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""Just below the Beaverburk limestone... probable elevation above the Coleman Junction of about 525 feet."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 15:10,24/11/2014 13:58,28847,sp.,Diadectes,7693,,290.1,279.3,Artinskian,,1,US,Diadectes sp.
295976,occ,NA,,28148,,Varanosaurus sp.,genus,38933,,Varanosaurus,NA,genus,38933,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38933,NA,NA,NA,individuals,-99.022781,33.687222,"Big Wichita, Cummins, 23 (Belle Plains Formation)",NA,"Locality 23 (Romer 1928), Locality Ve (Romer & Price 1940), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 6 mi southwest of locality.",gp_mid,-30.3,-1.05,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""Just below the Beaverburk limestone... probable elevation above the Coleman Junction of about 525 feet."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Varanosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 15:10,24/11/2014 13:58,28847,sp.,Varanosaurus,7693,,290.1,279.3,Artinskian,,1,US,Varanosaurus sp.
295977,occ,NA,,28148,,Clepsydrops n. sp. leptocephalus,species,138056,subjective synonym of,Ophiacodon retroversus,NA,species,138048,Cope,1884,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-99.022781,33.687222,"Big Wichita, Cummins, 23 (Belle Plains Formation)",NA,"Locality 23 (Romer 1928), Locality Ve (Romer & Price 1940), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 6 mi southwest of locality.",gp_mid,-30.3,-1.05,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""Just below the Beaverburk limestone... probable elevation above the Coleman Junction of about 525 feet."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Clepsydrops,,NA,NA,vertebrate,E. D. Cope. 1884. Fifth contribution to the knowledge of the fauna of the Permian formation of Texas and the Indian Territory. Paleontological Bulletin 39:28-47,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 15:10,24/11/2014 13:58,28847,leptocephalus,Ophiacodon,28847,n. sp.,290.1,279.3,Artinskian,,1,US,Ophiacodon leptocephalus
295978,occ,NA,,28148,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-99.022781,33.687222,"Big Wichita, Cummins, 23 (Belle Plains Formation)",NA,"Locality 23 (Romer 1928), Locality Ve (Romer & Price 1940), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 6 mi southwest of locality.",gp_mid,-30.3,-1.05,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""Just below the Beaverburk limestone... probable elevation above the Coleman Junction of about 525 feet."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 15:10,24/11/2014 13:58,28847,sp.,Dimetrodon,7693,,290.1,279.3,Artinskian,,2,US,Dimetrodon sp.
295979,occ,NA,,28149,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.812225,33.891945,"Beaver Creek, 24 (Belle Plains Formation)",NA,"Locality 24 (Romer 1928), Locality Vf (Romer & Price 1940), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""A number of specimens collected by Boll are stated by Cummins to have been obtained near the mouth of Beaver Creek and hence in this zone; but it is not impossible that some specimens may have come from Zones 1 or 3."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Beaver Creek.",gp_mid,-30.04,-0.97,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:14,07/02/2003 17:14,7693,sp.,Eryops,7693,,290.1,279.3,Artinskian,,2,US,Eryops sp.
295980,occ,NA,,28149,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-98.812225,33.891945,"Beaver Creek, 24 (Belle Plains Formation)",NA,"Locality 24 (Romer 1928), Locality Vf (Romer & Price 1940), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""A number of specimens collected by Boll are stated by Cummins to have been obtained near the mouth of Beaver Creek and hence in this zone; but it is not impossible that some specimens may have come from Zones 1 or 3."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Beaver Creek.",gp_mid,-30.04,-0.97,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:14,07/02/2003 17:14,7693,sp.,Diadectes,7693,,290.1,279.3,Artinskian,,1,US,Diadectes sp.
295981,occ,NA,,28149,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-98.812225,33.891945,"Beaver Creek, 24 (Belle Plains Formation)",NA,"Locality 24 (Romer 1928), Locality Vf (Romer & Price 1940), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""A number of specimens collected by Boll are stated by Cummins to have been obtained near the mouth of Beaver Creek and hence in this zone; but it is not impossible that some specimens may have come from Zones 1 or 3."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Beaver Creek.",gp_mid,-30.04,-0.97,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:14,07/02/2003 17:14,7693,sp.,Ophiacodon,7693,,290.1,279.3,Artinskian,,1,US,Ophiacodon sp.
295982,occ,NA,,28149,,Dimetrodon obtusidens,species,138130,recombined as,Secodontosaurus obtusidens,NA,species,138129,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38908,NA,NA,NA,specimens,-98.812225,33.891945,"Beaver Creek, 24 (Belle Plains Formation)",NA,"Locality 24 (Romer 1928), Locality Vf (Romer & Price 1940), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""A number of specimens collected by Boll are stated by Cummins to have been obtained near the mouth of Beaver Creek and hence in this zone; but it is not impossible that some specimens may have come from Zones 1 or 3."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Beaver Creek.",gp_mid,-30.04,-0.97,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:14,07/02/2003 17:14,7693,obtusidens,Secodontosaurus,7693,,290.1,279.3,Artinskian,,1,US,Secodontosaurus obtusidens
295983,occ,NA,,28149,,Edaphosaurus microdus,species,138136,,Edaphosaurus microdus,NA,species,138136,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,,-98.812225,33.891945,"Beaver Creek, 24 (Belle Plains Formation)",NA,"Locality 24 (Romer 1928), Locality Vf (Romer & Price 1940), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""A number of specimens collected by Boll are stated by Cummins to have been obtained near the mouth of Beaver Creek and hence in this zone; but it is not impossible that some specimens may have come from Zones 1 or 3."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Beaver Creek.",gp_mid,-30.04,-0.97,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, which is well above the Coleman Junction and whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:14,07/02/2003 17:14,7693,microdus,Edaphosaurus,7693,,290.1,279.3,Artinskian,,NA,US,Edaphosaurus microdus
295984,occ,NA,,28238,,Clepsydrops n. sp. macrospondylus,species,138122,recombined as,Dimetrodon macrospondylus,NA,species,138122,Cope,1884,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-98.901947,33.740276,"Tit Mountain, 21 (Belle Plains Formation)",NA,"Locality 21 (Romer 1928), Locality Vd (Romer & Price 1940), Corn Mountain, Corn Hill, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Tit Mountain or Corn Hill, an elevation just northeast of Dundee"" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 500 feet above the Coleman Junction."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Not the same as ""South side of Tit Mountain butte, TMM 40031"" locality (Langston 1986); that collection was obviously made much later than the Tit Mountain collection of Romer (1928), which has less detailed locality data.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Clepsydrops,,NA,NA,vertebrate,E. D. Cope. 1884. Fifth contribution to the knowledge of the fauna of the Permian formation of Texas and the Indian Territory. Paleontological Bulletin 39:28-47,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 15:16,24/11/2014 13:59,26948,macrospondylus,Dimetrodon,28847,n. sp.,290.1,279.3,Artinskian,,1,US,Dimetrodon macrospondylus
295985,occ,NA,,28249,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-99.022781,33.687222,"Northeast of Fulda, 26 (Waggoner Ranch Formation)",NA,"Locality 26 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,,based on nearby landmark,seconds,local area,"""lower portion of this [limestone] series northeast of Fulda."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Fulda. Numbered ""26"" with taxonomic list and on map, but is incorrectly numbered ""25"" in text.",gp_mid,-30.27,-1,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet.""\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:18,07/02/2003 17:18,7693,sp.,Ophiacodon,7693,,290.1,272.3,Artinskian,Kungurian,1,US,Ophiacodon sp.
295986,occ,NA,,28249,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-99.022781,33.687222,"Northeast of Fulda, 26 (Waggoner Ranch Formation)",NA,"Locality 26 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,,based on nearby landmark,seconds,local area,"""lower portion of this [limestone] series northeast of Fulda."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Fulda. Numbered ""26"" with taxonomic list and on map, but is incorrectly numbered ""25"" in text.",gp_mid,-30.27,-1,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet.""\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:18,07/02/2003 17:18,7693,sp.,Dimetrodon,7693,,290.1,272.3,Artinskian,Kungurian,1,US,Dimetrodon sp.
295987,occ,NA,,28241,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.694725,33.816113,"Bluff Bonebed of Udden, 27 (Waggoner Ranch Formation)",NA,"Locality 27 (Romer 1928), Clyde Formation, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Udden",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"Description says this locality is in ""western Wichita County"" but it is not shown on the locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Holliday in Archer County. Numbered ""27"" with taxonomic list, but is incorrectly numbered ""26"" in text.",gp_mid,-29.97,-1.03,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""65 feet above the Beaverburk"" Limestone. Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,some macrofossils,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Invertebrates and plants are present at this locality.,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:20,07/02/2003 17:20,7693,sp.,Eryops,7693,,290.1,272.3,Artinskian,Kungurian,3,US,Eryops sp.
295988,occ,NA,,28241,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-98.694725,33.816113,"Bluff Bonebed of Udden, 27 (Waggoner Ranch Formation)",NA,"Locality 27 (Romer 1928), Clyde Formation, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Udden",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"Description says this locality is in ""western Wichita County"" but it is not shown on the locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Holliday in Archer County. Numbered ""27"" with taxonomic list, but is incorrectly numbered ""26"" in text.",gp_mid,-29.97,-1.03,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""65 feet above the Beaverburk"" Limestone. Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,some macrofossils,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Invertebrates and plants are present at this locality.,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,4,J. Alroy,R. Whatley,J. Alroy,07/02/2003 15:20,17/12/2006 15:12,7693,sp.,Trimerorhachis,7693,,290.1,272.3,Artinskian,Kungurian,2,US,Trimerorhachis sp.
295989,occ,NA,,28241,,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,specimens,-98.694725,33.816113,"Bluff Bonebed of Udden, 27 (Waggoner Ranch Formation)",NA,"Locality 27 (Romer 1928), Clyde Formation, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Udden",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"Description says this locality is in ""western Wichita County"" but it is not shown on the locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Holliday in Archer County. Numbered ""27"" with taxonomic list, but is incorrectly numbered ""26"" in text.",gp_mid,-29.97,-1.03,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""65 feet above the Beaverburk"" Limestone. Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,some macrofossils,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Invertebrates and plants are present at this locality.,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:20,07/02/2003 17:20,7693,sp.,Diplocaulus,7693,,290.1,272.3,Artinskian,Kungurian,4,US,Diplocaulus sp.
295990,occ,NA,,28241,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-98.694725,33.816113,"Bluff Bonebed of Udden, 27 (Waggoner Ranch Formation)",NA,"Locality 27 (Romer 1928), Clyde Formation, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Udden",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"Description says this locality is in ""western Wichita County"" but it is not shown on the locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Holliday in Archer County. Numbered ""27"" with taxonomic list, but is incorrectly numbered ""26"" in text.",gp_mid,-29.97,-1.03,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""65 feet above the Beaverburk"" Limestone. Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,some macrofossils,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Invertebrates and plants are present at this locality.,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:20,07/02/2003 17:20,7693,sp.,Diadectes,7693,,290.1,272.3,Artinskian,Kungurian,2,US,Diadectes sp.
295991,occ,NA,,28241,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-98.694725,33.816113,"Bluff Bonebed of Udden, 27 (Waggoner Ranch Formation)",NA,"Locality 27 (Romer 1928), Clyde Formation, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Udden",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"Description says this locality is in ""western Wichita County"" but it is not shown on the locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Holliday in Archer County. Numbered ""27"" with taxonomic list, but is incorrectly numbered ""26"" in text.",gp_mid,-29.97,-1.03,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""65 feet above the Beaverburk"" Limestone. Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,some macrofossils,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Invertebrates and plants are present at this locality.,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:20,07/02/2003 17:20,7693,sp.,Ophiacodon,7693,,290.1,272.3,Artinskian,Kungurian,5,US,Ophiacodon sp.
295992,occ,NA,,28241,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-98.694725,33.816113,"Bluff Bonebed of Udden, 27 (Waggoner Ranch Formation)",NA,"Locality 27 (Romer 1928), Clyde Formation, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Udden",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"Description says this locality is in ""western Wichita County"" but it is not shown on the locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Holliday in Archer County. Numbered ""27"" with taxonomic list, but is incorrectly numbered ""26"" in text.",gp_mid,-29.97,-1.03,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""65 feet above the Beaverburk"" Limestone. Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,some macrofossils,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Invertebrates and plants are present at this locality.,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:20,07/02/2003 17:20,7693,sp.,Dimetrodon,7693,,290.1,272.3,Artinskian,Kungurian,2,US,Dimetrodon sp.
295993,occ,NA,,28242,,n. gen. Broiliellus n. sp. texensis,species,255228,,Broiliellus texensis,NA,species,255228,Williston,1914,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37024,NA,NA,NA,,-99.022781,33.687222,"Coal Creek, 28 (Waggoner Ranch Formation)",NA,"Locality 28 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near the mouth of this creek southeast of Maybelle."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Fulda. Numbered ""28"" with taxonomic list and on map, but is incorrectly numbered ""27"" in text. Listed as Miller Creek in Williston 1915.",gp_mid,-30.27,-1,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""about 100 feet above the Beaverburk"" Limestone. Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Broiliellus,n. gen.,NA,NA,vertebrate,"S. W. Williston. 1914. Broiliellus, a new genus of amphibians from the Permian of Texas. Journal of Geology 22:49-56",4,76,697,J. Alroy,R. Whatley,E. Dunne,07/02/2003 15:23,04/07/2016 06:33,42447,texensis,Broiliellus,59696,n. sp.,290.1,272.3,Artinskian,Kungurian,NA,US,Broiliellus texensis
295994,occ,NA,,28242,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-99.022781,33.687222,"Coal Creek, 28 (Waggoner Ranch Formation)",NA,"Locality 28 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near the mouth of this creek southeast of Maybelle."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Fulda. Numbered ""28"" with taxonomic list and on map, but is incorrectly numbered ""27"" in text. Listed as Miller Creek in Williston 1915.",gp_mid,-30.27,-1,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""about 100 feet above the Beaverburk"" Limestone. Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 15:23,25/07/2012 14:08,42447,sp.,Dimetrodon,7693,,290.1,272.3,Artinskian,Kungurian,1,US,Dimetrodon sp.
295995,occ,NA,,28250,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,individuals,-99.091667,33.733334,"Mitchell Creek, 29 (Waggoner Ranch Formation)",NA,"Locality 29 (Romer 1928), old Bar X pasture, Timber Creek, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Lucas Ranch",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near Mitchell and Timber Creeks, northeast of Maybelle in the old Bar X pasture."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"". Numbered ""29"" with taxonomic list and on map, but is incorrectly numbered ""28"" in text. Lat long is for area enclosed by Mitchell Creek (W), Big Wichita River (N), Timber Creek (E), and U.S. 277 (S).",gp_mid,-30.29,-0.93,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""It is about 150 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 15:30,11/06/2009 05:56,7693,sp.,Eryops,7693,,290.1,272.3,Artinskian,Kungurian,1,US,Eryops sp.
295996,occ,NA,,28250,,Broiliellus sp.,genus,37024,,Broiliellus,NA,genus,37024,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37024,NA,NA,NA,specimens,-99.091667,33.733334,"Mitchell Creek, 29 (Waggoner Ranch Formation)",NA,"Locality 29 (Romer 1928), old Bar X pasture, Timber Creek, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Lucas Ranch",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near Mitchell and Timber Creeks, northeast of Maybelle in the old Bar X pasture."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"". Numbered ""29"" with taxonomic list and on map, but is incorrectly numbered ""28"" in text. Lat long is for area enclosed by Mitchell Creek (W), Big Wichita River (N), Timber Creek (E), and U.S. 277 (S).",gp_mid,-30.29,-0.93,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""It is about 150 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Broiliellus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 15:30,11/06/2009 05:56,7693,sp.,Broiliellus,7693,,290.1,272.3,Artinskian,Kungurian,2,US,Broiliellus sp.
295997,occ,NA,,28250,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-99.091667,33.733334,"Mitchell Creek, 29 (Waggoner Ranch Formation)",NA,"Locality 29 (Romer 1928), old Bar X pasture, Timber Creek, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Lucas Ranch",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near Mitchell and Timber Creeks, northeast of Maybelle in the old Bar X pasture."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"". Numbered ""29"" with taxonomic list and on map, but is incorrectly numbered ""28"" in text. Lat long is for area enclosed by Mitchell Creek (W), Big Wichita River (N), Timber Creek (E), and U.S. 277 (S).",gp_mid,-30.29,-0.93,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""It is about 150 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 15:30,11/06/2009 05:56,7693,sp.,Trimerorhachis,7693,,290.1,272.3,Artinskian,Kungurian,3,US,Trimerorhachis sp.
295998,occ,NA,,28250,,Captorhinus sp.,genus,37497,,Captorhinus,NA,genus,37497,Romer,1928,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-99.091667,33.733334,"Mitchell Creek, 29 (Waggoner Ranch Formation)",NA,"Locality 29 (Romer 1928), old Bar X pasture, Timber Creek, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Lucas Ranch",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near Mitchell and Timber Creeks, northeast of Maybelle in the old Bar X pasture."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"". Numbered ""29"" with taxonomic list and on map, but is incorrectly numbered ""28"" in text. Lat long is for area enclosed by Mitchell Creek (W), Big Wichita River (N), Timber Creek (E), and U.S. 277 (S).",gp_mid,-30.29,-0.93,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""It is about 150 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 15:30,11/06/2009 05:56,7693,sp.,Captorhinus,7693,,290.1,272.3,Artinskian,Kungurian,1,US,Captorhinus sp.
295999,occ,NA,R,28250,,Labidosaurus sp.,genus,37501,,Labidosaurus,NA,genus,37501,Romer,1928,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,individuals,-99.091667,33.733334,"Mitchell Creek, 29 (Waggoner Ranch Formation)",NA,"Locality 29 (Romer 1928), old Bar X pasture, Timber Creek, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Lucas Ranch",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near Mitchell and Timber Creeks, northeast of Maybelle in the old Bar X pasture."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"". Numbered ""29"" with taxonomic list and on map, but is incorrectly numbered ""28"" in text. Lat long is for area enclosed by Mitchell Creek (W), Big Wichita River (N), Timber Creek (E), and U.S. 277 (S).",gp_mid,-30.29,-0.93,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""It is about 150 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,07/02/2003 15:30,24/08/2016 05:24,7693,sp.,Labidosaurus,7693,,290.1,272.3,Artinskian,Kungurian,1,US,Labidosaurus sp.
295999,occ,21135,R,28250,,Labidosaurus hamatus,species,134918,,Labidosaurus hamatus,NA,species,134856,Seltin,1959,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,individuals,-99.091667,33.733334,"Mitchell Creek, 29 (Waggoner Ranch Formation)",NA,"Locality 29 (Romer 1928), old Bar X pasture, Timber Creek, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Lucas Ranch",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near Mitchell and Timber Creeks, northeast of Maybelle in the old Bar X pasture."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"". Numbered ""29"" with taxonomic list and on map, but is incorrectly numbered ""28"" in text. Lat long is for area enclosed by Mitchell Creek (W), Big Wichita River (N), Timber Creek (E), and U.S. 277 (S).",gp_mid,-30.29,-0.93,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""It is about 150 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,vertebrate,R. J. Seltin. 1959. A review of the family Captorhinidae. Fieldiana: Geology 10(34):461-509,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,30/11/2008 18:07,01/12/2008 09:05,7693,hamatus,Labidosaurus,28359,,290.1,272.3,Artinskian,Kungurian,1,US,Labidosaurus hamatus
295999,occ,25942,,28250,,n. gen. Reiszorhinus n. sp. olsoni,species,204031,,Reiszorhinus olsoni,NA,species,204031,Sumida et al.,2010,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,204025,NA,NA,NA,individuals,-99.091667,33.733334,"Mitchell Creek, 29 (Waggoner Ranch Formation)",NA,"Locality 29 (Romer 1928), old Bar X pasture, Timber Creek, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Lucas Ranch",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near Mitchell and Timber Creeks, northeast of Maybelle in the old Bar X pasture."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"". Numbered ""29"" with taxonomic list and on map, but is incorrectly numbered ""28"" in text. Lat long is for area enclosed by Mitchell Creek (W), Big Wichita River (N), Timber Creek (E), and U.S. 277 (S).",gp_mid,-30.29,-0.93,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""It is about 150 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Reiszorhinus,n. gen.,NA,NA,vertebrate,"S. S. Sumida, J. Dodick, and A. Metcalf, G. Albright. 2010. Reiszorhinus olsoni, a New Single-Tooth-Rowed Captorhinid Reptile from the Lower Permian of Texas. Journal of Vertebrate Paleontology 30(3):704-714",315,334,0,J. Mueller,T. Liebrecht,,24/10/2011 23:52,24/10/2011 07:52,7693,olsoni,Reiszorhinus,38301,n. sp.,290.1,272.3,Artinskian,Kungurian,1,US,Reiszorhinus olsoni
296001,occ,NA,R,28250,,Varanosaurus sp.,genus,38933,,Varanosaurus,NA,genus,38933,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38933,NA,NA,NA,individuals,-99.091667,33.733334,"Mitchell Creek, 29 (Waggoner Ranch Formation)",NA,"Locality 29 (Romer 1928), old Bar X pasture, Timber Creek, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Lucas Ranch",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near Mitchell and Timber Creeks, northeast of Maybelle in the old Bar X pasture."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"". Numbered ""29"" with taxonomic list and on map, but is incorrectly numbered ""28"" in text. Lat long is for area enclosed by Mitchell Creek (W), Big Wichita River (N), Timber Creek (E), and U.S. 277 (S).",gp_mid,-30.29,-0.93,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""It is about 150 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Varanosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,07/02/2003 15:30,24/08/2016 05:24,7693,sp.,Varanosaurus,7693,,290.1,272.3,Artinskian,Kungurian,1,US,Varanosaurus sp.
296001,occ,21218,,28250,,Varanosaurus wichitaensis,species,139019,,Varanosaurus wichitaensis,NA,species,139019,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38933,NA,NA,NA,individuals,-99.091667,33.733334,"Mitchell Creek, 29 (Waggoner Ranch Formation)",NA,"Locality 29 (Romer 1928), old Bar X pasture, Timber Creek, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Lucas Ranch",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near Mitchell and Timber Creeks, northeast of Maybelle in the old Bar X pasture."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"". Numbered ""29"" with taxonomic list and on map, but is incorrectly numbered ""28"" in text. Lat long is for area enclosed by Mitchell Creek (W), Big Wichita River (N), Timber Creek (E), and U.S. 277 (S).",gp_mid,-30.29,-0.93,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""It is about 150 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Varanosaurus,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,0,J. Mueller,T. Liebrecht,,10/01/2009 12:13,10/01/2009 14:13,7693,wichitaensis,Varanosaurus,5692,,290.1,272.3,Artinskian,Kungurian,1,US,Varanosaurus wichitaensis
296002,occ,NA,,28250,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-99.091667,33.733334,"Mitchell Creek, 29 (Waggoner Ranch Formation)",NA,"Locality 29 (Romer 1928), old Bar X pasture, Timber Creek, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Lucas Ranch",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near Mitchell and Timber Creeks, northeast of Maybelle in the old Bar X pasture."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"". Numbered ""29"" with taxonomic list and on map, but is incorrectly numbered ""28"" in text. Lat long is for area enclosed by Mitchell Creek (W), Big Wichita River (N), Timber Creek (E), and U.S. 277 (S).",gp_mid,-30.29,-0.93,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""It is about 150 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 15:30,11/06/2009 05:56,7693,sp.,Ophiacodon,7693,,290.1,272.3,Artinskian,Kungurian,2,US,Ophiacodon sp.
296003,occ,NA,,28250,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-99.091667,33.733334,"Mitchell Creek, 29 (Waggoner Ranch Formation)",NA,"Locality 29 (Romer 1928), old Bar X pasture, Timber Creek, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Lucas Ranch",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near Mitchell and Timber Creeks, northeast of Maybelle in the old Bar X pasture."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"". Numbered ""29"" with taxonomic list and on map, but is incorrectly numbered ""28"" in text. Lat long is for area enclosed by Mitchell Creek (W), Big Wichita River (N), Timber Creek (E), and U.S. 277 (S).",gp_mid,-30.29,-0.93,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""It is about 150 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 15:30,11/06/2009 05:56,7693,sp.,Dimetrodon,7693,,290.1,272.3,Artinskian,Kungurian,2,US,Dimetrodon sp.
296004,occ,NA,,28242,,n. gen. Glaucosaurus n. sp. megalops,species,123517,,Glaucosaurus megalops,NA,species,123517,Williston,1915,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38925,NA,NA,NA,specimens,-99.022781,33.687222,"Coal Creek, 28 (Waggoner Ranch Formation)",NA,"Locality 28 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near the mouth of this creek southeast of Maybelle."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Fulda. Numbered ""28"" with taxonomic list and on map, but is incorrectly numbered ""27"" in text. Listed as Miller Creek in Williston 1915.",gp_mid,-30.27,-1,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""about 100 feet above the Beaverburk"" Limestone. Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Glaucosaurus,n. gen.,NA,NA,vertebrate,"S. W. Williston. 1915. New genera of Permian reptiles. The American Journal of Science, series 4 39(233):575-579",4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 15:33,25/07/2012 14:08,42447,megalops,Glaucosaurus,42447,n. sp.,290.1,272.3,Artinskian,Kungurian,1,US,Glaucosaurus megalops
296006,occ,NA,,28251,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-99.144997,33.755001,"Whiskey Creek, 30 (Waggoner Ranch Formation)",NA,"Locality 30 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor/Wilbarger,based on nearby landmark,seconds,local area,"""On the north side of the Big Wichita, not far below the Leauders"" Limestone. See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Lake Kemp dam. Numbered ""30"" with taxonomic list and on map, but is incorrectly numbered ""29"" in text.",gp_mid,-28.88,1.73,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""not far below the Leauders [Limestone]; about 200 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet.""\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:35,07/02/2003 17:35,7693,sp.,Eryops,7693,,279.3,272.3,Kungurian,,2,US,Eryops sp.
296007,occ,NA,,28251,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-99.144997,33.755001,"Whiskey Creek, 30 (Waggoner Ranch Formation)",NA,"Locality 30 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor/Wilbarger,based on nearby landmark,seconds,local area,"""On the north side of the Big Wichita, not far below the Leauders"" Limestone. See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Lake Kemp dam. Numbered ""30"" with taxonomic list and on map, but is incorrectly numbered ""29"" in text.",gp_mid,-28.88,1.73,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""not far below the Leauders [Limestone]; about 200 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet.""\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,4,J. Alroy,R. Whatley,J. Alroy,07/02/2003 15:35,17/12/2006 15:12,7693,sp.,Trimerorhachis,7693,,279.3,272.3,Kungurian,,1,US,Trimerorhachis sp.
296008,occ,NA,R,28251,,Labidosaurus sp.,genus,37501,,Labidosaurus,NA,genus,37501,Romer,1928,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,specimens,-99.144997,33.755001,"Whiskey Creek, 30 (Waggoner Ranch Formation)",NA,"Locality 30 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor/Wilbarger,based on nearby landmark,seconds,local area,"""On the north side of the Big Wichita, not far below the Leauders"" Limestone. See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Lake Kemp dam. Numbered ""30"" with taxonomic list and on map, but is incorrectly numbered ""29"" in text.",gp_mid,-28.88,1.73,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""not far below the Leauders [Limestone]; about 200 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet.""\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:35,07/02/2003 17:35,7693,sp.,Labidosaurus,7693,,279.3,272.3,Kungurian,,1,US,Labidosaurus sp.
296008,occ,21191,,28251,,Labidosaurus hamatus,species,134918,,Labidosaurus hamatus,NA,species,134856,Fox and Bowman,1966,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,specimens,-99.144997,33.755001,"Whiskey Creek, 30 (Waggoner Ranch Formation)",NA,"Locality 30 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor/Wilbarger,based on nearby landmark,seconds,local area,"""On the north side of the Big Wichita, not far below the Leauders"" Limestone. See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Lake Kemp dam. Numbered ""30"" with taxonomic list and on map, but is incorrectly numbered ""29"" in text.",gp_mid,-28.88,1.73,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""not far below the Leauders [Limestone]; about 200 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet.""\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,vertebrate,"R. C. Fox and M. C. Bowman. 1966. Osteology and Relationships of Captorhinus aguti (Cope) (Reptilia: Captorhinomorpha). The University of Kansas Paleontological Contributions, Series Vertebrata 11:1-79",315,334,0,J. Mueller,T. Liebrecht,,16/12/2008 07:26,16/12/2008 09:26,7693,hamatus,Labidosaurus,28784,,279.3,272.3,Kungurian,,1,US,Labidosaurus hamatus
296009,occ,NA,,28251,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-99.144997,33.755001,"Whiskey Creek, 30 (Waggoner Ranch Formation)",NA,"Locality 30 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor/Wilbarger,based on nearby landmark,seconds,local area,"""On the north side of the Big Wichita, not far below the Leauders"" Limestone. See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Lake Kemp dam. Numbered ""30"" with taxonomic list and on map, but is incorrectly numbered ""29"" in text.",gp_mid,-28.88,1.73,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""not far below the Leauders [Limestone]; about 200 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet.""\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:35,07/02/2003 17:35,7693,sp.,Dimetrodon,7693,,279.3,272.3,Kungurian,,1,US,Dimetrodon sp.
296010,occ,NA,,28251,,Chilonyx rapidens,species,120984,subjective synonym of,Diadectes sideropelicus,NA,species,320982,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-99.144997,33.755001,"Whiskey Creek, 30 (Waggoner Ranch Formation)",NA,"Locality 30 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor/Wilbarger,based on nearby landmark,seconds,local area,"""On the north side of the Big Wichita, not far below the Leauders"" Limestone. See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Lake Kemp dam. Numbered ""30"" with taxonomic list and on map, but is incorrectly numbered ""29"" in text.",gp_mid,-28.88,1.73,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""not far below the Leauders [Limestone]; about 200 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet.""\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Chilonyx,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:35,07/02/2003 17:35,7693,rapidens,Diadectes,7693,,279.3,272.3,Kungurian,,NA,US,Diadectes rapidens
296011,occ,NA,,28252,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-99.144997,33.755001,"Moonshine Creek, 31 (Waggoner Ranch Formation)",NA,"Locality 31 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""On the south side [of the Big Wichita], farther west.."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Lake Kemp dam. Numbered ""31"" with taxonomic list and on map, but is incorrectly numbered ""30"" in text.",gp_mid,-30.32,-0.89,101,US,,Waggoner Ranch,,,group of beds,,,,,,,NA,"About 150 feet above the Beaverburk. Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:41,07/02/2003 17:41,7693,sp.,Eryops,7693,,290.1,272.3,Artinskian,Kungurian,2,US,Eryops sp.
296012,occ,NA,,28252,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-99.144997,33.755001,"Moonshine Creek, 31 (Waggoner Ranch Formation)",NA,"Locality 31 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""On the south side [of the Big Wichita], farther west.."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Lake Kemp dam. Numbered ""31"" with taxonomic list and on map, but is incorrectly numbered ""30"" in text.",gp_mid,-30.32,-0.89,101,US,,Waggoner Ranch,,,group of beds,,,,,,,NA,"About 150 feet above the Beaverburk. Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:41,07/02/2003 17:41,7693,sp.,Diadectes,7693,,290.1,272.3,Artinskian,Kungurian,1,US,Diadectes sp.
296013,occ,NA,,28252,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-99.144997,33.755001,"Moonshine Creek, 31 (Waggoner Ranch Formation)",NA,"Locality 31 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""On the south side [of the Big Wichita], farther west.."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Lake Kemp dam. Numbered ""31"" with taxonomic list and on map, but is incorrectly numbered ""30"" in text.",gp_mid,-30.32,-0.89,101,US,,Waggoner Ranch,,,group of beds,,,,,,,NA,"About 150 feet above the Beaverburk. Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:41,07/02/2003 17:41,7693,sp.,Ophiacodon,7693,,290.1,272.3,Artinskian,Kungurian,1,US,Ophiacodon sp.
296014,occ,NA,,28252,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-99.144997,33.755001,"Moonshine Creek, 31 (Waggoner Ranch Formation)",NA,"Locality 31 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""On the south side [of the Big Wichita], farther west.."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Lake Kemp dam. Numbered ""31"" with taxonomic list and on map, but is incorrectly numbered ""30"" in text.",gp_mid,-30.32,-0.89,101,US,,Waggoner Ranch,,,group of beds,,,,,,,NA,"About 150 feet above the Beaverburk. Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:41,07/02/2003 17:41,7693,sp.,Dimetrodon,7693,,290.1,272.3,Artinskian,Kungurian,4,US,Dimetrodon sp.
296015,occ,NA,,28253,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-99.144997,33.755001,"Military Trail, 32 (Waggoner Ranch Formation)",NA,"Locality 32 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""This trail crossed the Big Wichita about a mile east of the present Kemp Lake dam. South of this it ran in Zone 3, and the same is true for several miles to the north; but while the finds are probably in this zone, the exact horizon cannot be stated."" The length of the trail is relatively well-constrained at about 2 - 3 miles. See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Kemp Lake dam. Numbered ""32"" with taxonomic list, but is incorrectly numbered ""31"" in text.",gp_mid,-30.32,-0.89,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,claystone,"red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:49,07/02/2003 17:49,7693,sp.,Eryops,7693,,290.1,272.3,Artinskian,Kungurian,1,US,Eryops sp.
296016,occ,NA,,28253,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-99.144997,33.755001,"Military Trail, 32 (Waggoner Ranch Formation)",NA,"Locality 32 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""This trail crossed the Big Wichita about a mile east of the present Kemp Lake dam. South of this it ran in Zone 3, and the same is true for several miles to the north; but while the finds are probably in this zone, the exact horizon cannot be stated."" The length of the trail is relatively well-constrained at about 2 - 3 miles. See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Kemp Lake dam. Numbered ""32"" with taxonomic list, but is incorrectly numbered ""31"" in text.",gp_mid,-30.32,-0.89,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,claystone,"red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:49,07/02/2003 17:49,7693,sp.,Diadectes,7693,,290.1,272.3,Artinskian,Kungurian,2,US,Diadectes sp.
296018,occ,NA,,28253,,n. gen. Helodectes n. sp. paridens,species,320978,subjective synonym of,Diadectes sideropelicus,NA,species,320982,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-99.144997,33.755001,"Military Trail, 32 (Waggoner Ranch Formation)",NA,"Locality 32 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""This trail crossed the Big Wichita about a mile east of the present Kemp Lake dam. South of this it ran in Zone 3, and the same is true for several miles to the north; but while the finds are probably in this zone, the exact horizon cannot be stated."" The length of the trail is relatively well-constrained at about 2 - 3 miles. See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Kemp Lake dam. Numbered ""32"" with taxonomic list, but is incorrectly numbered ""31"" in text.",gp_mid,-30.32,-0.89,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,claystone,"red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Helodectes,n. gen.,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,76,J. Alroy,R. Whatley,R. Whatley,07/02/2003 15:49,09/02/2003 16:49,7693,paridens,Diadectes,7693,n. sp.,290.1,272.3,Artinskian,Kungurian,1,US,Diadectes paridens
296019,occ,NA,,28253,,Helodectes n. sp. isaaci,species,320977,subjective synonym of,Diadectes sideropelicus,NA,species,320982,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-99.144997,33.755001,"Military Trail, 32 (Waggoner Ranch Formation)",NA,"Locality 32 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""This trail crossed the Big Wichita about a mile east of the present Kemp Lake dam. South of this it ran in Zone 3, and the same is true for several miles to the north; but while the finds are probably in this zone, the exact horizon cannot be stated."" The length of the trail is relatively well-constrained at about 2 - 3 miles. See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Kemp Lake dam. Numbered ""32"" with taxonomic list, but is incorrectly numbered ""31"" in text.",gp_mid,-30.32,-0.89,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,claystone,"red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Helodectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:49,07/02/2003 17:49,7693,isaaci,Diadectes,7693,n. sp.,290.1,272.3,Artinskian,Kungurian,NA,US,Diadectes isaaci
296020,occ,NA,R,28253,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,elements,-99.144997,33.755001,"Military Trail, 32 (Waggoner Ranch Formation)",NA,"Locality 32 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""This trail crossed the Big Wichita about a mile east of the present Kemp Lake dam. South of this it ran in Zone 3, and the same is true for several miles to the north; but while the finds are probably in this zone, the exact horizon cannot be stated."" The length of the trail is relatively well-constrained at about 2 - 3 miles. See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Kemp Lake dam. Numbered ""32"" with taxonomic list, but is incorrectly numbered ""31"" in text.",gp_mid,-30.32,-0.89,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,claystone,"red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 15:49,14/01/2009 04:14,7693,sp.,Ophiacodon,7693,,290.1,272.3,Artinskian,Kungurian,1,US,Ophiacodon sp.
296020,occ,21226,,28253,,Ophiacodon major,species,122336,,Ophiacodon major,NA,species,122336,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,elements,-99.144997,33.755001,"Military Trail, 32 (Waggoner Ranch Formation)",NA,"Locality 32 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""This trail crossed the Big Wichita about a mile east of the present Kemp Lake dam. South of this it ran in Zone 3, and the same is true for several miles to the north; but while the finds are probably in this zone, the exact horizon cannot be stated."" The length of the trail is relatively well-constrained at about 2 - 3 miles. See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Kemp Lake dam. Numbered ""32"" with taxonomic list, but is incorrectly numbered ""31"" in text.",gp_mid,-30.32,-0.89,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,claystone,"red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,0,J. Mueller,T. Liebrecht,,14/01/2009 02:14,14/01/2009 04:14,7693,major,Ophiacodon,5692,,290.1,272.3,Artinskian,Kungurian,1,US,Ophiacodon major
296021,occ,NA,,28253,,Dimetrodon gigas,species,138120,subjective synonym of,Eryops megacephalus,NA,species,70397,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-99.144997,33.755001,"Military Trail, 32 (Waggoner Ranch Formation)",NA,"Locality 32 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""This trail crossed the Big Wichita about a mile east of the present Kemp Lake dam. South of this it ran in Zone 3, and the same is true for several miles to the north; but while the finds are probably in this zone, the exact horizon cannot be stated."" The length of the trail is relatively well-constrained at about 2 - 3 miles. See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Kemp Lake dam. Numbered ""32"" with taxonomic list, but is incorrectly numbered ""31"" in text.",gp_mid,-30.32,-0.89,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,claystone,"red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:49,07/02/2003 17:49,7693,gigas,Eryops,7693,,290.1,272.3,Artinskian,Kungurian,NA,US,Eryops gigas
296022,occ,NA,,28253,,Dimetrodon obtusidens,species,138130,recombined as,Secodontosaurus obtusidens,NA,species,138129,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38908,NA,NA,NA,,-99.144997,33.755001,"Military Trail, 32 (Waggoner Ranch Formation)",NA,"Locality 32 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""This trail crossed the Big Wichita about a mile east of the present Kemp Lake dam. South of this it ran in Zone 3, and the same is true for several miles to the north; but while the finds are probably in this zone, the exact horizon cannot be stated."" The length of the trail is relatively well-constrained at about 2 - 3 miles. See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Kemp Lake dam. Numbered ""32"" with taxonomic list, but is incorrectly numbered ""31"" in text.",gp_mid,-30.32,-0.89,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,claystone,"red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 15:49,14/01/2009 04:21,7693,obtusidens,Secodontosaurus,7693,,290.1,272.3,Artinskian,Kungurian,NA,US,Secodontosaurus obtusidens
296023,occ,NA,,28253,,Dimetrodon n. sp. semiradicatus,species,70438,subjective synonym of,Dimetrodon limbatus,NA,species,70401,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.144997,33.755001,"Military Trail, 32 (Waggoner Ranch Formation)",NA,"Locality 32 (Romer 1928), faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""This trail crossed the Big Wichita about a mile east of the present Kemp Lake dam. South of this it ran in Zone 3, and the same is true for several miles to the north; but while the finds are probably in this zone, the exact horizon cannot be stated."" The length of the trail is relatively well-constrained at about 2 - 3 miles. See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"" Lat long is for Kemp Lake dam. Numbered ""32"" with taxonomic list, but is incorrectly numbered ""31"" in text.",gp_mid,-30.32,-0.89,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""\r\n\r\n","""limestone""",,,,,claystone,"red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,07/02/2003 15:49,07/02/2003 17:49,7693,semiradicatus,Dimetrodon,7693,n. sp.,290.1,272.3,Artinskian,Kungurian,NA,US,Dimetrodon semiradicatus
296024,occ,NA,,28256,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 16:23,10/04/2009 14:19,17702,sp.,Eryops,7693,,279.3,272.3,Kungurian,,14,US,Eryops sp.
296025,occ,NA,,28256,,Dissorophus multicinctus,species,255227,,Dissorophus multicinctus,NA,species,255227,Cope,1895,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37027,NA,NA,NA,specimens,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Dissorophus,,NA,NA,vertebrate,E. D. Cope. 1895. A batrachian armadillo. The American Naturalist 29:998,4,76,697,J. Alroy,R. Whatley,E. Dunne,07/02/2003 16:23,09/08/2016 05:32,17702,multicinctus,Dissorophus,54069,,279.3,272.3,Kungurian,,3,US,Dissorophus multicinctus
296026,occ,NA,,28256,,n. gen. Aspidosaurus n. sp. chiton,species,345458,,Aspidosaurus chiton,NA,species,345458,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37021,NA,NA,NA,specimens,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Aspidosaurus,n. gen.,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 16:23,10/04/2009 14:19,17702,chiton,Aspidosaurus,7693,n. sp.,279.3,272.3,Kungurian,,2,US,Aspidosaurus chiton
296027,occ,NA,,28256,,Zatrachys n. sp. microphthalmus,species,345490,recombined as,Dasyceps microphthalmus,NA,species,345490,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37054,NA,NA,NA,,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 16:23,10/04/2009 14:19,17702,microphthalmus,Dasyceps,7693,n. sp.,279.3,272.3,Kungurian,,NA,US,Dasyceps microphthalmus
296028,occ,NA,,28256,,Trimerorhachis n. sp. mesops,species,345111,,Trimerorhachis mesops,NA,species,345111,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 16:23,10/04/2009 14:19,17702,mesops,Trimerorhachis,7693,n. sp.,279.3,272.3,Kungurian,,8,US,Trimerorhachis mesops
296029,occ,NA,,28256,,Diplocaulus n. sp. limbatus,species,142461,subjective synonym of,Diplocaulus magnicornis,NA,species,81712,Cope,1896,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,E. D. Cope. 1896. The reptilian order Cotylosauria. Proceedings of the American Philosophical Society 34:436-457,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 16:23,22/04/2015 13:16,17702,limbatus,Diplocaulus,28342,n. sp.,279.3,272.3,Kungurian,,1,US,Diplocaulus limbatus
296030,occ,NA,,28256,,Diplocaulus n. sp. magnicornis,species,81712,,Diplocaulus magnicornis,NA,species,81712,Cope,1882,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,specimens,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,E. D. Cope. 1882. Third contribution to the history of the Vertebrata of the Permian formation of Texas. Proceedings of the American Philosophical Society 20:447-461,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 16:23,12/11/2014 17:09,17702,magnicornis,Diplocaulus,17702,n. sp.,279.3,272.3,Kungurian,,23,US,Diplocaulus magnicornis
296031,occ,NA,,28256,,Lysorophus sp.,genus,37322,,Lysorophus,NA,genus,37322,Romer,1928,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,specimens,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 16:23,10/04/2009 14:19,17702,sp.,Lysorophus,7693,,279.3,272.3,Kungurian,,54,US,Lysorophus sp.
296032,occ,NA,,28256,,n. gen. Cardiocephalus n. sp. sternbergi,species,90715,,Cardiocephalus sternbergi,NA,species,90715,Broili,1904,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37294,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Cardiocephalus,n. gen.,NA,NA,vertebrate,F. Broili. 1904. Permische Stegocephalen und Reptilien aus Texas. Palaeontographica 51:1-120,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 16:56,22/04/2015 13:17,17702,sternbergi,Cardiocephalus,28751,n. sp.,279.3,272.3,Kungurian,,2,US,Cardiocephalus sternbergi
296033,occ,NA,,28256,,n. gen. Seymouria n. sp. baylorensis,species,137488,,Seymouria baylorensis,NA,species,137488,Broili,1904,Chordata,33815,Osteichthyes,34881,,NA,Seymouriidae,37219,37223,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Seymouria,n. gen.,NA,NA,vertebrate,F. Broili. 1904. Permische Stegocephalen und Reptilien aus Texas. Palaeontographica 51:1-120,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 16:56,22/04/2015 13:18,17702,baylorensis,Seymouria,28751,n. sp.,279.3,272.3,Kungurian,,2,US,Seymouria baylorensis
296034,occ,NA,,28256,,n. gen. Desmospondylus n. sp. anomalus,species,151341,subjective synonym of,Seymouria baylorensis,NA,species,137488,Williston,1910,Chordata,33815,Osteichthyes,34881,,NA,Seymouriidae,37219,37223,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Desmospondylus,n. gen.,NA,NA,vertebrate,"S. W. Williston. 1910. Cacops, Desmospondylus; new genera of Permian vertebrates. Geological Society America Bulletin ",4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 16:56,22/04/2015 13:18,17702,anomalus,Seymouria,9272,n. sp.,279.3,272.3,Kungurian,,1,US,Seymouria anomalus
296035,occ,NA,,28256,,Diadectes n. sp. huenei,species,320983,subjective synonym of,Diadectes tenuitectes,NA,species,137873,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 16:56,10/04/2009 14:19,17702,huenei,Diadectes,7693,n. sp.,279.3,272.3,Kungurian,,24,US,Diadectes huenei
296036,occ,NA,,28256,,n. gen. Bolbodon n. sp. tenuitectes,species,137873,recombined as,Diadectes tenuitectes,NA,species,137873,Cope,1896,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Bolbodon,n. gen.,NA,NA,vertebrate,E. D. Cope. 1896. Second contribution to the history of the Cotylosauria. Proceedings of the American Philosophical Society 35(151):122-139,4,76,327,J. Alroy,R. Whatley,R. Butler,07/02/2003 16:56,08/08/2016 10:17,17702,tenuitectes,Diadectes,28358,n. sp.,279.3,272.3,Kungurian,,1,US,Diadectes tenuitectes
296037,occ,NA,,28256,,Pariotichus brachyops,species,136938,,Pariotichus brachyops,NA,species,136938,Romer,1928,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37299,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Pariotichus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 16:56,10/04/2009 14:19,17702,brachyops,Pariotichus,7693,,279.3,272.3,Kungurian,,1,US,Pariotichus brachyops
296038,occ,NA,,28256,,Pariotichus n. sp. isolomus,species,134882,subjective synonym of,Captorhinus aguti,NA,species,134887,Cope,1896,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Pariotichus,,NA,NA,vertebrate,E. D. Cope. 1896. The reptilian order Cotylosauria. Proceedings of the American Philosophical Society 34:436-457,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 16:56,22/04/2015 13:21,17702,isolomus,Captorhinus,28342,n. sp.,279.3,272.3,Kungurian,,1,US,Captorhinus isolomus
296039,occ,NA,,28256,,Ectocynodon n. sp. aguti,species,134887,recombined as,Captorhinus aguti,NA,species,134887,Cope,1882,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Ectocynodon,,NA,NA,vertebrate,E. D. Cope. 1882. Third contribution to the history of the Vertebrata of the Permian formation of Texas. Proceedings of the American Philosophical Society 20:447-461,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 16:56,12/11/2014 17:09,17702,aguti,Captorhinus,17702,n. sp.,279.3,272.3,Kungurian,,1,US,Captorhinus aguti
296040,occ,NA,,28256,,n. gen. Captorhinus n. sp. angusticeps,species,134911,subjective synonym of,Captorhinus aguti,NA,species,134887,Cope,1896,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,specimens,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,n. gen.,NA,NA,vertebrate,E. D. Cope. 1896. The reptilian order Cotylosauria. Proceedings of the American Philosophical Society 34:436-457,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 16:56,22/04/2015 13:21,17702,angusticeps,Captorhinus,28342,n. sp.,279.3,272.3,Kungurian,,37,US,Captorhinus angusticeps
296041,occ,NA,,28256,,n. gen. Hypopnous n. sp. squaliceps,species,136521,subjective synonym of,Captorhinus aguti,NA,species,134887,Romer,1928,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Hypopnous,n. gen.,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 16:56,10/04/2009 14:19,17702,squaliceps,Captorhinus,7693,n. sp.,279.3,272.3,Kungurian,,2,US,Captorhinus squaliceps
296042,occ,NA,,28256,,Pariotichus n. sp. hamatus,species,134856,recombined as,Labidosaurus hamatus,NA,species,134856,Seltin,1959,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Pariotichus,,NA,NA,vertebrate,R. J. Seltin. 1959. A review of the family Captorhinidae. Fieldiana: Geology 10(34):461-509,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,07/02/2003 16:56,10/04/2009 14:19,17702,hamatus,Labidosaurus,28359,n. sp.,279.3,272.3,Kungurian,,1,US,Labidosaurus hamatus
296043,occ,NA,,28256,,Labidosaurus n. sp. broilii,species,134855,subjective synonym of,Labidosaurus hamatus,NA,species,134856,Case,1911,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,vertebrate,E. C. Case. 1911. A revision of the Cotylosauria of North America. Carnegie Institution of Washington Publication 145:1-121,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 16:56,22/04/2015 13:20,17702,broilii,Labidosaurus,28341,n. sp.,279.3,272.3,Kungurian,,1,US,Labidosaurus broilii
296044,occ,NA,,28256,,n. gen. Ostodolepis n. sp. brevispinatus,species,150619,,Ostodolepis brevispinatus,NA,species,150619,Williston,1913,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Ostodolepidae,37301,37303,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Ostodolepis,n. gen.,NA,NA,vertebrate,"S. W. Williston. 1913. Ostodolepis brevispinatus, a new reptile from the Permian of Texas. Journal of Geology 21(4):363-366",4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 16:56,22/04/2015 13:16,17702,brevispinatus,Ostodolepis,30431,n. sp.,279.3,272.3,Kungurian,,1,US,Ostodolepis brevispinatus
296046,occ,NA,,28256,,n. gen. Poecilospondylus n. sp. francisi,species,137867,subjective synonym of,Varanosaurus acutirostris,NA,species,137915,Case,1910,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38933,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Poecilospondylus,n. gen.,NA,NA,vertebrate,"E. C. Case. 1910. The skeleton of Poecilospondylus francisi, a new genus and species of Pelycosauria. Bulletin of the American Museum of Natural History 23:183-188",4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 16:56,22/04/2015 13:19,17702,francisi,Varanosaurus,28818,n. sp.,279.3,272.3,Kungurian,,1,US,Varanosaurus francisi
296047,occ,NA,,28256,,n. gen. Tetraceratops n. sp. insignis,species,145255,,Tetraceratops insignis,NA,species,145255,Matthew,1908,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,38930,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tetraceratops,n. gen.,NA,NA,vertebrate,W. D. Matthew. 1908. A four-horned pelycosaurian from the Permian of Texas. Bulletin of the American Museum of Natural History 24:183-185,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 16:56,22/04/2015 13:20,17702,insignis,Tetraceratops,29679,n. sp.,279.3,272.3,Kungurian,,1,US,Tetraceratops insignis
296048,occ,NA,,28256,,Dimetrodon n. sp. gigashomogenes,species,138123,,Dimetrodon gigashomogenes,NA,species,138123,Case,1907,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,E. C. Case. 1907. Revision of the Pelycosauria of North America. Carnegie Institution of Washington 55:3-176,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 16:56,22/04/2015 13:20,17702,gigashomogenes,Dimetrodon,7374,n. sp.,279.3,272.3,Kungurian,,1,US,Dimetrodon gigashomogenes
296049,occ,NA,,28256,,Embolophorus n. sp. dollovianus,species,138126,recombined as,Dimetrodon dollovianus,NA,species,138126,Cope,1888,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Embolophorus,,NA,NA,vertebrate,"E. D. Cope. 1888. Systematic catalogue of the species of Vertebrata found in the beds of the Permian Epoch in North America with notes and descriptions. Transactions of the Philosophical Society of America, New Series 16(2):285-297",4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 16:56,22/04/2015 13:19,17702,dollovianus,Dimetrodon,28371,n. sp.,279.3,272.3,Kungurian,,1,US,Dimetrodon dollovianus
296050,occ,NA,,28256,,n. gen. Edaphosaurus n. sp. pogonias,species,81711,,Edaphosaurus pogonias,NA,species,81711,Cope,1882,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,n. gen.,NA,NA,vertebrate,E. D. Cope. 1882. Third contribution to the history of the Vertebrata of the Permian formation of Texas. Proceedings of the American Philosophical Society 20:447-461,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 16:56,12/11/2014 17:09,17702,pogonias,Edaphosaurus,17702,n. sp.,279.3,272.3,Kungurian,,1,US,Edaphosaurus pogonias
296051,occ,NA,,28256,,n. gen. Naosaurus n. sp. claviger,species,134988,subjective synonym of,Edaphosaurus pogonias,NA,species,81711,Cope,1886,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Naosaurus,n. gen.,NA,NA,vertebrate,E. D. Cope. 1886. The long-spined Theromorpha of the Permian Epoch. The American Naturalist 20(6):544-545,4,76,14,J. Alroy,R. Whatley,M. Carrano,07/02/2003 16:56,22/04/2015 13:19,17702,claviger,Edaphosaurus,28380,n. sp.,279.3,272.3,Kungurian,,1,US,Edaphosaurus claviger
296055,occ,NA,,28264,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,08/02/2003 12:30,22/04/2015 13:12,9228,sp.,Eryops,7693,,279.3,272.3,Kungurian,,6,US,Eryops sp.
296056,occ,NA,,28264,,Cacops n. sp. aspidephorus,species,56737,,Cacops aspidephorus,NA,species,56737,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37025,NA,NA,NA,specimens,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Cacops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,08/02/2003 12:30,22/04/2015 13:12,9228,aspidephorus,Cacops,7693,n. sp.,279.3,272.3,Kungurian,,21,US,Cacops aspidephorus
296057,occ,NA,,28264,,Trimerorhachis n. sp. insignis,species,36991,species not entered,Trimerorhachis,NA,genus,36991,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,08/02/2003 12:30,22/04/2015 13:12,9228,insignis,Trimerorhachis,7693,n. sp.,279.3,272.3,Kungurian,,4,US,Trimerorhachis insignis
296058,occ,NA,,28264,,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,specimens,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,08/02/2003 12:30,22/04/2015 13:12,9228,sp.,Diplocaulus,7693,,279.3,272.3,Kungurian,,5,US,Diplocaulus sp.
296059,occ,NA,,28264,,Seymouria baylorensis,species,137488,,Seymouria baylorensis,NA,species,137488,Williston,1911,Chordata,33815,Osteichthyes,34881,,NA,Seymouriidae,37219,37223,NA,NA,NA,specimens,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Seymouria,,NA,NA,vertebrate,S. W. Williston. 1911. American Permian Vertebrates ,4,76,14,J. Alroy,R. Whatley,M. Carrano,08/02/2003 12:30,22/04/2015 13:12,9228,baylorensis,Seymouria,9228,,279.3,272.3,Kungurian,,1,US,Seymouria baylorensis
296060,occ,NA,,28264,,Pariotichus n. sp. aduncus,species,134912,subjective synonym of,Captorhinus aguti,NA,species,134887,Romer,1928,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,specimens,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Pariotichus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,08/02/2003 12:30,22/04/2015 13:12,9228,aduncus,Captorhinus,7693,n. sp.,279.3,272.3,Kungurian,,1,US,Captorhinus aduncus
296061,occ,NA,,28264,,Pariotichus n. sp. megalops,species,120982,subjective synonym of,Isodectes obtusus,NA,species,137370,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Saurerpetontidae,36980,36983,NA,NA,NA,specimens,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Pariotichus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,08/02/2003 12:30,22/04/2015 13:12,9228,megalops,Isodectes,7693,n. sp.,279.3,272.3,Kungurian,,1,US,Isodectes megalops
296062,occ,NA,,28264,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,08/02/2003 12:30,22/04/2015 13:12,9228,sp.,Diadectes,7693,,279.3,272.3,Kungurian,,3,US,Diadectes sp.
296063,occ,NA,,28264,,Captorhinus sp.,genus,37497,,Captorhinus,NA,genus,37497,Romer,1928,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,specimens,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,08/02/2003 12:30,22/04/2015 13:12,9228,sp.,Captorhinus,7693,,279.3,272.3,Kungurian,,4,US,Captorhinus sp.
296064,occ,NA,,28264,,Labidosaurus sp.,genus,37501,,Labidosaurus,NA,genus,37501,Romer,1928,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,specimens,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,08/02/2003 12:30,22/04/2015 13:12,9228,sp.,Labidosaurus,7693,,279.3,272.3,Kungurian,,1,US,Labidosaurus sp.
296066,occ,NA,,28264,,Varanosaurus n. sp. brevirostris,species,122316,recombined as,Varanops brevirostris,NA,species,122316,Williston,1911,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,38897,NA,NA,NA,specimens,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Varanosaurus,,NA,NA,vertebrate,S. W. Williston. 1911. American Permian Vertebrates ,4,76,14,J. Alroy,R. Whatley,M. Carrano,08/02/2003 12:30,22/04/2015 13:12,9228,brevirostris,Varanops,9228,n. sp.,279.3,272.3,Kungurian,,99,US,Varanops brevirostris
296067,occ,NA,,28264,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,08/02/2003 12:30,22/04/2015 13:12,9228,sp.,Ophiacodon,7693,,279.3,272.3,Kungurian,,4,US,Ophiacodon sp.
296068,occ,NA,,28264,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,08/02/2003 12:30,22/04/2015 13:12,9228,sp.,Dimetrodon,7693,,279.3,272.3,Kungurian,,2,US,Dimetrodon sp.
296069,occ,NA,,28264,,Edaphosaurus sp.,genus,38911,,Edaphosaurus,NA,genus,38911,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,specimens,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,08/02/2003 12:30,22/04/2015 13:12,9228,sp.,Edaphosaurus,7693,,279.3,272.3,Kungurian,,5,US,Edaphosaurus sp.
296070,occ,NA,,28264,,n. gen. Casea n. sp. broilii,species,113850,,Casea broilii,NA,species,113850,Williston,1910,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38915,NA,NA,NA,individuals,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Casea,n. gen.,NA,NA,vertebrate,S. W. Williston. 1910. New Permian reptiles; rhachitomous vertebrae. Journal of Geology 18:585-600,4,76,14,J. Alroy,R. Whatley,M. Carrano,08/02/2003 12:30,22/04/2015 13:12,9228,broilii,Casea,9269,n. sp.,279.3,272.3,Kungurian,,1,US,Casea broilii
296071,occ,NA,,28261,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-99.144997,33.755001,"Pony Creek, 36 (Arroyo Formation)",NA,"Locality 36 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""A tributary of the Big Wichita on the south side, north of Seymour; the collections were made near the head of the creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Kemp Lake. Numbered ""36"" with taxonomic list and on map, but is incorrectly numbered ""35"" in text.",gp_mid,-28.88,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably about 100 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,08/02/2003 12:35,08/02/2003 14:35,7693,sp.,Eryops,7693,,279.3,272.3,Kungurian,,6,US,Eryops sp.
296072,occ,NA,,28261,,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,specimens,-99.144997,33.755001,"Pony Creek, 36 (Arroyo Formation)",NA,"Locality 36 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""A tributary of the Big Wichita on the south side, north of Seymour; the collections were made near the head of the creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Kemp Lake. Numbered ""36"" with taxonomic list and on map, but is incorrectly numbered ""35"" in text.",gp_mid,-28.88,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably about 100 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:35,02/03/2009 09:16,7693,sp.,Diplocaulus,7693,,279.3,272.3,Kungurian,,13,US,Diplocaulus sp.
296073,occ,NA,,28261,,Captorhinus sp.,genus,37497,,Captorhinus,NA,genus,37497,Romer,1928,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,specimens,-99.144997,33.755001,"Pony Creek, 36 (Arroyo Formation)",NA,"Locality 36 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""A tributary of the Big Wichita on the south side, north of Seymour; the collections were made near the head of the creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Kemp Lake. Numbered ""36"" with taxonomic list and on map, but is incorrectly numbered ""35"" in text.",gp_mid,-28.88,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably about 100 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,08/02/2003 12:35,08/02/2003 14:35,7693,sp.,Captorhinus,7693,,279.3,272.3,Kungurian,,1,US,Captorhinus sp.
296074,occ,NA,R,28261,,Labidosaurus sp.,genus,37501,,Labidosaurus,NA,genus,37501,Romer,1928,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,individuals,-99.144997,33.755001,"Pony Creek, 36 (Arroyo Formation)",NA,"Locality 36 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""A tributary of the Big Wichita on the south side, north of Seymour; the collections were made near the head of the creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Kemp Lake. Numbered ""36"" with taxonomic list and on map, but is incorrectly numbered ""35"" in text.",gp_mid,-28.88,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably about 100 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:35,30/11/2008 20:53,7693,sp.,Labidosaurus,7693,,279.3,272.3,Kungurian,,1,US,Labidosaurus sp.
296074,occ,21137,,28261,,Labidosaurus hamatus,species,134918,,Labidosaurus hamatus,NA,species,134856,Seltin,1959,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,individuals,-99.144997,33.755001,"Pony Creek, 36 (Arroyo Formation)",NA,"Locality 36 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""A tributary of the Big Wichita on the south side, north of Seymour; the collections were made near the head of the creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Kemp Lake. Numbered ""36"" with taxonomic list and on map, but is incorrectly numbered ""35"" in text.",gp_mid,-28.88,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably about 100 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,vertebrate,R. J. Seltin. 1959. A review of the family Captorhinidae. Fieldiana: Geology 10(34):461-509,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,30/11/2008 18:47,30/11/2008 20:53,7693,hamatus,Labidosaurus,28359,,279.3,272.3,Kungurian,,1,US,Labidosaurus hamatus
296075,occ,NA,,28261,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-99.144997,33.755001,"Pony Creek, 36 (Arroyo Formation)",NA,"Locality 36 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""A tributary of the Big Wichita on the south side, north of Seymour; the collections were made near the head of the creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Kemp Lake. Numbered ""36"" with taxonomic list and on map, but is incorrectly numbered ""35"" in text.",gp_mid,-28.88,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably about 100 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,08/02/2003 12:35,08/02/2003 14:35,7693,sp.,Ophiacodon,7693,,279.3,272.3,Kungurian,,10,US,Ophiacodon sp.
296076,occ,NA,,28261,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-99.144997,33.755001,"Pony Creek, 36 (Arroyo Formation)",NA,"Locality 36 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""A tributary of the Big Wichita on the south side, north of Seymour; the collections were made near the head of the creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Kemp Lake. Numbered ""36"" with taxonomic list and on map, but is incorrectly numbered ""35"" in text.",gp_mid,-28.88,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably about 100 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,08/02/2003 12:35,08/02/2003 14:35,7693,sp.,Dimetrodon,7693,,279.3,272.3,Kungurian,,3,US,Dimetrodon sp.
296077,occ,NA,,28266,,Dissorophus sp.,genus,37027,,Dissorophus,NA,genus,37027,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37027,NA,NA,NA,specimens,-99.144997,33.755001,"Gray's Creek, 37 (Arroyo Formation)",NA,"Locality 37 (Romer 1928), Craddock's ranch, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake.",gp_mid,-28.88,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Dissorophus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,08/02/2003 12:39,08/02/2003 14:39,7693,sp.,Dissorophus,7693,,279.3,272.3,Kungurian,,1,US,Dissorophus sp.
296078,occ,NA,,28266,,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,specimens,-99.144997,33.755001,"Gray's Creek, 37 (Arroyo Formation)",NA,"Locality 37 (Romer 1928), Craddock's ranch, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake.",gp_mid,-28.88,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,08/02/2003 12:39,08/02/2003 14:39,7693,sp.,Diplocaulus,7693,,279.3,272.3,Kungurian,,2,US,Diplocaulus sp.
296079,occ,NA,,28266,,n. gen. Otocoelus n. sp. testudineus,species,138239,subjective synonym of,Dissorophus multicinctus,NA,species,255227,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37027,NA,NA,NA,,-99.144997,33.755001,"Gray's Creek, 37 (Arroyo Formation)",NA,"Locality 37 (Romer 1928), Craddock's ranch, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake.",gp_mid,-28.88,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Otocoelus,n. gen.,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:39,27/12/2008 15:34,7693,testudineus,Dissorophus,7693,n. sp.,279.3,272.3,Kungurian,,NA,US,Dissorophus testudineus
296080,occ,NA,,28266,,Seymouria sp.,genus,37223,,Seymouria,NA,genus,37223,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Seymouriidae,37219,37223,NA,NA,NA,specimens,-99.144997,33.755001,"Gray's Creek, 37 (Arroyo Formation)",NA,"Locality 37 (Romer 1928), Craddock's ranch, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake.",gp_mid,-28.88,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Seymouria,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,08/02/2003 12:39,08/02/2003 14:39,7693,sp.,Seymouria,7693,,279.3,272.3,Kungurian,,1,US,Seymouria sp.
296081,occ,NA,,28266,,n. gen. Conodectes n. sp. favosus,species,138237,subjective synonym of,Seymouria baylorensis,NA,species,137488,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Seymouriidae,37219,37223,NA,NA,NA,,-99.144997,33.755001,"Gray's Creek, 37 (Arroyo Formation)",NA,"Locality 37 (Romer 1928), Craddock's ranch, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake.",gp_mid,-28.88,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Conodectes,n. gen.,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:39,27/12/2008 15:33,7693,favosus,Seymouria,7693,n. sp.,279.3,272.3,Kungurian,,NA,US,Seymouria favosus
296082,occ,NA,,28267,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,sp.,Eryops,7693,,279.3,272.3,Kungurian,,NA,US,Eryops sp.
296083,occ,NA,,28267,,Aspidosaurus ? n. sp. peltatus,species,345924,nomen dubium,Dissorophidae,NA,family,37017,Williston,1911,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,NA,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Aspidosaurus,?,NA,NA,vertebrate,S. W. Williston. 1911. American Permian Vertebrates ,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,peltatus,,9228,n. sp.,279.3,272.3,Kungurian,,NA,US, peltatus
296084,occ,NA,,28267,,Broiliellus n. sp. peltatus,species,345925,nomen dubium,Dissorophidae,NA,family,37017,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,NA,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Broiliellus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,peltatus,,7693,n. sp.,279.3,272.3,Kungurian,,NA,US, peltatus
296085,occ,NA,,28267,,Dissorophidae indet.,family,37017,,Dissorophidae,NA,family,37017,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,NA,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Dissorophidae,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,indet.,,7693,,279.3,272.3,Kungurian,,NA,US, indet.
296086,occ,NA,,28267,,Zatrachys sp.,genus,37056,,Zatrachys,NA,genus,37056,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,sp.,Zatrachys,7693,,279.3,272.3,Kungurian,,NA,US,Zatrachys sp.
296087,occ,NA,,28267,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Williston,1911,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,S. W. Williston. 1911. American Permian Vertebrates ,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,sp.,Trimerorhachis,9228,,279.3,272.3,Kungurian,,NA,US,Trimerorhachis sp.
296088,occ,NA,,28267,,Diplocaulus magnicornis,species,81712,,Diplocaulus magnicornis,NA,species,81712,Williston,1911,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,specimens,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,S. W. Williston. 1911. American Permian Vertebrates ,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,magnicornis,Diplocaulus,9228,,279.3,272.3,Kungurian,,7,US,Diplocaulus magnicornis
296089,occ,NA,,28267,,n. gen. Platyops n. sp. parvus,species,142455,subjective synonym of,Diplocaulus magnicornis,NA,species,81712,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,individuals,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Platyops,n. gen.,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,parvus,Diplocaulus,7693,n. sp.,279.3,272.3,Kungurian,,1,US,Diplocaulus parvus
296090,occ,NA,,28267,,Lysorophus sp.,genus,37322,,Lysorophus,NA,genus,37322,Romer,1928,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,sp.,Lysorophus,7693,,279.3,272.3,Kungurian,,NA,US,Lysorophus sp.
296092,occ,NA,,28267,,Seymouria sp.,genus,37223,,Seymouria,NA,genus,37223,Williston,1911,Chordata,33815,Osteichthyes,34881,,NA,Seymouriidae,37219,37223,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Seymouria,,NA,NA,vertebrate,S. W. Williston. 1911. American Permian Vertebrates ,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,sp.,Seymouria,9228,,279.3,272.3,Kungurian,,NA,US,Seymouria sp.
296093,occ,NA,,28267,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Williston,1911,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,S. W. Williston. 1911. American Permian Vertebrates ,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,sp.,Diadectes,9228,,279.3,272.3,Kungurian,,NA,US,Diadectes sp.
296094,occ,NA,,28267,,Edaphosaurus sp.,genus,38911,,Edaphosaurus,NA,genus,38911,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,sp.,Edaphosaurus,7693,,279.3,272.3,Kungurian,,NA,US,Edaphosaurus sp.
296095,occ,NA,,28267,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,sp.,Ophiacodon,7693,,279.3,272.3,Kungurian,,NA,US,Ophiacodon sp.
296096,occ,NA,,28267,,Dimetrodon incisivus,species,54986,subjective synonym of,Dimetrodon limbatus,NA,species,70401,Williston,1911,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,S. W. Williston. 1911. American Permian Vertebrates ,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,incisivus,Dimetrodon,9228,,279.3,272.3,Kungurian,,NA,US,Dimetrodon incisivus
296097,occ,NA,,28267,,Dimetrodon gigas,species,138120,subjective synonym of,Eryops megacephalus,NA,species,70397,Williston,1911,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,S. W. Williston. 1911. American Permian Vertebrates ,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,gigas,Eryops,9228,,279.3,272.3,Kungurian,,NA,US,Eryops gigas
296098,occ,NA,,28267,,n. gen. Trispondylus n. sp. texensis,species,113851,recombined as,Trichasaurus texensis,NA,species,113851,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38932,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Trispondylus,n. gen.,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,texensis,Trichasaurus,7693,n. sp.,279.3,272.3,Kungurian,,NA,US,Trichasaurus texensis
296099,occ,NA,,28267,,Bolosaurus sp.,genus,37511,,Bolosaurus,NA,genus,37511,Romer,1928,Chordata,33815,Reptilia,36322,,NA,Bolosauridae,37510,37511,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Bolosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,sp.,Bolosaurus,7693,,279.3,272.3,Kungurian,,NA,US,Bolosaurus sp.
296100,occ,NA,,28267,,n. gen. Araeoscelis n. sp. gracilis,species,113849,,Araeoscelis gracilis,NA,species,113849,Vaughn,1955,Chordata,33815,Reptilia,36322,Araeoscelidia,37769,Araeoscelidae,37772,37773,NA,NA,NA,individuals,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Araeoscelis,n. gen.,NA,NA,vertebrate,P. P. Vaughn. 1955. The Permian reptile Araeoscelis restudied. Bulletin of the Museum of Comparative Zoology 113(5):305-467,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,gracilis,Araeoscelis,4323,n. sp.,279.3,272.3,Kungurian,,5,US,Araeoscelis gracilis
296101,occ,NA,,28267,,n. gen. Trematops n. sp. milleri,species,137365,subjective synonym of,Acheloma cumminsi,NA,species,81713,Williston,1911,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,37048,NA,NA,NA,individuals,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Trematops,n. gen.,NA,NA,vertebrate,S. W. Williston. 1911. American Permian Vertebrates ,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 12:59,29/01/2010 07:32,9228,milleri,Acheloma,9228,n. sp.,279.3,272.3,Kungurian,,1,US,Acheloma milleri
296102,occ,NA,,28270,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-99.312775,33.714722,"Hog Creek, 39 (Arroyo Formation)",NA,"Locality 39 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""The next creek west of Brush Creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Hog Creek.",gp_mid,-29.02,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,08/02/2003 13:16,13/07/2016 06:39,7693,sp.,Eryops,7693,,279.3,272.3,Kungurian,,3,US,Eryops sp.
296103,occ,NA,,28270,,Dissorophus multicinctus,species,255227,,Dissorophus multicinctus,NA,species,255227,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37027,NA,NA,NA,specimens,-99.312775,33.714722,"Hog Creek, 39 (Arroyo Formation)",NA,"Locality 39 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""The next creek west of Brush Creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Hog Creek.",gp_mid,-29.02,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Dissorophus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,08/02/2003 13:16,13/07/2016 06:40,7693,multicinctus,Dissorophus,7693,,279.3,272.3,Kungurian,,1,US,Dissorophus multicinctus
296104,occ,NA,,28270,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-99.312775,33.714722,"Hog Creek, 39 (Arroyo Formation)",NA,"Locality 39 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""The next creek west of Brush Creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Hog Creek.",gp_mid,-29.02,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,08/02/2003 13:16,13/07/2016 06:39,7693,sp.,Trimerorhachis,7693,,279.3,272.3,Kungurian,,1,US,Trimerorhachis sp.
296105,occ,NA,,28270,,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,specimens,-99.312775,33.714722,"Hog Creek, 39 (Arroyo Formation)",NA,"Locality 39 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""The next creek west of Brush Creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Hog Creek.",gp_mid,-29.02,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,08/02/2003 13:16,13/07/2016 06:39,7693,sp.,Diplocaulus,7693,,279.3,272.3,Kungurian,,3,US,Diplocaulus sp.
296106,occ,NA,,28270,,Lysorophus sp.,genus,37322,,Lysorophus,NA,genus,37322,Romer,1928,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,specimens,-99.312775,33.714722,"Hog Creek, 39 (Arroyo Formation)",NA,"Locality 39 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""The next creek west of Brush Creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Hog Creek.",gp_mid,-29.02,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,08/02/2003 13:16,13/07/2016 06:39,7693,sp.,Lysorophus,7693,,279.3,272.3,Kungurian,,2,US,Lysorophus sp.
296107,occ,NA,R,28270,,Captorhinus sp.,genus,37497,,Captorhinus,NA,genus,37497,Romer,1928,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,specimens,-99.312775,33.714722,"Hog Creek, 39 (Arroyo Formation)",NA,"Locality 39 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""The next creek west of Brush Creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Hog Creek.",gp_mid,-29.02,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,08/02/2003 13:16,13/07/2016 06:40,7693,sp.,Captorhinus,7693,,279.3,272.3,Kungurian,,1,US,Captorhinus sp.
296107,occ,21189,,28270,,Captorhinus aguti,species,90718,,Captorhinus aguti,NA,species,134887,Seltin,1959,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,specimens,-99.312775,33.714722,"Hog Creek, 39 (Arroyo Formation)",NA,"Locality 39 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""The next creek west of Brush Creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Hog Creek.",gp_mid,-29.02,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,R. J. Seltin. 1959. A review of the family Captorhinidae. Fieldiana: Geology 10(34):461-509,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,15/12/2008 16:40,15/12/2008 18:40,7693,aguti,Captorhinus,28359,,279.3,272.3,Kungurian,,1,US,Captorhinus aguti
296108,occ,NA,,28270,,Labidosaurus sp.,genus,37501,,Labidosaurus,NA,genus,37501,Romer,1928,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,specimens,-99.312775,33.714722,"Hog Creek, 39 (Arroyo Formation)",NA,"Locality 39 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""The next creek west of Brush Creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Hog Creek.",gp_mid,-29.02,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,08/02/2003 13:16,13/07/2016 06:39,7693,sp.,Labidosaurus,7693,,279.3,272.3,Kungurian,,1,US,Labidosaurus sp.
296109,occ,NA,,28270,,Labidosaurus hamatus,species,134918,,Labidosaurus hamatus,NA,species,134856,Seltin,1959,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,individuals,-99.312775,33.714722,"Hog Creek, 39 (Arroyo Formation)",NA,"Locality 39 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""The next creek west of Brush Creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Hog Creek.",gp_mid,-29.02,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,vertebrate,R. J. Seltin. 1959. A review of the family Captorhinidae. Fieldiana: Geology 10(34):461-509,4,76,697,J. Alroy,R. Whatley,E. Dunne,08/02/2003 13:16,13/07/2016 06:39,7693,hamatus,Labidosaurus,28359,,279.3,272.3,Kungurian,,1,US,Labidosaurus hamatus
296110,occ,NA,,28270,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-99.312775,33.714722,"Hog Creek, 39 (Arroyo Formation)",NA,"Locality 39 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""The next creek west of Brush Creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Hog Creek.",gp_mid,-29.02,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,08/02/2003 13:16,13/07/2016 06:39,7693,sp.,Dimetrodon,7693,,279.3,272.3,Kungurian,,3,US,Dimetrodon sp.
296111,occ,NA,,28272,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-99.260002,33.594166,"Table Top Mountain, 40 (Arroyo Formation)",NA,"Locality 40 (Romer 1928), Table Top Mt., faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""to the south above Craddock's ranch and Brush Creek."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Seymour.",gp_mid,-29.05,1.64,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds perhaps average 200 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,"""A remnant of a former peneplain..""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,08/02/2003 13:20,08/02/2003 15:20,7693,sp.,Eryops,7693,,279.3,272.3,Kungurian,,2,US,Eryops sp.
296112,occ,NA,,28272,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-99.260002,33.594166,"Table Top Mountain, 40 (Arroyo Formation)",NA,"Locality 40 (Romer 1928), Table Top Mt., faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""to the south above Craddock's ranch and Brush Creek."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Seymour.",gp_mid,-29.05,1.64,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds perhaps average 200 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,"""A remnant of a former peneplain..""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,4,J. Alroy,R. Whatley,J. Alroy,08/02/2003 13:20,17/12/2006 15:12,7693,sp.,Trimerorhachis,7693,,279.3,272.3,Kungurian,,1,US,Trimerorhachis sp.
296113,occ,NA,,28272,,Diplocaulus n. sp. copei,species,142459,nomen vanum,Diplocaulus,NA,genus,37264,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,specimens,-99.260002,33.594166,"Table Top Mountain, 40 (Arroyo Formation)",NA,"Locality 40 (Romer 1928), Table Top Mt., faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""to the south above Craddock's ranch and Brush Creek."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Seymour.",gp_mid,-29.05,1.64,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds perhaps average 200 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,"""A remnant of a former peneplain..""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,76,J. Alroy,R. Whatley,R. Whatley,08/02/2003 13:20,08/02/2003 17:15,7693,copei,Diplocaulus,7693,n. sp.,279.3,272.3,Kungurian,,8,US,Diplocaulus copei
296114,occ,NA,,28272,,Platyops sp.,genus,142454,subjective synonym of,Diplocaulus,NA,genus,37264,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,specimens,-99.260002,33.594166,"Table Top Mountain, 40 (Arroyo Formation)",NA,"Locality 40 (Romer 1928), Table Top Mt., faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""to the south above Craddock's ranch and Brush Creek."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Seymour.",gp_mid,-29.05,1.64,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds perhaps average 200 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,"""A remnant of a former peneplain..""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Platyops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,08/02/2003 13:20,02/03/2009 05:46,7693,sp.,Diplocaulus,7693,,279.3,272.3,Kungurian,,6,US,Diplocaulus sp.
296115,occ,NA,,28272,,Seymouria sp.,genus,37223,,Seymouria,NA,genus,37223,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Seymouriidae,37219,37223,NA,NA,NA,specimens,-99.260002,33.594166,"Table Top Mountain, 40 (Arroyo Formation)",NA,"Locality 40 (Romer 1928), Table Top Mt., faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""to the south above Craddock's ranch and Brush Creek."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Seymour.",gp_mid,-29.05,1.64,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds perhaps average 200 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,"""A remnant of a former peneplain..""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Seymouria,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,08/02/2003 13:20,08/02/2003 15:20,7693,sp.,Seymouria,7693,,279.3,272.3,Kungurian,,1,US,Seymouria sp.
296116,occ,NA,,28272,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-99.260002,33.594166,"Table Top Mountain, 40 (Arroyo Formation)",NA,"Locality 40 (Romer 1928), Table Top Mt., faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""to the south above Craddock's ranch and Brush Creek."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Seymour.",gp_mid,-29.05,1.64,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds perhaps average 200 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,"""A remnant of a former peneplain..""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,08/02/2003 13:20,08/02/2003 15:20,7693,sp.,Diadectes,7693,,279.3,272.3,Kungurian,,2,US,Diadectes sp.
296117,occ,NA,,28272,,Captorhinus sp.,genus,37497,,Captorhinus,NA,genus,37497,Romer,1928,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,specimens,-99.260002,33.594166,"Table Top Mountain, 40 (Arroyo Formation)",NA,"Locality 40 (Romer 1928), Table Top Mt., faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""to the south above Craddock's ranch and Brush Creek."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Seymour.",gp_mid,-29.05,1.64,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds perhaps average 200 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,"""A remnant of a former peneplain..""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,08/02/2003 13:20,08/02/2003 15:20,7693,sp.,Captorhinus,7693,,279.3,272.3,Kungurian,,2,US,Captorhinus sp.
296118,occ,NA,,28272,,Poliosaurus sp.,genus,138052,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-99.260002,33.594166,"Table Top Mountain, 40 (Arroyo Formation)",NA,"Locality 40 (Romer 1928), Table Top Mt., faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""to the south above Craddock's ranch and Brush Creek."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Seymour.",gp_mid,-29.05,1.64,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds perhaps average 200 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,"""A remnant of a former peneplain..""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Poliosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,08/02/2003 13:20,08/02/2003 15:20,7693,sp.,Ophiacodon,7693,,279.3,272.3,Kungurian,,2,US,Ophiacodon sp.
296119,occ,NA,,28272,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-99.260002,33.594166,"Table Top Mountain, 40 (Arroyo Formation)",NA,"Locality 40 (Romer 1928), Table Top Mt., faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""to the south above Craddock's ranch and Brush Creek."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Seymour.",gp_mid,-29.05,1.64,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds perhaps average 200 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,"""A remnant of a former peneplain..""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,08/02/2003 13:20,08/02/2003 15:20,7693,sp.,Ophiacodon,7693,,279.3,272.3,Kungurian,,1,US,Ophiacodon sp.
296120,occ,NA,,28273,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-99.359444,33.733055,"Crooked Creek, 41 (Arroyo Formation)",NA,"Locality 41 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""On the north side of the river, west of Hog Creek."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for the lower reaches of Crooked Creek, just above junction with Wichita River.",gp_mid,-29.05,1.8,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds perhaps average 200 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,4,J. Alroy,R. Whatley,J. Alroy,08/02/2003 13:21,17/12/2006 15:12,7693,sp.,Trimerorhachis,7693,,279.3,272.3,Kungurian,,1,US,Trimerorhachis sp.
296121,occ,NA,,28273,,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,specimens,-99.359444,33.733055,"Crooked Creek, 41 (Arroyo Formation)",NA,"Locality 41 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""On the north side of the river, west of Hog Creek."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for the lower reaches of Crooked Creek, just above junction with Wichita River.",gp_mid,-29.05,1.8,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds perhaps average 200 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,08/02/2003 13:21,08/02/2003 15:21,7693,sp.,Diplocaulus,7693,,279.3,272.3,Kungurian,,3,US,Diplocaulus sp.
296122,occ,NA,,28273,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-99.359444,33.733055,"Crooked Creek, 41 (Arroyo Formation)",NA,"Locality 41 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""On the north side of the river, west of Hog Creek."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for the lower reaches of Crooked Creek, just above junction with Wichita River.",gp_mid,-29.05,1.8,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds perhaps average 200 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,08/02/2003 13:21,08/02/2003 15:21,7693,sp.,Diadectes,7693,,279.3,272.3,Kungurian,,1,US,Diadectes sp.
296123,occ,NA,,28273,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-99.359444,33.733055,"Crooked Creek, 41 (Arroyo Formation)",NA,"Locality 41 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""On the north side of the river, west of Hog Creek."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for the lower reaches of Crooked Creek, just above junction with Wichita River.",gp_mid,-29.05,1.8,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds perhaps average 200 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,08/02/2003 13:21,08/02/2003 15:21,7693,sp.,Ophiacodon,7693,,279.3,272.3,Kungurian,,4,US,Ophiacodon sp.
296128,occ,NA,,28275,,Zatrachys sp.,genus,37056,,Zatrachys,NA,genus,37056,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,specimens,-99.195557,33.973057,"Beaver Creek, 42 (Arroyo Formation)",NA,"Locality 42 (Romer 1928), Beaver Creek Wilbarger County, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Wilbarger,based on nearby landmark,seconds,outcrop,"""The upper reaches of the stream have yielded a few remains."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Beaver Creek.",gp_mid,-28.81,1.94,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""above the Lueders limestone, and quite probably correspond to the beds to the south of Coffee Creek."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,08/02/2003 15:13,10/05/2016 09:07,7693,sp.,Zatrachys,7693,,279.3,272.3,Kungurian,,1,US,Zatrachys sp.
296129,occ,NA,,28275,,n. gen. Diadectoides n. sp. cretin,species,321001,subjective synonym of,Diadectes tenuitectes,NA,species,137873,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-99.195557,33.973057,"Beaver Creek, 42 (Arroyo Formation)",NA,"Locality 42 (Romer 1928), Beaver Creek Wilbarger County, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Wilbarger,based on nearby landmark,seconds,outcrop,"""The upper reaches of the stream have yielded a few remains."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Beaver Creek.",gp_mid,-28.81,1.94,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""above the Lueders limestone, and quite probably correspond to the beds to the south of Coffee Creek."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectoides,n. gen.,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,08/02/2003 15:13,10/05/2016 09:07,7693,cretin,Diadectes,7693,n. sp.,279.3,272.3,Kungurian,,1,US,Diadectes cretin
296130,occ,NA,,28275,,Theropleura n. sp. grandis,species,138059,recombined as,Dimetrodon grandis,NA,species,138059,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-99.195557,33.973057,"Beaver Creek, 42 (Arroyo Formation)",NA,"Locality 42 (Romer 1928), Beaver Creek Wilbarger County, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Wilbarger,based on nearby landmark,seconds,outcrop,"""The upper reaches of the stream have yielded a few remains."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Beaver Creek.",gp_mid,-28.81,1.94,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""above the Lueders limestone, and quite probably correspond to the beds to the south of Coffee Creek."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,08/02/2003 15:13,10/05/2016 09:07,7693,grandis,Dimetrodon,7693,n. sp.,279.3,272.3,Kungurian,,1,US,Dimetrodon grandis
296131,occ,NA,,28275,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-99.195557,33.973057,"Beaver Creek, 42 (Arroyo Formation)",NA,"Locality 42 (Romer 1928), Beaver Creek Wilbarger County, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Wilbarger,based on nearby landmark,seconds,outcrop,"""The upper reaches of the stream have yielded a few remains."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Beaver Creek.",gp_mid,-28.81,1.94,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""above the Lueders limestone, and quite probably correspond to the beds to the south of Coffee Creek."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,08/02/2003 15:13,10/05/2016 09:07,7693,sp.,Dimetrodon,7693,,279.3,272.3,Kungurian,,1,US,Dimetrodon sp.
296132,occ,NA,,28275,,n. gen. Bathyglyptus n. sp. theodori,species,165041,,Bathyglyptus theodori,NA,species,165041,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,165040,NA,NA,NA,specimens,-99.195557,33.973057,"Beaver Creek, 42 (Arroyo Formation)",NA,"Locality 42 (Romer 1928), Beaver Creek Wilbarger County, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Wilbarger,based on nearby landmark,seconds,outcrop,"""The upper reaches of the stream have yielded a few remains."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Beaver Creek.",gp_mid,-28.81,1.94,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""above the Lueders limestone, and quite probably correspond to the beds to the south of Coffee Creek."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Bathyglyptus,n. gen.,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,08/02/2003 15:13,10/05/2016 09:07,7693,theodori,Bathyglyptus,7693,n. sp.,279.3,272.3,Kungurian,,1,US,Bathyglyptus theodori
296133,occ,NA,,28276,,Lysorophus sp.,genus,37322,,Lysorophus,NA,genus,37322,Romer,1928,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,specimens,-99.260002,33.594166,"Dead Man's Creek, 43 (Arroyo Formation)",NA,"Locality 43 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""on the south side of the Big Wichita."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Seymour.",gp_mid,-29.05,1.64,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""the highest horizon in which Permian vertebrate remains have been found in Texas... probably 250 to 300 feet above the base of the Clear Fork, although the horizon cannot be stated with certainty."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,09/02/2003 13:39,09/02/2003 15:39,7693,sp.,Lysorophus,7693,,279.3,272.3,Kungurian,,1,US,Lysorophus sp.
296134,occ,NA,,28276,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-99.260002,33.594166,"Dead Man's Creek, 43 (Arroyo Formation)",NA,"Locality 43 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""on the south side of the Big Wichita."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Seymour.",gp_mid,-29.05,1.64,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""the highest horizon in which Permian vertebrate remains have been found in Texas... probably 250 to 300 feet above the base of the Clear Fork, although the horizon cannot be stated with certainty."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,09/02/2003 13:39,09/02/2003 15:39,7693,sp.,Ophiacodon,7693,,279.3,272.3,Kungurian,,1,US,Ophiacodon sp.
296135,occ,NA,,28277,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-99.260002,33.594166,"Soap Creek, 44 (Arroyo Formation)",NA,"Locality 43 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""on the south side of the Big Wichita."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Seymour.",gp_mid,-29.05,1.64,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""the highest horizon in which Permian vertebrate remains have been found in Texas... probably 250 to 300 feet above the base of the Clear Fork, although the horizon cannot be stated with certainty."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,09/02/2003 13:40,09/02/2003 15:40,7693,sp.,Eryops,7693,,279.3,272.3,Kungurian,,1,US,Eryops sp.
296136,occ,NA,,28277,,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Romer,1928,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,specimens,-99.260002,33.594166,"Soap Creek, 44 (Arroyo Formation)",NA,"Locality 43 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""on the south side of the Big Wichita."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Seymour.",gp_mid,-29.05,1.64,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""the highest horizon in which Permian vertebrate remains have been found in Texas... probably 250 to 300 feet above the base of the Clear Fork, although the horizon cannot be stated with certainty."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,09/02/2003 13:40,09/02/2003 15:40,7693,sp.,Diplocaulus,7693,,279.3,272.3,Kungurian,,1,US,Diplocaulus sp.
296137,occ,NA,,28277,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-99.260002,33.594166,"Soap Creek, 44 (Arroyo Formation)",NA,"Locality 43 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""on the south side of the Big Wichita."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Seymour.",gp_mid,-29.05,1.64,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""the highest horizon in which Permian vertebrate remains have been found in Texas... probably 250 to 300 feet above the base of the Clear Fork, although the horizon cannot be stated with certainty."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,09/02/2003 13:40,09/02/2003 15:40,7693,sp.,Ophiacodon,7693,,279.3,272.3,Kungurian,,1,US,Ophiacodon sp.
296138,occ,NA,,28256,,Zatrachys n. sp. conchigerus,species,345926,nomen dubium,Temnospondyli,NA,unranked clade,36320,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,NA,NA,NA,NA,,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,09/02/2003 13:46,10/04/2009 14:19,17702,conchigerus,,7693,n. sp.,279.3,272.3,Kungurian,,NA,US, conchigerus
296139,occ,NA,,28324,,Cricotus n. sp. crassidiscus,species,309860,,Cricotus crassidiscus,NA,species,309860,Cope,1884,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37197,NA,NA,NA,specimens,-98.625275,33.595554,"North Fork of the Little Wichita, 8",NA,"Locality 8 (Romer 1928), Zone 0 or Zone 1, Texas red-beds, redbeds, Putnam or Admiral Formation, Boll, Cummins",US,Texas,Archer,based on nearby landmark,seconds,local area,"""collected by Boll and Cummins are known to have been obtained from the lower portion of the course of this stream [North Fork], but cannot be exactly located."" See detailed locality map in Romer 1928. Lat long is for Archer City.",gp_mid,-30.08,-1.33,101,US,,,,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: ""Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group- boundary is at the top of the Coleman Junction Limestone.""close to the line of the Coleman Junction."" Cisco Group is Pennsylvanian. Details for Zone 1: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Putnam is Sakmarian and the Admiral Artinskian (Wardlaw 2005, Permophiles)",,claystone,red,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection",AMNH,,,,Cope,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cricotus,,NA,NA,vertebrate,E. D. Cope. 1884. Fifth contribution to the knowledge of the fauna of the Permian formation of Texas and the Indian Territory. Paleontological Bulletin 39:28-47,4,76,14,J. Alroy,R. Whatley,M. Carrano,09/02/2003 14:23,24/11/2014 13:56,28847,crassidiscus,Cricotus,28847,n. sp.,295.5,279.3,Sakmarian,Artinskian,1,US,Cricotus crassidiscus
296140,occ,NA,,28324,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-98.625275,33.595554,"North Fork of the Little Wichita, 8",NA,"Locality 8 (Romer 1928), Zone 0 or Zone 1, Texas red-beds, redbeds, Putnam or Admiral Formation, Boll, Cummins",US,Texas,Archer,based on nearby landmark,seconds,local area,"""collected by Boll and Cummins are known to have been obtained from the lower portion of the course of this stream [North Fork], but cannot be exactly located."" See detailed locality map in Romer 1928. Lat long is for Archer City.",gp_mid,-30.08,-1.33,101,US,,,,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: ""Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group- boundary is at the top of the Coleman Junction Limestone.""close to the line of the Coleman Junction."" Cisco Group is Pennsylvanian. Details for Zone 1: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Putnam is Sakmarian and the Admiral Artinskian (Wardlaw 2005, Permophiles)",,claystone,red,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection",AMNH,,,,Cope,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,09/02/2003 14:23,24/11/2014 13:56,28847,sp.,Eryops,7693,,295.5,279.3,Sakmarian,Artinskian,6,US,Eryops sp.
296141,occ,NA,,28324,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-98.625275,33.595554,"North Fork of the Little Wichita, 8",NA,"Locality 8 (Romer 1928), Zone 0 or Zone 1, Texas red-beds, redbeds, Putnam or Admiral Formation, Boll, Cummins",US,Texas,Archer,based on nearby landmark,seconds,local area,"""collected by Boll and Cummins are known to have been obtained from the lower portion of the course of this stream [North Fork], but cannot be exactly located."" See detailed locality map in Romer 1928. Lat long is for Archer City.",gp_mid,-30.08,-1.33,101,US,,,,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: ""Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group- boundary is at the top of the Coleman Junction Limestone.""close to the line of the Coleman Junction."" Cisco Group is Pennsylvanian. Details for Zone 1: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Putnam is Sakmarian and the Admiral Artinskian (Wardlaw 2005, Permophiles)",,claystone,red,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection",AMNH,,,,Cope,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,09/02/2003 14:23,24/11/2014 13:56,28847,sp.,Trimerorhachis,7693,,295.5,279.3,Sakmarian,Artinskian,1,US,Trimerorhachis sp.
296142,occ,NA,,28324,,Diadectes n. sp. phaseolinus,species,320988,subjective synonym of,Diadectes sideropelicus,NA,species,320982,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,specimens,-98.625275,33.595554,"North Fork of the Little Wichita, 8",NA,"Locality 8 (Romer 1928), Zone 0 or Zone 1, Texas red-beds, redbeds, Putnam or Admiral Formation, Boll, Cummins",US,Texas,Archer,based on nearby landmark,seconds,local area,"""collected by Boll and Cummins are known to have been obtained from the lower portion of the course of this stream [North Fork], but cannot be exactly located."" See detailed locality map in Romer 1928. Lat long is for Archer City.",gp_mid,-30.08,-1.33,101,US,,,,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: ""Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group- boundary is at the top of the Coleman Junction Limestone.""close to the line of the Coleman Junction."" Cisco Group is Pennsylvanian. Details for Zone 1: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Putnam is Sakmarian and the Admiral Artinskian (Wardlaw 2005, Permophiles)",,claystone,red,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection",AMNH,,,,Cope,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,09/02/2003 14:23,24/11/2014 13:56,28847,phaseolinus,Diadectes,7693,n. sp.,295.5,279.3,Sakmarian,Artinskian,3,US,Diadectes phaseolinus
296144,occ,NA,,28324,,n. gen. Pariotichus n. sp. brachyops,species,136938,,Pariotichus brachyops,NA,species,136938,Romer,1928,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37299,NA,NA,NA,specimens,-98.625275,33.595554,"North Fork of the Little Wichita, 8",NA,"Locality 8 (Romer 1928), Zone 0 or Zone 1, Texas red-beds, redbeds, Putnam or Admiral Formation, Boll, Cummins",US,Texas,Archer,based on nearby landmark,seconds,local area,"""collected by Boll and Cummins are known to have been obtained from the lower portion of the course of this stream [North Fork], but cannot be exactly located."" See detailed locality map in Romer 1928. Lat long is for Archer City.",gp_mid,-30.08,-1.33,101,US,,,,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: ""Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group- boundary is at the top of the Coleman Junction Limestone.""close to the line of the Coleman Junction."" Cisco Group is Pennsylvanian. Details for Zone 1: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Putnam is Sakmarian and the Admiral Artinskian (Wardlaw 2005, Permophiles)",,claystone,red,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection",AMNH,,,,Cope,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Pariotichus,n. gen.,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,09/02/2003 14:23,24/11/2014 13:56,28847,brachyops,Pariotichus,7693,n. sp.,295.5,279.3,Sakmarian,Artinskian,1,US,Pariotichus brachyops
296145,occ,NA,,28324,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-98.625275,33.595554,"North Fork of the Little Wichita, 8",NA,"Locality 8 (Romer 1928), Zone 0 or Zone 1, Texas red-beds, redbeds, Putnam or Admiral Formation, Boll, Cummins",US,Texas,Archer,based on nearby landmark,seconds,local area,"""collected by Boll and Cummins are known to have been obtained from the lower portion of the course of this stream [North Fork], but cannot be exactly located."" See detailed locality map in Romer 1928. Lat long is for Archer City.",gp_mid,-30.08,-1.33,101,US,,,,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: ""Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group- boundary is at the top of the Coleman Junction Limestone.""close to the line of the Coleman Junction."" Cisco Group is Pennsylvanian. Details for Zone 1: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Putnam is Sakmarian and the Admiral Artinskian (Wardlaw 2005, Permophiles)",,claystone,red,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection",AMNH,,,,Cope,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,14,J. Alroy,R. Whatley,M. Carrano,09/02/2003 14:23,24/11/2014 13:56,28847,sp.,Dimetrodon,7693,,295.5,279.3,Sakmarian,Artinskian,3,US,Dimetrodon sp.
296146,occ,NA,,28256,,Alegeinosaurus sp.,genus,37018,,Alegeinosaurus,NA,genus,37018,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37018,NA,NA,NA,specimens,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Alegeinosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,09/02/2003 14:33,10/04/2009 14:19,17702,sp.,Alegeinosaurus,7693,,279.3,272.3,Kungurian,,1,US,Alegeinosaurus sp.
296147,occ,NA,,28256,,Anisodexis sp.,genus,309177,,Anisodexis,NA,genus,309177,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,309177,NA,NA,NA,specimens,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Anisodexis,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,09/02/2003 14:33,10/04/2009 14:19,17702,sp.,Anisodexis,7693,,279.3,272.3,Kungurian,,1,US,Anisodexis sp.
296148,occ,NA,,28256,,Acheloma sp.,genus,37048,,Acheloma,NA,genus,37048,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,37048,NA,NA,NA,specimens,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Acheloma,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,09/02/2003 14:33,29/01/2010 07:08,17702,sp.,Acheloma,7693,,279.3,272.3,Kungurian,,1,US,Acheloma sp.
296149,occ,NA,R,28275,,Gymnarthrus sp.,genus,137380,subjective synonym of,Cardiocephalus,NA,genus,37294,Romer,1928,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37294,NA,NA,NA,specimens,-99.195557,33.973057,"Beaver Creek, 42 (Arroyo Formation)",NA,"Locality 42 (Romer 1928), Beaver Creek Wilbarger County, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Wilbarger,based on nearby landmark,seconds,outcrop,"""The upper reaches of the stream have yielded a few remains."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Beaver Creek.",gp_mid,-28.81,1.94,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""above the Lueders limestone, and quite probably correspond to the beds to the south of Coffee Creek."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Gymnarthrus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,697,J. Alroy,R. Whatley,E. Dunne,09/02/2003 14:44,12/08/2016 10:53,7693,sp.,Cardiocephalus,7693,,279.3,272.3,Kungurian,,1,US,Cardiocephalus sp.
296149,occ,21172,,28275,,Gymnarthrus willoughbyi,species,137382,subjective synonym of,Cardiocephalus sternbergi,NA,species,90715,Gregory et al.,1956,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37294,NA,NA,NA,specimens,-99.195557,33.973057,"Beaver Creek, 42 (Arroyo Formation)",NA,"Locality 42 (Romer 1928), Beaver Creek Wilbarger County, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Wilbarger,based on nearby landmark,seconds,outcrop,"""The upper reaches of the stream have yielded a few remains."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Beaver Creek.",gp_mid,-28.81,1.94,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""above the Lueders limestone, and quite probably correspond to the beds to the south of Coffee Creek."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Gymnarthrus,,NA,NA,vertebrate,"J. T. Gregory, F. E. Peabody, and L. I. Price. 1956. Revision of the Gymnarthridae - American Permian Microsaurs. Bulletin of the Peabody Museum of Natural History 10:1-77",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,09/12/2008 17:07,09/12/2008 19:08,7693,willoughbyi,Cardiocephalus,28484,,279.3,272.3,Kungurian,,1,US,Cardiocephalus willoughbyi
296150,occ,NA,,28261,,Isodectes sp.,genus,36983,,Isodectes,NA,genus,36983,Romer,1928,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Saurerpetontidae,36980,36983,NA,NA,NA,specimens,-99.144997,33.755001,"Pony Creek, 36 (Arroyo Formation)",NA,"Locality 36 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""A tributary of the Big Wichita on the south side, north of Seymour; the collections were made near the head of the creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Kemp Lake. Numbered ""36"" with taxonomic list and on map, but is incorrectly numbered ""35"" in text.",gp_mid,-28.88,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably about 100 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Isodectes,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,4,76,0,J. Alroy,R. Whatley,,09/02/2003 14:46,09/02/2003 16:46,7693,sp.,Isodectes,7693,,279.3,272.3,Kungurian,,1,US,Isodectes sp.
296595,occ,NA,,28394,,Zatrachys serratus,species,255221,,Zatrachys serratus,NA,species,255221,Olson,1965,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,specimens,-97.049721,34.874168,"Byars, McClain County (""Gearyan strata"")",NA,,US,Oklahoma,McClain,based on nearby landmark,seconds,,"SW 1/4 SW 1/4 sec. 33, T 5 N, R 2 E, 3 miles southwest of Byars, McClain County. Lat long is for Byars.",gp_mid,-28.26,-0.85,101,US,,,,,,,,,,,,NA,"""Gearyan strata""\r\nWolfcamp = Asselian to Sakmarian according to Harland et al. 1989",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,"E. C. Olson. 1965. Zatrachys serratus Cope (Amphibia; labyrinthodontia) from McClain County, Oklahoma. Oklahoma Geology Notes 25(4):91-97",4,76,0,J. Alroy,R. Whatley,,11/02/2003 14:42,11/02/2003 16:42,7820,serratus,Zatrachys,7820,,296.4,268,Wolfcamp,,1,US,Zatrachys serratus
296596,occ,NA,,28394,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Olson,1965,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-97.049721,34.874168,"Byars, McClain County (""Gearyan strata"")",NA,,US,Oklahoma,McClain,based on nearby landmark,seconds,,"SW 1/4 SW 1/4 sec. 33, T 5 N, R 2 E, 3 miles southwest of Byars, McClain County. Lat long is for Byars.",gp_mid,-28.26,-0.85,101,US,,,,,,,,,,,,NA,"""Gearyan strata""\r\nWolfcamp = Asselian to Sakmarian according to Harland et al. 1989",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"E. C. Olson. 1965. Zatrachys serratus Cope (Amphibia; labyrinthodontia) from McClain County, Oklahoma. Oklahoma Geology Notes 25(4):91-97",4,76,0,J. Alroy,R. Whatley,,11/02/2003 14:42,11/02/2003 16:42,7820,sp.,Diadectes,7820,,296.4,268,Wolfcamp,,NA,US,Diadectes sp.
297321,occ,NA,,28463,,cf. Branchiosaurus petrolei,species,358775,,Branchiosaurus petrolei,NA,species,358774,Ronchi and Tintori,1997,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37039,NA,NA,NA,,9.2,40.200001,"Perdasdefogu Basin Level D, Sardinia",NA,,IT,Sardinia,Ogliastra region,based on nearby landmark,minutes,local area,"Level D corresponds to 7.5 cm bed in a half meter lucustrine sequence (see amphibian-bearing stratigraphic sequence, Fig. 2) occurring in the 20 square Km Perdasdefogu Basin, Ogliastra region, SE Sardinia. Lat long is for Barbagia.",gp_mid,NA,NA,coordinates not computable using this model,IT,,,,,bed,,,Level D,bottom to top,Perdasdefogu Basin,,NA,"""The amphibian-bearing bed [half meter total] possibly belongs to the upper part of the lower lacustrine sequence; the outcrop conditions and a nearby fault make it difficult to give this thin sequence a more precise stratigraphic attribution."" Level D is 7.5 cm thick","D. Gray, cohesive, laminated shale andsiltstone.","""shale""","planar lamination,gray",,,Y,siltstone,"planar lamination,gray",,,Y,pond,intramontane basin,"""swampy or shallow pond environment...palustrine habitat rich in organic matter, a few centimeters deep in which plants grew....millimetrical black volcanic glass levels alternating with white dolomitic ones"" suggesting regular pyroclastic episodes ""deposited in a quite subaqueous environment."" ",macrofossils,,,,,,NA,,body,poor,,,,,life position,,,,NA,,,taxonomic,field collection,,some macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchiosaurus,cf.,NA,NA,vertebrate,A. Ronchi and A. Tintori. 1997. First amphibian find in Early Permian from Sardinia (Italy). Rivista Italiana di Paleontologia e Stratigrafia 103(1):29-38,4,76,0,J. Alroy,R. Whatley,,14/02/2003 15:47,14/02/2003 17:47,7845,petrolei,Branchiosaurus,7845,,298.9,252.17,Autunian,Permian,NA,IT,Branchiosaurus petrolei
297323,occ,NA,,28464,,cf. Branchiosaurus petrolei,species,358775,,Branchiosaurus petrolei,NA,species,358774,Ronchi and Tintori,1997,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37039,NA,NA,NA,,9.2,40.200001,"Perdasdefogu Basin Level E, Sardinia",NA,,IT,Sardinia,Ogliastra region,based on nearby landmark,minutes,local area,"Level E corresponds to 9 cm bed in a half meter lucustrine sequence (see amphibian-bearing stratigraphic sequence, Fig. 2) occurring in the 20 square Km Perdasdefogu Basin, Ogliastra region, SE Sardinia. Lat long is for Barbagia.",gp_mid,NA,NA,coordinates not computable using this model,IT,,,,,bed,,,Level E,bottom to top,Perdasdefogu Basin,,NA,"""The amphibian-bearing bed [half meter total] possibly belongs to the upper part of the lower lacustrine sequence; the outcrop conditions and a nearby fault make it difficult to give this thin sequence a more precise stratigraphic attribution."" Level E is 9 cm thick.",E. Black coal bearing varved shale and siltstone with very thin laminae. ,"""shale""","planar lamination,black",,,Y,siltstone,"planar lamination,black",,,Y,pond,intramontane basin,"""swampy or shallow pond environment...palustrine habitat rich in organic matter, a few centimeters deep in which plants grew....millimetrical black volcanic glass levels alternating with white dolomitic ones"" suggesting regular pyroclastic episodes ""deposited in a quite subaqueous environment.""",,,,,,,NA,,body,poor,,snapshot,,#NAME?,life position,,well,,NA,,"""In this very fissile level there are at least two small layers with amphibian mass mortality multi-events. Scattered specimens have been found also throughout the bed together with plant remains....repeated mass-mortality events. The lack of sedimentary traces of desiccation, suggests that the basin bottom must have remained submerged."" Two event beds made up almost exclusively of fully articulated specimens of B. petrolei with no dessication-related distortion- mortality possibly caused by changes in water chemistry.",taxonomic,field collection,,some macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchiosaurus,cf.,NA,NA,vertebrate,A. Ronchi and A. Tintori. 1997. First amphibian find in Early Permian from Sardinia (Italy). Rivista Italiana di Paleontologia e Stratigrafia 103(1):29-38,4,76,0,J. Alroy,R. Whatley,,14/02/2003 15:54,14/02/2003 17:54,7845,petrolei,Branchiosaurus,7845,,298.9,252.17,Autunian,Permian,NA,IT,Branchiosaurus petrolei
297325,occ,NA,,28465,,cf. Branchiosaurus petrolei,species,358775,,Branchiosaurus petrolei,NA,species,358774,Ronchi and Tintori,1997,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37039,NA,NA,NA,,9.2,40.200001,"Perdasdefogu Basin Level G, Sardinia",NA,,IT,Sardinia,Ogliastra region,based on nearby landmark,minutes,local area,"Level G corresponds to 20 cm bed in a half meter lucustrine sequence (see amphibian-bearing stratigraphic sequence, Fig. 2) occurring in the 20 square Km Perdasdefogu Basin, Ogliastra region, SE Sardinia. Lat long is for Barbagia.",gp_mid,NA,NA,coordinates not computable using this model,IT,,,,,bed,,,Level G,bottom to top,Perdasdefogu Basin,,NA,"""The amphibian-bearing bed [half meter total] possibly belongs to the upper part of the lower lacustrine sequence; the outcrop conditions and a nearby fault make it difficult to give this thin sequence a more precise stratigraphic attribution."" Level D is 7.5 cm thick.","G. Light-gray laminated shale passing to siltstone toward the top, yielding very rare amphibians and more frequent floral remains. 20 cm thick.","""shale""","planar lamination,gray",,,,sandstone,"planar lamination,gray",,,,pond,intramontane basin,"""swampy or shallow pond environment...palustrine habitat rich in organic matter, a few centimeters deep in which plants grew....millimetrical black volcanic glass levels alternating with white dolomitic ones"" suggesting regular pyroclastic episodes ""deposited in a quite subaqueous environment.""",macrofossils,,,,,,NA,,body,poor,,,,,,,,,NA,,,taxonomic,field collection,,some macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchiosaurus,cf.,NA,NA,vertebrate,A. Ronchi and A. Tintori. 1997. First amphibian find in Early Permian from Sardinia (Italy). Rivista Italiana di Paleontologia e Stratigrafia 103(1):29-38,4,76,0,J. Alroy,R. Whatley,,14/02/2003 15:58,14/02/2003 17:58,7845,petrolei,Branchiosaurus,7845,,298.9,252.17,Autunian,Permian,NA,IT,Branchiosaurus petrolei
297327,occ,NA,,28466,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Vaughn,1958,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-80.482498,39.725834,One mile north of Ned (Dunkard Series),NA,,US,Pennsylvania,Greene,based on nearby landmark,seconds,small collection,"One mile north of Ned, in the southwesternmost part of Greene County, Pennsylvania. Lat long is for Ned.",gp_mid,-14.52,-2.63,101,US,,Greene,Dunkard,,bed,,,,,,,NA,""" [...] high in the Greene group, Dunkard series [...] "" (Vaughn, 1958).\r\nNotes: The ""Green group"" today has formational rank and the ""Dunkard series"" has group status (in the original entry the hierarchy of the lithostratigraphic units was erroneously reversed which has been corrected; TL).\r\nThe age of the Greene Fm. is not well constrained. Vaughn (1958), based on Romer (1952, Ann. Carneg. Mus. 33), states that the ""Dunkard series is probably roughly equivalent in age to the Wichita group, lower Permian of Texas."" Here, chronostratigraphy is based on correlation chart (fig. 4) in Wellstead (1991, Bull. AMNH 209) (original entry was >>Cisuralian<<; TL). ","""fresh-water limestone"" (Vaughn, 1958).","""limestone""",,,,Y,,,,,,lacustrine indet.,foreland basin,"""...a flat, well-watered coastal region with abundant swamps and lagoons..."" (Romer [1952, Ann. Carneg. Mus. 33] cited in Vaughn, 1958).\r\nNote: originally selected environment >>coastal indet.<< is replaced by >>lacustrine indet.<< (TL).",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,skull is crushed,taxonomic,survey of museum collection,USNM,,,,"J. J. Burke, W. E. Moran",1953,,Carnegie museum type specimen of Glaukerpeton avinoffi (No. 8593) is referred to Eryops based on comparison with the Dunkard Series specimen (U.S.N.M. No. 21860). ,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,P. P. Vaughn. 1958. On the geologic range of the labyrinthodont amphibian Eryops. Journal of Paleontology 32(5):918-922,4,76,0,J. Alroy,R. Whatley,,14/02/2003 16:59,14/02/2003 18:59,7822,sp.,Eryops,7822,,295.5,290.1,Sakmarian,,1,US,Eryops sp.
297336,occ,NA,R,28480,,Bolosaurus n. sp. traati,species,161883,,Bolosaurus traati,NA,species,161883,Tatarinov,1974,Chordata,33815,Reptilia,36322,,NA,Bolosauridae,37510,37511,NA,NA,NA,elements,55.182499,62.115002,"Shakhovykh homestead, Yuzhnaya Mylva River",NA,,RU,Komi,Ust'-Kulom,based on nearby landmark,seconds,small collection,"Komi ASSR, headwaters of Yuzhnaya Mylva River, outcrop below Shakhovykh homestead. Lat long is for Shakhovykh.",gp_mid,36.65,28.73,302,RU,,,,,bed,,,,,,,NA,"Specimen is correlated to the occurrence of Bolosaurs from the ""lower part of the Wichita Formation (basal part of the continental Lower Permian) of Texas.""",,"""limestone""",dolomitic,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,PIN,,,,Kh. O. Traat,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Bolosaurus,,NA,NA,vertebrate,L. P. Tatarinov. 1974. Discovery of a bolosaur in the Lower Permian of the USSR. Paleontological Journal 8(2):250-252,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,16/02/2003 13:51,19/01/2010 18:12,7855,traati,Bolosaurus,7855,n. sp.,298.9,295.5,Asselian,,1,RU,Bolosaurus traati
297336,occ,21670,,28480,,Bolosauridae indet.,family,37510,,Bolosauridae,NA,family,37510,Modesto and Rybczynski,2000,Chordata,33815,Reptilia,36322,,NA,Bolosauridae,37510,NA,NA,NA,NA,elements,55.182499,62.115002,"Shakhovykh homestead, Yuzhnaya Mylva River",NA,,RU,Komi,Ust'-Kulom,based on nearby landmark,seconds,small collection,"Komi ASSR, headwaters of Yuzhnaya Mylva River, outcrop below Shakhovykh homestead. Lat long is for Shakhovykh.",gp_mid,36.65,28.73,302,RU,,,,,bed,,,,,,,NA,"Specimen is correlated to the occurrence of Bolosaurs from the ""lower part of the Wichita Formation (basal part of the continental Lower Permian) of Texas.""",,"""limestone""",dolomitic,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,PIN,,,,Kh. O. Traat,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Bolosauridae,,NA,NA,vertebrate,"S. P. Modesto and N. Rybczynski. 2000. The amniote faunas of the Russian Permian: implications for Late Permian terrestrial vertebrate biogeography. In M. J. Benton, M. A. Shishkin, D. M. Unwin & E. N. Kurochkin (eds.), The Age of Dinosaurs in Russia and Mongolia, Cambridge University Press ",315,334,0,J. Mueller,T. Liebrecht,,16/04/2009 17:43,16/04/2009 19:43,7855,indet.,,28429,,298.9,295.5,Asselian,,1,RU, indet.
297337,occ,NA,R,28069,,Hylonomus lyelli,species,139093,,Hylonomus lyelli,NA,species,139093,Owen,1862,Chordata,33815,Reptilia,36322,,NA,Protorothyrididae,37486,37492,NA,NA,NA,specimens,-64.451385,45.698612,"Coal Mine Point; Divison 4, Section XV, coal-group 15",NA,South Joggins; Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Cliffs called the South Joggins (coast), about half a mile eastward of the Coal Pier.",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XV",coal-group 15,,,,NA,"From Steen (1934): ""top of the Joggins formation...Division 4, Section XV., Coal-group 15 of the Joggins section given in Dawson's 'Acadian Geology,' 1868, pp. 156-178."" From Lyell (1853): The fossils are from Bed 5 of a 25 ft section, composed of 7 beds. Bed 5 is approximately 600 ft below the main coal, ""King's Vein"".\r\nOriginal entry for Local Section name was ""South Joggins""; for Bed/horizon ""bed 5"". In Steen (1934) a ""bed 5"" is not mentioned in any way. Also, in papers published before and after Lyell's ""On the Remains of a Reptile..."" (1953) a different numbering is applied to the Joggins Section. Thus, it is more appropriate to follow the stratigraphic terminology used in Dawson (1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173), Steen (1934, see description above) and Carroll (1964). Coal-group 15 consists of 3 beds with a total thickness of 10 ft 6 in. (Dawson, 1878) (TL) \r\nOriginal entry for chronostratigraphy was simply ""Westphalian"". Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","From Lyell (1853): 5. Grey sandstone, with three erect trees, one having Stigmarian roots; erect Calamites and stems of unknown plants. (One of the erect trees in this bed contained the bones, teeth, &c. and land-shell above-mentioned.) ...9 ft;\r\n",sandstone,gray,,,Y,coal,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",good,,snapshot,,,,,,occasional,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" ",taxonomic,"bulk,selective quarrying,field collection,survey of museum collection",BMNH,,,,"J. W. Dawson, C. Lyell, among others",,"RM = Redpath Museum of McGill Unversity, Montreal","Listed by Steen (1934) as Indeterminate species: Hylerpeton dawsoni Owen; Hylerpeton longidentatum Dawson; Hylerpeton intermedium Dawson; Hylonomus multidens Dawson; Hylonomus wymani Dawson; Smilerpeton aciedentatus Dawson; Amblyodon problematicum Dawson; Sparodus sp. Dawson; Baphetes minor Dawson.\r\n\r\nAll catalogue numbers are from Steen (1934) and/or from Carroll (1967).\r\n\r\nThe taxon ""Batrachoididae indet."", entered under the reference Lyell & Dawson (1853), has been removed from the taxonomic list for it is a family of teleost fish. It probably referred to the ""batrachian"" affinities of the tetrapod bones noticed by Wyman (1853) but all these bones finally were assigned to Dendrerpeton acadianum n. gen. et sp. (see pls. II and III in Lyell & Dawson/Wyman/Owen, 1853). Thus the originally enterd taxon ""Dendrerpeton acadianum"", reference: Lyell & Dawson, was replaced by ""Batrachia indet."", reference: Wyman (1853), and re-identification by Owen (1853) was added (TL).\r\nRe-identification of ""Dendrerpeton oweni n. sp."" as ""Dendrerpeton acadianum"" by by Steen was removed after opinons on synonymy of the the former with the latter species were entered into the database (TL).",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Hylonomus,,NA,NA,vertebrate,"R. Owen. 1862. Description of Specimens of Fossil Reptilia discovered in the Coal-measures of the South Joggins, Nova Scotia, by Dr. J. W. Dawson, FGS, etc. Quarterly Journal of the Geological Society of London 18:238-244",4,76,697,J. Alroy,R. Whatley,E. Dunne,16/02/2003 15:59,20/01/2016 04:56,7856,lyelli,Hylonomus,32316,,318.1,314.6,Westphalian A,,1,CA,Hylonomus lyelli
297337,occ,10231,,28069,,Dendrerpeton n. sp. oweni,species,164850,subjective synonym of,Dendrerpeton acadianum,NA,species,164775,Dawson,1863,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dendrerpetonidae,36994,36995,NA,NA,NA,specimens,-64.451385,45.698612,"Coal Mine Point; Divison 4, Section XV, coal-group 15",NA,South Joggins; Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Cliffs called the South Joggins (coast), about half a mile eastward of the Coal Pier.",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XV",coal-group 15,,,,NA,"From Steen (1934): ""top of the Joggins formation...Division 4, Section XV., Coal-group 15 of the Joggins section given in Dawson's 'Acadian Geology,' 1868, pp. 156-178."" From Lyell (1853): The fossils are from Bed 5 of a 25 ft section, composed of 7 beds. Bed 5 is approximately 600 ft below the main coal, ""King's Vein"".\r\nOriginal entry for Local Section name was ""South Joggins""; for Bed/horizon ""bed 5"". In Steen (1934) a ""bed 5"" is not mentioned in any way. Also, in papers published before and after Lyell's ""On the Remains of a Reptile..."" (1953) a different numbering is applied to the Joggins Section. Thus, it is more appropriate to follow the stratigraphic terminology used in Dawson (1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173), Steen (1934, see description above) and Carroll (1964). Coal-group 15 consists of 3 beds with a total thickness of 10 ft 6 in. (Dawson, 1878) (TL) \r\nOriginal entry for chronostratigraphy was simply ""Westphalian"". Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","From Lyell (1853): 5. Grey sandstone, with three erect trees, one having Stigmarian roots; erect Calamites and stems of unknown plants. (One of the erect trees in this bed contained the bones, teeth, &c. and land-shell above-mentioned.) ...9 ft;\r\n",sandstone,gray,,,Y,coal,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",good,,snapshot,,,,,,occasional,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" ",taxonomic,"bulk,selective quarrying,field collection,survey of museum collection",BMNH,,,,"J. W. Dawson, C. Lyell, among others",,"RM = Redpath Museum of McGill Unversity, Montreal","Listed by Steen (1934) as Indeterminate species: Hylerpeton dawsoni Owen; Hylerpeton longidentatum Dawson; Hylerpeton intermedium Dawson; Hylonomus multidens Dawson; Hylonomus wymani Dawson; Smilerpeton aciedentatus Dawson; Amblyodon problematicum Dawson; Sparodus sp. Dawson; Baphetes minor Dawson.\r\n\r\nAll catalogue numbers are from Steen (1934) and/or from Carroll (1967).\r\n\r\nThe taxon ""Batrachoididae indet."", entered under the reference Lyell & Dawson (1853), has been removed from the taxonomic list for it is a family of teleost fish. It probably referred to the ""batrachian"" affinities of the tetrapod bones noticed by Wyman (1853) but all these bones finally were assigned to Dendrerpeton acadianum n. gen. et sp. (see pls. II and III in Lyell & Dawson/Wyman/Owen, 1853). Thus the originally enterd taxon ""Dendrerpeton acadianum"", reference: Lyell & Dawson, was replaced by ""Batrachia indet."", reference: Wyman (1853), and re-identification by Owen (1853) was added (TL).\r\nRe-identification of ""Dendrerpeton oweni n. sp."" as ""Dendrerpeton acadianum"" by by Steen was removed after opinons on synonymy of the the former with the latter species were entered into the database (TL).","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Dendrerpeton,,NA,NA,vertebrate,"J. W. Dawson. 1863. Notice of a New Species of Dendrerpeton, and of the Dermal Coverings of certain Carboniferous Reptiles. Quarterly Journal of the Geological Society of London 19:469-473",4,76,334,J. Alroy,R. Whatley,T. Liebrecht,16/02/2003 16:00,16/03/2010 00:05,7856,oweni,Dendrerpeton,32315,n. sp.,318.1,314.6,Westphalian A,,1,CA,Dendrerpeton oweni
297339,occ,NA,,28069,,n. gen. Dendrysekos n. sp. helogenes,species,336663,,Dendrysekos helogenes,NA,species,336663,Steen,1934,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dendrerpetonidae,36994,336660,NA,NA,NA,specimens,-64.451385,45.698612,"Coal Mine Point; Divison 4, Section XV, coal-group 15",NA,South Joggins; Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Cliffs called the South Joggins (coast), about half a mile eastward of the Coal Pier.",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XV",coal-group 15,,,,NA,"From Steen (1934): ""top of the Joggins formation...Division 4, Section XV., Coal-group 15 of the Joggins section given in Dawson's 'Acadian Geology,' 1868, pp. 156-178."" From Lyell (1853): The fossils are from Bed 5 of a 25 ft section, composed of 7 beds. Bed 5 is approximately 600 ft below the main coal, ""King's Vein"".\r\nOriginal entry for Local Section name was ""South Joggins""; for Bed/horizon ""bed 5"". In Steen (1934) a ""bed 5"" is not mentioned in any way. Also, in papers published before and after Lyell's ""On the Remains of a Reptile..."" (1953) a different numbering is applied to the Joggins Section. Thus, it is more appropriate to follow the stratigraphic terminology used in Dawson (1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173), Steen (1934, see description above) and Carroll (1964). Coal-group 15 consists of 3 beds with a total thickness of 10 ft 6 in. (Dawson, 1878) (TL) \r\nOriginal entry for chronostratigraphy was simply ""Westphalian"". Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","From Lyell (1853): 5. Grey sandstone, with three erect trees, one having Stigmarian roots; erect Calamites and stems of unknown plants. (One of the erect trees in this bed contained the bones, teeth, &c. and land-shell above-mentioned.) ...9 ft;\r\n",sandstone,gray,,,Y,coal,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",good,,snapshot,,,,,,occasional,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" ",taxonomic,"bulk,selective quarrying,field collection,survey of museum collection",BMNH,,,,"J. W. Dawson, C. Lyell, among others",,"RM = Redpath Museum of McGill Unversity, Montreal","Listed by Steen (1934) as Indeterminate species: Hylerpeton dawsoni Owen; Hylerpeton longidentatum Dawson; Hylerpeton intermedium Dawson; Hylonomus multidens Dawson; Hylonomus wymani Dawson; Smilerpeton aciedentatus Dawson; Amblyodon problematicum Dawson; Sparodus sp. Dawson; Baphetes minor Dawson.\r\n\r\nAll catalogue numbers are from Steen (1934) and/or from Carroll (1967).\r\n\r\nThe taxon ""Batrachoididae indet."", entered under the reference Lyell & Dawson (1853), has been removed from the taxonomic list for it is a family of teleost fish. It probably referred to the ""batrachian"" affinities of the tetrapod bones noticed by Wyman (1853) but all these bones finally were assigned to Dendrerpeton acadianum n. gen. et sp. (see pls. II and III in Lyell & Dawson/Wyman/Owen, 1853). Thus the originally enterd taxon ""Dendrerpeton acadianum"", reference: Lyell & Dawson, was replaced by ""Batrachia indet."", reference: Wyman (1853), and re-identification by Owen (1853) was added (TL).\r\nRe-identification of ""Dendrerpeton oweni n. sp."" as ""Dendrerpeton acadianum"" by by Steen was removed after opinons on synonymy of the the former with the latter species were entered into the database (TL).","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Dendrysekos,n. gen.,NA,NA,vertebrate,"M. C. Steen. 1934. The amphibian fauna from the South Joggins, Nova Scotia. Proceedings of the Zoological Society of London 1934:465-504",4,76,334,J. Alroy,R. Whatley,T. Liebrecht,16/02/2003 16:59,13/03/2010 21:28,7856,helogenes,Dendrysekos,7856,n. sp.,318.1,314.6,Westphalian A,,1,CA,Dendrysekos helogenes
297341,occ,NA,,28069,,n. gen. Calligenethlon n. sp. watsoni,species,320849,,Calligenethlon watsoni,NA,species,320849,Steen,1934,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37186,NA,NA,NA,specimens,-64.451385,45.698612,"Coal Mine Point; Divison 4, Section XV, coal-group 15",NA,South Joggins; Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Cliffs called the South Joggins (coast), about half a mile eastward of the Coal Pier.",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XV",coal-group 15,,,,NA,"From Steen (1934): ""top of the Joggins formation...Division 4, Section XV., Coal-group 15 of the Joggins section given in Dawson's 'Acadian Geology,' 1868, pp. 156-178."" From Lyell (1853): The fossils are from Bed 5 of a 25 ft section, composed of 7 beds. Bed 5 is approximately 600 ft below the main coal, ""King's Vein"".\r\nOriginal entry for Local Section name was ""South Joggins""; for Bed/horizon ""bed 5"". In Steen (1934) a ""bed 5"" is not mentioned in any way. Also, in papers published before and after Lyell's ""On the Remains of a Reptile..."" (1953) a different numbering is applied to the Joggins Section. Thus, it is more appropriate to follow the stratigraphic terminology used in Dawson (1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173), Steen (1934, see description above) and Carroll (1964). Coal-group 15 consists of 3 beds with a total thickness of 10 ft 6 in. (Dawson, 1878) (TL) \r\nOriginal entry for chronostratigraphy was simply ""Westphalian"". Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","From Lyell (1853): 5. Grey sandstone, with three erect trees, one having Stigmarian roots; erect Calamites and stems of unknown plants. (One of the erect trees in this bed contained the bones, teeth, &c. and land-shell above-mentioned.) ...9 ft;\r\n",sandstone,gray,,,Y,coal,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",good,,snapshot,,,,,,occasional,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" ",taxonomic,"bulk,selective quarrying,field collection,survey of museum collection",BMNH,,,,"J. W. Dawson, C. Lyell, among others",,"RM = Redpath Museum of McGill Unversity, Montreal","Listed by Steen (1934) as Indeterminate species: Hylerpeton dawsoni Owen; Hylerpeton longidentatum Dawson; Hylerpeton intermedium Dawson; Hylonomus multidens Dawson; Hylonomus wymani Dawson; Smilerpeton aciedentatus Dawson; Amblyodon problematicum Dawson; Sparodus sp. Dawson; Baphetes minor Dawson.\r\n\r\nAll catalogue numbers are from Steen (1934) and/or from Carroll (1967).\r\n\r\nThe taxon ""Batrachoididae indet."", entered under the reference Lyell & Dawson (1853), has been removed from the taxonomic list for it is a family of teleost fish. It probably referred to the ""batrachian"" affinities of the tetrapod bones noticed by Wyman (1853) but all these bones finally were assigned to Dendrerpeton acadianum n. gen. et sp. (see pls. II and III in Lyell & Dawson/Wyman/Owen, 1853). Thus the originally enterd taxon ""Dendrerpeton acadianum"", reference: Lyell & Dawson, was replaced by ""Batrachia indet."", reference: Wyman (1853), and re-identification by Owen (1853) was added (TL).\r\nRe-identification of ""Dendrerpeton oweni n. sp."" as ""Dendrerpeton acadianum"" by by Steen was removed after opinons on synonymy of the the former with the latter species were entered into the database (TL).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Calligenethlon,n. gen.,NA,NA,vertebrate,"M. C. Steen. 1934. The amphibian fauna from the South Joggins, Nova Scotia. Proceedings of the Zoological Society of London 1934:465-504",4,76,334,J. Alroy,R. Whatley,T. Liebrecht,16/02/2003 16:59,13/03/2010 21:28,7856,watsoni,Calligenethlon,7856,n. sp.,318.1,314.6,Westphalian A,,1,CA,Calligenethlon watsoni
297342,occ,NA,,28069,,n. gen. Hylonomus n. sp. lyelli,species,139093,,Hylonomus lyelli,NA,species,139093,Steen,1934,Chordata,33815,Reptilia,36322,,NA,Protorothyrididae,37486,37492,NA,NA,NA,specimens,-64.451385,45.698612,"Coal Mine Point; Divison 4, Section XV, coal-group 15",NA,South Joggins; Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Cliffs called the South Joggins (coast), about half a mile eastward of the Coal Pier.",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XV",coal-group 15,,,,NA,"From Steen (1934): ""top of the Joggins formation...Division 4, Section XV., Coal-group 15 of the Joggins section given in Dawson's 'Acadian Geology,' 1868, pp. 156-178."" From Lyell (1853): The fossils are from Bed 5 of a 25 ft section, composed of 7 beds. Bed 5 is approximately 600 ft below the main coal, ""King's Vein"".\r\nOriginal entry for Local Section name was ""South Joggins""; for Bed/horizon ""bed 5"". In Steen (1934) a ""bed 5"" is not mentioned in any way. Also, in papers published before and after Lyell's ""On the Remains of a Reptile..."" (1953) a different numbering is applied to the Joggins Section. Thus, it is more appropriate to follow the stratigraphic terminology used in Dawson (1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173), Steen (1934, see description above) and Carroll (1964). Coal-group 15 consists of 3 beds with a total thickness of 10 ft 6 in. (Dawson, 1878) (TL) \r\nOriginal entry for chronostratigraphy was simply ""Westphalian"". Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","From Lyell (1853): 5. Grey sandstone, with three erect trees, one having Stigmarian roots; erect Calamites and stems of unknown plants. (One of the erect trees in this bed contained the bones, teeth, &c. and land-shell above-mentioned.) ...9 ft;\r\n",sandstone,gray,,,Y,coal,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",good,,snapshot,,,,,,occasional,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" ",taxonomic,"bulk,selective quarrying,field collection,survey of museum collection",BMNH,,,,"J. W. Dawson, C. Lyell, among others",,"RM = Redpath Museum of McGill Unversity, Montreal","Listed by Steen (1934) as Indeterminate species: Hylerpeton dawsoni Owen; Hylerpeton longidentatum Dawson; Hylerpeton intermedium Dawson; Hylonomus multidens Dawson; Hylonomus wymani Dawson; Smilerpeton aciedentatus Dawson; Amblyodon problematicum Dawson; Sparodus sp. Dawson; Baphetes minor Dawson.\r\n\r\nAll catalogue numbers are from Steen (1934) and/or from Carroll (1967).\r\n\r\nThe taxon ""Batrachoididae indet."", entered under the reference Lyell & Dawson (1853), has been removed from the taxonomic list for it is a family of teleost fish. It probably referred to the ""batrachian"" affinities of the tetrapod bones noticed by Wyman (1853) but all these bones finally were assigned to Dendrerpeton acadianum n. gen. et sp. (see pls. II and III in Lyell & Dawson/Wyman/Owen, 1853). Thus the originally enterd taxon ""Dendrerpeton acadianum"", reference: Lyell & Dawson, was replaced by ""Batrachia indet."", reference: Wyman (1853), and re-identification by Owen (1853) was added (TL).\r\nRe-identification of ""Dendrerpeton oweni n. sp."" as ""Dendrerpeton acadianum"" by by Steen was removed after opinons on synonymy of the the former with the latter species were entered into the database (TL).",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Hylonomus,n. gen.,NA,NA,vertebrate,"M. C. Steen. 1934. The amphibian fauna from the South Joggins, Nova Scotia. Proceedings of the Zoological Society of London 1934:465-504",4,76,334,J. Alroy,R. Whatley,T. Liebrecht,16/02/2003 16:59,15/03/2010 20:44,7856,lyelli,Hylonomus,7856,n. sp.,318.1,314.6,Westphalian A,,3,CA,Hylonomus lyelli
297343,occ,NA,,28069,,"""Hylonomus"" latidens",species,37492,species not entered,Hylonomus,NA,genus,37492,Steen,1934,Chordata,33815,Reptilia,36322,,NA,Protorothyrididae,37486,37492,NA,NA,NA,specimens,-64.451385,45.698612,"Coal Mine Point; Divison 4, Section XV, coal-group 15",NA,South Joggins; Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Cliffs called the South Joggins (coast), about half a mile eastward of the Coal Pier.",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XV",coal-group 15,,,,NA,"From Steen (1934): ""top of the Joggins formation...Division 4, Section XV., Coal-group 15 of the Joggins section given in Dawson's 'Acadian Geology,' 1868, pp. 156-178."" From Lyell (1853): The fossils are from Bed 5 of a 25 ft section, composed of 7 beds. Bed 5 is approximately 600 ft below the main coal, ""King's Vein"".\r\nOriginal entry for Local Section name was ""South Joggins""; for Bed/horizon ""bed 5"". In Steen (1934) a ""bed 5"" is not mentioned in any way. Also, in papers published before and after Lyell's ""On the Remains of a Reptile..."" (1953) a different numbering is applied to the Joggins Section. Thus, it is more appropriate to follow the stratigraphic terminology used in Dawson (1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173), Steen (1934, see description above) and Carroll (1964). Coal-group 15 consists of 3 beds with a total thickness of 10 ft 6 in. (Dawson, 1878) (TL) \r\nOriginal entry for chronostratigraphy was simply ""Westphalian"". Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","From Lyell (1853): 5. Grey sandstone, with three erect trees, one having Stigmarian roots; erect Calamites and stems of unknown plants. (One of the erect trees in this bed contained the bones, teeth, &c. and land-shell above-mentioned.) ...9 ft;\r\n",sandstone,gray,,,Y,coal,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",good,,snapshot,,,,,,occasional,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" ",taxonomic,"bulk,selective quarrying,field collection,survey of museum collection",BMNH,,,,"J. W. Dawson, C. Lyell, among others",,"RM = Redpath Museum of McGill Unversity, Montreal","Listed by Steen (1934) as Indeterminate species: Hylerpeton dawsoni Owen; Hylerpeton longidentatum Dawson; Hylerpeton intermedium Dawson; Hylonomus multidens Dawson; Hylonomus wymani Dawson; Smilerpeton aciedentatus Dawson; Amblyodon problematicum Dawson; Sparodus sp. Dawson; Baphetes minor Dawson.\r\n\r\nAll catalogue numbers are from Steen (1934) and/or from Carroll (1967).\r\n\r\nThe taxon ""Batrachoididae indet."", entered under the reference Lyell & Dawson (1853), has been removed from the taxonomic list for it is a family of teleost fish. It probably referred to the ""batrachian"" affinities of the tetrapod bones noticed by Wyman (1853) but all these bones finally were assigned to Dendrerpeton acadianum n. gen. et sp. (see pls. II and III in Lyell & Dawson/Wyman/Owen, 1853). Thus the originally enterd taxon ""Dendrerpeton acadianum"", reference: Lyell & Dawson, was replaced by ""Batrachia indet."", reference: Wyman (1853), and re-identification by Owen (1853) was added (TL).\r\nRe-identification of ""Dendrerpeton oweni n. sp."" as ""Dendrerpeton acadianum"" by by Steen was removed after opinons on synonymy of the the former with the latter species were entered into the database (TL).",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Hylonomus,"""",NA,NA,vertebrate,"M. C. Steen. 1934. The amphibian fauna from the South Joggins, Nova Scotia. Proceedings of the Zoological Society of London 1934:465-504",4,76,334,J. Alroy,R. Whatley,T. Liebrecht,16/02/2003 16:59,13/03/2010 21:28,7856,latidens,Hylonomus,7856,,318.1,314.6,Westphalian A,,4,CA,Hylonomus latidens
297344,occ,NA,,28069,,Hylerpeton n. sp. curtidentatum,species,139140,subjective synonym of,Hylonomus lyelli,NA,species,139093,Steen,1934,Chordata,33815,Reptilia,36322,,NA,Protorothyrididae,37486,37492,NA,NA,NA,individuals,-64.451385,45.698612,"Coal Mine Point; Divison 4, Section XV, coal-group 15",NA,South Joggins; Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Cliffs called the South Joggins (coast), about half a mile eastward of the Coal Pier.",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XV",coal-group 15,,,,NA,"From Steen (1934): ""top of the Joggins formation...Division 4, Section XV., Coal-group 15 of the Joggins section given in Dawson's 'Acadian Geology,' 1868, pp. 156-178."" From Lyell (1853): The fossils are from Bed 5 of a 25 ft section, composed of 7 beds. Bed 5 is approximately 600 ft below the main coal, ""King's Vein"".\r\nOriginal entry for Local Section name was ""South Joggins""; for Bed/horizon ""bed 5"". In Steen (1934) a ""bed 5"" is not mentioned in any way. Also, in papers published before and after Lyell's ""On the Remains of a Reptile..."" (1953) a different numbering is applied to the Joggins Section. Thus, it is more appropriate to follow the stratigraphic terminology used in Dawson (1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173), Steen (1934, see description above) and Carroll (1964). Coal-group 15 consists of 3 beds with a total thickness of 10 ft 6 in. (Dawson, 1878) (TL) \r\nOriginal entry for chronostratigraphy was simply ""Westphalian"". Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","From Lyell (1853): 5. Grey sandstone, with three erect trees, one having Stigmarian roots; erect Calamites and stems of unknown plants. (One of the erect trees in this bed contained the bones, teeth, &c. and land-shell above-mentioned.) ...9 ft;\r\n",sandstone,gray,,,Y,coal,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",good,,snapshot,,,,,,occasional,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" ",taxonomic,"bulk,selective quarrying,field collection,survey of museum collection",BMNH,,,,"J. W. Dawson, C. Lyell, among others",,"RM = Redpath Museum of McGill Unversity, Montreal","Listed by Steen (1934) as Indeterminate species: Hylerpeton dawsoni Owen; Hylerpeton longidentatum Dawson; Hylerpeton intermedium Dawson; Hylonomus multidens Dawson; Hylonomus wymani Dawson; Smilerpeton aciedentatus Dawson; Amblyodon problematicum Dawson; Sparodus sp. Dawson; Baphetes minor Dawson.\r\n\r\nAll catalogue numbers are from Steen (1934) and/or from Carroll (1967).\r\n\r\nThe taxon ""Batrachoididae indet."", entered under the reference Lyell & Dawson (1853), has been removed from the taxonomic list for it is a family of teleost fish. It probably referred to the ""batrachian"" affinities of the tetrapod bones noticed by Wyman (1853) but all these bones finally were assigned to Dendrerpeton acadianum n. gen. et sp. (see pls. II and III in Lyell & Dawson/Wyman/Owen, 1853). Thus the originally enterd taxon ""Dendrerpeton acadianum"", reference: Lyell & Dawson, was replaced by ""Batrachia indet."", reference: Wyman (1853), and re-identification by Owen (1853) was added (TL).\r\nRe-identification of ""Dendrerpeton oweni n. sp."" as ""Dendrerpeton acadianum"" by by Steen was removed after opinons on synonymy of the the former with the latter species were entered into the database (TL).",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Hylerpeton,,NA,NA,vertebrate,"M. C. Steen. 1934. The amphibian fauna from the South Joggins, Nova Scotia. Proceedings of the Zoological Society of London 1934:465-504",4,76,334,J. Alroy,R. Whatley,T. Liebrecht,16/02/2003 16:59,13/03/2010 22:58,7856,curtidentatum,Hylonomus,7856,n. sp.,318.1,314.6,Westphalian A,,1,CA,Hylonomus curtidentatum
297345,occ,NA,,28069,,n. gen. Leiocephalikon n. sp. eutheton,species,137991,subjective synonym of,Leiocephalikon problematicum,NA,species,137993,Steen,1934,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37298,NA,NA,NA,individuals,-64.451385,45.698612,"Coal Mine Point; Divison 4, Section XV, coal-group 15",NA,South Joggins; Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Cliffs called the South Joggins (coast), about half a mile eastward of the Coal Pier.",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XV",coal-group 15,,,,NA,"From Steen (1934): ""top of the Joggins formation...Division 4, Section XV., Coal-group 15 of the Joggins section given in Dawson's 'Acadian Geology,' 1868, pp. 156-178."" From Lyell (1853): The fossils are from Bed 5 of a 25 ft section, composed of 7 beds. Bed 5 is approximately 600 ft below the main coal, ""King's Vein"".\r\nOriginal entry for Local Section name was ""South Joggins""; for Bed/horizon ""bed 5"". In Steen (1934) a ""bed 5"" is not mentioned in any way. Also, in papers published before and after Lyell's ""On the Remains of a Reptile..."" (1953) a different numbering is applied to the Joggins Section. Thus, it is more appropriate to follow the stratigraphic terminology used in Dawson (1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173), Steen (1934, see description above) and Carroll (1964). Coal-group 15 consists of 3 beds with a total thickness of 10 ft 6 in. (Dawson, 1878) (TL) \r\nOriginal entry for chronostratigraphy was simply ""Westphalian"". Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","From Lyell (1853): 5. Grey sandstone, with three erect trees, one having Stigmarian roots; erect Calamites and stems of unknown plants. (One of the erect trees in this bed contained the bones, teeth, &c. and land-shell above-mentioned.) ...9 ft;\r\n",sandstone,gray,,,Y,coal,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",good,,snapshot,,,,,,occasional,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" ",taxonomic,"bulk,selective quarrying,field collection,survey of museum collection",BMNH,,,,"J. W. Dawson, C. Lyell, among others",,"RM = Redpath Museum of McGill Unversity, Montreal","Listed by Steen (1934) as Indeterminate species: Hylerpeton dawsoni Owen; Hylerpeton longidentatum Dawson; Hylerpeton intermedium Dawson; Hylonomus multidens Dawson; Hylonomus wymani Dawson; Smilerpeton aciedentatus Dawson; Amblyodon problematicum Dawson; Sparodus sp. Dawson; Baphetes minor Dawson.\r\n\r\nAll catalogue numbers are from Steen (1934) and/or from Carroll (1967).\r\n\r\nThe taxon ""Batrachoididae indet."", entered under the reference Lyell & Dawson (1853), has been removed from the taxonomic list for it is a family of teleost fish. It probably referred to the ""batrachian"" affinities of the tetrapod bones noticed by Wyman (1853) but all these bones finally were assigned to Dendrerpeton acadianum n. gen. et sp. (see pls. II and III in Lyell & Dawson/Wyman/Owen, 1853). Thus the originally enterd taxon ""Dendrerpeton acadianum"", reference: Lyell & Dawson, was replaced by ""Batrachia indet."", reference: Wyman (1853), and re-identification by Owen (1853) was added (TL).\r\nRe-identification of ""Dendrerpeton oweni n. sp."" as ""Dendrerpeton acadianum"" by by Steen was removed after opinons on synonymy of the the former with the latter species were entered into the database (TL).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Leiocephalikon,n. gen.,NA,NA,vertebrate,"M. C. Steen. 1934. The amphibian fauna from the South Joggins, Nova Scotia. Proceedings of the Zoological Society of London 1934:465-504",4,76,334,J. Alroy,R. Whatley,T. Liebrecht,16/02/2003 16:59,13/03/2010 21:28,7856,eutheton,Leiocephalikon,7856,n. sp.,318.1,314.6,Westphalian A,,1,CA,Leiocephalikon eutheton
297346,occ,NA,,28069,,Lepospondyli indet.,unranked clade,37250,,Lepospondyli,NA,unranked clade,37250,Steen,1934,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,,-64.451385,45.698612,"Coal Mine Point; Divison 4, Section XV, coal-group 15",NA,South Joggins; Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Cliffs called the South Joggins (coast), about half a mile eastward of the Coal Pier.",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XV",coal-group 15,,,,NA,"From Steen (1934): ""top of the Joggins formation...Division 4, Section XV., Coal-group 15 of the Joggins section given in Dawson's 'Acadian Geology,' 1868, pp. 156-178."" From Lyell (1853): The fossils are from Bed 5 of a 25 ft section, composed of 7 beds. Bed 5 is approximately 600 ft below the main coal, ""King's Vein"".\r\nOriginal entry for Local Section name was ""South Joggins""; for Bed/horizon ""bed 5"". In Steen (1934) a ""bed 5"" is not mentioned in any way. Also, in papers published before and after Lyell's ""On the Remains of a Reptile..."" (1953) a different numbering is applied to the Joggins Section. Thus, it is more appropriate to follow the stratigraphic terminology used in Dawson (1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173), Steen (1934, see description above) and Carroll (1964). Coal-group 15 consists of 3 beds with a total thickness of 10 ft 6 in. (Dawson, 1878) (TL) \r\nOriginal entry for chronostratigraphy was simply ""Westphalian"". Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","From Lyell (1853): 5. Grey sandstone, with three erect trees, one having Stigmarian roots; erect Calamites and stems of unknown plants. (One of the erect trees in this bed contained the bones, teeth, &c. and land-shell above-mentioned.) ...9 ft;\r\n",sandstone,gray,,,Y,coal,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",good,,snapshot,,,,,,occasional,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" ",taxonomic,"bulk,selective quarrying,field collection,survey of museum collection",BMNH,,,,"J. W. Dawson, C. Lyell, among others",,"RM = Redpath Museum of McGill Unversity, Montreal","Listed by Steen (1934) as Indeterminate species: Hylerpeton dawsoni Owen; Hylerpeton longidentatum Dawson; Hylerpeton intermedium Dawson; Hylonomus multidens Dawson; Hylonomus wymani Dawson; Smilerpeton aciedentatus Dawson; Amblyodon problematicum Dawson; Sparodus sp. Dawson; Baphetes minor Dawson.\r\n\r\nAll catalogue numbers are from Steen (1934) and/or from Carroll (1967).\r\n\r\nThe taxon ""Batrachoididae indet."", entered under the reference Lyell & Dawson (1853), has been removed from the taxonomic list for it is a family of teleost fish. It probably referred to the ""batrachian"" affinities of the tetrapod bones noticed by Wyman (1853) but all these bones finally were assigned to Dendrerpeton acadianum n. gen. et sp. (see pls. II and III in Lyell & Dawson/Wyman/Owen, 1853). Thus the originally enterd taxon ""Dendrerpeton acadianum"", reference: Lyell & Dawson, was replaced by ""Batrachia indet."", reference: Wyman (1853), and re-identification by Owen (1853) was added (TL).\r\nRe-identification of ""Dendrerpeton oweni n. sp."" as ""Dendrerpeton acadianum"" by by Steen was removed after opinons on synonymy of the the former with the latter species were entered into the database (TL).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lepospondyli,,NA,NA,vertebrate,"M. C. Steen. 1934. The amphibian fauna from the South Joggins, Nova Scotia. Proceedings of the Zoological Society of London 1934:465-504",4,76,334,J. Alroy,R. Whatley,T. Liebrecht,16/02/2003 16:59,13/03/2010 21:28,7856,indet.,,7856,,318.1,314.6,Westphalian A,,NA,CA, indet.
346289,occ,NA,,11165,,Archeria crassidisca,species,345353,,Archeria crassidisca,NA,species,229309,Sander,1987,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,,-98.699997,33.683334,Geraldine Bonebed,NA,,US,Texas,Archer,estimated from map,minutes,small collection,Locality is around 3km (~2miles) east of the intersection of Highway 25 and another unnamed Highway.,gp_mid,-30.37,-1.69,101,US,,Nocona,Wichita,,group of beds,,,Geraldine Bonebed,,,,NA,"The Geraldine Bonebed has been placed in the Nocona Formation, the old assignment to the Admiral Formation has been revised, as the Admiral is now restriced to a marine limestone and shale unit lying to the southwest of the same age as the Nocona.","gray, blocky to flaky and rarely laminated claystone grading downwards into yellow clays...Notable is the occurrence of small ""blebs"" of azurite and malachite staining on joint faces. Some layers of small clay pebbles are present",claystone,"grading,gray,yellow",,,Y,,,,,,"""floodplain""",,"Extensive discussion of paleoenvironmental interpretation (p. 223-226; 233-234). The setting of the Geraldine Bobebed and vicinity was a lushly vegetated floodplain with small lakes and a swamp forest of Psaronius, Cordaites and some seed ferns. Forest and brush vegetation (Walchia, seed ferns) lived on the ""upland"" divides between drainages.",macrofossils,,,,,,NA,,"adpression,charcoalification,coalified",,parautochthonous,snapshot,,,,,,,NA,,"The gray-yellow color of the clays, the preservation of the wood and plant debris as coaly compression, andthe occurrence of copper minerals indicate a reducing environment of deposition.\r\n\r\nthe preservation of the wood and plant debris as coaly compressions (p. 226)",taxonomic,"selective quarrying,field collection",,some macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,,NA,NA,paleobotany,"P. M. Sander. 1987. Taphonomy of the Lower Permian Geraldine Bonebed in Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 61:221-236",15,15,174,H. Sims,H. Sims,J. Cassara,10/07/2003 14:52,21/02/2004 16:41,4113,crassidisca,Archeria,4113,,298.9,290.1,Asselian,Sakmarian,NA,US,Archeria crassidisca
346290,occ,NA,,11165,,Eryops megacephalus,species,70397,,Eryops megacephalus,NA,species,70397,Sander,1987,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-98.699997,33.683334,Geraldine Bonebed,NA,,US,Texas,Archer,estimated from map,minutes,small collection,Locality is around 3km (~2miles) east of the intersection of Highway 25 and another unnamed Highway.,gp_mid,-30.37,-1.69,101,US,,Nocona,Wichita,,group of beds,,,Geraldine Bonebed,,,,NA,"The Geraldine Bonebed has been placed in the Nocona Formation, the old assignment to the Admiral Formation has been revised, as the Admiral is now restriced to a marine limestone and shale unit lying to the southwest of the same age as the Nocona.","gray, blocky to flaky and rarely laminated claystone grading downwards into yellow clays...Notable is the occurrence of small ""blebs"" of azurite and malachite staining on joint faces. Some layers of small clay pebbles are present",claystone,"grading,gray,yellow",,,Y,,,,,,"""floodplain""",,"Extensive discussion of paleoenvironmental interpretation (p. 223-226; 233-234). The setting of the Geraldine Bobebed and vicinity was a lushly vegetated floodplain with small lakes and a swamp forest of Psaronius, Cordaites and some seed ferns. Forest and brush vegetation (Walchia, seed ferns) lived on the ""upland"" divides between drainages.",macrofossils,,,,,,NA,,"adpression,charcoalification,coalified",,parautochthonous,snapshot,,,,,,,NA,,"The gray-yellow color of the clays, the preservation of the wood and plant debris as coaly compression, andthe occurrence of copper minerals indicate a reducing environment of deposition.\r\n\r\nthe preservation of the wood and plant debris as coaly compressions (p. 226)",taxonomic,"selective quarrying,field collection",,some macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,paleobotany,"P. M. Sander. 1987. Taphonomy of the Lower Permian Geraldine Bonebed in Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 61:221-236",15,15,174,H. Sims,H. Sims,J. Cassara,10/07/2003 14:52,21/02/2004 16:41,4113,megacephalus,Eryops,4113,,298.9,290.1,Asselian,Sakmarian,NA,US,Eryops megacephalus
346291,occ,NA,,11165,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Sander,1987,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-98.699997,33.683334,Geraldine Bonebed,NA,,US,Texas,Archer,estimated from map,minutes,small collection,Locality is around 3km (~2miles) east of the intersection of Highway 25 and another unnamed Highway.,gp_mid,-30.37,-1.69,101,US,,Nocona,Wichita,,group of beds,,,Geraldine Bonebed,,,,NA,"The Geraldine Bonebed has been placed in the Nocona Formation, the old assignment to the Admiral Formation has been revised, as the Admiral is now restriced to a marine limestone and shale unit lying to the southwest of the same age as the Nocona.","gray, blocky to flaky and rarely laminated claystone grading downwards into yellow clays...Notable is the occurrence of small ""blebs"" of azurite and malachite staining on joint faces. Some layers of small clay pebbles are present",claystone,"grading,gray,yellow",,,Y,,,,,,"""floodplain""",,"Extensive discussion of paleoenvironmental interpretation (p. 223-226; 233-234). The setting of the Geraldine Bobebed and vicinity was a lushly vegetated floodplain with small lakes and a swamp forest of Psaronius, Cordaites and some seed ferns. Forest and brush vegetation (Walchia, seed ferns) lived on the ""upland"" divides between drainages.",macrofossils,,,,,,NA,,"adpression,charcoalification,coalified",,parautochthonous,snapshot,,,,,,,NA,,"The gray-yellow color of the clays, the preservation of the wood and plant debris as coaly compression, andthe occurrence of copper minerals indicate a reducing environment of deposition.\r\n\r\nthe preservation of the wood and plant debris as coaly compressions (p. 226)",taxonomic,"selective quarrying,field collection",,some macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,paleobotany,"P. M. Sander. 1987. Taphonomy of the Lower Permian Geraldine Bonebed in Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 61:221-236",15,15,174,H. Sims,H. Sims,J. Cassara,10/07/2003 14:52,21/02/2004 16:41,4113,sp.,Diadectes,4113,,298.9,290.1,Asselian,Sakmarian,NA,US,Diadectes sp.
346292,occ,NA,,11165,,Edaphosaurus boanerges,species,122352,,Edaphosaurus boanerges,NA,species,122352,Sander,1987,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,,-98.699997,33.683334,Geraldine Bonebed,NA,,US,Texas,Archer,estimated from map,minutes,small collection,Locality is around 3km (~2miles) east of the intersection of Highway 25 and another unnamed Highway.,gp_mid,-30.37,-1.69,101,US,,Nocona,Wichita,,group of beds,,,Geraldine Bonebed,,,,NA,"The Geraldine Bonebed has been placed in the Nocona Formation, the old assignment to the Admiral Formation has been revised, as the Admiral is now restriced to a marine limestone and shale unit lying to the southwest of the same age as the Nocona.","gray, blocky to flaky and rarely laminated claystone grading downwards into yellow clays...Notable is the occurrence of small ""blebs"" of azurite and malachite staining on joint faces. Some layers of small clay pebbles are present",claystone,"grading,gray,yellow",,,Y,,,,,,"""floodplain""",,"Extensive discussion of paleoenvironmental interpretation (p. 223-226; 233-234). The setting of the Geraldine Bobebed and vicinity was a lushly vegetated floodplain with small lakes and a swamp forest of Psaronius, Cordaites and some seed ferns. Forest and brush vegetation (Walchia, seed ferns) lived on the ""upland"" divides between drainages.",macrofossils,,,,,,NA,,"adpression,charcoalification,coalified",,parautochthonous,snapshot,,,,,,,NA,,"The gray-yellow color of the clays, the preservation of the wood and plant debris as coaly compression, andthe occurrence of copper minerals indicate a reducing environment of deposition.\r\n\r\nthe preservation of the wood and plant debris as coaly compressions (p. 226)",taxonomic,"selective quarrying,field collection",,some macrofossils,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,paleobotany,"P. M. Sander. 1987. Taphonomy of the Lower Permian Geraldine Bonebed in Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 61:221-236",15,15,174,H. Sims,H. Sims,J. Cassara,10/07/2003 14:52,21/02/2004 16:41,4113,boanerges,Edaphosaurus,4113,,298.9,290.1,Asselian,Sakmarian,NA,US,Edaphosaurus boanerges
346293,occ,NA,,11165,,Dimetrodon natalis,species,122781,,Dimetrodon natalis,NA,species,54971,Sander,1987,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-98.699997,33.683334,Geraldine Bonebed,NA,,US,Texas,Archer,estimated from map,minutes,small collection,Locality is around 3km (~2miles) east of the intersection of Highway 25 and another unnamed Highway.,gp_mid,-30.37,-1.69,101,US,,Nocona,Wichita,,group of beds,,,Geraldine Bonebed,,,,NA,"The Geraldine Bonebed has been placed in the Nocona Formation, the old assignment to the Admiral Formation has been revised, as the Admiral is now restriced to a marine limestone and shale unit lying to the southwest of the same age as the Nocona.","gray, blocky to flaky and rarely laminated claystone grading downwards into yellow clays...Notable is the occurrence of small ""blebs"" of azurite and malachite staining on joint faces. Some layers of small clay pebbles are present",claystone,"grading,gray,yellow",,,Y,,,,,,"""floodplain""",,"Extensive discussion of paleoenvironmental interpretation (p. 223-226; 233-234). The setting of the Geraldine Bobebed and vicinity was a lushly vegetated floodplain with small lakes and a swamp forest of Psaronius, Cordaites and some seed ferns. Forest and brush vegetation (Walchia, seed ferns) lived on the ""upland"" divides between drainages.",macrofossils,,,,,,NA,,"adpression,charcoalification,coalified",,parautochthonous,snapshot,,,,,,,NA,,"The gray-yellow color of the clays, the preservation of the wood and plant debris as coaly compression, andthe occurrence of copper minerals indicate a reducing environment of deposition.\r\n\r\nthe preservation of the wood and plant debris as coaly compressions (p. 226)",taxonomic,"selective quarrying,field collection",,some macrofossils,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,paleobotany,"P. M. Sander. 1987. Taphonomy of the Lower Permian Geraldine Bonebed in Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 61:221-236",15,15,174,H. Sims,H. Sims,J. Cassara,10/07/2003 14:52,21/02/2004 16:41,4113,natalis,Dimetrodon,4113,,298.9,290.1,Asselian,Sakmarian,NA,US,Dimetrodon natalis
346294,occ,NA,,11165,,Bolosaurus striatus,species,138029,,Bolosaurus striatus,NA,species,138029,Sander,1987,Chordata,33815,Reptilia,36322,,NA,Bolosauridae,37510,37511,NA,NA,NA,,-98.699997,33.683334,Geraldine Bonebed,NA,,US,Texas,Archer,estimated from map,minutes,small collection,Locality is around 3km (~2miles) east of the intersection of Highway 25 and another unnamed Highway.,gp_mid,-30.37,-1.69,101,US,,Nocona,Wichita,,group of beds,,,Geraldine Bonebed,,,,NA,"The Geraldine Bonebed has been placed in the Nocona Formation, the old assignment to the Admiral Formation has been revised, as the Admiral is now restriced to a marine limestone and shale unit lying to the southwest of the same age as the Nocona.","gray, blocky to flaky and rarely laminated claystone grading downwards into yellow clays...Notable is the occurrence of small ""blebs"" of azurite and malachite staining on joint faces. Some layers of small clay pebbles are present",claystone,"grading,gray,yellow",,,Y,,,,,,"""floodplain""",,"Extensive discussion of paleoenvironmental interpretation (p. 223-226; 233-234). The setting of the Geraldine Bobebed and vicinity was a lushly vegetated floodplain with small lakes and a swamp forest of Psaronius, Cordaites and some seed ferns. Forest and brush vegetation (Walchia, seed ferns) lived on the ""upland"" divides between drainages.",macrofossils,,,,,,NA,,"adpression,charcoalification,coalified",,parautochthonous,snapshot,,,,,,,NA,,"The gray-yellow color of the clays, the preservation of the wood and plant debris as coaly compression, andthe occurrence of copper minerals indicate a reducing environment of deposition.\r\n\r\nthe preservation of the wood and plant debris as coaly compressions (p. 226)",taxonomic,"selective quarrying,field collection",,some macrofossils,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Bolosaurus,,NA,NA,paleobotany,"P. M. Sander. 1987. Taphonomy of the Lower Permian Geraldine Bonebed in Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 61:221-236",15,15,174,H. Sims,H. Sims,J. Cassara,10/07/2003 14:52,21/02/2004 16:41,4113,striatus,Bolosaurus,4113,,298.9,290.1,Asselian,Sakmarian,NA,US,Bolosaurus striatus
349452,occ,NA,,11323,,Tetrapoda indet.,unranked clade,53190,,Tetrapoda,NA,unranked clade,53190,Mamay and Mapes,1992,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,,-106.25,34.75,Kinney Brick Quarry macroflora,NA,,US,New Mexico,Bernalillo,estimated from map,minutes,small collection,"Material has been collected by Mamay and Watt and otehrs since 1967 from this site in the Kinney clay pit (SE 1/4, sec. 18, T.9 N., R. 6 E). Manzanita Mountains; Kinney Brick Company Quarry. ",gp_mid,-35.49,1.77,101,US,,Wild Cow,Madera,Pine Shadow,bed,,,,,,,NA,"Exposure lies in a Pennsylvanian sequence previously known as the Madera Limestone: nomenclature has been revised by Myers. Classification of Myers combines the Madera Limestone and the Burnsum Fm into the Madera Group and divides the group into three formations, the middle of which is the Wild Cow Fm and contains fossils discussed here.","Rock section exposed by quarrying operations originally consisted of about 160 ft of limestone, siltstone, sandstone, shale, and conglomerate. The upper pit was then being excavated for the predominantly tan and olive shales.","""shale""","brown,green",,,Y,,,,,,,,,macrofossils,,,,,,NA,,"mold/impression,adpression",medium,,,,,,,,,NA,,,taxonomic,"selective quarrying,field collection","NMMNH,USNM",some macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tetrapoda,,NA,NA,paleobotany,"S. H. Mamay and G. Mapes. 1992. Early Virgilian plant megafossils from the Kinney Brick Company Quarry, Manzanita Mountains, New Mexico. New Mexico Bureau of Mines & Mineral Resources Bulletin 138:61-85",15,156,174,H. Sims,A. McGowan,J. Cassara,24/07/2003 11:47,31/01/2004 15:52,4164,indet.,,4164,,303.4,298.9,Virgilian,,NA,US, indet.
367508,occ,NA,R,28267,,Captorhinus ? sp.,genus,37497,,Captorhinus,NA,genus,37497,Williston,1911,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,?,NA,NA,vertebrate,S. W. Williston. 1911. American Permian Vertebrates ,4,76,697,J. Alroy,R. Whatley,E. Dunne,22/09/2003 16:48,16/08/2016 04:36,9228,sp.,Captorhinus,9228,,279.3,272.3,Kungurian,,1,US,Captorhinus sp.
367508,occ,21190,,28267,,Captorhinus aguti,species,90718,,Captorhinus aguti,NA,species,134887,Seltin,1959,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,R. J. Seltin. 1959. A review of the family Captorhinidae. Fieldiana: Geology 10(34):461-509,315,334,0,J. Mueller,T. Liebrecht,,15/12/2008 16:46,15/12/2008 18:46,9228,aguti,Captorhinus,28359,,279.3,272.3,Kungurian,,1,US,Captorhinus aguti
367509,occ,NA,,28267,,Clepsydrops natalis,species,54971,recombined as,Dimetrodon natalis,NA,species,54971,Williston,1911,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Clepsydrops,,NA,NA,vertebrate,S. W. Williston. 1911. American Permian Vertebrates ,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,22/09/2003 16:48,29/01/2010 07:32,9228,natalis,Dimetrodon,9228,,279.3,272.3,Kungurian,,NA,US,Dimetrodon natalis
367510,occ,NA,,34761,,n. gen. Elcabrosaurus n. sp. baldwini,species,54985,subjective synonym of,Sphenacodon ferox,NA,species,122487,Case,1907,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,individuals,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Elcabrosaurus,n. gen.,NA,NA,vertebrate,E. C. Case. 1907. Revision of the Pelycosauria of North America. Carnegie Institution of Washington 55:3-176,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,22/09/2003 19:31,21/08/2009 16:28,43845,baldwini,Sphenacodon,7374,n. sp.,303.4,298.9,Virgilian,,1,US,Sphenacodon baldwini
367591,occ,NA,,34761,,Dimetrodon n. sp. navajovicus,species,54987,recombined as,Ophiacodon navajovicus,NA,species,54987,Case,1907,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,E. C. Case. 1907. Revision of the Pelycosauria of North America. Carnegie Institution of Washington 55:3-176,4,76,334,J. Alroy,R. Whatley,T. Liebrecht,23/09/2003 11:26,21/08/2009 16:28,43845,navajovicus,Ophiacodon,7374,n. sp.,303.4,298.9,Virgilian,,9,US,Ophiacodon navajovicus
367864,occ,NA,,34797,,cf. Actinodon sp.,genus,37008,,Actinodon,NA,genus,37008,Heyler and Poplin,1990,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37008,NA,NA,NA,,2.966667,46.466667,Buxieres-les-Mines (Autunian shales),NA,"Buxieres les Mines, Allier, Autunien ",FR,,Allier,based on nearby landmark,minutes,outcrop,"Buxieres-les-Mines (near Moulins North of the Massif Central), Department of Allier",gp_mid,17.46,1.45,305,FR,,,,,,,,,,Buxieres,,NA,"middle Autunien, Autunien encompasses the Asselian and Sakmarian stages = lower Permian",,"""shale""",,lithified,,,,,,,,terrestrial indet.,,Autunian shales,macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,"surface (in situ),field collection",MNHN,,,,,,Museum d'Histoire Naturelle d'Autun (France),,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Actinodon,cf.,NA,NA,vertebrate,"D. Heyler and C. Poplin. 1990. Les Vertebres autuniens de Buxieres-les-Mines (Allier, France). [Autunian vertebrates from Buxieres-les-Mines, Allier, France]. Bulletin du Museum National d'Histoire Naturelle, Section C: Sciences de la Terre: Paleontologie, Geologie, Mineralogie 12(2):225-239",4,76,697,J. Alroy,R. Whatley,E. Dunne,25/09/2003 18:16,02/08/2016 12:58,9281,sp.,Actinodon,9197,,298.9,290.1,Asselian,Sakmarian,NA,FR,Actinodon sp.
368129,occ,NA,,11149,,Amphibia indet.,unranked clade,36319,,Amphibia,NA,unranked clade,36319,Mamay,1966,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,,-99.133331,33.75,Lake Kemp 1,NA,"USGS paleobotany loc. 10,000\r\nMabelle Limestone of Romer?",US,Texas,Baylor,based on nearby landmark,minutes,outcrop,"The productive outcrop is approximately 6 miles north of Mabelle, in Baylor County, Tex. It is reached by following U.S. Highway 183-283 north from Mabelle to a point 0.4 miles south of the highway bridge under which the Wichita River flows eastward from the spillway of Lake Kemp. At this point one sees a conspicous exposure of predominantly tan sedimentary rocks in a low wast-facing bluff about 125 yards west of the highway; this is the plant-bearing site. ",gp_mid,-30.34,-0.95,101,US,,Lueders,,,,,,,,,,NA,"Thus the plants occur near the middle of the Lower Permian which, according to Kummel (1961) and Dutro (1961) is equivalent to the Artinskian interval of the Urals section.","As exposed at this outcrop, the sequence consists of approximately 20 feet of siltstone and sandstone, mostly thin bedded with variable fissility, ranging in color from white to grey, bluish gray or tan and having considerable limonitic streaking. The section is capped by a limestone bed that is light gray in color, ranges from 2 to 3.5 feet in thickness and contains minor amounts of sand. This bed is the only conspicuous limestone in the vicinity of the plant beds and doubtless is the unit mapped my Garrett, Lloyd, and Laskey (1930) as the Mabelle Limestone of Romer (1928) This fossiliferous site will be referred to here as the Lake Kemp Locality (USGS paleobotany loc. 10,000)...Although finely comminuted plant debris is scattered through the entire sequence below the limestone unit, the best preserved plant material was found in a 1-foot unit of tan and blueish-gray siltstone, the base of which is about 5ft above the old roadbed.",sandstone,"gray,yellow,blue",,,Y,siltstone,"brown,gray,blue",,,Y,fine channel fill,,The beds in approximately the lower half of the section show minor angular unconformities and discordant bedding planes that suggest a channel-fill type of deposition.,macrofossils,,,,,,NA,,,,,,,,,,,,NA,,,taxonomic,field collection,USGS,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Amphibia,,NA,NA,paleobotany,"S. H. Mamay. 1966. Tinsleya, a new genus of seed-bearing callipterid plants from the Permian of north-central Texas. U.S. Geological Survey Professional Paper 523-E:1-15",15,156,174,H. Sims,A. McGowan,J. Cassara,03/10/2003 10:42,22/02/2004 11:37,4105,indet.,,4105,,290.1,279.3,Artinskian,,NA,US, indet.
384336,occ,NA,R,36571,,n. gen. Trematopsis n. sp. seltini,species,56734,invalid subgroup of,Cacops,NA,genus,37025,Olson,1956,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37025,NA,NA,NA,individuals,-99.257774,33.602222,Olson Locality Bac (Vale Formation),NA,"Beaver Creek, Bac locality",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"In drainage area of Beaver Creek, Locality Bac is defined by aerial photographic index as follows: CUM 4B 65, road at 5.1-0.9, along breaks east to 6.3-1.0, north and northeast along breaks to 7.0-3.3, east-southeast around nose of breaks to 7.8-4.0, west to 6.1-4.8, and along breaks to 5.1-0.9. This area included beds of Arroyo age along its eastern margin and lower Vale beds over the more western parts. Lat long is for Seymour.",gp_mid,-29.04,1.65,101,US,,Vale,Clear Fork,,bed,,,,,,,NA,"Lower part of the Vale Formation, about 100 feet above base. Lower Permian (Leonardian).\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top",,,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,,,,,occasional,NA,,,taxonomic,field collection,FMNH,,,,,,Original citation for type species Trematopsis seltini sp. nov. is Chicago Natural History Museum (CNHM). ,Milner 1985 reassigns the subjective synonym Trematopsis seltini to Cacops cf. aspidephorus. Cacops is a dissorophoid.\n[Trematopidae: Trematopsis seltini n. gen. et sp. Olson 1956],"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Trematopsis,n. gen.,NA,NA,vertebrate,E. C. Olson. 1956. Fauna of the Vale and Choza: 12. A new trematopsid amphibian from the Vale Formation. Fieldiana: Geology 10(26):323-328,4,76,0,J. Alroy,R. Whatley,,04/02/2004 16:49,04/02/2004 18:49,9784,seltini,Cacops,9784,n. sp.,279.3,272.3,Kungurian,,1,US,Cacops seltini
384336,occ,10506,,36571,,Cacops cf. aspidephorus,species,56737,,Cacops aspidephorus,NA,species,56737,Milner,1985,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37025,NA,NA,NA,individuals,-99.257774,33.602222,Olson Locality Bac (Vale Formation),NA,"Beaver Creek, Bac locality",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"In drainage area of Beaver Creek, Locality Bac is defined by aerial photographic index as follows: CUM 4B 65, road at 5.1-0.9, along breaks east to 6.3-1.0, north and northeast along breaks to 7.0-3.3, east-southeast around nose of breaks to 7.8-4.0, west to 6.1-4.8, and along breaks to 5.1-0.9. This area included beds of Arroyo age along its eastern margin and lower Vale beds over the more western parts. Lat long is for Seymour.",gp_mid,-29.04,1.65,101,US,,Vale,Clear Fork,,bed,,,,,,,NA,"Lower part of the Vale Formation, about 100 feet above base. Lower Permian (Leonardian).\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top",,,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,,,,,occasional,NA,,,taxonomic,field collection,FMNH,,,,,,Original citation for type species Trematopsis seltini sp. nov. is Chicago Natural History Museum (CNHM). ,Milner 1985 reassigns the subjective synonym Trematopsis seltini to Cacops cf. aspidephorus. Cacops is a dissorophoid.\n[Trematopidae: Trematopsis seltini n. gen. et sp. Olson 1956],"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Cacops,,NA,NA,vertebrate,"A. R. Milner. 1985. On the identity of Trematopsis seltini (Amphibia: Temnospondyli) from the Lower Permian of Texas. Neues Jahrbuch fuer Geologie und Palaeontologie. Monatshefte, Stuttgart : E. Schweizerbart'sche Verlagsbuchhandlung 1985(6):357-367",4,76,76,J. Alroy,R. Whatley,R. Whatley,24/02/2004 11:41,24/02/2004 13:41,9784,aspidephorus,Cacops,7821,cf.,279.3,272.3,Kungurian,,1,US,Cacops aspidephorus
390702,occ,NA,,37459,,Tetrapoda indet.,unranked clade,53190,,Tetrapoda,NA,unranked clade,53190,Mason,1878,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,,-76.166664,40.816666,Ellengowan Shaft,NA,,US,Pennsylvania,Schuylkill,estimated from map,minutes,outcrop,"Ellangowan colliery situated in E. Mahanoy Township, Schuylkill Co., about midway between Mahanoy city and Shenandoah, in a small valley diverging from the Mahanoy valley proper",gp_mid,-16.56,-10.92,101,US,,Llewellyn,,,formation,,,,,,,NA,"author doesn't give any stratigraphic info, these data were inferred from geologic maps",gray slaty sandstone overlying the mammoth seam of coal,coal,,,,,sandstone,gray,,silty,Y,,,,macrofossils,,,,,,NA,,trace,,,,,,,,,,NA,,,general faunal/floral,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tetrapoda,,NA,NA,vertebrate,"W. D. Mason. 1878. On the batrachian foot tracks from the Ellengowan Shaft, in Schuylkill County, Pennsylvania. Proceedings of the American Philosophical Society 17:716-719",4,128,0,J. Alroy,E. Leckey,,15/03/2004 12:57,15/03/2004 14:57,10033,indet.,,10033,,323.2,298.9,Pennsylvanian,,NA,US, indet.
399134,occ,NA,R,38320,,Discosauriscus indet.,genus,37209,,Discosauriscus,NA,genus,37209,Tatarinov,1964,Chordata,33815,Osteichthyes,34881,,NA,Discosauridae,320954,37209,NA,NA,NA,,69.985558,40.648609,Adrasman quarry,NA,,TJ,,,based on nearby landmark,seconds,outcrop,Latitude and longitude above are those of the settlement Adrasman. The quarry is 10km north-east from the settlement.,gp_mid,71.9,19.94,402,TJ,,,,,bed,,,,,,,NA,The author relates that the finds come form a pack of sediments interposed between vulcanic rocks on the southern flank of Sarytaipan Mountain.,,sandstone,"fine,black,gray,green",poorly lithified,"argillaceous,carbonaceous",Y,,,,,,fluvial-deltaic indet.,volcanic basin,,macrofossils,,,,,,NA,,"body,mold/impression",,autochthonous,time-averaged,,,,,,,NA,,,general faunal/floral,"selective quarrying,field collection",,,90 specimens,500 cm2 (area),,,The author states that most of the collection consisted of skeleton impressions. There were also some skulls and a shoulder girdle.,The taxonomic list is based on the skulls and the impressions in this collection.,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Discosauriscus,,NA,NA,vertebrate,L. P. Tatarinov. 1964. Novoe mestonakhozhdenie permskikh seimuriamorfov v SSSR [A new locality of Permian seymouriamorphs in the USSR]. Paleontologicheskii Zhurnal 1964(1):139-141,22,186,0,J. Hunter,D. Ehrenburg,,20/04/2004 07:57,20/04/2004 09:57,10284,indet.,Discosauriscus,10284,,298.9,254,Rotliegendes,,NA,TJ,Discosauriscus indet.
399134,occ,10568,,38320,,Ariekanerpeton indet.,genus,37208,,Ariekanerpeton,NA,genus,37208,Tatarinov,1964,Chordata,33815,Osteichthyes,34881,,NA,Discosauriscidae,37207,37208,NA,NA,NA,,69.985558,40.648609,Adrasman quarry,NA,,TJ,,,based on nearby landmark,seconds,outcrop,Latitude and longitude above are those of the settlement Adrasman. The quarry is 10km north-east from the settlement.,gp_mid,71.9,19.94,402,TJ,,,,,bed,,,,,,,NA,The author relates that the finds come form a pack of sediments interposed between vulcanic rocks on the southern flank of Sarytaipan Mountain.,,sandstone,"fine,black,gray,green",poorly lithified,"argillaceous,carbonaceous",Y,,,,,,fluvial-deltaic indet.,volcanic basin,,macrofossils,,,,,,NA,,"body,mold/impression",,autochthonous,time-averaged,,,,,,,NA,,,general faunal/floral,"selective quarrying,field collection",,,90 specimens,500 cm2 (area),,,The author states that most of the collection consisted of skeleton impressions. There were also some skulls and a shoulder girdle.,The taxonomic list is based on the skulls and the impressions in this collection.,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ariekanerpeton,,NA,NA,vertebrate,L. P. Tatarinov. 1964. Novoe mestonakhozhdenie permskikh seimuriamorfov v SSSR [A new locality of Permian seymouriamorphs in the USSR]. Paleontologicheskii Zhurnal 1964(1):139-141,22,186,186,J. Hunter,D. Ehrenburg,D. Ehrenburg,20/04/2004 08:13,20/04/2004 10:13,10284,indet.,Ariekanerpeton,10284,,298.9,254,Rotliegendes,,NA,TJ,Ariekanerpeton indet.
399135,occ,10569,,38320,,Ariekanerpeton indet.,genus,37208,,Ariekanerpeton,NA,genus,37208,Tatarinov,1964,Chordata,33815,Osteichthyes,34881,,NA,Discosauriscidae,37207,37208,NA,NA,NA,,69.985558,40.648609,Adrasman quarry,NA,,TJ,,,based on nearby landmark,seconds,outcrop,Latitude and longitude above are those of the settlement Adrasman. The quarry is 10km north-east from the settlement.,gp_mid,71.9,19.94,402,TJ,,,,,bed,,,,,,,NA,The author relates that the finds come form a pack of sediments interposed between vulcanic rocks on the southern flank of Sarytaipan Mountain.,,sandstone,"fine,black,gray,green",poorly lithified,"argillaceous,carbonaceous",Y,,,,,,fluvial-deltaic indet.,volcanic basin,,macrofossils,,,,,,NA,,"body,mold/impression",,autochthonous,time-averaged,,,,,,,NA,,,general faunal/floral,"selective quarrying,field collection",,,90 specimens,500 cm2 (area),,,The author states that most of the collection consisted of skeleton impressions. There were also some skulls and a shoulder girdle.,The taxonomic list is based on the skulls and the impressions in this collection.,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ariekanerpeton,,NA,NA,vertebrate,L. P. Tatarinov. 1964. Novoe mestonakhozhdenie permskikh seimuriamorfov v SSSR [A new locality of Permian seymouriamorphs in the USSR]. Paleontologicheskii Zhurnal 1964(1):139-141,22,186,186,J. Hunter,D. Ehrenburg,D. Ehrenburg,20/04/2004 08:13,20/04/2004 10:13,10284,indet.,Ariekanerpeton,10284,,298.9,254,Rotliegendes,,NA,TJ,Ariekanerpeton indet.
487397,occ,NA,,48897,,n. gen. Bathygnathus n. sp. borealis,species,65123,,Bathygnathus borealis,NA,species,65123,Leidy,1853,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38902,NA,NA,NA,specimens,-63.516666,46.516666,McLeod farm well,NA,,CA,Prince Edward Island,,based on nearby landmark,minutes,small collection,"from well on farm of Donald McLeod, at French River, near New London, N shore of PEI",gp_mid,-0.67,1.2,108,CA,,Orby Head,,,bed,,,,,,,NA,21 feet 9 inches below surface,fossil from a brick-red shale embedded in a sandstone matrix,"""shale""",red,,,Y,sandstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,medium,,snapshot,,dispersed,random,,,frequent,NA,,,taxonomic,"core,mechanical,field collection",,,,,D. McLeod,1845,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Bathygnathus,n. gen.,NA,NA,vertebrate,J. Leidy. 1853. [Fragment of a jaw of an extinct saurian animal]. Proceedings of the Academy of Natural Sciences of Philadelphia 6:404,14,14,0,M. Carrano,M. Carrano,,04/04/2005 07:33,04/04/2005 09:33,13005,borealis,Bathygnathus,13005,n. sp.,290.1,279.3,Artinskian,,1,CA,Bathygnathus borealis
492011,occ,NA,,49663,,Tetrapoda indet.,unranked clade,53190,,Tetrapoda,NA,unranked clade,53190,Schram and Schram,1979,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,individuals,-106.337997,35,Kinney Clay Pit (USNM coll),NA,,US,New Mexico,Bernalillo,estimated from map,degrees,small collection,"Site in the Kinney clay pit (SE 1/4, sec. 18, T.9 N., R. 6 E). Manzanita Mountains; Kinney Brick Company Quarry.",gp_mid,-36.67,-0.08,101,US,FED,Madera,,,bed,,Kinney Clay Pit,Kinney Clay Pit,,,,NA,"Recent fusulinid and conodont studies indicate a middle Missourian (Kasimovian) age - Lucas et al., 2011",No information given.,not reported,,,,,,,,,,lagoonal/restricted shallow subtidal,intermontane basin,Basins associated with Ancestral Rocky Mountains block faulting,macrofossils,,,,,,NA,,"body,adpression",,,,,,,,,,NA,,,taxonomic,,USNM,,,,Mamay,"1967, 1969",,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tetrapoda,,NA,NA,"marine invertebrate,paleoentomology","F. R. Schram and J. M. Schram. 1979. Some shrimp of the Madera Formation (Pennsylvanian) Manzanita Mountains, New Mexico. Journal of Paleontology 53(1):169-174",13,164,418,W. Kiessling,S. Nurnberg,J. Karr,23/04/2005 01:56,03/02/2012 11:50,13324,indet.,,13324,,307,303.7,Kasimovian,,1,US, indet.
504423,occ,NA,,51265,,Discosauriscus austriacus,species,229318,,Discosauriscus austriacus,NA,species,229318,Stamberg,1997,Chordata,33815,Osteichthyes,34881,,NA,Discosauridae,320954,37209,NA,NA,NA,,16.656111,49.493057,"Kochov-Novici stratigraphic section, Boskovice Furrow",NA,,CZ,,,based on nearby landmark,seconds,outcrop,"Stratigraphic section between the villages of Kochov and Novici, northern region of the Boskovice Furrow, Orlice Basin, Czech Republic. Lat/long estimate based on Boskovice Jihomoravsky.",gp_mid,25.51,6.77,305,CZ,,,,,group of beds,,,,,,,NA,"Region apparently contains both upper Carboniferous and lower Permian strata, but collection appears to be from lower Permian. Stratigraphic section is detailed, but does not identify localition(s) of fauna and flora.","Most material from single horizon within stratigraphic section, which comprises grey bituminous laminated limestone.","""limestone""",planar lamination,,carbonaceous,Y,,,,,,terrestrial indet.,,No environmental information provided.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"Insects preserved as ""fragments of wings"", fish as ""spines, fragments of skeletons, and more complete skulls"". No comments on preservation of plant materials.",taxonomic,"selective quarrying,acetic,field collection,survey of museum collection",,,,,,,"Vertebrate material extracted using dilute acetic acid. Material is possibly reposited in the ""Museum Vychodnich Cech"". Collections at Masaryk University (Brno) and the Museum in Brno also inspected","Fossil plants identified by Z. Simunck (Geological Survey, Prague).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Discosauriscus,,NA,NA,"paleobotany,vertebrate","S. Stamberg. 1997. New discoveries of palaeoniscoid fishes and other fauna and flora from the northern region of Boskovice Furrow, Czech Republic. Journal of the Czech Geological Society 42(1-2):111-120",167,167,0,A. Hendy,A. Hendy,,01/06/2005 14:52,01/06/2005 16:52,13653,austriacus,Discosauriscus,13653,,298.9,290.1,Asselian,Sakmarian,NA,CZ,Discosauriscus austriacus
517728,occ,NA,,52522,,Onchiodon labyrinthicus,species,66913,,Onchiodon labyrinthicus,NA,species,66913,Boy,1990,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37013,NA,NA,NA,,13.650278,50.999722,Niederhaslich,NA,Niederh_sslich; Niederh_slich; Nieder-H_sslich; Plauenscher Grund; D̦hlen Basin,DE,Saxony,Weieritzkreis,based on nearby landmark,seconds,outcrop,"Niederh_slich in the D̦hlen basin, today it is one part of the City of Freital, SW of Dresden in Sachsen; the outcrop does not exist anymore.",gp_mid,23.3,7.73,305,DE,,Niederh_slich-Schweinsdorf,Rotliegend,Niederh_slich limestone,member,,,,,,,NA,"""The Niederh_slich Formation belongs stratigraphically [...] to the Melanerpeton gracile-M. pulcherimus Zone, i. e. uppermost Unterrotliegend"" (U. Hoffman, 2002, Workshop _Oberkarbon - Untertrias in Zentraleuropa: Prozesse und ihr Timing [online] http://www.geo.tu-freiberg.de/palaeo/GeoTage-2002.pdf) (TL);\r\nthe Niederh_slich limestone is Asselian according to assorted references, e.g., Gebhardt and Schneider 1993 (JA)\r\nAccording to Roscher & Schneider (2006, in Lucas et al. (eds), Geol. Soc. Spec. Publ. 265) the Niederh_slich Fm. is Sakmarian in age (TL).",,"""limestone""",,,,,,,,,,lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Museum: Staatliches Museum f_r Mineralogie und Geologie, Dresden (SMMGD)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Onchiodon,,NA,NA,vertebrate,"J. Boy. 1990. ber einige Vertreter der Eryopoidea (Amphibia: Temnospondyli) aus dem europ_ischen Rotliegend (?h̦chstes Karbon - Perm), 3. Onchiodon; (On some representatives of the Eryopoidea (Amphibia: Temnospondyli) from the European Rotliegend (?Uppermost Carboniferous - Permian), 3. Onchiodon). Pal_ontologische Zeitschrift 64(3/4):287-312",4,175,697,J. Alroy,S. Kuemmell,E. Dunne,10/08/2005 02:34,02/08/2016 12:56,14125,labyrinthicus,Onchiodon,14125,,295.5,290.1,Sakmarian,,NA,DE,Onchiodon labyrinthicus
517729,occ,NA,,52522,,Onchiodon aff. labyrinthicus,species,66913,,Onchiodon labyrinthicus,NA,species,66913,Boy,1990,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37013,NA,NA,NA,,13.650278,50.999722,Niederhaslich,NA,Niederh_sslich; Niederh_slich; Nieder-H_sslich; Plauenscher Grund; D̦hlen Basin,DE,Saxony,Weieritzkreis,based on nearby landmark,seconds,outcrop,"Niederh_slich in the D̦hlen basin, today it is one part of the City of Freital, SW of Dresden in Sachsen; the outcrop does not exist anymore.",gp_mid,23.3,7.73,305,DE,,Niederh_slich-Schweinsdorf,Rotliegend,Niederh_slich limestone,member,,,,,,,NA,"""The Niederh_slich Formation belongs stratigraphically [...] to the Melanerpeton gracile-M. pulcherimus Zone, i. e. uppermost Unterrotliegend"" (U. Hoffman, 2002, Workshop _Oberkarbon - Untertrias in Zentraleuropa: Prozesse und ihr Timing [online] http://www.geo.tu-freiberg.de/palaeo/GeoTage-2002.pdf) (TL);\r\nthe Niederh_slich limestone is Asselian according to assorted references, e.g., Gebhardt and Schneider 1993 (JA)\r\nAccording to Roscher & Schneider (2006, in Lucas et al. (eds), Geol. Soc. Spec. Publ. 265) the Niederh_slich Fm. is Sakmarian in age (TL).",,"""limestone""",,,,,,,,,,lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Museum: Staatliches Museum f_r Mineralogie und Geologie, Dresden (SMMGD)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Onchiodon,,NA,NA,vertebrate,"J. Boy. 1990. ber einige Vertreter der Eryopoidea (Amphibia: Temnospondyli) aus dem europ_ischen Rotliegend (?h̦chstes Karbon - Perm), 3. Onchiodon; (On some representatives of the Eryopoidea (Amphibia: Temnospondyli) from the European Rotliegend (?Uppermost Carboniferous - Permian), 3. Onchiodon). Pal_ontologische Zeitschrift 64(3/4):287-312",4,175,697,J. Alroy,S. Kuemmell,E. Dunne,10/08/2005 02:34,02/08/2016 12:56,14125,labyrinthicus,Onchiodon,14125,aff.,295.5,290.1,Sakmarian,,NA,DE,Onchiodon labyrinthicus
517730,occ,NA,,52522,,Branchiosaurus gracilis,species,345815,,Branchiosaurus gracilis,NA,species,345815,Boy,1990,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37039,NA,NA,NA,,13.650278,50.999722,Niederhaslich,NA,Niederh_sslich; Niederh_slich; Nieder-H_sslich; Plauenscher Grund; D̦hlen Basin,DE,Saxony,Weieritzkreis,based on nearby landmark,seconds,outcrop,"Niederh_slich in the D̦hlen basin, today it is one part of the City of Freital, SW of Dresden in Sachsen; the outcrop does not exist anymore.",gp_mid,23.3,7.73,305,DE,,Niederh_slich-Schweinsdorf,Rotliegend,Niederh_slich limestone,member,,,,,,,NA,"""The Niederh_slich Formation belongs stratigraphically [...] to the Melanerpeton gracile-M. pulcherimus Zone, i. e. uppermost Unterrotliegend"" (U. Hoffman, 2002, Workshop _Oberkarbon - Untertrias in Zentraleuropa: Prozesse und ihr Timing [online] http://www.geo.tu-freiberg.de/palaeo/GeoTage-2002.pdf) (TL);\r\nthe Niederh_slich limestone is Asselian according to assorted references, e.g., Gebhardt and Schneider 1993 (JA)\r\nAccording to Roscher & Schneider (2006, in Lucas et al. (eds), Geol. Soc. Spec. Publ. 265) the Niederh_slich Fm. is Sakmarian in age (TL).",,"""limestone""",,,,,,,,,,lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Museum: Staatliches Museum f_r Mineralogie und Geologie, Dresden (SMMGD)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchiosaurus,,NA,NA,vertebrate,"J. Boy. 1990. ber einige Vertreter der Eryopoidea (Amphibia: Temnospondyli) aus dem europ_ischen Rotliegend (?h̦chstes Karbon - Perm), 3. Onchiodon; (On some representatives of the Eryopoidea (Amphibia: Temnospondyli) from the European Rotliegend (?Uppermost Carboniferous - Permian), 3. Onchiodon). Pal_ontologische Zeitschrift 64(3/4):287-312",4,175,697,J. Alroy,S. Kuemmell,E. Dunne,10/08/2005 02:34,02/08/2016 12:56,14125,gracilis,Branchiosaurus,14125,,295.5,290.1,Sakmarian,,NA,DE,Branchiosaurus gracilis
517731,occ,NA,,52522,,Branchierpeton amblystomum,species,345310,,Branchierpeton amblystomum,NA,species,255225,Boy,1990,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Micromelerpetontidae,37041,37042,NA,NA,NA,,13.650278,50.999722,Niederhaslich,NA,Niederh_sslich; Niederh_slich; Nieder-H_sslich; Plauenscher Grund; D̦hlen Basin,DE,Saxony,Weieritzkreis,based on nearby landmark,seconds,outcrop,"Niederh_slich in the D̦hlen basin, today it is one part of the City of Freital, SW of Dresden in Sachsen; the outcrop does not exist anymore.",gp_mid,23.3,7.73,305,DE,,Niederh_slich-Schweinsdorf,Rotliegend,Niederh_slich limestone,member,,,,,,,NA,"""The Niederh_slich Formation belongs stratigraphically [...] to the Melanerpeton gracile-M. pulcherimus Zone, i. e. uppermost Unterrotliegend"" (U. Hoffman, 2002, Workshop _Oberkarbon - Untertrias in Zentraleuropa: Prozesse und ihr Timing [online] http://www.geo.tu-freiberg.de/palaeo/GeoTage-2002.pdf) (TL);\r\nthe Niederh_slich limestone is Asselian according to assorted references, e.g., Gebhardt and Schneider 1993 (JA)\r\nAccording to Roscher & Schneider (2006, in Lucas et al. (eds), Geol. Soc. Spec. Publ. 265) the Niederh_slich Fm. is Sakmarian in age (TL).",,"""limestone""",,,,,,,,,,lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Museum: Staatliches Museum f_r Mineralogie und Geologie, Dresden (SMMGD)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchierpeton,,NA,NA,vertebrate,"J. Boy. 1990. ber einige Vertreter der Eryopoidea (Amphibia: Temnospondyli) aus dem europ_ischen Rotliegend (?h̦chstes Karbon - Perm), 3. Onchiodon; (On some representatives of the Eryopoidea (Amphibia: Temnospondyli) from the European Rotliegend (?Uppermost Carboniferous - Permian), 3. Onchiodon). Pal_ontologische Zeitschrift 64(3/4):287-312",4,175,697,J. Alroy,S. Kuemmell,E. Dunne,10/08/2005 02:34,02/08/2016 12:56,14125,amblystomum,Branchierpeton,14125,,295.5,290.1,Sakmarian,,NA,DE,Branchierpeton amblystomum
517732,occ,NA,,52522,,Acanthostomatops vorax,species,345489,,Acanthostomatops vorax,NA,species,150298,Boy,1990,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,345488,NA,NA,NA,,13.650278,50.999722,Niederhaslich,NA,Niederh_sslich; Niederh_slich; Nieder-H_sslich; Plauenscher Grund; D̦hlen Basin,DE,Saxony,Weieritzkreis,based on nearby landmark,seconds,outcrop,"Niederh_slich in the D̦hlen basin, today it is one part of the City of Freital, SW of Dresden in Sachsen; the outcrop does not exist anymore.",gp_mid,23.3,7.73,305,DE,,Niederh_slich-Schweinsdorf,Rotliegend,Niederh_slich limestone,member,,,,,,,NA,"""The Niederh_slich Formation belongs stratigraphically [...] to the Melanerpeton gracile-M. pulcherimus Zone, i. e. uppermost Unterrotliegend"" (U. Hoffman, 2002, Workshop _Oberkarbon - Untertrias in Zentraleuropa: Prozesse und ihr Timing [online] http://www.geo.tu-freiberg.de/palaeo/GeoTage-2002.pdf) (TL);\r\nthe Niederh_slich limestone is Asselian according to assorted references, e.g., Gebhardt and Schneider 1993 (JA)\r\nAccording to Roscher & Schneider (2006, in Lucas et al. (eds), Geol. Soc. Spec. Publ. 265) the Niederh_slich Fm. is Sakmarian in age (TL).",,"""limestone""",,,,,,,,,,lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Museum: Staatliches Museum f_r Mineralogie und Geologie, Dresden (SMMGD)",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Acanthostomatops,,NA,NA,vertebrate,"J. Boy. 1990. ber einige Vertreter der Eryopoidea (Amphibia: Temnospondyli) aus dem europ_ischen Rotliegend (?h̦chstes Karbon - Perm), 3. Onchiodon; (On some representatives of the Eryopoidea (Amphibia: Temnospondyli) from the European Rotliegend (?Uppermost Carboniferous - Permian), 3. Onchiodon). Pal_ontologische Zeitschrift 64(3/4):287-312",4,175,697,J. Alroy,S. Kuemmell,E. Dunne,10/08/2005 02:34,02/08/2016 12:56,14125,vorax,Acanthostomatops,14125,,295.5,290.1,Sakmarian,,NA,DE,Acanthostomatops vorax
559541,occ,NA,,58139,,Branchiosaurus umbrosus,species,345813,recombined as,Apateon umbrosus,NA,species,345813,Augusta,1938,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,16.335833,50.583889,"Olivt_n, Broumov City, Boheme",NA,"Olivetin, Oelberg bei Branau",CZ,Boheme,,based on nearby landmark,seconds,,"Olivet_n, close to the City Broumov, Boheme\r\nGerman name of Olivetin (Oelberg) given by Estes 1970, J Paleont",gp_mid,26.98,10.91,305,CZ,,,,,,,,,,,,NA,"Lower Permian (i.e., Rotliegendes: JA)",,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"Geologic-paleontological department of the National-Museum, Prag",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchiosaurus,,NA,NA,vertebrate,"J. Augusta. 1938. Prispevek k poznani ontogenetickeho vyvoje stegocephala Branchiosaurus umbrosus Fr. ze spodnopermskych vapencu z Olivetina u Broumova v Cechach.; (Contribution to the knowledge of the ontgenetic development of the stegocephalian Branchiosaurus umbrosus Fr. from the Lower Permian limestone of Olevetin, close to Broumov, Boheme). Vestnik Kralovske Ceske Spolecnosti Nauk, Trida Methematicko-Prirodovedecka; (Soc. Roy. Sci. Boheme, Mem.) 8:1-9",4,175,697,J. Alroy,S. Kuemmell,E. Dunne,24/01/2006 02:12,02/08/2016 12:51,15696,umbrosus,Apateon,15696,,298.9,254,Rotliegendes,,NA,CZ,Apateon umbrosus
559542,occ,NA,,58139,,Melanerpeton pulcherrimum,species,320961,,Melanerpeton pulcherrimum,NA,species,320961,Augusta,1938,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,260059,NA,NA,NA,,16.335833,50.583889,"Olivt_n, Broumov City, Boheme",NA,"Olivetin, Oelberg bei Branau",CZ,Boheme,,based on nearby landmark,seconds,,"Olivet_n, close to the City Broumov, Boheme\r\nGerman name of Olivetin (Oelberg) given by Estes 1970, J Paleont",gp_mid,26.98,10.91,305,CZ,,,,,,,,,,,,NA,"Lower Permian (i.e., Rotliegendes: JA)",,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"Geologic-paleontological department of the National-Museum, Prag",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Melanerpeton,,NA,NA,vertebrate,"J. Augusta. 1938. Prispevek k poznani ontogenetickeho vyvoje stegocephala Branchiosaurus umbrosus Fr. ze spodnopermskych vapencu z Olivetina u Broumova v Cechach.; (Contribution to the knowledge of the ontgenetic development of the stegocephalian Branchiosaurus umbrosus Fr. from the Lower Permian limestone of Olevetin, close to Broumov, Boheme). Vestnik Kralovske Ceske Spolecnosti Nauk, Trida Methematicko-Prirodovedecka; (Soc. Roy. Sci. Boheme, Mem.) 8:1-9",4,175,697,J. Alroy,S. Kuemmell,E. Dunne,24/01/2006 02:12,31/07/2016 15:25,15696,pulcherrimum,Melanerpeton,15696,,298.9,254,Rotliegendes,,NA,CZ,Melanerpeton pulcherrimum
628181,occ,NA,,67737,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Westgate,1989,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.75,32.130001,Taylor County Site 7 (Pelecypods),NA,B.E.G. 30996; W.P.A. quarry,US,Texas,Taylor,based on nearby landmark,2,small collection,"""souther part of Taylor County, Texas, in the SW 1/4 of section 436 of the M. P. King survey, on the property of Mr. C.O. Patterson, Route 1, Lawn, Texas... 6 miles southwest of the small town of Lawn"" (coordinate based on Lawn)",gp_mid,-30.15,0.6,101,US,,Vale,,,group of beds,,,,,,,NA,"""22 feet above the Vale-Standpipe contact""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""limestone, clay-pebble conglomerate which pinches out laterally""",conglomerate,,,argillaceous,,,,,,,coarse channel fill,,"""streams of running water""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"selective quarrying,field collection",,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,,"J. W. Westgate. 1989. Lower vertebrates from an estuarine facies of the Middle Eocene Laredo Formation (Claiborne Group), Webb County, Texas. Journal of Vertebrate Paleontology 9(3):282-294",4,4,0,J. Alroy,J. Alroy,,07/12/2006 13:36,07/12/2006 15:36,19359,sp.,Dimetrodon,702,,279.3,272.3,Kungurian,,NA,US,Dimetrodon sp.
629465,occ,NA,R,67862,,Eryops ? sp.,genus,37011,,Eryops,NA,genus,37011,Olson,1991,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,?,NA,NA,"paleoentomology,vertebrate","E. C. Olson. 1991. An Eryopid (Amphibia: Labyrinthodontia) from the Fort Sill Fissures, Lower Permian, Oklahoma. Journal of Vertebrate Paleontology 11(1):130-132",4,4,697,J. Alroy,J. Alroy,E. Dunne,13/12/2006 21:38,24/08/2016 08:20,19393,sp.,Eryops,28693,,290.1,268,Leonard,,1,US,Eryops sp.
629465,occ,24456,,67862,,Temnospondyli indet.,unranked clade,36320,,Temnospondyli,NA,unranked clade,36320,Polley and Reisz,2011,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,NA,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Temnospondyli,,NA,NA,"paleoentomology,vertebrate","B. P. Polley and R. R. Reisz. 2011. A new Lower Permian trematopid (Temnospondyli: Dissorophoidea) from Richards Spur, Oklahoma. Zoological Journal of the Linnean Society 161:789-815",327,327,327,R. Butler,R. Butler,R. Butler,22/03/2011 19:25,22/03/2011 03:25,19393,indet.,,35587,,290.1,268,Leonard,,1,US, indet.
629466,occ,NA,R,67862,,Cacops cf. aspidephorus,species,56737,,Cacops aspidephorus,NA,species,56737,Bolt,1977,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37025,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Cacops,,NA,NA,"paleoentomology,vertebrate","J. R. Bolt. 1977. Cacops (Amphibia: Labyrinthodontia) From the Fort Sill Locality, Lower Permian of Oklahoma. Fieldiana: Geology 37(3):61-73",4,4,697,J. Alroy,J. Alroy,E. Dunne,13/12/2006 21:38,24/08/2016 08:20,19393,aspidephorus,Cacops,29098,cf.,290.1,268,Leonard,,7,US,Cacops aspidephorus
629466,occ,23974,,67862,,Cacops n. sp. morrisi,species,175857,,Cacops morrisi,NA,species,175857,Reisz et al.,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37025,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Cacops,,NA,NA,"paleoentomology,vertebrate","R. R. Reisz, R. R. Schoch, and J. S. Anderson\r\n. 2009. The armoured dissorophid Cacops from the Early Permian of Oklahoma and the exploitation of the terrestrial realm by amphibians. Naturwissenschaften 96:789-796",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,30/01/2011 12:56,26/02/2012 20:55,19393,morrisi,Cacops,34955,n. sp.,290.1,268,Leonard,,7,US,Cacops morrisi
629467,occ,NA,,67862,,n. gen. Doleserpeton n. sp. annectens,species,140536,,Doleserpeton annectens,NA,species,140536,Bolt,1969,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,37046,NA,NA,NA,,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Doleserpeton,n. gen.,NA,NA,"paleoentomology,vertebrate",J. R. Bolt. 1969. Lissamphibian Origins: Possible Protolissamphibian from the Lower Permian of Oklahoma. Science 166:888-891,4,4,334,J. Alroy,J. Alroy,T. Liebrecht,13/12/2006 21:38,29/07/2009 11:27,19393,annectens,Doleserpeton,28686,n. sp.,290.1,268,Leonard,,NA,US,Doleserpeton annectens
629468,occ,NA,,67862,,Tersomius sp.,genus,37035,,Tersomius,NA,genus,37035,Bolt,1980,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,37035,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Tersomius,,NA,NA,"paleoentomology,vertebrate","J. R. Bolt. 1980. New tetrapods with bicuspid teeth from the Fort Sill Locality (Lower Permian, Oklahoma). Neues Jahrbuch f_r Geologie und Pal_ontologie, Monatshefte 1980(8):449-459",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,13/12/2006 21:38,29/07/2009 11:27,19393,sp.,Tersomius,28699,,290.1,268,Leonard,,1,US,Tersomius sp.
629469,occ,NA,,67862,,Trematopsidae indet.,family,37047,corrected to,Trematopidae,NA,family,37047,Bolt,1974,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,NA,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Trematopsidae,,NA,NA,"paleoentomology,vertebrate","J. R. Bolt. 1974. A Trematopsid Skull from the Lower Permian, and Analysis of Some Characters of the Dissorophoid (Amphibia: Labyrinthodontia) Otic Notch. Fieldiana: Geology 30(3):67-79",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,13/12/2006 21:38,29/07/2009 11:27,19393,indet.,,29097,,290.1,268,Leonard,,1,US, indet.
629470,occ,NA,,67862,,Seymouria sp.,genus,37223,,Seymouria,NA,genus,37223,Sullivan and Reisz,1999,Chordata,33815,Osteichthyes,34881,,NA,Seymouriidae,37219,37223,NA,NA,NA,elements,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Seymouria,,NA,NA,"paleoentomology,vertebrate","C. Sullivan and R. R. Reisz. 1999. First record of Seymouria (Vertebrata: Seymouriamorpha) from Early Permian fissure fills at Richards Spur, Oklahoma. Canadian Journal of Earth Sciences 36(8):1257-1266",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,13/12/2006 21:38,29/07/2009 11:27,19393,sp.,Seymouria,19393,,290.1,268,Leonard,,7,US,Seymouria sp.
629471,occ,NA,R,67862,,Aistopoda sp.,genus,156842,,Aistopoda,NA,suborder,37251,Gregory et al.,1956,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,,NA,NA,NA,NA,NA,specimens,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Aistopoda,,NA,NA,"paleoentomology,vertebrate","J. T. Gregory, F. E. Peabody, and L. I. Price. 1956. Revision of the Gymnarthridae - American Permian Microsaurs. Bulletin of the Peabody Museum of Natural History 10:1-77",4,4,697,J. Alroy,J. Alroy,E. Dunne,13/12/2006 21:38,24/08/2016 08:20,19393,sp.,,28484,,290.1,268,Leonard,,7,US, sp.
629471,occ,22349,R,67862,,Phlegethontia cf. longissima,species,156845,,Phlegethontia longissima,NA,species,156844,McGinnis,1967,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,37259,NA,NA,NA,specimens,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Phlegethontia,,NA,NA,"paleoentomology,vertebrate","H. J. McGinnis. 1967. The Osteology of Phlegethontia, a Carboniferous and Permian Astopod Amphibian. University of California Publications in Geological Sciences 71:1-46",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,03/11/2009 05:51,24/03/2010 13:26,19393,longissima,Phlegethontia,31050,cf.,290.1,268,Leonard,,7,US,Phlegethontia longissima
629471,occ,23009,,67862,,n. gen. Sillerpeton n. sp. permianum,species,156770,,Sillerpeton permianum,NA,species,156770,Lund,1978,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,156767,NA,NA,NA,specimens,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Sillerpeton,n. gen.,NA,NA,"paleoentomology,vertebrate","R. Lund. 1978. Anatomy and Relationships of the Family Phlegethontiidae (Amphibia, Astopoda). Annals of Carnegie Museum 47(4):53-79",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,24/03/2010 11:24,24/03/2010 13:26,19393,permianum,Sillerpeton,31052,n. sp.,290.1,268,Leonard,,7,US,Sillerpeton permianum
629472,occ,NA,R,67862,,Cardiocephalus cf. sternbergi,species,90715,,Cardiocephalus sternbergi,NA,species,90715,Gregory et al.,1956,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37294,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Cardiocephalus,,NA,NA,"paleoentomology,vertebrate","J. T. Gregory, F. E. Peabody, and L. I. Price. 1956. Revision of the Gymnarthridae - American Permian Microsaurs. Bulletin of the Peabody Museum of Natural History 10:1-77",4,4,697,J. Alroy,J. Alroy,E. Dunne,13/12/2006 21:38,24/08/2016 08:20,19393,sternbergi,Cardiocephalus,28484,cf.,290.1,268,Leonard,,25,US,Cardiocephalus sternbergi
629472,occ,23007,,67862,,Cardiocephalus n. sp. peabodyi,species,137293,,Cardiocephalus peabodyi,NA,species,137293,Carroll and Gaskill,1978,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37294,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Cardiocephalus,,NA,NA,"paleoentomology,vertebrate",R. L. Carroll and P. Gaskill. 1978. The Order Microsauria. Memoirs of the American Philosophical Society 126:1-211,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,24/03/2010 09:56,24/03/2010 12:22,19393,peabodyi,Cardiocephalus,28692,n. sp.,290.1,268,Leonard,,25,US,Cardiocephalus peabodyi
629473,occ,NA,R,67862,,Euryodus primus,species,120864,,Euryodus primus,NA,species,120864,Gregory et al.,1956,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37296,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Euryodus,,NA,NA,"paleoentomology,vertebrate","J. T. Gregory, F. E. Peabody, and L. I. Price. 1956. Revision of the Gymnarthridae - American Permian Microsaurs. Bulletin of the Peabody Museum of Natural History 10:1-77",4,4,697,J. Alroy,J. Alroy,E. Dunne,13/12/2006 21:38,24/08/2016 08:20,19393,primus,Euryodus,28484,,290.1,268,Leonard,,25,US,Euryodus primus
629473,occ,23008,,67862,,Euryodus cf. primus,species,120864,,Euryodus primus,NA,species,120864,Carroll and Gaskill,1978,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37296,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Euryodus,,NA,NA,"paleoentomology,vertebrate",R. L. Carroll and P. Gaskill. 1978. The Order Microsauria. Memoirs of the American Philosophical Society 126:1-211,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,24/03/2010 09:58,24/03/2010 12:19,19393,primus,Euryodus,28692,cf.,290.1,268,Leonard,,25,US,Euryodus primus
629474,occ,NA,,67862,,n. gen. Llistrofus n. sp. pricei,species,137291,,Llistrofus pricei,NA,species,137291,Carroll and Gaskill,1978,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Hapsidopareiontidae,37285,37287,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Llistrofus,n. gen.,NA,NA,"paleoentomology,vertebrate",R. L. Carroll and P. Gaskill. 1978. The Order Microsauria. Memoirs of the American Philosophical Society 126:1-211,4,4,334,J. Alroy,J. Alroy,T. Liebrecht,13/12/2006 21:38,29/07/2009 11:27,19393,pricei,Llistrofus,28692,n. sp.,290.1,268,Leonard,,1,US,Llistrofus pricei
629475,occ,NA,R,67862,,Parareptilia indet.,subclass,138228,,Parareptilia,NA,subclass,99778,Sullivan and Reisz,1999,Chordata,33815,Reptilia,36322,,NA,,NA,NA,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Parareptilia,,NA,NA,"paleoentomology,vertebrate","C. Sullivan and R. R. Reisz. 1999. First record of Seymouria (Vertebrata: Seymouriamorpha) from Early Permian fissure fills at Richards Spur, Oklahoma. Canadian Journal of Earth Sciences 36(8):1257-1266",4,4,697,J. Alroy,J. Alroy,E. Dunne,13/12/2006 21:38,24/08/2016 08:20,19393,indet.,,19393,,290.1,268,Leonard,,45,US, indet.
629475,occ,26482,,67862,,Bolterpeton ? sp.,genus,223733,,Bolterpeton,NA,genus,223733,Anderson and Reisz,2003,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,223733,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Bolterpeton,?,NA,NA,"paleoentomology,vertebrate","J. S. Anderson and R. R. Reisz. 2003. A new microsaur (Tetrapoda: Lepospondyli) from the Lower Permian of Richards Spur (Fort Sill), Oklahoma. Canadian Journal of Earth Sciences 40(4):499-505",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,27/02/2012 13:09,24/01/2013 15:28,19393,sp.,Bolterpeton,40439,,290.1,268,Leonard,,45,US,Bolterpeton sp.
629476,occ,NA,,67862,,n. gen. Colobomycter n. sp. pholeter,species,123513,,Colobomycter pholeter,NA,species,123513,Vaughn,1958,Chordata,33815,Reptilia,36322,,NA,Acleistorhinidae,37514,38921,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Colobomycter,n. gen.,NA,NA,"paleoentomology,vertebrate","P. P. Vaughn. 1958. On a New Pelycosaur from the Lower Permian of Oklahoma, and on the Origin of the Family Caseidae. Journal of Paleontology 32(5):981-991",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,13/12/2006 21:42,25/03/2010 11:17,19393,pholeter,Colobomycter,28627,n. sp.,290.1,268,Leonard,,3,US,Colobomycter pholeter
629477,occ,NA,,67862,,Captorhinus aguti,species,90718,,Captorhinus aguti,NA,species,134887,Sullivan and Reisz,1999,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,"paleoentomology,vertebrate","C. Sullivan and R. R. Reisz. 1999. First record of Seymouria (Vertebrata: Seymouriamorpha) from Early Permian fissure fills at Richards Spur, Oklahoma. Canadian Journal of Earth Sciences 36(8):1257-1266",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,13/12/2006 21:42,25/03/2010 11:17,19393,aguti,Captorhinus,19393,,290.1,268,Leonard,,91,US,Captorhinus aguti
629479,occ,NA,,67862,,Captorhinidae sp.,genus,37495,,Captorhinidae,NA,family,37495,Modesto,1996,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,NA,NA,NA,NA,specimens,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinidae,,NA,NA,"paleoentomology,vertebrate","S. P. Modesto. 1996. A Basal Captorhinid Reptile from the Fort Sill Fissures, Lower Permian of Oklahoma. Oklahoma Geology Notes 56:4-14",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,13/12/2006 21:42,29/07/2009 11:27,19393,sp.,,28422,,290.1,268,Leonard,,2,US, sp.
629480,occ,NA,,67862,,n. gen. Baeotherates n. sp. fortsillensis,species,137519,,Baeotherates fortsillensis,NA,species,137519,May and Cifelli,1998,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,137518,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Baeotherates,n. gen.,NA,NA,"paleoentomology,vertebrate","W. J. May and R. L. Cifelli. 1998. Baeotherates fortsillensis, A New Captorhinid Reptile from the Fort Sill Fissures, Lower Permian of Oklahoma. Oklahoma Geology Notes 58:128-137",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,13/12/2006 21:42,29/07/2009 11:27,19393,fortsillensis,Baeotherates,28772,n. sp.,290.1,268,Leonard,,1,US,Baeotherates fortsillensis
629481,occ,NA,R,67862,,Bolosaurus sp.,genus,37511,,Bolosaurus,NA,genus,37511,Sullivan and Reisz,1999,Chordata,33815,Reptilia,36322,,NA,Bolosauridae,37510,37511,NA,NA,NA,elements,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Bolosaurus,,NA,NA,"paleoentomology,vertebrate","C. Sullivan and R. R. Reisz. 1999. First record of Seymouria (Vertebrata: Seymouriamorpha) from Early Permian fissure fills at Richards Spur, Oklahoma. Canadian Journal of Earth Sciences 36(8):1257-1266",4,4,697,J. Alroy,J. Alroy,E. Dunne,13/12/2006 21:42,24/08/2016 08:20,19393,sp.,Bolosaurus,19393,,290.1,268,Leonard,,3,US,Bolosaurus sp.
629481,occ,21274,,67862,,Bolosaurus n. sp. grandis,species,140523,,Bolosaurus grandis,NA,species,140523,Reisz et al.,2002,Chordata,33815,Reptilia,36322,,NA,Bolosauridae,37510,37511,NA,NA,NA,elements,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Bolosaurus,,NA,NA,"paleoentomology,vertebrate","R. R. Reisz, V. Barkas, and D. Scott. 2002. A New Early Permian Bolosaurid Reptile from the Richards Spur Dolese Brothers Quarry, near Fort Sill, Oklahoma. Journal of Vertebrate Paleontology 22(1):23-28",315,334,0,J. Mueller,T. Liebrecht,,30/01/2009 04:31,30/01/2009 06:31,19393,grandis,Bolosaurus,29094,n. sp.,290.1,268,Leonard,,3,US,Bolosaurus grandis
629482,occ,NA,,67862,,n. gen. Delorhynchus n. sp. priscus,species,123514,,Delorhynchus priscus,NA,species,123514,Fox,1962,Chordata,33815,Reptilia,36322,,NA,,NA,38922,NA,NA,NA,fragments,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Delorhynchus,n. gen.,NA,NA,"paleoentomology,vertebrate","R. C. Fox. 1962. Two New Pelycosaurs from the Lower Permian of Oklahoma. University of Kansas Publications, Museum of Natural History 12(6):297-307",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,13/12/2006 21:42,19/03/2010 20:30,19393,priscus,Delorhynchus,29090,n. sp.,290.1,268,Leonard,,3,US,Delorhynchus priscus
629483,occ,NA,,67862,,n. gen. Thrausmosaurus n. sp. serratidens,species,140504,nomen dubium,Varanopidae,NA,family,95329,Fox,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,NA,NA,NA,NA,fragments,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Thrausmosaurus,n. gen.,NA,NA,"paleoentomology,vertebrate","R. C. Fox. 1962. Two New Pelycosaurs from the Lower Permian of Oklahoma. University of Kansas Publications, Museum of Natural History 12(6):297-307",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,13/12/2006 21:42,19/03/2010 20:31,19393,serratidens,,29090,n. sp.,290.1,268,Leonard,,3,US, serratidens
629484,occ,NA,R,67862,,Caseidae indet.,family,38913,,Caseidae,NA,family,38913,Sullivan and Reisz,1999,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,NA,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Caseidae,,NA,NA,"paleoentomology,vertebrate","C. Sullivan and R. R. Reisz. 1999. First record of Seymouria (Vertebrata: Seymouriamorpha) from Early Permian fissure fills at Richards Spur, Oklahoma. Canadian Journal of Earth Sciences 36(8):1257-1266",4,4,697,J. Alroy,J. Alroy,E. Dunne,13/12/2006 21:42,24/08/2016 08:20,19393,indet.,,19393,,290.1,268,Leonard,,1,US, indet.
629484,occ,21250,,67862,,n. gen. Oromycter n. sp. dolesorum,species,140367,,Oromycter dolesorum,NA,species,140367,Reisz,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,140366,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Oromycter,n. gen.,NA,NA,"paleoentomology,vertebrate","R. R. Reisz. 2005. Oromycter, a New Caseid from the Lower Permian of Oklahoma. Journal of Vertebrate Paleontology 25(4):905-910",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,26/01/2009 09:40,26/01/2009 11:42,19393,dolesorum,Oromycter,29061,n. sp.,290.1,268,Leonard,,1,US,Oromycter dolesorum
629485,occ,NA,R,67862,,Mycterosaurus ? sp.,genus,38895,,Mycterosaurus,NA,genus,38895,Olson,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,38895,NA,NA,NA,elements,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Mycterosaurus,?,NA,NA,"paleoentomology,vertebrate",E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,4,4,697,J. Alroy,J. Alroy,E. Dunne,13/12/2006 21:42,24/08/2016 08:20,19393,sp.,Mycterosaurus,28557,,290.1,268,Leonard,,10,US,Mycterosaurus sp.
629485,occ,23011,,67862,,Mycterosaurus longiceps,species,122319,,Mycterosaurus longiceps,NA,species,122319,Reisz et al.,1997,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,38895,NA,NA,NA,elements,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Mycterosaurus,,NA,NA,"paleoentomology,vertebrate","R. R. Reisz, H. Wilson, and D. Scott. 1997. Varanopseid Synapsid Skeletal Elements from Richards Spur, a Lower Permian Fissure Fill Near Fort Sill, Oklahoma. Oklahoma Geology Notes 57(5):160-170",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,24/03/2010 12:19,24/03/2010 14:26,19393,longiceps,Mycterosaurus,32334,,290.1,268,Leonard,,10,US,Mycterosaurus longiceps
629486,occ,NA,R,67862,,Varanopseidae indet.,family,38892,obsolete variant of,Varanopidae,NA,family,95329,Sullivan and Reisz,1999,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,NA,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Varanopseidae,,NA,NA,"paleoentomology,vertebrate","C. Sullivan and R. R. Reisz. 1999. First record of Seymouria (Vertebrata: Seymouriamorpha) from Early Permian fissure fills at Richards Spur, Oklahoma. Canadian Journal of Earth Sciences 36(8):1257-1266",4,4,697,J. Alroy,J. Alroy,E. Dunne,13/12/2006 21:42,24/08/2016 08:20,19393,indet.,,19393,,290.1,268,Leonard,,3,US, indet.
629486,occ,18844,,67862,,Varanops cf. brevirostris,species,91795,,Varanops brevirostris,NA,species,122316,Maddin et al.,2006,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,38897,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Varanops,,NA,NA,"paleoentomology,vertebrate","H. C. Maddin, D. C. Evans, and R. R. Reisz. 2006. An Early Permian varanodontine varanopid (Synapsida: Eupelycosauria) from the Richards Spur locality, Oklahoma. Journal of Vertebrate Paleontology 26(4):957-966",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,05/01/2007 15:38,30/01/2009 08:54,19393,brevirostris,Varanops,19596,cf.,290.1,268,Leonard,,3,US,Varanops brevirostris
629487,occ,NA,R,67862,,Diapsida ? indet.,unranked clade,37768,,Diapsida,NA,unranked clade,37768,Carroll,1968,Chordata,33815,Reptilia,36322,,NA,,NA,NA,NA,NA,NA,elements,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diapsida,?,NA,NA,"paleoentomology,vertebrate","R. L. Carroll. 1968. A ?Diapsid Parietal from the Lower Permian of Oklahoma. Postilla, Peabody Museum of Natural History, Yale University 117:1-7",4,4,697,J. Alroy,J. Alroy,E. Dunne,13/12/2006 21:42,24/08/2016 08:20,19393,indet.,,29096,,290.1,268,Leonard,,1,US, indet.
629487,occ,21275,,67862,,Neodiapsida indet.,unranked clade,92209,,Neodiapsida,NA,unranked clade,92209,Sullivan and Reisz,1999,Chordata,33815,Reptilia,36322,Eosuchia,37795,,NA,NA,NA,NA,NA,elements,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Neodiapsida,,NA,NA,"paleoentomology,vertebrate","C. Sullivan and R. R. Reisz. 1999. First record of Seymouria (Vertebrata: Seymouriamorpha) from Early Permian fissure fills at Richards Spur, Oklahoma. Canadian Journal of Earth Sciences 36(8):1257-1266",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,30/01/2009 07:25,30/01/2009 09:26,19393,indet.,,19393,,290.1,268,Leonard,,1,US, indet.
629488,occ,NA,,67862,,Acheloma cf. cumminsi,species,81713,,Acheloma cumminsi,NA,species,81713,Sullivan et al.,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,37048,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Acheloma,,NA,NA,"paleoentomology,vertebrate","C. Sullivan, R. R. Reisz, and W. J. May. 2000. Large dissorophoid skeletal elements from the Lower Permian Richards Spur fissures, Oklahoma, and their paleoecological implications. Journal of Vertebrate Paleontology 20(3):456-461",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,13/12/2006 21:54,29/07/2009 11:27,19393,cumminsi,Acheloma,19394,cf.,290.1,268,Leonard,,2,US,Acheloma cumminsi
629489,occ,NA,,67862,,cf. Cacops sp.,genus,37025,,Cacops,NA,genus,37025,Sullivan et al.,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37025,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Cacops,cf.,NA,NA,"paleoentomology,vertebrate","C. Sullivan, R. R. Reisz, and W. J. May. 2000. Large dissorophoid skeletal elements from the Lower Permian Richards Spur fissures, Oklahoma, and their paleoecological implications. Journal of Vertebrate Paleontology 20(3):456-461",4,4,334,J. Alroy,J. Alroy,T. Liebrecht,13/12/2006 21:54,29/07/2009 11:27,19393,sp.,Cacops,19394,,290.1,268,Leonard,,1,US,Cacops sp.
631438,occ,NA,,67945,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Daly,1973,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,fragments,-98.787781,34.18972,South Grandfield,NA,,US,Oklahoma,Tillman,stated in text,seconds,small collection,"""SW1/4 SE1/4 SE1/4 sec. 20, T. 4 S, R. 15 W. This is 6 1/2 miles southwest of Grandfield... 3 miles north of the Red River...""\neast side of ""a depression about fifty feet deep... near the top... [fossils] from the surface of a nose or ridge... three to four feet high and ten to twenty-five fee in area.""",gp_mid,-28.41,1.95,101,US,,Hennessey,,,bed,,,,,,,NA,"""lower third"" of a 9 foot bed\n""when the known lower boundary of the Arroyo [Formation] is extrapolated northward... it passes through the South Grandfield site.""\nthe Arroyo is within the Clear Fork Group, all of which is Kungurian (see discussion of Romer 1928 collections)","""Red shale spotted with pale green, containing lenses of fissile red sandstone and of stratified dark red fine conglomerate.""","""shale""","green,red",,,,sandstone,"""cross stratification"",red",poorly lithified,,,fluvial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""remains were assembled by moving water, after transport for a long or short distance... It is usual for the skull specimens... to have the mandibles in place... This suggests that the predators and scavengers... may have customarily discarded the heads... cranial remains have been selectively preserved...""\ncounts are given of 281 skulls and skull parts; 346 vertebrae, strings of vertebrae, and pieces of vertebrae; 109 limb bones and pieces of limb bones; and 29 partial girdles",general faunal/floral,"surface (float),field collection,survey of museum collection",FMNH,,,,,,"""Bone and bone-containing nodules may be collected from the surface... An effort to excavate for fossils was not productive... about forty pounds of red shale... was washed [and] five scraps of bone were recovered, none identifiable.""\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",not the same as the two West Grandfield sites of Olson 1967,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,E. Daly. 1973. A Lower Permian vertebrate fauna from southern Oklahoma. Journal of Paleontology 47(3):562-589,4,4,697,J. Alroy,J. Alroy,E. Dunne,18/12/2006 14:47,21/07/2016 07:19,19411,sp.,Trimerorhachis,19411,,279.3,272.3,Kungurian,,7,US,Trimerorhachis sp.
631439,occ,NA,,67945,,Tersomius cf. texensis,species,90713,,Tersomius texensis,NA,species,90713,Daly,1973,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,37035,NA,NA,NA,specimens,-98.787781,34.18972,South Grandfield,NA,,US,Oklahoma,Tillman,stated in text,seconds,small collection,"""SW1/4 SE1/4 SE1/4 sec. 20, T. 4 S, R. 15 W. This is 6 1/2 miles southwest of Grandfield... 3 miles north of the Red River...""\neast side of ""a depression about fifty feet deep... near the top... [fossils] from the surface of a nose or ridge... three to four feet high and ten to twenty-five fee in area.""",gp_mid,-28.41,1.95,101,US,,Hennessey,,,bed,,,,,,,NA,"""lower third"" of a 9 foot bed\n""when the known lower boundary of the Arroyo [Formation] is extrapolated northward... it passes through the South Grandfield site.""\nthe Arroyo is within the Clear Fork Group, all of which is Kungurian (see discussion of Romer 1928 collections)","""Red shale spotted with pale green, containing lenses of fissile red sandstone and of stratified dark red fine conglomerate.""","""shale""","green,red",,,,sandstone,"""cross stratification"",red",poorly lithified,,,fluvial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""remains were assembled by moving water, after transport for a long or short distance... It is usual for the skull specimens... to have the mandibles in place... This suggests that the predators and scavengers... may have customarily discarded the heads... cranial remains have been selectively preserved...""\ncounts are given of 281 skulls and skull parts; 346 vertebrae, strings of vertebrae, and pieces of vertebrae; 109 limb bones and pieces of limb bones; and 29 partial girdles",general faunal/floral,"surface (float),field collection,survey of museum collection",FMNH,,,,,,"""Bone and bone-containing nodules may be collected from the surface... An effort to excavate for fossils was not productive... about forty pounds of red shale... was washed [and] five scraps of bone were recovered, none identifiable.""\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",not the same as the two West Grandfield sites of Olson 1967,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Tersomius,,NA,NA,vertebrate,E. Daly. 1973. A Lower Permian vertebrate fauna from southern Oklahoma. Journal of Paleontology 47(3):562-589,4,4,334,J. Alroy,J. Alroy,T. Liebrecht,18/12/2006 14:47,25/08/2009 10:54,19411,texensis,Tersomius,19411,cf.,279.3,272.3,Kungurian,,80,US,Tersomius texensis
631440,occ,NA,,67945,,Peronedon primus,species,119362,recombined as,Diplocaulus primus,NA,species,119362,Haglund,1977,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,specimens,-98.787781,34.18972,South Grandfield,NA,,US,Oklahoma,Tillman,stated in text,seconds,small collection,"""SW1/4 SE1/4 SE1/4 sec. 20, T. 4 S, R. 15 W. This is 6 1/2 miles southwest of Grandfield... 3 miles north of the Red River...""\neast side of ""a depression about fifty feet deep... near the top... [fossils] from the surface of a nose or ridge... three to four feet high and ten to twenty-five fee in area.""",gp_mid,-28.41,1.95,101,US,,Hennessey,,,bed,,,,,,,NA,"""lower third"" of a 9 foot bed\n""when the known lower boundary of the Arroyo [Formation] is extrapolated northward... it passes through the South Grandfield site.""\nthe Arroyo is within the Clear Fork Group, all of which is Kungurian (see discussion of Romer 1928 collections)","""Red shale spotted with pale green, containing lenses of fissile red sandstone and of stratified dark red fine conglomerate.""","""shale""","green,red",,,,sandstone,"""cross stratification"",red",poorly lithified,,,fluvial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""remains were assembled by moving water, after transport for a long or short distance... It is usual for the skull specimens... to have the mandibles in place... This suggests that the predators and scavengers... may have customarily discarded the heads... cranial remains have been selectively preserved...""\ncounts are given of 281 skulls and skull parts; 346 vertebrae, strings of vertebrae, and pieces of vertebrae; 109 limb bones and pieces of limb bones; and 29 partial girdles",general faunal/floral,"surface (float),field collection,survey of museum collection",FMNH,,,,,,"""Bone and bone-containing nodules may be collected from the surface... An effort to excavate for fossils was not productive... about forty pounds of red shale... was washed [and] five scraps of bone were recovered, none identifiable.""\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",not the same as the two West Grandfield sites of Olson 1967,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Peronedon,,NA,NA,vertebrate,T. R. Haglund. 1977. New Occurences and Paleoecology of Peronedon primus Olson (Nectridea). Journal of Paleontology 51(5):982-985,4,4,334,J. Alroy,J. Alroy,T. Liebrecht,18/12/2006 14:47,25/08/2009 11:19,19411,primus,Diplocaulus,30419,,279.3,272.3,Kungurian,,3,US,Diplocaulus primus
631441,occ,NA,,67945,,Lysorophus cf. tricarinatus,species,70395,,Lysorophus tricarinatus,NA,species,70395,Daly,1973,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,individuals,-98.787781,34.18972,South Grandfield,NA,,US,Oklahoma,Tillman,stated in text,seconds,small collection,"""SW1/4 SE1/4 SE1/4 sec. 20, T. 4 S, R. 15 W. This is 6 1/2 miles southwest of Grandfield... 3 miles north of the Red River...""\neast side of ""a depression about fifty feet deep... near the top... [fossils] from the surface of a nose or ridge... three to four feet high and ten to twenty-five fee in area.""",gp_mid,-28.41,1.95,101,US,,Hennessey,,,bed,,,,,,,NA,"""lower third"" of a 9 foot bed\n""when the known lower boundary of the Arroyo [Formation] is extrapolated northward... it passes through the South Grandfield site.""\nthe Arroyo is within the Clear Fork Group, all of which is Kungurian (see discussion of Romer 1928 collections)","""Red shale spotted with pale green, containing lenses of fissile red sandstone and of stratified dark red fine conglomerate.""","""shale""","green,red",,,,sandstone,"""cross stratification"",red",poorly lithified,,,fluvial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""remains were assembled by moving water, after transport for a long or short distance... It is usual for the skull specimens... to have the mandibles in place... This suggests that the predators and scavengers... may have customarily discarded the heads... cranial remains have been selectively preserved...""\ncounts are given of 281 skulls and skull parts; 346 vertebrae, strings of vertebrae, and pieces of vertebrae; 109 limb bones and pieces of limb bones; and 29 partial girdles",general faunal/floral,"surface (float),field collection,survey of museum collection",FMNH,,,,,,"""Bone and bone-containing nodules may be collected from the surface... An effort to excavate for fossils was not productive... about forty pounds of red shale... was washed [and] five scraps of bone were recovered, none identifiable.""\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",not the same as the two West Grandfield sites of Olson 1967,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,E. Daly. 1973. A Lower Permian vertebrate fauna from southern Oklahoma. Journal of Paleontology 47(3):562-589,4,4,334,J. Alroy,J. Alroy,T. Liebrecht,18/12/2006 14:47,25/08/2009 10:54,19411,tricarinatus,Lysorophus,19411,cf.,279.3,272.3,Kungurian,,1,US,Lysorophus tricarinatus
631442,occ,NA,,67945,,Cardiocephalus cf. sternbergi,species,90715,,Cardiocephalus sternbergi,NA,species,90715,Daly,1973,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37294,NA,NA,NA,specimens,-98.787781,34.18972,South Grandfield,NA,,US,Oklahoma,Tillman,stated in text,seconds,small collection,"""SW1/4 SE1/4 SE1/4 sec. 20, T. 4 S, R. 15 W. This is 6 1/2 miles southwest of Grandfield... 3 miles north of the Red River...""\neast side of ""a depression about fifty feet deep... near the top... [fossils] from the surface of a nose or ridge... three to four feet high and ten to twenty-five fee in area.""",gp_mid,-28.41,1.95,101,US,,Hennessey,,,bed,,,,,,,NA,"""lower third"" of a 9 foot bed\n""when the known lower boundary of the Arroyo [Formation] is extrapolated northward... it passes through the South Grandfield site.""\nthe Arroyo is within the Clear Fork Group, all of which is Kungurian (see discussion of Romer 1928 collections)","""Red shale spotted with pale green, containing lenses of fissile red sandstone and of stratified dark red fine conglomerate.""","""shale""","green,red",,,,sandstone,"""cross stratification"",red",poorly lithified,,,fluvial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""remains were assembled by moving water, after transport for a long or short distance... It is usual for the skull specimens... to have the mandibles in place... This suggests that the predators and scavengers... may have customarily discarded the heads... cranial remains have been selectively preserved...""\ncounts are given of 281 skulls and skull parts; 346 vertebrae, strings of vertebrae, and pieces of vertebrae; 109 limb bones and pieces of limb bones; and 29 partial girdles",general faunal/floral,"surface (float),field collection,survey of museum collection",FMNH,,,,,,"""Bone and bone-containing nodules may be collected from the surface... An effort to excavate for fossils was not productive... about forty pounds of red shale... was washed [and] five scraps of bone were recovered, none identifiable.""\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",not the same as the two West Grandfield sites of Olson 1967,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Cardiocephalus,,NA,NA,vertebrate,E. Daly. 1973. A Lower Permian vertebrate fauna from southern Oklahoma. Journal of Paleontology 47(3):562-589,4,4,334,J. Alroy,J. Alroy,T. Liebrecht,18/12/2006 14:47,25/08/2009 11:18,19411,sternbergi,Cardiocephalus,19411,cf.,279.3,272.3,Kungurian,,3,US,Cardiocephalus sternbergi
631443,occ,NA,,67945,,n. gen. Hapsidopareion n. sp. lepton,species,90683,,Hapsidopareion lepton,NA,species,90683,Daly,1973,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Hapsidopareiontidae,37285,37286,NA,NA,NA,specimens,-98.787781,34.18972,South Grandfield,NA,,US,Oklahoma,Tillman,stated in text,seconds,small collection,"""SW1/4 SE1/4 SE1/4 sec. 20, T. 4 S, R. 15 W. This is 6 1/2 miles southwest of Grandfield... 3 miles north of the Red River...""\neast side of ""a depression about fifty feet deep... near the top... [fossils] from the surface of a nose or ridge... three to four feet high and ten to twenty-five fee in area.""",gp_mid,-28.41,1.95,101,US,,Hennessey,,,bed,,,,,,,NA,"""lower third"" of a 9 foot bed\n""when the known lower boundary of the Arroyo [Formation] is extrapolated northward... it passes through the South Grandfield site.""\nthe Arroyo is within the Clear Fork Group, all of which is Kungurian (see discussion of Romer 1928 collections)","""Red shale spotted with pale green, containing lenses of fissile red sandstone and of stratified dark red fine conglomerate.""","""shale""","green,red",,,,sandstone,"""cross stratification"",red",poorly lithified,,,fluvial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""remains were assembled by moving water, after transport for a long or short distance... It is usual for the skull specimens... to have the mandibles in place... This suggests that the predators and scavengers... may have customarily discarded the heads... cranial remains have been selectively preserved...""\ncounts are given of 281 skulls and skull parts; 346 vertebrae, strings of vertebrae, and pieces of vertebrae; 109 limb bones and pieces of limb bones; and 29 partial girdles",general faunal/floral,"surface (float),field collection,survey of museum collection",FMNH,,,,,,"""Bone and bone-containing nodules may be collected from the surface... An effort to excavate for fossils was not productive... about forty pounds of red shale... was washed [and] five scraps of bone were recovered, none identifiable.""\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",not the same as the two West Grandfield sites of Olson 1967,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Hapsidopareion,n. gen.,NA,NA,vertebrate,E. Daly. 1973. A Lower Permian vertebrate fauna from southern Oklahoma. Journal of Paleontology 47(3):562-589,4,4,334,J. Alroy,J. Alroy,T. Liebrecht,18/12/2006 14:47,25/08/2009 11:18,19411,lepton,Hapsidopareion,19411,n. sp.,279.3,272.3,Kungurian,,9,US,Hapsidopareion lepton
631444,occ,NA,,67945,,n. gen. Micraroter n. sp. erythrogeios,species,90684,,Micraroter erythrogeios,NA,species,90684,Daly,1973,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Ostodolepidae,37301,37302,NA,NA,NA,specimens,-98.787781,34.18972,South Grandfield,NA,,US,Oklahoma,Tillman,stated in text,seconds,small collection,"""SW1/4 SE1/4 SE1/4 sec. 20, T. 4 S, R. 15 W. This is 6 1/2 miles southwest of Grandfield... 3 miles north of the Red River...""\neast side of ""a depression about fifty feet deep... near the top... [fossils] from the surface of a nose or ridge... three to four feet high and ten to twenty-five fee in area.""",gp_mid,-28.41,1.95,101,US,,Hennessey,,,bed,,,,,,,NA,"""lower third"" of a 9 foot bed\n""when the known lower boundary of the Arroyo [Formation] is extrapolated northward... it passes through the South Grandfield site.""\nthe Arroyo is within the Clear Fork Group, all of which is Kungurian (see discussion of Romer 1928 collections)","""Red shale spotted with pale green, containing lenses of fissile red sandstone and of stratified dark red fine conglomerate.""","""shale""","green,red",,,,sandstone,"""cross stratification"",red",poorly lithified,,,fluvial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""remains were assembled by moving water, after transport for a long or short distance... It is usual for the skull specimens... to have the mandibles in place... This suggests that the predators and scavengers... may have customarily discarded the heads... cranial remains have been selectively preserved...""\ncounts are given of 281 skulls and skull parts; 346 vertebrae, strings of vertebrae, and pieces of vertebrae; 109 limb bones and pieces of limb bones; and 29 partial girdles",general faunal/floral,"surface (float),field collection,survey of museum collection",FMNH,,,,,,"""Bone and bone-containing nodules may be collected from the surface... An effort to excavate for fossils was not productive... about forty pounds of red shale... was washed [and] five scraps of bone were recovered, none identifiable.""\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",not the same as the two West Grandfield sites of Olson 1967,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Micraroter,n. gen.,NA,NA,vertebrate,E. Daly. 1973. A Lower Permian vertebrate fauna from southern Oklahoma. Journal of Paleontology 47(3):562-589,4,4,334,J. Alroy,J. Alroy,T. Liebrecht,18/12/2006 14:47,25/08/2009 11:18,19411,erythrogeios,Micraroter,19411,n. sp.,279.3,272.3,Kungurian,,4,US,Micraroter erythrogeios
631445,occ,NA,,67945,,Captorhinus aguti,species,90718,,Captorhinus aguti,NA,species,134887,Daly,1973,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,specimens,-98.787781,34.18972,South Grandfield,NA,,US,Oklahoma,Tillman,stated in text,seconds,small collection,"""SW1/4 SE1/4 SE1/4 sec. 20, T. 4 S, R. 15 W. This is 6 1/2 miles southwest of Grandfield... 3 miles north of the Red River...""\neast side of ""a depression about fifty feet deep... near the top... [fossils] from the surface of a nose or ridge... three to four feet high and ten to twenty-five fee in area.""",gp_mid,-28.41,1.95,101,US,,Hennessey,,,bed,,,,,,,NA,"""lower third"" of a 9 foot bed\n""when the known lower boundary of the Arroyo [Formation] is extrapolated northward... it passes through the South Grandfield site.""\nthe Arroyo is within the Clear Fork Group, all of which is Kungurian (see discussion of Romer 1928 collections)","""Red shale spotted with pale green, containing lenses of fissile red sandstone and of stratified dark red fine conglomerate.""","""shale""","green,red",,,,sandstone,"""cross stratification"",red",poorly lithified,,,fluvial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""remains were assembled by moving water, after transport for a long or short distance... It is usual for the skull specimens... to have the mandibles in place... This suggests that the predators and scavengers... may have customarily discarded the heads... cranial remains have been selectively preserved...""\ncounts are given of 281 skulls and skull parts; 346 vertebrae, strings of vertebrae, and pieces of vertebrae; 109 limb bones and pieces of limb bones; and 29 partial girdles",general faunal/floral,"surface (float),field collection,survey of museum collection",FMNH,,,,,,"""Bone and bone-containing nodules may be collected from the surface... An effort to excavate for fossils was not productive... about forty pounds of red shale... was washed [and] five scraps of bone were recovered, none identifiable.""\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",not the same as the two West Grandfield sites of Olson 1967,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,E. Daly. 1973. A Lower Permian vertebrate fauna from southern Oklahoma. Journal of Paleontology 47(3):562-589,4,4,334,J. Alroy,J. Alroy,T. Liebrecht,18/12/2006 14:47,25/08/2009 11:18,19411,aguti,Captorhinus,19411,,279.3,272.3,Kungurian,,20,US,Captorhinus aguti
631446,occ,NA,,67945,,Labidosaurus sp.,genus,37501,,Labidosaurus,NA,genus,37501,Daly,1973,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,fragments,-98.787781,34.18972,South Grandfield,NA,,US,Oklahoma,Tillman,stated in text,seconds,small collection,"""SW1/4 SE1/4 SE1/4 sec. 20, T. 4 S, R. 15 W. This is 6 1/2 miles southwest of Grandfield... 3 miles north of the Red River...""\neast side of ""a depression about fifty feet deep... near the top... [fossils] from the surface of a nose or ridge... three to four feet high and ten to twenty-five fee in area.""",gp_mid,-28.41,1.95,101,US,,Hennessey,,,bed,,,,,,,NA,"""lower third"" of a 9 foot bed\n""when the known lower boundary of the Arroyo [Formation] is extrapolated northward... it passes through the South Grandfield site.""\nthe Arroyo is within the Clear Fork Group, all of which is Kungurian (see discussion of Romer 1928 collections)","""Red shale spotted with pale green, containing lenses of fissile red sandstone and of stratified dark red fine conglomerate.""","""shale""","green,red",,,,sandstone,"""cross stratification"",red",poorly lithified,,,fluvial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""remains were assembled by moving water, after transport for a long or short distance... It is usual for the skull specimens... to have the mandibles in place... This suggests that the predators and scavengers... may have customarily discarded the heads... cranial remains have been selectively preserved...""\ncounts are given of 281 skulls and skull parts; 346 vertebrae, strings of vertebrae, and pieces of vertebrae; 109 limb bones and pieces of limb bones; and 29 partial girdles",general faunal/floral,"surface (float),field collection,survey of museum collection",FMNH,,,,,,"""Bone and bone-containing nodules may be collected from the surface... An effort to excavate for fossils was not productive... about forty pounds of red shale... was washed [and] five scraps of bone were recovered, none identifiable.""\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",not the same as the two West Grandfield sites of Olson 1967,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,vertebrate,E. Daly. 1973. A Lower Permian vertebrate fauna from southern Oklahoma. Journal of Paleontology 47(3):562-589,4,4,334,J. Alroy,J. Alroy,T. Liebrecht,18/12/2006 14:47,25/08/2009 11:18,19411,sp.,Labidosaurus,19411,,279.3,272.3,Kungurian,,1,US,Labidosaurus sp.
631447,occ,NA,,67945,,n. gen. Acleistorhinus n. sp. pteroticus,species,90735,,Acleistorhinus pteroticus,NA,species,90735,Daly,1973,Chordata,33815,Reptilia,36322,,NA,Acleistorhinidae,37514,37515,NA,NA,NA,individuals,-98.787781,34.18972,South Grandfield,NA,,US,Oklahoma,Tillman,stated in text,seconds,small collection,"""SW1/4 SE1/4 SE1/4 sec. 20, T. 4 S, R. 15 W. This is 6 1/2 miles southwest of Grandfield... 3 miles north of the Red River...""\neast side of ""a depression about fifty feet deep... near the top... [fossils] from the surface of a nose or ridge... three to four feet high and ten to twenty-five fee in area.""",gp_mid,-28.41,1.95,101,US,,Hennessey,,,bed,,,,,,,NA,"""lower third"" of a 9 foot bed\n""when the known lower boundary of the Arroyo [Formation] is extrapolated northward... it passes through the South Grandfield site.""\nthe Arroyo is within the Clear Fork Group, all of which is Kungurian (see discussion of Romer 1928 collections)","""Red shale spotted with pale green, containing lenses of fissile red sandstone and of stratified dark red fine conglomerate.""","""shale""","green,red",,,,sandstone,"""cross stratification"",red",poorly lithified,,,fluvial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""remains were assembled by moving water, after transport for a long or short distance... It is usual for the skull specimens... to have the mandibles in place... This suggests that the predators and scavengers... may have customarily discarded the heads... cranial remains have been selectively preserved...""\ncounts are given of 281 skulls and skull parts; 346 vertebrae, strings of vertebrae, and pieces of vertebrae; 109 limb bones and pieces of limb bones; and 29 partial girdles",general faunal/floral,"surface (float),field collection,survey of museum collection",FMNH,,,,,,"""Bone and bone-containing nodules may be collected from the surface... An effort to excavate for fossils was not productive... about forty pounds of red shale... was washed [and] five scraps of bone were recovered, none identifiable.""\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",not the same as the two West Grandfield sites of Olson 1967,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Acleistorhinus,n. gen.,NA,NA,vertebrate,E. Daly. 1973. A Lower Permian vertebrate fauna from southern Oklahoma. Journal of Paleontology 47(3):562-589,4,4,334,J. Alroy,J. Alroy,T. Liebrecht,18/12/2006 14:47,26/07/2009 16:45,19411,pteroticus,Acleistorhinus,19411,n. sp.,279.3,272.3,Kungurian,,1,US,Acleistorhinus pteroticus
631448,occ,NA,,67945,,Dimetrodon loomisi,species,90738,,Dimetrodon loomisi,NA,species,90738,Daly,1973,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-98.787781,34.18972,South Grandfield,NA,,US,Oklahoma,Tillman,stated in text,seconds,small collection,"""SW1/4 SE1/4 SE1/4 sec. 20, T. 4 S, R. 15 W. This is 6 1/2 miles southwest of Grandfield... 3 miles north of the Red River...""\neast side of ""a depression about fifty feet deep... near the top... [fossils] from the surface of a nose or ridge... three to four feet high and ten to twenty-five fee in area.""",gp_mid,-28.41,1.95,101,US,,Hennessey,,,bed,,,,,,,NA,"""lower third"" of a 9 foot bed\n""when the known lower boundary of the Arroyo [Formation] is extrapolated northward... it passes through the South Grandfield site.""\nthe Arroyo is within the Clear Fork Group, all of which is Kungurian (see discussion of Romer 1928 collections)","""Red shale spotted with pale green, containing lenses of fissile red sandstone and of stratified dark red fine conglomerate.""","""shale""","green,red",,,,sandstone,"""cross stratification"",red",poorly lithified,,,fluvial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""remains were assembled by moving water, after transport for a long or short distance... It is usual for the skull specimens... to have the mandibles in place... This suggests that the predators and scavengers... may have customarily discarded the heads... cranial remains have been selectively preserved...""\ncounts are given of 281 skulls and skull parts; 346 vertebrae, strings of vertebrae, and pieces of vertebrae; 109 limb bones and pieces of limb bones; and 29 partial girdles",general faunal/floral,"surface (float),field collection,survey of museum collection",FMNH,,,,,,"""Bone and bone-containing nodules may be collected from the surface... An effort to excavate for fossils was not productive... about forty pounds of red shale... was washed [and] five scraps of bone were recovered, none identifiable.""\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",not the same as the two West Grandfield sites of Olson 1967,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,E. Daly. 1973. A Lower Permian vertebrate fauna from southern Oklahoma. Journal of Paleontology 47(3):562-589,4,4,334,J. Alroy,J. Alroy,T. Liebrecht,18/12/2006 14:47,25/08/2009 11:18,19411,loomisi,Dimetrodon,19411,,279.3,272.3,Kungurian,,3,US,Dimetrodon loomisi
631449,occ,NA,,67945,,Edaphosaurus sp.,genus,38911,,Edaphosaurus,NA,genus,38911,Daly,1973,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,fragments,-98.787781,34.18972,South Grandfield,NA,,US,Oklahoma,Tillman,stated in text,seconds,small collection,"""SW1/4 SE1/4 SE1/4 sec. 20, T. 4 S, R. 15 W. This is 6 1/2 miles southwest of Grandfield... 3 miles north of the Red River...""\neast side of ""a depression about fifty feet deep... near the top... [fossils] from the surface of a nose or ridge... three to four feet high and ten to twenty-five fee in area.""",gp_mid,-28.41,1.95,101,US,,Hennessey,,,bed,,,,,,,NA,"""lower third"" of a 9 foot bed\n""when the known lower boundary of the Arroyo [Formation] is extrapolated northward... it passes through the South Grandfield site.""\nthe Arroyo is within the Clear Fork Group, all of which is Kungurian (see discussion of Romer 1928 collections)","""Red shale spotted with pale green, containing lenses of fissile red sandstone and of stratified dark red fine conglomerate.""","""shale""","green,red",,,,sandstone,"""cross stratification"",red",poorly lithified,,,fluvial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""remains were assembled by moving water, after transport for a long or short distance... It is usual for the skull specimens... to have the mandibles in place... This suggests that the predators and scavengers... may have customarily discarded the heads... cranial remains have been selectively preserved...""\ncounts are given of 281 skulls and skull parts; 346 vertebrae, strings of vertebrae, and pieces of vertebrae; 109 limb bones and pieces of limb bones; and 29 partial girdles",general faunal/floral,"surface (float),field collection,survey of museum collection",FMNH,,,,,,"""Bone and bone-containing nodules may be collected from the surface... An effort to excavate for fossils was not productive... about forty pounds of red shale... was washed [and] five scraps of bone were recovered, none identifiable.""\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",not the same as the two West Grandfield sites of Olson 1967,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,E. Daly. 1973. A Lower Permian vertebrate fauna from southern Oklahoma. Journal of Paleontology 47(3):562-589,4,4,334,J. Alroy,J. Alroy,T. Liebrecht,18/12/2006 14:47,25/08/2009 11:18,19411,sp.,Edaphosaurus,19411,,279.3,272.3,Kungurian,,1,US,Edaphosaurus sp.
633270,occ,NA,,68171,,Varanops brevirostris,species,91795,,Varanops brevirostris,NA,species,122316,Reisz and Tsuji,2006,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,38897,NA,NA,NA,individuals,-99.730003,32.450001,Southwest of Abilene,NA,,US,Texas,Taylor,based on nearby landmark,2,outcrop,"""southwest of Abilene, in Taylor County""\ntwo skeletons were ""found near"" each other",gp_mid,-29.97,0.86,101,US,,Arroyo,,,,,,,,,,NA,see discussion of collections such as 28256,none given,not reported,,,,,,,,,,terrestrial indet.,,none given,macrofossils,,,,,tooth marks,NA,,body,,,,,,,,,,NA,,"the Varanops and Diadectes specimens are both partially articulated and are mostly complete\nVaranops skeleton ""exposed for some time permitting weathering"" based on extensive cracking",taphonomic,"selective quarrying,field collection",TMM,,,,,,"""specimens [discovered] with a backhoe""",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Varanops,,NA,NA,vertebrate,R. R. Reisz and L. A. Tsuji. 2006. An articulated skeleton of Varanops with bite marks: the oldest known evidence of scavenging among terrestrial vertebrates. Journal of Vertebrate Paleontology 26(4):1021-1023,4,4,334,J. Alroy,J. Alroy,T. Liebrecht,05/01/2007 18:04,10/04/2009 15:20,19599,brevirostris,Varanops,19599,,279.3,272.3,Kungurian,,1,US,Varanops brevirostris
633271,occ,NA,,68171,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Reisz and Tsuji,2006,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,individuals,-99.730003,32.450001,Southwest of Abilene,NA,,US,Texas,Taylor,based on nearby landmark,2,outcrop,"""southwest of Abilene, in Taylor County""\ntwo skeletons were ""found near"" each other",gp_mid,-29.97,0.86,101,US,,Arroyo,,,,,,,,,,NA,see discussion of collections such as 28256,none given,not reported,,,,,,,,,,terrestrial indet.,,none given,macrofossils,,,,,tooth marks,NA,,body,,,,,,,,,,NA,,"the Varanops and Diadectes specimens are both partially articulated and are mostly complete\nVaranops skeleton ""exposed for some time permitting weathering"" based on extensive cracking",taphonomic,"selective quarrying,field collection",TMM,,,,,,"""specimens [discovered] with a backhoe""",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,R. R. Reisz and L. A. Tsuji. 2006. An articulated skeleton of Varanops with bite marks: the oldest known evidence of scavenging among terrestrial vertebrates. Journal of Vertebrate Paleontology 26(4):1021-1023,4,4,334,J. Alroy,J. Alroy,T. Liebrecht,05/01/2007 18:04,10/04/2009 15:20,19599,sp.,Diadectes,19599,,279.3,272.3,Kungurian,,1,US,Diadectes sp.
635045,occ,NA,,68318,,n. gen. Whatcheeria n. sp. deltae,species,92128,,Whatcheeria deltae,NA,species,92128,Lombard and Bolt,1995,Chordata,33815,Osteichthyes,34881,,NA,Whatcheeriidae,179034,92127,NA,NA,NA,,-92.333336,41.316666,Delta,NA,,US,Iowa,Keokuk,based on nearby landmark,minutes,outcrop,"""SW1/4, SW1/4, section 15, T75N, R13W"" near Delta, Iowa (coordinate based on Delta)\n""two adjacent palaeodepressions or collapse structures, exposed in the walls of an inactive limestone quarry""",gp_mid,-47.48,-23.84,101,US,,St. Louis,,Waugh,member,,,,,,,NA,"St. Louis Formation in Iowa may correlate not with the St. Louis Formation in its type section, but with the Genevieve Formation in Missouri and Illinois","unclear: collapse structures are within a limestone quarry, but the Waugh Member elsewhere includes ""sandstones, shales, and lime mudstones""",,,,,,,,,,,sinkhole,,"general environment is ""primarily lacustrine, fresh-water to brackish, with possible intermittent incursion of marine waters"" but fossils are from ""fills within two adjacent collapse structures""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,FMNH,,,,,,"""Over 600 tetrapod specimens were recovered... along with several hundred fish and some invertebrate and plant fossils""",definitely not the same as the paleobotanical What Cheer locality (collection 13999),"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Whatcheeria,n. gen.,NA,NA,vertebrate,"R. E. Lombard and J. R. Bolt. 1995. A new primitive tetrapod, Whatcheeria deltae, from the Lower Carboniferous of Iowa. Palaeontology 38(3):471-494",4,4,0,J. Alroy,J. Alroy,,15/01/2007 21:56,15/01/2007 23:56,19656,deltae,Whatcheeria,19656,n. sp.,339.4,336,Asbian,,NA,US,Whatcheeria deltae
635046,occ,NA,,68318,,Embolomeri indet.,suborder,37178,,Embolomeri,NA,suborder,37178,Lombard and Bolt,1995,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,,-92.333336,41.316666,Delta,NA,,US,Iowa,Keokuk,based on nearby landmark,minutes,outcrop,"""SW1/4, SW1/4, section 15, T75N, R13W"" near Delta, Iowa (coordinate based on Delta)\n""two adjacent palaeodepressions or collapse structures, exposed in the walls of an inactive limestone quarry""",gp_mid,-47.48,-23.84,101,US,,St. Louis,,Waugh,member,,,,,,,NA,"St. Louis Formation in Iowa may correlate not with the St. Louis Formation in its type section, but with the Genevieve Formation in Missouri and Illinois","unclear: collapse structures are within a limestone quarry, but the Waugh Member elsewhere includes ""sandstones, shales, and lime mudstones""",,,,,,,,,,,sinkhole,,"general environment is ""primarily lacustrine, fresh-water to brackish, with possible intermittent incursion of marine waters"" but fossils are from ""fills within two adjacent collapse structures""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,FMNH,,,,,,"""Over 600 tetrapod specimens were recovered... along with several hundred fish and some invertebrate and plant fossils""",definitely not the same as the paleobotanical What Cheer locality (collection 13999),"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Embolomeri,,NA,NA,vertebrate,"R. E. Lombard and J. R. Bolt. 1995. A new primitive tetrapod, Whatcheeria deltae, from the Lower Carboniferous of Iowa. Palaeontology 38(3):471-494",4,4,0,J. Alroy,J. Alroy,,15/01/2007 21:56,15/01/2007 23:56,19656,indet.,,19656,,339.4,336,Asbian,,NA,US, indet.
635047,occ,NA,,68318,,Colosteidae indet.,family,36975,,Colosteidae,NA,family,36975,Lombard and Bolt,1995,Chordata,33815,Osteichthyes,34881,,NA,Colosteidae,36975,NA,NA,NA,NA,,-92.333336,41.316666,Delta,NA,,US,Iowa,Keokuk,based on nearby landmark,minutes,outcrop,"""SW1/4, SW1/4, section 15, T75N, R13W"" near Delta, Iowa (coordinate based on Delta)\n""two adjacent palaeodepressions or collapse structures, exposed in the walls of an inactive limestone quarry""",gp_mid,-47.48,-23.84,101,US,,St. Louis,,Waugh,member,,,,,,,NA,"St. Louis Formation in Iowa may correlate not with the St. Louis Formation in its type section, but with the Genevieve Formation in Missouri and Illinois","unclear: collapse structures are within a limestone quarry, but the Waugh Member elsewhere includes ""sandstones, shales, and lime mudstones""",,,,,,,,,,,sinkhole,,"general environment is ""primarily lacustrine, fresh-water to brackish, with possible intermittent incursion of marine waters"" but fossils are from ""fills within two adjacent collapse structures""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,FMNH,,,,,,"""Over 600 tetrapod specimens were recovered... along with several hundred fish and some invertebrate and plant fossils""",definitely not the same as the paleobotanical What Cheer locality (collection 13999),"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Colosteidae,,NA,NA,vertebrate,"R. E. Lombard and J. R. Bolt. 1995. A new primitive tetrapod, Whatcheeria deltae, from the Lower Carboniferous of Iowa. Palaeontology 38(3):471-494",4,4,4,J. Alroy,J. Alroy,J. Alroy,15/01/2007 21:56,15/01/2007 23:58,19656,indet.,,19656,,339.4,336,Asbian,,NA,US, indet.
635056,occ,NA,R,68319,,Colosteidae indet.,family,36975,,Colosteidae,NA,family,36975,Lombard and Bolt,1999,Chordata,33815,Osteichthyes,34881,,NA,Colosteidae,36975,NA,NA,NA,NA,,-88.966667,37.549999,Goreville,NA,KU-IL-10,US,Illinois,Johnston,based on nearby landmark,minutes,outcrop,"""an inactive limestone quarry on private property in T12S R2E, some six km south of Goreville"" (coordinate based on Goreville)",gp_mid,-35.6,-18.77,101,US,FED,Kinkaid,,Cave Hill,member,,,,,,,NA,,"""a sequence of gray and red sandy mudstones... vertebrates... occur in calcareous nodules within the mudstone""",mudstone,"gray,red",,"sandy,calcareous",,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""matrix around the bone is a yellow-brown mudstone with calcareous inclusions""",taxonomic,"surface (in situ),mechanical,field collection",,,,,,,"collection of ""specimens accessible at the surface of the exposure""",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Colosteidae,,NA,NA,vertebrate,E. R. Lombard and J. R. Bolt. 1999. Microsaur from the Mississippian of Illinois and a standard format for morphological characters. Journal of Paleontology 73(5):908-923,4,4,697,J. Alroy,J. Alroy,E. Dunne,15/01/2007 22:13,23/08/2016 11:09,19657,indet.,,19657,,326.4,318.1,Arnsbergian,,NA,US, indet.
635056,occ,18868,,68319,,Greererpeton burkmorani,species,36977,species not entered,Greererpeton,NA,genus,36977,Bolt and Lombard,2001,Chordata,33815,Osteichthyes,34881,,NA,Colosteidae,36975,36977,NA,NA,NA,,-88.966667,37.549999,Goreville,NA,KU-IL-10,US,Illinois,Johnston,based on nearby landmark,minutes,outcrop,"""an inactive limestone quarry on private property in T12S R2E, some six km south of Goreville"" (coordinate based on Goreville)",gp_mid,-35.6,-18.77,101,US,FED,Kinkaid,,Cave Hill,member,,,,,,,NA,,"""a sequence of gray and red sandy mudstones... vertebrates... occur in calcareous nodules within the mudstone""",mudstone,"gray,red",,"sandy,calcareous",,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""matrix around the bone is a yellow-brown mudstone with calcareous inclusions""",taxonomic,"surface (in situ),mechanical,field collection",,,,,,,"collection of ""specimens accessible at the surface of the exposure""",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Greererpeton,,NA,NA,vertebrate,"J. R. Bolt and R. E. Lombard. 2001. The mandible of the primitive tetrapod Greererpeton, and the early evolution of the tetrapod lower jaw. Journal of Paleontology 75(5):1016-1042",4,4,0,J. Alroy,J. Alroy,,15/01/2007 22:14,16/01/2007 00:14,19657,burkmorani,Greererpeton,19655,,326.4,318.1,Arnsbergian,,NA,US,Greererpeton burkmorani
635057,occ,NA,,68319,,Microsauria indet.,unranked clade,37278,,Microsauria,NA,unranked clade,37278,Lombard and Bolt,1999,Chordata,33815,Osteichthyes,34881,Microsauria,37278,,NA,NA,NA,NA,NA,,-88.966667,37.549999,Goreville,NA,KU-IL-10,US,Illinois,Johnston,based on nearby landmark,minutes,outcrop,"""an inactive limestone quarry on private property in T12S R2E, some six km south of Goreville"" (coordinate based on Goreville)",gp_mid,-35.6,-18.77,101,US,FED,Kinkaid,,Cave Hill,member,,,,,,,NA,,"""a sequence of gray and red sandy mudstones... vertebrates... occur in calcareous nodules within the mudstone""",mudstone,"gray,red",,"sandy,calcareous",,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""matrix around the bone is a yellow-brown mudstone with calcareous inclusions""",taxonomic,"surface (in situ),mechanical,field collection",,,,,,,"collection of ""specimens accessible at the surface of the exposure""",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Microsauria,,NA,NA,vertebrate,E. R. Lombard and J. R. Bolt. 1999. Microsaur from the Mississippian of Illinois and a standard format for morphological characters. Journal of Paleontology 73(5):908-923,4,4,697,J. Alroy,J. Alroy,E. Dunne,15/01/2007 22:13,03/02/2016 06:19,19657,indet.,,19657,,326.4,318.1,Arnsbergian,,NA,US, indet.
636301,occ,NA,,68427,,n. gen. Concordia n. sp. cunninghami,species,92485,recombined as,Euconcordia cunninghami,NA,species,92485,M_ller and Reisz,2005,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,348714,NA,NA,NA,individuals,-96.113892,37.986111,Hamilton Quarry,NA,,US,Kansas,Greenwood,estimated from map,seconds,,"about 5 km E of Hamilton, Greenwood Co., Kansas, in secs. 5 and 6, T. 24 S., R. 12 E. (Virgil 7.5' quadrangle)",gp_mid,-26.91,-0.1,101,US,,Calhouns Shale,Shawnee,,,,,,,,,NA,"Virgillian Series, Upper Pennsylvanian; late Kasimovian according to Modesto et al. (2015)",,"""shale""",,,,,,,,,,estuary/bay,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Concordia,n. gen.,NA,NA,vertebrate,"J. M_ller and R. R. Reisz. 2005. An early captorhinid reptile (Amniota, Eureptilia) from the Upper Carboniferous of Hamilton, Kansas. Journal of Vertebrate Paleontology 25(3):561-568",18,18,334,M. Uhen,M. Uhen,T. Liebrecht,22/01/2007 06:27,23/12/2016 14:16,19706,cunninghami,Euconcordia,19706,n. sp.,303.4,298.9,Virgilian,,2,US,Euconcordia cunninghami
665544,occ,NA,,71671,,n. gen. Eumatthevia n. sp. bolli,species,99568,subjective synonym of,Mycterosaurus longiceps,NA,species,122319,Broom,1930,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,38895,NA,NA,NA,individuals,-99.091667,33.733334,"""Copper Shept""",NA,?Mitchell Creek,US,Texas,Baylor,based on nearby landmark,minutes,small collection,"""at Copper Shept, apparently in Texas"": the only place name in Texas associated with Permian deposits is Copper Breaks State Park (basis of coordinate) in Hardeman County.\nReisz (1986, Encyclopedia of Paleoherpetology 17A) states that the type of Eumatthevia probably is from the same locality as the holotype of Mycterosaurus longiceps which is Mitchell Creek, NE from Maybelle, Baylor Co. Thus, polar coordinates (originally entered as >> 36 6' North, 99 45' West << ) are changed to the position coordinates of Mitchell Creek area. Given that the collection date is 1880, a point in time at which no collections were made in the post-""Arroyo"" beds of the Clear Fork Group, and that the specimen was detected in the Cope Collection of the AMNH it is quite plausible to assume that the type of Eumatthevia bolli does not come from Hardeman Co. but from a locality farther to the east. (TL)",gp_mid,-30.29,-0.93,101,US,,,,,bed,,,,,,,NA,Chronostratigraphy originally entered as >> Permian << .\nNew stratigraphic data are uncertain and based on the assumption that the fossil comes from the Mitchell Creek area (see comments on geography) from a locality which is either in the upper Wichita or the lower Clear Fork Group. (TL),none given,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,specimen consists of a slab and counter-slab,taxonomic,survey of museum collection,AMNH,,,,J. Boll,1880,"""collected in 1880 by Cope's collector Jacob Boll""",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Eumatthevia,n. gen.,NA,NA,vertebrate,R. Broom. 1930. On a new primitive theromorph (Eumatthevia bolli). American Museum Novitates 446:1-4,4,4,334,J. Alroy,J. Alroy,T. Liebrecht,05/05/2007 14:10,11/06/2009 05:27,4338,bolli,Mycterosaurus,4338,n. sp.,290.1,272.3,Artinskian,Kungurian,1,US,Mycterosaurus bolli
699400,occ,NA,I,75090,,n. gen. Puertollanopus n. sp. omicrodactylus,species,108506,,Puertollanopus omicrodactylus,NA,species,108506,Soler-Gij_n and Moratalla,2001,Chordata,33815,Osteichthyes,34881,Microsauria,37278,,NA,108505,NA,NA,NA,,-4.116667,38.683334,Emma Quarry Amphibian Bed,NA,Puertollano,ES,Castilla-La Manacha,,based on nearby landmark,minutes,outcrop,"from an area of ""approximately 5 hectares"" within Emma Quarry, about 6 k WSW of Puertollano (basis of coordinate)",gp_mid,10.97,-6.38,304,ES,,,,,bed,,,,,,,NA,single bedding plane,"""siltstone""",siltstone,,,,,,,,,,estuary/bay,,"""intertidal""",macrofossils,,,,,,NA,,trace,,,snapshot,,,,,,,NA,,,paleoecologic,field collection,,,,,,1994,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Puertollanopus,n. gen.,NA,NA,vertebrate,"R. Soler-Gij_n and J. J. Moratalla. 2001. Fish and tetrapod trace fossils from the Upper Carboniferous of Puertollano, Spain. Palaeogeography, Palaeoclimatology, Palaeoecology 171(1-2):1-28",4,4,697,J. Alroy,J. Alroy,E. Dunne,21/09/2007 15:07,07/07/2016 08:17,25351,omicrodactylus,Puertollanopus,25351,n. sp.,303.4,301.2,Stephanian C,,NA,ES,Puertollanopus omicrodactylus
719384,occ,NA,,22726,,Embolomeri ? indet.,suborder,37178,,Embolomeri,NA,suborder,37178,Andrews et al.,1977,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,,-3.35,56.1166,Cowdenbeath Amphibian Bonebed,NA,ETE Locality 1605; Dora Opencast Coal Site,UK,,,,4,outcrop,"""south-east of Cowdenbeath... a section 30 m long""",gp_mid,0.18,-9.49,313,UK,,,Limestone Coal,,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min\r\n""lower Namurian A... 62 m beneath the base of the Index Limestone [which is]... at the junction between the top of the Pendleian (E1) and the base of the Arnsbergian (E2) stages"": originally entered as Namurian to Bashkirian","ETE rock type adj: ""rooty,muddy"", ETE lithology comments: 0\r\n""a localised patch in a seatrock (rooty, muddy siltstone)""",siltstone,,,,,,,,,,terrestrial indet.,,,,,,,,,NA,,,,,,,,,,,,NA,,,general faunal/floral,,,,7 specimens,,,1974 and 1975,"ETE Size: .; ETE reference list: 478, 479, 483, 482, 485, 454, 81, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Embolomeri,?,NA,NA,,"S. M. Andrews, M.A.E. Browne, and AL Panchen, and SP Wood. 1977. Discovery of amphibians in the Namurian (Upper Carboniferous of Fife). Nature 265:529-532",4,4,697,J. Alroy,J. Alroy,E. Dunne,30/12/2007 17:36,01/12/2015 08:45,5931,indet.,,5931,,326.4,318.1,Pendleian,,NA,UK, indet.
719385,occ,NA,,22726,,cf. Colosteidae indet.,family,36975,,Colosteidae,NA,family,36975,Andrews et al.,1977,Chordata,33815,Osteichthyes,34881,,NA,Colosteidae,36975,NA,NA,NA,NA,,-3.35,56.1166,Cowdenbeath Amphibian Bonebed,NA,ETE Locality 1605; Dora Opencast Coal Site,UK,,,,4,outcrop,"""south-east of Cowdenbeath... a section 30 m long""",gp_mid,0.18,-9.49,313,UK,,,Limestone Coal,,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min\r\n""lower Namurian A... 62 m beneath the base of the Index Limestone [which is]... at the junction between the top of the Pendleian (E1) and the base of the Arnsbergian (E2) stages"": originally entered as Namurian to Bashkirian","ETE rock type adj: ""rooty,muddy"", ETE lithology comments: 0\r\n""a localised patch in a seatrock (rooty, muddy siltstone)""",siltstone,,,,,,,,,,terrestrial indet.,,,,,,,,,NA,,,,,,,,,,,,NA,,,general faunal/floral,,,,7 specimens,,,1974 and 1975,"ETE Size: .; ETE reference list: 478, 479, 483, 482, 485, 454, 81, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Colosteidae,cf.,NA,NA,,"S. M. Andrews, M.A.E. Browne, and AL Panchen, and SP Wood. 1977. Discovery of amphibians in the Namurian (Upper Carboniferous of Fife). Nature 265:529-532",4,4,697,J. Alroy,J. Alroy,E. Dunne,30/12/2007 17:36,01/12/2015 08:45,5931,indet.,,5931,,326.4,318.1,Pendleian,,NA,UK, indet.
721482,occ,NA,,77412,,Limnosceloides n. sp. brachycoles,species,142127,nomen dubium,Tetrapoda,NA,unranked clade,53190,Langston,1966,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,elements,-106.639442,36.157223,UCMP V-2814,NA,Camp Quarry,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"""southeast slope of a small butte, 410 yards south of New Mexico State Highway 96, about 940 yards southeast of the Rio Puerco bridge at Arroyo del Agua, section 8, T.22N., R.3E., Rio Arriba County, New Mexico"" (Langston, 1965 p. 6; 1966 p.691)",gp_mid,-34.09,4.48,101,US,FED,Abo/Cutler,,,group of beds,,,,,,,NA,All specimens appear to come from about the same stratigraphic level (38-36 m below top of the butte). Whether these beds are uppermost Carboniferous or lower Permian is a subject of controversy.\r\n,"""soft brick-red clayey siltstone"" (Langston, 1965 p. 6; 1966 p.691; Langston & Reisz, 1981 p. 74)",siltstone,red,,argillaceous,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,general faunal/floral,"bulk,surface (float),survey of museum collection",UCMP,all macrofossils,,,"C. L. Camp, among others","1928, 1934, 1935","""Berman & Reisz reopened this quarry in 1979, but despite extensive digging by a team of five people, only a few scattered bone fragments were recovered. It appears that the site has been completeley exhausted"" (Langston & Reisz, 1981 p. 74).\r\nType of Rhiodenticulatus heatoni was ""probably not found in the main bone level of the quarry, but rather as float on the slope of Loma Salazar a few feet away and presumably at or just above the quarry bone level."" (Berman & Reisz, 1986).","""Captorhinomorphs and Diadectomorphs"" (Langston 1966 p.690)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Limnosceloides,,NA,NA,vertebrate,"W. Langston, Jr. 1966. Limnosceloides brachycoles (reptilia: Captorhinomorpha), a new species From the Lower Permian of New Mexico. Journal of Paleontology 40(3):690-695",310,310,334,R. Reisz,R. Reisz,T. Liebrecht,11/01/2008 09:59,20/06/2009 07:50,26206,brachycoles,,26206,n. sp.,303.4,268,Virgilian,Wolfcamp,12,US, brachycoles
731086,occ,NA,,78559,,Kahneria seltina,species,119509,,Kahneria seltina,NA,species,119509,Olson,1962,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37506,NA,NA,NA,individuals,-99.907776,33.718056,Locality KS (Upper San Angelo Fm.),NA,Alexander Ranch,US,Texas,Knox,estimated from map,seconds,small collection,"Maverick Flats 7.5' qdr; ""on the east and west flanks of a divide between two tributaries that flow south into the South Fork of the Wichita River""; For details see maps on pp. 98, 119 in Olson (1962)",gp_mid,-28.76,3.34,101,US,,San Angelo,Pease River,Flowerpot Shale,group of beds,,,,,,,NA,,not much reported,"""shale""",red,,,Y,"""shale""","green,red",,sandy,,fluvial-deltaic indet.,foreland basin,"""This locality includes Flower Pot, terrestrial in the eastern part but grading into marginal facies in the west. No strictly offshore facies are present, although these occur to the west of the limit of the locality.""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Kahneria,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,08/02/2008 02:46,02/12/2008 05:44,26846,seltina,Kahneria,26846,,279.3,268.8,Kungurian,Roadian,1,US,Kahneria seltina
737131,occ,NA,,79162,,n. gen. Romeria n. sp. texana,species,134834,,Romeria texana,NA,species,134834,Price,1937,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37504,NA,NA,NA,individuals,-98.650002,33.583332,Archer City Bonebed 1 (Putnam Fm.),NA,"Locality IIIf (Romer & Price, 1940)",US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Romeria,n. gen.,NA,NA,vertebrate,L.I. Price. 1937. Two new cotylosaurs from the Permian of Texas. Proceedings of the New England Zo̦logical Club 16:97-102,315,316,14,J. Mueller,J. Dummasch,M. Carrano,27/02/2008 02:38,10/12/2012 14:44,43845,texana,Romeria,26570,n. sp.,296.4,268,Wolfcamp,,1,US,Romeria texana
739043,occ,NA,,79402,,Cricotillus brachydens,species,119132,,Cricotillus brachydens,NA,species,119132,Olson,1970,Chordata,33815,Osteichthyes,34881,,NA,Cricotidae,119131,119130,NA,NA,NA,individuals,-97.340553,36.161667,"Orlando site, Noble Co. (Wellington Fm.)",NA,,US,Oklahoma,Noble,stated in text,seconds,,"""about 2 miles northeast of Orlando in Noble County in SE1/4 sec. 31, T. 20 N., R. 1 W."" (Olson, 1967 p. 44); Note: the town of Orlando itself lies in Logan Co., the fossil site, however, lies just across the border in Noble Co. Lat long is based on the map given by Olson (1967 p. 38).",gp_mid,-27.83,0.34,101,US,,Wellington,Sumner,,,,,,,,,NA,"""about 100 feet below the contact of the Wellington and the Garber formations"" Olson (1970 p. 360). The Artinskian age of the Wellington Fm. given here is taken from Mazzullo (1995, in Scholle et al. (eds.) The Permian of Northern Pangaea vol. II)",,claystone,gray,,,,ironstone,concretionary,,sandy,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,rare,,,NA,,"""For the most part, specimens are fragmentary and occur in sandy ironstone nodules. They have been collected from surface concentrations that have formed as the gray shale in which the nodules are formed has weathered. The concentration in the parent bed is so low that attempts to get material by excavating it have had little success."" Olson (1970 p. 360)",taxonomic,"surface (float),survey of museum collection",,,,,,,"""collecting has been almost entirely from the surface"" Olson (1967 p. 45)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Cricotillus,,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,07/03/2008 02:03,23/11/2008 09:21,28557,brachydens,Cricotillus,26635,,290.1,279.3,Artinskian,,2,US,Cricotillus brachydens
739044,occ,NA,R,79402,,Pleuristion brachycoelous,species,119134,nomen dubium,Protocaptorhinus,NA,genus,37505,Olson,1970,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37505,NA,NA,NA,specimens,-97.340553,36.161667,"Orlando site, Noble Co. (Wellington Fm.)",NA,,US,Oklahoma,Noble,stated in text,seconds,,"""about 2 miles northeast of Orlando in Noble County in SE1/4 sec. 31, T. 20 N., R. 1 W."" (Olson, 1967 p. 44); Note: the town of Orlando itself lies in Logan Co., the fossil site, however, lies just across the border in Noble Co. Lat long is based on the map given by Olson (1967 p. 38).",gp_mid,-27.83,0.34,101,US,,Wellington,Sumner,,,,,,,,,NA,"""about 100 feet below the contact of the Wellington and the Garber formations"" Olson (1970 p. 360). The Artinskian age of the Wellington Fm. given here is taken from Mazzullo (1995, in Scholle et al. (eds.) The Permian of Northern Pangaea vol. II)",,claystone,gray,,,,ironstone,concretionary,,sandy,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,rare,,,NA,,"""For the most part, specimens are fragmentary and occur in sandy ironstone nodules. They have been collected from surface concentrations that have formed as the gray shale in which the nodules are formed has weathered. The concentration in the parent bed is so low that attempts to get material by excavating it have had little success."" Olson (1970 p. 360)",taxonomic,"surface (float),survey of museum collection",,,,,,,"""collecting has been almost entirely from the surface"" Olson (1967 p. 45)",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Pleuristion,,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,07/03/2008 02:03,23/11/2008 10:12,28557,brachycoelous,Protocaptorhinus,26635,,290.1,279.3,Artinskian,,50,US,Protocaptorhinus brachycoelous
739044,occ,21105,,79402,,Protocaptorhinus pricei,species,135429,,Protocaptorhinus pricei,NA,species,135429,Olson,1984,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37505,NA,NA,NA,specimens,-97.340553,36.161667,"Orlando site, Noble Co. (Wellington Fm.)",NA,,US,Oklahoma,Noble,stated in text,seconds,,"""about 2 miles northeast of Orlando in Noble County in SE1/4 sec. 31, T. 20 N., R. 1 W."" (Olson, 1967 p. 44); Note: the town of Orlando itself lies in Logan Co., the fossil site, however, lies just across the border in Noble Co. Lat long is based on the map given by Olson (1967 p. 38).",gp_mid,-27.83,0.34,101,US,,Wellington,Sumner,,,,,,,,,NA,"""about 100 feet below the contact of the Wellington and the Garber formations"" Olson (1970 p. 360). The Artinskian age of the Wellington Fm. given here is taken from Mazzullo (1995, in Scholle et al. (eds.) The Permian of Northern Pangaea vol. II)",,claystone,gray,,,,ironstone,concretionary,,sandy,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,rare,,,NA,,"""For the most part, specimens are fragmentary and occur in sandy ironstone nodules. They have been collected from surface concentrations that have formed as the gray shale in which the nodules are formed has weathered. The concentration in the parent bed is so low that attempts to get material by excavating it have had little success."" Olson (1970 p. 360)",taxonomic,"surface (float),survey of museum collection",,,,,,,"""collecting has been almost entirely from the surface"" Olson (1967 p. 45)",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Protocaptorhinus,,NA,NA,vertebrate,E. C. Olson. 1984. The Taxonomic Status and Morphology of Pleuristion brachycoelus Case; Referred to Protocaptorhinus pricei Clark and Carroll (Reptilia: Captorhinomorpha). Journal of Paleontology 58(5):1282-1295,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,09/11/2008 09:55,23/11/2008 10:11,28557,pricei,Protocaptorhinus,28423,,290.1,279.3,Artinskian,,50,US,Protocaptorhinus pricei
739076,occ,NA,,79408,,n. gen. Dictybolos n. sp. tener,species,119139,,Dictybolos tener,NA,species,119139,Olson,1970,Chordata,33815,Reptilia,36322,Araeosceloidea,119138,,NA,119136,NA,NA,NA,individuals,-97.433334,36.349998,"Perry site 6, bed 21",NA,,US,Oklahoma,Noble,estimated from map,minutes,,"""about nine miles northwest of Perry, Logan County, Oklahoma, SE1/4 SE1/4 sec. 26 T. 23 N, R. 2 W""",gp_mid,-27.41,1.27,101,US,,Wellington,Sumner,,bed,,Perry site 6,21,bottom to top,,,NA,,,dolomite,gray,,argillaceous,Y,,,,,,lacustrine indet.,foreland basin,"""These [...] beds [...] appear to have originated in a lake, very near to shore.""",macrofossils,,,,,,NA,,"body,mold/impression",,,,,,,,,,NA,,"""[...]one specimen in the dolomite [...] was a partially articulated individual [...]. It has been rather badly damaged by ground water action, and some of the bones are preserved only as molds. The skull in the dolomite specimen is not well preserved [...].""",taxonomic,field collection,,,,,E. C. Olson,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dictybolos,n. gen.,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,07/03/2008 02:59,25/11/2008 08:08,26635,tener,Dictybolos,26635,n. sp.,290.1,268,Leonard,,1,US,Dictybolos tener
739839,occ,NA,,79531,,Captorhinikos n. sp. parvus,species,119499,,Captorhinikos parvus,NA,species,119499,Olson,1970,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37496,NA,NA,NA,specimens,-97.368614,35.169445,Norman,NA,Amos Moses estate,US,Oklahoma,Cleveland,stated in text,seconds,outcrop,"short distance southeast of the campus of the University of Oklahoma, Norman, Oklahoma; on the property of Mr. Amos Moses of Norman, Oklahoma (SW 1/4 , NW 1/4 , sec. 13, T. 8 N., R. 2 W.)",gp_mid,-26.9,2.21,101,US,,Hennessey,,Fairmont Shale,group of beds,,,,,,,NA,"bed 5 of general section of Olson (1967, Oklahoma Geol. Surv. Circ. 74), about 70 feet above the base of Hennessey Fm. Haglund (1977 J. Paleont. 51(5)) additionally states that the locality is in the ""Fairmont Shale"" of the Hennessey Fm. Haglund (1977) also states, that these beds are equivalents of the Choza Fm. of the Clear Fork Group of Texas. The base and top of the Clear Fork Group are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top. Original chronostratigraphic entry >>Leonardian<< is replaced by >>Kungurian<< (TL).","""[...] the quarry [...] lies in the upper part of a thick bed of red shale. Not far above the upper level of the bone producing layer are coarser sandy shales. These, of course, bear no relationship to the deposition of the sediments of the quarry. The sediment of the quarry basically is a red-shale. Structureless red clay-shale makes up at least 80 per cent of the total. Irregularly disposed patches of lighter colored, somewhat sandier shale occur and in places small patches of pebbles, 1 to 5 mm. in diameter, are present. The most distinctive sediment is a greenish-brown, brecciated, slightly sandy shale. It shows no regular disposition either vertically or horizontally.""","""shale""",red,,,Y,"""shale""",red or brown,,sandy,,fluvial-lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,coprolite",variable,autochthonous,time-averaged,,,,common,,,NA,,for details see Olson (1970 p. 396/397),taxonomic,"field collection,survey of museum collection,observed (not collected)",FMNH,,,,"J. W. Stovall, E. C. Olson",,"OUSM = Oklahoma University Stovall Museum, Oklahoma","""individual bones, partial skeletons, skulls, jaws and occasional teeth of lungfish, scales of palaeoniscoids, small amphibians and reptiles""\r\n""To date the excavation has covered an area of about 350 square feet and approximately 1,500 cubic feet of sediment have been examined for fossils. Although the specimens are somewhat clumped in occurrence, it can be estimated fairly that they average about three per cubic foot. Thus the total number of specimens in the materials studied ranges in the neighborhood of 4,500. Of these, of course, only a small part, several hundred, has been collected. Much of the material is very fragmentary and with a few exceptions only articulated specimens, skulls, jaws and well preserved single bones were kept. Over one-half of all specimens found pertain to Lysorophus, usually consisting of vertebrae and ribs. In general, remains of this amphibian were collected only when preservation was exceptionally good, much of an individual was present, or skulls were found, either alone or associated with skeletons [!].""",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinikos,,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,12/03/2008 03:06,27/07/2009 07:45,26635,parvus,Captorhinikos,26635,n. sp.,279.3,272.3,Kungurian,,32,US,Captorhinikos parvus
739840,occ,NA,,79531,,Captorhinikos chozaensis,species,120856,,Captorhinikos chozaensis,NA,species,120856,Olson,1970,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37496,NA,NA,NA,individuals,-97.368614,35.169445,Norman,NA,Amos Moses estate,US,Oklahoma,Cleveland,stated in text,seconds,outcrop,"short distance southeast of the campus of the University of Oklahoma, Norman, Oklahoma; on the property of Mr. Amos Moses of Norman, Oklahoma (SW 1/4 , NW 1/4 , sec. 13, T. 8 N., R. 2 W.)",gp_mid,-26.9,2.21,101,US,,Hennessey,,Fairmont Shale,group of beds,,,,,,,NA,"bed 5 of general section of Olson (1967, Oklahoma Geol. Surv. Circ. 74), about 70 feet above the base of Hennessey Fm. Haglund (1977 J. Paleont. 51(5)) additionally states that the locality is in the ""Fairmont Shale"" of the Hennessey Fm. Haglund (1977) also states, that these beds are equivalents of the Choza Fm. of the Clear Fork Group of Texas. The base and top of the Clear Fork Group are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top. Original chronostratigraphic entry >>Leonardian<< is replaced by >>Kungurian<< (TL).","""[...] the quarry [...] lies in the upper part of a thick bed of red shale. Not far above the upper level of the bone producing layer are coarser sandy shales. These, of course, bear no relationship to the deposition of the sediments of the quarry. The sediment of the quarry basically is a red-shale. Structureless red clay-shale makes up at least 80 per cent of the total. Irregularly disposed patches of lighter colored, somewhat sandier shale occur and in places small patches of pebbles, 1 to 5 mm. in diameter, are present. The most distinctive sediment is a greenish-brown, brecciated, slightly sandy shale. It shows no regular disposition either vertically or horizontally.""","""shale""",red,,,Y,"""shale""",red or brown,,sandy,,fluvial-lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,coprolite",variable,autochthonous,time-averaged,,,,common,,,NA,,for details see Olson (1970 p. 396/397),taxonomic,"field collection,survey of museum collection,observed (not collected)",FMNH,,,,"J. W. Stovall, E. C. Olson",,"OUSM = Oklahoma University Stovall Museum, Oklahoma","""individual bones, partial skeletons, skulls, jaws and occasional teeth of lungfish, scales of palaeoniscoids, small amphibians and reptiles""\r\n""To date the excavation has covered an area of about 350 square feet and approximately 1,500 cubic feet of sediment have been examined for fossils. Although the specimens are somewhat clumped in occurrence, it can be estimated fairly that they average about three per cubic foot. Thus the total number of specimens in the materials studied ranges in the neighborhood of 4,500. Of these, of course, only a small part, several hundred, has been collected. Much of the material is very fragmentary and with a few exceptions only articulated specimens, skulls, jaws and well preserved single bones were kept. Over one-half of all specimens found pertain to Lysorophus, usually consisting of vertebrae and ribs. In general, remains of this amphibian were collected only when preservation was exceptionally good, much of an individual was present, or skulls were found, either alone or associated with skeletons [!].""",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinikos,,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,12/03/2008 03:06,21/01/2010 16:10,26635,chozaensis,Captorhinikos,26635,,279.3,272.3,Kungurian,,2,US,Captorhinikos chozaensis
739841,occ,NA,,79531,,Tersomius n. sp. mosesi,species,90714,,Tersomius mosesi,NA,species,90714,Olson,1970,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,37035,NA,NA,NA,specimens,-97.368614,35.169445,Norman,NA,Amos Moses estate,US,Oklahoma,Cleveland,stated in text,seconds,outcrop,"short distance southeast of the campus of the University of Oklahoma, Norman, Oklahoma; on the property of Mr. Amos Moses of Norman, Oklahoma (SW 1/4 , NW 1/4 , sec. 13, T. 8 N., R. 2 W.)",gp_mid,-26.9,2.21,101,US,,Hennessey,,Fairmont Shale,group of beds,,,,,,,NA,"bed 5 of general section of Olson (1967, Oklahoma Geol. Surv. Circ. 74), about 70 feet above the base of Hennessey Fm. Haglund (1977 J. Paleont. 51(5)) additionally states that the locality is in the ""Fairmont Shale"" of the Hennessey Fm. Haglund (1977) also states, that these beds are equivalents of the Choza Fm. of the Clear Fork Group of Texas. The base and top of the Clear Fork Group are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top. Original chronostratigraphic entry >>Leonardian<< is replaced by >>Kungurian<< (TL).","""[...] the quarry [...] lies in the upper part of a thick bed of red shale. Not far above the upper level of the bone producing layer are coarser sandy shales. These, of course, bear no relationship to the deposition of the sediments of the quarry. The sediment of the quarry basically is a red-shale. Structureless red clay-shale makes up at least 80 per cent of the total. Irregularly disposed patches of lighter colored, somewhat sandier shale occur and in places small patches of pebbles, 1 to 5 mm. in diameter, are present. The most distinctive sediment is a greenish-brown, brecciated, slightly sandy shale. It shows no regular disposition either vertically or horizontally.""","""shale""",red,,,Y,"""shale""",red or brown,,sandy,,fluvial-lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,coprolite",variable,autochthonous,time-averaged,,,,common,,,NA,,for details see Olson (1970 p. 396/397),taxonomic,"field collection,survey of museum collection,observed (not collected)",FMNH,,,,"J. W. Stovall, E. C. Olson",,"OUSM = Oklahoma University Stovall Museum, Oklahoma","""individual bones, partial skeletons, skulls, jaws and occasional teeth of lungfish, scales of palaeoniscoids, small amphibians and reptiles""\r\n""To date the excavation has covered an area of about 350 square feet and approximately 1,500 cubic feet of sediment have been examined for fossils. Although the specimens are somewhat clumped in occurrence, it can be estimated fairly that they average about three per cubic foot. Thus the total number of specimens in the materials studied ranges in the neighborhood of 4,500. Of these, of course, only a small part, several hundred, has been collected. Much of the material is very fragmentary and with a few exceptions only articulated specimens, skulls, jaws and well preserved single bones were kept. Over one-half of all specimens found pertain to Lysorophus, usually consisting of vertebrae and ribs. In general, remains of this amphibian were collected only when preservation was exceptionally good, much of an individual was present, or skulls were found, either alone or associated with skeletons [!].""","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Tersomius,,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,12/03/2008 03:06,27/07/2009 07:45,26635,mosesi,Tersomius,26635,n. sp.,279.3,272.3,Kungurian,,17,US,Tersomius mosesi
739842,occ,NA,,79531,,Goniorhynchus n. sp. stovalli,species,119360,recombined as,Rhynchonkos stovalli,NA,species,119360,Olson,1970,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Goniorhynchidae,37307,37308,NA,NA,NA,specimens,-97.368614,35.169445,Norman,NA,Amos Moses estate,US,Oklahoma,Cleveland,stated in text,seconds,outcrop,"short distance southeast of the campus of the University of Oklahoma, Norman, Oklahoma; on the property of Mr. Amos Moses of Norman, Oklahoma (SW 1/4 , NW 1/4 , sec. 13, T. 8 N., R. 2 W.)",gp_mid,-26.9,2.21,101,US,,Hennessey,,Fairmont Shale,group of beds,,,,,,,NA,"bed 5 of general section of Olson (1967, Oklahoma Geol. Surv. Circ. 74), about 70 feet above the base of Hennessey Fm. Haglund (1977 J. Paleont. 51(5)) additionally states that the locality is in the ""Fairmont Shale"" of the Hennessey Fm. Haglund (1977) also states, that these beds are equivalents of the Choza Fm. of the Clear Fork Group of Texas. The base and top of the Clear Fork Group are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top. Original chronostratigraphic entry >>Leonardian<< is replaced by >>Kungurian<< (TL).","""[...] the quarry [...] lies in the upper part of a thick bed of red shale. Not far above the upper level of the bone producing layer are coarser sandy shales. These, of course, bear no relationship to the deposition of the sediments of the quarry. The sediment of the quarry basically is a red-shale. Structureless red clay-shale makes up at least 80 per cent of the total. Irregularly disposed patches of lighter colored, somewhat sandier shale occur and in places small patches of pebbles, 1 to 5 mm. in diameter, are present. The most distinctive sediment is a greenish-brown, brecciated, slightly sandy shale. It shows no regular disposition either vertically or horizontally.""","""shale""",red,,,Y,"""shale""",red or brown,,sandy,,fluvial-lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,coprolite",variable,autochthonous,time-averaged,,,,common,,,NA,,for details see Olson (1970 p. 396/397),taxonomic,"field collection,survey of museum collection,observed (not collected)",FMNH,,,,"J. W. Stovall, E. C. Olson",,"OUSM = Oklahoma University Stovall Museum, Oklahoma","""individual bones, partial skeletons, skulls, jaws and occasional teeth of lungfish, scales of palaeoniscoids, small amphibians and reptiles""\r\n""To date the excavation has covered an area of about 350 square feet and approximately 1,500 cubic feet of sediment have been examined for fossils. Although the specimens are somewhat clumped in occurrence, it can be estimated fairly that they average about three per cubic foot. Thus the total number of specimens in the materials studied ranges in the neighborhood of 4,500. Of these, of course, only a small part, several hundred, has been collected. Much of the material is very fragmentary and with a few exceptions only articulated specimens, skulls, jaws and well preserved single bones were kept. Over one-half of all specimens found pertain to Lysorophus, usually consisting of vertebrae and ribs. In general, remains of this amphibian were collected only when preservation was exceptionally good, much of an individual was present, or skulls were found, either alone or associated with skeletons [!].""","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Goniorhynchus,,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,12/03/2008 03:06,27/07/2009 07:45,26635,stovalli,Rhynchonkos,26635,n. sp.,279.3,272.3,Kungurian,,11,US,Rhynchonkos stovalli
739843,occ,NA,,79531,,Lysorophus tricarinatus,species,70395,,Lysorophus tricarinatus,NA,species,70395,Olson,1970,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,individuals,-97.368614,35.169445,Norman,NA,Amos Moses estate,US,Oklahoma,Cleveland,stated in text,seconds,outcrop,"short distance southeast of the campus of the University of Oklahoma, Norman, Oklahoma; on the property of Mr. Amos Moses of Norman, Oklahoma (SW 1/4 , NW 1/4 , sec. 13, T. 8 N., R. 2 W.)",gp_mid,-26.9,2.21,101,US,,Hennessey,,Fairmont Shale,group of beds,,,,,,,NA,"bed 5 of general section of Olson (1967, Oklahoma Geol. Surv. Circ. 74), about 70 feet above the base of Hennessey Fm. Haglund (1977 J. Paleont. 51(5)) additionally states that the locality is in the ""Fairmont Shale"" of the Hennessey Fm. Haglund (1977) also states, that these beds are equivalents of the Choza Fm. of the Clear Fork Group of Texas. The base and top of the Clear Fork Group are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top. Original chronostratigraphic entry >>Leonardian<< is replaced by >>Kungurian<< (TL).","""[...] the quarry [...] lies in the upper part of a thick bed of red shale. Not far above the upper level of the bone producing layer are coarser sandy shales. These, of course, bear no relationship to the deposition of the sediments of the quarry. The sediment of the quarry basically is a red-shale. Structureless red clay-shale makes up at least 80 per cent of the total. Irregularly disposed patches of lighter colored, somewhat sandier shale occur and in places small patches of pebbles, 1 to 5 mm. in diameter, are present. The most distinctive sediment is a greenish-brown, brecciated, slightly sandy shale. It shows no regular disposition either vertically or horizontally.""","""shale""",red,,,Y,"""shale""",red or brown,,sandy,,fluvial-lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,coprolite",variable,autochthonous,time-averaged,,,,common,,,NA,,for details see Olson (1970 p. 396/397),taxonomic,"field collection,survey of museum collection,observed (not collected)",FMNH,,,,"J. W. Stovall, E. C. Olson",,"OUSM = Oklahoma University Stovall Museum, Oklahoma","""individual bones, partial skeletons, skulls, jaws and occasional teeth of lungfish, scales of palaeoniscoids, small amphibians and reptiles""\r\n""To date the excavation has covered an area of about 350 square feet and approximately 1,500 cubic feet of sediment have been examined for fossils. Although the specimens are somewhat clumped in occurrence, it can be estimated fairly that they average about three per cubic foot. Thus the total number of specimens in the materials studied ranges in the neighborhood of 4,500. Of these, of course, only a small part, several hundred, has been collected. Much of the material is very fragmentary and with a few exceptions only articulated specimens, skulls, jaws and well preserved single bones were kept. Over one-half of all specimens found pertain to Lysorophus, usually consisting of vertebrae and ribs. In general, remains of this amphibian were collected only when preservation was exceptionally good, much of an individual was present, or skulls were found, either alone or associated with skeletons [!].""","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,12/03/2008 03:06,27/07/2009 07:45,26635,tricarinatus,Lysorophus,26635,,279.3,272.3,Kungurian,,16,US,Lysorophus tricarinatus
739844,occ,NA,,79531,,n. gen. Peronedon n. sp. primus,species,119361,"subjective synonym of, species not entered",Diplocaulus,NA,genus,37264,Olson,1970,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,individuals,-97.368614,35.169445,Norman,NA,Amos Moses estate,US,Oklahoma,Cleveland,stated in text,seconds,outcrop,"short distance southeast of the campus of the University of Oklahoma, Norman, Oklahoma; on the property of Mr. Amos Moses of Norman, Oklahoma (SW 1/4 , NW 1/4 , sec. 13, T. 8 N., R. 2 W.)",gp_mid,-26.9,2.21,101,US,,Hennessey,,Fairmont Shale,group of beds,,,,,,,NA,"bed 5 of general section of Olson (1967, Oklahoma Geol. Surv. Circ. 74), about 70 feet above the base of Hennessey Fm. Haglund (1977 J. Paleont. 51(5)) additionally states that the locality is in the ""Fairmont Shale"" of the Hennessey Fm. Haglund (1977) also states, that these beds are equivalents of the Choza Fm. of the Clear Fork Group of Texas. The base and top of the Clear Fork Group are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top. Original chronostratigraphic entry >>Leonardian<< is replaced by >>Kungurian<< (TL).","""[...] the quarry [...] lies in the upper part of a thick bed of red shale. Not far above the upper level of the bone producing layer are coarser sandy shales. These, of course, bear no relationship to the deposition of the sediments of the quarry. The sediment of the quarry basically is a red-shale. Structureless red clay-shale makes up at least 80 per cent of the total. Irregularly disposed patches of lighter colored, somewhat sandier shale occur and in places small patches of pebbles, 1 to 5 mm. in diameter, are present. The most distinctive sediment is a greenish-brown, brecciated, slightly sandy shale. It shows no regular disposition either vertically or horizontally.""","""shale""",red,,,Y,"""shale""",red or brown,,sandy,,fluvial-lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,coprolite",variable,autochthonous,time-averaged,,,,common,,,NA,,for details see Olson (1970 p. 396/397),taxonomic,"field collection,survey of museum collection,observed (not collected)",FMNH,,,,"J. W. Stovall, E. C. Olson",,"OUSM = Oklahoma University Stovall Museum, Oklahoma","""individual bones, partial skeletons, skulls, jaws and occasional teeth of lungfish, scales of palaeoniscoids, small amphibians and reptiles""\r\n""To date the excavation has covered an area of about 350 square feet and approximately 1,500 cubic feet of sediment have been examined for fossils. Although the specimens are somewhat clumped in occurrence, it can be estimated fairly that they average about three per cubic foot. Thus the total number of specimens in the materials studied ranges in the neighborhood of 4,500. Of these, of course, only a small part, several hundred, has been collected. Much of the material is very fragmentary and with a few exceptions only articulated specimens, skulls, jaws and well preserved single bones were kept. Over one-half of all specimens found pertain to Lysorophus, usually consisting of vertebrae and ribs. In general, remains of this amphibian were collected only when preservation was exceptionally good, much of an individual was present, or skulls were found, either alone or associated with skeletons [!].""","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Peronedon,n. gen.,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,12/03/2008 03:06,27/07/2009 07:46,26635,primus,Diplocaulus,26635,n. sp.,279.3,272.3,Kungurian,,6,US,Diplocaulus primus
740366,occ,NA,,79598,,n. gen. Cephalerpeton n. sp. ventriarmatum,species,119506,,Cephalerpeton ventriarmatum,NA,species,119506,Carroll and Baird,1972,Chordata,33815,Reptilia,36322,,NA,Protorothyrididae,37486,37490,NA,NA,NA,individuals,-88.139999,41.267223,Mazon Creek,NA,"Mazon Creek Vertebrate Fauna, Braidwood Fauna, pit 11",US,Illinois,Grundy/Will,based on political unit,seconds,local area,"Lat Long is for SW Will Co., Illinois",gp_mid,-23.34,-5.09,101,US,,Carbondale,,Francis Creek Shale,,,,,,,,NA,"""Francis Creek Shale above Morris (no. 2) Coal, Carbondale Formation, Westphalian D, Middle Pennsylvanian"" (Carroll & Baird, 1972)\r\nBaird et al. (1985) refer to the no. 2 coal as Colchester or Croweburg Coal Member.","""Concretions occur typically in laminated to weakly rippled, silty mudstone deposits which typically show little or no evidence of bioturbation. Small-scale sedimentary structures in nodule-bearing sequences include climbing ripple drift, and soft-sediment load-failure..."" (Baird et al., 1985 p.90). Note that this is a general description of the fossil bearing strata of the Francis Creek Shale Member which does not refer specifically to the occurences in the Mazon Creek area proper.",mudstone,"current ripples,deformed bedding",,silty,,siderite,nodular,,,Y,deltaic indet.,foreland basin,"""...these indicate rapid and often episodic mud deposition in interdistributary bay and prodelta settings."" (Baird et al., 1985 p.90)",macrofossils,,,,,,NA,,"mold/impression,concretion,soft parts,replaced with other",good,parautochthonous,,,,,,,,NA,,"""Outlines of the limbs can be seen in the matrix, indicating the extent of the soft tissue and the texture of the skin. The bone itself was represented by a very soft, claylike material that had been removed from the hard, ironstone matrix."" (Carroll, & Baird, 1972 p. 323)\r\nBones are replaced by clay minerals such as Kaolinite (Gregory, 1948 p. 637).",taxonomic,"mechanical,survey of museum collection","FMNH,MCZ,USNM,YPM","species names,ichnofossils",,,"R. L. Moodie, P. Turnbull, among others","1871, 1953",,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cephalerpeton,n. gen.,NA,NA,vertebrate,R. L. Carroll and D. Baird. 1972. Carboniferous Stem-Reptiles of the Family Romeriidae. Bulletin of the Museum of Comparative Zoology 143(5):321-363,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,14/03/2008 06:18,03/11/2009 21:21,28608,ventriarmatum,Cephalerpeton,28608,n. sp.,311.45,306.95,Westphalian D,,1,US,Cephalerpeton ventriarmatum
740382,occ,NA,,79600,,n. gen. Kahneria n. sp. seltina,species,119509,,Kahneria seltina,NA,species,119509,Olson,1962,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37506,NA,NA,NA,individuals,-99.938332,33.66,Locality KAC (Lower Flowerpot Shale),NA,"Kahn Quarry, Driver Ranch",US,Texas,Knox,estimated from map,seconds,small collection,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork."" For details see map on p. 98 in Olson (1962).",gp_mid,-28.81,3.3,101,US,,San Angelo,Pease River,Flowerpot Shale,member,,,,,,,NA,"The upper San Angelo Fm. of Olson (1962) is widely identical to the lower part of the Flowerpot Shale Member of the upper San Angelo Fm. (sensu Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 114 ff.),claystone,"gypsiferous,green,red or brown",,,Y,sandstone,red or brown,,conglomeratic,Y,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,E. C. Olson,1958,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Kahneria,n. gen.,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,14/03/2008 06:56,26/07/2009 08:56,26846,seltina,Kahneria,26846,n. sp.,279.3,268.8,Kungurian,Roadian,4,US,Kahneria seltina
740383,occ,NA,,79601,,Labidosaurikos n. sp. barkeri,species,119514,subjective synonym of,Labidosaurikos meachami,NA,species,119515,Olson,1954,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37500,NA,NA,NA,specimens,-99.558334,33.816666,Locality FA - Pipe Site,NA,,US,Texas,Foard,estimated from map,seconds,outcrop,"southeastern corner of Foard Co.; Lat long estimation is based on map in fig. 1 in Olson (1951, J. Geol. 59(2), pp. 178-181) ",gp_mid,-30.21,0,101,US,,Choza,Clear Fork,,,,,,,,,NA,Lower part of the Choza Fm.,"""The deposits at the 'pipe site' are extremely interesting and unlike those encountered anywhere else in the Wichita or Clear Fork sections. The bed from which the fossils come is a deep red shale, exposed on a series of hills over an area about an eighth of a mile on each side. This bed is capped in many places by a thin, dense siltstone. Overlying the siltstone is an orange-red shale that carries gypsum biscuits. Underlying the producing layer, which averages about four feet in thickness, is a brownish-red shale that is devoid\r\nof fossils. The most distinctive feature of the bone-bearing shale, outside of the fact that it has fossils, is the occurrence of two types of vertically oriented ovoid structures. One type consists of mottled red and green, hard nodules that range from one to four inches in maximum diameter and up to eighteen inches in length. They are rich in vertebrate remains. They appear to have formed around the bones after deposition, presumably as a result of the reducing action of organic materials. Their vertical orientation is somewhat\r\npuzzling. The contained vertebrate remains are usually oriented with their long axes vertical, and it seems quite certain that this position was attained after the formation of the nodules. Specimens of vertebrates free in the shale rather than in nodules are orientated with their long axes horizontal and have been subjected to considerable distortion and breakage. The most reasonable suggestion seems to be that the vertical orientation of the nodules was developed during compaction of the shales, which has been extensive, with the long axes shifting to become normal to the compacting forces.\r\nThe other vertical structures [...] have been termed pipes and have given the name to the site. They pass from the base to the top of the fossiliferous bed and, at the top, are continuous with the siltstone layer that caps the bed. Their composition is similar to the capping siltstone. The pipes are oval in cross section with maximum diameters from about four to twelve inches. Orientation of the long diameters is random, even in the 'clumps' in which the pipes tend to occur. These structures do not contain vertebrates, although specimens are found 'plastered' to their sides and occasionally penetrating the pipe for a short distance.\r\nThe origin of the pipes is by no means certain. It is thought that they were formed in open holes by the introduction of the sediment that formed the siltstone layer. Superficially, they resemble lungfish burrows of the Arroyo and Vale (Romer and Olson, 1954), but the shape, size, composition, weathering, and fossil content differ. The most probable explanation is that these openings were formed by the root-like shafts of some type of plant, possibly some\r\nEquisetales, that rotted to leave openings that were later filled by sediment. There is no question that the red shales surrounding the pipes were deposited in a shallow pond, and such a pond might well have provided suitable habitat for the type of vegetation envisaged."" (Olson, 1955 pp. 60-63)","""shale""",red or brown,,,Y,,,,,,pond,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,abundant,,,NA,,,taxonomic,,,,,,E. C. Olson,1949,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurikos,,NA,NA,vertebrate,E. C. Olson. 1954. Fauna of the Vale and Choza: 9. Captorhinomorpha. Fieldiana: Geology 10(19):211-218,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,14/03/2008 07:18,18/11/2008 10:52,28508,barkeri,Labidosaurikos,26907,n. sp.,290.1,268,Leonard,,4,US,Labidosaurikos barkeri
740384,occ,NA,,79602,,n. gen. Labidosaurikos n. sp. meachami,species,119515,,Labidosaurikos meachami,NA,species,119515,Bruner,1991,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37500,NA,NA,NA,individuals,-97.583336,35.950001,Crescent,NA,,US,Oklahoma,Logan,based on nearby landmark,minutes,small collection,About 1.5 miles (2.5 km) NE of Crescent,gp_mid,-26.67,2.98,101,US,,Hennessey,,,bed,,,,,,,NA,"Stovall (1950) states that the fossil comes from the Hennessey shale. Heaton (1979, Oklahoma Geol. Surv. Bull. 127), however, assigns the locality to the uppermost part of the Garber Sandstone. Both units are correllated with the Clear Fork Group of North Texas by Heaton (1979). The base and top of the Clear Fork Group are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top. Original chronostratigraphic entry >>Leonardian<< is replaced by >>Kungurian<< (TL).",,"""siliciclastic""",hematitic,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,"mechanical,survey of museum collection",,,,,,1939,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurikos,n. gen.,NA,NA,vertebrate,J. C. Bruner. 1991. A Catalogue of Type Specimen of Fossil Vertebrates in the Field Museum of Natural History. Fieldiana: Geology (22),315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,14/03/2008 07:34,17/11/2008 14:38,26714,meachami,Labidosaurikos,26714,n. sp.,279.3,272.3,Kungurian,,1,US,Labidosaurikos meachami
741100,occ,NA,,79694,,n. gen. Rothia n. sp. multidonta,species,119703,recombined as,Rothianiscus multidonta,NA,species,119703,Olson and Beerbower,1953,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37507,NA,NA,NA,individuals,-99.73333,34.099998,"Locality HA (""Lower San Angelo Fm."")",NA,Pease River,US,Texas,Hardeman,estimated from map,minutes,outcrop,"North of Pease River, 1 mile west of Crowell-Quanah highway",gp_mid,-28.44,3.59,101,US,,San Angelo,Pease River,Flowerpot Shale,,,,,,,,NA,"""15 ft below top of section"" (Olson & Beerbower, 1953)\r\n""Re-examination, after study of the Flower Pot-San Angelo relationship elsewhere, showed without question that Flower Pot assignment is correct. [...] The age of this is herewith corrected from the original San Angelo assignment to Flower Pot."" (Olson, 1962)\r\nThe terrestrial part of Olson's Flower Pot Formation is equivalent to the Flowerpot Member of the Upper San Angelo Formation (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80) ",for details see Olson (1962 p. 121 f.),claystone,red or brown,,"silty,sandy",Y,conglomerate,red or brown,,,Y,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,,,,,,,,,,,NA,,,taxonomic,field collection,,,,,E. C. Olson,1950,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Rothia,n. gen.,NA,NA,vertebrate,"E. C. Olson and J. R. Beerbower. 1953. The San Angelo Formation, Permian of Texas, and its Vertebrates. Journal of Geology 61(5):389-423",315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,18/03/2008 08:20,01/12/2008 14:02,28373,multidonta,Rothianiscus,28373,n. sp.,279.3,268.8,Kungurian,Roadian,2,US,Rothianiscus multidonta
743415,occ,NA,,79815,,Eocaptorhinus laticeps,species,134878,recombined as,Captorhinus laticeps,NA,species,120324,Heaton,1979,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-97.417778,36.738609,McCann Quarry,NA,"""McCaren quarry""; Nardin site, Eddy site, OMNH locality V128",US,Oklahoma,Kay,stated in text,seconds,outcrop,"""3 km northeast of Eddy, Kay Co., OK"" (Heaton & Reisz, 1986);\r\n""The Quarry is on Deer Creek, 8 Miles west and 4 Miles south of Blackwell [...] in NE1/4 sec. 16 and SW1/4 sec. 9, T. 26 N., R. 2 W."" (Olson, 1967)\r\nLat long is for intersection of lines dividing secs. 9 and 16 and eastern and western half of both secs.",gp_mid,-27.2,1.6,101,US,,Wellington,Sumner,McCann Sandstone,member,,,,,,,NA,,,sandstone,"""cross stratification"",coarse,red or brown",,,Y,sandstone,"planar lamination,gray,yellow",,,Y,fluvial-deltaic indet.,foreland basin,"""predominantly nearshore [...], in part marine"" (Olson, 1967)",macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,"""Vertebrate remains occur in all phases of the sandstone, mostly as small fragments.""",taxonomic,"field collection,survey of museum collection,observed (not collected)",,,,,,,,"""Along with the bone fragments are abundant conchostracans, called Estheria by Gould (1900). Few remains of plants have been found."" Olson (1967)",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Eocaptorhinus,,NA,NA,vertebrate,"M. J. Heaton. 1979. Cranial Anatomy of Primitive Captorhinid Reptiles from the Late Pennsylvanian and Early Permian, Oklahoma and Texas. Oklahoma Geological Survey, Bulletin 127:1-83",315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,25/03/2008 08:27,11/03/2010 10:51,28557,laticeps,Captorhinus,28362,,290.1,268,Leonard,,7,US,Captorhinus laticeps
747147,occ,NA,,80014,,Kahneria seltina,species,119509,,Kahneria seltina,NA,species,119509,Olson,1962,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37506,NA,NA,NA,individuals,-99.934441,33.621944,Locality KZ (Upper San Angelo Fm.),NA,Driver Ranch,US,Texas,Knox,estimated from map,seconds,outcrop,"about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork."" For details see map on p. 98 in Olson (1962).",gp_mid,-28.83,3.26,101,US,,San Angelo,Pease River,Flowerpot Shale,group of beds,,,,,,,NA,"The upper San Angelo Fm. and basal Flowerpot Fm. of Olson (1962) are widely identical to the Flowerpot Shale Member of the upper San Angelo Fm. (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)","The Flower Pot overlies the San Angelo on a somewhat irregular surface. Its\r\nbase is marked by the usual green sandy shale, rich in gypsum. The clastic materials could have heen derived from the uppermost beds of the San Angelo and\r\nin places there is transition rather than sharp contact. Overlying this bed are clean red shales, with their continuity interrupted in the central part of the area channel deposits of green standstone and fine conglomerate. About fifty feet from these channel beds, in the red shale was found a series of green nodules, some of which carried rather poorly preserved remains of two or three skeletons of Kahneria."" (Olson, 1965 p. 112)","""shale""",red,,,,,,,,,fluvial indet.,foreland basin,"""The exposures show a fair development of terrestrial facies, identified on the basis of the nature of the red shale, the lack of gypsum, and the presence of channel sands. Basin facies, formed in the offshore zone, occur in the southwestern part of KZ"" (Olson, 1965 p. 112)",macrofossils,,,,,,NA,,"body,concretion",poor,,,,,,rare,,,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Kahneria,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,01/04/2008 07:34,03/12/2008 07:02,26846,seltina,Kahneria,26846,,279.3,268.8,Kungurian,Roadian,2,US,Kahneria seltina
748669,occ,NA,,12976,,Reptilia indet.,class,36322,,Reptilia,NA,class,36322,Olson,1956,Chordata,33815,Reptilia,36322,,NA,,NA,NA,NA,NA,NA,specimens,-99.599998,33.703335,Locality KD,NA,(Upper Vale Fm.) Main site,US,Texas,Knox,estimated from map,seconds,outcrop,"""Valley of South Wichita River, north of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.88,101,US,,Vale,Clear Fork,"""Bullwagon""",group of beds,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surfacer and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,siltstone,lenticular,,,Y,dry floodplain,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",mesofossils,,,,,,NA,,body,variable,,snapshot,,,,,,occasional,NA,,,taxonomic,field collection,FMNH,,,,"E. C. Olson, E. L. Yochelson, S. H. Mamay","1946-1948, 1955","Olson (1958) divided the locality into Quarry Site and Weathered Boulder Site, leaving the main one for recording scattered finds",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Reptilia,,NA,NA,vertebrate,"E. C. Olson. 1956. Fauna of the Vale and Choza: 13. Diadectes, Xenacanthus, and specimens of uncertain affinities. Fieldiana: Geology 10(27):329-334",14,14,697,M. Carrano,M. Carrano,E. Dunne,02/04/2008 13:41,16/03/2016 05:13,28928,indet.,,26910,,279.3,272.3,Kungurian,,1,US, indet.
748675,occ,NA,,27704,,Dimetrodon gigashomogenes,species,138123,,Dimetrodon gigashomogenes,NA,species,138123,Olson,1954,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,individuals,-99.557777,33.731667,Locality KF (Middle Vale Formation),NA,"three-channel hill, ""fish quarry""",US,Texas,Knox,estimated from map,seconds,small collection,"""approx. seven miles north of Vera, Knox County, Texas"" (Olson, 1951)\r\n""North wall of valley of South Wichita River, east of Vera-Gilliland road"" (Olson, 1948); for details see map on p. 188 in Olson (1948)",gp_mid,-29.19,1.89,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""The locality [...] KF, was assigned to the upper Vale in an earlier paper. More recent field work has shown that it comprises beds that must be assigned to the middle rather than the upper part of the Vale."" (Olson, 1954 p. 213)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191);\r\nspecimen ""was preserved in a nodule that had weathered from a conglomeratic deposit of channel origin."" (Olson, 1951 p. 89) other specimens are from a quarry in fine-grained, green channel deposits",conglomerate,"pebbly,green,red",,,Y,"""siliciclastic""","fine,green",,,Y,"""channel""",foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,,,,NA,,"""Fragmentation of the specimens occurred before and during deposition, probably as the materials were transported by the waters of the streams. This group of animals cannot be considered to represent a life assemblage."" (Olson, 1955 p. 258)",taxonomic,field collection,FMNH,,,,E. C. Olson,1946-1948,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,E. C. Olson. 1954. Fauna of the Vale and Choza: 8. Pelycosauria: Dimetrodon. Fieldiana: Geology 10(18):205-210,14,14,697,M. Carrano,M. Carrano,E. Dunne,02/04/2008 13:46,15/03/2016 11:15,28928,gigashomogenes,Dimetrodon,26926,,279.3,272.3,Kungurian,,1,US,Dimetrodon gigashomogenes
748676,occ,NA,,27705,,Labidosaurikos barkeri,species,119514,subjective synonym of,Labidosaurikos meachami,NA,species,119515,Olson,1954,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37500,NA,NA,NA,specimens,-99.585556,33.721111,Locality KI (Upper Vale Formation),NA,,US,Texas,Knox,based on nearby landmark,seconds,small collection,"Lat long is estimated from map on p. 188 in Olson (1948) using the aerial photograph indices given in the footnote in Olson (1951, p. 104).",gp_mid,-29.21,1.89,101,US,,Vale,Clear Fork,,formation,,,,,,,NA,"""base of upper part of the Vale Formation"" (Olson, 1954)\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top",,conglomerate,,,,Y,,,,,,terrestrial indet.,,,mesofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurikos,,NA,NA,vertebrate,E. C. Olson. 1954. Fauna of the Vale and Choza: 9. Captorhinomorpha. Fieldiana: Geology 10(19):211-218,14,14,0,M. Carrano,M. Carrano,,02/04/2008 13:49,02/04/2008 15:49,4326,barkeri,Labidosaurikos,26907,,279.3,272.3,Kungurian,,1,US,Labidosaurikos barkeri
748677,occ,NA,,27705,,Captorhinikos valensis,species,120855,,Captorhinikos valensis,NA,species,120855,Olson,1954,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37496,NA,NA,NA,specimens,-99.585556,33.721111,Locality KI (Upper Vale Formation),NA,,US,Texas,Knox,based on nearby landmark,seconds,small collection,"Lat long is estimated from map on p. 188 in Olson (1948) using the aerial photograph indices given in the footnote in Olson (1951, p. 104).",gp_mid,-29.21,1.89,101,US,,Vale,Clear Fork,,formation,,,,,,,NA,"""base of upper part of the Vale Formation"" (Olson, 1954)\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top",,conglomerate,,,,Y,,,,,,terrestrial indet.,,,mesofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinikos,,NA,NA,vertebrate,E. C. Olson. 1954. Fauna of the Vale and Choza: 9. Captorhinomorpha. Fieldiana: Geology 10(19):211-218,14,14,0,M. Carrano,M. Carrano,,02/04/2008 13:49,02/04/2008 15:49,4326,valensis,Captorhinikos,26907,,279.3,272.3,Kungurian,,1,US,Captorhinikos valensis
748678,occ,NA,,27704,,Captorhinikos valensis,species,120855,,Captorhinikos valensis,NA,species,120855,Olson,1954,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37496,NA,NA,NA,individuals,-99.557777,33.731667,Locality KF (Middle Vale Formation),NA,"three-channel hill, ""fish quarry""",US,Texas,Knox,estimated from map,seconds,small collection,"""approx. seven miles north of Vera, Knox County, Texas"" (Olson, 1951)\r\n""North wall of valley of South Wichita River, east of Vera-Gilliland road"" (Olson, 1948); for details see map on p. 188 in Olson (1948)",gp_mid,-29.19,1.89,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""The locality [...] KF, was assigned to the upper Vale in an earlier paper. More recent field work has shown that it comprises beds that must be assigned to the middle rather than the upper part of the Vale."" (Olson, 1954 p. 213)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191);\r\nspecimen ""was preserved in a nodule that had weathered from a conglomeratic deposit of channel origin."" (Olson, 1951 p. 89) other specimens are from a quarry in fine-grained, green channel deposits",conglomerate,"pebbly,green,red",,,Y,"""siliciclastic""","fine,green",,,Y,"""channel""",foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,,,,NA,,"""Fragmentation of the specimens occurred before and during deposition, probably as the materials were transported by the waters of the streams. This group of animals cannot be considered to represent a life assemblage."" (Olson, 1955 p. 258)",taxonomic,field collection,FMNH,,,,E. C. Olson,1946-1948,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinikos,,NA,NA,vertebrate,E. C. Olson. 1954. Fauna of the Vale and Choza: 9. Captorhinomorpha. Fieldiana: Geology 10(19):211-218,14,14,697,M. Carrano,M. Carrano,E. Dunne,02/04/2008 13:51,15/03/2016 11:15,28928,valensis,Captorhinikos,26907,,279.3,272.3,Kungurian,,1,US,Captorhinikos valensis
748679,occ,NA,,12976,,Diplocaulus n. sp. recurvatus,species,120886,,Diplocaulus recurvatus,NA,species,120886,Olson,1952,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,individuals,-99.599998,33.703335,Locality KD,NA,(Upper Vale Fm.) Main site,US,Texas,Knox,estimated from map,seconds,outcrop,"""Valley of South Wichita River, north of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.88,101,US,,Vale,Clear Fork,"""Bullwagon""",group of beds,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surfacer and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,siltstone,lenticular,,,Y,dry floodplain,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",mesofossils,,,,,,NA,,body,variable,,snapshot,,,,,,occasional,NA,,,taxonomic,field collection,FMNH,,,,"E. C. Olson, E. L. Yochelson, S. H. Mamay","1946-1948, 1955","Olson (1958) divided the locality into Quarry Site and Weathered Boulder Site, leaving the main one for recording scattered finds",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,E. C. Olson. 1952. Fauna of the upper Vale and Choza: 6. Diplocaulus. Fieldiana: Geology 10(14):147-166,14,14,697,M. Carrano,M. Carrano,E. Dunne,02/04/2008 13:55,16/03/2016 05:13,28928,recurvatus,Diplocaulus,26927,n. sp.,279.3,272.3,Kungurian,,9,US,Diplocaulus recurvatus
749053,occ,NA,,80110,,Tseajaia n. sp. campi,species,120742,,Tseajaia campi,NA,species,120742,Vaughn,1964,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Tseajaiidae,37239,37240,NA,NA,NA,,-110.063057,37.035,Organ Rock Shale,NA,Cutler Group,US,Utah,San Juan,stated in text,seconds,local area,"""... a couple of miles southeast of Monument Pass, in the southern part of of Sec. 17 E. and northern part of sec. 20, T. 43 S., R. 17 E.""",gp_mid,-35.74,6.88,101,US,,Cutler,,Organ Rock Shale,,,,,,,,NA,,"""... the fossils occur in conglomerates and in cross-bedded sandstones immediately above, below and at the lateral edges of the lenses of comglomerate. There are also fossiliferous lenses of cross-bedded sandstone within the bodies of the comglomerates"".",conglomerate,"medium,pebbly",lithified,,Y,sandstone,"""cross stratification""",lithified,,,"""floodplain""",,,macrofossils,,,,,,NA,,"permineralized,coprolite",good,,time-averaged,,,,common,,,NA,,,taxonomic,"surface (in situ),survey of museum collection",UCMP,,,,Prof. Charles C. Camp,1942,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tseajaia,,NA,NA,,"P. P. Vaughn. 1964. Vertebrates from the Organ Rock Shale of the Cutler Group, Permian of Monument Valley and vicinity, Utah and Arizona. Journal of Paleontology 38(3):567-583",310,310,0,R. Reisz,R. Reisz,,04/04/2008 11:47,04/04/2008 13:47,5803,campi,Tseajaia,5803,n. sp.,296.4,268,Wolfcamp,Leonard,NA,US,Tseajaia campi
749054,occ,NA,,80110,,Ophiacodon sp.,genus,38888,,Ophiacodon,NA,genus,38888,Vaughn,1964,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-110.063057,37.035,Organ Rock Shale,NA,Cutler Group,US,Utah,San Juan,stated in text,seconds,local area,"""... a couple of miles southeast of Monument Pass, in the southern part of of Sec. 17 E. and northern part of sec. 20, T. 43 S., R. 17 E.""",gp_mid,-35.74,6.88,101,US,,Cutler,,Organ Rock Shale,,,,,,,,NA,,"""... the fossils occur in conglomerates and in cross-bedded sandstones immediately above, below and at the lateral edges of the lenses of comglomerate. There are also fossiliferous lenses of cross-bedded sandstone within the bodies of the comglomerates"".",conglomerate,"medium,pebbly",lithified,,Y,sandstone,"""cross stratification""",lithified,,,"""floodplain""",,,macrofossils,,,,,,NA,,"permineralized,coprolite",good,,time-averaged,,,,common,,,NA,,,taxonomic,"surface (in situ),survey of museum collection",UCMP,,,,Prof. Charles C. Camp,1942,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,,"P. P. Vaughn. 1964. Vertebrates from the Organ Rock Shale of the Cutler Group, Permian of Monument Valley and vicinity, Utah and Arizona. Journal of Paleontology 38(3):567-583",310,310,0,R. Reisz,R. Reisz,,04/04/2008 11:47,04/04/2008 13:47,5803,sp.,Ophiacodon,5803,,296.4,268,Wolfcamp,Leonard,NA,US,Ophiacodon sp.
749055,occ,NA,,80110,,Eryops ? sp.,genus,37011,,Eryops,NA,genus,37011,Vaughn,1964,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,fragments,-110.063057,37.035,Organ Rock Shale,NA,Cutler Group,US,Utah,San Juan,stated in text,seconds,local area,"""... a couple of miles southeast of Monument Pass, in the southern part of of Sec. 17 E. and northern part of sec. 20, T. 43 S., R. 17 E.""",gp_mid,-35.74,6.88,101,US,,Cutler,,Organ Rock Shale,,,,,,,,NA,,"""... the fossils occur in conglomerates and in cross-bedded sandstones immediately above, below and at the lateral edges of the lenses of comglomerate. There are also fossiliferous lenses of cross-bedded sandstone within the bodies of the comglomerates"".",conglomerate,"medium,pebbly",lithified,,Y,sandstone,"""cross stratification""",lithified,,,"""floodplain""",,,macrofossils,,,,,,NA,,"permineralized,coprolite",good,,time-averaged,,,,common,,,NA,,,taxonomic,"surface (in situ),survey of museum collection",UCMP,,,,Prof. Charles C. Camp,1942,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,?,NA,NA,,"P. P. Vaughn. 1964. Vertebrates from the Organ Rock Shale of the Cutler Group, Permian of Monument Valley and vicinity, Utah and Arizona. Journal of Paleontology 38(3):567-583",310,310,334,R. Reisz,R. Reisz,T. Liebrecht,04/04/2008 11:47,11/12/2008 11:39,5803,sp.,Eryops,5803,,296.4,268,Wolfcamp,Leonard,2,US,Eryops sp.
749056,occ,NA,,80110,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Vaughn,1964,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-110.063057,37.035,Organ Rock Shale,NA,Cutler Group,US,Utah,San Juan,stated in text,seconds,local area,"""... a couple of miles southeast of Monument Pass, in the southern part of of Sec. 17 E. and northern part of sec. 20, T. 43 S., R. 17 E.""",gp_mid,-35.74,6.88,101,US,,Cutler,,Organ Rock Shale,,,,,,,,NA,,"""... the fossils occur in conglomerates and in cross-bedded sandstones immediately above, below and at the lateral edges of the lenses of comglomerate. There are also fossiliferous lenses of cross-bedded sandstone within the bodies of the comglomerates"".",conglomerate,"medium,pebbly",lithified,,Y,sandstone,"""cross stratification""",lithified,,,"""floodplain""",,,macrofossils,,,,,,NA,,"permineralized,coprolite",good,,time-averaged,,,,common,,,NA,,,taxonomic,"surface (in situ),survey of museum collection",UCMP,,,,Prof. Charles C. Camp,1942,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,,"P. P. Vaughn. 1964. Vertebrates from the Organ Rock Shale of the Cutler Group, Permian of Monument Valley and vicinity, Utah and Arizona. Journal of Paleontology 38(3):567-583",310,310,0,R. Reisz,R. Reisz,,04/04/2008 11:47,04/04/2008 13:47,5803,sp.,Diadectes,5803,,296.4,268,Wolfcamp,Leonard,NA,US,Diadectes sp.
749057,occ,NA,,80110,,Sphenacodon cf. ferocior,species,122488,,Sphenacodon ferocior,NA,species,122488,Vaughn,1964,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,,-110.063057,37.035,Organ Rock Shale,NA,Cutler Group,US,Utah,San Juan,stated in text,seconds,local area,"""... a couple of miles southeast of Monument Pass, in the southern part of of Sec. 17 E. and northern part of sec. 20, T. 43 S., R. 17 E.""",gp_mid,-35.74,6.88,101,US,,Cutler,,Organ Rock Shale,,,,,,,,NA,,"""... the fossils occur in conglomerates and in cross-bedded sandstones immediately above, below and at the lateral edges of the lenses of comglomerate. There are also fossiliferous lenses of cross-bedded sandstone within the bodies of the comglomerates"".",conglomerate,"medium,pebbly",lithified,,Y,sandstone,"""cross stratification""",lithified,,,"""floodplain""",,,macrofossils,,,,,,NA,,"permineralized,coprolite",good,,time-averaged,,,,common,,,NA,,,taxonomic,"surface (in situ),survey of museum collection",UCMP,,,,Prof. Charles C. Camp,1942,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,,"P. P. Vaughn. 1964. Vertebrates from the Organ Rock Shale of the Cutler Group, Permian of Monument Valley and vicinity, Utah and Arizona. Journal of Paleontology 38(3):567-583",310,310,334,R. Reisz,R. Reisz,T. Liebrecht,04/04/2008 11:48,11/12/2008 11:39,5803,ferocior,Sphenacodon,5803,cf.,296.4,268,Wolfcamp,Leonard,NA,US,Sphenacodon ferocior
749058,occ,NA,,80110,,Ctenospondylus aff. casei,species,122592,,Ctenospondylus casei,NA,species,122592,Vaughn,1964,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38903,NA,NA,NA,,-110.063057,37.035,Organ Rock Shale,NA,Cutler Group,US,Utah,San Juan,stated in text,seconds,local area,"""... a couple of miles southeast of Monument Pass, in the southern part of of Sec. 17 E. and northern part of sec. 20, T. 43 S., R. 17 E.""",gp_mid,-35.74,6.88,101,US,,Cutler,,Organ Rock Shale,,,,,,,,NA,,"""... the fossils occur in conglomerates and in cross-bedded sandstones immediately above, below and at the lateral edges of the lenses of comglomerate. There are also fossiliferous lenses of cross-bedded sandstone within the bodies of the comglomerates"".",conglomerate,"medium,pebbly",lithified,,Y,sandstone,"""cross stratification""",lithified,,,"""floodplain""",,,macrofossils,,,,,,NA,,"permineralized,coprolite",good,,time-averaged,,,,common,,,NA,,,taxonomic,"surface (in situ),survey of museum collection",UCMP,,,,Prof. Charles C. Camp,1942,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ctenospondylus,,NA,NA,,"P. P. Vaughn. 1964. Vertebrates from the Organ Rock Shale of the Cutler Group, Permian of Monument Valley and vicinity, Utah and Arizona. Journal of Paleontology 38(3):567-583",310,310,334,R. Reisz,R. Reisz,T. Liebrecht,04/04/2008 11:48,11/12/2008 11:39,5803,casei,Ctenospondylus,5803,aff.,296.4,268,Wolfcamp,Leonard,NA,US,Ctenospondylus casei
749059,occ,NA,,80111,,n. gen. Limnostygis n. sp. relictus,species,120760,,Limnostygis relictus,NA,species,120760,Carroll,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Limnoscelidae,37231,37235,NA,NA,NA,individuals,-60.266666,46.290001,Dominion Coal Co. strip mine No. 7,NA,"Sydney coal field; Florence, Cape Breton",CA,Nova Scotia,Cape Breton Island,estimated from map,seconds,small collection,"Dominion Coal Co. strip mine No. 7, about 2 miles north of the town of Florence",gp_mid,-3.96,-8.17,108,CA,,,Morien,,group of beds,,,,,,,NA,"""... above the Lloyd Cove (Lower Bonar) coal of the Morien group."" ",,coal,,,,Y,"""shale""",,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,permineralized,,autochthonous,snapshot,,,,,,,NA,,the vertebrate remains come from the interior of fossilized tree stumps and are completely disarticulated,taxonomic,"selective quarrying,survey of museum collection",MCZ,,,,A.S. Romer,1956,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Limnostygis,n. gen.,NA,NA,,R. L. Carroll. 1967. A Limnoscelid Reptile from the Middle Pennsylvanian. Journal of Paleontology 41(5):1256-1261,310,310,697,R. Reisz,R. Reisz,E. Dunne,04/04/2008 13:03,25/08/2016 08:12,26895,relictus,Limnostygis,26895,n. sp.,314.6,306.95,Westphalian C,Westphalian D,1,CA,Limnostygis relictus
749060,occ,NA,,80111,,Clepsydrops sp.,genus,38887,,Clepsydrops,NA,genus,38887,Carroll,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38887,NA,NA,NA,,-60.266666,46.290001,Dominion Coal Co. strip mine No. 7,NA,"Sydney coal field; Florence, Cape Breton",CA,Nova Scotia,Cape Breton Island,estimated from map,seconds,small collection,"Dominion Coal Co. strip mine No. 7, about 2 miles north of the town of Florence",gp_mid,-3.96,-8.17,108,CA,,,Morien,,group of beds,,,,,,,NA,"""... above the Lloyd Cove (Lower Bonar) coal of the Morien group."" ",,coal,,,,Y,"""shale""",,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,permineralized,,autochthonous,snapshot,,,,,,,NA,,the vertebrate remains come from the interior of fossilized tree stumps and are completely disarticulated,taxonomic,"selective quarrying,survey of museum collection",MCZ,,,,A.S. Romer,1956,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Clepsydrops,,NA,NA,,R. L. Carroll. 1967. A Limnoscelid Reptile from the Middle Pennsylvanian. Journal of Paleontology 41(5):1256-1261,310,310,697,R. Reisz,R. Reisz,E. Dunne,04/04/2008 13:03,25/08/2016 08:12,26895,sp.,Clepsydrops,26895,,314.6,306.95,Westphalian C,Westphalian D,NA,CA,Clepsydrops sp.
749061,occ,NA,,80111,,Cochleosaurus sp.,genus,37001,,Cochleosaurus,NA,genus,37001,Carroll,1967,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Cochleosauridae,36999,37001,NA,NA,NA,,-60.266666,46.290001,Dominion Coal Co. strip mine No. 7,NA,"Sydney coal field; Florence, Cape Breton",CA,Nova Scotia,Cape Breton Island,estimated from map,seconds,small collection,"Dominion Coal Co. strip mine No. 7, about 2 miles north of the town of Florence",gp_mid,-3.96,-8.17,108,CA,,,Morien,,group of beds,,,,,,,NA,"""... above the Lloyd Cove (Lower Bonar) coal of the Morien group."" ",,coal,,,,Y,"""shale""",,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,permineralized,,autochthonous,snapshot,,,,,,,NA,,the vertebrate remains come from the interior of fossilized tree stumps and are completely disarticulated,taxonomic,"selective quarrying,survey of museum collection",MCZ,,,,A.S. Romer,1956,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Cochleosaurus,,NA,NA,,R. L. Carroll. 1967. A Limnoscelid Reptile from the Middle Pennsylvanian. Journal of Paleontology 41(5):1256-1261,310,310,697,R. Reisz,R. Reisz,E. Dunne,04/04/2008 13:03,25/08/2016 08:12,26895,sp.,Cochleosaurus,26895,,314.6,306.95,Westphalian C,Westphalian D,NA,CA,Cochleosaurus sp.
749065,occ,NA,,80112,,Diadectes n. sp. absitus,species,120883,recombined as,Silvadectes absitus,NA,species,120883,Berman et al.,1998,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,345912,NA,NA,NA,specimens,10.618889,50.809723,Bromacker Quarry (upper level of Tambach sandstone),NA,,DE,Thuringia,Gotha,based on nearby landmark,seconds,outcrop,"""...middle part of the Thuringian Forest near the village of Tambach-Dietharz and about 20 km south of the town of Gotha, central Germany.""",gp_mid,21.71,7.41,305,DE,,Tambach,Rotliegend,Tambach-Sandstein,group of beds,,,,,,,NA,"""At the Bromacker quarry site are two superimposed stratigraphic successions that can be characterized by their facies associations and are referred to as the Lower Beds and Upper Beds (Eberth et al. 2000). All the vertebrates from the Bromacker quarry come from the Upper Beds [...]. The vertebrates are almost exclusively restricted to two [... horizons ...] which are separated by 50 cm in a stratigraphic interval of 1.2 m."" (Berman et al., 2001)\r\nThe Tambach Formation is of Artinskian age according to ""Stratigraphische Tabelle von Deutschland 2002"", however, a Kungurian age is proposed by L_tzner (2006) in LITHOLEX stratigraphic online database [http://www.bgr.de/app/LithoLex/gesamt_ausgabe_neu.php5?id=25]","""massive, red-brown, very fine-grained sandstone and siltstone"" (Berman et al., 2001).\r\nFor further details see Eberth et al. (2000).",sandstone,"very fine,brown,red",lithified,,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,"""alluvial paleochannel and sheetflood facies and lacustrine suspension deposits"" (Berman et al., 2001).\r\n""During the time that the Lower and Upper beds were deposited, the Tambach Basin was internally-drained and probably characterized by a wet-and-dry tropical or wetter climate that was hot year-round with seasonal-to-subseasonal cycles of rainfall and drying. [...] In the Bromacker area, the floodbasin was never deeply desiccated or heavily vegetated between flooding events."" Eberth et al. (2000).",macrofossils,,,,,,NA,,"body,permineralized",excellent,,snapshot,,,,,,,NA,,,taxonomic,"bulk,field collection",,all macrofossils,,,,,"MNG = Museum der Natur, Gotha",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"D.S. Berman, S.S. Sumida, and T. Martens. 1998. Diadectes (Diadectomorpha: Diadectidae) from the Early Permian of Central Germany, with description of a new species. Annals of Carnegie Museum 67(1):53-93",310,310,697,R. Reisz,R. Reisz,E. Dunne,04/04/2008 13:52,08/08/2016 04:59,26922,absitus,Silvadectes,26922,n. sp.,290.1,279.3,Artinskian,,4,DE,Silvadectes absitus
752530,occ,NA,,28238,,n. gen. Eothyris n. sp. parkeyi,species,122195,,Eothyris parkeyi,NA,species,122195,Romer,1937,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Eothyrididae,38898,38899,NA,NA,NA,individuals,-98.901947,33.740276,"Tit Mountain, 21 (Belle Plains Formation)",NA,"Locality 21 (Romer 1928), Locality Vd (Romer & Price 1940), Corn Mountain, Corn Hill, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Tit Mountain or Corn Hill, an elevation just northeast of Dundee"" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 500 feet above the Coleman Junction."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Not the same as ""South side of Tit Mountain butte, TMM 40031"" locality (Langston 1986); that collection was obviously made much later than the Tit Mountain collection of Romer (1928), which has less detailed locality data.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Eothyris,n. gen.,NA,NA,vertebrate,A. S. Romer. 1937. New genera and species of pelycosaurian reptiles. Proceedings of the New England Zo̦logical Club 16:89-95,315,316,14,J. Mueller,J. Dummasch,M. Carrano,28/04/2008 02:36,10/12/2012 14:28,26948,parkeyi,Eothyris,43845,n. sp.,290.1,279.3,Artinskian,,1,US,Eothyris parkeyi
752568,occ,NA,,80574,,Casea n. sp. halselli,species,120854,,Casea halselli,NA,species,120854,Olson,1954,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38915,NA,NA,NA,individuals,-99.633331,33.849998,Locality FC (Middle Choza Fm.),NA,Halsell Ranch,US,Texas,Foard,estimated from map,minutes,small collection,"""Locality FC has not been previously mentioned in the papers on the Vale and Choza. It is located on aerial photographs as follows: CZW 2C 45, pipeline road at 6.9-7.1 south along road to 6.6-4.1, west to hill at 3.3-4.3, northeast along divide to 4.4-7.0 and along breaks to 6.9-7.1. As for all cited photo-indexes, co-ordinates are measured in inches right from the left picture margin and then up from the lower picture margin. The specific location of the type specimen of Casea halselli is CZW 2C 45 4.81-7.79.""",gp_mid,-30.24,0.07,101,US,,Choza,Clear Fork,,bed,,,,,,,NA,"""Middle part of Choza Formation""",,"""shale""",red,,,Y,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Casea,,NA,NA,vertebrate,E. C. Olson. 1954. Fauna of the Vale and Choza: 7. Pelycosauria: family Caseidae. Fieldiana: Geology 10(17):193-204,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,28/04/2008 04:45,26/01/2009 10:47,26906,halselli,Casea,26906,n. sp.,290.1,268,Leonard,,1,US,Casea halselli
752569,occ,NA,,80576,,Casea n. sp. rutena,species,122217,recombined as,Euromycter rutena,NA,species,122217,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,345995,NA,NA,NA,,2.42849,44.470924,Saint-Christophe-Vallon,NA,1km east of Saint Christophe Vallon,FR,Aveyron,,stated in text,6,outcrop,"""1 km east to the village of SaintChristophe-Vallon, town of Valady, departement of Aveyron, Southern France"" Reisz et al. (2011)",gp_mid,19.6,3.43,305,FR,,,Gr̬s Rouge,,,,,,,Rodez,M1-M2,NA,"""Top of the red pelitic beds of the M1 Member, Gr̬s Rouge Group of the Rodez Basin, Saxo-Thuringian, upper Sakmarian to lower Lopingian (Lopez et al. 2005, 2008), middle Early-early Late Permian."" Reisz et al. (2011)",,sandstone,red,,,Y,conglomerate,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MNHN,,,,,,"The specimen MNHN.F.MCL-2 (Casea rutena) comes from the pelitic beds on the top of the first member (M1), whereas MNHN.F.MCL-1, found 120 m above stratigraphically, comes from the upper part of the second member (M2) (Bourges 1987; Gand pers. comm. 2009) - Reisz et al. (2011)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Casea,,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,315,316,697,J. Mueller,J. Dummasch,E. Dunne,28/04/2008 05:37,13/08/2016 11:02,27105,rutena,Euromycter,27105,n. sp.,295.5,254.17,Sakmarian,Wuchiapingian,NA,FR,Euromycter rutena
752575,occ,NA,,80578,,n. gen. Cotylorhynchus n. sp. romeri,species,122218,,Cotylorhynchus romeri,NA,species,122218,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38917,NA,NA,NA,,-97.47583,35.798332,Navina,NA,,US,Oklahoma,Logan,estimated from map,seconds,,"""4 3/4 miles west of Navina, Logan County, Oklahoma (NW 1/4 Sec. 4, T 15 N, R 4 W)""",gp_mid,-26.67,2.8,101,US,,Hennessey,,,,,,,,,,NA,about 200 feet above Garber-Hennessey contact,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cotylorhynchus,n. gen.,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,28/04/2008 06:59,14/12/2008 16:43,27105,romeri,Cotylorhynchus,27105,n. sp.,279.3,272.3,Kungurian,,NA,US,Cotylorhynchus romeri
753219,occ,NA,,80668,,Cotylorhynchus hancocki,species,122303,,Cotylorhynchus hancocki,NA,species,122303,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38917,NA,NA,NA,individuals,-99.926941,33.621944,Locality KX (Upper San Angelo Fm.),NA,Driver Ranch,US,Texas,Knox,estimated from map,seconds,outcrop,"about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork."" For details see map on p. 98 in Olson (1962)",gp_mid,-28.82,3.26,101,US,,San Angelo,Pease River,Flowerpot Shale,group of beds,,,,,,,NA,"The upper San Angelo Fm. and basal Flowerpot Fm. of Olson (1962) are widely identical to the Flowerpot Shale Member of the upper San Angelo Fm. (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",,"""shale""","green,red",,sandy,Y,conglomerate,red,,,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"""an aggregation of bones, apparently a single individual, badly scattered [...] specimen was buried a short distance from a channel deposit and appears to have been laid down in an offchannel backwash of the drainage system represented by the channel""",taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cotylorhynchus,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,03/05/2008 02:32,02/12/2008 13:09,26846,hancocki,Cotylorhynchus,26846,,279.3,268.8,Kungurian,Roadian,1,US,Cotylorhynchus hancocki
753220,occ,NA,,80669,,Angelosaurus n. sp. greeni,species,122304,,Angelosaurus greeni,NA,species,122304,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38914,NA,NA,NA,individuals,-99.917778,33.712502,Locality KR (Upper San Angelo Fm.),NA,Alexander Ranch,US,Texas,Knox,estimated from map,seconds,outcrop,"Maverick Flats 7.5' qdr; ""on the east and west flanks of a divide between two tributaries that flow south into the South Fork of the Wichita River""; For details see maps on pp. 98, 119 in Olson (1962)",gp_mid,-28.77,3.34,101,US,,San Angelo,Pease River,Flowerpot Shale,formation,,,,,,,NA,"""Exposures in this locality are predominantly San Angelo with the Flower Pot preserved on some high erosion remnants."" (Olson, 1962)\r\nThe upper San Angelo Fm. and basal Flowerpot Fm. of Olson (1962) are widely identical to the Flowerpot Shale Member of the upper San Angelo Fm. (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 119),"""shale""","green,red",,"argillaceous,sandy",,sandstone,,,,,terrestrial indet.,cratonic basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Angelosaurus,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,03/05/2008 03:44,01/12/2008 13:10,26846,greeni,Angelosaurus,26846,n. sp.,279.3,268.8,Kungurian,Roadian,2,US,Angelosaurus greeni
753601,occ,NA,,80689,,Rothia multidonta,species,119703,recombined as,Rothianiscus multidonta,NA,species,119703,Olson,1962,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37507,NA,NA,NA,individuals,-99.953613,33.690834,Locality KV (San Angelo Fm.),NA,MacFayden Ranch; Swanson Quarry,US,Texas,Knox,estimated from map,seconds,,"Maverick Flats 7.5' qdr; ""just to the north of the valley of the South Fork of the Wichita River""; close to the western border of Knox Co. For details see map on p. 98 in Olson (1962).",gp_mid,-28.81,3.33,101,US,,San Angelo,Pease River,,member,,,,,,,NA,"Middle and Upper San Angelo Formation sensu Olson (1962), corresponding to the upper Duncan Sandstone Member and lower Flowerpot Shale Member of the San Angelo Formation sensu Smith (1974)",for details see Olson (1962 p. 118),"""shale""",red,,sandy,Y,conglomerate,,,,Y,"""floodplain""",cratonic basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"Fossil vertebrates found [...] appear to have been laid down as partial skeletons. The nature of disarticulation and breakage suggests that they were\r\nscattered, probably by action of flesh-eaters, prior to burial. [...] the preserved animals give every evidence of having lived close to the sites of deposition.",taxonomic,field collection,FMNH,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Rothia,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,05/05/2008 06:21,24/07/2009 17:07,26846,multidonta,Rothianiscus,26846,,279.3,268.8,Kungurian,Roadian,2,US,Rothianiscus multidonta
753620,occ,NA,,80690,,Ophiacodon n. sp. major,species,122336,,Ophiacodon major,NA,species,122336,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-99.139442,33.669724,Maybelle,NA,"Locality VIc (Romer & Price 1940), Mabelle",US,Texas,Baylor,based on nearby landmark,seconds,,"""north of Maybelle, Baylor County, Texas""; Lat Long is for Maybelle",gp_mid,-29.99,-0.3,101,US,,Waggoner Ranch,Wichita,,,,,,,,,NA,"Waggoner Ranch Fm. is formerly known as Clyde Fm. (see Hentz, 1988, The University of Texas at Austin Bureau of Economic Geology, Report of Investigations, 170, pp. 1-55)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,05/05/2008 06:59,28/11/2008 21:47,27105,major,Ophiacodon,27105,n. sp.,290.1,268,Leonard,,1,US,Ophiacodon major
753711,occ,NA,,80714,,n. gen. Clepsydrops n. sp. collettii,species,122329,,Clepsydrops collettii,NA,species,122329,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38887,NA,NA,NA,specimens,-87.775002,40.108334,Danville Locality (Vertebrates),NA,Oakwood Locality; Horseshoe Bend; Vermillion River; Illinois bonebed,US,Illinois,Vermilion,based on nearby landmark,seconds,outcrop,"""the well-known Danville or 'Oakwood' locality [...] Horseshoe Bend locality near the SE/C of Sec. 23-19N-13W"" (DeMar, 1970)\r\n""Vermilion River, near Danville"" (Reisz, 1986)\r\nLat Long is for Oakwood",gp_mid,-21.51,-3.52,101,US,,Bond,McLeansboro,,group of beds,,,,,,,NA,"""We believe the vertebrates have been collected from a zone 10 feet or so below the Shoal Creek Member of the Bond Formation"" (DeMar, 1970)\r\nNote: Shoal Creek Member is equivalent to Carthage Limestone Member, a name now used throughout the Illinois Basin for that lithological unit; see Jacobson (2002) A summary of references with changes in Pennsylvanian stratigraphic nomenclature at the ISGS since Bulletin 95. [Online] http://www.isgs.illinois.edu/maps-data-pub/coal-maps/pennstratigraphy.shtml ",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Clepsydrops,n. gen.,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,316,14,J. Mueller,J. Dummasch,M. Carrano,06/05/2008 02:07,29/06/2015 11:47,28640,collettii,Clepsydrops,5692,n. sp.,305.9,303.4,Missourian,,14,US,Clepsydrops collettii
753718,occ,NA,,80716,,Stereorhachis dominans,species,122330,,Stereorhachis dominans,NA,species,122330,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Eothyrididae,38898,38891,NA,NA,NA,,4.383333,47.049999,Igornay,NA,,FR,Bourgogne,,based on nearby landmark,minutes,,"Igornay, near Autun",gp_mid,17.05,0.37,305,FR,,,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Stereorhachis,,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,315,316,0,J. Mueller,J. Dummasch,,06/05/2008 02:43,06/05/2008 04:43,27105,dominans,Stereorhachis,27105,,306.95,298.9,Stephanian,,NA,FR,Stereorhachis dominans
753719,occ,NA,,80717,,Slaugenhopia texensis,species,349879,,Slaugenhopia texensis,NA,species,349879,Olson,1962,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Tupilakosauridae,150320,36990,NA,NA,NA,individuals,-99.974998,33.524445,Locality KO (Upper San Angelo Fm.),NA,Little Croton Creek; MacFayden Ranch; JR Pasture,US,Texas,Knox,estimated from map,seconds,outcrop,"Cedar Mountain 7.5' qdr. Locality comprises exposures south of Little Croton Creek, just east of pipeline road. For details see map on p. 108 in Olson (1962).",gp_mid,-28.91,3.2,101,US,,San Angelo,Pease River,Flowerpot Shale,bed,,,,,,,NA,"The upper San Angelo Fm. and basal Flowerpot Fm. of Olson (1962) are widely identical to the Flowerpot Shale Member of the upper San Angelo Fm. (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 111),siltstone,"green,white",,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,rare,,,NA,,,taxonomic,field collection,FMNH,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Slaugenhopia,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,06/05/2008 02:55,26/01/2009 19:14,26846,texensis,Slaugenhopia,26846,,279.3,268.8,Kungurian,Roadian,1,US,Slaugenhopia texensis
753746,occ,NA,,80720,,Baldwinonus dunkardensis,species,122332,,Baldwinonus dunkardensis,NA,species,122332,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Eothyrididae,38898,38886,NA,NA,NA,,-80.933334,39.766666,"Locality 6, near Cameron",NA,,US,Ohio,Monroe,based on nearby landmark,minutes,,"Locality 6, near Cameron",gp_mid,-14.93,-2.65,101,US,,,Washington,,,,,,,,,NA,"Dunkard series = Asselian - Sakmarian (Wellstead, 1991)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Baldwinonus,,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,315,316,697,J. Mueller,J. Dummasch,E. Dunne,06/05/2008 03:21,18/08/2016 10:13,27105,dunkardensis,Baldwinonus,27105,,298.9,290.1,Asselian,Sakmarian,NA,US,Baldwinonus dunkardensis
753759,occ,NA,,80723,,n. gen. Stereophallodon n. sp. ciscoensis,species,122333,,Stereophallodon ciscoensis,NA,species,122333,Romer,1937,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Eothyrididae,38898,38890,NA,NA,NA,individuals,-98.433334,33.566666,southeast of Windthorst,NA,Stereophallodon type,US,Texas,Clay,based on nearby landmark,minutes,small collection,4 miles south-southeast of Windthorst,gp_mid,-29.92,-1.37,101,US,,Pueblo,Cisco,,bed,,,,,,,NA,now may belong to Wichita Group,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,some,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Stereophallodon,n. gen.,NA,NA,vertebrate,A. S. Romer. 1937. New genera and species of pelycosaurian reptiles. Proceedings of the New England Zo̦logical Club 16:89-95,315,316,14,J. Mueller,J. Dummasch,M. Carrano,06/05/2008 04:47,10/12/2012 14:30,43845,ciscoensis,Stereophallodon,43845,n. sp.,296.4,268,Wolfcamp,,1,US,Stereophallodon ciscoensis
753788,occ,NA,,80732,,n. gen. Winfieldia n. sp. hilli,species,137372,recombined as,Ophiacodon hilli,NA,species,137372,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-96.98333,37.233334,Wildcat Canyon,NA,,US,Kansas,Cowley,based on nearby landmark,minutes,small collection,"Wildcat Canyon, near Winfield; Lat long is for Winfield",gp_mid,-27.04,1.08,101,US,,Barneston Limestone,Chase,Fort Riley Limestone,member,,,,,,,NA,"""The equivalents of the Stillwater in southern Kansas and in Osage and Kay counties, Oklahoma, consist of a series of limestones and shales [...] named, in ascending order as follows: Cottonwood limestone and Garrison shale of the Council Grove group, the Wreford limestone, Matfield shale, Florence flint, Fort Riley limestone, Doyle shale, and Winfield limestone of the Chase group, and the Luta limestone, Enterprise shale, and Herington limestone members of the Marion formation of the Sumner group [...] The Stillwater forms the lowest division of the Oklahoma Permian red beds, its base being placed at the base of cottonwood limestone which is accepted as the base of the Kansas Permian"" (Gould, 1930, Proceedings of the Oklahoma Academy of Science for 1930). The Stillwater beds are considered ""contemporaneous"" to the Wichita beds of Texas (Gould, 1930).\r\nThe stratigraphic chart of Sawin et al. (2008, Current Research in Earth Sciences, Bulletin 254, part 2 [http://www.kgs.ku.edu/Current/2008/Sawin/index.html]) shows the Fort Riley Limestone as the topmost member of the Barneston Ls. Fm., the latter, according to the authors, being the Late Sakmar-Early Artinsk in age. ",,not reported,,,,,,,,,,marine indet.,,"""The equivalent of the Stillwater beds in Kansas are recognized to be the result of marine deposition"" (Gould, 1930)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Winfieldia,n. gen.,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,06/05/2008 07:41,11/01/2009 18:36,27105,hilli,Ophiacodon,27105,n. sp.,295.5,279.3,Sakmarian,Artinskian,1,US,Ophiacodon hilli
753830,occ,NA,R,80741,,Captorhinus aguti,species,90718,,Captorhinus aguti,NA,species,134887,Fox and Bowman,1966,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-98.966667,33.666668,Trematops locality (Belle Plains Fm.),NA,west of Williams Ranch,US,Texas,Baylor,stated in text,minutes,outcrop,"""west of Williams Ranch, J. Gibbs Survey A-566, southeast of Fulda,\r\nBaylor County, Texas"" (Clark & Carroll, 1973)\r\n""West of Williams, Baylor County"" (Pawley, 2007 Appendix [http://www.journalofpaleontology.org/Archives/Volume_81/81(5)/Pawley/Appendix.doc]",gp_mid,-30.27,-1.09,101,US,,Petrolia,Wichita,,,,,,,,,NA,"Petrolia Fm. is formerly known as Belle Plains Fm. (see Hentz, 1988, The University of Texas at Austin Bureau of Economic Geology, Report of Investigations, 170, pp. 1-55)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,,Further specimens probably coming from this site may be included in collections (22669) and (22668).,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,"R. C. Fox and M. C. Bowman. 1966. Osteology and Relationships of Captorhinus aguti (Cope) (Reptilia: Captorhinomorpha). The University of Kansas Paleontological Contributions, Series Vertebrata 11:1-79",315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,06/05/2008 08:09,15/12/2008 12:25,28415,aguti,Captorhinus,28784,,290.1,279.3,Artinskian,,1,US,Captorhinus aguti
753830,occ,21184,,80741,,"""Captorhinus"" laticeps",species,134970,,Captorhinus laticeps,NA,species,120324,Clark and Carroll,1973,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-98.966667,33.666668,Trematops locality (Belle Plains Fm.),NA,west of Williams Ranch,US,Texas,Baylor,stated in text,minutes,outcrop,"""west of Williams Ranch, J. Gibbs Survey A-566, southeast of Fulda,\r\nBaylor County, Texas"" (Clark & Carroll, 1973)\r\n""West of Williams, Baylor County"" (Pawley, 2007 Appendix [http://www.journalofpaleontology.org/Archives/Volume_81/81(5)/Pawley/Appendix.doc]",gp_mid,-30.27,-1.09,101,US,,Petrolia,Wichita,,,,,,,,,NA,"Petrolia Fm. is formerly known as Belle Plains Fm. (see Hentz, 1988, The University of Texas at Austin Bureau of Economic Geology, Report of Investigations, 170, pp. 1-55)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,,Further specimens probably coming from this site may be included in collections (22669) and (22668).,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,"""",NA,NA,vertebrate,J. Clark and R. L. Carroll. 1973. Romeriid Reptiles from the Lower Permian. Bulletin of the Museum of Comparative Zoology 144(5):353-407,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,15/12/2008 10:27,15/12/2008 16:06,28415,laticeps,Captorhinus,28415,,290.1,279.3,Artinskian,,1,US,Captorhinus laticeps
754185,occ,NA,,80770,,Edaphosaurus n. sp. novomexicanus,species,122351,,Edaphosaurus novomexicanus,NA,species,122351,Williston and Case,1913,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,individuals,-106.616386,36.1175,Arroyo del Agua type locality of Edaphosaurus novomexicanus,NA,,US,New Mexico,Rio Arriba,based on nearby landmark,seconds,small collection,"""vicinity of Arroyo de Agua, New Mexico"" (Williston & Case, 1913). Lat long is for village of Arroyo del Agua.",gp_mid,-34.08,4.48,101,US,FED,Abo/Cutler,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,F. von Huene,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,S. W. Williston and E. C. Case. 1913. A Description of Edaphosaurus Cope. In E. C. Case et al. Permo-Carboniferous Vertebrates from New Mexico. Carnegie Institution of Washington Publication 181:71-81,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,07/05/2008 04:17,02/12/2008 12:14,28377,novomexicanus,Edaphosaurus,28377,n. sp.,296.4,268,Wolfcamp,,1,US,Edaphosaurus novomexicanus
754217,occ,NA,,80773,,n. gen. Datheosaurus n. sp. macrourus,species,147881,,Datheosaurus macrourus,NA,species,147881,Schroeder,1905,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,147880,NA,NA,NA,individuals,16.520279,50.573055,Nowa Ruda,NA,Neurode; Intrasudetic Basin,PL,Lower Silesia,"Kodzko (Glatz, Kladsko)",estimated from map,seconds,small collection,"""Der Fund wurde in dem Steinbruche bei den Schindelh_usern, welcher Eigentum des Bergwerksbesitzers Herrn Dr. jur. Linarz ist, von Steinbrechern gemacht. Die rtlichkeit befindet sich 1,5 km ̦stlich der Stadt Neurode und 0,37 km westlich der Chaussee Neurode-Schlegel."" [""The find was made by quarrymen in the Quarry at Schindelh_user which is property of Mr. LL. D. Linarz. The locality is 1.5 km east of the town of Nowa Ruda and 0.37 km west of Nowa Ruda-Supiec road.""] (Dathe, 1900, cited in Schroeder, 1905; German town names replaced by Polish names in the translation).\r\nPolar coordinates are based on ""Geologic Map of Prussia and Adjacent States"" (sheet Neurode).",gp_mid,24.77,7.37,305,PL,,Ludwikowice,Rotliegend,,group of beds,,,,,,,NA,"Dathe (1900, cited in Schroeder, 1905) gives the stratigraphic horizon as ""unterste Stufe der Unteren Kuseler Schichten, n_mlich die der rotbraunen Sandsteine und Konglomerate mit Porphyrger̦llen"" [""lowermost Lower Kusel Beds, namely the reddish brown sandstones and conglomerates with porphyry pebbles""] and says that it represents the ""_lteste und tiefste Rotliegend Stufe"" [""oldest and lowermost Rotliegend""].\r\nThese beds are mentioned as ""reddish brown sandstones and conglomerates with porphyry pebbles"" by Dathe (1904, Erl_uterungen zur Geologischen Karte von Preuen und benachbarten Bundesstaaten, Blatt Neurode) and as ""Plate Sandstone"" by Jerzykiewicz (1987, Palynology 11) and are said/figured to underlie the beds called ""Anthracosia shale"". The latter unit is assigned to the Krajan_w Formation of modern nomenclature. So it appears that Dathe's ""reddish brown sandstones and conglomerates with porphyry pebbles"" correspond to the Ludwikowice Formation that is overlain by the Krajan_w Formation in the Intrasudetic Basin (see Kurowski, 1998, GeoLines (Prague) 6).\r\n""According to Schroeder (1904), the specimen was excavated from the lowermost unit of the Untere Kuseler Schichten (Lower Kusel beds), Lower Rotliegend (Lower Autunian) as part of the IntraSudetic Basin, Poland. It was correlated to the lowermost Permian by Huene (1956) and recently recalibrated to the Late Carboniferous Ludwikowice Formation (Niedzwiedzki & Bojanowski, 2012). Its probable age is Stephanian C, respectively Gzhelian (Nowak, 1998; Awdankiewicz et al., 2003; Schneider & Werneburg, 2012; Schneider et al., 2014)."" (Spindler, 2015)",,sandstone,,,muddy,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,The deposits of the Intrasudetic Basin (considered a intramontane basin) are in part of fluvial and in part of lacustrine origin.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"selective quarrying,survey of museum collection",MfN,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Datheosaurus,n. gen.,NA,NA,vertebrate,H. Schroeder. 1905. Datheosaurus macrourus nov. gen. nov. sp. aus dem Rotliegenden von Neurode. Jahrbuch der K̦niglich Preussischen Geologischen Landesanstalt und Bergakademie 25(2):282-294,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,07/05/2008 05:26,14/07/2009 05:42,30036,macrourus,Datheosaurus,30036,n. sp.,301.2,298.9,Kuzel,,1,PL,Datheosaurus macrourus
754218,occ,NA,,80775,,Edaphosaurus n. sp. raymondi,species,346039,nomen vanum,Edaphosauridae,NA,family,38910,Modesto and Reisz,1990,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,NA,NA,NA,NA,fragments,-79.77639,40.405834,"Pitcairn, PA",NA,,US,Pennsylvania,Allegheny,based on nearby landmark,seconds,,,gp_mid,-15.75,-5.63,101,US,,Glenshaw,Conemaugh,Pittsburgh red shale,bed,,,,,,,NA,"The Pittsburgh red shale belongs to the Glenshaw Fm. (Cecil et al., 2004, USGS Circ. 1264: 77-136) the latter being entirely Missourian in age (Eble et al., 2006, GSA Spec. Pap. 399: 197-222)",,not reported,,,,,,,,,,lacustrine indet.,foreland basin,"The Pittsburgh red shale is interpreted as a lacustrine deposit (Eble et al., 2006, GSA Spec. Pap. 399: 197-222).",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,CM,,,,P. E. Raymond,around 1908,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,S. P. Modesto and R. R. Reisz. 1990. Taxonomic status of Edaphosaurus raymondi Case. Journal of Paleontology 64(6):1049-1051,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,07/05/2008 05:39,20/02/2012 08:37,40303,raymondi,,40303,n. sp.,305.9,303.4,Missourian,,1,US, raymondi
754240,occ,NA,,80777,,n. gen. Haptodus n. sp. baylei,species,122354,,Haptodus baylei,NA,species,122354,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,38905,NA,NA,NA,,4.302778,46.984165,Les Telots,NA,"Les T̩lots, Autunois",FR,Bourgogne,Sa̫ne-et-Loire,based on nearby landmark,seconds,,"Les Telots, near Autun; polar coordinates are for Les T̩lots",gp_mid,18.55,2.72,305,FR,,,,,,,,,,,,NA,"""The localitiy yields outcrops of the Millery Formation (Autunian, Rotliegend) of Artinskian age (formerly Sakmarian; see Werneburg & Schneider, 2006; Schneider et al., 2014)"" (Spindler, 2015)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Haptodus,n. gen.,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,315,316,697,J. Mueller,J. Dummasch,E. Dunne,07/05/2008 06:08,14/03/2016 08:48,27105,baylei,Haptodus,27105,n. sp.,290.1,279.3,Artinskian,,NA,FR,Haptodus baylei
754405,occ,NA,,80783,,Haptodus n. sp. grandis,species,122357,recombined as,Hypselohaptodus grandis,NA,species,122357,Paton,1974,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,345962,NA,NA,NA,individuals,-1.575,52.375,Kenilworth,NA,,UK,England,Warwickshire,based on nearby landmark,seconds,small collection,""" [...] close to Kenilworth [...] "". Paton (1974) states that all the material collected from near Kenilworth comes from a single locality whose precise location is not known. Locality is ""probably now obscured by buildings"" (Paton 1974).",gp_mid,13.51,6.65,315,UK,,Kenilworth Sandstone,Warwickshire,,group of beds,,,,,,,NA,"The Kenilworth Sandstone is lowest Permian, possibly uppermost Carboniferous, and is a subunit of the Warwickshire Group (e.g., Powell et al., 2000, British Geological Survey Research Report RR/00/01; Ruffell et al., 2006, in Brenchley & Rawson (eds.), The Geology of England and Wales).","The Kenilworth Sandstone Formation is represented mainly by coarse grained siliciclastics (sandstones, conglomerates, breccias) deposited by freshwater action (Powell et al., 2000; Ruffell et al., 2006). ","""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,BGS,,,,,,GSM = Geological Survey Museum (British Geological Survey)\r\nGz = Warwick County Museum,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Haptodus,,NA,NA,vertebrate,R. L. Paton. 1974. Lower Permian Pelycosaurs from the English Midlands. Palaeontology 17(3):541-552,315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,08/05/2008 05:31,10/06/2009 13:47,30063,grandis,Hypselohaptodus,30063,n. sp.,298.9,295.5,Asselian,,1,UK,Hypselohaptodus grandis
754406,occ,NA,,80784,,Haptodus n. sp. garnettensis,species,122358,recombined as,Eohaptodus garnettensis,NA,species,122358,Currie,1977,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,345964,NA,NA,NA,specimens,-95.259048,38.378502,Garnett Quarry,NA,"Garnett Vertebrate Fauna, Charles Hardesty farm",US,Kansas,Anderson,estimated from map,6,outcrop,"""6 miles northwest of Garnett"" (Reisz, 1986); ""NW 1/4, NE 1/4, sec. 5, tp. 20 S, rge. 19 E, Putnam Township, Anderson County, Kansas"" (Reisz & Berman, 1986)\r\n""Charles A. Hardest farm, NW/4 NE/4 sec. 5 T20S R19E, Putnam Township, Anderson County, Kansas. The Universal Transverse Mercantor (UTM) coordinates of the quarry are 15STN963466. Locality is close to Garnett, Kansas."" (Laurin 1993). ",gp_mid,-27.44,-2.3,101,US,,Stanton,Lansing,Rock Lake Shale,group of beds,,,,,,,NA,"""Rock Lake Member, Stanton Formation, Lansing Group, Missourian Series, Upper Pennsylvanian"" (Reisz & Berman, 1996)\r\nall vertebrate remains seem to come exclusively from the basal part of the Rock Lake Shale (see Reisz et al., 1982)","""dark greyishbrown, moderately well bedded, very carbonaceous, calcareous mudstone"" (Reisz et al., 1982)",mudstone,brown,,"calcareous,carbonaceous",Y,,,,,,fine channel fill,foreland basin,"""The Rock Lake Shale is a rather thin but otherwise typical ۪outside۪ shale of a ۪Kansas Megacyclothem۪ sequence formed as a change from regressive to transgressive conditions occurred [...] The site is located along the western edge of what was, during the Late Pennsylvanian, a shallow, forested stream valley or channel that was eroded into a limestone coastal plain during the latter stages of a major eustatic fall in sea level. As the succeeding rise in sea level occurred, the valley was gradually flooded by estuarine waters"" (Reisz et al., 1982).\r\nSequence stratigraphy is interpreted from the description given by Reisz et al. (1982). The surface of the underlying limestone is the sequence boundary merged with the transgressive surface and the Lake Rock Shale is the basalmost deposit of the transgressive systems tract.",macrofossils,some,some,,,,NA,,body,good,,snapshot,,,,,,,NA,,,taxonomic,"bulk,mechanical",ROM,,,,"F. E. Peabody, R. Camp, R. L. Carroll, R. R. Reisz, M. J. Heaton, B. R. Pynn, G. MacDonald","1953-1956, 1965, 1980, 1981",,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Haptodus,,NA,NA,vertebrate,P. Currie. 1977. A New Haptodontine Sphenacodont (Reptilia: Pelycosauria) from the Upper Pennsylvanian of North America. Journal of Paleontology 51(5):927-942,315,316,327,J. Mueller,J. Dummasch,R. Butler,08/05/2008 05:42,16/10/2015 08:01,28862,garnettensis,Eohaptodus,28870,n. sp.,305.9,303.4,Missourian,,17,US,Eohaptodus garnettensis
754935,occ,NA,,80833,,n. gen. Sphenacodon n. sp. ferox,species,122487,,Sphenacodon ferox,NA,species,122487,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,individuals,-106.671387,36.184723,Baldwin bonebed,85339,"type horizon of Sphenacodon ferox & Ophiacodon mirus, Arroya de Agua",US,New Mexico,Rio Arriba,estimated from map,seconds,small collection,"""about a mile and a half above the confluence of the Poleo creek with the Puerco, and near the Mexican village of Arroya de Agua."" (Williston, 1916)\r\nApparently is what Williston (1916) calls the Poleo Creek a northwestern headstream of the Rio Puerco (see Williston & Case, 1913 p. 1 fig. 1, Inst. Washington Publ. 181), however, in modern maps a southwestern headstream is designated as Poleo Creek. ",gp_mid,-34.08,4.56,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,D. A. Baldwin,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,n. gen.,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,315,316,697,J. Mueller,J. Dummasch,E. Dunne,14/05/2008 03:10,08/07/2016 10:29,27105,ferox,Sphenacodon,27105,n. sp.,296.4,268,Wolfcamp,,1,US,Sphenacodon ferox
755453,occ,NA,,80877,,Ctenospondylus ninevehensis,species,122593,,Ctenospondylus ninevehensis,NA,species,122593,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38903,NA,NA,NA,,-80.900002,39.724998,Clark Hill,NA,,US,Ohio,Monroe,based on political unit,seconds,,"""from Clark Hill on County Route 43 near junction with State Route, Salem Township""\r\nPolar coordinates approx. mark center of Salem Township.",gp_mid,-14.82,-2.52,101,US,,Greene,Dunkard,Niniveh Limestone,bed,,,,,,,NA,"Note: The age of the Greene Fm., wich is not well constrained, here is based on correlation chart (fig. 4) in Wellstead (1991, Bull. AMNH 209).",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ctenospondylus,,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,315,316,697,J. Mueller,J. Dummasch,E. Dunne,19/05/2008 05:38,08/08/2016 03:48,27105,ninevehensis,Ctenospondylus,27105,,295.5,290.1,Sakmarian,,NA,US,Ctenospondylus ninevehensis
755725,occ,NA,,80917,,Cotylorhynchus hancocki,species,122303,,Cotylorhynchus hancocki,NA,species,122303,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38917,NA,NA,NA,individuals,-99.930557,33.627499,Locality KW (Upper San Angelo Fm.),NA,Driver Ranch,US,Texas,Knox,estimated from map,seconds,outcrop,"about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork."" For details see map on p. 98 in Olson (1962).",gp_mid,-28.82,3.27,101,US,,San Angelo,Pease River,Flowerpot Shale,group of beds,,,,,,,NA,"The upper San Angelo Fm. and basal Flowerpot Fm. of Olson (1962) are widely identical to the Flowerpot Shale Member of the upper San Angelo Fm. (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",,"""shale""",green,,sandy,,,,,,,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,FMNH,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cotylorhynchus,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,316,334,J. Mueller,J. Dummasch,T. Liebrecht,21/05/2008 02:35,04/12/2008 09:31,26846,hancocki,Cotylorhynchus,26846,,279.3,268.8,Kungurian,Roadian,1,US,Cotylorhynchus hancocki
758320,occ,NA,,81114,,n. gen. Milosaurus n. sp. mccordi,species,123521,,Milosaurus mccordi,NA,species,123521,DeMar,1970,Chordata,33815,Osteichthyes,34881,Pelycosauria,38883,,NA,38927,NA,NA,NA,individuals,-88.158333,38.991669,Falmouth Locality,NA,Newton Locality; type beds of Milosaurus mccordi,US,Illinois,Jasper,based on nearby landmark,seconds,outcrop,"SW 1/4 sec 15, T. 7N, R 10E; Lat Long is for Newton",gp_mid,-21.61,-3.29,101,US,,Mattoon,McLeansboro,,group of beds,,,,,,,NA,"""Stratigraphically, the beds are not more than 20 feet above the Reisner Limestone""\r\nIn the paper the McLeansboro Group is referred to as ""McCleansboro Group"".","""Most of the tetrapod remains are preserved in about two feet of cross-bedded siltstones, sandstones and shales which lie above a fresh water limestone, ranging in thickness from six inches to two feet or more, containing abundant remains of xenacanth sharks and lungfish. [...] the top six inches to one foot of the limestone was seen to grade into the clastic zone mentioned above.""","""mixed carbonate-siliciclastic""","""cross stratification""",,"silty,sandy",Y,,,,,,lacustrine deltaic indet.,,"""It appears [...] that the tetrapod remains are preserved in pond margin deposits of deltaic origin.""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"""The specimens are generally disarticulated (except for the holotype of M. mccordi) and appear to have been washed into the deposits.""",taxonomic,survey of museum collection,FMNH,,,,,,,"The referred specimens ""were found close to the holotype and no other large pelycosaur has been recovered from the deposit so it is concluded that these specimens are from the same species, and perhaps from the same individual as the holotype.""",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Milosaurus,n. gen.,NA,NA,vertebrate,R. DeMar. 1970. A Primitive Pelycosaur from the Pennsylvanian of Illinois. Journal of Paleontology 44(1):154-163,315,316,697,J. Mueller,J. Dummasch,E. Dunne,06/06/2008 04:53,11/05/2016 05:53,28640,mccordi,Milosaurus,28640,n. sp.,306.95,298.9,Stephanian,Virgilian,1,US,Milosaurus mccordi
762761,occ,NA,I,81525,,Matthewichnus caudifer,species,125552,,Matthewichnus caudifer,NA,species,125552,Haubold et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,125551,NA,NA,NA,,-87.166664,33.81361,Union Chapel Mine,NA,Steven C. Minkin Paleozoic Footprint Site,US,Alabama,Walker,unpublished field data,6,local area,,gp_mid,-29.2,-15.44,101,US,,Pottsville,,Mary Lee coal zone,,,,,,,,NA,Westphalian A,,"""shale""",,lithified,,,sandstone,,lithified,,,lagoonal/restricted shallow subtidal,foreland basin,,,,,,,,NA,,"mold/impression,trace",,,,,,,,,,NA,,,taphonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Matthewichnus,,NA,NA,vertebrate,"H. Haubold, A. Allen, and T. P. Atkinson, R. J. Buta, J. A. Lacefield, S. C. Minkin, B. A. Relihan. 2005. Interpretation of the tetrapod footprints from the early Pennsylvanian of Alabama. Pennsylvanian Footprints in the Black Warrior Basin of Alabama ",18,18,18,M. Uhen,M. Uhen,M. Uhen,29/06/2008 15:28,29/06/2008 17:33,27502,caudifer,Matthewichnus,27502,,318.1,306.95,Westphalian,,NA,US,Matthewichnus caudifer
762762,occ,NA,I,81525,,Nanopus n. sp. reidiae,species,125557,,Nanopus reidiae,NA,species,125557,Haubold et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,125555,NA,NA,NA,,-87.166664,33.81361,Union Chapel Mine,NA,Steven C. Minkin Paleozoic Footprint Site,US,Alabama,Walker,unpublished field data,6,local area,,gp_mid,-29.2,-15.44,101,US,,Pottsville,,Mary Lee coal zone,,,,,,,,NA,Westphalian A,,"""shale""",,lithified,,,sandstone,,lithified,,,lagoonal/restricted shallow subtidal,foreland basin,,,,,,,,NA,,"mold/impression,trace",,,,,,,,,,NA,,,taphonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Nanopus,,NA,NA,vertebrate,"H. Haubold, A. Allen, and T. P. Atkinson, R. J. Buta, J. A. Lacefield, S. C. Minkin, B. A. Relihan. 2005. Interpretation of the tetrapod footprints from the early Pennsylvanian of Alabama. Pennsylvanian Footprints in the Black Warrior Basin of Alabama ",18,18,0,M. Uhen,M. Uhen,,29/06/2008 15:28,29/06/2008 17:28,27502,reidiae,Nanopus,27502,n. sp.,318.1,306.95,Westphalian,,NA,US,Nanopus reidiae
762763,occ,NA,I,81525,,Attenosaurus subulensis,species,125100,,Attenosaurus subulensis,NA,species,125100,Haubold et al.,2005,Chordata,33815,Osteichthyes,34881,,NA,,NA,125099,NA,NA,NA,,-87.166664,33.81361,Union Chapel Mine,NA,Steven C. Minkin Paleozoic Footprint Site,US,Alabama,Walker,unpublished field data,6,local area,,gp_mid,-29.2,-15.44,101,US,,Pottsville,,Mary Lee coal zone,,,,,,,,NA,Westphalian A,,"""shale""",,lithified,,,sandstone,,lithified,,,lagoonal/restricted shallow subtidal,foreland basin,,,,,,,,NA,,"mold/impression,trace",,,,,,,,,,NA,,,taphonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Attenosaurus,,NA,NA,vertebrate,"H. Haubold, A. Allen, and T. P. Atkinson, R. J. Buta, J. A. Lacefield, S. C. Minkin, B. A. Relihan. 2005. Interpretation of the tetrapod footprints from the early Pennsylvanian of Alabama. Pennsylvanian Footprints in the Black Warrior Basin of Alabama ",18,18,0,M. Uhen,M. Uhen,,29/06/2008 15:28,29/06/2008 17:28,27502,subulensis,Attenosaurus,27502,,318.1,306.95,Westphalian,,NA,US,Attenosaurus subulensis
762764,occ,NA,,81525,,Notalacerta missouriensis,species,54512,,Notalacerta missouriensis,NA,species,54512,Haubold et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,54511,NA,NA,NA,,-87.166664,33.81361,Union Chapel Mine,NA,Steven C. Minkin Paleozoic Footprint Site,US,Alabama,Walker,unpublished field data,6,local area,,gp_mid,-29.2,-15.44,101,US,,Pottsville,,Mary Lee coal zone,,,,,,,,NA,Westphalian A,,"""shale""",,lithified,,,sandstone,,lithified,,,lagoonal/restricted shallow subtidal,foreland basin,,,,,,,,NA,,"mold/impression,trace",,,,,,,,,,NA,,,taphonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Notalacerta,,NA,NA,vertebrate,"H. Haubold, A. Allen, and T. P. Atkinson, R. J. Buta, J. A. Lacefield, S. C. Minkin, B. A. Relihan. 2005. Interpretation of the tetrapod footprints from the early Pennsylvanian of Alabama. Pennsylvanian Footprints in the Black Warrior Basin of Alabama ",18,18,0,M. Uhen,M. Uhen,,29/06/2008 15:28,29/06/2008 17:28,27502,missouriensis,Notalacerta,27502,,318.1,306.95,Westphalian,,NA,US,Notalacerta missouriensis
781260,occ,NA,I,84135,,n. gen. Attenosaurus n. sp. indistinctus,species,125101,,Attenosaurus indistinctus,NA,species,125101,Aldrich and Jones,1930,Chordata,33815,Osteichthyes,34881,,NA,,NA,125099,NA,NA,NA,,-87.523888,33.896111,Galloway No. 11 Mine,NA,,US,Alabama,Walker,estimated from map,seconds,,"near Carbon Hill, southwest slope; coordinates are for Carbon Hill",gp_mid,-29.42,-15.22,101,US,,Pottsville,,,formation,,,,,,,NA,,,"""shale""",,,,Y,,,,,,delta plain,,,macrofossils,,,,,,NA,,trace,,,,,,,,,,NA,,,general faunal/floral,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Attenosaurus,n. gen.,NA,NA,vertebrate,T. H. Aldrich and W. B. Jones. 1930. Footprints from the coal measures of Alabama. Alabama Museum of Natural History Museum Paper 9:1-64,18,18,0,M. Uhen,M. Uhen,,18/09/2008 08:44,18/09/2008 10:44,NA,indistinctus,Attenosaurus,28166,n. sp.,318.1,306.95,Westphalian,,NA,US,Attenosaurus indistinctus
781261,occ,NA,I,84135,,Attenosaurus n. sp. subulensis,species,125100,,Attenosaurus subulensis,NA,species,125100,Aldrich and Jones,1930,Chordata,33815,Osteichthyes,34881,,NA,,NA,125099,NA,NA,NA,,-87.523888,33.896111,Galloway No. 11 Mine,NA,,US,Alabama,Walker,estimated from map,seconds,,"near Carbon Hill, southwest slope; coordinates are for Carbon Hill",gp_mid,-29.42,-15.22,101,US,,Pottsville,,,formation,,,,,,,NA,,,"""shale""",,,,Y,,,,,,delta plain,,,macrofossils,,,,,,NA,,trace,,,,,,,,,,NA,,,general faunal/floral,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Attenosaurus,,NA,NA,vertebrate,T. H. Aldrich and W. B. Jones. 1930. Footprints from the coal measures of Alabama. Alabama Museum of Natural History Museum Paper 9:1-64,18,18,0,M. Uhen,M. Uhen,,18/09/2008 08:47,18/09/2008 10:47,NA,subulensis,Attenosaurus,28166,n. sp.,318.1,306.95,Westphalian,,NA,US,Attenosaurus subulensis
781267,occ,NA,I,84135,,Ctenerpeton n. sp. primum,species,133575,,Ctenerpeton primum,NA,species,133575,Aldrich and Jones,1930,Chordata,33815,Osteichthyes,34881,,NA,Urocordylidae,37270,37272,NA,NA,NA,,-87.523888,33.896111,Galloway No. 11 Mine,NA,,US,Alabama,Walker,estimated from map,seconds,,"near Carbon Hill, southwest slope; coordinates are for Carbon Hill",gp_mid,-29.42,-15.22,101,US,,Pottsville,,,formation,,,,,,,NA,,,"""shale""",,,,Y,,,,,,delta plain,,,macrofossils,,,,,,NA,,trace,,,,,,,,,,NA,,,general faunal/floral,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Ctenerpeton,,NA,NA,vertebrate,T. H. Aldrich and W. B. Jones. 1930. Footprints from the coal measures of Alabama. Alabama Museum of Natural History Museum Paper 9:1-64,18,18,0,M. Uhen,M. Uhen,,18/09/2008 08:47,18/09/2008 10:47,NA,primum,Ctenerpeton,28166,n. sp.,318.1,306.95,Westphalian,,NA,US,Ctenerpeton primum
781270,occ,NA,I,84135,,n. gen. Quadropedia n. sp. prima,species,125110,,Quadropedia prima,NA,species,125110,Aldrich and Jones,1930,Chordata,33815,Osteichthyes,34881,,NA,,NA,125109,NA,NA,NA,,-87.523888,33.896111,Galloway No. 11 Mine,NA,,US,Alabama,Walker,estimated from map,seconds,,"near Carbon Hill, southwest slope; coordinates are for Carbon Hill",gp_mid,-29.42,-15.22,101,US,,Pottsville,,,formation,,,,,,,NA,,,"""shale""",,,,Y,,,,,,delta plain,,,macrofossils,,,,,,NA,,trace,,,,,,,,,,NA,,,general faunal/floral,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Quadropedia,n. gen.,NA,NA,vertebrate,T. H. Aldrich and W. B. Jones. 1930. Footprints from the coal measures of Alabama. Alabama Museum of Natural History Museum Paper 9:1-64,18,18,0,M. Uhen,M. Uhen,,18/09/2008 08:48,18/09/2008 10:48,NA,prima,Quadropedia,28166,n. sp.,318.1,306.95,Westphalian,,NA,US,Quadropedia prima
785850,occ,NA,,84715,,Romeria texana,species,134834,,Romeria texana,NA,species,134834,Clark and Carroll,1973,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37504,NA,NA,NA,individuals,-98.433334,33.608334,Zott Pasture (Putnam Fm.),NA,,US,Texas,Archer,estimated from map,seconds,,"Zott Pasture, southwest corner, section 55, block 3, Clark and Plumb Survey, 3 miles north of Windthorst",gp_mid,-29.9,-1.34,101,US,,Putnam,Wichita,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,1 specimens,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Romeria,,NA,NA,vertebrate,J. Clark and R. L. Carroll. 1973. Romeriid Reptiles from the Lower Permian. Bulletin of the Museum of Comparative Zoology 144(5):353-407,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,08/11/2008 10:00,24/08/2016 05:26,28415,texana,Romeria,28415,,296.4,268,Wolfcamp,,1,US,Romeria texana
785851,occ,NA,,84716,,n. gen. Protocaptorhinus n. sp. pricei,species,135429,,Protocaptorhinus pricei,NA,species,135429,Clark and Carroll,1973,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37505,NA,NA,NA,individuals,-98.900002,33.641666,Rattlesnake Canyon (Admiral Fm.),NA,Locality IVc (Romer & Price 1940); Cummins' Headquarters; Lyles Place,US,Texas,Archer,estimated from map,seconds,outcrop,"Rattlesnake Canyon, Archer County, Texas. Lat long is estimated from map on p. 397 in Clark & Carroll (1973).",gp_mid,-30.23,-1.14,101,US,,Petrolia,Wichita,,,,,,,,,NA,"""Uppermost Admiral Formation"" (Clark & Carroll, 1973); the uppermost part of the traditional Admiral Fm. today is considered the lowermost part of the Petrolia Fm. (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Protocaptorhinus,n. gen.,NA,NA,vertebrate,J. Clark and R. L. Carroll. 1973. Romeriid Reptiles from the Lower Permian. Bulletin of the Museum of Comparative Zoology 144(5):353-407,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,08/11/2008 10:21,25/07/2016 04:42,28415,pricei,Protocaptorhinus,28415,n. sp.,290.1,279.3,Artinskian,,1,US,Protocaptorhinus pricei
785871,occ,NA,R,84718,,Naosaurus n. sp. uralensis,species,134990,recombined as,Riabininus uralensis,NA,species,134990,Ivakhnenko,1990,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,134991,NA,NA,NA,individuals,57.648335,58.677223,Us'va,NA,,RU,Perm,Gremyatchinsk,based on nearby landmark,seconds,local area,Lat long is for the village of Us'va.,gp_mid,41.15,28.03,302,RU,,,,,,,,,,,,NA,"Locality biostratigraphically lies within the Inta Assemblage Zone (Inta Kompleks) (Ivakhnenko, 1990; Modesto & Rybczynski, 2000), which is Asselian to Ufimian in age (Modesto & Rybczynski, 2000). Ivakhnenko (2008 p. 87) states that the locality is Artinskian in age.",,sandstone,,,,Y,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Naosaurus,,NA,NA,vertebrate,M. F. Ivakhnenko. 1990. Rannepermskie elementy faunicheskikh kompleksov tetrapod vostochnoy evropy. Paleontologicheskii Zhurnal 1990(2):102-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,09/11/2008 15:56,22/11/2008 08:43,28378,uralensis,Riabininus,28378,n. sp.,290.1,279.3,Artinskian,,1,RU,Riabininus uralensis
785871,occ,21668,,84718,,Captorhinidae indet.,family,37495,,Captorhinidae,NA,family,37495,Modesto and Rybczynski,2000,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,NA,NA,NA,NA,individuals,57.648335,58.677223,Us'va,NA,,RU,Perm,Gremyatchinsk,based on nearby landmark,seconds,local area,Lat long is for the village of Us'va.,gp_mid,41.15,28.03,302,RU,,,,,,,,,,,,NA,"Locality biostratigraphically lies within the Inta Assemblage Zone (Inta Kompleks) (Ivakhnenko, 1990; Modesto & Rybczynski, 2000), which is Asselian to Ufimian in age (Modesto & Rybczynski, 2000). Ivakhnenko (2008 p. 87) states that the locality is Artinskian in age.",,sandstone,,,,Y,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinidae,,NA,NA,vertebrate,"S. P. Modesto and N. Rybczynski. 2000. The amniote faunas of the Russian Permian: implications for Late Permian terrestrial vertebrate biogeography. In M. J. Benton, M. A. Shishkin, D. M. Unwin & E. N. Kurochkin (eds.), The Age of Dinosaurs in Russia and Mongolia, Cambridge University Press ",315,334,0,J. Mueller,T. Liebrecht,,16/04/2009 17:38,16/04/2009 19:38,28378,indet.,,28429,,290.1,279.3,Artinskian,,1,RU, indet.
785872,occ,NA,R,84719,,Riabininus uralensis,species,134992,,Riabininus uralensis,NA,species,134990,Ivakhnenko,1990,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,134991,NA,NA,NA,specimens,60.049999,66.033333,Inta city,NA,,RU,Komi,Inta,stated in text,minutes,small collection,Pechora Basin; Lat Long is from Olson (1957),gp_mid,35.28,33.63,302,RU,,Inta,,,,,,,,,,NA,"Locality biostratigraphically lies within the Inta Assemblage Zone (Inta Kompleks) (Ivakhnenko, 1990; Modesto & Rybczynski, 2000), which is Asselian to Ufimian in age (Modesto & Rybczynski, 2000). Ivakhnenko (1990, fig. 1) and Shishkin et al. (2000) say that the locality is of Ufimian age; Ivakhnenko (2008 p. 87) states that the locality is Artinskian in age (""same age"" as type locality of Riabininus uralensis, see collection (84718)).","""Carbonaceous shales and channel sandstone"" (Olson, 1957)","""shale""",,,carbonaceous,,sandstone,,,,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,PIN,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Riabininus,,NA,NA,vertebrate,M. F. Ivakhnenko. 1990. Rannepermskie elementy faunicheskikh kompleksov tetrapod vostochnoy evropy. Paleontologicheskii Zhurnal 1990(2):102-111,315,334,327,J. Mueller,T. Liebrecht,R. Butler,09/11/2008 16:07,17/07/2017 08:25,28378,uralensis,Riabininus,28378,,290.1,272.5,Artinskian,Ufimian,3,RU,Riabininus uralensis
785872,occ,21669,,84719,,Captorhinidae indet.,family,37495,,Captorhinidae,NA,family,37495,Modesto and Rybczynski,2000,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,NA,NA,NA,NA,specimens,60.049999,66.033333,Inta city,NA,,RU,Komi,Inta,stated in text,minutes,small collection,Pechora Basin; Lat Long is from Olson (1957),gp_mid,35.28,33.63,302,RU,,Inta,,,,,,,,,,NA,"Locality biostratigraphically lies within the Inta Assemblage Zone (Inta Kompleks) (Ivakhnenko, 1990; Modesto & Rybczynski, 2000), which is Asselian to Ufimian in age (Modesto & Rybczynski, 2000). Ivakhnenko (1990, fig. 1) and Shishkin et al. (2000) say that the locality is of Ufimian age; Ivakhnenko (2008 p. 87) states that the locality is Artinskian in age (""same age"" as type locality of Riabininus uralensis, see collection (84718)).","""Carbonaceous shales and channel sandstone"" (Olson, 1957)","""shale""",,,carbonaceous,,sandstone,,,,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,PIN,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinidae,,NA,NA,vertebrate,"S. P. Modesto and N. Rybczynski. 2000. The amniote faunas of the Russian Permian: implications for Late Permian terrestrial vertebrate biogeography. In M. J. Benton, M. A. Shishkin, D. M. Unwin & E. N. Kurochkin (eds.), The Age of Dinosaurs in Russia and Mongolia, Cambridge University Press ",315,334,0,J. Mueller,T. Liebrecht,,16/04/2009 17:40,16/04/2009 19:40,28378,indet.,,28429,,290.1,272.5,Artinskian,Ufimian,3,RU, indet.
786798,occ,NA,,77412,,n. gen. Rhiodenticulatus n. sp. heatoni,species,135851,,Rhiodenticulatus heatoni,NA,species,135851,Berman and Reisz,1986,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37503,NA,NA,NA,individuals,-106.639442,36.157223,UCMP V-2814,NA,Camp Quarry,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"""southeast slope of a small butte, 410 yards south of New Mexico State Highway 96, about 940 yards southeast of the Rio Puerco bridge at Arroyo del Agua, section 8, T.22N., R.3E., Rio Arriba County, New Mexico"" (Langston, 1965 p. 6; 1966 p.691)",gp_mid,-34.09,4.48,101,US,FED,Abo/Cutler,,,group of beds,,,,,,,NA,All specimens appear to come from about the same stratigraphic level (38-36 m below top of the butte). Whether these beds are uppermost Carboniferous or lower Permian is a subject of controversy.\r\n,"""soft brick-red clayey siltstone"" (Langston, 1965 p. 6; 1966 p.691; Langston & Reisz, 1981 p. 74)",siltstone,red,,argillaceous,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,general faunal/floral,"bulk,surface (float),survey of museum collection",UCMP,all macrofossils,,,"C. L. Camp, among others","1928, 1934, 1935","""Berman & Reisz reopened this quarry in 1979, but despite extensive digging by a team of five people, only a few scattered bone fragments were recovered. It appears that the site has been completeley exhausted"" (Langston & Reisz, 1981 p. 74).\r\nType of Rhiodenticulatus heatoni was ""probably not found in the main bone level of the quarry, but rather as float on the slope of Loma Salazar a few feet away and presumably at or just above the quarry bone level."" (Berman & Reisz, 1986).","""Captorhinomorphs and Diadectomorphs"" (Langston 1966 p.690)",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Rhiodenticulatus,n. gen.,NA,NA,vertebrate,"D. S. Berman and R. R. Reisz. 1986. Captorhinid reptiles from the Early Permian of New Mexico, with description of a new genus and species. Annals of Carnegie Museum 55:1-28",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,17/11/2008 12:01,20/06/2009 07:50,26206,heatoni,Rhiodenticulatus,28464,n. sp.,303.4,268,Virgilian,Wolfcamp,2,US,Rhiodenticulatus heatoni
786799,occ,NA,,79602,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Stovall,1950,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,individuals,-97.583336,35.950001,Crescent,NA,,US,Oklahoma,Logan,based on nearby landmark,minutes,small collection,About 1.5 miles (2.5 km) NE of Crescent,gp_mid,-26.67,2.98,101,US,,Hennessey,,,bed,,,,,,,NA,"Stovall (1950) states that the fossil comes from the Hennessey shale. Heaton (1979, Oklahoma Geol. Surv. Bull. 127), however, assigns the locality to the uppermost part of the Garber Sandstone. Both units are correllated with the Clear Fork Group of North Texas by Heaton (1979). The base and top of the Clear Fork Group are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top. Original chronostratigraphic entry >>Leonardian<< is replaced by >>Kungurian<< (TL).",,"""siliciclastic""",hematitic,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,"mechanical,survey of museum collection",,,,,,1939,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,J. W. Stovall. 1950. A New Cotylosaur from North Central Oklahoma. American Journal of Science 248(1):46-54,315,334,0,J. Mueller,T. Liebrecht,,17/11/2008 12:54,17/11/2008 14:54,26714,sp.,Dimetrodon,28374,,279.3,272.3,Kungurian,,1,US,Dimetrodon sp.
786835,occ,NA,,79815,,Labidosaurus n. sp. oklahomensis,species,135366,subjective synonym of,Captorhinus laticeps,NA,species,120324,Heaton,1979,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-97.417778,36.738609,McCann Quarry,NA,"""McCaren quarry""; Nardin site, Eddy site, OMNH locality V128",US,Oklahoma,Kay,stated in text,seconds,outcrop,"""3 km northeast of Eddy, Kay Co., OK"" (Heaton & Reisz, 1986);\r\n""The Quarry is on Deer Creek, 8 Miles west and 4 Miles south of Blackwell [...] in NE1/4 sec. 16 and SW1/4 sec. 9, T. 26 N., R. 2 W."" (Olson, 1967)\r\nLat long is for intersection of lines dividing secs. 9 and 16 and eastern and western half of both secs.",gp_mid,-27.2,1.6,101,US,,Wellington,Sumner,McCann Sandstone,member,,,,,,,NA,,,sandstone,"""cross stratification"",coarse,red or brown",,,Y,sandstone,"planar lamination,gray,yellow",,,Y,fluvial-deltaic indet.,foreland basin,"""predominantly nearshore [...], in part marine"" (Olson, 1967)",macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,"""Vertebrate remains occur in all phases of the sandstone, mostly as small fragments.""",taxonomic,"field collection,survey of museum collection,observed (not collected)",,,,,,,,"""Along with the bone fragments are abundant conchostracans, called Estheria by Gould (1900). Few remains of plants have been found."" Olson (1967)",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,vertebrate,"M. J. Heaton. 1979. Cranial Anatomy of Primitive Captorhinid Reptiles from the Late Pennsylvanian and Early Permian, Oklahoma and Texas. Oklahoma Geological Survey, Bulletin 127:1-83",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,18/11/2008 04:11,11/03/2010 10:51,28557,oklahomensis,Captorhinus,28362,n. sp.,290.1,268,Leonard,,1,US,Captorhinus oklahomensis
786931,occ,NA,,84941,,Dictybolos tener,species,119139,,Dictybolos tener,NA,species,119139,Olson,1970,Chordata,33815,Reptilia,36322,Araeosceloidea,119138,,NA,119136,NA,NA,NA,specimens,-97.433334,36.349998,"Perry site 6, beds 18+19",NA,,US,Oklahoma,Noble,estimated from map,minutes,,"""about nine miles northwest of Perry, Logan County, Oklahoma, SE1/4 SE1/4 sec. 26 T. 23 N, R. 2 W""",gp_mid,-27.41,1.27,101,US,,Wellington,Sumner,,group of beds,,Perry site 6,18+19,bottom to top,,,NA,,"""[...] red sandstone, bed 19 of the section. [...] small lenses that lie just under the red sandstone, in bed 18 of the section. These lenses [...] run from two to five feet in diameter, and are roughly ovoid in shape. The rock is a heterogeneous mixture of sandy shale, shale, sandstone, and masses of mud which are rich in organic remains. [...] The bed below the sandstone, of which these lenses make up the topmost part, is predominantly a dark, red to brown, sandy shale. In its upper part it also carries some lenses of very fine, chocolate colored sandy shale, with very fine sand and some mica.""",sandstone,red,,,Y,"""shale""","lenticular,red or brown",,"silty,sandy",Y,lacustrine indet.,foreland basin,"""These [...] beds [...] appear to have originated in a lake, very near to shore.""",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,common,,,NA,,"""The best preserved occur in the red sandstone, bed 19 of the section. In this bed, however, they are widely scattered. The condition of these bones is excellent; they are essentially unmineralized and uncrushed. Although some moderate concentrations occur in sandstone, there is no evidence that the clustering has any relationship to life associations. [...] By far the greatest concentration of bones occurs in small lenses that lie just under the red sandstone, in bed 18 of the section. [...] Some of these lenses have high concentrations of bones, with the new reptile predominant but with remains of other reptiles, some amphibians, and fish, making up as much as 5 per cent of the total. The matrix appears to have been highly compressible and the con-tained vertebrate remains are always severely crushed. These pockets are much the most prolific source of bones, but the crushing has limited their morphological value.""",taxonomic,field collection,,,,,E. C. Olson,,,"""Tooth plates, listed as Sphaerolepis arcata in Olson (1967), are a common associate of Platysomus and occur rather widely in both beds 18 and 19. It seems quite possible that these actually represent tooth plates of Platysomus.""\r\nBesides the taxa listed, ""indeterminate remains of a small amphibian"" are present.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dictybolos,,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,18/11/2008 07:06,18/11/2008 09:11,26635,tener,Dictybolos,26635,,290.1,268,Leonard,,131,US,Dictybolos tener
786933,occ,NA,,79601,,Trimerorhachis n. sp. rogersi,species,136359,,Trimerorhachis rogersi,NA,species,136359,Olson,1955,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-99.558334,33.816666,Locality FA - Pipe Site,NA,,US,Texas,Foard,estimated from map,seconds,outcrop,"southeastern corner of Foard Co.; Lat long estimation is based on map in fig. 1 in Olson (1951, J. Geol. 59(2), pp. 178-181) ",gp_mid,-30.21,0,101,US,,Choza,Clear Fork,,,,,,,,,NA,Lower part of the Choza Fm.,"""The deposits at the 'pipe site' are extremely interesting and unlike those encountered anywhere else in the Wichita or Clear Fork sections. The bed from which the fossils come is a deep red shale, exposed on a series of hills over an area about an eighth of a mile on each side. This bed is capped in many places by a thin, dense siltstone. Overlying the siltstone is an orange-red shale that carries gypsum biscuits. Underlying the producing layer, which averages about four feet in thickness, is a brownish-red shale that is devoid\r\nof fossils. The most distinctive feature of the bone-bearing shale, outside of the fact that it has fossils, is the occurrence of two types of vertically oriented ovoid structures. One type consists of mottled red and green, hard nodules that range from one to four inches in maximum diameter and up to eighteen inches in length. They are rich in vertebrate remains. They appear to have formed around the bones after deposition, presumably as a result of the reducing action of organic materials. Their vertical orientation is somewhat\r\npuzzling. The contained vertebrate remains are usually oriented with their long axes vertical, and it seems quite certain that this position was attained after the formation of the nodules. Specimens of vertebrates free in the shale rather than in nodules are orientated with their long axes horizontal and have been subjected to considerable distortion and breakage. The most reasonable suggestion seems to be that the vertical orientation of the nodules was developed during compaction of the shales, which has been extensive, with the long axes shifting to become normal to the compacting forces.\r\nThe other vertical structures [...] have been termed pipes and have given the name to the site. They pass from the base to the top of the fossiliferous bed and, at the top, are continuous with the siltstone layer that caps the bed. Their composition is similar to the capping siltstone. The pipes are oval in cross section with maximum diameters from about four to twelve inches. Orientation of the long diameters is random, even in the 'clumps' in which the pipes tend to occur. These structures do not contain vertebrates, although specimens are found 'plastered' to their sides and occasionally penetrating the pipe for a short distance.\r\nThe origin of the pipes is by no means certain. It is thought that they were formed in open holes by the introduction of the sediment that formed the siltstone layer. Superficially, they resemble lungfish burrows of the Arroyo and Vale (Romer and Olson, 1954), but the shape, size, composition, weathering, and fossil content differ. The most probable explanation is that these openings were formed by the root-like shafts of some type of plant, possibly some\r\nEquisetales, that rotted to leave openings that were later filled by sediment. There is no question that the red shales surrounding the pipes were deposited in a shallow pond, and such a pond might well have provided suitable habitat for the type of vegetation envisaged."" (Olson, 1955 pp. 60-63)","""shale""",red or brown,,,Y,,,,,,pond,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,abundant,,,NA,,,taxonomic,,,,,,E. C. Olson,1949,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,E. C. Olson. 1955. Fauna of the Vale and Choza: 10. Trimerorhachis: Including a Revison of Pre-Vale Species. Fieldiana: Geology 10(21):225-274,315,334,0,J. Mueller,T. Liebrecht,,18/11/2008 09:53,18/11/2008 11:53,28508,rogersi,Trimerorhachis,28508,n. sp.,290.1,268,Leonard,,13,US,Trimerorhachis rogersi
786936,occ,NA,,27704,,Trimerorhachis cf. insignis,species,90711,,Trimerorhachis insignis,NA,species,90711,Olson,1955,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-99.557777,33.731667,Locality KF (Middle Vale Formation),NA,"three-channel hill, ""fish quarry""",US,Texas,Knox,estimated from map,seconds,small collection,"""approx. seven miles north of Vera, Knox County, Texas"" (Olson, 1951)\r\n""North wall of valley of South Wichita River, east of Vera-Gilliland road"" (Olson, 1948); for details see map on p. 188 in Olson (1948)",gp_mid,-29.19,1.89,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""The locality [...] KF, was assigned to the upper Vale in an earlier paper. More recent field work has shown that it comprises beds that must be assigned to the middle rather than the upper part of the Vale."" (Olson, 1954 p. 213)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191);\r\nspecimen ""was preserved in a nodule that had weathered from a conglomeratic deposit of channel origin."" (Olson, 1951 p. 89) other specimens are from a quarry in fine-grained, green channel deposits",conglomerate,"pebbly,green,red",,,Y,"""siliciclastic""","fine,green",,,Y,"""channel""",foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,,,,NA,,"""Fragmentation of the specimens occurred before and during deposition, probably as the materials were transported by the waters of the streams. This group of animals cannot be considered to represent a life assemblage."" (Olson, 1955 p. 258)",taxonomic,field collection,FMNH,,,,E. C. Olson,1946-1948,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,E. C. Olson. 1955. Fauna of the Vale and Choza: 10. Trimerorhachis: Including a Revison of Pre-Vale Species. Fieldiana: Geology 10(21):225-274,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,18/11/2008 10:50,15/03/2016 11:15,28928,insignis,Trimerorhachis,28508,cf.,279.3,272.3,Kungurian,,13,US,Trimerorhachis insignis
787181,occ,NA,,84940,,n. gen. Casineria n. sp. kiddi,species,136422,,Casineria kiddi,NA,species,136422,Paton et al.,1999,Chordata,33815,Osteichthyes,34881,,NA,,NA,136421,NA,NA,NA,individuals,-2.827778,56.03611,Cheese Bay Shrimp Bed,NA,,UK,Scotland,East Lothian,estimated from map,seconds,outcrop,"Cheese Bay, Gullane, East Lothian (formerly Haddingtonshire), Scotland; Lat long is for Gullane",gp_mid,-8.43,-27.1,313,UK,,Gullane,Strathclyde,,bed,,Cheese Bay,Shrimp Bed,,,,NA,"""The Shrimp Bed is a localized facies [...] bounded by the Garleton Hills Volcanic Rocks and the MacGregor Marine Bands. It is considered to be equivalent in age to the Wardie Shales in which the snake-like tetrapod Lethiscus was found.""\r\nPalynostratigraphical the Shrimp Bed is located within the Perotrilites tessellatus/Schulzospora campyloptera zone (TC).\r\nSupplementary data on litho- and chronostratigraphy from Table 1 in Galtier et al. (1993, Spec. Paper Paleont. 49, pp. 57-74)",,dolomite,planar lamination,,,,lime mudstone,planar lamination,,,,carbonate indet.,,"""The laminated dolomites and mudstones containing the Shrimp Bed were probably deposited in a thermally stratified freshwater lake or brackish lagoon""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,"""The shrimp Tealliocaris is abundant [...] The fauna also includes hydroids, scorpions and occasional specimens of fishes found elsewhere in the Scottish Vis̩an.""","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Casineria,n. gen.,NA,NA,vertebrate,"R. L. Paton, T. R. Smithson, and J. A. Clack. 1999. An amniote-like skeleton from the Early Carboniferous of Scotland. Nature 398:508-513",315,334,14,J. Mueller,T. Liebrecht,M. Carrano,19/11/2008 13:30,08/08/2011 17:48,28517,kiddi,Casineria,28517,n. sp.,339.4,336,Asbian,,1,UK,Casineria kiddi
787182,occ,NA,,77412,,n. gen. Oedaleops n. sp. campi,species,122198,,Oedaleops campi,NA,species,122198,Langston,1965,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Eothyrididae,38898,38900,NA,NA,NA,individuals,-106.639442,36.157223,UCMP V-2814,NA,Camp Quarry,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"""southeast slope of a small butte, 410 yards south of New Mexico State Highway 96, about 940 yards southeast of the Rio Puerco bridge at Arroyo del Agua, section 8, T.22N., R.3E., Rio Arriba County, New Mexico"" (Langston, 1965 p. 6; 1966 p.691)",gp_mid,-34.09,4.48,101,US,FED,Abo/Cutler,,,group of beds,,,,,,,NA,All specimens appear to come from about the same stratigraphic level (38-36 m below top of the butte). Whether these beds are uppermost Carboniferous or lower Permian is a subject of controversy.\r\n,"""soft brick-red clayey siltstone"" (Langston, 1965 p. 6; 1966 p.691; Langston & Reisz, 1981 p. 74)",siltstone,red,,argillaceous,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,general faunal/floral,"bulk,surface (float),survey of museum collection",UCMP,all macrofossils,,,"C. L. Camp, among others","1928, 1934, 1935","""Berman & Reisz reopened this quarry in 1979, but despite extensive digging by a team of five people, only a few scattered bone fragments were recovered. It appears that the site has been completeley exhausted"" (Langston & Reisz, 1981 p. 74).\r\nType of Rhiodenticulatus heatoni was ""probably not found in the main bone level of the quarry, but rather as float on the slope of Loma Salazar a few feet away and presumably at or just above the quarry bone level."" (Berman & Reisz, 1986).","""Captorhinomorphs and Diadectomorphs"" (Langston 1966 p.690)",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Oedaleops,n. gen.,NA,NA,vertebrate,"W. Langston, Jr. 1965. Oedaleops campi (Reptilia: Pelycosauria) New Genus and Species from the Lower Permian of New Mexico, and the Family Eothyrididae. Bulletin of the Texas Memorial Museum 9:1-47",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,19/11/2008 15:49,20/06/2009 08:19,26206,campi,Oedaleops,30116,n. sp.,303.4,268,Virgilian,Wolfcamp,4,US,Oedaleops campi
787183,occ,NA,,77412,,Aerosaurus n. sp. wellesi,species,122318,,Aerosaurus wellesi,NA,species,122318,Langston and Reisz,1981,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,38893,NA,NA,NA,individuals,-106.639442,36.157223,UCMP V-2814,NA,Camp Quarry,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"""southeast slope of a small butte, 410 yards south of New Mexico State Highway 96, about 940 yards southeast of the Rio Puerco bridge at Arroyo del Agua, section 8, T.22N., R.3E., Rio Arriba County, New Mexico"" (Langston, 1965 p. 6; 1966 p.691)",gp_mid,-34.09,4.48,101,US,FED,Abo/Cutler,,,group of beds,,,,,,,NA,All specimens appear to come from about the same stratigraphic level (38-36 m below top of the butte). Whether these beds are uppermost Carboniferous or lower Permian is a subject of controversy.\r\n,"""soft brick-red clayey siltstone"" (Langston, 1965 p. 6; 1966 p.691; Langston & Reisz, 1981 p. 74)",siltstone,red,,argillaceous,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,general faunal/floral,"bulk,surface (float),survey of museum collection",UCMP,all macrofossils,,,"C. L. Camp, among others","1928, 1934, 1935","""Berman & Reisz reopened this quarry in 1979, but despite extensive digging by a team of five people, only a few scattered bone fragments were recovered. It appears that the site has been completeley exhausted"" (Langston & Reisz, 1981 p. 74).\r\nType of Rhiodenticulatus heatoni was ""probably not found in the main bone level of the quarry, but rather as float on the slope of Loma Salazar a few feet away and presumably at or just above the quarry bone level."" (Berman & Reisz, 1986).","""Captorhinomorphs and Diadectomorphs"" (Langston 1966 p.690)",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Aerosaurus,,NA,NA,vertebrate,"W. Langston, Jr. and R. R. Reisz. 1981. Aerosaurus wellesi, new species, a varanopseid mammal-like reptile (Synapsida: Pelycosauria) from the Lower Permian of New Mexico. Journal of Vertebrate Paleontology 1(1):73-96",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,19/11/2008 15:49,20/06/2009 08:19,26206,wellesi,Aerosaurus,28910,n. sp.,303.4,268,Virgilian,Wolfcamp,3,US,Aerosaurus wellesi
787457,occ,NA,,79402,,Archeria sp.,genus,37196,,Archeria,NA,genus,37196,Olson,1967,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,,-97.340553,36.161667,"Orlando site, Noble Co. (Wellington Fm.)",NA,,US,Oklahoma,Noble,stated in text,seconds,,"""about 2 miles northeast of Orlando in Noble County in SE1/4 sec. 31, T. 20 N., R. 1 W."" (Olson, 1967 p. 44); Note: the town of Orlando itself lies in Logan Co., the fossil site, however, lies just across the border in Noble Co. Lat long is based on the map given by Olson (1967 p. 38).",gp_mid,-27.83,0.34,101,US,,Wellington,Sumner,,,,,,,,,NA,"""about 100 feet below the contact of the Wellington and the Garber formations"" Olson (1970 p. 360). The Artinskian age of the Wellington Fm. given here is taken from Mazzullo (1995, in Scholle et al. (eds.) The Permian of Northern Pangaea vol. II)",,claystone,gray,,,,ironstone,concretionary,,sandy,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,rare,,,NA,,"""For the most part, specimens are fragmentary and occur in sandy ironstone nodules. They have been collected from surface concentrations that have formed as the gray shale in which the nodules are formed has weathered. The concentration in the parent bed is so low that attempts to get material by excavating it have had little success."" Olson (1970 p. 360)",taxonomic,"surface (float),survey of museum collection",,,,,,,"""collecting has been almost entirely from the surface"" Olson (1967 p. 45)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,23/11/2008 06:54,23/11/2008 09:29,28557,sp.,Archeria,28557,,290.1,279.3,Artinskian,,NA,US,Archeria sp.
787458,occ,NA,,79402,,Trimerorhachis insignis,species,90711,,Trimerorhachis insignis,NA,species,90711,Olson,1967,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-97.340553,36.161667,"Orlando site, Noble Co. (Wellington Fm.)",NA,,US,Oklahoma,Noble,stated in text,seconds,,"""about 2 miles northeast of Orlando in Noble County in SE1/4 sec. 31, T. 20 N., R. 1 W."" (Olson, 1967 p. 44); Note: the town of Orlando itself lies in Logan Co., the fossil site, however, lies just across the border in Noble Co. Lat long is based on the map given by Olson (1967 p. 38).",gp_mid,-27.83,0.34,101,US,,Wellington,Sumner,,,,,,,,,NA,"""about 100 feet below the contact of the Wellington and the Garber formations"" Olson (1970 p. 360). The Artinskian age of the Wellington Fm. given here is taken from Mazzullo (1995, in Scholle et al. (eds.) The Permian of Northern Pangaea vol. II)",,claystone,gray,,,,ironstone,concretionary,,sandy,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,rare,,,NA,,"""For the most part, specimens are fragmentary and occur in sandy ironstone nodules. They have been collected from surface concentrations that have formed as the gray shale in which the nodules are formed has weathered. The concentration in the parent bed is so low that attempts to get material by excavating it have had little success."" Olson (1970 p. 360)",taxonomic,"surface (float),survey of museum collection",,,,,,,"""collecting has been almost entirely from the surface"" Olson (1967 p. 45)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,23/11/2008 06:54,23/11/2008 10:14,28557,insignis,Trimerorhachis,28557,,290.1,279.3,Artinskian,,NA,US,Trimerorhachis insignis
787459,occ,NA,,79402,,Eryops megacephalus,species,70397,,Eryops megacephalus,NA,species,70397,Olson,1967,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-97.340553,36.161667,"Orlando site, Noble Co. (Wellington Fm.)",NA,,US,Oklahoma,Noble,stated in text,seconds,,"""about 2 miles northeast of Orlando in Noble County in SE1/4 sec. 31, T. 20 N., R. 1 W."" (Olson, 1967 p. 44); Note: the town of Orlando itself lies in Logan Co., the fossil site, however, lies just across the border in Noble Co. Lat long is based on the map given by Olson (1967 p. 38).",gp_mid,-27.83,0.34,101,US,,Wellington,Sumner,,,,,,,,,NA,"""about 100 feet below the contact of the Wellington and the Garber formations"" Olson (1970 p. 360). The Artinskian age of the Wellington Fm. given here is taken from Mazzullo (1995, in Scholle et al. (eds.) The Permian of Northern Pangaea vol. II)",,claystone,gray,,,,ironstone,concretionary,,sandy,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,rare,,,NA,,"""For the most part, specimens are fragmentary and occur in sandy ironstone nodules. They have been collected from surface concentrations that have formed as the gray shale in which the nodules are formed has weathered. The concentration in the parent bed is so low that attempts to get material by excavating it have had little success."" Olson (1970 p. 360)",taxonomic,"surface (float),survey of museum collection",,,,,,,"""collecting has been almost entirely from the surface"" Olson (1967 p. 45)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,23/11/2008 06:54,23/11/2008 09:29,28557,megacephalus,Eryops,28557,,290.1,279.3,Artinskian,,NA,US,Eryops megacephalus
787460,occ,NA,,79402,,Diplocaulus magnicornis,species,81712,,Diplocaulus magnicornis,NA,species,81712,Olson,1967,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-97.340553,36.161667,"Orlando site, Noble Co. (Wellington Fm.)",NA,,US,Oklahoma,Noble,stated in text,seconds,,"""about 2 miles northeast of Orlando in Noble County in SE1/4 sec. 31, T. 20 N., R. 1 W."" (Olson, 1967 p. 44); Note: the town of Orlando itself lies in Logan Co., the fossil site, however, lies just across the border in Noble Co. Lat long is based on the map given by Olson (1967 p. 38).",gp_mid,-27.83,0.34,101,US,,Wellington,Sumner,,,,,,,,,NA,"""about 100 feet below the contact of the Wellington and the Garber formations"" Olson (1970 p. 360). The Artinskian age of the Wellington Fm. given here is taken from Mazzullo (1995, in Scholle et al. (eds.) The Permian of Northern Pangaea vol. II)",,claystone,gray,,,,ironstone,concretionary,,sandy,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,rare,,,NA,,"""For the most part, specimens are fragmentary and occur in sandy ironstone nodules. They have been collected from surface concentrations that have formed as the gray shale in which the nodules are formed has weathered. The concentration in the parent bed is so low that attempts to get material by excavating it have had little success."" Olson (1970 p. 360)",taxonomic,"surface (float),survey of museum collection",,,,,,,"""collecting has been almost entirely from the surface"" Olson (1967 p. 45)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,23/11/2008 06:54,23/11/2008 10:14,28557,magnicornis,Diplocaulus,28557,,290.1,279.3,Artinskian,,NA,US,Diplocaulus magnicornis
787461,occ,NA,,79402,,n. gen. Crossotelos n. sp. annulatus,species,137515,,Crossotelos annulatus,NA,species,137515,Olson,1967,Chordata,33815,Osteichthyes,34881,,NA,Urocordylidae,37270,37271,NA,NA,NA,,-97.340553,36.161667,"Orlando site, Noble Co. (Wellington Fm.)",NA,,US,Oklahoma,Noble,stated in text,seconds,,"""about 2 miles northeast of Orlando in Noble County in SE1/4 sec. 31, T. 20 N., R. 1 W."" (Olson, 1967 p. 44); Note: the town of Orlando itself lies in Logan Co., the fossil site, however, lies just across the border in Noble Co. Lat long is based on the map given by Olson (1967 p. 38).",gp_mid,-27.83,0.34,101,US,,Wellington,Sumner,,,,,,,,,NA,"""about 100 feet below the contact of the Wellington and the Garber formations"" Olson (1970 p. 360). The Artinskian age of the Wellington Fm. given here is taken from Mazzullo (1995, in Scholle et al. (eds.) The Permian of Northern Pangaea vol. II)",,claystone,gray,,,,ironstone,concretionary,,sandy,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,rare,,,NA,,"""For the most part, specimens are fragmentary and occur in sandy ironstone nodules. They have been collected from surface concentrations that have formed as the gray shale in which the nodules are formed has weathered. The concentration in the parent bed is so low that attempts to get material by excavating it have had little success."" Olson (1970 p. 360)",taxonomic,"surface (float),survey of museum collection",,,,,,,"""collecting has been almost entirely from the surface"" Olson (1967 p. 45)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Crossotelos,n. gen.,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,23/11/2008 06:54,12/12/2008 05:54,28557,annulatus,Crossotelos,28557,n. sp.,290.1,279.3,Artinskian,,NA,US,Crossotelos annulatus
787462,occ,NA,,79402,,Lysorophus tricarinatus,species,70395,,Lysorophus tricarinatus,NA,species,70395,Olson,1967,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-97.340553,36.161667,"Orlando site, Noble Co. (Wellington Fm.)",NA,,US,Oklahoma,Noble,stated in text,seconds,,"""about 2 miles northeast of Orlando in Noble County in SE1/4 sec. 31, T. 20 N., R. 1 W."" (Olson, 1967 p. 44); Note: the town of Orlando itself lies in Logan Co., the fossil site, however, lies just across the border in Noble Co. Lat long is based on the map given by Olson (1967 p. 38).",gp_mid,-27.83,0.34,101,US,,Wellington,Sumner,,,,,,,,,NA,"""about 100 feet below the contact of the Wellington and the Garber formations"" Olson (1970 p. 360). The Artinskian age of the Wellington Fm. given here is taken from Mazzullo (1995, in Scholle et al. (eds.) The Permian of Northern Pangaea vol. II)",,claystone,gray,,,,ironstone,concretionary,,sandy,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,rare,,,NA,,"""For the most part, specimens are fragmentary and occur in sandy ironstone nodules. They have been collected from surface concentrations that have formed as the gray shale in which the nodules are formed has weathered. The concentration in the parent bed is so low that attempts to get material by excavating it have had little success."" Olson (1970 p. 360)",taxonomic,"surface (float),survey of museum collection",,,,,,,"""collecting has been almost entirely from the surface"" Olson (1967 p. 45)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,23/11/2008 06:54,23/11/2008 09:29,28557,tricarinatus,Lysorophus,28557,,290.1,279.3,Artinskian,,NA,US,Lysorophus tricarinatus
787463,occ,NA,,79402,,Seymouria baylorensis,species,137488,,Seymouria baylorensis,NA,species,137488,Olson,1967,Chordata,33815,Osteichthyes,34881,,NA,Seymouriidae,37219,37223,NA,NA,NA,,-97.340553,36.161667,"Orlando site, Noble Co. (Wellington Fm.)",NA,,US,Oklahoma,Noble,stated in text,seconds,,"""about 2 miles northeast of Orlando in Noble County in SE1/4 sec. 31, T. 20 N., R. 1 W."" (Olson, 1967 p. 44); Note: the town of Orlando itself lies in Logan Co., the fossil site, however, lies just across the border in Noble Co. Lat long is based on the map given by Olson (1967 p. 38).",gp_mid,-27.83,0.34,101,US,,Wellington,Sumner,,,,,,,,,NA,"""about 100 feet below the contact of the Wellington and the Garber formations"" Olson (1970 p. 360). The Artinskian age of the Wellington Fm. given here is taken from Mazzullo (1995, in Scholle et al. (eds.) The Permian of Northern Pangaea vol. II)",,claystone,gray,,,,ironstone,concretionary,,sandy,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,rare,,,NA,,"""For the most part, specimens are fragmentary and occur in sandy ironstone nodules. They have been collected from surface concentrations that have formed as the gray shale in which the nodules are formed has weathered. The concentration in the parent bed is so low that attempts to get material by excavating it have had little success."" Olson (1970 p. 360)",taxonomic,"surface (float),survey of museum collection",,,,,,,"""collecting has been almost entirely from the surface"" Olson (1967 p. 45)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Seymouria,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,23/11/2008 06:54,23/11/2008 09:29,28557,baylorensis,Seymouria,28557,,290.1,279.3,Artinskian,,NA,US,Seymouria baylorensis
787464,occ,NA,,79402,,Captorhinus cf. aguti,species,90718,,Captorhinus aguti,NA,species,134887,Olson,1967,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,,-97.340553,36.161667,"Orlando site, Noble Co. (Wellington Fm.)",NA,,US,Oklahoma,Noble,stated in text,seconds,,"""about 2 miles northeast of Orlando in Noble County in SE1/4 sec. 31, T. 20 N., R. 1 W."" (Olson, 1967 p. 44); Note: the town of Orlando itself lies in Logan Co., the fossil site, however, lies just across the border in Noble Co. Lat long is based on the map given by Olson (1967 p. 38).",gp_mid,-27.83,0.34,101,US,,Wellington,Sumner,,,,,,,,,NA,"""about 100 feet below the contact of the Wellington and the Garber formations"" Olson (1970 p. 360). The Artinskian age of the Wellington Fm. given here is taken from Mazzullo (1995, in Scholle et al. (eds.) The Permian of Northern Pangaea vol. II)",,claystone,gray,,,,ironstone,concretionary,,sandy,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,rare,,,NA,,"""For the most part, specimens are fragmentary and occur in sandy ironstone nodules. They have been collected from surface concentrations that have formed as the gray shale in which the nodules are formed has weathered. The concentration in the parent bed is so low that attempts to get material by excavating it have had little success."" Olson (1970 p. 360)",taxonomic,"surface (float),survey of museum collection",,,,,,,"""collecting has been almost entirely from the surface"" Olson (1967 p. 45)",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,23/11/2008 06:56,23/11/2008 09:29,28557,aguti,Captorhinus,28557,cf.,290.1,279.3,Artinskian,,NA,US,Captorhinus aguti
787465,occ,NA,,79402,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Olson,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-97.340553,36.161667,"Orlando site, Noble Co. (Wellington Fm.)",NA,,US,Oklahoma,Noble,stated in text,seconds,,"""about 2 miles northeast of Orlando in Noble County in SE1/4 sec. 31, T. 20 N., R. 1 W."" (Olson, 1967 p. 44); Note: the town of Orlando itself lies in Logan Co., the fossil site, however, lies just across the border in Noble Co. Lat long is based on the map given by Olson (1967 p. 38).",gp_mid,-27.83,0.34,101,US,,Wellington,Sumner,,,,,,,,,NA,"""about 100 feet below the contact of the Wellington and the Garber formations"" Olson (1970 p. 360). The Artinskian age of the Wellington Fm. given here is taken from Mazzullo (1995, in Scholle et al. (eds.) The Permian of Northern Pangaea vol. II)",,claystone,gray,,,,ironstone,concretionary,,sandy,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,rare,,,NA,,"""For the most part, specimens are fragmentary and occur in sandy ironstone nodules. They have been collected from surface concentrations that have formed as the gray shale in which the nodules are formed has weathered. The concentration in the parent bed is so low that attempts to get material by excavating it have had little success."" Olson (1970 p. 360)",taxonomic,"surface (float),survey of museum collection",,,,,,,"""collecting has been almost entirely from the surface"" Olson (1967 p. 45)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,23/11/2008 06:56,23/11/2008 09:29,28557,sp.,Dimetrodon,28557,,290.1,279.3,Artinskian,,NA,US,Dimetrodon sp.
787466,occ,NA,,79402,,Edaphosaurus sp.,genus,38911,,Edaphosaurus,NA,genus,38911,Olson,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,,-97.340553,36.161667,"Orlando site, Noble Co. (Wellington Fm.)",NA,,US,Oklahoma,Noble,stated in text,seconds,,"""about 2 miles northeast of Orlando in Noble County in SE1/4 sec. 31, T. 20 N., R. 1 W."" (Olson, 1967 p. 44); Note: the town of Orlando itself lies in Logan Co., the fossil site, however, lies just across the border in Noble Co. Lat long is based on the map given by Olson (1967 p. 38).",gp_mid,-27.83,0.34,101,US,,Wellington,Sumner,,,,,,,,,NA,"""about 100 feet below the contact of the Wellington and the Garber formations"" Olson (1970 p. 360). The Artinskian age of the Wellington Fm. given here is taken from Mazzullo (1995, in Scholle et al. (eds.) The Permian of Northern Pangaea vol. II)",,claystone,gray,,,,ironstone,concretionary,,sandy,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,rare,,,NA,,"""For the most part, specimens are fragmentary and occur in sandy ironstone nodules. They have been collected from surface concentrations that have formed as the gray shale in which the nodules are formed has weathered. The concentration in the parent bed is so low that attempts to get material by excavating it have had little success."" Olson (1970 p. 360)",taxonomic,"surface (float),survey of museum collection",,,,,,,"""collecting has been almost entirely from the surface"" Olson (1967 p. 45)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,23/11/2008 06:56,23/11/2008 09:29,28557,sp.,Edaphosaurus,28557,,290.1,279.3,Artinskian,,NA,US,Edaphosaurus sp.
787528,occ,NA,,84941,,Trimerorhachis cf. insignis,species,90711,,Trimerorhachis insignis,NA,species,90711,Olson,1970,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-97.433334,36.349998,"Perry site 6, beds 18+19",NA,,US,Oklahoma,Noble,estimated from map,minutes,,"""about nine miles northwest of Perry, Logan County, Oklahoma, SE1/4 SE1/4 sec. 26 T. 23 N, R. 2 W""",gp_mid,-27.41,1.27,101,US,,Wellington,Sumner,,group of beds,,Perry site 6,18+19,bottom to top,,,NA,,"""[...] red sandstone, bed 19 of the section. [...] small lenses that lie just under the red sandstone, in bed 18 of the section. These lenses [...] run from two to five feet in diameter, and are roughly ovoid in shape. The rock is a heterogeneous mixture of sandy shale, shale, sandstone, and masses of mud which are rich in organic remains. [...] The bed below the sandstone, of which these lenses make up the topmost part, is predominantly a dark, red to brown, sandy shale. In its upper part it also carries some lenses of very fine, chocolate colored sandy shale, with very fine sand and some mica.""",sandstone,red,,,Y,"""shale""","lenticular,red or brown",,"silty,sandy",Y,lacustrine indet.,foreland basin,"""These [...] beds [...] appear to have originated in a lake, very near to shore.""",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,common,,,NA,,"""The best preserved occur in the red sandstone, bed 19 of the section. In this bed, however, they are widely scattered. The condition of these bones is excellent; they are essentially unmineralized and uncrushed. Although some moderate concentrations occur in sandstone, there is no evidence that the clustering has any relationship to life associations. [...] By far the greatest concentration of bones occurs in small lenses that lie just under the red sandstone, in bed 18 of the section. [...] Some of these lenses have high concentrations of bones, with the new reptile predominant but with remains of other reptiles, some amphibians, and fish, making up as much as 5 per cent of the total. The matrix appears to have been highly compressible and the con-tained vertebrate remains are always severely crushed. These pockets are much the most prolific source of bones, but the crushing has limited their morphological value.""",taxonomic,field collection,,,,,E. C. Olson,,,"""Tooth plates, listed as Sphaerolepis arcata in Olson (1967), are a common associate of Platysomus and occur rather widely in both beds 18 and 19. It seems quite possible that these actually represent tooth plates of Platysomus.""\r\nBesides the taxa listed, ""indeterminate remains of a small amphibian"" are present.","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,24/11/2008 06:32,25/11/2008 07:39,26635,insignis,Trimerorhachis,26635,cf.,290.1,268,Leonard,,NA,US,Trimerorhachis insignis
787529,occ,NA,,84941,,Ophiacodon sp.,genus,38888,,Ophiacodon,NA,genus,38888,Olson,1970,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-97.433334,36.349998,"Perry site 6, beds 18+19",NA,,US,Oklahoma,Noble,estimated from map,minutes,,"""about nine miles northwest of Perry, Logan County, Oklahoma, SE1/4 SE1/4 sec. 26 T. 23 N, R. 2 W""",gp_mid,-27.41,1.27,101,US,,Wellington,Sumner,,group of beds,,Perry site 6,18+19,bottom to top,,,NA,,"""[...] red sandstone, bed 19 of the section. [...] small lenses that lie just under the red sandstone, in bed 18 of the section. These lenses [...] run from two to five feet in diameter, and are roughly ovoid in shape. The rock is a heterogeneous mixture of sandy shale, shale, sandstone, and masses of mud which are rich in organic remains. [...] The bed below the sandstone, of which these lenses make up the topmost part, is predominantly a dark, red to brown, sandy shale. In its upper part it also carries some lenses of very fine, chocolate colored sandy shale, with very fine sand and some mica.""",sandstone,red,,,Y,"""shale""","lenticular,red or brown",,"silty,sandy",Y,lacustrine indet.,foreland basin,"""These [...] beds [...] appear to have originated in a lake, very near to shore.""",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,common,,,NA,,"""The best preserved occur in the red sandstone, bed 19 of the section. In this bed, however, they are widely scattered. The condition of these bones is excellent; they are essentially unmineralized and uncrushed. Although some moderate concentrations occur in sandstone, there is no evidence that the clustering has any relationship to life associations. [...] By far the greatest concentration of bones occurs in small lenses that lie just under the red sandstone, in bed 18 of the section. [...] Some of these lenses have high concentrations of bones, with the new reptile predominant but with remains of other reptiles, some amphibians, and fish, making up as much as 5 per cent of the total. The matrix appears to have been highly compressible and the con-tained vertebrate remains are always severely crushed. These pockets are much the most prolific source of bones, but the crushing has limited their morphological value.""",taxonomic,field collection,,,,,E. C. Olson,,,"""Tooth plates, listed as Sphaerolepis arcata in Olson (1967), are a common associate of Platysomus and occur rather widely in both beds 18 and 19. It seems quite possible that these actually represent tooth plates of Platysomus.""\r\nBesides the taxa listed, ""indeterminate remains of a small amphibian"" are present.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,24/11/2008 06:32,25/11/2008 07:39,26635,sp.,Ophiacodon,26635,,290.1,268,Leonard,,1,US,Ophiacodon sp.
787530,occ,NA,,84941,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Olson,1970,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-97.433334,36.349998,"Perry site 6, beds 18+19",NA,,US,Oklahoma,Noble,estimated from map,minutes,,"""about nine miles northwest of Perry, Logan County, Oklahoma, SE1/4 SE1/4 sec. 26 T. 23 N, R. 2 W""",gp_mid,-27.41,1.27,101,US,,Wellington,Sumner,,group of beds,,Perry site 6,18+19,bottom to top,,,NA,,"""[...] red sandstone, bed 19 of the section. [...] small lenses that lie just under the red sandstone, in bed 18 of the section. These lenses [...] run from two to five feet in diameter, and are roughly ovoid in shape. The rock is a heterogeneous mixture of sandy shale, shale, sandstone, and masses of mud which are rich in organic remains. [...] The bed below the sandstone, of which these lenses make up the topmost part, is predominantly a dark, red to brown, sandy shale. In its upper part it also carries some lenses of very fine, chocolate colored sandy shale, with very fine sand and some mica.""",sandstone,red,,,Y,"""shale""","lenticular,red or brown",,"silty,sandy",Y,lacustrine indet.,foreland basin,"""These [...] beds [...] appear to have originated in a lake, very near to shore.""",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,common,,,NA,,"""The best preserved occur in the red sandstone, bed 19 of the section. In this bed, however, they are widely scattered. The condition of these bones is excellent; they are essentially unmineralized and uncrushed. Although some moderate concentrations occur in sandstone, there is no evidence that the clustering has any relationship to life associations. [...] By far the greatest concentration of bones occurs in small lenses that lie just under the red sandstone, in bed 18 of the section. [...] Some of these lenses have high concentrations of bones, with the new reptile predominant but with remains of other reptiles, some amphibians, and fish, making up as much as 5 per cent of the total. The matrix appears to have been highly compressible and the con-tained vertebrate remains are always severely crushed. These pockets are much the most prolific source of bones, but the crushing has limited their morphological value.""",taxonomic,field collection,,,,,E. C. Olson,,,"""Tooth plates, listed as Sphaerolepis arcata in Olson (1967), are a common associate of Platysomus and occur rather widely in both beds 18 and 19. It seems quite possible that these actually represent tooth plates of Platysomus.""\r\nBesides the taxa listed, ""indeterminate remains of a small amphibian"" are present.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,24/11/2008 06:33,25/11/2008 07:39,26635,sp.,Dimetrodon,26635,,290.1,268,Leonard,,NA,US,Dimetrodon sp.
787560,occ,NA,,79815,,Archeria n. sp. victori,species,136663,,Archeria victori,NA,species,136663,Olson,1967,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,individuals,-97.417778,36.738609,McCann Quarry,NA,"""McCaren quarry""; Nardin site, Eddy site, OMNH locality V128",US,Oklahoma,Kay,stated in text,seconds,outcrop,"""3 km northeast of Eddy, Kay Co., OK"" (Heaton & Reisz, 1986);\r\n""The Quarry is on Deer Creek, 8 Miles west and 4 Miles south of Blackwell [...] in NE1/4 sec. 16 and SW1/4 sec. 9, T. 26 N., R. 2 W."" (Olson, 1967)\r\nLat long is for intersection of lines dividing secs. 9 and 16 and eastern and western half of both secs.",gp_mid,-27.2,1.6,101,US,,Wellington,Sumner,McCann Sandstone,member,,,,,,,NA,,,sandstone,"""cross stratification"",coarse,red or brown",,,Y,sandstone,"planar lamination,gray,yellow",,,Y,fluvial-deltaic indet.,foreland basin,"""predominantly nearshore [...], in part marine"" (Olson, 1967)",macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,"""Vertebrate remains occur in all phases of the sandstone, mostly as small fragments.""",taxonomic,"field collection,survey of museum collection,observed (not collected)",,,,,,,,"""Along with the bone fragments are abundant conchostracans, called Estheria by Gould (1900). Few remains of plants have been found."" Olson (1967)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,24/11/2008 10:25,11/03/2010 10:51,28557,victori,Archeria,28557,n. sp.,290.1,268,Leonard,,1,US,Archeria victori
787561,occ,NA,,79815,,Trimerorhachis insignis,species,90711,,Trimerorhachis insignis,NA,species,90711,Olson,1967,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,specimens,-97.417778,36.738609,McCann Quarry,NA,"""McCaren quarry""; Nardin site, Eddy site, OMNH locality V128",US,Oklahoma,Kay,stated in text,seconds,outcrop,"""3 km northeast of Eddy, Kay Co., OK"" (Heaton & Reisz, 1986);\r\n""The Quarry is on Deer Creek, 8 Miles west and 4 Miles south of Blackwell [...] in NE1/4 sec. 16 and SW1/4 sec. 9, T. 26 N., R. 2 W."" (Olson, 1967)\r\nLat long is for intersection of lines dividing secs. 9 and 16 and eastern and western half of both secs.",gp_mid,-27.2,1.6,101,US,,Wellington,Sumner,McCann Sandstone,member,,,,,,,NA,,,sandstone,"""cross stratification"",coarse,red or brown",,,Y,sandstone,"planar lamination,gray,yellow",,,Y,fluvial-deltaic indet.,foreland basin,"""predominantly nearshore [...], in part marine"" (Olson, 1967)",macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,"""Vertebrate remains occur in all phases of the sandstone, mostly as small fragments.""",taxonomic,"field collection,survey of museum collection,observed (not collected)",,,,,,,,"""Along with the bone fragments are abundant conchostracans, called Estheria by Gould (1900). Few remains of plants have been found."" Olson (1967)","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,24/11/2008 10:25,11/03/2010 10:51,28557,insignis,Trimerorhachis,28557,,290.1,268,Leonard,,9,US,Trimerorhachis insignis
787562,occ,NA,,79815,,Eryops cf. megacephalus,species,70397,,Eryops megacephalus,NA,species,70397,Olson,1967,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,individuals,-97.417778,36.738609,McCann Quarry,NA,"""McCaren quarry""; Nardin site, Eddy site, OMNH locality V128",US,Oklahoma,Kay,stated in text,seconds,outcrop,"""3 km northeast of Eddy, Kay Co., OK"" (Heaton & Reisz, 1986);\r\n""The Quarry is on Deer Creek, 8 Miles west and 4 Miles south of Blackwell [...] in NE1/4 sec. 16 and SW1/4 sec. 9, T. 26 N., R. 2 W."" (Olson, 1967)\r\nLat long is for intersection of lines dividing secs. 9 and 16 and eastern and western half of both secs.",gp_mid,-27.2,1.6,101,US,,Wellington,Sumner,McCann Sandstone,member,,,,,,,NA,,,sandstone,"""cross stratification"",coarse,red or brown",,,Y,sandstone,"planar lamination,gray,yellow",,,Y,fluvial-deltaic indet.,foreland basin,"""predominantly nearshore [...], in part marine"" (Olson, 1967)",macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,"""Vertebrate remains occur in all phases of the sandstone, mostly as small fragments.""",taxonomic,"field collection,survey of museum collection,observed (not collected)",,,,,,,,"""Along with the bone fragments are abundant conchostracans, called Estheria by Gould (1900). Few remains of plants have been found."" Olson (1967)","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,24/11/2008 10:25,22/08/2016 10:35,28557,megacephalus,Eryops,28557,cf.,290.1,268,Leonard,,1,US,Eryops megacephalus
787563,occ,NA,,79815,,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Olson,1967,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,individuals,-97.417778,36.738609,McCann Quarry,NA,"""McCaren quarry""; Nardin site, Eddy site, OMNH locality V128",US,Oklahoma,Kay,stated in text,seconds,outcrop,"""3 km northeast of Eddy, Kay Co., OK"" (Heaton & Reisz, 1986);\r\n""The Quarry is on Deer Creek, 8 Miles west and 4 Miles south of Blackwell [...] in NE1/4 sec. 16 and SW1/4 sec. 9, T. 26 N., R. 2 W."" (Olson, 1967)\r\nLat long is for intersection of lines dividing secs. 9 and 16 and eastern and western half of both secs.",gp_mid,-27.2,1.6,101,US,,Wellington,Sumner,McCann Sandstone,member,,,,,,,NA,,,sandstone,"""cross stratification"",coarse,red or brown",,,Y,sandstone,"planar lamination,gray,yellow",,,Y,fluvial-deltaic indet.,foreland basin,"""predominantly nearshore [...], in part marine"" (Olson, 1967)",macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,"""Vertebrate remains occur in all phases of the sandstone, mostly as small fragments.""",taxonomic,"field collection,survey of museum collection,observed (not collected)",,,,,,,,"""Along with the bone fragments are abundant conchostracans, called Estheria by Gould (1900). Few remains of plants have been found."" Olson (1967)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,24/11/2008 10:25,11/03/2010 10:51,28557,sp.,Diplocaulus,28557,,290.1,268,Leonard,,1,US,Diplocaulus sp.
787564,occ,NA,,79815,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Olson,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-97.417778,36.738609,McCann Quarry,NA,"""McCaren quarry""; Nardin site, Eddy site, OMNH locality V128",US,Oklahoma,Kay,stated in text,seconds,outcrop,"""3 km northeast of Eddy, Kay Co., OK"" (Heaton & Reisz, 1986);\r\n""The Quarry is on Deer Creek, 8 Miles west and 4 Miles south of Blackwell [...] in NE1/4 sec. 16 and SW1/4 sec. 9, T. 26 N., R. 2 W."" (Olson, 1967)\r\nLat long is for intersection of lines dividing secs. 9 and 16 and eastern and western half of both secs.",gp_mid,-27.2,1.6,101,US,,Wellington,Sumner,McCann Sandstone,member,,,,,,,NA,,,sandstone,"""cross stratification"",coarse,red or brown",,,Y,sandstone,"planar lamination,gray,yellow",,,Y,fluvial-deltaic indet.,foreland basin,"""predominantly nearshore [...], in part marine"" (Olson, 1967)",macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,"""Vertebrate remains occur in all phases of the sandstone, mostly as small fragments.""",taxonomic,"field collection,survey of museum collection,observed (not collected)",,,,,,,,"""Along with the bone fragments are abundant conchostracans, called Estheria by Gould (1900). Few remains of plants have been found."" Olson (1967)",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,24/11/2008 10:25,11/03/2010 10:51,28557,sp.,Dimetrodon,28557,,290.1,268,Leonard,,5,US,Dimetrodon sp.
787565,occ,NA,,79815,,Edaphosaurus sp.,genus,38911,,Edaphosaurus,NA,genus,38911,Olson,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,elements,-97.417778,36.738609,McCann Quarry,NA,"""McCaren quarry""; Nardin site, Eddy site, OMNH locality V128",US,Oklahoma,Kay,stated in text,seconds,outcrop,"""3 km northeast of Eddy, Kay Co., OK"" (Heaton & Reisz, 1986);\r\n""The Quarry is on Deer Creek, 8 Miles west and 4 Miles south of Blackwell [...] in NE1/4 sec. 16 and SW1/4 sec. 9, T. 26 N., R. 2 W."" (Olson, 1967)\r\nLat long is for intersection of lines dividing secs. 9 and 16 and eastern and western half of both secs.",gp_mid,-27.2,1.6,101,US,,Wellington,Sumner,McCann Sandstone,member,,,,,,,NA,,,sandstone,"""cross stratification"",coarse,red or brown",,,Y,sandstone,"planar lamination,gray,yellow",,,Y,fluvial-deltaic indet.,foreland basin,"""predominantly nearshore [...], in part marine"" (Olson, 1967)",macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,"""Vertebrate remains occur in all phases of the sandstone, mostly as small fragments.""",taxonomic,"field collection,survey of museum collection,observed (not collected)",,,,,,,,"""Along with the bone fragments are abundant conchostracans, called Estheria by Gould (1900). Few remains of plants have been found."" Olson (1967)",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,24/11/2008 10:25,11/03/2010 10:51,28557,sp.,Edaphosaurus,28557,,290.1,268,Leonard,,3,US,Edaphosaurus sp.
787580,occ,NA,,79815,,Eryops megacephalus,species,70397,,Eryops megacephalus,NA,species,70397,Olson,1967,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,-97.417778,36.738609,McCann Quarry,NA,"""McCaren quarry""; Nardin site, Eddy site, OMNH locality V128",US,Oklahoma,Kay,stated in text,seconds,outcrop,"""3 km northeast of Eddy, Kay Co., OK"" (Heaton & Reisz, 1986);\r\n""The Quarry is on Deer Creek, 8 Miles west and 4 Miles south of Blackwell [...] in NE1/4 sec. 16 and SW1/4 sec. 9, T. 26 N., R. 2 W."" (Olson, 1967)\r\nLat long is for intersection of lines dividing secs. 9 and 16 and eastern and western half of both secs.",gp_mid,-27.2,1.6,101,US,,Wellington,Sumner,McCann Sandstone,member,,,,,,,NA,,,sandstone,"""cross stratification"",coarse,red or brown",,,Y,sandstone,"planar lamination,gray,yellow",,,Y,fluvial-deltaic indet.,foreland basin,"""predominantly nearshore [...], in part marine"" (Olson, 1967)",macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,"""Vertebrate remains occur in all phases of the sandstone, mostly as small fragments.""",taxonomic,"field collection,survey of museum collection,observed (not collected)",,,,,,,,"""Along with the bone fragments are abundant conchostracans, called Estheria by Gould (1900). Few remains of plants have been found."" Olson (1967)","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,24/11/2008 11:01,11/03/2010 10:51,28557,megacephalus,Eryops,28557,,290.1,268,Leonard,,9,US,Eryops megacephalus
787989,occ,NA,,85112,,Protocaptorhinus pricei,species,135429,,Protocaptorhinus pricei,NA,species,135429,Clark and Carroll,1973,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37505,NA,NA,NA,individuals,-98.933334,33.566666,Woodrum's (Belle Plains Fm.),NA,,US,Texas,Archer,estimated from map,seconds,outcrop,"""NW of Woodrum's"", Archer County, Texas. Lat long is estimated from map on p. 397 in Clark & Carroll (1973).",gp_mid,-30.3,-1.19,101,US,,Petrolia,Wichita,,,,,,,,,NA,"Petrolia Fm. is formerly known as Belle Plains Fm. (see Hentz, 1988, The University of Texas at Austin Bureau of Economic Geology, Report of Investigations, 170, pp. 1-55)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Protocaptorhinus,,NA,NA,vertebrate,J. Clark and R. L. Carroll. 1973. Romeriid Reptiles from the Lower Permian. Bulletin of the Museum of Comparative Zoology 144(5):353-407,315,334,0,J. Mueller,T. Liebrecht,,28/11/2008 17:19,28/11/2008 19:19,28415,pricei,Protocaptorhinus,28415,,290.1,279.3,Artinskian,,1,US,Protocaptorhinus pricei
787990,occ,NA,,80741,,Trimerorhachis insignis,species,90711,,Trimerorhachis insignis,NA,species,90711,Pawley,2007,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,individuals,-98.966667,33.666668,Trematops locality (Belle Plains Fm.),NA,west of Williams Ranch,US,Texas,Baylor,stated in text,minutes,outcrop,"""west of Williams Ranch, J. Gibbs Survey A-566, southeast of Fulda,\r\nBaylor County, Texas"" (Clark & Carroll, 1973)\r\n""West of Williams, Baylor County"" (Pawley, 2007 Appendix [http://www.journalofpaleontology.org/Archives/Volume_81/81(5)/Pawley/Appendix.doc]",gp_mid,-30.27,-1.09,101,US,,Petrolia,Wichita,,,,,,,,,NA,"Petrolia Fm. is formerly known as Belle Plains Fm. (see Hentz, 1988, The University of Texas at Austin Bureau of Economic Geology, Report of Investigations, 170, pp. 1-55)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,,Further specimens probably coming from this site may be included in collections (22669) and (22668).,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,"K. Pawley. 2007. The Postcranial Skeleton of Trimerorhachis insignis Cope, 1878 (Temnospondyli: Trimerorhachidae): A Plesiomorphic Temnospondyl from the Lower Permian of North America. Journal of Paleontology 81(5):873-894",315,334,0,J. Mueller,T. Liebrecht,,28/11/2008 19:21,28/11/2008 21:21,28415,insignis,Trimerorhachis,28611,,290.1,279.3,Artinskian,,1,US,Trimerorhachis insignis
787992,occ,NA,,28250,,Pariotichus n. sp. laticeps,species,120324,recombined as,Captorhinus laticeps,NA,species,120324,Heaton,1979,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-99.091667,33.733334,"Mitchell Creek, 29 (Waggoner Ranch Formation)",NA,"Locality 29 (Romer 1928), old Bar X pasture, Timber Creek, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Lucas Ranch",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near Mitchell and Timber Creeks, northeast of Maybelle in the old Bar X pasture."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"". Numbered ""29"" with taxonomic list and on map, but is incorrectly numbered ""28"" in text. Lat long is for area enclosed by Mitchell Creek (W), Big Wichita River (N), Timber Creek (E), and U.S. 277 (S).",gp_mid,-30.29,-0.93,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""It is about 150 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Pariotichus,,NA,NA,vertebrate,"M. J. Heaton. 1979. Cranial Anatomy of Primitive Captorhinid Reptiles from the Late Pennsylvanian and Early Permian, Oklahoma and Texas. Oklahoma Geological Survey, Bulletin 127:1-83",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,28/11/2008 20:09,11/06/2009 05:56,7693,laticeps,Captorhinus,28362,n. sp.,290.1,272.3,Artinskian,Kungurian,1,US,Captorhinus laticeps
787993,occ,NA,,28250,,n. gen. Mycterosaurus n. sp. longiceps,species,122319,,Mycterosaurus longiceps,NA,species,122319,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,38895,NA,NA,NA,individuals,-99.091667,33.733334,"Mitchell Creek, 29 (Waggoner Ranch Formation)",NA,"Locality 29 (Romer 1928), old Bar X pasture, Timber Creek, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Lucas Ranch",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near Mitchell and Timber Creeks, northeast of Maybelle in the old Bar X pasture."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"". Numbered ""29"" with taxonomic list and on map, but is incorrectly numbered ""28"" in text. Lat long is for area enclosed by Mitchell Creek (W), Big Wichita River (N), Timber Creek (E), and U.S. 277 (S).",gp_mid,-30.29,-0.93,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""It is about 150 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Mycterosaurus,n. gen.,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,28/11/2008 20:24,11/06/2009 06:10,7693,longiceps,Mycterosaurus,5692,n. sp.,290.1,272.3,Artinskian,Kungurian,2,US,Mycterosaurus longiceps
787996,occ,NA,R,79813,,"""Captorhinus"" laticeps",species,134970,,Captorhinus laticeps,NA,species,120324,Clark and Carroll,1973,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-98.966667,34.008331,Weiss Locality (Waggoner Ranch Fm.),NA,Red Pasture Line House,US,Texas,Wilbarger,estimated from map,seconds,hand sample,"""sec. 7, block 5, H. and T.C.R.R., Willbarger County, Texas"". Lat long is estimated from map on p. 397 in Clark & Carroll (1973).",gp_mid,-29.69,-0.09,101,US,,Waggoner Ranch,Wichita,,bed,,,,,,,NA,"Waggoner Ranch Fm. is formerly known as Clyde Fm. (see Hentz, 1988, The University of Texas at Austin Bureau of Economic Geology, Report of Investigations, 170, pp. 1-55)","""very hard clay matrix"" (Heaton, 1979)",claystone,,lithified,,Y,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,"body,replaced with silica",,,,,,,,,,NA,,"""bone replaced by silica(?); some crushing of back of skull."" (Heaton, 1979).",taxonomic,survey of museum collection,MCZ,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,"""",NA,NA,vertebrate,J. Clark and R. L. Carroll. 1973. Romeriid Reptiles from the Lower Permian. Bulletin of the Museum of Comparative Zoology 144(5):353-407,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,28/11/2008 21:37,28/11/2008 23:39,28415,laticeps,Captorhinus,28415,,290.1,268,Leonard,,1,US,Captorhinus laticeps
787996,occ,21175,,79813,,Eocaptorhinus laticeps,species,134878,recombined as,Captorhinus laticeps,NA,species,120324,Heaton,1979,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-98.966667,34.008331,Weiss Locality (Waggoner Ranch Fm.),NA,Red Pasture Line House,US,Texas,Wilbarger,estimated from map,seconds,hand sample,"""sec. 7, block 5, H. and T.C.R.R., Willbarger County, Texas"". Lat long is estimated from map on p. 397 in Clark & Carroll (1973).",gp_mid,-29.69,-0.09,101,US,,Waggoner Ranch,Wichita,,bed,,,,,,,NA,"Waggoner Ranch Fm. is formerly known as Clyde Fm. (see Hentz, 1988, The University of Texas at Austin Bureau of Economic Geology, Report of Investigations, 170, pp. 1-55)","""very hard clay matrix"" (Heaton, 1979)",claystone,,lithified,,Y,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,"body,replaced with silica",,,,,,,,,,NA,,"""bone replaced by silica(?); some crushing of back of skull."" (Heaton, 1979).",taxonomic,survey of museum collection,MCZ,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Eocaptorhinus,,NA,NA,vertebrate,"M. J. Heaton. 1979. Cranial Anatomy of Primitive Captorhinid Reptiles from the Late Pennsylvanian and Early Permian, Oklahoma and Texas. Oklahoma Geological Survey, Bulletin 127:1-83",315,334,0,J. Mueller,T. Liebrecht,,11/12/2008 18:45,11/12/2008 20:45,28415,laticeps,Captorhinus,28362,,290.1,268,Leonard,,1,US,Captorhinus laticeps
788094,occ,NA,,67862,,n. gen. Basicranodon n. sp. fortsillensis,species,122320,subjective synonym of,Mycterosaurus longiceps,NA,species,122319,Olson,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,38895,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Basicranodon,n. gen.,NA,NA,"paleoentomology,vertebrate",E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,30/11/2008 09:27,25/03/2010 11:34,19393,fortsillensis,Mycterosaurus,28557,n. sp.,290.1,268,Leonard,,1,US,Mycterosaurus fortsillensis
788095,occ,NA,,80691,,Captorhinus sp.,genus,37497,,Captorhinus,NA,genus,37497,Olson,1967,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,,-98.64167,34.968056,South Carnegie Site,NA,"Roosevelt Company Quarry, Bally Mountain Locality, Bally Mountain Quarry",US,Oklahoma,Kiowa,estimated from map,seconds,small collection,"Olson (1967:36) originally describes the site as abandoned quarry of the Roosevelt Materials Company Carnegie plant; 11.2 miles south of the center of Carnegie, Caddo County, [...] NE 1/4 sec. 6, T. 5 N., R. 13 W. (Alden 7,5' quadrangle).\r\nLeBlanc et al. (2015) report captorhinid fossils from fissure fills in an abandoned limestone quarry on Bally Mountain in Kiowa County. They refer it to as Bally Mountain locality, but say that it is the same locality as Olsons South Carnegie site. Bally Mountain, however, is located 6 km WNW from the PLSS coordinates cited by Olson (1967). Bridges (1985:63, MSc thesis, Oklahoma State University) already has noted that Olsons description is wrong and gave the PLSS coordinates NE 1/4 sec. 26, T. 6 N., R. 14 W. (Bally Mountain 7,5' quadrangle) for the South Carnegie site. Although this is still about 2 km NE from the ridge that is labelled Bally Mountain on the maps, the originally entered DMS coordinates (3457'19"" N 9836'55"" W) are changed according to the PLSS coordinates given by Bridges (1985).",gp_mid,-28.96,0.59,101,US,,,,,,,,,,,,NA,"As far as can be determined, the deposits were formed in the same way and at the same time as were those at Richards Spur” (Olson, 1967; see collection 67862).","clay and conglomerates, much as at Richards Spur (Olson, 1967; see collection 67862)",claystone,,,,,conglomerate,,,,,fissure fill,non-subsiding area,,macrofossils,none,,"maxillae,mandibles",,,NA,,body,variable,,,concentrate,,,common,,frequent,NA,,"Olson (1967) states that preservation, however, is poor and only rather badly broken specimens have been found. [...] the prospects for finding significant amounts are poor, but subsequent collecting has brought many speciemens to light that are quite good preserved and determinable on species level (cf. LeBlanc et al., 2015).",taxonomic,field collection,"FMNH,ROM",,,,"E. C. Olson (FMNH), W. May (OMNH, ROM)",,OMNH = Sam Noble Oklahoma Museum of Natural History,"Simpson (1979; Oklahoma Geol. Notes 39(1)) in his table 1 (p. 7) lists the pelycosaur Basicranodon fortsilensis (sic) as the only known taxon from South Carnegie but in the text (p. 5) also mentions a large number of specimens of Captorhinus aguti from this site. LeBlanc et al. (2015) mention synapsids to be present but do not give a specific subtaxon. They, however, explicitly mention the anamniote Doleserpeton with regard to the similarity of the faunal composition of the Bally Mountain and Richards Spur localities. Since Doleserpeton is very abundant at Richards Spur and Olson (1967) says that the (then unnamed) amphibian taxa from South Carnegie and Richards Spur are the same, the Olson-based. taxon Amphibia indet. is re-identified as Doleserpeton sp..",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,30/11/2008 10:17,23/12/2016 07:12,28557,sp.,Captorhinus,28557,,290.1,268,Leonard,,NA,US,Captorhinus sp.
788096,occ,NA,R,80691,,Amphibia sp.,genus,36319,,Amphibia,NA,unranked clade,36319,Olson,1967,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,,-98.64167,34.968056,South Carnegie Site,NA,"Roosevelt Company Quarry, Bally Mountain Locality, Bally Mountain Quarry",US,Oklahoma,Kiowa,estimated from map,seconds,small collection,"Olson (1967:36) originally describes the site as abandoned quarry of the Roosevelt Materials Company Carnegie plant; 11.2 miles south of the center of Carnegie, Caddo County, [...] NE 1/4 sec. 6, T. 5 N., R. 13 W. (Alden 7,5' quadrangle).\r\nLeBlanc et al. (2015) report captorhinid fossils from fissure fills in an abandoned limestone quarry on Bally Mountain in Kiowa County. They refer it to as Bally Mountain locality, but say that it is the same locality as Olsons South Carnegie site. Bally Mountain, however, is located 6 km WNW from the PLSS coordinates cited by Olson (1967). Bridges (1985:63, MSc thesis, Oklahoma State University) already has noted that Olsons description is wrong and gave the PLSS coordinates NE 1/4 sec. 26, T. 6 N., R. 14 W. (Bally Mountain 7,5' quadrangle) for the South Carnegie site. Although this is still about 2 km NE from the ridge that is labelled Bally Mountain on the maps, the originally entered DMS coordinates (3457'19"" N 9836'55"" W) are changed according to the PLSS coordinates given by Bridges (1985).",gp_mid,-28.96,0.59,101,US,,,,,,,,,,,,NA,"As far as can be determined, the deposits were formed in the same way and at the same time as were those at Richards Spur” (Olson, 1967; see collection 67862).","clay and conglomerates, much as at Richards Spur (Olson, 1967; see collection 67862)",claystone,,,,,conglomerate,,,,,fissure fill,non-subsiding area,,macrofossils,none,,"maxillae,mandibles",,,NA,,body,variable,,,concentrate,,,common,,frequent,NA,,"Olson (1967) states that preservation, however, is poor and only rather badly broken specimens have been found. [...] the prospects for finding significant amounts are poor, but subsequent collecting has brought many speciemens to light that are quite good preserved and determinable on species level (cf. LeBlanc et al., 2015).",taxonomic,field collection,"FMNH,ROM",,,,"E. C. Olson (FMNH), W. May (OMNH, ROM)",,OMNH = Sam Noble Oklahoma Museum of Natural History,"Simpson (1979; Oklahoma Geol. Notes 39(1)) in his table 1 (p. 7) lists the pelycosaur Basicranodon fortsilensis (sic) as the only known taxon from South Carnegie but in the text (p. 5) also mentions a large number of specimens of Captorhinus aguti from this site. LeBlanc et al. (2015) mention synapsids to be present but do not give a specific subtaxon. They, however, explicitly mention the anamniote Doleserpeton with regard to the similarity of the faunal composition of the Bally Mountain and Richards Spur localities. Since Doleserpeton is very abundant at Richards Spur and Olson (1967) says that the (then unnamed) amphibian taxa from South Carnegie and Richards Spur are the same, the Olson-based. taxon Amphibia indet. is re-identified as Doleserpeton sp..","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Amphibia,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,30/11/2008 10:17,23/12/2016 11:01,28557,sp.,,28557,,290.1,268,Leonard,,NA,US, sp.
788096,occ,33006,,80691,,Doleserpeton sp.,genus,37046,,Doleserpeton,NA,genus,37046,LeBlanc et al.,2015,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,37046,NA,NA,NA,,-98.64167,34.968056,South Carnegie Site,NA,"Roosevelt Company Quarry, Bally Mountain Locality, Bally Mountain Quarry",US,Oklahoma,Kiowa,estimated from map,seconds,small collection,"Olson (1967:36) originally describes the site as abandoned quarry of the Roosevelt Materials Company Carnegie plant; 11.2 miles south of the center of Carnegie, Caddo County, [...] NE 1/4 sec. 6, T. 5 N., R. 13 W. (Alden 7,5' quadrangle).\r\nLeBlanc et al. (2015) report captorhinid fossils from fissure fills in an abandoned limestone quarry on Bally Mountain in Kiowa County. They refer it to as Bally Mountain locality, but say that it is the same locality as Olsons South Carnegie site. Bally Mountain, however, is located 6 km WNW from the PLSS coordinates cited by Olson (1967). Bridges (1985:63, MSc thesis, Oklahoma State University) already has noted that Olsons description is wrong and gave the PLSS coordinates NE 1/4 sec. 26, T. 6 N., R. 14 W. (Bally Mountain 7,5' quadrangle) for the South Carnegie site. Although this is still about 2 km NE from the ridge that is labelled Bally Mountain on the maps, the originally entered DMS coordinates (3457'19"" N 9836'55"" W) are changed according to the PLSS coordinates given by Bridges (1985).",gp_mid,-28.96,0.59,101,US,,,,,,,,,,,,NA,"As far as can be determined, the deposits were formed in the same way and at the same time as were those at Richards Spur” (Olson, 1967; see collection 67862).","clay and conglomerates, much as at Richards Spur (Olson, 1967; see collection 67862)",claystone,,,,,conglomerate,,,,,fissure fill,non-subsiding area,,macrofossils,none,,"maxillae,mandibles",,,NA,,body,variable,,,concentrate,,,common,,frequent,NA,,"Olson (1967) states that preservation, however, is poor and only rather badly broken specimens have been found. [...] the prospects for finding significant amounts are poor, but subsequent collecting has brought many speciemens to light that are quite good preserved and determinable on species level (cf. LeBlanc et al., 2015).",taxonomic,field collection,"FMNH,ROM",,,,"E. C. Olson (FMNH), W. May (OMNH, ROM)",,OMNH = Sam Noble Oklahoma Museum of Natural History,"Simpson (1979; Oklahoma Geol. Notes 39(1)) in his table 1 (p. 7) lists the pelycosaur Basicranodon fortsilensis (sic) as the only known taxon from South Carnegie but in the text (p. 5) also mentions a large number of specimens of Captorhinus aguti from this site. LeBlanc et al. (2015) mention synapsids to be present but do not give a specific subtaxon. They, however, explicitly mention the anamniote Doleserpeton with regard to the similarity of the faunal composition of the Bally Mountain and Richards Spur localities. Since Doleserpeton is very abundant at Richards Spur and Olson (1967) says that the (then unnamed) amphibian taxa from South Carnegie and Richards Spur are the same, the Olson-based. taxon Amphibia indet. is re-identified as Doleserpeton sp..","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Doleserpeton,,NA,NA,vertebrate,"A. R. H. LeBlanc, A. K. Brar, and W. May, R. R. Reisz. 2015. Multiple tooth-rowed captorhinids from the early Permian fissure fills of the Bally Mountain Locality of Oklahoma. Vertebrate Anatomy Morphology Palaeontology 1:35-49",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,23/12/2016 07:23,23/12/2016 10:56,28557,sp.,Doleserpeton,61256,,290.1,268,Leonard,,NA,US,Doleserpeton sp.
788176,occ,NA,,85125,,Labidosaurikos barkeri,species,119514,subjective synonym of,Labidosaurikos meachami,NA,species,119515,Olson,1954,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37500,NA,NA,NA,individuals,-99.371666,33.760277,Fish Creek,NA,,US,Texas,Baylor,estimated from map,seconds,outcrop,"""Fish Creek, Baylor County, Texas"" no further locality descriptions are given.",gp_mid,-29.04,1.83,101,US,,Vale,Clear Fork,,formation,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurikos,,NA,NA,vertebrate,E. C. Olson. 1954. Fauna of the Vale and Choza: 9. Captorhinomorpha. Fieldiana: Geology 10(19):211-218,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 08:41,15/12/2008 07:04,26907,barkeri,Labidosaurikos,26907,,279.3,272.3,Kungurian,,2,US,Labidosaurikos barkeri
788177,occ,NA,,79600,,Rothia multidonta,species,119703,recombined as,Rothianiscus multidonta,NA,species,119703,Olson,1962,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37507,NA,NA,NA,individuals,-99.938332,33.66,Locality KAC (Lower Flowerpot Shale),NA,"Kahn Quarry, Driver Ranch",US,Texas,Knox,estimated from map,seconds,small collection,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork."" For details see map on p. 98 in Olson (1962).",gp_mid,-28.81,3.3,101,US,,San Angelo,Pease River,Flowerpot Shale,member,,,,,,,NA,"The upper San Angelo Fm. of Olson (1962) is widely identical to the lower part of the Flowerpot Shale Member of the upper San Angelo Fm. (sensu Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 114 ff.),claystone,"gypsiferous,green,red or brown",,,Y,sandstone,red or brown,,conglomeratic,Y,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,E. C. Olson,1958,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Rothia,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 09:54,26/07/2009 08:56,26846,multidonta,Rothianiscus,26846,,279.3,268.8,Kungurian,Roadian,2,US,Rothianiscus multidonta
788179,occ,NA,,79600,,n. gen. Slaugenhopia n. sp. texensis,species,349879,,Slaugenhopia texensis,NA,species,349879,Olson,1962,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Tupilakosauridae,150320,36990,NA,NA,NA,individuals,-99.938332,33.66,Locality KAC (Lower Flowerpot Shale),NA,"Kahn Quarry, Driver Ranch",US,Texas,Knox,estimated from map,seconds,small collection,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork."" For details see map on p. 98 in Olson (1962).",gp_mid,-28.81,3.3,101,US,,San Angelo,Pease River,Flowerpot Shale,member,,,,,,,NA,"The upper San Angelo Fm. of Olson (1962) is widely identical to the lower part of the Flowerpot Shale Member of the upper San Angelo Fm. (sensu Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 114 ff.),claystone,"gypsiferous,green,red or brown",,,Y,sandstone,red or brown,,conglomeratic,Y,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,E. C. Olson,1958,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Slaugenhopia,n. gen.,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 09:54,26/07/2009 08:56,26846,texensis,Slaugenhopia,26846,n. sp.,279.3,268.8,Kungurian,Roadian,1,US,Slaugenhopia texensis
788180,occ,NA,,79600,,Cotylorhynchus hancocki,species,122303,,Cotylorhynchus hancocki,NA,species,122303,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38917,NA,NA,NA,individuals,-99.938332,33.66,Locality KAC (Lower Flowerpot Shale),NA,"Kahn Quarry, Driver Ranch",US,Texas,Knox,estimated from map,seconds,small collection,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork."" For details see map on p. 98 in Olson (1962).",gp_mid,-28.81,3.3,101,US,,San Angelo,Pease River,Flowerpot Shale,member,,,,,,,NA,"The upper San Angelo Fm. of Olson (1962) is widely identical to the lower part of the Flowerpot Shale Member of the upper San Angelo Fm. (sensu Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 114 ff.),claystone,"gypsiferous,green,red or brown",,,Y,sandstone,red or brown,,conglomeratic,Y,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,E. C. Olson,1958,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cotylorhynchus,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 09:54,26/07/2009 08:56,26846,hancocki,Cotylorhynchus,26846,,279.3,268.8,Kungurian,Roadian,15,US,Cotylorhynchus hancocki
788181,occ,NA,,79600,,n. gen. Eosyodon n. sp. hudsoni,species,150424,,Eosyodon hudsoni,NA,species,150424,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Brithopodidae,38951,38961,NA,NA,NA,individuals,-99.938332,33.66,Locality KAC (Lower Flowerpot Shale),NA,"Kahn Quarry, Driver Ranch",US,Texas,Knox,estimated from map,seconds,small collection,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork."" For details see map on p. 98 in Olson (1962).",gp_mid,-28.81,3.3,101,US,,San Angelo,Pease River,Flowerpot Shale,member,,,,,,,NA,"The upper San Angelo Fm. of Olson (1962) is widely identical to the lower part of the Flowerpot Shale Member of the upper San Angelo Fm. (sensu Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 114 ff.),claystone,"gypsiferous,green,red or brown",,,Y,sandstone,red or brown,,conglomeratic,Y,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,E. C. Olson,1958,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Eosyodon,n. gen.,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 09:54,26/07/2009 09:03,26846,hudsoni,Eosyodon,26846,n. sp.,279.3,268.8,Kungurian,Roadian,3,US,Eosyodon hudsoni
788182,occ,NA,,79600,,n. gen. Gorgodon n. sp. minutus,species,142568,,Gorgodon minutus,NA,species,142568,Olson,1962,Chordata,33815,Osteichthyes,34881,Theriodontia,56648,Phthinosuchidae,38942,38945,NA,NA,NA,individuals,-99.938332,33.66,Locality KAC (Lower Flowerpot Shale),NA,"Kahn Quarry, Driver Ranch",US,Texas,Knox,estimated from map,seconds,small collection,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork."" For details see map on p. 98 in Olson (1962).",gp_mid,-28.81,3.3,101,US,,San Angelo,Pease River,Flowerpot Shale,member,,,,,,,NA,"The upper San Angelo Fm. of Olson (1962) is widely identical to the lower part of the Flowerpot Shale Member of the upper San Angelo Fm. (sensu Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 114 ff.),claystone,"gypsiferous,green,red or brown",,,Y,sandstone,red or brown,,conglomeratic,Y,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,E. C. Olson,1958,,,terrestrial,NA,actively mobile,,NA,carnivore,,,hydroxyapatite,,NA,,Gorgodon,n. gen.,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 09:54,26/07/2009 08:56,26846,minutus,Gorgodon,26846,n. sp.,279.3,268.8,Kungurian,Roadian,2,US,Gorgodon minutus
788183,occ,NA,,79600,,Phthinosuchidae sp.,genus,38942,,Phthinosuchidae,NA,family,38942,Olson,1962,Chordata,33815,Osteichthyes,34881,Theriodontia,56648,Phthinosuchidae,38942,NA,NA,NA,NA,individuals,-99.938332,33.66,Locality KAC (Lower Flowerpot Shale),NA,"Kahn Quarry, Driver Ranch",US,Texas,Knox,estimated from map,seconds,small collection,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork."" For details see map on p. 98 in Olson (1962).",gp_mid,-28.81,3.3,101,US,,San Angelo,Pease River,Flowerpot Shale,member,,,,,,,NA,"The upper San Angelo Fm. of Olson (1962) is widely identical to the lower part of the Flowerpot Shale Member of the upper San Angelo Fm. (sensu Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 114 ff.),claystone,"gypsiferous,green,red or brown",,,Y,sandstone,red or brown,,conglomeratic,Y,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,E. C. Olson,1958,,,terrestrial,NA,actively mobile,,NA,carnivore,,,hydroxyapatite,,NA,,Phthinosuchidae,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 09:54,26/07/2009 08:56,26846,sp.,,26846,,279.3,268.8,Kungurian,Roadian,1,US, sp.
788184,occ,NA,,79600,,n. gen. Knoxosaurus n. sp. niteckii,species,142569,,Knoxosaurus niteckii,NA,species,142569,Olson,1962,Chordata,33815,Osteichthyes,34881,Theriodontia,56648,Phthinosuchidae,38942,38946,NA,NA,NA,individuals,-99.938332,33.66,Locality KAC (Lower Flowerpot Shale),NA,"Kahn Quarry, Driver Ranch",US,Texas,Knox,estimated from map,seconds,small collection,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork."" For details see map on p. 98 in Olson (1962).",gp_mid,-28.81,3.3,101,US,,San Angelo,Pease River,Flowerpot Shale,member,,,,,,,NA,"The upper San Angelo Fm. of Olson (1962) is widely identical to the lower part of the Flowerpot Shale Member of the upper San Angelo Fm. (sensu Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 114 ff.),claystone,"gypsiferous,green,red or brown",,,Y,sandstone,red or brown,,conglomeratic,Y,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,E. C. Olson,1958,,,terrestrial,NA,actively mobile,,NA,carnivore,,,hydroxyapatite,,NA,,Knoxosaurus,n. gen.,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 09:54,26/07/2009 08:56,26846,niteckii,Knoxosaurus,26846,n. sp.,279.3,268.8,Kungurian,Roadian,2,US,Knoxosaurus niteckii
788185,occ,NA,,80669,,Cotylorhynchus hancocki,species,122303,,Cotylorhynchus hancocki,NA,species,122303,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38917,NA,NA,NA,individuals,-99.917778,33.712502,Locality KR (Upper San Angelo Fm.),NA,Alexander Ranch,US,Texas,Knox,estimated from map,seconds,outcrop,"Maverick Flats 7.5' qdr; ""on the east and west flanks of a divide between two tributaries that flow south into the South Fork of the Wichita River""; For details see maps on pp. 98, 119 in Olson (1962)",gp_mid,-28.77,3.34,101,US,,San Angelo,Pease River,Flowerpot Shale,formation,,,,,,,NA,"""Exposures in this locality are predominantly San Angelo with the Flower Pot preserved on some high erosion remnants."" (Olson, 1962)\r\nThe upper San Angelo Fm. and basal Flowerpot Fm. of Olson (1962) are widely identical to the Flowerpot Shale Member of the upper San Angelo Fm. (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 119),"""shale""","green,red",,"argillaceous,sandy",,sandstone,,,,,terrestrial indet.,cratonic basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cotylorhynchus,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 11:10,04/12/2008 09:58,26846,hancocki,Cotylorhynchus,26846,,279.3,268.8,Kungurian,Roadian,1,US,Cotylorhynchus hancocki
788186,occ,NA,,80669,,Kahneria seltina,species,119509,,Kahneria seltina,NA,species,119509,Olson,1962,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37506,NA,NA,NA,individuals,-99.917778,33.712502,Locality KR (Upper San Angelo Fm.),NA,Alexander Ranch,US,Texas,Knox,estimated from map,seconds,outcrop,"Maverick Flats 7.5' qdr; ""on the east and west flanks of a divide between two tributaries that flow south into the South Fork of the Wichita River""; For details see maps on pp. 98, 119 in Olson (1962)",gp_mid,-28.77,3.34,101,US,,San Angelo,Pease River,Flowerpot Shale,formation,,,,,,,NA,"""Exposures in this locality are predominantly San Angelo with the Flower Pot preserved on some high erosion remnants."" (Olson, 1962)\r\nThe upper San Angelo Fm. and basal Flowerpot Fm. of Olson (1962) are widely identical to the Flowerpot Shale Member of the upper San Angelo Fm. (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 119),"""shale""","green,red",,"argillaceous,sandy",,sandstone,,,,,terrestrial indet.,cratonic basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Kahneria,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,01/12/2008 11:10,01/12/2008 13:10,26846,seltina,Kahneria,26846,,279.3,268.8,Kungurian,Roadian,2,US,Kahneria seltina
788187,occ,NA,,80669,,Caseopsis cf. agilis,species,123400,,Caseopsis agilis,NA,species,123400,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38916,NA,NA,NA,individuals,-99.917778,33.712502,Locality KR (Upper San Angelo Fm.),NA,Alexander Ranch,US,Texas,Knox,estimated from map,seconds,outcrop,"Maverick Flats 7.5' qdr; ""on the east and west flanks of a divide between two tributaries that flow south into the South Fork of the Wichita River""; For details see maps on pp. 98, 119 in Olson (1962)",gp_mid,-28.77,3.34,101,US,,San Angelo,Pease River,Flowerpot Shale,formation,,,,,,,NA,"""Exposures in this locality are predominantly San Angelo with the Flower Pot preserved on some high erosion remnants."" (Olson, 1962)\r\nThe upper San Angelo Fm. and basal Flowerpot Fm. of Olson (1962) are widely identical to the Flowerpot Shale Member of the upper San Angelo Fm. (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 119),"""shale""","green,red",,"argillaceous,sandy",,sandstone,,,,,terrestrial indet.,cratonic basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Caseopsis,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 11:10,04/12/2008 09:58,26846,agilis,Caseopsis,26846,cf.,279.3,268.8,Kungurian,Roadian,1,US,Caseopsis agilis
788189,occ,NA,,80729,,Rothia multidonta,species,119703,recombined as,Rothianiscus multidonta,NA,species,119703,Olson,1962,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37507,NA,NA,NA,individuals,-99.961113,33.519722,Locality KN (San Angelo Fm.),NA,Little Croton Creek; MacFayden Ranch; JR Pasture,US,Texas,Knox,estimated from map,seconds,outcrop,Cedar Mountain 7.5' qdr. Locality comprises exposures south of Little Croton Creek. For details see map on p. 108 in Olson (1962).,gp_mid,-28.9,3.19,101,US,,San Angelo,Pease River,,formation,,,,,,,NA,,for details see Olson (1962 p. 111),"""shale""","gypsiferous,green,red or brown",,sandy,,conglomerate,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,few,,,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Rothia,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,01/12/2008 20:28,01/12/2008 22:28,26846,multidonta,Rothianiscus,26846,,279.3,268.8,Kungurian,Roadian,1,US,Rothianiscus multidonta
788190,occ,NA,,80729,,n. gen. Angelosaurus n. sp. dolani,species,123401,,Angelosaurus dolani,NA,species,123401,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38914,NA,NA,NA,individuals,-99.961113,33.519722,Locality KN (San Angelo Fm.),NA,Little Croton Creek; MacFayden Ranch; JR Pasture,US,Texas,Knox,estimated from map,seconds,outcrop,Cedar Mountain 7.5' qdr. Locality comprises exposures south of Little Croton Creek. For details see map on p. 108 in Olson (1962).,gp_mid,-28.9,3.19,101,US,,San Angelo,Pease River,,formation,,,,,,,NA,,for details see Olson (1962 p. 111),"""shale""","gypsiferous,green,red or brown",,sandy,,conglomerate,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,few,,,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Angelosaurus,n. gen.,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,01/12/2008 20:28,01/12/2008 22:28,26846,dolani,Angelosaurus,26846,n. sp.,279.3,268.8,Kungurian,Roadian,2,US,Angelosaurus dolani
788191,occ,NA,,80729,,n. gen. Tappenosaurus n. sp. magnus,species,136987,,Tappenosaurus magnus,NA,species,136987,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Tappenosauridae,136988,136986,NA,NA,NA,individuals,-99.961113,33.519722,Locality KN (San Angelo Fm.),NA,Little Croton Creek; MacFayden Ranch; JR Pasture,US,Texas,Knox,estimated from map,seconds,outcrop,Cedar Mountain 7.5' qdr. Locality comprises exposures south of Little Croton Creek. For details see map on p. 108 in Olson (1962).,gp_mid,-28.9,3.19,101,US,,San Angelo,Pease River,,formation,,,,,,,NA,,for details see Olson (1962 p. 111),"""shale""","gypsiferous,green,red or brown",,sandy,,conglomerate,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,few,,,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tappenosaurus,n. gen.,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,01/12/2008 20:28,01/12/2008 22:28,26846,magnus,Tappenosaurus,26846,n. sp.,279.3,268.8,Kungurian,Roadian,1,US,Tappenosaurus magnus
788192,occ,NA,,80692,,n. gen. Caseoides n. sp. sanangeloensis,species,123414,,Caseoides sanangeloensis,NA,species,123414,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38919,NA,NA,NA,individuals,-99.987503,33.530277,Locality KP (San Angelo Fm.),NA,Little Croton Creek; MacFayden Ranch; JR Pasture,US,Texas,Knox,estimated from map,seconds,outcrop,"Cedar Mountain 7.5' qdr. Locality comprises exposures north and south of Little Croton Creek, close to the western border of Knox Co. For details see map on p. 108 in Olson (1962).",gp_mid,-28.91,3.21,101,US,,San Angelo,Pease River,,formation,,,,,,,NA,,for details see Olson (1962 p. 111),"""shale""",green,,,Y,conglomerate,,,,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,taxonomic,,FMNH,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Caseoides,n. gen.,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,01/12/2008 21:33,01/12/2008 23:33,26846,sanangeloensis,Caseoides,26846,n. sp.,279.3,268.8,Kungurian,Roadian,2,US,Caseoides sanangeloensis
788193,occ,NA,,80692,,Tetrapoda indet.,unranked clade,53190,,Tetrapoda,NA,unranked clade,53190,Olson,1962,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,individuals,-99.987503,33.530277,Locality KP (San Angelo Fm.),NA,Little Croton Creek; MacFayden Ranch; JR Pasture,US,Texas,Knox,estimated from map,seconds,outcrop,"Cedar Mountain 7.5' qdr. Locality comprises exposures north and south of Little Croton Creek, close to the western border of Knox Co. For details see map on p. 108 in Olson (1962).",gp_mid,-28.91,3.21,101,US,,San Angelo,Pease River,,formation,,,,,,,NA,,for details see Olson (1962 p. 111),"""shale""",green,,,Y,conglomerate,,,,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,taxonomic,,FMNH,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tetrapoda,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,01/12/2008 21:33,01/12/2008 23:33,26846,indet.,,26846,,279.3,268.8,Kungurian,Roadian,1,US, indet.
788194,occ,NA,,80692,,Captorhinidae sp.,genus,37495,,Captorhinidae,NA,family,37495,Olson,1962,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,NA,NA,NA,NA,individuals,-99.987503,33.530277,Locality KP (San Angelo Fm.),NA,Little Croton Creek; MacFayden Ranch; JR Pasture,US,Texas,Knox,estimated from map,seconds,outcrop,"Cedar Mountain 7.5' qdr. Locality comprises exposures north and south of Little Croton Creek, close to the western border of Knox Co. For details see map on p. 108 in Olson (1962).",gp_mid,-28.91,3.21,101,US,,San Angelo,Pease River,,formation,,,,,,,NA,,for details see Olson (1962 p. 111),"""shale""",green,,,Y,conglomerate,,,,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,taxonomic,,FMNH,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinidae,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,01/12/2008 21:33,01/12/2008 23:33,26846,sp.,,26846,,279.3,268.8,Kungurian,Roadian,1,US, sp.
788195,occ,NA,,80729,,Cotylorhynchus hancocki,species,122303,,Cotylorhynchus hancocki,NA,species,122303,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38917,NA,NA,NA,individuals,-99.961113,33.519722,Locality KN (San Angelo Fm.),NA,Little Croton Creek; MacFayden Ranch; JR Pasture,US,Texas,Knox,estimated from map,seconds,outcrop,Cedar Mountain 7.5' qdr. Locality comprises exposures south of Little Croton Creek. For details see map on p. 108 in Olson (1962).,gp_mid,-28.9,3.19,101,US,,San Angelo,Pease River,,formation,,,,,,,NA,,for details see Olson (1962 p. 111),"""shale""","gypsiferous,green,red or brown",,sandy,,conglomerate,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,few,,,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cotylorhynchus,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 21:56,01/12/2008 23:57,26846,hancocki,Cotylorhynchus,26846,,279.3,268.8,Kungurian,Roadian,1,US,Cotylorhynchus hancocki
788196,occ,NA,,79694,,Cotylorhynchus n. sp. hancocki,species,122303,,Cotylorhynchus hancocki,NA,species,122303,Olson and Beerbower,1953,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38917,NA,NA,NA,individuals,-99.73333,34.099998,"Locality HA (""Lower San Angelo Fm."")",NA,Pease River,US,Texas,Hardeman,estimated from map,minutes,outcrop,"North of Pease River, 1 mile west of Crowell-Quanah highway",gp_mid,-28.44,3.59,101,US,,San Angelo,Pease River,Flowerpot Shale,,,,,,,,NA,"""15 ft below top of section"" (Olson & Beerbower, 1953)\r\n""Re-examination, after study of the Flower Pot-San Angelo relationship elsewhere, showed without question that Flower Pot assignment is correct. [...] The age of this is herewith corrected from the original San Angelo assignment to Flower Pot."" (Olson, 1962)\r\nThe terrestrial part of Olson's Flower Pot Formation is equivalent to the Flowerpot Member of the Upper San Angelo Formation (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80) ",for details see Olson (1962 p. 121 f.),claystone,red or brown,,"silty,sandy",Y,conglomerate,red or brown,,,Y,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,,,,,,,,,,,NA,,,taxonomic,field collection,,,,,E. C. Olson,1950,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cotylorhynchus,,NA,NA,vertebrate,"E. C. Olson and J. R. Beerbower. 1953. The San Angelo Formation, Permian of Texas, and its Vertebrates. Journal of Geology 61(5):389-423",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 22:04,09/12/2008 17:45,28373,hancocki,Cotylorhynchus,28373,n. sp.,279.3,268.8,Kungurian,Roadian,4,US,Cotylorhynchus hancocki
788197,occ,NA,,80689,,Dimetrodon n. sp. angelensis,species,123424,,Dimetrodon angelensis,NA,species,123424,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,individuals,-99.953613,33.690834,Locality KV (San Angelo Fm.),NA,MacFayden Ranch; Swanson Quarry,US,Texas,Knox,estimated from map,seconds,,"Maverick Flats 7.5' qdr; ""just to the north of the valley of the South Fork of the Wichita River""; close to the western border of Knox Co. For details see map on p. 98 in Olson (1962).",gp_mid,-28.81,3.33,101,US,,San Angelo,Pease River,,member,,,,,,,NA,"Middle and Upper San Angelo Formation sensu Olson (1962), corresponding to the upper Duncan Sandstone Member and lower Flowerpot Shale Member of the San Angelo Formation sensu Smith (1974)",for details see Olson (1962 p. 118),"""shale""",red,,sandy,Y,conglomerate,,,,Y,"""floodplain""",cratonic basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"Fossil vertebrates found [...] appear to have been laid down as partial skeletons. The nature of disarticulation and breakage suggests that they were\r\nscattered, probably by action of flesh-eaters, prior to burial. [...] the preserved animals give every evidence of having lived close to the sites of deposition.",taxonomic,field collection,FMNH,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 23:02,24/07/2009 17:07,26846,angelensis,Dimetrodon,26846,n. sp.,279.3,268.8,Kungurian,Roadian,1,US,Dimetrodon angelensis
788198,occ,NA,,80689,,Caseopsis n. sp. agilis,species,123400,,Caseopsis agilis,NA,species,123400,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38916,NA,NA,NA,individuals,-99.953613,33.690834,Locality KV (San Angelo Fm.),NA,MacFayden Ranch; Swanson Quarry,US,Texas,Knox,estimated from map,seconds,,"Maverick Flats 7.5' qdr; ""just to the north of the valley of the South Fork of the Wichita River""; close to the western border of Knox Co. For details see map on p. 98 in Olson (1962).",gp_mid,-28.81,3.33,101,US,,San Angelo,Pease River,,member,,,,,,,NA,"Middle and Upper San Angelo Formation sensu Olson (1962), corresponding to the upper Duncan Sandstone Member and lower Flowerpot Shale Member of the San Angelo Formation sensu Smith (1974)",for details see Olson (1962 p. 118),"""shale""",red,,sandy,Y,conglomerate,,,,Y,"""floodplain""",cratonic basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"Fossil vertebrates found [...] appear to have been laid down as partial skeletons. The nature of disarticulation and breakage suggests that they were\r\nscattered, probably by action of flesh-eaters, prior to burial. [...] the preserved animals give every evidence of having lived close to the sites of deposition.",taxonomic,field collection,FMNH,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Caseopsis,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 23:02,24/07/2009 17:07,26846,agilis,Caseopsis,26846,n. sp.,279.3,268.8,Kungurian,Roadian,1,US,Caseopsis agilis
788199,occ,NA,,80689,,Cotylorhynchus hancocki,species,122303,,Cotylorhynchus hancocki,NA,species,122303,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38917,NA,NA,NA,individuals,-99.953613,33.690834,Locality KV (San Angelo Fm.),NA,MacFayden Ranch; Swanson Quarry,US,Texas,Knox,estimated from map,seconds,,"Maverick Flats 7.5' qdr; ""just to the north of the valley of the South Fork of the Wichita River""; close to the western border of Knox Co. For details see map on p. 98 in Olson (1962).",gp_mid,-28.81,3.33,101,US,,San Angelo,Pease River,,member,,,,,,,NA,"Middle and Upper San Angelo Formation sensu Olson (1962), corresponding to the upper Duncan Sandstone Member and lower Flowerpot Shale Member of the San Angelo Formation sensu Smith (1974)",for details see Olson (1962 p. 118),"""shale""",red,,sandy,Y,conglomerate,,,,Y,"""floodplain""",cratonic basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"Fossil vertebrates found [...] appear to have been laid down as partial skeletons. The nature of disarticulation and breakage suggests that they were\r\nscattered, probably by action of flesh-eaters, prior to burial. [...] the preserved animals give every evidence of having lived close to the sites of deposition.",taxonomic,field collection,FMNH,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cotylorhynchus,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 23:02,24/07/2009 17:07,26846,hancocki,Cotylorhynchus,26846,,279.3,268.8,Kungurian,Roadian,4,US,Cotylorhynchus hancocki
788200,occ,NA,,80130,,Diasparactus zenos,species,157286,recombined as,Diadectes zenos,NA,species,157286,Case and Williston,1913,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,individuals,-106.356941,36.283333,"AMNH ?, based on AMNH 4794",34761,horizon of Diasparactus zenos; El Cobre Canyon,US,New Mexico,Rio Arriba,,minutes,small collection,Latitude & longitude from Vaughn (1963),gp_mid,-33.81,4.49,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,Not much is described in this publication,"""a reddish, clayey sandstone somewhat below the middle of the Permo-Carboniferous strata of El Cobre Canyon, in Rio Arriba, New Mexico."" (Case and Williston 1913, p.17)",sandstone,red,lithified,,Y,conglomerate,,lithified,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,"bulk,field collection",AMNH,,,,E.C. Case,1910,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diasparactus,,NA,NA,,E. C. Case and S. W. Williston. 1913. Description of a nearly complete skeleton of Diasparactus zenos Case. Carnegie Institution of Washington Publication 181:17-35,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 23:09,02/12/2008 01:11,26921,zenos,Diadectes,26921,,296.4,268,Wolfcamp,,1,US,Diadectes zenos
788201,occ,NA,,34761,,n. gen. Baldwinonus n. sp. trux,species,122331,,Baldwinonus trux,NA,species,122331,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Eothyrididae,38898,38886,NA,NA,NA,individuals,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Baldwinonus,n. gen.,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 23:20,21/08/2009 16:28,43845,trux,Baldwinonus,27105,n. sp.,303.4,298.9,Virgilian,,1,US,Baldwinonus trux
788202,occ,NA,,34761,,n. gen. Ruthiromia n. sp. elcobriensis,species,122322,,Ruthiromia elcobriensis,NA,species,122322,Eberth and Brinkman,1983,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,122321,NA,NA,NA,individuals,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ruthiromia,n. gen.,NA,NA,vertebrate,"D. A. Eberth and D. Brinkman. 1983. Ruthiromia elcobriensis, a New Pelycosaur from El Cobre Canyon, New Mexico. Breviora 474:1-26",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,01/12/2008 23:20,21/08/2009 16:28,43845,elcobriensis,Ruthiromia,30572,n. sp.,303.4,298.9,Virgilian,,1,US,Ruthiromia elcobriensis
788203,occ,NA,,34761,,n. gen. Aerosaurus n. sp. greenleeorum,species,122317,,Aerosaurus greenleeorum,NA,species,122317,Romer,1937,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,38893,NA,NA,NA,individuals,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Aerosaurus,n. gen.,NA,NA,vertebrate,A. S. Romer. 1937. New genera and species of pelycosaurian reptiles. Proceedings of the New England Zo̦logical Club 16:89-95,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,01/12/2008 23:23,10/12/2012 14:42,43845,greenleeorum,Aerosaurus,43845,n. sp.,303.4,298.9,Virgilian,,1,US,Aerosaurus greenleeorum
788205,occ,NA,,34761,,Chamasaurus dolichognathus,species,242820,,Chamasaurus dolichognathus,NA,species,242820,Vaughn,1963,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,242819,NA,NA,NA,,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Chamasaurus,,NA,NA,vertebrate,"P. P. Vaughn. 1963. The Age and Locality of the Late Paleozoic Vertebrates from El Cobre Canyon, Rio Arriba County, New Mexico. Journal of Paleontology 37(1):283-286",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,02/12/2008 00:54,21/08/2009 16:28,43845,dolichognathus,Chamasaurus,28637,,303.4,298.9,Virgilian,,NA,US,Chamasaurus dolichognathus
788206,occ,NA,,34761,,Limnoscelis paludis,species,113848,,Limnoscelis paludis,NA,species,113848,Vaughn,1963,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Limnoscelidae,37231,37232,NA,NA,NA,,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Limnoscelis,,NA,NA,vertebrate,"P. P. Vaughn. 1963. The Age and Locality of the Late Paleozoic Vertebrates from El Cobre Canyon, Rio Arriba County, New Mexico. Journal of Paleontology 37(1):283-286",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,02/12/2008 00:54,21/08/2009 16:28,43845,paludis,Limnoscelis,28637,,303.4,298.9,Virgilian,,NA,US,Limnoscelis paludis
788207,occ,NA,,34761,,n. gen. Nitosaurus n. sp. jacksonorum,species,123522,,Nitosaurus jacksonorum,NA,species,123522,Romer,1937,Chordata,33815,Osteichthyes,34881,Pelycosauria,38883,,NA,38928,NA,NA,NA,individuals,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Nitosaurus,n. gen.,NA,NA,vertebrate,A. S. Romer. 1937. New genera and species of pelycosaurian reptiles. Proceedings of the New England Zo̦logical Club 16:89-95,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,02/12/2008 00:54,10/12/2012 14:43,43845,jacksonorum,Nitosaurus,43845,n. sp.,303.4,298.9,Virgilian,,1,US,Nitosaurus jacksonorum
788211,occ,NA,,78559,,Rothia multidonta,species,119703,recombined as,Rothianiscus multidonta,NA,species,119703,Olson,1962,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37507,NA,NA,NA,individuals,-99.907776,33.718056,Locality KS (Upper San Angelo Fm.),NA,Alexander Ranch,US,Texas,Knox,estimated from map,seconds,small collection,"Maverick Flats 7.5' qdr; ""on the east and west flanks of a divide between two tributaries that flow south into the South Fork of the Wichita River""; For details see maps on pp. 98, 119 in Olson (1962)",gp_mid,-28.76,3.34,101,US,,San Angelo,Pease River,Flowerpot Shale,group of beds,,,,,,,NA,,not much reported,"""shale""",red,,,Y,"""shale""","green,red",,sandy,,fluvial-deltaic indet.,foreland basin,"""This locality includes Flower Pot, terrestrial in the eastern part but grading into marginal facies in the west. No strictly offshore facies are present, although these occur to the west of the limit of the locality.""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Rothia,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,02/12/2008 03:44,02/12/2008 05:44,26846,multidonta,Rothianiscus,26846,,279.3,268.8,Kungurian,Roadian,1,US,Rothianiscus multidonta
788212,occ,NA,,78559,,Angelosaurus greeni,species,122304,,Angelosaurus greeni,NA,species,122304,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38914,NA,NA,NA,individuals,-99.907776,33.718056,Locality KS (Upper San Angelo Fm.),NA,Alexander Ranch,US,Texas,Knox,estimated from map,seconds,small collection,"Maverick Flats 7.5' qdr; ""on the east and west flanks of a divide between two tributaries that flow south into the South Fork of the Wichita River""; For details see maps on pp. 98, 119 in Olson (1962)",gp_mid,-28.76,3.34,101,US,,San Angelo,Pease River,Flowerpot Shale,group of beds,,,,,,,NA,,not much reported,"""shale""",red,,,Y,"""shale""","green,red",,sandy,,fluvial-deltaic indet.,foreland basin,"""This locality includes Flower Pot, terrestrial in the eastern part but grading into marginal facies in the west. No strictly offshore facies are present, although these occur to the west of the limit of the locality.""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Angelosaurus,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,02/12/2008 03:44,02/12/2008 05:44,26846,greeni,Angelosaurus,26846,,279.3,268.8,Kungurian,Roadian,1,US,Angelosaurus greeni
788489,occ,NA,,79162,,Dimetrodon n. sp. milleri,species,122782,,Dimetrodon milleri,NA,species,122782,Romer,1937,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,individuals,-98.650002,33.583332,Archer City Bonebed 1 (Putnam Fm.),NA,"Locality IIIf (Romer & Price, 1940)",US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1937. New genera and species of pelycosaurian reptiles. Proceedings of the New England Zo̦logical Club 16:89-95,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,04/12/2008 05:54,10/12/2012 14:44,43845,milleri,Dimetrodon,43845,n. sp.,296.4,268,Wolfcamp,,1,US,Dimetrodon milleri
788507,occ,NA,,85170,,n. gen. Mastersonia n. sp. driverensis,species,137162,,Mastersonia driverensis,NA,species,137162,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Mastersoniidae,137161,38995,NA,NA,NA,individuals,-99.927498,33.639168,Locality KY (San Angelo Fm.),NA,Driver Ranch,US,Texas,Knox,estimated from map,seconds,outcrop,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork.""\r\nFor details see map on p. 98 in Olson (1962)",gp_mid,-28.81,3.28,101,US,,San Angelo,Pease River,,formation,,,,,,,NA,"""Fossils occur in the upper red shale of the middle San Angelo, in the channel deposits of the upper San Angelo, and in the overlying sandy shales, which, in the proposed scheme, fall in the basal Flower Pot.""\r\nNote: The Middle San Angelo Fm. of Olson's ""proposed scheme"" is the upper part of the Duncan Sandstone Member of the lower San Angelo Fm. and Olson's upper San Angelo Fm. and basal Flower Pot Fm. belong to the Flowerpot Shale Member of the upper San Angelo Fm. (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 113),"""shale""","green,red",,,,sandstone,red or brown,,,,fluvial-deltaic indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"""Evidently there was disarticulation and transport after death and before burial. [...] Apparently vertebrate remains were rafted in and deposited either partially complete or after considerable disarticulation. Some of the bones are fairly well preserved, but many have suffered serious damage, apparently as the result of the abundant gypsum which, by recrystallization, has damaged and distorted the bones.""",taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Mastersonia,n. gen.,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,04/12/2008 09:01,04/12/2008 11:01,26846,driverensis,Mastersonia,26846,n. sp.,279.3,268.8,Kungurian,Roadian,1,US,Mastersonia driverensis
788508,occ,NA,,85170,,Dimetrodon angelensis,species,123424,,Dimetrodon angelensis,NA,species,123424,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,individuals,-99.927498,33.639168,Locality KY (San Angelo Fm.),NA,Driver Ranch,US,Texas,Knox,estimated from map,seconds,outcrop,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork.""\r\nFor details see map on p. 98 in Olson (1962)",gp_mid,-28.81,3.28,101,US,,San Angelo,Pease River,,formation,,,,,,,NA,"""Fossils occur in the upper red shale of the middle San Angelo, in the channel deposits of the upper San Angelo, and in the overlying sandy shales, which, in the proposed scheme, fall in the basal Flower Pot.""\r\nNote: The Middle San Angelo Fm. of Olson's ""proposed scheme"" is the upper part of the Duncan Sandstone Member of the lower San Angelo Fm. and Olson's upper San Angelo Fm. and basal Flower Pot Fm. belong to the Flowerpot Shale Member of the upper San Angelo Fm. (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 113),"""shale""","green,red",,,,sandstone,red or brown,,,,fluvial-deltaic indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"""Evidently there was disarticulation and transport after death and before burial. [...] Apparently vertebrate remains were rafted in and deposited either partially complete or after considerable disarticulation. Some of the bones are fairly well preserved, but many have suffered serious damage, apparently as the result of the abundant gypsum which, by recrystallization, has damaged and distorted the bones.""",taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,04/12/2008 09:01,04/12/2008 11:01,26846,angelensis,Dimetrodon,26846,,279.3,268.8,Kungurian,Roadian,1,US,Dimetrodon angelensis
788509,occ,NA,,85170,,Cotylorhynchus hancocki,species,122303,,Cotylorhynchus hancocki,NA,species,122303,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38917,NA,NA,NA,individuals,-99.927498,33.639168,Locality KY (San Angelo Fm.),NA,Driver Ranch,US,Texas,Knox,estimated from map,seconds,outcrop,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork.""\r\nFor details see map on p. 98 in Olson (1962)",gp_mid,-28.81,3.28,101,US,,San Angelo,Pease River,,formation,,,,,,,NA,"""Fossils occur in the upper red shale of the middle San Angelo, in the channel deposits of the upper San Angelo, and in the overlying sandy shales, which, in the proposed scheme, fall in the basal Flower Pot.""\r\nNote: The Middle San Angelo Fm. of Olson's ""proposed scheme"" is the upper part of the Duncan Sandstone Member of the lower San Angelo Fm. and Olson's upper San Angelo Fm. and basal Flower Pot Fm. belong to the Flowerpot Shale Member of the upper San Angelo Fm. (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 113),"""shale""","green,red",,,,sandstone,red or brown,,,,fluvial-deltaic indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"""Evidently there was disarticulation and transport after death and before burial. [...] Apparently vertebrate remains were rafted in and deposited either partially complete or after considerable disarticulation. Some of the bones are fairly well preserved, but many have suffered serious damage, apparently as the result of the abundant gypsum which, by recrystallization, has damaged and distorted the bones.""",taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cotylorhynchus,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,04/12/2008 09:01,04/12/2008 11:01,26846,hancocki,Cotylorhynchus,26846,,279.3,268.8,Kungurian,Roadian,3,US,Cotylorhynchus hancocki
788511,occ,NA,,80112,,Dimetrodon n. sp. teutonis,species,137166,,Dimetrodon teutonis,NA,species,137166,Berman et al.,2001,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,individuals,10.618889,50.809723,Bromacker Quarry (upper level of Tambach sandstone),NA,,DE,Thuringia,Gotha,based on nearby landmark,seconds,outcrop,"""...middle part of the Thuringian Forest near the village of Tambach-Dietharz and about 20 km south of the town of Gotha, central Germany.""",gp_mid,21.71,7.41,305,DE,,Tambach,Rotliegend,Tambach-Sandstein,group of beds,,,,,,,NA,"""At the Bromacker quarry site are two superimposed stratigraphic successions that can be characterized by their facies associations and are referred to as the Lower Beds and Upper Beds (Eberth et al. 2000). All the vertebrates from the Bromacker quarry come from the Upper Beds [...]. The vertebrates are almost exclusively restricted to two [... horizons ...] which are separated by 50 cm in a stratigraphic interval of 1.2 m."" (Berman et al., 2001)\r\nThe Tambach Formation is of Artinskian age according to ""Stratigraphische Tabelle von Deutschland 2002"", however, a Kungurian age is proposed by L_tzner (2006) in LITHOLEX stratigraphic online database [http://www.bgr.de/app/LithoLex/gesamt_ausgabe_neu.php5?id=25]","""massive, red-brown, very fine-grained sandstone and siltstone"" (Berman et al., 2001).\r\nFor further details see Eberth et al. (2000).",sandstone,"very fine,brown,red",lithified,,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,"""alluvial paleochannel and sheetflood facies and lacustrine suspension deposits"" (Berman et al., 2001).\r\n""During the time that the Lower and Upper beds were deposited, the Tambach Basin was internally-drained and probably characterized by a wet-and-dry tropical or wetter climate that was hot year-round with seasonal-to-subseasonal cycles of rainfall and drying. [...] In the Bromacker area, the floodbasin was never deeply desiccated or heavily vegetated between flooding events."" Eberth et al. (2000).",macrofossils,,,,,,NA,,"body,permineralized",excellent,,snapshot,,,,,,,NA,,,taxonomic,"bulk,field collection",,all macrofossils,,,,,"MNG = Museum der Natur, Gotha",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"D. S. Berman, R. R. Reisz, and T. Martens, A. C. Henrici. 2001. A new species of Dimetrodon (Synapsida: Sphenacodontidae) from the Lower Permian of Germany records first occurrence of genus outside of North America. Canadian Journal of Earth Sciences 38(5):803-812",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,04/12/2008 10:01,26/08/2009 12:13,26922,teutonis,Dimetrodon,28661,n. sp.,290.1,279.3,Artinskian,,1,DE,Dimetrodon teutonis
788516,occ,NA,,85171,,Rothia multidonta,species,119703,recombined as,Rothianiscus multidonta,NA,species,119703,Olson,1962,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37507,NA,NA,NA,individuals,-99.925835,33.645557,Locality KAB (Upper San Angelo Fm.),NA,Driver Ranch,US,Texas,Knox,estimated from map,seconds,outcrop,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork.""\r\nFor details see map on p. 98 in Olson (1962)",gp_mid,-28.81,3.28,101,US,,San Angelo,Pease River,Flowerpot Shale,member,,,,,,,NA,"Olson's Upper San Angelo Fm. and basal Flower Pot Fm. belong to the Flowerpot Shale Member of the Upper San Angelo Fm. (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)","""The upper part of the San Angelo [here] is composed largely of brown and green\r\nsandstone, and sandy shale channel deposits are poorly developed. Transition to the Flower Pot is rather abrupt, with only a thin, green sandy shale member above the contact""",sandstone,"brown,green",,,,"""shale""",,,sandy,,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,abundant,,,NA,,"""The upper part of the San Angelo in this locality is rich in fossils. Specimens occur in the sandy shales and appear to have been washed in by river currents during flood stages. Partial to complete articulation is the rule.""",taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Rothia,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,04/12/2008 11:17,04/12/2008 13:17,26846,multidonta,Rothianiscus,26846,,279.3,268.8,Kungurian,Roadian,1,US,Rothianiscus multidonta
788517,occ,NA,,85171,,Cotylorhynchus hancocki,species,122303,,Cotylorhynchus hancocki,NA,species,122303,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38917,NA,NA,NA,individuals,-99.925835,33.645557,Locality KAB (Upper San Angelo Fm.),NA,Driver Ranch,US,Texas,Knox,estimated from map,seconds,outcrop,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork.""\r\nFor details see map on p. 98 in Olson (1962)",gp_mid,-28.81,3.28,101,US,,San Angelo,Pease River,Flowerpot Shale,member,,,,,,,NA,"Olson's Upper San Angelo Fm. and basal Flower Pot Fm. belong to the Flowerpot Shale Member of the Upper San Angelo Fm. (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)","""The upper part of the San Angelo [here] is composed largely of brown and green\r\nsandstone, and sandy shale channel deposits are poorly developed. Transition to the Flower Pot is rather abrupt, with only a thin, green sandy shale member above the contact""",sandstone,"brown,green",,,,"""shale""",,,sandy,,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,abundant,,,NA,,"""The upper part of the San Angelo in this locality is rich in fossils. Specimens occur in the sandy shales and appear to have been washed in by river currents during flood stages. Partial to complete articulation is the rule.""",taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cotylorhynchus,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,04/12/2008 11:17,04/12/2008 13:17,26846,hancocki,Cotylorhynchus,26846,,279.3,268.8,Kungurian,Roadian,2,US,Cotylorhynchus hancocki
788518,occ,NA,,85171,,Tappenosaurus magnus,species,136987,,Tappenosaurus magnus,NA,species,136987,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Tappenosauridae,136988,136986,NA,NA,NA,individuals,-99.925835,33.645557,Locality KAB (Upper San Angelo Fm.),NA,Driver Ranch,US,Texas,Knox,estimated from map,seconds,outcrop,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork.""\r\nFor details see map on p. 98 in Olson (1962)",gp_mid,-28.81,3.28,101,US,,San Angelo,Pease River,Flowerpot Shale,member,,,,,,,NA,"Olson's Upper San Angelo Fm. and basal Flower Pot Fm. belong to the Flowerpot Shale Member of the Upper San Angelo Fm. (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)","""The upper part of the San Angelo [here] is composed largely of brown and green\r\nsandstone, and sandy shale channel deposits are poorly developed. Transition to the Flower Pot is rather abrupt, with only a thin, green sandy shale member above the contact""",sandstone,"brown,green",,,,"""shale""",,,sandy,,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,abundant,,,NA,,"""The upper part of the San Angelo in this locality is rich in fossils. Specimens occur in the sandy shales and appear to have been washed in by river currents during flood stages. Partial to complete articulation is the rule.""",taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tappenosaurus,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,04/12/2008 11:17,04/12/2008 13:17,26846,magnus,Tappenosaurus,26846,,279.3,268.8,Kungurian,Roadian,1,US,Tappenosaurus magnus
788519,occ,NA,,85171,,Dimacrodon sp.,genus,38993,,Dimacrodon,NA,genus,38993,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Dimacrodontidae,137164,38993,NA,NA,NA,individuals,-99.925835,33.645557,Locality KAB (Upper San Angelo Fm.),NA,Driver Ranch,US,Texas,Knox,estimated from map,seconds,outcrop,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork.""\r\nFor details see map on p. 98 in Olson (1962)",gp_mid,-28.81,3.28,101,US,,San Angelo,Pease River,Flowerpot Shale,member,,,,,,,NA,"Olson's Upper San Angelo Fm. and basal Flower Pot Fm. belong to the Flowerpot Shale Member of the Upper San Angelo Fm. (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)","""The upper part of the San Angelo [here] is composed largely of brown and green\r\nsandstone, and sandy shale channel deposits are poorly developed. Transition to the Flower Pot is rather abrupt, with only a thin, green sandy shale member above the contact""",sandstone,"brown,green",,,,"""shale""",,,sandy,,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,abundant,,,NA,,"""The upper part of the San Angelo in this locality is rich in fossils. Specimens occur in the sandy shales and appear to have been washed in by river currents during flood stages. Partial to complete articulation is the rule.""",taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,herbivore,,,hydroxyapatite,,NA,,Dimacrodon,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,04/12/2008 11:17,04/12/2008 13:17,26846,sp.,Dimacrodon,26846,,279.3,268.8,Kungurian,Roadian,1,US,Dimacrodon sp.
788527,occ,NA,,79694,,n. gen. Dimacrodon n. sp. hottoni,species,137165,,Dimacrodon hottoni,NA,species,137165,Olson and Beerbower,1953,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Dimacrodontidae,137164,38993,NA,NA,NA,individuals,-99.73333,34.099998,"Locality HA (""Lower San Angelo Fm."")",NA,Pease River,US,Texas,Hardeman,estimated from map,minutes,outcrop,"North of Pease River, 1 mile west of Crowell-Quanah highway",gp_mid,-28.44,3.59,101,US,,San Angelo,Pease River,Flowerpot Shale,,,,,,,,NA,"""15 ft below top of section"" (Olson & Beerbower, 1953)\r\n""Re-examination, after study of the Flower Pot-San Angelo relationship elsewhere, showed without question that Flower Pot assignment is correct. [...] The age of this is herewith corrected from the original San Angelo assignment to Flower Pot."" (Olson, 1962)\r\nThe terrestrial part of Olson's Flower Pot Formation is equivalent to the Flowerpot Member of the Upper San Angelo Formation (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80) ",for details see Olson (1962 p. 121 f.),claystone,red or brown,,"silty,sandy",Y,conglomerate,red or brown,,,Y,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,,,,,,,,,,,NA,,,taxonomic,field collection,,,,,E. C. Olson,1950,,,terrestrial,NA,actively mobile,,NA,herbivore,,,hydroxyapatite,,NA,,Dimacrodon,n. gen.,NA,NA,vertebrate,"E. C. Olson and J. R. Beerbower. 1953. The San Angelo Formation, Permian of Texas, and its Vertebrates. Journal of Geology 61(5):389-423",315,334,0,J. Mueller,T. Liebrecht,,04/12/2008 12:22,04/12/2008 14:22,28373,hottoni,Dimacrodon,28373,n. sp.,279.3,268.8,Kungurian,Roadian,3,US,Dimacrodon hottoni
788570,occ,NA,,85178,,n. gen. Melanothyris n. sp. morani,species,137220,recombined as,Protorothyris morani,NA,species,137220,Romer,1952,Chordata,33815,Reptilia,36322,,NA,Protorothyrididae,37486,37494,NA,NA,NA,individuals,-80.210831,39.72028,Blacksville,NA,Dunkard Locality 9,US,West Virginia,Monongalia,based on nearby landmark,seconds,outcrop,"""Clay District, Monongalia County, West Virginia\r\nThis locality is a road cut on the east side of the Blacksville-Hundred Road (West Virginia Route No.7) about one and one-half miles west of Blacksville, West Virginia"" (Moran, 1952)\r\nLat Long is for Blacksville",gp_mid,-14.53,-3.08,101,US,,Washington,Dunkard,Upper Marietta Sandstone,bed,,,,,,,NA,"""The stratigraphic position [...] is not certain, but appears, to be about 40 feet beneath the Hundred sandstone at the stratigraphic horizon of the Upper Marietta sandstone."" (Moran, 1952).\r\nNote: The age of the Washington Fm., wich is not well constrained, here is based on correlation chart (fig. 4) in Wellstead (1991, Bull. AMNH 209).","""Fossils were found in a siliceous limestone lens about 15 feet in length which had a maximum thickness of six inches"" (Moran, 1952)","""limestone""",,lithified,,Y,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Melanothyris,n. gen.,NA,NA,vertebrate,A. S. Romer. 1952. Late Pennsylvanian and Early Permian Vertebrates of the Pittsburgh-West Virginia Region. Annals of Carnegie Museum 33:47-113,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,05/12/2008 11:01,20/12/2008 16:11,28669,morani,Protorothyris,28669,n. sp.,298.9,295.5,Asselian,,7,US,Protorothyris morani
788638,occ,NA,,80112,,n. gen. Thuringothyris n. sp. mahlendorffae,species,137223,,Thuringothyris mahlendorffae,NA,species,137223,M_ller et al.,2006,Chordata,33815,Reptilia,36322,,NA,,NA,137222,NA,NA,NA,individuals,10.618889,50.809723,Bromacker Quarry (upper level of Tambach sandstone),NA,,DE,Thuringia,Gotha,based on nearby landmark,seconds,outcrop,"""...middle part of the Thuringian Forest near the village of Tambach-Dietharz and about 20 km south of the town of Gotha, central Germany.""",gp_mid,21.71,7.41,305,DE,,Tambach,Rotliegend,Tambach-Sandstein,group of beds,,,,,,,NA,"""At the Bromacker quarry site are two superimposed stratigraphic successions that can be characterized by their facies associations and are referred to as the Lower Beds and Upper Beds (Eberth et al. 2000). All the vertebrates from the Bromacker quarry come from the Upper Beds [...]. The vertebrates are almost exclusively restricted to two [... horizons ...] which are separated by 50 cm in a stratigraphic interval of 1.2 m."" (Berman et al., 2001)\r\nThe Tambach Formation is of Artinskian age according to ""Stratigraphische Tabelle von Deutschland 2002"", however, a Kungurian age is proposed by L_tzner (2006) in LITHOLEX stratigraphic online database [http://www.bgr.de/app/LithoLex/gesamt_ausgabe_neu.php5?id=25]","""massive, red-brown, very fine-grained sandstone and siltstone"" (Berman et al., 2001).\r\nFor further details see Eberth et al. (2000).",sandstone,"very fine,brown,red",lithified,,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,"""alluvial paleochannel and sheetflood facies and lacustrine suspension deposits"" (Berman et al., 2001).\r\n""During the time that the Lower and Upper beds were deposited, the Tambach Basin was internally-drained and probably characterized by a wet-and-dry tropical or wetter climate that was hot year-round with seasonal-to-subseasonal cycles of rainfall and drying. [...] In the Bromacker area, the floodbasin was never deeply desiccated or heavily vegetated between flooding events."" Eberth et al. (2000).",macrofossils,,,,,,NA,,"body,permineralized",excellent,,snapshot,,,,,,,NA,,,taxonomic,"bulk,field collection",,all macrofossils,,,,,"MNG = Museum der Natur, Gotha",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Thuringothyris,n. gen.,NA,NA,vertebrate,"J. M_ller, D. S. Berman, and A. C. Henrici, T. Martens, S. S. Sumida. 2006. The Basal Reptile Thuringothyris mahlendorffae (Amniota: Eureptilia) from the Lower Permian of Germany. Journal of Paleontology 80(4):726-739",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,06/12/2008 07:42,26/08/2009 12:13,26922,mahlendorffae,Thuringothyris,28678,n. sp.,290.1,279.3,Artinskian,,8,DE,Thuringothyris mahlendorffae
788639,occ,NA,,80112,,n. gen. Eudibamus n. sp. cursoris,species,137225,,Eudibamus cursoris,NA,species,137225,Berman et al.,2000,Chordata,33815,Reptilia,36322,,NA,Bolosauridae,37510,137224,NA,NA,NA,individuals,10.618889,50.809723,Bromacker Quarry (upper level of Tambach sandstone),NA,,DE,Thuringia,Gotha,based on nearby landmark,seconds,outcrop,"""...middle part of the Thuringian Forest near the village of Tambach-Dietharz and about 20 km south of the town of Gotha, central Germany.""",gp_mid,21.71,7.41,305,DE,,Tambach,Rotliegend,Tambach-Sandstein,group of beds,,,,,,,NA,"""At the Bromacker quarry site are two superimposed stratigraphic successions that can be characterized by their facies associations and are referred to as the Lower Beds and Upper Beds (Eberth et al. 2000). All the vertebrates from the Bromacker quarry come from the Upper Beds [...]. The vertebrates are almost exclusively restricted to two [... horizons ...] which are separated by 50 cm in a stratigraphic interval of 1.2 m."" (Berman et al., 2001)\r\nThe Tambach Formation is of Artinskian age according to ""Stratigraphische Tabelle von Deutschland 2002"", however, a Kungurian age is proposed by L_tzner (2006) in LITHOLEX stratigraphic online database [http://www.bgr.de/app/LithoLex/gesamt_ausgabe_neu.php5?id=25]","""massive, red-brown, very fine-grained sandstone and siltstone"" (Berman et al., 2001).\r\nFor further details see Eberth et al. (2000).",sandstone,"very fine,brown,red",lithified,,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,"""alluvial paleochannel and sheetflood facies and lacustrine suspension deposits"" (Berman et al., 2001).\r\n""During the time that the Lower and Upper beds were deposited, the Tambach Basin was internally-drained and probably characterized by a wet-and-dry tropical or wetter climate that was hot year-round with seasonal-to-subseasonal cycles of rainfall and drying. [...] In the Bromacker area, the floodbasin was never deeply desiccated or heavily vegetated between flooding events."" Eberth et al. (2000).",macrofossils,,,,,,NA,,"body,permineralized",excellent,,snapshot,,,,,,,NA,,,taxonomic,"bulk,field collection",,all macrofossils,,,,,"MNG = Museum der Natur, Gotha",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Eudibamus,n. gen.,NA,NA,vertebrate,"D. S. Berman, R. R. Reisz, and D. Scott, A. C. Henrici, S. S. Sumida, T. Martens. 2000. Early Permian Bipedal Reptile. Science 290:969-972",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,06/12/2008 08:27,26/08/2009 12:13,26922,cursoris,Eudibamus,28679,n. sp.,290.1,279.3,Artinskian,,1,DE,Eudibamus cursoris
788965,occ,NA,,85280,,Cotylorhynchus hancocki,species,122303,,Cotylorhynchus hancocki,NA,species,122303,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38917,NA,NA,NA,individuals,-99.949997,33.652779,Locality KAD (Upper San Angelo Fm.),NA,Driver Ranch,US,Texas,Knox,estimated from map,seconds,outcrop,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork.""\r\nFor details see map on p. 98 in Olson (1962).",gp_mid,-28.82,3.3,101,US,,San Angelo,Pease River,Flowerpot Shale,member,,,,,,,NA,"Olson's Upper San Angelo Fm. and basal Flower Pot Fm. belong to the Flowerpot Shale Member of the Upper San Angelo Fm. (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)","""Sediments are predominantly green and red sandy shales, sandstone beds and lenses, and local lenses of grits and fine conglomerates"".","""shale""","green,red",,sandy,,"""siliciclastic""","lenticular,coarse,very coarse",,,,"""floodplain""",foreland basin,"""The beds appear to represent deposits formed at some distance from major channels of the streams"" except for the coarser clastics.",macrofossils,,,,,,NA,,body,,,,,,,rare,,,NA,,"""Fossils are rare. [...] fragments are the rule""",taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cotylorhynchus,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,09/12/2008 14:36,09/12/2008 16:36,26846,hancocki,Cotylorhynchus,26846,,279.3,268.8,Kungurian,Roadian,3,US,Cotylorhynchus hancocki
788966,occ,NA,,85281,,Cotylorhynchus hancocki,species,122303,,Cotylorhynchus hancocki,NA,species,122303,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38917,NA,NA,NA,individuals,-99.948059,33.642776,Locality KAE (Upper San Angelo Fm.),NA,Driver Ranch,US,Texas,Knox,estimated from map,seconds,outcrop,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork.""\r\nFor details see map on p. 98 in Olson (1962).",gp_mid,-28.83,3.29,101,US,,San Angelo,Pease River,Flowerpot Shale,member,,,,,,,NA,"Olson's Upper San Angelo Fm. and basal Flower Pot Fm. belong to the Flowerpot Shale Member of the Upper San Angelo Fm. (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)","migrating channels, filled with coarser clastics, wedging into sandy shales","""shale""","green,red",,sandy,,"""siliciclastic""",coarse,,,,"""floodplain""",foreland basin,"""The lateral stringers of sandstone and fine conglomerate represent deposits laid down in the off-levee zone. The sandy shales [...] appear to be flood-plain deposits"".",macrofossils,,,,,,NA,,body,poor,,,,,,,,,NA,,"""only scraps of fossils have heen found. A large amount of scrap [...] indicates that at least one fairly complete skeleton was present""",taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cotylorhynchus,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,09/12/2008 15:04,09/12/2008 17:04,26846,hancocki,Cotylorhynchus,26846,,279.3,268.8,Kungurian,Roadian,1,US,Cotylorhynchus hancocki
788969,occ,NA,,79694,,n. gen. Steppesaurus n. sp. gurleyi,species,140370,,Steppesaurus gurleyi,NA,species,140370,Olson and Beerbower,1953,Chordata,33815,Osteichthyes,34881,Theriodontia,56648,Phthinosuchidae,38942,38947,NA,NA,NA,individuals,-99.73333,34.099998,"Locality HA (""Lower San Angelo Fm."")",NA,Pease River,US,Texas,Hardeman,estimated from map,minutes,outcrop,"North of Pease River, 1 mile west of Crowell-Quanah highway",gp_mid,-28.44,3.59,101,US,,San Angelo,Pease River,Flowerpot Shale,,,,,,,,NA,"""15 ft below top of section"" (Olson & Beerbower, 1953)\r\n""Re-examination, after study of the Flower Pot-San Angelo relationship elsewhere, showed without question that Flower Pot assignment is correct. [...] The age of this is herewith corrected from the original San Angelo assignment to Flower Pot."" (Olson, 1962)\r\nThe terrestrial part of Olson's Flower Pot Formation is equivalent to the Flowerpot Member of the Upper San Angelo Formation (see Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80) ",for details see Olson (1962 p. 121 f.),claystone,red or brown,,"silty,sandy",Y,conglomerate,red or brown,,,Y,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,,,,,,,,,,,NA,,,taxonomic,field collection,,,,,E. C. Olson,1950,,,terrestrial,NA,actively mobile,,NA,carnivore,,,hydroxyapatite,,NA,,Steppesaurus,n. gen.,NA,NA,vertebrate,"E. C. Olson and J. R. Beerbower. 1953. The San Angelo Formation, Permian of Texas, and its Vertebrates. Journal of Geology 61(5):389-423",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,09/12/2008 15:51,09/12/2008 17:52,28373,gurleyi,Steppesaurus,28373,n. sp.,279.3,268.8,Kungurian,Roadian,1,US,Steppesaurus gurleyi
788972,occ,NA,,28256,,n. gen. Gymnarthrus n. sp. willoughbyi,species,137382,subjective synonym of,Cardiocephalus sternbergi,NA,species,90715,Case,1910,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37294,NA,NA,NA,specimens,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Gymnarthrus,n. gen.,NA,NA,vertebrate,E. C. Case. 1910. New or little known reptiles and amphibians from the Permian (?) of Texas. Bulletin of the American Museum of Natural History 28:163-181,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,09/12/2008 17:16,10/04/2009 14:19,17702,willoughbyi,Cardiocephalus,28729,n. sp.,279.3,272.3,Kungurian,,1,US,Cardiocephalus willoughbyi
788994,occ,NA,,85292,,Sauropleura n. sp. latithorax,species,137427,subjective synonym of,Isodectes obtusus,NA,species,137370,Cope,1897,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Saurerpetontidae,36980,36983,NA,NA,NA,individuals,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sauropleura,,NA,NA,vertebrate,"E. D. Cope. 1897. On New Paleozoic Vertebrata from Illinois, Ohio and Pennsylvania. Proceedings of the American Philosophical Society 36:71-91",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,10/12/2008 17:15,03/11/2009 10:09,28831,latithorax,Isodectes,28740,n. sp.,311.45,306.95,Westphalian D,,1,US,Isodectes latithorax
788995,occ,NA,,85292,,Dendrerpeton n. sp. obtusum,species,137370,recombined as,Isodectes obtusus,NA,species,137370,Cope,1868,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Saurerpetontidae,36980,36983,NA,NA,NA,individuals,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Dendrerpeton,,NA,NA,vertebrate,E. D. Cope. 1868. Synopsis of the Extinct Batrachia of North America. Proceedings of the Academy of Natural Sciences of Philadelphia 1868:208-221,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,10/12/2008 17:42,03/11/2009 10:09,28831,obtusum,Isodectes,28717,n. sp.,311.45,306.95,Westphalian D,,1,US,Isodectes obtusum
789018,occ,NA,,80110,,Zatracheidae ? indet.,family,37053,,Zatracheidae,NA,family,37053,Vaughn,1964,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,NA,NA,NA,NA,,-110.063057,37.035,Organ Rock Shale,NA,Cutler Group,US,Utah,San Juan,stated in text,seconds,local area,"""... a couple of miles southeast of Monument Pass, in the southern part of of Sec. 17 E. and northern part of sec. 20, T. 43 S., R. 17 E.""",gp_mid,-35.74,6.88,101,US,,Cutler,,Organ Rock Shale,,,,,,,,NA,,"""... the fossils occur in conglomerates and in cross-bedded sandstones immediately above, below and at the lateral edges of the lenses of comglomerate. There are also fossiliferous lenses of cross-bedded sandstone within the bodies of the comglomerates"".",conglomerate,"medium,pebbly",lithified,,Y,sandstone,"""cross stratification""",lithified,,,"""floodplain""",,,macrofossils,,,,,,NA,,"permineralized,coprolite",good,,time-averaged,,,,common,,,NA,,,taxonomic,"surface (in situ),survey of museum collection",UCMP,,,,Prof. Charles C. Camp,1942,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatracheidae,?,NA,NA,,"P. P. Vaughn. 1964. Vertebrates from the Organ Rock Shale of the Cutler Group, Permian of Monument Valley and vicinity, Utah and Arizona. Journal of Paleontology 38(3):567-583",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,11/12/2008 09:39,11/12/2008 11:39,5803,indet.,,5803,,296.4,268,Wolfcamp,Leonard,NA,US, indet.
789021,occ,NA,,28250,,Eocaptorhinus laticeps,species,134878,recombined as,Captorhinus laticeps,NA,species,120324,Heaton,1979,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-99.091667,33.733334,"Mitchell Creek, 29 (Waggoner Ranch Formation)",NA,"Locality 29 (Romer 1928), old Bar X pasture, Timber Creek, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Lucas Ranch",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near Mitchell and Timber Creeks, northeast of Maybelle in the old Bar X pasture."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"". Numbered ""29"" with taxonomic list and on map, but is incorrectly numbered ""28"" in text. Lat long is for area enclosed by Mitchell Creek (W), Big Wichita River (N), Timber Creek (E), and U.S. 277 (S).",gp_mid,-30.29,-0.93,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""It is about 150 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Eocaptorhinus,,NA,NA,vertebrate,"M. J. Heaton. 1979. Cranial Anatomy of Primitive Captorhinid Reptiles from the Late Pennsylvanian and Early Permian, Oklahoma and Texas. Oklahoma Geological Survey, Bulletin 127:1-83",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,11/12/2008 18:59,11/06/2009 05:56,7693,laticeps,Captorhinus,28362,,290.1,272.3,Artinskian,Kungurian,6,US,Captorhinus laticeps
789051,occ,NA,,85299,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Berman,1970,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-99.119446,33.746387,Lueders Fm. Locality 1,NA,Tit Butte and S.W. Butte,US,Texas,Baylor,estimated from map,seconds,small collection,"""1.2 miles southeast of where U. S. Highway 183-283 crosses the Wichita River""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.3,-0.91,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,2 to 3 feet below the Aa2 submember of the Maybelle limestone,"2 layers of graded grain-supported rock composed of vertebrate and invertebrate fossil debris, coprolites, and fecal pellets accompanied with pebbles and cobbles (""6 inch or more in largest diameter"") of unfossiliferous impure lime mudstone and a matrix of sparry calcite, separated by about an inch of unfossiliferous mudstone",grainstone,grading,lithified,,Y,mudstone,,lithified,,,lagoonal/restricted shallow subtidal,foreland basin,"""composition [of the rocks] is interpreted as indicating deposition in relatively calm, shallow, near-shore, marine waters, possibly lagoonal or estuarine, and near the mouth of a freshwater stream""","macrofossils,mesofossils,microfossils",,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"""These deposits [... contain ....] for the most part only broken and disarticulated bone fragments""",taxonomic,"surface (in situ),acetic,field collection",,"all microfossils,some macrofossils",,,,,,"Kissel (2002, Can. J. Earth Sci. 39(9)) suspects the single tooth-rowed captorhinid jaws (UCLA VP 1973-1977) to belong to Captorhinus magnus, but concludes that ""the incomplete nature of the specimens prevents positive assignment.""","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,0,J. Mueller,T. Liebrecht,,12/12/2008 00:07,12/12/2008 02:07,28758,sp.,Trimerorhachis,28758,,290.1,272.3,Artinskian,Kungurian,NA,US,Trimerorhachis sp.
789052,occ,NA,,85299,,Crossotelos annulatus,species,137515,,Crossotelos annulatus,NA,species,137515,Berman,1970,Chordata,33815,Osteichthyes,34881,,NA,Urocordylidae,37270,37271,NA,NA,NA,elements,-99.119446,33.746387,Lueders Fm. Locality 1,NA,Tit Butte and S.W. Butte,US,Texas,Baylor,estimated from map,seconds,small collection,"""1.2 miles southeast of where U. S. Highway 183-283 crosses the Wichita River""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.3,-0.91,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,2 to 3 feet below the Aa2 submember of the Maybelle limestone,"2 layers of graded grain-supported rock composed of vertebrate and invertebrate fossil debris, coprolites, and fecal pellets accompanied with pebbles and cobbles (""6 inch or more in largest diameter"") of unfossiliferous impure lime mudstone and a matrix of sparry calcite, separated by about an inch of unfossiliferous mudstone",grainstone,grading,lithified,,Y,mudstone,,lithified,,,lagoonal/restricted shallow subtidal,foreland basin,"""composition [of the rocks] is interpreted as indicating deposition in relatively calm, shallow, near-shore, marine waters, possibly lagoonal or estuarine, and near the mouth of a freshwater stream""","macrofossils,mesofossils,microfossils",,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"""These deposits [... contain ....] for the most part only broken and disarticulated bone fragments""",taxonomic,"surface (in situ),acetic,field collection",,"all microfossils,some macrofossils",,,,,,"Kissel (2002, Can. J. Earth Sci. 39(9)) suspects the single tooth-rowed captorhinid jaws (UCLA VP 1973-1977) to belong to Captorhinus magnus, but concludes that ""the incomplete nature of the specimens prevents positive assignment.""","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Crossotelos,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,12/12/2008 00:07,12/12/2008 04:37,28758,annulatus,Crossotelos,28758,,290.1,272.3,Artinskian,Kungurian,1,US,Crossotelos annulatus
789053,occ,NA,,85299,,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Berman,1970,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.119446,33.746387,Lueders Fm. Locality 1,NA,Tit Butte and S.W. Butte,US,Texas,Baylor,estimated from map,seconds,small collection,"""1.2 miles southeast of where U. S. Highway 183-283 crosses the Wichita River""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.3,-0.91,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,2 to 3 feet below the Aa2 submember of the Maybelle limestone,"2 layers of graded grain-supported rock composed of vertebrate and invertebrate fossil debris, coprolites, and fecal pellets accompanied with pebbles and cobbles (""6 inch or more in largest diameter"") of unfossiliferous impure lime mudstone and a matrix of sparry calcite, separated by about an inch of unfossiliferous mudstone",grainstone,grading,lithified,,Y,mudstone,,lithified,,,lagoonal/restricted shallow subtidal,foreland basin,"""composition [of the rocks] is interpreted as indicating deposition in relatively calm, shallow, near-shore, marine waters, possibly lagoonal or estuarine, and near the mouth of a freshwater stream""","macrofossils,mesofossils,microfossils",,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"""These deposits [... contain ....] for the most part only broken and disarticulated bone fragments""",taxonomic,"surface (in situ),acetic,field collection",,"all microfossils,some macrofossils",,,,,,"Kissel (2002, Can. J. Earth Sci. 39(9)) suspects the single tooth-rowed captorhinid jaws (UCLA VP 1973-1977) to belong to Captorhinus magnus, but concludes that ""the incomplete nature of the specimens prevents positive assignment.""","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,0,J. Mueller,T. Liebrecht,,12/12/2008 00:07,12/12/2008 02:07,28758,sp.,Diplocaulus,28758,,290.1,272.3,Artinskian,Kungurian,NA,US,Diplocaulus sp.
789054,occ,NA,,85299,,Phlegethontia ? sp.,genus,37259,,Phlegethontia,NA,genus,37259,Berman,1970,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,37259,NA,NA,NA,,-99.119446,33.746387,Lueders Fm. Locality 1,NA,Tit Butte and S.W. Butte,US,Texas,Baylor,estimated from map,seconds,small collection,"""1.2 miles southeast of where U. S. Highway 183-283 crosses the Wichita River""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.3,-0.91,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,2 to 3 feet below the Aa2 submember of the Maybelle limestone,"2 layers of graded grain-supported rock composed of vertebrate and invertebrate fossil debris, coprolites, and fecal pellets accompanied with pebbles and cobbles (""6 inch or more in largest diameter"") of unfossiliferous impure lime mudstone and a matrix of sparry calcite, separated by about an inch of unfossiliferous mudstone",grainstone,grading,lithified,,Y,mudstone,,lithified,,,lagoonal/restricted shallow subtidal,foreland basin,"""composition [of the rocks] is interpreted as indicating deposition in relatively calm, shallow, near-shore, marine waters, possibly lagoonal or estuarine, and near the mouth of a freshwater stream""","macrofossils,mesofossils,microfossils",,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"""These deposits [... contain ....] for the most part only broken and disarticulated bone fragments""",taxonomic,"surface (in situ),acetic,field collection",,"all microfossils,some macrofossils",,,,,,"Kissel (2002, Can. J. Earth Sci. 39(9)) suspects the single tooth-rowed captorhinid jaws (UCLA VP 1973-1977) to belong to Captorhinus magnus, but concludes that ""the incomplete nature of the specimens prevents positive assignment.""","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Phlegethontia,?,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,0,J. Mueller,T. Liebrecht,,12/12/2008 00:07,12/12/2008 02:07,28758,sp.,Phlegethontia,28758,,290.1,272.3,Artinskian,Kungurian,NA,US,Phlegethontia sp.
789055,occ,NA,,85299,,Lysorophus cf. tricarinatus,species,70395,,Lysorophus tricarinatus,NA,species,70395,Berman,1970,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-99.119446,33.746387,Lueders Fm. Locality 1,NA,Tit Butte and S.W. Butte,US,Texas,Baylor,estimated from map,seconds,small collection,"""1.2 miles southeast of where U. S. Highway 183-283 crosses the Wichita River""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.3,-0.91,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,2 to 3 feet below the Aa2 submember of the Maybelle limestone,"2 layers of graded grain-supported rock composed of vertebrate and invertebrate fossil debris, coprolites, and fecal pellets accompanied with pebbles and cobbles (""6 inch or more in largest diameter"") of unfossiliferous impure lime mudstone and a matrix of sparry calcite, separated by about an inch of unfossiliferous mudstone",grainstone,grading,lithified,,Y,mudstone,,lithified,,,lagoonal/restricted shallow subtidal,foreland basin,"""composition [of the rocks] is interpreted as indicating deposition in relatively calm, shallow, near-shore, marine waters, possibly lagoonal or estuarine, and near the mouth of a freshwater stream""","macrofossils,mesofossils,microfossils",,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"""These deposits [... contain ....] for the most part only broken and disarticulated bone fragments""",taxonomic,"surface (in situ),acetic,field collection",,"all microfossils,some macrofossils",,,,,,"Kissel (2002, Can. J. Earth Sci. 39(9)) suspects the single tooth-rowed captorhinid jaws (UCLA VP 1973-1977) to belong to Captorhinus magnus, but concludes that ""the incomplete nature of the specimens prevents positive assignment.""","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,0,J. Mueller,T. Liebrecht,,12/12/2008 00:07,12/12/2008 02:07,28758,tricarinatus,Lysorophus,28758,cf.,290.1,272.3,Artinskian,Kungurian,NA,US,Lysorophus tricarinatus
789056,occ,NA,R,85299,,Gymnarthridae ? sp.,genus,37293,,Gymnarthridae,NA,family,37293,Berman,1970,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,NA,NA,NA,NA,specimens,-99.119446,33.746387,Lueders Fm. Locality 1,NA,Tit Butte and S.W. Butte,US,Texas,Baylor,estimated from map,seconds,small collection,"""1.2 miles southeast of where U. S. Highway 183-283 crosses the Wichita River""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.3,-0.91,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,2 to 3 feet below the Aa2 submember of the Maybelle limestone,"2 layers of graded grain-supported rock composed of vertebrate and invertebrate fossil debris, coprolites, and fecal pellets accompanied with pebbles and cobbles (""6 inch or more in largest diameter"") of unfossiliferous impure lime mudstone and a matrix of sparry calcite, separated by about an inch of unfossiliferous mudstone",grainstone,grading,lithified,,Y,mudstone,,lithified,,,lagoonal/restricted shallow subtidal,foreland basin,"""composition [of the rocks] is interpreted as indicating deposition in relatively calm, shallow, near-shore, marine waters, possibly lagoonal or estuarine, and near the mouth of a freshwater stream""","macrofossils,mesofossils,microfossils",,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"""These deposits [... contain ....] for the most part only broken and disarticulated bone fragments""",taxonomic,"surface (in situ),acetic,field collection",,"all microfossils,some macrofossils",,,,,,"Kissel (2002, Can. J. Earth Sci. 39(9)) suspects the single tooth-rowed captorhinid jaws (UCLA VP 1973-1977) to belong to Captorhinus magnus, but concludes that ""the incomplete nature of the specimens prevents positive assignment.""","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Gymnarthridae,?,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,0,J. Mueller,T. Liebrecht,,12/12/2008 00:07,12/12/2008 02:07,28758,sp.,,28758,,290.1,272.3,Artinskian,Kungurian,5,US, sp.
789056,occ,21176,,85299,,Eocaptorhinus sp.,genus,37499,subjective synonym of,Captorhinus,NA,genus,37497,Heaton,1979,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,specimens,-99.119446,33.746387,Lueders Fm. Locality 1,NA,Tit Butte and S.W. Butte,US,Texas,Baylor,estimated from map,seconds,small collection,"""1.2 miles southeast of where U. S. Highway 183-283 crosses the Wichita River""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.3,-0.91,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,2 to 3 feet below the Aa2 submember of the Maybelle limestone,"2 layers of graded grain-supported rock composed of vertebrate and invertebrate fossil debris, coprolites, and fecal pellets accompanied with pebbles and cobbles (""6 inch or more in largest diameter"") of unfossiliferous impure lime mudstone and a matrix of sparry calcite, separated by about an inch of unfossiliferous mudstone",grainstone,grading,lithified,,Y,mudstone,,lithified,,,lagoonal/restricted shallow subtidal,foreland basin,"""composition [of the rocks] is interpreted as indicating deposition in relatively calm, shallow, near-shore, marine waters, possibly lagoonal or estuarine, and near the mouth of a freshwater stream""","macrofossils,mesofossils,microfossils",,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"""These deposits [... contain ....] for the most part only broken and disarticulated bone fragments""",taxonomic,"surface (in situ),acetic,field collection",,"all microfossils,some macrofossils",,,,,,"Kissel (2002, Can. J. Earth Sci. 39(9)) suspects the single tooth-rowed captorhinid jaws (UCLA VP 1973-1977) to belong to Captorhinus magnus, but concludes that ""the incomplete nature of the specimens prevents positive assignment.""",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Eocaptorhinus,,NA,NA,vertebrate,"M. J. Heaton. 1979. Cranial Anatomy of Primitive Captorhinid Reptiles from the Late Pennsylvanian and Early Permian, Oklahoma and Texas. Oklahoma Geological Survey, Bulletin 127:1-83",315,334,0,J. Mueller,T. Liebrecht,,12/12/2008 00:49,12/12/2008 02:49,28758,sp.,Captorhinus,28362,,290.1,272.3,Artinskian,Kungurian,5,US,Captorhinus sp.
789057,occ,NA,,85299,,Ophiacodon cf. major,species,122336,,Ophiacodon major,NA,species,122336,Berman,1970,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-99.119446,33.746387,Lueders Fm. Locality 1,NA,Tit Butte and S.W. Butte,US,Texas,Baylor,estimated from map,seconds,small collection,"""1.2 miles southeast of where U. S. Highway 183-283 crosses the Wichita River""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.3,-0.91,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,2 to 3 feet below the Aa2 submember of the Maybelle limestone,"2 layers of graded grain-supported rock composed of vertebrate and invertebrate fossil debris, coprolites, and fecal pellets accompanied with pebbles and cobbles (""6 inch or more in largest diameter"") of unfossiliferous impure lime mudstone and a matrix of sparry calcite, separated by about an inch of unfossiliferous mudstone",grainstone,grading,lithified,,Y,mudstone,,lithified,,,lagoonal/restricted shallow subtidal,foreland basin,"""composition [of the rocks] is interpreted as indicating deposition in relatively calm, shallow, near-shore, marine waters, possibly lagoonal or estuarine, and near the mouth of a freshwater stream""","macrofossils,mesofossils,microfossils",,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"""These deposits [... contain ....] for the most part only broken and disarticulated bone fragments""",taxonomic,"surface (in situ),acetic,field collection",,"all microfossils,some macrofossils",,,,,,"Kissel (2002, Can. J. Earth Sci. 39(9)) suspects the single tooth-rowed captorhinid jaws (UCLA VP 1973-1977) to belong to Captorhinus magnus, but concludes that ""the incomplete nature of the specimens prevents positive assignment.""",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,0,J. Mueller,T. Liebrecht,,12/12/2008 00:07,12/12/2008 02:07,28758,major,Ophiacodon,28758,cf.,290.1,272.3,Artinskian,Kungurian,1,US,Ophiacodon major
789058,occ,NA,,85299,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Berman,1970,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.119446,33.746387,Lueders Fm. Locality 1,NA,Tit Butte and S.W. Butte,US,Texas,Baylor,estimated from map,seconds,small collection,"""1.2 miles southeast of where U. S. Highway 183-283 crosses the Wichita River""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.3,-0.91,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,2 to 3 feet below the Aa2 submember of the Maybelle limestone,"2 layers of graded grain-supported rock composed of vertebrate and invertebrate fossil debris, coprolites, and fecal pellets accompanied with pebbles and cobbles (""6 inch or more in largest diameter"") of unfossiliferous impure lime mudstone and a matrix of sparry calcite, separated by about an inch of unfossiliferous mudstone",grainstone,grading,lithified,,Y,mudstone,,lithified,,,lagoonal/restricted shallow subtidal,foreland basin,"""composition [of the rocks] is interpreted as indicating deposition in relatively calm, shallow, near-shore, marine waters, possibly lagoonal or estuarine, and near the mouth of a freshwater stream""","macrofossils,mesofossils,microfossils",,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"""These deposits [... contain ....] for the most part only broken and disarticulated bone fragments""",taxonomic,"surface (in situ),acetic,field collection",,"all microfossils,some macrofossils",,,,,,"Kissel (2002, Can. J. Earth Sci. 39(9)) suspects the single tooth-rowed captorhinid jaws (UCLA VP 1973-1977) to belong to Captorhinus magnus, but concludes that ""the incomplete nature of the specimens prevents positive assignment.""",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,0,J. Mueller,T. Liebrecht,,12/12/2008 00:07,12/12/2008 02:07,28758,sp.,Dimetrodon,28758,,290.1,272.3,Artinskian,Kungurian,NA,US,Dimetrodon sp.
789059,occ,NA,,85299,,Tetrapoda indet.,unranked clade,137279,,Tetrapoda,NA,unranked clade,53190,Berman,1970,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,specimens,-99.119446,33.746387,Lueders Fm. Locality 1,NA,Tit Butte and S.W. Butte,US,Texas,Baylor,estimated from map,seconds,small collection,"""1.2 miles southeast of where U. S. Highway 183-283 crosses the Wichita River""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.3,-0.91,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,2 to 3 feet below the Aa2 submember of the Maybelle limestone,"2 layers of graded grain-supported rock composed of vertebrate and invertebrate fossil debris, coprolites, and fecal pellets accompanied with pebbles and cobbles (""6 inch or more in largest diameter"") of unfossiliferous impure lime mudstone and a matrix of sparry calcite, separated by about an inch of unfossiliferous mudstone",grainstone,grading,lithified,,Y,mudstone,,lithified,,,lagoonal/restricted shallow subtidal,foreland basin,"""composition [of the rocks] is interpreted as indicating deposition in relatively calm, shallow, near-shore, marine waters, possibly lagoonal or estuarine, and near the mouth of a freshwater stream""","macrofossils,mesofossils,microfossils",,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"""These deposits [... contain ....] for the most part only broken and disarticulated bone fragments""",taxonomic,"surface (in situ),acetic,field collection",,"all microfossils,some macrofossils",,,,,,"Kissel (2002, Can. J. Earth Sci. 39(9)) suspects the single tooth-rowed captorhinid jaws (UCLA VP 1973-1977) to belong to Captorhinus magnus, but concludes that ""the incomplete nature of the specimens prevents positive assignment.""","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tetrapoda,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,12/12/2008 00:07,12/12/2008 02:07,28758,indet.,,28758,,290.1,272.3,Artinskian,Kungurian,1,US, indet.
789060,occ,NA,,85300,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Berman,1970,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-99.145836,33.751389,Lueders Fm. Locality 2,NA,Lake Kemp dam,US,Texas,Baylor,estimated from map,seconds,small collection,"""a bluff along the shore of Lake Kemp, beginning close to the southern end of the Lake Kemp dam.""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.32,-0.89,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,8 feet below the Aa2 submember of the Maybelle limestone,"""The fossiliferous layer found at site 2 is a gray, clay-pebble conglomerate. The pebbles are generally under 0.5 inch in diameter and are surrounded by a gray argillaceous matrix.""",conglomerate,"pebbly,gray",,argillaceous,Y,,,,,,shallow subtidal indet.,foreland basin,"""This layer is hesistantly suspected of having been deposited in a near-shore, marine situation""","macrofossils,mesofossils",,,,,,NA,,body,variable,,snapshot,,,,common,,,NA,,,taxonomic,"surface (in situ),acetic,field collection",,some macrofossils,,,,,,"UCLA VP 2030 was originally identified as Captorhinus aguti by Berman (1970), based on Seltin's (1959, Field. Geol.) conclusion that Captorhinus is a monospecific genus. Given that currently there are three recognized species of Captorhinus, the specimen is left without assignment to a species in the taxonomic list. ","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,12/12/2008 00:08,24/03/2010 11:01,28758,sp.,Trimerorhachis,28758,,290.1,272.3,Artinskian,Kungurian,NA,US,Trimerorhachis sp.
789061,occ,NA,,85300,,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Berman,1970,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.145836,33.751389,Lueders Fm. Locality 2,NA,Lake Kemp dam,US,Texas,Baylor,estimated from map,seconds,small collection,"""a bluff along the shore of Lake Kemp, beginning close to the southern end of the Lake Kemp dam.""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.32,-0.89,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,8 feet below the Aa2 submember of the Maybelle limestone,"""The fossiliferous layer found at site 2 is a gray, clay-pebble conglomerate. The pebbles are generally under 0.5 inch in diameter and are surrounded by a gray argillaceous matrix.""",conglomerate,"pebbly,gray",,argillaceous,Y,,,,,,shallow subtidal indet.,foreland basin,"""This layer is hesistantly suspected of having been deposited in a near-shore, marine situation""","macrofossils,mesofossils",,,,,,NA,,body,variable,,snapshot,,,,common,,,NA,,,taxonomic,"surface (in situ),acetic,field collection",,some macrofossils,,,,,,"UCLA VP 2030 was originally identified as Captorhinus aguti by Berman (1970), based on Seltin's (1959, Field. Geol.) conclusion that Captorhinus is a monospecific genus. Given that currently there are three recognized species of Captorhinus, the specimen is left without assignment to a species in the taxonomic list. ","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,12/12/2008 00:08,24/03/2010 11:01,28758,sp.,Diplocaulus,28758,,290.1,272.3,Artinskian,Kungurian,NA,US,Diplocaulus sp.
789062,occ,NA,,85300,,Phlegethontia ? sp.,genus,37259,,Phlegethontia,NA,genus,37259,Berman,1970,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,37259,NA,NA,NA,,-99.145836,33.751389,Lueders Fm. Locality 2,NA,Lake Kemp dam,US,Texas,Baylor,estimated from map,seconds,small collection,"""a bluff along the shore of Lake Kemp, beginning close to the southern end of the Lake Kemp dam.""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.32,-0.89,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,8 feet below the Aa2 submember of the Maybelle limestone,"""The fossiliferous layer found at site 2 is a gray, clay-pebble conglomerate. The pebbles are generally under 0.5 inch in diameter and are surrounded by a gray argillaceous matrix.""",conglomerate,"pebbly,gray",,argillaceous,Y,,,,,,shallow subtidal indet.,foreland basin,"""This layer is hesistantly suspected of having been deposited in a near-shore, marine situation""","macrofossils,mesofossils",,,,,,NA,,body,variable,,snapshot,,,,common,,,NA,,,taxonomic,"surface (in situ),acetic,field collection",,some macrofossils,,,,,,"UCLA VP 2030 was originally identified as Captorhinus aguti by Berman (1970), based on Seltin's (1959, Field. Geol.) conclusion that Captorhinus is a monospecific genus. Given that currently there are three recognized species of Captorhinus, the specimen is left without assignment to a species in the taxonomic list. ","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Phlegethontia,?,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,12/12/2008 00:08,24/03/2010 11:01,28758,sp.,Phlegethontia,28758,,290.1,272.3,Artinskian,Kungurian,NA,US,Phlegethontia sp.
789063,occ,NA,,85300,,Lysorophus cf. tricarinatus,species,70395,,Lysorophus tricarinatus,NA,species,70395,Berman,1970,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-99.145836,33.751389,Lueders Fm. Locality 2,NA,Lake Kemp dam,US,Texas,Baylor,estimated from map,seconds,small collection,"""a bluff along the shore of Lake Kemp, beginning close to the southern end of the Lake Kemp dam.""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.32,-0.89,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,8 feet below the Aa2 submember of the Maybelle limestone,"""The fossiliferous layer found at site 2 is a gray, clay-pebble conglomerate. The pebbles are generally under 0.5 inch in diameter and are surrounded by a gray argillaceous matrix.""",conglomerate,"pebbly,gray",,argillaceous,Y,,,,,,shallow subtidal indet.,foreland basin,"""This layer is hesistantly suspected of having been deposited in a near-shore, marine situation""","macrofossils,mesofossils",,,,,,NA,,body,variable,,snapshot,,,,common,,,NA,,,taxonomic,"surface (in situ),acetic,field collection",,some macrofossils,,,,,,"UCLA VP 2030 was originally identified as Captorhinus aguti by Berman (1970), based on Seltin's (1959, Field. Geol.) conclusion that Captorhinus is a monospecific genus. Given that currently there are three recognized species of Captorhinus, the specimen is left without assignment to a species in the taxonomic list. ","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,12/12/2008 00:08,24/03/2010 11:01,28758,tricarinatus,Lysorophus,28758,cf.,290.1,272.3,Artinskian,Kungurian,NA,US,Lysorophus tricarinatus
789064,occ,NA,,85300,,Captorhinus sp.,genus,37497,,Captorhinus,NA,genus,37497,Berman,1970,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,elements,-99.145836,33.751389,Lueders Fm. Locality 2,NA,Lake Kemp dam,US,Texas,Baylor,estimated from map,seconds,small collection,"""a bluff along the shore of Lake Kemp, beginning close to the southern end of the Lake Kemp dam.""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.32,-0.89,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,8 feet below the Aa2 submember of the Maybelle limestone,"""The fossiliferous layer found at site 2 is a gray, clay-pebble conglomerate. The pebbles are generally under 0.5 inch in diameter and are surrounded by a gray argillaceous matrix.""",conglomerate,"pebbly,gray",,argillaceous,Y,,,,,,shallow subtidal indet.,foreland basin,"""This layer is hesistantly suspected of having been deposited in a near-shore, marine situation""","macrofossils,mesofossils",,,,,,NA,,body,variable,,snapshot,,,,common,,,NA,,,taxonomic,"surface (in situ),acetic,field collection",,some macrofossils,,,,,,"UCLA VP 2030 was originally identified as Captorhinus aguti by Berman (1970), based on Seltin's (1959, Field. Geol.) conclusion that Captorhinus is a monospecific genus. Given that currently there are three recognized species of Captorhinus, the specimen is left without assignment to a species in the taxonomic list. ",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,12/12/2008 00:08,24/03/2010 11:01,28758,sp.,Captorhinus,28758,,290.1,272.3,Artinskian,Kungurian,1,US,Captorhinus sp.
789065,occ,NA,,85300,,Ophiacodon cf. major,species,122336,,Ophiacodon major,NA,species,122336,Berman,1970,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,elements,-99.145836,33.751389,Lueders Fm. Locality 2,NA,Lake Kemp dam,US,Texas,Baylor,estimated from map,seconds,small collection,"""a bluff along the shore of Lake Kemp, beginning close to the southern end of the Lake Kemp dam.""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.32,-0.89,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,8 feet below the Aa2 submember of the Maybelle limestone,"""The fossiliferous layer found at site 2 is a gray, clay-pebble conglomerate. The pebbles are generally under 0.5 inch in diameter and are surrounded by a gray argillaceous matrix.""",conglomerate,"pebbly,gray",,argillaceous,Y,,,,,,shallow subtidal indet.,foreland basin,"""This layer is hesistantly suspected of having been deposited in a near-shore, marine situation""","macrofossils,mesofossils",,,,,,NA,,body,variable,,snapshot,,,,common,,,NA,,,taxonomic,"surface (in situ),acetic,field collection",,some macrofossils,,,,,,"UCLA VP 2030 was originally identified as Captorhinus aguti by Berman (1970), based on Seltin's (1959, Field. Geol.) conclusion that Captorhinus is a monospecific genus. Given that currently there are three recognized species of Captorhinus, the specimen is left without assignment to a species in the taxonomic list. ",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,12/12/2008 00:08,24/03/2010 11:01,28758,major,Ophiacodon,28758,cf.,290.1,272.3,Artinskian,Kungurian,1,US,Ophiacodon major
789066,occ,NA,,85300,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Berman,1970,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.145836,33.751389,Lueders Fm. Locality 2,NA,Lake Kemp dam,US,Texas,Baylor,estimated from map,seconds,small collection,"""a bluff along the shore of Lake Kemp, beginning close to the southern end of the Lake Kemp dam.""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.32,-0.89,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,8 feet below the Aa2 submember of the Maybelle limestone,"""The fossiliferous layer found at site 2 is a gray, clay-pebble conglomerate. The pebbles are generally under 0.5 inch in diameter and are surrounded by a gray argillaceous matrix.""",conglomerate,"pebbly,gray",,argillaceous,Y,,,,,,shallow subtidal indet.,foreland basin,"""This layer is hesistantly suspected of having been deposited in a near-shore, marine situation""","macrofossils,mesofossils",,,,,,NA,,body,variable,,snapshot,,,,common,,,NA,,,taxonomic,"surface (in situ),acetic,field collection",,some macrofossils,,,,,,"UCLA VP 2030 was originally identified as Captorhinus aguti by Berman (1970), based on Seltin's (1959, Field. Geol.) conclusion that Captorhinus is a monospecific genus. Given that currently there are three recognized species of Captorhinus, the specimen is left without assignment to a species in the taxonomic list. ",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,12/12/2008 00:08,24/03/2010 11:01,28758,sp.,Dimetrodon,28758,,290.1,272.3,Artinskian,Kungurian,NA,US,Dimetrodon sp.
789067,occ,NA,,85301,,Eryops megacephalus,species,70397,,Eryops megacephalus,NA,species,70397,Berman,1970,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,individuals,-99.138885,33.784168,Lueders Fm. Locality 3,NA,,US,Texas,Baylor,estimated from map,seconds,small collection,"""2 miles north and 1 mile east of where U. S. Highway 183-283 crosses the Wichita River""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.3,-0.87,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,36 feet below the Aa2 submember of the Maybelle limestone,"""The deposit [...] consists mostly of light-gray to blue mudstones. [...] A dark-brown, stream-channel conglomerate lies at the base of and lateral to the deposit.""",mudstone,"gray,blue",,,Y,conglomerate,brown,,,,lacustrine indet.,foreland basin,"""The sediments of the fossiliferous deposit at site 3 is [...] referred to as a pond or lake deposit. [...] As far as known this is the first genuinely terrestrial fossiliferous deposit yet described in the Lueders Formation.""","macrofossils,mesofossils",,,,,,NA,,"body,coprolite",,,snapshot,,,,,,,NA,,,taxonomic,"surface (in situ),acetic,field collection",,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,12/12/2008 00:08,12/12/2008 02:10,28758,megacephalus,Eryops,28758,,290.1,272.3,Artinskian,Kungurian,1,US,Eryops megacephalus
789068,occ,NA,,85301,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Berman,1970,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,elements,-99.138885,33.784168,Lueders Fm. Locality 3,NA,,US,Texas,Baylor,estimated from map,seconds,small collection,"""2 miles north and 1 mile east of where U. S. Highway 183-283 crosses the Wichita River""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.3,-0.87,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,36 feet below the Aa2 submember of the Maybelle limestone,"""The deposit [...] consists mostly of light-gray to blue mudstones. [...] A dark-brown, stream-channel conglomerate lies at the base of and lateral to the deposit.""",mudstone,"gray,blue",,,Y,conglomerate,brown,,,,lacustrine indet.,foreland basin,"""The sediments of the fossiliferous deposit at site 3 is [...] referred to as a pond or lake deposit. [...] As far as known this is the first genuinely terrestrial fossiliferous deposit yet described in the Lueders Formation.""","macrofossils,mesofossils",,,,,,NA,,"body,coprolite",,,snapshot,,,,,,,NA,,,taxonomic,"surface (in situ),acetic,field collection",,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,12/12/2008 00:08,12/12/2008 02:10,28758,sp.,Diadectes,28758,,290.1,272.3,Artinskian,Kungurian,1,US,Diadectes sp.
789069,occ,NA,,85301,,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Berman,1970,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.138885,33.784168,Lueders Fm. Locality 3,NA,,US,Texas,Baylor,estimated from map,seconds,small collection,"""2 miles north and 1 mile east of where U. S. Highway 183-283 crosses the Wichita River""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.3,-0.87,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,36 feet below the Aa2 submember of the Maybelle limestone,"""The deposit [...] consists mostly of light-gray to blue mudstones. [...] A dark-brown, stream-channel conglomerate lies at the base of and lateral to the deposit.""",mudstone,"gray,blue",,,Y,conglomerate,brown,,,,lacustrine indet.,foreland basin,"""The sediments of the fossiliferous deposit at site 3 is [...] referred to as a pond or lake deposit. [...] As far as known this is the first genuinely terrestrial fossiliferous deposit yet described in the Lueders Formation.""","macrofossils,mesofossils",,,,,,NA,,"body,coprolite",,,snapshot,,,,,,,NA,,,taxonomic,"surface (in situ),acetic,field collection",,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,0,J. Mueller,T. Liebrecht,,12/12/2008 00:08,12/12/2008 02:08,28758,sp.,Diplocaulus,28758,,290.1,272.3,Artinskian,Kungurian,NA,US,Diplocaulus sp.
789070,occ,NA,,85301,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Berman,1970,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.138885,33.784168,Lueders Fm. Locality 3,NA,,US,Texas,Baylor,estimated from map,seconds,small collection,"""2 miles north and 1 mile east of where U. S. Highway 183-283 crosses the Wichita River""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.3,-0.87,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,36 feet below the Aa2 submember of the Maybelle limestone,"""The deposit [...] consists mostly of light-gray to blue mudstones. [...] A dark-brown, stream-channel conglomerate lies at the base of and lateral to the deposit.""",mudstone,"gray,blue",,,Y,conglomerate,brown,,,,lacustrine indet.,foreland basin,"""The sediments of the fossiliferous deposit at site 3 is [...] referred to as a pond or lake deposit. [...] As far as known this is the first genuinely terrestrial fossiliferous deposit yet described in the Lueders Formation.""","macrofossils,mesofossils",,,,,,NA,,"body,coprolite",,,snapshot,,,,,,,NA,,,taxonomic,"surface (in situ),acetic,field collection",,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,0,J. Mueller,T. Liebrecht,,12/12/2008 00:08,12/12/2008 02:08,28758,sp.,Dimetrodon,28758,,290.1,272.3,Artinskian,Kungurian,NA,US,Dimetrodon sp.
789071,occ,NA,,85301,,Edaphosaurus aff. cruciger,species,346264,,Edaphosaurus cruciger,NA,species,138134,Berman,1970,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,specimens,-99.138885,33.784168,Lueders Fm. Locality 3,NA,,US,Texas,Baylor,estimated from map,seconds,small collection,"""2 miles north and 1 mile east of where U. S. Highway 183-283 crosses the Wichita River""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.3,-0.87,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,36 feet below the Aa2 submember of the Maybelle limestone,"""The deposit [...] consists mostly of light-gray to blue mudstones. [...] A dark-brown, stream-channel conglomerate lies at the base of and lateral to the deposit.""",mudstone,"gray,blue",,,Y,conglomerate,brown,,,,lacustrine indet.,foreland basin,"""The sediments of the fossiliferous deposit at site 3 is [...] referred to as a pond or lake deposit. [...] As far as known this is the first genuinely terrestrial fossiliferous deposit yet described in the Lueders Formation.""","macrofossils,mesofossils",,,,,,NA,,"body,coprolite",,,snapshot,,,,,,,NA,,,taxonomic,"surface (in situ),acetic,field collection",,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,"D. S. Berman. 1970. Vertebrate Fossils from the Lueders Formation, Lower Permian of North-Central Texas. University of California Publications in Geological Sciences 86:1-61",315,334,0,J. Mueller,T. Liebrecht,,12/12/2008 00:08,12/12/2008 02:08,28758,cruciger,Edaphosaurus,28758,aff.,290.1,272.3,Artinskian,Kungurian,2,US,Edaphosaurus cruciger
789104,occ,NA,,67862,,Captorhinus n. sp. magnus,species,134993,,Captorhinus magnus,NA,species,134993,Kissel et al.,2002,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,"paleoentomology,vertebrate","R. A. Kissel, D. W. Dilkes, and R. R. Reisz. 2002. Captorhinus magnus, a new captorhinid (Amniota: Eureptilia) from the Lower Permian of Oklahoma, with new evidence on the homology of the astragalus. Canadian Journal of Earth Sciences 39(9):1363-1372",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,12/12/2008 08:48,29/07/2009 11:27,19393,magnus,Captorhinus,28381,n. sp.,290.1,268,Leonard,,6,US,Captorhinus magnus
789379,occ,NA,,80833,,n. gen. Ophiacodon n. sp. mirus,species,123418,,Ophiacodon mirus,NA,species,123418,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-106.671387,36.184723,Baldwin bonebed,85339,"type horizon of Sphenacodon ferox & Ophiacodon mirus, Arroya de Agua",US,New Mexico,Rio Arriba,estimated from map,seconds,small collection,"""about a mile and a half above the confluence of the Poleo creek with the Puerco, and near the Mexican village of Arroya de Agua."" (Williston, 1916)\r\nApparently is what Williston (1916) calls the Poleo Creek a northwestern headstream of the Rio Puerco (see Williston & Case, 1913 p. 1 fig. 1, Inst. Washington Publ. 181), however, in modern maps a southwestern headstream is designated as Poleo Creek. ",gp_mid,-34.08,4.56,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,D. A. Baldwin,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,n. gen.,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,15/12/2008 07:55,08/07/2016 10:29,27105,mirus,Ophiacodon,27105,n. sp.,296.4,268,Wolfcamp,,1,US,Ophiacodon mirus
789382,occ,NA,,85337,,Ophiacodon mirus,species,123418,,Ophiacodon mirus,NA,species,123418,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-106.673889,36.178612,Miller Bonebed,85339,Bone Quarry; Arroya de Agua; Poleo Creek,US,New Mexico,Rio Arriba,estimated from map,seconds,small collection,"1 mile ""above the confluence of the Poleo creek with the Puerco, and near the Mexican village of Arroya de Agua."" (Williston, 1916)\r\nApparently is what Williston (1916) calls the Poleo Creek a northwestern headstream of the Rio Puerco (see Williston & Case, 1913 p. 1 fig. 1, Carnegie Inst. Washington Publ. 181), however, in modern maps a southwestern headstream is designated as Poleo Creek. ",gp_mid,-34.08,4.56,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,"""same horizon"" as the Baldwin Bonebed (see coll. 80833)","""hard, dark brown clay""",claystone,brown,lithified,,Y,sandstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"""numerous isolated bones of Sphenacodon and Ophiacodon Marsh, together with a very perfect skeleton of the latter, were obtained"" (Williston, 1916)",taxonomic,"bulk,mechanical",,,,,"S. W. Williston, E. C. Case, P. Miller",1911,"for details see Williston & Case (1913 p. 38, Carnegie Inst. Washington Publ. 181)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,15/12/2008 09:08,11/01/2009 13:06,27105,mirus,Ophiacodon,27105,,296.4,268,Wolfcamp,,2,US,Ophiacodon mirus
789387,occ,NA,R,85339,,Captorhinus aguti,species,90718,,Captorhinus aguti,NA,species,134887,Fox and Bowman,1966,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-106.677498,36.181389,Poleo Creek,NA,"Arroyo del Agua, Arroyo de Agua, Arroya de Agua",US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"Poleo Creek is a headstream of the Rio Puerco River, whose lower reach cuts through Permian strata near Arroyo del Agua, Rio Arriba Co., NM.",gp_mid,-34.08,4.56,101,US,FED,Abo/Cutler,,,formation,,,,,,,NA,,,not reported,,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,"R. C. Fox and M. C. Bowman. 1966. Osteology and Relationships of Captorhinus aguti (Cope) (Reptilia: Captorhinomorpha). The University of Kansas Paleontological Contributions, Series Vertebrata 11:1-79",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,15/12/2008 09:52,21/01/2009 16:06,28784,aguti,Captorhinus,28784,,296.4,268,Wolfcamp,,1,US,Captorhinus aguti
789387,occ,21185,,85339,,Captorhinidae indet.,family,37495,,Captorhinidae,NA,family,37495,Clark and Carroll,1973,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,NA,NA,NA,NA,individuals,-106.677498,36.181389,Poleo Creek,NA,"Arroyo del Agua, Arroyo de Agua, Arroya de Agua",US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"Poleo Creek is a headstream of the Rio Puerco River, whose lower reach cuts through Permian strata near Arroyo del Agua, Rio Arriba Co., NM.",gp_mid,-34.08,4.56,101,US,FED,Abo/Cutler,,,formation,,,,,,,NA,,,not reported,,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinidae,,NA,NA,vertebrate,J. Clark and R. L. Carroll. 1973. Romeriid Reptiles from the Lower Permian. Bulletin of the Museum of Comparative Zoology 144(5):353-407,315,334,0,J. Mueller,T. Liebrecht,,15/12/2008 10:34,15/12/2008 12:34,28784,indet.,,28415,,296.4,268,Wolfcamp,,1,US, indet.
789389,occ,NA,,28250,,Captorhinus aguti,species,90718,,Captorhinus aguti,NA,species,134887,Fox and Bowman,1966,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-99.091667,33.733334,"Mitchell Creek, 29 (Waggoner Ranch Formation)",NA,"Locality 29 (Romer 1928), old Bar X pasture, Timber Creek, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Lucas Ranch",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near Mitchell and Timber Creeks, northeast of Maybelle in the old Bar X pasture."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"". Numbered ""29"" with taxonomic list and on map, but is incorrectly numbered ""28"" in text. Lat long is for area enclosed by Mitchell Creek (W), Big Wichita River (N), Timber Creek (E), and U.S. 277 (S).",gp_mid,-30.29,-0.93,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""It is about 150 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,"R. C. Fox and M. C. Bowman. 1966. Osteology and Relationships of Captorhinus aguti (Cope) (Reptilia: Captorhinomorpha). The University of Kansas Paleontological Contributions, Series Vertebrata 11:1-79",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,15/12/2008 12:14,11/06/2009 05:56,7693,aguti,Captorhinus,28784,,290.1,272.3,Artinskian,Kungurian,3,US,Captorhinus aguti
789394,occ,NA,R,85341,,Captorhinus aguti,species,90718,,Captorhinus aguti,NA,species,134887,Fox and Bowman,1966,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-99.01667,33.75,Wichita River near Vernon Crossing,NA,,US,Texas,Baylor,estimated from map,minutes,small collection,"""Near Vernon Crossing, Wichita River, Baylor County, Texas"" (Clark & Carroll, 1973). There is no such place designated on the 7.5' quadrangle maps. Polar coordinates are for intersection of outcrop of Bead Mt. Limestone (top of ""Belle Plains Fm."") and Wichita River according to map (fig. 23) in Clark & Carroll (1973). ",gp_mid,-30.23,-0.95,101,US,,Petrolia/Waggoner Ranch,Wichita,,bed,,,,,,,NA,"Informations in the literature on the stratigraphic position of that collection are contratictory: Fox & Bowman (1966) and Heaton (1979) say Belle Plains Formation, Clark and Carroll (1973) say Clyde Formation. Because the exact geographic position of the locality is stated nowhere, stratigraphy cannot be clarified by using a geological map. \r\nPetrolia Fm. is formerly known as Belle Plains Fm. Waggoner Ranch Fm. is formerly known as Clyde Fm. (see Hentz, 1988, The University of Texas at Austin Bureau of Economic Geology, Report of Investigations, 170, pp. 1-55)",,not reported,,,,,,"red,blue",,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,"R. C. Fox and M. C. Bowman. 1966. Osteology and Relationships of Captorhinus aguti (Cope) (Reptilia: Captorhinomorpha). The University of Kansas Paleontological Contributions, Series Vertebrata 11:1-79",315,334,0,J. Mueller,T. Liebrecht,,15/12/2008 13:59,15/12/2008 15:59,28784,aguti,Captorhinus,28784,,290.1,272.3,Artinskian,Kungurian,1,US,Captorhinus aguti
789394,occ,21186,R,85341,,"""Captorhinus"" laticeps",species,134970,,Captorhinus laticeps,NA,species,120324,Clark and Carroll,1973,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-99.01667,33.75,Wichita River near Vernon Crossing,NA,,US,Texas,Baylor,estimated from map,minutes,small collection,"""Near Vernon Crossing, Wichita River, Baylor County, Texas"" (Clark & Carroll, 1973). There is no such place designated on the 7.5' quadrangle maps. Polar coordinates are for intersection of outcrop of Bead Mt. Limestone (top of ""Belle Plains Fm."") and Wichita River according to map (fig. 23) in Clark & Carroll (1973). ",gp_mid,-30.23,-0.95,101,US,,Petrolia/Waggoner Ranch,Wichita,,bed,,,,,,,NA,"Informations in the literature on the stratigraphic position of that collection are contratictory: Fox & Bowman (1966) and Heaton (1979) say Belle Plains Formation, Clark and Carroll (1973) say Clyde Formation. Because the exact geographic position of the locality is stated nowhere, stratigraphy cannot be clarified by using a geological map. \r\nPetrolia Fm. is formerly known as Belle Plains Fm. Waggoner Ranch Fm. is formerly known as Clyde Fm. (see Hentz, 1988, The University of Texas at Austin Bureau of Economic Geology, Report of Investigations, 170, pp. 1-55)",,not reported,,,,,,"red,blue",,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,"""",NA,NA,vertebrate,J. Clark and R. L. Carroll. 1973. Romeriid Reptiles from the Lower Permian. Bulletin of the Museum of Comparative Zoology 144(5):353-407,315,334,0,J. Mueller,T. Liebrecht,,15/12/2008 14:04,15/12/2008 16:04,28784,laticeps,Captorhinus,28415,,290.1,272.3,Artinskian,Kungurian,1,US,Captorhinus laticeps
789394,occ,21187,,85341,,Protocaptorhinus cf. pricei,species,135429,,Protocaptorhinus pricei,NA,species,135429,Heaton,1979,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37505,NA,NA,NA,individuals,-99.01667,33.75,Wichita River near Vernon Crossing,NA,,US,Texas,Baylor,estimated from map,minutes,small collection,"""Near Vernon Crossing, Wichita River, Baylor County, Texas"" (Clark & Carroll, 1973). There is no such place designated on the 7.5' quadrangle maps. Polar coordinates are for intersection of outcrop of Bead Mt. Limestone (top of ""Belle Plains Fm."") and Wichita River according to map (fig. 23) in Clark & Carroll (1973). ",gp_mid,-30.23,-0.95,101,US,,Petrolia/Waggoner Ranch,Wichita,,bed,,,,,,,NA,"Informations in the literature on the stratigraphic position of that collection are contratictory: Fox & Bowman (1966) and Heaton (1979) say Belle Plains Formation, Clark and Carroll (1973) say Clyde Formation. Because the exact geographic position of the locality is stated nowhere, stratigraphy cannot be clarified by using a geological map. \r\nPetrolia Fm. is formerly known as Belle Plains Fm. Waggoner Ranch Fm. is formerly known as Clyde Fm. (see Hentz, 1988, The University of Texas at Austin Bureau of Economic Geology, Report of Investigations, 170, pp. 1-55)",,not reported,,,,,,"red,blue",,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Protocaptorhinus,,NA,NA,vertebrate,"M. J. Heaton. 1979. Cranial Anatomy of Primitive Captorhinid Reptiles from the Late Pennsylvanian and Early Permian, Oklahoma and Texas. Oklahoma Geological Survey, Bulletin 127:1-83",315,334,0,J. Mueller,T. Liebrecht,,15/12/2008 14:16,15/12/2008 16:16,28784,pricei,Protocaptorhinus,28362,cf.,290.1,272.3,Artinskian,Kungurian,1,US,Protocaptorhinus pricei
789396,occ,NA,,85342,,Captorhinus aguti,species,90718,,Captorhinus aguti,NA,species,134887,Fox and Bowman,1966,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-99.316666,33.75,Big Wichita River (Arroyo Fm.),NA,,US,Texas,Baylor,estimated from map,minutes,small collection,"""North side Big Wichita River, Baylor County, Texas""",gp_mid,-29.01,1.8,101,US,,Arroyo,Clear Fork,,bed,,,,,,,NA,,,"""shale""",gray,,,Y,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,medium,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,"R. C. Fox and M. C. Bowman. 1966. Osteology and Relationships of Captorhinus aguti (Cope) (Reptilia: Captorhinomorpha). The University of Kansas Paleontological Contributions, Series Vertebrata 11:1-79",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,15/12/2008 15:34,18/03/2016 11:30,28784,aguti,Captorhinus,28784,,279.3,272.3,Kungurian,,1,US,Captorhinus aguti
789397,occ,NA,,28264,,Labidosaurus hamatus,species,134918,,Labidosaurus hamatus,NA,species,134856,Williston,1917,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,specimens,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,vertebrate,"S. W. Williston. 1917. Labidosaurus Cope, a Lower Permian cotylosaur reptile from Texas. Journal of Geology 25(4):309-321",315,334,14,J. Mueller,T. Liebrecht,M. Carrano,15/12/2008 16:29,22/04/2015 13:12,9228,hamatus,Labidosaurus,55127,,279.3,272.3,Kungurian,,6,US,Labidosaurus hamatus
789398,occ,NA,,28264,,Captorhinus aguti,species,90718,,Captorhinus aguti,NA,species,134887,Seltin,1959,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,R. J. Seltin. 1959. A review of the family Captorhinidae. Fieldiana: Geology 10(34):461-509,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,15/12/2008 16:29,22/04/2015 13:12,9228,aguti,Captorhinus,28359,,279.3,272.3,Kungurian,,2,US,Captorhinus aguti
789399,occ,NA,,28270,,Theropleura sp.,genus,138047,subjective synonym of,Ophiacodon,NA,genus,38888,Romer,1928,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-99.312775,33.714722,"Hog Creek, 39 (Arroyo Formation)",NA,"Locality 39 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""The next creek west of Brush Creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Hog Creek.",gp_mid,-29.02,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,15/12/2008 16:39,13/07/2016 06:39,7693,sp.,Ophiacodon,7693,,279.3,272.3,Kungurian,,5,US,Ophiacodon sp.
789473,occ,NA,,85361,,Captorhinikos n. sp. chozaensis,species,120856,,Captorhinikos chozaensis,NA,species,120856,Olson,1954,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37496,NA,NA,NA,individuals,-99.558334,33.816666,Locality FA - Green Nodule Site,NA,,US,Texas,Foard,estimated from map,seconds,outcrop,"southeastern corner of Foard Co.; Lat long estimation is based on map in fig. 1 in Olson (1951, J. Geol. 59(2), pp. 178-181) ",gp_mid,-30.21,0,101,US,,Choza,Clear Fork,,,,,,,,,NA,"""Middle of lower part of Choza Formation""",,not reported,,,,Y,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinikos,,NA,NA,vertebrate,E. C. Olson. 1954. Fauna of the Vale and Choza: 9. Captorhinomorpha. Fieldiana: Geology 10(19):211-218,315,334,0,J. Mueller,T. Liebrecht,,16/12/2008 10:22,16/12/2008 12:22,26907,chozaensis,Captorhinikos,26907,n. sp.,290.1,268,Leonard,,1,US,Captorhinikos chozaensis
789474,occ,NA,,79601,,Captorhinikos chozaensis,species,120856,,Captorhinikos chozaensis,NA,species,120856,Olson,1954,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37496,NA,NA,NA,individuals,-99.558334,33.816666,Locality FA - Pipe Site,NA,,US,Texas,Foard,estimated from map,seconds,outcrop,"southeastern corner of Foard Co.; Lat long estimation is based on map in fig. 1 in Olson (1951, J. Geol. 59(2), pp. 178-181) ",gp_mid,-30.21,0,101,US,,Choza,Clear Fork,,,,,,,,,NA,Lower part of the Choza Fm.,"""The deposits at the 'pipe site' are extremely interesting and unlike those encountered anywhere else in the Wichita or Clear Fork sections. The bed from which the fossils come is a deep red shale, exposed on a series of hills over an area about an eighth of a mile on each side. This bed is capped in many places by a thin, dense siltstone. Overlying the siltstone is an orange-red shale that carries gypsum biscuits. Underlying the producing layer, which averages about four feet in thickness, is a brownish-red shale that is devoid\r\nof fossils. The most distinctive feature of the bone-bearing shale, outside of the fact that it has fossils, is the occurrence of two types of vertically oriented ovoid structures. One type consists of mottled red and green, hard nodules that range from one to four inches in maximum diameter and up to eighteen inches in length. They are rich in vertebrate remains. They appear to have formed around the bones after deposition, presumably as a result of the reducing action of organic materials. Their vertical orientation is somewhat\r\npuzzling. The contained vertebrate remains are usually oriented with their long axes vertical, and it seems quite certain that this position was attained after the formation of the nodules. Specimens of vertebrates free in the shale rather than in nodules are orientated with their long axes horizontal and have been subjected to considerable distortion and breakage. The most reasonable suggestion seems to be that the vertical orientation of the nodules was developed during compaction of the shales, which has been extensive, with the long axes shifting to become normal to the compacting forces.\r\nThe other vertical structures [...] have been termed pipes and have given the name to the site. They pass from the base to the top of the fossiliferous bed and, at the top, are continuous with the siltstone layer that caps the bed. Their composition is similar to the capping siltstone. The pipes are oval in cross section with maximum diameters from about four to twelve inches. Orientation of the long diameters is random, even in the 'clumps' in which the pipes tend to occur. These structures do not contain vertebrates, although specimens are found 'plastered' to their sides and occasionally penetrating the pipe for a short distance.\r\nThe origin of the pipes is by no means certain. It is thought that they were formed in open holes by the introduction of the sediment that formed the siltstone layer. Superficially, they resemble lungfish burrows of the Arroyo and Vale (Romer and Olson, 1954), but the shape, size, composition, weathering, and fossil content differ. The most probable explanation is that these openings were formed by the root-like shafts of some type of plant, possibly some\r\nEquisetales, that rotted to leave openings that were later filled by sediment. There is no question that the red shales surrounding the pipes were deposited in a shallow pond, and such a pond might well have provided suitable habitat for the type of vegetation envisaged."" (Olson, 1955 pp. 60-63)","""shale""",red or brown,,,Y,,,,,,pond,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,abundant,,,NA,,,taxonomic,,,,,,E. C. Olson,1949,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinikos,,NA,NA,vertebrate,E. C. Olson. 1954. Fauna of the Vale and Choza: 9. Captorhinomorpha. Fieldiana: Geology 10(19):211-218,315,334,0,J. Mueller,T. Liebrecht,,16/12/2008 10:36,16/12/2008 12:36,28508,chozaensis,Captorhinikos,26907,,290.1,268,Leonard,,1,US,Captorhinikos chozaensis
789475,occ,NA,,85362,,Captorhinikos chozaensis,species,120856,,Captorhinikos chozaensis,NA,species,120856,Olson,1954,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37496,NA,NA,NA,individuals,-99.558334,33.816666,Locality FA - Diplocaulus Site,NA,,US,Texas,Foard,estimated from map,seconds,outcrop,"southeastern corner of Foard Co. Aerial photographic index of site: CZW 1C 59, 2.49-3.79.",gp_mid,-30.21,0,101,US,,Choza,Clear Fork,,group of beds,,,,,,,NA,"""top of lower part of Choza Formation""","""The specimens occur in fine-grained siltstones that were formed in a series of small channels. Lateral to the channels are somewhat coarser siltstones, in Which a few non-aquatic animals are preserved."" (Olson, 1956 p. 317)",siltstone,fine,,,Y,siltstone,medium,,,Y,"""channel""",foreland basin,,macrofossils,,,,,,NA,,"body,mold/impression",good,,,,,,abundant,,,NA,,"""Fossil remains are fairly abundant in the channel deposits, but are, for the most part, scattered and broken. The initial porosity of the matrix, and small cracks, developed during weathering, have permitted waters bearing calcium sulphate to percolate to the bones. Crystallization of this salt has resulted in destruction of most of the bone, so that the majority of specimens consist of natural molds. The molds, fortunately, are in excellent condition, so that latex casts reproduce much of the surface detail of the destroyed bone."" (Olson, 1956)",taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinikos,,NA,NA,vertebrate,E. C. Olson. 1954. Fauna of the Vale and Choza: 9. Captorhinomorpha. Fieldiana: Geology 10(19):211-218,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,16/12/2008 10:51,15/03/2016 12:14,26907,chozaensis,Captorhinikos,26907,,290.1,268,Leonard,,1,US,Captorhinikos chozaensis
789665,occ,NA,,80112,,Seymouria sanjuanensis,species,93510,,Seymouria sanjuanensis,NA,species,93510,Berman et al.,2000,Chordata,33815,Osteichthyes,34881,,NA,Seymouriidae,37219,37223,NA,NA,NA,individuals,10.618889,50.809723,Bromacker Quarry (upper level of Tambach sandstone),NA,,DE,Thuringia,Gotha,based on nearby landmark,seconds,outcrop,"""...middle part of the Thuringian Forest near the village of Tambach-Dietharz and about 20 km south of the town of Gotha, central Germany.""",gp_mid,21.71,7.41,305,DE,,Tambach,Rotliegend,Tambach-Sandstein,group of beds,,,,,,,NA,"""At the Bromacker quarry site are two superimposed stratigraphic successions that can be characterized by their facies associations and are referred to as the Lower Beds and Upper Beds (Eberth et al. 2000). All the vertebrates from the Bromacker quarry come from the Upper Beds [...]. The vertebrates are almost exclusively restricted to two [... horizons ...] which are separated by 50 cm in a stratigraphic interval of 1.2 m."" (Berman et al., 2001)\r\nThe Tambach Formation is of Artinskian age according to ""Stratigraphische Tabelle von Deutschland 2002"", however, a Kungurian age is proposed by L_tzner (2006) in LITHOLEX stratigraphic online database [http://www.bgr.de/app/LithoLex/gesamt_ausgabe_neu.php5?id=25]","""massive, red-brown, very fine-grained sandstone and siltstone"" (Berman et al., 2001).\r\nFor further details see Eberth et al. (2000).",sandstone,"very fine,brown,red",lithified,,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,"""alluvial paleochannel and sheetflood facies and lacustrine suspension deposits"" (Berman et al., 2001).\r\n""During the time that the Lower and Upper beds were deposited, the Tambach Basin was internally-drained and probably characterized by a wet-and-dry tropical or wetter climate that was hot year-round with seasonal-to-subseasonal cycles of rainfall and drying. [...] In the Bromacker area, the floodbasin was never deeply desiccated or heavily vegetated between flooding events."" Eberth et al. (2000).",macrofossils,,,,,,NA,,"body,permineralized",excellent,,snapshot,,,,,,,NA,,,taxonomic,"bulk,field collection",,all macrofossils,,,,,"MNG = Museum der Natur, Gotha",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Seymouria,,NA,NA,vertebrate,"D. S. Berman, A. C. Henrici, and S. S. Sumida, T. Martens. 2000. Redescription of Seymouria sanjuanensis (Seymouriomorpha) from the Lower Permian of Germany based on complete, mature specimens with a discussion of paleoecology of Bromacker locality assemblage. Journal of Vertebrate Paleontology 20(2):253-268",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,18/12/2008 07:14,26/08/2009 12:13,26922,sanjuanensis,Seymouria,5765,,290.1,279.3,Artinskian,,4,DE,Seymouria sanjuanensis
789669,occ,NA,,85337,,n. gen. Puercosaurus n. sp. obtusidens,species,137857,nomen dubium,Reptilia,NA,class,36322,Berman and Reisz,1986,Chordata,33815,Reptilia,36322,,NA,,NA,NA,NA,NA,NA,individuals,-106.673889,36.178612,Miller Bonebed,85339,Bone Quarry; Arroya de Agua; Poleo Creek,US,New Mexico,Rio Arriba,estimated from map,seconds,small collection,"1 mile ""above the confluence of the Poleo creek with the Puerco, and near the Mexican village of Arroya de Agua."" (Williston, 1916)\r\nApparently is what Williston (1916) calls the Poleo Creek a northwestern headstream of the Rio Puerco (see Williston & Case, 1913 p. 1 fig. 1, Carnegie Inst. Washington Publ. 181), however, in modern maps a southwestern headstream is designated as Poleo Creek. ",gp_mid,-34.08,4.56,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,"""same horizon"" as the Baldwin Bonebed (see coll. 80833)","""hard, dark brown clay""",claystone,brown,lithified,,Y,sandstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"""numerous isolated bones of Sphenacodon and Ophiacodon Marsh, together with a very perfect skeleton of the latter, were obtained"" (Williston, 1916)",taxonomic,"bulk,mechanical",,,,,"S. W. Williston, E. C. Case, P. Miller",1911,"for details see Williston & Case (1913 p. 38, Carnegie Inst. Washington Publ. 181)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Puercosaurus,n. gen.,NA,NA,vertebrate,"D. S. Berman and R. R. Reisz. 1986. Captorhinid reptiles from the Early Permian of New Mexico, with description of a new genus and species. Annals of Carnegie Museum 55:1-28",315,334,0,J. Mueller,T. Liebrecht,,18/12/2008 09:57,18/12/2008 11:57,27105,obtusidens,,28464,n. sp.,296.4,268,Wolfcamp,,1,US, obtusidens
789670,occ,NA,,85433,,Captorhinidae sp.,genus,37495,,Captorhinidae,NA,family,37495,Berman and Reisz,1986,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,NA,NA,NA,NA,individuals,-106.650558,36.162224,Rio Puerco,NA,"Arroyo del Agua, Arroyo de Agua, Arroya de Agua",US,New Mexico,Rio Arriba,based on nearby landmark,seconds,,"""on the Rio Puerco a few miles below Arroyo de Agua""; Lat long is for Arroyo del Agua",gp_mid,-34.08,4.53,101,US,FED,Abo/Cutler,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,P. Miller,1911,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinidae,,NA,NA,vertebrate,"D. S. Berman and R. R. Reisz. 1986. Captorhinid reptiles from the Early Permian of New Mexico, with description of a new genus and species. Annals of Carnegie Museum 55:1-28",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,18/12/2008 10:13,18/12/2008 13:31,28464,sp.,,28464,,296.4,268,Wolfcamp,,2,US, sp.
789671,occ,NA,,85434,,Captorhinidae sp.,genus,37495,,Captorhinidae,NA,family,37495,Berman and Reisz,1986,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,NA,NA,NA,NA,individuals,-106.639442,36.172501,NE Arroyo de Agua,NA,"Arroyo del Agua, Arroya de Agua",US,New Mexico,Rio Arriba,estimated from map,seconds,small collection,"""NE1/4 SW1/4 NE1/4 sec. 5, T. 22 N., R. 3 E. about 1.5 km northeast of Arroyo de Agua""",gp_mid,-34.06,4.54,101,US,FED,Abo/Cutler,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,"D. S. Berman, R. R. Reisz",,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinidae,,NA,NA,vertebrate,"D. S. Berman and R. R. Reisz. 1986. Captorhinid reptiles from the Early Permian of New Mexico, with description of a new genus and species. Annals of Carnegie Museum 55:1-28",315,334,0,J. Mueller,T. Liebrecht,,18/12/2008 11:22,18/12/2008 13:22,28464,sp.,,28464,,296.4,268,Wolfcamp,,1,US, sp.
789673,occ,NA,,85435,,Captorhinidae sp.,genus,37495,,Captorhinidae,NA,family,37495,Berman and Reisz,1986,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,NA,NA,NA,NA,individuals,-106.638336,36.151669,SE Arroyo de Agua,NA,"Arroyo del Agua, Arroya de Agua",US,New Mexico,Rio Arriba,estimated from map,seconds,small collection,"""N1/4 SW1/4 SE1/4 sec. 8, T. 22 N., R. 3 E. about 1.6 km southeast of Arroyo de Agua.""",gp_mid,-34.07,4.52,101,US,FED,Abo/Cutler,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,"D. S. Berman, R. R. Reisz",,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinidae,,NA,NA,vertebrate,"D. S. Berman and R. R. Reisz. 1986. Captorhinid reptiles from the Early Permian of New Mexico, with description of a new genus and species. Annals of Carnegie Museum 55:1-28",315,334,0,J. Mueller,T. Liebrecht,,18/12/2008 11:53,18/12/2008 13:53,28464,sp.,,28464,,296.4,268,Wolfcamp,,1,US, sp.
789674,occ,NA,,85436,,Captorhinidae sp.,genus,37495,,Captorhinidae,NA,family,37495,Berman and Reisz,1986,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,NA,NA,NA,NA,individuals,-106.748055,34.173889,NE Socorro,NA,Gallina Well,US,New Mexico,Socorro,estimated from map,seconds,small collection,"""about 20 (or 19.2km) km northeast of Socorro [...] in SE1/4 NE1/4 W1/4 of sec. 14, T. 2 S., R. 3 E""",gp_mid,-35.31,2.97,101,US,FED,Abo/Cutler,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""elements of the skull and postcranial skeleton of an individual that are randomly associated and densely concentrated in a small, strongly indurated, red concretion""",taxonomic,,,,,,"D. S. Berman, R. R. Reisz",,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinidae,,NA,NA,vertebrate,"D. S. Berman and R. R. Reisz. 1986. Captorhinid reptiles from the Early Permian of New Mexico, with description of a new genus and species. Annals of Carnegie Museum 55:1-28",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,18/12/2008 12:08,18/08/2016 06:52,28464,sp.,,28464,,296.4,268,Wolfcamp,,1,US, sp.
789675,occ,NA,,85437,,Captorhinidae sp.,genus,37495,,Captorhinidae,NA,family,37495,Berman and Reisz,1986,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,NA,NA,NA,NA,specimens,-105.517502,35.386944,SE Santa Fe,NA,,US,New Mexico,San Miguel,estimated from map,seconds,small collection,"""approximately 50 km southeast of Santa Fe in the northeastern part of the state in NE 1/4 sec. 36, T. 14 N., R. 13 E""",gp_mid,-33.78,3.37,101,US,FED,Sangre de Cristo,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,"D. S. Berman, R. R. Reisz",,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinidae,,NA,NA,vertebrate,"D. S. Berman and R. R. Reisz. 1986. Captorhinid reptiles from the Early Permian of New Mexico, with description of a new genus and species. Annals of Carnegie Museum 55:1-28",315,334,0,J. Mueller,T. Liebrecht,,18/12/2008 15:29,18/12/2008 17:29,28464,sp.,,28464,,296.4,268,Wolfcamp,,2,US, sp.
789745,occ,NA,,28267,,n. gen. Varanosaurus n. sp. acutirostris,species,137915,,Varanosaurus acutirostris,NA,species,137915,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38933,NA,NA,NA,individuals,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Varanosaurus,n. gen.,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,19/12/2008 08:13,29/01/2010 07:32,9228,acutirostris,Varanosaurus,27105,n. sp.,279.3,272.3,Kungurian,,2,US,Varanosaurus acutirostris
789746,occ,NA,,28267,,n. gen. Bayloria n. sp. morei,species,120863,subjective synonym of,Captorhinus aguti,NA,species,134887,Reisz and Heaton,1982,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Bayloria,n. gen.,NA,NA,vertebrate,"R. R. Reisz and M. J. Heaton. 1982. Bayloria morei Olson 1941 identified as an immature specimen of the Permian reptile Captorhinus aguti (Cope, 1882). Canadian Journal of Earth Sciences 19(6):1323-1234",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,19/12/2008 08:15,29/01/2010 07:32,9228,morei,Captorhinus,28483,n. sp.,279.3,272.3,Kungurian,,1,US,Captorhinus morei
789747,occ,NA,,79598,,Phlegethontia n. sp. mazonensis,species,156824,subjective synonym of,Phlegethontia longissima,NA,species,156844,Gregory,1948,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,37259,NA,NA,NA,specimens,-88.139999,41.267223,Mazon Creek,NA,"Mazon Creek Vertebrate Fauna, Braidwood Fauna, pit 11",US,Illinois,Grundy/Will,based on political unit,seconds,local area,"Lat Long is for SW Will Co., Illinois",gp_mid,-23.34,-5.09,101,US,,Carbondale,,Francis Creek Shale,,,,,,,,NA,"""Francis Creek Shale above Morris (no. 2) Coal, Carbondale Formation, Westphalian D, Middle Pennsylvanian"" (Carroll & Baird, 1972)\r\nBaird et al. (1985) refer to the no. 2 coal as Colchester or Croweburg Coal Member.","""Concretions occur typically in laminated to weakly rippled, silty mudstone deposits which typically show little or no evidence of bioturbation. Small-scale sedimentary structures in nodule-bearing sequences include climbing ripple drift, and soft-sediment load-failure..."" (Baird et al., 1985 p.90). Note that this is a general description of the fossil bearing strata of the Francis Creek Shale Member which does not refer specifically to the occurences in the Mazon Creek area proper.",mudstone,"current ripples,deformed bedding",,silty,,siderite,nodular,,,Y,deltaic indet.,foreland basin,"""...these indicate rapid and often episodic mud deposition in interdistributary bay and prodelta settings."" (Baird et al., 1985 p.90)",macrofossils,,,,,,NA,,"mold/impression,concretion,soft parts,replaced with other",good,parautochthonous,,,,,,,,NA,,"""Outlines of the limbs can be seen in the matrix, indicating the extent of the soft tissue and the texture of the skin. The bone itself was represented by a very soft, claylike material that had been removed from the hard, ironstone matrix."" (Carroll, & Baird, 1972 p. 323)\r\nBones are replaced by clay minerals such as Kaolinite (Gregory, 1948 p. 637).",taxonomic,"mechanical,survey of museum collection","FMNH,MCZ,USNM,YPM","species names,ichnofossils",,,"R. L. Moodie, P. Turnbull, among others","1871, 1953",,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Phlegethontia,,NA,NA,vertebrate,"J. T. Gregory. 1948. A New Limbless Vertebrate from the Pennsylvanian of Mazon Creek, Illinois. American Journal of Science 246:636-663",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,19/12/2008 10:44,04/11/2009 16:31,28608,mazonensis,Phlegethontia,28829,n. sp.,311.45,306.95,Westphalian D,,8,US,Phlegethontia mazonensis
789748,occ,NA,R,79598,,cf. Phlegethontia mazonensis,species,156824,subjective synonym of,Phlegethontia longissima,NA,species,156844,Turnbull and Turnbull,1955,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,37259,NA,NA,NA,individuals,-88.139999,41.267223,Mazon Creek,NA,"Mazon Creek Vertebrate Fauna, Braidwood Fauna, pit 11",US,Illinois,Grundy/Will,based on political unit,seconds,local area,"Lat Long is for SW Will Co., Illinois",gp_mid,-23.34,-5.09,101,US,,Carbondale,,Francis Creek Shale,,,,,,,,NA,"""Francis Creek Shale above Morris (no. 2) Coal, Carbondale Formation, Westphalian D, Middle Pennsylvanian"" (Carroll & Baird, 1972)\r\nBaird et al. (1985) refer to the no. 2 coal as Colchester or Croweburg Coal Member.","""Concretions occur typically in laminated to weakly rippled, silty mudstone deposits which typically show little or no evidence of bioturbation. Small-scale sedimentary structures in nodule-bearing sequences include climbing ripple drift, and soft-sediment load-failure..."" (Baird et al., 1985 p.90). Note that this is a general description of the fossil bearing strata of the Francis Creek Shale Member which does not refer specifically to the occurences in the Mazon Creek area proper.",mudstone,"current ripples,deformed bedding",,silty,,siderite,nodular,,,Y,deltaic indet.,foreland basin,"""...these indicate rapid and often episodic mud deposition in interdistributary bay and prodelta settings."" (Baird et al., 1985 p.90)",macrofossils,,,,,,NA,,"mold/impression,concretion,soft parts,replaced with other",good,parautochthonous,,,,,,,,NA,,"""Outlines of the limbs can be seen in the matrix, indicating the extent of the soft tissue and the texture of the skin. The bone itself was represented by a very soft, claylike material that had been removed from the hard, ironstone matrix."" (Carroll, & Baird, 1972 p. 323)\r\nBones are replaced by clay minerals such as Kaolinite (Gregory, 1948 p. 637).",taxonomic,"mechanical,survey of museum collection","FMNH,MCZ,USNM,YPM","species names,ichnofossils",,,"R. L. Moodie, P. Turnbull, among others","1871, 1953",,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Phlegethontia,cf.,NA,NA,vertebrate,W. D. Turnbull and P. F. Turnbull. 1955. A Recently Discovered Phlegethontia from Illinois. Fieldiana Zoology 37(19):523-535,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,19/12/2008 10:52,22/07/2016 06:51,28608,mazonensis,Phlegethontia,31099,,311.45,306.95,Westphalian D,,1,US,Phlegethontia mazonensis
789748,occ,22370,R,79598,,Phlegethontia cf. longissima,species,156845,,Phlegethontia longissima,NA,species,156844,McGinnis,1967,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,37259,NA,NA,NA,individuals,-88.139999,41.267223,Mazon Creek,NA,"Mazon Creek Vertebrate Fauna, Braidwood Fauna, pit 11",US,Illinois,Grundy/Will,based on political unit,seconds,local area,"Lat Long is for SW Will Co., Illinois",gp_mid,-23.34,-5.09,101,US,,Carbondale,,Francis Creek Shale,,,,,,,,NA,"""Francis Creek Shale above Morris (no. 2) Coal, Carbondale Formation, Westphalian D, Middle Pennsylvanian"" (Carroll & Baird, 1972)\r\nBaird et al. (1985) refer to the no. 2 coal as Colchester or Croweburg Coal Member.","""Concretions occur typically in laminated to weakly rippled, silty mudstone deposits which typically show little or no evidence of bioturbation. Small-scale sedimentary structures in nodule-bearing sequences include climbing ripple drift, and soft-sediment load-failure..."" (Baird et al., 1985 p.90). Note that this is a general description of the fossil bearing strata of the Francis Creek Shale Member which does not refer specifically to the occurences in the Mazon Creek area proper.",mudstone,"current ripples,deformed bedding",,silty,,siderite,nodular,,,Y,deltaic indet.,foreland basin,"""...these indicate rapid and often episodic mud deposition in interdistributary bay and prodelta settings."" (Baird et al., 1985 p.90)",macrofossils,,,,,,NA,,"mold/impression,concretion,soft parts,replaced with other",good,parautochthonous,,,,,,,,NA,,"""Outlines of the limbs can be seen in the matrix, indicating the extent of the soft tissue and the texture of the skin. The bone itself was represented by a very soft, claylike material that had been removed from the hard, ironstone matrix."" (Carroll, & Baird, 1972 p. 323)\r\nBones are replaced by clay minerals such as Kaolinite (Gregory, 1948 p. 637).",taxonomic,"mechanical,survey of museum collection","FMNH,MCZ,USNM,YPM","species names,ichnofossils",,,"R. L. Moodie, P. Turnbull, among others","1871, 1953",,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Phlegethontia,,NA,NA,vertebrate,"H. J. McGinnis. 1967. The Osteology of Phlegethontia, a Carboniferous and Permian Astopod Amphibian. University of California Publications in Geological Sciences 71:1-46",315,334,0,J. Mueller,T. Liebrecht,,04/11/2009 14:25,04/11/2009 16:25,28608,longissima,Phlegethontia,31050,cf.,311.45,306.95,Westphalian D,,1,US,Phlegethontia longissima
789748,occ,22372,,79598,,n. gen. Pseudophlegethontia n. sp. turnbullorum,species,137947,,Pseudophlegethontia turnbullorum,NA,species,137947,Anderson,2003,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Pseudophlegethontiidae,137943,137946,NA,NA,NA,individuals,-88.139999,41.267223,Mazon Creek,NA,"Mazon Creek Vertebrate Fauna, Braidwood Fauna, pit 11",US,Illinois,Grundy/Will,based on political unit,seconds,local area,"Lat Long is for SW Will Co., Illinois",gp_mid,-23.34,-5.09,101,US,,Carbondale,,Francis Creek Shale,,,,,,,,NA,"""Francis Creek Shale above Morris (no. 2) Coal, Carbondale Formation, Westphalian D, Middle Pennsylvanian"" (Carroll & Baird, 1972)\r\nBaird et al. (1985) refer to the no. 2 coal as Colchester or Croweburg Coal Member.","""Concretions occur typically in laminated to weakly rippled, silty mudstone deposits which typically show little or no evidence of bioturbation. Small-scale sedimentary structures in nodule-bearing sequences include climbing ripple drift, and soft-sediment load-failure..."" (Baird et al., 1985 p.90). Note that this is a general description of the fossil bearing strata of the Francis Creek Shale Member which does not refer specifically to the occurences in the Mazon Creek area proper.",mudstone,"current ripples,deformed bedding",,silty,,siderite,nodular,,,Y,deltaic indet.,foreland basin,"""...these indicate rapid and often episodic mud deposition in interdistributary bay and prodelta settings."" (Baird et al., 1985 p.90)",macrofossils,,,,,,NA,,"mold/impression,concretion,soft parts,replaced with other",good,parautochthonous,,,,,,,,NA,,"""Outlines of the limbs can be seen in the matrix, indicating the extent of the soft tissue and the texture of the skin. The bone itself was represented by a very soft, claylike material that had been removed from the hard, ironstone matrix."" (Carroll, & Baird, 1972 p. 323)\r\nBones are replaced by clay minerals such as Kaolinite (Gregory, 1948 p. 637).",taxonomic,"mechanical,survey of museum collection","FMNH,MCZ,USNM,YPM","species names,ichnofossils",,,"R. L. Moodie, P. Turnbull, among others","1871, 1953",,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Pseudophlegethontia,n. gen.,NA,NA,vertebrate,"J. S. Anderson. 2003. A New Astopod (Tetrapoda: Lepospondyli) from Mazon Creek, Illinois. Journal of Vertebrate Paleontology 23(1):79-88",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,04/11/2009 14:27,04/11/2009 16:30,28608,turnbullorum,Pseudophlegethontia,28830,n. sp.,311.45,306.95,Westphalian D,,1,US,Pseudophlegethontia turnbullorum
789749,occ,NA,,85292,,Sauropleura n. sp. longipes,species,137949,recombined as,Anthracodromeus longipes,NA,species,137949,Cope,1875,Chordata,33815,Reptilia,36322,,NA,Protorothyrididae,37486,37487,NA,NA,NA,individuals,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sauropleura,,NA,NA,vertebrate,"E. D. Cope. 1875. Supplement to the Extinct Batrachia and Reptilia of North America I. Catalogue of the Air Breathing Vertebrata from the Coal Measures of Linton, Ohio. Transactions of the American Philosophical Society, New Series 15(2):261-278",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,19/12/2008 11:42,03/11/2009 10:09,28831,longipes,Anthracodromeus,28831,n. sp.,311.45,306.95,Westphalian D,,1,US,Anthracodromeus longipes
789750,occ,NA,,84835,,n. gen. Brouffia n. sp. orientalis,species,137952,,Brouffia orientalis,NA,species,137952,Carroll and Baird,1972,Chordata,33815,Reptilia,36322,,NA,Protorothyrididae,37486,37489,NA,NA,NA,individuals,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Brouffia,n. gen.,NA,NA,vertebrate,R. L. Carroll and D. Baird. 1972. Carboniferous Stem-Reptiles of the Family Romeriidae. Bulletin of the Museum of Comparative Zoology 143(5):321-363,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,19/12/2008 14:35,04/11/2009 19:28,28608,orientalis,Brouffia,28608,n. sp.,311.45,306.95,Westphalian D,,1,CZ,Brouffia orientalis
789751,occ,NA,,84835,,n. gen. Coelostegus n. sp. prothales,species,137953,,Coelostegus prothales,NA,species,137953,Carroll and Baird,1972,Chordata,33815,Reptilia,36322,,NA,Protorothyrididae,37486,37491,NA,NA,NA,individuals,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Coelostegus,n. gen.,NA,NA,vertebrate,R. L. Carroll and D. Baird. 1972. Carboniferous Stem-Reptiles of the Family Romeriidae. Bulletin of the Museum of Comparative Zoology 143(5):321-363,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,19/12/2008 14:42,04/11/2009 19:28,28608,prothales,Coelostegus,28608,n. sp.,311.45,306.95,Westphalian D,,1,CZ,Coelostegus prothales
789752,occ,NA,,84835,,Gephyrostegus n. sp. watsoni,species,137954,,Gephyrostegus watsoni,NA,species,137954,Brough and Brough,1967,Chordata,33815,Osteichthyes,34881,,NA,Gephyrostegidae,37202,37205,NA,NA,NA,individuals,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Gephyrostegus,,NA,NA,vertebrate,"M. C. Brough and J. Brough. 1967. Studies on Early Tetrapods III. The Genus Gephyrostegus. Philosophical Transactions of the Royal Society of London, Series B 252:147-165",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,19/12/2008 15:19,03/11/2009 20:09,28608,watsoni,Gephyrostegus,28833,n. sp.,311.45,306.95,Westphalian D,,1,CZ,Gephyrostegus watsoni
789753,occ,NA,,84835,,Amniota indet.,unranked clade,92208,,Amniota,NA,unranked clade,53189,Carroll and Baird,1972,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,NA,NA,NA,NA,individuals,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Amniota,,NA,NA,vertebrate,R. L. Carroll and D. Baird. 1972. Carboniferous Stem-Reptiles of the Family Romeriidae. Bulletin of the Museum of Comparative Zoology 143(5):321-363,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,19/12/2008 15:26,03/11/2009 20:09,28608,indet.,,28608,,311.45,306.95,Westphalian D,,1,CZ, indet.
789755,occ,NA,,84835,,n. gen. Gephyrostegus n. sp. bohemicus,species,137955,,Gephyrostegus bohemicus,NA,species,137955,Brough and Brough,1967,Chordata,33815,Osteichthyes,34881,,NA,Gephyrostegidae,37202,37205,NA,NA,NA,individuals,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Gephyrostegus,n. gen.,NA,NA,vertebrate,"M. C. Brough and J. Brough. 1967. Studies on Early Tetrapods III. The Genus Gephyrostegus. Philosophical Transactions of the Royal Society of London, Series B 252:147-165",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,19/12/2008 15:51,03/11/2009 20:09,28608,bohemicus,Gephyrostegus,28833,n. sp.,311.45,306.95,Westphalian D,,1,CZ,Gephyrostegus bohemicus
789756,occ,NA,,84835,,Microbrachis pelikani,species,227043,,Microbrachis pelikani,NA,species,227043,Milner,2008,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Microbrachidae,37310,37311,NA,NA,NA,individuals,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Microbrachis,,NA,NA,vertebrate,A.. R. Milner. 2008. The tail of Microbrachis (Tetrapoda; Microsauria). Lethaia 41(3):257-261,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,19/12/2008 16:26,03/11/2009 20:09,28608,pelikani,Microbrachis,28832,,311.45,306.95,Westphalian D,,7,CZ,Microbrachis pelikani
789757,occ,NA,,28267,,Secodontosaurus n. sp. willistoni,species,122486,,Secodontosaurus willistoni,NA,species,122486,Romer,1936,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38908,NA,NA,NA,elements,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Secodontosaurus,,NA,NA,vertebrate,A. S. Romer. 1936. Studies on American Permo-Carboniferous reptiles. Problems of Paleontology 1:85-93,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,20/12/2008 08:37,10/12/2012 13:48,9228,willistoni,Secodontosaurus,43841,n. sp.,279.3,272.3,Kungurian,,14,US,Secodontosaurus willistoni
789758,occ,NA,,85451,,Batropetes n. sp. niederkirchensis,species,340813,,Batropetes niederkirchensis,NA,species,340813,Carroll,1991,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Brachystelechidae,37314,37513,NA,NA,NA,individuals,7.696111,49.578056,Niederkirchen/Westpfalz,NA,Gemeindeburg near Niederkirchen,DE,Rhineland-Palatinate,Kaiserslautern,based on nearby landmark,seconds,small collection,"Niederkirchen (Westpfalz), 16 km north of the city of Kaiserslautern; Lat long is for Niederkirchen. Locality lies in the Saar-Nahe district. Location described by Glienke (2013) as ""Gemeindeburg near Niederkirchen/Westpfalz, Saar-Nahe Basin)",gp_mid,19.79,4.99,315,DE,,Meisenheim,Rotliegend,,member,,M6,M6,,,,NA,"""Biostratigraphically, the find can be attributed to Boy's Leptorophus humbergensis-Apateon caducus association. This association is part of the Apateon caducus group and has an upper 'Autunian' age. This corresponds to the lower Sakmarian of international stratigraphy""\r\nThe Jeckenbach Subformation, however, is of Asselian age according to ""Stratigraphische Tabelle von Deutschland 2002""","""laminated silty grey shale""","""shale""","planar lamination,gray",,silty,Y,,,,,,lacustrine - large,intermontane basin,"""deposited in a large, shallow, eutrophic lake"" - Carroll (1991)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Batropetes,,NA,NA,vertebrate,"R. L. Carroll. 1991. Batropetes from the Lower Permian of Europe - a Microsaur, not a Reptile. Journal of Vertebrate Paleontology 11(2):229-242",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,21/12/2008 15:29,13/05/2016 05:47,28837,niederkirchensis,Batropetes,28837,n. sp.,298.9,295.5,Asselian,,1,DE,Batropetes niederkirchensis
789786,occ,NA,,80111,,n. gen. Paleothyris n. sp. acadiana,species,138002,,Paleothyris acadiana,NA,species,138002,Carroll,1969,Chordata,33815,Reptilia,36322,,NA,Protorothyrididae,37486,37493,NA,NA,NA,specimens,-60.266666,46.290001,Dominion Coal Co. strip mine No. 7,NA,"Sydney coal field; Florence, Cape Breton",CA,Nova Scotia,Cape Breton Island,estimated from map,seconds,small collection,"Dominion Coal Co. strip mine No. 7, about 2 miles north of the town of Florence",gp_mid,-3.96,-8.17,108,CA,,,Morien,,group of beds,,,,,,,NA,"""... above the Lloyd Cove (Lower Bonar) coal of the Morien group."" ",,coal,,,,Y,"""shale""",,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,permineralized,,autochthonous,snapshot,,,,,,,NA,,the vertebrate remains come from the interior of fossilized tree stumps and are completely disarticulated,taxonomic,"selective quarrying,survey of museum collection",MCZ,,,,A.S. Romer,1956,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Paleothyris,n. gen.,NA,NA,,"R. L. Carroll. 1969. A Middle Pennsylvanian Captorhinomorph, and the Interrelationships of Primitive Reptiles. Journal of Paleontology 43(1):151-170",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,22/12/2008 01:27,11/02/2016 10:43,26895,acadiana,Paleothyris,28609,n. sp.,314.6,306.95,Westphalian C,Westphalian D,18,CA,Paleothyris acadiana
789818,occ,NA,,80714,,n. gen. Archaeobelus n. sp. vellicatus,species,70400,subjective synonym of,Clepsydrops collettii,NA,species,122329,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38887,NA,NA,NA,individuals,-87.775002,40.108334,Danville Locality (Vertebrates),NA,Oakwood Locality; Horseshoe Bend; Vermillion River; Illinois bonebed,US,Illinois,Vermilion,based on nearby landmark,seconds,outcrop,"""the well-known Danville or 'Oakwood' locality [...] Horseshoe Bend locality near the SE/C of Sec. 23-19N-13W"" (DeMar, 1970)\r\n""Vermilion River, near Danville"" (Reisz, 1986)\r\nLat Long is for Oakwood",gp_mid,-21.51,-3.52,101,US,,Bond,McLeansboro,,group of beds,,,,,,,NA,"""We believe the vertebrates have been collected from a zone 10 feet or so below the Shoal Creek Member of the Bond Formation"" (DeMar, 1970)\r\nNote: Shoal Creek Member is equivalent to Carthage Limestone Member, a name now used throughout the Illinois Basin for that lithological unit; see Jacobson (2002) A summary of references with changes in Pennsylvanian stratigraphic nomenclature at the ISGS since Bulletin 95. [Online] http://www.isgs.illinois.edu/maps-data-pub/coal-maps/pennstratigraphy.shtml ",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archaeobelus,n. gen.,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,22/12/2008 09:06,29/06/2015 11:47,28640,vellicatus,Clepsydrops,5692,n. sp.,305.9,303.4,Missourian,,1,US,Clepsydrops vellicatus
789819,occ,NA,,80714,,Clepsydrops n. sp. pedunculatus,species,138092,subjective synonym of,Clepsydrops collettii,NA,species,122329,Case,1907,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38887,NA,NA,NA,elements,-87.775002,40.108334,Danville Locality (Vertebrates),NA,Oakwood Locality; Horseshoe Bend; Vermillion River; Illinois bonebed,US,Illinois,Vermilion,based on nearby landmark,seconds,outcrop,"""the well-known Danville or 'Oakwood' locality [...] Horseshoe Bend locality near the SE/C of Sec. 23-19N-13W"" (DeMar, 1970)\r\n""Vermilion River, near Danville"" (Reisz, 1986)\r\nLat Long is for Oakwood",gp_mid,-21.51,-3.52,101,US,,Bond,McLeansboro,,group of beds,,,,,,,NA,"""We believe the vertebrates have been collected from a zone 10 feet or so below the Shoal Creek Member of the Bond Formation"" (DeMar, 1970)\r\nNote: Shoal Creek Member is equivalent to Carthage Limestone Member, a name now used throughout the Illinois Basin for that lithological unit; see Jacobson (2002) A summary of references with changes in Pennsylvanian stratigraphic nomenclature at the ISGS since Bulletin 95. [Online] http://www.isgs.illinois.edu/maps-data-pub/coal-maps/pennstratigraphy.shtml ",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Clepsydrops,,NA,NA,vertebrate,E. C. Case. 1907. Revision of the Pelycosauria of North America. Carnegie Institution of Washington 55:3-176,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,22/12/2008 09:45,29/06/2015 11:47,28640,pedunculatus,Clepsydrops,7374,n. sp.,305.9,303.4,Missourian,,2,US,Clepsydrops pedunculatus
789820,occ,NA,,80714,,Clepsydrops n. sp. vinslovii,species,123416,,Clepsydrops vinslovii,NA,species,123416,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38887,NA,NA,NA,specimens,-87.775002,40.108334,Danville Locality (Vertebrates),NA,Oakwood Locality; Horseshoe Bend; Vermillion River; Illinois bonebed,US,Illinois,Vermilion,based on nearby landmark,seconds,outcrop,"""the well-known Danville or 'Oakwood' locality [...] Horseshoe Bend locality near the SE/C of Sec. 23-19N-13W"" (DeMar, 1970)\r\n""Vermilion River, near Danville"" (Reisz, 1986)\r\nLat Long is for Oakwood",gp_mid,-21.51,-3.52,101,US,,Bond,McLeansboro,,group of beds,,,,,,,NA,"""We believe the vertebrates have been collected from a zone 10 feet or so below the Shoal Creek Member of the Bond Formation"" (DeMar, 1970)\r\nNote: Shoal Creek Member is equivalent to Carthage Limestone Member, a name now used throughout the Illinois Basin for that lithological unit; see Jacobson (2002) A summary of references with changes in Pennsylvanian stratigraphic nomenclature at the ISGS since Bulletin 95. [Online] http://www.isgs.illinois.edu/maps-data-pub/coal-maps/pennstratigraphy.shtml ",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Clepsydrops,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,22/12/2008 09:47,29/06/2015 11:47,28640,vinslovii,Clepsydrops,5692,n. sp.,305.9,303.4,Missourian,,9,US,Clepsydrops vinslovii
789843,occ,NA,,28256,,Dimetrodon loomisi,species,90738,,Dimetrodon loomisi,NA,species,90738,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,22/12/2008 20:00,10/04/2009 14:19,17702,loomisi,Dimetrodon,27105,,279.3,272.3,Kungurian,,13,US,Dimetrodon loomisi
789940,occ,NA,,80784,,n. gen. Ianthasaurus n. sp. hardestii,species,138227,corrected to,Ianthasaurus hardestiorum,NA,species,138227,Reisz and Berman,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38912,NA,NA,NA,individuals,-95.259048,38.378502,Garnett Quarry,NA,"Garnett Vertebrate Fauna, Charles Hardesty farm",US,Kansas,Anderson,estimated from map,6,outcrop,"""6 miles northwest of Garnett"" (Reisz, 1986); ""NW 1/4, NE 1/4, sec. 5, tp. 20 S, rge. 19 E, Putnam Township, Anderson County, Kansas"" (Reisz & Berman, 1986)\r\n""Charles A. Hardest farm, NW/4 NE/4 sec. 5 T20S R19E, Putnam Township, Anderson County, Kansas. The Universal Transverse Mercantor (UTM) coordinates of the quarry are 15STN963466. Locality is close to Garnett, Kansas."" (Laurin 1993). ",gp_mid,-27.44,-2.3,101,US,,Stanton,Lansing,Rock Lake Shale,group of beds,,,,,,,NA,"""Rock Lake Member, Stanton Formation, Lansing Group, Missourian Series, Upper Pennsylvanian"" (Reisz & Berman, 1996)\r\nall vertebrate remains seem to come exclusively from the basal part of the Rock Lake Shale (see Reisz et al., 1982)","""dark greyishbrown, moderately well bedded, very carbonaceous, calcareous mudstone"" (Reisz et al., 1982)",mudstone,brown,,"calcareous,carbonaceous",Y,,,,,,fine channel fill,foreland basin,"""The Rock Lake Shale is a rather thin but otherwise typical ۪outside۪ shale of a ۪Kansas Megacyclothem۪ sequence formed as a change from regressive to transgressive conditions occurred [...] The site is located along the western edge of what was, during the Late Pennsylvanian, a shallow, forested stream valley or channel that was eroded into a limestone coastal plain during the latter stages of a major eustatic fall in sea level. As the succeeding rise in sea level occurred, the valley was gradually flooded by estuarine waters"" (Reisz et al., 1982).\r\nSequence stratigraphy is interpreted from the description given by Reisz et al. (1982). The surface of the underlying limestone is the sequence boundary merged with the transgressive surface and the Lake Rock Shale is the basalmost deposit of the transgressive systems tract.",macrofossils,some,some,,,,NA,,body,good,,snapshot,,,,,,,NA,,,taxonomic,"bulk,mechanical",ROM,,,,"F. E. Peabody, R. Camp, R. L. Carroll, R. R. Reisz, M. J. Heaton, B. R. Pynn, G. MacDonald","1953-1956, 1965, 1980, 1981",,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ianthasaurus,n. gen.,NA,NA,vertebrate,"R. R. Reisz and D. S. Berman. 1986. Ianthasaurus hardestii n. sp., a primitive edaphosaur (Reptilia, Pelycosauria) from the Upper Pennsylvanian Rock Lake Shale near Garnett, Kansas. Canadian Journal of Earth Sciences 23(1):77-91",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,23/12/2008 15:42,19/10/2015 11:22,28862,hardestii,Ianthasaurus,28860,n. sp.,305.9,303.4,Missourian,,5,US,Ianthasaurus hardestii
789941,occ,NA,,80784,,Amniota indet.,unranked clade,53189,,Amniota,NA,unranked clade,53189,Reisz and Berman,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,NA,NA,NA,NA,individuals,-95.259048,38.378502,Garnett Quarry,NA,"Garnett Vertebrate Fauna, Charles Hardesty farm",US,Kansas,Anderson,estimated from map,6,outcrop,"""6 miles northwest of Garnett"" (Reisz, 1986); ""NW 1/4, NE 1/4, sec. 5, tp. 20 S, rge. 19 E, Putnam Township, Anderson County, Kansas"" (Reisz & Berman, 1986)\r\n""Charles A. Hardest farm, NW/4 NE/4 sec. 5 T20S R19E, Putnam Township, Anderson County, Kansas. The Universal Transverse Mercantor (UTM) coordinates of the quarry are 15STN963466. Locality is close to Garnett, Kansas."" (Laurin 1993). ",gp_mid,-27.44,-2.3,101,US,,Stanton,Lansing,Rock Lake Shale,group of beds,,,,,,,NA,"""Rock Lake Member, Stanton Formation, Lansing Group, Missourian Series, Upper Pennsylvanian"" (Reisz & Berman, 1996)\r\nall vertebrate remains seem to come exclusively from the basal part of the Rock Lake Shale (see Reisz et al., 1982)","""dark greyishbrown, moderately well bedded, very carbonaceous, calcareous mudstone"" (Reisz et al., 1982)",mudstone,brown,,"calcareous,carbonaceous",Y,,,,,,fine channel fill,foreland basin,"""The Rock Lake Shale is a rather thin but otherwise typical ۪outside۪ shale of a ۪Kansas Megacyclothem۪ sequence formed as a change from regressive to transgressive conditions occurred [...] The site is located along the western edge of what was, during the Late Pennsylvanian, a shallow, forested stream valley or channel that was eroded into a limestone coastal plain during the latter stages of a major eustatic fall in sea level. As the succeeding rise in sea level occurred, the valley was gradually flooded by estuarine waters"" (Reisz et al., 1982).\r\nSequence stratigraphy is interpreted from the description given by Reisz et al. (1982). The surface of the underlying limestone is the sequence boundary merged with the transgressive surface and the Lake Rock Shale is the basalmost deposit of the transgressive systems tract.",macrofossils,some,some,,,,NA,,body,good,,snapshot,,,,,,,NA,,,taxonomic,"bulk,mechanical",ROM,,,,"F. E. Peabody, R. Camp, R. L. Carroll, R. R. Reisz, M. J. Heaton, B. R. Pynn, G. MacDonald","1953-1956, 1965, 1980, 1981",,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Amniota,,NA,NA,vertebrate,"R. R. Reisz and D. S. Berman. 1986. Ianthasaurus hardestii n. sp., a primitive edaphosaur (Reptilia, Pelycosauria) from the Upper Pennsylvanian Rock Lake Shale near Garnett, Kansas. Canadian Journal of Earth Sciences 23(1):77-91",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,23/12/2008 15:42,16/10/2015 05:42,28862,indet.,,28860,,305.9,303.4,Missourian,,1,US, indet.
789942,occ,NA,,80784,,Edaphosaurus n. sp. ecordi,species,138229,recombined as,Xyrospondylus ecordi,NA,species,138229,Reisz et al.,1982,Chordata,33815,Osteichthyes,34881,Pelycosauria,38883,,NA,38934,NA,NA,NA,individuals,-95.259048,38.378502,Garnett Quarry,NA,"Garnett Vertebrate Fauna, Charles Hardesty farm",US,Kansas,Anderson,estimated from map,6,outcrop,"""6 miles northwest of Garnett"" (Reisz, 1986); ""NW 1/4, NE 1/4, sec. 5, tp. 20 S, rge. 19 E, Putnam Township, Anderson County, Kansas"" (Reisz & Berman, 1986)\r\n""Charles A. Hardest farm, NW/4 NE/4 sec. 5 T20S R19E, Putnam Township, Anderson County, Kansas. The Universal Transverse Mercantor (UTM) coordinates of the quarry are 15STN963466. Locality is close to Garnett, Kansas."" (Laurin 1993). ",gp_mid,-27.44,-2.3,101,US,,Stanton,Lansing,Rock Lake Shale,group of beds,,,,,,,NA,"""Rock Lake Member, Stanton Formation, Lansing Group, Missourian Series, Upper Pennsylvanian"" (Reisz & Berman, 1996)\r\nall vertebrate remains seem to come exclusively from the basal part of the Rock Lake Shale (see Reisz et al., 1982)","""dark greyishbrown, moderately well bedded, very carbonaceous, calcareous mudstone"" (Reisz et al., 1982)",mudstone,brown,,"calcareous,carbonaceous",Y,,,,,,fine channel fill,foreland basin,"""The Rock Lake Shale is a rather thin but otherwise typical ۪outside۪ shale of a ۪Kansas Megacyclothem۪ sequence formed as a change from regressive to transgressive conditions occurred [...] The site is located along the western edge of what was, during the Late Pennsylvanian, a shallow, forested stream valley or channel that was eroded into a limestone coastal plain during the latter stages of a major eustatic fall in sea level. As the succeeding rise in sea level occurred, the valley was gradually flooded by estuarine waters"" (Reisz et al., 1982).\r\nSequence stratigraphy is interpreted from the description given by Reisz et al. (1982). The surface of the underlying limestone is the sequence boundary merged with the transgressive surface and the Lake Rock Shale is the basalmost deposit of the transgressive systems tract.",macrofossils,some,some,,,,NA,,body,good,,snapshot,,,,,,,NA,,,taxonomic,"bulk,mechanical",ROM,,,,"F. E. Peabody, R. Camp, R. L. Carroll, R. R. Reisz, M. J. Heaton, B. R. Pynn, G. MacDonald","1953-1956, 1965, 1980, 1981",,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,"R. R. Reisz, M. J. Heaton, and B. R. Pynn. 1982. Vertebrate Fauna of Late Pennsylvanian Rock Lake Shale near Garnett, Kansas: Pelycosauria. Journal of Paleontology 56(3):741-750",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,23/12/2008 18:10,16/10/2015 05:42,28862,ecordi,Xyrospondylus,28862,n. sp.,305.9,303.4,Missourian,,1,US,Xyrospondylus ecordi
789943,occ,NA,,80784,,n. gen. Petrolacosaurus n. sp. kansensis,species,138231,,Petrolacosaurus kansensis,NA,species,138231,Peabody,1952,Chordata,33815,Reptilia,36322,Araeoscelidia,37769,Petrolacosauridae,37770,37771,NA,NA,NA,individuals,-95.259048,38.378502,Garnett Quarry,NA,"Garnett Vertebrate Fauna, Charles Hardesty farm",US,Kansas,Anderson,estimated from map,6,outcrop,"""6 miles northwest of Garnett"" (Reisz, 1986); ""NW 1/4, NE 1/4, sec. 5, tp. 20 S, rge. 19 E, Putnam Township, Anderson County, Kansas"" (Reisz & Berman, 1986)\r\n""Charles A. Hardest farm, NW/4 NE/4 sec. 5 T20S R19E, Putnam Township, Anderson County, Kansas. The Universal Transverse Mercantor (UTM) coordinates of the quarry are 15STN963466. Locality is close to Garnett, Kansas."" (Laurin 1993). ",gp_mid,-27.44,-2.3,101,US,,Stanton,Lansing,Rock Lake Shale,group of beds,,,,,,,NA,"""Rock Lake Member, Stanton Formation, Lansing Group, Missourian Series, Upper Pennsylvanian"" (Reisz & Berman, 1996)\r\nall vertebrate remains seem to come exclusively from the basal part of the Rock Lake Shale (see Reisz et al., 1982)","""dark greyishbrown, moderately well bedded, very carbonaceous, calcareous mudstone"" (Reisz et al., 1982)",mudstone,brown,,"calcareous,carbonaceous",Y,,,,,,fine channel fill,foreland basin,"""The Rock Lake Shale is a rather thin but otherwise typical ۪outside۪ shale of a ۪Kansas Megacyclothem۪ sequence formed as a change from regressive to transgressive conditions occurred [...] The site is located along the western edge of what was, during the Late Pennsylvanian, a shallow, forested stream valley or channel that was eroded into a limestone coastal plain during the latter stages of a major eustatic fall in sea level. As the succeeding rise in sea level occurred, the valley was gradually flooded by estuarine waters"" (Reisz et al., 1982).\r\nSequence stratigraphy is interpreted from the description given by Reisz et al. (1982). The surface of the underlying limestone is the sequence boundary merged with the transgressive surface and the Lake Rock Shale is the basalmost deposit of the transgressive systems tract.",macrofossils,some,some,,,,NA,,body,good,,snapshot,,,,,,,NA,,,taxonomic,"bulk,mechanical",ROM,,,,"F. E. Peabody, R. Camp, R. L. Carroll, R. R. Reisz, M. J. Heaton, B. R. Pynn, G. MacDonald","1953-1956, 1965, 1980, 1981",,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Petrolacosaurus,n. gen.,NA,NA,vertebrate,"F. E. Peabody. 1952. Petrolacosaurus kansensis Lane, a Pennsylvanian Reptile from Kansas. The University of Kansas Paleontological Contributions, Series Vertebrata 1:1-41",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,23/12/2008 22:38,16/10/2015 05:42,28862,kansensis,Petrolacosaurus,28865,n. sp.,305.9,303.4,Missourian,,10,US,Petrolacosaurus kansensis
789944,occ,NA,,80784,,n. gen. Podargosaurus n. sp. hibbardi,species,138233,subjective synonym of,Petrolacosaurus kansensis,NA,species,138231,Peabody,1952,Chordata,33815,Reptilia,36322,Araeoscelidia,37769,Petrolacosauridae,37770,37771,NA,NA,NA,individuals,-95.259048,38.378502,Garnett Quarry,NA,"Garnett Vertebrate Fauna, Charles Hardesty farm",US,Kansas,Anderson,estimated from map,6,outcrop,"""6 miles northwest of Garnett"" (Reisz, 1986); ""NW 1/4, NE 1/4, sec. 5, tp. 20 S, rge. 19 E, Putnam Township, Anderson County, Kansas"" (Reisz & Berman, 1986)\r\n""Charles A. Hardest farm, NW/4 NE/4 sec. 5 T20S R19E, Putnam Township, Anderson County, Kansas. The Universal Transverse Mercantor (UTM) coordinates of the quarry are 15STN963466. Locality is close to Garnett, Kansas."" (Laurin 1993). ",gp_mid,-27.44,-2.3,101,US,,Stanton,Lansing,Rock Lake Shale,group of beds,,,,,,,NA,"""Rock Lake Member, Stanton Formation, Lansing Group, Missourian Series, Upper Pennsylvanian"" (Reisz & Berman, 1996)\r\nall vertebrate remains seem to come exclusively from the basal part of the Rock Lake Shale (see Reisz et al., 1982)","""dark greyishbrown, moderately well bedded, very carbonaceous, calcareous mudstone"" (Reisz et al., 1982)",mudstone,brown,,"calcareous,carbonaceous",Y,,,,,,fine channel fill,foreland basin,"""The Rock Lake Shale is a rather thin but otherwise typical ۪outside۪ shale of a ۪Kansas Megacyclothem۪ sequence formed as a change from regressive to transgressive conditions occurred [...] The site is located along the western edge of what was, during the Late Pennsylvanian, a shallow, forested stream valley or channel that was eroded into a limestone coastal plain during the latter stages of a major eustatic fall in sea level. As the succeeding rise in sea level occurred, the valley was gradually flooded by estuarine waters"" (Reisz et al., 1982).\r\nSequence stratigraphy is interpreted from the description given by Reisz et al. (1982). The surface of the underlying limestone is the sequence boundary merged with the transgressive surface and the Lake Rock Shale is the basalmost deposit of the transgressive systems tract.",macrofossils,some,some,,,,NA,,body,good,,snapshot,,,,,,,NA,,,taxonomic,"bulk,mechanical",ROM,,,,"F. E. Peabody, R. Camp, R. L. Carroll, R. R. Reisz, M. J. Heaton, B. R. Pynn, G. MacDonald","1953-1956, 1965, 1980, 1981",,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Podargosaurus,n. gen.,NA,NA,vertebrate,"F. E. Peabody. 1952. Petrolacosaurus kansensis Lane, a Pennsylvanian Reptile from Kansas. The University of Kansas Paleontological Contributions, Series Vertebrata 1:1-41",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,23/12/2008 22:38,16/10/2015 05:42,28862,hibbardi,Petrolacosaurus,28865,n. sp.,305.9,303.4,Missourian,,1,US,Petrolacosaurus hibbardi
789965,occ,NA,,79162,,Eryops megacephalus,species,70397,,Eryops megacephalus,NA,species,70397,Sander,1989,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-98.650002,33.583332,Archer City Bonebed 1 (Putnam Fm.),NA,"Locality IIIf (Romer & Price, 1940)",US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"P. M. Sander. 1989. Early Permian Depositional Environments of Pond Bonebeds in Central Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 69:1-21",315,334,14,J. Mueller,T. Liebrecht,M. Carrano,27/12/2008 10:06,10/12/2012 14:44,43845,megacephalus,Eryops,5743,,296.4,268,Wolfcamp,,NA,US,Eryops megacephalus
789966,occ,NA,,79162,,Zatrachys serratus,species,255221,,Zatrachys serratus,NA,species,255221,Sander,1989,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,,-98.650002,33.583332,Archer City Bonebed 1 (Putnam Fm.),NA,"Locality IIIf (Romer & Price, 1940)",US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,"P. M. Sander. 1989. Early Permian Depositional Environments of Pond Bonebeds in Central Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 69:1-21",315,334,14,J. Mueller,T. Liebrecht,M. Carrano,27/12/2008 10:06,10/12/2012 14:44,43845,serratus,Zatrachys,5743,,296.4,268,Wolfcamp,,NA,US,Zatrachys serratus
789967,occ,NA,,79162,,Acheloma cumminsi,species,81713,,Acheloma cumminsi,NA,species,81713,Sander,1989,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,37048,NA,NA,NA,individuals,-98.650002,33.583332,Archer City Bonebed 1 (Putnam Fm.),NA,"Locality IIIf (Romer & Price, 1940)",US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Acheloma,,NA,NA,vertebrate,"P. M. Sander. 1989. Early Permian Depositional Environments of Pond Bonebeds in Central Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 69:1-21",315,334,14,J. Mueller,T. Liebrecht,M. Carrano,27/12/2008 10:16,10/12/2012 14:44,43845,cumminsi,Acheloma,5743,,296.4,268,Wolfcamp,,1,US,Acheloma cumminsi
789968,occ,NA,,79162,,Acheloma n. sp. pricei,species,230701,recombined as,Phonerpeton pricei,NA,species,230701,Sander,1989,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,230700,NA,NA,NA,individuals,-98.650002,33.583332,Archer City Bonebed 1 (Putnam Fm.),NA,"Locality IIIf (Romer & Price, 1940)",US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Acheloma,,NA,NA,vertebrate,"P. M. Sander. 1989. Early Permian Depositional Environments of Pond Bonebeds in Central Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 69:1-21",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,27/12/2008 10:16,08/07/2016 06:14,43845,pricei,Phonerpeton,5743,n. sp.,296.4,268,Wolfcamp,,1,US,Phonerpeton pricei
789969,occ,NA,,79162,,Archeria crassidisca,species,345353,,Archeria crassidisca,NA,species,229309,Sander,1989,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,individuals,-98.650002,33.583332,Archer City Bonebed 1 (Putnam Fm.),NA,"Locality IIIf (Romer & Price, 1940)",US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,,NA,NA,vertebrate,"P. M. Sander. 1989. Early Permian Depositional Environments of Pond Bonebeds in Central Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 69:1-21",315,334,14,J. Mueller,T. Liebrecht,M. Carrano,27/12/2008 10:16,10/12/2012 14:44,43845,crassidisca,Archeria,5743,,296.4,268,Wolfcamp,,1,US,Archeria crassidisca
789970,occ,NA,,79162,,Bolosaurus striatus,species,138029,,Bolosaurus striatus,NA,species,138029,Sander,1989,Chordata,33815,Reptilia,36322,,NA,Bolosauridae,37510,37511,NA,NA,NA,individuals,-98.650002,33.583332,Archer City Bonebed 1 (Putnam Fm.),NA,"Locality IIIf (Romer & Price, 1940)",US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Bolosaurus,,NA,NA,vertebrate,"P. M. Sander. 1989. Early Permian Depositional Environments of Pond Bonebeds in Central Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 69:1-21",315,334,14,J. Mueller,T. Liebrecht,M. Carrano,27/12/2008 10:16,10/12/2012 14:44,43845,striatus,Bolosaurus,5743,,296.4,268,Wolfcamp,,1,US,Bolosaurus striatus
789971,occ,NA,,79162,,n. gen. Theropleura n. sp. uniformis,species,138049,recombined as,Ophiacodon uniformis,NA,species,138049,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-98.650002,33.583332,Archer City Bonebed 1 (Putnam Fm.),NA,"Locality IIIf (Romer & Price, 1940)",US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,n. gen.,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,27/12/2008 10:16,10/12/2012 14:44,43845,uniformis,Ophiacodon,5692,n. sp.,296.4,268,Wolfcamp,,2,US,Ophiacodon uniformis
789976,occ,NA,,52522,,n. gen. Palaeohatteria n. sp. longicaudata,species,138242,subjective synonym of,Haptodus baylei,NA,species,122354,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,38905,NA,NA,NA,,13.650278,50.999722,Niederhaslich,NA,Niederh_sslich; Niederh_slich; Nieder-H_sslich; Plauenscher Grund; D̦hlen Basin,DE,Saxony,Weieritzkreis,based on nearby landmark,seconds,outcrop,"Niederh_slich in the D̦hlen basin, today it is one part of the City of Freital, SW of Dresden in Sachsen; the outcrop does not exist anymore.",gp_mid,23.3,7.73,305,DE,,Niederh_slich-Schweinsdorf,Rotliegend,Niederh_slich limestone,member,,,,,,,NA,"""The Niederh_slich Formation belongs stratigraphically [...] to the Melanerpeton gracile-M. pulcherimus Zone, i. e. uppermost Unterrotliegend"" (U. Hoffman, 2002, Workshop _Oberkarbon - Untertrias in Zentraleuropa: Prozesse und ihr Timing [online] http://www.geo.tu-freiberg.de/palaeo/GeoTage-2002.pdf) (TL);\r\nthe Niederh_slich limestone is Asselian according to assorted references, e.g., Gebhardt and Schneider 1993 (JA)\r\nAccording to Roscher & Schneider (2006, in Lucas et al. (eds), Geol. Soc. Spec. Publ. 265) the Niederh_slich Fm. is Sakmarian in age (TL).",,"""limestone""",,,,,,,,,,lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Museum: Staatliches Museum f_r Mineralogie und Geologie, Dresden (SMMGD)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Palaeohatteria,n. gen.,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,327,J. Mueller,T. Liebrecht,R. Butler,27/12/2008 19:56,07/07/2015 11:27,14125,longicaudata,Haptodus,5692,n. sp.,295.5,290.1,Sakmarian,,NA,DE,Haptodus longicaudata
789977,occ,NA,,85474,,n. gen. Pantelosaurus n. sp. saxonicus,species,138246,subjective synonym of,Haptodus baylei,NA,species,122354,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,38905,NA,NA,NA,individuals,13.638056,51.018612,Konigin-Carola-Schacht,NA,"Queen Carola Pit; Plauenscher Grund; D̦hlen Basin, K̦nigin-Carola-Schacht",DE,Saxony,Weieritzkreis,based on nearby landmark,seconds,small collection,The abandoned coal pit K̦nigin-Carola-Schacht is situated in the district Zauckerode of the town of Freital near Dresden. Lat long is for Zauckerode. ,gp_mid,23.06,7.42,305,DE,,D̦hlen,Rotliegend,1. Fl̦z (1st seam),bed,,,,,,,NA,"""Cuseler Stufe, lower Rotliegend"" (Romer & Price, 1940);\r\n"" [...] die Skelettreste [...] sind [...] eindeutig der D̦hlen-Formation zuzuordnen."" [""...the skeletal remains [...] are unequivocally assignable to the D̦hlen-Formation.""] (Reichel & Schauer, 2006 p. 20/21, ""Das D̦hlener Becken bei Dresden - Geologie und Bergbau"" [online] http://www.umwelt.sachsen.de/de/wu/umwelt/lfug/lfug-internet/veroeffentlichungen/verzeichnis/Boden/Bergbau%20in%20Sachsen/BBB12.Ansicht.neu.pdf);\r\nThe 1st seam of the D̦hlen-Formation comprises the uppermost part of the latter. This part of the D̦hlen-Formation is Asselian in age, according to ""Stratigraphische Tabelle von Deutschland 2002""","""Die _Gr_ne Schale ist ein bis 20 cm m_chtiger grauer, feinschichtiger bis bl_ttriger pelitischer Horizont mit lindgr_nen Schmitzen, vermutlich ein Tuffit."" [""The 'Gr_ne Schale' is an up to 20 cm thick, grey, laminated or foliated, pelitic horizon with pastel green clay fragments, presumably a tuffite""] (Reichel & Schauer, 2006 p. 20, ""Das D̦hlener Becken bei Dresden - Geologie und Bergbau"" [online] http://www.umwelt.sachsen.de/de/wu/umwelt/lfug/lfug-internet/veroeffentlichungen/verzeichnis/Boden/Bergbau%20in%20Sachsen/BBB12.Ansicht.neu.pdf)","""shale""",gray,lithified,,,,,,,,fine channel fill,intramontane basin,"""[...] stratiforme, relativ schmale rinnen_hnliche Zonen, in denen Klastite als Suspensionen _ber das Flachmoor transportiert wurden."" [...stratiform, relatively narrow, channel-like zones, in which clastites were transported as suspension across the swamp.""] (Reichel & Schauer, 2006 p. 21)",macrofossils,,,,,,NA,,"body,adpression",good,autochthonous,snapshot,,,,,,,NA,,"""Die _bereinander liegenden Skelette zeigen keinerlei Anzeichen von Disartikulation. [...] Es hat also keinerlei Transport stattgefunden, die Skelette wurden nicht zusammengeschwemmt. [""The skeletons lying upon another do not show any sign of disarticulation. [...] Hence, no transport took place, the skeletons were not washed together.""] (Reichel & Schauer, 2006 p. 21, ""Das D̦hlener Becken bei Dresden - Geologie und Bergbau"" [online] http://www.umwelt.sachsen.de/de/wu/umwelt/lfug/lfug-internet/veroeffentlichungen/verzeichnis/Boden/Bergbau%20in%20Sachsen/BBB12.Ansicht.neu.pdf)",taxonomic,,,,,,,1901,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Pantelosaurus,n. gen.,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,28/12/2008 10:44,21/03/2016 09:04,5692,saxonicus,Haptodus,5692,n. sp.,298.9,295.5,Asselian,,6,DE,Haptodus saxonicus
789978,occ,NA,,85475,,n. gen. Cutleria n. sp. wilmarthi,species,138249,,Cutleria wilmarthi,NA,species,138249,Lewis and Vaughn,1965,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,138248,NA,NA,NA,individuals,-108.046387,38.02,Placerville Localities 3 + 4,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,about half a mile ENE from Placerville; north wall of San Miguel Canyon; see map on p. C9 in Lewis & Vaughn (1965),gp_mid,-33.86,6.69,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"about 80-90 feet below top of Cutler Fm.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)\r\n","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"bulk,field collection","MCZ,USNM",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cutleria,n. gen.,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,0,J. Mueller,T. Liebrecht,,29/12/2008 08:59,29/12/2008 10:59,28872,wilmarthi,Cutleria,28872,n. sp.,296.4,268,Wolfcamp,,1,US,Cutleria wilmarthi
789979,occ,NA,,85475,,Limnoscelops longifemur,species,138250,nomen dubium,Diadectomorpha,NA,unranked clade,95313,Lewis and Vaughn,1965,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,NA,NA,NA,NA,individuals,-108.046387,38.02,Placerville Localities 3 + 4,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,about half a mile ENE from Placerville; north wall of San Miguel Canyon; see map on p. C9 in Lewis & Vaughn (1965),gp_mid,-33.86,6.69,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"about 80-90 feet below top of Cutler Fm.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)\r\n","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"bulk,field collection","MCZ,USNM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Limnoscelops,,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,0,J. Mueller,T. Liebrecht,,29/12/2008 08:59,29/12/2008 10:59,28872,longifemur,,28872,,296.4,268,Wolfcamp,,1,US, longifemur
789980,occ,NA,,85476,,Ophiacodon sp.,genus,38888,,Ophiacodon,NA,genus,38888,Lewis and Vaughn,1965,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-108.123611,38.036388,Placerville Locality 1,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,about 4 miles WNW from Placerville; north wall of San Miguel Canyon; see map on p. C9 in Lewis & Vaughn (1965),gp_mid,-33.9,6.74,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"about 450-470 feet below top of Cutler Fm.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)\r\n","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"bulk,field collection",MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,0,J. Mueller,T. Liebrecht,,29/12/2008 09:23,29/12/2008 11:23,28872,sp.,Ophiacodon,28872,,296.4,268,Wolfcamp,,1,US,Ophiacodon sp.
789981,occ,NA,,85476,,Pelycosauria ? indet.,order,138244,,Pelycosauria,NA,order,38883,Lewis and Vaughn,1965,Chordata,33815,Osteichthyes,34881,Pelycosauria,38883,,NA,NA,NA,NA,NA,individuals,-108.123611,38.036388,Placerville Locality 1,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,about 4 miles WNW from Placerville; north wall of San Miguel Canyon; see map on p. C9 in Lewis & Vaughn (1965),gp_mid,-33.9,6.74,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"about 450-470 feet below top of Cutler Fm.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)\r\n","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"bulk,field collection",MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Pelycosauria,?,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,29/12/2008 09:33,29/12/2008 11:34,28872,indet.,,28872,,296.4,268,Wolfcamp,,1,US, indet.
789982,occ,NA,,85477,,Pelycosauria sp.,genus,138244,,Pelycosauria,NA,order,38883,Lewis and Vaughn,1965,Chordata,33815,Osteichthyes,34881,Pelycosauria,38883,,NA,NA,NA,NA,NA,individuals,-108.114723,38.037777,Placerville Locality 2,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,about 3 1/2 miles WNW from Placerville; north wall of San Miguel Canyon; see map on p. C9 in Lewis & Vaughn (1965),gp_mid,-33.89,6.74,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"about 250-260 feet below top of Cutler Fm.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)\r\n","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,"body,mold/impression",,,,,,,,,,NA,,,taxonomic,"bulk,field collection",MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Pelycosauria,,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,29/12/2008 09:40,29/12/2008 11:40,28872,sp.,,28872,,296.4,268,Wolfcamp,,1,US, sp.
789983,occ,NA,,85478,,Mycterosaurus smithae,species,138251,recombined as,Vaughnictis smithae,NA,species,138251,Lewis and Vaughn,1965,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Eothyrididae,38898,345991,NA,NA,NA,individuals,-108.042221,38.006111,Placerville Localities 5 + 6,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,about 1 mile SE from Placerville; north wall of San Miguel Canyon; see map on p. C9 in Lewis & Vaughn (1965),gp_mid,-33.87,6.68,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"about 860-885 feet below top of Cutler Fm.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"bulk,field collection","MCZ,USNM",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Mycterosaurus,,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,0,J. Mueller,T. Liebrecht,,29/12/2008 09:54,29/12/2008 11:54,28872,smithae,Vaughnictis,28872,,296.4,268,Wolfcamp,,1,US,Vaughnictis smithae
789984,occ,NA,,85478,,Eryops cf. grandis,species,345659,,Eryops grandis,NA,species,345657,Lewis and Vaughn,1965,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,individuals,-108.042221,38.006111,Placerville Localities 5 + 6,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,about 1 mile SE from Placerville; north wall of San Miguel Canyon; see map on p. C9 in Lewis & Vaughn (1965),gp_mid,-33.87,6.68,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"about 860-885 feet below top of Cutler Fm.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"bulk,field collection","MCZ,USNM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,0,J. Mueller,T. Liebrecht,,29/12/2008 09:54,29/12/2008 11:54,28872,grandis,Eryops,28872,cf.,296.4,268,Wolfcamp,,1,US,Eryops grandis
789985,occ,NA,,85479,,Captorhinidae ? indet.,family,37495,,Captorhinidae,NA,family,37495,Lewis and Vaughn,1965,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,NA,NA,NA,NA,elements,-108.035835,38.005554,Placerville Localities 7-10,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,about 1.20 miles SE from Placerville; north wall of San Miguel Canyon; see map on p. C9 in Lewis & Vaughn (1965),gp_mid,-33.86,6.67,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"about 550-620 feet below top of Cutler Fm.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"bulk,field collection",MCZ,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinidae,?,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,29/12/2008 10:06,23/08/2016 06:42,28872,indet.,,28872,,296.4,268,Wolfcamp,,1,US, indet.
789986,occ,NA,,85479,,Platyhystrix rugosus,species,345923,,Platyhystrix rugosus,NA,species,194929,Lewis and Vaughn,1965,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37034,NA,NA,NA,individuals,-108.035835,38.005554,Placerville Localities 7-10,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,about 1.20 miles SE from Placerville; north wall of San Miguel Canyon; see map on p. C9 in Lewis & Vaughn (1965),gp_mid,-33.86,6.67,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"about 550-620 feet below top of Cutler Fm.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"bulk,field collection",MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Platyhystrix,,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,29/12/2008 10:10,23/08/2016 06:42,28872,rugosus,Platyhystrix,28872,,296.4,268,Wolfcamp,,1,US,Platyhystrix rugosus
789987,occ,NA,,85479,,Seymouria sp.,genus,37223,,Seymouria,NA,genus,37223,Lewis and Vaughn,1965,Chordata,33815,Osteichthyes,34881,,NA,Seymouriidae,37219,37223,NA,NA,NA,individuals,-108.035835,38.005554,Placerville Localities 7-10,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,about 1.20 miles SE from Placerville; north wall of San Miguel Canyon; see map on p. C9 in Lewis & Vaughn (1965),gp_mid,-33.86,6.67,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"about 550-620 feet below top of Cutler Fm.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"bulk,field collection",MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Seymouria,,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,29/12/2008 10:10,23/08/2016 06:42,28872,sp.,Seymouria,28872,,296.4,268,Wolfcamp,,1,US,Seymouria sp.
789988,occ,NA,,85479,,n. gen. Limnoscelops n. sp. longifemur,species,138250,nomen dubium,Diadectomorpha,NA,unranked clade,95313,Lewis and Vaughn,1965,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,NA,NA,NA,NA,individuals,-108.035835,38.005554,Placerville Localities 7-10,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,about 1.20 miles SE from Placerville; north wall of San Miguel Canyon; see map on p. C9 in Lewis & Vaughn (1965),gp_mid,-33.86,6.67,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"about 550-620 feet below top of Cutler Fm.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"bulk,field collection",MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Limnoscelops,n. gen.,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,29/12/2008 10:10,23/08/2016 06:42,28872,longifemur,,28872,n. sp.,296.4,268,Wolfcamp,,1,US, longifemur
789989,occ,NA,,85479,,Pelycosauria sp.,genus,138244,,Pelycosauria,NA,order,38883,Lewis and Vaughn,1965,Chordata,33815,Osteichthyes,34881,Pelycosauria,38883,,NA,NA,NA,NA,NA,elements,-108.035835,38.005554,Placerville Localities 7-10,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,about 1.20 miles SE from Placerville; north wall of San Miguel Canyon; see map on p. C9 in Lewis & Vaughn (1965),gp_mid,-33.86,6.67,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"about 550-620 feet below top of Cutler Fm.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"bulk,field collection",MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Pelycosauria,,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,29/12/2008 10:27,23/08/2016 06:42,28872,sp.,,28872,,296.4,268,Wolfcamp,,1,US, sp.
789990,occ,NA,,85480,,Mycterosaurus n. sp. smithae,species,138251,recombined as,Vaughnictis smithae,NA,species,138251,Lewis and Vaughn,1965,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Eothyrididae,38898,345991,NA,NA,NA,individuals,-108.029167,37.999443,Placerville Localities 11-13,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,about 1.80 miles SE from Placerville; north wall of San Miguel Canyon; see map on p. C9 in Lewis & Vaughn (1965),gp_mid,-33.86,6.66,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"about 100-200 feet below top of Cutler Fm.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"bulk,field collection",MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Mycterosaurus,,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,29/12/2008 10:32,11/08/2016 08:22,28872,smithae,Vaughnictis,28872,n. sp.,296.4,268,Wolfcamp,,1,US,Vaughnictis smithae
789991,occ,NA,,85480,,Pelycosauria sp.,genus,138244,,Pelycosauria,NA,order,38883,Lewis and Vaughn,1965,Chordata,33815,Osteichthyes,34881,Pelycosauria,38883,,NA,NA,NA,NA,NA,individuals,-108.029167,37.999443,Placerville Localities 11-13,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,about 1.80 miles SE from Placerville; north wall of San Miguel Canyon; see map on p. C9 in Lewis & Vaughn (1965),gp_mid,-33.86,6.66,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"about 100-200 feet below top of Cutler Fm.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"bulk,field collection",MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Pelycosauria,,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,29/12/2008 10:32,11/08/2016 08:22,28872,sp.,,28872,,296.4,268,Wolfcamp,,2,US, sp.
789992,occ,NA,,85480,,Cutleria wilmarthi,species,138249,,Cutleria wilmarthi,NA,species,138249,Lewis and Vaughn,1965,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,138248,NA,NA,NA,individuals,-108.029167,37.999443,Placerville Localities 11-13,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,about 1.80 miles SE from Placerville; north wall of San Miguel Canyon; see map on p. C9 in Lewis & Vaughn (1965),gp_mid,-33.86,6.66,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"about 100-200 feet below top of Cutler Fm.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"bulk,field collection",MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cutleria,,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,29/12/2008 10:32,11/08/2016 08:23,28872,wilmarthi,Cutleria,28872,,296.4,268,Wolfcamp,,1,US,Cutleria wilmarthi
789993,occ,NA,,85481,,Diadectes n. sp. sanmiguelensis,species,138330,recombined as,Oradectes sanmiguelensis,NA,species,138330,Lewis and Vaughn,1965,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,345910,NA,NA,NA,individuals,-108.020279,37.996387,Placerville Locality 14,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,about 2.70 miles SE from Placerville; north wall of San Miguel Canyon; see map on p. C9 in Lewis & Vaughn (1965),gp_mid,-33.86,6.66,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"about 550-575 feet below top of Cutler Fm.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"bulk,field collection",MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,0,J. Mueller,T. Liebrecht,,29/12/2008 10:50,29/12/2008 12:50,28872,sanmiguelensis,Oradectes,28872,n. sp.,296.4,268,Wolfcamp,,1,US,Oradectes sanmiguelensis
789994,occ,NA,,85482,,Ophiacodontia indet.,suborder,138253,,Ophiacodontia,NA,suborder,138253,Lewis and Vaughn,1965,Chordata,33815,Osteichthyes,34881,Pelycosauria,38883,,NA,NA,NA,NA,NA,individuals,-108.000557,37.99472,Placerville Locality 15 + 16,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,"No exact position is given for these localities. Because the localities 1 to 14 (see collections 85475-85481) are numbered ascending from west to east, the localities with higher number than 14 must be located east of locality 14. Lat long here is for Sawpit, a settlement about 3.5 miles SE of Placerville. ",gp_mid,-33.85,6.65,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"No exact stratigraphic position is given for this locality.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"bulk,field collection",MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodontia,,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,0,J. Mueller,T. Liebrecht,,29/12/2008 11:15,29/12/2008 13:15,28872,indet.,,28872,,296.4,268,Wolfcamp,,1,US, indet.
790002,occ,NA,,85482,,Pelycosauria indet.,order,138244,,Pelycosauria,NA,order,38883,Lewis and Vaughn,1965,Chordata,33815,Osteichthyes,34881,Pelycosauria,38883,,NA,NA,NA,NA,NA,fragments,-108.000557,37.99472,Placerville Locality 15 + 16,NA,San Miguel Canyon,US,Colorado,San Miguel,estimated from map,seconds,small collection,"No exact position is given for these localities. Because the localities 1 to 14 (see collections 85475-85481) are numbered ascending from west to east, the localities with higher number than 14 must be located east of locality 14. Lat long here is for Sawpit, a settlement about 3.5 miles SE of Placerville. ",gp_mid,-33.85,6.65,101,US,FED,Cutler,,,group of beds,,,,,,,NA,"No exact stratigraphic position is given for this locality.\r\n"" [...] the present [...] study [...] has convinced us that the age is Early Permian beyond all reasonable doubt, equivalent to that of the Moran, Putnam, and Admiral Formations of Texas."" (Lewis & Vaughn, 1965 p. C41). According to that statement the collection is of Wolfcampian age. \r\n","""In the Placerville area, the Cutler Formation is made up of interbedded, interlensing conglomerate, sandstone, siltstone, and shale. [...] The coarse clastic rock outcrops are generally a dark red to maroon, but they are gray to \r\ngreenish gray in some places. [...] Crossbedding is common. Torrential deposition took place, as shown by lateral gradation, interlensing, and interbed\r\nding between sandstone and conglomerate. No individual beds of conglomerate can be traced laterally for more than a few hundred feet. Finer grained micaceous sandstone, siltstone, and shale that weather to hematite red commonly contain bleached zones from 1 to 75 mm in diameter; these zones seemingly have organic centers. These finer clastics yielded almost all the fossil vertebrates; they contain many mud cracks and raindrop and other impressions including footprints."" (Lewis & Vaughn, 1965 p. C5)","""siliciclastic""","desiccation cracks,very fine,fine,micaceous,red",,,Y,conglomerate,"lenticular,""cross stratification"",gray,red or brown",,,,fluvial-lacustrine indet.,,No interpretation is given by the authors. The description of the rocks suggests that they represent a playa setting with periodically active alluvial fans.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"bulk,field collection",MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Pelycosauria,,NA,NA,vertebrate,"G. E. Lewis and P. P. Vaughn. 1965. Early Permian Vertebrates from the Cutler Formation of the Placerville Area, Colorado. United States Geological Survey Professional Papers 503-C:C1-C46",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,30/12/2008 07:39,30/12/2008 09:40,28872,indet.,,28872,,296.4,268,Wolfcamp,,1,US, indet.
790003,occ,NA,,80112,,n. gen. Georgenthalia n. sp. clavinasica,species,123084,,Georgenthalia clavinasica,NA,species,123084,Anderson et al.,2008,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,123078,NA,NA,NA,individuals,10.618889,50.809723,Bromacker Quarry (upper level of Tambach sandstone),NA,,DE,Thuringia,Gotha,based on nearby landmark,seconds,outcrop,"""...middle part of the Thuringian Forest near the village of Tambach-Dietharz and about 20 km south of the town of Gotha, central Germany.""",gp_mid,21.71,7.41,305,DE,,Tambach,Rotliegend,Tambach-Sandstein,group of beds,,,,,,,NA,"""At the Bromacker quarry site are two superimposed stratigraphic successions that can be characterized by their facies associations and are referred to as the Lower Beds and Upper Beds (Eberth et al. 2000). All the vertebrates from the Bromacker quarry come from the Upper Beds [...]. The vertebrates are almost exclusively restricted to two [... horizons ...] which are separated by 50 cm in a stratigraphic interval of 1.2 m."" (Berman et al., 2001)\r\nThe Tambach Formation is of Artinskian age according to ""Stratigraphische Tabelle von Deutschland 2002"", however, a Kungurian age is proposed by L_tzner (2006) in LITHOLEX stratigraphic online database [http://www.bgr.de/app/LithoLex/gesamt_ausgabe_neu.php5?id=25]","""massive, red-brown, very fine-grained sandstone and siltstone"" (Berman et al., 2001).\r\nFor further details see Eberth et al. (2000).",sandstone,"very fine,brown,red",lithified,,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,"""alluvial paleochannel and sheetflood facies and lacustrine suspension deposits"" (Berman et al., 2001).\r\n""During the time that the Lower and Upper beds were deposited, the Tambach Basin was internally-drained and probably characterized by a wet-and-dry tropical or wetter climate that was hot year-round with seasonal-to-subseasonal cycles of rainfall and drying. [...] In the Bromacker area, the floodbasin was never deeply desiccated or heavily vegetated between flooding events."" Eberth et al. (2000).",macrofossils,,,,,,NA,,"body,permineralized",excellent,,snapshot,,,,,,,NA,,,taxonomic,"bulk,field collection",,all macrofossils,,,,,"MNG = Museum der Natur, Gotha",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Georgenthalia,n. gen.,NA,NA,vertebrate,"J. S. Anderson, A. C. Henrici, and S. S. Sumida, T. Martens, D. S. Berman. 2008. Georgenthalia clavinasica, a new genus and species of dissorophoid temnospondyl from the Early Permian of Germany, and the relationships of the family Amphibamidae. Journal of Vertebrate Paleontology 28(1):61-75",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,30/12/2008 09:43,14/02/2012 14:44,26922,clavinasica,Georgenthalia,27263,n. sp.,290.1,279.3,Artinskian,,1,DE,Georgenthalia clavinasica
790154,occ,NA,,68427,,n. gen. Archaeovenator n. sp. hamiltonensis,species,138746,,Archaeovenator hamiltonensis,NA,species,138746,Reisz and Dilkes,2003,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,91796,NA,NA,NA,individuals,-96.113892,37.986111,Hamilton Quarry,NA,,US,Kansas,Greenwood,estimated from map,seconds,,"about 5 km E of Hamilton, Greenwood Co., Kansas, in secs. 5 and 6, T. 24 S., R. 12 E. (Virgil 7.5' quadrangle)",gp_mid,-26.91,-0.1,101,US,,Calhouns Shale,Shawnee,,,,,,,,,NA,"Virgillian Series, Upper Pennsylvanian; late Kasimovian according to Modesto et al. (2015)",,"""shale""",,,,,,,,,,estuary/bay,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archaeovenator,n. gen.,NA,NA,vertebrate,"R. R. Reisz and D. W. Dilkes. 2003. Archaeovenator hamiltonensis, a new varanopid (Synapsida: Eupelycosauria) from the Upper Carboniferous of Kansas. Canadian Journal of Earth Sciences 40(4):667-678",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,05/01/2009 18:06,23/12/2016 14:15,19706,hamiltonensis,Archaeovenator,28909,n. sp.,303.4,298.9,Virgilian,,1,US,Archaeovenator hamiltonensis
790298,occ,NA,,79162,,n. gen. Apsisaurus n. sp. witteri,species,138856,,Apsisaurus witteri,NA,species,138856,Laurin,1991,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,138851,NA,NA,NA,individuals,-98.650002,33.583332,Archer City Bonebed 1 (Putnam Fm.),NA,"Locality IIIf (Romer & Price, 1940)",US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Apsisaurus,n. gen.,NA,NA,vertebrate,M. Laurin. 1991. The osteology of a Lower Permian eosuchian from Texas and a review of diapsid phylogeny. Zoological Journal of the Linnean Society 101(1):59-95,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,07/01/2009 09:26,10/12/2012 14:44,43845,witteri,Apsisaurus,28920,n. sp.,296.4,268,Wolfcamp,,1,US,Apsisaurus witteri
790356,occ,NA,,85551,,Captorhinus sp.,genus,37497,,Captorhinus,NA,genus,37497,Olson,1948,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,,-99.576942,33.676109,Locality KB (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""Valley of South Wichita River, south of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.85,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,E. C. Olson,1946-1953,,"Although Olson (1956:331) stated that FMNH UR 29 was collected from locality KC (also in the upper part of the Clear Fork Formation; Olson, 1958: table 1), this is likely a lapsus calami, judging from his statement that this specimen was preserved in association with Captorhinus, and from his faunal lists for localities KB and KC in Olson (1958:430), which list Captorhinus and Edaphosaurid, n. gen., unnamed for the locality KB, whereas neither taxon is listed for KC in the 1958 publication. (Modesto et al, 2016).",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,E. C. Olson. 1948. A Preliminary Report on Vertebrates from the Permian Vale Formation of Texas. Journal of Geology 56:186-198,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,08/01/2009 08:00,15/03/2016 12:08,28928,sp.,Captorhinus,28928,,279.3,272.3,Kungurian,,NA,US,Captorhinus sp.
790357,occ,NA,,85551,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Olson,1948,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.576942,33.676109,Locality KB (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""Valley of South Wichita River, south of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.85,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,E. C. Olson,1946-1953,,"Although Olson (1956:331) stated that FMNH UR 29 was collected from locality KC (also in the upper part of the Clear Fork Formation; Olson, 1958: table 1), this is likely a lapsus calami, judging from his statement that this specimen was preserved in association with Captorhinus, and from his faunal lists for localities KB and KC in Olson (1958:430), which list Captorhinus and Edaphosaurid, n. gen., unnamed for the locality KB, whereas neither taxon is listed for KC in the 1958 publication. (Modesto et al, 2016).",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,E. C. Olson. 1948. A Preliminary Report on Vertebrates from the Permian Vale Formation of Texas. Journal of Geology 56:186-198,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,08/01/2009 08:00,15/03/2016 12:08,28928,sp.,Dimetrodon,28928,,279.3,272.3,Kungurian,,NA,US,Dimetrodon sp.
790358,occ,NA,R,85551,,Edaphosauridae sp.,genus,38910,,Edaphosauridae,NA,family,38910,Olson,1948,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,NA,NA,NA,NA,individuals,-99.576942,33.676109,Locality KB (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""Valley of South Wichita River, south of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.85,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,E. C. Olson,1946-1953,,"Although Olson (1956:331) stated that FMNH UR 29 was collected from locality KC (also in the upper part of the Clear Fork Formation; Olson, 1958: table 1), this is likely a lapsus calami, judging from his statement that this specimen was preserved in association with Captorhinus, and from his faunal lists for localities KB and KC in Olson (1958:430), which list Captorhinus and Edaphosaurid, n. gen., unnamed for the locality KB, whereas neither taxon is listed for KC in the 1958 publication. (Modesto et al, 2016).",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosauridae,,NA,NA,vertebrate,E. C. Olson. 1948. A Preliminary Report on Vertebrates from the Permian Vale Formation of Texas. Journal of Geology 56:186-198,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,08/01/2009 08:01,06/01/2017 07:18,28928,sp.,,28928,,279.3,272.3,Kungurian,,1,US, sp.
790358,occ,33055,,85551,,Moradisaurinae indet.,subfamily,134808,,Moradisaurinae,NA,subfamily,134808,Modesto et al.,2016,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,NA,NA,NA,NA,individuals,-99.576942,33.676109,Locality KB (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""Valley of South Wichita River, south of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.85,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,E. C. Olson,1946-1953,,"Although Olson (1956:331) stated that FMNH UR 29 was collected from locality KC (also in the upper part of the Clear Fork Formation; Olson, 1958: table 1), this is likely a lapsus calami, judging from his statement that this specimen was preserved in association with Captorhinus, and from his faunal lists for localities KB and KC in Olson (1958:430), which list Captorhinus and Edaphosaurid, n. gen., unnamed for the locality KB, whereas neither taxon is listed for KC in the 1958 publication. (Modesto et al, 2016).",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Moradisaurinae,,NA,NA,vertebrate,"S. Modesto, V. J. Flear, and M. M. Dilney, R. R. Reisz. 2016. A large moradisaurine tooth plate from the Lower Permian of Texas and its biostratigraphic implications. 36(6):e1221832",315,334,0,J. Mueller,T. Liebrecht,,06/01/2017 07:26,06/01/2017 07:26,28928,indet.,,61333,,279.3,272.3,Kungurian,,1,US, indet.
790361,occ,NA,,85552,,Dimetrodon ? sp.,genus,38904,,Dimetrodon,NA,genus,38904,Olson,1948,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.575836,33.665001,Locality KC (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""South Walls of valley of South Wichita River, west of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.24,1.84,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,E. C. Olson,"1946, 1947",,"The taxon Edaphosauridae sp., represented by the specimen CNHM UR 29, was removed from the taxon list according to Modesto et al. (2016; cf. PBD collection no. 85551)",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,?,NA,NA,vertebrate,E. C. Olson. 1948. A Preliminary Report on Vertebrates from the Permian Vale Formation of Texas. Journal of Geology 56:186-198,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,08/01/2009 08:06,15/03/2016 12:09,28928,sp.,Dimetrodon,28928,,279.3,272.3,Kungurian,,NA,US,Dimetrodon sp.
790363,occ,NA,,12976,,Gymnarthridae indet.,family,37293,,Gymnarthridae,NA,family,37293,Olson,1948,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,NA,NA,NA,NA,,-99.599998,33.703335,Locality KD,NA,(Upper Vale Fm.) Main site,US,Texas,Knox,estimated from map,seconds,outcrop,"""Valley of South Wichita River, north of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.88,101,US,,Vale,Clear Fork,"""Bullwagon""",group of beds,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surfacer and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,siltstone,lenticular,,,Y,dry floodplain,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",mesofossils,,,,,,NA,,body,variable,,snapshot,,,,,,occasional,NA,,,taxonomic,field collection,FMNH,,,,"E. C. Olson, E. L. Yochelson, S. H. Mamay","1946-1948, 1955","Olson (1958) divided the locality into Quarry Site and Weathered Boulder Site, leaving the main one for recording scattered finds",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Gymnarthridae,,NA,NA,vertebrate,E. C. Olson. 1948. A Preliminary Report on Vertebrates from the Permian Vale Formation of Texas. Journal of Geology 56:186-198,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,08/01/2009 08:23,16/03/2016 05:13,28928,indet.,,28928,,279.3,272.3,Kungurian,,NA,US, indet.
790364,occ,NA,,12976,,Lysorophus tricarinatus,species,70395,,Lysorophus tricarinatus,NA,species,70395,Olson,1948,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-99.599998,33.703335,Locality KD,NA,(Upper Vale Fm.) Main site,US,Texas,Knox,estimated from map,seconds,outcrop,"""Valley of South Wichita River, north of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.88,101,US,,Vale,Clear Fork,"""Bullwagon""",group of beds,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surfacer and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,siltstone,lenticular,,,Y,dry floodplain,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",mesofossils,,,,,,NA,,body,variable,,snapshot,,,,,,occasional,NA,,,taxonomic,field collection,FMNH,,,,"E. C. Olson, E. L. Yochelson, S. H. Mamay","1946-1948, 1955","Olson (1958) divided the locality into Quarry Site and Weathered Boulder Site, leaving the main one for recording scattered finds",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,E. C. Olson. 1948. A Preliminary Report on Vertebrates from the Permian Vale Formation of Texas. Journal of Geology 56:186-198,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,08/01/2009 08:23,16/03/2016 05:13,28928,tricarinatus,Lysorophus,28928,,279.3,272.3,Kungurian,,NA,US,Lysorophus tricarinatus
790366,occ,NA,,12976,,Labidosaurus barkeri,species,37501,species not entered,Labidosaurus,NA,genus,37501,Olson,1948,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,,-99.599998,33.703335,Locality KD,NA,(Upper Vale Fm.) Main site,US,Texas,Knox,estimated from map,seconds,outcrop,"""Valley of South Wichita River, north of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.88,101,US,,Vale,Clear Fork,"""Bullwagon""",group of beds,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surfacer and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,siltstone,lenticular,,,Y,dry floodplain,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",mesofossils,,,,,,NA,,body,variable,,snapshot,,,,,,occasional,NA,,,taxonomic,field collection,FMNH,,,,"E. C. Olson, E. L. Yochelson, S. H. Mamay","1946-1948, 1955","Olson (1958) divided the locality into Quarry Site and Weathered Boulder Site, leaving the main one for recording scattered finds",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,vertebrate,E. C. Olson. 1948. A Preliminary Report on Vertebrates from the Permian Vale Formation of Texas. Journal of Geology 56:186-198,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,08/01/2009 08:23,16/03/2016 05:13,28928,barkeri,Labidosaurus,28928,,279.3,272.3,Kungurian,,NA,US,Labidosaurus barkeri
790368,occ,NA,,12976,,Edaphosauridae sp.,genus,38910,,Edaphosauridae,NA,family,38910,Olson,1948,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,NA,NA,NA,NA,,-99.599998,33.703335,Locality KD,NA,(Upper Vale Fm.) Main site,US,Texas,Knox,estimated from map,seconds,outcrop,"""Valley of South Wichita River, north of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.88,101,US,,Vale,Clear Fork,"""Bullwagon""",group of beds,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surfacer and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,siltstone,lenticular,,,Y,dry floodplain,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",mesofossils,,,,,,NA,,body,variable,,snapshot,,,,,,occasional,NA,,,taxonomic,field collection,FMNH,,,,"E. C. Olson, E. L. Yochelson, S. H. Mamay","1946-1948, 1955","Olson (1958) divided the locality into Quarry Site and Weathered Boulder Site, leaving the main one for recording scattered finds",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosauridae,,NA,NA,vertebrate,E. C. Olson. 1948. A Preliminary Report on Vertebrates from the Permian Vale Formation of Texas. Journal of Geology 56:186-198,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,08/01/2009 08:23,16/03/2016 05:13,28928,sp.,,28928,,279.3,272.3,Kungurian,,NA,US, sp.
790369,occ,NA,,85552,,Captorhinus aguti,species,90718,,Captorhinus aguti,NA,species,134887,Olson,1954,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-99.575836,33.665001,Locality KC (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""South Walls of valley of South Wichita River, west of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.24,1.84,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,E. C. Olson,"1946, 1947",,"The taxon Edaphosauridae sp., represented by the specimen CNHM UR 29, was removed from the taxon list according to Modesto et al. (2016; cf. PBD collection no. 85551)",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,E. C. Olson. 1954. Fauna of the Vale and Choza: 9. Captorhinomorpha. Fieldiana: Geology 10(19):211-218,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,08/01/2009 08:34,15/03/2016 12:09,28928,aguti,Captorhinus,26907,,279.3,272.3,Kungurian,,1,US,Captorhinus aguti
790374,occ,NA,,85553,,Dimetrodon gigashomogenes,species,138123,,Dimetrodon gigashomogenes,NA,species,138123,Olson,1948,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.574448,33.721668,Locality KE (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""Valley of South Wichita River, north of River and east of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.21,1.88,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,E. C. Olson,"1946, 1947",,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,E. C. Olson. 1948. A Preliminary Report on Vertebrates from the Permian Vale Formation of Texas. Journal of Geology 56:186-198,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,08/01/2009 09:50,15/03/2016 11:18,28928,gigashomogenes,Dimetrodon,28928,,279.3,272.3,Kungurian,,NA,US,Dimetrodon gigashomogenes
790376,occ,NA,,27704,,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Olson,1948,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.557777,33.731667,Locality KF (Middle Vale Formation),NA,"three-channel hill, ""fish quarry""",US,Texas,Knox,estimated from map,seconds,small collection,"""approx. seven miles north of Vera, Knox County, Texas"" (Olson, 1951)\r\n""North wall of valley of South Wichita River, east of Vera-Gilliland road"" (Olson, 1948); for details see map on p. 188 in Olson (1948)",gp_mid,-29.19,1.89,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""The locality [...] KF, was assigned to the upper Vale in an earlier paper. More recent field work has shown that it comprises beds that must be assigned to the middle rather than the upper part of the Vale."" (Olson, 1954 p. 213)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191);\r\nspecimen ""was preserved in a nodule that had weathered from a conglomeratic deposit of channel origin."" (Olson, 1951 p. 89) other specimens are from a quarry in fine-grained, green channel deposits",conglomerate,"pebbly,green,red",,,Y,"""siliciclastic""","fine,green",,,Y,"""channel""",foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,,,,NA,,"""Fragmentation of the specimens occurred before and during deposition, probably as the materials were transported by the waters of the streams. This group of animals cannot be considered to represent a life assemblage."" (Olson, 1955 p. 258)",taxonomic,field collection,FMNH,,,,E. C. Olson,1946-1948,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,E. C. Olson. 1948. A Preliminary Report on Vertebrates from the Permian Vale Formation of Texas. Journal of Geology 56:186-198,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,08/01/2009 10:57,15/03/2016 11:15,28928,sp.,Diplocaulus,28928,,279.3,272.3,Kungurian,,NA,US,Diplocaulus sp.
790377,occ,NA,,27704,,Gymnarthridae indet.,family,37293,,Gymnarthridae,NA,family,37293,Olson,1948,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,NA,NA,NA,NA,,-99.557777,33.731667,Locality KF (Middle Vale Formation),NA,"three-channel hill, ""fish quarry""",US,Texas,Knox,estimated from map,seconds,small collection,"""approx. seven miles north of Vera, Knox County, Texas"" (Olson, 1951)\r\n""North wall of valley of South Wichita River, east of Vera-Gilliland road"" (Olson, 1948); for details see map on p. 188 in Olson (1948)",gp_mid,-29.19,1.89,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""The locality [...] KF, was assigned to the upper Vale in an earlier paper. More recent field work has shown that it comprises beds that must be assigned to the middle rather than the upper part of the Vale."" (Olson, 1954 p. 213)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191);\r\nspecimen ""was preserved in a nodule that had weathered from a conglomeratic deposit of channel origin."" (Olson, 1951 p. 89) other specimens are from a quarry in fine-grained, green channel deposits",conglomerate,"pebbly,green,red",,,Y,"""siliciclastic""","fine,green",,,Y,"""channel""",foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,,,,NA,,"""Fragmentation of the specimens occurred before and during deposition, probably as the materials were transported by the waters of the streams. This group of animals cannot be considered to represent a life assemblage."" (Olson, 1955 p. 258)",taxonomic,field collection,FMNH,,,,E. C. Olson,1946-1948,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Gymnarthridae,,NA,NA,vertebrate,E. C. Olson. 1948. A Preliminary Report on Vertebrates from the Permian Vale Formation of Texas. Journal of Geology 56:186-198,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,08/01/2009 10:57,15/03/2016 11:15,28928,indet.,,28928,,279.3,272.3,Kungurian,,NA,US, indet.
790378,occ,NA,,27704,,Lysorophus sp.,genus,37322,,Lysorophus,NA,genus,37322,Olson,1948,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-99.557777,33.731667,Locality KF (Middle Vale Formation),NA,"three-channel hill, ""fish quarry""",US,Texas,Knox,estimated from map,seconds,small collection,"""approx. seven miles north of Vera, Knox County, Texas"" (Olson, 1951)\r\n""North wall of valley of South Wichita River, east of Vera-Gilliland road"" (Olson, 1948); for details see map on p. 188 in Olson (1948)",gp_mid,-29.19,1.89,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""The locality [...] KF, was assigned to the upper Vale in an earlier paper. More recent field work has shown that it comprises beds that must be assigned to the middle rather than the upper part of the Vale."" (Olson, 1954 p. 213)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191);\r\nspecimen ""was preserved in a nodule that had weathered from a conglomeratic deposit of channel origin."" (Olson, 1951 p. 89) other specimens are from a quarry in fine-grained, green channel deposits",conglomerate,"pebbly,green,red",,,Y,"""siliciclastic""","fine,green",,,Y,"""channel""",foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,,,,NA,,"""Fragmentation of the specimens occurred before and during deposition, probably as the materials were transported by the waters of the streams. This group of animals cannot be considered to represent a life assemblage."" (Olson, 1955 p. 258)",taxonomic,field collection,FMNH,,,,E. C. Olson,1946-1948,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,E. C. Olson. 1948. A Preliminary Report on Vertebrates from the Permian Vale Formation of Texas. Journal of Geology 56:186-198,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,08/01/2009 10:57,15/03/2016 11:15,28928,sp.,Lysorophus,28928,,279.3,272.3,Kungurian,,NA,US,Lysorophus sp.
790380,occ,NA,,27704,,Edaphosaurus ? sp.,genus,38911,,Edaphosaurus,NA,genus,38911,Olson,1948,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,,-99.557777,33.731667,Locality KF (Middle Vale Formation),NA,"three-channel hill, ""fish quarry""",US,Texas,Knox,estimated from map,seconds,small collection,"""approx. seven miles north of Vera, Knox County, Texas"" (Olson, 1951)\r\n""North wall of valley of South Wichita River, east of Vera-Gilliland road"" (Olson, 1948); for details see map on p. 188 in Olson (1948)",gp_mid,-29.19,1.89,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""The locality [...] KF, was assigned to the upper Vale in an earlier paper. More recent field work has shown that it comprises beds that must be assigned to the middle rather than the upper part of the Vale."" (Olson, 1954 p. 213)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191);\r\nspecimen ""was preserved in a nodule that had weathered from a conglomeratic deposit of channel origin."" (Olson, 1951 p. 89) other specimens are from a quarry in fine-grained, green channel deposits",conglomerate,"pebbly,green,red",,,Y,"""siliciclastic""","fine,green",,,Y,"""channel""",foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,,,,NA,,"""Fragmentation of the specimens occurred before and during deposition, probably as the materials were transported by the waters of the streams. This group of animals cannot be considered to represent a life assemblage."" (Olson, 1955 p. 258)",taxonomic,field collection,FMNH,,,,E. C. Olson,1946-1948,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,?,NA,NA,vertebrate,E. C. Olson. 1948. A Preliminary Report on Vertebrates from the Permian Vale Formation of Texas. Journal of Geology 56:186-198,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,08/01/2009 10:57,15/03/2016 11:15,28928,sp.,Edaphosaurus,28928,,279.3,272.3,Kungurian,,NA,US,Edaphosaurus sp.
790382,occ,NA,,85554,,Dimetrodon ? sp.,genus,38904,,Dimetrodon,NA,genus,38904,Olson,1948,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.586945,33.737221,Locality KG (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""North wall of valley of South Wichita River, east of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.21,1.9,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,E. C. Olson,"1946, 1947",,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,?,NA,NA,vertebrate,E. C. Olson. 1948. A Preliminary Report on Vertebrates from the Permian Vale Formation of Texas. Journal of Geology 56:186-198,315,334,0,J. Mueller,T. Liebrecht,,08/01/2009 11:14,08/01/2009 13:14,28928,sp.,Dimetrodon,28928,,279.3,272.3,Kungurian,,NA,US,Dimetrodon sp.
790388,occ,NA,,85556,,Labidosaurikos barkeri,species,119514,subjective synonym of,Labidosaurikos meachami,NA,species,119515,Olson,1954,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37500,NA,NA,NA,individuals,-99.40667,33.736942,Crooked Creek (Lower Vale Fm.),NA,,US,Texas,Baylor,estimated from map,seconds,outcrop,"""Crooked Creek area""",gp_mid,-29.08,1.83,101,US,,Vale,Clear Fork,,group of beds,,,,,,,NA,"""Lower Part of Vale formation""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,medium,,snapshot,,,,,,,NA,,,taxonomic,field collection,,,,,E. C. Olson,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurikos,,NA,NA,vertebrate,E. C. Olson. 1954. Fauna of the Vale and Choza: 9. Captorhinomorpha. Fieldiana: Geology 10(19):211-218,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,08/01/2009 11:59,08/01/2009 14:03,26910,barkeri,Labidosaurikos,26907,,279.3,272.3,Kungurian,,2,US,Labidosaurikos barkeri
790389,occ,NA,,85555,,Labidosaurikos barkeri,species,119514,subjective synonym of,Labidosaurikos meachami,NA,species,119515,Olson,1954,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37500,NA,NA,NA,individuals,-99.548615,33.7575,Locality KH (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,outcrop,"""Southern margin of valley of North Wichita River""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.17,1.9,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" (Olson, 1948 p. 190);\r\n""base of upper part of Vale"" (Olson, 1954)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,E. C. Olson,"1946, 1947",,"This collection represents the scattered finds at the locality. Olson (1958) subdivided the locality into four sub-locations: Clay Hill site, Diplocaulus Quarry Site, and Chocolate Hill Site.",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurikos,,NA,NA,vertebrate,E. C. Olson. 1954. Fauna of the Vale and Choza: 9. Captorhinomorpha. Fieldiana: Geology 10(19):211-218,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,08/01/2009 12:13,15/03/2016 11:19,28928,barkeri,Labidosaurikos,26907,,279.3,272.3,Kungurian,,1,US,Labidosaurikos barkeri
790482,occ,NA,,85555,,Captorhinikos valensis,species,120855,,Captorhinikos valensis,NA,species,120855,Olson,1954,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37496,NA,NA,NA,individuals,-99.548615,33.7575,Locality KH (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,outcrop,"""Southern margin of valley of North Wichita River""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.17,1.9,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" (Olson, 1948 p. 190);\r\n""base of upper part of Vale"" (Olson, 1954)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,E. C. Olson,"1946, 1947",,"This collection represents the scattered finds at the locality. Olson (1958) subdivided the locality into four sub-locations: Clay Hill site, Diplocaulus Quarry Site, and Chocolate Hill Site.",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinikos,,NA,NA,vertebrate,E. C. Olson. 1954. Fauna of the Vale and Choza: 9. Captorhinomorpha. Fieldiana: Geology 10(19):211-218,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,09/01/2009 04:49,15/03/2016 11:19,28928,valensis,Captorhinikos,26907,,279.3,272.3,Kungurian,,1,US,Captorhinikos valensis
790483,occ,NA,,85551,,Captorhinikos valensis,species,120855,,Captorhinikos valensis,NA,species,120855,Olson,1954,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37496,NA,NA,NA,individuals,-99.576942,33.676109,Locality KB (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""Valley of South Wichita River, south of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.85,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,E. C. Olson,1946-1953,,"Although Olson (1956:331) stated that FMNH UR 29 was collected from locality KC (also in the upper part of the Clear Fork Formation; Olson, 1958: table 1), this is likely a lapsus calami, judging from his statement that this specimen was preserved in association with Captorhinus, and from his faunal lists for localities KB and KC in Olson (1958:430), which list Captorhinus and Edaphosaurid, n. gen., unnamed for the locality KB, whereas neither taxon is listed for KC in the 1958 publication. (Modesto et al, 2016).",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinikos,,NA,NA,vertebrate,E. C. Olson. 1954. Fauna of the Vale and Choza: 9. Captorhinomorpha. Fieldiana: Geology 10(19):211-218,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,09/01/2009 04:53,15/03/2016 12:08,28928,valensis,Captorhinikos,26907,,279.3,272.3,Kungurian,,1,US,Captorhinikos valensis
790486,occ,NA,,79163,,n. gen. Protorothyris n. sp. archeri,species,135430,,Protorothyris archeri,NA,species,135430,Clark and Carroll,1973,Chordata,33815,Reptilia,36322,,NA,Protorothyrididae,37486,37494,NA,NA,NA,individuals,-98.777496,33.449722,Cottonwood Creek (Moran Fm.),NA,Locality IIb (Romer & Price),US,Texas,Archer,estimated from map,seconds,outcrop,"Cottonwood Creek is a tributary of the south fork of the Little Wichita River (about 10 miles south of Archer City). Locality is ""near the head of Cottonwood Creek, close to the southern border of Archer Co."" (Romer & Price, 1940) ",gp_mid,-30.65,-2.02,101,US,,Archer City,Wichita,,group of beds,,,,,,,NA,"""about 50 feet below the Sedwick limestone equivalent"" (Clark & Carroll, 1973)\r\nThe former Moran Formation comprises the lower part of the Archer City Formation (Hentz, 1988, The University of Texas at Austin, Bureau of Economic Geology, Report of Investigations, 170).",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,observed (not collected),MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Protorothyris,n. gen.,NA,NA,vertebrate,J. Clark and R. L. Carroll. 1973. Romeriid Reptiles from the Lower Permian. Bulletin of the Museum of Comparative Zoology 144(5):353-407,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,09/01/2009 08:22,10/12/2012 14:38,28415,archeri,Protorothyris,28415,n. sp.,298.9,295.5,Asselian,,5,US,Protorothyris archeri
790487,occ,NA,,79163,,Romeria n. sp. primus,species,135431,corrected to,Romeria prima,NA,species,135431,Clark and Carroll,1973,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37504,NA,NA,NA,individuals,-98.777496,33.449722,Cottonwood Creek (Moran Fm.),NA,Locality IIb (Romer & Price),US,Texas,Archer,estimated from map,seconds,outcrop,"Cottonwood Creek is a tributary of the south fork of the Little Wichita River (about 10 miles south of Archer City). Locality is ""near the head of Cottonwood Creek, close to the southern border of Archer Co."" (Romer & Price, 1940) ",gp_mid,-30.65,-2.02,101,US,,Archer City,Wichita,,group of beds,,,,,,,NA,"""about 50 feet below the Sedwick limestone equivalent"" (Clark & Carroll, 1973)\r\nThe former Moran Formation comprises the lower part of the Archer City Formation (Hentz, 1988, The University of Texas at Austin, Bureau of Economic Geology, Report of Investigations, 170).",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,observed (not collected),MCZ,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Romeria,,NA,NA,vertebrate,J. Clark and R. L. Carroll. 1973. Romeriid Reptiles from the Lower Permian. Bulletin of the Museum of Comparative Zoology 144(5):353-407,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,09/01/2009 08:22,10/12/2012 14:38,28415,primus,Romeria,28415,n. sp.,298.9,295.5,Asselian,,1,US,Romeria primus
790491,occ,NA,,85567,,Trimerorhachis cf. insignis,species,90711,,Trimerorhachis insignis,NA,species,90711,Olson,1970,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-97.433334,36.349998,"Perry site 6, bed 16",NA,"""swamp assemblage""",US,Oklahoma,Noble,estimated from map,minutes,,"""about nine miles northwest of Perry, Logan County, Oklahoma, SE1/4 SE1/4 sec. 26 T. 23 N, R. 2 W""",gp_mid,-27.41,1.27,101,US,,Wellington,Sumner,,bed,,Perry site 6,16,bottom to top,,,NA,,"""Bed 16 consists of a grey to yellow and red shale, with occasional sandstone lenses. The shales have the highly leached appearance which is characteristic of swamp deposits from this time and contain selenite crystals.""","""shale""","gypsiferous,gray,red,yellow",,,Y,sandstone,lenticular,,,Y,mire/swamp,foreland basin,"""swamp deposits formed close to the margin of fresh water lakes""",macrofossils,,,,,,NA,,"body,mold/impression",,,snapshot,,,,,,,NA,,,taxonomic,field collection,FMNH,,,,E. C. Olson,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,334,0,J. Mueller,T. Liebrecht,,09/01/2009 09:01,09/01/2009 11:01,26635,insignis,Trimerorhachis,26635,cf.,290.1,268,Leonard,,NA,US,Trimerorhachis insignis
790492,occ,NA,,85567,,Eryops cf. megacephalus,species,70397,,Eryops megacephalus,NA,species,70397,Olson,1970,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-97.433334,36.349998,"Perry site 6, bed 16",NA,"""swamp assemblage""",US,Oklahoma,Noble,estimated from map,minutes,,"""about nine miles northwest of Perry, Logan County, Oklahoma, SE1/4 SE1/4 sec. 26 T. 23 N, R. 2 W""",gp_mid,-27.41,1.27,101,US,,Wellington,Sumner,,bed,,Perry site 6,16,bottom to top,,,NA,,"""Bed 16 consists of a grey to yellow and red shale, with occasional sandstone lenses. The shales have the highly leached appearance which is characteristic of swamp deposits from this time and contain selenite crystals.""","""shale""","gypsiferous,gray,red,yellow",,,Y,sandstone,lenticular,,,Y,mire/swamp,foreland basin,"""swamp deposits formed close to the margin of fresh water lakes""",macrofossils,,,,,,NA,,"body,mold/impression",,,snapshot,,,,,,,NA,,,taxonomic,field collection,FMNH,,,,E. C. Olson,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,334,0,J. Mueller,T. Liebrecht,,09/01/2009 09:01,09/01/2009 11:01,26635,megacephalus,Eryops,26635,cf.,290.1,268,Leonard,,NA,US,Eryops megacephalus
790493,occ,NA,,85567,,Diplocaulus cf. magnicornis,species,81712,,Diplocaulus magnicornis,NA,species,81712,Olson,1970,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-97.433334,36.349998,"Perry site 6, bed 16",NA,"""swamp assemblage""",US,Oklahoma,Noble,estimated from map,minutes,,"""about nine miles northwest of Perry, Logan County, Oklahoma, SE1/4 SE1/4 sec. 26 T. 23 N, R. 2 W""",gp_mid,-27.41,1.27,101,US,,Wellington,Sumner,,bed,,Perry site 6,16,bottom to top,,,NA,,"""Bed 16 consists of a grey to yellow and red shale, with occasional sandstone lenses. The shales have the highly leached appearance which is characteristic of swamp deposits from this time and contain selenite crystals.""","""shale""","gypsiferous,gray,red,yellow",,,Y,sandstone,lenticular,,,Y,mire/swamp,foreland basin,"""swamp deposits formed close to the margin of fresh water lakes""",macrofossils,,,,,,NA,,"body,mold/impression",,,snapshot,,,,,,,NA,,,taxonomic,field collection,FMNH,,,,E. C. Olson,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,334,0,J. Mueller,T. Liebrecht,,09/01/2009 09:01,09/01/2009 11:01,26635,magnicornis,Diplocaulus,26635,cf.,290.1,268,Leonard,,NA,US,Diplocaulus magnicornis
790494,occ,NA,,85567,,Ophiacodon uniformis,species,123419,,Ophiacodon uniformis,NA,species,138049,Olson,1970,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-97.433334,36.349998,"Perry site 6, bed 16",NA,"""swamp assemblage""",US,Oklahoma,Noble,estimated from map,minutes,,"""about nine miles northwest of Perry, Logan County, Oklahoma, SE1/4 SE1/4 sec. 26 T. 23 N, R. 2 W""",gp_mid,-27.41,1.27,101,US,,Wellington,Sumner,,bed,,Perry site 6,16,bottom to top,,,NA,,"""Bed 16 consists of a grey to yellow and red shale, with occasional sandstone lenses. The shales have the highly leached appearance which is characteristic of swamp deposits from this time and contain selenite crystals.""","""shale""","gypsiferous,gray,red,yellow",,,Y,sandstone,lenticular,,,Y,mire/swamp,foreland basin,"""swamp deposits formed close to the margin of fresh water lakes""",macrofossils,,,,,,NA,,"body,mold/impression",,,snapshot,,,,,,,NA,,,taxonomic,field collection,FMNH,,,,E. C. Olson,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,334,0,J. Mueller,T. Liebrecht,,09/01/2009 09:01,09/01/2009 11:01,26635,uniformis,Ophiacodon,26635,,290.1,268,Leonard,,NA,US,Ophiacodon uniformis
790495,occ,NA,,85567,,Dimetrodon cf. limbatus,species,344229,,Dimetrodon limbatus,NA,species,70401,Olson,1970,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-97.433334,36.349998,"Perry site 6, bed 16",NA,"""swamp assemblage""",US,Oklahoma,Noble,estimated from map,minutes,,"""about nine miles northwest of Perry, Logan County, Oklahoma, SE1/4 SE1/4 sec. 26 T. 23 N, R. 2 W""",gp_mid,-27.41,1.27,101,US,,Wellington,Sumner,,bed,,Perry site 6,16,bottom to top,,,NA,,"""Bed 16 consists of a grey to yellow and red shale, with occasional sandstone lenses. The shales have the highly leached appearance which is characteristic of swamp deposits from this time and contain selenite crystals.""","""shale""","gypsiferous,gray,red,yellow",,,Y,sandstone,lenticular,,,Y,mire/swamp,foreland basin,"""swamp deposits formed close to the margin of fresh water lakes""",macrofossils,,,,,,NA,,"body,mold/impression",,,snapshot,,,,,,,NA,,,taxonomic,field collection,FMNH,,,,E. C. Olson,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,E. C. Olson. 1970. New and little known genera and species of vertebrates from the Lower Permian of Oklahoma. Fieldiana: Geology 18(3):359-434,315,334,0,J. Mueller,T. Liebrecht,,09/01/2009 09:01,09/01/2009 11:01,26635,limbatus,Dimetrodon,26635,cf.,290.1,268,Leonard,,NA,US,Dimetrodon limbatus
790500,occ,NA,,11165,,Zatrachys sp.,genus,37056,,Zatrachys,NA,genus,37056,Sander,1987,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,,-98.699997,33.683334,Geraldine Bonebed,NA,,US,Texas,Archer,estimated from map,minutes,small collection,Locality is around 3km (~2miles) east of the intersection of Highway 25 and another unnamed Highway.,gp_mid,-30.37,-1.69,101,US,,Nocona,Wichita,,group of beds,,,Geraldine Bonebed,,,,NA,"The Geraldine Bonebed has been placed in the Nocona Formation, the old assignment to the Admiral Formation has been revised, as the Admiral is now restriced to a marine limestone and shale unit lying to the southwest of the same age as the Nocona.","gray, blocky to flaky and rarely laminated claystone grading downwards into yellow clays...Notable is the occurrence of small ""blebs"" of azurite and malachite staining on joint faces. Some layers of small clay pebbles are present",claystone,"grading,gray,yellow",,,Y,,,,,,"""floodplain""",,"Extensive discussion of paleoenvironmental interpretation (p. 223-226; 233-234). The setting of the Geraldine Bobebed and vicinity was a lushly vegetated floodplain with small lakes and a swamp forest of Psaronius, Cordaites and some seed ferns. Forest and brush vegetation (Walchia, seed ferns) lived on the ""upland"" divides between drainages.",macrofossils,,,,,,NA,,"adpression,charcoalification,coalified",,parautochthonous,snapshot,,,,,,,NA,,"The gray-yellow color of the clays, the preservation of the wood and plant debris as coaly compression, andthe occurrence of copper minerals indicate a reducing environment of deposition.\r\n\r\nthe preservation of the wood and plant debris as coaly compressions (p. 226)",taxonomic,"selective quarrying,field collection",,some macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,paleobotany,"P. M. Sander. 1987. Taphonomy of the Lower Permian Geraldine Bonebed in Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 61:221-236",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,09/01/2009 10:19,09/01/2009 12:22,4113,sp.,Zatrachys,4113,,298.9,290.1,Asselian,Sakmarian,NA,US,Zatrachys sp.
790501,occ,NA,,11165,,Trimerorhachis insignis,species,90711,,Trimerorhachis insignis,NA,species,90711,Sander,1987,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-98.699997,33.683334,Geraldine Bonebed,NA,,US,Texas,Archer,estimated from map,minutes,small collection,Locality is around 3km (~2miles) east of the intersection of Highway 25 and another unnamed Highway.,gp_mid,-30.37,-1.69,101,US,,Nocona,Wichita,,group of beds,,,Geraldine Bonebed,,,,NA,"The Geraldine Bonebed has been placed in the Nocona Formation, the old assignment to the Admiral Formation has been revised, as the Admiral is now restriced to a marine limestone and shale unit lying to the southwest of the same age as the Nocona.","gray, blocky to flaky and rarely laminated claystone grading downwards into yellow clays...Notable is the occurrence of small ""blebs"" of azurite and malachite staining on joint faces. Some layers of small clay pebbles are present",claystone,"grading,gray,yellow",,,Y,,,,,,"""floodplain""",,"Extensive discussion of paleoenvironmental interpretation (p. 223-226; 233-234). The setting of the Geraldine Bobebed and vicinity was a lushly vegetated floodplain with small lakes and a swamp forest of Psaronius, Cordaites and some seed ferns. Forest and brush vegetation (Walchia, seed ferns) lived on the ""upland"" divides between drainages.",macrofossils,,,,,,NA,,"adpression,charcoalification,coalified",,parautochthonous,snapshot,,,,,,,NA,,"The gray-yellow color of the clays, the preservation of the wood and plant debris as coaly compression, andthe occurrence of copper minerals indicate a reducing environment of deposition.\r\n\r\nthe preservation of the wood and plant debris as coaly compressions (p. 226)",taxonomic,"selective quarrying,field collection",,some macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,paleobotany,"P. M. Sander. 1987. Taphonomy of the Lower Permian Geraldine Bonebed in Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 61:221-236",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,09/01/2009 10:19,09/01/2009 12:22,4113,insignis,Trimerorhachis,4113,,298.9,290.1,Asselian,Sakmarian,NA,US,Trimerorhachis insignis
790502,occ,NA,,11165,,Ophiacodon uniformis,species,123419,,Ophiacodon uniformis,NA,species,138049,Sander,1987,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-98.699997,33.683334,Geraldine Bonebed,NA,,US,Texas,Archer,estimated from map,minutes,small collection,Locality is around 3km (~2miles) east of the intersection of Highway 25 and another unnamed Highway.,gp_mid,-30.37,-1.69,101,US,,Nocona,Wichita,,group of beds,,,Geraldine Bonebed,,,,NA,"The Geraldine Bonebed has been placed in the Nocona Formation, the old assignment to the Admiral Formation has been revised, as the Admiral is now restriced to a marine limestone and shale unit lying to the southwest of the same age as the Nocona.","gray, blocky to flaky and rarely laminated claystone grading downwards into yellow clays...Notable is the occurrence of small ""blebs"" of azurite and malachite staining on joint faces. Some layers of small clay pebbles are present",claystone,"grading,gray,yellow",,,Y,,,,,,"""floodplain""",,"Extensive discussion of paleoenvironmental interpretation (p. 223-226; 233-234). The setting of the Geraldine Bobebed and vicinity was a lushly vegetated floodplain with small lakes and a swamp forest of Psaronius, Cordaites and some seed ferns. Forest and brush vegetation (Walchia, seed ferns) lived on the ""upland"" divides between drainages.",macrofossils,,,,,,NA,,"adpression,charcoalification,coalified",,parautochthonous,snapshot,,,,,,,NA,,"The gray-yellow color of the clays, the preservation of the wood and plant debris as coaly compression, andthe occurrence of copper minerals indicate a reducing environment of deposition.\r\n\r\nthe preservation of the wood and plant debris as coaly compressions (p. 226)",taxonomic,"selective quarrying,field collection",,some macrofossils,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,paleobotany,"P. M. Sander. 1987. Taphonomy of the Lower Permian Geraldine Bonebed in Archer County, Texas. Palaeogeography, Palaeoclimatology, Palaeoecology 61:221-236",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,09/01/2009 10:19,09/01/2009 12:22,4113,uniformis,Ophiacodon,4113,,298.9,290.1,Asselian,Sakmarian,1,US,Ophiacodon uniformis
790503,occ,NA,,28142,,Theropleura n. sp. obtusidens,species,138129,recombined as,Secodontosaurus obtusidens,NA,species,138129,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38908,NA,NA,NA,individuals,-98.694725,33.816113,"Mount Barry, 12 (Admiral Formation)",NA,"Locality 12 (Romer 1928), Locality IVf (Romer & Price 1940), Mt. Barry, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""10 miles west of Wichita Falls."" Lat long is for Holliday, approx. 5 mi southeast of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,"""Many of Cope's types are from this region.""",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,09/01/2009 13:23,14/01/2009 02:22,7693,obtusidens,Secodontosaurus,5692,n. sp.,290.1,279.3,Artinskian,,1,US,Secodontosaurus obtusidens
790517,occ,NA,,80916,,Sphenacodon ferocior,species,122488,,Sphenacodon ferocior,NA,species,122488,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,individuals,-106.650276,36.162224,Rito Puerco,NA,,US,New Mexico,Rio Arriba,based on nearby landmark,seconds,small collection,"""unknown localty called 'Rito Puerco' by David Baldwin, somwhere in the Arroyo Agua area, New Mexico""; Lat long is for Arroyo del Agua",gp_mid,-34.08,4.53,101,US,FED,Abo/Cutler,,,group of beds,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,D. Baldwin,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,315,334,0,J. Mueller,T. Liebrecht,,09/01/2009 20:12,09/01/2009 22:12,27105,ferocior,Sphenacodon,27105,,296.4,268,Wolfcamp,,1,US,Sphenacodon ferocior
790518,occ,NA,,80714,,Clepsydrops sp.,genus,38887,,Clepsydrops,NA,genus,38887,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38887,NA,NA,NA,specimens,-87.775002,40.108334,Danville Locality (Vertebrates),NA,Oakwood Locality; Horseshoe Bend; Vermillion River; Illinois bonebed,US,Illinois,Vermilion,based on nearby landmark,seconds,outcrop,"""the well-known Danville or 'Oakwood' locality [...] Horseshoe Bend locality near the SE/C of Sec. 23-19N-13W"" (DeMar, 1970)\r\n""Vermilion River, near Danville"" (Reisz, 1986)\r\nLat Long is for Oakwood",gp_mid,-21.51,-3.52,101,US,,Bond,McLeansboro,,group of beds,,,,,,,NA,"""We believe the vertebrates have been collected from a zone 10 feet or so below the Shoal Creek Member of the Bond Formation"" (DeMar, 1970)\r\nNote: Shoal Creek Member is equivalent to Carthage Limestone Member, a name now used throughout the Illinois Basin for that lithological unit; see Jacobson (2002) A summary of references with changes in Pennsylvanian stratigraphic nomenclature at the ISGS since Bulletin 95. [Online] http://www.isgs.illinois.edu/maps-data-pub/coal-maps/pennstratigraphy.shtml ",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Clepsydrops,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,10/01/2009 10:29,29/06/2015 11:47,28640,sp.,Clepsydrops,5692,,305.9,303.4,Missourian,,18,US,Clepsydrops sp.
790519,occ,NA,,80714,,Captorhinus ? n. sp. illinoisensis,species,139018,subjective synonym of,Clepsydrops vinslovii,NA,species,123416,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38887,NA,NA,NA,elements,-87.775002,40.108334,Danville Locality (Vertebrates),NA,Oakwood Locality; Horseshoe Bend; Vermillion River; Illinois bonebed,US,Illinois,Vermilion,based on nearby landmark,seconds,outcrop,"""the well-known Danville or 'Oakwood' locality [...] Horseshoe Bend locality near the SE/C of Sec. 23-19N-13W"" (DeMar, 1970)\r\n""Vermilion River, near Danville"" (Reisz, 1986)\r\nLat Long is for Oakwood",gp_mid,-21.51,-3.52,101,US,,Bond,McLeansboro,,group of beds,,,,,,,NA,"""We believe the vertebrates have been collected from a zone 10 feet or so below the Shoal Creek Member of the Bond Formation"" (DeMar, 1970)\r\nNote: Shoal Creek Member is equivalent to Carthage Limestone Member, a name now used throughout the Illinois Basin for that lithological unit; see Jacobson (2002) A summary of references with changes in Pennsylvanian stratigraphic nomenclature at the ISGS since Bulletin 95. [Online] http://www.isgs.illinois.edu/maps-data-pub/coal-maps/pennstratigraphy.shtml ",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Captorhinus,?,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,10/01/2009 11:22,29/06/2015 11:47,28640,illinoisensis,Clepsydrops,5692,n. sp.,305.9,303.4,Missourian,,1,US,Clepsydrops illinoisensis
790521,occ,NA,,28256,,Varanosaurus acutirostris,species,137915,,Varanosaurus acutirostris,NA,species,137915,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38933,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Varanosaurus,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,10/01/2009 12:24,10/04/2009 14:19,17702,acutirostris,Varanosaurus,5692,,279.3,272.3,Kungurian,,1,US,Varanosaurus acutirostris
790523,occ,NA,,28067,,Sphenacodon ferocior,species,122488,,Sphenacodon ferocior,NA,species,122488,Romer,1937,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,individuals,-106.783333,35.716667,"UCMP 39179, Jemez Canyon (Abo Formation)",NA,"Harvard locality, Canyon de San Diego",US,New Mexico,Sandoval,stated in text,minutes,small collection,"4.5 mi south of Jemez Springs, Sandoval County, New Mexico. Western side of the Permian Basin. Lat long is for Jemez Springs.\n"" [...] on east side of Canyon de San Diego, east of State Highway 4, about 4 1/2 miles south of Jemez Springs, approximately lat 35 43' N.; long 106 47' W., Sandoval County, New Mexico"" (Berman, 1977)",gp_mid,-34.43,4.24,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)","""shale""",red,,,Y,sandstone,"coarse,micaceous,red",,,Y,fluvial indet.,non-subsiding area,"""relative abundance of micaceous and coarse arkosic detritus often associated with the bone-beds suggest that these Abo sediments were laid down nearer their source and under conditions of better regional drainage than contemporary ""deltaic"" Wichita rocks in Texas. The late Pennsylvanian and early Permian uplifts of the near-by ""Ancestral Rockies"" were evidently responsible for this early advent of red-bed deposition on the west side of the Permian Basin...""",macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,field collection,UCMP,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,vertebrate,A. S. Romer. 1937. New genera and species of pelycosaurian reptiles. Proceedings of the New England Zo̦logical Club 16:89-95,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,11/01/2009 09:17,18/08/2016 06:46,43845,ferocior,Sphenacodon,43845,,296.4,268,Wolfcamp,,1,US,Sphenacodon ferocior
790524,occ,NA,,28067,,Dimetrodon n. sp. occidentalis,species,123425,,Dimetrodon occidentalis,NA,species,123425,Berman,1977,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,individuals,-106.783333,35.716667,"UCMP 39179, Jemez Canyon (Abo Formation)",NA,"Harvard locality, Canyon de San Diego",US,New Mexico,Sandoval,stated in text,minutes,small collection,"4.5 mi south of Jemez Springs, Sandoval County, New Mexico. Western side of the Permian Basin. Lat long is for Jemez Springs.\n"" [...] on east side of Canyon de San Diego, east of State Highway 4, about 4 1/2 miles south of Jemez Springs, approximately lat 35 43' N.; long 106 47' W., Sandoval County, New Mexico"" (Berman, 1977)",gp_mid,-34.43,4.24,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)","""shale""",red,,,Y,sandstone,"coarse,micaceous,red",,,Y,fluvial indet.,non-subsiding area,"""relative abundance of micaceous and coarse arkosic detritus often associated with the bone-beds suggest that these Abo sediments were laid down nearer their source and under conditions of better regional drainage than contemporary ""deltaic"" Wichita rocks in Texas. The late Pennsylvanian and early Permian uplifts of the near-by ""Ancestral Rockies"" were evidently responsible for this early advent of red-bed deposition on the west side of the Permian Basin...""",macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,field collection,UCMP,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"D. S. Berman. 1977. A New Species of Dimetrodon (Reptilia, Pelycosauria) from a Non-Deltaic Facies in the Lower Permian of North-Central New Mexico. Journal of Paleontology 51(1):108-115",315,334,14,J. Mueller,T. Liebrecht,M. Carrano,11/01/2009 09:17,10/12/2012 14:40,43845,occidentalis,Dimetrodon,28943,n. sp.,296.4,268,Wolfcamp,,1,US,Dimetrodon occidentalis
790525,occ,NA,,85337,,n. gen. Chenoprosopus n. sp. milleri,species,139020,,Chenoprosopus milleri,NA,species,139020,Mehl,1913,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Cochleosauridae,36999,37000,NA,NA,NA,individuals,-106.673889,36.178612,Miller Bonebed,85339,Bone Quarry; Arroya de Agua; Poleo Creek,US,New Mexico,Rio Arriba,estimated from map,seconds,small collection,"1 mile ""above the confluence of the Poleo creek with the Puerco, and near the Mexican village of Arroya de Agua."" (Williston, 1916)\r\nApparently is what Williston (1916) calls the Poleo Creek a northwestern headstream of the Rio Puerco (see Williston & Case, 1913 p. 1 fig. 1, Carnegie Inst. Washington Publ. 181), however, in modern maps a southwestern headstream is designated as Poleo Creek. ",gp_mid,-34.08,4.56,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,"""same horizon"" as the Baldwin Bonebed (see coll. 80833)","""hard, dark brown clay""",claystone,brown,lithified,,Y,sandstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"""numerous isolated bones of Sphenacodon and Ophiacodon Marsh, together with a very perfect skeleton of the latter, were obtained"" (Williston, 1916)",taxonomic,"bulk,mechanical",,,,,"S. W. Williston, E. C. Case, P. Miller",1911,"for details see Williston & Case (1913 p. 38, Carnegie Inst. Washington Publ. 181)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Chenoprosopus,n. gen.,NA,NA,vertebrate,M. G. Mehl. 1913. A Description of Chenoprosopus milleri gen. et sp. nov. Carnegie Institution of Washington Publication 181:11-16,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,11/01/2009 09:31,11/01/2009 11:43,27105,milleri,Chenoprosopus,28944,n. sp.,296.4,268,Wolfcamp,,1,US,Chenoprosopus milleri
790527,occ,NA,,85433,,Ophiacodon mirus,species,123418,,Ophiacodon mirus,NA,species,123418,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-106.650558,36.162224,Rio Puerco,NA,"Arroyo del Agua, Arroyo de Agua, Arroya de Agua",US,New Mexico,Rio Arriba,based on nearby landmark,seconds,,"""on the Rio Puerco a few miles below Arroyo de Agua""; Lat long is for Arroyo del Agua",gp_mid,-34.08,4.53,101,US,FED,Abo/Cutler,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,P. Miller,1911,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,0,J. Mueller,T. Liebrecht,,11/01/2009 15:39,11/01/2009 17:39,28464,mirus,Ophiacodon,5692,,296.4,268,Wolfcamp,,NA,US,Ophiacodon mirus
790528,occ,NA,,80690,,Ophiacodon uniformis,species,123419,,Ophiacodon uniformis,NA,species,138049,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-99.139442,33.669724,Maybelle,NA,"Locality VIc (Romer & Price 1940), Mabelle",US,Texas,Baylor,based on nearby landmark,seconds,,"""north of Maybelle, Baylor County, Texas""; Lat Long is for Maybelle",gp_mid,-29.99,-0.3,101,US,,Waggoner Ranch,Wichita,,,,,,,,,NA,"Waggoner Ranch Fm. is formerly known as Clyde Fm. (see Hentz, 1988, The University of Texas at Austin Bureau of Economic Geology, Report of Investigations, 170, pp. 1-55)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,0,J. Mueller,T. Liebrecht,,11/01/2009 15:51,11/01/2009 17:51,27105,uniformis,Ophiacodon,5692,,290.1,268,Leonard,,1,US,Ophiacodon uniformis
790529,occ,NA,,13080,,Ophiacodon uniformis,species,123419,,Ophiacodon uniformis,NA,species,138049,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-98.856941,33.622501,Briar Creek,NA,"(Admiral Formation) Locality 13 (Romer 1928), Locality IVd (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds; Brier Creek",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""the collecting ground being mainly on the east side a few miles from the mouth, near and in the bone bed discovered by Case."" Lat long is for Dundee, approx. 9 mi south of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""; DMS coordinates are for the mouth of Briar Creek into Lake Kickapoo",gp_mid,-30.21,-1.18,101,US,,Admiral,Wichita,,bed,,,,,,,NA,"""about 190 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Admiral Formation and middle Wichita Group are both Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones."" ",claystone,red,,,,sandstone,red,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,11/01/2009 15:55,16/08/2016 05:30,7693,uniformis,Ophiacodon,5692,,290.1,279.3,Artinskian,,14,US,Ophiacodon uniformis
790531,occ,NA,,28145,,Ophiacodon uniformis,species,123419,,Ophiacodon uniformis,NA,species,138049,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,elements,-99.022781,33.687222,"South of Fulda, 19 (Belle Plains)",NA,"Locality 19 (Romer 1928), Locality Vb (Romer & Price 1940), S. of Fulda, Hackberry Creek, North Side Little Wichita, South Side Little Wichita, North Side of Godwin Creek, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""Numerous exposures occur in the valley of the Little Wichita south and southeast of Fulda."" Specimens are labeled with various locality names, see aka above. See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 2 mi north of locality.",gp_mid,-30.3,-1.05,101,US,,Petrolia,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,Cope,1908,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,11/01/2009 16:13,09/08/2011 14:25,28729,uniformis,Ophiacodon,5692,,290.1,279.3,Artinskian,,1,US,Ophiacodon uniformis
790532,occ,NA,,84716,,Ophiacodon uniformis,species,123419,,Ophiacodon uniformis,NA,species,138049,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,elements,-98.900002,33.641666,Rattlesnake Canyon (Admiral Fm.),NA,Locality IVc (Romer & Price 1940); Cummins' Headquarters; Lyles Place,US,Texas,Archer,estimated from map,seconds,outcrop,"Rattlesnake Canyon, Archer County, Texas. Lat long is estimated from map on p. 397 in Clark & Carroll (1973).",gp_mid,-30.23,-1.14,101,US,,Petrolia,Wichita,,,,,,,,,NA,"""Uppermost Admiral Formation"" (Clark & Carroll, 1973); the uppermost part of the traditional Admiral Fm. today is considered the lowermost part of the Petrolia Fm. (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,11/01/2009 16:19,25/07/2016 04:42,28415,uniformis,Ophiacodon,5692,,290.1,279.3,Artinskian,,1,US,Ophiacodon uniformis
790533,occ,NA,,79162,,Ophiacodon uniformis,species,123419,,Ophiacodon uniformis,NA,species,138049,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-98.650002,33.583332,Archer City Bonebed 1 (Putnam Fm.),NA,"Locality IIIf (Romer & Price, 1940)",US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,11/01/2009 16:23,10/12/2012 14:44,43845,uniformis,Ophiacodon,5692,,296.4,268,Wolfcamp,,1,US,Ophiacodon uniformis
790535,occ,NA,,28142,,Theropleura n. sp. triangulata,species,138051,subjective synonym of,Ophiacodon retroversus,NA,species,138048,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-98.694725,33.816113,"Mount Barry, 12 (Admiral Formation)",NA,"Locality 12 (Romer 1928), Locality IVf (Romer & Price 1940), Mt. Barry, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""10 miles west of Wichita Falls."" Lat long is for Holliday, approx. 5 mi southeast of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,"""Many of Cope's types are from this region.""",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Theropleura,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,11/01/2009 19:39,11/01/2009 21:42,7693,triangulata,Ophiacodon,5692,n. sp.,290.1,279.3,Artinskian,,1,US,Ophiacodon triangulata
790998,occ,NA,,28146,,n. gen. Ctenospondylus n. sp. casei,species,122592,,Ctenospondylus casei,NA,species,122592,Romer,1936,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38903,NA,NA,NA,individuals,-98.901947,33.740276,"Slippery Creek, 20 (Belle Plains Formation)",NA,"Locality 20 (Romer 1928), Locality Vc (Romer & Price 1940), Lyle locality, Pearce locality, Young locality, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Slippery Creek is a tributary of the Little Wichita on the north side. Along it's course, nearly due south of Dundee, is a series of breaks. Lyle's, Pearce's, and Young's localities of Case were in this neighborhood."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee, approx. 4 mi due north of locality.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ctenospondylus,n. gen.,NA,NA,vertebrate,A. S. Romer. 1936. Studies on American Permo-Carboniferous reptiles. Problems of Paleontology 1:85-93,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,12/01/2009 14:57,10/12/2012 13:54,7693,casei,Ctenospondylus,43841,n. sp.,290.1,279.3,Artinskian,,1,US,Ctenospondylus casei
790999,occ,NA,,28146,,Varanosaurus n. sp. wichitaensis,species,139019,,Varanosaurus wichitaensis,NA,species,139019,Romer,1937,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38933,NA,NA,NA,specimens,-98.901947,33.740276,"Slippery Creek, 20 (Belle Plains Formation)",NA,"Locality 20 (Romer 1928), Locality Vc (Romer & Price 1940), Lyle locality, Pearce locality, Young locality, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Slippery Creek is a tributary of the Little Wichita on the north side. Along it's course, nearly due south of Dundee, is a series of breaks. Lyle's, Pearce's, and Young's localities of Case were in this neighborhood."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee, approx. 4 mi due north of locality.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Varanosaurus,,NA,NA,vertebrate,A. S. Romer. 1937. New genera and species of pelycosaurian reptiles. Proceedings of the New England Zo̦logical Club 16:89-95,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,12/01/2009 14:57,10/12/2012 14:39,7693,wichitaensis,Varanosaurus,43845,n. sp.,290.1,279.3,Artinskian,,3,US,Varanosaurus wichitaensis
791000,occ,NA,,28146,,Ophiacodon uniformis,species,123419,,Ophiacodon uniformis,NA,species,138049,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-98.901947,33.740276,"Slippery Creek, 20 (Belle Plains Formation)",NA,"Locality 20 (Romer 1928), Locality Vc (Romer & Price 1940), Lyle locality, Pearce locality, Young locality, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Slippery Creek is a tributary of the Little Wichita on the north side. Along it's course, nearly due south of Dundee, is a series of breaks. Lyle's, Pearce's, and Young's localities of Case were in this neighborhood."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee, approx. 4 mi due north of locality.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,12/01/2009 14:57,10/12/2012 13:54,7693,uniformis,Ophiacodon,5692,,290.1,279.3,Artinskian,,1,US,Ophiacodon uniformis
791003,occ,NA,,80111,,n. gen. Archaeothyris n. sp. florensis,species,122328,,Archaeothyris florensis,NA,species,122328,Reisz,1972,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38885,NA,NA,NA,specimens,-60.266666,46.290001,Dominion Coal Co. strip mine No. 7,NA,"Sydney coal field; Florence, Cape Breton",CA,Nova Scotia,Cape Breton Island,estimated from map,seconds,small collection,"Dominion Coal Co. strip mine No. 7, about 2 miles north of the town of Florence",gp_mid,-3.96,-8.17,108,CA,,,Morien,,group of beds,,,,,,,NA,"""... above the Lloyd Cove (Lower Bonar) coal of the Morien group."" ",,coal,,,,Y,"""shale""",,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,permineralized,,autochthonous,snapshot,,,,,,,NA,,the vertebrate remains come from the interior of fossilized tree stumps and are completely disarticulated,taxonomic,"selective quarrying,survey of museum collection",MCZ,,,,A.S. Romer,1956,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archaeothyris,n. gen.,NA,NA,,R. R. Reisz. 1972. Pelycosaurian Reptiles from the Middle Pennsylvanian of North America. Bulletin of the Museum of Comparative Zoology 144(2):27-60,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,12/01/2009 18:35,11/02/2016 10:43,26895,florensis,Archaeothyris,28957,n. sp.,314.6,306.95,Westphalian C,Westphalian D,10,CA,Archaeothyris florensis
791553,occ,NA,,80111,,n. gen. Echinerpeton n. sp. intermedium,species,123515,,Echinerpeton intermedium,NA,species,123515,Reisz,1972,Chordata,33815,Osteichthyes,34881,Pelycosauria,38883,,NA,38923,NA,NA,NA,specimens,-60.266666,46.290001,Dominion Coal Co. strip mine No. 7,NA,"Sydney coal field; Florence, Cape Breton",CA,Nova Scotia,Cape Breton Island,estimated from map,seconds,small collection,"Dominion Coal Co. strip mine No. 7, about 2 miles north of the town of Florence",gp_mid,-3.96,-8.17,108,CA,,,Morien,,group of beds,,,,,,,NA,"""... above the Lloyd Cove (Lower Bonar) coal of the Morien group."" ",,coal,,,,Y,"""shale""",,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,permineralized,,autochthonous,snapshot,,,,,,,NA,,the vertebrate remains come from the interior of fossilized tree stumps and are completely disarticulated,taxonomic,"selective quarrying,survey of museum collection",MCZ,,,,A.S. Romer,1956,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Echinerpeton,n. gen.,NA,NA,,R. R. Reisz. 1972. Pelycosaurian Reptiles from the Middle Pennsylvanian of North America. Bulletin of the Museum of Comparative Zoology 144(2):27-60,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,13/01/2009 16:22,11/02/2016 10:43,26895,intermedium,Echinerpeton,28957,n. sp.,314.6,306.95,Westphalian C,Westphalian D,6,CA,Echinerpeton intermedium
791557,occ,NA,,84835,,Archaeothyris sp.,genus,38885,,Archaeothyris,NA,genus,38885,Reisz,1975,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38885,NA,NA,NA,individuals,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archaeothyris,,NA,NA,vertebrate,"R. R. Reisz. 1975. Pennsylvanian Pelycosaurs from Linton, Ohio and N_any, Czechoslovakia. Journal of Paleontology 49(3):522-527",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,13/01/2009 18:58,03/11/2009 20:09,28608,sp.,Archaeothyris,5939,,311.45,306.95,Westphalian D,,1,CZ,Archaeothyris sp.
791558,occ,NA,,85292,,Archaeothyris sp.,genus,38885,,Archaeothyris,NA,genus,38885,Reisz,1975,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38885,NA,NA,NA,individuals,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archaeothyris,,NA,NA,vertebrate,"R. R. Reisz. 1975. Pennsylvanian Pelycosaurs from Linton, Ohio and N_any, Czechoslovakia. Journal of Paleontology 49(3):522-527",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,13/01/2009 20:06,03/11/2009 10:09,28831,sp.,Archaeothyris,5939,,311.45,306.95,Westphalian D,,2,US,Archaeothyris sp.
791559,occ,NA,,85292,,Pelycosauria indet.,order,138244,,Pelycosauria,NA,order,38883,Reisz,1975,Chordata,33815,Osteichthyes,34881,Pelycosauria,38883,,NA,NA,NA,NA,NA,individuals,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Pelycosauria,,NA,NA,vertebrate,"R. R. Reisz. 1975. Pennsylvanian Pelycosaurs from Linton, Ohio and N_any, Czechoslovakia. Journal of Paleontology 49(3):522-527",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,13/01/2009 20:06,03/11/2009 10:09,28831,indet.,,5939,,311.45,306.95,Westphalian D,,1,US, indet.
791560,occ,NA,,85292,,n. gen. Sauropleura n. sp. digitata,species,139230,recombined as,Eusauropleura digitata,NA,species,139230,Carroll,1970,Chordata,33815,Osteichthyes,34881,,NA,Gephyrostegidae,37202,37204,NA,NA,NA,individuals,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sauropleura,n. gen.,NA,NA,vertebrate,"R. L. Carroll. 1970. The Ancestry of Reptiles. Philosophical Transactions of the Royal Society of London, Series B 257:267-308",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,13/01/2009 20:06,03/11/2009 10:09,28831,digitata,Eusauropleura,28959,n. sp.,311.45,306.95,Westphalian D,,2,US,Eusauropleura digitata
791561,occ,NA,,85292,,Eusauropleura ? digitata,species,139231,,Eusauropleura digitata,NA,species,139230,Carroll,1970,Chordata,33815,Osteichthyes,34881,,NA,Gephyrostegidae,37202,37204,NA,NA,NA,individuals,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Eusauropleura,?,NA,NA,vertebrate,"R. L. Carroll. 1970. The Ancestry of Reptiles. Philosophical Transactions of the Royal Society of London, Series B 257:267-308",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,13/01/2009 21:57,03/11/2009 10:09,28831,digitata,Eusauropleura,28959,,311.45,306.95,Westphalian D,,1,US,Eusauropleura digitata
791563,occ,NA,,28146,,Ophiacodon retroversus,species,123420,,Ophiacodon retroversus,NA,species,138048,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-98.901947,33.740276,"Slippery Creek, 20 (Belle Plains Formation)",NA,"Locality 20 (Romer 1928), Locality Vc (Romer & Price 1940), Lyle locality, Pearce locality, Young locality, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Slippery Creek is a tributary of the Little Wichita on the north side. Along it's course, nearly due south of Dundee, is a series of breaks. Lyle's, Pearce's, and Young's localities of Case were in this neighborhood."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee, approx. 4 mi due north of locality.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,13/01/2009 23:25,10/12/2012 13:54,7693,retroversus,Ophiacodon,5692,,290.1,279.3,Artinskian,,2,US,Ophiacodon retroversus
791564,occ,NA,,84716,,Ophiacodon retroversus,species,123420,,Ophiacodon retroversus,NA,species,138048,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-98.900002,33.641666,Rattlesnake Canyon (Admiral Fm.),NA,Locality IVc (Romer & Price 1940); Cummins' Headquarters; Lyles Place,US,Texas,Archer,estimated from map,seconds,outcrop,"Rattlesnake Canyon, Archer County, Texas. Lat long is estimated from map on p. 397 in Clark & Carroll (1973).",gp_mid,-30.23,-1.14,101,US,,Petrolia,Wichita,,,,,,,,,NA,"""Uppermost Admiral Formation"" (Clark & Carroll, 1973); the uppermost part of the traditional Admiral Fm. today is considered the lowermost part of the Petrolia Fm. (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,13/01/2009 23:28,25/07/2016 04:42,28415,retroversus,Ophiacodon,5692,,290.1,279.3,Artinskian,,14,US,Ophiacodon retroversus
791565,occ,NA,,79162,,Ophiacodon retroversus,species,123420,,Ophiacodon retroversus,NA,species,138048,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-98.650002,33.583332,Archer City Bonebed 1 (Putnam Fm.),NA,"Locality IIIf (Romer & Price, 1940)",US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,14/01/2009 00:02,10/12/2012 14:44,43845,retroversus,Ophiacodon,5692,,296.4,268,Wolfcamp,,1,US,Ophiacodon retroversus
791566,occ,NA,,28123,,Ophiacodon retroversus,species,123420,,Ophiacodon retroversus,NA,species,138048,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-98.625275,33.595554,"Three Forks of the Little Wichita, 5 (Putnam Formation)",NA,"Locality 5 (Romer 1928), Locality IVb (Romer & Price, 1940) faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Three Forks of the Little Wichita, northwest of Archer City."" Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group - boundary is at the top of the Coleman Junction Limestone.""close to the line of the Coleman Junction."" Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984).\nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,14/01/2009 00:05,14/01/2009 02:38,7693,retroversus,Ophiacodon,5692,,295.5,290.1,Sakmarian,,2,US,Ophiacodon retroversus
791567,occ,NA,,28150,,Ophiacodon retroversus,species,123420,,Ophiacodon retroversus,NA,species,138048,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-98.92083,33.601391,"Godwin Creek, 14 (Admiral Formation)",NA,"Locality 14 (Romer 1928), Locality IVe (Romer & Price 1940), Southeast side of Godwin creek, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""specimens appear to come from the southeast side of this creek."" See detailed locality map in Romer 1928. ""Zone 1. Lat long is for Godwin Creek, USGS Dundee SW, Archer County.",gp_mid,-30.27,-1.17,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"""The horizon is about 250-300 feet above the base of the formation."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,, terrestrial and near-shore deposition\n,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,"AMNH,FMNH,MCZ",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,14/01/2009 00:10,18/07/2016 10:55,7693,retroversus,Ophiacodon,5692,,290.1,279.3,Artinskian,,6,US,Ophiacodon retroversus
791568,occ,NA,,28145,,Ophiacodon retroversus,species,123420,,Ophiacodon retroversus,NA,species,138048,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-99.022781,33.687222,"South of Fulda, 19 (Belle Plains)",NA,"Locality 19 (Romer 1928), Locality Vb (Romer & Price 1940), S. of Fulda, Hackberry Creek, North Side Little Wichita, South Side Little Wichita, North Side of Godwin Creek, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""Numerous exposures occur in the valley of the Little Wichita south and southeast of Fulda."" Specimens are labeled with various locality names, see aka above. See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 2 mi north of locality.",gp_mid,-30.3,-1.05,101,US,,Petrolia,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,Cope,1908,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,14/01/2009 00:19,09/08/2011 14:25,28729,retroversus,Ophiacodon,5692,,290.1,279.3,Artinskian,,4,US,Ophiacodon retroversus
791569,occ,NA,,28142,,Ophiacodon retroversus,species,123420,,Ophiacodon retroversus,NA,species,138048,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-98.694725,33.816113,"Mount Barry, 12 (Admiral Formation)",NA,"Locality 12 (Romer 1928), Locality IVf (Romer & Price 1940), Mt. Barry, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Wichita,based on nearby landmark,seconds,local area,"""10 miles west of Wichita Falls."" Lat long is for Holliday, approx. 5 mi southeast of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""",gp_mid,-30,-1.09,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,"""Many of Cope's types are from this region.""",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,14/01/2009 00:22,14/01/2009 02:31,7693,retroversus,Ophiacodon,5692,,290.1,279.3,Artinskian,,2,US,Ophiacodon retroversus
791570,occ,NA,,11165,,Ophiacodon retroversus,species,123420,,Ophiacodon retroversus,NA,species,138048,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-98.699997,33.683334,Geraldine Bonebed,NA,,US,Texas,Archer,estimated from map,minutes,small collection,Locality is around 3km (~2miles) east of the intersection of Highway 25 and another unnamed Highway.,gp_mid,-30.37,-1.69,101,US,,Nocona,Wichita,,group of beds,,,Geraldine Bonebed,,,,NA,"The Geraldine Bonebed has been placed in the Nocona Formation, the old assignment to the Admiral Formation has been revised, as the Admiral is now restriced to a marine limestone and shale unit lying to the southwest of the same age as the Nocona.","gray, blocky to flaky and rarely laminated claystone grading downwards into yellow clays...Notable is the occurrence of small ""blebs"" of azurite and malachite staining on joint faces. Some layers of small clay pebbles are present",claystone,"grading,gray,yellow",,,Y,,,,,,"""floodplain""",,"Extensive discussion of paleoenvironmental interpretation (p. 223-226; 233-234). The setting of the Geraldine Bobebed and vicinity was a lushly vegetated floodplain with small lakes and a swamp forest of Psaronius, Cordaites and some seed ferns. Forest and brush vegetation (Walchia, seed ferns) lived on the ""upland"" divides between drainages.",macrofossils,,,,,,NA,,"adpression,charcoalification,coalified",,parautochthonous,snapshot,,,,,,,NA,,"The gray-yellow color of the clays, the preservation of the wood and plant debris as coaly compression, andthe occurrence of copper minerals indicate a reducing environment of deposition.\r\n\r\nthe preservation of the wood and plant debris as coaly compressions (p. 226)",taxonomic,"selective quarrying,field collection",,some macrofossils,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,paleobotany,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,0,J. Mueller,T. Liebrecht,,14/01/2009 00:43,14/01/2009 02:43,4113,retroversus,Ophiacodon,5692,,298.9,290.1,Asselian,Sakmarian,1,US,Ophiacodon retroversus
791571,occ,NA,,79163,,Ophiacodon retroversus,species,123420,,Ophiacodon retroversus,NA,species,138048,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-98.777496,33.449722,Cottonwood Creek (Moran Fm.),NA,Locality IIb (Romer & Price),US,Texas,Archer,estimated from map,seconds,outcrop,"Cottonwood Creek is a tributary of the south fork of the Little Wichita River (about 10 miles south of Archer City). Locality is ""near the head of Cottonwood Creek, close to the southern border of Archer Co."" (Romer & Price, 1940) ",gp_mid,-30.65,-2.02,101,US,,Archer City,Wichita,,group of beds,,,,,,,NA,"""about 50 feet below the Sedwick limestone equivalent"" (Clark & Carroll, 1973)\r\nThe former Moran Formation comprises the lower part of the Archer City Formation (Hentz, 1988, The University of Texas at Austin, Bureau of Economic Geology, Report of Investigations, 170).",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,observed (not collected),MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,14/01/2009 00:57,10/12/2012 14:38,28415,retroversus,Ophiacodon,5692,,298.9,295.5,Asselian,,1,US,Ophiacodon retroversus
791574,occ,NA,,28238,,Ophiacodon retroversus,species,123420,,Ophiacodon retroversus,NA,species,138048,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-98.901947,33.740276,"Tit Mountain, 21 (Belle Plains Formation)",NA,"Locality 21 (Romer 1928), Locality Vd (Romer & Price 1940), Corn Mountain, Corn Hill, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Tit Mountain or Corn Hill, an elevation just northeast of Dundee"" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 500 feet above the Coleman Junction."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Not the same as ""South side of Tit Mountain butte, TMM 40031"" locality (Langston 1986); that collection was obviously made much later than the Tit Mountain collection of Romer (1928), which has less detailed locality data.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,14/01/2009 01:28,10/12/2012 14:28,26948,retroversus,Ophiacodon,5692,,290.1,279.3,Artinskian,,1,US,Ophiacodon retroversus
791586,occ,NA,,28148,,Ophiacodon major,species,122336,,Ophiacodon major,NA,species,122336,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-99.022781,33.687222,"Big Wichita, Cummins, 23 (Belle Plains Formation)",NA,"Locality 23 (Romer 1928), Locality Ve (Romer & Price 1940), faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 6 mi southwest of locality.",gp_mid,-30.3,-1.05,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""Just below the Beaverburk limestone... probable elevation above the Coleman Junction of about 525 feet."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,14,J. Mueller,T. Liebrecht,M. Carrano,14/01/2009 02:25,24/11/2014 13:58,28847,major,Ophiacodon,5692,,290.1,279.3,Artinskian,,1,US,Ophiacodon major
791587,occ,NA,,28120,,Ophiacodon major,species,122336,,Ophiacodon major,NA,species,122336,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-98.625275,33.595554,"Elm Creek, 2 (Putnam Formation)",NA,"Locality 2 (Romer 1928), Locality IIIa (Romer & Price (1940), faunal Zone 0, Cisco Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Elm Creek, stated by Cummins to be 12 miles southwest of Archer City; its exact position is uncertain.."" Lat long is for Archer City, but see detailed locality map in Romer 1928.",gp_mid,-30.26,-1.62,101,US,,Putnam,Cisco,,group of beds,,,,,,,NA,"Details for Faunal Zone 0 of Romer 1928: Plummer and Moore 1921 assign the Putnam Formation to the Cisco Group- boundary is at the top of the Coleman Junction Limestone. ""probably about 100 feet below the Coleman Junction."" Though stated to be Pennsylvanian by Romer, the Putnam F. is now widely regarded as Lower Permian (Shelley 1984). \nthe ""Putnam Formation"" falls between the Moran and Admiral formations (cf., Ross and Ross 1962, Fig. 3), and therefore equates to the Sedwick Formation, Santa Ana Branch Shale, and Coleman Junction Formation, all of which are Sakmarian (Wardlaw 2005, Permophiles)","red-beds, ""strata consist mainly of red or variegated clays and shales with sandstones and conglomerates.""\r\n\r\n",claystone,red,,,,"""shale""",red,,"sandy,conglomeratic",,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,0,J. Mueller,T. Liebrecht,,14/01/2009 02:32,14/01/2009 04:32,7693,major,Ophiacodon,5692,,295.5,290.1,Sakmarian,,1,US,Ophiacodon major
791588,occ,NA,,85733,,Ophiacodon major,species,122336,,Ophiacodon major,NA,species,122336,Romer and Price,1940,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-98.59861,34.295834,Deep Red Run,NA,"Deep Red Creek; Cope's ""Indian Territory""",US,Oklahoma,Cotton,estimated from map,seconds,outcrop,"""There was at one time a small fort called Fort Auger on the north side of Red River about opposite where the town of Iowa Park is now located. There was a road leading from Fort Auger to Fort Sill. Near the crossing of Deep Red Creek by this old road is the locality at which I collected the vertebrates in Cope's collection labelled 'Indian Territory.' "" (Cummins, 1908).\r\n""This site is in Cotton County [...]. The site is several miles northwest of Randlett, but we were not able to locate it more precisely."" (Olson, 1967, Oklahoma Geol. Surv. Circ. 74).\r\nLat long is for Deep Red Creek immediately east of Tillman-Cotton County line (sec. 18, T.3S. R.13W., Whites Lake 7.5' quadrangle).",gp_mid,-29.65,-0.67,101,US,,Garber,Sumner,,member,,,,,,,NA,"""The trend of the strike of the texas beds suggests that the locality lies in the Clyde formation. [...] The presence of a large Dimetrodon [...] suggests a higher position; of Cricotus a lower one; of Ophiacodon major the Clyde itself. The somewhat conflicting evidence is thus on the whole agreeable to an approximate Clyde determination."" (Romer & Price, 1940).\r\nIn the chart (fig. 2) of Olson (1967, Oklahoma Geol. Surv. Circ. 74) the relevant stratigraphic unit is given as ""Hennessey Shale"" but is correlated with the Garber Sandstone of other parts of Oklahoma.\r\nIn the stratigraphic chart (table 1) of Heaton (1979, Oklahoma Geol. Surv. Bull. 127) the Deep Red Run locality is assigned to the middle part of the Garber Sandstone, the latter being correlated with the Lueders Fm. of Texas.",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,W. F. Cummins,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,A. S. Romer and L. I. Price. 1940. Review of the Pelycosauria. Geological Society of America Special Paper 28:1-538,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,14/01/2009 03:42,11/06/2009 11:37,30068,major,Ophiacodon,5692,,290.1,272.3,Artinskian,Kungurian,1,US,Ophiacodon major
791884,occ,NA,,28069,,n. gen. Protoclepsydrops n. sp. haplous,species,123523,,Protoclepsydrops haplous,NA,species,123523,Carroll,1964,Chordata,33815,Osteichthyes,34881,Pelycosauria,38883,,NA,38889,NA,NA,NA,individuals,-64.451385,45.698612,"Coal Mine Point; Divison 4, Section XV, coal-group 15",NA,South Joggins; Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Cliffs called the South Joggins (coast), about half a mile eastward of the Coal Pier.",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XV",coal-group 15,,,,NA,"From Steen (1934): ""top of the Joggins formation...Division 4, Section XV., Coal-group 15 of the Joggins section given in Dawson's 'Acadian Geology,' 1868, pp. 156-178."" From Lyell (1853): The fossils are from Bed 5 of a 25 ft section, composed of 7 beds. Bed 5 is approximately 600 ft below the main coal, ""King's Vein"".\r\nOriginal entry for Local Section name was ""South Joggins""; for Bed/horizon ""bed 5"". In Steen (1934) a ""bed 5"" is not mentioned in any way. Also, in papers published before and after Lyell's ""On the Remains of a Reptile..."" (1953) a different numbering is applied to the Joggins Section. Thus, it is more appropriate to follow the stratigraphic terminology used in Dawson (1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173), Steen (1934, see description above) and Carroll (1964). Coal-group 15 consists of 3 beds with a total thickness of 10 ft 6 in. (Dawson, 1878) (TL) \r\nOriginal entry for chronostratigraphy was simply ""Westphalian"". Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","From Lyell (1853): 5. Grey sandstone, with three erect trees, one having Stigmarian roots; erect Calamites and stems of unknown plants. (One of the erect trees in this bed contained the bones, teeth, &c. and land-shell above-mentioned.) ...9 ft;\r\n",sandstone,gray,,,Y,coal,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",good,,snapshot,,,,,,occasional,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" ",taxonomic,"bulk,selective quarrying,field collection,survey of museum collection",BMNH,,,,"J. W. Dawson, C. Lyell, among others",,"RM = Redpath Museum of McGill Unversity, Montreal","Listed by Steen (1934) as Indeterminate species: Hylerpeton dawsoni Owen; Hylerpeton longidentatum Dawson; Hylerpeton intermedium Dawson; Hylonomus multidens Dawson; Hylonomus wymani Dawson; Smilerpeton aciedentatus Dawson; Amblyodon problematicum Dawson; Sparodus sp. Dawson; Baphetes minor Dawson.\r\n\r\nAll catalogue numbers are from Steen (1934) and/or from Carroll (1967).\r\n\r\nThe taxon ""Batrachoididae indet."", entered under the reference Lyell & Dawson (1853), has been removed from the taxonomic list for it is a family of teleost fish. It probably referred to the ""batrachian"" affinities of the tetrapod bones noticed by Wyman (1853) but all these bones finally were assigned to Dendrerpeton acadianum n. gen. et sp. (see pls. II and III in Lyell & Dawson/Wyman/Owen, 1853). Thus the originally enterd taxon ""Dendrerpeton acadianum"", reference: Lyell & Dawson, was replaced by ""Batrachia indet."", reference: Wyman (1853), and re-identification by Owen (1853) was added (TL).\r\nRe-identification of ""Dendrerpeton oweni n. sp."" as ""Dendrerpeton acadianum"" by by Steen was removed after opinons on synonymy of the the former with the latter species were entered into the database (TL).",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Protoclepsydrops,n. gen.,NA,NA,vertebrate,R. L. Carroll. 1964. The earliest reptiles. Journal of the Linnean Society (Zoology) 45(304):61-83,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,15/01/2009 09:05,13/03/2010 21:31,7856,haplous,Protoclepsydrops,28956,n. sp.,318.1,314.6,Westphalian A,,1,CA,Protoclepsydrops haplous
792606,occ,NA,R,85950,,Captorhinidae indet.,family,37495,,Captorhinidae,NA,family,37495,Fox and Bowman,1966,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,NA,NA,NA,NA,individuals,-98.915001,34.013889,Electra (Clyde Fm.),NA,HT&B RR Survey A-137,US,Texas,Wichita,estimated from map,seconds,hand sample,"""1 mile south of Electra, HT&B RR Survey A-137, about middle of north section line, Wichita County, Texas."" (Heaton, 1979)",gp_mid,-30.02,-0.77,101,US,,Waggoner Ranch,Wichita,,bed,,,,,,,NA,"The Waggoner Ranch Fm. is formerly known as the Clyde Fm. (see Hentz, 1988, The University of Texas at Austin Bureau of Economic Geology, Report of Investigations, 170, pp. 1-55)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,poor,,,,,,,,,NA,,,taxonomic,,MCZ,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinidae,,NA,NA,vertebrate,"R. C. Fox and M. C. Bowman. 1966. Osteology and Relationships of Captorhinus aguti (Cope) (Reptilia: Captorhinomorpha). The University of Kansas Paleontological Contributions, Series Vertebrata 11:1-79",315,334,0,J. Mueller,T. Liebrecht,,21/01/2009 09:53,21/01/2009 11:53,28784,indet.,,28784,,290.1,272.3,Artinskian,Kungurian,1,US, indet.
792606,occ,21239,,85950,,Eocaptorhinus laticeps,species,134878,recombined as,Captorhinus laticeps,NA,species,120324,Heaton,1979,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-98.915001,34.013889,Electra (Clyde Fm.),NA,HT&B RR Survey A-137,US,Texas,Wichita,estimated from map,seconds,hand sample,"""1 mile south of Electra, HT&B RR Survey A-137, about middle of north section line, Wichita County, Texas."" (Heaton, 1979)",gp_mid,-30.02,-0.77,101,US,,Waggoner Ranch,Wichita,,bed,,,,,,,NA,"The Waggoner Ranch Fm. is formerly known as the Clyde Fm. (see Hentz, 1988, The University of Texas at Austin Bureau of Economic Geology, Report of Investigations, 170, pp. 1-55)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,poor,,,,,,,,,NA,,,taxonomic,,MCZ,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Eocaptorhinus,,NA,NA,vertebrate,"M. J. Heaton. 1979. Cranial Anatomy of Primitive Captorhinid Reptiles from the Late Pennsylvanian and Early Permian, Oklahoma and Texas. Oklahoma Geological Survey, Bulletin 127:1-83",315,334,0,J. Mueller,T. Liebrecht,,21/01/2009 09:55,21/01/2009 11:55,28784,laticeps,Captorhinus,28362,,290.1,272.3,Artinskian,Kungurian,1,US,Captorhinus laticeps
794392,occ,NA,,85552,,Casea n. sp. nicholsi,species,120853,,Casea nicholsi,NA,species,120853,Olson,1954,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38915,NA,NA,NA,individuals,-99.575836,33.665001,Locality KC (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""South Walls of valley of South Wichita River, west of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.24,1.84,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,E. C. Olson,"1946, 1947",,"The taxon Edaphosauridae sp., represented by the specimen CNHM UR 29, was removed from the taxon list according to Modesto et al. (2016; cf. PBD collection no. 85551)",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Casea,,NA,NA,vertebrate,E. C. Olson. 1954. Fauna of the Vale and Choza: 7. Pelycosauria: family Caseidae. Fieldiana: Geology 10(17):193-204,315,334,697,J. Mueller,T. Liebrecht,E. Dunne,26/01/2009 08:54,15/03/2016 12:09,28928,nicholsi,Casea,26906,n. sp.,279.3,272.3,Kungurian,,2,US,Casea nicholsi
795195,occ,NA,,68427,,n. gen. Spinoaequalis n. sp. schultzei,species,140495,,Spinoaequalis schultzei,NA,species,140495,deBraga and Reisz,1995,Chordata,33815,Reptilia,36322,Araeoscelidia,37769,,NA,140494,NA,NA,NA,individuals,-96.113892,37.986111,Hamilton Quarry,NA,,US,Kansas,Greenwood,estimated from map,seconds,,"about 5 km E of Hamilton, Greenwood Co., Kansas, in secs. 5 and 6, T. 24 S., R. 12 E. (Virgil 7.5' quadrangle)",gp_mid,-26.91,-0.1,101,US,,Calhouns Shale,Shawnee,,,,,,,,,NA,"Virgillian Series, Upper Pennsylvanian; late Kasimovian according to Modesto et al. (2015)",,"""shale""",,,,,,,,,,estuary/bay,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Spinoaequalis,n. gen.,NA,NA,vertebrate,M. deBraga and R. R. Reisz. 1995. A new diapsid reptile from the uppermost Carboniferous (Stephanian) of Kansas. Palaeontology 38(1):199-212,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,29/01/2009 07:42,23/12/2016 14:15,19706,schultzei,Spinoaequalis,29087,n. sp.,303.4,298.9,Virgilian,,1,US,Spinoaequalis schultzei
795226,occ,NA,,28267,,n. gen. Euryodus n. sp. primus,species,120864,,Euryodus primus,NA,species,120864,Gregory et al.,1956,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37296,NA,NA,NA,individuals,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Euryodus,n. gen.,NA,NA,vertebrate,"J. T. Gregory, F. E. Peabody, and L. I. Price. 1956. Revision of the Gymnarthridae - American Permian Microsaurs. Bulletin of the Peabody Museum of Natural History 10:1-77",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,29/01/2009 12:06,29/01/2010 07:32,9228,primus,Euryodus,28484,n. sp.,279.3,272.3,Kungurian,,5,US,Euryodus primus
795287,occ,NA,R,79601,,Cacops cf. aspidophorus,species,140537,"misspelling of, obsolete variant of",Cacops aspidephorus,NA,species,56737,Olson,1956,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37025,NA,NA,NA,elements,-99.558334,33.816666,Locality FA - Pipe Site,NA,,US,Texas,Foard,estimated from map,seconds,outcrop,"southeastern corner of Foard Co.; Lat long estimation is based on map in fig. 1 in Olson (1951, J. Geol. 59(2), pp. 178-181) ",gp_mid,-30.21,0,101,US,,Choza,Clear Fork,,,,,,,,,NA,Lower part of the Choza Fm.,"""The deposits at the 'pipe site' are extremely interesting and unlike those encountered anywhere else in the Wichita or Clear Fork sections. The bed from which the fossils come is a deep red shale, exposed on a series of hills over an area about an eighth of a mile on each side. This bed is capped in many places by a thin, dense siltstone. Overlying the siltstone is an orange-red shale that carries gypsum biscuits. Underlying the producing layer, which averages about four feet in thickness, is a brownish-red shale that is devoid\r\nof fossils. The most distinctive feature of the bone-bearing shale, outside of the fact that it has fossils, is the occurrence of two types of vertically oriented ovoid structures. One type consists of mottled red and green, hard nodules that range from one to four inches in maximum diameter and up to eighteen inches in length. They are rich in vertebrate remains. They appear to have formed around the bones after deposition, presumably as a result of the reducing action of organic materials. Their vertical orientation is somewhat\r\npuzzling. The contained vertebrate remains are usually oriented with their long axes vertical, and it seems quite certain that this position was attained after the formation of the nodules. Specimens of vertebrates free in the shale rather than in nodules are orientated with their long axes horizontal and have been subjected to considerable distortion and breakage. The most reasonable suggestion seems to be that the vertical orientation of the nodules was developed during compaction of the shales, which has been extensive, with the long axes shifting to become normal to the compacting forces.\r\nThe other vertical structures [...] have been termed pipes and have given the name to the site. They pass from the base to the top of the fossiliferous bed and, at the top, are continuous with the siltstone layer that caps the bed. Their composition is similar to the capping siltstone. The pipes are oval in cross section with maximum diameters from about four to twelve inches. Orientation of the long diameters is random, even in the 'clumps' in which the pipes tend to occur. These structures do not contain vertebrates, although specimens are found 'plastered' to their sides and occasionally penetrating the pipe for a short distance.\r\nThe origin of the pipes is by no means certain. It is thought that they were formed in open holes by the introduction of the sediment that formed the siltstone layer. Superficially, they resemble lungfish burrows of the Arroyo and Vale (Romer and Olson, 1954), but the shape, size, composition, weathering, and fossil content differ. The most probable explanation is that these openings were formed by the root-like shafts of some type of plant, possibly some\r\nEquisetales, that rotted to leave openings that were later filled by sediment. There is no question that the red shales surrounding the pipes were deposited in a shallow pond, and such a pond might well have provided suitable habitat for the type of vegetation envisaged."" (Olson, 1955 pp. 60-63)","""shale""",red or brown,,,Y,,,,,,pond,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,abundant,,,NA,,,taxonomic,,,,,,E. C. Olson,1949,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Cacops,,NA,NA,vertebrate,"E. C. Olson. 1956. Fauna of the Vale and Choza: 11. Lysorophus: Vale and Choza. Diplocaulus, Cacops and Eryopidae: Choza. Fieldiana: Geology 10(25):313-322",315,334,0,J. Mueller,T. Liebrecht,,30/01/2009 10:16,30/01/2009 12:16,28508,aspidophorus,Cacops,29099,cf.,290.1,268,Leonard,,2,US,Cacops aspidophorus
795287,occ,21277,,79601,,Dissorophidae ? indet.,family,37017,,Dissorophidae,NA,family,37017,Bolt,1977,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,NA,NA,NA,NA,elements,-99.558334,33.816666,Locality FA - Pipe Site,NA,,US,Texas,Foard,estimated from map,seconds,outcrop,"southeastern corner of Foard Co.; Lat long estimation is based on map in fig. 1 in Olson (1951, J. Geol. 59(2), pp. 178-181) ",gp_mid,-30.21,0,101,US,,Choza,Clear Fork,,,,,,,,,NA,Lower part of the Choza Fm.,"""The deposits at the 'pipe site' are extremely interesting and unlike those encountered anywhere else in the Wichita or Clear Fork sections. The bed from which the fossils come is a deep red shale, exposed on a series of hills over an area about an eighth of a mile on each side. This bed is capped in many places by a thin, dense siltstone. Overlying the siltstone is an orange-red shale that carries gypsum biscuits. Underlying the producing layer, which averages about four feet in thickness, is a brownish-red shale that is devoid\r\nof fossils. The most distinctive feature of the bone-bearing shale, outside of the fact that it has fossils, is the occurrence of two types of vertically oriented ovoid structures. One type consists of mottled red and green, hard nodules that range from one to four inches in maximum diameter and up to eighteen inches in length. They are rich in vertebrate remains. They appear to have formed around the bones after deposition, presumably as a result of the reducing action of organic materials. Their vertical orientation is somewhat\r\npuzzling. The contained vertebrate remains are usually oriented with their long axes vertical, and it seems quite certain that this position was attained after the formation of the nodules. Specimens of vertebrates free in the shale rather than in nodules are orientated with their long axes horizontal and have been subjected to considerable distortion and breakage. The most reasonable suggestion seems to be that the vertical orientation of the nodules was developed during compaction of the shales, which has been extensive, with the long axes shifting to become normal to the compacting forces.\r\nThe other vertical structures [...] have been termed pipes and have given the name to the site. They pass from the base to the top of the fossiliferous bed and, at the top, are continuous with the siltstone layer that caps the bed. Their composition is similar to the capping siltstone. The pipes are oval in cross section with maximum diameters from about four to twelve inches. Orientation of the long diameters is random, even in the 'clumps' in which the pipes tend to occur. These structures do not contain vertebrates, although specimens are found 'plastered' to their sides and occasionally penetrating the pipe for a short distance.\r\nThe origin of the pipes is by no means certain. It is thought that they were formed in open holes by the introduction of the sediment that formed the siltstone layer. Superficially, they resemble lungfish burrows of the Arroyo and Vale (Romer and Olson, 1954), but the shape, size, composition, weathering, and fossil content differ. The most probable explanation is that these openings were formed by the root-like shafts of some type of plant, possibly some\r\nEquisetales, that rotted to leave openings that were later filled by sediment. There is no question that the red shales surrounding the pipes were deposited in a shallow pond, and such a pond might well have provided suitable habitat for the type of vegetation envisaged."" (Olson, 1955 pp. 60-63)","""shale""",red or brown,,,Y,,,,,,pond,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,abundant,,,NA,,,taxonomic,,,,,,E. C. Olson,1949,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Dissorophidae,?,NA,NA,vertebrate,"J. R. Bolt. 1977. Cacops (Amphibia: Labyrinthodontia) From the Fort Sill Locality, Lower Permian of Oklahoma. Fieldiana: Geology 37(3):61-73",315,334,0,J. Mueller,T. Liebrecht,,30/01/2009 10:22,30/01/2009 12:22,28508,indet.,,29098,,290.1,268,Leonard,,2,US, indet.
795288,occ,NA,,67862,,Dissorophidae indet.,family,37017,,Dissorophidae,NA,family,37017,Sullivan et al.,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,NA,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Dissorophidae,,NA,NA,"paleoentomology,vertebrate","C. Sullivan, R. R. Reisz, and W. J. May. 2000. Large dissorophoid skeletal elements from the Lower Permian Richards Spur fissures, Oklahoma, and their paleoecological implications. Journal of Vertebrate Paleontology 20(3):456-461",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,30/01/2009 10:52,29/07/2009 11:27,19393,indet.,,19394,,290.1,268,Leonard,,1,US, indet.
798713,occ,NA,,86885,,n. gen. Limnosceloides n. sp. dunkardensis,species,142126,nomen dubium,Tetrapoda,NA,unranked clade,53190,Romer,1952,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,individuals,-81.895836,38.823612,SW Cottageville,NA,"Locality N (Moran, 1952)",US,West Virginia,Mason,estimated from map,seconds,hand sample,"""About five miles southwest of Cottageville, Jackson County, West Virginia"" (Moran, 1952; Romer 1952); exact geographic position of locality is not known (Moran, 1952); lat long is based on map in Moran (1952)",gp_mid,-15.97,-3.26,101,US,,,Dunkard,,bed,,,,,,,NA,"""This area lies in the Dunkard group, but the horizon is uncertain"" (Romer, 1952).\r\nThe age of the Dunkard group, wich is not well constrained, here is based on correlation chart (fig. 4) in Wellstead (1991, Bull. AMNH 209).","""This specimen [...] was apparently found in a sandstone.""",sandstone,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,,taxonomic,,USNM,,,,Boyd C. Baker,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Limnosceloides,n. gen.,NA,NA,vertebrate,A. S. Romer. 1952. Late Pennsylvanian and Early Permian Vertebrates of the Pittsburgh-West Virginia Region. Annals of Carnegie Museum 33:47-113,315,334,0,J. Mueller,T. Liebrecht,,23/02/2009 09:09,23/02/2009 11:09,28669,dunkardensis,,28669,n. sp.,298.9,290.1,Asselian,Sakmarian,1,US, dunkardensis
798809,occ,NA,,86910,,n. gen. Romeriscus n. sp. periallus,species,142138,nomen dubium,Tetrapoda,NA,unranked clade,53190,Baird and Carroll,1967,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,individuals,-61.549999,46.040279,Cape Linzee,NA,,CA,Nova Scotia,Iverness,based on nearby landmark,seconds,,"""Cove northeast of Cape Linzee, north-northwest of Port Hood, Inverness County, Nova, Scotia."" (Baird & Carroll, 1967); lat long is for Cape Linzee",gp_mid,-8.19,-13.32,108,CA,,Port Hood,Cumberland,,bed,,,,,,,NA,"""near the middle of the Port Hood Formation, part of the coarse fluvial facies of Belt [1964, Am. J. Sci. 262] and the Riversdalean Stage of earlier authors. On the basis of nonmarine crustaceans [Copeland, 1957, Geol. Surv. Can. Mem. 286], plants [Bell, 1944, Geol. Surv. Can. Mem. 238], and microspores [Belt, 1964] the age of the Port Hood Formation is Early Pennsylvanian and equivalent to the Westphalian A of Europe."" (Baird & Carroll, 1967)","""Small lentil in 1.2-m bed of buff sandstone between Ten Inch and Four Inch Coal seams"" (Baird & Carroll, 1967)",sandstone,"lenticular,brown,yellow",,,Y,coal,,,,,wet floodplain,intermontane basin,,macrofossils,,,,,,NA,,"body,adpression,replaced with carbon",medium,,snapshot,,,,,,,NA,,"""Most bones are represented by a thin film of black, carbonaceous material on which we can see no surface detail and which we cannot prepare"" (Laurin & Reisz, 1992)",taxonomic,,,,,,"D. Baird, W. F. Take",1959,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Romeriscus,n. gen.,NA,NA,vertebrate,"D. Baird and R. L. Carroll. 1967. Romeriscus, the Oldest known Reptile. Science 157:56-59",315,334,0,J. Mueller,T. Liebrecht,,24/02/2009 04:13,24/02/2009 06:13,29243,periallus,,29243,n. sp.,318.1,314.6,Westphalian A,,1,CA, periallus
799207,occ,NA,,86946,,n. gen. Archerpeton n. sp. anthracos,species,142232,,Archerpeton anthracos,NA,species,142232,Carroll,1964,Chordata,33815,Osteichthyes,34881,Microsauria,37278,,NA,37488,NA,NA,NA,specimens,-64.451385,45.698612,"Joggins; Divison 4, Section XII, coal-group 26",NA,Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Division 4 ""of the section extends from McCairn's Cove to the end of the high cliff beyond 'Coal-mine Point'."" (Dawson, 1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173 p. 162); Lat long is approx. for Coal Mine Point",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XII",coal-group 26,,,,NA,"Coal-group 26 has a total thickness of 118 ft (including a 4 inch coaly shale). (Dawson, 1878 p. 170). Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","""Gray sandstone and shale, with erect Sigillaria; at four or five levels, and two Stigmarian underclays"" (Dawson, 1878 p. 170)",sandstone,gray,,,,claystone,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",,,snapshot,,,,,,,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" (Lyell, 1853, Quart. J. Geol. Soc. 9)",taxonomic,"field collection,survey of museum collection,observed (not collected)",,,,,"J. W. Dawson, P. W. McNaughton, among others",,,"Dawson (1878, Acadian Geology, 3rd ed.) reports Stigmaria sp. from this site","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Archerpeton,n. gen.,NA,NA,vertebrate,R. L. Carroll. 1964. The earliest reptiles. Journal of the Linnean Society (Zoology) 45(304):61-83,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,25/02/2009 07:50,13/03/2010 22:48,28956,anthracos,Archerpeton,28956,n. sp.,318.1,314.6,Westphalian A,,3,CA,Archerpeton anthracos
799210,occ,NA,,86946,,Tetrapoda indet.,unranked clade,137279,,Tetrapoda,NA,unranked clade,53190,Reisz and Modesto,1996,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,elements,-64.451385,45.698612,"Joggins; Divison 4, Section XII, coal-group 26",NA,Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Division 4 ""of the section extends from McCairn's Cove to the end of the high cliff beyond 'Coal-mine Point'."" (Dawson, 1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173 p. 162); Lat long is approx. for Coal Mine Point",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XII",coal-group 26,,,,NA,"Coal-group 26 has a total thickness of 118 ft (including a 4 inch coaly shale). (Dawson, 1878 p. 170). Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","""Gray sandstone and shale, with erect Sigillaria; at four or five levels, and two Stigmarian underclays"" (Dawson, 1878 p. 170)",sandstone,gray,,,,claystone,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",,,snapshot,,,,,,,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" (Lyell, 1853, Quart. J. Geol. Soc. 9)",taxonomic,"field collection,survey of museum collection,observed (not collected)",,,,,"J. W. Dawson, P. W. McNaughton, among others",,,"Dawson (1878, Acadian Geology, 3rd ed.) reports Stigmaria sp. from this site","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tetrapoda,,NA,NA,vertebrate,"R. R. Reisz and S. P. Modesto. 1996. Archerpeton anthracos from the Joggins Formation of Nova Scotia: a microsaur, not a reptile. Canadian Journal of Earth Sciences 33(5):703-709",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,25/02/2009 08:26,13/03/2010 22:48,28956,indet.,,29250,,318.1,314.6,Westphalian A,,4,CA, indet.
799787,occ,NA,,28256,,Diplocaulus n. sp. brevirostris,species,142470,,Diplocaulus brevirostris,NA,species,142470,Olson,1951,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1951. Diplocaulus, a Study in Growth and Variation. Fieldiana: Geology 11(2):57-154",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,02/03/2009 06:11,10/04/2009 14:19,17702,brevirostris,Diplocaulus,29284,n. sp.,279.3,272.3,Kungurian,,4,US,Diplocaulus brevirostris
799788,occ,NA,,28267,,Diplocaulus n. sp. primigenius,species,142473,subjective synonym of,Diplocaulus magnicornis,NA,species,81712,Olson,1951,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,individuals,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1951. Diplocaulus, a Study in Growth and Variation. Fieldiana: Geology 11(2):57-154",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,02/03/2009 06:31,29/01/2010 07:32,9228,primigenius,Diplocaulus,29284,n. sp.,279.3,272.3,Kungurian,,1,US,Diplocaulus primigenius
799789,occ,NA,,28267,,Diplocaulus brevirostris,species,142470,,Diplocaulus brevirostris,NA,species,142470,Olson,1951,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,individuals,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1951. Diplocaulus, a Study in Growth and Variation. Fieldiana: Geology 11(2):57-154",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,02/03/2009 06:49,29/01/2010 07:32,9228,brevirostris,Diplocaulus,29284,,279.3,272.3,Kungurian,,1,US,Diplocaulus brevirostris
799790,occ,NA,,28256,,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Olson,1951,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,specimens,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1951. Diplocaulus, a Study in Growth and Variation. Fieldiana: Geology 11(2):57-154",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,02/03/2009 06:54,10/04/2009 14:19,17702,sp.,Diplocaulus,29284,,279.3,272.3,Kungurian,,44,US,Diplocaulus sp.
799791,occ,NA,,28275,,Diplocaulus magnicornis,species,81712,,Diplocaulus magnicornis,NA,species,81712,Olson,1951,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,specimens,-99.195557,33.973057,"Beaver Creek, 42 (Arroyo Formation)",NA,"Locality 42 (Romer 1928), Beaver Creek Wilbarger County, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Wilbarger,based on nearby landmark,seconds,outcrop,"""The upper reaches of the stream have yielded a few remains."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Beaver Creek.",gp_mid,-28.81,1.94,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""above the Lueders limestone, and quite probably correspond to the beds to the south of Coffee Creek."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1951. Diplocaulus, a Study in Growth and Variation. Fieldiana: Geology 11(2):57-154",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,02/03/2009 07:14,10/05/2016 09:07,7693,magnicornis,Diplocaulus,29284,,279.3,272.3,Kungurian,,2,US,Diplocaulus magnicornis
799792,occ,NA,,28261,,Diplocaulus magnicornis,species,81712,,Diplocaulus magnicornis,NA,species,81712,Olson,1951,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,individuals,-99.144997,33.755001,"Pony Creek, 36 (Arroyo Formation)",NA,"Locality 36 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""A tributary of the Big Wichita on the south side, north of Seymour; the collections were made near the head of the creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Kemp Lake. Numbered ""36"" with taxonomic list and on map, but is incorrectly numbered ""35"" in text.",gp_mid,-28.88,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably about 100 feet above the Lueders"" Limestone. Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1951. Diplocaulus, a Study in Growth and Variation. Fieldiana: Geology 11(2):57-154",315,334,0,J. Mueller,T. Liebrecht,,02/03/2009 07:16,02/03/2009 09:16,7693,magnicornis,Diplocaulus,29284,,279.3,272.3,Kungurian,,1,US,Diplocaulus magnicornis
799793,occ,NA,,28270,,Diplocaulus magnicornis,species,81712,,Diplocaulus magnicornis,NA,species,81712,Olson,1951,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,specimens,-99.312775,33.714722,"Hog Creek, 39 (Arroyo Formation)",NA,"Locality 39 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,outcrop,"""The next creek west of Brush Creek.."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Hog Creek.",gp_mid,-29.02,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1951. Diplocaulus, a Study in Growth and Variation. Fieldiana: Geology 11(2):57-154",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,02/03/2009 07:24,13/07/2016 06:39,7693,magnicornis,Diplocaulus,29284,,279.3,272.3,Kungurian,,3,US,Diplocaulus magnicornis
799799,occ,NA,,87054,,Bolosaurus striatus,species,138029,,Bolosaurus striatus,NA,species,138029,Czaplewski et al.,1994,Chordata,33815,Reptilia,36322,,NA,Bolosauridae,37510,37511,NA,NA,NA,individuals,-97.76667,36.766666,OMNH locality V114,NA,"Grant Co., OK",US,Oklahoma,Grant,based on political unit,minutes,small collection,exact position not stated,gp_mid,-27.42,1.76,101,US,,Garber,Sumner,,formation,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,G. N. Smith,,"All specimens apparently were collected by G. N. Smith as part of a M. S. thesis, written in 1927. Since then, many specimens were lost. ",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Bolosaurus,,NA,NA,vertebrate,"N. J. Czaplewski, R. L. Cifelli, and W. Langston Jr. 1994. Catalog of type and figured fossil vertebrates, Oklahoma Museum of Natural History. Oklahoma Geological Survey Special Publication 94-1:1-35",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,02/03/2009 08:28,02/06/2009 12:00,14253,striatus,Bolosaurus,14253,,290.1,268,Leonard,,1,US,Bolosaurus striatus
799800,occ,NA,,87054,,Poliosaurus uniformis,species,138053,recombined as,Ophiacodon uniformis,NA,species,138049,Czaplewski et al.,1994,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-97.76667,36.766666,OMNH locality V114,NA,"Grant Co., OK",US,Oklahoma,Grant,based on political unit,minutes,small collection,exact position not stated,gp_mid,-27.42,1.76,101,US,,Garber,Sumner,,formation,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,G. N. Smith,,"All specimens apparently were collected by G. N. Smith as part of a M. S. thesis, written in 1927. Since then, many specimens were lost. ",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Poliosaurus,,NA,NA,vertebrate,"N. J. Czaplewski, R. L. Cifelli, and W. Langston Jr. 1994. Catalog of type and figured fossil vertebrates, Oklahoma Museum of Natural History. Oklahoma Geological Survey Special Publication 94-1:1-35",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,02/03/2009 08:28,02/06/2009 12:00,14253,uniformis,Ophiacodon,14253,,290.1,268,Leonard,,1,US,Ophiacodon uniformis
799801,occ,NA,,87054,,Clepsydrops sp.,genus,38887,,Clepsydrops,NA,genus,38887,Czaplewski et al.,1994,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38887,NA,NA,NA,individuals,-97.76667,36.766666,OMNH locality V114,NA,"Grant Co., OK",US,Oklahoma,Grant,based on political unit,minutes,small collection,exact position not stated,gp_mid,-27.42,1.76,101,US,,Garber,Sumner,,formation,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,G. N. Smith,,"All specimens apparently were collected by G. N. Smith as part of a M. S. thesis, written in 1927. Since then, many specimens were lost. ",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Clepsydrops,,NA,NA,vertebrate,"N. J. Czaplewski, R. L. Cifelli, and W. Langston Jr. 1994. Catalog of type and figured fossil vertebrates, Oklahoma Museum of Natural History. Oklahoma Geological Survey Special Publication 94-1:1-35",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,02/03/2009 08:28,02/06/2009 12:00,14253,sp.,Clepsydrops,14253,,290.1,268,Leonard,,1,US,Clepsydrops sp.
799802,occ,NA,,87054,,Dimetrodon sp.,genus,38904,,Dimetrodon,NA,genus,38904,Czaplewski et al.,1994,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,individuals,-97.76667,36.766666,OMNH locality V114,NA,"Grant Co., OK",US,Oklahoma,Grant,based on political unit,minutes,small collection,exact position not stated,gp_mid,-27.42,1.76,101,US,,Garber,Sumner,,formation,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,G. N. Smith,,"All specimens apparently were collected by G. N. Smith as part of a M. S. thesis, written in 1927. Since then, many specimens were lost. ",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"N. J. Czaplewski, R. L. Cifelli, and W. Langston Jr. 1994. Catalog of type and figured fossil vertebrates, Oklahoma Museum of Natural History. Oklahoma Geological Survey Special Publication 94-1:1-35",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,02/03/2009 08:28,02/06/2009 12:00,14253,sp.,Dimetrodon,14253,,290.1,268,Leonard,,1,US,Dimetrodon sp.
799808,occ,NA,,87054,,Eryops megacephalus,species,70397,,Eryops megacephalus,NA,species,70397,Czaplewski et al.,1994,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,individuals,-97.76667,36.766666,OMNH locality V114,NA,"Grant Co., OK",US,Oklahoma,Grant,based on political unit,minutes,small collection,exact position not stated,gp_mid,-27.42,1.76,101,US,,Garber,Sumner,,formation,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,G. N. Smith,,"All specimens apparently were collected by G. N. Smith as part of a M. S. thesis, written in 1927. Since then, many specimens were lost. ",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"N. J. Czaplewski, R. L. Cifelli, and W. Langston Jr. 1994. Catalog of type and figured fossil vertebrates, Oklahoma Museum of Natural History. Oklahoma Geological Survey Special Publication 94-1:1-35",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,02/03/2009 08:28,02/06/2009 12:00,14253,megacephalus,Eryops,14253,,290.1,268,Leonard,,1,US,Eryops megacephalus
799809,occ,NA,,87054,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Czaplewski et al.,1994,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,individuals,-97.76667,36.766666,OMNH locality V114,NA,"Grant Co., OK",US,Oklahoma,Grant,based on political unit,minutes,small collection,exact position not stated,gp_mid,-27.42,1.76,101,US,,Garber,Sumner,,formation,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,G. N. Smith,,"All specimens apparently were collected by G. N. Smith as part of a M. S. thesis, written in 1927. Since then, many specimens were lost. ",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,"N. J. Czaplewski, R. L. Cifelli, and W. Langston Jr. 1994. Catalog of type and figured fossil vertebrates, Oklahoma Museum of Natural History. Oklahoma Geological Survey Special Publication 94-1:1-35",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,02/03/2009 08:31,02/06/2009 12:00,14253,sp.,Trimerorhachis,14253,,290.1,268,Leonard,,1,US,Trimerorhachis sp.
800077,occ,NA,,87091,,Captorhinikos chozaensis,species,120856,,Captorhinikos chozaensis,NA,species,120856,Olson,1962,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37496,NA,NA,NA,individuals,-97.433334,35.233334,Norman,NA,,US,Oklahoma,Cleveland,stated in text,seconds,small collection,"""ditch along a secondary road in the NE 1/4 NW 1/4, sec. 29 T. 9 N., R. 2 W.""\r\nThis today is in the northern outskirts of Norman, OK.",gp_mid,-26.92,2.3,101,US,,Hennessey,,,bed,,,,,,,NA,"Heaton (1979, Oklahoma Geol. Surv. Bull. 127, table 1) correllates the Hennessey Shale with the Clear Fork Group of North Texas. The base and top of the Clear Fork Group are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top. Original chronostratigraphic entry >>Leonardian<< is replaced by >>Kungurian<< (TL).",,"""shale""",,,sandy,Y,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,medium,autochthonous,snapshot,,,,,,,NA,,"""Water carried in the road-side ditch and seeping into the shales, not only had damaged all of the specimens rather badly but also made it difficult to see the bone in the shale.""",taxonomic,"bulk,mechanical",FMNH,,,,E. C. Olson,1961,"""During excavation, when it was not realized that a full skeleton was present, a break was made between two blocks, each of which included part of the specimen [CNHM UR 857].""",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinikos,,NA,NA,vertebrate,"E. C. Olson. 1962. Permian vertebrates from Oklahoma and Texas. Part II - The Osteology of Captorhinikos chozaensis Olson. Oklahoma Geological Survey, Circular 59:49-68",315,334,0,J. Mueller,T. Liebrecht,,03/03/2009 16:06,03/03/2009 18:06,28600,chozaensis,Captorhinikos,28600,,279.3,272.3,Kungurian,,3,US,Captorhinikos chozaensis
800078,occ,NA,,87092,,Captorhinikos chozaensis,species,120856,,Captorhinikos chozaensis,NA,species,120856,Vaughn,1958,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37496,NA,NA,NA,individuals,-97.35833,35.141666,Noble,NA,USNM 21275,US,Oklahoma,Cleveland,stated in text,seconds,hand sample,"""the southern half of section 24, T. 8 N., R. 2 W., Cleveland County, Oklahoma""; this is about 1 Mile E of Noble, Cleveland Co., OK",gp_mid,-26.91,2.19,101,US,,Hennessey,,,bed,,,,,,,NA,"Heaton (1979, Oklahoma Geol. Surv. Bull. 127, table 1) correllates the Hennessey Shale with the Clear Fork Group of North Texas. The base and top of the Clear Fork Group are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top. Original chronostratigraphic entry >>Leonardian<< is replaced by >>Kungurian<< (TL).",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,,UNSM,,,,"D. H. Dunkle, F. H. Pearce",1953,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinikos,,NA,NA,vertebrate,"P. P. Vaughn. 1958. A Specimen of the Captorhinid Reptile Captorhinikos chozaensis Olson, 1954, from the Hennessey Formation, Lower Permian of Oklahoma. Journal of Geology 66(3):327-332",315,334,0,J. Mueller,T. Liebrecht,,03/03/2009 17:10,03/03/2009 19:10,29303,chozaensis,Captorhinikos,29303,,279.3,272.3,Kungurian,,1,US,Captorhinikos chozaensis
800079,occ,NA,,84719,,n. gen. Intasuchus n. sp. silvicola,species,142538,,Intasuchus silvicola,NA,species,142538,Olson,1957,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Intasuchidae,137935,37012,NA,NA,NA,,60.049999,66.033333,Inta city,NA,,RU,Komi,Inta,stated in text,minutes,small collection,Pechora Basin; Lat Long is from Olson (1957),gp_mid,35.28,33.63,302,RU,,Inta,,,,,,,,,,NA,"Locality biostratigraphically lies within the Inta Assemblage Zone (Inta Kompleks) (Ivakhnenko, 1990; Modesto & Rybczynski, 2000), which is Asselian to Ufimian in age (Modesto & Rybczynski, 2000). Ivakhnenko (1990, fig. 1) and Shishkin et al. (2000) say that the locality is of Ufimian age; Ivakhnenko (2008 p. 87) states that the locality is Artinskian in age (""same age"" as type locality of Riabininus uralensis, see collection (84718)).","""Carbonaceous shales and channel sandstone"" (Olson, 1957)","""shale""",,,carbonaceous,,sandstone,,,,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,PIN,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Intasuchus,n. gen.,NA,NA,vertebrate,E. C. Olson. 1957. Catalogue of Localities of Permian and Triassic Terrestrial Vertebrates of the Territiories of the USSR. Journal of Geology 65(2):196-226,315,334,327,J. Mueller,T. Liebrecht,R. Butler,03/03/2009 17:37,17/07/2017 08:25,28378,silvicola,Intasuchus,5921,n. sp.,290.1,272.5,Artinskian,Ufimian,NA,RU,Intasuchus silvicola
800080,occ,NA,,84719,,n. gen. Syndyodosuchus n. sp. tetricus,species,142539,,Syndyodosuchus tetricus,NA,species,142539,Olson,1957,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Actinodontidae,66914,37016,NA,NA,NA,,60.049999,66.033333,Inta city,NA,,RU,Komi,Inta,stated in text,minutes,small collection,Pechora Basin; Lat Long is from Olson (1957),gp_mid,35.28,33.63,302,RU,,Inta,,,,,,,,,,NA,"Locality biostratigraphically lies within the Inta Assemblage Zone (Inta Kompleks) (Ivakhnenko, 1990; Modesto & Rybczynski, 2000), which is Asselian to Ufimian in age (Modesto & Rybczynski, 2000). Ivakhnenko (1990, fig. 1) and Shishkin et al. (2000) say that the locality is of Ufimian age; Ivakhnenko (2008 p. 87) states that the locality is Artinskian in age (""same age"" as type locality of Riabininus uralensis, see collection (84718)).","""Carbonaceous shales and channel sandstone"" (Olson, 1957)","""shale""",,,carbonaceous,,sandstone,,,,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,PIN,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Syndyodosuchus,n. gen.,NA,NA,vertebrate,E. C. Olson. 1957. Catalogue of Localities of Permian and Triassic Terrestrial Vertebrates of the Territiories of the USSR. Journal of Geology 65(2):196-226,315,334,327,J. Mueller,T. Liebrecht,R. Butler,03/03/2009 17:37,17/07/2017 08:25,28378,tetricus,Syndyodosuchus,5921,n. sp.,290.1,272.5,Artinskian,Ufimian,NA,RU,Syndyodosuchus tetricus
806750,occ,NA,,28250,,Araeoscelis casei,species,138984,,Araeoscelis casei,NA,species,138981,Vaughn,1955,Chordata,33815,Reptilia,36322,Araeoscelidia,37769,Araeoscelidae,37772,37773,NA,NA,NA,individuals,-99.091667,33.733334,"Mitchell Creek, 29 (Waggoner Ranch Formation)",NA,"Locality 29 (Romer 1928), old Bar X pasture, Timber Creek, faunal Zone 3, Upper Wichita Group, Texas red-beds, redbeds, Lucas Ranch",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""near Mitchell and Timber Creeks, northeast of Maybelle in the old Bar X pasture."" See detailed locality map in Romer 1928. ""Zone 3. Upper Wichita; to the Leuders Limestone; Clyde Formation?"". Numbered ""29"" with taxonomic list and on map, but is incorrectly numbered ""28"" in text. Lat long is for area enclosed by Mitchell Creek (W), Big Wichita River (N), Timber Creek (E), and U.S. 277 (S).",gp_mid,-30.29,-0.93,101,US,,Waggoner Ranch,Wichita,,group of beds,,,,,,,NA,"""It is about 150 feet above the Beaverburk."" Details for Faunal Zone 3 of Romer 1928: ""approximately 230 feet in thickness...The total thickness of the Wichita group, as thus defined is, in this region, approximately 780 feet."" Clyde Formation is approx. equivalent to Waggoner Ranch Formation (Hetz and Brown 1987).\nthe Waggoner Ranch Formation is equivalent to the Bead Mountain through Lueders formations (Tabor et al. 2002), which are late Artinskian and early Kungurian according to Wardlaw 2005, Permophiles (JA)","""limestones, often impure, with blue and red shales.""","""limestone""",,,,,"""shale""","red,blue",,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Araeoscelis,,NA,NA,vertebrate,P. P. Vaughn. 1955. The Permian reptile Araeoscelis restudied. Bulletin of the Museum of Comparative Zoology 113(5):305-467,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,02/04/2009 12:33,11/06/2009 05:56,7693,casei,Araeoscelis,4323,,290.1,272.3,Artinskian,Kungurian,5,US,Araeoscelis casei
806953,occ,NA,,28256,,Labidosaurus hamatus,species,134918,,Labidosaurus hamatus,NA,species,134856,Romer,1928,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,specimens,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,vertebrate,A. S. Romer. 1928. Vertebrate faunal horizons in the Texas Permo-Carboniferous red beds. University of Texas Bulletin 2801:67-108,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,03/04/2009 04:58,10/04/2009 14:19,17702,hamatus,Labidosaurus,7693,,279.3,272.3,Kungurian,,32,US,Labidosaurus hamatus
814375,occ,NA,,80783,,n. gen. Oxyodon n. sp. britannicus,species,147996,recombined as,Sphenacodon britannicus,NA,species,147996,Paton,1974,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,individuals,-1.575,52.375,Kenilworth,NA,,UK,England,Warwickshire,based on nearby landmark,seconds,small collection,""" [...] close to Kenilworth [...] "". Paton (1974) states that all the material collected from near Kenilworth comes from a single locality whose precise location is not known. Locality is ""probably now obscured by buildings"" (Paton 1974).",gp_mid,13.51,6.65,315,UK,,Kenilworth Sandstone,Warwickshire,,group of beds,,,,,,,NA,"The Kenilworth Sandstone is lowest Permian, possibly uppermost Carboniferous, and is a subunit of the Warwickshire Group (e.g., Powell et al., 2000, British Geological Survey Research Report RR/00/01; Ruffell et al., 2006, in Brenchley & Rawson (eds.), The Geology of England and Wales).","The Kenilworth Sandstone Formation is represented mainly by coarse grained siliciclastics (sandstones, conglomerates, breccias) deposited by freshwater action (Powell et al., 2000; Ruffell et al., 2006). ","""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,BGS,,,,,,GSM = Geological Survey Museum (British Geological Survey)\r\nGz = Warwick County Museum,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Oxyodon,n. gen.,NA,NA,vertebrate,R. L. Paton. 1974. Lower Permian Pelycosaurs from the English Midlands. Palaeontology 17(3):541-552,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,10/06/2009 11:47,10/06/2009 13:49,30063,britannicus,Sphenacodon,30063,n. sp.,298.9,295.5,Asselian,,1,UK,Sphenacodon britannicus
814377,occ,NA,,89649,,Ophiacodon sp.,genus,38888,,Ophiacodon,NA,genus,38888,Paton,1974,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,specimens,-1.519444,52.413891,Coventry,NA,,UK,England,Warwickshire,stated in text,seconds,hand sample,"""One mile north-west of Coventry"". Paton (1974) gives the British Grid Reference as ST 327 797 which in fact is relatively close to the center of Greater Coventry. Locality is ""probably now obscured by buildings"" (Paton 1974).",gp_mid,13.54,6.7,315,UK,,Kenilworth Sandstone,Warwickshire,,bed,,,,,,,NA,"Given as ""Kenilworth Breccia"" in the primary reference. This term is redundant and synonymous with Kenilworth Sandstone according to the British Geological Survey Lexicon of Lexicon of Named Rock Units (http://www.bgs.ac.uk/lexicon/lexicon.cfm?pub=KHS). The Kenilworth Sandstone is lowest Permian, possibly uppermost Carboniferous, and is a subunit of the Warwickshire Group (e.g., Powell et al., 2000, British Geological Survey Research Report RR/00/01; Ruffell et al., 2006, in Brenchley & Rawson (eds.), The Geology of England and Wales).",""" [...] coarse, red, loosely cemented sandstone containing pellets of red clay [...] "" Paton (1974).\r\nThe Kenilworth Sandstone Formation in general is represented mainly by coarse grained siliciclastics (sandstones, conglomerates, breccias) deposited by freshwater action (Powell et al., 2000; Ruffell et al., 2006). ",sandstone,"coarse,red",poorly lithified,,Y,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Gz = Warwick County Museum,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,R. L. Paton. 1974. Lower Permian Pelycosaurs from the English Midlands. Palaeontology 17(3):541-552,315,334,0,J. Mueller,T. Liebrecht,,10/06/2009 12:31,10/06/2009 14:31,30063,sp.,Ophiacodon,30063,,298.9,295.5,Asselian,,1,UK,Ophiacodon sp.
814504,occ,NA,,85733,,Cricotus hypantricus,species,346339,subjective synonym of,Cricotus crassidiscus,NA,species,309860,Cummins,1908,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37197,NA,NA,NA,,-98.59861,34.295834,Deep Red Run,NA,"Deep Red Creek; Cope's ""Indian Territory""",US,Oklahoma,Cotton,estimated from map,seconds,outcrop,"""There was at one time a small fort called Fort Auger on the north side of Red River about opposite where the town of Iowa Park is now located. There was a road leading from Fort Auger to Fort Sill. Near the crossing of Deep Red Creek by this old road is the locality at which I collected the vertebrates in Cope's collection labelled 'Indian Territory.' "" (Cummins, 1908).\r\n""This site is in Cotton County [...]. The site is several miles northwest of Randlett, but we were not able to locate it more precisely."" (Olson, 1967, Oklahoma Geol. Surv. Circ. 74).\r\nLat long is for Deep Red Creek immediately east of Tillman-Cotton County line (sec. 18, T.3S. R.13W., Whites Lake 7.5' quadrangle).",gp_mid,-29.65,-0.67,101,US,,Garber,Sumner,,member,,,,,,,NA,"""The trend of the strike of the texas beds suggests that the locality lies in the Clyde formation. [...] The presence of a large Dimetrodon [...] suggests a higher position; of Cricotus a lower one; of Ophiacodon major the Clyde itself. The somewhat conflicting evidence is thus on the whole agreeable to an approximate Clyde determination."" (Romer & Price, 1940).\r\nIn the chart (fig. 2) of Olson (1967, Oklahoma Geol. Surv. Circ. 74) the relevant stratigraphic unit is given as ""Hennessey Shale"" but is correlated with the Garber Sandstone of other parts of Oklahoma.\r\nIn the stratigraphic chart (table 1) of Heaton (1979, Oklahoma Geol. Surv. Bull. 127) the Deep Red Run locality is assigned to the middle part of the Garber Sandstone, the latter being correlated with the Lueders Fm. of Texas.",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,W. F. Cummins,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cricotus,,NA,NA,vertebrate,W. F. Cummins. 1908. The Localities and Horizons of Permian Vertebrate Fossils in Texas. Journal of Geology 16(8):737-745,315,334,0,J. Mueller,T. Liebrecht,,11/06/2009 09:45,11/06/2009 11:45,30068,hypantricus,Cricotus,30068,,290.1,272.3,Artinskian,Kungurian,NA,US,Cricotus hypantricus
814505,occ,NA,,85733,,Dimetrodon gigas,species,138120,subjective synonym of,Eryops megacephalus,NA,species,70397,Cummins,1908,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-98.59861,34.295834,Deep Red Run,NA,"Deep Red Creek; Cope's ""Indian Territory""",US,Oklahoma,Cotton,estimated from map,seconds,outcrop,"""There was at one time a small fort called Fort Auger on the north side of Red River about opposite where the town of Iowa Park is now located. There was a road leading from Fort Auger to Fort Sill. Near the crossing of Deep Red Creek by this old road is the locality at which I collected the vertebrates in Cope's collection labelled 'Indian Territory.' "" (Cummins, 1908).\r\n""This site is in Cotton County [...]. The site is several miles northwest of Randlett, but we were not able to locate it more precisely."" (Olson, 1967, Oklahoma Geol. Surv. Circ. 74).\r\nLat long is for Deep Red Creek immediately east of Tillman-Cotton County line (sec. 18, T.3S. R.13W., Whites Lake 7.5' quadrangle).",gp_mid,-29.65,-0.67,101,US,,Garber,Sumner,,member,,,,,,,NA,"""The trend of the strike of the texas beds suggests that the locality lies in the Clyde formation. [...] The presence of a large Dimetrodon [...] suggests a higher position; of Cricotus a lower one; of Ophiacodon major the Clyde itself. The somewhat conflicting evidence is thus on the whole agreeable to an approximate Clyde determination."" (Romer & Price, 1940).\r\nIn the chart (fig. 2) of Olson (1967, Oklahoma Geol. Surv. Circ. 74) the relevant stratigraphic unit is given as ""Hennessey Shale"" but is correlated with the Garber Sandstone of other parts of Oklahoma.\r\nIn the stratigraphic chart (table 1) of Heaton (1979, Oklahoma Geol. Surv. Bull. 127) the Deep Red Run locality is assigned to the middle part of the Garber Sandstone, the latter being correlated with the Lueders Fm. of Texas.",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,W. F. Cummins,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,W. F. Cummins. 1908. The Localities and Horizons of Permian Vertebrate Fossils in Texas. Journal of Geology 16(8):737-745,315,334,0,J. Mueller,T. Liebrecht,,11/06/2009 09:45,11/06/2009 11:45,30068,gigas,Eryops,30068,,290.1,272.3,Artinskian,Kungurian,NA,US,Eryops gigas
814506,occ,NA,,85733,,Dimetrodon macrospondylus,species,138127,,Dimetrodon macrospondylus,NA,species,138122,Cummins,1908,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-98.59861,34.295834,Deep Red Run,NA,"Deep Red Creek; Cope's ""Indian Territory""",US,Oklahoma,Cotton,estimated from map,seconds,outcrop,"""There was at one time a small fort called Fort Auger on the north side of Red River about opposite where the town of Iowa Park is now located. There was a road leading from Fort Auger to Fort Sill. Near the crossing of Deep Red Creek by this old road is the locality at which I collected the vertebrates in Cope's collection labelled 'Indian Territory.' "" (Cummins, 1908).\r\n""This site is in Cotton County [...]. The site is several miles northwest of Randlett, but we were not able to locate it more precisely."" (Olson, 1967, Oklahoma Geol. Surv. Circ. 74).\r\nLat long is for Deep Red Creek immediately east of Tillman-Cotton County line (sec. 18, T.3S. R.13W., Whites Lake 7.5' quadrangle).",gp_mid,-29.65,-0.67,101,US,,Garber,Sumner,,member,,,,,,,NA,"""The trend of the strike of the texas beds suggests that the locality lies in the Clyde formation. [...] The presence of a large Dimetrodon [...] suggests a higher position; of Cricotus a lower one; of Ophiacodon major the Clyde itself. The somewhat conflicting evidence is thus on the whole agreeable to an approximate Clyde determination."" (Romer & Price, 1940).\r\nIn the chart (fig. 2) of Olson (1967, Oklahoma Geol. Surv. Circ. 74) the relevant stratigraphic unit is given as ""Hennessey Shale"" but is correlated with the Garber Sandstone of other parts of Oklahoma.\r\nIn the stratigraphic chart (table 1) of Heaton (1979, Oklahoma Geol. Surv. Bull. 127) the Deep Red Run locality is assigned to the middle part of the Garber Sandstone, the latter being correlated with the Lueders Fm. of Texas.",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,W. F. Cummins,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,W. F. Cummins. 1908. The Localities and Horizons of Permian Vertebrate Fossils in Texas. Journal of Geology 16(8):737-745,315,334,0,J. Mueller,T. Liebrecht,,11/06/2009 09:45,11/06/2009 11:45,30068,macrospondylus,Dimetrodon,30068,,290.1,272.3,Artinskian,Kungurian,NA,US,Dimetrodon macrospondylus
814507,occ,NA,,85733,,Dimetrodon dollovianus,species,122785,,Dimetrodon dollovianus,NA,species,138126,Cummins,1908,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-98.59861,34.295834,Deep Red Run,NA,"Deep Red Creek; Cope's ""Indian Territory""",US,Oklahoma,Cotton,estimated from map,seconds,outcrop,"""There was at one time a small fort called Fort Auger on the north side of Red River about opposite where the town of Iowa Park is now located. There was a road leading from Fort Auger to Fort Sill. Near the crossing of Deep Red Creek by this old road is the locality at which I collected the vertebrates in Cope's collection labelled 'Indian Territory.' "" (Cummins, 1908).\r\n""This site is in Cotton County [...]. The site is several miles northwest of Randlett, but we were not able to locate it more precisely."" (Olson, 1967, Oklahoma Geol. Surv. Circ. 74).\r\nLat long is for Deep Red Creek immediately east of Tillman-Cotton County line (sec. 18, T.3S. R.13W., Whites Lake 7.5' quadrangle).",gp_mid,-29.65,-0.67,101,US,,Garber,Sumner,,member,,,,,,,NA,"""The trend of the strike of the texas beds suggests that the locality lies in the Clyde formation. [...] The presence of a large Dimetrodon [...] suggests a higher position; of Cricotus a lower one; of Ophiacodon major the Clyde itself. The somewhat conflicting evidence is thus on the whole agreeable to an approximate Clyde determination."" (Romer & Price, 1940).\r\nIn the chart (fig. 2) of Olson (1967, Oklahoma Geol. Surv. Circ. 74) the relevant stratigraphic unit is given as ""Hennessey Shale"" but is correlated with the Garber Sandstone of other parts of Oklahoma.\r\nIn the stratigraphic chart (table 1) of Heaton (1979, Oklahoma Geol. Surv. Bull. 127) the Deep Red Run locality is assigned to the middle part of the Garber Sandstone, the latter being correlated with the Lueders Fm. of Texas.",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,W. F. Cummins,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,W. F. Cummins. 1908. The Localities and Horizons of Permian Vertebrate Fossils in Texas. Journal of Geology 16(8):737-745,315,334,0,J. Mueller,T. Liebrecht,,11/06/2009 09:45,11/06/2009 11:45,30068,dollovianus,Dimetrodon,30068,,290.1,272.3,Artinskian,Kungurian,NA,US,Dimetrodon dollovianus
814508,occ,NA,,85733,,Dimetrodon platycentrus,species,138128,subjective synonym of,Dimetrodon macrospondylus,NA,species,138122,Cummins,1908,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-98.59861,34.295834,Deep Red Run,NA,"Deep Red Creek; Cope's ""Indian Territory""",US,Oklahoma,Cotton,estimated from map,seconds,outcrop,"""There was at one time a small fort called Fort Auger on the north side of Red River about opposite where the town of Iowa Park is now located. There was a road leading from Fort Auger to Fort Sill. Near the crossing of Deep Red Creek by this old road is the locality at which I collected the vertebrates in Cope's collection labelled 'Indian Territory.' "" (Cummins, 1908).\r\n""This site is in Cotton County [...]. The site is several miles northwest of Randlett, but we were not able to locate it more precisely."" (Olson, 1967, Oklahoma Geol. Surv. Circ. 74).\r\nLat long is for Deep Red Creek immediately east of Tillman-Cotton County line (sec. 18, T.3S. R.13W., Whites Lake 7.5' quadrangle).",gp_mid,-29.65,-0.67,101,US,,Garber,Sumner,,member,,,,,,,NA,"""The trend of the strike of the texas beds suggests that the locality lies in the Clyde formation. [...] The presence of a large Dimetrodon [...] suggests a higher position; of Cricotus a lower one; of Ophiacodon major the Clyde itself. The somewhat conflicting evidence is thus on the whole agreeable to an approximate Clyde determination."" (Romer & Price, 1940).\r\nIn the chart (fig. 2) of Olson (1967, Oklahoma Geol. Surv. Circ. 74) the relevant stratigraphic unit is given as ""Hennessey Shale"" but is correlated with the Garber Sandstone of other parts of Oklahoma.\r\nIn the stratigraphic chart (table 1) of Heaton (1979, Oklahoma Geol. Surv. Bull. 127) the Deep Red Run locality is assigned to the middle part of the Garber Sandstone, the latter being correlated with the Lueders Fm. of Texas.",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,W. F. Cummins,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,W. F. Cummins. 1908. The Localities and Horizons of Permian Vertebrate Fossils in Texas. Journal of Geology 16(8):737-745,315,334,0,J. Mueller,T. Liebrecht,,11/06/2009 09:45,11/06/2009 11:45,30068,platycentrus,Dimetrodon,30068,,290.1,272.3,Artinskian,Kungurian,NA,US,Dimetrodon platycentrus
814509,occ,NA,,85733,,Naosaurus cruciger,species,138135,recombined as,Edaphosaurus cruciger,NA,species,138134,Cummins,1908,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,,-98.59861,34.295834,Deep Red Run,NA,"Deep Red Creek; Cope's ""Indian Territory""",US,Oklahoma,Cotton,estimated from map,seconds,outcrop,"""There was at one time a small fort called Fort Auger on the north side of Red River about opposite where the town of Iowa Park is now located. There was a road leading from Fort Auger to Fort Sill. Near the crossing of Deep Red Creek by this old road is the locality at which I collected the vertebrates in Cope's collection labelled 'Indian Territory.' "" (Cummins, 1908).\r\n""This site is in Cotton County [...]. The site is several miles northwest of Randlett, but we were not able to locate it more precisely."" (Olson, 1967, Oklahoma Geol. Surv. Circ. 74).\r\nLat long is for Deep Red Creek immediately east of Tillman-Cotton County line (sec. 18, T.3S. R.13W., Whites Lake 7.5' quadrangle).",gp_mid,-29.65,-0.67,101,US,,Garber,Sumner,,member,,,,,,,NA,"""The trend of the strike of the texas beds suggests that the locality lies in the Clyde formation. [...] The presence of a large Dimetrodon [...] suggests a higher position; of Cricotus a lower one; of Ophiacodon major the Clyde itself. The somewhat conflicting evidence is thus on the whole agreeable to an approximate Clyde determination."" (Romer & Price, 1940).\r\nIn the chart (fig. 2) of Olson (1967, Oklahoma Geol. Surv. Circ. 74) the relevant stratigraphic unit is given as ""Hennessey Shale"" but is correlated with the Garber Sandstone of other parts of Oklahoma.\r\nIn the stratigraphic chart (table 1) of Heaton (1979, Oklahoma Geol. Surv. Bull. 127) the Deep Red Run locality is assigned to the middle part of the Garber Sandstone, the latter being correlated with the Lueders Fm. of Texas.",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,W. F. Cummins,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Naosaurus,,NA,NA,vertebrate,W. F. Cummins. 1908. The Localities and Horizons of Permian Vertebrate Fossils in Texas. Journal of Geology 16(8):737-745,315,334,0,J. Mueller,T. Liebrecht,,11/06/2009 09:45,11/06/2009 11:45,30068,cruciger,Edaphosaurus,30068,,290.1,272.3,Artinskian,Kungurian,NA,US,Edaphosaurus cruciger
817103,occ,NA,,77412,,Oedaleops ? campi,species,122198,,Oedaleops campi,NA,species,122198,Langston,1965,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Eothyrididae,38898,38900,NA,NA,NA,individuals,-106.639442,36.157223,UCMP V-2814,NA,Camp Quarry,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"""southeast slope of a small butte, 410 yards south of New Mexico State Highway 96, about 940 yards southeast of the Rio Puerco bridge at Arroyo del Agua, section 8, T.22N., R.3E., Rio Arriba County, New Mexico"" (Langston, 1965 p. 6; 1966 p.691)",gp_mid,-34.09,4.48,101,US,FED,Abo/Cutler,,,group of beds,,,,,,,NA,All specimens appear to come from about the same stratigraphic level (38-36 m below top of the butte). Whether these beds are uppermost Carboniferous or lower Permian is a subject of controversy.\r\n,"""soft brick-red clayey siltstone"" (Langston, 1965 p. 6; 1966 p.691; Langston & Reisz, 1981 p. 74)",siltstone,red,,argillaceous,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,general faunal/floral,"bulk,surface (float),survey of museum collection",UCMP,all macrofossils,,,"C. L. Camp, among others","1928, 1934, 1935","""Berman & Reisz reopened this quarry in 1979, but despite extensive digging by a team of five people, only a few scattered bone fragments were recovered. It appears that the site has been completeley exhausted"" (Langston & Reisz, 1981 p. 74).\r\nType of Rhiodenticulatus heatoni was ""probably not found in the main bone level of the quarry, but rather as float on the slope of Loma Salazar a few feet away and presumably at or just above the quarry bone level."" (Berman & Reisz, 1986).","""Captorhinomorphs and Diadectomorphs"" (Langston 1966 p.690)",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Oedaleops,?,NA,NA,vertebrate,"W. Langston, Jr. 1965. Oedaleops campi (Reptilia: Pelycosauria) New Genus and Species from the Lower Permian of New Mexico, and the Family Eothyrididae. Bulletin of the Texas Memorial Museum 9:1-47",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,20/06/2009 05:50,20/06/2009 07:51,26206,campi,Oedaleops,30116,,303.4,268,Virgilian,Wolfcamp,1,US,Oedaleops campi
820357,occ,NA,,90190,,Mesosauridae indet.,family,37578,,Mesosauridae,NA,family,37578,Rossmann and Maisch,1999,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Mesosauridae,37578,NA,NA,NA,NA,individuals,-50.422222,-25.844444,Ṣo Mateus do Sul,NA,"? Petrosix quarry, ? Petrobrs Six quarry; Paran Basin",BR,Paran,Ṣo Mateus do Sul,estimated from map,seconds,outcrop,""" [...] Sao Mateus do Sul (Steinbruch des Petrobas), Parana, Brasilien."" (Rossmann & Maisch, 1999). Note: ""Steinbruch des Petrobas"" very likely refers to the large Petrosix or Petrobrs/Six quarry about 5 km NW of Ṣo Mateus do Sul. Specimens listed to come from Ṣo Mateus do Sul in other papers than that of Rossman & Maisch (1999) may also come from that quarry or at least from the immediate vicinity of the town. DMS coordinates are for Petrosix quarry.",gp_mid,-31.49,-47.4,201,BR,,Irati,Passa Dois,,member,,,,,,,NA,"The authors state that the fossils come from the Irati Formation but only give ""Lower Permian"" as the most precise age specification. However, in a fairly recent publication it is stated that the Irati Formation is Artinskian in age, based on absolute ages obtained from zircons from a bentonite layer (Santos et al., 2006, Gondwana Res. 9). ","""Exemplare [... sind ...] in einem schwarzen bitumenreichen Schiefer (l- oder Schwarzschiefer) eingebettet [...]"" [Specimens [... are ...] embedded in a black bituminous shale (oil or black shale)]. (Rossmann & Maisch, 1999). Same data is given in Rossmann (2000) and Karl et al. (2007).","""shale""",black,,,Y,,,,,,offshore,cratonic basin,,macrofossils,,,,,,NA,,"body,mold/impression",good,,time-averaged,,,,,,,NA,,"Even though at least the tip of the snout and/or the distal part of the tail is missing in some otherwise fully articulated skeletons, these specimens are regarded as ""articulated whole bodies"" in the collection record. Some skeletons are disassociated. Almost all specimens are represented by moulds. Bone preservation is rare and occurs only in parts of the skeletons. ",taxonomic,survey of museum collection,"BSP,SMF",,,,,,"BSP = Bayerische Staatssammlung f_r Pal_ontologie und Historische Geologie, M_nchen [Bavarian State Collection of Palaeontology and Historical Geology, Munich]\r\nGZG.V = Vertebrate Collection of Geoscience Center of G̦ttingen University (Geowisschenschafliches Zentrum der Universit_t G̦ttingen)\r\nSMF = Senckenberg Museum, Frankfurt/Main",Specimens listed by Rossmann & Maisch (1999) are taxonomically revised and may originally have been referred to different taxa (in most cases this may have been the junior synonyms of the taxa currently considered valid).\r\nSpecimens listed by Karl et al. (2007) are revised as well and were previously identified as Mesosaurus brasiliensis.,"coastal,marine,brackish",NA,actively mobile,amphibious,NA,piscivore,dispersal=direct/internal,"addition of parts,modification of parts",hydroxyapatite,,NA,,Mesosauridae,,NA,NA,vertebrate,T. Rossmann and M. W. Maisch. 1999. Das Mesosaurier-Material in der Bayerischen Staatssammlung f_r Pal_ontologie und Historische Geologie: bersicht und neue Erkenntnisse. Mitteilungen der Bayerischen Staatssammlung f_r Pal_ontologie und Historische Geologie 39:69-83,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,13/07/2009 10:19,13/07/2009 12:20,30263,indet.,,30263,,290.1,279.3,Artinskian,,3,BR, indet.
820711,occ,NA,,90257,,Mesosaurus n. sp. pleurogaster,species,149587,nomen dubium,Mesosauridae,NA,family,37578,Seeley,1892,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Mesosauridae,37578,NA,NA,NA,NA,individuals,24.766666,-28.737499,Kimberley,NA,"""Burghersdorp""",ZA,Northern Cape,Frances Baard,based on nearby landmark,seconds,outcrop,"All specimens of Mesosaurus pleurogaster either come immediately from the town of Kimberley or from the diamond open-cast mines in the immediate vicinity of Kimberley. DMS coordinates are for Kimberley, Frances Baard District Municipality, Northern Cape Province, South Africa.",gp_mid,-41.44,-63.64,701,ZA,,Whitehill,Ecca,,formation,,,,,,,NA,"No formational name is given by Seeley (1892). The geographic position of Kimberley suggests that the fossils come from either the Prince Albert or the Whitehill Fm. of the Ecca Group (see fig. 24 in Catuneanu et al., 2005, Afr. J. Earth Sci. 43). Also, Rossmann (2000) explicitly states that the type specimens are from the Whitehill Formation.\r\nRadiometric ages of the Collinson Fm. (overlying the Whitehill Fm.) vary between 270 and 275 Ma (Turner, 1999, J. Afr. Earth Sci. 28(1); Fildani et al., 2007 J. Sedim. Res. 77), and radiometric ages of the basal beds of the Prince Albert Fm. (underlying the Whitehill Fm.) vary between 293 and 285 Ma (Bangert et al., 1999, J. Afr. Earth Sci. 29(1)), implying an Artinskian age for the Whitehill Fm. (cf. time scales of Gradstein et al. (2004) and Ogg et al. (2008)). Radiometric dating within the Whitehill Fm. of southern Namibia (Werner, 2006, PhD thesis, http://www.opus-bayern.de/uni-wuerzburg/volltexte/2007/2175/pdf/00-Complete_thesis-STD.pdf) corroborates an assigment to the Artinskian.",,"""shale""",white,,calcareous,Y,"""shale""",,poorly lithified,,Y,offshore,foreland basin,,macrofossils,,,,,,NA,,mold/impression,good,,time-averaged,,,,,,,NA,,,taxonomic,"selective quarrying,survey of museum collection",BMNH,,,,,1878,"Plaster casts of BMNH 49971 and 49972 are reposited in the collections of the Museum f_r Naturkunde Berlin (Liebrecht & M_ller, 2009). A plaster cast of one specimen of the type series (apparently not the one figured by Seeley, 1892, fig. 1 pl. 18) is reposited under SMF-R-4953 in the collections of the Senckenberg Museum, Frankfurt/Main.","The Mesosaurus sp. specimen is said to come ""from near Burghersdorp"" by Seeley (1892) without giving any further geographic details. ""Burghersdorp"" probably refers to the town of Burgersdorp in the Eastern Cape Province of South Africa. This town, however, is located on outcrop of terrestrial deposits of the uppermost Beaufort Group (Lower Triassic), about 100 km SE from the Ecca-Beaufort contact. Thus, it is very unlikely that the fossil described by Seeley (1892, pp. 597/598) comes from the vicinity of Burgersdorp, Eastern Cape. It may rather come from what today is the Northern Cape Province.\r\nS. Sch̦nland (in an endnote of a paper by Broom, 1905, Rec. Albany Mus. 1(4) p. 278) notes that the ""Mesosaurus in the Albany Museum"" actually is not from near Burgersdorp but from Kimberley. Hence, the Mesosaurus sp. specimen is included here.","coastal,marine,brackish",NA,actively mobile,amphibious,NA,piscivore,dispersal=direct/internal,"addition of parts,modification of parts",hydroxyapatite,,NA,,Mesosaurus,,NA,NA,vertebrate,H. G. Seeley. 1892. The Mesosauria of South Africa. Quarterly Journal of the Geological Society of London 48:586-604,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,15/07/2009 10:22,15/07/2009 12:23,30298,pleurogaster,,30298,n. sp.,290.1,279.3,Artinskian,,3,ZA, pleurogaster
821127,occ,NA,,90358,,Mesosauridae indet.,family,37578,,Mesosauridae,NA,family,37578,Rossmann,2000,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Mesosauridae,37578,NA,NA,NA,NA,individuals,-47.716667,-23.1,"Mayro limestone quarry, Tiet̻",NA,Paran Basin,BR,Ṣo Paulo,Tiet̻,based on nearby landmark,minutes,hand sample,"""Kalksteinbruch von J. Mayro, Tiet̻, Sao Paulo, S_dbrasilien."" (Rossmann, 2000).\r\nPolar coordinates are for town of Tiet̻.",gp_mid,-26.55,-45.94,201,BR,,Irati,Passa Dois,Assistencia,bed,,,,,,,NA,"Rossmann (2000) states that the fossils come from the Irati Formation but only gives ""Lower Permian"" as the most precise age specification. However, in a quite recent publication it is stated that the Irati Formation is Artinskian in age, based on absolute ages obtained from zircons from a bentonite layer (Santos et al., 2006, Gondwana Res. 9). Preservation in limestone suggests that the fossils come from the Assist̻ncia Member of the Irati Fm. (see Santos et al., 2009, J. S. Am. Earth Sci., Article in Press, doi:10.1016/j.jsames.2008.12.002).",light yellow limestone,"""limestone""","white,yellow",,,Y,,,,,,carbonate indet.,cratonic basin,,macrofossils,,,,,,NA,,body,good,,time-averaged,,,,,,,NA,,white bone preservation,taxonomic,survey of museum collection,SMF,,,,,,"SMF = Senckenberg Museum, Frankfurt/Main",,"coastal,marine,brackish",NA,actively mobile,amphibious,NA,piscivore,dispersal=direct/internal,"addition of parts,modification of parts",hydroxyapatite,,NA,,Mesosauridae,,NA,NA,vertebrate,"T. Rossmann. 2000. Studien an Mesosauriern (Amniota inc sed: Mesosauridae): 2 Neue Erkenntnisse zur Anatomie, mit Ber_cksichtigung der Taxonomie von Mesosaurus pleurogaster (Seeley). Senckenbergiana lethaea 80(1):13-28",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,17/07/2009 13:27,17/07/2009 15:28,30341,indet.,,30341,,290.1,279.3,Artinskian,,3,BR, indet.
821155,occ,NA,,90227,,Mesosauridae indet.,family,37578,,Mesosauridae,NA,family,37578,Rossmann,2000,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Mesosauridae,37578,NA,NA,NA,NA,individuals,-50.650002,-25.475,"Irati Formation, PR",NA,Paran Basin of State of Paran,BR,Paran,,based on nearby landmark,seconds,local area,"This collection contains specimens from the Irati Formation (Passa Dois Group) of the Brazilian State of Paran for which no precise locality data is available. Polar coordinates are for the city of Irati in the central part of the state.\r\nRossmann (2000) lists several specimens of which he says that they come from 400 km south of Ṣo Paulo (City). Assuming that he actually meant southwest of Ṣo Paulo (otherwise the locality was at the continental slope of South America) this roughly approximates the geographic position of the town of Irati in the State of Paran. Hence, these specimens are listed here.",gp_mid,-31.52,-46.98,201,BR,,Irati,Passa Dois,,formation,,,,,,,NA,"Rossmann & Maisch (1999) and Rossmann (2000, 2002) state that the fossils come from the Irati Formation but only give ""Lower Permian"" as the most precise age specification. However, in a quite recent publication it is stated that the Irati Formation is Artinskian in age, based on absolute ages obtained from zircons from a bentonite layer (Santos et al., 2006, Gondwana Res. 9).",shale may be black and bituminous or non-bituminous and laminated,"""limestone""",,,,Y,"""shale""",,,,Y,marine indet.,cratonic basin,,macrofossils,,,,,,NA,,"body,mold/impression",good,,time-averaged,,,,,,,NA,,Specimens listed by Rossmann (2000) show white bone preservation except SMF-R-4710 in which the bone is brownish black.,taxonomic,survey of museum collection,"BSP,SMF",,,,,,"BSP = Bayerische Staatssammlung f_r Pal_ontologie und Historische Geologie, M_nchen [Bavarian State Collection of Palaeontology and Historical Geology, Munich]\r\nPIMUZ = Pal_ontologisches Institut und Museum der Universit_t Z_rich [Department and Museum of Palaeontology of Zurich University]\r\nSMF = Senckenberg Museum, Frankfurt/Main",Specimens listed by Rossmann & Maisch (1999) are taxonomically revised and may originally have been referred to different taxa (in most cases this may have been the junior synonyms of the taxa currently considered valid). ,"coastal,marine,brackish",NA,actively mobile,amphibious,NA,piscivore,dispersal=direct/internal,"addition of parts,modification of parts",hydroxyapatite,,NA,,Mesosauridae,,NA,NA,vertebrate,"T. Rossmann. 2000. Studien an Mesosauriern (Amniota inc sed: Mesosauridae): 2 Neue Erkenntnisse zur Anatomie, mit Ber_cksichtigung der Taxonomie von Mesosaurus pleurogaster (Seeley). Senckenbergiana lethaea 80(1):13-28",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,17/07/2009 13:32,17/07/2009 15:37,30263,indet.,,30341,,290.1,279.3,Artinskian,,3,BR, indet.
821158,occ,NA,,90193,,Mesosauridae indet.,family,37578,,Mesosauridae,NA,family,37578,Rossmann,2000,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Mesosauridae,37578,NA,NA,NA,NA,individuals,-47.861111,-22.977501,"Irati Formation, SP",NA,Paran Basin of eastern State of Ṣo Paulo,BR,Ṣo Paulo,,based on nearby landmark,seconds,local area,"This collection contains specimens from the Irati Formation (Passa Dois Group) of the Brazilian State of Ṣo Paulo for which no precise locality data is available. The relatively narrow outcrop belt of the Passa Dois Group is located in the eastern part of the state, about 150 km NW, W, and SW of the city of Ṣo Paulo. Polar coordinates are the same as for PBDB locality 90192 (Ribeiṛo da On̤a) which is halfway between the famous Irati localities of Itapeteninga to the south and Rio Claro to the north.",gp_mid,-26.66,-45.77,201,BR,,Irati,Passa Dois,,formation,,,,,,,NA,"Rossmann & Maisch (1999) state that the fossils come from the Irati Formation but only give ""Lower Permian"" as the most precise age specification. However, in a quite recent publication it is stated that the Irati Formation is Artinskian in age, based on absolute ages obtained from zircons from a bentonite layer (Santos et al., 2006, Gondwana Res. 9).",BSP 1982 I 27 is the only specimen preserved in black shale.,"""limestone""","white,yellow",,,Y,"""shale""",black,,,Y,marine indet.,cratonic basin,,macrofossils,,,,,,NA,,"body,mold/impression",good,,time-averaged,,,,,,,NA,,"All specimens of B. sanpauloensis listed by Rossmann & Maisch (1999) as well as all specimens listed by Rossmann (2000) show white bone preservation except of the specimen of B. sanpauloensis listed by Rossmann (2000) the bones of which show black, coaly preservation and often are weathered away.\r\nPIMUZ specimen listed by Rossmann (2002) shows brown bone preservation.",taxonomic,survey of museum collection,"BSP,SMF",,,,,,"BSP = Bayerische Staatssammlung f_r Pal_ontologie und Historische Geologie, M_nchen [Bavarian State Collection of Palaeontology and Historical Geology, Munich]\r\nIGP = Institut f_r Geologie und Pal_ontologie der Technischen Universit_t Clausthal [Department of Geology and Palaeontology of the Clausthal University of Technology]\r\nPIMUZ = Pal_ontologisches Institut und Museum der Universit_t Z_rich [Department and Museum of Palaeontology of Zurich University]\r\nSMF = Senckenberg Museum, Frankfurt/Main",Specimens listed by Rossmann & Maisch (1999) are taxonomically revised and may originally have been referred to different taxa (in most cases this may have been the junior synonyms of the taxa currently considered valid). ,"coastal,marine,brackish",NA,actively mobile,amphibious,NA,piscivore,dispersal=direct/internal,"addition of parts,modification of parts",hydroxyapatite,,NA,,Mesosauridae,,NA,NA,vertebrate,"T. Rossmann. 2000. Studien an Mesosauriern (Amniota inc sed: Mesosauridae): 2 Neue Erkenntnisse zur Anatomie, mit Ber_cksichtigung der Taxonomie von Mesosaurus pleurogaster (Seeley). Senckenbergiana lethaea 80(1):13-28",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,17/07/2009 13:42,17/07/2009 15:57,30263,indet.,,30341,,290.1,279.3,Artinskian,,10,BR, indet.
821237,occ,NA,,90226,,Mesosauridae indet.,family,37578,,Mesosauridae,NA,family,37578,Rossmann,2002,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Mesosauridae,37578,NA,NA,NA,NA,individuals,-47.650002,-22.733334,Piracicaba,NA,Pirasicaba; Paran Basin,BR,Ṣo Paulo,Piracicaba,based on nearby landmark,minutes,outcrop,"""Irati Formation von Pirasicaba, Sao Paulo, Brasilien."" (Rossmann & Maisch, 1999). Nor further details given. Note: The name ""Pirasicaba"" most likely refers to the city or municipality of Piracicaba in the State of Ṣo Paulo, which is on the outcrop of the Permian Passa Dois Group. Polar coordinates are for city of Piracicaba.",gp_mid,-26.26,-45.63,201,BR,,Irati,Passa Dois,,formation,,,,,,,NA,"Rossmann & Maisch (1999) and Rossmann (2002) state that the fossils come from the Irati Formation but only give ""Lower Permian"" as the most precise age specification. However, in a fairly recent publication it is stated that the Irati Formation is Artinskian in age, based on absolute ages obtained from zircons from a bentonite layer (Santos et al., 2006, Gondwana Res. 9).",,"""shale""",black,,,Y,"""limestone""",,,,Y,marine indet.,cratonic basin,,macrofossils,,,,,,NA,,body,good,,time-averaged,,,,,,,NA,,Specimen listed by Rossmann & Maisch (1999) is preserved in oil shale with bone preservation. Specimen listed by Rossmann (2002) is preserved in flaggy/platy limestone showing light gray bone preservation. ,taxonomic,survey of museum collection,BSP,,,,,,"BSP = Bayerische Staatssammlung f_r Pal_ontologie und Historische Geologie, M_nchen [Bavarian State Collection of Palaeontology and Historical Geology, Munich]\r\nPIMUZ = Pal_ontologisches Institut und Museum der Universit_t Z_rich [Department and Museum of Palaeontology of Zurich University] ",Specimens listed by Rossmann & Maisch (1999) are taxonomically revised and may originally have been referred to different taxa (in most cases this may have been the junior synonyms of the taxa currently considered valid).,"coastal,marine,brackish",NA,actively mobile,amphibious,NA,piscivore,dispersal=direct/internal,"addition of parts,modification of parts",hydroxyapatite,,NA,,Mesosauridae,,NA,NA,vertebrate,"T. Rossmann. 2002. Studien an Mesosauriern (Amniota inc sed, Mesosauridae): 3 Neue Aspekte zur Anatomie, Erhaltung und Pal_o̦kologie aufgrund der Exemplare im Pal_ontologischen Institut der Universit_t Z_rich. [Studies on mesosaurs (Amniota inc sed, Mesosauridae): 3 New aspects on the anatomy, preservation and palaeoecology, based on the specimens from the Palaeontological Institute of the University of Zurich]. Neues Jahrbuch f_r Geologie und Pal_ontologie, Abhandlungen 224(2):197-221",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,17/07/2009 14:42,17/07/2009 16:42,30263,indet.,,30355,,290.1,279.3,Artinskian,,1,BR, indet.
821345,occ,NA,,79927,,Mesosauridae indet.,family,37578,,Mesosauridae,NA,family,37578,Soares,2003,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Mesosauridae,37578,NA,NA,NA,NA,individuals,-54.325001,-30.341667,"Passo Ṣo Borja, tempestite bed",90191,"Passo de Ṣo Borja, Ṣo Gabriel",BR,Rio Grande do Sul,Ṣo Gabriel,based on nearby landmark,seconds,small collection,""" [...] outcrop at Passo de Ṣo Borja, in the township of Ṣo Gabriel, on the right bank of the Santa Maria River [...] "" (Soares, 2003). Polar coordinates are for town of Ṣo Gabriel.",gp_mid,-39.28,-49.75,201,BR,,Irati,Passa Dois,Assistencia,bed,,,,,,,NA,"Soares (2003) states that the fossils come from the Irati Formation but only gives ""Permian"" as the most precise age specification. However, in a quite recent publication it is stated that the Irati Formation is Artinskian in age, based on absolute ages obtained from zircons from a bentonite layer (Santos et al., 2006, Gondwana Res. 9).",""" [...] succession of shales and black siltites, both bituminous and non-bituminous. These fine grained siliciclastic facies interbed an up to 1 m thick carbonate bed. A 10-20 cm thick calcirudite layer occurs at the bottom of this bed, which grades upwards to 20 to 40 cm thick, fine grained calcarenite beds. These calcarenite beds show wave lamination and hummocky cross stratification (HCS) and would correspond to proximal tempestite deposits\r\n(Fig. 4; Della Fvera, 1987; Lavina et al., 1989, 1991).\r\nSome partially-articulated mesosaur skeletons (Class II) and many isolated bone fragments (bone-beds; Class IIIA and IIIB) occur in great concentration at the base of the calcarenite beds. Shell-beds made up by crustacean carapaces and silicified tree-trunks occur at the same level."" (Soares, 2003).\r\nNote: Three isolated bones are listed as coming from ""siltite"", whithout specification whether this refers to the carbonate bed mentioned above or to a separate siliciclastic bed (TL).",grainstone,,,,Y,,,,,,shoreface,cratonic basin,""" [...] shallowest environment (probably ranging from 10 m to 80 m) [...] "" (Soares, 2003).",macrofossils,,,,,,NA,,,,parautochthonous,,,,,,,,NA,,taphonomic class I = almost complete and fully articulated skeletons: 0%\r\ntaphonomic class II = partially articulated skeletons: 15%\r\ntaphonomic classes IIIa (complete isolated bones) and IIIb (fragments of isolated bones): 85%,taxonomic,survey of museum collection,,,,,,,"Specimens are reposited in the collections of the Universidade Federal do Rio Grande do Sul, Porto Alegre (UFRGS).","The presence of at least six individuals is assumed based on the six partially articulated skeletons listed by Soares (2003). Since no anatomic data on the isolated bones are given, no further estimation of the number of individuals present in the sample is possible.","coastal,marine,brackish",NA,actively mobile,amphibious,NA,piscivore,dispersal=direct/internal,"addition of parts,modification of parts",hydroxyapatite,,NA,,Mesosauridae,,NA,NA,vertebrate,"M. B. Soares. 2003. A taphonomic model for the Mesosauridae assemblage of the Irati Formation (Paran Basin, Brazil). Geologica Acta 1(4):349-361",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,18/07/2009 13:58,20/07/2009 08:36,30368,indet.,,30368,,290.1,279.3,Artinskian,,6,BR, indet.
821456,occ,NA,,90429,,Mesosauridae indet.,family,37578,,Mesosauridae,NA,family,37578,Soares,2003,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Mesosauridae,37578,NA,NA,NA,NA,individuals,-47.584721,-22.498611,Rio Claro municipality,NA,Paran Basin,BR,Ṣo Paulo,Rio Claro,based on nearby landmark,seconds,outcrop,""" [...] township of Rio Claro."" (Soares, 2003).\r\nPolar coordinates are the same as for PBDB collection no. 90217 (Assist̻ncia, about 7 km south of Rio Claro and 150 km NW of Ṣo Paulo City).",gp_mid,-26.05,-45.44,201,BR,,Irati,Passa Dois,Assistencia,group of beds,,,,,,,NA,"Soares (2003) states that the fossils come from the Irati Formation but only gives ""Permian"" as the most precise age specification. However, in a quite recent publication it is stated that the Irati Formation is Artinskian in age, based on absolute ages obtained from zircons from a bentonite layer (Santos et al., 2006, Gondwana Res. 9). Presence of dolomites within the succession (see lithology description) suggests that the fossils comes from the Assist̻ncia Member of the Irati Fm. (see Santos et al., 2009, J. S. Am. Earth Sci., Article in Press, doi:10.1016/j.jsames.2008.12.002).","A thick dolomite bed occurs at the base of the sequence, which consists mainly of laminated dolomitic calcilutites with undulated lamination. Interleaved with the calcilutites there are dolomitic calcarenite horizons rich in bioclasts (mesosaur bones, crustacean shells, ostracodes, foraminifera and stromatolite clasts). This carbonate facies assemblage (the so-called dolomitic bank) is overlain by dark-grey and bituminous black shales interbedded with limestones and dolomites (rhythmic zone; Fig. 5). Crustacean shell-beds also occur in this facies. According to Lavina (1991) this rhythmic facies, with recurrently associated carbonates and shales, are distal tempestites linked to deposition from turbulent currents induced by storms and deposited below the baselevel of the storm wave action. Most of the articulated mesosaur specimens (Class I) have been collected from the top of the lower dolomitic bed, close to its boundary with the overlying rhythmic facies. Semi-articulated (Class II) and disarticulated (Classes IIIA and IIIB) bone-bed materials occur both at this level and in the rhythmically stratified deposits."" (Soares, 2003).","""limestone""",dolomitic,,,Y,"""mixed carbonate-siliciclastic""",tabular,,,Y,carbonate indet.,cratonic basin,,macrofossils,,,,,,NA,,,good,,time-averaged,,,,,,,NA,,taphonomic class I = almost complete and fully articulated skeletons: 33%\r\ntaphonomic class II = partially articulated skeletons: 25%\r\ntaphonomic classes IIIa (complete isolated bones) and IIIb (fragments of isolated bones): 42%,taxonomic,survey of museum collection,,"some macrofossils,some microfossils",,,,,"UFRGS PV = vertebrate palaeontoloogy collections of the Universidade Federal do Rio Grande do Sul, Porto Alegre\r\nDGM = Diviṣo de Geologia e Mineralogia, Departamento Nacional de Prodṳ̣o Mineral\r\nPI = specimens in private collections",Soares (2003) gives no specific assignment of the mesosaurs. Since all mesosaur genera are considerd monotypic the Stereosternum specimens listed by Soares (2003) are referred to as Stereosternum tumidum and the Brazilosaurus specimens are referred to as Brazilosaurus sanpauloensis in the taxonomic list.,"coastal,marine,brackish",NA,actively mobile,amphibious,NA,piscivore,dispersal=direct/internal,"addition of parts,modification of parts",hydroxyapatite,,NA,,Mesosauridae,,NA,NA,vertebrate,"M. B. Soares. 2003. A taphonomic model for the Mesosauridae assemblage of the Irati Formation (Paran Basin, Brazil). Geologica Acta 1(4):349-361",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,20/07/2009 07:55,20/07/2009 09:55,30368,indet.,,30368,,290.1,279.3,Artinskian,,9,BR, indet.
821523,occ,NA,,90437,,Stereospondyli indet.,unranked clade,130884,,Stereospondyli,NA,unranked clade,130884,Warren et al.,2001,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,NA,NA,NA,NA,individuals,14.193889,-20.681667,Huab Basin amphibian locality,NA,"Damaraland, Karroo, Karoo",NA,Erongo,,stated in text,seconds,small collection,,gp_mid,-26.31,-48.53,701,NA,,Gai-As,"""Ecca""",,group of beds,,,,,,,NA,"""Within the uppermost Gai-As Formation, close to its transitional contact with the Doros Formation, [...] 14 m below a conspicuous fallout tuff horizon which provides our age control [...] "" (Warren et al., 2001).\r\nNote: In the stratigraphic column in fig. 3 of Warren et al. (2001) a siltstone bed in the middle part of the Gai-As Fm. is labelled with ""Stereospondylous amphibian"" which is contradictory to the statement in the above cited text.\r\n""Recent U/Pb SHRIMP dating of zircons from two of several fallout tuff beds in the Gai-As Formation 14 m above the stereospondyl find gave weighted mean values of 272+/-1.8 Ma and 265+/-2.5 Ma (Wanke, in prep.), both equivalent to late Early Permian (cf. Ross et al., 1994; Haq and Eysinga, 1998)."" (Warren et al., 2001). According to the time scales of Gradstein et al. (2004) and Ogg et al. (2008) the ages obtained from the ash beds correspond to an interval spanning the Kungurian to the lowest Capitanian. Given that the finding horizon is considerably below the dated ash bed, the collection is assigned to the Kungurian and Roadian (TL).","The Gai-As Fm. is said to generally consist of ""plane bedded, pink and maroon mudrocks"" (Warren et al., 2001).",mudstone,"tabular,brown,red",,silty,Y,,brown,,,,lacustrine indet.,,"""After Whitehill deposition the Huab Basin became more restricted with the rejuvenation of northerly trending marginal rift faults, resulting in the more closely confined lacustrine-mud deposition of the the Gai-As Formation."" (Warren et al., 2001).",macrofossils,,,,,,NA,,body,medium,,,,,,,,,NA,,"stereospondylous intercentra, in some cases preserved in articulation with their associated neural arches and ribs, in some cases part of a series of articulated vertebrae; isolated left occipital condyle including a small part of the parasphenoid; isolated fragments of tooth bearing elements",biostratigraphic,field collection,,,,,,,fossils are reposited in the collections of the Geological Survey of Namibia (GSN),,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Stereospondyli,,NA,NA,vertebrate,"A. A. Warren, B. S. Rubidge, and I. G. Stanistreet, H. Stollhofen, A. Wanke, E. M. Latimer, C. A. Marsicano, R. J. Damiani. 2001. Oldest Known Stereospondylous Amphibian from the Early Permian of Namibia. Journal of Vertebrate Paleontology 21(1):34-39",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,21/07/2009 08:06,21/07/2009 10:16,30395,indet.,,30395,,279.3,268.8,Kungurian,Roadian,1,NA, indet.
821617,occ,NA,,80689,,n. gen. Driveria n. sp. ponderosa,species,150379,,Driveria ponderosa,NA,species,150379,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Driveriidae,150378,38994,NA,NA,NA,individuals,-99.953613,33.690834,Locality KV (San Angelo Fm.),NA,MacFayden Ranch; Swanson Quarry,US,Texas,Knox,estimated from map,seconds,,"Maverick Flats 7.5' qdr; ""just to the north of the valley of the South Fork of the Wichita River""; close to the western border of Knox Co. For details see map on p. 98 in Olson (1962).",gp_mid,-28.81,3.33,101,US,,San Angelo,Pease River,,member,,,,,,,NA,"Middle and Upper San Angelo Formation sensu Olson (1962), corresponding to the upper Duncan Sandstone Member and lower Flowerpot Shale Member of the San Angelo Formation sensu Smith (1974)",for details see Olson (1962 p. 118),"""shale""",red,,sandy,Y,conglomerate,,,,Y,"""floodplain""",cratonic basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"Fossil vertebrates found [...] appear to have been laid down as partial skeletons. The nature of disarticulation and breakage suggests that they were\r\nscattered, probably by action of flesh-eaters, prior to burial. [...] the preserved animals give every evidence of having lived close to the sites of deposition.",taxonomic,field collection,FMNH,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Driveria,n. gen.,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,24/07/2009 15:07,24/07/2009 19:15,26846,ponderosa,Driveria,26846,n. sp.,279.3,268.8,Kungurian,Roadian,1,US,Driveria ponderosa
821619,occ,NA,,79600,,Tappenosaurus magnus,species,136987,,Tappenosaurus magnus,NA,species,136987,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Tappenosauridae,136988,136986,NA,NA,NA,individuals,-99.938332,33.66,Locality KAC (Lower Flowerpot Shale),NA,"Kahn Quarry, Driver Ranch",US,Texas,Knox,estimated from map,seconds,small collection,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork."" For details see map on p. 98 in Olson (1962).",gp_mid,-28.81,3.3,101,US,,San Angelo,Pease River,Flowerpot Shale,member,,,,,,,NA,"The upper San Angelo Fm. of Olson (1962) is widely identical to the lower part of the Flowerpot Shale Member of the upper San Angelo Fm. (sensu Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 114 ff.),claystone,"gypsiferous,green,red or brown",,,Y,sandstone,red or brown,,conglomeratic,Y,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,E. C. Olson,1958,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tappenosaurus,,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,26/07/2009 06:56,26/07/2009 09:05,26846,magnus,Tappenosaurus,26846,,279.3,268.8,Kungurian,Roadian,1,US,Tappenosaurus magnus
821620,occ,NA,,79600,,Eosyodon ? hudsoni,species,150424,,Eosyodon hudsoni,NA,species,150424,Olson,1962,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Brithopodidae,38951,38961,NA,NA,NA,individuals,-99.938332,33.66,Locality KAC (Lower Flowerpot Shale),NA,"Kahn Quarry, Driver Ranch",US,Texas,Knox,estimated from map,seconds,small collection,"""about twelve miles north of Little Croton Creek, south of the South Fork of the Wichita River, sometimes called South Wichita River. It lies largely on a divide between two northerly flowing tributaries of the South Fork."" For details see map on p. 98 in Olson (1962).",gp_mid,-28.81,3.3,101,US,,San Angelo,Pease River,Flowerpot Shale,member,,,,,,,NA,"The upper San Angelo Fm. of Olson (1962) is widely identical to the lower part of the Flowerpot Shale Member of the upper San Angelo Fm. (sensu Smith, 1974, University of Texas Bureau of Economic Geology, Report of Investigations No. 80)",for details see Olson (1962 p. 114 ff.),claystone,"gypsiferous,green,red or brown",,,Y,sandstone,red or brown,,conglomeratic,Y,fluvial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,E. C. Olson,1958,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Eosyodon,?,NA,NA,vertebrate,"E. C. Olson. 1962. Late Permian terrestrial vertebrates, U.S.A. and U.S.S.R. Transactions of the American Philosophical Society, New Series 52(2):1-224",315,334,0,J. Mueller,T. Liebrecht,,26/07/2009 07:03,26/07/2009 09:03,26846,hudsoni,Eosyodon,26846,,279.3,268.8,Kungurian,Roadian,1,US,Eosyodon hudsoni
821622,occ,NA,R,90452,,Reptilia indet.,class,36322,,Reptilia,NA,class,36322,Olson and Bolles,1975,Chordata,33815,Reptilia,36322,,NA,,NA,NA,NA,NA,NA,individuals,-99.474998,33.783611,Vale site 1919,NA,,US,Texas,Baylor/Foard,based on nearby landmark,seconds,small collection,"Road cut ""on Texas Farm Road 1919 near the boundary between Baylor and Foard Counties."" (Olson & Bolles, 1975). Unfortunately, it is not stated on which side of the border the locality actually is situated. Polar coordinates are for intersection of Texas Ranch Road 1919 with Baylor/Foard County line.",gp_mid,-29.1,1.9,101,US,,Vale,Clear Fork,,group of beds,,,,,,,NA,"The base and top of the Clear Fork Group are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top.","No detailed description of the rocks is given in Olson & Bolles (1975), however, an X-ray diffractogramm (fig. 5) shows quartz as the main component of the matrix, followed by feldspar and dolomite.","""siliciclastic""","dolomitic,red",,argillaceous,Y,,,,,,lacustrine - small,foreland basin,,macrofossils,,,,,,NA,,body,,autochthonous,time-averaged,,,,,,,NA,,,taxonomic,"bulk,mechanical,acetic,field collection,survey of museum collection",FMNH,ichnofossils,,,E. C. Olson,"1972, 1973","Site actually is a trace fossil locality where some scattered remains of vertebrates have been found.\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Reptilia,,NA,NA,vertebrate,E. C. Olson and K. Bolles. 1975. Permo-Carboniferous Fresh Water Burrows. Fieldiana: Geology 33(15):271-290,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,26/07/2009 16:13,26/07/2009 18:54,30420,indet.,,30420,,279.3,272.3,Kungurian,,1,US, indet.
821622,occ,21910,,90452,,Peronedon ? sp.,genus,119361,subjective synonym of,Diplocaulus,NA,genus,37264,Haglund,1977,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,individuals,-99.474998,33.783611,Vale site 1919,NA,,US,Texas,Baylor/Foard,based on nearby landmark,seconds,small collection,"Road cut ""on Texas Farm Road 1919 near the boundary between Baylor and Foard Counties."" (Olson & Bolles, 1975). Unfortunately, it is not stated on which side of the border the locality actually is situated. Polar coordinates are for intersection of Texas Ranch Road 1919 with Baylor/Foard County line.",gp_mid,-29.1,1.9,101,US,,Vale,Clear Fork,,group of beds,,,,,,,NA,"The base and top of the Clear Fork Group are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top.","No detailed description of the rocks is given in Olson & Bolles (1975), however, an X-ray diffractogramm (fig. 5) shows quartz as the main component of the matrix, followed by feldspar and dolomite.","""siliciclastic""","dolomitic,red",,argillaceous,Y,,,,,,lacustrine - small,foreland basin,,macrofossils,,,,,,NA,,body,,autochthonous,time-averaged,,,,,,,NA,,,taxonomic,"bulk,mechanical,acetic,field collection,survey of museum collection",FMNH,ichnofossils,,,E. C. Olson,"1972, 1973","Site actually is a trace fossil locality where some scattered remains of vertebrates have been found.\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Peronedon,?,NA,NA,vertebrate,T. R. Haglund. 1977. New Occurences and Paleoecology of Peronedon primus Olson (Nectridea). Journal of Paleontology 51(5):982-985,315,334,0,J. Mueller,T. Liebrecht,,26/07/2009 16:58,26/07/2009 18:58,30420,sp.,Diplocaulus,30419,,279.3,272.3,Kungurian,,1,US,Diplocaulus sp.
821623,occ,NA,,90452,,Lysorophus sp.,genus,37322,,Lysorophus,NA,genus,37322,Olson and Bolles,1975,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-99.474998,33.783611,Vale site 1919,NA,,US,Texas,Baylor/Foard,based on nearby landmark,seconds,small collection,"Road cut ""on Texas Farm Road 1919 near the boundary between Baylor and Foard Counties."" (Olson & Bolles, 1975). Unfortunately, it is not stated on which side of the border the locality actually is situated. Polar coordinates are for intersection of Texas Ranch Road 1919 with Baylor/Foard County line.",gp_mid,-29.1,1.9,101,US,,Vale,Clear Fork,,group of beds,,,,,,,NA,"The base and top of the Clear Fork Group are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top.","No detailed description of the rocks is given in Olson & Bolles (1975), however, an X-ray diffractogramm (fig. 5) shows quartz as the main component of the matrix, followed by feldspar and dolomite.","""siliciclastic""","dolomitic,red",,argillaceous,Y,,,,,,lacustrine - small,foreland basin,,macrofossils,,,,,,NA,,body,,autochthonous,time-averaged,,,,,,,NA,,,taxonomic,"bulk,mechanical,acetic,field collection,survey of museum collection",FMNH,ichnofossils,,,E. C. Olson,"1972, 1973","Site actually is a trace fossil locality where some scattered remains of vertebrates have been found.\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,E. C. Olson and K. Bolles. 1975. Permo-Carboniferous Fresh Water Burrows. Fieldiana: Geology 33(15):271-290,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,26/07/2009 16:13,26/07/2009 18:25,30420,sp.,Lysorophus,30420,,279.3,272.3,Kungurian,,NA,US,Lysorophus sp.
821624,occ,NA,R,90452,,aff. Peronedon sp.,genus,119361,subjective synonym of,Diplocaulus,NA,genus,37264,Olson and Bolles,1975,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,individuals,-99.474998,33.783611,Vale site 1919,NA,,US,Texas,Baylor/Foard,based on nearby landmark,seconds,small collection,"Road cut ""on Texas Farm Road 1919 near the boundary between Baylor and Foard Counties."" (Olson & Bolles, 1975). Unfortunately, it is not stated on which side of the border the locality actually is situated. Polar coordinates are for intersection of Texas Ranch Road 1919 with Baylor/Foard County line.",gp_mid,-29.1,1.9,101,US,,Vale,Clear Fork,,group of beds,,,,,,,NA,"The base and top of the Clear Fork Group are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top.","No detailed description of the rocks is given in Olson & Bolles (1975), however, an X-ray diffractogramm (fig. 5) shows quartz as the main component of the matrix, followed by feldspar and dolomite.","""siliciclastic""","dolomitic,red",,argillaceous,Y,,,,,,lacustrine - small,foreland basin,,macrofossils,,,,,,NA,,body,,autochthonous,time-averaged,,,,,,,NA,,,taxonomic,"bulk,mechanical,acetic,field collection,survey of museum collection",FMNH,ichnofossils,,,E. C. Olson,"1972, 1973","Site actually is a trace fossil locality where some scattered remains of vertebrates have been found.\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Peronedon,aff.,NA,NA,vertebrate,E. C. Olson and K. Bolles. 1975. Permo-Carboniferous Fresh Water Burrows. Fieldiana: Geology 33(15):271-290,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,26/07/2009 16:13,26/07/2009 18:54,30420,sp.,Diplocaulus,30420,,279.3,272.3,Kungurian,,1,US,Diplocaulus sp.
821624,occ,21911,,90452,,Peronedon primus,species,119362,recombined as,Diplocaulus primus,NA,species,119362,Haglund,1977,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,individuals,-99.474998,33.783611,Vale site 1919,NA,,US,Texas,Baylor/Foard,based on nearby landmark,seconds,small collection,"Road cut ""on Texas Farm Road 1919 near the boundary between Baylor and Foard Counties."" (Olson & Bolles, 1975). Unfortunately, it is not stated on which side of the border the locality actually is situated. Polar coordinates are for intersection of Texas Ranch Road 1919 with Baylor/Foard County line.",gp_mid,-29.1,1.9,101,US,,Vale,Clear Fork,,group of beds,,,,,,,NA,"The base and top of the Clear Fork Group are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top.","No detailed description of the rocks is given in Olson & Bolles (1975), however, an X-ray diffractogramm (fig. 5) shows quartz as the main component of the matrix, followed by feldspar and dolomite.","""siliciclastic""","dolomitic,red",,argillaceous,Y,,,,,,lacustrine - small,foreland basin,,macrofossils,,,,,,NA,,body,,autochthonous,time-averaged,,,,,,,NA,,,taxonomic,"bulk,mechanical,acetic,field collection,survey of museum collection",FMNH,ichnofossils,,,E. C. Olson,"1972, 1973","Site actually is a trace fossil locality where some scattered remains of vertebrates have been found.\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Peronedon,,NA,NA,vertebrate,T. R. Haglund. 1977. New Occurences and Paleoecology of Peronedon primus Olson (Nectridea). Journal of Paleontology 51(5):982-985,315,334,0,J. Mueller,T. Liebrecht,,26/07/2009 16:58,26/07/2009 18:58,30420,primus,Diplocaulus,30419,,279.3,272.3,Kungurian,,1,US,Diplocaulus primus
821690,occ,NA,,28256,,n. gen. Pelodosotis n. sp. elongatum,species,150625,,Pelodosotis elongatum,NA,species,150625,Carroll and Gaskill,1978,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Ostodolepidae,37301,37304,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Pelodosotis,n. gen.,NA,NA,vertebrate,R. L. Carroll and P. Gaskill. 1978. The Order Microsauria. Memoirs of the American Philosophical Society 126:1-211,315,334,0,J. Mueller,T. Liebrecht,,29/07/2009 08:10,29/07/2009 10:10,17702,elongatum,Pelodosotis,28692,n. sp.,279.3,272.3,Kungurian,,1,US,Pelodosotis elongatum
821691,occ,NA,,28256,,Micraroter ? erythrogeios,species,90684,,Micraroter erythrogeios,NA,species,90684,Carroll and Gaskill,1978,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Ostodolepidae,37301,37302,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Micraroter,?,NA,NA,vertebrate,R. L. Carroll and P. Gaskill. 1978. The Order Microsauria. Memoirs of the American Philosophical Society 126:1-211,315,334,0,J. Mueller,T. Liebrecht,,29/07/2009 08:14,29/07/2009 10:14,17702,erythrogeios,Micraroter,28692,,279.3,272.3,Kungurian,,1,US,Micraroter erythrogeios
821692,occ,NA,,67862,,n. gen. Nannaroter n. sp. mckinziei,species,150627,,Nannaroter mckinziei,NA,species,150627,Anderson et al.,2009,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Ostodolepidae,37301,150626,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Nannaroter,n. gen.,NA,NA,"paleoentomology,vertebrate","J. S. Anderson, D. Scott, and R. R. Reisz. 2009. Nannaroter mckinziei, a New Ostodolepid Microsaur۪ (Tetrapoda, Lepospondyli, Recumbirostra) from the Early Permian of Richards Spur (Ft. Sill), Oklahoma. Journal of Vertebrate Paleontology 29(2):379-388",315,334,0,J. Mueller,T. Liebrecht,,29/07/2009 09:27,29/07/2009 11:27,19393,mckinziei,Nannaroter,30433,n. sp.,290.1,268,Leonard,,1,US,Nannaroter mckinziei
824206,occ,NA,,90832,,Mesosauridae indet.,family,37578,,Mesosauridae,NA,family,37578,Beder,1923,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Mesosauridae,37578,NA,NA,NA,NA,,-56.450001,-25.783333,Villarrica,NA,"Villa Rica; Espinillo; Yhovy, Jhovy; Paran Basin",PY,Guair,,based on nearby landmark,minutes,local area,"Beder (1923) reports reptile remains from three different quarries in the immediate vicinity of the town of Villarrica (owned by the se̱ors Gervasio Barretto, Honorio Gonzlez, and Andr̩s Battochi, respectively) the exact locality of each being only vaguely described. Furthermore, Beder is convinced that the fossil figured by Frech (1901, Lethaea geognostica part I: Lethaea palaeozoica, vol. 2, issue 3) comes from one of these localities. Later, Filippi Ambile (2001, Bol. Mus. Nac. Hist. Nat. Paraguay 13) reports further findings from two of Beder's localities. Frech's (1901) most precise locality description is restricted to the statement that the fossil comes from ""Villa Rica"" but the DMS coordinates given by him (2550'S, 5640'W) do not really coincide with the position of that town (cf. coordinates entered).",gp_mid,-38.41,-44.86,201,PY,,? San Miguel,Independencia,,group of beds,,,,,,,NA,"The beds in question were not mentioned under a formational name by Beder (1923) but were correlated with the ""Rio Rasto"" and ""Estrada Nova"" beds of the Passa Dois Group of Brazil. Bez Presser et al. (2004, Bol. Mus. Nac. Hist. Nat. Paraguay 15) apply the modern stratigraphic nomenclature and suspect that all(?) mesosaur remains from the Paran Basin of Paraguay are from the San Miguel Formation, the lower of the two formations of the Independencia Group. Rapalini et al. (2006, Earth Planets Space 58), based on magnetostratigraphy, ascertain a late Middle Permian/early Late Permian age for the Tacuary Fm. which overlies the San Miguel Fm. Given that the Tacuary Fm. comprises the most part of the Independencia Group (see fig. 2 in F̼lfaro et al., 1997, Int. Geol. Rev. 39(8)) and that mesosaur remains in the San Miguel Fm. strongly argue for a Lower Permian age (for details see comments on stratigraphy in other PBDB collections containing mesosaurids), the present collection is tentatively assigned to the Artinskian.",,sandstone,"ooidal,red,white,yellow",,cherty/siliceous,Y,claystone,"black,red,blue",,,,marine indet.,cratonic basin,There is no consensus about the true nature (lacustrine/brackish/fully marine) of the water body in which the mesosaurs lived. The environment is tentatively chosen to have been marine. The deposits appear to represent a nearshore equivalent of the lime/dolo mudstones and shales of the Irati Formation of Brazil.,macrofossils,,,,,,NA,,mold/impression,variable,,,,,,,,,NA,,"Specimens are preserved as impressions in the sandstone. Material mostly consists of ribs and vertebrae but also isolated teeth are present (Beder, 1923; Filippi Ambile, 2001).",taxonomic,"selective quarrying,surface (float),field collection,observed (not collected)",,,,,"R. Beder, V.O. Filippi Ambile, among others",,"The specimen figured by Frech (1901, Lethaea geognostica part I: Lethaea palaeozoica, vol. 2, issue 3) must have been collected on the threshold of the 20th century and was then reposited in the ""Hamburger Museum"" (and still is?). The specimens reported by Beder (1923) were collected in the early 20s of the 20th century and were then stored in the Bureau of Mines and Energy in Buenos Aires but now are unlocatable (Filippi Ambile, 2001, Bol. Mus. Nac. Hist. Nat. Paraguay 13). Beder did not find complete individuals but was told that quarry workers did so who did not keep them because they did not know about their scientific value. The newest findings were made by Filippi Ambile on the threshold of the 21st century and these specimens are reposited in the National Museum of Natural History of Paraguay (Filippi Ambile, 2001).",,"coastal,marine,brackish",NA,actively mobile,amphibious,NA,piscivore,dispersal=direct/internal,"addition of parts,modification of parts",hydroxyapatite,,NA,,Mesosauridae,,NA,NA,vertebrate,R. Beder. 1923. Sobre un Hallazgo de F_siles P̩rmicos en Villarrica (Rep̼blica del Paraguay). Bolet_n da la Academia Nacional de Ciencias en C_rdoba (Rep̼blica Argentina) 27(1/2):9-12,315,334,0,J. Mueller,T. Liebrecht,,18/08/2009 18:45,18/08/2009 20:45,30556,indet.,,30556,,290.1,279.3,Artinskian,,NA,PY, indet.
824848,occ,NA,,67945,,Diplocaulus cf. magnicornis,species,81712,,Diplocaulus magnicornis,NA,species,81712,Daly,1973,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,specimens,-98.787781,34.18972,South Grandfield,NA,,US,Oklahoma,Tillman,stated in text,seconds,small collection,"""SW1/4 SE1/4 SE1/4 sec. 20, T. 4 S, R. 15 W. This is 6 1/2 miles southwest of Grandfield... 3 miles north of the Red River...""\neast side of ""a depression about fifty feet deep... near the top... [fossils] from the surface of a nose or ridge... three to four feet high and ten to twenty-five fee in area.""",gp_mid,-28.41,1.95,101,US,,Hennessey,,,bed,,,,,,,NA,"""lower third"" of a 9 foot bed\n""when the known lower boundary of the Arroyo [Formation] is extrapolated northward... it passes through the South Grandfield site.""\nthe Arroyo is within the Clear Fork Group, all of which is Kungurian (see discussion of Romer 1928 collections)","""Red shale spotted with pale green, containing lenses of fissile red sandstone and of stratified dark red fine conglomerate.""","""shale""","green,red",,,,sandstone,"""cross stratification"",red",poorly lithified,,,fluvial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""remains were assembled by moving water, after transport for a long or short distance... It is usual for the skull specimens... to have the mandibles in place... This suggests that the predators and scavengers... may have customarily discarded the heads... cranial remains have been selectively preserved...""\ncounts are given of 281 skulls and skull parts; 346 vertebrae, strings of vertebrae, and pieces of vertebrae; 109 limb bones and pieces of limb bones; and 29 partial girdles",general faunal/floral,"surface (float),field collection,survey of museum collection",FMNH,,,,,,"""Bone and bone-containing nodules may be collected from the surface... An effort to excavate for fossils was not productive... about forty pounds of red shale... was washed [and] five scraps of bone were recovered, none identifiable.""\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",not the same as the two West Grandfield sites of Olson 1967,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,E. Daly. 1973. A Lower Permian vertebrate fauna from southern Oklahoma. Journal of Paleontology 47(3):562-589,315,334,0,J. Mueller,T. Liebrecht,,20/08/2009 18:31,20/08/2009 20:31,19411,magnicornis,Diplocaulus,19411,cf.,279.3,272.3,Kungurian,,1,US,Diplocaulus magnicornis
825243,occ,NA,,67862,,n. gen. Pasawioops n. sp. mayi,species,152839,,Pasawioops mayi,NA,species,152839,Fr̦bisch and Reisz,2008,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,152838,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Pasawioops,n. gen.,NA,NA,"paleoentomology,vertebrate","N. B. Fr̦bisch and R. R. Reisz. 2008. A New Lower Permian Amphibamid (Dissorophoidea, Temnospondyli) from the Fissure Fill Deposits near Richards Spur, Oklahoma. Journal of Vertebrate Paleontology 28(4):1015-1030",315,334,0,J. Mueller,T. Liebrecht,,25/08/2009 07:53,25/08/2009 09:53,19393,mayi,Pasawioops,30585,n. sp.,290.1,268,Leonard,,2,US,Pasawioops mayi
825244,occ,NA,,67945,,Cardiocephalus sp.,genus,37294,,Cardiocephalus,NA,genus,37294,Daly,1973,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37294,NA,NA,NA,elements,-98.787781,34.18972,South Grandfield,NA,,US,Oklahoma,Tillman,stated in text,seconds,small collection,"""SW1/4 SE1/4 SE1/4 sec. 20, T. 4 S, R. 15 W. This is 6 1/2 miles southwest of Grandfield... 3 miles north of the Red River...""\neast side of ""a depression about fifty feet deep... near the top... [fossils] from the surface of a nose or ridge... three to four feet high and ten to twenty-five fee in area.""",gp_mid,-28.41,1.95,101,US,,Hennessey,,,bed,,,,,,,NA,"""lower third"" of a 9 foot bed\n""when the known lower boundary of the Arroyo [Formation] is extrapolated northward... it passes through the South Grandfield site.""\nthe Arroyo is within the Clear Fork Group, all of which is Kungurian (see discussion of Romer 1928 collections)","""Red shale spotted with pale green, containing lenses of fissile red sandstone and of stratified dark red fine conglomerate.""","""shale""","green,red",,,,sandstone,"""cross stratification"",red",poorly lithified,,,fluvial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""remains were assembled by moving water, after transport for a long or short distance... It is usual for the skull specimens... to have the mandibles in place... This suggests that the predators and scavengers... may have customarily discarded the heads... cranial remains have been selectively preserved...""\ncounts are given of 281 skulls and skull parts; 346 vertebrae, strings of vertebrae, and pieces of vertebrae; 109 limb bones and pieces of limb bones; and 29 partial girdles",general faunal/floral,"surface (float),field collection,survey of museum collection",FMNH,,,,,,"""Bone and bone-containing nodules may be collected from the surface... An effort to excavate for fossils was not productive... about forty pounds of red shale... was washed [and] five scraps of bone were recovered, none identifiable.""\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",not the same as the two West Grandfield sites of Olson 1967,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Cardiocephalus,,NA,NA,vertebrate,E. Daly. 1973. A Lower Permian vertebrate fauna from southern Oklahoma. Journal of Paleontology 47(3):562-589,315,334,0,J. Mueller,T. Liebrecht,,25/08/2009 09:01,25/08/2009 11:01,19411,sp.,Cardiocephalus,19411,,279.3,272.3,Kungurian,,60,US,Cardiocephalus sp.
825283,occ,NA,,80112,,n. gen. Tambachia n. sp. trogallas,species,152960,,Tambachia trogallas,NA,species,152960,Sumida et al.,1998,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,152959,NA,NA,NA,individuals,10.618889,50.809723,Bromacker Quarry (upper level of Tambach sandstone),NA,,DE,Thuringia,Gotha,based on nearby landmark,seconds,outcrop,"""...middle part of the Thuringian Forest near the village of Tambach-Dietharz and about 20 km south of the town of Gotha, central Germany.""",gp_mid,21.71,7.41,305,DE,,Tambach,Rotliegend,Tambach-Sandstein,group of beds,,,,,,,NA,"""At the Bromacker quarry site are two superimposed stratigraphic successions that can be characterized by their facies associations and are referred to as the Lower Beds and Upper Beds (Eberth et al. 2000). All the vertebrates from the Bromacker quarry come from the Upper Beds [...]. The vertebrates are almost exclusively restricted to two [... horizons ...] which are separated by 50 cm in a stratigraphic interval of 1.2 m."" (Berman et al., 2001)\r\nThe Tambach Formation is of Artinskian age according to ""Stratigraphische Tabelle von Deutschland 2002"", however, a Kungurian age is proposed by L_tzner (2006) in LITHOLEX stratigraphic online database [http://www.bgr.de/app/LithoLex/gesamt_ausgabe_neu.php5?id=25]","""massive, red-brown, very fine-grained sandstone and siltstone"" (Berman et al., 2001).\r\nFor further details see Eberth et al. (2000).",sandstone,"very fine,brown,red",lithified,,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,"""alluvial paleochannel and sheetflood facies and lacustrine suspension deposits"" (Berman et al., 2001).\r\n""During the time that the Lower and Upper beds were deposited, the Tambach Basin was internally-drained and probably characterized by a wet-and-dry tropical or wetter climate that was hot year-round with seasonal-to-subseasonal cycles of rainfall and drying. [...] In the Bromacker area, the floodbasin was never deeply desiccated or heavily vegetated between flooding events."" Eberth et al. (2000).",macrofossils,,,,,,NA,,"body,permineralized",excellent,,snapshot,,,,,,,NA,,,taxonomic,"bulk,field collection",,all macrofossils,,,,,"MNG = Museum der Natur, Gotha",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Tambachia,n. gen.,NA,NA,vertebrate,"S. S. Sumida, D. S. Berman, and T. Martens. 1998. A New Trematopid Amphibian from the Lower Permian of Central Germany. Palaeontology 41(4):605-629",315,334,0,J. Mueller,T. Liebrecht,,26/08/2009 10:13,26/08/2009 12:13,26922,trogallas,Tambachia,30596,n. sp.,290.1,279.3,Artinskian,,1,DE,Tambachia trogallas
825943,occ,NA,,91038,,n. gen. Gerobatrachus n. sp. hottoni,species,153288,,Gerobatrachus hottoni,NA,species,153288,Anderson et al.,2008,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,153287,NA,NA,NA,individuals,-99.40667,33.736942,USNM Locality 40971,NA,Don's Dump Fish Quarry,US,Texas,Baylor,estimated from map,seconds,hand sample,"""Locality number USNM 40971, 'Don's Dump Fish Quarry', Clear Fork Group. Baylor County, Texas, USGS Soap Creek 7.5' quad. More specific locality information is on file at the USNM."" (Anderson et al., 2008).\r\nNote: This locality is not the same as the ""Fish Quarry"" (Knox Co.) in PBDB coll. no. 27704. Polar coordinates are the same as for PBDB coll. 85556 (Crooked Creek).",gp_mid,-29.08,1.83,101,US,,Arroyo or Vale,Clear Fork,,bed,,,,,,,NA,No further stratigraphic informations given by Anderson et al. (2008). The geographic data suggest that the locality is either in the upper part of the Arroyo Formation or in the lower part of the Vale Formation.\r\n,"""[...] two foot thick lens of fine-grained red siltstone [...]"" (Anderson et al., 2008).",siltstone,"fine,red",,,Y,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,"""[...] preserved fully articulated in ventral view, and is missing only the stylopods, zeugopods, and ventral portions of the skull and pectoral girdle."" (Anderson et al., 2008).",taxonomic,survey of museum collection,USNM,,,,P. Kroehler,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Gerobatrachus,n. gen.,NA,NA,vertebrate,"J. S. Anderson, R. R. Reisz, and D. Scott, N. B. Fr̦bisch, S. S. Sumida. 2008. A stem batrachian from the Early Permian of Texas and the origin of frogs and salamanders. Nature 453:515-518",315,334,0,J. Mueller,T. Liebrecht,,01/09/2009 12:44,01/09/2009 14:44,30637,hottoni,Gerobatrachus,30637,n. sp.,279.3,272.3,Kungurian,,1,US,Gerobatrachus hottoni
828777,occ,NA,,80112,,n. gen. Orobates n. sp. pabsti,species,154063,,Orobates pabsti,NA,species,154063,Berman et al.,2004,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,154059,NA,NA,NA,individuals,10.618889,50.809723,Bromacker Quarry (upper level of Tambach sandstone),NA,,DE,Thuringia,Gotha,based on nearby landmark,seconds,outcrop,"""...middle part of the Thuringian Forest near the village of Tambach-Dietharz and about 20 km south of the town of Gotha, central Germany.""",gp_mid,21.71,7.41,305,DE,,Tambach,Rotliegend,Tambach-Sandstein,group of beds,,,,,,,NA,"""At the Bromacker quarry site are two superimposed stratigraphic successions that can be characterized by their facies associations and are referred to as the Lower Beds and Upper Beds (Eberth et al. 2000). All the vertebrates from the Bromacker quarry come from the Upper Beds [...]. The vertebrates are almost exclusively restricted to two [... horizons ...] which are separated by 50 cm in a stratigraphic interval of 1.2 m."" (Berman et al., 2001)\r\nThe Tambach Formation is of Artinskian age according to ""Stratigraphische Tabelle von Deutschland 2002"", however, a Kungurian age is proposed by L_tzner (2006) in LITHOLEX stratigraphic online database [http://www.bgr.de/app/LithoLex/gesamt_ausgabe_neu.php5?id=25]","""massive, red-brown, very fine-grained sandstone and siltstone"" (Berman et al., 2001).\r\nFor further details see Eberth et al. (2000).",sandstone,"very fine,brown,red",lithified,,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,"""alluvial paleochannel and sheetflood facies and lacustrine suspension deposits"" (Berman et al., 2001).\r\n""During the time that the Lower and Upper beds were deposited, the Tambach Basin was internally-drained and probably characterized by a wet-and-dry tropical or wetter climate that was hot year-round with seasonal-to-subseasonal cycles of rainfall and drying. [...] In the Bromacker area, the floodbasin was never deeply desiccated or heavily vegetated between flooding events."" Eberth et al. (2000).",macrofossils,,,,,,NA,,"body,permineralized",excellent,,snapshot,,,,,,,NA,,,taxonomic,"bulk,field collection",,all macrofossils,,,,,"MNG = Museum der Natur, Gotha",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Orobates,n. gen.,NA,NA,vertebrate,"D. S. Berman, A. C. Henrici, and R. A. Kissel, S. S. Sumida, T. Martens. 2004. A New Diadectid (Diadectomorpha), Orobates pabsti, from the Early Permian of Central Germany. Bulletin of Carnegie Museum of Natural History 35(1):1-36",315,334,0,J. Mueller,T. Liebrecht,,16/09/2009 10:33,16/09/2009 12:33,26922,pabsti,Orobates,30738,n. sp.,290.1,279.3,Artinskian,,4,DE,Orobates pabsti
832387,occ,NA,,85292,,n. gen. Phlegethontia n. sp. linearis,species,156820,,Phlegethontia linearis,NA,species,156820,Anderson,2002,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,37259,NA,NA,NA,individuals,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Phlegethontia,n. gen.,NA,NA,vertebrate,J. S. Anderson. 2002. Revision of the Astopod Genus Phlegethontia (Tetrapoda: Lepospondyli). Journal of Paleontology 76(6):1029-1046,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,03/11/2009 08:09,03/11/2009 11:00,28831,linearis,Phlegethontia,31059,n. sp.,311.45,306.95,Westphalian D,,1,US,Phlegethontia linearis
832388,occ,NA,,85292,,Phlegethontia n. sp. serpens,species,156821,subjective synonym of,Phlegethontia longissima,NA,species,156844,Anderson,2002,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,37259,NA,NA,NA,individuals,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Phlegethontia,,NA,NA,vertebrate,J. S. Anderson. 2002. Revision of the Astopod Genus Phlegethontia (Tetrapoda: Lepospondyli). Journal of Paleontology 76(6):1029-1046,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,03/11/2009 08:09,03/11/2009 10:23,28831,serpens,Phlegethontia,31059,n. sp.,311.45,306.95,Westphalian D,,1,US,Phlegethontia serpens
832390,occ,NA,,85292,,Phlegethontia longissima,species,156845,,Phlegethontia longissima,NA,species,156844,Anderson,2002,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,37259,NA,NA,NA,specimens,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Phlegethontia,,NA,NA,vertebrate,J. S. Anderson. 2002. Revision of the Astopod Genus Phlegethontia (Tetrapoda: Lepospondyli). Journal of Paleontology 76(6):1029-1046,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,03/11/2009 08:09,03/11/2009 10:26,28831,longissima,Phlegethontia,31059,,311.45,306.95,Westphalian D,,19,US,Phlegethontia longissima
832401,occ,NA,,84835,,Dolichosoma n. sp. longissimum,species,156844,recombined as,Phlegethontia longissima,NA,species,156844,McGinnis,1967,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,37259,NA,NA,NA,individuals,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Dolichosoma,,NA,NA,vertebrate,"H. J. McGinnis. 1967. The Osteology of Phlegethontia, a Carboniferous and Permian Astopod Amphibian. University of California Publications in Geological Sciences 71:1-46",315,334,0,J. Mueller,T. Liebrecht,,03/11/2009 18:09,03/11/2009 20:09,28608,longissimum,Phlegethontia,31050,n. sp.,311.45,306.95,Westphalian D,,1,CZ,Phlegethontia longissimum
832402,occ,NA,,84835,,Phlegethontia longissima,species,156845,,Phlegethontia longissima,NA,species,156844,Anderson,2002,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,37259,NA,NA,NA,individuals,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Phlegethontia,,NA,NA,vertebrate,J. S. Anderson. 2002. Revision of the Astopod Genus Phlegethontia (Tetrapoda: Lepospondyli). Journal of Paleontology 76(6):1029-1046,315,334,0,J. Mueller,T. Liebrecht,,03/11/2009 18:42,03/11/2009 20:42,28608,longissima,Phlegethontia,31059,,311.45,306.95,Westphalian D,,1,CZ,Phlegethontia longissima
832560,occ,NA,,92271,,Ophiderpeton n. sp. swisshelmense,species,156888,,Ophiderpeton swisshelmense,NA,species,156888,Thayer,1985,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Ophiderpetontidae,37252,37254,NA,NA,NA,elements,-109.566666,31.733334,Swisshelm Mts. amphibian site,NA,UALP 7205,US,Arizona,Cochise,estimated from map,minutes,small collection,"""The Swisshelm Mountain Site [...] is located at an elevation of 1,585 meters on a southwest-facing ridge of the northern Swisshelm Mountains, Cochise County, Arizona."" (Thayer, 1985).",gp_mid,-47.77,-7.44,101,US,,Black Prince Limestone,,,bed,,,,,,,NA,"""The amphibian bed [is] located one meter below the top of the Black Prince [Limestone] [...] The Swisshelm Mountain amphibian bed is dated near the Morrowan-Derryan(= Atokan) boundary, equivalent to the boundary of Westphalian A and B of Europe"" (Thayer, 1985).","""light yellow-gray, silty intrabiomicrudit""","""limestone""","intraclastic,shelly/skeletal,gray,yellow",,silty,Y,,,,,,shallow subtidal indet.,,"""The interpretation best fitting the evidence is a partially protected estuarine environment (for the algal oncolites and marine fauna), close to the outlet of a sluggish coastal river (for transporting the terrestrial and freshwater faunal elements)."" (Thayer, 1985).","macrofossils,microfossils",,,,,,NA,,body,variable,allochthonous,time-averaged,,,,,,,NA,,"Some bones show traces of wear through transport, others are completely unworn but may have been transported as a whole carcass into the environment before burial and disarticulation by burrowing organisms. (Thayer, 1985).",taxonomic,"bulk,acetic",,"some macrofossils,difficult macrofossils",,,,,"""Disarticulated faunal elements were obtained by digesting blocks of limestone and silty limestone in a 15 percent solution of acetic acid. The insoluble residue was washed through a 28-mesh screen to remove fine material."" (thayer, 1985).\r\nUALP = University of Arizona Laboratory of Paleontology",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Ophiderpeton,,NA,NA,"micropaleontology,vertebrate","D. W. Thayer. 1985. New Pennsylvanian Lepospondyl Amphibians from the Swisshelm Mountains, Arizona. Journal of Paleontology 59(3):684-700",315,334,0,J. Mueller,T. Liebrecht,,04/11/2009 10:49,04/11/2009 12:49,31089,swisshelmense,Ophiderpeton,31089,n. sp.,318.1,314.6,Westphalian A,Westphalian B,15,US,Ophiderpeton swisshelmense
832561,occ,NA,,92271,,Phlegethontia n. sp. phanerhapha,species,156889,nomen dubium,Phlegethontia,NA,genus,37259,Thayer,1985,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,37259,NA,NA,NA,specimens,-109.566666,31.733334,Swisshelm Mts. amphibian site,NA,UALP 7205,US,Arizona,Cochise,estimated from map,minutes,small collection,"""The Swisshelm Mountain Site [...] is located at an elevation of 1,585 meters on a southwest-facing ridge of the northern Swisshelm Mountains, Cochise County, Arizona."" (Thayer, 1985).",gp_mid,-47.77,-7.44,101,US,,Black Prince Limestone,,,bed,,,,,,,NA,"""The amphibian bed [is] located one meter below the top of the Black Prince [Limestone] [...] The Swisshelm Mountain amphibian bed is dated near the Morrowan-Derryan(= Atokan) boundary, equivalent to the boundary of Westphalian A and B of Europe"" (Thayer, 1985).","""light yellow-gray, silty intrabiomicrudit""","""limestone""","intraclastic,shelly/skeletal,gray,yellow",,silty,Y,,,,,,shallow subtidal indet.,,"""The interpretation best fitting the evidence is a partially protected estuarine environment (for the algal oncolites and marine fauna), close to the outlet of a sluggish coastal river (for transporting the terrestrial and freshwater faunal elements)."" (Thayer, 1985).","macrofossils,microfossils",,,,,,NA,,body,variable,allochthonous,time-averaged,,,,,,,NA,,"Some bones show traces of wear through transport, others are completely unworn but may have been transported as a whole carcass into the environment before burial and disarticulation by burrowing organisms. (Thayer, 1985).",taxonomic,"bulk,acetic",,"some macrofossils,difficult macrofossils",,,,,"""Disarticulated faunal elements were obtained by digesting blocks of limestone and silty limestone in a 15 percent solution of acetic acid. The insoluble residue was washed through a 28-mesh screen to remove fine material."" (thayer, 1985).\r\nUALP = University of Arizona Laboratory of Paleontology",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Phlegethontia,,NA,NA,"micropaleontology,vertebrate","D. W. Thayer. 1985. New Pennsylvanian Lepospondyl Amphibians from the Swisshelm Mountains, Arizona. Journal of Paleontology 59(3):684-700",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,04/11/2009 10:49,14/03/2016 07:17,31089,phanerhapha,Phlegethontia,31089,n. sp.,318.1,314.6,Westphalian A,Westphalian B,2,US,Phlegethontia phanerhapha
832562,occ,NA,,92271,,n. gen. Elfridia n. sp. bulbidens,species,156879,,Elfridia bulbidens,NA,species,156879,Thayer,1985,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37295,NA,NA,NA,elements,-109.566666,31.733334,Swisshelm Mts. amphibian site,NA,UALP 7205,US,Arizona,Cochise,estimated from map,minutes,small collection,"""The Swisshelm Mountain Site [...] is located at an elevation of 1,585 meters on a southwest-facing ridge of the northern Swisshelm Mountains, Cochise County, Arizona."" (Thayer, 1985).",gp_mid,-47.77,-7.44,101,US,,Black Prince Limestone,,,bed,,,,,,,NA,"""The amphibian bed [is] located one meter below the top of the Black Prince [Limestone] [...] The Swisshelm Mountain amphibian bed is dated near the Morrowan-Derryan(= Atokan) boundary, equivalent to the boundary of Westphalian A and B of Europe"" (Thayer, 1985).","""light yellow-gray, silty intrabiomicrudit""","""limestone""","intraclastic,shelly/skeletal,gray,yellow",,silty,Y,,,,,,shallow subtidal indet.,,"""The interpretation best fitting the evidence is a partially protected estuarine environment (for the algal oncolites and marine fauna), close to the outlet of a sluggish coastal river (for transporting the terrestrial and freshwater faunal elements)."" (Thayer, 1985).","macrofossils,microfossils",,,,,,NA,,body,variable,allochthonous,time-averaged,,,,,,,NA,,"Some bones show traces of wear through transport, others are completely unworn but may have been transported as a whole carcass into the environment before burial and disarticulation by burrowing organisms. (Thayer, 1985).",taxonomic,"bulk,acetic",,"some macrofossils,difficult macrofossils",,,,,"""Disarticulated faunal elements were obtained by digesting blocks of limestone and silty limestone in a 15 percent solution of acetic acid. The insoluble residue was washed through a 28-mesh screen to remove fine material."" (thayer, 1985).\r\nUALP = University of Arizona Laboratory of Paleontology",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Elfridia,n. gen.,NA,NA,"micropaleontology,vertebrate","D. W. Thayer. 1985. New Pennsylvanian Lepospondyl Amphibians from the Swisshelm Mountains, Arizona. Journal of Paleontology 59(3):684-700",315,334,0,J. Mueller,T. Liebrecht,,04/11/2009 10:49,04/11/2009 12:49,31089,bulbidens,Elfridia,31089,n. sp.,318.1,314.6,Westphalian A,Westphalian B,21,US,Elfridia bulbidens
832563,occ,NA,,92271,,Ptyonius ? n. sp. olisthmonaias,species,156895,,Ptyonius olisthmonaias,NA,species,156895,Thayer,1985,Chordata,33815,Osteichthyes,34881,,NA,Urocordylidae,37270,37274,NA,NA,NA,elements,-109.566666,31.733334,Swisshelm Mts. amphibian site,NA,UALP 7205,US,Arizona,Cochise,estimated from map,minutes,small collection,"""The Swisshelm Mountain Site [...] is located at an elevation of 1,585 meters on a southwest-facing ridge of the northern Swisshelm Mountains, Cochise County, Arizona."" (Thayer, 1985).",gp_mid,-47.77,-7.44,101,US,,Black Prince Limestone,,,bed,,,,,,,NA,"""The amphibian bed [is] located one meter below the top of the Black Prince [Limestone] [...] The Swisshelm Mountain amphibian bed is dated near the Morrowan-Derryan(= Atokan) boundary, equivalent to the boundary of Westphalian A and B of Europe"" (Thayer, 1985).","""light yellow-gray, silty intrabiomicrudit""","""limestone""","intraclastic,shelly/skeletal,gray,yellow",,silty,Y,,,,,,shallow subtidal indet.,,"""The interpretation best fitting the evidence is a partially protected estuarine environment (for the algal oncolites and marine fauna), close to the outlet of a sluggish coastal river (for transporting the terrestrial and freshwater faunal elements)."" (Thayer, 1985).","macrofossils,microfossils",,,,,,NA,,body,variable,allochthonous,time-averaged,,,,,,,NA,,"Some bones show traces of wear through transport, others are completely unworn but may have been transported as a whole carcass into the environment before burial and disarticulation by burrowing organisms. (Thayer, 1985).",taxonomic,"bulk,acetic",,"some macrofossils,difficult macrofossils",,,,,"""Disarticulated faunal elements were obtained by digesting blocks of limestone and silty limestone in a 15 percent solution of acetic acid. The insoluble residue was washed through a 28-mesh screen to remove fine material."" (thayer, 1985).\r\nUALP = University of Arizona Laboratory of Paleontology",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Ptyonius,?,NA,NA,"micropaleontology,vertebrate","D. W. Thayer. 1985. New Pennsylvanian Lepospondyl Amphibians from the Swisshelm Mountains, Arizona. Journal of Paleontology 59(3):684-700",315,334,0,J. Mueller,T. Liebrecht,,04/11/2009 11:11,04/11/2009 13:11,31089,olisthmonaias,Ptyonius,31089,n. sp.,318.1,314.6,Westphalian A,Westphalian B,14,US,Ptyonius olisthmonaias
832564,occ,NA,,92271,,n. gen. Arizonerpeton n. sp. wellsi,species,156896,,Arizonerpeton wellsi,NA,species,156896,Thayer,1985,Chordata,33815,Osteichthyes,34881,,NA,,NA,37277,NA,NA,NA,elements,-109.566666,31.733334,Swisshelm Mts. amphibian site,NA,UALP 7205,US,Arizona,Cochise,estimated from map,minutes,small collection,"""The Swisshelm Mountain Site [...] is located at an elevation of 1,585 meters on a southwest-facing ridge of the northern Swisshelm Mountains, Cochise County, Arizona."" (Thayer, 1985).",gp_mid,-47.77,-7.44,101,US,,Black Prince Limestone,,,bed,,,,,,,NA,"""The amphibian bed [is] located one meter below the top of the Black Prince [Limestone] [...] The Swisshelm Mountain amphibian bed is dated near the Morrowan-Derryan(= Atokan) boundary, equivalent to the boundary of Westphalian A and B of Europe"" (Thayer, 1985).","""light yellow-gray, silty intrabiomicrudit""","""limestone""","intraclastic,shelly/skeletal,gray,yellow",,silty,Y,,,,,,shallow subtidal indet.,,"""The interpretation best fitting the evidence is a partially protected estuarine environment (for the algal oncolites and marine fauna), close to the outlet of a sluggish coastal river (for transporting the terrestrial and freshwater faunal elements)."" (Thayer, 1985).","macrofossils,microfossils",,,,,,NA,,body,variable,allochthonous,time-averaged,,,,,,,NA,,"Some bones show traces of wear through transport, others are completely unworn but may have been transported as a whole carcass into the environment before burial and disarticulation by burrowing organisms. (Thayer, 1985).",taxonomic,"bulk,acetic",,"some macrofossils,difficult macrofossils",,,,,"""Disarticulated faunal elements were obtained by digesting blocks of limestone and silty limestone in a 15 percent solution of acetic acid. The insoluble residue was washed through a 28-mesh screen to remove fine material."" (thayer, 1985).\r\nUALP = University of Arizona Laboratory of Paleontology",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Arizonerpeton,n. gen.,NA,NA,"micropaleontology,vertebrate","D. W. Thayer. 1985. New Pennsylvanian Lepospondyl Amphibians from the Swisshelm Mountains, Arizona. Journal of Paleontology 59(3):684-700",315,334,0,J. Mueller,T. Liebrecht,,04/11/2009 11:11,04/11/2009 13:11,31089,wellsi,Arizonerpeton,31089,n. sp.,318.1,314.6,Westphalian A,Westphalian B,24,US,Arizonerpeton wellsi
832565,occ,NA,,92271,,Lepospondyli ? indet.,unranked clade,152857,,Lepospondyli,NA,unranked clade,37250,Thayer,1985,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,elements,-109.566666,31.733334,Swisshelm Mts. amphibian site,NA,UALP 7205,US,Arizona,Cochise,estimated from map,minutes,small collection,"""The Swisshelm Mountain Site [...] is located at an elevation of 1,585 meters on a southwest-facing ridge of the northern Swisshelm Mountains, Cochise County, Arizona."" (Thayer, 1985).",gp_mid,-47.77,-7.44,101,US,,Black Prince Limestone,,,bed,,,,,,,NA,"""The amphibian bed [is] located one meter below the top of the Black Prince [Limestone] [...] The Swisshelm Mountain amphibian bed is dated near the Morrowan-Derryan(= Atokan) boundary, equivalent to the boundary of Westphalian A and B of Europe"" (Thayer, 1985).","""light yellow-gray, silty intrabiomicrudit""","""limestone""","intraclastic,shelly/skeletal,gray,yellow",,silty,Y,,,,,,shallow subtidal indet.,,"""The interpretation best fitting the evidence is a partially protected estuarine environment (for the algal oncolites and marine fauna), close to the outlet of a sluggish coastal river (for transporting the terrestrial and freshwater faunal elements)."" (Thayer, 1985).","macrofossils,microfossils",,,,,,NA,,body,variable,allochthonous,time-averaged,,,,,,,NA,,"Some bones show traces of wear through transport, others are completely unworn but may have been transported as a whole carcass into the environment before burial and disarticulation by burrowing organisms. (Thayer, 1985).",taxonomic,"bulk,acetic",,"some macrofossils,difficult macrofossils",,,,,"""Disarticulated faunal elements were obtained by digesting blocks of limestone and silty limestone in a 15 percent solution of acetic acid. The insoluble residue was washed through a 28-mesh screen to remove fine material."" (thayer, 1985).\r\nUALP = University of Arizona Laboratory of Paleontology",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lepospondyli,?,NA,NA,"micropaleontology,vertebrate","D. W. Thayer. 1985. New Pennsylvanian Lepospondyl Amphibians from the Swisshelm Mountains, Arizona. Journal of Paleontology 59(3):684-700",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,04/11/2009 11:11,04/11/2009 13:31,31089,indet.,,31089,,318.1,314.6,Westphalian A,Westphalian B,23,US, indet.
832566,occ,NA,,92271,,Tetrapoda indet.,unranked clade,53190,,Tetrapoda,NA,unranked clade,53190,Thayer,1985,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,,-109.566666,31.733334,Swisshelm Mts. amphibian site,NA,UALP 7205,US,Arizona,Cochise,estimated from map,minutes,small collection,"""The Swisshelm Mountain Site [...] is located at an elevation of 1,585 meters on a southwest-facing ridge of the northern Swisshelm Mountains, Cochise County, Arizona."" (Thayer, 1985).",gp_mid,-47.77,-7.44,101,US,,Black Prince Limestone,,,bed,,,,,,,NA,"""The amphibian bed [is] located one meter below the top of the Black Prince [Limestone] [...] The Swisshelm Mountain amphibian bed is dated near the Morrowan-Derryan(= Atokan) boundary, equivalent to the boundary of Westphalian A and B of Europe"" (Thayer, 1985).","""light yellow-gray, silty intrabiomicrudit""","""limestone""","intraclastic,shelly/skeletal,gray,yellow",,silty,Y,,,,,,shallow subtidal indet.,,"""The interpretation best fitting the evidence is a partially protected estuarine environment (for the algal oncolites and marine fauna), close to the outlet of a sluggish coastal river (for transporting the terrestrial and freshwater faunal elements)."" (Thayer, 1985).","macrofossils,microfossils",,,,,,NA,,body,variable,allochthonous,time-averaged,,,,,,,NA,,"Some bones show traces of wear through transport, others are completely unworn but may have been transported as a whole carcass into the environment before burial and disarticulation by burrowing organisms. (Thayer, 1985).",taxonomic,"bulk,acetic",,"some macrofossils,difficult macrofossils",,,,,"""Disarticulated faunal elements were obtained by digesting blocks of limestone and silty limestone in a 15 percent solution of acetic acid. The insoluble residue was washed through a 28-mesh screen to remove fine material."" (thayer, 1985).\r\nUALP = University of Arizona Laboratory of Paleontology",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tetrapoda,,NA,NA,"micropaleontology,vertebrate","D. W. Thayer. 1985. New Pennsylvanian Lepospondyl Amphibians from the Swisshelm Mountains, Arizona. Journal of Paleontology 59(3):684-700",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,04/11/2009 11:11,04/11/2009 13:31,31089,indet.,,31089,,318.1,314.6,Westphalian A,Westphalian B,NA,US, indet.
843497,occ,NA,,28256,,Acheloma ? n. sp. casei,species,162311,subjective synonym of,Isodectes obtusus,NA,species,137370,Broili,1913,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Saurerpetontidae,36980,36983,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Acheloma,?,NA,NA,vertebrate,"F. Broili. 1913. ber zwei Stegocephalenreste aus dem texanischen Perm. Neues Jahrbuch f_r Mineralogie, Geologie und Pal_ontologie 1913(1):96-100",315,334,0,J. Mueller,T. Liebrecht,,29/01/2010 05:08,29/01/2010 07:08,17702,casei,Isodectes,31846,n. sp.,279.3,272.3,Kungurian,,1,US,Isodectes casei
851020,occ,NA,,67862,,Acleistorhinidae sp.,genus,37514,,Acleistorhinidae,NA,family,37514,Modesto et al.,2009,Chordata,33815,Reptilia,36322,,NA,Acleistorhinidae,37514,NA,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Acleistorhinidae,,NA,NA,"paleoentomology,vertebrate","S. P. Modesto, D. M. Scott, and R. R. Reisz. 2009. Arthropod remains in the oral cavities of fossil reptiles support inference of early insectivory. Biology Letters 5(6):838-840",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,04/03/2010 14:03,13/01/2016 18:20,19393,sp.,,32221,,290.1,268,Leonard,,1,US, sp.
853385,occ,NA,,86946,,Hylonomus lyelli,species,139093,,Hylonomus lyelli,NA,species,139093,Carroll,1964,Chordata,33815,Reptilia,36322,,NA,Protorothyrididae,37486,37492,NA,NA,NA,individuals,-64.451385,45.698612,"Joggins; Divison 4, Section XII, coal-group 26",NA,Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Division 4 ""of the section extends from McCairn's Cove to the end of the high cliff beyond 'Coal-mine Point'."" (Dawson, 1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173 p. 162); Lat long is approx. for Coal Mine Point",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XII",coal-group 26,,,,NA,"Coal-group 26 has a total thickness of 118 ft (including a 4 inch coaly shale). (Dawson, 1878 p. 170). Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","""Gray sandstone and shale, with erect Sigillaria; at four or five levels, and two Stigmarian underclays"" (Dawson, 1878 p. 170)",sandstone,gray,,,,claystone,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",,,snapshot,,,,,,,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" (Lyell, 1853, Quart. J. Geol. Soc. 9)",taxonomic,"field collection,survey of museum collection,observed (not collected)",,,,,"J. W. Dawson, P. W. McNaughton, among others",,,"Dawson (1878, Acadian Geology, 3rd ed.) reports Stigmaria sp. from this site",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Hylonomus,,NA,NA,vertebrate,R. L. Carroll. 1964. The earliest reptiles. Journal of the Linnean Society (Zoology) 45(304):61-83,315,334,0,J. Mueller,T. Liebrecht,,13/03/2010 20:48,13/03/2010 22:48,28956,lyelli,Hylonomus,28956,,318.1,314.6,Westphalian A,,2,CA,Hylonomus lyelli
853419,occ,NA,,28069,,Hylonomus n. sp. aciedentatus,species,164848,subjective synonym of,Dendrerpeton acadianum,NA,species,164775,Dawson,1860,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dendrerpetonidae,36994,36995,NA,NA,NA,specimens,-64.451385,45.698612,"Coal Mine Point; Divison 4, Section XV, coal-group 15",NA,South Joggins; Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Cliffs called the South Joggins (coast), about half a mile eastward of the Coal Pier.",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XV",coal-group 15,,,,NA,"From Steen (1934): ""top of the Joggins formation...Division 4, Section XV., Coal-group 15 of the Joggins section given in Dawson's 'Acadian Geology,' 1868, pp. 156-178."" From Lyell (1853): The fossils are from Bed 5 of a 25 ft section, composed of 7 beds. Bed 5 is approximately 600 ft below the main coal, ""King's Vein"".\r\nOriginal entry for Local Section name was ""South Joggins""; for Bed/horizon ""bed 5"". In Steen (1934) a ""bed 5"" is not mentioned in any way. Also, in papers published before and after Lyell's ""On the Remains of a Reptile..."" (1953) a different numbering is applied to the Joggins Section. Thus, it is more appropriate to follow the stratigraphic terminology used in Dawson (1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173), Steen (1934, see description above) and Carroll (1964). Coal-group 15 consists of 3 beds with a total thickness of 10 ft 6 in. (Dawson, 1878) (TL) \r\nOriginal entry for chronostratigraphy was simply ""Westphalian"". Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","From Lyell (1853): 5. Grey sandstone, with three erect trees, one having Stigmarian roots; erect Calamites and stems of unknown plants. (One of the erect trees in this bed contained the bones, teeth, &c. and land-shell above-mentioned.) ...9 ft;\r\n",sandstone,gray,,,Y,coal,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",good,,snapshot,,,,,,occasional,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" ",taxonomic,"bulk,selective quarrying,field collection,survey of museum collection",BMNH,,,,"J. W. Dawson, C. Lyell, among others",,"RM = Redpath Museum of McGill Unversity, Montreal","Listed by Steen (1934) as Indeterminate species: Hylerpeton dawsoni Owen; Hylerpeton longidentatum Dawson; Hylerpeton intermedium Dawson; Hylonomus multidens Dawson; Hylonomus wymani Dawson; Smilerpeton aciedentatus Dawson; Amblyodon problematicum Dawson; Sparodus sp. Dawson; Baphetes minor Dawson.\r\n\r\nAll catalogue numbers are from Steen (1934) and/or from Carroll (1967).\r\n\r\nThe taxon ""Batrachoididae indet."", entered under the reference Lyell & Dawson (1853), has been removed from the taxonomic list for it is a family of teleost fish. It probably referred to the ""batrachian"" affinities of the tetrapod bones noticed by Wyman (1853) but all these bones finally were assigned to Dendrerpeton acadianum n. gen. et sp. (see pls. II and III in Lyell & Dawson/Wyman/Owen, 1853). Thus the originally enterd taxon ""Dendrerpeton acadianum"", reference: Lyell & Dawson, was replaced by ""Batrachia indet."", reference: Wyman (1853), and re-identification by Owen (1853) was added (TL).\r\nRe-identification of ""Dendrerpeton oweni n. sp."" as ""Dendrerpeton acadianum"" by by Steen was removed after opinons on synonymy of the the former with the latter species were entered into the database (TL).","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Hylonomus,,NA,NA,vertebrate,"J. W. Dawson. 1860. On a Terrestrial Mollusk, a Chilognathous Myriapod, and some New Species of Reptiles, from the Coal-Formation of Nova Scotia. Quarterly Journal of the Geological Society of London 16:268-277",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,15/03/2010 19:45,16/03/2010 00:27,7856,aciedentatus,Dendrerpeton,32301,n. sp.,318.1,314.6,Westphalian A,,1,CA,Dendrerpeton aciedentatus
853420,occ,NA,,28069,,Hylonomus n. sp. wymani,species,164849,,Hylonomus wymani,NA,species,164849,Dawson,1860,Chordata,33815,Reptilia,36322,,NA,Protorothyrididae,37486,37492,NA,NA,NA,specimens,-64.451385,45.698612,"Coal Mine Point; Divison 4, Section XV, coal-group 15",NA,South Joggins; Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Cliffs called the South Joggins (coast), about half a mile eastward of the Coal Pier.",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XV",coal-group 15,,,,NA,"From Steen (1934): ""top of the Joggins formation...Division 4, Section XV., Coal-group 15 of the Joggins section given in Dawson's 'Acadian Geology,' 1868, pp. 156-178."" From Lyell (1853): The fossils are from Bed 5 of a 25 ft section, composed of 7 beds. Bed 5 is approximately 600 ft below the main coal, ""King's Vein"".\r\nOriginal entry for Local Section name was ""South Joggins""; for Bed/horizon ""bed 5"". In Steen (1934) a ""bed 5"" is not mentioned in any way. Also, in papers published before and after Lyell's ""On the Remains of a Reptile..."" (1953) a different numbering is applied to the Joggins Section. Thus, it is more appropriate to follow the stratigraphic terminology used in Dawson (1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173), Steen (1934, see description above) and Carroll (1964). Coal-group 15 consists of 3 beds with a total thickness of 10 ft 6 in. (Dawson, 1878) (TL) \r\nOriginal entry for chronostratigraphy was simply ""Westphalian"". Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","From Lyell (1853): 5. Grey sandstone, with three erect trees, one having Stigmarian roots; erect Calamites and stems of unknown plants. (One of the erect trees in this bed contained the bones, teeth, &c. and land-shell above-mentioned.) ...9 ft;\r\n",sandstone,gray,,,Y,coal,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",good,,snapshot,,,,,,occasional,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" ",taxonomic,"bulk,selective quarrying,field collection,survey of museum collection",BMNH,,,,"J. W. Dawson, C. Lyell, among others",,"RM = Redpath Museum of McGill Unversity, Montreal","Listed by Steen (1934) as Indeterminate species: Hylerpeton dawsoni Owen; Hylerpeton longidentatum Dawson; Hylerpeton intermedium Dawson; Hylonomus multidens Dawson; Hylonomus wymani Dawson; Smilerpeton aciedentatus Dawson; Amblyodon problematicum Dawson; Sparodus sp. Dawson; Baphetes minor Dawson.\r\n\r\nAll catalogue numbers are from Steen (1934) and/or from Carroll (1967).\r\n\r\nThe taxon ""Batrachoididae indet."", entered under the reference Lyell & Dawson (1853), has been removed from the taxonomic list for it is a family of teleost fish. It probably referred to the ""batrachian"" affinities of the tetrapod bones noticed by Wyman (1853) but all these bones finally were assigned to Dendrerpeton acadianum n. gen. et sp. (see pls. II and III in Lyell & Dawson/Wyman/Owen, 1853). Thus the originally enterd taxon ""Dendrerpeton acadianum"", reference: Lyell & Dawson, was replaced by ""Batrachia indet."", reference: Wyman (1853), and re-identification by Owen (1853) was added (TL).\r\nRe-identification of ""Dendrerpeton oweni n. sp."" as ""Dendrerpeton acadianum"" by by Steen was removed after opinons on synonymy of the the former with the latter species were entered into the database (TL).",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Hylonomus,,NA,NA,vertebrate,"J. W. Dawson. 1860. On a Terrestrial Mollusk, a Chilognathous Myriapod, and some New Species of Reptiles, from the Coal-Formation of Nova Scotia. Quarterly Journal of the Geological Society of London 16:268-277",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,15/03/2010 19:45,16/03/2010 00:09,7856,wymani,Hylonomus,32301,n. sp.,318.1,314.6,Westphalian A,,1,CA,Hylonomus wymani
853421,occ,NA,,28069,,n. gen. Hylerpeton n. sp. dawsoni,species,164852,,Hylerpeton dawsoni,NA,species,164852,Owen,1862,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37297,NA,NA,NA,specimens,-64.451385,45.698612,"Coal Mine Point; Divison 4, Section XV, coal-group 15",NA,South Joggins; Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Cliffs called the South Joggins (coast), about half a mile eastward of the Coal Pier.",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XV",coal-group 15,,,,NA,"From Steen (1934): ""top of the Joggins formation...Division 4, Section XV., Coal-group 15 of the Joggins section given in Dawson's 'Acadian Geology,' 1868, pp. 156-178."" From Lyell (1853): The fossils are from Bed 5 of a 25 ft section, composed of 7 beds. Bed 5 is approximately 600 ft below the main coal, ""King's Vein"".\r\nOriginal entry for Local Section name was ""South Joggins""; for Bed/horizon ""bed 5"". In Steen (1934) a ""bed 5"" is not mentioned in any way. Also, in papers published before and after Lyell's ""On the Remains of a Reptile..."" (1953) a different numbering is applied to the Joggins Section. Thus, it is more appropriate to follow the stratigraphic terminology used in Dawson (1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173), Steen (1934, see description above) and Carroll (1964). Coal-group 15 consists of 3 beds with a total thickness of 10 ft 6 in. (Dawson, 1878) (TL) \r\nOriginal entry for chronostratigraphy was simply ""Westphalian"". Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","From Lyell (1853): 5. Grey sandstone, with three erect trees, one having Stigmarian roots; erect Calamites and stems of unknown plants. (One of the erect trees in this bed contained the bones, teeth, &c. and land-shell above-mentioned.) ...9 ft;\r\n",sandstone,gray,,,Y,coal,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",good,,snapshot,,,,,,occasional,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" ",taxonomic,"bulk,selective quarrying,field collection,survey of museum collection",BMNH,,,,"J. W. Dawson, C. Lyell, among others",,"RM = Redpath Museum of McGill Unversity, Montreal","Listed by Steen (1934) as Indeterminate species: Hylerpeton dawsoni Owen; Hylerpeton longidentatum Dawson; Hylerpeton intermedium Dawson; Hylonomus multidens Dawson; Hylonomus wymani Dawson; Smilerpeton aciedentatus Dawson; Amblyodon problematicum Dawson; Sparodus sp. Dawson; Baphetes minor Dawson.\r\n\r\nAll catalogue numbers are from Steen (1934) and/or from Carroll (1967).\r\n\r\nThe taxon ""Batrachoididae indet."", entered under the reference Lyell & Dawson (1853), has been removed from the taxonomic list for it is a family of teleost fish. It probably referred to the ""batrachian"" affinities of the tetrapod bones noticed by Wyman (1853) but all these bones finally were assigned to Dendrerpeton acadianum n. gen. et sp. (see pls. II and III in Lyell & Dawson/Wyman/Owen, 1853). Thus the originally enterd taxon ""Dendrerpeton acadianum"", reference: Lyell & Dawson, was replaced by ""Batrachia indet."", reference: Wyman (1853), and re-identification by Owen (1853) was added (TL).\r\nRe-identification of ""Dendrerpeton oweni n. sp."" as ""Dendrerpeton acadianum"" by by Steen was removed after opinons on synonymy of the the former with the latter species were entered into the database (TL).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Hylerpeton,n. gen.,NA,NA,vertebrate,"R. Owen. 1862. Description of Specimens of Fossil Reptilia discovered in the Coal-measures of the South Joggins, Nova Scotia, by Dr. J. W. Dawson, FGS, etc. Quarterly Journal of the Geological Society of London 18:238-244",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,15/03/2010 21:44,16/03/2010 00:05,7856,dawsoni,Hylerpeton,32316,n. sp.,318.1,314.6,Westphalian A,,1,CA,Hylerpeton dawsoni
853657,occ,NA,,94802,,Ophiacodon cf. uniformis,species,123419,,Ophiacodon uniformis,NA,species,138049,Stephens,1964,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,individuals,-81,39.71389,"East side of King's Knob, near Laings Post Office",NA,,US,Ohio,Monroe,stated in text,seconds,small collection,""" [...] collected about 1000 yards east of the crossroads community of Liangs Post Office, Green Township, Monroe County, Ohio. The exact location was on the east side of King's Knob, SW 1/4, Sec. 27, T. 3N., R. 4W."" (Stephens, 1964).\r\nNote: This is in Green Township, Antioch 7,5' quadrangle.",gp_mid,-14.9,-2.5,101,US,FED,Greene,Dunkard,,,,,,,,,NA,"""The area of collection lies well within the mapped area of the Dunkard Group in eastern Ohio (Stauffer and Schroyer, 1920). Field examination revealed that the specimen probably came from a sandstone exposed at an elevation of 1100 ft. Comparison of this elevation with the measured section (no. 9908, on file with the Ohio Geological Survey) indicates that the standstone lies appreciably above the Washington 'A' coal and belongs to the Green Formation of Stauffer and Schroyer (1920). Horace Collins, Coal Geologist for the Ohio Geological Survey, confirms the assignment of this sandstone to the Green Formation of Lower Permian (Wichita) age."" (Stephens, 1964).\r\nNote: The age of the Greene Fm., wich is not well constrained, here is based on correlation chart (fig. 4) in Wellstead (1991, Bull. AMNH 209).",,sandstone,micaceous,,,Y,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,F. L. Williams,about 1915,"""Approximately fifty years ago, Fred L. Williams, now of Woodsfield, Ohio, while plowing a field just east of Liangs Post Office, Monroe County, Ohio, struck and split open a large slab of micaceous sandstone. On examining the slab he noted that it contained the bones of some animal. He removed the specimen and placed it in his barn. In September of 1957 he turned over the specimen to Elmer Templeton, a student at Marietta College. Mr. Templeton in turn gave the specimen to George Hayfield, then an instructor of geology at Marietta College. The specimen was sent to the Ohio Geological Survey for identification and then to Professor Claude W. Hibbard, Museum of Paleontology, The University of Michigan. At The University of Michigan the specimen was prepared by Dr. Thomas M. Oelrich but owing to other commitments he did not finish his work on the specimen and it was returned to the Ohio Geological Survey in June of 1959. I uncovered the specimen in March, 1961. Since Mr. Templeton gave the specimen to Marietta College for study, he decided to donate the specimen to Princeton University. The specimen is now on display at Princeton and has been assigned Princeton University number 17800."" (Stephens, 1964).",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,J. J. Stephens. 1964. Ophiacodon from Ohio. The Ohio Journal of Science 64(3):217-220,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,19/03/2010 16:06,19/03/2010 18:11,32327,uniformis,Ophiacodon,32327,cf.,295.5,290.1,Sakmarian,,1,US,Ophiacodon uniformis
853658,occ,NA,,67862,,Sphenacodontidae indet.,family,38901,,Sphenacodontidae,NA,family,38901,Evans et al.,2009,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,NA,NA,NA,NA,specimens,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodontidae,,NA,NA,"paleoentomology,vertebrate","D. C. Evans, H. C. Maddin, and R. R. Reisz. 2009. A Re-Evaluation of Sphenacodontid Synapsid Material from the Lower Permian Fissure Fills near Richards Spur, Oklahoma. Palaeontology 52(1):219-227",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,19/03/2010 18:25,19/03/2010 20:25,19393,indet.,,32328,,290.1,268,Leonard,,6,US, indet.
853659,occ,NA,,67862,,Mycterosaurinae sp.,genus,91798,,Mycterosaurinae,NA,subfamily,91798,Evans et al.,2009,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,NA,NA,NA,NA,specimens,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Mycterosaurinae,,NA,NA,"paleoentomology,vertebrate","D. C. Evans, H. C. Maddin, and R. R. Reisz. 2009. A Re-Evaluation of Sphenacodontid Synapsid Material from the Lower Permian Fissure Fills near Richards Spur, Oklahoma. Palaeontology 52(1):219-227",315,334,0,J. Mueller,T. Liebrecht,,19/03/2010 19:38,19/03/2010 21:38,19393,sp.,,32328,,290.1,268,Leonard,,3,US, sp.
853669,occ,NA,,67862,,Protorothyrididae indet.,family,37486,,Protorothyrididae,NA,family,37486,Reisz,1980,Chordata,33815,Reptilia,36322,,NA,Protorothyrididae,37486,NA,NA,NA,NA,elements,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Protorothyrididae,,NA,NA,"paleoentomology,vertebrate","R. R. Reisz. 1980. A Protorothyridid Captorhinomorph Reptile from the Lower Permian of Oklahoma. Life Sciences Contributions, Royal Ontario Museum 121:1-16",315,334,0,J. Mueller,T. Liebrecht,,24/03/2010 03:12,24/03/2010 05:12,19393,indet.,,28667,,290.1,268,Leonard,,9,US, indet.
853693,occ,NA,R,67862,,Labidosaurus sp.,genus,37501,,Labidosaurus,NA,genus,37501,Gregory et al.,1956,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,specimens,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,"paleoentomology,vertebrate","J. T. Gregory, F. E. Peabody, and L. I. Price. 1956. Revision of the Gymnarthridae - American Permian Microsaurs. Bulletin of the Peabody Museum of Natural History 10:1-77",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,24/03/2010 11:20,03/08/2016 10:40,19393,sp.,Labidosaurus,28484,,290.1,268,Leonard,,6,US,Labidosaurus sp.
853693,occ,23010,R,67862,,Labidosaurus cf. hamatus,species,134918,,Labidosaurus hamatus,NA,species,134856,Olson,1967,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,specimens,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,"paleoentomology,vertebrate",E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,24/03/2010 11:34,24/03/2010 14:27,19393,hamatus,Labidosaurus,28557,cf.,290.1,268,Leonard,,6,US,Labidosaurus hamatus
853693,occ,23012,R,67862,,Eocaptorhinus laticeps,species,134878,recombined as,Captorhinus laticeps,NA,species,120324,Heaton,1979,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,specimens,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Eocaptorhinus,,NA,NA,"paleoentomology,vertebrate","M. J. Heaton. 1979. Cranial Anatomy of Primitive Captorhinid Reptiles from the Late Pennsylvanian and Early Permian, Oklahoma and Texas. Oklahoma Geological Survey, Bulletin 127:1-83",315,334,0,J. Mueller,T. Liebrecht,,24/03/2010 12:29,24/03/2010 14:29,19393,laticeps,Captorhinus,28362,,290.1,268,Leonard,,6,US,Captorhinus laticeps
853693,occ,23013,,67862,,Captorhinus sp.,genus,37497,,Captorhinus,NA,genus,37497,Kissel et al.,2002,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,specimens,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,"paleoentomology,vertebrate","R. A. Kissel, D. W. Dilkes, and R. R. Reisz. 2002. Captorhinus magnus, a new captorhinid (Amniota: Eureptilia) from the Lower Permian of Oklahoma, with new evidence on the homology of the astragalus. Canadian Journal of Earth Sciences 39(9):1363-1372",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,24/03/2010 12:34,25/03/2010 11:14,19393,sp.,Captorhinus,28381,,290.1,268,Leonard,,6,US,Captorhinus sp.
929106,occ,NA,,106270,,n. gen. Pederpes n. sp. finneyae,species,179035,,Pederpes finneyae,NA,species,179035,Clack,2002,Chordata,33815,Osteichthyes,34881,,NA,Whatcheeriidae,179034,179033,NA,NA,NA,individuals,-4.53654,55.972,Auchenreoch Glen,NA,,UK,Scotland,,based on nearby landmark,3,small collection,"Auchenreoch Glen, near Maryland Farm, 23 km north of Dumbarton, Scotland",gp_mid,-13.51,-31.85,313,UK,,Ballagan,Inverclyde,,bed,,,,,,,NA,claviger-macra (CM) palynozone (possibly from the lower part of this zone); Tournaisian Tn3c,"""The formation consists of pale grey, fine- grained nodular cementstones with calcareous mudstones and limestones. The specimen is preserved in a clayey limestone nodule typical of a cementstone facies.""","""limestone""","fine,concretionary,gray",,argillaceous,Y,mudstone,,,calcareous,,lagoonal,,"""shallow-water environment, probably a lagoon or coastal flat that was subject to marked fluctuations in salinity and periodic desiccation""","macrofossils,mesofossils",some,,,,,NA,,body,excellent,,snapshot,,dispersed,,rare,,occasional,NA,,,taxonomic,field collection,,,,,,1971,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Pederpes,n. gen.,NA,NA,vertebrate,"J. A. Clack. 2002. An early tetrapod from ""Romer۪s Gap"". Nature 418:72-76",14,14,0,M. Carrano,M. Carrano,,05/03/2011 02:14,04/03/2011 09:14,35414,finneyae,Pederpes,35414,n. sp.,353.8,345.3,Ivorian,,1,UK,Pederpes finneyae
930782,occ,NA,,67862,,Acheloma n. sp. dunni,species,180406,,Acheloma dunni,NA,species,180406,Polley and Reisz,2011,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,37048,NA,NA,NA,specimens,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Acheloma,,NA,NA,"paleoentomology,vertebrate","B. P. Polley and R. R. Reisz. 2011. A new Lower Permian trematopid (Temnospondyli: Dissorophoidea) from Richards Spur, Oklahoma. Zoological Journal of the Linnean Society 161:789-815",327,327,0,R. Butler,R. Butler,,22/03/2011 19:35,22/03/2011 03:35,19393,dunni,Acheloma,35587,n. sp.,290.1,268,Leonard,,6,US,Acheloma dunni
945307,occ,NA,,109702,,n. gen. Cryptovenator n. sp. hirschbergeri,species,185994,,Cryptovenator hirschbergeri,NA,species,185994,Fr̦bisch et al.,2011,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,185993,NA,NA,NA,individuals,7.434722,49.924442,Remigiusberg Quarry,NA,,DE,Rhineland-Palatinate,Kusel,stated in text,seconds,,,gp_mid,19.03,4.57,315,DE,,Remigiusberg,Rotliegend,,,,quarry profile,26,bottom to top,,,NA,,"""calcareous, finegrained sandstone of graybluegreen colour with coarse silty lamina""",sandstone,,lithified,silty,Y,,,,,,lacustrine indet.,intramontane basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"""The bones, scales, and teeth have a bright white coloration as a result of contact metamorphosis of the sediments with subvolcanic intrusions.""",taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cryptovenator,n. gen.,NA,NA,vertebrate,"J. Fr̦bisch, R. R. Schoch, and J. M_ller, T. Schindler, D. Schweiss. 2011. A new basal sphenacodontid synapsid from the Late Carboniferous of the SaarNahe Basin, Germany. Acta Palaeontologica Polonica 56(1):113-120",425,425,334,J. Fr̦bisch,J. Fr̦bisch,T. Liebrecht,22/05/2011 22:27,24/10/2011 10:32,36207,hirschbergeri,Cryptovenator,36207,n. sp.,303.7,298.9,Gzhelian,,1,DE,Cryptovenator hirschbergeri
963873,occ,NA,,79598,,n. gen. Micrerpeton n. sp. caudatum,species,192950,subjective synonym of,Amphibamus grandiceps,NA,species,229305,Moodie,1909,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,37019,NA,NA,NA,,-88.139999,41.267223,Mazon Creek,NA,"Mazon Creek Vertebrate Fauna, Braidwood Fauna, pit 11",US,Illinois,Grundy/Will,based on political unit,seconds,local area,"Lat Long is for SW Will Co., Illinois",gp_mid,-23.34,-5.09,101,US,,Carbondale,,Francis Creek Shale,,,,,,,,NA,"""Francis Creek Shale above Morris (no. 2) Coal, Carbondale Formation, Westphalian D, Middle Pennsylvanian"" (Carroll & Baird, 1972)\r\nBaird et al. (1985) refer to the no. 2 coal as Colchester or Croweburg Coal Member.","""Concretions occur typically in laminated to weakly rippled, silty mudstone deposits which typically show little or no evidence of bioturbation. Small-scale sedimentary structures in nodule-bearing sequences include climbing ripple drift, and soft-sediment load-failure..."" (Baird et al., 1985 p.90). Note that this is a general description of the fossil bearing strata of the Francis Creek Shale Member which does not refer specifically to the occurences in the Mazon Creek area proper.",mudstone,"current ripples,deformed bedding",,silty,,siderite,nodular,,,Y,deltaic indet.,foreland basin,"""...these indicate rapid and often episodic mud deposition in interdistributary bay and prodelta settings."" (Baird et al., 1985 p.90)",macrofossils,,,,,,NA,,"mold/impression,concretion,soft parts,replaced with other",good,parautochthonous,,,,,,,,NA,,"""Outlines of the limbs can be seen in the matrix, indicating the extent of the soft tissue and the texture of the skin. The bone itself was represented by a very soft, claylike material that had been removed from the hard, ironstone matrix."" (Carroll, & Baird, 1972 p. 323)\r\nBones are replaced by clay minerals such as Kaolinite (Gregory, 1948 p. 637).",taxonomic,"mechanical,survey of museum collection","FMNH,MCZ,USNM,YPM","species names,ichnofossils",,,"R. L. Moodie, P. Turnbull, among others","1871, 1953",,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Micrerpeton,n. gen.,NA,NA,vertebrate,R. L. Moodie. 1909. A contribution to a monograph of the extinct Amphibia of North America. New forms from the Carboniferous. Journal of Geology 17(1):38-82,14,14,0,M. Carrano,M. Carrano,,28/07/2011 05:57,27/07/2011 14:57,28608,caudatum,Amphibamus,28743,n. sp.,311.45,306.95,Westphalian D,,NA,US,Amphibamus caudatum
963874,occ,NA,,85292,,Diceratosaurus n. sp. laevis,species,192954,subjective synonym of,Erpetosaurus radiatus,NA,species,336710,Moodie,1909,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,36982,NA,NA,NA,individuals,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Diceratosaurus,,NA,NA,vertebrate,R. L. Moodie. 1909. A contribution to a monograph of the extinct Amphibia of North America. New forms from the Carboniferous. Journal of Geology 17(1):38-82,14,14,14,M. Carrano,M. Carrano,M. Carrano,28/07/2011 06:02,27/07/2011 15:03,28831,laevis,Erpetosaurus,28743,n. sp.,311.45,306.95,Westphalian D,,1,US,Erpetosaurus laevis
963875,occ,NA,,85292,,Diceratosaurus n. sp. robustus,species,192955,subjective synonym of,Erpetosaurus radiatus,NA,species,336710,Moodie,1909,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,36982,NA,NA,NA,individuals,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Diceratosaurus,,NA,NA,vertebrate,R. L. Moodie. 1909. A contribution to a monograph of the extinct Amphibia of North America. New forms from the Carboniferous. Journal of Geology 17(1):38-82,14,14,0,M. Carrano,M. Carrano,,28/07/2011 06:03,27/07/2011 15:03,28831,robustus,Erpetosaurus,28743,n. sp.,311.45,306.95,Westphalian D,,1,US,Erpetosaurus robustus
963876,occ,NA,,85292,,Ichthyerpeton n. sp. squamosum,species,192957,,Ichthyerpeton squamosum,NA,species,192957,Moodie,1909,Chordata,33815,Osteichthyes,34881,,NA,Colosteidae,36975,192956,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ichthyerpeton,,NA,NA,vertebrate,R. L. Moodie. 1909. A contribution to a monograph of the extinct Amphibia of North America. New forms from the Carboniferous. Journal of Geology 17(1):38-82,14,14,0,M. Carrano,M. Carrano,,28/07/2011 06:05,27/07/2011 15:05,28831,squamosum,Ichthyerpeton,28743,n. sp.,311.45,306.95,Westphalian D,,NA,US,Ichthyerpeton squamosum
964693,occ,NA,,113555,,n. gen. Rubeostratilia n. sp. texensis,species,193400,,Rubeostratilia texensis,NA,species,193400,Bourget and Anderson,2011,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,193399,NA,NA,NA,,-98.199997,33.816666,East of Henrietta,NA,TMM 31226,US,Texas,Clay,based on nearby landmark,minutes,small collection,"""east of Henrietta""",gp_mid,-29.94,-1.8,101,US,,Nocona,Wichita,,,,,,,,,NA,,"lithology not discussed, but figured specimen appears to be preserved in a siltstone or mudstone","""siliciclastic""",,lithified,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,TMM,,,,,1941,"collected ""by a Work Projects Administration"" project",additional fauna not discussed,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Rubeostratilia,n. gen.,NA,NA,vertebrate,H. Bourget and J. S. Anderson. 2011. A new amphibamid (Temnospondyli: Dissorophoidea) from the Early Permian of Texas. Journal of Vertebrate Paleontology 31(1):32-49,4,4,0,J. Alroy,J. Alroy,,01/08/2011 13:17,31/07/2011 22:17,36836,texensis,Rubeostratilia,36836,n. sp.,298.9,290.1,Asselian,Sakmarian,NA,US,Rubeostratilia texensis
968981,occ,NA,,80784,,n. gen. Ianthodon n. sp. schultzei,species,196920,,Ianthodon schultzei,NA,species,196920,Kissel and Reisz,2004,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,196919,NA,NA,NA,,-95.259048,38.378502,Garnett Quarry,NA,"Garnett Vertebrate Fauna, Charles Hardesty farm",US,Kansas,Anderson,estimated from map,6,outcrop,"""6 miles northwest of Garnett"" (Reisz, 1986); ""NW 1/4, NE 1/4, sec. 5, tp. 20 S, rge. 19 E, Putnam Township, Anderson County, Kansas"" (Reisz & Berman, 1986)\r\n""Charles A. Hardest farm, NW/4 NE/4 sec. 5 T20S R19E, Putnam Township, Anderson County, Kansas. The Universal Transverse Mercantor (UTM) coordinates of the quarry are 15STN963466. Locality is close to Garnett, Kansas."" (Laurin 1993). ",gp_mid,-27.44,-2.3,101,US,,Stanton,Lansing,Rock Lake Shale,group of beds,,,,,,,NA,"""Rock Lake Member, Stanton Formation, Lansing Group, Missourian Series, Upper Pennsylvanian"" (Reisz & Berman, 1996)\r\nall vertebrate remains seem to come exclusively from the basal part of the Rock Lake Shale (see Reisz et al., 1982)","""dark greyishbrown, moderately well bedded, very carbonaceous, calcareous mudstone"" (Reisz et al., 1982)",mudstone,brown,,"calcareous,carbonaceous",Y,,,,,,fine channel fill,foreland basin,"""The Rock Lake Shale is a rather thin but otherwise typical ۪outside۪ shale of a ۪Kansas Megacyclothem۪ sequence formed as a change from regressive to transgressive conditions occurred [...] The site is located along the western edge of what was, during the Late Pennsylvanian, a shallow, forested stream valley or channel that was eroded into a limestone coastal plain during the latter stages of a major eustatic fall in sea level. As the succeeding rise in sea level occurred, the valley was gradually flooded by estuarine waters"" (Reisz et al., 1982).\r\nSequence stratigraphy is interpreted from the description given by Reisz et al. (1982). The surface of the underlying limestone is the sequence boundary merged with the transgressive surface and the Lake Rock Shale is the basalmost deposit of the transgressive systems tract.",macrofossils,some,some,,,,NA,,body,good,,snapshot,,,,,,,NA,,,taxonomic,"bulk,mechanical",ROM,,,,"F. E. Peabody, R. Camp, R. L. Carroll, R. R. Reisz, M. J. Heaton, B. R. Pynn, G. MacDonald","1953-1956, 1965, 1980, 1981",,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ianthodon,n. gen.,NA,NA,vertebrate,"R. A. Kissel and R. R. Reisz. 2004. Synapsid fauna of the Upper Pennsylvanian Rock Lake Shale near Garnett, Kansas and the diversity pattern of early amniotes. In G. Arratia, M. V. H. Wilson and R. Cloutier (eds.), Recent Advances in the Origin and Early Radiation of Vertebrates. Verlag Dr. Friedrich Pfeil, Munich ",425,446,0,J. Fr̦bisch,M. Walther,,24/08/2011 23:17,24/08/2011 08:17,28862,schultzei,Ianthodon,28867,n. sp.,305.9,303.4,Missourian,,NA,US,Ianthodon schultzei
990481,occ,NA,,119428,,Reiszorhinus olsoni,species,204031,,Reiszorhinus olsoni,NA,species,204031,Sumida et al.,2010,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,204025,NA,NA,NA,individuals,-99.091667,33.733334,E. C. Olson locality near Mitchell Creek,NA,,US,Texas,Baylor,based on nearby landmark,seconds,hand sample,"""The late E. C. Olson collected CM 81785 (formerly UCLA VP 2597) from a locality near Mitchell Creek, but did not provide more detailed locality data.""\r\nPolar coordinates are the same as for PBDB coll. no. 28250.",gp_mid,-30.29,-0.93,101,US,,Waggoner Ranch,Wichita,,bed,,,,,,,NA,"""Its [i.e. the present collection; TL] proximity to the locality yielding FMNH UC183 [i.e. Mitchell Creek; TL] would suggest that it can also be considered to be from the Waggoner Ranch Formation.""",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,CM,,,,E. C. Olson,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Reiszorhinus,,NA,NA,vertebrate,"S. S. Sumida, J. Dodick, and A. Metcalf, G. Albright. 2010. Reiszorhinus olsoni, a New Single-Tooth-Rowed Captorhinid Reptile from the Lower Permian of Texas. Journal of Vertebrate Paleontology 30(3):704-714",315,334,0,J. Mueller,T. Liebrecht,,25/10/2011 01:17,24/10/2011 09:17,38301,olsoni,Reiszorhinus,38301,,290.1,272.3,Artinskian,Kungurian,1,US,Reiszorhinus olsoni
990494,occ,NA,,67862,,n. gen. Microleter n. sp. mckinzieorum,species,204049,,Microleter mckinzieorum,NA,species,204049,Tsuji et al.,2010,Chordata,33815,Reptilia,36322,,NA,,NA,204048,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Microleter,n. gen.,NA,NA,"paleoentomology,vertebrate","L. A. Tsuji, J. M_ller, and R. R. Reisz. 2010. Microleter mckinzieorum gen. et sp. nov. from the Lower Permian of Oklahoma: the basalmost parareptile from Laurasia. Journal of Systematic Palaeontology 8(2):245-255",315,334,0,J. Mueller,T. Liebrecht,,25/10/2011 02:57,24/10/2011 10:57,19393,mckinzieorum,Microleter,38310,n. sp.,290.1,268,Leonard,,1,US,Microleter mckinzieorum
1000938,occ,NA,,121601,,n. gen. Tambaroter n. sp. carrolli,species,207729,,Tambaroter carrolli,NA,species,207729,Henrici et al.,2011,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Ostodolepidae,37301,207728,NA,NA,NA,individuals,10.616667,50.783333,Tambach-Dietharz temporary excavation site,NA,type locality of Tambaroter carrolli,DE,Thuringia,Gotha,based on nearby landmark,minutes,hand sample,"""An excavation site for a market in Tambach-Dietharz, Thuringia, Germany. [...] Exact locality information on file at MNG.""",gp_mid,21.71,7.38,305,DE,,Tambach,Rotliegend,Finsterbergen conglomerate,bed,,,,,,,NA,"""The upper [i.e. the Finsterbergen] conglomerate, which is 10 to 50 m thick, contains crystalline clasts derived from the Ruhla crystalline uplift located northwest of the Bromacker locality in addition to rhyolite clasts from the Oberhof uplift. A conglomerate near the top of the exposed section at the discovery site contains crystalline clasts, indicating that the exposed strata are of the upper conglomerate, most likely from the lowermost portion of this unit.""\r\nIn the primary reference the Tambach Fm. is said to to be of Wolfcampian (i.e. early lower Permian) age. Other authors (see here for example), however, favor an assignment to the Kungurian (i.e. late lower Permian). So, assignment of this collection to the Artinskian is a compromise between both views.",No detailed information on the host rock of the Tambaroter skull is given in the reference.,"""siliciclastic""",,,,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,"The Tambach Basin generally is regarded as an intramontane basin (for details see Eberth et al., 2000, Palaios 15(4) pp. 293-313).",macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,,,,,,,,"MNG = Museum der Natur, Gotha",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Tambaroter,n. gen.,NA,NA,vertebrate,"A. C. Henrici, T. Martens, and D. S. Berman, S. S. Sumida. 2011. An Ostodolepid Microsaur۪ (Lepospondyli) from the Lower Permian Tambach Formation of Central Germany. Journal of Vertebrate Paleontology 31(5):997-1004",315,334,0,J. Mueller,T. Liebrecht,,08/12/2011 14:46,07/12/2011 21:46,38771,carrolli,Tambaroter,38771,n. sp.,290.1,279.3,Artinskian,,1,DE,Tambaroter carrolli
1016620,occ,NA,R,80112,,Trematopidae informal new sp.,family,123219,,Trematopidae,NA,family,37047,Martens et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,NA,NA,NA,NA,,10.618889,50.809723,Bromacker Quarry (upper level of Tambach sandstone),NA,,DE,Thuringia,Gotha,based on nearby landmark,seconds,outcrop,"""...middle part of the Thuringian Forest near the village of Tambach-Dietharz and about 20 km south of the town of Gotha, central Germany.""",gp_mid,21.71,7.41,305,DE,,Tambach,Rotliegend,Tambach-Sandstein,group of beds,,,,,,,NA,"""At the Bromacker quarry site are two superimposed stratigraphic successions that can be characterized by their facies associations and are referred to as the Lower Beds and Upper Beds (Eberth et al. 2000). All the vertebrates from the Bromacker quarry come from the Upper Beds [...]. The vertebrates are almost exclusively restricted to two [... horizons ...] which are separated by 50 cm in a stratigraphic interval of 1.2 m."" (Berman et al., 2001)\r\nThe Tambach Formation is of Artinskian age according to ""Stratigraphische Tabelle von Deutschland 2002"", however, a Kungurian age is proposed by L_tzner (2006) in LITHOLEX stratigraphic online database [http://www.bgr.de/app/LithoLex/gesamt_ausgabe_neu.php5?id=25]","""massive, red-brown, very fine-grained sandstone and siltstone"" (Berman et al., 2001).\r\nFor further details see Eberth et al. (2000).",sandstone,"very fine,brown,red",lithified,,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,"""alluvial paleochannel and sheetflood facies and lacustrine suspension deposits"" (Berman et al., 2001).\r\n""During the time that the Lower and Upper beds were deposited, the Tambach Basin was internally-drained and probably characterized by a wet-and-dry tropical or wetter climate that was hot year-round with seasonal-to-subseasonal cycles of rainfall and drying. [...] In the Bromacker area, the floodbasin was never deeply desiccated or heavily vegetated between flooding events."" Eberth et al. (2000).",macrofossils,,,,,,NA,,"body,permineralized",excellent,,snapshot,,,,,,,NA,,,taxonomic,"bulk,field collection",,all macrofossils,,,,,"MNG = Museum der Natur, Gotha",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Trematopidae,,NA,NA,vertebrate,"T. Martens, D. S. Berman, and A. C. Henrici, S. S. Sumida. 2005. The Bromacker Quarry - the Most Important Locality of Lower Permian Terrestrial Vertebrate Fossils Outside of North America. The Nonmarine Permian. New Mexico Museum of Natural History and Science Bulletin 30:214-215",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,15/02/2012 10:55,08/08/2016 04:59,26922,new sp.,,40162,informal,290.1,279.3,Artinskian,,NA,DE, new sp.
1016620,occ,26468,,80112,,n. gen. Rotaryus n. sp. gothae,species,221859,,Rotaryus gothae,NA,species,221859,Berman et al.,2011,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,221858,NA,NA,NA,,10.618889,50.809723,Bromacker Quarry (upper level of Tambach sandstone),NA,,DE,Thuringia,Gotha,based on nearby landmark,seconds,outcrop,"""...middle part of the Thuringian Forest near the village of Tambach-Dietharz and about 20 km south of the town of Gotha, central Germany.""",gp_mid,21.71,7.41,305,DE,,Tambach,Rotliegend,Tambach-Sandstein,group of beds,,,,,,,NA,"""At the Bromacker quarry site are two superimposed stratigraphic successions that can be characterized by their facies associations and are referred to as the Lower Beds and Upper Beds (Eberth et al. 2000). All the vertebrates from the Bromacker quarry come from the Upper Beds [...]. The vertebrates are almost exclusively restricted to two [... horizons ...] which are separated by 50 cm in a stratigraphic interval of 1.2 m."" (Berman et al., 2001)\r\nThe Tambach Formation is of Artinskian age according to ""Stratigraphische Tabelle von Deutschland 2002"", however, a Kungurian age is proposed by L_tzner (2006) in LITHOLEX stratigraphic online database [http://www.bgr.de/app/LithoLex/gesamt_ausgabe_neu.php5?id=25]","""massive, red-brown, very fine-grained sandstone and siltstone"" (Berman et al., 2001).\r\nFor further details see Eberth et al. (2000).",sandstone,"very fine,brown,red",lithified,,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,"""alluvial paleochannel and sheetflood facies and lacustrine suspension deposits"" (Berman et al., 2001).\r\n""During the time that the Lower and Upper beds were deposited, the Tambach Basin was internally-drained and probably characterized by a wet-and-dry tropical or wetter climate that was hot year-round with seasonal-to-subseasonal cycles of rainfall and drying. [...] In the Bromacker area, the floodbasin was never deeply desiccated or heavily vegetated between flooding events."" Eberth et al. (2000).",macrofossils,,,,,,NA,,"body,permineralized",excellent,,snapshot,,,,,,,NA,,,taxonomic,"bulk,field collection",,all macrofossils,,,,,"MNG = Museum der Natur, Gotha",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Rotaryus,n. gen.,NA,NA,vertebrate,"D. S. Berman, A. C. Henrici, and T. Martens, S. S. Sumida, J. S. Anderson. 2011. Rotaryus gothae, a New Trematopid (Temnospondyli: Dissorophoidea) from the Lower Permian of Central Germany. Annals of Carnegie Museum 80(1):49-65",315,334,0,J. Mueller,T. Liebrecht,,21/02/2012 02:30,20/02/2012 09:30,26922,gothae,Rotaryus,40304,n. sp.,290.1,279.3,Artinskian,,NA,DE,Rotaryus gothae
1016622,occ,NA,,80112,,Dissorophidae informal new sp. ,family,37017,obsolete variant of,Dissorophidae,NA,family,37017,Martens et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,NA,NA,NA,NA,,10.618889,50.809723,Bromacker Quarry (upper level of Tambach sandstone),NA,,DE,Thuringia,Gotha,based on nearby landmark,seconds,outcrop,"""...middle part of the Thuringian Forest near the village of Tambach-Dietharz and about 20 km south of the town of Gotha, central Germany.""",gp_mid,21.71,7.41,305,DE,,Tambach,Rotliegend,Tambach-Sandstein,group of beds,,,,,,,NA,"""At the Bromacker quarry site are two superimposed stratigraphic successions that can be characterized by their facies associations and are referred to as the Lower Beds and Upper Beds (Eberth et al. 2000). All the vertebrates from the Bromacker quarry come from the Upper Beds [...]. The vertebrates are almost exclusively restricted to two [... horizons ...] which are separated by 50 cm in a stratigraphic interval of 1.2 m."" (Berman et al., 2001)\r\nThe Tambach Formation is of Artinskian age according to ""Stratigraphische Tabelle von Deutschland 2002"", however, a Kungurian age is proposed by L_tzner (2006) in LITHOLEX stratigraphic online database [http://www.bgr.de/app/LithoLex/gesamt_ausgabe_neu.php5?id=25]","""massive, red-brown, very fine-grained sandstone and siltstone"" (Berman et al., 2001).\r\nFor further details see Eberth et al. (2000).",sandstone,"very fine,brown,red",lithified,,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,"""alluvial paleochannel and sheetflood facies and lacustrine suspension deposits"" (Berman et al., 2001).\r\n""During the time that the Lower and Upper beds were deposited, the Tambach Basin was internally-drained and probably characterized by a wet-and-dry tropical or wetter climate that was hot year-round with seasonal-to-subseasonal cycles of rainfall and drying. [...] In the Bromacker area, the floodbasin was never deeply desiccated or heavily vegetated between flooding events."" Eberth et al. (2000).",macrofossils,,,,,,NA,,"body,permineralized",excellent,,snapshot,,,,,,,NA,,,taxonomic,"bulk,field collection",,all macrofossils,,,,,"MNG = Museum der Natur, Gotha",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Dissorophidae,,NA,NA,vertebrate,"T. Martens, D. S. Berman, and A. C. Henrici, S. S. Sumida. 2005. The Bromacker Quarry - the Most Important Locality of Lower Permian Terrestrial Vertebrate Fossils Outside of North America. The Nonmarine Permian. New Mexico Museum of Natural History and Science Bulletin 30:214-215",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,15/02/2012 10:55,20/02/2012 13:30,26922,new sp. ,,40162,informal,290.1,279.3,Artinskian,,NA,DE, new sp.
1016623,occ,NA,,80112,,Dissorophoidea informal new sp.,unranked clade,175854,,Dissorophoidea,NA,unranked clade,90712,Martens et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,NA,NA,NA,NA,,10.618889,50.809723,Bromacker Quarry (upper level of Tambach sandstone),NA,,DE,Thuringia,Gotha,based on nearby landmark,seconds,outcrop,"""...middle part of the Thuringian Forest near the village of Tambach-Dietharz and about 20 km south of the town of Gotha, central Germany.""",gp_mid,21.71,7.41,305,DE,,Tambach,Rotliegend,Tambach-Sandstein,group of beds,,,,,,,NA,"""At the Bromacker quarry site are two superimposed stratigraphic successions that can be characterized by their facies associations and are referred to as the Lower Beds and Upper Beds (Eberth et al. 2000). All the vertebrates from the Bromacker quarry come from the Upper Beds [...]. The vertebrates are almost exclusively restricted to two [... horizons ...] which are separated by 50 cm in a stratigraphic interval of 1.2 m."" (Berman et al., 2001)\r\nThe Tambach Formation is of Artinskian age according to ""Stratigraphische Tabelle von Deutschland 2002"", however, a Kungurian age is proposed by L_tzner (2006) in LITHOLEX stratigraphic online database [http://www.bgr.de/app/LithoLex/gesamt_ausgabe_neu.php5?id=25]","""massive, red-brown, very fine-grained sandstone and siltstone"" (Berman et al., 2001).\r\nFor further details see Eberth et al. (2000).",sandstone,"very fine,brown,red",lithified,,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,"""alluvial paleochannel and sheetflood facies and lacustrine suspension deposits"" (Berman et al., 2001).\r\n""During the time that the Lower and Upper beds were deposited, the Tambach Basin was internally-drained and probably characterized by a wet-and-dry tropical or wetter climate that was hot year-round with seasonal-to-subseasonal cycles of rainfall and drying. [...] In the Bromacker area, the floodbasin was never deeply desiccated or heavily vegetated between flooding events."" Eberth et al. (2000).",macrofossils,,,,,,NA,,"body,permineralized",excellent,,snapshot,,,,,,,NA,,,taxonomic,"bulk,field collection",,all macrofossils,,,,,"MNG = Museum der Natur, Gotha",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Dissorophoidea,,NA,NA,vertebrate,"T. Martens, D. S. Berman, and A. C. Henrici, S. S. Sumida. 2005. The Bromacker Quarry - the Most Important Locality of Lower Permian Terrestrial Vertebrate Fossils Outside of North America. The Nonmarine Permian. New Mexico Museum of Natural History and Science Bulletin 30:214-215",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,15/02/2012 10:55,20/02/2012 13:33,26922,new sp.,,40162,informal,290.1,279.3,Artinskian,,NA,DE, new sp.
1016624,occ,NA,,80112,,Caseidae informal new sp.,family,38913,,Caseidae,NA,family,38913,Martens et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,NA,NA,NA,NA,,10.618889,50.809723,Bromacker Quarry (upper level of Tambach sandstone),NA,,DE,Thuringia,Gotha,based on nearby landmark,seconds,outcrop,"""...middle part of the Thuringian Forest near the village of Tambach-Dietharz and about 20 km south of the town of Gotha, central Germany.""",gp_mid,21.71,7.41,305,DE,,Tambach,Rotliegend,Tambach-Sandstein,group of beds,,,,,,,NA,"""At the Bromacker quarry site are two superimposed stratigraphic successions that can be characterized by their facies associations and are referred to as the Lower Beds and Upper Beds (Eberth et al. 2000). All the vertebrates from the Bromacker quarry come from the Upper Beds [...]. The vertebrates are almost exclusively restricted to two [... horizons ...] which are separated by 50 cm in a stratigraphic interval of 1.2 m."" (Berman et al., 2001)\r\nThe Tambach Formation is of Artinskian age according to ""Stratigraphische Tabelle von Deutschland 2002"", however, a Kungurian age is proposed by L_tzner (2006) in LITHOLEX stratigraphic online database [http://www.bgr.de/app/LithoLex/gesamt_ausgabe_neu.php5?id=25]","""massive, red-brown, very fine-grained sandstone and siltstone"" (Berman et al., 2001).\r\nFor further details see Eberth et al. (2000).",sandstone,"very fine,brown,red",lithified,,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,"""alluvial paleochannel and sheetflood facies and lacustrine suspension deposits"" (Berman et al., 2001).\r\n""During the time that the Lower and Upper beds were deposited, the Tambach Basin was internally-drained and probably characterized by a wet-and-dry tropical or wetter climate that was hot year-round with seasonal-to-subseasonal cycles of rainfall and drying. [...] In the Bromacker area, the floodbasin was never deeply desiccated or heavily vegetated between flooding events."" Eberth et al. (2000).",macrofossils,,,,,,NA,,"body,permineralized",excellent,,snapshot,,,,,,,NA,,,taxonomic,"bulk,field collection",,all macrofossils,,,,,"MNG = Museum der Natur, Gotha",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Caseidae,,NA,NA,vertebrate,"T. Martens, D. S. Berman, and A. C. Henrici, S. S. Sumida. 2005. The Bromacker Quarry - the Most Important Locality of Lower Permian Terrestrial Vertebrate Fossils Outside of North America. The Nonmarine Permian. New Mexico Museum of Natural History and Science Bulletin 30:214-215",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,15/02/2012 10:55,14/02/2012 18:03,26922,new sp.,,40162,informal,290.1,279.3,Artinskian,,NA,DE, new sp.
1016625,occ,NA,R,80112,,Varanopseidae informal new sp.,family,38892,obsolete variant of,Varanopidae,NA,family,95329,Martens et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,NA,NA,NA,NA,specimens,10.618889,50.809723,Bromacker Quarry (upper level of Tambach sandstone),NA,,DE,Thuringia,Gotha,based on nearby landmark,seconds,outcrop,"""...middle part of the Thuringian Forest near the village of Tambach-Dietharz and about 20 km south of the town of Gotha, central Germany.""",gp_mid,21.71,7.41,305,DE,,Tambach,Rotliegend,Tambach-Sandstein,group of beds,,,,,,,NA,"""At the Bromacker quarry site are two superimposed stratigraphic successions that can be characterized by their facies associations and are referred to as the Lower Beds and Upper Beds (Eberth et al. 2000). All the vertebrates from the Bromacker quarry come from the Upper Beds [...]. The vertebrates are almost exclusively restricted to two [... horizons ...] which are separated by 50 cm in a stratigraphic interval of 1.2 m."" (Berman et al., 2001)\r\nThe Tambach Formation is of Artinskian age according to ""Stratigraphische Tabelle von Deutschland 2002"", however, a Kungurian age is proposed by L_tzner (2006) in LITHOLEX stratigraphic online database [http://www.bgr.de/app/LithoLex/gesamt_ausgabe_neu.php5?id=25]","""massive, red-brown, very fine-grained sandstone and siltstone"" (Berman et al., 2001).\r\nFor further details see Eberth et al. (2000).",sandstone,"very fine,brown,red",lithified,,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,"""alluvial paleochannel and sheetflood facies and lacustrine suspension deposits"" (Berman et al., 2001).\r\n""During the time that the Lower and Upper beds were deposited, the Tambach Basin was internally-drained and probably characterized by a wet-and-dry tropical or wetter climate that was hot year-round with seasonal-to-subseasonal cycles of rainfall and drying. [...] In the Bromacker area, the floodbasin was never deeply desiccated or heavily vegetated between flooding events."" Eberth et al. (2000).",macrofossils,,,,,,NA,,"body,permineralized",excellent,,snapshot,,,,,,,NA,,,taxonomic,"bulk,field collection",,all macrofossils,,,,,"MNG = Museum der Natur, Gotha",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Varanopseidae,,NA,NA,vertebrate,"T. Martens, D. S. Berman, and A. C. Henrici, S. S. Sumida. 2005. The Bromacker Quarry - the Most Important Locality of Lower Permian Terrestrial Vertebrate Fossils Outside of North America. The Nonmarine Permian. New Mexico Museum of Natural History and Science Bulletin 30:214-215",315,334,697,J. Mueller,T. Liebrecht,E. Dunne,15/02/2012 10:55,08/08/2016 04:59,26922,new sp.,,40162,informal,290.1,279.3,Artinskian,,2,DE, new sp.
1016625,occ,32378,,80112,,n. gen. Tambacarnifex n. sp. unguifalcatus,species,292125,,Tambacarnifex unguifalcatus,NA,species,292125,Berman et al.,2014,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,292124,NA,NA,NA,specimens,10.618889,50.809723,Bromacker Quarry (upper level of Tambach sandstone),NA,,DE,Thuringia,Gotha,based on nearby landmark,seconds,outcrop,"""...middle part of the Thuringian Forest near the village of Tambach-Dietharz and about 20 km south of the town of Gotha, central Germany.""",gp_mid,21.71,7.41,305,DE,,Tambach,Rotliegend,Tambach-Sandstein,group of beds,,,,,,,NA,"""At the Bromacker quarry site are two superimposed stratigraphic successions that can be characterized by their facies associations and are referred to as the Lower Beds and Upper Beds (Eberth et al. 2000). All the vertebrates from the Bromacker quarry come from the Upper Beds [...]. The vertebrates are almost exclusively restricted to two [... horizons ...] which are separated by 50 cm in a stratigraphic interval of 1.2 m."" (Berman et al., 2001)\r\nThe Tambach Formation is of Artinskian age according to ""Stratigraphische Tabelle von Deutschland 2002"", however, a Kungurian age is proposed by L_tzner (2006) in LITHOLEX stratigraphic online database [http://www.bgr.de/app/LithoLex/gesamt_ausgabe_neu.php5?id=25]","""massive, red-brown, very fine-grained sandstone and siltstone"" (Berman et al., 2001).\r\nFor further details see Eberth et al. (2000).",sandstone,"very fine,brown,red",lithified,,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,"""alluvial paleochannel and sheetflood facies and lacustrine suspension deposits"" (Berman et al., 2001).\r\n""During the time that the Lower and Upper beds were deposited, the Tambach Basin was internally-drained and probably characterized by a wet-and-dry tropical or wetter climate that was hot year-round with seasonal-to-subseasonal cycles of rainfall and drying. [...] In the Bromacker area, the floodbasin was never deeply desiccated or heavily vegetated between flooding events."" Eberth et al. (2000).",macrofossils,,,,,,NA,,"body,permineralized",excellent,,snapshot,,,,,,,NA,,,taxonomic,"bulk,field collection",,all macrofossils,,,,,"MNG = Museum der Natur, Gotha",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tambacarnifex,n. gen.,NA,NA,vertebrate,"D. S. Berman, A. C. Henrici, and S. S. Sumida, T. Martens, V. Pelletier. 2014. First European record of a Varanodontine (Synapsida: Varanopidae): member of a unique Early Permian upland paleoecosystem, Tambach Basin, central Germany. In C. F. Kammerer, K. D. Angielczyk, J. Fr̦bsich (eds.), Early Evolutionary History of the Synapsida ",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,26/05/2016 17:09,26/05/2016 17:11,26922,unguifalcatus,Tambacarnifex,50796,n. sp.,290.1,279.3,Artinskian,,2,DE,Tambacarnifex unguifalcatus
1019911,occ,NA,,67862,,n. gen. Bolterpeton n. sp. carrolli,species,223734,,Bolterpeton carrolli,NA,species,223734,Anderson and Reisz,2003,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,223733,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Bolterpeton,n. gen.,NA,NA,"paleoentomology,vertebrate","J. S. Anderson and R. R. Reisz. 2003. A new microsaur (Tetrapoda: Lepospondyli) from the Lower Permian of Richards Spur (Fort Sill), Oklahoma. Canadian Journal of Earth Sciences 40(4):499-505",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,27/02/2012 12:31,26/02/2012 20:01,19393,carrolli,Bolterpeton,40439,n. sp.,290.1,268,Leonard,,2,US,Bolterpeton carrolli
1020735,occ,NA,,124949,,Greererpeton burkemorani,species,227037,,Greererpeton burkemorani,NA,species,227037,Godfrey,1988,Chordata,33815,Osteichthyes,34881,,NA,Colosteidae,36975,36977,NA,NA,NA,,-79.848999,39.571999,Greer,NA,,US,West Virginia,Monongalia,,3,,,gp_mid,-28.08,-21,101,US,,Bluefield,,Bickett Shale,member,,,,,,,NA,,,"""shale""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,"vertebrae,limb elements",,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,"selective quarrying,survey of museum collection",,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Greererpeton,,NA,NA,vertebrate,S. J. Godfrey. 1988. Isolated tetrapod remains from the Carboniferous of West Virginia. Kirtlandia 43:27-36,18,385,0,M. Uhen,M. Shalap,,01/03/2012 05:48,29/02/2012 12:48,40904,burkemorani,Greererpeton,40494,,326.4,318.1,Arnsbergian,,NA,US,Greererpeton burkemorani
1020736,occ,NA,,124949,,Proterogyrinus scheelei,species,137378,,Proterogyrinus scheelei,NA,species,137378,Godfrey,1988,Chordata,33815,Osteichthyes,34881,,NA,Proterogyrinidae,37181,37183,NA,NA,NA,,-79.848999,39.571999,Greer,NA,,US,West Virginia,Monongalia,,3,,,gp_mid,-28.08,-21,101,US,,Bluefield,,Bickett Shale,member,,,,,,,NA,,,"""shale""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,"vertebrae,limb elements",,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,"selective quarrying,survey of museum collection",,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Proterogyrinus,,NA,NA,vertebrate,S. J. Godfrey. 1988. Isolated tetrapod remains from the Carboniferous of West Virginia. Kirtlandia 43:27-36,18,385,0,M. Uhen,M. Shalap,,01/03/2012 05:48,29/02/2012 12:48,40904,scheelei,Proterogyrinus,40494,,326.4,318.1,Arnsbergian,,NA,US,Proterogyrinus scheelei
1021829,occ,NA,,125140,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Werneburg et al.,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-106.050003,36.049999,NMMNH 6121,NA,,US,New Mexico,,based on nearby landmark,minutes,,NMMHNH 6121. El Cobre Canyon Formation.,gp_mid,-39.19,-3.1,101,US,,El Cobre Canyon,,,,,,,,,,NA,,"The skull was collected from a muddy sandstone together with bones of an embolomere and Platyhystrix, as well as pelycosaurian-grade synapsids.",sandstone,,,muddy,,,,,,,terrestrial indet.,,,macrofossils,,,,partial skulls,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,field collection,,all macrofossils,,,,,The skull was collected from a muddy sandstone.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,,"R. Werneburg, S. G. Lucas, and J. W. Schneider, L. F. Rinehart. 2010. First Pennsylvanian Eryops (Temnospondyli) and its Permian Record from New Mexico. Bulletin of the New Mexico Museum of Natural History and Science (49):129-136",18,385,0,M. Uhen,M. Shalap,,05/03/2012 13:23,04/03/2012 20:23,40598,sp.,Eryops,40598,,323.2,298.9,Pennsylvanian,,NA,US,Eryops sp.
1021845,occ,NA,,125142,,Zatrachys serratus,species,255221,,Zatrachys serratus,NA,species,255221,Urban and Berman,2007,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,,-80.65139,40.045555,near Elm Groove,NA,,US,West Virginia,Ohio,estimated from map,seconds,small collection,"""Interstate 70 road cut 34 mi east of Elm Grove, Ohio County, West Virginia"" Urban & Berman",gp_mid,-15.21,-3.49,101,US,,Pittsburgh,,Benwood Limestone,,,,,,,,NA,,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,"M. Urban and D. S. Berman. 2007. First occurrence of the late Paleozoic amphibian Zatrachys serratus (Temnospondyli, Zatrachydidae) in the Eastern United States. Annals of Carnegie Museum 76(3):157-164",18,385,697,M. Uhen,M. Shalap,E. Dunne,05/03/2012 15:06,09/08/2016 08:21,40605,serratus,Zatrachys,40605,,303.4,298.9,Virgilian,,NA,US,Zatrachys serratus
1033164,occ,NA,,126535,,Diploceraspis conemaughensis,species,345341,subjective synonym of,Diploceraspis burkei,NA,species,227035,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,specimens,-79.966667,40.444443,Soho Street Quarry,NA,Locality 1 of Moran (1952),US,Pennsylvania,Allegheny,estimated from map,seconds,,"Location details given by Wellstead (1991): ""a quarry on east side of Soho Street, approximately 0.25km north of Fifth Avenue, Pittsburgh, Allegheny County Pennsylvania. The site is now covered by a housing development.""",gp_mid,-15.23,-4.42,101,US,,,Conemaugh,,bed,,,,,,,NA,"""Freshwater limestone bed within the Pittsburgh Limestone, lying 12m below the base of the Conemaugh Group, Upper Pennsylvanian (=Stephanian)"" (Wellstead, 1991)",,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,"CM,MCZ",,,,Burke party,1936,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,697,M. Uhen,M. Uhen,E. Dunne,06/04/2012 04:32,18/07/2016 06:22,41027,conemaughensis,Diploceraspis,41027,,306.95,298.9,Stephanian,,1,US,Diploceraspis conemaughensis
1033165,occ,NA,,126536,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.998055,39.764999,Adams Township,NA,,US,Ohio,Monroe,estimated from map,seconds,,,gp_mid,-15.19,-3,101,US,,Washington,Dunkard,lower,member,,,,,,,NA,,,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,06/04/2012 04:36,05/04/2012 13:36,41027,sp.,Diploceraspis,41027,,306.95,290.1,Stephanian,Sakmarian,NA,US,Diploceraspis sp.
1033218,occ,NA,,126541,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.584999,39.987499,Sand Hill,NA,,US,West Virginia,Marshall,estimated from map,seconds,,,gp_mid,-14.81,-2.91,101,US,,Washington,Dunkard,,,,,,,,,NA,,,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,06/04/2012 08:31,05/04/2012 17:31,41027,sp.,Diploceraspis,41027,,306.95,290.1,Stephanian,Sakmarian,NA,US,Diploceraspis sp.
1033219,occ,NA,,126542,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.823891,39.710278,Proctor,NA,,US,West Virginia,Wetzel,estimated from map,seconds,,,gp_mid,-14.77,-2.55,101,US,,Greene,Dunkard,lower,,,,,,,,NA,,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,06/04/2012 08:37,05/04/2012 17:37,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033220,occ,NA,,126543,,Diploceraspis burkei,species,227035,,Diploceraspis burkei,NA,species,227035,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.549446,39.783054,Liberty District,NA,,US,West Virginia,Marshall,estimated from map,seconds,,,gp_mid,-14.55,-2.56,101,US,,Greene,Dunkard,lower,,,,,,,,NA,,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,697,M. Uhen,M. Uhen,E. Dunne,06/04/2012 08:45,18/07/2016 06:30,41027,burkei,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis burkei
1033221,occ,NA,,126544,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-81.4925,39.046944,Tucker District,NA,,US,West Virginia,Wirt,estimated from map,seconds,,,gp_mid,-15.49,-2.99,101,US,,Greene,Dunkard,middle,,,,,,,,NA,,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,06/04/2012 08:53,05/04/2012 17:53,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033222,occ,NA,,126545,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.774445,39.904167,Clay District,NA,,US,West Virginia,Marshall,estimated from map,seconds,,,gp_mid,-14.67,-2.38,101,US,,Greeene,Dunkard,middle,member,,,,,,,NA,,,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,06/04/2012 09:26,05/04/2012 18:26,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033223,occ,NA,,126546,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-79.840836,39.750557,Springhill Township,NA,,US,West Virginia,Greene,estimated from map,seconds,,,gp_mid,-14.05,-2.78,101,US,,Greene,Dunkard,middle,,,,,,,,NA,,,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,06/04/2012 09:29,05/04/2012 18:29,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033224,occ,NA,,126547,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.601944,39.776943,Meade District,NA,,US,West Virginia,Marshall,estimated from map,seconds,,,gp_mid,-14.59,-2.55,101,US,,Greene,Dunkard,upper,,,,,,,,NA,,,"""limestone""",,,,,,,,,,marine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,18,M. Uhen,M. Uhen,M. Uhen,06/04/2012 09:39,05/04/2012 18:39,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033225,occ,NA,,126548,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.314445,39.677223,Battelle District,NA,,US,West Virginia,Monogalia,estimated from map,seconds,,,gp_mid,-14.42,-2.72,101,US,,Greene,Dunkard,upper,,,,,,,,NA,,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,06/04/2012 09:46,05/04/2012 18:46,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033226,occ,NA,,126549,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.8125,39.796112,Franklin District,NA,,US,West Virginia,Marshall,estimated from map,seconds,,,gp_mid,-14.73,-2.47,101,US,,Greene,Dunkard,upper,,,,,,,,NA,,,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,06/04/2012 09:50,05/04/2012 18:50,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033336,occ,NA,,126570,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.682503,39.870834,Lafayette 5-55,NA,,US,West Virginia,,stated in text,seconds,,0.5 miles E of intersection of W. Va. 89 and US 250 in cut on W. Va. Rt 89,gp_mid,-14.61,-2.44,101,US,,Greene,Dunkard,middle,member,,,,,,,NA,,,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,07/04/2012 05:34,06/04/2012 14:34,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033337,occ,NA,,126571,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.54361,39.992779,Lafayette 6-55,NA,,US,West Virginia,Marshall,stated in text,seconds,outcrop,"0.2-0.3 mi north of boundary of Sherrard on W. VA. Rt. 88, Union District",gp_mid,-14.47,-2.36,101,US,,Greene,Dunkard,middle,member,,,,,,,NA,,lime sandstone,sandstone,,,calcareous,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,07/04/2012 05:37,06/04/2012 14:37,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033338,occ,NA,,126572,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.693054,40.006111,Lafayette 7-55,NA,,US,West Virginia,Marshall,stated in text,seconds,outcrop,"1.5 mi N of north boundary of Sherrard on W. Va. rt. 88, Union District",gp_mid,-14.57,-2.31,101,US,,Greene,Dunkard,middle,member,,,,,,,NA,,,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,07/04/2012 05:41,06/04/2012 14:41,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033340,occ,NA,,126574,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.389725,39.864445,Lafayette 9-55,NA,,US,Pennsylvania,Greene,stated in text,seconds,,"0.7 mi E. of Bristoria on Holbrook Road, Richhill Township",gp_mid,-14.41,-2.52,101,US,,Greene,Dunkard,lower,member,,,,,,,NA,,,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,07/04/2012 05:46,06/04/2012 14:46,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033341,occ,NA,,126575,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.400002,39.66,Lafayette 13-55,NA,Locality 28 of Moran,US,West Virginia,Monongalia,stated in text,seconds,,Battelle District,gp_mid,-14.49,-2.71,101,US,,Greene,Dunkard,upper,member,,,,,,,NA,,,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,07/04/2012 05:50,06/04/2012 14:50,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033343,occ,NA,,126577,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.573059,39.633331,Lafayette 15-55,NA,,US,West Virginia,Wetzel,stated in text,minutes,,"ridge crest west of Uniontown on W. Va. Rt. 7, Center District",gp_mid,-14.62,-2.69,101,US,,Greene,Dunkard,upper,member,,,,,,,NA,,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,07/04/2012 05:52,06/04/2012 14:52,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033344,occ,NA,,126578,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.531113,39.646389,Lafayette 17-55,NA,,US,West Virginia,Wetzel,stated in text,seconds,,"on east side of hill east of Knob Fork, Center District",gp_mid,-14.58,-2.69,101,US,,Greene,Dunkard,middle,member,,,,,,,NA,,,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,07/04/2012 05:54,06/04/2012 14:54,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033345,occ,NA,,126579,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.844444,39.773609,Lafayette 18-55,NA,,US,West Virginia,Marshall,stated in text,seconds,,"road running SE to Wayne Ridge from W. Va. Rt. 2 just north of Kent, Franklin District",gp_mid,-14.77,-2.49,101,US,,Greene,Dunkard,middle,member,,,,,,,NA,,,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,07/04/2012 05:56,06/04/2012 14:56,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033346,occ,NA,,126580,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.64917,39.623055,Lafayette 21-55,NA,,US,West Virginia,Wetzel,stated in text,seconds,,"Great House Hill Road north of W. Va. Rt. 7, 0.5 miles east of Wileyville, Center District",gp_mid,-14.68,-2.68,101,US,,Greene,Dunkard,upper,member,,,,,,,NA,,,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,07/04/2012 05:58,06/04/2012 14:58,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033347,occ,NA,,126581,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.701942,39.625,Lafayette 22-55,NA,,US,West Virginia,Wetzel,stated in text,seconds,,"Brock Ridge Road north of W. Va. Rt. 7, about 1 mi. west of Wileyville, Proctor District",gp_mid,-14.72,-2.66,101,US,,Greene,Dunkard,middle,member,,,,,,,NA,,,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,07/04/2012 06:00,06/04/2012 15:00,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033348,occ,NA,,126582,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-81.461113,39.241669,Lafayette 1-56,NA,,US,West Virginia,Wood,estimated from map,seconds,,"2.0-1.75 miles west of Murphytown on U.S. Rt. 50, Clay District",gp_mid,-15.4,-2.81,101,US,,Greene,Dunkard,middle,member,,,,,,,NA,,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,07/04/2012 06:03,06/04/2012 15:03,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033349,occ,NA,,126583,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-81.413887,39.244446,Lafayette 2-56,NA,,US,West Virginia,Wood,stated in text,seconds,,"Montgomery Hill east of Murphytown on U.S. Rt. 50, Clay district",gp_mid,-15.37,-2.82,101,US,,Greene,Dunkard,mdidle,member,,,,,,,NA,,,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,07/04/2012 06:05,06/04/2012 15:05,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1033350,occ,NA,,126584,,Diploceraspis sp.,genus,37265,,Diploceraspis,NA,genus,37265,Beerbower,1963,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-81.538887,39.048058,Lafayette 4-56,NA,,US,West Virginia,Wood,stated in text,seconds,,Limestone Hill on Gates Road 0.4 mi west of US 21 (probably Moran's localities L and 31),gp_mid,-15.53,-2.97,101,US,,Greene,Dunkard,upper,member,,,,,,,NA,,,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"J. R. Beerbower. 1963. Morphology, paleoecology, and phylogeny of the Permo-Pennsylvania amphibian Diploceraspis. Bulletin of the Museum of Comparative Zoology 130:31-108",18,18,0,M. Uhen,M. Uhen,,07/04/2012 06:07,06/04/2012 15:07,41027,sp.,Diploceraspis,41027,,295.5,290.1,Sakmarian,,NA,US,Diploceraspis sp.
1037627,occ,NA,,127038,,Megamolgophis agostini,species,37323,species not entered,Megamolgophis,NA,genus,37323,Wellstead,2005,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37323,NA,NA,NA,,-81.376114,39.064999,Limestone Hill,NA,,US,Maryland,,estimated from map,seconds,,,gp_mid,-15.4,-3,101,US,,Greene,Dunkard,,,,,,,,,NA,"""In the early 1930s, R. W. Whipple of Marietta College (Ohio) collected two series of lepospondylous vertebrae from the Ninevah Limestone (Greene Formation, Dunkard Group, Permian) at Limestone Hill, WV.""",,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,many,vertebrae,,,NA,"""One specimen consists of an articulated series of approximately 17 dorsal and six caudal vertebrae. The dorsal centra are large for a lepospondyl (1.6 cm long). The caudal centra, seemingly from tail's end, are smaller, approximately 0.5 cm long. The second specimen consists of two articulated, but fragmentary, caudal vertebrae whose centra are about 1.5 cm long.""",body,,,,,,,,,,NA,,,general faunal/floral,survey of museum collection,,,2 specimens,,R. W. Whipple,Early 1930s,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Megamolgophis,,NA,NA,,"C. Wellstead. 2005. R. W. Whipple's specimens referable to Megamolgophis agostini Romer, 1952 (Amphibia, Lepospondyli). Journal of Vertebrate Paleontology 25(3):128A",18,385,0,M. Uhen,M. Shalap,,23/04/2012 07:40,22/04/2012 16:40,41252,agostini,Megamolgophis,41252,,295.5,290.1,Sakmarian,,NA,US,Megamolgophis agostini
1037998,occ,NA,,127110,,Zatrachys serratus,species,255221,,Zatrachys serratus,NA,species,255221,Urban and Berman,2007,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,,-80.65139,40.045555,near MacDale,NA,,US,West Virginia,Monongalia,estimated from map,seconds,small collection,"""road cut at the intersection of Route 7 and Delta Road 48 to Brave, Pennsylvania, west of Blacksville, Monongalia County, West Virginia"" Urban & Berman",gp_mid,-14.31,-1.83,101,US,,Washington,,Middle Washington Limestone,member,,,,,,,NA,,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,"M. Urban and D. S. Berman. 2007. First occurrence of the late Paleozoic amphibian Zatrachys serratus (Temnospondyli, Zatrachydidae) in the Eastern United States. Annals of Carnegie Museum 76(3):157-164",18,385,697,M. Uhen,M. Shalap,E. Dunne,25/04/2012 08:18,09/08/2016 08:22,40605,serratus,Zatrachys,40605,,296.4,268,Wolfcamp,,NA,US,Zatrachys serratus
1038047,occ,NA,,125947,,Reptilia indet.,class,36322,,Reptilia,NA,class,36322,Tilton,1926,Chordata,33815,Reptilia,36322,,NA,,NA,NA,NA,NA,NA,,-80.856392,39.365833,"Island Creek, near West Union",NA,,US,West Virginia,,estimated from map,seconds,,,gp_mid,-13.24,0.45,101,US,,Waynesburg,Dunkard,,formation,,,,,,,NA,, waterhole bonebeds,sandstone,,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,trace,,,,,,,,,,NA,,footprints,general faunal/floral,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Reptilia,,NA,NA,,J. L. Tilton. 1926. Permian vertebrates from West Virginia. Bulletin of the Geological Society of America 37:385-396,18,18,18,M. Uhen,M. Uhen,M. Uhen,26/04/2012 01:00,25/04/2012 10:01,40891,indet.,,40891,,298.9,252.17,Permian,,NA,US, indet.
1038738,occ,NA,R,127181,,Pareiasaurus ? n. sp. henneni,species,233434,,Pareiasaurus henneni,NA,species,233434,Case,1917,Chordata,33815,Reptilia,36322,,NA,,NA,37564,NA,NA,NA,specimens,-80.615829,38.768612,Saltlick Bridge,NA,,US,West Virginia,Braxton,estimated from map,seconds,,"Braxon County, West Virginia, 0.7 mile north of Saltlick Bridge P.O., on the west side of the public road and west hillside, at an elevation of 975 to 1000 ft above sea level",gp_mid,-13.27,-0.17,101,US,,,Monongahela,,,,,,,,,NA,"""Monongahela Series""",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,none,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,,,,,,,,,terrestrial,NA,actively mobile,,NA,herbivore,,,hydroxyapatite,,NA,,Pareiasaurus,?,NA,NA,vertebrate,"E. C. Case. 1917. Notes on the possible evidence of the presence of a Pareiasaurus-like reptile in the Conemaugh Series of West Virginia. In R. V. Hennen (ed.), West Virginia Geological Survey: Braxton and Clay Counties ",18,18,327,M. Uhen,M. Uhen,R. Butler,02/05/2012 01:09,09/07/2015 09:35,NA,henneni,Pareiasaurus,41362,n. sp.,298.9,252.17,Permian,,1,US,Pareiasaurus henneni
1058895,occ,NA,,130829,,Labyrinthodontia indet.,superorder,95779,,Labyrinthodontia,NA,superorder,36960,Schultze,1985,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,,-96.697998,37.250999,"Road cut on Hwy 38, Cowley Co., low. low. up. Speiser Sh.",NA,,US,Kansas,Cowley,estimated from map,3,,"Road cut on KS Hwy. 38, SE 1/4 SE 1/4 sec. 20, T. 32S., R. 7E., Cowley Co.",gp_mid,-27.01,0.67,101,US,,Speiser Shale,Chase,,,,,,,,,NA,"Low. low. up. Speiser Sh.\r\nVertebrate remains extracted from the same horizons throughout the Wreford Megacyclothem, Chase Group, Gearyan Stage, Lower Permian.",,"""shale""",green,lithified,,,"""limestone""",,,,,offshore,,,macrofossils,,,,,,NA,,"body,mold/impression",,,,,,,,,,NA,,,taxonomic,acetic,,,,,,,"Repository: Museum of Natural History, University of Kansas (KUVP)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Labyrinthodontia,,NA,NA,vertebrate,H. Schultze. 1985. Marine to Onshore Vertebrates in the Lower Permian of Kansas and their Paleoenvironmental Implications. University of Kansas Paleontological Contributions 113:1-18,166,513,513,M. Clapham,P. Vazquez,P. Vazquez,14/07/2012 09:41,13/07/2012 18:44,42284,indet.,,42284,,295.5,290.1,Sakmarian,,NA,US, indet.
1064710,occ,NA,,131670,,Silvanerpeton miripedes,species,243094,,Silvanerpeton miripedes,NA,species,243094,Clack,1994,Chordata,33815,Osteichthyes,34881,,NA,,NA,243093,NA,NA,NA,specimens,-3.2,55.950001,"Dry stone wall (Wall F), near East Kirkton",NA,,UK,Scotland,West Lothian,based on nearby landmark,4,basin,,gp_mid,-4.83,-20.31,313,UK,,East Kirkton Limestone,Upper Oil Shale,,bed,,,,,,,NA,Units assumed based on East Kirkton locality (22725),,not reported,,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,mold/impression",,,,,,,,,,NA,,,taxonomic,"salvage,peel or thin section,field collection",,,,,S. P. Wood,1980s,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Silvanerpeton,,NA,NA,,"J. A. Clack. 1994. Silvanerpeton miripedes, a new anthracosauroid from the Vis̩an of East Kirkton, West Lothian, Scotland. Transactions of the Royal Society of Edinburgh: Earth Sciences 84:369-376",447,447,0,R. Benson,R. Benson,,27/07/2012 19:43,27/07/2012 04:43,42473,miripedes,Silvanerpeton,42473,,336,326.4,Brigantian,,1,UK,Silvanerpeton miripedes
1064711,occ,NA,,22725,,Ophiderpeton n. sp. kirktonense,species,243096,,Ophiderpeton kirktonense,NA,species,243096,Milner,1994,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Ophiderpetontidae,37252,37254,NA,NA,NA,specimens,-3.2,55.950001,East Kirkton site (Units 70-82: East Kirkton Limestone),NA,ETE Locality 1604,UK,Scotland,West Lothian,based on nearby landmark,4,basin,"East Kirkton quarry, near Bathgate, West Lothian, Scotland; ca. 27 km W of Edinburgh (Grid reference NS 991690).",gp_mid,-4.83,-20.31,313,UK,,East Kirkton Limestone,Upper Oil Shale,East Kirkton Limestone,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min. Bed 82 - bed ""b""; lower part of Brigantian","Many specimens are from Unit 82, 'the black shale member'. But others come from the range of units 70-82, including adjacent limestone units or spoil heaps at East Kirkton.","""shale""",black,,,Y,"""limestone""",,,,Y,spring,,"ETE sed env 1: volcanic, ETE sed env 2: spring ETE event: ., ETE env comment: toxic water poss.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: attritional, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",general faunal/floral,"selective quarrying,surface (in situ),mechanical,field collection",BMNH,,66 specimens,,S. P. Wood,1988,"ETE reference list: 478, 479, 483, 482\r\nNMS (National Museum of Scotland, Edinburgh), UMZC (University Museum of Zoology, Cambridge), and GLAHM (Hunerian Museum, Glasgow) collections",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Ophiderpeton,,NA,NA,,"A. C. Milner. 1994. The astopod amphibian from the Vis̩an of East Kirkton, West Lothian, Scotland. Transactions of the Royal Society of Edinburgh: Earth Sciences 84:363-368",447,447,0,R. Benson,R. Benson,,27/07/2012 19:52,27/07/2012 04:52,4596,kirktonense,Ophiderpeton,42474,n. sp.,336,326.4,Brigantian,,4,UK,Ophiderpeton kirktonense
1064712,occ,NA,,22725,,Temnospondyli informal large taxon,species,152955,species not entered,Temnospondyli,NA,unranked clade,36320,Milner and Sequeira,1994,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,NA,NA,NA,NA,specimens,-3.2,55.950001,East Kirkton site (Units 70-82: East Kirkton Limestone),NA,ETE Locality 1604,UK,Scotland,West Lothian,based on nearby landmark,4,basin,"East Kirkton quarry, near Bathgate, West Lothian, Scotland; ca. 27 km W of Edinburgh (Grid reference NS 991690).",gp_mid,-4.83,-20.31,313,UK,,East Kirkton Limestone,Upper Oil Shale,East Kirkton Limestone,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min. Bed 82 - bed ""b""; lower part of Brigantian","Many specimens are from Unit 82, 'the black shale member'. But others come from the range of units 70-82, including adjacent limestone units or spoil heaps at East Kirkton.","""shale""",black,,,Y,"""limestone""",,,,Y,spring,,"ETE sed env 1: volcanic, ETE sed env 2: spring ETE event: ., ETE env comment: toxic water poss.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: attritional, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",general faunal/floral,"selective quarrying,surface (in situ),mechanical,field collection",BMNH,,66 specimens,,S. P. Wood,1988,"ETE reference list: 478, 479, 483, 482\r\nNMS (National Museum of Scotland, Edinburgh), UMZC (University Museum of Zoology, Cambridge), and GLAHM (Hunerian Museum, Glasgow) collections",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Temnospondyli,,NA,NA,,"A. R. Milner and S. E. K. Sequeira. 1994. The temnospondyl amphibians from the Vis̩an of East Kirkton, West Lothian, Scotland. Transactions of the Royal Society of Edinburgh: Earth Sciences 84:331-361",447,447,447,R. Benson,R. Benson,R. Benson,27/07/2012 20:02,27/07/2012 05:04,4596,large taxon,,42475,informal,336,326.4,Brigantian,,3,UK, large taxon
1071216,occ,NA,,67862,,n. gen. Feeserpeton n. sp. oklahomensis,species,246046,,Feeserpeton oklahomensis,NA,species,246046,MacDougall and Reisz,2012,Chordata,33815,Reptilia,36322,,NA,,NA,246045,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Feeserpeton,n. gen.,NA,NA,"paleoentomology,vertebrate","M. J. MacDougall and R. Reisz. 2012. A new parareptile (Parareptilia, Lanthanosuchoidea) from the Early Permian of Oklahoma. Journal of Vertebrate Paleontology 32(5):1018-1026",447,447,334,R. Benson,R. Benson,T. Liebrecht,29/08/2012 18:11,13/01/2016 17:46,19393,oklahomensis,Feeserpeton,42791,n. sp.,290.1,268,Leonard,,1,US,Feeserpeton oklahomensis
1091168,occ,NA,,87877,,n. gen. Spinarerpeton n. sp. brevicephalum,species,252454,,Spinarerpeton brevicephalum,NA,species,252454,Klembara,2009,Chordata,33815,Osteichthyes,34881,,NA,Discosauriscidae,37207,252452,NA,NA,NA,individuals,16.612778,49.565277,"Kochov, Boskovice Furrow",NA,Boskovice Basin,CZ,Moravia,,based on nearby landmark,seconds,small collection,"Boskovice Furrow (or Boskovice Basin) in Moravia (Czech Republic); Kochov-L, about 500 m NE from Kochov (near Letovice).",gp_mid,25.35,6.67,305,CZ,,Middle Letovice,,,bed,Xenacanthus decheni,,,,,,NA,"Xenacanthus decheni (Goldfuss, 1847) biozone, Middle Letovice Formation, Autunian, Lower Permian","""laminated limestone""","""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,some,,,skeletons,,NA,,body,good,,snapshot,,,,,,,NA,,,taxonomic,chemical,,,,,,,"SNM: Slovak National Museum in Bratislava, Slovakia.",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Spinarerpeton,n. gen.,NA,NA,vertebrate,J. Klembara. 2009. The skeletal anatomy and relationships of a new discosauriscid seymouriamorph from the Lower Permian of Moravia (Czech Republic). Annals of Carnegie Museum 77(4):451-483,327,327,0,R. Butler,R. Butler,,11/12/2012 06:58,10/12/2012 13:58,43843,brevicephalum,Spinarerpeton,43843,n. sp.,298.9,295,Autunian,,1,CZ,Spinarerpeton brevicephalum
1091172,occ,NA,,79163,,n. gen. Lupeosaurus n. sp. kayi,species,252456,"subjective synonym of, species not entered",Eryops,NA,genus,37011,Romer,1937,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,individuals,-98.777496,33.449722,Cottonwood Creek (Moran Fm.),NA,Locality IIb (Romer & Price),US,Texas,Archer,estimated from map,seconds,outcrop,"Cottonwood Creek is a tributary of the south fork of the Little Wichita River (about 10 miles south of Archer City). Locality is ""near the head of Cottonwood Creek, close to the southern border of Archer Co."" (Romer & Price, 1940) ",gp_mid,-30.65,-2.02,101,US,,Archer City,Wichita,,group of beds,,,,,,,NA,"""about 50 feet below the Sedwick limestone equivalent"" (Clark & Carroll, 1973)\r\nThe former Moran Formation comprises the lower part of the Archer City Formation (Hentz, 1988, The University of Texas at Austin, Bureau of Economic Geology, Report of Investigations, 170).",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,observed (not collected),MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Lupeosaurus,n. gen.,NA,NA,vertebrate,A. S. Romer. 1937. New genera and species of pelycosaurian reptiles. Proceedings of the New England Zo̦logical Club 16:89-95,14,14,0,M. Carrano,M. Carrano,,11/12/2012 07:38,10/12/2012 14:38,28415,kayi,Eryops,43845,n. sp.,298.9,295.5,Asselian,,1,US,Eryops kayi
1091174,occ,NA,,28267,,Dimetrodon n. sp. kempae,species,123426,nomen dubium,Sphenacodontidae,NA,family,38901,Romer,1937,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,NA,NA,NA,NA,specimens,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1937. New genera and species of pelycosaurian reptiles. Proceedings of the New England Zo̦logical Club 16:89-95,14,14,0,M. Carrano,M. Carrano,,11/12/2012 07:48,10/12/2012 14:48,9228,kempae,,43845,n. sp.,279.3,272.3,Kungurian,,1,US, kempae
1091175,occ,NA,,28267,,Dimetrodon n. sp. loomisi,species,90738,,Dimetrodon loomisi,NA,species,90738,Romer,1937,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,specimens,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,A. S. Romer. 1937. New genera and species of pelycosaurian reptiles. Proceedings of the New England Zo̦logical Club 16:89-95,14,14,0,M. Carrano,M. Carrano,,11/12/2012 07:48,10/12/2012 14:48,9228,loomisi,Dimetrodon,43845,n. sp.,279.3,272.3,Kungurian,,1,US,Dimetrodon loomisi
1098337,occ,NA,,67862,,n. gen. Orovenator n. sp. mayorum,species,64877,,Orovenator mayorum,NA,species,64877,Reisz et al.,2011,Chordata,33815,Reptilia,36322,Eosuchia,37795,,NA,64876,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Orovenator,n. gen.,NA,NA,"paleoentomology,vertebrate","R. R. Reisz, S. P. Modesto, and D. M. Scott. 2011. A new Early Permian reptile and its significance in early diapsid evolution. Proceedings of the Royal Society B 278 :3731-3737",315,334,0,J. Mueller,T. Liebrecht,,25/01/2013 10:08,24/01/2013 17:08,19393,mayorum,Orovenator,44430,n. sp.,290.1,268,Leonard,,2,US,Orovenator mayorum
1202387,occ,NA,,68427,,n. gen. Eocasea n. sp. martini,species,292123,,Eocasea martini,NA,species,292123,Reisz and Fr̦bisch,2014,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,292122,NA,NA,NA,individuals,-96.113892,37.986111,Hamilton Quarry,NA,,US,Kansas,Greenwood,estimated from map,seconds,,"about 5 km E of Hamilton, Greenwood Co., Kansas, in secs. 5 and 6, T. 24 S., R. 12 E. (Virgil 7.5' quadrangle)",gp_mid,-26.91,-0.1,101,US,,Calhouns Shale,Shawnee,,,,,,,,,NA,"Virgillian Series, Upper Pennsylvanian; late Kasimovian according to Modesto et al. (2015)",,"""shale""",,,,,,,,,,estuary/bay,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Eocasea,n. gen.,NA,NA,vertebrate,"R. R. Reisz and J. Fr̦bisch. 2014. The oldest caseid synapsid from the Late Pennsylvanian of Kansas, and the evolution of herbivory in terrestrial vertebrates. PLoS One 9(4):e94518",447,447,0,R. Benson,R. Benson,,17/04/2014 04:12,17/04/2014 04:12,19706,martini,Eocasea,50795,n. sp.,303.4,298.9,Virgilian,,1,US,Eocasea martini
1211081,occ,NA,,157227,,n. gen. Palaeogyrinus n. sp. decorus,species,296846,recombined as,Palaeoherpeton decorum,NA,species,296846,Watson,1926,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37192,NA,NA,NA,individuals,-2.996578,56.19632,Pirnie Colliery,NA,,UK,Scotland,Fifeshire,,6,small collection,"Pirnie colliery, Fifeshire",gp_mid,5.7,0.38,313,UK,,Parrot Coal,,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,some,,,,,NA,,body,good,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,J. W. Kirkby,,"orig. in Hancock Museum, Newcastle",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Palaeogyrinus,n. gen.,NA,NA,vertebrate,"D. M. S. Watson. 1926. Croonian lecture.The evolution and origin of the Amphibia. Proceedings of the Royal Society of London, Series B 214:189-257",14,14,0,M. Carrano,M. Carrano,,09/06/2014 15:28,09/06/2014 15:28,57610,decorus,Palaeoherpeton,51608,n. sp.,313.8,311.45,Kashirian,,1,UK,Palaeoherpeton decorus
1226616,occ,NA,,161206,,n. gen. Alierasaurus n. sp. ronchii,species,69704,,Alierasaurus ronchii,NA,species,69704,Romano and Nicosia,2014,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,304604,NA,NA,NA,specimens,8.426949,40.641567,Promontory of Torre del Porticciolo,NA,,IT,Sardinia,,based on nearby landmark,6,small collection,,gp_mid,NA,NA,coordinates not computable using this model,IT,,Cala del Vino,,,bed,,,,,,,NA,late early Permian to early middle Permian in age (here treated as Artinskian-Roadian),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Alierasaurus,n. gen.,NA,NA,vertebrate,"M. Romano and U. Nicosia. 2014. Alierasaurus ronchii, gen. et sp. nov., a caseid from the Permian of Sardinia, Italy. Journal of Vertebrate Paleontology 34(4):900-913",18,18,0,M. Uhen,M. Uhen,,02/09/2014 18:21,02/09/2014 18:21,52526,ronchii,Alierasaurus,52526,n. sp.,290.1,268.8,Artinskian,Roadian,1,IT,Alierasaurus ronchii
1237952,occ,NA,,163064,,n. gen. Perryella n. sp. olsoni,species,242727,,Perryella olsoni,NA,species,242727,Carlson,1987,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,242726,NA,NA,NA,specimens,-97.329308,36.339088,Perry site 5,NA,,US,Oklahoma,Noble,stated in text,5,small collection,"roadcut 0.24 mi. S of NE 1/4, sec 32, T22N, R1W",gp_mid,-27.34,1.22,101,US,,Wellington,Sumner,,bed,,,,,,,NA,"middle of formation, 0.9 m above ""insect beds""",,not reported,burrows,,,Y,,,,,,lacustrine - small,foreland basin,"""a floodplain lake or pond""",macrofossils,,some,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection",,,,,E. C. Olson,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Perryella,n. gen.,NA,NA,vertebrate,"K. J. Carlson. 1987. Perryella, a new temnospondylous amphibian from the Lower Permian of Oklahoma. Journal of Paleontology 61(1):135-147",14,14,0,M. Carrano,M. Carrano,,10/10/2014 16:03,10/10/2014 16:03,42433,olsoni,Perryella,42433,n. sp.,290.1,268,Leonard,,18,US,Perryella olsoni
1237954,occ,NA,,163064,,Crossotelos sp.,genus,37271,,Crossotelos,NA,genus,37271,Carlson,1987,Chordata,33815,Osteichthyes,34881,,NA,Urocordylidae,37270,37271,NA,NA,NA,,-97.329308,36.339088,Perry site 5,NA,,US,Oklahoma,Noble,stated in text,5,small collection,"roadcut 0.24 mi. S of NE 1/4, sec 32, T22N, R1W",gp_mid,-27.34,1.22,101,US,,Wellington,Sumner,,bed,,,,,,,NA,"middle of formation, 0.9 m above ""insect beds""",,not reported,burrows,,,Y,,,,,,lacustrine - small,foreland basin,"""a floodplain lake or pond""",macrofossils,,some,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection",,,,,E. C. Olson,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Crossotelos,,NA,NA,vertebrate,"K. J. Carlson. 1987. Perryella, a new temnospondylous amphibian from the Lower Permian of Oklahoma. Journal of Paleontology 61(1):135-147",14,14,0,M. Carrano,M. Carrano,,10/10/2014 16:03,10/10/2014 16:03,42433,sp.,Crossotelos,42433,,290.1,268,Leonard,,NA,US,Crossotelos sp.
1242744,occ,NA,,28256,,n. gen. Anisodexis n. sp. imbricarius,species,309178,subjective synonym of,Eryops megacephalus,NA,species,70397,Cope,1882,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,individuals,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Anisodexis,n. gen.,NA,NA,vertebrate,E. D. Cope. 1882. Third contribution to the history of the Vertebrata of the Permian formation of Texas. Proceedings of the American Philosophical Society 20:447-461,14,14,0,M. Carrano,M. Carrano,,12/11/2014 17:12,12/11/2014 17:12,17702,imbricarius,Eryops,17702,n. sp.,279.3,272.3,Kungurian,,1,US,Eryops imbricarius
1247644,occ,NA,,164623,,Belebey n. sp. augustodunensis,species,310820,,Belebey augustodunensis,NA,species,310820,Falconnet,2012,Chordata,33815,Reptilia,36322,,NA,Bolosauridae,37510,137775,NA,NA,NA,individuals,4.301111,46.950832,Autunois Bolosauridae,NA,,FR,Burgundy,Sa̫ne-et-Loire,based on nearby landmark,seconds,small collection,"""Exact provenance unknown, Autunois, Sa̫ne-et-Loire, Burgundy, France."" Coordinates based on Autun",gp_mid,18,1.68,305,FR,,Millery,,,bed,,,,,,,NA,"""Bituminous beds of the Autunian۪ series, Autun basin. There was unfortunately no indication of the geographical or stratigraphical provenance on the label found with MNHN.F.AUT 891 or in the registration catalogue when it was originally numbered R-142. However, the preservation state of the specimen, as well as its embedding matrix, are very similar than those of the holotype of Haptodus baylei (MNHN 1884-26-3A and B), therefore suggesting MNHN.F.AUT 891 was collected from the same Millery Formation. Notwithstanding these uncertainties, MNHN.F.AUT 891 can be relatively well dated, thanks to the abundant macro- and microflora produced by the whole Autunian۪ series (Moloy to Millery formations) [e.g., Ch̢teauneuf et al., 1992; Broutin et al., 1999]. A similar Autunian flora have indeed been identified in other Peri-Tethyan basins, notably in the Donets basin [Izart, Briand et al., 1998; Broutin in Izart, Vaslet et al., 1998; Stchegolev in Izart, Vaslet et al., 1998] in which the presence of marine interbedding allowed the stratigraphic correlation of the Autunian with the late Gzhelian (= Orenburgian Russian stage) to Asselian interval on the basis of fusulinids and conodonts [Izart, Briand et al., 1998; Izart, Vaslet et al., 1998]. In the Donets basin, the underlying Stephanian C۪ is correlated to the early Gzhelian (= Gzhelian sensu stricto Russian stage), but the Stephanian C۪/Autunian boundary remains uncertain as long as the Autunian can be defined by either the First Appearance Datum (FAD) or the acme of meso-xerophytic flora [Izart, Vaslet et al., 1998]. In addition, the absence of younger flora precludes the identification of the upper Autunian boundary in the overlying early Sakmarian strata.""",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,none,some,,,,NA,,body,medium,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,MNHN,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Belebey,,NA,NA,vertebrate,J. Falconnet. 2012. First evidence of a bolosaurid parareptile in France (latest Carboniferous-earliest Permian of the Autun basin) and the spatiotemporal distribution of the Bolosauridae. Bulletin de la Soci̩t̩ g̩ologique de France 183(6):495-508,327,327,0,R. Butler,R. Butler,,07/12/2014 09:36,07/12/2014 09:36,53781,augustodunensis,Belebey,53781,n. sp.,303.7,295.5,Gzhelian,Asselian,1,FR,Belebey augustodunensis
1252540,occ,NA,,165526,,n. gen. Ctenerpeton n. sp. alveolatum,species,227032,subjective synonym of,Ctenerpeton remex,NA,species,320823,Cope,1897,Chordata,33815,Osteichthyes,34881,,NA,Urocordylidae,37270,37272,NA,NA,NA,individuals,-80.474998,40.798,Cannelton,NA,,US,Pennsylvania,Beaver,based on nearby landmark,3,small collection,Coordinates based on the location of Cannelton,gp_mid,-21.08,-11.59,101,US,,Upper Kittanning Coal,Allegheny,,group of beds,,,,,,,NA,"""Coal Measures""",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,many,,,,,NA,,"body,adpression",,,snapshot,,dispersed,,,,,NA,,,taxonomic,survey of museum collection,,,,,R. D. Lacoe,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Ctenerpeton,n. gen.,NA,NA,vertebrate,"E. D. Cope. 1897. On New Paleozoic Vertebrata from Illinois, Ohio and Pennsylvania. Proceedings of the American Philosophical Society 36:71-91",14,14,0,M. Carrano,M. Carrano,,21/01/2015 16:10,21/01/2015 16:10,28740,alveolatum,Ctenerpeton,28740,n. sp.,318.1,306.95,Westphalian,,1,US,Ctenerpeton alveolatum
1284666,occ,NA,,80714,,Reptilia indet.,class,36322,,Reptilia,NA,class,36322,Paton,1975,Chordata,33815,Reptilia,36322,,NA,,NA,NA,NA,NA,NA,specimens,-87.775002,40.108334,Danville Locality (Vertebrates),NA,Oakwood Locality; Horseshoe Bend; Vermillion River; Illinois bonebed,US,Illinois,Vermilion,based on nearby landmark,seconds,outcrop,"""the well-known Danville or 'Oakwood' locality [...] Horseshoe Bend locality near the SE/C of Sec. 23-19N-13W"" (DeMar, 1970)\r\n""Vermilion River, near Danville"" (Reisz, 1986)\r\nLat Long is for Oakwood",gp_mid,-21.51,-3.52,101,US,,Bond,McLeansboro,,group of beds,,,,,,,NA,"""We believe the vertebrates have been collected from a zone 10 feet or so below the Shoal Creek Member of the Bond Formation"" (DeMar, 1970)\r\nNote: Shoal Creek Member is equivalent to Carthage Limestone Member, a name now used throughout the Illinois Basin for that lithological unit; see Jacobson (2002) A summary of references with changes in Pennsylvanian stratigraphic nomenclature at the ISGS since Bulletin 95. [Online] http://www.isgs.illinois.edu/maps-data-pub/coal-maps/pennstratigraphy.shtml ",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Reptilia,,NA,NA,vertebrate,"R. L. Paton. 1975. A Catalogue of Fossil Vertebrates in the Royal Scottish Museum, Edinburgh. Part Four / Amphibia & Reptilia. Royal Scottish Museum Information Series. Geology 5 ",14,14,0,M. Carrano,M. Carrano,,29/06/2015 11:47,29/06/2015 11:47,28640,indet.,,55639,,305.9,303.4,Missourian,,4,US, indet.
1285848,occ,NA,,171344,,n. gen. Erpetonyx n. sp. arsenaultorum,species,324114,,Erpetonyx arsenaultorum,NA,species,324114,Modesto et al.,2015,Chordata,33815,Reptilia,36322,,NA,,NA,324113,NA,NA,NA,individuals,-64.099998,46.402779,Cape Egmont,NA,,CA,Prince Edward Island,,based on nearby landmark,seconds,small collection,Google Earth coordinates for Cape Egmont,gp_mid,-1.95,-0.46,108,CA,,Egmont Bay,,,bed,,,,,,,NA,"""The Egmont Bay Formation crops out along the western part of the island, and is regarded to be latest Pennsylvanian (Stephanian) in geological age on the basis of plant body fossils and pollen""",,sandstone,,,,,,,,,,terrestrial indet.,,,macrofossils,some,,,skeletons,,NA,,body,good,,snapshot,,,,,,,NA,,,taxonomic,mechanical,ROM,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Erpetonyx,n. gen.,NA,NA,vertebrate,"S. P. Modesto, D. M. Scott, and M. J. MacDougall, H.-D. Sues, D. C. Evans, R. R. Reisz. 2015. The oldest parareptile and the early diversification of reptiles. Proceedings of the Royal Society B 282:20141912",327,327,0,R. Butler,R. Butler,,07/07/2015 05:13,07/07/2015 05:13,55727,arsenaultorum,Erpetonyx,55727,n. sp.,303.7,298.9,Gzhelian,,1,CA,Erpetonyx arsenaultorum
1285874,occ,NA,,171346,,n. gen. Zarcasaurus n. sp. tanyderus,species,324120,,Zarcasaurus tanyderus,NA,species,324120,Brinkman et al.,1984,Chordata,33815,Reptilia,36322,Araeoscelidia,37769,Araeoscelidae,37772,37774,NA,NA,NA,individuals,-106.652222,36.159443,Valley floor of east Camp Quarry,NA,1 km SE Arroyo del Agua,US,New Mexico,Rio Arriba,based on nearby landmark,seconds,small collection,"Coordinates are for the area 1 km southeast of the small village of Arroyo del Agua, Rio Arriba County, New Mexico. See Lucas et al. (2005) for detailed map of other fossil-bearing locations in the area.",gp_mid,-34.08,4.53,101,US,FED,Cutler,,,bed,,,,,,,NA,,,"""siliciclastic""",,,,,,,,,,fine channel fill,,,macrofossils,,some,,partial skeletons,,NA,,"mold/impression,adpression",,,,,,,,,,NA,,,taxonomic,field collection,CM,,,,,1982,,"""Numerous articulated specimens have been collected from the valley floor immediately east of the Camp quarry."" Lucas et a. (2005)",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Zarcasaurus,n. gen.,NA,NA,vertebrate,"D. B. Brinkman, D. S. Berman, and D. A. Eberth. 1984. A new araeoscelid reptile, Zarcasaurus tanyderus, from the Cutler Formation (Lower Permian) of north-central New Mexico. New Mexico Geology 6(2):34-39",327,327,0,R. Butler,R. Butler,,07/07/2015 09:13,07/07/2015 09:13,NA,tanyderus,Zarcasaurus,55729,n. sp.,296.4,268,Wolfcamp,,1,US,Zarcasaurus tanyderus
1285898,occ,NA,,52522,,n. gen. Kadaliosaurus n. sp. priscus,species,324121,,Kadaliosaurus priscus,NA,species,324121,Credner,1889,Chordata,33815,Reptilia,36322,Araeoscelidia,37769,Araeoscelidae,37772,37775,NA,NA,NA,individuals,13.650278,50.999722,Niederhaslich,NA,Niederh_sslich; Niederh_slich; Nieder-H_sslich; Plauenscher Grund; D̦hlen Basin,DE,Saxony,Weieritzkreis,based on nearby landmark,seconds,outcrop,"Niederh_slich in the D̦hlen basin, today it is one part of the City of Freital, SW of Dresden in Sachsen; the outcrop does not exist anymore.",gp_mid,23.3,7.73,305,DE,,Niederh_slich-Schweinsdorf,Rotliegend,Niederh_slich limestone,member,,,,,,,NA,"""The Niederh_slich Formation belongs stratigraphically [...] to the Melanerpeton gracile-M. pulcherimus Zone, i. e. uppermost Unterrotliegend"" (U. Hoffman, 2002, Workshop _Oberkarbon - Untertrias in Zentraleuropa: Prozesse und ihr Timing [online] http://www.geo.tu-freiberg.de/palaeo/GeoTage-2002.pdf) (TL);\r\nthe Niederh_slich limestone is Asselian according to assorted references, e.g., Gebhardt and Schneider 1993 (JA)\r\nAccording to Roscher & Schneider (2006, in Lucas et al. (eds), Geol. Soc. Spec. Publ. 265) the Niederh_slich Fm. is Sakmarian in age (TL).",,"""limestone""",,,,,,,,,,lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Museum: Staatliches Museum f_r Mineralogie und Geologie, Dresden (SMMGD)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Kadaliosaurus,n. gen.,NA,NA,vertebrate,H. Credner. 1889. Die Stegocephalen und Saurier aus dem Rothliegenden des Plauen'schen Grundes bei Dresden. Zeitschrift der Deutschen Geologischen Gesellschaft 41:319-342,327,327,0,R. Butler,R. Butler,,07/07/2015 11:27,07/07/2015 11:27,14125,priscus,Kadaliosaurus,55731,n. sp.,295.5,290.1,Sakmarian,,1,DE,Kadaliosaurus priscus
1285904,occ,NA,,171350,,n. gen. Aphelosaurus n. sp. lutevensis,species,324123,,Aphelosaurus lutevensis,NA,species,324123,Gervais,1858,Chordata,33815,Reptilia,36322,Araeoscelidia,37769,Araeoscelidae,37772,324122,NA,NA,NA,individuals,3.313889,43.733612,"Les Tuilieres, Lodeve",NA,"Les Tuili̬res, Lod̬ve",FR,Languedoc-Roussillon,H̩rault,based on nearby landmark,seconds,small collection,,gp_mid,18.1,-1.36,305,FR,,UsclasSaint-Privas,,,bed,,,,,,,NA,,,"""siliciclastic""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MNHN,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Aphelosaurus,n. gen.,NA,NA,vertebrate,"P. Gervais. 1858. Description de l۪Aphelosaurus lutevensis, saurien fossile des schistes permiens de Lod̬ve. Annales des Sciences naturelles, 4̬me S̩rie, Zoologie 10:233-235",327,327,0,R. Butler,R. Butler,,07/07/2015 12:00,07/07/2015 12:00,55733,lutevensis,Aphelosaurus,55733,n. sp.,298.9,295.5,Asselian,,1,FR,Aphelosaurus lutevensis
1285988,occ,NA,,67862,,Delorhynchus n. sp. cifellii,species,324159,,Delorhynchus cifellii,NA,species,324159,Reisz et al.,2014,Chordata,33815,Reptilia,36322,,NA,,NA,38922,NA,NA,NA,specimens,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Delorhynchus,,NA,NA,"paleoentomology,vertebrate","R. R. Reisz, M. J. MacDougall, and S. P. Modesto. 2014. A new species of the parareptile genus Delorhynchus, based on articulated skeletal remains from Richards Spur, Lower Permian of Oklahoma. Journal of Vertebrate Paleontology 34(5):1033-1043",327,327,334,R. Butler,R. Butler,T. Liebrecht,08/07/2015 08:54,13/01/2016 18:18,19393,cifellii,Delorhynchus,55745,n. sp.,290.1,268,Leonard,,4,US,Delorhynchus cifellii
1297470,occ,NA,,173058,,Endothiodon n. sp. tolani,species,39012,species not entered,Endothiodon,NA,genus,39012,Cox and Angielczyk,2015,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,39012,NA,NA,NA,specimens,35.116669,-10.383333,Locality L4,NA,,TZ,,,estimated from map,minutes,outcrop,,gp_mid,7.89,-60.43,701,TZ,,Ruhuhu,Songea,,,,,,,,,NA,middle Permian; middle tetrapod-bearing horizon,"calcareous, stromatolites",mudstone,,,calcareous,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,surface (in situ),,,,,,,,,terrestrial,NA,actively mobile,,NA,herbivore,,,hydroxyapatite,,NA,,Endothiodon,,NA,NA,vertebrate,"C. B. Cox and K. D. Angielczyk. 2015. A new endothiodont dicynodont (Therapsida, Anomodontia) from the Permian Ruhuhu Formation (Songea Group) of Tanzania and its feeding system. Journal of Vertebrate Paleontology 35(4):e935388",18,18,18,M. Uhen,M. Uhen,M. Uhen,08/09/2015 12:53,08/09/2015 12:54,56255,tolani,Endothiodon,56255,n. sp.,298.9,252.17,Permian,,6,TZ,Endothiodon tolani
1297471,occ,NA,,173059,,Endothiodon tolani,species,39012,species not entered,Endothiodon,NA,genus,39012,Cox and Angielczyk,2015,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,39012,NA,NA,NA,specimens,35.116669,-10.383333,Locality L2,NA,,TZ,,,estimated from map,minutes,outcrop,,gp_mid,7.89,-60.43,701,TZ,,Ruhuhu,Songea,,,,,,,,,NA,middle Permian; middle tetrapod-bearing horizon,"calcareous, stromatolites",mudstone,,,calcareous,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,surface (in situ),,,,,,,,,terrestrial,NA,actively mobile,,NA,herbivore,,,hydroxyapatite,,NA,,Endothiodon,,NA,NA,vertebrate,"C. B. Cox and K. D. Angielczyk. 2015. A new endothiodont dicynodont (Therapsida, Anomodontia) from the Permian Ruhuhu Formation (Songea Group) of Tanzania and its feeding system. Journal of Vertebrate Paleontology 35(4):e935388",18,18,0,M. Uhen,M. Uhen,,08/09/2015 12:56,08/09/2015 12:56,56255,tolani,Endothiodon,56255,,298.9,252.17,Permian,,2,TZ,Endothiodon tolani
1300960,occ,NA,,173721,,n. gen. Scapanops n. sp. neglecta,species,330108,,Scapanops neglecta,NA,species,330108,Schoch and Sues,2013,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,330106,NA,NA,NA,,-98.201385,33.760277,Halsell Hill,NA,,US,Texas,Clay County,based on political unit,seconds,small collection,"Precise coordinates not available, coordinates based on the centre of the County",gp_mid,-30.08,-2.01,101,US,,Nocona,Wichita,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,some,some,,,,NA,,body,medium,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,A. S. Romer,April 18 1950,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Scapanops,n. gen.,NA,NA,,R. R. Schoch and H.-D. Sues. 2013. A new dissorophid temnospondyl from the Lower Permian of\r\nnorth-central Texas. Comptes Rendus Palevol 12:437-445,327,698,0,R. Butler,D. Cashmore,,12/10/2015 11:04,12/10/2015 11:04,56628,neglecta,Scapanops,56628,n. sp.,298.9,295.5,Asselian,,NA,US,Scapanops neglecta
1301296,occ,NA,,173814,,n. gen. Conjunctio n. sp. multidens,species,330110,,Conjunctio multidens,NA,species,330110,Schoch and Sues,2013,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37026,NA,NA,NA,,-106.599998,36.200001,"West side of Puerco River, opposite Youngsville, ""El Rito""",NA,,US,New Mexico,Rio Arriba,estimated from map,minutes,small collection,"West side of Puerco River, opposite Youngsville (in the earlier literature given as El Rito, which is now the official name of a larger town some 30 miles (48 km) to the north; Langston, 1953), Rio Arriba County, New Mexico, USA.",gp_mid,-34.29,4.04,101,US,FED,Abo,,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,some,,,,,NA,,body,medium,,,,,,,,,NA,,,taxonomic,,FMNH,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Conjunctio,n. gen.,NA,NA,,R. R. Schoch and H.-D. Sues. 2013. A new dissorophid temnospondyl from the Lower Permian of\r\nnorth-central Texas. Comptes Rendus Palevol 12:437-445,327,698,0,R. Butler,D. Cashmore,,14/10/2015 08:37,14/10/2015 08:37,56628,multidens,Conjunctio,56628,n. sp.,298.9,290.1,Asselian,Sakmarian,NA,US,Conjunctio multidens
1301297,occ,NA,,77412,,Conjunctio multidens,species,330110,,Conjunctio multidens,NA,species,330110,Schoch and Sues,2013,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37026,NA,NA,NA,,-106.639442,36.157223,UCMP V-2814,NA,Camp Quarry,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"""southeast slope of a small butte, 410 yards south of New Mexico State Highway 96, about 940 yards southeast of the Rio Puerco bridge at Arroyo del Agua, section 8, T.22N., R.3E., Rio Arriba County, New Mexico"" (Langston, 1965 p. 6; 1966 p.691)",gp_mid,-34.09,4.48,101,US,FED,Abo/Cutler,,,group of beds,,,,,,,NA,All specimens appear to come from about the same stratigraphic level (38-36 m below top of the butte). Whether these beds are uppermost Carboniferous or lower Permian is a subject of controversy.\r\n,"""soft brick-red clayey siltstone"" (Langston, 1965 p. 6; 1966 p.691; Langston & Reisz, 1981 p. 74)",siltstone,red,,argillaceous,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,general faunal/floral,"bulk,surface (float),survey of museum collection",UCMP,all macrofossils,,,"C. L. Camp, among others","1928, 1934, 1935","""Berman & Reisz reopened this quarry in 1979, but despite extensive digging by a team of five people, only a few scattered bone fragments were recovered. It appears that the site has been completeley exhausted"" (Langston & Reisz, 1981 p. 74).\r\nType of Rhiodenticulatus heatoni was ""probably not found in the main bone level of the quarry, but rather as float on the slope of Loma Salazar a few feet away and presumably at or just above the quarry bone level."" (Berman & Reisz, 1986).","""Captorhinomorphs and Diadectomorphs"" (Langston 1966 p.690)","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Conjunctio,,NA,NA,vertebrate,R. R. Schoch and H.-D. Sues. 2013. A new dissorophid temnospondyl from the Lower Permian of\r\nnorth-central Texas. Comptes Rendus Palevol 12:437-445,327,698,0,R. Butler,D. Cashmore,,14/10/2015 08:42,14/10/2015 08:42,26206,multidens,Conjunctio,56628,,303.4,268,Virgilian,Wolfcamp,NA,US,Conjunctio multidens
1301420,occ,NA,,173815,,Tetrapoda indet.,unranked clade,137279,,Tetrapoda,NA,unranked clade,53190,Sookias et al.,2014,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,,-64.459442,45.412777,Diligent River,NA,,CA,Nova Scotia,,based on nearby landmark,seconds,small collection,"west of Parrsboro, Nova Scotia, close to the town of Diligent River",gp_mid,-10.35,-13.59,108,CA,,Parrsboro,,,bed,,,,,,,NA,"""Assigned to the lowermost Pennsylvanian (formerly Westphalian A) by macrophyte and microspore fossils"" (Sookias et al., 2014)",,sandstone,coarse,,,Y,,,,,,terrestrial indet.,,,macrofossils,none,none,,,,NA,,mold/impression,medium,,,,,,,,,NA,,,taxonomic,peel or thin section,,,,,,1987,NSM (Nova Scotia Museum),,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tetrapoda,,NA,NA,vertebrate,"R. B. Sookias, C. B̦hmer, and J. A. Clack. 2014. Redescription and Phylogenetic Analysis of the Mandible of an Enigmatic Pennsylvanian (Late Carboniferous) Tetrapod from Nova Scotia, and the Lability of Meckelian Jaw Ossification. PLoS ONE 9(10):e109717",327,697,697,R. Butler,E. Dunne,E. Dunne,16/10/2015 06:07,16/10/2015 06:07,56671,indet.,,56671,,318.1,314.6,Westphalian A,,NA,CA, indet.
1301947,occ,NA,,173986,members,n. gen. Occidens n. sp. portlocki,species,330459,,Occidens portlocki,NA,species,330459,Clack and Ahlberg,2004,Chordata,33815,Osteichthyes,34881,,NA,Whatcheeriidae,179034,330458,NA,NA,NA,,-6.7,54.799999,"near Maghera/Draperstown, Londonderry",NA,,UK,Northern Ireland,Derry,based on nearby landmark,1,outcrop,"Locality ""uncertain, probably Londonderry, Northern Ireland.""\r\n""Localities near Maghera or Draperstown may be more likely to have yielded the jaw specimen.""",gp_mid,-13.84,-31.87,313,UK,,,,,,,,,,,,NA,"""Early-mid Carboniferous (probably late Tournisian or late Visean"" (Clack & Ahlberg, 2004)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,adpression",,,,,,,,,,NA,,,taxonomic,,,,,,,,"Specimen GSM 28498 (Geological Survey Museum) housed at the British Geological Survey (BGS), Keyworth, Nottinghamshire, UK",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Occidens,n. gen.,NA,NA,vertebrate,"J. A. Clack and P. E. Ahlberg. 2004. A new stem tetrapod from the Early Carboniferous of Northern Ireland. In G. Arratia, M. V. H. Wilson & R. Coutier (eds.), Recent Advances in the Origin and Early Radiation of Vertebrates ",327,697,0,R. Butler,E. Dunne,,22/10/2015 09:34,22/10/2015 09:34,NA,portlocki,Occidens,56722,n. sp.,358.9,330.9,Tournaisian,Visean,NA,UK,Occidens portlocki
1301948,occ,NA,,173987,members,Clepsydrops n. sp. magnus,species,137373,,Clepsydrops magnus,NA,species,137373,Romer,1961,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38887,NA,NA,NA,,-80.050003,40.540001,McKnight Road 6 miles north of Pittsburgh,NA,"On the east side, near the junction of Brown's lane",US,Pennsylvania,Pittsburgh,estimated from map,2,outcrop,"""Along the course of McKnight Road, about 6 miles north of Pittsburgh, Pennsylvania, there has recently been considerable quarrying.... Inquiry made it rather certain that the material was excavated from a locality on the east of side of McKnight Road near the junction of Brown's Lane"" (Romer, 1961)",gp_mid,-14.93,-3.75,101,US,,Casselman,Conemaugh,,,,,,,,,NA,"Stratigraphically, the sandstone excavated here is positioned just above the Ames limestone, suggesting that it pertains to the upper part of the Conemaugh Group and possessing a latest Missourian to earliest Virgilian age (Romer, 1961).",,"""shale""",,,,,siltstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"CMHN 13942 (Carnegie Museum, Pittsburgh)",No other taxa were recovered from the site.,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Clepsydrops,,NA,NA,vertebrate,A. S. Romer. 1961. A large ophiacodont pelycosaur from the Pennsylvanian of the Pittsburgh region. Breviora 144:1-7,327,697,697,R. Butler,E. Dunne,E. Dunne,22/10/2015 11:18,26/10/2015 11:41,NA,magnus,Clepsydrops,28724,n. sp.,305.9,298.9,Missourian,Virgilian,NA,US,Clepsydrops magnus
1302340,occ,NA,,174063,members,n. gen. Palaeomolgophis n. sp. scoticus,species,320835,,Palaeomolgophis scoticus,NA,species,320835,Brough and Brough,1967,Chordata,33815,Osteichthyes,34881,Adelospondyli,320812,Adelogyrinidae,37325,37329,NA,NA,NA,,-3.4928,55.905899,"Curley Shale, Pumpherston",NA,,UK,Scotland,,based on nearby landmark,4,outcrop,"Curley Shale, Pumpherston, Scotland",gp_mid,-9.43,-28.19,313,UK,,,Lower Oil Shale,,,,,,,,,NA,"Pumpherston Shale (curly seam). Oil Shale Group, now known as the Strathclyde Group.",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,some,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Originally RSM (Royal Scottish Museum, Edinburgh), now Geology Department, National\r\nMuseums of Scotland (abbreviated to NMS.G.)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Palaeomolgophis,n. gen.,NA,NA,vertebrate,M. C. Brough and J. Brough. 1967. Studies on Early Tetrapods I: The Lower Carboniferous Microsaurs. Philosophical Transactions of the Royal Society of London B: Biological Sciences 252(776):107-129,327,697,697,R. Butler,E. Dunne,E. Dunne,26/10/2015 09:52,26/10/2015 10:54,NA,scoticus,Palaeomolgophis,56763,n. sp.,346.7,330.9,Visean,,NA,UK,Palaeomolgophis scoticus
1302352,occ,NA,,140937,,n. gen. Lethiscus n. sp. stocki,species,229330,,Lethiscus stocki,NA,species,229330,Wellstead,1982,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Lethiscidae,37255,37256,NA,NA,NA,,-3.21,55.98,"Wardie Shore, north of Edinburgh",NA,"Granton, near Edinburgh (BMNH)",UK,Scotland,,estimated from map,2,outcrop,Fish beds located east of Granton harbour,gp_mid,-9.25,-28.12,313,UK,,,,,group of beds,,,,,,,NA,Calciferous Sandstones. Lower Oil-Shale Group (Holkerian-Asbian) of the Lower Carboniferous Calciferous Sandstone Measures,,"""shale""",,lithified,carbonaceous,,,,,,,lacustrine indet.,,"They are largely non-marine and were apparently deposited in a large freshwater or brackish lake extending into West Lothian and Fife and as far as the Pentland Hills. This lake, however, was subject to a periodic marine influence from the east, which became more manifest through time. Marine fossils in the Edinburgh district are confined to thin bands only.",macrofossils,some,,,,,NA,,"body,adpression",,,,,,,,,,NA,,,taxonomic,,"BMNH,MCZ",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lethiscus,n. gen.,NA,NA,vertebrate,C. F. Wellstead. 1982. A Lower Carboniferous Aistopod Amphibian from Scotland. Palaeontology 25(1):193-208,327,697,0,R. Butler,E. Dunne,,26/10/2015 11:51,26/10/2015 11:51,38758,stocki,Lethiscus,56770,n. sp.,342.8,336,Holkerian,Asbian,NA,UK,Lethiscus stocki
1302376,occ,NA,,68318,,n. gen. Sigournea n. sp. multidentata,species,330701,,Sigournea multidentata,NA,species,330701,Bolt and Lombard,2006,Chordata,33815,Osteichthyes,34881,,NA,,NA,330700,NA,NA,NA,,-92.333336,41.316666,Delta,NA,,US,Iowa,Keokuk,based on nearby landmark,minutes,outcrop,"""SW1/4, SW1/4, section 15, T75N, R13W"" near Delta, Iowa (coordinate based on Delta)\n""two adjacent palaeodepressions or collapse structures, exposed in the walls of an inactive limestone quarry""",gp_mid,-47.48,-23.84,101,US,,St. Louis,,Waugh,member,,,,,,,NA,"St. Louis Formation in Iowa may correlate not with the St. Louis Formation in its type section, but with the Genevieve Formation in Missouri and Illinois","unclear: collapse structures are within a limestone quarry, but the Waugh Member elsewhere includes ""sandstones, shales, and lime mudstones""",,,,,,,,,,,sinkhole,,"general environment is ""primarily lacustrine, fresh-water to brackish, with possible intermittent incursion of marine waters"" but fossils are from ""fills within two adjacent collapse structures""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,FMNH,,,,,,"""Over 600 tetrapod specimens were recovered... along with several hundred fish and some invertebrate and plant fossils""",definitely not the same as the paleobotanical What Cheer locality (collection 13999),"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sigournea,n. gen.,NA,NA,vertebrate,"J. R. Bolt and R. E. Lombard. 2006. Sigournea multidentata, a New Stem Tetrapod from the Upper Mississippian of Iowa, USA. Journal of Paleontology 80(4):717-725",327,697,697,R. Butler,E. Dunne,E. Dunne,27/10/2015 07:06,27/10/2015 08:45,19656,multidentata,Sigournea,56778,n. sp.,339.4,336,Asbian,,NA,US,Sigournea multidentata
1302377,occ,NA,,68318,,n. gen. Deltaherpeton n. sp. hiemstrae,species,330704,,Deltaherpeton hiemstrae,NA,species,330704,Bolt and Lombard,2010,Chordata,33815,Osteichthyes,34881,,NA,Colosteidae,36975,330703,NA,NA,NA,,-92.333336,41.316666,Delta,NA,,US,Iowa,Keokuk,based on nearby landmark,minutes,outcrop,"""SW1/4, SW1/4, section 15, T75N, R13W"" near Delta, Iowa (coordinate based on Delta)\n""two adjacent palaeodepressions or collapse structures, exposed in the walls of an inactive limestone quarry""",gp_mid,-47.48,-23.84,101,US,,St. Louis,,Waugh,member,,,,,,,NA,"St. Louis Formation in Iowa may correlate not with the St. Louis Formation in its type section, but with the Genevieve Formation in Missouri and Illinois","unclear: collapse structures are within a limestone quarry, but the Waugh Member elsewhere includes ""sandstones, shales, and lime mudstones""",,,,,,,,,,,sinkhole,,"general environment is ""primarily lacustrine, fresh-water to brackish, with possible intermittent incursion of marine waters"" but fossils are from ""fills within two adjacent collapse structures""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,FMNH,,,,,,"""Over 600 tetrapod specimens were recovered... along with several hundred fish and some invertebrate and plant fossils""",definitely not the same as the paleobotanical What Cheer locality (collection 13999),"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Deltaherpeton,n. gen.,NA,NA,vertebrate,"J. R. Bolt and R. E. Lombard. 2010. Deltaherpeton hiemstrae, a new colosteid tetrapod from the Mississippian of Iowa. Journal of Paleontology 84(6):1135-1151",327,697,697,R. Butler,E. Dunne,E. Dunne,27/10/2015 08:45,27/10/2015 08:45,19656,hiemstrae,Deltaherpeton,56779,n. sp.,339.4,336,Asbian,,NA,US,Deltaherpeton hiemstrae
1304510,occ,NA,,174420,members,n. gen. Kirktonecta n. sp. milnerae,species,331369,,Kirktonecta milnerae,NA,species,331369,Clack,2011,Chordata,33815,Osteichthyes,34881,,NA,,NA,331368,NA,NA,NA,,-3.6162,55.9058,East Kirkton Quarry,NA,East Kirkton Limestone,UK,Scotland,West Lothian,estimated from map,4,outcrop,Quarry situation on the east side of Limefield Road near Bathgate town,gp_mid,-9.51,-28.19,313,UK,,Bathgate Hills Volcanic,,,,,,,,,,NA,Bed 82۪ East Kirkton Limestone,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,skeletons,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Kirktonecta,n. gen.,NA,NA,vertebrate,"J. A. Clack. 2011. A new Microsaur from the Early Carboniferous (Visean) of East Kirkton Scotland, showing soft tissue evidence. Special Papers in Palaeontology 86:1-11",327,697,697,R. Butler,E. Dunne,E. Dunne,17/11/2015 06:50,17/11/2015 09:49,NA,milnerae,Kirktonecta,56918,n. sp.,346.7,330.9,Visean,,NA,UK,Kirktonecta milnerae
1304514,occ,NA,,174421,members,Eoherpeton watsoni,species,229321,,Eoherpeton watsoni,NA,species,229321,Smithson,1985,Chordata,33815,Osteichthyes,34881,,NA,Eoherpetontidae,37179,37180,NA,NA,NA,,-3.148056,55.877777,"Burghlee Ironstone, Loanhead, Midlothian",NA,Rumbles Ironstone,UK,Scotland,Midlothian,based on nearby landmark,seconds,outcrop,,gp_mid,0.32,-9.71,313,UK,,Limestone Coal,Clackmannan,,,,,,,,,NA,,,ironstone,,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,skeletons,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Some specimens reside in RSM (Royal Scottish Museum, Edinburgh).\r\n","RSM 1967/13/1 Acherontiscus caledoniae is though to have come from this location based on sediment analysis (Carroll, 1969)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Eoherpeton,,NA,NA,vertebrate,T. R. Smithson. 1985. The morphology and relationships of the Carboniferous amphibian Eoherpeton watsoni Panchen. Zoological Journal of the Linnean Society 85:317-410,327,697,0,R. Butler,E. Dunne,,17/11/2015 06:59,17/11/2015 06:59,NA,watsoni,Eoherpeton,56998,,326.4,318.1,Pendleian,,NA,UK,Eoherpeton watsoni
1304517,occ,NA,,174420,members,n. gen. Eldeceeon n. sp. rolfei,species,331591,,Eldeceeon rolfei,NA,species,331591,Smithson,1993,Chordata,33815,Osteichthyes,34881,,NA,,NA,331590,NA,NA,NA,,-3.6162,55.9058,East Kirkton Quarry,NA,East Kirkton Limestone,UK,Scotland,West Lothian,estimated from map,4,outcrop,Quarry situation on the east side of Limefield Road near Bathgate town,gp_mid,-9.51,-28.19,313,UK,,Bathgate Hills Volcanic,,,,,,,,,,NA,Bed 82۪ East Kirkton Limestone,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,skeletons,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Eldeceeon,n. gen.,NA,NA,vertebrate,"T. R. Smithson. 1993. Eldeceeon rolfei, a new reptiliomorph from the Visean of East Kirkton, West Lothian, Scotland. Transactions of the Royal Society of Edinburgh: Earth Sciences 84:377-382",327,697,0,R. Butler,E. Dunne,,17/11/2015 09:53,17/11/2015 09:53,NA,rolfei,Eldeceeon,56996,n. sp.,346.7,330.9,Visean,,NA,UK,Eldeceeon rolfei
1304611,occ,NA,,132778,,Pholidogaster pisciformis,species,320855,,Pholidogaster pisciformis,NA,species,320855,Huxley,1862,Chordata,33815,Osteichthyes,34881,,NA,Colosteidae,36975,36978,NA,NA,NA,,-3.13,55.91,Gilmerton,NA,,UK,,Edinburgh,,2,,,gp_mid,-4.79,-20.35,313,UK,,,,,,,,,,,,NA,,,"""shale""",,,,,,,,,,marine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Repository: Geological Museum of the University of Cambridge (Sedgwick Museum of Earth Sciences),,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Pholidogaster,,NA,NA,vertebrate,T. H. Huxley. 1862. On new labyrinthodonts from the Edinburgh coal-field. Quarterly Journal of the Geological Society of London 18:291-296,327,697,0,R. Butler,E. Dunne,,19/11/2015 11:22,19/11/2015 11:22,21664,pisciformis,Pholidogaster,57017,,336,326.4,Brigantian,,NA,UK,Pholidogaster pisciformis
1304612,occ,NA,,174420,members,n. gen. Eucritta n. sp. melanolimnetes,species,229324,,Eucritta melanolimnetes,NA,species,229324,Clack,1998,Chordata,33815,Osteichthyes,34881,,NA,,NA,229323,NA,NA,NA,,-3.6162,55.9058,East Kirkton Quarry,NA,East Kirkton Limestone,UK,Scotland,West Lothian,estimated from map,4,outcrop,Quarry situation on the east side of Limefield Road near Bathgate town,gp_mid,-9.51,-28.19,313,UK,,Bathgate Hills Volcanic,,,,,,,,,,NA,Bed 82۪ East Kirkton Limestone,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,skeletons,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Eucritta,n. gen.,NA,NA,vertebrate,J. A. Clack. 1998. A new Early Carboniferous tetrapod with a m̩lange of crown-group characters. Nature 394:66-69,327,697,0,R. Butler,E. Dunne,,19/11/2015 11:35,19/11/2015 11:35,NA,melanolimnetes,Eucritta,40836,n. sp.,346.7,330.9,Visean,,NA,UK,Eucritta melanolimnetes
1304700,occ,NA,,132778,,Doragnathus woodi,species,334443,,Doragnathus woodi,NA,species,334443,Panchen,1973,Chordata,33815,Osteichthyes,34881,,NA,,NA,36986,NA,NA,NA,,-3.13,55.91,Gilmerton,NA,,UK,,Edinburgh,,2,,,gp_mid,-4.79,-20.35,313,UK,,,,,,,,,,,,NA,,,"""shale""",,,,,,,,,,marine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Repository: Geological Museum of the University of Cambridge (Sedgwick Museum of Earth Sciences),,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Doragnathus,,NA,NA,vertebrate,"A. L. Panchen. 1973. On Crassigyrinus scoticus Watson, a primitive amphibian from the Lower Carboniferous of Scotland. Palaeontology 16(1):179-193",327,697,0,R. Butler,E. Dunne,,20/11/2015 10:58,20/11/2015 10:58,21664,woodi,Doragnathus,57037,,336,326.4,Brigantian,,NA,UK,Doragnathus woodi
1304974,occ,NA,IF,174685,,Herpetichnus n. sp. bucklandi,species,332079,,Herpetichnus bucklandi,NA,species,332079,Jardine,1850,Chordata,33815,Reptilia,36322,,NA,,NA,332077,NA,NA,NA,,-3.43837,55.161156,Corncockle Quarry,NA,Corncockle Muir,UK,Scotland,Dumfries and Galloway,based on nearby landmark,6,outcrop,"Corncockle Quarry (= Corncockle Muir), , an elevated ridge ca. 1 mi. or more in length, nearly in the center (E-W) of the Annan River valley, at ca. 2/3 its length from its upper/northern end; near Templand, 2 mi. from Lochmaben",gp_mid,12.48,10.03,313,UK,,Corncockle Sandstone,Stewartry,,group of beds,,,,,,,NA,,,sandstone,,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,footprints,,,NA,,trace,,autochthonous,snapshot,,,life position,,,,NA,,,general faunal/floral,"surface (in situ),observed (not collected)",,,,,,"18131814, 1827",,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Herpetichnus,,NA,NA,vertebrate,"W. Jardine. 1850. Note to Mr. Harkness's paper on ""The position of the impressions of footsteps in the Bunter Sandstone of Dumfries-shire"". Annals and Magazine of Natural History, series 2 6(33):208-209",14,14,0,M. Carrano,M. Carrano,,24/11/2015 10:32,24/11/2015 10:32,NA,bucklandi,Herpetichnus,57077,n. sp.,298.9,272.3,Cisuralian,,NA,UK,Herpetichnus bucklandi
1304975,occ,NA,IF,174685,,n. gen. Herpetichnus n. sp. sauroplesius,species,332078,,Herpetichnus sauroplesius,NA,species,332078,Jardine,1850,Chordata,33815,Reptilia,36322,,NA,,NA,332077,NA,NA,NA,,-3.43837,55.161156,Corncockle Quarry,NA,Corncockle Muir,UK,Scotland,Dumfries and Galloway,based on nearby landmark,6,outcrop,"Corncockle Quarry (= Corncockle Muir), , an elevated ridge ca. 1 mi. or more in length, nearly in the center (E-W) of the Annan River valley, at ca. 2/3 its length from its upper/northern end; near Templand, 2 mi. from Lochmaben",gp_mid,12.48,10.03,313,UK,,Corncockle Sandstone,Stewartry,,group of beds,,,,,,,NA,,,sandstone,,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,footprints,,,NA,,trace,,autochthonous,snapshot,,,life position,,,,NA,,,general faunal/floral,"surface (in situ),observed (not collected)",,,,,,"18131814, 1827",,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Herpetichnus,n. gen.,NA,NA,vertebrate,"W. Jardine. 1850. Note to Mr. Harkness's paper on ""The position of the impressions of footsteps in the Bunter Sandstone of Dumfries-shire"". Annals and Magazine of Natural History, series 2 6(33):208-209",14,14,0,M. Carrano,M. Carrano,,24/11/2015 10:32,24/11/2015 10:32,NA,sauroplesius,Herpetichnus,57077,n. sp.,298.9,272.3,Cisuralian,,NA,UK,Herpetichnus sauroplesius
1306526,occ,NA,,174421,members,n. gen. Caerorhachis n. sp. bairdi,species,229315,,Caerorhachis bairdi,NA,species,229315,Holmes and Carroll,1977,Chordata,33815,Osteichthyes,34881,,NA,Caerorhachidae,36992,36993,NA,NA,NA,,-3.148056,55.877777,"Burghlee Ironstone, Loanhead, Midlothian",NA,Rumbles Ironstone,UK,Scotland,Midlothian,based on nearby landmark,seconds,outcrop,,gp_mid,0.32,-9.71,313,UK,,Limestone Coal,Clackmannan,,,,,,,,,NA,,,ironstone,,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,skeletons,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Some specimens reside in RSM (Royal Scottish Museum, Edinburgh).\r\n","RSM 1967/13/1 Acherontiscus caledoniae is though to have come from this location based on sediment analysis (Carroll, 1969)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Caerorhachis,n. gen.,NA,NA,vertebrate,R. B. Holmes and R. L. Carroll. 1977. A temnospondyl amphibian from the Mississippian of Scotland. Bulletin of the Museum of Comparative Zoology 147:489-511,327,697,697,R. Butler,E. Dunne,E. Dunne,01/12/2015 06:03,04/12/2015 09:45,NA,bairdi,Caerorhachis,57189,n. sp.,326.4,318.1,Pendleian,,NA,UK,Caerorhachis bairdi
1306606,occ,NA,,22726,,n. gen. Doragnathus n. sp. woodi,species,334443,,Doragnathus woodi,NA,species,334443,Smithson,1980,Chordata,33815,Osteichthyes,34881,,NA,,NA,36986,NA,NA,NA,,-3.35,56.1166,Cowdenbeath Amphibian Bonebed,NA,ETE Locality 1605; Dora Opencast Coal Site,UK,,,,4,outcrop,"""south-east of Cowdenbeath... a section 30 m long""",gp_mid,0.18,-9.49,313,UK,,,Limestone Coal,,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min\r\n""lower Namurian A... 62 m beneath the base of the Index Limestone [which is]... at the junction between the top of the Pendleian (E1) and the base of the Arnsbergian (E2) stages"": originally entered as Namurian to Bashkirian","ETE rock type adj: ""rooty,muddy"", ETE lithology comments: 0\r\n""a localised patch in a seatrock (rooty, muddy siltstone)""",siltstone,,,,,,,,,,terrestrial indet.,,,,,,,,,NA,,,,,,,,,,,,NA,,,general faunal/floral,,,,7 specimens,,,1974 and 1975,"ETE Size: .; ETE reference list: 478, 479, 483, 482, 485, 454, 81, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Doragnathus,n. gen.,NA,NA,,T. R. Smithson. 1980. A new labyrinthodont amphibian from the Carboniferous of Scotland. Palaeontology 23(4):915-923,327,697,0,R. Butler,E. Dunne,,01/12/2015 08:45,01/12/2015 08:45,5931,woodi,Doragnathus,57195,n. sp.,326.4,318.1,Pendleian,,NA,UK,Doragnathus woodi
1307360,occ,NA,,175174,members,n. gen. Pholiderpeton n. sp. scutigerum,species,229337,,Pholiderpeton scutigerum,NA,species,229337,Huxley,1869,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37193,NA,NA,NA,,-1.7143,53.7626,Toftshaw near Bradford,NA,,UK,England,,,4,,P. scutigerum found in the Black-Bed or Royd's Coal at the location,gp_mid,4.95,-5.02,315,UK,,Lower Coal Measures,,,,,,,,,,NA,"""Black bed"" appears correlative of Mickley 3 coal of the upper Langsettian.",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,some,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Pholiderpeton,n. gen.,NA,NA,vertebrate,T. H. Huxley. 1869. On a new labyrinthodont from Bradford. Quarterly Journal of the Geological Society 25:309-311,327,697,0,R. Butler,E. Dunne,,04/12/2015 09:32,04/12/2015 09:32,NA,scutigerum,Pholiderpeton,57221,n. sp.,318.1,314.6,Westphalian A,,NA,UK,Pholiderpeton scutigerum
1307364,occ,NA,,174421,members,n. gen. Acherontiscus n. sp. caledoniae,species,229304,,Acherontiscus caledoniae,NA,species,229304,Carroll,1969,Chordata,33815,Osteichthyes,34881,,NA,Acherontiscidae,37330,37331,NA,NA,NA,,-3.148056,55.877777,"Burghlee Ironstone, Loanhead, Midlothian",NA,Rumbles Ironstone,UK,Scotland,Midlothian,based on nearby landmark,seconds,outcrop,,gp_mid,0.32,-9.71,313,UK,,Limestone Coal,Clackmannan,,,,,,,,,NA,,,ironstone,,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,skeletons,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Some specimens reside in RSM (Royal Scottish Museum, Edinburgh).\r\n","RSM 1967/13/1 Acherontiscus caledoniae is though to have come from this location based on sediment analysis (Carroll, 1969)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Acherontiscus,n. gen.,NA,NA,vertebrate,R. L. Carroll. 1969. A new family of Carboniferous amphibians. Palaeontology 12,327,697,697,R. Butler,E. Dunne,E. Dunne,04/12/2015 09:45,01/03/2016 07:07,NA,caledoniae,Acherontiscus,40832,n. sp.,326.4,318.1,Pendleian,,NA,UK,Acherontiscus caledoniae
1307512,occ,NA,,80783,,Labyrinthodon n. sp. bucklandi,species,157514,recombined as,Dasyceps bucklandi,NA,species,157514,Paton,1975,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37054,NA,NA,NA,individuals,-1.575,52.375,Kenilworth,NA,,UK,England,Warwickshire,based on nearby landmark,seconds,small collection,""" [...] close to Kenilworth [...] "". Paton (1974) states that all the material collected from near Kenilworth comes from a single locality whose precise location is not known. Locality is ""probably now obscured by buildings"" (Paton 1974).",gp_mid,13.51,6.65,315,UK,,Kenilworth Sandstone,Warwickshire,,group of beds,,,,,,,NA,"The Kenilworth Sandstone is lowest Permian, possibly uppermost Carboniferous, and is a subunit of the Warwickshire Group (e.g., Powell et al., 2000, British Geological Survey Research Report RR/00/01; Ruffell et al., 2006, in Brenchley & Rawson (eds.), The Geology of England and Wales).","The Kenilworth Sandstone Formation is represented mainly by coarse grained siliciclastics (sandstones, conglomerates, breccias) deposited by freshwater action (Powell et al., 2000; Ruffell et al., 2006). ","""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,BGS,,,,,,GSM = Geological Survey Museum (British Geological Survey)\r\nGz = Warwick County Museum,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Labyrinthodon,,NA,NA,vertebrate,R. L. Paton. 1975. A Lower Permian temnospondylus amphibian from the English Midlands. Palaeontology 18(4):831-845,327,327,0,R. Butler,R. Butler,,07/12/2015 10:59,07/12/2015 10:59,30063,bucklandi,Dasyceps,57259,n. sp.,298.9,295.5,Asselian,,1,UK,Dasyceps bucklandi
1307605,occ,NA,,175248,members,Spathicephalus n. sp. pereger,species,332981,,Spathicephalus pereger,NA,species,332981,Baird,1962,Chordata,33815,Osteichthyes,34881,,NA,Spathicephalidae,332447,36973,NA,NA,NA,,-60.271,46.168999,near Point Edward,NA,"Sydney Harbour, Cape Breton",CA,Nova Scotia,,based on nearby landmark,3,local area,,gp_mid,-12.09,-20.77,108,CA,,Point Edward,Canso,,,,,,,,,NA,,,siltstone,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Spathicephalus,,NA,NA,vertebrate,D. Baird. 1962. A rhachitomous amphibian Spathicephalus from the Mississippian of Nova Scotia. Breviora 157:1-10,327,697,0,R. Butler,E. Dunne,,08/12/2015 07:03,08/12/2015 07:03,NA,pereger,Spathicephalus,57209,n. sp.,330.9,315.2,Serpukhovian,Bashkirian,NA,CA,Spathicephalus pereger
1307606,occ,NA,,175248,members,Pholiderpeton n. sp. bretonense,species,320847,,Pholiderpeton bretonense,NA,species,320847,Romer,1958,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37193,NA,NA,NA,,-60.271,46.168999,near Point Edward,NA,"Sydney Harbour, Cape Breton",CA,Nova Scotia,,based on nearby landmark,3,local area,,gp_mid,-12.09,-20.77,108,CA,,Point Edward,Canso,,,,,,,,,NA,,,siltstone,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Pholiderpeton,,NA,NA,vertebrate,A. S. Romer. 1958. An embolomere jaw from the mid-Carboniferous of Nova Scotia. Breviora 87:1-8,327,697,0,R. Butler,E. Dunne,,08/12/2015 07:07,08/12/2015 07:07,NA,bretonense,Pholiderpeton,57252,n. sp.,330.9,315.2,Serpukhovian,Bashkirian,NA,CA,Pholiderpeton bretonense
1307886,occ,NA,,117869,,n. gen. Utaherpeton n. sp. franklini,species,227377,,Utaherpeton franklini,NA,species,227377,Carroll et al.,1991,Chordata,33815,Osteichthyes,34881,Microsauria,37278,,NA,227376,NA,NA,NA,,-111.989998,40.41,"Traverse Mountains, Lehi",NA,,US,Utah,,based on nearby landmark,2,outcrop,Approximately 3 km north of Highway 73 and 16 km to the west to northwest of Lehi,gp_mid,-44.45,-2.17,101,US,FED,Manning Canyon,,,group of beds,,,,,,,NA,Lowestmost Pennsylvanian (Namurian B),,"""shale""",,lithified,,,,,,,,marginal marine indet.,,,macrofossils,,,,,,NA,,"adpression,soft parts",,,,,,,,,,NA,,,taxonomic,,,,,,Thomas Black,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Utaherpeton,n. gen.,NA,NA,vertebrate,"R. L. Carroll, P. Bybee, and W. D. Tidwell. 1991. The Oldest Microsaur (Amphibia). Palaeontology 65(2):314-322",327,697,0,R. Butler,E. Dunne,,10/12/2015 11:48,10/12/2015 11:48,37888,franklini,Utaherpeton,57328,n. sp.,323.2,315.2,Bashkirian,,NA,US,Utaherpeton franklini
1309988,occ,NA,,175806,members,Ophiderpeton n. sp. brownriggi,species,243095,,Ophiderpeton brownriggi,NA,species,243095,Wright and Huxley,1871,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Ophiderpetontidae,37252,37254,NA,NA,NA,,-7.203734,52.806236,Jarrow Colliery,NA,,IE,Lenister,,based on nearby landmark,6,local area,"located near Castlecomer, Co. Kilkenny",gp_mid,1.79,-6.34,315,IE,,,,,,,,,,,,NA,"Westphalian A according to Clack & Ahlberg, 2004",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,"Taxonomic list from location published in Wyse Jackson P. N. & Monaghan, N.T. (1995) Transfer of the Huxley and Wright (1867) Carboniferous amphibian and fish material to Trinity College Dublin from the National Museum of Ireland. J. Paleont. 69(3) pp. 602-603","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Ophiderpeton,,NA,NA,vertebrate,"E. P. Wright and T. H. Huxley. 1871. On a Collection of Fossil Vertebrata, from the Jarrow Colliery, County\r\nof Kilkenny, Ireland. Transactions of the Royal Irish Academy 24:351-370",327,697,697,R. Butler,E. Dunne,E. Dunne,12/01/2016 10:27,12/01/2016 10:28,NA,brownriggi,Ophiderpeton,57586,n. sp.,318.1,314.6,Westphalian A,,NA,IE,Ophiderpeton brownriggi
1310100,occ,NA,,175811,members,n. gen. Adelogyrinus n. sp. simorhynchus,species,227001,,Adelogyrinus simorhynchus,NA,species,227001,Watson,1929,Chordata,33815,Osteichthyes,34881,Adelospondyli,320812,Adelogyrinidae,37325,37326,NA,NA,NA,,-3.169395,55.883301,"Pentland Oil Works, near Loanhead",NA,,UK,Scotland,,based on nearby landmark,6,outcrop,Coordinates provided on Museum of the Scottish Shale Oil Industry website,gp_mid,-9.23,-28.22,313,UK,,,Oil Shale,,,,,,,,,NA,Part of the Dunnet Shale of the Oil Shale Group (now the Strathclyde Group),,"""shale""",,,,,,,,,,marine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Adelogyrinus,n. gen.,NA,NA,vertebrate,D. M. S. Watson. 1929. The Carboniferous Amphibia of Scotland. Palaeontologia Hungarica 1:223-252,327,697,0,R. Butler,E. Dunne,,13/01/2016 05:31,13/01/2016 05:31,NA,simorhynchus,Adelogyrinus,57610,n. sp.,346.7,330.9,Visean,,NA,UK,Adelogyrinus simorhynchus
1310101,occ,NA,,175812,members,n. gen. Dolichopareias n. sp. disjectus,species,229319,,Dolichopareias disjectus,NA,species,229319,Watson,1929,Chordata,33815,Osteichthyes,34881,Adelospondyli,320812,Adelogyrinidae,37325,37328,NA,NA,NA,,-3.161183,55.89584,"Burdiehouse Limestone, Burdiehouse, near Edinburgh",NA,,UK,Scotland,,based on nearby landmark,6,outcrop,,gp_mid,-9.22,-28.21,313,UK,,,Strathclyde,,,,,,,,,NA,"The Strathclyde Group (previously named the ""Oil Shale Group"") has been dated between the Chadian (Moliniacian) and Brigantian (Upper Dinantian) sub-ages according to the BGS.",,"""shale""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Royal Scottish Museum (RSM),,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Dolichopareias,n. gen.,NA,NA,vertebrate,D. M. S. Watson. 1929. The Carboniferous Amphibia of Scotland. Palaeontologia Hungarica 1:223-252,327,697,697,R. Butler,E. Dunne,E. Dunne,13/01/2016 05:53,03/02/2016 05:35,NA,disjectus,Dolichopareias,57610,n. sp.,346.7,330.9,Visean,,NA,UK,Dolichopareias disjectus
1310112,occ,NA,,175813,members,Dolichopareias disjectus,species,229319,,Dolichopareias disjectus,NA,species,229319,Watson,1929,Chordata,33815,Osteichthyes,34881,Adelospondyli,320812,Adelogyrinidae,37325,37328,NA,NA,NA,,-3.429201,56.061047,"Pitcorthie, Dunfermline",NA,"Pitcorthie, Fifeshire",UK,Scotland,,based on nearby landmark,6,outcrop,,gp_mid,-13.5,-32.42,313,UK,,,,,,,,,,,,NA,Calciferous Sandstone Series,,sandstone,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Royal Scottish Museum (RSM),,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Dolichopareias,,NA,NA,vertebrate,D. M. S. Watson. 1929. The Carboniferous Amphibia of Scotland. Palaeontologia Hungarica 1:223-252,327,697,0,R. Butler,E. Dunne,,13/01/2016 06:03,13/01/2016 06:03,NA,disjectus,Dolichopareias,57610,,358.9,346.7,Tournaisian,,NA,UK,Dolichopareias disjectus
1310125,occ,NA,,175821,members,n. gen. Crassigyrinus n. sp. scoticus,species,229317,,Crassigyrinus scoticus,NA,species,229317,Watson,1929,Chordata,33815,Osteichthyes,34881,,NA,Crassigyrinidae,339411,36967,NA,NA,NA,,-3.1268,55.910568,Gilmerton Ironstone,NA,near Ferniehill,UK,Scotland,,based on nearby landmark,6,outcrop,,gp_mid,-4.79,-20.35,313,UK,,,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Royal Scottish Museum (RSM),"RSM 272 C. scoticus is thought to be from here following analysis of the matrix characteristics (Watson, 1929)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Crassigyrinus,n. gen.,NA,NA,,D. M. S. Watson. 1929. The Carboniferous Amphibia of Scotland. Palaeontologia Hungarica 1:223-252,327,697,0,R. Butler,E. Dunne,,13/01/2016 07:54,13/01/2016 07:54,NA,scoticus,Crassigyrinus,57610,n. sp.,336,326.4,Brigantian,,NA,UK,Crassigyrinus scoticus
1310177,occ,NA,,174421,members,n. gen. Spathicephalus n. sp. mirus,species,332435,,Spathicephalus mirus,NA,species,332435,Watson,1929,Chordata,33815,Osteichthyes,34881,,NA,Spathicephalidae,332447,36973,NA,NA,NA,,-3.148056,55.877777,"Burghlee Ironstone, Loanhead, Midlothian",NA,Rumbles Ironstone,UK,Scotland,Midlothian,based on nearby landmark,seconds,outcrop,,gp_mid,0.32,-9.71,313,UK,,Limestone Coal,Clackmannan,,,,,,,,,NA,,,ironstone,,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,skeletons,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Some specimens reside in RSM (Royal Scottish Museum, Edinburgh).\r\n","RSM 1967/13/1 Acherontiscus caledoniae is though to have come from this location based on sediment analysis (Carroll, 1969)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Spathicephalus,n. gen.,NA,NA,vertebrate,D. M. S. Watson. 1929. The Carboniferous Amphibia of Scotland. Palaeontologia Hungarica 1:223-252,327,697,0,R. Butler,E. Dunne,,13/01/2016 09:49,13/01/2016 09:49,NA,mirus,Spathicephalus,57610,n. sp.,326.4,318.1,Pendleian,,NA,UK,Spathicephalus mirus
1310220,occ,NA,,67862,,n. gen. Opisthodontosaurus n. sp. carrolli,species,334471,,Opisthodontosaurus carrolli,NA,species,334471,Reisz et al.,2015,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,334470,NA,NA,NA,individuals,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Opisthodontosaurus,n. gen.,NA,NA,"paleoentomology,vertebrate","R. R. Reisz, A. R. H. LeBlanc, and C. A. Sidor, D. Scott, W. May. 2015. A new captorhinid reptile from the Lower Permian of Oklahoma showing remarkable dental and mandibular convergence with microsaurian tetrapods. The Science of Nature 102(9-10):50",315,334,0,J. Mueller,T. Liebrecht,,13/01/2016 17:46,13/01/2016 17:46,19393,carrolli,Opisthodontosaurus,57627,n. sp.,290.1,268,Leonard,,6,US,Opisthodontosaurus carrolli
1310610,occ,NA,,175907,members,n. gen. Bruktererpeton n. sp. fiebigi,species,229314,,Bruktererpeton fiebigi,NA,species,229314,Boy and Bandel,1973,Chordata,33815,Osteichthyes,34881,,NA,Gephyrostegidae,37202,37203,NA,NA,NA,,7.252115,51.316868,Schmiedestrasse Brickworks near Wuppertal,NA,,DE,Westphalia,,based on nearby landmark,6,outcrop,"The Quarry on the site of the Brickworks, Schmiedestrasse in Hasslinghausen, near Wuppertal (Westphalia, Germany)",gp_mid,10.84,-6.19,315,DE,,,,,,,,,,,,NA,"Namurian B = early Bashkirian, Marsdenian",,"""shale""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Specimens at Bergbaumuseum Bochum,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Bruktererpeton,n. gen.,NA,NA,vertebrate,J. A. Boy and K. Bandel. 1973. Bruktererpeton fiebili n. gen n. sp. (Amphibia: Gephyrostegida) Der erste Tetrapode au dem Rheinisch-Westfalischen barbon (Namur B; W.-Deutschland)\r\n(Bruktererpeton fiebili n. gen n. sp. (Amphibia: Gephyrostegida) The first Tetrapod form the Carboniferous of the Rhein-Ruhr-District (Namurian B; West-Germany)). Palaeontographica. Abteilung A A145(1-3):39-77,327,697,0,R. Butler,E. Dunne,,18/01/2016 07:40,18/01/2016 07:40,NA,fiebigi,Bruktererpeton,57650,n. sp.,318.1,314.6,Marsdenian,,NA,DE,Bruktererpeton fiebigi
1310769,occ,NA,,174421,members,Adelospondylus watsoni,species,229306,,Adelospondylus watsoni,NA,species,229306,Andrews and Carroll,1991,Chordata,33815,Osteichthyes,34881,Adelospondyli,320812,Adelogyrinidae,37325,37327,NA,NA,NA,,-3.148056,55.877777,"Burghlee Ironstone, Loanhead, Midlothian",NA,Rumbles Ironstone,UK,Scotland,Midlothian,based on nearby landmark,seconds,outcrop,,gp_mid,0.32,-9.71,313,UK,,Limestone Coal,Clackmannan,,,,,,,,,NA,,,ironstone,,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,skeletons,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Some specimens reside in RSM (Royal Scottish Museum, Edinburgh).\r\n","RSM 1967/13/1 Acherontiscus caledoniae is though to have come from this location based on sediment analysis (Carroll, 1969)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Adelospondylus,,NA,NA,vertebrate,S. M. Andrews and R. L. Carroll. 1991. The Order Adelospondyli: Carboniferous lepospondyl amphibians. Transactions of the Royal Society of Edinburgh 82(3):239-275,327,697,0,R. Butler,E. Dunne,,20/01/2016 04:39,20/01/2016 04:39,NA,watsoni,Adelospondylus,57679,,326.4,318.1,Pendleian,,NA,UK,Adelospondylus watsoni
1310771,occ,NA,,175937,members,Dendrysekos helogenes,species,336663,,Dendrysekos helogenes,NA,species,336663,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dendrerpetonidae,36994,336660,NA,NA,NA,,-64.451584,45.69809,Beach near Joggins,NA,"Head of Bay of Fundy, Coal Measures",CA,Nova Scotia,,based on nearby landmark,6,outcrop,"Coordinates based on the beach next to the Joggins Fossil Cliffs, Nova Scotia.",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,bed,,,,,,,NA,"Currently, the Cumberland Group is considered equivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163)",,sandstone,gray,,,,"""shale""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,coalified",,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Dendrysekos,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,697,R. Butler,E. Dunne,E. Dunne,20/01/2016 05:03,18/07/2016 05:23,NA,helogenes,Dendrysekos,57795,,318.1,314.6,Westphalian A,,NA,CA,Dendrysekos helogenes
1310935,occ,NA,,175806,members,Dendrerpeton n. sp. rugosum,species,334838,,Dendrerpeton rugosum,NA,species,334838,Clack and Milner,2015,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dendrerpetonidae,36994,36995,NA,NA,NA,,-7.203734,52.806236,Jarrow Colliery,NA,,IE,Lenister,,based on nearby landmark,6,local area,"located near Castlecomer, Co. Kilkenny",gp_mid,1.79,-6.34,315,IE,,,,,,,,,,,,NA,"Westphalian A according to Clack & Ahlberg, 2004",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,"Taxonomic list from location published in Wyse Jackson P. N. & Monaghan, N.T. (1995) Transfer of the Huxley and Wright (1867) Carboniferous amphibian and fish material to Trinity College Dublin from the National Museum of Ireland. J. Paleont. 69(3) pp. 602-603","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Dendrerpeton,,NA,NA,vertebrate,"J. A. Clack and A. R. Milner. 2015. Handbook of Paleoherpetology, Part 3A1: Basal Tetrapoda. ",327,697,0,R. Butler,E. Dunne,,20/01/2016 10:32,20/01/2016 10:32,NA,rugosum,Dendrerpeton,57666,n. sp.,318.1,314.6,Westphalian A,,NA,IE,Dendrerpeton rugosum
1310940,occ,NA,,175970,members,Eugyrinus n. sp. wildi,species,334979,,Eugyrinus wildi,NA,species,334840,Woodward,1891,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,36997,NA,NA,NA,,-2.135361,53.845917,"Carre Heys near Trawden, Lancashire",NA,,UK,,,based on nearby landmark,6,outcrop,,gp_mid,4.69,-4.97,315,UK,,Lower Coal Measures,,,,,,,,,,NA,Horizon - Langsettian (Western Europe),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eugyrinus,,NA,NA,vertebrate,A. S. Woodward. 1891. A microsaurian (Hylonomus wildi sp. nov.) from the Lancashire coalfield. Geological Magazine 8(3):211-213,327,697,0,R. Butler,E. Dunne,,20/01/2016 11:01,20/01/2016 11:01,NA,wildi,Eugyrinus,57697,n. sp.,318.1,314.6,Westphalian A,,NA,UK,Eugyrinus wildi
1311107,occ,NA,,157227,,Baphetes n. sp. kirkbyi,species,229310,,Baphetes kirkbyi,NA,species,229310,Watson,1929,Chordata,33815,Osteichthyes,34881,,NA,Baphetidae,227378,36970,NA,NA,NA,,-2.996578,56.19632,Pirnie Colliery,NA,,UK,Scotland,Fifeshire,,6,small collection,"Pirnie colliery, Fifeshire",gp_mid,5.7,0.38,313,UK,,Parrot Coal,,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,some,,,,,NA,,body,good,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,J. W. Kirkby,,"orig. in Hancock Museum, Newcastle",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Baphetes,,NA,NA,vertebrate,D. M. S. Watson. 1929. The Carboniferous Amphibia of Scotland. Palaeontologia Hungarica 1:223-252,327,697,0,R. Butler,E. Dunne,,22/01/2016 08:31,22/01/2016 08:31,57610,kirkbyi,Baphetes,57610,n. sp.,313.8,311.45,Kashirian,,NA,UK,Baphetes kirkbyi
1311118,occ,NA,,176017,members,Baphetes n. sp. planiceps,species,95780,,Baphetes planiceps,NA,species,95780,Clack and Milner,2015,Chordata,33815,Osteichthyes,34881,,NA,Baphetidae,227378,36970,NA,NA,NA,,-62.674999,45.565556,"Albion Mine, Stellarton",NA,,CA,Nova Scotia,,based on nearby landmark,seconds,outcrop,,gp_mid,-5.73,-8.68,108,CA,,,,,,,,,,,,NA,,,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,NHMUK,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Baphetes,,NA,NA,vertebrate,"J. A. Clack and A. R. Milner. 2015. Handbook of Paleoherpetology, Part 3A1: Basal Tetrapoda. ",327,697,0,R. Butler,E. Dunne,,22/01/2016 09:49,22/01/2016 09:49,NA,planiceps,Baphetes,57666,n. sp.,315.2,307,Moscovian,,NA,CA,Baphetes planiceps
1311120,occ,NA,,84835,,Baphetes n. sp. orientalis,species,335018,,Baphetes orientalis,NA,species,335018,Milner et al.,2009,Chordata,33815,Osteichthyes,34881,,NA,Baphetidae,227378,36970,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Baphetes,,NA,NA,vertebrate,"A. C. Milner, A. R. Milner, and S. A. Walsh. 2009. A new specimen of Baphetes from Nyrany, Czech Republic and the intrinsic relationships of the Baphetidae. Acta Zoologica 90:318-334",327,697,697,R. Butler,E. Dunne,E. Dunne,22/01/2016 10:02,11/03/2016 05:26,28608,orientalis,Baphetes,57720,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Baphetes orientalis
1311732,occ,NA,,175806,members,n. gen. Procochleosaurus n. sp. jarrowensis,species,204061,,Procochleosaurus jarrowensis,NA,species,204061,Sequeira,1996,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Cochleosauridae,36999,91480,NA,NA,NA,,-7.203734,52.806236,Jarrow Colliery,NA,,IE,Lenister,,based on nearby landmark,6,local area,"located near Castlecomer, Co. Kilkenny",gp_mid,1.79,-6.34,315,IE,,,,,,,,,,,,NA,"Westphalian A according to Clack & Ahlberg, 2004",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,"Taxonomic list from location published in Wyse Jackson P. N. & Monaghan, N.T. (1995) Transfer of the Huxley and Wright (1867) Carboniferous amphibian and fish material to Trinity College Dublin from the National Museum of Ireland. J. Paleont. 69(3) pp. 602-603","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Procochleosaurus,n. gen.,NA,NA,vertebrate,S. E. K. Sequeira. 1996. A cochleosaurid amphibian from the Upper Carboniferous of Ireland. Special Papers in Palaentology 52:65-80,327,697,0,R. Butler,E. Dunne,,27/01/2016 09:13,27/01/2016 09:13,NA,jarrowensis,Procochleosaurus,57796,n. sp.,318.1,314.6,Westphalian A,,NA,IE,Procochleosaurus jarrowensis
1311733,occ,NA,,176082,members,n. gen. Arkanserpeton n. sp. arcuatum,species,335284,nomen dubium,Temnospondyli,NA,unranked clade,36320,Lane,1932,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,NA,NA,NA,NA,,-93.767746,35.293682,"Paris, Logan County",NA,,US,Arkansas,,based on nearby landmark,6,small collection,"Based on location ""one mile west of Paris, Arkansas"" (Lane, 1932)",gp_mid,-27.97,-5.56,101,US,,Allegheny,Paris Shale,,,,,,,,,NA,"""Upper, but not uppermost, Pennsylvanian"" (Lane, 1932. Univ. Kansas. Science Bulletin: 17, 313-317)","Collections comes from the Eureka mine. The coal lies in the form of a saucer and the mine is ""located near the centre and bottom of the 'saucer'"" (Lane, 1932. Univ. Kansas. Science Bulletin: 17, 313-317)",coal,,,,,"""shale""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,KUVP,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Arkanserpeton,n. gen.,NA,NA,vertebrate,H. H. Lane. 1932. A new stegocephalian from the Pennsylvanian of Arkansas. Kansas University Science Bulletin 20:313-315,327,697,0,R. Butler,E. Dunne,,27/01/2016 09:36,27/01/2016 09:36,NA,arcuatum,,57797,n. sp.,307,303.7,Kasimovian,,NA,US, arcuatum
1311766,occ,NA,,176092,members,Colosteus scutellatus,species,344231,,Colosteus scutellatus,NA,species,335313,Hook and Baird,1994,Chordata,33815,Osteichthyes,34881,,NA,Colosteidae,36975,36976,NA,NA,NA,,-80.612236,40.989132,Five Points Coal Mine,NA,,US,Ohio,Mahoning County,based on nearby landmark,6,outcrop,"""Five Points, south of Youngstown, Mahoning County, Ohio"" Sues et al. (2013) Atl Geol.",gp_mid,-18.98,-8.63,101,US,,,Allegheny,,,,,,,,,NA,,,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Colosteus,,NA,NA,vertebrate,"R. W. Hook and D. Baird. 1994. A new fish and tetrapod assemblage from the Allegheny Group (late Westphalian, Upper Carboniferous) of eastern Ohio, USA. In U. Heidtke (ed.), New Research on Permo-Carboniferous Faunas ",327,697,0,R. Butler,E. Dunne,,28/01/2016 09:29,28/01/2016 09:29,NA,scutellatus,Colosteus,57803,,313.8,305.9,Desmoinesian,,NA,US,Colosteus scutellatus
1311815,occ,NA,,85292,,n. gen. Adamanterpeton n. sp. ohioensis,species,204060,,Adamanterpeton ohioensis,NA,species,204060,Milner and Sequeira,1998,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Cochleosauridae,36999,91481,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Adamanterpeton,n. gen.,NA,NA,vertebrate,"A. R. Milner and S. E. K. Sequeira. 1998. A cochleosaurid temnospondyl amphibian from the Middle Pennsylvanian of Linton, Ohio, U.S.A. Zoological Journal of the Linnean Society 122:261-290",327,697,0,R. Butler,E. Dunne,,28/01/2016 10:59,28/01/2016 10:59,28831,ohioensis,Adamanterpeton,57805,n. sp.,311.45,306.95,Westphalian D,,NA,US,Adamanterpeton ohioensis
1311853,occ,NA,,176110,members,n. gen. Astreptorhachis n. sp. ohioensis,species,335336,,Astreptorhachis ohioensis,NA,species,335336,Vaughn,1971,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37022,NA,NA,NA,,-80.769684,40.370838,near Steubenville,NA,,US,Ohio,Jefferson,estimated from map,6,outcrop,"Approximately 10 miles west of Steubenville, Wayne Township, Jefferson County",gp_mid,-15.18,-3.16,101,US,,,Conemaugh,,,,,,,,,NA,Fossils come from approx. 12 feet above Ames Limestone and 11 feet below Duquesne Coal. Conodonts indicate early Gzhelian age for Ames Limestone.,,"""shale""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,USNM,,,,,1953,Fossils collected by members of the Ohio Geological Society and the U.S. National Museum in the summer of 1953. ,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Astreptorhachis,n. gen.,NA,NA,vertebrate,"P. P. Vaughn. 1971. A Platyhystrix-like Amphibian with Fused Vertebrae, from the Upper Pennsylvanian of Ohio. Journal of Paleontology 45(3):464-469",327,697,0,R. Butler,E. Dunne,,29/01/2016 06:01,29/01/2016 06:01,NA,ohioensis,Astreptorhachis,57814,n. sp.,303.7,298.9,Gzhelian,,NA,US,Astreptorhachis ohioensis
1311891,occ,NA,,176119,members,n. gen. Ossinodus n. sp. pueri,species,242725,,Ossinodus pueri,NA,species,242725,Warren and Turner,2004,Chordata,33815,Osteichthyes,34881,,NA,Whatcheeriidae,179034,242723,NA,NA,NA,,147.383331,-23.933332,Middle Paddock site,NA,Queensland Museum Locality L1117,AU,Queensland,,stated in text,seconds,small collection,,gp_mid,151.34,-22.3,801,AU,,Ducabrook,,,formation,,,,,,,NA,,,sandstone,,,,,"""limestone""",,,,,deltaic indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Queensland Museum (QM F),,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ossinodus,n. gen.,NA,NA,vertebrate,A. A. Warren and S. Turner. 2004. The first stem tetrapod from the Early Carboniferous of Gondwana. Palaeontology 47(1):151-184,327,697,0,R. Butler,E. Dunne,,29/01/2016 08:45,29/01/2016 08:45,NA,pueri,Ossinodus,42429,n. sp.,346.7,330.9,Visean,,NA,AU,Ossinodus pueri
1311892,occ,NA,,176121,members,n. gen. Antlerpeton n. sp. clarkii,species,335354,,Antlerpeton clarkii,NA,species,335354,Thomson et al.,1998,Chordata,33815,Osteichthyes,34881,,NA,,NA,335353,NA,NA,NA,,-115.818565,39.582539,Upper part of Diamond Peak Formation,NA,,US,Nevada,Eureka,based on nearby landmark,6,small collection,"Upper part of the Diamond Peak Formation, Rock Canyon, Eureka County, Nevada (Diamond Springs 15' Quadrangle).",gp_mid,-57.17,-8.55,101,US,FED,,,,bed,,,,,,,NA,,,mudstone,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Antlerpeton,n. gen.,NA,NA,vertebrate,"K. S. Thomson, N. S. Shubin, and F. G. Poole. 1998. A problematic early tetrapod from the Mississippian of Nevada. Journal of Vertebrate Paleontology 18(2):315-320",327,697,0,R. Butler,E. Dunne,,29/01/2016 10:24,29/01/2016 10:24,NA,clarkii,Antlerpeton,57821,n. sp.,346.7,330.9,Visean,,NA,US,Antlerpeton clarkii
1313002,occ,NA,,175806,members,Ichthyerpeton bradleyae,species,320859,nomen dubium,Ichthyerpeton,NA,genus,192956,Clack and Milner,2015,Chordata,33815,Osteichthyes,34881,,NA,Colosteidae,36975,192956,NA,NA,NA,,-7.203734,52.806236,Jarrow Colliery,NA,,IE,Lenister,,based on nearby landmark,6,local area,"located near Castlecomer, Co. Kilkenny",gp_mid,1.79,-6.34,315,IE,,,,,,,,,,,,NA,"Westphalian A according to Clack & Ahlberg, 2004",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,"Taxonomic list from location published in Wyse Jackson P. N. & Monaghan, N.T. (1995) Transfer of the Huxley and Wright (1867) Carboniferous amphibian and fish material to Trinity College Dublin from the National Museum of Ireland. J. Paleont. 69(3) pp. 602-603","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ichthyerpeton,,NA,NA,vertebrate,"J. A. Clack and A. R. Milner. 2015. Handbook of Paleoherpetology, Part 3A1: Basal Tetrapoda. ",327,697,0,R. Butler,E. Dunne,,01/02/2016 03:33,01/02/2016 03:33,NA,bradleyae,Ichthyerpeton,57666,,318.1,314.6,Westphalian A,,NA,IE,Ichthyerpeton bradleyae
1313217,occ,NA,,175812,members,n. gen. Otocratia n. sp. modesta,species,335635,objective synonym of,Pholidogaster pisciformis,NA,species,320855,Watson,1929,Chordata,33815,Osteichthyes,34881,,NA,Colosteidae,36975,36978,NA,NA,NA,,-3.161183,55.89584,"Burdiehouse Limestone, Burdiehouse, near Edinburgh",NA,,UK,Scotland,,based on nearby landmark,6,outcrop,,gp_mid,-9.22,-28.21,313,UK,,,Strathclyde,,,,,,,,,NA,"The Strathclyde Group (previously named the ""Oil Shale Group"") has been dated between the Chadian (Moliniacian) and Brigantian (Upper Dinantian) sub-ages according to the BGS.",,"""shale""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Royal Scottish Museum (RSM),,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Otocratia,n. gen.,NA,NA,vertebrate,D. M. S. Watson. 1929. The Carboniferous Amphibia of Scotland. Palaeontologia Hungarica 1:223-252,327,697,0,R. Butler,E. Dunne,,03/02/2016 05:35,03/02/2016 05:35,NA,modesta,Pholidogaster,57610,n. sp.,346.7,330.9,Visean,,NA,UK,Pholidogaster modesta
1313219,occ,NA,,176232,members,Greererpeton sp.,genus,36977,,Greererpeton,NA,genus,36977,Clack and Milner,2015,Chordata,33815,Osteichthyes,34881,,NA,Colosteidae,36975,36977,NA,NA,NA,,-80.879997,37.66,Hinton District,NA,,US,West Virginia,,based on nearby landmark,2,small collection,Carboniferous shales of the Hinton District of West Virginia,gp_mid,-34.55,-26.46,101,US,,Hinton,Much Chunk,,,,,,,,,NA,,,"""shale""",,,,,sandstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Greererpeton,,NA,NA,vertebrate,"J. A. Clack and A. R. Milner. 2015. Handbook of Paleoherpetology, Part 3A1: Basal Tetrapoda. ",327,697,0,R. Butler,E. Dunne,,03/02/2016 06:18,03/02/2016 06:18,NA,sp.,Greererpeton,57666,,330.9,323.2,Serpukhovian,,NA,US,Greererpeton sp.
1313220,occ,NA,,68319,,Greererpeton sp.,genus,36977,,Greererpeton,NA,genus,36977,Clack and Milner,2015,Chordata,33815,Osteichthyes,34881,,NA,Colosteidae,36975,36977,NA,NA,NA,,-88.966667,37.549999,Goreville,NA,KU-IL-10,US,Illinois,Johnston,based on nearby landmark,minutes,outcrop,"""an inactive limestone quarry on private property in T12S R2E, some six km south of Goreville"" (coordinate based on Goreville)",gp_mid,-35.6,-18.77,101,US,FED,Kinkaid,,Cave Hill,member,,,,,,,NA,,"""a sequence of gray and red sandy mudstones... vertebrates... occur in calcareous nodules within the mudstone""",mudstone,"gray,red",,"sandy,calcareous",,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""matrix around the bone is a yellow-brown mudstone with calcareous inclusions""",taxonomic,"surface (in situ),mechanical,field collection",,,,,,,"collection of ""specimens accessible at the surface of the exposure""",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Greererpeton,,NA,NA,vertebrate,"J. A. Clack and A. R. Milner. 2015. Handbook of Paleoherpetology, Part 3A1: Basal Tetrapoda. ",327,697,0,R. Butler,E. Dunne,,03/02/2016 06:19,03/02/2016 06:19,19657,sp.,Greererpeton,57666,,326.4,318.1,Arnsbergian,,NA,US,Greererpeton sp.
1313221,occ,NA,,124949,,Crassigyrinus sp.,genus,36967,,Crassigyrinus,NA,genus,36967,Godfrey,1988,Chordata,33815,Osteichthyes,34881,,NA,Crassigyrinidae,339411,36967,NA,NA,NA,,-79.848999,39.571999,Greer,NA,,US,West Virginia,Monongalia,,3,,,gp_mid,-28.08,-21,101,US,,Bluefield,,Bickett Shale,member,,,,,,,NA,,,"""shale""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,"vertebrae,limb elements",,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,"selective quarrying,survey of museum collection",,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Crassigyrinus,,NA,NA,vertebrate,S. J. Godfrey. 1988. Isolated tetrapod remains from the Carboniferous of West Virginia. Kirtlandia 43:27-36,327,697,0,R. Butler,E. Dunne,,03/02/2016 06:28,03/02/2016 06:28,40904,sp.,Crassigyrinus,40494,,326.4,318.1,Arnsbergian,,NA,US,Crassigyrinus sp.
1313222,occ,NA,,176232,members,Crassigyrinus sp.,genus,36967,,Crassigyrinus,NA,genus,36967,Godfrey,1988,Chordata,33815,Osteichthyes,34881,,NA,Crassigyrinidae,339411,36967,NA,NA,NA,,-80.879997,37.66,Hinton District,NA,,US,West Virginia,,based on nearby landmark,2,small collection,Carboniferous shales of the Hinton District of West Virginia,gp_mid,-34.55,-26.46,101,US,,Hinton,Much Chunk,,,,,,,,,NA,,,"""shale""",,,,,sandstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Crassigyrinus,,NA,NA,vertebrate,S. J. Godfrey. 1988. Isolated tetrapod remains from the Carboniferous of West Virginia. Kirtlandia 43:27-36,327,697,0,R. Butler,E. Dunne,,03/02/2016 06:29,03/02/2016 06:29,NA,sp.,Crassigyrinus,40494,,330.9,323.2,Serpukhovian,,NA,US,Crassigyrinus sp.
1313223,occ,NA,,176232,members,Crassigyrinus indet.,genus,36967,,Crassigyrinus,NA,genus,36967,Panchen and Smithson,1990,Chordata,33815,Osteichthyes,34881,,NA,Crassigyrinidae,339411,36967,NA,NA,NA,,-80.879997,37.66,Hinton District,NA,,US,West Virginia,,based on nearby landmark,2,small collection,Carboniferous shales of the Hinton District of West Virginia,gp_mid,-34.55,-26.46,101,US,,Hinton,Much Chunk,,,,,,,,,NA,,,"""shale""",,,,,sandstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Crassigyrinus,,NA,NA,vertebrate,A. L. Panchen and T. R. Smithson. 1990. The pelvic girdle and hind limb of Crassigyrinus scoticus (Lydekker) from the Scottish Carboniferous and the origin of the tetrapod pelvic skeleton. Transactions of the Royal Society of Edinburgh 81:31-44,327,697,0,R. Butler,E. Dunne,,03/02/2016 06:38,03/02/2016 06:38,NA,indet.,Crassigyrinus,57900,,330.9,323.2,Serpukhovian,,NA,US,Crassigyrinus indet.
1313224,occ,NA,,175248,members,Colosteidae indet.,family,36975,,Colosteidae,NA,family,36975,Carroll et al.,1972,Chordata,33815,Osteichthyes,34881,,NA,Colosteidae,36975,NA,NA,NA,NA,,-60.271,46.168999,near Point Edward,NA,"Sydney Harbour, Cape Breton",CA,Nova Scotia,,based on nearby landmark,3,local area,,gp_mid,-12.09,-20.77,108,CA,,Point Edward,Canso,,,,,,,,,NA,,,siltstone,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Colosteidae,,NA,NA,vertebrate,"R. L. Carroll, E. S. Belt, and D. L. Dineley, D. Baird, D. C. McGregor . 1972. In D. J. Glass (ed.), Guidebook: Excursion A59. Vertebrate Palaeontology of Eastern Canada ",327,697,0,R. Butler,E. Dunne,,03/02/2016 06:55,03/02/2016 06:55,NA,indet.,,57902,,330.9,315.2,Serpukhovian,Bashkirian,NA,CA, indet.
1313230,occ,NA,,176233,members,Greererpeton indet.,genus,36977,,Greererpeton,NA,genus,36977,Panchen,1975,Chordata,33815,Osteichthyes,34881,,NA,Colosteidae,36975,36977,NA,NA,NA,,-61.032768,46.55032,Grand Etang,NA,,CA,Nova Scotia,Cape Breton Island,based on nearby landmark,6,small collection,,gp_mid,-15.63,-24.76,108,CA,,Pomquet,Mabou,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Greererpeton,,NA,NA,vertebrate,A. L. Panchen. 1975. A new genus and species of anthracosaur amphibian from the Lower Carboniferous of Scotland and the status of Pholidogaster pisciformis Huxley. Transactions of the Royal Society of London B 269:581-640,327,697,697,R. Butler,E. Dunne,E. Dunne,03/02/2016 08:18,03/02/2016 08:18,NA,indet.,Greererpeton,57903,,330.9,323.2,Serpukhovian,,NA,CA,Greererpeton indet.
1313231,occ,NA,,176234,members,Colosteidae indet.,family,36975,,Colosteidae,NA,family,36975,Clack et al.,2012,Chordata,33815,Osteichthyes,34881,,NA,Colosteidae,36975,NA,NA,NA,NA,,-90.21302,38.554279,Upper St. Louis Limestone,NA,,US,Missouri,,based on nearby landmark,6,,"Exact location of where fossils were found cannot be determined (Clack et al., 2012)",gp_mid,-49.87,-27.14,101,US,,,,,,,,,,,,NA,,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Colosteidae,,NA,NA,vertebrate,"J. A. Clack, F. Witzmann, and J. Muller, D. Snyder. 2012. A Colosteid-Like Early Tetrapod from the St. Louis Limestone (Early Carboniferous, Meramecian), St. Louis, Missouri, USA. Fieldiana: Life and Earth Sciences 5:17-39",327,697,0,R. Butler,E. Dunne,,03/02/2016 08:37,03/02/2016 08:37,NA,indet.,,57904,,346.7,330.9,Visean,,NA,US, indet.
1313276,occ,NA,,176241,members,Baphetes kirkbyi,species,229310,,Baphetes kirkbyi,NA,species,229310,Milner and Lindsay,1998,Chordata,33815,Osteichthyes,34881,,NA,Baphetidae,227378,36970,NA,NA,NA,,-2.680268,53.523235,opencast coal mine at Winstanley,NA,Tan Pit Slip opencast coal mining site,UK,England,,based on nearby landmark,6,small collection,,gp_mid,2.62,-8.46,315,UK,,,,,,,,,,,,NA,Ince Coals,,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Baphetes,,NA,NA,vertebrate,A. C. Milner and W. Lindsay. 1998. Postcranial remains of Buphetes and their bearing on the relationships of the Baphetidae (=Loxommatidae). Zoological Journal of the Linnean Society 122:211-235,327,697,0,R. Butler,E. Dunne,,03/02/2016 11:17,03/02/2016 11:17,NA,kirkbyi,Baphetes,57908,,323.2,315.2,Bashkirian,,NA,UK,Baphetes kirkbyi
1313310,occ,NA,,176242,members,Baphetes kirkbyi,species,229310,,Baphetes kirkbyi,NA,species,229310,Smithson,1985,Chordata,33815,Osteichthyes,34881,,NA,Baphetidae,227378,36970,NA,NA,NA,,-4.035153,55.740074,"Quarter, near Hamilton, Strathclyde Region",NA,,UK,Scotland,,based on nearby landmark,6,small collection,,gp_mid,5.18,-0.15,313,UK,,,,,,,,,,,,NA,"Airdie or ""Mushet's"" Black Bank Ironstone. Middle Coal Measures, Westphalian, Silesian.",,sandstone,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Baphetes,,NA,NA,vertebrate,T. R. Smithson. 1985. Scottish Carboniferous amphibian localities. Scottish Journal of Geology 21(2):123-142,327,697,0,R. Butler,E. Dunne,,03/02/2016 12:15,03/02/2016 12:15,NA,kirkbyi,Baphetes,57909,,318.1,306.95,Westphalian,,NA,UK,Baphetes kirkbyi
1313311,occ,NA,,176242,members,Anthracosaurus russelli,species,229307,,Anthracosaurus russelli,NA,species,229307,Smithson,1985,Chordata,33815,Osteichthyes,34881,,NA,Anthracosauridae,37199,37200,NA,NA,NA,,-4.035153,55.740074,"Quarter, near Hamilton, Strathclyde Region",NA,,UK,Scotland,,based on nearby landmark,6,small collection,,gp_mid,5.18,-0.15,313,UK,,,,,,,,,,,,NA,"Airdie or ""Mushet's"" Black Bank Ironstone. Middle Coal Measures, Westphalian, Silesian.",,sandstone,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Anthracosaurus,,NA,NA,vertebrate,T. R. Smithson. 1985. Scottish Carboniferous amphibian localities. Scottish Journal of Geology 21(2):123-142,327,697,0,R. Butler,E. Dunne,,03/02/2016 12:15,03/02/2016 12:15,NA,russelli,Anthracosaurus,57909,,318.1,306.95,Westphalian,,NA,UK,Anthracosaurus russelli
1313312,occ,NA,,176242,members,Pholiderpeton sp.,genus,37193,,Pholiderpeton,NA,genus,37193,Smithson,1985,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37193,NA,NA,NA,,-4.035153,55.740074,"Quarter, near Hamilton, Strathclyde Region",NA,,UK,Scotland,,based on nearby landmark,6,small collection,,gp_mid,5.18,-0.15,313,UK,,,,,,,,,,,,NA,"Airdie or ""Mushet's"" Black Bank Ironstone. Middle Coal Measures, Westphalian, Silesian.",,sandstone,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Pholiderpeton,,NA,NA,vertebrate,T. R. Smithson. 1985. Scottish Carboniferous amphibian localities. Scottish Journal of Geology 21(2):123-142,327,697,0,R. Butler,E. Dunne,,03/02/2016 12:15,03/02/2016 12:15,NA,sp.,Pholiderpeton,57909,,318.1,306.95,Westphalian,,NA,UK,Pholiderpeton sp.
1313314,occ,NA,,176232,members,Doragnathus sp.,genus,36986,,Doragnathus,NA,genus,36986,Clack and Milner,2015,Chordata,33815,Osteichthyes,34881,,NA,,NA,36986,NA,NA,NA,,-80.879997,37.66,Hinton District,NA,,US,West Virginia,,based on nearby landmark,2,small collection,Carboniferous shales of the Hinton District of West Virginia,gp_mid,-34.55,-26.46,101,US,,Hinton,Much Chunk,,,,,,,,,NA,,,"""shale""",,,,,sandstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Doragnathus,,NA,NA,vertebrate,"J. A. Clack and A. R. Milner. 2015. Handbook of Paleoherpetology, Part 3A1: Basal Tetrapoda. ",327,697,0,R. Butler,E. Dunne,,03/02/2016 12:36,03/02/2016 12:36,NA,sp.,Doragnathus,57666,,330.9,323.2,Serpukhovian,,NA,US,Doragnathus sp.
1313315,occ,NA,,22726,,Doragnathus sp.,genus,36986,,Doragnathus,NA,genus,36986,Smithson and Clack,2013,Chordata,33815,Osteichthyes,34881,,NA,,NA,36986,NA,NA,NA,,-3.35,56.1166,Cowdenbeath Amphibian Bonebed,NA,ETE Locality 1605; Dora Opencast Coal Site,UK,,,,4,outcrop,"""south-east of Cowdenbeath... a section 30 m long""",gp_mid,0.18,-9.49,313,UK,,,Limestone Coal,,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min\r\n""lower Namurian A... 62 m beneath the base of the Index Limestone [which is]... at the junction between the top of the Pendleian (E1) and the base of the Arnsbergian (E2) stages"": originally entered as Namurian to Bashkirian","ETE rock type adj: ""rooty,muddy"", ETE lithology comments: 0\r\n""a localised patch in a seatrock (rooty, muddy siltstone)""",siltstone,,,,,,,,,,terrestrial indet.,,,,,,,,,NA,,,,,,,,,,,,NA,,,general faunal/floral,,,,7 specimens,,,1974 and 1975,"ETE Size: .; ETE reference list: 478, 479, 483, 482, 485, 454, 81, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Doragnathus,,NA,NA,,T. R. Smithson and J. A. Clack. 2013. Tetrapod appendicular skeletal elements from the Early Carboniferous of Scotland. Comptes Rendus Palevol 12:405-417,327,697,0,R. Butler,E. Dunne,,03/02/2016 12:46,03/02/2016 12:46,5931,sp.,Doragnathus,57910,,326.4,318.1,Pendleian,,NA,UK,Doragnathus sp.
1313317,occ,NA,,176243,members,Doragnathus ? sp.,genus,36986,,Doragnathus,NA,genus,36986,Smithson and Clack,2013,Chordata,33815,Osteichthyes,34881,,NA,,NA,36986,NA,NA,NA,,-3.136601,56.033024,Isle of Inchkeith,NA,,UK,Scotland,Fife,based on nearby landmark,6,small collection,,gp_mid,-9.2,-28.07,313,UK,,,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Doragnathus,?,NA,NA,vertebrate,T. R. Smithson and J. A. Clack. 2013. Tetrapod appendicular skeletal elements from the Early Carboniferous of Scotland. Comptes Rendus Palevol 12:405-417,327,697,0,R. Butler,E. Dunne,,03/02/2016 12:57,03/02/2016 12:57,NA,sp.,Doragnathus,57910,,346.7,330.9,Visean,,NA,UK,Doragnathus sp.
1314461,occ,NA,,175806,members,Ophiderpeton sp.,genus,37254,,Ophiderpeton,NA,genus,37254,Milner,1994,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Ophiderpetontidae,37252,37254,NA,NA,NA,,-7.203734,52.806236,Jarrow Colliery,NA,,IE,Lenister,,based on nearby landmark,6,local area,"located near Castlecomer, Co. Kilkenny",gp_mid,1.79,-6.34,315,IE,,,,,,,,,,,,NA,"Westphalian A according to Clack & Ahlberg, 2004",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,"Taxonomic list from location published in Wyse Jackson P. N. & Monaghan, N.T. (1995) Transfer of the Huxley and Wright (1867) Carboniferous amphibian and fish material to Trinity College Dublin from the National Museum of Ireland. J. Paleont. 69(3) pp. 602-603","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Ophiderpeton,,NA,NA,vertebrate,"A. C. Milner. 1994. The astopod amphibian from the Vis̩an of East Kirkton, West Lothian, Scotland. Transactions of the Royal Society of Edinburgh: Earth Sciences 84:363-368",327,697,0,R. Butler,E. Dunne,,09/02/2016 07:57,09/02/2016 07:57,NA,sp.,Ophiderpeton,42474,,318.1,314.6,Westphalian A,,NA,IE,Ophiderpeton sp.
1314652,occ,NA,,125662,,Cochleosaurus bohemicus,species,204052,,Cochleosaurus bohemicus,NA,species,204051,Augusta,1947,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Cochleosauridae,36999,37001,NA,NA,NA,,13.395,49.814999,Tremosna,NA,"Temon̩, Temon",CZ,,,based on nearby landmark,3,outcrop,,gp_mid,19.75,0.69,305,CZ,,Kladno,,Nyrany,,,,,,,,NA,Tremosna in B̦hmen. Mittleres Obercarbon.,,not reported,,,,,coal,,,,,terrestrial indet.,rift,"Central-West Bohemian basin; extensional basin developed within Variscan zone along simple asymmetric mega-graben formed on the Central Bohemian and Litomerice fault zones, with some contribution from transtensional wrench faults.",macrofossils,,,,,,NA,,mold/impression,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Cochleosaurus,,NA,NA,"paleoentomology,vertebrate",J. Augusta. 1947. Prispevek k poznani stegocephalu z Tremosenskeho svrchniho Karbonu (Cochleosaurus bohemicus Fr.) [in Czech]. Priroda Brno 39:145-149,327,697,0,R. Butler,E. Dunne,,11/02/2016 10:07,11/02/2016 10:07,50906,bohemicus,Cochleosaurus,58036,,311.45,306.95,Westphalian D,,NA,CZ,Cochleosaurus bohemicus
1314660,occ,NA,,80111,,Cochleosaurus n. sp. florensis,species,204062,,Cochleosaurus florensis,NA,species,204062,Rieppel,1980,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Cochleosauridae,36999,37001,NA,NA,NA,,-60.266666,46.290001,Dominion Coal Co. strip mine No. 7,NA,"Sydney coal field; Florence, Cape Breton",CA,Nova Scotia,Cape Breton Island,estimated from map,seconds,small collection,"Dominion Coal Co. strip mine No. 7, about 2 miles north of the town of Florence",gp_mid,-3.96,-8.17,108,CA,,,Morien,,group of beds,,,,,,,NA,"""... above the Lloyd Cove (Lower Bonar) coal of the Morien group."" ",,coal,,,,Y,"""shale""",,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,permineralized,,autochthonous,snapshot,,,,,,,NA,,the vertebrate remains come from the interior of fossilized tree stumps and are completely disarticulated,taxonomic,"selective quarrying,survey of museum collection",MCZ,,,,A.S. Romer,1956,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Cochleosaurus,,NA,NA,,O. Rieppel. 1980. The edopoid amphibian Cochleosaurus from the middle Pennsylvanian of Nova Scotia. Palaeontology 23:143-150,327,697,0,R. Butler,E. Dunne,,11/02/2016 10:43,11/02/2016 10:43,26895,florensis,Cochleosaurus,58037,n. sp.,314.6,306.95,Westphalian C,Westphalian D,NA,CA,Cochleosaurus florensis
1314749,occ,NA,,79162,,Neldasaurus wrightae,species,229335,,Neldasaurus wrightae,NA,species,229335,Chase,1965,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,36989,NA,NA,NA,individuals,-98.650002,33.583332,Archer City Bonebed 1 (Putnam Fm.),NA,"Locality IIIf (Romer & Price, 1940)",US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Neldasaurus,,NA,NA,vertebrate,"J. N. Chase. 1965. Neldasaurus wrightae, a new rhachitomous labyrinthodont from the Texas Lower Permian. Bulletin of the Museum of Comparative Zoology 133:153-225",327,697,697,R. Butler,E. Dunne,E. Dunne,12/02/2016 05:39,24/08/2016 05:22,43845,wrightae,Neldasaurus,58054,,296.4,268,Wolfcamp,,2,US,Neldasaurus wrightae
1314750,occ,NA,,176438,members,n. gen. Neldasaurus n. sp. wrightae,species,229335,,Neldasaurus wrightae,NA,species,229335,Chase,1965,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,36989,NA,NA,NA,,-98.777206,33.42646,"Terrapin School, Archer County",NA,,US,Texas,Archer,based on nearby landmark,6,small collection,,gp_mid,-30.24,-1.34,101,US,,Archer City,Bowie,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,A. S. Romer Party 1954,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Neldasaurus,n. gen.,NA,NA,vertebrate,"J. N. Chase. 1965. Neldasaurus wrightae, a new rhachitomous labyrinthodont from the Texas Lower Permian. Bulletin of the Museum of Comparative Zoology 133:153-225",327,697,0,R. Butler,E. Dunne,,12/02/2016 06:03,12/02/2016 06:03,NA,wrightae,Neldasaurus,58054,n. sp.,296.4,268,Wolfcamp,,NA,US,Neldasaurus wrightae
1314753,occ,NA,,137131,,Neldasaurus wrightae,species,229335,,Neldasaurus wrightae,NA,species,229335,Chase,1965,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,36989,NA,NA,NA,,-98,33,northwest of Padgett,NA,,US,Texas,Young,based on nearby landmark,degrees,small collection,1 mile NNW of Padgett,gp_mid,-29.94,-2.1,101,US,,Moran,Wichita,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,MCZ,,,,A. Romer,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Neldasaurus,,NA,NA,vertebrate,"J. N. Chase. 1965. Neldasaurus wrightae, a new rhachitomous labyrinthodont from the Texas Lower Permian. Bulletin of the Museum of Comparative Zoology 133:153-225",327,697,0,R. Butler,E. Dunne,,12/02/2016 08:37,12/02/2016 08:37,43841,wrightae,Neldasaurus,58054,,298.9,272.3,Asselian,Kungurian,NA,US,Neldasaurus wrightae
1314763,occ,NA,,176442,members,Neldasaurus wrightae,species,229335,,Neldasaurus wrightae,NA,species,229335,Chase,1965,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,36989,NA,NA,NA,,-98.627838,33.65551,South Fork of the Little Wichita River,NA,,US,Texas,Archer County,stated in text,6,small collection,"""10 miles west of Anarene in Archer County"" (Chase, 1965)",gp_mid,-30.01,-1.21,101,US,,Putnam,Wichita,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,R. V. Witter,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Neldasaurus,,NA,NA,vertebrate,"J. N. Chase. 1965. Neldasaurus wrightae, a new rhachitomous labyrinthodont from the Texas Lower Permian. Bulletin of the Museum of Comparative Zoology 133:153-225",327,697,0,R. Butler,E. Dunne,,12/02/2016 09:31,12/02/2016 09:31,NA,wrightae,Neldasaurus,58054,,296.4,268,Wolfcamp,,NA,US,Neldasaurus wrightae
1315229,occ,NA,,176495,members,n. gen. Edops n. sp. craigi,species,252444,,Edops craigi,NA,species,252444,Romer,1936,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Edopidae,37004,37005,NA,NA,NA,,-98.910736,33.301155,"Padgett, Young County (Archer City Formation)",NA,,US,Texas,Young County,based on nearby landmark,6,small collection,,gp_mid,-30.43,-1.44,101,US,,Archer City,Bowie,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"MCZ,USNM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Edops,n. gen.,NA,NA,vertebrate,A. S. Romer. 1936. Studies on American Permo-Carboniferous reptiles. Problems of Paleontology 1:85-93,327,697,0,R. Butler,E. Dunne,,15/02/2016 04:39,15/02/2016 04:39,NA,craigi,Edops,43841,n. sp.,303.7,268,Gzhelian,Wolfcamp,NA,US,Edops craigi
1315230,occ,NA,,176438,members,Edops craigi,species,252444,,Edops craigi,NA,species,252444,Romer and Witter,1942,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Edopidae,37004,37005,NA,NA,NA,,-98.777206,33.42646,"Terrapin School, Archer County",NA,,US,Texas,Archer,based on nearby landmark,6,small collection,,gp_mid,-30.24,-1.34,101,US,,Archer City,Bowie,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,A. S. Romer Party 1954,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Edops,,NA,NA,vertebrate,"A. S. Romer and R. V. Witter. 1942. Edops, a primitive rhachitomous amphibian from the Texas Red Beds. Journal of Geology 50:925-960",327,697,0,R. Butler,E. Dunne,,15/02/2016 04:45,15/02/2016 04:45,NA,craigi,Edops,58099,,296.4,268,Wolfcamp,,NA,US,Edops craigi
1315231,occ,NA,,132661,,Edops craigi,species,252444,,Edops craigi,NA,species,252444,Romer and Witter,1942,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Edopidae,37004,37005,NA,NA,NA,,-98.777496,33.449722,Cottonwood Creek (Moran Fm.),NA,,US,Texas,Archer,estimated from map,seconds,outcrop,Cottonwood creek (headwaters),gp_mid,-30.65,-2.02,101,US,,Archer City,Wichita,,group of beds,,,,,,,NA,"Moran Formation, Wichita Group.",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Edops,,NA,NA,vertebrate,"A. S. Romer and R. V. Witter. 1942. Edops, a primitive rhachitomous amphibian from the Texas Red Beds. Journal of Geology 50:925-960",327,697,0,R. Butler,E. Dunne,,15/02/2016 04:59,15/02/2016 04:59,42726,craigi,Edops,58099,,298.9,295.5,Asselian,,NA,US,Edops craigi
1315232,occ,NA,,176496,members,Edops craigi,species,252444,,Edops craigi,NA,species,252444,Romer and Witter,1942,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Edopidae,37004,37005,NA,NA,NA,specimens,-98.36972,33.608334,"Antelope, Jack County (Pueblo Formation)",NA,,US,Texas,Jack Couty,based on nearby landmark,seconds,small collection,,gp_mid,-30.28,-2.07,101,US,,Pueblo,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Edops,,NA,NA,vertebrate,"A. S. Romer and R. V. Witter. 1942. Edops, a primitive rhachitomous amphibian from the Texas Red Beds. Journal of Geology 50:925-960",327,697,697,R. Butler,E. Dunne,E. Dunne,15/02/2016 05:26,01/09/2017 06:58,NA,craigi,Edops,58099,,298.9,295.5,Asselian,,2,US,Edops craigi
1315233,occ,NA,,176497,members,Edops sp.,genus,37005,,Edops,NA,genus,37005,Vaughn,1969,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Edopidae,37004,37005,NA,NA,NA,,-105.991135,33.018906,Domingo Quarry (Abo Formation),NA,,US,New Mexico,Otero County,based on nearby landmark,6,small collection,,gp_mid,-35.48,1.67,101,US,,Abo,,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Edops,,NA,NA,vertebrate,P. P. Vaughn. 1969. Upper Pennsylvanian vertebrates from the Sangre de Cristo Formation of central Colorado. Los Angeles County Museum Contributions in Science 164:1-28,327,697,0,R. Butler,E. Dunne,,15/02/2016 05:50,15/02/2016 05:50,NA,sp.,Edops,57813,,296.4,268,Wolfcamp,Leonard,NA,US,Edops sp.
1315234,occ,NA,,176498,members,Edops sp.,genus,37005,,Edops,NA,genus,37005,Hlavin,1972,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Edopidae,37004,37005,NA,NA,NA,,-81.605141,39.289009,"Belpre, Washington County",NA,,US,Ohio,,based on nearby landmark,6,small collection,,gp_mid,-15.49,-2.73,101,US,,Washington,Dunkard,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Edops,,NA,NA,,"W. J. Hlavin. 1972. Early Permian vertebrate from the Upper Washington Formation at Belpre, Ohio. In: I.C. White Memorial Symposium Field Trip Guide ",327,697,697,R. Butler,E. Dunne,E. Dunne,15/02/2016 05:58,15/02/2016 05:59,NA,sp.,Edops,58100,,295.5,290.1,Sakmarian,,NA,US,Edops sp.
1315235,occ,NA,,176499,members,Chenoprosopus n. sp. lewisi,species,204063,subjective synonym of,Chenoprosopus milleri,NA,species,139020,Hook,1993,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Cochleosauridae,36999,37000,NA,NA,NA,,-98.258888,33.473888,"Shannon, Clay County",NA,,US,Texas,Clay County,based on nearby landmark,6,small collection,,gp_mid,-29.87,-1.58,101,US,,Markley,Bowie,,,,,,,,,NA,Location at Vigilian/Wolfcampian boundary,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,adpression",,,,,,,,,,NA,,,taxonomic,,UNSM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Chenoprosopus,,NA,NA,vertebrate,"R. W. Hook. 1993. Chenoprosopus lewisi, a new cochleosaurid amphibian (Amphibia: Temnospondyli) from the Permo-Carboniferous of north-central Texas. Annals of Carnegie Museum 62:273-291",327,697,0,R. Butler,E. Dunne,,15/02/2016 06:42,15/02/2016 06:42,NA,lewisi,Chenoprosopus,58101,n. sp.,303.4,268,Virgilian,Wolfcamp,NA,US,Chenoprosopus lewisi
1315301,occ,NA,,176523,members,n. gen. Lafonius n. sp. lehmani,species,336709,,Lafonius lehmani,NA,species,336709,Berman,1973,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36987,NA,NA,NA,,-106.398697,35.011879,Manzanita Mountains,NA,,US,New Mexico,Bernalillo,based on nearby landmark,6,,"Collected from a shale bed exposed over an area of about 1/2 acre just west of State Highway 10 and about 13.7 km (8.5 miles) south of its intersection with U. S. Highway 66, in SE1V sec. 18, T. 9 N., R. 6 E. Bernalillo County, New Mexico. ",gp_mid,-35.43,2.05,101,US,FED,Atrasado,Madera,Pine Shadow,bed,,,,,,,NA,"""Unit C of Madera Formation."" Middle Virgilian in age.",,"""shale""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,adpression",,,,,,,,,,NA,,,taxonomic,,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Lafonius,n. gen.,NA,NA,vertebrate,D. S. Berman. 1973. A trimerorhachid amphibian from the Upper Pennsylvanian of New Mexico. Journal of Paleontology 47:932-945,327,697,0,R. Butler,E. Dunne,,16/02/2016 04:44,16/02/2016 04:44,NA,lehmani,Lafonius,58129,n. sp.,303.7,298.9,Gzhelian,,NA,US,Lafonius lehmani
1315325,occ,NA,,154179,,n. gen. Dawsonia n. sp. polydens,species,336780,recombined as,Dawsonerpeton polydens,NA,species,336780,Fritsch,1879,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,336806,NA,NA,NA,,13.675,50.209999,"Kounov, Rakovnik District",NA,Kounova,CZ,,,based on nearby landmark,2,outcrop,"""Kounova lies some 35 miles northwest of Prague in the Rakonitz coal basin"" Romer (1945)\r\nPreviously in area known as Bohemia",gp_mid,21.74,4.64,305,CZ,,Slany,,Kounov,group of beds,,,,,,,NA,,,"""siliciclastic""",,lithified,,,,,,,,terrestrial indet.,rift,"Central-West Bohemian basin; extensional basin developed within Variscan zone along simple asymmetric mega-graben formed on the Central Bohemian and Litomerice fault zones, with some contribution from transtensional wrench faults.\r\nThe sediments at Kounova suggest deposition in the bottom of a quiet pool, and the environment seems to have been that of a coal-swamp region. (Kissel, 2010)\r\n",macrofossils,,,,,,NA,,mold/impression,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Repository: National Museum, Prague (CGH)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Dawsonia,n. gen.,NA,NA,"paleoentomology,vertebrate",A. Fritsch. 1879. Fauna der Gaskohle und der Kalksteine der Permformations Bohmens. 1(1),327,697,0,R. Butler,E. Dunne,,16/02/2016 10:47,16/02/2016 10:47,37199,polydens,Dawsonerpeton,58134,n. sp.,304.8,303.4,Stephanian B,,NA,CZ,Dawsonerpeton polydens
1315463,occ,NA,,176531,members,Branchierpeton n. sp. reinholdi,species,336838,,Branchierpeton reinholdi,NA,species,336838,Werneburg,1988,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Micromelerpetontidae,37041,37042,NA,NA,NA,,10.502759,50.866585,Tabarz,NA,Cabarz,DE,Thuringia,Gotha District,based on nearby landmark,6,small collection,"Coordinates are based on the centre of the municipality Tabarz in the district of Gotha, in Thuringia. Locality is in the Thuringian Forest. ",gp_mid,21.2,6.7,305,DE,,Goldlauter,,,group of beds,,Lower Goldlauter Beds,Lower Goldlauter Beds,,,,NA,Lower Goldlauter Beds,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchierpeton,,NA,NA,vertebrate,"R. Werneburg. 1988. Die Stegocephalen (Amphibia) der Goldlauterer Schichten (Unterroliegendes, Perm) des Thuringer Waldes. Teil 3. Apateon dracyensis (Boy), Branchierpeton reinholdin. sp. und andere. Veroffentlichungen des Naturkundemuseums 7:80-96",327,697,0,R. Butler,E. Dunne,,17/02/2016 07:55,17/02/2016 07:55,NA,reinholdi,Branchierpeton,58145,n. sp.,298.9,295.5,Asselian,,NA,DE,Branchierpeton reinholdi
1315479,occ,NA,,176535,members,Branchierpeton reinholdi,species,336838,,Branchierpeton reinholdi,NA,species,336838,Werneburg,1988,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Micromelerpetontidae,37041,37042,NA,NA,NA,,12.925204,51.199074,"Clennen, Saxony",NA,,DE,Mittelsachsen,Bockelwitz,based on nearby landmark,6,small collection,"Coordinates based on the location of Clennen, a small populated area in Saxony, Germany.",gp_mid,22.57,7.46,305,DE,,Bortewitz,,,group of beds,,Clennen tuffite,Clennen tuffite,,,,NA,B̦rtewitz Formation,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchierpeton,,NA,NA,vertebrate,"R. Werneburg. 1988. Die Stegocephalen (Amphibia) der Goldlauterer Schichten (Unterroliegendes, Perm) des Thuringer Waldes. Teil 3. Apateon dracyensis (Boy), Branchierpeton reinholdin. sp. und andere. Veroffentlichungen des Naturkundemuseums 7:80-96",327,697,0,R. Butler,E. Dunne,,17/02/2016 08:08,17/02/2016 08:08,NA,reinholdi,Branchierpeton,58145,,298.9,295,Autunian,,NA,DE,Branchierpeton reinholdi
1315480,occ,NA,,176536,members,Branchierpeton n. sp. saalense,species,336840,,Branchierpeton saalense,NA,species,336840,Werneburg,1990,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Micromelerpetontidae,37041,37042,NA,NA,NA,,11.964779,51.593925,"Petersburg, near Halle",NA,,DE,Sachsen-Anhalt,,based on nearby landmark,6,small collection,"Coordinates based on the location of Petersburg Museum (Alte Hallesche Str. 28, 06193 Petersberg, Germany)",gp_mid,20.62,6.05,315,DE,,Wettin,,,,,Wettin Beds,Wettin Beds,,,,NA,"Wettin Beds, now known as the Wettin Subformatin, was placed in the Uppermost Stephanian by Fritsch (1888) and subsequently confirmed by palaeozooloigcal and palaeobotanical analyses (Gsiewicz & Sowakiewicz (eds.), 2013, Geo. Soc. Sp. Pub. 376)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchierpeton,,NA,NA,vertebrate,R. Werneburg. 1990. Dissorophoiden (Amphibia) aus dem Grenzbereich Karbon/Perm der Saale-Senke und des Ilfelder Beckens (DDR). Zeitschrift fur geologische Wissenschaften Berlin 18:665-677,327,697,0,R. Butler,E. Dunne,,17/02/2016 09:04,17/02/2016 09:04,NA,saalense,Branchierpeton,58149,n. sp.,306.95,298.9,Stephanian,,NA,DE,Branchierpeton saalense
1315481,occ,NA,,176537,,Branchierpeton saalense,species,336840,,Branchierpeton saalense,NA,species,336840,Werneburg,1990,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Micromelerpetontidae,37041,37042,NA,NA,NA,,11.886034,51.632187,"Lobejun drill hole, north of Halle",NA,,DE,Saxony-Anhalt,,based on nearby landmark,6,small collection,"Coordinates based on the location of the Lobejun quarry just outside the town of Lobejun in Saxony, Germany.",gp_mid,21.28,6.98,315,DE,,Wettin,,,bed,,Wettin Beds,Wettin Beds,,,,NA,"The drill hole contains the top part of the Wettin beds (Stephanian) or the basal Halle beds (autunian)\r\nWettin Beds, now known as the Wettin Subformatin, was placed in the Uppermost Stephanian by Fritsch (1888) and subsequently confirmed by palaeozooloigcal and palaeobotanical analyses (Gsiewicz & Sowakiewicz (eds.), 2013, Geo. Soc. Sp. Pub. 376).",,"""limestone""",gray,,,,,,,,,lacustrine indet.,,See: Gsiewicz & Sowakiewicz (eds.) (2013) Geo. Soc. Sp. Pub. 376,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,From drill core,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchierpeton,,NA,NA,vertebrate,R. Werneburg. 1990. Dissorophoiden (Amphibia) aus dem Grenzbereich Karbon/Perm der Saale-Senke und des Ilfelder Beckens (DDR). Zeitschrift fur geologische Wissenschaften Berlin 18:665-677,327,697,0,R. Butler,E. Dunne,,17/02/2016 09:13,17/02/2016 09:13,58149,saalense,Branchierpeton,58149,,306.95,295,Stephanian,Autunian,NA,DE,Branchierpeton saalense
1315482,occ,NA,,176538,members,Branchierpeton saalense,species,336840,,Branchierpeton saalense,NA,species,336840,Werneburg,1990,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Micromelerpetontidae,37041,37042,NA,NA,NA,,10.85653,50.666248,"Moosbach, near Manebach Thuringia",NA,,DE,,,based on nearby landmark,6,small collection,,gp_mid,20.24,4.96,305,DE,,Mohrenbach,,,,,,,,,,NA,"The Th_ringer Wald (Thuringian Forest) reveals an Upper Stephanian-Rotliegend succession that can be subdivided into eleven formations - including the Mohrenbach formation. The fossil content of sedimentary horizons in the basal or lower part of the formation indicates a late Stephanian age. (Harald et al., 2012)","The Georgenthal and M̦hrenbach Formations unconformably overlie the folded Variscan basement, which consists of Proterozoic to Lower Palaeozoic formations of the Saxothuringian zone in the SE, a deeply-weathered granitic massif in the middle part (Th_ringer Hauptgranit, Vis̩), and metamorphic rocks of the Ruhla Crystalline Complex in the NW. The Georgenthal and M̦hrenbach formations mainly consist of trachyticlatitic volcanics, pyroclastics and intrusives. In addition, the M̦hrenbach Formation contains acid volcanics that become increasingly acid upwards.","""volcaniclastic""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchierpeton,,NA,NA,vertebrate,R. Werneburg. 1990. Dissorophoiden (Amphibia) aus dem Grenzbereich Karbon/Perm der Saale-Senke und des Ilfelder Beckens (DDR). Zeitschrift fur geologische Wissenschaften Berlin 18:665-677,327,697,0,R. Butler,E. Dunne,,17/02/2016 09:24,17/02/2016 09:24,NA,saalense,Branchierpeton,58149,,306.95,298.9,Stephanian,,NA,DE,Branchierpeton saalense
1315483,occ,NA,,176539,members,Branchierpeton saalense,species,336840,,Branchierpeton saalense,NA,species,336840,Zajic et al.,1990,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Micromelerpetontidae,37041,37042,NA,NA,NA,,14.44295,50.417114,Libechov,NA,Libchov,CZ,Bohemian Region,,,6,,"Coordinates are based on the location of Libchov, a small town in Central Bohemian Region of the Czech Republic located about 36 km north of Prague on right bank of the Elbe River.",gp_mid,22.84,5.89,305,CZ,,Line,,,,,,,,,,NA,,,not reported,,,,,,,,,,marine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchierpeton,,NA,NA,vertebrate,"J. A. Zajic, A. R. Milner, and J. Klembara. 1990. The first partially articulated amphibian (Temnospondlyi: Dissorophoidea) from the Line Formation (Stephanian C, central Bohemia). Vestnik Ustredniho Ustavu Geologickeho 65:329-337",327,697,0,R. Butler,E. Dunne,,17/02/2016 10:17,17/02/2016 10:17,NA,saalense,Branchierpeton,58151,,303.4,301.2,Stephanian C,,NA,CZ,Branchierpeton saalense
1315505,occ,NA,,176543,members,Limnerpeton n. sp. edani,species,37043,species not entered,Limnerpeton,NA,genus,37043,Werneburg,1989,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Micromelerpetontidae,37041,37043,NA,NA,NA,,10.453702,50.877323,Sembachtal near Winterstein,NA,,DE,Thuringia,Emsetal,based on nearby landmark,6,small collection,,gp_mid,20.64,6,305,DE,,Ilmenau,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Limnerpeton,,NA,NA,vertebrate,"R. Werneburg. 1989. Die Amphibienfauna der Manebacher Schichten (Unterrotliegendes, Unterperm) des Thuringer Waldes. Veroffentlichungen des Naturhistorischen Museum Schleusingen 4:55-68",327,697,0,R. Butler,E. Dunne,,17/02/2016 11:59,17/02/2016 11:59,NA,edani,Limnerpeton,58155,n. sp.,303.7,298.9,Gzhelian,,NA,DE,Limnerpeton edani
1316469,occ,NA,,175806,members,n. gen. Lepterpeton n. sp. dobbsii,species,227041,,Lepterpeton dobbsii,NA,species,227041,Wright and Huxley,1866,Chordata,33815,Osteichthyes,34881,,NA,Urocordylidae,37270,37273,NA,NA,NA,,-7.203734,52.806236,Jarrow Colliery,NA,,IE,Lenister,,based on nearby landmark,6,local area,"located near Castlecomer, Co. Kilkenny",gp_mid,1.79,-6.34,315,IE,,,,,,,,,,,,NA,"Westphalian A according to Clack & Ahlberg, 2004",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,"Taxonomic list from location published in Wyse Jackson P. N. & Monaghan, N.T. (1995) Transfer of the Huxley and Wright (1867) Carboniferous amphibian and fish material to Trinity College Dublin from the National Museum of Ireland. J. Paleont. 69(3) pp. 602-603","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lepterpeton,n. gen.,NA,NA,vertebrate,"E. P. Wright and T. H. Huxley. 1866. Pn a collection of fossils from the Jarrow Colliery, Kilkenny. Geological Magazine 3:165-171",327,697,697,R. Butler,E. Dunne,E. Dunne,24/02/2016 12:00,24/02/2016 12:05,NA,dobbsii,Lepterpeton,58258,n. sp.,318.1,314.6,Westphalian A,,NA,IE,Lepterpeton dobbsii
1316470,occ,NA,,175806,members,n. gen. Urocordylus n. sp. wandesfordii,species,227065,,Urocordylus wandesfordii,NA,species,227065,Wright and Huxley,1866,Chordata,33815,Osteichthyes,34881,,NA,Urocordylidae,37270,37276,NA,NA,NA,,-7.203734,52.806236,Jarrow Colliery,NA,,IE,Lenister,,based on nearby landmark,6,local area,"located near Castlecomer, Co. Kilkenny",gp_mid,1.79,-6.34,315,IE,,,,,,,,,,,,NA,"Westphalian A according to Clack & Ahlberg, 2004",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,"Taxonomic list from location published in Wyse Jackson P. N. & Monaghan, N.T. (1995) Transfer of the Huxley and Wright (1867) Carboniferous amphibian and fish material to Trinity College Dublin from the National Museum of Ireland. J. Paleont. 69(3) pp. 602-603","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Urocordylus,n. gen.,NA,NA,vertebrate,"E. P. Wright and T. H. Huxley. 1866. Pn a collection of fossils from the Jarrow Colliery, Kilkenny. Geological Magazine 3:165-171",327,697,0,R. Butler,E. Dunne,,24/02/2016 12:05,24/02/2016 12:05,NA,wandesfordii,Urocordylus,58258,n. sp.,318.1,314.6,Westphalian A,,NA,IE,Urocordylus wandesfordii
1316471,occ,NA,,175806,members,n. gen. Keraterpeton n. sp. galvani,species,227370,,Keraterpeton galvani,NA,species,227370,Wright and Huxley,1866,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37266,NA,NA,NA,,-7.203734,52.806236,Jarrow Colliery,NA,,IE,Lenister,,based on nearby landmark,6,local area,"located near Castlecomer, Co. Kilkenny",gp_mid,1.79,-6.34,315,IE,,,,,,,,,,,,NA,"Westphalian A according to Clack & Ahlberg, 2004",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,"Taxonomic list from location published in Wyse Jackson P. N. & Monaghan, N.T. (1995) Transfer of the Huxley and Wright (1867) Carboniferous amphibian and fish material to Trinity College Dublin from the National Museum of Ireland. J. Paleont. 69(3) pp. 602-603","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Keraterpeton,n. gen.,NA,NA,vertebrate,"E. P. Wright and T. H. Huxley. 1866. Pn a collection of fossils from the Jarrow Colliery, Kilkenny. Geological Magazine 3:165-171",327,697,0,R. Butler,E. Dunne,,24/02/2016 12:23,24/02/2016 12:23,NA,galvani,Keraterpeton,58258,n. sp.,318.1,314.6,Westphalian A,,NA,IE,Keraterpeton galvani
1316612,occ,NA,,176673,members,Adelogyrinus simorhynchus,species,227001,,Adelogyrinus simorhynchus,NA,species,227001,Carroll et al.,1998,Chordata,33815,Osteichthyes,34881,Adelospondyli,320812,Adelogyrinidae,37325,37326,NA,NA,NA,,-4.166993,55.884312,"Straiton, Edinburgh",NA,,UK,Scotland,Loanhead,based on nearby landmark,6,small collection,,gp_mid,-9.86,-28.2,313,UK,,,Upper Oil Shale,,,,Dunnet Shale,Dunnet Shale,,,,NA,,,"""shale""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,adpression",,,,,,,,,,NA,,,taxonomic,,,,,,,,NMS collection,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Adelogyrinus,,NA,NA,vertebrate,"R. L. Carroll, K. A. Bossy, and A. C. Milner, S. M. Andrews, C. F. Wellstead. 1998. Handbuch der Palaoherpetologie / Encyclopedia of Paleoherpetology Teil 1 / Part 1 Lepospondyli: Microsauria, Nectridea, Lysorophia, Adelospondyli, Aistopoda, Acherontiscidae. ",327,697,0,R. Butler,E. Dunne,,26/02/2016 09:32,26/02/2016 09:32,NA,simorhynchus,Adelogyrinus,55379,,346.7,330.9,Visean,,NA,UK,Adelogyrinus simorhynchus
1316613,occ,NA,,175806,members,n. gen. Dolichosoma n. sp. emersoni,species,320840,,Dolichosoma emersoni,NA,species,320840,Huxley and Wright,1867,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,37258,NA,NA,NA,,-7.203734,52.806236,Jarrow Colliery,NA,,IE,Lenister,,based on nearby landmark,6,local area,"located near Castlecomer, Co. Kilkenny",gp_mid,1.79,-6.34,315,IE,,,,,,,,,,,,NA,"Westphalian A according to Clack & Ahlberg, 2004",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,"Taxonomic list from location published in Wyse Jackson P. N. & Monaghan, N.T. (1995) Transfer of the Huxley and Wright (1867) Carboniferous amphibian and fish material to Trinity College Dublin from the National Museum of Ireland. J. Paleont. 69(3) pp. 602-603","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Dolichosoma,n. gen.,NA,NA,vertebrate,"T. H. Huxley and E. P. Wright. 1867. On a collection of fossil Vertebrata from the Jarrow Colliery, County of Kilkenny, Ireland. Transactions of the Royal Irish Academy 24:351-368",327,697,0,R. Butler,E. Dunne,,26/02/2016 09:54,26/02/2016 09:54,NA,emersoni,Dolichosoma,58276,n. sp.,318.1,314.6,Westphalian A,,NA,IE,Dolichosoma emersoni
1316960,occ,NA,,176771,members,Micromelerpeton n. sp. boyi,species,337384,,Micromelerpeton boyi,NA,species,337384,Heyler,1994,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Micromelerpetontidae,37041,37044,NA,NA,NA,,4.291074,46.940742,Saone et Laoire (Autun Formation),NA,,FR,Burgundy,,based on nearby landmark,6,small collection,Coordinates based on the location of the town of Autun,gp_mid,18.16,1.92,305,FR,,Autun,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,adpression,,,,,,,,,,NA,,,taxonomic,,MNHN,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Micromelerpeton,,NA,NA,vertebrate,"D. Heyler. 1994. Les branchiosaures stephaniens et permiens de Montceau-les-Mines et des bassins du Massif central. In C. Poplin, D. Heyler (eds.), Quand le Massiff central etait sous l'equateur un ecosysteme carbonifere a Montceau-les-Mines ",327,697,0,R. Butler,E. Dunne,,01/03/2016 12:20,01/03/2016 12:20,NA,boyi,Micromelerpeton,58316,n. sp.,298.9,295,Autunian,,NA,FR,Micromelerpeton boyi
1317355,occ,NA,,171346,,n. gen. Stegotretus n. sp. agyrus,species,227375,,Stegotretus agyrus,NA,species,227375,Berman et al.,1988,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,227374,NA,NA,NA,,-106.652222,36.159443,Valley floor of east Camp Quarry,NA,1 km SE Arroyo del Agua,US,New Mexico,Rio Arriba,based on nearby landmark,seconds,small collection,"Coordinates are for the area 1 km southeast of the small village of Arroyo del Agua, Rio Arriba County, New Mexico. See Lucas et al. (2005) for detailed map of other fossil-bearing locations in the area.",gp_mid,-34.08,4.53,101,US,FED,Cutler,,,bed,,,,,,,NA,,,"""siliciclastic""",,,,,,,,,,fine channel fill,,,macrofossils,,some,,partial skeletons,,NA,,"mold/impression,adpression",,,,,,,,,,NA,,,taxonomic,field collection,CM,,,,,1982,,"""Numerous articulated specimens have been collected from the valley floor immediately east of the Camp quarry."" Lucas et a. (2005)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Stegotretus,n. gen.,NA,NA,vertebrate,"D. S. Berman, D. A. Eberth, and D. B. Brinkman. 1988. Stegotretus agyrus a new genus and species of microsaur (amphibian) from the Permo-Pennsylvanian of New Mexico. Annals of Carnegie Museum 57:293-323",327,697,0,R. Butler,E. Dunne,,08/03/2016 06:42,08/03/2016 06:42,NA,agyrus,Stegotretus,58387,n. sp.,296.4,268,Wolfcamp,,NA,US,Stegotretus agyrus
1317623,occ,NA,,176968,members,n. gen. Trihecaton n. sp. howardinus,species,320818,,Trihecaton howardinus,NA,species,320818,Vaughn,1972,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Trihecatontidae,37305,37306,NA,NA,NA,,-105.836998,38.448879,Interval 300 of section of the Sangre de Cristo Formation,NA,,US,Colorado,Fremont County,based on nearby landmark,6,,"Coordinates based on the location of Howard, a town nearby to the site where the fossils were collected. \r\nFull description of the locality by Vaughn (1972): ""Interval 300 of the section of the Sangre de Cristo Formation measured by Brill (1952:870), about 1450 feet above the base of the formation in NW1/4 NE1/4 SW1/4 sec. 22, T 49 N, R 10 E, Fremont County, Colorado.""",gp_mid,-37.49,-1.4,101,US,FED,Sangre de Cristo,,,bed,,,,,,,NA,"""The age is Late Pennsylvanian, probably Missourian. In European terms, the horizon would be within the lower part of the Stephanian Series."" (Vaughn, 1972)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,mold/impression,,,,,,,,,,NA,,,taxonomic,,,,,,,"166, 1970","Collected by a field party of the University of California, Los Angeles in the summers of 1966 and 1970 and deposited in the collections at UCLA.",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Trihecaton,n. gen.,NA,NA,vertebrate,P. P. Vaughn. 1972. More vertebrates including a new microsaur from the Upper Pennsylvanian of central Colorado. Los Angeles County Museum Contributions in Science 223:1-30,327,697,0,R. Butler,E. Dunne,,10/03/2016 10:35,10/03/2016 10:35,NA,howardinus,Trihecaton,57812,n. sp.,315.2,307,Moscovian,,NA,US,Trihecaton howardinus
1317624,occ,NA,,176968,members,n. gen. Coloraderpeton n. sp. brilli,species,320839,,Coloraderpeton brilli,NA,species,320839,Vaughn,1969,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Ophiderpetontidae,37252,37253,NA,NA,NA,,-105.836998,38.448879,Interval 300 of section of the Sangre de Cristo Formation,NA,,US,Colorado,Fremont County,based on nearby landmark,6,,"Coordinates based on the location of Howard, a town nearby to the site where the fossils were collected. \r\nFull description of the locality by Vaughn (1972): ""Interval 300 of the section of the Sangre de Cristo Formation measured by Brill (1952:870), about 1450 feet above the base of the formation in NW1/4 NE1/4 SW1/4 sec. 22, T 49 N, R 10 E, Fremont County, Colorado.""",gp_mid,-37.49,-1.4,101,US,FED,Sangre de Cristo,,,bed,,,,,,,NA,"""The age is Late Pennsylvanian, probably Missourian. In European terms, the horizon would be within the lower part of the Stephanian Series."" (Vaughn, 1972)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,mold/impression,,,,,,,,,,NA,,,taxonomic,,,,,,,"166, 1970","Collected by a field party of the University of California, Los Angeles in the summers of 1966 and 1970 and deposited in the collections at UCLA.",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Coloraderpeton,n. gen.,NA,NA,vertebrate,P. P. Vaughn. 1969. Upper Pennsylvanian vertebrates from the Sangre de Cristo Formation of central Colorado. Los Angeles County Museum Contributions in Science 164:1-28,327,697,0,R. Butler,E. Dunne,,10/03/2016 10:42,10/03/2016 10:42,NA,brilli,Coloraderpeton,57813,n. sp.,315.2,307,Moscovian,,NA,US,Coloraderpeton brilli
1317625,occ,NA,,85292,,Pygopterus n. sp. scutellatus,species,335313,recombined as,Colosteus scutellatus,NA,species,335313,Clack and Milner,2015,Chordata,33815,Osteichthyes,34881,,NA,Colosteidae,36975,36976,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Pygopterus,,NA,NA,vertebrate,"J. A. Clack and A. R. Milner. 2015. Handbook of Paleoherpetology, Part 3A1: Basal Tetrapoda. ",327,697,327,R. Butler,E. Dunne,R. Butler,10/03/2016 11:10,29/06/2016 15:45,28831,scutellatus,Colosteus,57666,n. sp.,311.45,306.95,Westphalian D,,NA,US,Colosteus scutellatus
1317648,occ,NA,,85292,,n. gen. Oestocephalus n. sp. amphiuminum,species,230699,,Oestocephalus amphiuminum,NA,species,230699,Cope,1868,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Oestocephalidae,230698,230697,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Oestocephalus,n. gen.,NA,NA,vertebrate,E. D. Cope. 1868. Synopsis of the Extinct Batrachia of North America. Proceedings of the Academy of Natural Sciences of Philadelphia 1868:208-221,327,697,0,R. Butler,E. Dunne,,11/03/2016 05:20,11/03/2016 05:20,28831,amphiuminum,Oestocephalus,28717,n. sp.,311.45,306.95,Westphalian D,,NA,US,Oestocephalus amphiuminum
1317649,occ,NA,,84835,,Ophiderpeton n. sp. granulosum,species,320837,recombined as,Oestocephalus granulosum,NA,species,320837,Fritsch,1880,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Oestocephalidae,230698,230697,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Ophiderpeton,,NA,NA,vertebrate,A. Fritsch. 1880. Fauna der Gaskohle und der Kalksteine der Permformation Bohmens. 1(2),327,697,0,R. Butler,E. Dunne,,11/03/2016 05:26,11/03/2016 05:26,28608,granulosum,Oestocephalus,58421,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Oestocephalus granulosum
1317652,occ,NA,,176015,members,Oestocephalus amphiuminum,species,230699,,Oestocephalus amphiuminum,NA,species,230699,Carroll et al.,1998,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Oestocephalidae,230698,230697,NA,NA,NA,,-80.474998,40.796112,Mansfield's Mine,NA,,US,Pennsylvania,Beaver County,based on nearby landmark,seconds,small collection,"Coordinates based on the location of Cannelton town, Darlingtown Township, Beaver County, Pennsylvania.",gp_mid,-18.25,-7.93,101,US,,,Allegheny,Upper Kittanning Coal,,,,,,,,NA,,,coal,,,,,"""shale""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,adpression",,,,,,,,,,NA,,,taxonomic,,AMNH,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Oestocephalus,,NA,NA,vertebrate,"R. L. Carroll, K. A. Bossy, and A. C. Milner, S. M. Andrews, C. F. Wellstead. 1998. Handbuch der Palaoherpetologie / Encyclopedia of Paleoherpetology Teil 1 / Part 1 Lepospondyli: Microsauria, Nectridea, Lysorophia, Adelospondyli, Aistopoda, Acherontiscidae. ",327,697,0,R. Butler,E. Dunne,,11/03/2016 06:12,11/03/2016 06:12,NA,amphiuminum,Oestocephalus,55379,,311.45,306.95,Westphalian D,,NA,US,Oestocephalus amphiuminum
1317697,occ,NA,,84835,,Ricnodon n. sp. limnophyes,species,337663,recombined as,Crinodon limnophyes,NA,species,337663,Steen,1938,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Tuditanidae,37280,37283,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Ricnodon,,NA,NA,vertebrate,M. C. Steen. 1938. On the fossil Amphibia from the Gas Coal of Nyrany and other deposits of Czechoslovakia. Proceedings of the Zoological Society of London 108:205-283,327,697,0,R. Butler,E. Dunne,,14/03/2016 04:29,14/03/2016 04:29,28608,limnophyes,Crinodon,58385,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Crinodon limnophyes
1317698,occ,NA,,84835,,n. gen. Nyranerpeton n. sp. amilneri,species,337469,,Nyranerpeton amilneri,NA,species,337469,Werneburg,2012,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Micromelerpetontidae,37041,337468,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Nyranerpeton,n. gen.,NA,NA,vertebrate,"R. Werneburg. 2012. Dissorophoide Amphibien aus dem Asturian (Ober-Karbon) von Nyrany in Bohmen (Tschechische Republik) - der Schlussel zum Verstandnis der fruhen ""Branchiosaurier"". Ver̦ffentlichungen des Naturhistorischen Museums Schleusingen 27:3-50",327,697,0,R. Butler,E. Dunne,,14/03/2016 04:31,14/03/2016 04:31,28608,amilneri,Nyranerpeton,58325,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Nyranerpeton amilneri
1317699,occ,NA,,84835,,n. gen. Cochleosaurus n. sp. bohemicus,species,204052,,Cochleosaurus bohemicus,NA,species,204051,Fritsch,1885,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Cochleosauridae,36999,37001,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Cochleosaurus,n. gen.,NA,NA,vertebrate,A. Fritsch. 1885. Fauna der Gaskohle under der Kalksteine der Permformatons Bohmens. 2(1),327,697,0,R. Butler,E. Dunne,,14/03/2016 04:34,14/03/2016 04:34,28608,bohemicus,Cochleosaurus,58035,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Cochleosaurus bohemicus
1317700,occ,NA,,176090,members,n. gen. Sauravus n. sp. costei,species,320829,,Sauravus costei,NA,species,320829,Thevenin,1906,Chordata,33815,Osteichthyes,34881,,NA,Scincosauridae,37267,37268,NA,NA,NA,,4.387342,46.696396,"Montceau-les-Mines, Saone et Loire",NA,"Blanzy, Sa̫ne-et-Loire",FR,Bourgogne,,based on nearby landmark,6,,"Coordinates based on Blanzy, a commune in the Sa̫ne-et-Loire department in the region of Bourgogne in eastern France",gp_mid,17.13,0.02,305,FR,,,,,bed,,,,,,,NA,Locatity situated in the Montceau Basin,,not reported,,,,,,,,,,terrestrial indet.,,"No further information available on stratigraphy aside from that presented in Carroll et al. (1998, Handbuch der Palaoherpetologie 1)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MNHN,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Sauravus,n. gen.,NA,NA,vertebrate,A. Thevenin. 1906. Amphibiens et reptiles du terrain Houiller de France. Annales de Paleontologie 1:145-163,327,697,0,R. Butler,E. Dunne,,14/03/2016 08:41,14/03/2016 08:41,NA,costei,Sauravus,58431,n. sp.,304.8,301.2,Stephanian B,Stephanian C,NA,FR,Sauravus costei
1317701,occ,NA,,80777,,Sauravus n. sp. cambrayi,species,320830,,Sauravus cambrayi,NA,species,320830,Thevenin,1910,Chordata,33815,Osteichthyes,34881,,NA,Scincosauridae,37267,37268,NA,NA,NA,,4.302778,46.984165,Les Telots,NA,"Les T̩lots, Autunois",FR,Bourgogne,Sa̫ne-et-Loire,based on nearby landmark,seconds,,"Les Telots, near Autun; polar coordinates are for Les T̩lots",gp_mid,18.55,2.72,305,FR,,,,,,,,,,,,NA,"""The localitiy yields outcrops of the Millery Formation (Autunian, Rotliegend) of Artinskian age (formerly Sakmarian; see Werneburg & Schneider, 2006; Schneider et al., 2014)"" (Spindler, 2015)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Sauravus,,NA,NA,vertebrate,A. Thevenin. 1910. Les plus anciens quadrupedes de France. Annales de Paleontologie 5:1-63,327,697,0,R. Butler,E. Dunne,,14/03/2016 08:48,14/03/2016 08:48,27105,cambrayi,Sauravus,58433,n. sp.,290.1,279.3,Artinskian,,NA,FR,Sauravus cambrayi
1317897,occ,NA,,80714,,n. gen. Diplocaulus n. sp. salamandroides,species,70396,,Diplocaulus salamandroides,NA,species,70396,Cope,1877,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-87.775002,40.108334,Danville Locality (Vertebrates),NA,Oakwood Locality; Horseshoe Bend; Vermillion River; Illinois bonebed,US,Illinois,Vermilion,based on nearby landmark,seconds,outcrop,"""the well-known Danville or 'Oakwood' locality [...] Horseshoe Bend locality near the SE/C of Sec. 23-19N-13W"" (DeMar, 1970)\r\n""Vermilion River, near Danville"" (Reisz, 1986)\r\nLat Long is for Oakwood",gp_mid,-21.51,-3.52,101,US,,Bond,McLeansboro,,group of beds,,,,,,,NA,"""We believe the vertebrates have been collected from a zone 10 feet or so below the Shoal Creek Member of the Bond Formation"" (DeMar, 1970)\r\nNote: Shoal Creek Member is equivalent to Carthage Limestone Member, a name now used throughout the Illinois Basin for that lithological unit; see Jacobson (2002) A summary of references with changes in Pennsylvanian stratigraphic nomenclature at the ISGS since Bulletin 95. [Online] http://www.isgs.illinois.edu/maps-data-pub/coal-maps/pennstratigraphy.shtml ",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,n. gen.,NA,NA,vertebrate,E. D. Cope. 1877. A continuation of researches among the Batrachia of the Coal Measures of Ohio. Proceedings of the American Philosophical Society 22:573-578,327,697,0,R. Butler,E. Dunne,,15/03/2016 05:44,15/03/2016 05:44,28640,salamandroides,Diplocaulus,57922,n. sp.,305.9,303.4,Missourian,,NA,US,Diplocaulus salamandroides
1317898,occ,NA,,176408,members,Diplocaulus salamandroides,species,70396,,Diplocaulus salamandroides,NA,species,70396,Cope,1877,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-79.788071,40.406403,Percy Raymond's Bonebed,NA,,US,Pennsylvania,,based on nearby landmark,6,small collection,"Coordinates based on quarry outside of Pitcairn near Pittsburgh, Pennsylvania, USA",gp_mid,-14.47,-3.38,101,US,,Casselman,Conemaugh,,group of beds,,Round Knobs Redbeds,Round Knobs Redbeds,,,,NA,,,mudstone,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,E. D. Cope. 1877. A continuation of researches among the Batrachia of the Coal Measures of Ohio. Proceedings of the American Philosophical Society 22:573-578,327,697,0,R. Butler,E. Dunne,,15/03/2016 07:14,15/03/2016 07:14,NA,salamandroides,Diplocaulus,57922,,303.4,298.9,Virgilian,,NA,US,Diplocaulus salamandroides
1317905,occ,NA,,27704,,Diplocaulus recurvatus,species,120886,,Diplocaulus recurvatus,NA,species,120886,Olson,1958,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.557777,33.731667,Locality KF (Middle Vale Formation),NA,"three-channel hill, ""fish quarry""",US,Texas,Knox,estimated from map,seconds,small collection,"""approx. seven miles north of Vera, Knox County, Texas"" (Olson, 1951)\r\n""North wall of valley of South Wichita River, east of Vera-Gilliland road"" (Olson, 1948); for details see map on p. 188 in Olson (1948)",gp_mid,-29.19,1.89,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""The locality [...] KF, was assigned to the upper Vale in an earlier paper. More recent field work has shown that it comprises beds that must be assigned to the middle rather than the upper part of the Vale."" (Olson, 1954 p. 213)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191);\r\nspecimen ""was preserved in a nodule that had weathered from a conglomeratic deposit of channel origin."" (Olson, 1951 p. 89) other specimens are from a quarry in fine-grained, green channel deposits",conglomerate,"pebbly,green,red",,,Y,"""siliciclastic""","fine,green",,,Y,"""channel""",foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,,,,NA,,"""Fragmentation of the specimens occurred before and during deposition, probably as the materials were transported by the waters of the streams. This group of animals cannot be considered to represent a life assemblage."" (Olson, 1955 p. 258)",taxonomic,field collection,FMNH,,,,E. C. Olson,1946-1948,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 11:15,15/03/2016 11:15,28928,recurvatus,Diplocaulus,58444,,279.3,272.3,Kungurian,,NA,US,Diplocaulus recurvatus
1317906,occ,NA,,85553,,Diplocaulus recurvatus,species,120886,,Diplocaulus recurvatus,NA,species,120886,Olson,1958,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.574448,33.721668,Locality KE (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""Valley of South Wichita River, north of River and east of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.21,1.88,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,E. C. Olson,"1946, 1947",,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 11:18,15/03/2016 11:18,28928,recurvatus,Diplocaulus,58444,,279.3,272.3,Kungurian,,NA,US,Diplocaulus recurvatus
1317907,occ,NA,,85555,,Diplocaulus recurvatus,species,120886,,Diplocaulus recurvatus,NA,species,120886,Olson,1958,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.548615,33.7575,Locality KH (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,outcrop,"""Southern margin of valley of North Wichita River""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.17,1.9,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" (Olson, 1948 p. 190);\r\n""base of upper part of Vale"" (Olson, 1954)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,E. C. Olson,"1946, 1947",,"This collection represents the scattered finds at the locality. Olson (1958) subdivided the locality into four sub-locations: Clay Hill site, Diplocaulus Quarry Site, and Chocolate Hill Site.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,697,R. Butler,E. Dunne,E. Dunne,15/03/2016 11:19,15/03/2016 11:24,28928,recurvatus,Diplocaulus,58444,,279.3,272.3,Kungurian,,NA,US,Diplocaulus recurvatus
1317915,occ,NA,,177000,members,Diplocaulus recurvatus,species,120886,,Diplocaulus recurvatus,NA,species,120886,Olson,1958,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.548615,33.7575,Locality KH Clay Hill site,NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""Southern margin of valley of North Wichita River""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.17,1.9,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" (Olson, 1948 p. 190);\r\n""base of upper part of Vale"" (Olson, 1954)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,,,"Olson (1958) subdivided Locality KH into four sub-locations: Clay Hill site, Diplocaulus Quarry Site, and Chocolate Hill Site.",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 11:41,15/03/2016 11:41,NA,recurvatus,Diplocaulus,58444,,279.3,272.3,Kungurian,,NA,US,Diplocaulus recurvatus
1317916,occ,NA,,177000,members,Dimetrodon gigashomogenes,species,138123,,Dimetrodon gigashomogenes,NA,species,138123,Olson,1958,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.548615,33.7575,Locality KH Clay Hill site,NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""Southern margin of valley of North Wichita River""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.17,1.9,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" (Olson, 1948 p. 190);\r\n""base of upper part of Vale"" (Olson, 1954)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,,,"Olson (1958) subdivided Locality KH into four sub-locations: Clay Hill site, Diplocaulus Quarry Site, and Chocolate Hill Site.",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 11:41,15/03/2016 11:41,NA,gigashomogenes,Dimetrodon,58444,,279.3,272.3,Kungurian,,NA,US,Dimetrodon gigashomogenes
1317917,occ,NA,,177000,members,Eryops megacephalus,species,70397,,Eryops megacephalus,NA,species,70397,Olson,1958,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-99.548615,33.7575,Locality KH Clay Hill site,NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""Southern margin of valley of North Wichita River""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.17,1.9,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" (Olson, 1948 p. 190);\r\n""base of upper part of Vale"" (Olson, 1954)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,,,"Olson (1958) subdivided Locality KH into four sub-locations: Clay Hill site, Diplocaulus Quarry Site, and Chocolate Hill Site.",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 11:41,15/03/2016 11:41,NA,megacephalus,Eryops,58444,,279.3,272.3,Kungurian,,NA,US,Eryops megacephalus
1317919,occ,NA,,177001,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Olson,1958,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-99.548615,33.7575,Locality KH Chocolate Hill site,NA,,US,Texas,Knox,estimated from map,seconds,outcrop,"""Southern margin of valley of North Wichita River""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.17,1.9,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" (Olson, 1948 p. 190);\r\n""base of upper part of Vale"" (Olson, 1954)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,,,,"Olson (1958) subdivided the main locality into four sub-locations: Clay Hill site, Diplocaulus Quarry Site, and Chocolate Hill site.","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 11:44,15/03/2016 11:44,58444,sp.,Trimerorhachis,58444,,279.3,272.3,Kungurian,,NA,US,Trimerorhachis sp.
1317920,occ,NA,,177002,members,Diplocaulus recurvatus,species,120886,,Diplocaulus recurvatus,NA,species,120886,Olson,1958,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.548615,33.7575,Locality KH Diplocaulus Quarry site,NA,,US,Texas,Knox,estimated from map,seconds,outcrop,"""Southern margin of valley of North Wichita River""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.17,1.9,101,US,,Vale,Clear Fork,,member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" (Olson, 1948 p. 190);\r\n""base of upper part of Vale"" (Olson, 1954)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,,,,"Olson (1958) subdivided the main locality into four sub-locations: Clay Hill site, Diplocaulus Quarry Site, and Chocolate Hill Site.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 11:45,15/03/2016 11:45,NA,recurvatus,Diplocaulus,58444,,279.3,272.3,Kungurian,,NA,US,Diplocaulus recurvatus
1317921,occ,NA,,177003,members,Dimetrodon gigashomogenes,species,138123,,Dimetrodon gigashomogenes,NA,species,138123,Olson,1958,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.571114,33.6675,Locality KA Quarry site,NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""South wall of valley of South Wichita River east of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.84,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,"field collection,survey of museum collection",FMNH,,,,,,Olson (1958) subdivided the main locality into two sites: Quarry site and High channel site.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 11:50,15/03/2016 11:50,NA,gigashomogenes,Dimetrodon,58444,,279.3,272.3,Kungurian,,NA,US,Dimetrodon gigashomogenes
1317922,occ,NA,,177003,members,Labidosaurikos barkeri,species,119514,subjective synonym of,Labidosaurikos meachami,NA,species,119515,Olson,1958,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37500,NA,NA,NA,,-99.571114,33.6675,Locality KA Quarry site,NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""South wall of valley of South Wichita River east of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.84,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,"field collection,survey of museum collection",FMNH,,,,,,Olson (1958) subdivided the main locality into two sites: Quarry site and High channel site.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurikos,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 11:50,15/03/2016 11:50,NA,barkeri,Labidosaurikos,58444,,279.3,272.3,Kungurian,,NA,US,Labidosaurikos barkeri
1317923,occ,NA,,177003,members,Captorhinus aguti,species,90718,,Captorhinus aguti,NA,species,134887,Fox and Bowman,1966,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,,-99.571114,33.6675,Locality KA Quarry site,NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""South wall of valley of South Wichita River east of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.84,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,"field collection,survey of museum collection",FMNH,,,,,,Olson (1958) subdivided the main locality into two sites: Quarry site and High channel site.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,"R. C. Fox and M. C. Bowman. 1966. Osteology and Relationships of Captorhinus aguti (Cope) (Reptilia: Captorhinomorpha). The University of Kansas Paleontological Contributions, Series Vertebrata 11:1-79",327,697,697,R. Butler,E. Dunne,E. Dunne,15/03/2016 11:50,15/03/2016 11:56,NA,aguti,Captorhinus,28784,,279.3,272.3,Kungurian,,NA,US,Captorhinus aguti
1317925,occ,NA,,177003,members,n. gen. Captorhinikos n. sp. valensis,species,120855,,Captorhinikos valensis,NA,species,120855,Olson,1954,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37496,NA,NA,NA,,-99.571114,33.6675,Locality KA Quarry site,NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""South wall of valley of South Wichita River east of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.84,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,"field collection,survey of museum collection",FMNH,,,,,,Olson (1958) subdivided the main locality into two sites: Quarry site and High channel site.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinikos,n. gen.,NA,NA,vertebrate,E. C. Olson. 1954. Fauna of the Vale and Choza: 9. Captorhinomorpha. Fieldiana: Geology 10(19):211-218,327,697,697,R. Butler,E. Dunne,E. Dunne,15/03/2016 11:50,15/03/2016 11:56,NA,valensis,Captorhinikos,26907,n. sp.,279.3,272.3,Kungurian,,NA,US,Captorhinikos valensis
1317928,occ,NA,,85550,,Lysorophus tricarinatus,species,70395,,Lysorophus tricarinatus,NA,species,70395,Olson,1958,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-99.571114,33.6675,Locality KA (Upper Vale Fm.) Main site,NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""South wall of valley of South Wichita River east of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.84,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,"field collection,survey of museum collection",FMNH,,,,E. C. Olson,1946-1948,Olson (1958) further subdivided the locality into Quarry site and High Channel site leaving one for scattered finds,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 11:55,15/03/2016 11:55,28928,tricarinatus,Lysorophus,58444,,279.3,272.3,Kungurian,,NA,US,Lysorophus tricarinatus
1317929,occ,NA,,177005,members,Diplocaulus recurvatus,species,120886,,Diplocaulus recurvatus,NA,species,120886,Olson,1958,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.571114,33.6675,Locality KA High Channel site,NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""South wall of valley of South Wichita River east of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.84,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,"field collection,survey of museum collection",FMNH,,,,,,Olson (1958) further subdivided the main locality into Quarry site and High Channel site,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 12:07,15/03/2016 12:07,NA,recurvatus,Diplocaulus,58444,,279.3,272.3,Kungurian,,NA,US,Diplocaulus recurvatus
1317930,occ,NA,,85551,,Diplocaulus recurvatus,species,120886,,Diplocaulus recurvatus,NA,species,120886,Olson,1958,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.576942,33.676109,Locality KB (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""Valley of South Wichita River, south of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.85,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,E. C. Olson,1946-1953,,"Although Olson (1956:331) stated that FMNH UR 29 was collected from locality KC (also in the upper part of the Clear Fork Formation; Olson, 1958: table 1), this is likely a lapsus calami, judging from his statement that this specimen was preserved in association with Captorhinus, and from his faunal lists for localities KB and KC in Olson (1958:430), which list Captorhinus and Edaphosaurid, n. gen., unnamed for the locality KB, whereas neither taxon is listed for KC in the 1958 publication. (Modesto et al, 2016).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 12:08,15/03/2016 12:08,28928,recurvatus,Diplocaulus,58444,,279.3,272.3,Kungurian,,NA,US,Diplocaulus recurvatus
1317931,occ,NA,,85552,,Diplocaulus recurvatus,species,120886,,Diplocaulus recurvatus,NA,species,120886,Olson,1958,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.575836,33.665001,Locality KC (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""South Walls of valley of South Wichita River, west of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.24,1.84,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,,,,,,coarse channel fill,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",macrofossils,,,,,,NA,,body,variable,,snapshot,,,,,,,NA,,for details see Olson (1948 p. 193),taxonomic,field collection,FMNH,,,,E. C. Olson,"1946, 1947",,"The taxon Edaphosauridae sp., represented by the specimen CNHM UR 29, was removed from the taxon list according to Modesto et al. (2016; cf. PBD collection no. 85551)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 12:09,15/03/2016 12:09,28928,recurvatus,Diplocaulus,58444,,279.3,272.3,Kungurian,,NA,US,Diplocaulus recurvatus
1317932,occ,NA,,85362,,Diplocaulus recurvatus,species,120886,,Diplocaulus recurvatus,NA,species,120886,Olson,1958,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.558334,33.816666,Locality FA - Diplocaulus Site,NA,,US,Texas,Foard,estimated from map,seconds,outcrop,"southeastern corner of Foard Co. Aerial photographic index of site: CZW 1C 59, 2.49-3.79.",gp_mid,-30.21,0,101,US,,Choza,Clear Fork,,group of beds,,,,,,,NA,"""top of lower part of Choza Formation""","""The specimens occur in fine-grained siltstones that were formed in a series of small channels. Lateral to the channels are somewhat coarser siltstones, in Which a few non-aquatic animals are preserved."" (Olson, 1956 p. 317)",siltstone,fine,,,Y,siltstone,medium,,,Y,"""channel""",foreland basin,,macrofossils,,,,,,NA,,"body,mold/impression",good,,,,,,abundant,,,NA,,"""Fossil remains are fairly abundant in the channel deposits, but are, for the most part, scattered and broken. The initial porosity of the matrix, and small cracks, developed during weathering, have permitted waters bearing calcium sulphate to percolate to the bones. Crystallization of this salt has resulted in destruction of most of the bone, so that the majority of specimens consist of natural molds. The molds, fortunately, are in excellent condition, so that latex casts reproduce much of the surface detail of the destroyed bone."" (Olson, 1956)",taxonomic,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 12:14,15/03/2016 12:14,26907,recurvatus,Diplocaulus,58444,,290.1,268,Leonard,,NA,US,Diplocaulus recurvatus
1317933,occ,NA,,85362,,Dimetrodon gigashomogenes,species,138123,,Dimetrodon gigashomogenes,NA,species,138123,Olson,1958,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.558334,33.816666,Locality FA - Diplocaulus Site,NA,,US,Texas,Foard,estimated from map,seconds,outcrop,"southeastern corner of Foard Co. Aerial photographic index of site: CZW 1C 59, 2.49-3.79.",gp_mid,-30.21,0,101,US,,Choza,Clear Fork,,group of beds,,,,,,,NA,"""top of lower part of Choza Formation""","""The specimens occur in fine-grained siltstones that were formed in a series of small channels. Lateral to the channels are somewhat coarser siltstones, in Which a few non-aquatic animals are preserved."" (Olson, 1956 p. 317)",siltstone,fine,,,Y,siltstone,medium,,,Y,"""channel""",foreland basin,,macrofossils,,,,,,NA,,"body,mold/impression",good,,,,,,abundant,,,NA,,"""Fossil remains are fairly abundant in the channel deposits, but are, for the most part, scattered and broken. The initial porosity of the matrix, and small cracks, developed during weathering, have permitted waters bearing calcium sulphate to percolate to the bones. Crystallization of this salt has resulted in destruction of most of the bone, so that the majority of specimens consist of natural molds. The molds, fortunately, are in excellent condition, so that latex casts reproduce much of the surface detail of the destroyed bone."" (Olson, 1956)",taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 12:14,15/03/2016 12:14,26907,gigashomogenes,Dimetrodon,58444,,290.1,268,Leonard,,NA,US,Dimetrodon gigashomogenes
1317935,occ,NA,,177006,,Lysorophus tricarinatus,species,70395,,Lysorophus tricarinatus,NA,species,70395,Olson,1958,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-99.558334,33.816666,Locality FA (Choza Fm.) Main site,NA,,US,Texas,Foard,estimated from map,seconds,outcrop,"southeastern corner of Foard Co.; Lat long estimation is based on map in fig. 1 in Olson (1951, J. Geol. 59(2), pp. 178-181) ",gp_mid,-30.21,0,101,US,,Choza,Clear Fork,,,,,,,,,NA,Lower part of the Choza Fm.,"""The deposits at the 'pipe site' are extremely interesting and unlike those encountered anywhere else in the Wichita or Clear Fork sections. The bed from which the fossils come is a deep red shale, exposed on a series of hills over an area about an eighth of a mile on each side. This bed is capped in many places by a thin, dense siltstone. Overlying the siltstone is an orange-red shale that carries gypsum biscuits. Underlying the producing layer, which averages about four feet in thickness, is a brownish-red shale that is devoid\r\nof fossils. The most distinctive feature of the bone-bearing shale, outside of the fact that it has fossils, is the occurrence of two types of vertically oriented ovoid structures. One type consists of mottled red and green, hard nodules that range from one to four inches in maximum diameter and up to eighteen inches in length. They are rich in vertebrate remains. They appear to have formed around the bones after deposition, presumably as a result of the reducing action of organic materials. Their vertical orientation is somewhat\r\npuzzling. The contained vertebrate remains are usually oriented with their long axes vertical, and it seems quite certain that this position was attained after the formation of the nodules. Specimens of vertebrates free in the shale rather than in nodules are orientated with their long axes horizontal and have been subjected to considerable distortion and breakage. The most reasonable suggestion seems to be that the vertical orientation of the nodules was developed during compaction of the shales, which has been extensive, with the long axes shifting to become normal to the compacting forces.\r\nThe other vertical structures [...] have been termed pipes and have given the name to the site. They pass from the base to the top of the fossiliferous bed and, at the top, are continuous with the siltstone layer that caps the bed. Their composition is similar to the capping siltstone. The pipes are oval in cross section with maximum diameters from about four to twelve inches. Orientation of the long diameters is random, even in the 'clumps' in which the pipes tend to occur. These structures do not contain vertebrates, although specimens are found 'plastered' to their sides and occasionally penetrating the pipe for a short distance.\r\nThe origin of the pipes is by no means certain. It is thought that they were formed in open holes by the introduction of the sediment that formed the siltstone layer. Superficially, they resemble lungfish burrows of the Arroyo and Vale (Romer and Olson, 1954), but the shape, size, composition, weathering, and fossil content differ. The most probable explanation is that these openings were formed by the root-like shafts of some type of plant, possibly some\r\nEquisetales, that rotted to leave openings that were later filled by sediment. There is no question that the red shales surrounding the pipes were deposited in a shallow pond, and such a pond might well have provided suitable habitat for the type of vegetation envisaged."" (Olson, 1955 pp. 60-63)","""shale""",red or brown,,,Y,,,,,,pond,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,abundant,,,NA,,,taxonomic,,,,,,E. C. Olson,1949,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 12:17,15/03/2016 12:17,58444,tricarinatus,Lysorophus,58444,,290.1,268,Leonard,,NA,US,Lysorophus tricarinatus
1317936,occ,NA,,177006,,Diplocaulus recurvatus,species,120886,,Diplocaulus recurvatus,NA,species,120886,Olson,1958,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.558334,33.816666,Locality FA (Choza Fm.) Main site,NA,,US,Texas,Foard,estimated from map,seconds,outcrop,"southeastern corner of Foard Co.; Lat long estimation is based on map in fig. 1 in Olson (1951, J. Geol. 59(2), pp. 178-181) ",gp_mid,-30.21,0,101,US,,Choza,Clear Fork,,,,,,,,,NA,Lower part of the Choza Fm.,"""The deposits at the 'pipe site' are extremely interesting and unlike those encountered anywhere else in the Wichita or Clear Fork sections. The bed from which the fossils come is a deep red shale, exposed on a series of hills over an area about an eighth of a mile on each side. This bed is capped in many places by a thin, dense siltstone. Overlying the siltstone is an orange-red shale that carries gypsum biscuits. Underlying the producing layer, which averages about four feet in thickness, is a brownish-red shale that is devoid\r\nof fossils. The most distinctive feature of the bone-bearing shale, outside of the fact that it has fossils, is the occurrence of two types of vertically oriented ovoid structures. One type consists of mottled red and green, hard nodules that range from one to four inches in maximum diameter and up to eighteen inches in length. They are rich in vertebrate remains. They appear to have formed around the bones after deposition, presumably as a result of the reducing action of organic materials. Their vertical orientation is somewhat\r\npuzzling. The contained vertebrate remains are usually oriented with their long axes vertical, and it seems quite certain that this position was attained after the formation of the nodules. Specimens of vertebrates free in the shale rather than in nodules are orientated with their long axes horizontal and have been subjected to considerable distortion and breakage. The most reasonable suggestion seems to be that the vertical orientation of the nodules was developed during compaction of the shales, which has been extensive, with the long axes shifting to become normal to the compacting forces.\r\nThe other vertical structures [...] have been termed pipes and have given the name to the site. They pass from the base to the top of the fossiliferous bed and, at the top, are continuous with the siltstone layer that caps the bed. Their composition is similar to the capping siltstone. The pipes are oval in cross section with maximum diameters from about four to twelve inches. Orientation of the long diameters is random, even in the 'clumps' in which the pipes tend to occur. These structures do not contain vertebrates, although specimens are found 'plastered' to their sides and occasionally penetrating the pipe for a short distance.\r\nThe origin of the pipes is by no means certain. It is thought that they were formed in open holes by the introduction of the sediment that formed the siltstone layer. Superficially, they resemble lungfish burrows of the Arroyo and Vale (Romer and Olson, 1954), but the shape, size, composition, weathering, and fossil content differ. The most probable explanation is that these openings were formed by the root-like shafts of some type of plant, possibly some\r\nEquisetales, that rotted to leave openings that were later filled by sediment. There is no question that the red shales surrounding the pipes were deposited in a shallow pond, and such a pond might well have provided suitable habitat for the type of vegetation envisaged."" (Olson, 1955 pp. 60-63)","""shale""",red or brown,,,Y,,,,,,pond,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,abundant,,,NA,,,taxonomic,,,,,,E. C. Olson,1949,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 12:17,15/03/2016 12:17,58444,recurvatus,Diplocaulus,58444,,290.1,268,Leonard,,NA,US,Diplocaulus recurvatus
1317937,occ,NA,,177006,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Olson,1958,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-99.558334,33.816666,Locality FA (Choza Fm.) Main site,NA,,US,Texas,Foard,estimated from map,seconds,outcrop,"southeastern corner of Foard Co.; Lat long estimation is based on map in fig. 1 in Olson (1951, J. Geol. 59(2), pp. 178-181) ",gp_mid,-30.21,0,101,US,,Choza,Clear Fork,,,,,,,,,NA,Lower part of the Choza Fm.,"""The deposits at the 'pipe site' are extremely interesting and unlike those encountered anywhere else in the Wichita or Clear Fork sections. The bed from which the fossils come is a deep red shale, exposed on a series of hills over an area about an eighth of a mile on each side. This bed is capped in many places by a thin, dense siltstone. Overlying the siltstone is an orange-red shale that carries gypsum biscuits. Underlying the producing layer, which averages about four feet in thickness, is a brownish-red shale that is devoid\r\nof fossils. The most distinctive feature of the bone-bearing shale, outside of the fact that it has fossils, is the occurrence of two types of vertically oriented ovoid structures. One type consists of mottled red and green, hard nodules that range from one to four inches in maximum diameter and up to eighteen inches in length. They are rich in vertebrate remains. They appear to have formed around the bones after deposition, presumably as a result of the reducing action of organic materials. Their vertical orientation is somewhat\r\npuzzling. The contained vertebrate remains are usually oriented with their long axes vertical, and it seems quite certain that this position was attained after the formation of the nodules. Specimens of vertebrates free in the shale rather than in nodules are orientated with their long axes horizontal and have been subjected to considerable distortion and breakage. The most reasonable suggestion seems to be that the vertical orientation of the nodules was developed during compaction of the shales, which has been extensive, with the long axes shifting to become normal to the compacting forces.\r\nThe other vertical structures [...] have been termed pipes and have given the name to the site. They pass from the base to the top of the fossiliferous bed and, at the top, are continuous with the siltstone layer that caps the bed. Their composition is similar to the capping siltstone. The pipes are oval in cross section with maximum diameters from about four to twelve inches. Orientation of the long diameters is random, even in the 'clumps' in which the pipes tend to occur. These structures do not contain vertebrates, although specimens are found 'plastered' to their sides and occasionally penetrating the pipe for a short distance.\r\nThe origin of the pipes is by no means certain. It is thought that they were formed in open holes by the introduction of the sediment that formed the siltstone layer. Superficially, they resemble lungfish burrows of the Arroyo and Vale (Romer and Olson, 1954), but the shape, size, composition, weathering, and fossil content differ. The most probable explanation is that these openings were formed by the root-like shafts of some type of plant, possibly some\r\nEquisetales, that rotted to leave openings that were later filled by sediment. There is no question that the red shales surrounding the pipes were deposited in a shallow pond, and such a pond might well have provided suitable habitat for the type of vegetation envisaged."" (Olson, 1955 pp. 60-63)","""shale""",red or brown,,,Y,,,,,,pond,foreland basin,,macrofossils,,,,,,NA,,"body,concretion",variable,,,,,,abundant,,,NA,,,taxonomic,,,,,,E. C. Olson,1949,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,15/03/2016 12:17,15/03/2016 12:17,58444,sp.,Trimerorhachis,58444,,290.1,268,Leonard,,NA,US,Trimerorhachis sp.
1317969,occ,NA,,177014,members,Diplocaulus recurvatus,species,120886,,Diplocaulus recurvatus,NA,species,120886,Olson,1958,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.599998,33.703335,Locality KD Quarry site,NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""Valley of South Wichita River, north of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.88,101,US,,Vale,Clear Fork,"""Bullwagon""",bed,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surfacer and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,siltstone,lenticular,,,Y,dry floodplain,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",mesofossils,,,,,,NA,,body,variable,,snapshot,,,,,,occasional,NA,,,taxonomic,field collection,,,,,"E. C. Olson, E. L. Yochelson, S. H. Mamay","1946-1948, 1955","Olson (1958) divided the main locality into Quarry Site and Weathered Boulder Site, leaving the main one for recording scattered finds",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,16/03/2016 05:06,16/03/2016 05:06,NA,recurvatus,Diplocaulus,58444,,279.3,272.3,Kungurian,,NA,US,Diplocaulus recurvatus
1317970,occ,NA,,177014,members,Dimetrodon gigashomogenes,species,138123,,Dimetrodon gigashomogenes,NA,species,138123,Olson,1958,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.599998,33.703335,Locality KD Quarry site,NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""Valley of South Wichita River, north of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.88,101,US,,Vale,Clear Fork,"""Bullwagon""",bed,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surfacer and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,siltstone,lenticular,,,Y,dry floodplain,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",mesofossils,,,,,,NA,,body,variable,,snapshot,,,,,,occasional,NA,,,taxonomic,field collection,,,,,"E. C. Olson, E. L. Yochelson, S. H. Mamay","1946-1948, 1955","Olson (1958) divided the main locality into Quarry Site and Weathered Boulder Site, leaving the main one for recording scattered finds",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,16/03/2016 05:06,16/03/2016 05:06,NA,gigashomogenes,Dimetrodon,58444,,279.3,272.3,Kungurian,,NA,US,Dimetrodon gigashomogenes
1317973,occ,NA,,177015,members,Lysorophus tricarinatus,species,70395,,Lysorophus tricarinatus,NA,species,70395,Olson,1958,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-99.599998,33.703335,Locality KD Weathered Boulder site,NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""Valley of South Wichita River, north of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.88,101,US,,Vale,Clear Fork,"""Bullwagon""",bed,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surfacer and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,siltstone,lenticular,,,Y,dry floodplain,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",mesofossils,,,,,,NA,,body,variable,,snapshot,,,,,,occasional,NA,,,taxonomic,field collection,,,,,"E. C. Olson, E. L. Yochelson, S. H. Mamay","1946-1948, 1955","Olson (1958) divided the main locality into Quarry Site and Weathered Boulder Site, leaving the main one for recording scattered finds",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,16/03/2016 05:08,16/03/2016 05:08,NA,tricarinatus,Lysorophus,58444,,279.3,272.3,Kungurian,,NA,US,Lysorophus tricarinatus
1317974,occ,NA,,177015,members,Diplocaulus recurvatus,species,120886,,Diplocaulus recurvatus,NA,species,120886,Olson,1958,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.599998,33.703335,Locality KD Weathered Boulder site,NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""Valley of South Wichita River, north of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.88,101,US,,Vale,Clear Fork,"""Bullwagon""",bed,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surfacer and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,siltstone,lenticular,,,Y,dry floodplain,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",mesofossils,,,,,,NA,,body,variable,,snapshot,,,,,,occasional,NA,,,taxonomic,field collection,,,,,"E. C. Olson, E. L. Yochelson, S. H. Mamay","1946-1948, 1955","Olson (1958) divided the main locality into Quarry Site and Weathered Boulder Site, leaving the main one for recording scattered finds",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,16/03/2016 05:08,16/03/2016 05:08,NA,recurvatus,Diplocaulus,58444,,279.3,272.3,Kungurian,,NA,US,Diplocaulus recurvatus
1317975,occ,NA,,177015,members,Captorhinikos valensis,species,120855,,Captorhinikos valensis,NA,species,120855,Olson,1958,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37496,NA,NA,NA,,-99.599998,33.703335,Locality KD Weathered Boulder site,NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""Valley of South Wichita River, north of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.88,101,US,,Vale,Clear Fork,"""Bullwagon""",bed,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surfacer and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,siltstone,lenticular,,,Y,dry floodplain,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",mesofossils,,,,,,NA,,body,variable,,snapshot,,,,,,occasional,NA,,,taxonomic,field collection,,,,,"E. C. Olson, E. L. Yochelson, S. H. Mamay","1946-1948, 1955","Olson (1958) divided the main locality into Quarry Site and Weathered Boulder Site, leaving the main one for recording scattered finds",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinikos,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,16/03/2016 05:08,16/03/2016 05:08,NA,valensis,Captorhinikos,58444,,279.3,272.3,Kungurian,,NA,US,Captorhinikos valensis
1317976,occ,NA,,177015,members,Captorhinus ? sp.,genus,37497,,Captorhinus,NA,genus,37497,Olson,1958,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,,-99.599998,33.703335,Locality KD Weathered Boulder site,NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""Valley of South Wichita River, north of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.88,101,US,,Vale,Clear Fork,"""Bullwagon""",bed,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surfacer and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,siltstone,lenticular,,,Y,dry floodplain,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",mesofossils,,,,,,NA,,body,variable,,snapshot,,,,,,occasional,NA,,,taxonomic,field collection,,,,,"E. C. Olson, E. L. Yochelson, S. H. Mamay","1946-1948, 1955","Olson (1958) divided the main locality into Quarry Site and Weathered Boulder Site, leaving the main one for recording scattered finds",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,?,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,16/03/2016 05:08,16/03/2016 05:08,NA,sp.,Captorhinus,58444,,279.3,272.3,Kungurian,,NA,US,Captorhinus sp.
1317977,occ,NA,,12976,,Waggoneria knoxensis,species,120859,,Waggoneria knoxensis,NA,species,120859,Olson,1958,Chordata,33815,Osteichthyes,34881,,NA,Waggoneriidae,120858,120857,NA,NA,NA,,-99.599998,33.703335,Locality KD,NA,(Upper Vale Fm.) Main site,US,Texas,Knox,estimated from map,seconds,outcrop,"""Valley of South Wichita River, north of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.88,101,US,,Vale,Clear Fork,"""Bullwagon""",group of beds,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surfacer and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,siltstone,lenticular,,,Y,dry floodplain,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",mesofossils,,,,,,NA,,body,variable,,snapshot,,,,,,occasional,NA,,,taxonomic,field collection,FMNH,,,,"E. C. Olson, E. L. Yochelson, S. H. Mamay","1946-1948, 1955","Olson (1958) divided the locality into Quarry Site and Weathered Boulder Site, leaving the main one for recording scattered finds",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Waggoneria,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,697,R. Butler,E. Dunne,E. Dunne,16/03/2016 05:13,19/08/2016 10:20,28928,knoxensis,Waggoneria,58444,,279.3,272.3,Kungurian,,NA,US,Waggoneria knoxensis
1317978,occ,NA,,12976,,Dimetrodon gigashomogenes,species,138123,,Dimetrodon gigashomogenes,NA,species,138123,Olson,1958,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.599998,33.703335,Locality KD,NA,(Upper Vale Fm.) Main site,US,Texas,Knox,estimated from map,seconds,outcrop,"""Valley of South Wichita River, north of River and East of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.23,1.88,101,US,,Vale,Clear Fork,"""Bullwagon""",group of beds,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surfacer and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190);\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)",conglomerate,"pebbly,green,red",,,Y,siltstone,lenticular,,,Y,dry floodplain,foreland basin,"""The channels are evidence that a rather large, braided stream passed north or south over the area in a valley of considerable width. The region must have had a moderately high annual rainfall to support the fauna and flora. The total rainfall was perhaps not greatly different from what it is today, and the temperature may have been quite similar, with possibly less seasonal variation. The rains, however appear to have been periodic and torrential [...] "" Olson (1948, p. 192)",mesofossils,,,,,,NA,,body,variable,,snapshot,,,,,,occasional,NA,,,taxonomic,field collection,FMNH,,,,"E. C. Olson, E. L. Yochelson, S. H. Mamay","1946-1948, 1955","Olson (1958) divided the locality into Quarry Site and Weathered Boulder Site, leaving the main one for recording scattered finds",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,16/03/2016 05:13,16/03/2016 05:13,28928,gigashomogenes,Dimetrodon,58444,,279.3,272.3,Kungurian,,NA,US,Dimetrodon gigashomogenes
1317979,occ,NA,,177017,members,Lysorophus tricarinatus,species,70395,,Lysorophus tricarinatus,NA,species,70395,Olson,1958,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-99.586945,33.737221,Locality KJ (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""North wall of valley of South Wichita River, east of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.21,1.9,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)","""shale""","green,red",,,Y,sandstone,,,,,wet floodplain,,"""Even red and green shales with interbedded thick layers of sandstone and thin sheets of conglomerate. All apparently flood plain in origin. One large channel deposit and a few fine-grained channel deposits. Occasional pond deposits of light red shale. Westernmost beds transitional between Vale and Choza Formations."" (Olson, 1958)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,E. C. Olson,"1946, 1947",,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,16/03/2016 05:22,16/03/2016 05:22,NA,tricarinatus,Lysorophus,58444,,279.3,272.3,Kungurian,,NA,US,Lysorophus tricarinatus
1317980,occ,NA,,177017,members,Diplocaulus recurvatus,species,120886,,Diplocaulus recurvatus,NA,species,120886,Olson,1958,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.586945,33.737221,Locality KJ (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""North wall of valley of South Wichita River, east of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.21,1.9,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)","""shale""","green,red",,,Y,sandstone,,,,,wet floodplain,,"""Even red and green shales with interbedded thick layers of sandstone and thin sheets of conglomerate. All apparently flood plain in origin. One large channel deposit and a few fine-grained channel deposits. Occasional pond deposits of light red shale. Westernmost beds transitional between Vale and Choza Formations."" (Olson, 1958)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,E. C. Olson,"1946, 1947",,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,16/03/2016 05:22,16/03/2016 05:22,NA,recurvatus,Diplocaulus,58444,,279.3,272.3,Kungurian,,NA,US,Diplocaulus recurvatus
1317981,occ,NA,,177017,members,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Olson,1958,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-99.586945,33.737221,Locality KJ (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""North wall of valley of South Wichita River, east of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.21,1.9,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)","""shale""","green,red",,,Y,sandstone,,,,,wet floodplain,,"""Even red and green shales with interbedded thick layers of sandstone and thin sheets of conglomerate. All apparently flood plain in origin. One large channel deposit and a few fine-grained channel deposits. Occasional pond deposits of light red shale. Westernmost beds transitional between Vale and Choza Formations."" (Olson, 1958)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,E. C. Olson,"1946, 1947",,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,16/03/2016 05:22,16/03/2016 05:22,NA,sp.,Trimerorhachis,58444,,279.3,272.3,Kungurian,,NA,US,Trimerorhachis sp.
1317982,occ,NA,,177017,members,Dimetrodon gigashomogenes,species,138123,,Dimetrodon gigashomogenes,NA,species,138123,Olson,1958,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.586945,33.737221,Locality KJ (Upper Vale Fm.),NA,,US,Texas,Knox,estimated from map,seconds,small collection,"""North wall of valley of South Wichita River, east of Vera-Gilliland Road""; for details see map on p. 188 in Olson (1948)",gp_mid,-29.21,1.9,101,US,,Vale,Clear Fork,"""Bullwagon""",member,,,,,,,NA,"""Robert Roth, of the Humble Oil and Refining Company of Wichita Falls, Texas, believes that surface and subsurface data show that the beds in question are part of the 'Bullwagon' member of the Vale formation. This places the section high in the Vale, just below the Choza."" Olson (1948 p. 190)\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""The channel fill is largely clay pebble conglomerate, with pebbles ranging from a few millimeters to about 8 cm. in diameter. Rounding of the pebbles is uniformly high, but sphericity is varied. [...] The coarsest material tend to lie at the center of the channel, whereas the marginal parts are predominantly sand or clay with fine scattered pebbles."" Olson (1948, p. 191)","""shale""","green,red",,,Y,sandstone,,,,,wet floodplain,,"""Even red and green shales with interbedded thick layers of sandstone and thin sheets of conglomerate. All apparently flood plain in origin. One large channel deposit and a few fine-grained channel deposits. Occasional pond deposits of light red shale. Westernmost beds transitional between Vale and Choza Formations."" (Olson, 1958)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,E. C. Olson,"1946, 1947",,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,16/03/2016 05:22,16/03/2016 05:22,NA,gigashomogenes,Dimetrodon,58444,,279.3,272.3,Kungurian,,NA,US,Dimetrodon gigashomogenes
1317984,occ,NA,,177018,members,Diplocaulus recurvatus,species,120886,,Diplocaulus recurvatus,NA,species,120886,Olson,1958,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.558334,33.816666,Locality KM (Lower Choza Fm.) ,NA,,US,Texas,Foard,estimated from map,seconds,outcrop,"Southeastern corner of Foard Co.; Lat long estimation is based on map in fig. 1 in Olson (1951, J. Geol. 59(2), pp. 178-181) ",gp_mid,-30.21,0,101,US,,Choza,Clear Fork,,,,,,,,,NA,Lower part of the Choza Fm.,"""Varied red, green, and yellow shales, with evenness of bedding increasing to west. Anhydrite abundant in western part. Pond shales in western half of area. A thin sheet of fine conglomerate, with lenses suggesting channels, is present over a wide area in the central and western parts of the locality. It occurs near the base of the exposed section."" (Olson, 1958)","""shale""","green,red,yellow",,,Y,conglomerate,,,,,pond,foreland basin,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,taxonomic,,,,,,E. C. Olson,1949,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,16/03/2016 05:29,16/03/2016 05:29,NA,recurvatus,Diplocaulus,58444,,290.1,268,Leonard,,NA,US,Diplocaulus recurvatus
1317985,occ,NA,,177019,members,Diplocaulus magnicornis,species,81712,,Diplocaulus magnicornis,NA,species,81712,Olson,1958,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.25,33.599998,Locality BR (Lower Vale Fm.),NA,,US,Texas,Baylor,based on nearby landmark,minutes,small collection,"For detailed map of area, see Olson (1958)",gp_mid,-29.04,1.64,101,US,,Vale,Clear Fork,,bed,,,,,,,NA,"Lower part of the Vale Formation, about 100 feet above base. Lower Permian (Leonardian). The base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""Irregularly distributed sandstone, silts, red shales, and fine conglomerates. A few poorly developed channel deposits. Deposition mainly on flood plains lateral to principal stream channels. Some pond deposits of red shale."" (Olson, 1958)",sandstone,,,,,siltstone,,,,,dry floodplain,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,16/03/2016 05:40,16/03/2016 05:40,NA,magnicornis,Diplocaulus,58444,,279.3,272.3,Kungurian,,NA,US,Diplocaulus magnicornis
1317986,occ,NA,,177019,members,Trimerorhachis insignis,species,90711,,Trimerorhachis insignis,NA,species,90711,Olson,1958,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-99.25,33.599998,Locality BR (Lower Vale Fm.),NA,,US,Texas,Baylor,based on nearby landmark,minutes,small collection,"For detailed map of area, see Olson (1958)",gp_mid,-29.04,1.64,101,US,,Vale,Clear Fork,,bed,,,,,,,NA,"Lower part of the Vale Formation, about 100 feet above base. Lower Permian (Leonardian). The base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""Irregularly distributed sandstone, silts, red shales, and fine conglomerates. A few poorly developed channel deposits. Deposition mainly on flood plains lateral to principal stream channels. Some pond deposits of red shale."" (Olson, 1958)",sandstone,,,,,siltstone,,,,,dry floodplain,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,16/03/2016 05:40,16/03/2016 05:40,NA,insignis,Trimerorhachis,58444,,279.3,272.3,Kungurian,,NA,US,Trimerorhachis insignis
1317987,occ,NA,,177019,members,Eryops megacephalus,species,70397,,Eryops megacephalus,NA,species,70397,Olson,1958,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-99.25,33.599998,Locality BR (Lower Vale Fm.),NA,,US,Texas,Baylor,based on nearby landmark,minutes,small collection,"For detailed map of area, see Olson (1958)",gp_mid,-29.04,1.64,101,US,,Vale,Clear Fork,,bed,,,,,,,NA,"Lower part of the Vale Formation, about 100 feet above base. Lower Permian (Leonardian). The base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""Irregularly distributed sandstone, silts, red shales, and fine conglomerates. A few poorly developed channel deposits. Deposition mainly on flood plains lateral to principal stream channels. Some pond deposits of red shale."" (Olson, 1958)",sandstone,,,,,siltstone,,,,,dry floodplain,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,16/03/2016 05:40,16/03/2016 05:40,NA,megacephalus,Eryops,58444,,279.3,272.3,Kungurian,,NA,US,Eryops megacephalus
1317988,occ,NA,,177019,members,Labidosaurikos barkeri,species,119514,subjective synonym of,Labidosaurikos meachami,NA,species,119515,Olson,1958,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37500,NA,NA,NA,,-99.25,33.599998,Locality BR (Lower Vale Fm.),NA,,US,Texas,Baylor,based on nearby landmark,minutes,small collection,"For detailed map of area, see Olson (1958)",gp_mid,-29.04,1.64,101,US,,Vale,Clear Fork,,bed,,,,,,,NA,"Lower part of the Vale Formation, about 100 feet above base. Lower Permian (Leonardian). The base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""Irregularly distributed sandstone, silts, red shales, and fine conglomerates. A few poorly developed channel deposits. Deposition mainly on flood plains lateral to principal stream channels. Some pond deposits of red shale."" (Olson, 1958)",sandstone,,,,,siltstone,,,,,dry floodplain,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurikos,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,16/03/2016 05:40,16/03/2016 05:40,NA,barkeri,Labidosaurikos,58444,,279.3,272.3,Kungurian,,NA,US,Labidosaurikos barkeri
1317989,occ,NA,,177019,members,Dimetrodon gigashomogenes,species,138123,,Dimetrodon gigashomogenes,NA,species,138123,Olson,1958,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.25,33.599998,Locality BR (Lower Vale Fm.),NA,,US,Texas,Baylor,based on nearby landmark,minutes,small collection,"For detailed map of area, see Olson (1958)",gp_mid,-29.04,1.64,101,US,,Vale,Clear Fork,,bed,,,,,,,NA,"Lower part of the Vale Formation, about 100 feet above base. Lower Permian (Leonardian). The base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""Irregularly distributed sandstone, silts, red shales, and fine conglomerates. A few poorly developed channel deposits. Deposition mainly on flood plains lateral to principal stream channels. Some pond deposits of red shale."" (Olson, 1958)",sandstone,,,,,siltstone,,,,,dry floodplain,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,16/03/2016 05:40,16/03/2016 05:40,NA,gigashomogenes,Dimetrodon,58444,,279.3,272.3,Kungurian,,NA,US,Dimetrodon gigashomogenes
1318094,occ,NA,,85292,,n. gen. Pleuroptyx n. sp. clavatus,species,320832,,Pleuroptyx clavatus,NA,species,320832,Cope,1875,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,Cocytinidae,320813,320831,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Pleuroptyx,n. gen.,NA,NA,vertebrate,E. D. Cope. 1875. Synopsis of the Extinct Batrachia from the Coal Measures. Report of the Geological Survey of Ohio 2:349-411,327,697,0,R. Butler,E. Dunne,,18/03/2016 05:20,18/03/2016 05:20,28831,clavatus,Pleuroptyx,28747,n. sp.,311.45,306.95,Westphalian D,,NA,US,Pleuroptyx clavatus
1318095,occ,NA,,85292,,n. gen. Molgophis n. sp. macrurus,species,320834,,Molgophis macrurus,NA,species,320834,Cope,1868,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37324,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Molgophis,n. gen.,NA,NA,vertebrate,E. D. Cope. 1868. Synopsis of the Extinct Batrachia of North America. Proceedings of the Academy of Natural Sciences of Philadelphia 1868:208-221,327,697,0,R. Butler,E. Dunne,,18/03/2016 05:28,18/03/2016 05:28,28831,macrurus,Molgophis,28717,n. sp.,311.45,306.95,Westphalian D,,NA,US,Molgophis macrurus
1318096,occ,NA,,85292,,n. gen. Brachydectes n. sp. newberryi,species,229312,,Brachydectes newberryi,NA,species,229312,Cope,1868,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,Cocytinidae,320813,227167,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Brachydectes,n. gen.,NA,NA,vertebrate,E. D. Cope. 1868. Synopsis of the Extinct Batrachia of North America. Proceedings of the Academy of Natural Sciences of Philadelphia 1868:208-221,327,697,0,R. Butler,E. Dunne,,18/03/2016 05:31,18/03/2016 05:31,28831,newberryi,Brachydectes,28717,n. sp.,311.45,306.95,Westphalian D,,NA,US,Brachydectes newberryi
1318097,occ,NA,,177046,members,Molgophis macrurus,species,320834,,Molgophis macrurus,NA,species,320834,Carroll et al.,1998,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37324,NA,NA,NA,,-81.331436,39.796654,"Summerfield limestone, Noble County",NA,,US,Ohio,Noble,based on nearby landmark,6,small collection,Coordinates based on the town of Summerfield after which Condit (1912) named the Summerfield Limestone.,gp_mid,-16.44,-4.66,101,US,,,Conemaugh,,,,,,,,,NA,"Summerfield Limestone lies 25 feet below the Pittsburgh coal bed at Summerfield, Ohio, USA (Condit, 1912)",,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Molgophis,,NA,NA,vertebrate,"R. L. Carroll, K. A. Bossy, and A. C. Milner, S. M. Andrews, C. F. Wellstead. 1998. Handbuch der Palaoherpetologie / Encyclopedia of Paleoherpetology Teil 1 / Part 1 Lepospondyli: Microsauria, Nectridea, Lysorophia, Adelospondyli, Aistopoda, Acherontiscidae. ",327,697,0,R. Butler,E. Dunne,,18/03/2016 05:56,18/03/2016 05:56,NA,macrurus,Molgophis,55379,,306.95,298.9,Stephanian,,NA,US,Molgophis macrurus
1318128,occ,NA,,79598,,Brachydectes newberryi,species,229312,,Brachydectes newberryi,NA,species,229312,Carroll et al.,1998,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,Cocytinidae,320813,227167,NA,NA,NA,,-88.139999,41.267223,Mazon Creek,NA,"Mazon Creek Vertebrate Fauna, Braidwood Fauna, pit 11",US,Illinois,Grundy/Will,based on political unit,seconds,local area,"Lat Long is for SW Will Co., Illinois",gp_mid,-23.34,-5.09,101,US,,Carbondale,,Francis Creek Shale,,,,,,,,NA,"""Francis Creek Shale above Morris (no. 2) Coal, Carbondale Formation, Westphalian D, Middle Pennsylvanian"" (Carroll & Baird, 1972)\r\nBaird et al. (1985) refer to the no. 2 coal as Colchester or Croweburg Coal Member.","""Concretions occur typically in laminated to weakly rippled, silty mudstone deposits which typically show little or no evidence of bioturbation. Small-scale sedimentary structures in nodule-bearing sequences include climbing ripple drift, and soft-sediment load-failure..."" (Baird et al., 1985 p.90). Note that this is a general description of the fossil bearing strata of the Francis Creek Shale Member which does not refer specifically to the occurences in the Mazon Creek area proper.",mudstone,"current ripples,deformed bedding",,silty,,siderite,nodular,,,Y,deltaic indet.,foreland basin,"""...these indicate rapid and often episodic mud deposition in interdistributary bay and prodelta settings."" (Baird et al., 1985 p.90)",macrofossils,,,,,,NA,,"mold/impression,concretion,soft parts,replaced with other",good,parautochthonous,,,,,,,,NA,,"""Outlines of the limbs can be seen in the matrix, indicating the extent of the soft tissue and the texture of the skin. The bone itself was represented by a very soft, claylike material that had been removed from the hard, ironstone matrix."" (Carroll, & Baird, 1972 p. 323)\r\nBones are replaced by clay minerals such as Kaolinite (Gregory, 1948 p. 637).",taxonomic,"mechanical,survey of museum collection","FMNH,MCZ,USNM,YPM","species names,ichnofossils",,,"R. L. Moodie, P. Turnbull, among others","1871, 1953",,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Brachydectes,,NA,NA,vertebrate,"R. L. Carroll, K. A. Bossy, and A. C. Milner, S. M. Andrews, C. F. Wellstead. 1998. Handbuch der Palaoherpetologie / Encyclopedia of Paleoherpetology Teil 1 / Part 1 Lepospondyli: Microsauria, Nectridea, Lysorophia, Adelospondyli, Aistopoda, Acherontiscidae. ",327,697,0,R. Butler,E. Dunne,,18/03/2016 07:31,18/03/2016 07:31,28608,newberryi,Brachydectes,55379,,311.45,306.95,Westphalian D,,NA,US,Brachydectes newberryi
1318131,occ,NA,,177058,members,Brachydectes newberryi,species,229312,,Brachydectes newberryi,NA,species,229312,Carroll et al.,1998,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,Cocytinidae,320813,227167,NA,NA,NA,,-80.657288,40.04414,Elm Grove,NA,,US,West Virginia,Ohio,estimated from map,6,small collection,"Coordinates based on Elm Grove, within Wheeling city limits in Ohio County, West Virginia, United States. The Elm Grove locality is found along a road cut on Interstate Highway 70, near the town of Elm Grove.",gp_mid,-15.22,-3.49,101,US,,Pittsburgh,Monongahela,"Monongahela ""B"" freshwater Limestone",bed,,,,,,,NA,"Stratigraphy originally recorded as ""Stephanian"" (Carroll et al., 1998). Update: The Pittsburgh Fm. is the lower unit of the Monongahela Group and is entirely within the Virgilian (see, e.g. Eble et al., 2006, pp. 197-222 in GSA Spec. Pap. 399) . \r\n""The fossiliferous horizon is Limestone B of the Pittsburgh Formation of the Monongahela Group (Berman, 1979), which is considered Virgilian in age (Berman et al., 1997)."" Kissel (2010)",,"""limestone""",,,,,,,,,,fluvial indet.,foreland basin,"The deposit preserved at the Elm Grove locality is interpreted as a meander cutoff channel that filled very slowly (Lund, 1972).",macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,"selective quarrying,surface (in situ),mechanical,field collection,survey of museum collection",CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Brachydectes,,NA,NA,vertebrate,"R. L. Carroll, K. A. Bossy, and A. C. Milner, S. M. Andrews, C. F. Wellstead. 1998. Handbuch der Palaoherpetologie / Encyclopedia of Paleoherpetology Teil 1 / Part 1 Lepospondyli: Microsauria, Nectridea, Lysorophia, Adelospondyli, Aistopoda, Acherontiscidae. ",327,697,327,R. Butler,E. Dunne,R. Butler,18/03/2016 07:45,06/05/2016 11:12,NA,newberryi,Brachydectes,55379,,303.4,298.9,Virgilian,,NA,US,Brachydectes newberryi
1318145,occ,NA,,177062,members,Brachydectes n. sp. elongatus,species,229311,,Brachydectes elongatus,NA,species,229311,Olson,1971,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,Cocytinidae,320813,227167,NA,NA,NA,,-97.382202,35.150566,"SW/4, NW/4, sec 13, T8N, R2W, Cleveland County",NA,5 miles SE of the University of Oklahoma main campus,US,Oklahoma,Cleveland,estimated from map,6,small collection,,gp_mid,-27.98,0.22,101,US,,fairmont Shale,Hennessey,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Brachydectes,,NA,NA,vertebrate,E. C. Olson. 1971. A skeleton of Lysorophus tricarinatus (Amphibia; Lepospondyli) from the Hennessey Formation (Permian) of Oklahoma. Journal of Paleontology 45:443-449,327,697,0,R. Butler,E. Dunne,,18/03/2016 11:21,18/03/2016 11:21,NA,elongatus,Brachydectes,58494,n. sp.,290.1,268,Leonard,,NA,US,Brachydectes elongatus
1318147,occ,NA,,28267,,Brachydectes elongatus,species,229311,,Brachydectes elongatus,NA,species,229311,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,Cocytinidae,320813,227167,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Brachydectes,,NA,NA,vertebrate,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,0,R. Butler,E. Dunne,,18/03/2016 11:28,18/03/2016 11:28,9228,elongatus,Brachydectes,58492,,279.3,272.3,Kungurian,,NA,US,Brachydectes elongatus
1318148,occ,NA,,85342,,Brachydectes elongatus,species,229311,,Brachydectes elongatus,NA,species,229311,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,Cocytinidae,320813,227167,NA,NA,NA,,-99.316666,33.75,Big Wichita River (Arroyo Fm.),NA,,US,Texas,Baylor,estimated from map,minutes,small collection,"""North side Big Wichita River, Baylor County, Texas""",gp_mid,-29.01,1.8,101,US,,Arroyo,Clear Fork,,bed,,,,,,,NA,,,"""shale""",gray,,,Y,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,medium,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Brachydectes,,NA,NA,vertebrate,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,0,R. Butler,E. Dunne,,18/03/2016 11:30,18/03/2016 11:30,28784,elongatus,Brachydectes,58492,,279.3,272.3,Kungurian,,NA,US,Brachydectes elongatus
1318150,occ,NA,,28256,,Brachydectes elongatus,species,229311,,Brachydectes elongatus,NA,species,229311,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,Cocytinidae,320813,227167,NA,NA,NA,,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Brachydectes,,NA,NA,vertebrate,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,0,R. Butler,E. Dunne,,18/03/2016 11:33,18/03/2016 11:33,17702,elongatus,Brachydectes,58492,,279.3,272.3,Kungurian,,NA,US,Brachydectes elongatus
1318157,occ,NA,,177067,members,Brachydectes sp.,genus,227167,,Brachydectes,NA,genus,227167,Moran,1952,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,Cocytinidae,320813,227167,NA,NA,NA,,-80.599998,39.766666,"Greene Formation, Marshall County",NA,,US,West Virginia,Marshall,based on nearby landmark,minutes,small collection,,gp_mid,-14.59,-2.56,101,US,,Greene,Dunkard,,bed,,,,,,,NA,,,"""limestone""",,,,,,,,,,marine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Brachydectes,,NA,NA,vertebrate,"W. E. Moran. 1952. Location and Stratigraphy of Known Occurrences of Fossil Tetrapods in the Upper Pennsylvanian and Permian of Pennsylvania, West Virginia, and Ohio. Annals of Carnegie Museum 33:1-45",327,697,697,R. Butler,E. Dunne,E. Dunne,18/03/2016 12:01,18/03/2016 12:01,NA,sp.,Brachydectes,28677,,295.5,290.1,Sakmarian,,NA,US,Brachydectes sp.
1318298,occ,NA,,80714,,n. gen. Lysorophus n. sp. tricarinatus,species,70395,,Lysorophus tricarinatus,NA,species,70395,Case,1900,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-87.775002,40.108334,Danville Locality (Vertebrates),NA,Oakwood Locality; Horseshoe Bend; Vermillion River; Illinois bonebed,US,Illinois,Vermilion,based on nearby landmark,seconds,outcrop,"""the well-known Danville or 'Oakwood' locality [...] Horseshoe Bend locality near the SE/C of Sec. 23-19N-13W"" (DeMar, 1970)\r\n""Vermilion River, near Danville"" (Reisz, 1986)\r\nLat Long is for Oakwood",gp_mid,-21.51,-3.52,101,US,,Bond,McLeansboro,,group of beds,,,,,,,NA,"""We believe the vertebrates have been collected from a zone 10 feet or so below the Shoal Creek Member of the Bond Formation"" (DeMar, 1970)\r\nNote: Shoal Creek Member is equivalent to Carthage Limestone Member, a name now used throughout the Illinois Basin for that lithological unit; see Jacobson (2002) A summary of references with changes in Pennsylvanian stratigraphic nomenclature at the ISGS since Bulletin 95. [Online] http://www.isgs.illinois.edu/maps-data-pub/coal-maps/pennstratigraphy.shtml ",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,n. gen.,NA,NA,vertebrate,E. C. Case. 1900. The vertebrates from the Permian bone bed of Vermillion County Illinois. Journal of Geology 8:698-729,327,697,0,R. Butler,E. Dunne,,20/03/2016 13:19,20/03/2016 13:19,28640,tricarinatus,Lysorophus,58512,n. sp.,305.9,303.4,Missourian,,NA,US,Lysorophus tricarinatus
1318299,occ,NA,,177138,members,Lysorophus n. sp. dunkardensis,species,320833,,Lysorophus dunkardensis,NA,species,320833,Romer,1952,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-80.642616,39.704937,"Silver Hill, Proctor District",NA,CM Locality 37,US,West Virginia,Marshall,based on nearby landmark,6,small collection,"Coordinates based on Macedonia Cemetry, Marshall County, WV. Location described by Wellstead (1991) as: ""Approximately 1.1km west of Silver Hill, Proctor District, Wetzel County, West Virginia, on the east side of the road to Macedonia School",gp_mid,-14.43,-2.16,101,US,,Greene,Dunkard,,bed,,,,,,,NA,,"""A four-inch thick brown, limey clay of uncertain stratagraphic position within the Greene Formation""",claystone,brown,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,CM,,,,Burke party,1937,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,A. S. Romer. 1952. Late Pennsylvanian and Early Permian Vertebrates of the Pittsburgh-West Virginia Region. Annals of Carnegie Museum 33:47-113,327,697,0,R. Butler,E. Dunne,,20/03/2016 13:28,20/03/2016 13:28,NA,dunkardensis,Lysorophus,28669,n. sp.,296.4,268,Wolfcamp,,NA,US,Lysorophus dunkardensis
1318301,occ,NA,,177139,members,Lysorophus sp.,genus,37322,,Lysorophus,NA,genus,37322,Boyd,1980,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,individuals,-1.52138,55.105228,"Hannah Pit, Newsham",NA,Newsham Colliery,UK,England,Yorkshire,stated in text,6,small collection,"Coordinates are those of the Hannah pit as shown on the First Edition Ordnance Survey map of 1865. The pit was ""sunk in 1860 to the Low Main seam, recorded as a depth of 99 fathoms (181m)""",gp_mid,3.06,-6.8,315,UK,,Middle Coal Measures,,,,,,,,,,NA,"""The horizon lies within the Upper Modiolaris zone of the Middle Coal Measures (Land 1974) and is Westphalian B in age"" (Boyd, 1980)",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,M. J. Boyd. 1980. A lysorophid amphibian from the Coal Measures of northern England. Palaeontology 23:925-929,327,697,327,R. Butler,E. Dunne,R. Butler,20/03/2016 13:49,02/12/2016 08:57,NA,sp.,Lysorophus,58513,,323.2,315.2,Bashkirian,,1,UK,Lysorophus sp.
1318302,occ,NA,,175174,members,Lysorophus sp.,genus,37322,,Lysorophus,NA,genus,37322,Boyd,1980,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-1.7143,53.7626,Toftshaw near Bradford,NA,,UK,England,,,4,,P. scutigerum found in the Black-Bed or Royd's Coal at the location,gp_mid,4.95,-5.02,315,UK,,Lower Coal Measures,,,,,,,,,,NA,"""Black bed"" appears correlative of Mickley 3 coal of the upper Langsettian.",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,some,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,M. J. Boyd. 1980. A lysorophid amphibian from the Coal Measures of northern England. Palaeontology 23:925-929,327,697,0,R. Butler,E. Dunne,,20/03/2016 13:51,20/03/2016 13:51,NA,sp.,Lysorophus,58513,,318.1,314.6,Westphalian A,,NA,UK,Lysorophus sp.
1318303,occ,NA,,85474,,Hylonomus n. sp. geinitzi,species,227058,recombined as,Saxonerpeton geinitzi,NA,species,227058,Credner,1890,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Hapsidopareiontidae,37285,37289,NA,NA,NA,,13.638056,51.018612,Konigin-Carola-Schacht,NA,"Queen Carola Pit; Plauenscher Grund; D̦hlen Basin, K̦nigin-Carola-Schacht",DE,Saxony,Weieritzkreis,based on nearby landmark,seconds,small collection,The abandoned coal pit K̦nigin-Carola-Schacht is situated in the district Zauckerode of the town of Freital near Dresden. Lat long is for Zauckerode. ,gp_mid,23.06,7.42,305,DE,,D̦hlen,Rotliegend,1. Fl̦z (1st seam),bed,,,,,,,NA,"""Cuseler Stufe, lower Rotliegend"" (Romer & Price, 1940);\r\n"" [...] die Skelettreste [...] sind [...] eindeutig der D̦hlen-Formation zuzuordnen."" [""...the skeletal remains [...] are unequivocally assignable to the D̦hlen-Formation.""] (Reichel & Schauer, 2006 p. 20/21, ""Das D̦hlener Becken bei Dresden - Geologie und Bergbau"" [online] http://www.umwelt.sachsen.de/de/wu/umwelt/lfug/lfug-internet/veroeffentlichungen/verzeichnis/Boden/Bergbau%20in%20Sachsen/BBB12.Ansicht.neu.pdf);\r\nThe 1st seam of the D̦hlen-Formation comprises the uppermost part of the latter. This part of the D̦hlen-Formation is Asselian in age, according to ""Stratigraphische Tabelle von Deutschland 2002""","""Die _Gr_ne Schale ist ein bis 20 cm m_chtiger grauer, feinschichtiger bis bl_ttriger pelitischer Horizont mit lindgr_nen Schmitzen, vermutlich ein Tuffit."" [""The 'Gr_ne Schale' is an up to 20 cm thick, grey, laminated or foliated, pelitic horizon with pastel green clay fragments, presumably a tuffite""] (Reichel & Schauer, 2006 p. 20, ""Das D̦hlener Becken bei Dresden - Geologie und Bergbau"" [online] http://www.umwelt.sachsen.de/de/wu/umwelt/lfug/lfug-internet/veroeffentlichungen/verzeichnis/Boden/Bergbau%20in%20Sachsen/BBB12.Ansicht.neu.pdf)","""shale""",gray,lithified,,,,,,,,fine channel fill,intramontane basin,"""[...] stratiforme, relativ schmale rinnen_hnliche Zonen, in denen Klastite als Suspensionen _ber das Flachmoor transportiert wurden."" [...stratiform, relatively narrow, channel-like zones, in which clastites were transported as suspension across the swamp.""] (Reichel & Schauer, 2006 p. 21)",macrofossils,,,,,,NA,,"body,adpression",good,autochthonous,snapshot,,,,,,,NA,,"""Die _bereinander liegenden Skelette zeigen keinerlei Anzeichen von Disartikulation. [...] Es hat also keinerlei Transport stattgefunden, die Skelette wurden nicht zusammengeschwemmt. [""The skeletons lying upon another do not show any sign of disarticulation. [...] Hence, no transport took place, the skeletons were not washed together.""] (Reichel & Schauer, 2006 p. 21, ""Das D̦hlener Becken bei Dresden - Geologie und Bergbau"" [online] http://www.umwelt.sachsen.de/de/wu/umwelt/lfug/lfug-internet/veroeffentlichungen/verzeichnis/Boden/Bergbau%20in%20Sachsen/BBB12.Ansicht.neu.pdf)",taxonomic,,,,,,,1901,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Hylonomus,,NA,NA,vertebrate,"H. Credner. 1890. Die stegocephalen und Saurier aus dem Rothliegenden des Plauen'schen Grundes bei Dresden, IX Theil. Hylonomus geinitzi Cred. Petrobates truncatus Cred. Discosaurus Permianus Cred. Zeitschrift der Deutschen Geologischen Gesellschaft 42:240-277",327,697,0,R. Butler,E. Dunne,,21/03/2016 09:04,21/03/2016 09:04,5692,geinitzi,Saxonerpeton,58521,n. sp.,298.9,295.5,Asselian,,NA,DE,Saxonerpeton geinitzi
1318308,occ,NA,,84835,,n. gen. Ricnodon n. sp. copei,species,37288,species not entered,Ricnodon,NA,genus,37288,Carroll and Gaskill,1978,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Hapsidopareiontidae,37285,37288,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Ricnodon,n. gen.,NA,NA,vertebrate,R. L. Carroll and P. Gaskill. 1978. The Order Microsauria. Memoirs of the American Philosophical Society 126:1-211,327,697,0,R. Butler,E. Dunne,,21/03/2016 11:54,21/03/2016 11:54,28608,copei,Ricnodon,28692,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Ricnodon copei
1318309,occ,NA,,86946,,Ricnodon sp.,genus,37288,,Ricnodon,NA,genus,37288,Carroll and Gaskill,1978,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Hapsidopareiontidae,37285,37288,NA,NA,NA,,-64.451385,45.698612,"Joggins; Divison 4, Section XII, coal-group 26",NA,Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Division 4 ""of the section extends from McCairn's Cove to the end of the high cliff beyond 'Coal-mine Point'."" (Dawson, 1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173 p. 162); Lat long is approx. for Coal Mine Point",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XII",coal-group 26,,,,NA,"Coal-group 26 has a total thickness of 118 ft (including a 4 inch coaly shale). (Dawson, 1878 p. 170). Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","""Gray sandstone and shale, with erect Sigillaria; at four or five levels, and two Stigmarian underclays"" (Dawson, 1878 p. 170)",sandstone,gray,,,,claystone,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",,,snapshot,,,,,,,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" (Lyell, 1853, Quart. J. Geol. Soc. 9)",taxonomic,"field collection,survey of museum collection,observed (not collected)",,,,,"J. W. Dawson, P. W. McNaughton, among others",,,"Dawson (1878, Acadian Geology, 3rd ed.) reports Stigmaria sp. from this site","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Ricnodon,,NA,NA,vertebrate,R. L. Carroll and P. Gaskill. 1978. The Order Microsauria. Memoirs of the American Philosophical Society 126:1-211,327,697,0,R. Butler,E. Dunne,,21/03/2016 11:59,21/03/2016 11:59,28956,sp.,Ricnodon,28692,,318.1,314.6,Westphalian A,,NA,CA,Ricnodon sp.
1318310,occ,NA,,67945,,Euryodus n. sp. dalyae,species,227036,,Euryodus dalyae,NA,species,227036,Carroll and Gaskill,1978,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37296,NA,NA,NA,,-98.787781,34.18972,South Grandfield,NA,,US,Oklahoma,Tillman,stated in text,seconds,small collection,"""SW1/4 SE1/4 SE1/4 sec. 20, T. 4 S, R. 15 W. This is 6 1/2 miles southwest of Grandfield... 3 miles north of the Red River...""\neast side of ""a depression about fifty feet deep... near the top... [fossils] from the surface of a nose or ridge... three to four feet high and ten to twenty-five fee in area.""",gp_mid,-28.41,1.95,101,US,,Hennessey,,,bed,,,,,,,NA,"""lower third"" of a 9 foot bed\n""when the known lower boundary of the Arroyo [Formation] is extrapolated northward... it passes through the South Grandfield site.""\nthe Arroyo is within the Clear Fork Group, all of which is Kungurian (see discussion of Romer 1928 collections)","""Red shale spotted with pale green, containing lenses of fissile red sandstone and of stratified dark red fine conglomerate.""","""shale""","green,red",,,,sandstone,"""cross stratification"",red",poorly lithified,,,fluvial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""remains were assembled by moving water, after transport for a long or short distance... It is usual for the skull specimens... to have the mandibles in place... This suggests that the predators and scavengers... may have customarily discarded the heads... cranial remains have been selectively preserved...""\ncounts are given of 281 skulls and skull parts; 346 vertebrae, strings of vertebrae, and pieces of vertebrae; 109 limb bones and pieces of limb bones; and 29 partial girdles",general faunal/floral,"surface (float),field collection,survey of museum collection",FMNH,,,,,,"""Bone and bone-containing nodules may be collected from the surface... An effort to excavate for fossils was not productive... about forty pounds of red shale... was washed [and] five scraps of bone were recovered, none identifiable.""\r\n\r\nUCLA VP = Vertebrate paleontology collections of the University of California, Los Angeles",not the same as the two West Grandfield sites of Olson 1967,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Euryodus,,NA,NA,vertebrate,R. L. Carroll and P. Gaskill. 1978. The Order Microsauria. Memoirs of the American Philosophical Society 126:1-211,327,697,0,R. Butler,E. Dunne,,21/03/2016 12:06,21/03/2016 12:06,19411,dalyae,Euryodus,28692,n. sp.,279.3,272.3,Kungurian,,NA,US,Euryodus dalyae
1318311,occ,NA,,177144,members,Euryodus n. sp. bonneri,species,320817,,Euryodus bonneri,NA,species,320817,Schultze and Foreman,1981,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37296,NA,NA,NA,,-96.14563,38.870136,1.5 miles NW of Eskridge,NA,Roadcut on Kansas State Highway 99,US,Kansas,Wabaunsee,estimated from map,6,small collection,Coordinates based on part of Highway 99 lying 1.5 miles northwest of Eskridge,gp_mid,-25.81,1.84,101,US,,Speiser Shale,,,bed,,,,,,,NA,,Tan mud shale.,"""shale""",brown,lithified,muddy,,,,,,,marine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Euryodus,,NA,NA,vertebrate,H. P. Schultze and B. Foreman. 1981. A new gymnarthrid microsaur from the Lower Permian of Kansas with a review of the tuditanomorph microsaurs (Amphibia). Occ. Pap. Mus. Nat. Hist. Univ. Kan 91:1-25,327,697,697,R. Butler,E. Dunne,E. Dunne,21/03/2016 12:28,21/03/2016 12:29,NA,bonneri,Euryodus,58524,n. sp.,295.5,290.1,Sakmarian,,NA,US,Euryodus bonneri
1318312,occ,NA,,84835,,n. gen. Sparodus n. sp. validus,species,338124,,Sparodus validus,NA,species,338124,Fritsch,1876,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37300,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Sparodus,n. gen.,NA,NA,vertebrate,A. Fritsch. 1876. ber die Fauna der Gaskohle des Pilsner und Rakonitzer Beckens. Sitzungs-Berichte der koniglichen bohmischen Gellschaft der Wissenschaften Prag 1875:70-78,327,697,0,R. Butler,E. Dunne,,21/03/2016 12:39,21/03/2016 12:39,28608,validus,Sparodus,58031,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Sparodus validus
1318313,occ,NA,,28256,,n. gen. Quasicaecilia n. sp. texana,species,227373,,Quasicaecilia texana,NA,species,227373,Carroll,1990,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Brachystelechidae,37314,227371,NA,NA,NA,,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Quasicaecilia,n. gen.,NA,NA,vertebrate,R. L. Carroll. 1990. A tiny microsaur from the lower Permian of Texas: size constraints in Palaeozoic tetrapods. Palaeontology 33:893-909,327,697,0,R. Butler,E. Dunne,,21/03/2016 13:43,21/03/2016 13:43,17702,texana,Quasicaecilia,58525,n. sp.,279.3,272.3,Kungurian,,NA,US,Quasicaecilia texana
1318314,occ,NA,,85292,,n. gen. Odonterpeton n. sp. triangulare,species,227046,,Odonterpeton triangulare,NA,species,227046,Moodie,1909,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Odonterpetontidae,37317,37318,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Odonterpeton,n. gen.,NA,NA,vertebrate,R. L. Moodie. 1909. Carboniferous air-breathing vertebrates of the United States National Museum. Proceedings of the United States National Museum 37:11-28,327,697,0,R. Butler,E. Dunne,,21/03/2016 13:50,21/03/2016 13:50,28831,triangulare,Odonterpeton,58526,n. sp.,311.45,306.95,Westphalian D,,NA,US,Odonterpeton triangulare
1318361,occ,NA,,85292,,n. gen. Sauropleura n. sp. pectinata,species,230692,,Sauropleura pectinata,NA,species,230692,Cope,1868,Chordata,33815,Osteichthyes,34881,,NA,Urocordylidae,37270,37275,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Sauropleura,n. gen.,NA,NA,vertebrate,E. D. Cope. 1868. Synopsis of the Extinct Batrachia of North America. Proceedings of the Academy of Natural Sciences of Philadelphia 1868:208-221,327,697,0,R. Butler,E. Dunne,,22/03/2016 05:18,22/03/2016 05:18,28831,pectinata,Sauropleura,28717,n. sp.,311.45,306.95,Westphalian D,,NA,US,Sauropleura pectinata
1318368,occ,NA,,79162,,Sauropleura n. sp. bairdi,species,227053,,Sauropleura bairdi,NA,species,227053,Carroll et al.,1998,Chordata,33815,Osteichthyes,34881,,NA,Urocordylidae,37270,37275,NA,NA,NA,specimens,-98.650002,33.583332,Archer City Bonebed 1 (Putnam Fm.),NA,"Locality IIIf (Romer & Price, 1940)",US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Sauropleura,,NA,NA,vertebrate,"R. L. Carroll, K. A. Bossy, and A. C. Milner, S. M. Andrews, C. F. Wellstead. 1998. Handbuch der Palaoherpetologie / Encyclopedia of Paleoherpetology Teil 1 / Part 1 Lepospondyli: Microsauria, Nectridea, Lysorophia, Adelospondyli, Aistopoda, Acherontiscidae. ",327,697,697,R. Butler,E. Dunne,E. Dunne,22/03/2016 05:34,24/08/2016 05:22,43845,bairdi,Sauropleura,55379,n. sp.,296.4,268,Wolfcamp,,1,US,Sauropleura bairdi
1318378,occ,NA,,84835,,Urocordylus n. sp. scalaris,species,227056,recombined as,Sauropleura scalaris,NA,species,227056,Fritsch,1883,Chordata,33815,Osteichthyes,34881,,NA,Urocordylidae,37270,37275,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Urocordylus,,NA,NA,vertebrate,A. Fritsch. 1883. Fauna der Gaskohle und der Kalksteine der Permformation Bohmens. Band 1 (1879-1883). 1,327,697,0,R. Butler,E. Dunne,,22/03/2016 05:48,22/03/2016 05:48,28608,scalaris,Sauropleura,58542,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Sauropleura scalaris
1318379,occ,NA,,176090,members,Sauropleura n. sp. longidentata,species,192960,recombined as,Montcellia longidentata,NA,species,192960,Dutuit and Heyler,1994,Chordata,33815,Osteichthyes,34881,,NA,Urocordylidae,37270,320821,NA,NA,NA,,4.387342,46.696396,"Montceau-les-Mines, Saone et Loire",NA,"Blanzy, Sa̫ne-et-Loire",FR,Bourgogne,,based on nearby landmark,6,,"Coordinates based on Blanzy, a commune in the Sa̫ne-et-Loire department in the region of Bourgogne in eastern France",gp_mid,17.13,0.02,305,FR,,,,,bed,,,,,,,NA,Locatity situated in the Montceau Basin,,not reported,,,,,,,,,,terrestrial indet.,,"No further information available on stratigraphy aside from that presented in Carroll et al. (1998, Handbuch der Palaoherpetologie 1)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MNHN,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Sauropleura,,NA,NA,vertebrate,"J. M. Dutuit and D. Heyler. 1994. Rachitomes, L̩pospondyles et Reptiles due Stephanien (Carbonifere superieur) du basin de Montceau-les-Mines (Massif central, France). In: Quand le Massif Central etait sout l'equateur: un ecosysteme Carbonifere a Montceau-les-Mines. In C. Poplin, D. Heyler (eds.), Memoires de la section des Sciences 12:249-266",327,697,0,R. Butler,E. Dunne,,22/03/2016 06:37,22/03/2016 06:37,NA,longidentata,Montcellia,58544,n. sp.,304.8,301.2,Stephanian B,Stephanian C,NA,FR,Montcellia longidentata
1318380,occ,NA,,84835,,n. gen. Scincosaurus n. sp. crassus,species,230694,,Scincosaurus crassus,NA,species,230694,Fritsch,1876,Chordata,33815,Osteichthyes,34881,,NA,Scincosauridae,37267,37269,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Scincosaurus,n. gen.,NA,NA,vertebrate,A. Fritsch. 1876. ber die Fauna der Gaskohle des Pilsner und Rakonitzer Beckens. Sitzungs-Berichte der koniglichen bohmischen Gellschaft der Wissenschaften Prag 1875:70-78,327,697,0,R. Butler,E. Dunne,,22/03/2016 06:54,22/03/2016 06:54,28608,crassus,Scincosaurus,58031,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Scincosaurus crassus
1318484,occ,NA,,176090,members,Scincosaurus n. sp. spinosus,species,320828,,Scincosaurus spinosus,NA,species,320828,Civet,1982,Chordata,33815,Osteichthyes,34881,,NA,Scincosauridae,37267,37269,NA,NA,NA,,4.387342,46.696396,"Montceau-les-Mines, Saone et Loire",NA,"Blanzy, Sa̫ne-et-Loire",FR,Bourgogne,,based on nearby landmark,6,,"Coordinates based on Blanzy, a commune in the Sa̫ne-et-Loire department in the region of Bourgogne in eastern France",gp_mid,17.13,0.02,305,FR,,,,,bed,,,,,,,NA,Locatity situated in the Montceau Basin,,not reported,,,,,,,,,,terrestrial indet.,,"No further information available on stratigraphy aside from that presented in Carroll et al. (1998, Handbuch der Palaoherpetologie 1)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MNHN,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Scincosaurus,,NA,NA,vertebrate,"C. Civet. 1982. Etude d'un nouvel Amphibien Fosile du Basin Houiller de Montceau-les-Mines Scincosuarus spinosus nov. sp. ""La Physiophile"" Societe d'etudes des sciences Naturelles et Historigues de Montceau-les-Mines 96:73-79",327,697,0,R. Butler,E. Dunne,,22/03/2016 13:00,22/03/2016 13:00,NA,spinosus,Scincosaurus,58554,n. sp.,304.8,301.2,Stephanian B,Stephanian C,NA,FR,Scincosaurus spinosus
1318485,occ,NA,,177139,members,Urocordylidae indet.,family,37270,,Urocordylidae,NA,family,37270,Boyd,1982,Chordata,33815,Osteichthyes,34881,,NA,Urocordylidae,37270,NA,NA,NA,NA,individuals,-1.52138,55.105228,"Hannah Pit, Newsham",NA,Newsham Colliery,UK,England,Yorkshire,stated in text,6,small collection,"Coordinates are those of the Hannah pit as shown on the First Edition Ordnance Survey map of 1865. The pit was ""sunk in 1860 to the Low Main seam, recorded as a depth of 99 fathoms (181m)""",gp_mid,3.06,-6.8,315,UK,,Middle Coal Measures,,,,,,,,,,NA,"""The horizon lies within the Upper Modiolaris zone of the Middle Coal Measures (Land 1974) and is Westphalian B in age"" (Boyd, 1980)",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Urocordylidae,,NA,NA,vertebrate,M. J. Boyd. 1982. A urocordylid nectridean (Amphibia) from the Westphalian of Northumberland. Transactions of the Natural History Society of Northumbria 48:9-12,327,697,327,R. Butler,E. Dunne,R. Butler,22/03/2016 13:06,02/12/2016 08:57,NA,indet.,,58555,,323.2,315.2,Bashkirian,,1,UK, indet.
1318807,occ,NA,,176262,members,Keraterpeton n. sp. longtoni,species,320825,,Keraterpeton longtoni,NA,species,320825,Carroll et al.,1998,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37266,NA,NA,NA,,-2.138221,52.990681,"Longton, Staffordshire",NA,Longton Hall Colliery,UK,England,Staffordshire,based on nearby landmark,6,small collection,,gp_mid,3.02,-8.94,315,UK,,,Middle Coal Measures,,,,,,,,,NA,,,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Keraterpeton,,NA,NA,vertebrate,"R. L. Carroll, K. A. Bossy, and A. C. Milner, S. M. Andrews, C. F. Wellstead. 1998. Handbuch der Palaoherpetologie / Encyclopedia of Paleoherpetology Teil 1 / Part 1 Lepospondyli: Microsauria, Nectridea, Lysorophia, Adelospondyli, Aistopoda, Acherontiscidae. ",327,697,697,R. Butler,E. Dunne,E. Dunne,23/03/2016 07:50,23/03/2016 07:50,NA,longtoni,Keraterpeton,55379,n. sp.,323.2,315.2,Bashkirian,,NA,UK,Keraterpeton longtoni
1319239,occ,NA,,85292,,n. gen. Tuditanus n. sp. punctulatus,species,227062,,Tuditanus punctulatus,NA,species,227062,Cope,1875,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Tuditanidae,37280,37284,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Tuditanus,n. gen.,NA,NA,vertebrate,E. D. Cope. 1875. The extinct Batrachia of Ohio. Proceedings of the Academy of Natural Sciences of Philadelphia 16,327,697,697,R. Butler,E. Dunne,E. Dunne,24/03/2016 07:38,24/03/2016 07:56,28831,punctulatus,Tuditanus,58586,n. sp.,311.45,306.95,Westphalian D,,NA,US,Tuditanus punctulatus
1319240,occ,NA,,85292,,Tuditanus n. sp. radiatus,species,336710,recombined as,Erpetosaurus radiatus,NA,species,336710,Cope ,1874,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,36982,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Tuditanus,,NA,NA,vertebrate,"E. D. Cope . 1874. Supplement to the extinct Batrachia and Reptilia of North America. I. Catalogue of the air-breathing Vertebrata from the Coal-measures of Linton, Ohio. Transactions of the American Philosophical Society 15:261-278",327,697,0,R. Butler,E. Dunne,,24/03/2016 08:00,24/03/2016 08:00,28831,radiatus,Erpetosaurus,58130,n. sp.,311.45,306.95,Westphalian D,,NA,US,Erpetosaurus radiatus
1319421,occ,NA,,177359,members,Batropetes fritschia,species,137990,,Batropetes fritschia,NA,species,137988,Geinitz and Deichmuller,1882,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Brachystelechidae,37314,37513,NA,NA,NA,,13.670425,50.987778,Windberg near Niederhaslich,NA,,DE,Saxony,,based on nearby landmark,6,small collection,"""Windberg near Niederhaslich (part of Freital/Saxony), Dohlen Basin"" (Glienke, 2013)",gp_mid,23.31,7.72,305,DE,,,Rotliegend,,,,,,,,,NA,Saar Nahe Basin,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Batropetes,,NA,NA,vertebrate,H. B. Geinitz and J. V. Deichmuller. 1882. Die fossilen Saurier in dem Kalke des Rothliegenden von Niderhasslich im Plauen'schen Grunde bei Dresden. MIneral-geol. Praehist. Mus. Dresden P3,327,697,697,R. Butler,E. Dunne,E. Dunne,24/03/2016 12:03,24/08/2016 09:07,NA,fritschia,Batropetes,58589,,295.5,290.1,Sakmarian,,NA,DE,Batropetes fritschia
1322340,occ,NA,,22726,,Crassigyrinus scoticus,species,229317,,Crassigyrinus scoticus,NA,species,229317,Clack and Milner,2015,Chordata,33815,Osteichthyes,34881,,NA,Crassigyrinidae,339411,36967,NA,NA,NA,,-3.35,56.1166,Cowdenbeath Amphibian Bonebed,NA,ETE Locality 1605; Dora Opencast Coal Site,UK,,,,4,outcrop,"""south-east of Cowdenbeath... a section 30 m long""",gp_mid,0.18,-9.49,313,UK,,,Limestone Coal,,bed,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_min\r\n""lower Namurian A... 62 m beneath the base of the Index Limestone [which is]... at the junction between the top of the Pendleian (E1) and the base of the Arnsbergian (E2) stages"": originally entered as Namurian to Bashkirian","ETE rock type adj: ""rooty,muddy"", ETE lithology comments: 0\r\n""a localised patch in a seatrock (rooty, muddy siltstone)""",siltstone,,,,,,,,,,terrestrial indet.,,,,,,,,,NA,,,,,,,,,,,,NA,,,general faunal/floral,,,,7 specimens,,,1974 and 1975,"ETE Size: .; ETE reference list: 478, 479, 483, 482, 485, 454, 81, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Crassigyrinus,,NA,NA,,"J. A. Clack and A. R. Milner. 2015. Handbook of Paleoherpetology, Part 3A1: Basal Tetrapoda. ",327,697,0,R. Butler,E. Dunne,,12/04/2016 04:55,12/04/2016 04:55,5931,scoticus,Crassigyrinus,57666,,326.4,318.1,Pendleian,,NA,UK,Crassigyrinus scoticus
1326570,occ,NA,,84835,,n. gen. Stelliosaurus n. sp. longicostatus,species,227039,recombined as,Hyloplesion longicostatum,NA,species,227039,Fritsch,1875,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Hyloplesiontidae,37312,37313,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Stelliosaurus,n. gen.,NA,NA,vertebrate,A. Fritsch. 1875. Uber die Fauna der Gaskohle des Pilsner und Rakonitzer Beckens. Sitz. K. boehmischen Gesellsch. der Wiss. In Prag. Jahrgang ,327,697,0,R. Butler,E. Dunne,,25/04/2016 04:38,25/04/2016 04:38,28608,longicostatus,Hyloplesion,58983,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Hyloplesion longicostatus
1326571,occ,NA,,125662,,Stelliosaurus longicostatus,species,227039,recombined as,Hyloplesion longicostatum,NA,species,227039,Fritsch,1875,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Hyloplesiontidae,37312,37313,NA,NA,NA,,13.395,49.814999,Tremosna,NA,"Temon̩, Temon",CZ,,,based on nearby landmark,3,outcrop,,gp_mid,19.75,0.69,305,CZ,,Kladno,,Nyrany,,,,,,,,NA,Tremosna in B̦hmen. Mittleres Obercarbon.,,not reported,,,,,coal,,,,,terrestrial indet.,rift,"Central-West Bohemian basin; extensional basin developed within Variscan zone along simple asymmetric mega-graben formed on the Central Bohemian and Litomerice fault zones, with some contribution from transtensional wrench faults.",macrofossils,,,,,,NA,,mold/impression,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Stelliosaurus,,NA,NA,"paleoentomology,vertebrate",A. Fritsch. 1875. Uber die Fauna der Gaskohle des Pilsner und Rakonitzer Beckens. Sitz. K. boehmischen Gesellsch. der Wiss. In Prag. Jahrgang ,327,697,0,R. Butler,E. Dunne,,25/04/2016 04:39,25/04/2016 04:39,50906,longicostatus,Hyloplesion,58983,,311.45,306.95,Westphalian D,,NA,CZ,Hyloplesion longicostatus
1326572,occ,NA,,85292,,Colosteus n. sp. marshii,species,230691,recombined as,Ptyonius marshii,NA,species,230691,Cope,1869,Chordata,33815,Osteichthyes,34881,,NA,Urocordylidae,37270,37274,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Colosteus,,NA,NA,vertebrate,"E. D. Cope. 1869. Synopsis of the extinct Batrachia, Reptilia, and Aves of North America. Part 1. Transactions of the American Philosophical Society 14:1-252",327,697,0,R. Butler,E. Dunne,,25/04/2016 08:35,25/04/2016 08:35,28831,marshii,Ptyonius,58984,n. sp.,311.45,306.95,Westphalian D,,NA,US,Ptyonius marshii
1326573,occ,NA,,85292,,Sauropleura n. sp. remex,species,320823,recombined as,Ctenerpeton remex,NA,species,320823,Cope,1868,Chordata,33815,Osteichthyes,34881,,NA,Urocordylidae,37270,37272,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Sauropleura,,NA,NA,vertebrate,E. D. Cope. 1868. Synopsis of the Extinct Batrachia of North America. Proceedings of the Academy of Natural Sciences of Philadelphia 1868:208-221,327,697,0,R. Butler,E. Dunne,,25/04/2016 08:52,25/04/2016 08:52,28831,remex,Ctenerpeton,28717,n. sp.,311.45,306.95,Westphalian D,,NA,US,Ctenerpeton remex
1326580,occ,NA,,177139,members,Urocordylus reticulatus,species,227003,recombined as,Batrachiderpeton reticulatum,NA,species,227003,Hancock and Atthey,1869,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37262,NA,NA,NA,individuals,-1.52138,55.105228,"Hannah Pit, Newsham",NA,Newsham Colliery,UK,England,Yorkshire,stated in text,6,small collection,"Coordinates are those of the Hannah pit as shown on the First Edition Ordnance Survey map of 1865. The pit was ""sunk in 1860 to the Low Main seam, recorded as a depth of 99 fathoms (181m)""",gp_mid,3.06,-6.8,315,UK,,Middle Coal Measures,,,,,,,,,,NA,"""The horizon lies within the Upper Modiolaris zone of the Middle Coal Measures (Land 1974) and is Westphalian B in age"" (Boyd, 1980)",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Urocordylus,,NA,NA,vertebrate,"A. Hancock and T. Atthey. 1869. On a new labyrinthodont from the Northumberland coal field, and on the occurrence in the same locality of Anthracosaurus russelli. Annals and Magazine of Natural History 4(4):182-189",327,697,327,R. Butler,E. Dunne,R. Butler,26/04/2016 06:12,02/12/2016 08:57,NA,reticulatus,Batrachiderpeton,58986,,323.2,315.2,Bashkirian,,1,UK,Batrachiderpeton reticulatus
1326581,occ,NA,,85292,,Tuditanus n. sp. brevirostris,species,227033,recombined as,Diceratosaurus brevirostris,NA,species,227033,Cope,1875,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37263,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Tuditanus,,NA,NA,vertebrate,E. D. Cope. 1875. The extinct Batrachia of Ohio. Proceedings of the Academy of Natural Sciences of Philadelphia 16,327,697,0,R. Butler,E. Dunne,,26/04/2016 06:35,26/04/2016 06:35,28831,brevirostris,Diceratosaurus,58586,n. sp.,311.45,306.95,Westphalian D,,NA,US,Diceratosaurus brevirostris
1326582,occ,NA,,176092,members,Diceratosaurus brevirostris,species,340056,,Diceratosaurus brevirostris,NA,species,227033,Carroll et al.,1998,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37263,NA,NA,NA,,-80.612236,40.989132,Five Points Coal Mine,NA,,US,Ohio,Mahoning County,based on nearby landmark,6,outcrop,"""Five Points, south of Youngstown, Mahoning County, Ohio"" Sues et al. (2013) Atl Geol.",gp_mid,-18.98,-8.63,101,US,,,Allegheny,,,,,,,,,NA,,,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diceratosaurus,,NA,NA,vertebrate,"R. L. Carroll, K. A. Bossy, and A. C. Milner, S. M. Andrews, C. F. Wellstead. 1998. Handbuch der Palaoherpetologie / Encyclopedia of Paleoherpetology Teil 1 / Part 1 Lepospondyli: Microsauria, Nectridea, Lysorophia, Adelospondyli, Aistopoda, Acherontiscidae. ",327,697,0,R. Butler,E. Dunne,,26/04/2016 06:42,26/04/2016 06:42,NA,brevirostris,Diceratosaurus,55379,,313.8,305.9,Desmoinesian,,NA,US,Diceratosaurus brevirostris
1326946,occ,NA,,178269,members,Phlegethontia sp.,genus,37259,,Phlegethontia,NA,genus,37259,Germain,2008,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,37259,NA,NA,NA,,4.375,46.689999,"D̩couverte, Montceau-les-Mines",NA,,FR,,,estimated from map,2,outcrop,"Locality is an open coal pit of SaintLouis, basin of Montceau-les-Mines, Sa̫ne-et Loire, France.",gp_mid,16.8,-0.46,305,FR,,,,,,,,,,,,NA,,The Phlegethontia specimen was discovered in a phosphateous nodule of approximately 6 cm long.,not reported,,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,concretion,replaced with phosphate",good,,,,,,,,,NA,,The Phlegethontia specimen was too small and too poorly preserved to allow a mechanical or chemical preparation without damage.,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Phlegethontia,,NA,NA,vertebrate,"D. Germain. 2008. A new phlegethontiid specimen (Lepospondyli, Aistopoda) from the Late Carboniferous of Montceau-les-Mines (Sa̫ne-et-Loire, France). Geodiversitas 30(4):669-680",327,697,0,R. Butler,E. Dunne,,29/04/2016 08:27,29/04/2016 08:27,NA,sp.,Phlegethontia,59019,,304.8,303.4,Stephanian B,,NA,FR,Phlegethontia sp.
1326947,occ,NA,,178269,members,Phlegethontia sp.,genus,37259,,Phlegethontia,NA,genus,37259,Germain,2008,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,37259,NA,NA,NA,,4.375,46.689999,"D̩couverte, Montceau-les-Mines",NA,,FR,,,estimated from map,2,outcrop,"Locality is an open coal pit of SaintLouis, basin of Montceau-les-Mines, Sa̫ne-et Loire, France.",gp_mid,16.8,-0.46,305,FR,,,,,,,,,,,,NA,,The Phlegethontia specimen was discovered in a phosphateous nodule of approximately 6 cm long.,not reported,,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,concretion,replaced with phosphate",good,,,,,,,,,NA,,The Phlegethontia specimen was too small and too poorly preserved to allow a mechanical or chemical preparation without damage.,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Phlegethontia,,NA,NA,vertebrate,"D. Germain. 2008. A new phlegethontiid specimen (Lepospondyli, Aistopoda) from the Late Carboniferous of Montceau-les-Mines (Sa̫ne-et-Loire, France). Geodiversitas 30(4):669-680",327,697,0,R. Butler,E. Dunne,,29/04/2016 08:27,29/04/2016 08:27,NA,sp.,Phlegethontia,59019,,304.8,303.4,Stephanian B,,NA,FR,Phlegethontia sp.
1326948,occ,NA,,84835,,Oestocephalus amphiuminum,species,230699,,Oestocephalus amphiuminum,NA,species,230699,Anderson,2003,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Oestocephalidae,230698,230697,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Oestocephalus,,NA,NA,vertebrate,"J. S. Anderson. 2003. Cranial anatomy of Coloraderpeton brilli, postcranial anatomy of Oestocephalus amphiuminus, and reconsideration of Ophiderpetontidae (Tetrapoda: Lepospondyli: Aistopoda). Journal of Vertebrate Paleontology 23(3):532-543",327,697,0,R. Butler,E. Dunne,,29/04/2016 08:37,29/04/2016 08:37,28608,amphiuminum,Oestocephalus,41001,,311.45,306.95,Westphalian D,,NA,CZ,Oestocephalus amphiuminum
1326950,occ,NA,,178271,members,n. gen. Altenglanerpeton n. sp. schroederi,species,340225,,Altenglanerpeton schroederi,NA,species,340225,Glienke,2012,Chordata,33815,Osteichthyes,34881,Microsauria,37278,,NA,340224,NA,NA,NA,,7.230833,49.450832,Werschweiler near St. Wendel-Saar,NA,,DE,,,based on nearby landmark,seconds,small collection,"Coordinates based on town of Etschberg, Located in the Saar-Nahe Basin, SW Germany.",gp_mid,19.52,4.79,315,DE,,Altengan,Glan,,,,,,,,,NA,"Rotliegend, Carboniferous/Permian transititon",,"""carbonate""",,,,,,,,,,lacustrine indet.,,"""Microsaur specimen was found in the vicinity of Werschweiler near St. Wendel in a carbonate layer that is now regarded as part of the Altenglan Formation. According to Boy (1989) the strata of the Altenglan Formation formed in large lakes. The lacustrine units each reach a thickness of up to 10 m and are partially separated by more coarse-grained deltaic deposits. The lakes were predominantly eutrophic with intermittently aerated bottom layers (Stapf 1990). Boy (1976, 1987) noted that the precise\r\nhorizon from which the microsaur۪۪ was recovered is uncertain but, on the basis of the information provided by Schroder (1939), it probably belonged to the Hauptkalk Lake. This lake covered large areas of the SaarNahe Basin and was uniformly shallow with little sediment input (Boy 1989). "" Glienke (2012)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Altenglanerpeton,n. gen.,NA,NA,vertebrate,S. Glienke. 2012. A new microsaur۪۪ (Amphibia; Lepospondyli) from the Rotliegend of the SaarPalatinate region (Carboniferous/Permian transition; West Germany). Palaeontologische Zeitschrift 86:297-311,327,697,0,R. Butler,E. Dunne,,29/04/2016 09:03,29/04/2016 09:03,NA,schroederi,Altenglanerpeton,59020,n. sp.,298.9,295.5,Asselian,,NA,DE,Altenglanerpeton schroederi
1328158,occ,NA,,178666,members,Brachydectes elongatus,species,229311,,Brachydectes elongatus,NA,species,229311,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,Cocytinidae,320813,227167,NA,NA,NA,,-96.408699,39.40102,"South of State Lake, Westmoreland",NA,Blue Rapids Shale,US,Kansas,Pottawatomie,based on nearby landmark,6,small collection,"Coordinates based in the location of Wsetmoreland. Exact location given as: ""SE 1/4, sec 4, T7S, R9E, south of State Lake, Westmoreland, Pottawatomie County, Kansas"" (Wellstead, 1991)",gp_mid,-25.52,2.79,101,US,,Council Grove,,,bed,,,,,,,NA,"Blue Rapids Shale, just below the Funston Limesone",,"""shale""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,R. W. Coldiron and W. D. Coldiron,1974,Repository: University of Kansas (KU),,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Brachydectes,,NA,NA,vertebrate,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,697,R. Butler,E. Dunne,E. Dunne,10/05/2016 09:02,10/05/2016 09:18,NA,elongatus,Brachydectes,58492,,296.4,268,Wolfcamp,,NA,US,Brachydectes elongatus
1328160,occ,NA,,28275,,Brachydectes elongatus,species,229311,,Brachydectes elongatus,NA,species,229311,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,Cocytinidae,320813,227167,NA,NA,NA,,-99.195557,33.973057,"Beaver Creek, 42 (Arroyo Formation)",NA,"Locality 42 (Romer 1928), Beaver Creek Wilbarger County, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Wilbarger,based on nearby landmark,seconds,outcrop,"""The upper reaches of the stream have yielded a few remains."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Beaver Creek.",gp_mid,-28.81,1.94,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""above the Lueders limestone, and quite probably correspond to the beds to the south of Coffee Creek."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Brachydectes,,NA,NA,vertebrate,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,0,R. Butler,E. Dunne,,10/05/2016 09:07,10/05/2016 09:07,7693,elongatus,Brachydectes,58492,,279.3,272.3,Kungurian,,NA,US,Brachydectes elongatus
1328176,occ,NA,,178669,members,Brachydectes elongatus,species,229311,,Brachydectes elongatus,NA,species,229311,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,Cocytinidae,320813,227167,NA,NA,NA,,-99.260002,33.594166,"Seltin Locality, Soap Creek",NA,,US,Texas,Baylor,based on nearby landmark,seconds,small collection,"Coordinates are for Seymour. Exact location noted by Wellstead (1991): ""N 1/2, NW 1/4, Soap Creek, Baylor County, Texas, 7.5' quadrangle.""",gp_mid,-30.51,-1.03,101,US,,Vale,Clear Fork,,group of beds,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,Rochard Seltin,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Brachydectes,,NA,NA,vertebrate,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,0,R. Butler,E. Dunne,,10/05/2016 10:26,10/05/2016 10:26,NA,elongatus,Brachydectes,58492,,290.1,279.3,Artinskian,,NA,US,Brachydectes elongatus
1328184,occ,NA,,178674,members,Lysorophus dunkardensis,species,320833,,Lysorophus dunkardensis,NA,species,320833,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-80.70977,39.675247,"Newdale, Proctor District",NA,CM Locality 34,US,West Virginia,Wetzel,based on nearby landmark,6,small collection,"Coordinates based on Newdale. Location described by Wellstead (1991) as: ""north side of Newdale-West P.O. Road, Proctor District, Wetzel County, West Virginia, about 0.33km northeast of Newdale, West Virginia.",gp_mid,-14.49,-2.17,101,US,,Greene,Dunkard,,bed,,,,,,,NA,"Freshwater limestone bed approximately 15m below Windy Gap Coal, Greene formation, Dunkard Group"" (Wellstead, 1991)",,"""limestone""",,,,,,,,,,fluvial-lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,CM,,,,Burke party,1934-35,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,0,R. Butler,E. Dunne,,10/05/2016 11:00,10/05/2016 11:00,NA,dunkardensis,Lysorophus,58492,,296.4,268,Wolfcamp,,NA,US,Lysorophus dunkardensis
1328186,occ,NA,,178675,members,Lysorophus dunkardensis,species,320833,,Lysorophus dunkardensis,NA,species,320833,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-80.821877,39.710094,"Silver Hill Road, Proctor District",NA,CM Locality 35,US,West Virginia,Wetzel,based on nearby landmark,6,small collection,"Coordinates based on Proctor, WV. Location described by Wellstead (1991) as: ""south side of West P.O. - Silver Hill Road, about 1km east of West P.O., Proctor District, Wetzel County, West Virginia.",gp_mid,-14.55,-2.1,101,US,,Greene,Dunkard,,bed,,,,,,,NA,,"""A 60cm thick brown, sandy shale apparently underlying the Windy Gap Coal horizon by approximately 1m""","""shale""",,,sandy,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,CM,,,,Burke party,1934-37,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,0,R. Butler,E. Dunne,,10/05/2016 12:00,10/05/2016 12:00,NA,dunkardensis,Lysorophus,58492,,296.4,268,Wolfcamp,,NA,US,Lysorophus dunkardensis
1328187,occ,NA,,178676,members,Lysorophus dunkardensis,species,320833,,Lysorophus dunkardensis,NA,species,320833,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-80.986664,39.768333,Adams Township,NA,CM Locality 6,US,Ohio,Monroe,based on nearby landmark,seconds,small collection,"Coordinates based on Adams Township. Detailed location given by Wellstead (1991): ""an outcrop in SW 1/4 sec 18, T3N, R2W, Adams Township, Monroe County, Ohio.""",gp_mid,-14.65,-2,101,US,,Washington,Dunkard,,bed,,,,,,,NA,,"""Interbedded limestone and shale at a horizon equivilent to the Mount Morris Limestone of West Virginia and Pennsylvania, approximately 2.3cm beneath the Waynesburg ""A"" Coal, Washington formation, Dunkard Group."" (Wellstead, 1991)","""limestone""",,,,,"""shale""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,CM,,,,Burke party,1937,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,0,R. Butler,E. Dunne,,10/05/2016 12:14,10/05/2016 12:14,NA,dunkardensis,Lysorophus,58492,,296.4,268,Wolfcamp,,NA,US,Lysorophus dunkardensis
1328188,occ,NA,,126535,,Lysorophus dunkardensis,species,320833,,Lysorophus dunkardensis,NA,species,320833,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-79.966667,40.444443,Soho Street Quarry,NA,Locality 1 of Moran (1952),US,Pennsylvania,Allegheny,estimated from map,seconds,,"Location details given by Wellstead (1991): ""a quarry on east side of Soho Street, approximately 0.25km north of Fifth Avenue, Pittsburgh, Allegheny County Pennsylvania. The site is now covered by a housing development.""",gp_mid,-15.23,-4.42,101,US,,,Conemaugh,,bed,,,,,,,NA,"""Freshwater limestone bed within the Pittsburgh Limestone, lying 12m below the base of the Conemaugh Group, Upper Pennsylvanian (=Stephanian)"" (Wellstead, 1991)",,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,"CM,MCZ",,,,Burke party,1936,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,0,R. Butler,E. Dunne,,10/05/2016 12:21,10/05/2016 12:21,41027,dunkardensis,Lysorophus,58492,,306.95,298.9,Stephanian,,NA,US,Lysorophus dunkardensis
1328189,occ,NA,,178677,members,Lysorophus dunkardensis,species,320833,,Lysorophus dunkardensis,NA,species,320833,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-80.974373,39.578487,"Owl Run, north of Sistersville",NA,CM Locality 3 / Locality 3 of Moran (1952),US,West Virginia,Tyler,based on nearby landmark,6,small collection,"Location description by Wellstead (1991): ""an outcrop just north of Owl Run, approximately 1km northeast of Sistersville, Lincoln District, Tyler County, West Virginia, on the west side of the West Virginia Route 2 to Paden City, West Virginia.""",gp_mid,-16.26,-4.96,101,US,,Uniontown Limestone,Monongahela,,,,,,,,,NA,,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,CM,,,,Burke party,1937,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,0,R. Butler,E. Dunne,,10/05/2016 13:14,10/05/2016 13:14,NA,dunkardensis,Lysorophus,58492,,306.95,298.9,Stephanian,,NA,US,Lysorophus dunkardensis
1328229,occ,NA,,127038,,Lysorophus sp.,genus,37322,,Lysorophus,NA,genus,37322,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-81.376114,39.064999,Limestone Hill,NA,,US,Maryland,,estimated from map,seconds,,,gp_mid,-15.4,-3,101,US,,Greene,Dunkard,,,,,,,,,NA,"""In the early 1930s, R. W. Whipple of Marietta College (Ohio) collected two series of lepospondylous vertebrae from the Ninevah Limestone (Greene Formation, Dunkard Group, Permian) at Limestone Hill, WV.""",,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,many,vertebrae,,,NA,"""One specimen consists of an articulated series of approximately 17 dorsal and six caudal vertebrae. The dorsal centra are large for a lepospondyl (1.6 cm long). The caudal centra, seemingly from tail's end, are smaller, approximately 0.5 cm long. The second specimen consists of two articulated, but fragmentary, caudal vertebrae whose centra are about 1.5 cm long.""",body,,,,,,,,,,NA,,,general faunal/floral,survey of museum collection,,,2 specimens,,R. W. Whipple,Early 1930s,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,0,R. Butler,E. Dunne,,11/05/2016 05:34,11/05/2016 05:34,41252,sp.,Lysorophus,58492,,295.5,290.1,Sakmarian,,NA,US,Lysorophus sp.
1328230,occ,NA,,178681,members,Lysorophus sp.,genus,37322,,Lysorophus,NA,genus,37322,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-80.193886,40.165279,Washington Stone Company quarry,NA,,US,Pennsylvania,Washington,based on nearby landmark,seconds,small collection,"Coordinates based on Vance, Washington County, Pennsylvania. Details given by Wellstead (1991): ""Washington Stone Company quarry, Vance, Pennsylvania, just north of the intersection of interstate highways 70 and 79, east of Washington, Washington County, Pennsylvania (Washington East, pennsylvania, 7.5' quadrangle, 1953).",gp_mid,-13.94,-1.84,101,US,,Washington,Dunkard,,,,,,,,,NA,Upper Washington Limestone,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,0,R. Butler,E. Dunne,,11/05/2016 05:44,11/05/2016 05:44,NA,sp.,Lysorophus,58492,,296.4,268,Wolfcamp,,NA,US,Lysorophus sp.
1328231,occ,NA,,81114,,Lysorophus sp.,genus,37322,,Lysorophus,NA,genus,37322,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-88.158333,38.991669,Falmouth Locality,NA,Newton Locality; type beds of Milosaurus mccordi,US,Illinois,Jasper,based on nearby landmark,seconds,outcrop,"SW 1/4 sec 15, T. 7N, R 10E; Lat Long is for Newton",gp_mid,-21.61,-3.29,101,US,,Mattoon,McLeansboro,,group of beds,,,,,,,NA,"""Stratigraphically, the beds are not more than 20 feet above the Reisner Limestone""\r\nIn the paper the McLeansboro Group is referred to as ""McCleansboro Group"".","""Most of the tetrapod remains are preserved in about two feet of cross-bedded siltstones, sandstones and shales which lie above a fresh water limestone, ranging in thickness from six inches to two feet or more, containing abundant remains of xenacanth sharks and lungfish. [...] the top six inches to one foot of the limestone was seen to grade into the clastic zone mentioned above.""","""mixed carbonate-siliciclastic""","""cross stratification""",,"silty,sandy",Y,,,,,,lacustrine deltaic indet.,,"""It appears [...] that the tetrapod remains are preserved in pond margin deposits of deltaic origin.""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"""The specimens are generally disarticulated (except for the holotype of M. mccordi) and appear to have been washed into the deposits.""",taxonomic,survey of museum collection,FMNH,,,,,,,"The referred specimens ""were found close to the holotype and no other large pelycosaur has been recovered from the deposit so it is concluded that these specimens are from the same species, and perhaps from the same individual as the holotype.""","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,697,R. Butler,E. Dunne,E. Dunne,11/05/2016 05:53,10/08/2016 09:23,28640,sp.,Lysorophus,58492,,306.95,298.9,Stephanian,Virgilian,NA,US,Lysorophus sp.
1328232,occ,NA,,178682,members,Molgophis macrurus,species,320834,,Molgophis macrurus,NA,species,320834,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37324,NA,NA,NA,,-81.52066,39.754532,West Fork of Duck Creek,NA,Locality P-c-4a,US,Ohio,Noble,based on nearby landmark,6,small collection,"Detailed location according to Wellstead (1991): ""Central section 30, T8N, R91, Noble Township, Noble County, Ohio (Caldwell North, Ohio, 7.5' quadrangle, 1961)",gp_mid,-19.4,-8.6,101,US,,,Conemaugh,,,,,,,,,NA,Freshwater Ewing limestone,,"""limestone""",,,,,,,,,,fluvial-lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,D. & L. Baird,1955,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Molgophis,,NA,NA,vertebrate,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,0,R. Butler,E. Dunne,,11/05/2016 06:41,11/05/2016 06:41,NA,macrurus,Molgophis,58492,,311.45,306.95,Westphalian D,,NA,US,Molgophis macrurus
1328266,occ,NA,,178696,members,Molgophis macrurus,species,320834,,Molgophis macrurus,NA,species,320834,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37324,NA,NA,NA,,-80.807915,40.36721,Jefferson County Route 36 viaduct,NA,"Locality P-c-5, west of Skelly Station/Broadacre/Fairplay",US,Ohio,Jefferson,,6,,"Location details given by Wellstead (1991): ""under Jefferson County Route 36 viaduct on a long, abandoned railway cut about 1.6km west of Skelly Station (also called Broadacre or Fairplay), Wayne Township, Jefferson County, Ohio; also SW 1/4, SE 1/4, SE 1/4, sec 24, Wayne Township, Ohio.""",gp_mid,-18.65,-8.24,101,US,,,Conemaugh,,bed,,,,,,,NA,Freshwater Ewing Limestone,,"""limestone""",,,,,,,,,,fluvial-lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,D. & L. Baird,1955,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Molgophis,,NA,NA,vertebrate,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,0,R. Butler,E. Dunne,,12/05/2016 05:17,12/05/2016 05:17,NA,macrurus,Molgophis,58492,,311.45,306.95,Westphalian D,,NA,US,Molgophis macrurus
1328267,occ,NA,,178697,members,Molgophis macrurus,species,320834,,Molgophis macrurus,NA,species,320834,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37324,NA,NA,NA,,-81.499886,39.854607,Locality P-c-4b,NA,US Route 21 junction with Noble County Route 37,US,Ohio,Noble,based on nearby landmark,6,small collection,"Detailed location given by Wellstead (1991): ""cut on east side of US Route 21, just north of junction with Noble County Route 37. SE 1/4, NW 1/4, sec 7, T7N, R9W, Noble Township, Noble County, Ohio (Caldwell North, Ohio, 7.5' quadrangle, 1961).""",gp_mid,-19.35,-8.51,101,US,,,Conemaugh,,bed,,,,,,,NA,,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,L. & D. Baird,1955,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Molgophis,,NA,NA,vertebrate,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,0,R. Butler,E. Dunne,,12/05/2016 05:27,12/05/2016 05:27,NA,macrurus,Molgophis,58492,,311.45,306.95,Westphalian D,,NA,US,Molgophis macrurus
1328269,occ,NA,,178698,members,Molgophis macrurus,species,320834,,Molgophis macrurus,NA,species,320834,Wellstead,1991,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37324,NA,NA,NA,,-81.047119,40.37957,Condit's Jewett bonebed,NA,,US,Ohio,Harrison,based on nearby landmark,6,small collection,"Details of locality given by Wellstead (1991): ""Conduit's Jewett bonebed; first cut on north side of railroad tracks, west of grade crossing of Ohio Route 151, about 1.3km west of town limits of Jewett, Ohio. SE 1/4, NW1/4 sec 7, T7N, R9W, Rumley township, Harrison County, Ohio (Jewett, Ohio - Harrison County, 7.5' quadrangle, 1961)"".",gp_mid,-18.82,-8.16,101,US,,,Conemaugh,,,,,,,,,NA,Freshwater Ewing Limestone,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,L. & D. Baird,1955,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Molgophis,,NA,NA,vertebrate,"C. F. Wellstead. 1991. Taxonomic revision of the Lysorophia, Permo-Carboniferous lepospondyl amphibians. Bulletin of the American Museum of Natural History 209:1-90",327,697,0,R. Butler,E. Dunne,,12/05/2016 05:48,12/05/2016 05:48,NA,macrurus,Molgophis,58492,,311.45,306.95,Westphalian D,,NA,US,Molgophis macrurus
1328459,occ,NA,,178735,members,Batropetes n. sp. appelensis,species,340815,,Batropetes appelensis,NA,species,340815,Glienke,2015,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Brachystelechidae,37314,37513,NA,NA,NA,,7.778986,49.802879,Niederhausen/Appel,NA,,DE,Rhineland-Palatinate,Bad Kreuznach,based on nearby landmark,6,small collection,"""Niederhausen/Appel, Saar-Nahe Basin"" (Glienke, 2015). Coordinates based on the location of Niederhausen.",gp_mid,19.79,5.22,315,DE,,Meisenheim,Rotliegend,,bed,,,,,,,NA,"Saar-Nahe Basin, Kappeln Bank, Meisenheim Formation (M9)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Repository: MNHM (Museum National d۪Histoire Naturelle, Paris, France)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Batropetes,,NA,NA,vertebrate,"S. Glienke. 2015. Two new species of the genus Batropetes (Tetrapoda, Lepospondyli) from the Central European Rotliegend (basal Permian) in Germany. Journal of Vertebrate Paleontology 35(2):1-27",327,697,697,R. Butler,E. Dunne,E. Dunne,13/05/2016 06:14,13/05/2016 06:16,NA,appelensis,Batropetes,59143,n. sp.,298.9,295.5,Asselian,,NA,DE,Batropetes appelensis
1328460,occ,NA,,178735,members,Batropetes n. sp. palatinus,species,340814,,Batropetes palatinus,NA,species,340814,Glienke,2015,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Brachystelechidae,37314,37513,NA,NA,NA,,7.778986,49.802879,Niederhausen/Appel,NA,,DE,Rhineland-Palatinate,Bad Kreuznach,based on nearby landmark,6,small collection,"""Niederhausen/Appel, Saar-Nahe Basin"" (Glienke, 2015). Coordinates based on the location of Niederhausen.",gp_mid,19.79,5.22,315,DE,,Meisenheim,Rotliegend,,bed,,,,,,,NA,"Saar-Nahe Basin, Kappeln Bank, Meisenheim Formation (M9)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Repository: MNHM (Museum National d۪Histoire Naturelle, Paris, France)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Batropetes,,NA,NA,vertebrate,"S. Glienke. 2015. Two new species of the genus Batropetes (Tetrapoda, Lepospondyli) from the Central European Rotliegend (basal Permian) in Germany. Journal of Vertebrate Paleontology 35(2):1-27",327,697,0,R. Butler,E. Dunne,,13/05/2016 06:16,13/05/2016 06:16,NA,palatinus,Batropetes,59143,n. sp.,298.9,295.5,Asselian,,NA,DE,Batropetes palatinus
1328461,occ,NA,,178736,members,Batropetes palatinus,species,340814,,Batropetes palatinus,NA,species,340814,Glienke,2015,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Brachystelechidae,37314,37513,NA,NA,NA,,7.602687,49.711227,"Jeckenbach, near Meisenheim",NA,,DE,Rhineland-Palatine,Bad Kreuznach,based on nearby landmark,6,small collection,"""Jeckenbach, Saar-Nahe Basin"" (Glienke, 2015). Coordinates based on the location of Jeckenbach.",gp_mid,19.7,5.1,315,DE,,Meisenheim,Rotliegend,,bed,,,,,,,NA,"Jecken- bach Bank (M6), Rotliegend",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Repository: MNHM (Museum National d۪Histoire Naturelle, Paris, France)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Batropetes,,NA,NA,vertebrate,"S. Glienke. 2015. Two new species of the genus Batropetes (Tetrapoda, Lepospondyli) from the Central European Rotliegend (basal Permian) in Germany. Journal of Vertebrate Paleontology 35(2):1-27",327,697,0,R. Butler,E. Dunne,,13/05/2016 06:20,13/05/2016 06:20,NA,palatinus,Batropetes,59143,,298.9,295,Autunian,,NA,DE,Batropetes palatinus
1328465,occ,NA,,67735,,Lysorophus tricarinatus,species,70395,,Lysorophus tricarinatus,NA,species,70395,Olson and Mead,1982,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-99.75,32.130001,Taylor County Site 7,NA,B.E.G. 30996; W.P.A. quarry; Sid McAdams Locality,US,Texas,Taylor,based on nearby landmark,2,small collection,"""souther part of Taylor County, Texas, in the SW 1/4 of section 436 of the M. P. King survey, on the property of Mr. C.O. Patterson, Route 1, Lawn, Texas... 6 miles southwest of the small town of Lawn"" (coordinate based on Lawn).\r\nAccording to Olson & Mead (1982) this locality contains a number of different sub-localities (""sites""), which here at treated as one locality.",gp_mid,-30.15,0.6,101,US,,Vale,,,group of beds,,,,,,,NA,"""22 feet above the Vale-Standpipe contact""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""siliceous clays""",claystone,,,sandy,,,,,,,delta plain,,"""low delta or floodplain... very still water""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"selective quarrying,field collection",,species names,,,,,University of Texas,"Locality number TMM 30966 preceeds specimens found at this location (Olson & Mead, 1982)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:28,13/05/2016 08:28,19359,tricarinatus,Lysorophus,59144,,279.3,272.3,Kungurian,,NA,US,Lysorophus tricarinatus
1328466,occ,NA,,67735,,Diplocaulus magnicornis,species,81712,,Diplocaulus magnicornis,NA,species,81712,Olson and Mead,1982,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.75,32.130001,Taylor County Site 7,NA,B.E.G. 30996; W.P.A. quarry; Sid McAdams Locality,US,Texas,Taylor,based on nearby landmark,2,small collection,"""souther part of Taylor County, Texas, in the SW 1/4 of section 436 of the M. P. King survey, on the property of Mr. C.O. Patterson, Route 1, Lawn, Texas... 6 miles southwest of the small town of Lawn"" (coordinate based on Lawn).\r\nAccording to Olson & Mead (1982) this locality contains a number of different sub-localities (""sites""), which here at treated as one locality.",gp_mid,-30.15,0.6,101,US,,Vale,,,group of beds,,,,,,,NA,"""22 feet above the Vale-Standpipe contact""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""siliceous clays""",claystone,,,sandy,,,,,,,delta plain,,"""low delta or floodplain... very still water""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"selective quarrying,field collection",,species names,,,,,University of Texas,"Locality number TMM 30966 preceeds specimens found at this location (Olson & Mead, 1982)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:28,13/05/2016 08:28,19359,magnicornis,Diplocaulus,59144,,279.3,272.3,Kungurian,,NA,US,Diplocaulus magnicornis
1328467,occ,NA,,67735,,Peronedon primus,species,119362,recombined as,Diplocaulus primus,NA,species,119362,Olson and Mead,1982,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.75,32.130001,Taylor County Site 7,NA,B.E.G. 30996; W.P.A. quarry; Sid McAdams Locality,US,Texas,Taylor,based on nearby landmark,2,small collection,"""souther part of Taylor County, Texas, in the SW 1/4 of section 436 of the M. P. King survey, on the property of Mr. C.O. Patterson, Route 1, Lawn, Texas... 6 miles southwest of the small town of Lawn"" (coordinate based on Lawn).\r\nAccording to Olson & Mead (1982) this locality contains a number of different sub-localities (""sites""), which here at treated as one locality.",gp_mid,-30.15,0.6,101,US,,Vale,,,group of beds,,,,,,,NA,"""22 feet above the Vale-Standpipe contact""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""siliceous clays""",claystone,,,sandy,,,,,,,delta plain,,"""low delta or floodplain... very still water""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"selective quarrying,field collection",,species names,,,,,University of Texas,"Locality number TMM 30966 preceeds specimens found at this location (Olson & Mead, 1982)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Peronedon,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:28,13/05/2016 08:28,19359,primus,Diplocaulus,59144,,279.3,272.3,Kungurian,,NA,US,Diplocaulus primus
1328468,occ,NA,,67735,,Eryops megacephalus,species,70397,,Eryops megacephalus,NA,species,70397,Olson and Mead,1982,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-99.75,32.130001,Taylor County Site 7,NA,B.E.G. 30996; W.P.A. quarry; Sid McAdams Locality,US,Texas,Taylor,based on nearby landmark,2,small collection,"""souther part of Taylor County, Texas, in the SW 1/4 of section 436 of the M. P. King survey, on the property of Mr. C.O. Patterson, Route 1, Lawn, Texas... 6 miles southwest of the small town of Lawn"" (coordinate based on Lawn).\r\nAccording to Olson & Mead (1982) this locality contains a number of different sub-localities (""sites""), which here at treated as one locality.",gp_mid,-30.15,0.6,101,US,,Vale,,,group of beds,,,,,,,NA,"""22 feet above the Vale-Standpipe contact""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""siliceous clays""",claystone,,,sandy,,,,,,,delta plain,,"""low delta or floodplain... very still water""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"selective quarrying,field collection",,species names,,,,,University of Texas,"Locality number TMM 30966 preceeds specimens found at this location (Olson & Mead, 1982)","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:28,13/05/2016 08:28,19359,megacephalus,Eryops,59144,,279.3,272.3,Kungurian,,NA,US,Eryops megacephalus
1328469,occ,NA,,67735,,Trimerorhachis insignis,species,90711,,Trimerorhachis insignis,NA,species,90711,Olson and Mead,1982,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-99.75,32.130001,Taylor County Site 7,NA,B.E.G. 30996; W.P.A. quarry; Sid McAdams Locality,US,Texas,Taylor,based on nearby landmark,2,small collection,"""souther part of Taylor County, Texas, in the SW 1/4 of section 436 of the M. P. King survey, on the property of Mr. C.O. Patterson, Route 1, Lawn, Texas... 6 miles southwest of the small town of Lawn"" (coordinate based on Lawn).\r\nAccording to Olson & Mead (1982) this locality contains a number of different sub-localities (""sites""), which here at treated as one locality.",gp_mid,-30.15,0.6,101,US,,Vale,,,group of beds,,,,,,,NA,"""22 feet above the Vale-Standpipe contact""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""siliceous clays""",claystone,,,sandy,,,,,,,delta plain,,"""low delta or floodplain... very still water""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"selective quarrying,field collection",,species names,,,,,University of Texas,"Locality number TMM 30966 preceeds specimens found at this location (Olson & Mead, 1982)","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:28,13/05/2016 08:28,19359,insignis,Trimerorhachis,59144,,279.3,272.3,Kungurian,,NA,US,Trimerorhachis insignis
1328470,occ,NA,,67735,,Waggoneria knoxensis,species,120859,,Waggoneria knoxensis,NA,species,120859,Olson and Mead,1982,Chordata,33815,Osteichthyes,34881,,NA,Waggoneriidae,120858,120857,NA,NA,NA,,-99.75,32.130001,Taylor County Site 7,NA,B.E.G. 30996; W.P.A. quarry; Sid McAdams Locality,US,Texas,Taylor,based on nearby landmark,2,small collection,"""souther part of Taylor County, Texas, in the SW 1/4 of section 436 of the M. P. King survey, on the property of Mr. C.O. Patterson, Route 1, Lawn, Texas... 6 miles southwest of the small town of Lawn"" (coordinate based on Lawn).\r\nAccording to Olson & Mead (1982) this locality contains a number of different sub-localities (""sites""), which here at treated as one locality.",gp_mid,-30.15,0.6,101,US,,Vale,,,group of beds,,,,,,,NA,"""22 feet above the Vale-Standpipe contact""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""siliceous clays""",claystone,,,sandy,,,,,,,delta plain,,"""low delta or floodplain... very still water""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"selective quarrying,field collection",,species names,,,,,University of Texas,"Locality number TMM 30966 preceeds specimens found at this location (Olson & Mead, 1982)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Waggoneria,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,697,R. Butler,E. Dunne,E. Dunne,13/05/2016 08:28,19/08/2016 10:21,19359,knoxensis,Waggoneria,59144,,279.3,272.3,Kungurian,,NA,US,Waggoneria knoxensis
1328471,occ,NA,,67735,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Olson and Mead,1982,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-99.75,32.130001,Taylor County Site 7,NA,B.E.G. 30996; W.P.A. quarry; Sid McAdams Locality,US,Texas,Taylor,based on nearby landmark,2,small collection,"""souther part of Taylor County, Texas, in the SW 1/4 of section 436 of the M. P. King survey, on the property of Mr. C.O. Patterson, Route 1, Lawn, Texas... 6 miles southwest of the small town of Lawn"" (coordinate based on Lawn).\r\nAccording to Olson & Mead (1982) this locality contains a number of different sub-localities (""sites""), which here at treated as one locality.",gp_mid,-30.15,0.6,101,US,,Vale,,,group of beds,,,,,,,NA,"""22 feet above the Vale-Standpipe contact""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""siliceous clays""",claystone,,,sandy,,,,,,,delta plain,,"""low delta or floodplain... very still water""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"selective quarrying,field collection",,species names,,,,,University of Texas,"Locality number TMM 30966 preceeds specimens found at this location (Olson & Mead, 1982)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:29,13/05/2016 08:29,19359,sp.,Diadectes,59144,,279.3,272.3,Kungurian,,NA,US,Diadectes sp.
1328472,occ,NA,,67735,,Seymouria baylorensis,species,137488,,Seymouria baylorensis,NA,species,137488,Olson and Mead,1982,Chordata,33815,Osteichthyes,34881,,NA,Seymouriidae,37219,37223,NA,NA,NA,,-99.75,32.130001,Taylor County Site 7,NA,B.E.G. 30996; W.P.A. quarry; Sid McAdams Locality,US,Texas,Taylor,based on nearby landmark,2,small collection,"""souther part of Taylor County, Texas, in the SW 1/4 of section 436 of the M. P. King survey, on the property of Mr. C.O. Patterson, Route 1, Lawn, Texas... 6 miles southwest of the small town of Lawn"" (coordinate based on Lawn).\r\nAccording to Olson & Mead (1982) this locality contains a number of different sub-localities (""sites""), which here at treated as one locality.",gp_mid,-30.15,0.6,101,US,,Vale,,,group of beds,,,,,,,NA,"""22 feet above the Vale-Standpipe contact""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""siliceous clays""",claystone,,,sandy,,,,,,,delta plain,,"""low delta or floodplain... very still water""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"selective quarrying,field collection",,species names,,,,,University of Texas,"Locality number TMM 30966 preceeds specimens found at this location (Olson & Mead, 1982)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Seymouria,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:29,13/05/2016 08:29,19359,baylorensis,Seymouria,59144,,279.3,272.3,Kungurian,,NA,US,Seymouria baylorensis
1328473,occ,NA,,67735,,Captorhinus aguti,species,90718,,Captorhinus aguti,NA,species,134887,Olson and Mead,1982,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,,-99.75,32.130001,Taylor County Site 7,NA,B.E.G. 30996; W.P.A. quarry; Sid McAdams Locality,US,Texas,Taylor,based on nearby landmark,2,small collection,"""souther part of Taylor County, Texas, in the SW 1/4 of section 436 of the M. P. King survey, on the property of Mr. C.O. Patterson, Route 1, Lawn, Texas... 6 miles southwest of the small town of Lawn"" (coordinate based on Lawn).\r\nAccording to Olson & Mead (1982) this locality contains a number of different sub-localities (""sites""), which here at treated as one locality.",gp_mid,-30.15,0.6,101,US,,Vale,,,group of beds,,,,,,,NA,"""22 feet above the Vale-Standpipe contact""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""siliceous clays""",claystone,,,sandy,,,,,,,delta plain,,"""low delta or floodplain... very still water""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"selective quarrying,field collection",,species names,,,,,University of Texas,"Locality number TMM 30966 preceeds specimens found at this location (Olson & Mead, 1982)",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:29,13/05/2016 08:29,19359,aguti,Captorhinus,59144,,279.3,272.3,Kungurian,,NA,US,Captorhinus aguti
1328474,occ,NA,,67735,,Captorhinikos valensis,species,120855,,Captorhinikos valensis,NA,species,120855,Olson and Mead,1982,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37496,NA,NA,NA,,-99.75,32.130001,Taylor County Site 7,NA,B.E.G. 30996; W.P.A. quarry; Sid McAdams Locality,US,Texas,Taylor,based on nearby landmark,2,small collection,"""souther part of Taylor County, Texas, in the SW 1/4 of section 436 of the M. P. King survey, on the property of Mr. C.O. Patterson, Route 1, Lawn, Texas... 6 miles southwest of the small town of Lawn"" (coordinate based on Lawn).\r\nAccording to Olson & Mead (1982) this locality contains a number of different sub-localities (""sites""), which here at treated as one locality.",gp_mid,-30.15,0.6,101,US,,Vale,,,group of beds,,,,,,,NA,"""22 feet above the Vale-Standpipe contact""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""siliceous clays""",claystone,,,sandy,,,,,,,delta plain,,"""low delta or floodplain... very still water""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"selective quarrying,field collection",,species names,,,,,University of Texas,"Locality number TMM 30966 preceeds specimens found at this location (Olson & Mead, 1982)",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinikos,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:29,13/05/2016 08:29,19359,valensis,Captorhinikos,59144,,279.3,272.3,Kungurian,,NA,US,Captorhinikos valensis
1328475,occ,NA,,67735,,Captorhinoides valensis,species,120860,,Captorhinoides valensis,NA,species,120860,Olson and Mead,1982,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37498,NA,NA,NA,,-99.75,32.130001,Taylor County Site 7,NA,B.E.G. 30996; W.P.A. quarry; Sid McAdams Locality,US,Texas,Taylor,based on nearby landmark,2,small collection,"""souther part of Taylor County, Texas, in the SW 1/4 of section 436 of the M. P. King survey, on the property of Mr. C.O. Patterson, Route 1, Lawn, Texas... 6 miles southwest of the small town of Lawn"" (coordinate based on Lawn).\r\nAccording to Olson & Mead (1982) this locality contains a number of different sub-localities (""sites""), which here at treated as one locality.",gp_mid,-30.15,0.6,101,US,,Vale,,,group of beds,,,,,,,NA,"""22 feet above the Vale-Standpipe contact""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""siliceous clays""",claystone,,,sandy,,,,,,,delta plain,,"""low delta or floodplain... very still water""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"selective quarrying,field collection",,species names,,,,,University of Texas,"Locality number TMM 30966 preceeds specimens found at this location (Olson & Mead, 1982)",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinoides,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:29,13/05/2016 08:29,19359,valensis,Captorhinoides,59144,,279.3,272.3,Kungurian,,NA,US,Captorhinoides valensis
1328476,occ,NA,,67735,,Labidosaurikos meachami,species,119515,,Labidosaurikos meachami,NA,species,119515,Olson and Mead,1982,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37500,NA,NA,NA,,-99.75,32.130001,Taylor County Site 7,NA,B.E.G. 30996; W.P.A. quarry; Sid McAdams Locality,US,Texas,Taylor,based on nearby landmark,2,small collection,"""souther part of Taylor County, Texas, in the SW 1/4 of section 436 of the M. P. King survey, on the property of Mr. C.O. Patterson, Route 1, Lawn, Texas... 6 miles southwest of the small town of Lawn"" (coordinate based on Lawn).\r\nAccording to Olson & Mead (1982) this locality contains a number of different sub-localities (""sites""), which here at treated as one locality.",gp_mid,-30.15,0.6,101,US,,Vale,,,group of beds,,,,,,,NA,"""22 feet above the Vale-Standpipe contact""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""siliceous clays""",claystone,,,sandy,,,,,,,delta plain,,"""low delta or floodplain... very still water""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"selective quarrying,field collection",,species names,,,,,University of Texas,"Locality number TMM 30966 preceeds specimens found at this location (Olson & Mead, 1982)",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurikos,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:30,13/05/2016 08:30,19359,meachami,Labidosaurikos,59144,,279.3,272.3,Kungurian,,NA,US,Labidosaurikos meachami
1328477,occ,NA,,67735,,Dimetrodon gigashomogenes,species,138123,,Dimetrodon gigashomogenes,NA,species,138123,Olson and Mead,1982,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.75,32.130001,Taylor County Site 7,NA,B.E.G. 30996; W.P.A. quarry; Sid McAdams Locality,US,Texas,Taylor,based on nearby landmark,2,small collection,"""souther part of Taylor County, Texas, in the SW 1/4 of section 436 of the M. P. King survey, on the property of Mr. C.O. Patterson, Route 1, Lawn, Texas... 6 miles southwest of the small town of Lawn"" (coordinate based on Lawn).\r\nAccording to Olson & Mead (1982) this locality contains a number of different sub-localities (""sites""), which here at treated as one locality.",gp_mid,-30.15,0.6,101,US,,Vale,,,group of beds,,,,,,,NA,"""22 feet above the Vale-Standpipe contact""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""siliceous clays""",claystone,,,sandy,,,,,,,delta plain,,"""low delta or floodplain... very still water""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"selective quarrying,field collection",,species names,,,,,University of Texas,"Locality number TMM 30966 preceeds specimens found at this location (Olson & Mead, 1982)",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:30,13/05/2016 08:30,19359,gigashomogenes,Dimetrodon,59144,,279.3,272.3,Kungurian,,NA,US,Dimetrodon gigashomogenes
1328478,occ,NA,,67735,,Casea nicholsi,species,120853,,Casea nicholsi,NA,species,120853,Olson and Mead,1982,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38915,NA,NA,NA,,-99.75,32.130001,Taylor County Site 7,NA,B.E.G. 30996; W.P.A. quarry; Sid McAdams Locality,US,Texas,Taylor,based on nearby landmark,2,small collection,"""souther part of Taylor County, Texas, in the SW 1/4 of section 436 of the M. P. King survey, on the property of Mr. C.O. Patterson, Route 1, Lawn, Texas... 6 miles southwest of the small town of Lawn"" (coordinate based on Lawn).\r\nAccording to Olson & Mead (1982) this locality contains a number of different sub-localities (""sites""), which here at treated as one locality.",gp_mid,-30.15,0.6,101,US,,Vale,,,group of beds,,,,,,,NA,"""22 feet above the Vale-Standpipe contact""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""siliceous clays""",claystone,,,sandy,,,,,,,delta plain,,"""low delta or floodplain... very still water""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"selective quarrying,field collection",,species names,,,,,University of Texas,"Locality number TMM 30966 preceeds specimens found at this location (Olson & Mead, 1982)",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Casea,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:31,13/05/2016 08:31,19359,nicholsi,Casea,59144,,279.3,272.3,Kungurian,,NA,US,Casea nicholsi
1328480,occ,NA,,178738,members,Diplocaulus recurvatus,species,120886,,Diplocaulus recurvatus,NA,species,120886,Olson and Mead,1982,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.830101,32.234524,Blackwood Locality,NA,South of Buffalo Gap,US,Texas,Taylor,based on nearby landmark,6,outcrop,"Locaility on the property of Mr. L. A. Blackwood about 3.5km south of Buffalo Gap, Taylor County, Texas. The locality covers an area that measures about 1.5km north-south and 1km east-west. ",gp_mid,-30.16,0.72,101,US,,Vale,Clear Fork,,member,,,,,,,NA,Extensive discussion of the vale formation can be found in Olson & Mead (1982),,siltstone,red,,,,sandstone,,,,,wet floodplain,,"Outcrops are made up predominantly of red and maroon siltstones with irregularly distributed beds and lenses of sandstone, mudstone, and conglomerate.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Location discovered by David Berman of the Carnegie Museum, Pittsburgh, Pennsylvania.",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:48,13/05/2016 08:48,NA,recurvatus,Diplocaulus,59144,,279.3,272.3,Kungurian,,NA,US,Diplocaulus recurvatus
1328481,occ,NA,,178738,members,Eryops megacephalus,species,70397,,Eryops megacephalus,NA,species,70397,Olson and Mead,1982,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-99.830101,32.234524,Blackwood Locality,NA,South of Buffalo Gap,US,Texas,Taylor,based on nearby landmark,6,outcrop,"Locaility on the property of Mr. L. A. Blackwood about 3.5km south of Buffalo Gap, Taylor County, Texas. The locality covers an area that measures about 1.5km north-south and 1km east-west. ",gp_mid,-30.16,0.72,101,US,,Vale,Clear Fork,,member,,,,,,,NA,Extensive discussion of the vale formation can be found in Olson & Mead (1982),,siltstone,red,,,,sandstone,,,,,wet floodplain,,"Outcrops are made up predominantly of red and maroon siltstones with irregularly distributed beds and lenses of sandstone, mudstone, and conglomerate.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Location discovered by David Berman of the Carnegie Museum, Pittsburgh, Pennsylvania.",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:48,13/05/2016 08:48,NA,megacephalus,Eryops,59144,,279.3,272.3,Kungurian,,NA,US,Eryops megacephalus
1328482,occ,NA,,178738,members,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Olson and Mead,1982,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-99.830101,32.234524,Blackwood Locality,NA,South of Buffalo Gap,US,Texas,Taylor,based on nearby landmark,6,outcrop,"Locaility on the property of Mr. L. A. Blackwood about 3.5km south of Buffalo Gap, Taylor County, Texas. The locality covers an area that measures about 1.5km north-south and 1km east-west. ",gp_mid,-30.16,0.72,101,US,,Vale,Clear Fork,,member,,,,,,,NA,Extensive discussion of the vale formation can be found in Olson & Mead (1982),,siltstone,red,,,,sandstone,,,,,wet floodplain,,"Outcrops are made up predominantly of red and maroon siltstones with irregularly distributed beds and lenses of sandstone, mudstone, and conglomerate.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Location discovered by David Berman of the Carnegie Museum, Pittsburgh, Pennsylvania.",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:48,13/05/2016 08:48,NA,sp.,Diadectes,59144,,279.3,272.3,Kungurian,,NA,US,Diadectes sp.
1328483,occ,NA,,178738,members,Seymouria grandis,species,346166,,Seymouria grandis,NA,species,346166,Olson,1979,Chordata,33815,Osteichthyes,34881,,NA,Seymouriidae,37219,37223,NA,NA,NA,specimens,-99.830101,32.234524,Blackwood Locality,NA,South of Buffalo Gap,US,Texas,Taylor,based on nearby landmark,6,outcrop,"Locaility on the property of Mr. L. A. Blackwood about 3.5km south of Buffalo Gap, Taylor County, Texas. The locality covers an area that measures about 1.5km north-south and 1km east-west. ",gp_mid,-30.16,0.72,101,US,,Vale,Clear Fork,,member,,,,,,,NA,Extensive discussion of the vale formation can be found in Olson & Mead (1982),,siltstone,red,,,,sandstone,,,,,wet floodplain,,"Outcrops are made up predominantly of red and maroon siltstones with irregularly distributed beds and lenses of sandstone, mudstone, and conglomerate.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Location discovered by David Berman of the Carnegie Museum, Pittsburgh, Pennsylvania.",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Seymouria,,NA,NA,vertebrate,E. C. Olson. 1979. Seymouria grandis n. sp. (Batrachosauria: Amphibia) from the Middle Clear Fork (Permian) of Oklahoma and Texas. Journal of Paleontology 53(3):720-728,327,697,697,R. Butler,E. Dunne,E. Dunne,13/05/2016 08:48,19/08/2016 09:26,NA,grandis,Seymouria,60165,,279.3,272.3,Kungurian,,6,US,Seymouria grandis
1328484,occ,NA,,178738,members,Labidosaurikos sp.,genus,37500,,Labidosaurikos,NA,genus,37500,Olson and Mead,1982,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37500,NA,NA,NA,,-99.830101,32.234524,Blackwood Locality,NA,South of Buffalo Gap,US,Texas,Taylor,based on nearby landmark,6,outcrop,"Locaility on the property of Mr. L. A. Blackwood about 3.5km south of Buffalo Gap, Taylor County, Texas. The locality covers an area that measures about 1.5km north-south and 1km east-west. ",gp_mid,-30.16,0.72,101,US,,Vale,Clear Fork,,member,,,,,,,NA,Extensive discussion of the vale formation can be found in Olson & Mead (1982),,siltstone,red,,,,sandstone,,,,,wet floodplain,,"Outcrops are made up predominantly of red and maroon siltstones with irregularly distributed beds and lenses of sandstone, mudstone, and conglomerate.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Location discovered by David Berman of the Carnegie Museum, Pittsburgh, Pennsylvania.",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurikos,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:48,13/05/2016 08:48,NA,sp.,Labidosaurikos,59144,,279.3,272.3,Kungurian,,NA,US,Labidosaurikos sp.
1328485,occ,NA,,178738,members,Captorhinus aguti,species,90718,,Captorhinus aguti,NA,species,134887,Olson and Mead,1982,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,,-99.830101,32.234524,Blackwood Locality,NA,South of Buffalo Gap,US,Texas,Taylor,based on nearby landmark,6,outcrop,"Locaility on the property of Mr. L. A. Blackwood about 3.5km south of Buffalo Gap, Taylor County, Texas. The locality covers an area that measures about 1.5km north-south and 1km east-west. ",gp_mid,-30.16,0.72,101,US,,Vale,Clear Fork,,member,,,,,,,NA,Extensive discussion of the vale formation can be found in Olson & Mead (1982),,siltstone,red,,,,sandstone,,,,,wet floodplain,,"Outcrops are made up predominantly of red and maroon siltstones with irregularly distributed beds and lenses of sandstone, mudstone, and conglomerate.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Location discovered by David Berman of the Carnegie Museum, Pittsburgh, Pennsylvania.",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:48,13/05/2016 08:48,NA,aguti,Captorhinus,59144,,279.3,272.3,Kungurian,,NA,US,Captorhinus aguti
1328486,occ,NA,,178738,members,Captorhinikos chozaensis,species,120856,,Captorhinikos chozaensis,NA,species,120856,Olson and Mead,1982,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37496,NA,NA,NA,,-99.830101,32.234524,Blackwood Locality,NA,South of Buffalo Gap,US,Texas,Taylor,based on nearby landmark,6,outcrop,"Locaility on the property of Mr. L. A. Blackwood about 3.5km south of Buffalo Gap, Taylor County, Texas. The locality covers an area that measures about 1.5km north-south and 1km east-west. ",gp_mid,-30.16,0.72,101,US,,Vale,Clear Fork,,member,,,,,,,NA,Extensive discussion of the vale formation can be found in Olson & Mead (1982),,siltstone,red,,,,sandstone,,,,,wet floodplain,,"Outcrops are made up predominantly of red and maroon siltstones with irregularly distributed beds and lenses of sandstone, mudstone, and conglomerate.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Location discovered by David Berman of the Carnegie Museum, Pittsburgh, Pennsylvania.",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinikos,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:48,13/05/2016 08:48,NA,chozaensis,Captorhinikos,59144,,279.3,272.3,Kungurian,,NA,US,Captorhinikos chozaensis
1328487,occ,NA,,178738,members,Labidosaurikos barkeri,species,119514,subjective synonym of,Labidosaurikos meachami,NA,species,119515,Olson and Mead,1982,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37500,NA,NA,NA,,-99.830101,32.234524,Blackwood Locality,NA,South of Buffalo Gap,US,Texas,Taylor,based on nearby landmark,6,outcrop,"Locaility on the property of Mr. L. A. Blackwood about 3.5km south of Buffalo Gap, Taylor County, Texas. The locality covers an area that measures about 1.5km north-south and 1km east-west. ",gp_mid,-30.16,0.72,101,US,,Vale,Clear Fork,,member,,,,,,,NA,Extensive discussion of the vale formation can be found in Olson & Mead (1982),,siltstone,red,,,,sandstone,,,,,wet floodplain,,"Outcrops are made up predominantly of red and maroon siltstones with irregularly distributed beds and lenses of sandstone, mudstone, and conglomerate.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Location discovered by David Berman of the Carnegie Museum, Pittsburgh, Pennsylvania.",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurikos,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:48,13/05/2016 08:48,NA,barkeri,Labidosaurikos,59144,,279.3,272.3,Kungurian,,NA,US,Labidosaurikos barkeri
1328488,occ,NA,,178738,members,Labidosaurus hamatus,species,134918,,Labidosaurus hamatus,NA,species,134856,Olson and Mead,1982,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,,-99.830101,32.234524,Blackwood Locality,NA,South of Buffalo Gap,US,Texas,Taylor,based on nearby landmark,6,outcrop,"Locaility on the property of Mr. L. A. Blackwood about 3.5km south of Buffalo Gap, Taylor County, Texas. The locality covers an area that measures about 1.5km north-south and 1km east-west. ",gp_mid,-30.16,0.72,101,US,,Vale,Clear Fork,,member,,,,,,,NA,Extensive discussion of the vale formation can be found in Olson & Mead (1982),,siltstone,red,,,,sandstone,,,,,wet floodplain,,"Outcrops are made up predominantly of red and maroon siltstones with irregularly distributed beds and lenses of sandstone, mudstone, and conglomerate.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Location discovered by David Berman of the Carnegie Museum, Pittsburgh, Pennsylvania.",,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:48,13/05/2016 08:48,NA,hamatus,Labidosaurus,59144,,279.3,272.3,Kungurian,,NA,US,Labidosaurus hamatus
1328489,occ,NA,,178738,members,Dimetrodon gigashomogenes,species,138123,,Dimetrodon gigashomogenes,NA,species,138123,Olson and Mead,1982,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.830101,32.234524,Blackwood Locality,NA,South of Buffalo Gap,US,Texas,Taylor,based on nearby landmark,6,outcrop,"Locaility on the property of Mr. L. A. Blackwood about 3.5km south of Buffalo Gap, Taylor County, Texas. The locality covers an area that measures about 1.5km north-south and 1km east-west. ",gp_mid,-30.16,0.72,101,US,,Vale,Clear Fork,,member,,,,,,,NA,Extensive discussion of the vale formation can be found in Olson & Mead (1982),,siltstone,red,,,,sandstone,,,,,wet floodplain,,"Outcrops are made up predominantly of red and maroon siltstones with irregularly distributed beds and lenses of sandstone, mudstone, and conglomerate.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Location discovered by David Berman of the Carnegie Museum, Pittsburgh, Pennsylvania.",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,0,R. Butler,E. Dunne,,13/05/2016 08:48,13/05/2016 08:48,NA,gigashomogenes,Dimetrodon,59144,,279.3,272.3,Kungurian,,NA,US,Dimetrodon gigashomogenes
1328491,occ,NA,,178739,members,Diplocaulus recurvatus,species,120886,,Diplocaulus recurvatus,NA,species,120886,Olson and Mead,1982,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.854408,32.978802,Stamford Locality (Vale Formation),NA,,US,Texas,Haskell ,based on nearby landmark,6,outcrop,"The locality lies just north of the Jones-Haskell County line, Texas, about 3km northwest of the centre of Stamford, Texas. The sediments that carry most of the vertebrates at this locality form a roughly heart-shaped area about 15m to 20m in length and width.",gp_mid,-30.86,-0.58,101,US,,Vale,Clear Fork,,member,,,,,,,NA,,,siltstone,"gray,green",lithified,,,claystone,red or brown,,,,fluvial indet.,,This site was first collected and reported upon by Dalquest and Mamay (1963) and the geology of the location discussed therein.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,all macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,697,R. Butler,E. Dunne,E. Dunne,13/05/2016 08:59,19/07/2016 04:44,NA,recurvatus,Diplocaulus,59144,,290.1,268,Leonard,,NA,US,Diplocaulus recurvatus
1328492,occ,NA,,178739,members,Trimerorhachis insignis,species,90711,,Trimerorhachis insignis,NA,species,90711,Olson and Mead,1982,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-99.854408,32.978802,Stamford Locality (Vale Formation),NA,,US,Texas,Haskell ,based on nearby landmark,6,outcrop,"The locality lies just north of the Jones-Haskell County line, Texas, about 3km northwest of the centre of Stamford, Texas. The sediments that carry most of the vertebrates at this locality form a roughly heart-shaped area about 15m to 20m in length and width.",gp_mid,-30.86,-0.58,101,US,,Vale,Clear Fork,,member,,,,,,,NA,,,siltstone,"gray,green",lithified,,,claystone,red or brown,,,,fluvial indet.,,This site was first collected and reported upon by Dalquest and Mamay (1963) and the geology of the location discussed therein.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,all macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,697,R. Butler,E. Dunne,E. Dunne,13/05/2016 08:59,19/07/2016 05:30,NA,insignis,Trimerorhachis,59144,,290.1,268,Leonard,,NA,US,Trimerorhachis insignis
1328493,occ,NA,,178739,members,Trimerorhachis mesops,species,345111,,Trimerorhachis mesops,NA,species,345111,Olson and Mead,1982,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-99.854408,32.978802,Stamford Locality (Vale Formation),NA,,US,Texas,Haskell ,based on nearby landmark,6,outcrop,"The locality lies just north of the Jones-Haskell County line, Texas, about 3km northwest of the centre of Stamford, Texas. The sediments that carry most of the vertebrates at this locality form a roughly heart-shaped area about 15m to 20m in length and width.",gp_mid,-30.86,-0.58,101,US,,Vale,Clear Fork,,member,,,,,,,NA,,,siltstone,"gray,green",lithified,,,claystone,red or brown,,,,fluvial indet.,,This site was first collected and reported upon by Dalquest and Mamay (1963) and the geology of the location discussed therein.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,all macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,E. C. Olson and J. G. Mead. 1982. The Vale Formation (Lower Permian): Its Vertebrates and Paleoecology. Texas Memorial Museum Bulletin 29,327,697,697,R. Butler,E. Dunne,E. Dunne,13/05/2016 08:59,19/07/2016 04:51,NA,mesops,Trimerorhachis,59144,,290.1,268,Leonard,,NA,US,Trimerorhachis mesops
1328833,occ,NA,,178804,members,Eogyrinus attheyi,species,296848,recombined as,Pholiderpeton attheyi,NA,species,296848,Panchen,1972,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37193,NA,NA,NA,specimens,-3.962895,55.865932,"Airdrie, Lanarkshire",NA,,UK,Scotland,Lanarkshire,based on nearby landmark,7,small collection,Coordinates based on Airdrie town centre,gp_mid,5.21,-0.02,313,UK,,Pennine Middle Coal Measures,Pennine Coal Measures,,,,,,,,,NA,,,coal,,,,,,,,,,fluvial-deltaic indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Eogyrinus,,NA,NA,vertebrate,A. L. Panchen. 1972. The Skull and Skeleton of Eogyrinus attheyi Watson (Amphibia: Labyrinthodontia). Philosophical Transactions of the Royal Society B 263(851):279-326,327,697,697,R. Butler,E. Dunne,E. Dunne,16/05/2016 07:16,01/09/2017 06:53,NA,attheyi,Pholiderpeton,59156,,314.6,311.45,Westphalian B,Westphalian C,1,UK,Pholiderpeton attheyi
1328914,occ,NA,,177139,members,n. gen. Pteroplax n. sp. cornuta,species,320846,corrected to,Pteroplax cornutus,NA,species,320846,Boyd,1980,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37194,NA,NA,NA,,-1.52138,55.105228,"Hannah Pit, Newsham",NA,Newsham Colliery,UK,England,Yorkshire,stated in text,6,small collection,"Coordinates are those of the Hannah pit as shown on the First Edition Ordnance Survey map of 1865. The pit was ""sunk in 1860 to the Low Main seam, recorded as a depth of 99 fathoms (181m)""",gp_mid,3.06,-6.8,315,UK,,Middle Coal Measures,,,,,,,,,,NA,"""The horizon lies within the Upper Modiolaris zone of the Middle Coal Measures (Land 1974) and is Westphalian B in age"" (Boyd, 1980)",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Pteroplax,n. gen.,NA,NA,vertebrate,M. J. Boyd. 1980. The axial skeleton of the Carboniferous amphibian Pteroplax cornutus. Palaeontology 23(2):273-285,327,697,0,R. Butler,E. Dunne,,17/05/2016 06:45,17/05/2016 06:45,NA,cornuta,Pteroplax,59162,n. sp.,323.2,315.2,Bashkirian,,NA,UK,Pteroplax cornuta
1328916,occ,NA,,177139,members,Ophiderpeton n. sp. nanum,species,320836,recombined as,Oestocephalus nanum,NA,species,320836,Fritsch,1880,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Oestocephalidae,230698,230697,NA,NA,NA,,-1.52138,55.105228,"Hannah Pit, Newsham",NA,Newsham Colliery,UK,England,Yorkshire,stated in text,6,small collection,"Coordinates are those of the Hannah pit as shown on the First Edition Ordnance Survey map of 1865. The pit was ""sunk in 1860 to the Low Main seam, recorded as a depth of 99 fathoms (181m)""",gp_mid,3.06,-6.8,315,UK,,Middle Coal Measures,,,,,,,,,,NA,"""The horizon lies within the Upper Modiolaris zone of the Middle Coal Measures (Land 1974) and is Westphalian B in age"" (Boyd, 1980)",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Ophiderpeton,,NA,NA,vertebrate,A. Fritsch. 1880. Fauna der Gaskohle und der Kalksteine der Permformation Bohmens. 1(2),327,697,0,R. Butler,E. Dunne,,17/05/2016 06:50,17/05/2016 06:50,NA,nanum,Oestocephalus,58421,n. sp.,323.2,315.2,Bashkirian,,NA,UK,Oestocephalus nanum
1328917,occ,NA,,177139,members,n. gen. Eogyrinus n. sp. attheyi,species,296848,recombined as,Pholiderpeton attheyi,NA,species,296848,Watson,1926,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37193,NA,NA,NA,,-1.52138,55.105228,"Hannah Pit, Newsham",NA,Newsham Colliery,UK,England,Yorkshire,stated in text,6,small collection,"Coordinates are those of the Hannah pit as shown on the First Edition Ordnance Survey map of 1865. The pit was ""sunk in 1860 to the Low Main seam, recorded as a depth of 99 fathoms (181m)""",gp_mid,3.06,-6.8,315,UK,,Middle Coal Measures,,,,,,,,,,NA,"""The horizon lies within the Upper Modiolaris zone of the Middle Coal Measures (Land 1974) and is Westphalian B in age"" (Boyd, 1980)",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Eogyrinus,n. gen.,NA,NA,vertebrate,"D. M. S. Watson. 1926. Croonian lecture.The evolution and origin of the Amphibia. Proceedings of the Royal Society of London, Series B 214:189-257",327,697,0,R. Butler,E. Dunne,,17/05/2016 06:52,17/05/2016 06:52,NA,attheyi,Pholiderpeton,51608,n. sp.,323.2,315.2,Bashkirian,,NA,UK,Pholiderpeton attheyi
1328919,occ,NA,,84835,,n. gen. Solenodonsaurus n. sp. janenschi,species,136800,,Solenodonsaurus janenschi,NA,species,136800,Broili,1924,Chordata,33815,Osteichthyes,34881,,NA,,NA,37238,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Solenodonsaurus,n. gen.,NA,NA,vertebrate,F. Broili. 1924. Ein Cotylosaurier aus der oberkarbonischen Gaskohle von N_rschan in B̦hmen. Sitzungsberichte der Mathematisch-Naturwissenschaftlichen Abteilung der Bayerischen Akademie der Wissenschaften zu M_nchen ,327,697,0,R. Butler,E. Dunne,,17/05/2016 07:12,17/05/2016 07:12,28608,janenschi,Solenodonsaurus,59164,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Solenodonsaurus janenschi
1328952,occ,NA,,85292,,n. gen. Leptophractus n. sp. obsoletus,species,320853,,Leptophractus obsoletus,NA,species,320853,Cope,1873,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37190,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Leptophractus,n. gen.,NA,NA,vertebrate,"E. D. Cope. 1873. On some new Batrachia and fishes from the Coal Measures of Linton, Ohio. Proceedings of the Academy of Natural Science of Philadelphia ",327,697,0,R. Butler,E. Dunne,,18/05/2016 04:59,18/05/2016 04:59,28831,obsoletus,Leptophractus,59179,n. sp.,311.45,306.95,Westphalian D,,NA,US,Leptophractus obsoletus
1328954,occ,NA,,125662,,n. gen. Nummulosaurus n. sp. kolbii,species,320852,,Nummulosaurus kolbii,NA,species,320852,Fritsch,1901,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,320843,NA,NA,NA,,13.395,49.814999,Tremosna,NA,"Temon̩, Temon",CZ,,,based on nearby landmark,3,outcrop,,gp_mid,19.75,0.69,305,CZ,,Kladno,,Nyrany,,,,,,,,NA,Tremosna in B̦hmen. Mittleres Obercarbon.,,not reported,,,,,coal,,,,,terrestrial indet.,rift,"Central-West Bohemian basin; extensional basin developed within Variscan zone along simple asymmetric mega-graben formed on the Central Bohemian and Litomerice fault zones, with some contribution from transtensional wrench faults.",macrofossils,,,,,,NA,,mold/impression,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Nummulosaurus,n. gen.,NA,NA,"paleoentomology,vertebrate","A. Fritsch. 1901. Fauna der Gaskohle und der Kalksteine der Permformation B̦hmens. Vierter Band, Heft III ",327,697,0,R. Butler,E. Dunne,,18/05/2016 05:05,18/05/2016 05:05,50906,kolbii,Nummulosaurus,50656,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Nummulosaurus kolbii
1328959,occ,NA,,178804,members,n. gen. Baphetes n. sp. latirostris,species,335636,objective synonym of,Baphetes kirkbyi,NA,species,229310,Watson,1929,Chordata,33815,Osteichthyes,34881,,NA,Baphetidae,227378,36970,NA,NA,NA,specimens,-3.962895,55.865932,"Airdrie, Lanarkshire",NA,,UK,Scotland,Lanarkshire,based on nearby landmark,7,small collection,Coordinates based on Airdrie town centre,gp_mid,5.21,-0.02,313,UK,,Pennine Middle Coal Measures,Pennine Coal Measures,,,,,,,,,NA,,,coal,,,,,,,,,,fluvial-deltaic indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Baphetes,n. gen.,NA,NA,vertebrate,D. M. S. Watson. 1929. The Carboniferous Amphibia of Scotland. Palaeontologia Hungarica 1:223-252,327,697,697,R. Butler,E. Dunne,E. Dunne,18/05/2016 06:20,01/09/2017 06:53,NA,latirostris,Baphetes,57610,n. sp.,314.6,311.45,Westphalian B,Westphalian C,1,UK,Baphetes latirostris
1328961,occ,NA,,178804,members,n. gen. Anthracosaurus n. sp. russelli,species,229307,,Anthracosaurus russelli,NA,species,229307,Panchen,1970,Chordata,33815,Osteichthyes,34881,,NA,Anthracosauridae,37199,37200,NA,NA,NA,specimens,-3.962895,55.865932,"Airdrie, Lanarkshire",NA,,UK,Scotland,Lanarkshire,based on nearby landmark,7,small collection,Coordinates based on Airdrie town centre,gp_mid,5.21,-0.02,313,UK,,Pennine Middle Coal Measures,Pennine Coal Measures,,,,,,,,,NA,,,coal,,,,,,,,,,fluvial-deltaic indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Anthracosaurus,n. gen.,NA,NA,vertebrate,A. L. Panchen. 1970. Handbuch der Palaoherpetologie / Encyclopedia of Paleoherpetology Teil 5 / Part 5 Batrachosauria Teil A / Part A Anthracosauria. ,327,697,697,R. Butler,E. Dunne,E. Dunne,18/05/2016 06:46,01/09/2017 06:53,NA,russelli,Anthracosaurus,55380,n. sp.,314.6,311.45,Westphalian B,Westphalian C,1,UK,Anthracosaurus russelli
1328962,occ,NA,,178845,members,Anthracosaurus russelli,species,229307,,Anthracosaurus russelli,NA,species,229307,Panchen et al.,1967,Chordata,33815,Osteichthyes,34881,,NA,Anthracosauridae,37199,37200,NA,NA,NA,,-1.530306,54.913498,Usworth Colliery,NA,,UK,England,Durham,based on nearby landmark,6,small collection,"Coordiates based on the location of Usworth near Wsshinghton, Tyne and Wear, Co. Durham.",gp_mid,4.88,-3.86,315,UK,,Lower Coal Measures,Pennine Coal Measures,,group of beds,,,,,,,NA,"Top Busty Seam, Communis Zone",,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Anthracosaurus,,NA,NA,vertebrate,"A. L. Panchen, E. H. Tilley, and C. A. B. Steel. 1967. Discovery of an anthracosaur skull in the Durham Coal Measures. Nature 214:1001",327,697,0,R. Butler,E. Dunne,,18/05/2016 06:59,18/05/2016 06:59,NA,russelli,Anthracosaurus,59182,,318.1,314.6,Westphalian A,,NA,UK,Anthracosaurus russelli
1328963,occ,NA,,85292,,Anthracosaurus n. sp. lancifer,species,137376,,Anthracosaurus lancifer,NA,species,137375,Newberry,1856,Chordata,33815,Osteichthyes,34881,,NA,Anthracosauridae,37199,37200,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Anthracosaurus,,NA,NA,vertebrate,J. S. Newberry. 1856. Description of several new genera and species of fossil fishes from the Carboniferous strata of Ohio. Proceedings of the Academy of Natural Sciences of Philadelphia 8:96-100,327,697,0,R. Butler,E. Dunne,,18/05/2016 09:52,18/05/2016 09:52,28831,lancifer,Anthracosaurus,57799,n. sp.,311.45,306.95,Westphalian D,,NA,US,Anthracosaurus lancifer
1328964,occ,NA,,178846,members,n. gen. Eobaphetes n. sp. kansensis,species,320845,,Eobaphetes kansensis,NA,species,320845,Moodie,1911,Chordata,33815,Osteichthyes,34881,,NA,Anthracosauridae,37199,320841,NA,NA,NA,,-94.313438,35.892696,"Baldwin Coal, Washington Co.",NA,,US,Arkansas,Washington,based on nearby landmark,6,small collection,"Coordinates based on the type locality for the Bloyd Shale: 9 miles southwest of Fayetteville, Washington County, Arkansas",gp_mid,-36.17,-13.65,101,US,,Bloyd,,Woolsey,,,,,,,,NA,,,"""shale""",gray,,,,siltstone,,,,,terrestrial indet.,,"The Woolsey Member is composed of terrestrial sediments comprised of dark-gray, fissile shale, often interbedded with thin siltstones. A thin coal bed, called the Baldwin Coal, occurs at or near the top of the Woolsey Member.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Eobaphetes,n. gen.,NA,NA,vertebrate,R. L. Moodie. 1911. A new labyrinthodont from the Kansas coal measures. Proceedings of the United States National Museum 39:489-495,327,697,0,R. Butler,E. Dunne,,18/05/2016 11:26,18/05/2016 11:26,NA,kansensis,Eobaphetes,59185,n. sp.,326.4,306.95,Namurian,Westphalian,NA,US,Eobaphetes kansensis
1329833,occ,NA,,80714,,n. gen. Cricotus n. sp. heteroclitus,species,170123,,Cricotus heteroclitus,NA,species,170123,Cope,1875,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37197,NA,NA,NA,,-87.775002,40.108334,Danville Locality (Vertebrates),NA,Oakwood Locality; Horseshoe Bend; Vermillion River; Illinois bonebed,US,Illinois,Vermilion,based on nearby landmark,seconds,outcrop,"""the well-known Danville or 'Oakwood' locality [...] Horseshoe Bend locality near the SE/C of Sec. 23-19N-13W"" (DeMar, 1970)\r\n""Vermilion River, near Danville"" (Reisz, 1986)\r\nLat Long is for Oakwood",gp_mid,-21.51,-3.52,101,US,,Bond,McLeansboro,,group of beds,,,,,,,NA,"""We believe the vertebrates have been collected from a zone 10 feet or so below the Shoal Creek Member of the Bond Formation"" (DeMar, 1970)\r\nNote: Shoal Creek Member is equivalent to Carthage Limestone Member, a name now used throughout the Illinois Basin for that lithological unit; see Jacobson (2002) A summary of references with changes in Pennsylvanian stratigraphic nomenclature at the ISGS since Bulletin 95. [Online] http://www.isgs.illinois.edu/maps-data-pub/coal-maps/pennstratigraphy.shtml ",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cricotus,n. gen.,NA,NA,vertebrate,E. D. Cope. 1875. On fossil remains of Reptilia and fishes from Illinois. Proceedings of the Academy of Natural Sciences of Philadelphia 27(1):404-411,327,697,0,R. Butler,E. Dunne,,26/05/2016 05:00,26/05/2016 05:00,28640,heteroclitus,Cricotus,28850,n. sp.,305.9,303.4,Missourian,,NA,US,Cricotus heteroclitus
1329835,occ,NA,,80714,,Cricotus n. sp. discophorus,species,70394,subjective synonym of,Cricotus heteroclitus,NA,species,170123,Cope,1877,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37197,NA,NA,NA,,-87.775002,40.108334,Danville Locality (Vertebrates),NA,Oakwood Locality; Horseshoe Bend; Vermillion River; Illinois bonebed,US,Illinois,Vermilion,based on nearby landmark,seconds,outcrop,"""the well-known Danville or 'Oakwood' locality [...] Horseshoe Bend locality near the SE/C of Sec. 23-19N-13W"" (DeMar, 1970)\r\n""Vermilion River, near Danville"" (Reisz, 1986)\r\nLat Long is for Oakwood",gp_mid,-21.51,-3.52,101,US,,Bond,McLeansboro,,group of beds,,,,,,,NA,"""We believe the vertebrates have been collected from a zone 10 feet or so below the Shoal Creek Member of the Bond Formation"" (DeMar, 1970)\r\nNote: Shoal Creek Member is equivalent to Carthage Limestone Member, a name now used throughout the Illinois Basin for that lithological unit; see Jacobson (2002) A summary of references with changes in Pennsylvanian stratigraphic nomenclature at the ISGS since Bulletin 95. [Online] http://www.isgs.illinois.edu/maps-data-pub/coal-maps/pennstratigraphy.shtml ",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cricotus,,NA,NA,vertebrate,E. D. Cope. 1877. Descriptions of extinct Vertebrata from the Permian and Triassic formations of the United States. Proceedings of the American Philosophical Society 17(100):182-193,327,697,0,R. Butler,E. Dunne,,26/05/2016 05:06,26/05/2016 05:06,28640,discophorus,Cricotus,15657,n. sp.,305.9,303.4,Missourian,,NA,US,Cricotus discophorus
1329836,occ,NA,,80714,,Cricotus n. sp. gibsonii,species,70393,subjective synonym of,Cricotus heteroclitus,NA,species,170123,Cope,1877,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37197,NA,NA,NA,,-87.775002,40.108334,Danville Locality (Vertebrates),NA,Oakwood Locality; Horseshoe Bend; Vermillion River; Illinois bonebed,US,Illinois,Vermilion,based on nearby landmark,seconds,outcrop,"""the well-known Danville or 'Oakwood' locality [...] Horseshoe Bend locality near the SE/C of Sec. 23-19N-13W"" (DeMar, 1970)\r\n""Vermilion River, near Danville"" (Reisz, 1986)\r\nLat Long is for Oakwood",gp_mid,-21.51,-3.52,101,US,,Bond,McLeansboro,,group of beds,,,,,,,NA,"""We believe the vertebrates have been collected from a zone 10 feet or so below the Shoal Creek Member of the Bond Formation"" (DeMar, 1970)\r\nNote: Shoal Creek Member is equivalent to Carthage Limestone Member, a name now used throughout the Illinois Basin for that lithological unit; see Jacobson (2002) A summary of references with changes in Pennsylvanian stratigraphic nomenclature at the ISGS since Bulletin 95. [Online] http://www.isgs.illinois.edu/maps-data-pub/coal-maps/pennstratigraphy.shtml ",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,FMNH,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cricotus,,NA,NA,vertebrate,E. D. Cope. 1877. Descriptions of extinct Vertebrata from the Permian and Triassic formations of the United States. Proceedings of the American Philosophical Society 17(100):182-193,327,697,0,R. Butler,E. Dunne,,26/05/2016 05:06,26/05/2016 05:06,28640,gibsonii,Cricotus,15657,n. sp.,305.9,303.4,Missourian,,NA,US,Cricotus gibsonii
1329838,occ,NA,,84835,,n. gen. Diplovertebron n. sp. punctatum,species,320851,,Diplovertebron punctatum,NA,species,320851,Fritsch,1879,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37188,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diplovertebron,n. gen.,NA,NA,vertebrate,A. Fritsch. 1879. Fauna der Gaskohle und der Kalksteine der Permformations Bohmens. 1(1),327,697,0,R. Butler,E. Dunne,,26/05/2016 05:13,26/05/2016 05:13,28608,punctatum,Diplovertebron,58134,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Diplovertebron punctatum
1329850,occ,NA,,79598,,n. gen. Spondylerpeton n. sp. spinatum,species,320854,nomen vanum,Spondylerpeton,NA,genus,37198,Moodie,1912,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37198,NA,NA,NA,,-88.139999,41.267223,Mazon Creek,NA,"Mazon Creek Vertebrate Fauna, Braidwood Fauna, pit 11",US,Illinois,Grundy/Will,based on political unit,seconds,local area,"Lat Long is for SW Will Co., Illinois",gp_mid,-23.34,-5.09,101,US,,Carbondale,,Francis Creek Shale,,,,,,,,NA,"""Francis Creek Shale above Morris (no. 2) Coal, Carbondale Formation, Westphalian D, Middle Pennsylvanian"" (Carroll & Baird, 1972)\r\nBaird et al. (1985) refer to the no. 2 coal as Colchester or Croweburg Coal Member.","""Concretions occur typically in laminated to weakly rippled, silty mudstone deposits which typically show little or no evidence of bioturbation. Small-scale sedimentary structures in nodule-bearing sequences include climbing ripple drift, and soft-sediment load-failure..."" (Baird et al., 1985 p.90). Note that this is a general description of the fossil bearing strata of the Francis Creek Shale Member which does not refer specifically to the occurences in the Mazon Creek area proper.",mudstone,"current ripples,deformed bedding",,silty,,siderite,nodular,,,Y,deltaic indet.,foreland basin,"""...these indicate rapid and often episodic mud deposition in interdistributary bay and prodelta settings."" (Baird et al., 1985 p.90)",macrofossils,,,,,,NA,,"mold/impression,concretion,soft parts,replaced with other",good,parautochthonous,,,,,,,,NA,,"""Outlines of the limbs can be seen in the matrix, indicating the extent of the soft tissue and the texture of the skin. The bone itself was represented by a very soft, claylike material that had been removed from the hard, ironstone matrix."" (Carroll, & Baird, 1972 p. 323)\r\nBones are replaced by clay minerals such as Kaolinite (Gregory, 1948 p. 637).",taxonomic,"mechanical,survey of museum collection","FMNH,MCZ,USNM,YPM","species names,ichnofossils",,,"R. L. Moodie, P. Turnbull, among others","1871, 1953",,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Spondylerpeton,n. gen.,NA,NA,vertebrate,"R. L. Moodie. 1912. The Pennsylvanic Amphibia of the Mazon Creek, Illinois, Shales. Kansas University Science Bulletin 6(2):232-259",327,697,0,R. Butler,E. Dunne,,26/05/2016 05:43,26/05/2016 05:43,28608,spinatum,Spondylerpeton,30634,n. sp.,311.45,306.95,Westphalian D,,NA,US,Spondylerpeton spinatum
1329857,occ,NA,,179045,members,Neopteroplax conemaughensis,species,137374,,Neopteroplax conemaughensis,NA,species,137374,Romer,1963,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37191,NA,NA,NA,,-80.74485,40.359989,near Reeds Mill,NA,,US,Ohio,Jefferson,based on nearby landmark,6,small collection,"Coordinates based on Reeds Mill, Cross Creek Township, Jefferson County Ohio.",gp_mid,-15.81,-4.29,101,US,,Summerfield limestone,Conemaugh,,,,,,,,,NA,"Summerfield Limestone lies 25 feet below the Pittsburgh coal bed at Summerfield, Ohio, USA (Condit, 1912)",,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Neopteroplax,,NA,NA,vertebrate,A. S. Romer. 1963. The larger embolomerous amphibians of the American Carboniferous. Bulletin of the Museum of Comparative Zoology 128(9):415-454,327,697,0,R. Butler,E. Dunne,,26/05/2016 06:42,26/05/2016 06:42,NA,conemaughensis,Neopteroplax,28726,,306.95,298.9,Stephanian,,NA,US,Neopteroplax conemaughensis
1329858,occ,NA,,175919,members,Neopteroplax relictus ?,species,137377,,Neopteroplax relictus,NA,species,137377,Romer,1963,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37191,NA,NA,NA,,-98.56646,33.102467,"Near Graham, Young County",NA,,US,Texas,Young,based on nearby landmark,6,small collection,"Coordinates based on the city of Graham, Young County, Texas.",gp_mid,-31.84,-4.28,101,US,,,Thrifty,,,,,,,,,NA,"Below Blach Ranch Limestone, Cisco series.",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Neopteroplax,,NA,NA,vertebrate,A. S. Romer. 1963. The larger embolomerous amphibians of the American Carboniferous. Bulletin of the Museum of Comparative Zoology 128(9):415-454,327,697,0,R. Butler,E. Dunne,,26/05/2016 06:54,26/05/2016 06:54,NA,relictus,Neopteroplax,28726,?,306.95,298.9,Stephanian,,NA,US,Neopteroplax relictus
1329859,occ,NA,,178844,members,n. gen. Neopteroplax n. sp. conemaughensis,species,137374,,Neopteroplax conemaughensis,NA,species,137374,Romer,1963,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37191,NA,NA,NA,,-80.820381,40.431633,"Bloomingdale, Jefferson County",NA,,US,Ohio,Jefferson,based on nearby landmark,6,small collection,,gp_mid,-15.84,-4.21,101,US,,,Conemaugh,,,,,,,,,NA,Above Ames Limestone,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,USNM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Neopteroplax,n. gen.,NA,NA,vertebrate,A. S. Romer. 1963. The larger embolomerous amphibians of the American Carboniferous. Bulletin of the Museum of Comparative Zoology 128(9):415-454,327,697,0,R. Butler,E. Dunne,,26/05/2016 07:13,26/05/2016 07:13,NA,conemaughensis,Neopteroplax,28726,n. sp.,306.95,298.9,Stephanian,,NA,US,Neopteroplax conemaughensis
1329869,occ,NA,,176254,members,Palaeogyrinus decorus,species,296846,recombined as,Palaeoherpeton decorum,NA,species,296846,Panchen,1970,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37192,NA,NA,NA,,-1.391069,53.084061,Swanwick Colliery,NA,,UK,England,Derbyshire,based on nearby landmark,6,small collection,In the northern part of the Swanwick Parish an industrial estate on the former Swanwick Colliery site incorporates the Thornton's Confectionery factory along with other businesses.,gp_mid,5.25,-5.66,315,UK,,,Lower Coal Measures,,,,,,,,,NA,,,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Some specimens in NHMUK collection,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Palaeogyrinus,,NA,NA,vertebrate,A. L. Panchen. 1970. Handbuch der Palaoherpetologie / Encyclopedia of Paleoherpetology Teil 5 / Part 5 Batrachosauria Teil A / Part A Anthracosauria. ,327,697,0,R. Butler,E. Dunne,,26/05/2016 09:40,26/05/2016 09:40,NA,decorus,Palaeoherpeton,55380,,318.1,314.6,Westphalian A,,NA,UK,Palaeoherpeton decorus
1329892,occ,NA,,137311,,Pholiderpeton scutigerum,species,229337,,Pholiderpeton scutigerum,NA,species,229337,Panchen,1970,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37193,NA,NA,NA,,-1.76,53.75,"Low-moor, Yorkshire (BMNH)",NA,Low Moor,UK,,,,2,,,gp_mid,8.01,0.12,315,UK,,,,,,,,,,,,NA,Coal measures,,not reported,,lithified,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,BMNH,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Pholiderpeton,,NA,NA,vertebrate,A. L. Panchen. 1970. Handbuch der Palaoherpetologie / Encyclopedia of Paleoherpetology Teil 5 / Part 5 Batrachosauria Teil A / Part A Anthracosauria. ,327,697,0,R. Butler,E. Dunne,,26/05/2016 10:17,26/05/2016 10:17,43905,scutigerum,Pholiderpeton,55380,,315.2,307,Moscovian,,NA,UK,Pholiderpeton scutigerum
1329895,occ,NA,,175922,members,Pholiderpeton scutigerum,species,229337,,Pholiderpeton scutigerum,NA,species,229337,Panchen,1970,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37193,NA,NA,NA,,-3.835925,55.735779,"Castlehill, near Carluke",NA,,UK,Scotland,,,6,,,gp_mid,3.46,-3.24,313,UK,,Lower Coal Measures,,,group of beds,,,,,,,NA,,,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Pholiderpeton,,NA,NA,vertebrate,A. L. Panchen. 1970. Handbuch der Palaoherpetologie / Encyclopedia of Paleoherpetology Teil 5 / Part 5 Batrachosauria Teil A / Part A Anthracosauria. ,327,697,0,R. Butler,E. Dunne,,26/05/2016 10:23,26/05/2016 10:23,NA,scutigerum,Pholiderpeton,55380,,318.1,314.6,Westphalian A,,NA,UK,Pholiderpeton scutigerum
1329897,occ,NA,,176254,members,Pholiderpeton scutigerum,species,229337,,Pholiderpeton scutigerum,NA,species,229337,Panchen,1970,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37193,NA,NA,NA,,-1.391069,53.084061,Swanwick Colliery,NA,,UK,England,Derbyshire,based on nearby landmark,6,small collection,In the northern part of the Swanwick Parish an industrial estate on the former Swanwick Colliery site incorporates the Thornton's Confectionery factory along with other businesses.,gp_mid,5.25,-5.66,315,UK,,,Lower Coal Measures,,,,,,,,,NA,,,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Some specimens in NHMUK collection,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Pholiderpeton,,NA,NA,vertebrate,A. L. Panchen. 1970. Handbuch der Palaoherpetologie / Encyclopedia of Paleoherpetology Teil 5 / Part 5 Batrachosauria Teil A / Part A Anthracosauria. ,327,697,0,R. Butler,E. Dunne,,26/05/2016 10:25,26/05/2016 10:25,NA,scutigerum,Pholiderpeton,55380,,318.1,314.6,Westphalian A,,NA,UK,Pholiderpeton scutigerum
1329900,occ,NA,,176264,members,Eogyrinus attheyi,species,296848,recombined as,Pholiderpeton attheyi,NA,species,296848,Panchen,1970,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37193,NA,NA,NA,,-2.161343,52.999149,"Fenton, Staffordshire",NA,,UK,England,Staffordshire,based on nearby landmark,6,small collection,,gp_mid,3.01,-8.94,315,UK,,,Middle Coal Measures,,,,,,,,,NA,,,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,LIVCM collection,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Eogyrinus,,NA,NA,vertebrate,A. L. Panchen. 1970. Handbuch der Palaoherpetologie / Encyclopedia of Paleoherpetology Teil 5 / Part 5 Batrachosauria Teil A / Part A Anthracosauria. ,327,697,0,R. Butler,E. Dunne,,26/05/2016 10:28,26/05/2016 10:28,NA,attheyi,Pholiderpeton,55380,,323.2,315.2,Bashkirian,,NA,UK,Pholiderpeton attheyi
1329904,occ,NA,,179053,members,Eogyrinus attheyi,species,296848,recombined as,Pholiderpeton attheyi,NA,species,296848,Panchen,1970,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37193,NA,NA,NA,,-3.936014,55.814552,"Newcarthill, Lanarkshire",NA,,UK,Scotland,Lanarkshire,based on nearby landmark,6,small collection,,gp_mid,5.23,-0.07,313,UK,,Middle Coal Measures,,,group of beds,,,,,,,NA,,,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Eogyrinus,,NA,NA,vertebrate,A. L. Panchen. 1970. Handbuch der Palaoherpetologie / Encyclopedia of Paleoherpetology Teil 5 / Part 5 Batrachosauria Teil A / Part A Anthracosauria. ,327,697,0,R. Butler,E. Dunne,,26/05/2016 11:03,26/05/2016 11:03,NA,attheyi,Pholiderpeton,55380,,318.1,306.95,Westphalian,,NA,UK,Pholiderpeton attheyi
1329927,occ,NA,,28067,,Archeria sp.,genus,37196,,Archeria,NA,genus,37196,Panchen,1970,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,,-106.783333,35.716667,"UCMP 39179, Jemez Canyon (Abo Formation)",NA,"Harvard locality, Canyon de San Diego",US,New Mexico,Sandoval,stated in text,minutes,small collection,"4.5 mi south of Jemez Springs, Sandoval County, New Mexico. Western side of the Permian Basin. Lat long is for Jemez Springs.\n"" [...] on east side of Canyon de San Diego, east of State Highway 4, about 4 1/2 miles south of Jemez Springs, approximately lat 35 43' N.; long 106 47' W., Sandoval County, New Mexico"" (Berman, 1977)",gp_mid,-34.43,4.24,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)","""shale""",red,,,Y,sandstone,"coarse,micaceous,red",,,Y,fluvial indet.,non-subsiding area,"""relative abundance of micaceous and coarse arkosic detritus often associated with the bone-beds suggest that these Abo sediments were laid down nearer their source and under conditions of better regional drainage than contemporary ""deltaic"" Wichita rocks in Texas. The late Pennsylvanian and early Permian uplifts of the near-by ""Ancestral Rockies"" were evidently responsible for this early advent of red-bed deposition on the west side of the Permian Basin...""",macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,field collection,UCMP,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,,NA,NA,vertebrate,A. L. Panchen. 1970. Handbuch der Palaoherpetologie / Encyclopedia of Paleoherpetology Teil 5 / Part 5 Batrachosauria Teil A / Part A Anthracosauria. ,327,697,0,R. Butler,E. Dunne,,27/05/2016 05:39,27/05/2016 05:39,43845,sp.,Archeria,55380,,296.4,268,Wolfcamp,,NA,US,Archeria sp.
1330336,occ,NA,,179127,members,n. gen. Branchiosaurus n. sp. credneri,species,229334,recombined as,Micromelerpeton credneri,NA,species,229334,Bulman and Whittard,1926,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Micromelerpetontidae,37041,37044,NA,NA,NA,,7.702733,49.75246,Vineyards south of Odernheim am Glan,NA,"Odernheimer Kalkbank, M8)",DE,Rheinland-Pfalz,Bad Kreuznach,based on nearby landmark,6,small collection,Coordinates based on location south of Obernheim am Glan next to Glan river where vineyards are visible on a satellite image.,gp_mid,19.75,5.16,315,DE,,Meisenheim,,,group of beds,,Obernheim beds,Obernheim beds,,,,NA,"Meisenheim Formation (M6-M10), Saar-Nahe Basin, Germany\r\nObernheimer Kalkbank (""limestone bank"") M8",,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchiosaurus,n. gen.,NA,NA,vertebrate,O. M. B. Bulman and W. F. Whittard. 1926. On Branchiosaurus and allied genera. Proceedings of the Zoological Society of London 1926:533-579,327,697,0,R. Butler,E. Dunne,,31/05/2016 11:11,31/05/2016 11:11,NA,credneri,Micromelerpeton,59275,n. sp.,298.9,295,Autunian,,NA,DE,Micromelerpeton credneri
1330421,occ,NA,,176535,members,Melanerpeton n. sp. tener,species,229329,recombined as,Leptorophus tener,NA,species,229329,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,229328,NA,NA,NA,,12.925204,51.199074,"Clennen, Saxony",NA,,DE,Mittelsachsen,Bockelwitz,based on nearby landmark,6,small collection,"Coordinates based on the location of Clennen, a small populated area in Saxony, Germany.",gp_mid,22.57,7.46,305,DE,,Bortewitz,,,group of beds,,Clennen tuffite,Clennen tuffite,,,,NA,B̦rtewitz Formation,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Melanerpeton,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,01/06/2016 06:39,01/06/2016 06:39,NA,tener,Leptorophus,57795,n. sp.,298.9,295,Autunian,,NA,DE,Leptorophus tener
1330422,occ,NA,,80784,,n. gen. Hesperoherpeton n. sp. garnettense,species,320979,nomen dubium,Temnospondyli,NA,unranked clade,36320,Peabody,1958,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,NA,NA,NA,NA,,-95.259048,38.378502,Garnett Quarry,NA,"Garnett Vertebrate Fauna, Charles Hardesty farm",US,Kansas,Anderson,estimated from map,6,outcrop,"""6 miles northwest of Garnett"" (Reisz, 1986); ""NW 1/4, NE 1/4, sec. 5, tp. 20 S, rge. 19 E, Putnam Township, Anderson County, Kansas"" (Reisz & Berman, 1986)\r\n""Charles A. Hardest farm, NW/4 NE/4 sec. 5 T20S R19E, Putnam Township, Anderson County, Kansas. The Universal Transverse Mercantor (UTM) coordinates of the quarry are 15STN963466. Locality is close to Garnett, Kansas."" (Laurin 1993). ",gp_mid,-27.44,-2.3,101,US,,Stanton,Lansing,Rock Lake Shale,group of beds,,,,,,,NA,"""Rock Lake Member, Stanton Formation, Lansing Group, Missourian Series, Upper Pennsylvanian"" (Reisz & Berman, 1996)\r\nall vertebrate remains seem to come exclusively from the basal part of the Rock Lake Shale (see Reisz et al., 1982)","""dark greyishbrown, moderately well bedded, very carbonaceous, calcareous mudstone"" (Reisz et al., 1982)",mudstone,brown,,"calcareous,carbonaceous",Y,,,,,,fine channel fill,foreland basin,"""The Rock Lake Shale is a rather thin but otherwise typical ۪outside۪ shale of a ۪Kansas Megacyclothem۪ sequence formed as a change from regressive to transgressive conditions occurred [...] The site is located along the western edge of what was, during the Late Pennsylvanian, a shallow, forested stream valley or channel that was eroded into a limestone coastal plain during the latter stages of a major eustatic fall in sea level. As the succeeding rise in sea level occurred, the valley was gradually flooded by estuarine waters"" (Reisz et al., 1982).\r\nSequence stratigraphy is interpreted from the description given by Reisz et al. (1982). The surface of the underlying limestone is the sequence boundary merged with the transgressive surface and the Lake Rock Shale is the basalmost deposit of the transgressive systems tract.",macrofossils,some,some,,,,NA,,body,good,,snapshot,,,,,,,NA,,,taxonomic,"bulk,mechanical",ROM,,,,"F. E. Peabody, R. Camp, R. L. Carroll, R. R. Reisz, M. J. Heaton, B. R. Pynn, G. MacDonald","1953-1956, 1965, 1980, 1981",,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Hesperoherpeton,n. gen.,NA,NA,vertebrate,F. E. Peabody. 1958. An embolomerous amphibian in the Garnett fauna (Pennsylvanian) of Kansas. Journal of Paleontology 32:571-573,327,697,0,R. Butler,E. Dunne,,01/06/2016 06:50,01/06/2016 06:50,28862,garnettense,,59289,n. sp.,305.9,303.4,Missourian,,NA,US, garnettense
1332794,occ,NA,,179595,members,n. gen. Acroplous n. sp. vorax,species,255215,,Acroplous vorax,NA,species,255215,Hotton,1959,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eobrachyopidae,150302,36981,NA,NA,NA,,-96.709267,39.225281,"Keats, Riley County",NA,,US,Kansas,Riley,based on nearby landmark,6,small collection,"Coordinates based on the location of Keats, Riley County, Kansas.\r\n""Streamcut in SE 1/4, SW 1/4, NE 1/4, Sec. 36, T9S, R6E, near Keats, Riley County, Kansas"" Foreman (1990)",gp_mid,-26,2.37,101,US,,Speiser Shale,Council Grove,,,,,,,,,NA,,,"""shale""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,KUVP collections,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Acroplous,n. gen.,NA,NA,vertebrate,"N. Hotton. 1959. Acroplous vorax, a new and unusual labyrinthodont amphibian from the Kansas Permian. Journal of Paleontology 33:161-178",327,697,697,R. Butler,E. Dunne,E. Dunne,21/06/2016 11:14,21/06/2016 11:16,NA,vorax,Acroplous,59481,n. sp.,295.5,290.1,Sakmarian,,NA,US,Acroplous vorax
1332972,occ,NA,,162676,,Acroplous vorax,species,255215,,Acroplous vorax,NA,species,255215,Huttenlocker et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eobrachyopidae,150302,36981,NA,NA,NA,,-95.884819,40.139584,Raney Farm,NA,"Location 2, near Humboldt (DMNH loc. 2075, UNSM loc. Rh 104)",US,Nebraska,Richardson,stated in text,6,outcrop,"Location 2 of 3 fossil-bearing locations approximately 2 miles east of Humboldt, Nebraska. For map see Huttenlocker et al. (2005).",gp_mid,-25.19,2.48,101,US,,Eskridge,Council Grove,,bed,,,,,,,NA,"Within the lower P2 paleosol. This unit lies well above the first occurrence of the Permian index fossil Streptognathodus isolatus in the Bennet Shale Member of the Red Eagle Limestone but is below the first occurrence of the Sakmarian indicator species Sweetognathus merrilli in the Eiss Limestone member of the Bader Limestone, constraining the age to the Asselian (298.9295.0 Ma).",Greyish-green vertisol with moderate pedogenesis,siltstone,"gray,green",lithified,,,,,,,,pond,,Ephemeral pond setting,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,UNSM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Acroplous,,NA,NA,vertebrate,"A. K. Huttenlocker, J. D. Pardo, and B. J. Small. 2005. An earliest Permian nonmarine vertebrate assemblage from the Eskridge Formation, Nebraska. New Mexico Museum of Natural History and Science, Bulletin 30:133-143",327,697,0,R. Butler,E. Dunne,,22/06/2016 06:51,22/06/2016 06:51,52964,vorax,Acroplous,59496,,298.9,295.5,Asselian,,NA,US,Acroplous vorax
1332973,occ,NA,,162676,,Trimerorhachidae indet.,family,36985,,Trimerorhachidae,NA,family,36985,Huttenlocker et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,NA,NA,NA,NA,,-95.884819,40.139584,Raney Farm,NA,"Location 2, near Humboldt (DMNH loc. 2075, UNSM loc. Rh 104)",US,Nebraska,Richardson,stated in text,6,outcrop,"Location 2 of 3 fossil-bearing locations approximately 2 miles east of Humboldt, Nebraska. For map see Huttenlocker et al. (2005).",gp_mid,-25.19,2.48,101,US,,Eskridge,Council Grove,,bed,,,,,,,NA,"Within the lower P2 paleosol. This unit lies well above the first occurrence of the Permian index fossil Streptognathodus isolatus in the Bennet Shale Member of the Red Eagle Limestone but is below the first occurrence of the Sakmarian indicator species Sweetognathus merrilli in the Eiss Limestone member of the Bader Limestone, constraining the age to the Asselian (298.9295.0 Ma).",Greyish-green vertisol with moderate pedogenesis,siltstone,"gray,green",lithified,,,,,,,,pond,,Ephemeral pond setting,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,UNSM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachidae,,NA,NA,vertebrate,"A. K. Huttenlocker, J. D. Pardo, and B. J. Small. 2005. An earliest Permian nonmarine vertebrate assemblage from the Eskridge Formation, Nebraska. New Mexico Museum of Natural History and Science, Bulletin 30:133-143",327,697,0,R. Butler,E. Dunne,,22/06/2016 06:51,22/06/2016 06:51,52964,indet.,,59496,,298.9,295.5,Asselian,,NA,US, indet.
1332974,occ,NA,,162676,,Temnospondyli indet.,unranked clade,204050,,Temnospondyli,NA,unranked clade,36320,Huttenlocker et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,NA,NA,NA,NA,,-95.884819,40.139584,Raney Farm,NA,"Location 2, near Humboldt (DMNH loc. 2075, UNSM loc. Rh 104)",US,Nebraska,Richardson,stated in text,6,outcrop,"Location 2 of 3 fossil-bearing locations approximately 2 miles east of Humboldt, Nebraska. For map see Huttenlocker et al. (2005).",gp_mid,-25.19,2.48,101,US,,Eskridge,Council Grove,,bed,,,,,,,NA,"Within the lower P2 paleosol. This unit lies well above the first occurrence of the Permian index fossil Streptognathodus isolatus in the Bennet Shale Member of the Red Eagle Limestone but is below the first occurrence of the Sakmarian indicator species Sweetognathus merrilli in the Eiss Limestone member of the Bader Limestone, constraining the age to the Asselian (298.9295.0 Ma).",Greyish-green vertisol with moderate pedogenesis,siltstone,"gray,green",lithified,,,,,,,,pond,,Ephemeral pond setting,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,UNSM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Temnospondyli,,NA,NA,vertebrate,"A. K. Huttenlocker, J. D. Pardo, and B. J. Small. 2005. An earliest Permian nonmarine vertebrate assemblage from the Eskridge Formation, Nebraska. New Mexico Museum of Natural History and Science, Bulletin 30:133-143",327,697,697,R. Butler,E. Dunne,E. Dunne,22/06/2016 06:51,22/06/2016 06:52,52964,indet.,,59496,,298.9,295.5,Asselian,,NA,US, indet.
1332975,occ,NA,,162676,,Brachydectes indet.,genus,227167,,Brachydectes,NA,genus,227167,Huttenlocker et al.,2005,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,Cocytinidae,320813,227167,NA,NA,NA,,-95.884819,40.139584,Raney Farm,NA,"Location 2, near Humboldt (DMNH loc. 2075, UNSM loc. Rh 104)",US,Nebraska,Richardson,stated in text,6,outcrop,"Location 2 of 3 fossil-bearing locations approximately 2 miles east of Humboldt, Nebraska. For map see Huttenlocker et al. (2005).",gp_mid,-25.19,2.48,101,US,,Eskridge,Council Grove,,bed,,,,,,,NA,"Within the lower P2 paleosol. This unit lies well above the first occurrence of the Permian index fossil Streptognathodus isolatus in the Bennet Shale Member of the Red Eagle Limestone but is below the first occurrence of the Sakmarian indicator species Sweetognathus merrilli in the Eiss Limestone member of the Bader Limestone, constraining the age to the Asselian (298.9295.0 Ma).",Greyish-green vertisol with moderate pedogenesis,siltstone,"gray,green",lithified,,,,,,,,pond,,Ephemeral pond setting,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,UNSM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Brachydectes,,NA,NA,vertebrate,"A. K. Huttenlocker, J. D. Pardo, and B. J. Small. 2005. An earliest Permian nonmarine vertebrate assemblage from the Eskridge Formation, Nebraska. New Mexico Museum of Natural History and Science, Bulletin 30:133-143",327,697,697,R. Butler,E. Dunne,E. Dunne,22/06/2016 06:51,22/06/2016 06:52,52964,indet.,Brachydectes,59496,,298.9,295.5,Asselian,,NA,US,Brachydectes indet.
1332976,occ,NA,,162676,,Edaphosauridae indet.,family,38910,,Edaphosauridae,NA,family,38910,Huttenlocker et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,NA,NA,NA,NA,,-95.884819,40.139584,Raney Farm,NA,"Location 2, near Humboldt (DMNH loc. 2075, UNSM loc. Rh 104)",US,Nebraska,Richardson,stated in text,6,outcrop,"Location 2 of 3 fossil-bearing locations approximately 2 miles east of Humboldt, Nebraska. For map see Huttenlocker et al. (2005).",gp_mid,-25.19,2.48,101,US,,Eskridge,Council Grove,,bed,,,,,,,NA,"Within the lower P2 paleosol. This unit lies well above the first occurrence of the Permian index fossil Streptognathodus isolatus in the Bennet Shale Member of the Red Eagle Limestone but is below the first occurrence of the Sakmarian indicator species Sweetognathus merrilli in the Eiss Limestone member of the Bader Limestone, constraining the age to the Asselian (298.9295.0 Ma).",Greyish-green vertisol with moderate pedogenesis,siltstone,"gray,green",lithified,,,,,,,,pond,,Ephemeral pond setting,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,UNSM,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosauridae,,NA,NA,vertebrate,"A. K. Huttenlocker, J. D. Pardo, and B. J. Small. 2005. An earliest Permian nonmarine vertebrate assemblage from the Eskridge Formation, Nebraska. New Mexico Museum of Natural History and Science, Bulletin 30:133-143",327,697,0,R. Butler,E. Dunne,,22/06/2016 06:51,22/06/2016 06:51,52964,indet.,,59496,,298.9,295.5,Asselian,,NA,US, indet.
1332980,occ,NA,,179619,members,Temnospondyli indet.,unranked clade,204050,,Temnospondyli,NA,unranked clade,36320,Huttenlocker et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,NA,NA,NA,NA,,-95.875076,40.145981,Shot in the Dark Quarry,NA,"Location 3, near Humboldt (DMNH loc.2077, UNSM loc. Rh 102)",US,Nebraska,Richardson,stated in text,6,outcrop,"Location 3 of 3 fossil-bearing locations approximately 2 miles east of Humboldt, Nebraska. For map see Huttenlocker et al. (2005).",gp_mid,-25.18,2.48,101,US,,Eskridge,Council Grove,,bed,,,,,,,NA,"Within the lower P2 paleosol. This unit lies well above the first occurrence of the Permian index fossil Streptognathodus isolatus in the Bennet Shale Member of the Red Eagle Limestone but is below the first occurrence of the Sakmarian indicator species Sweetognathus merrilli in the Eiss Limestone member of the Bader Limestone, constraining the age to the Asselian (298.9295.0 Ma).",Greyish-green vertisol with moderate pedogenesis,siltstone,"gray,green",lithified,,,,,,,,pond,,Ephemeral pond setting,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"DMNH,UNSM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Temnospondyli,,NA,NA,vertebrate,"A. K. Huttenlocker, J. D. Pardo, and B. J. Small. 2005. An earliest Permian nonmarine vertebrate assemblage from the Eskridge Formation, Nebraska. New Mexico Museum of Natural History and Science, Bulletin 30:133-143",327,697,697,R. Butler,E. Dunne,E. Dunne,22/06/2016 06:55,22/06/2016 06:55,NA,indet.,,59496,,298.9,295.5,Asselian,,NA,US, indet.
1332981,occ,NA,,179619,members,Brachydectes elongatus,species,229311,,Brachydectes elongatus,NA,species,229311,Huttenlocker et al.,2005,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,Cocytinidae,320813,227167,NA,NA,NA,,-95.875076,40.145981,Shot in the Dark Quarry,NA,"Location 3, near Humboldt (DMNH loc.2077, UNSM loc. Rh 102)",US,Nebraska,Richardson,stated in text,6,outcrop,"Location 3 of 3 fossil-bearing locations approximately 2 miles east of Humboldt, Nebraska. For map see Huttenlocker et al. (2005).",gp_mid,-25.18,2.48,101,US,,Eskridge,Council Grove,,bed,,,,,,,NA,"Within the lower P2 paleosol. This unit lies well above the first occurrence of the Permian index fossil Streptognathodus isolatus in the Bennet Shale Member of the Red Eagle Limestone but is below the first occurrence of the Sakmarian indicator species Sweetognathus merrilli in the Eiss Limestone member of the Bader Limestone, constraining the age to the Asselian (298.9295.0 Ma).",Greyish-green vertisol with moderate pedogenesis,siltstone,"gray,green",lithified,,,,,,,,pond,,Ephemeral pond setting,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"DMNH,UNSM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Brachydectes,,NA,NA,vertebrate,"A. K. Huttenlocker, J. D. Pardo, and B. J. Small. 2005. An earliest Permian nonmarine vertebrate assemblage from the Eskridge Formation, Nebraska. New Mexico Museum of Natural History and Science, Bulletin 30:133-143",327,697,0,R. Butler,E. Dunne,,22/06/2016 06:55,22/06/2016 06:55,NA,elongatus,Brachydectes,59496,,298.9,295.5,Asselian,,NA,US,Brachydectes elongatus
1332982,occ,NA,,179619,members,Brachydectes indet.,genus,227167,,Brachydectes,NA,genus,227167,Huttenlocker et al.,2005,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,Cocytinidae,320813,227167,NA,NA,NA,,-95.875076,40.145981,Shot in the Dark Quarry,NA,"Location 3, near Humboldt (DMNH loc.2077, UNSM loc. Rh 102)",US,Nebraska,Richardson,stated in text,6,outcrop,"Location 3 of 3 fossil-bearing locations approximately 2 miles east of Humboldt, Nebraska. For map see Huttenlocker et al. (2005).",gp_mid,-25.18,2.48,101,US,,Eskridge,Council Grove,,bed,,,,,,,NA,"Within the lower P2 paleosol. This unit lies well above the first occurrence of the Permian index fossil Streptognathodus isolatus in the Bennet Shale Member of the Red Eagle Limestone but is below the first occurrence of the Sakmarian indicator species Sweetognathus merrilli in the Eiss Limestone member of the Bader Limestone, constraining the age to the Asselian (298.9295.0 Ma).",Greyish-green vertisol with moderate pedogenesis,siltstone,"gray,green",lithified,,,,,,,,pond,,Ephemeral pond setting,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"DMNH,UNSM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Brachydectes,,NA,NA,vertebrate,"A. K. Huttenlocker, J. D. Pardo, and B. J. Small. 2005. An earliest Permian nonmarine vertebrate assemblage from the Eskridge Formation, Nebraska. New Mexico Museum of Natural History and Science, Bulletin 30:133-143",327,697,697,R. Butler,E. Dunne,E. Dunne,22/06/2016 06:55,22/06/2016 06:55,NA,indet.,Brachydectes,59496,,298.9,295.5,Asselian,,NA,US,Brachydectes indet.
1332987,occ,NA,,179620,members,Acroplous vorax,species,255215,,Acroplous vorax,NA,species,255215,Huttenlocker et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eobrachyopidae,150302,36981,NA,NA,NA,,-95.896446,40.147099,Mayer Farm,NA,"Location 1, near Humboldt (DMNH loc. 2076, UNSM loc. Rh 103)",US,Nebraska,Richardson,stated in text,6,outcrop,"Location 1 of 3 fossil-bearing locations approximately 2 miles east of Humboldt, Nebraska. For map see Huttenlocker et al. (2005).",gp_mid,-25.19,2.49,101,US,,Eskridge,Council Grove,,bed,,,,,,,NA,"Within the lower P2 paleosol. This unit lies well above the first occurrence of the Permian index fossil Streptognathodus isolatus in the Bennet Shale Member of the Red Eagle Limestone but is below the first occurrence of the Sakmarian indicator species Sweetognathus merrilli in the Eiss Limestone member of the Bader Limestone, constraining the age to the Asselian (298.9295.0 Ma).",Greyish-green vertisol with moderate pedogenesis,siltstone,"gray,green",lithified,,,,,,,,pond,,Ephemeral pond setting,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"DMNH,UNSM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Acroplous,,NA,NA,vertebrate,"A. K. Huttenlocker, J. D. Pardo, and B. J. Small. 2005. An earliest Permian nonmarine vertebrate assemblage from the Eskridge Formation, Nebraska. New Mexico Museum of Natural History and Science, Bulletin 30:133-143",327,697,0,R. Butler,E. Dunne,,22/06/2016 07:00,22/06/2016 07:00,NA,vorax,Acroplous,59496,,298.9,295.5,Asselian,,NA,US,Acroplous vorax
1332988,occ,NA,,179620,members,Temnospondyli indet.,unranked clade,204050,,Temnospondyli,NA,unranked clade,36320,Huttenlocker et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,NA,NA,NA,NA,,-95.896446,40.147099,Mayer Farm,NA,"Location 1, near Humboldt (DMNH loc. 2076, UNSM loc. Rh 103)",US,Nebraska,Richardson,stated in text,6,outcrop,"Location 1 of 3 fossil-bearing locations approximately 2 miles east of Humboldt, Nebraska. For map see Huttenlocker et al. (2005).",gp_mid,-25.19,2.49,101,US,,Eskridge,Council Grove,,bed,,,,,,,NA,"Within the lower P2 paleosol. This unit lies well above the first occurrence of the Permian index fossil Streptognathodus isolatus in the Bennet Shale Member of the Red Eagle Limestone but is below the first occurrence of the Sakmarian indicator species Sweetognathus merrilli in the Eiss Limestone member of the Bader Limestone, constraining the age to the Asselian (298.9295.0 Ma).",Greyish-green vertisol with moderate pedogenesis,siltstone,"gray,green",lithified,,,,,,,,pond,,Ephemeral pond setting,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"DMNH,UNSM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Temnospondyli,,NA,NA,vertebrate,"A. K. Huttenlocker, J. D. Pardo, and B. J. Small. 2005. An earliest Permian nonmarine vertebrate assemblage from the Eskridge Formation, Nebraska. New Mexico Museum of Natural History and Science, Bulletin 30:133-143",327,697,697,R. Butler,E. Dunne,E. Dunne,22/06/2016 07:00,22/06/2016 07:00,NA,indet.,,59496,,298.9,295.5,Asselian,,NA,US, indet.
1332989,occ,NA,,179620,members,Amphibamidae sp.,genus,123081,,Amphibamidae,NA,family,123081,Huttenlocker et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,NA,NA,NA,NA,,-95.896446,40.147099,Mayer Farm,NA,"Location 1, near Humboldt (DMNH loc. 2076, UNSM loc. Rh 103)",US,Nebraska,Richardson,stated in text,6,outcrop,"Location 1 of 3 fossil-bearing locations approximately 2 miles east of Humboldt, Nebraska. For map see Huttenlocker et al. (2005).",gp_mid,-25.19,2.49,101,US,,Eskridge,Council Grove,,bed,,,,,,,NA,"Within the lower P2 paleosol. This unit lies well above the first occurrence of the Permian index fossil Streptognathodus isolatus in the Bennet Shale Member of the Red Eagle Limestone but is below the first occurrence of the Sakmarian indicator species Sweetognathus merrilli in the Eiss Limestone member of the Bader Limestone, constraining the age to the Asselian (298.9295.0 Ma).",Greyish-green vertisol with moderate pedogenesis,siltstone,"gray,green",lithified,,,,,,,,pond,,Ephemeral pond setting,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"DMNH,UNSM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Amphibamidae,,NA,NA,vertebrate,"A. K. Huttenlocker, J. D. Pardo, and B. J. Small. 2005. An earliest Permian nonmarine vertebrate assemblage from the Eskridge Formation, Nebraska. New Mexico Museum of Natural History and Science, Bulletin 30:133-143",327,697,0,R. Butler,E. Dunne,,22/06/2016 07:00,22/06/2016 07:00,NA,sp.,,59496,,298.9,295.5,Asselian,,NA,US, sp.
1332990,occ,NA,,179620,members,Brachydectes elongatus,species,229311,,Brachydectes elongatus,NA,species,229311,Huttenlocker et al.,2005,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,Cocytinidae,320813,227167,NA,NA,NA,,-95.896446,40.147099,Mayer Farm,NA,"Location 1, near Humboldt (DMNH loc. 2076, UNSM loc. Rh 103)",US,Nebraska,Richardson,stated in text,6,outcrop,"Location 1 of 3 fossil-bearing locations approximately 2 miles east of Humboldt, Nebraska. For map see Huttenlocker et al. (2005).",gp_mid,-25.19,2.49,101,US,,Eskridge,Council Grove,,bed,,,,,,,NA,"Within the lower P2 paleosol. This unit lies well above the first occurrence of the Permian index fossil Streptognathodus isolatus in the Bennet Shale Member of the Red Eagle Limestone but is below the first occurrence of the Sakmarian indicator species Sweetognathus merrilli in the Eiss Limestone member of the Bader Limestone, constraining the age to the Asselian (298.9295.0 Ma).",Greyish-green vertisol with moderate pedogenesis,siltstone,"gray,green",lithified,,,,,,,,pond,,Ephemeral pond setting,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"DMNH,UNSM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Brachydectes,,NA,NA,vertebrate,"A. K. Huttenlocker, J. D. Pardo, and B. J. Small. 2005. An earliest Permian nonmarine vertebrate assemblage from the Eskridge Formation, Nebraska. New Mexico Museum of Natural History and Science, Bulletin 30:133-143",327,697,0,R. Butler,E. Dunne,,22/06/2016 07:00,22/06/2016 07:00,NA,elongatus,Brachydectes,59496,,298.9,295.5,Asselian,,NA,US,Brachydectes elongatus
1332991,occ,NA,,179620,members,Brachydectes newberryi,species,229312,,Brachydectes newberryi,NA,species,229312,Huttenlocker et al.,2005,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,Cocytinidae,320813,227167,NA,NA,NA,,-95.896446,40.147099,Mayer Farm,NA,"Location 1, near Humboldt (DMNH loc. 2076, UNSM loc. Rh 103)",US,Nebraska,Richardson,stated in text,6,outcrop,"Location 1 of 3 fossil-bearing locations approximately 2 miles east of Humboldt, Nebraska. For map see Huttenlocker et al. (2005).",gp_mid,-25.19,2.49,101,US,,Eskridge,Council Grove,,bed,,,,,,,NA,"Within the lower P2 paleosol. This unit lies well above the first occurrence of the Permian index fossil Streptognathodus isolatus in the Bennet Shale Member of the Red Eagle Limestone but is below the first occurrence of the Sakmarian indicator species Sweetognathus merrilli in the Eiss Limestone member of the Bader Limestone, constraining the age to the Asselian (298.9295.0 Ma).",Greyish-green vertisol with moderate pedogenesis,siltstone,"gray,green",lithified,,,,,,,,pond,,Ephemeral pond setting,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"DMNH,UNSM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Brachydectes,,NA,NA,vertebrate,"A. K. Huttenlocker, J. D. Pardo, and B. J. Small. 2005. An earliest Permian nonmarine vertebrate assemblage from the Eskridge Formation, Nebraska. New Mexico Museum of Natural History and Science, Bulletin 30:133-143",327,697,0,R. Butler,E. Dunne,,22/06/2016 07:00,22/06/2016 07:00,NA,newberryi,Brachydectes,59496,,298.9,295.5,Asselian,,NA,US,Brachydectes newberryi
1332992,occ,NA,,179620,members,Microsauria sp.,genus,37278,,Microsauria,NA,unranked clade,37278,Huttenlocker et al.,2005,Chordata,33815,Osteichthyes,34881,Microsauria,37278,,NA,NA,NA,NA,NA,,-95.896446,40.147099,Mayer Farm,NA,"Location 1, near Humboldt (DMNH loc. 2076, UNSM loc. Rh 103)",US,Nebraska,Richardson,stated in text,6,outcrop,"Location 1 of 3 fossil-bearing locations approximately 2 miles east of Humboldt, Nebraska. For map see Huttenlocker et al. (2005).",gp_mid,-25.19,2.49,101,US,,Eskridge,Council Grove,,bed,,,,,,,NA,"Within the lower P2 paleosol. This unit lies well above the first occurrence of the Permian index fossil Streptognathodus isolatus in the Bennet Shale Member of the Red Eagle Limestone but is below the first occurrence of the Sakmarian indicator species Sweetognathus merrilli in the Eiss Limestone member of the Bader Limestone, constraining the age to the Asselian (298.9295.0 Ma).",Greyish-green vertisol with moderate pedogenesis,siltstone,"gray,green",lithified,,,,,,,,pond,,Ephemeral pond setting,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"DMNH,UNSM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Microsauria,,NA,NA,vertebrate,"A. K. Huttenlocker, J. D. Pardo, and B. J. Small. 2005. An earliest Permian nonmarine vertebrate assemblage from the Eskridge Formation, Nebraska. New Mexico Museum of Natural History and Science, Bulletin 30:133-143",327,697,697,R. Butler,E. Dunne,E. Dunne,22/06/2016 07:00,22/06/2016 07:00,NA,sp.,,59496,,298.9,295.5,Asselian,,NA,US, sp.
1332993,occ,NA,,179620,members,Diadectidae indet.,family,37246,,Diadectidae,NA,family,37246,Huttenlocker et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,NA,NA,NA,NA,,-95.896446,40.147099,Mayer Farm,NA,"Location 1, near Humboldt (DMNH loc. 2076, UNSM loc. Rh 103)",US,Nebraska,Richardson,stated in text,6,outcrop,"Location 1 of 3 fossil-bearing locations approximately 2 miles east of Humboldt, Nebraska. For map see Huttenlocker et al. (2005).",gp_mid,-25.19,2.49,101,US,,Eskridge,Council Grove,,bed,,,,,,,NA,"Within the lower P2 paleosol. This unit lies well above the first occurrence of the Permian index fossil Streptognathodus isolatus in the Bennet Shale Member of the Red Eagle Limestone but is below the first occurrence of the Sakmarian indicator species Sweetognathus merrilli in the Eiss Limestone member of the Bader Limestone, constraining the age to the Asselian (298.9295.0 Ma).",Greyish-green vertisol with moderate pedogenesis,siltstone,"gray,green",lithified,,,,,,,,pond,,Ephemeral pond setting,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"DMNH,UNSM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectidae,,NA,NA,vertebrate,"A. K. Huttenlocker, J. D. Pardo, and B. J. Small. 2005. An earliest Permian nonmarine vertebrate assemblage from the Eskridge Formation, Nebraska. New Mexico Museum of Natural History and Science, Bulletin 30:133-143",327,697,697,R. Butler,E. Dunne,E. Dunne,22/06/2016 07:00,22/06/2016 07:00,NA,indet.,,59496,,298.9,295.5,Asselian,,NA,US, indet.
1333239,occ,NA,,179644,members,n. gen. Micromelerpeton n. sp. ulmetense,species,343368,,Micromelerpeton ulmetense,NA,species,343368,Boy,2002,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Micromelerpetontidae,37041,37044,NA,NA,NA,,7.466911,49.588936,"Locality S1, Ulmet",NA,,DE,Rhineland-Pfalz,Kusel district,based on nearby landmark,6,,"Coordinates based on the location of Ulmet, Phineland-Pflaz, Germany",gp_mid,19.13,4.25,315,DE,,Meisenheim,Glan,,group of beds,,Ulmet Lake beds,Ulmet Lake beds,,,,NA,"Saar-Nahe basin, Lower Meisenheim",,not reported,,,,,,,,,,lacustrine deltaic indet.,,"Site represents a lake with distinct deltaic influence and a very low-diversity, detritus-based community (Boy, 2002)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,Boy,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Micromelerpeton,n. gen.,NA,NA,vertebrate,J. A. Boy. 2002. ber die Mircomelerpetonidae (Amphibia: Temnospondyli). 2. Micromelerpeton ulmetense n. sp. und Micromelerpeton(?) boyi Heyler. Neues Jahrbuch f_r Geologie und Pal_ontologie Abhandlungen 223:241-274,327,697,0,R. Butler,E. Dunne,,23/06/2016 07:11,23/06/2016 07:11,NA,ulmetense,Micromelerpeton,59510,n. sp.,303.7,298.9,Gzhelian,,NA,DE,Micromelerpeton ulmetense
1333888,occ,NA,,179620,members,n. gen. Plemmyradytes n. sp. shintoni,species,344178,,Plemmyradytes shintoni,NA,species,344178,Huttenlocker et al.,2007,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,193398,NA,NA,NA,,-95.896446,40.147099,Mayer Farm,NA,"Location 1, near Humboldt (DMNH loc. 2076, UNSM loc. Rh 103)",US,Nebraska,Richardson,stated in text,6,outcrop,"Location 1 of 3 fossil-bearing locations approximately 2 miles east of Humboldt, Nebraska. For map see Huttenlocker et al. (2005).",gp_mid,-25.19,2.49,101,US,,Eskridge,Council Grove,,bed,,,,,,,NA,"Within the lower P2 paleosol. This unit lies well above the first occurrence of the Permian index fossil Streptognathodus isolatus in the Bennet Shale Member of the Red Eagle Limestone but is below the first occurrence of the Sakmarian indicator species Sweetognathus merrilli in the Eiss Limestone member of the Bader Limestone, constraining the age to the Asselian (298.9295.0 Ma).",Greyish-green vertisol with moderate pedogenesis,siltstone,"gray,green",lithified,,,,,,,,pond,,Ephemeral pond setting,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"DMNH,UNSM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Plemmyradytes,n. gen.,NA,NA,vertebrate,"A. K. Huttenlocker, J. D. Pardo, and B. K. Small. 2007. Plemmyradytes shintoni, gen. et sp. nov., an Early Permian amphibian (Temnospondyli: Dissorophoidea) from the Eskridge Formation, Nebraska. Journal of Vertebrate Paleontology 27:316-328",327,697,0,R. Butler,E. Dunne,,29/06/2016 07:48,29/06/2016 07:48,NA,shintoni,Plemmyradytes,59594,n. sp.,298.9,295.5,Asselian,,NA,US,Plemmyradytes shintoni
1334848,occ,NA,,179596,members,n. gen. Fedexia n. sp. striegeli,species,344537,,Fedexia striegeli,NA,species,344537,Berman et al.,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,344536,NA,NA,NA,,-80.147697,40.521099,24km NW of Pittsburgh,NA,Fedexia site,US,Pennsylvania,Allegheny,estimated from map,4,small collection,"Coordinates based on the location stated in Berman et al. (2010) as ""road cut about 24km northwest of Pittsburgh that exposes a 120m section of the Casselman Formation""",gp_mid,-14.69,-3.18,101,US,,Casselman,Conemaugh,,bed,,Birmingham Shale,Birmingham Shale,,,,NA,Horizon determined using geochemical analysis,,"""limestone""",,,,,,,,,,terrestrial indet.,,Freshwater limestone,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,CM,,,,,2004,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Fedexia,n. gen.,NA,NA,vertebrate,"D. S. Berman, A. C. Henrici, and D. K. Brezinki, A. D. Kollar. 2010. A new trematopid amphibian (Temnospondyli: Dissorophoidea) from the Upper Pennsylvanian of western Pennsylvania:earliest record of terrestrial vertebrates responding to a warmer, dryer climate. Annals of Carnegie Museum 78:289-318",327,697,0,R. Butler,E. Dunne,,04/07/2016 04:53,04/07/2016 04:53,NA,striegeli,Fedexia,59692,n. sp.,303.4,298.9,Virgilian,,NA,US,Fedexia striegeli
1334849,occ,NA,,79162,,Dissorophus n. sp. augustus,species,344540,subjective synonym of,Broiliellus brevis,NA,species,229313,Carroll,1964,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37024,NA,NA,NA,specimens,-98.650002,33.583332,Archer City Bonebed 1 (Putnam Fm.),NA,"Locality IIIf (Romer & Price, 1940)",US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Dissorophus,,NA,NA,vertebrate,R. L. Carroll. 1964. Early evolution of the dissorophid amphibians. Bulletin of the Museum of Comparative Zoology 131:161-250,327,697,697,R. Butler,E. Dunne,E. Dunne,04/07/2016 06:11,24/08/2016 05:22,43845,augustus,Broiliellus,59694,n. sp.,296.4,268,Wolfcamp,,1,US,Broiliellus augustus
1334850,occ,NA,,79162,,Broiliellus n. sp. brevis,species,229313,,Broiliellus brevis,NA,species,229313,Carroll,1964,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37024,NA,NA,NA,specimens,-98.650002,33.583332,Archer City Bonebed 1 (Putnam Fm.),NA,"Locality IIIf (Romer & Price, 1940)",US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Broiliellus,,NA,NA,vertebrate,R. L. Carroll. 1964. Early evolution of the dissorophid amphibians. Bulletin of the Museum of Comparative Zoology 131:161-250,327,697,697,R. Butler,E. Dunne,E. Dunne,04/07/2016 06:11,24/08/2016 05:22,43845,brevis,Broiliellus,59694,n. sp.,296.4,268,Wolfcamp,,2,US,Broiliellus brevis
1334885,occ,NA,,179932,members,Broiliellus n. sp. reiszi,species,344543,,Broiliellus reiszi,NA,species,344543,Holmes et al.,2013,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37024,NA,NA,NA,,-106.656174,36.161781,Arroyo del Agua,NA,Uppermost part of El Cobre Canyon Formation,US,New Mexico,Rio Arriba,based on nearby landmark,6,small collection,"Location of is of the ""uppermost part of the [El Cobre] formation on the outskirts of the village of Arroyo del Agua from sediments equivalent in age to the Archer City Formation of North-central Texas"".",gp_mid,-34.08,4.54,101,US,FED,El Cobre Canyon,Cutler,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Broiliellus,,NA,NA,vertebrate,"R. B. Holmes, D. S. Berman, and J. S. Anderson. 2013. A new dissorophid (Temnospondyli, Dissorophoidea) from the Early Permian of New Mexico (United States). Comptes Rendus Palevol 12:419-435",327,697,0,R. Butler,E. Dunne,,04/07/2016 08:40,04/07/2016 08:40,NA,reiszi,Broiliellus,59698,n. sp.,296.4,268,Wolfcamp,,NA,US,Broiliellus reiszi
1334886,occ,NA,,179932,members,Sphenacodon ferox,species,122487,,Sphenacodon ferox,NA,species,122487,Holmes et al.,2013,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,,-106.656174,36.161781,Arroyo del Agua,NA,Uppermost part of El Cobre Canyon Formation,US,New Mexico,Rio Arriba,based on nearby landmark,6,small collection,"Location of is of the ""uppermost part of the [El Cobre] formation on the outskirts of the village of Arroyo del Agua from sediments equivalent in age to the Archer City Formation of North-central Texas"".",gp_mid,-34.08,4.54,101,US,FED,El Cobre Canyon,Cutler,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,CM,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,vertebrate,"R. B. Holmes, D. S. Berman, and J. S. Anderson. 2013. A new dissorophid (Temnospondyli, Dissorophoidea) from the Early Permian of New Mexico (United States). Comptes Rendus Palevol 12:419-435",327,697,0,R. Butler,E. Dunne,,04/07/2016 08:41,04/07/2016 08:41,NA,ferox,Sphenacodon,59698,,296.4,268,Wolfcamp,,NA,US,Sphenacodon ferox
1334970,occ,NA,,176535,members,n. gen. Schoenfelderpeton n. sp. prescheri,species,230693,,Schoenfelderpeton prescheri,NA,species,230693,Boy,1986,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37040,NA,NA,NA,,12.925204,51.199074,"Clennen, Saxony",NA,,DE,Mittelsachsen,Bockelwitz,based on nearby landmark,6,small collection,"Coordinates based on the location of Clennen, a small populated area in Saxony, Germany.",gp_mid,22.57,7.46,305,DE,,Bortewitz,,,group of beds,,Clennen tuffite,Clennen tuffite,,,,NA,B̦rtewitz Formation,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Schoenfelderpeton,n. gen.,NA,NA,vertebrate,J. A. Boy. 1986. Studien _ber die Branchiosauridae (Amphibia: Temnospondyli) 1. Neue und wenig bekannte Arten aus dem mitteleurop_ischen Rotligenden (?oberstes Karbon bis unteres Perm). Palaeontologische Zeitschrift 60:131-166,327,697,0,R. Butler,E. Dunne,,05/07/2016 05:15,05/07/2016 05:15,NA,prescheri,Schoenfelderpeton,59288,n. sp.,298.9,295,Autunian,,NA,DE,Schoenfelderpeton prescheri
1334971,occ,NA,,79598,,n. gen. Eumicrerpeton n. sp. parvum,species,320814,,Eumicrerpeton parvum,NA,species,320814,Moodie,1910,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,338120,NA,NA,NA,,-88.139999,41.267223,Mazon Creek,NA,"Mazon Creek Vertebrate Fauna, Braidwood Fauna, pit 11",US,Illinois,Grundy/Will,based on political unit,seconds,local area,"Lat Long is for SW Will Co., Illinois",gp_mid,-23.34,-5.09,101,US,,Carbondale,,Francis Creek Shale,,,,,,,,NA,"""Francis Creek Shale above Morris (no. 2) Coal, Carbondale Formation, Westphalian D, Middle Pennsylvanian"" (Carroll & Baird, 1972)\r\nBaird et al. (1985) refer to the no. 2 coal as Colchester or Croweburg Coal Member.","""Concretions occur typically in laminated to weakly rippled, silty mudstone deposits which typically show little or no evidence of bioturbation. Small-scale sedimentary structures in nodule-bearing sequences include climbing ripple drift, and soft-sediment load-failure..."" (Baird et al., 1985 p.90). Note that this is a general description of the fossil bearing strata of the Francis Creek Shale Member which does not refer specifically to the occurences in the Mazon Creek area proper.",mudstone,"current ripples,deformed bedding",,silty,,siderite,nodular,,,Y,deltaic indet.,foreland basin,"""...these indicate rapid and often episodic mud deposition in interdistributary bay and prodelta settings."" (Baird et al., 1985 p.90)",macrofossils,,,,,,NA,,"mold/impression,concretion,soft parts,replaced with other",good,parautochthonous,,,,,,,,NA,,"""Outlines of the limbs can be seen in the matrix, indicating the extent of the soft tissue and the texture of the skin. The bone itself was represented by a very soft, claylike material that had been removed from the hard, ironstone matrix."" (Carroll, & Baird, 1972 p. 323)\r\nBones are replaced by clay minerals such as Kaolinite (Gregory, 1948 p. 637).",taxonomic,"mechanical,survey of museum collection","FMNH,MCZ,USNM,YPM","species names,ichnofossils",,,"R. L. Moodie, P. Turnbull, among others","1871, 1953",,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eumicrerpeton,n. gen.,NA,NA,vertebrate,R. L. Moodie. 1910. The alimentary canal of a Carboniferous salamander. American Naturalist 44:367-375,327,697,0,R. Butler,E. Dunne,,05/07/2016 05:21,05/07/2016 05:21,28608,parvum,Eumicrerpeton,58523,n. sp.,311.45,306.95,Westphalian D,,NA,US,Eumicrerpeton parvum
1334974,occ,NA,,79598,,n. gen. Amphibamus n. sp. grandiceps,species,229305,,Amphibamus grandiceps,NA,species,229305,Cope,1865,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,37019,NA,NA,NA,,-88.139999,41.267223,Mazon Creek,NA,"Mazon Creek Vertebrate Fauna, Braidwood Fauna, pit 11",US,Illinois,Grundy/Will,based on political unit,seconds,local area,"Lat Long is for SW Will Co., Illinois",gp_mid,-23.34,-5.09,101,US,,Carbondale,,Francis Creek Shale,,,,,,,,NA,"""Francis Creek Shale above Morris (no. 2) Coal, Carbondale Formation, Westphalian D, Middle Pennsylvanian"" (Carroll & Baird, 1972)\r\nBaird et al. (1985) refer to the no. 2 coal as Colchester or Croweburg Coal Member.","""Concretions occur typically in laminated to weakly rippled, silty mudstone deposits which typically show little or no evidence of bioturbation. Small-scale sedimentary structures in nodule-bearing sequences include climbing ripple drift, and soft-sediment load-failure..."" (Baird et al., 1985 p.90). Note that this is a general description of the fossil bearing strata of the Francis Creek Shale Member which does not refer specifically to the occurences in the Mazon Creek area proper.",mudstone,"current ripples,deformed bedding",,silty,,siderite,nodular,,,Y,deltaic indet.,foreland basin,"""...these indicate rapid and often episodic mud deposition in interdistributary bay and prodelta settings."" (Baird et al., 1985 p.90)",macrofossils,,,,,,NA,,"mold/impression,concretion,soft parts,replaced with other",good,parautochthonous,,,,,,,,NA,,"""Outlines of the limbs can be seen in the matrix, indicating the extent of the soft tissue and the texture of the skin. The bone itself was represented by a very soft, claylike material that had been removed from the hard, ironstone matrix."" (Carroll, & Baird, 1972 p. 323)\r\nBones are replaced by clay minerals such as Kaolinite (Gregory, 1948 p. 637).",taxonomic,"mechanical,survey of museum collection","FMNH,MCZ,USNM,YPM","species names,ichnofossils",,,"R. L. Moodie, P. Turnbull, among others","1871, 1953",,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Amphibamus,n. gen.,NA,NA,vertebrate,"E. D. Cope. 1865. On Amphibamus grandiceps, a new Batrachian from the Coal Measures. Proceedings of the National Academy of Sciences ",327,697,0,R. Butler,E. Dunne,,05/07/2016 06:25,05/07/2016 06:25,28608,grandiceps,Amphibamus,40834,n. sp.,311.45,306.95,Westphalian D,,NA,US,Amphibamus grandiceps
1334976,occ,NA,,68427,,n. gen. Eoscopus n. sp. lockardi,species,229322,,Eoscopus lockardi,NA,species,229322,Daly,1994,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,123090,NA,NA,NA,individuals,-96.113892,37.986111,Hamilton Quarry,NA,,US,Kansas,Greenwood,estimated from map,seconds,,"about 5 km E of Hamilton, Greenwood Co., Kansas, in secs. 5 and 6, T. 24 S., R. 12 E. (Virgil 7.5' quadrangle)",gp_mid,-26.91,-0.1,101,US,,Calhouns Shale,Shawnee,,,,,,,,,NA,"Virgillian Series, Upper Pennsylvanian; late Kasimovian according to Modesto et al. (2015)",,"""shale""",,,,,,,,,,estuary/bay,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eoscopus,n. gen.,NA,NA,vertebrate,"E. Daly. 1994. The Amphibamidae (Amphibia: Temnospondyli), with a description of a new genus from the Upper Pennsylvanian of Kansas. University of Kansas Museum of Natural History, Miscellaneous Publications 85:1-59",327,697,334,R. Butler,E. Dunne,T. Liebrecht,05/07/2016 07:56,23/12/2016 14:15,19706,lockardi,Eoscopus,59720,n. sp.,303.4,298.9,Virgilian,,1,US,Eoscopus lockardi
1335602,occ,NA,,75090,,n. gen. Iberospondylus n. sp. schultzei,species,344739,,Iberospondylus schultzei,NA,species,344739,Laurin and Soler-Gij_n,2001,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,260248,NA,NA,NA,,-4.116667,38.683334,Emma Quarry Amphibian Bed,NA,Puertollano,ES,Castilla-La Manacha,,based on nearby landmark,minutes,outcrop,"from an area of ""approximately 5 hectares"" within Emma Quarry, about 6 k WSW of Puertollano (basis of coordinate)",gp_mid,10.97,-6.38,304,ES,,,,,bed,,,,,,,NA,single bedding plane,"""siltstone""",siltstone,,,,,,,,,,estuary/bay,,"""intertidal""",macrofossils,,,,,,NA,,trace,,,snapshot,,,,,,,NA,,,paleoecologic,field collection,,,,,,1994,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Iberospondylus,n. gen.,NA,NA,vertebrate,M. Laurin and R. Soler-Gij_n. 2001. The oldest stegocephalian from the Iberian Peninsula: evidence that temnospondyls were euryhaline. Comptes Rendus de l'Acad̩mie des Sciences - Series III - Sciences de la Vie 324:495-501,327,697,0,R. Butler,E. Dunne,,07/07/2016 08:17,07/07/2016 08:17,25351,schultzei,Iberospondylus,59743,n. sp.,303.4,301.2,Stephanian C,,NA,ES,Iberospondylus schultzei
1335603,occ,NA,,67862,,Tersomius n. sp. dolesensis,species,344740,,Tersomius dolesensis,NA,species,344740,Anderson and Bolt,2013,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,37035,NA,NA,NA,,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Tersomius,,NA,NA,"paleoentomology,vertebrate","J. S. Anderson and J. R. Bolt. 2013. New information on amphibamids (Tetrapoda, Temnospondyli) from Richards Spur (Fort Sill), Oklahoma. Journal of Vertebrate Paleontology 33:553-567",327,697,0,R. Butler,E. Dunne,,07/07/2016 08:28,07/07/2016 08:28,19393,dolesensis,Tersomius,59744,n. sp.,290.1,268,Leonard,,NA,US,Tersomius dolesensis
1335607,occ,NA,,180106,members,n. gen. Ecolsonia n. sp. cutlerensis,species,229320,,Ecolsonia cutlerensis,NA,species,229320,Vaughn,1969,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,37028,NA,NA,NA,,-106.621315,36.139988,Van der Hoof Quarry,NA,Ecolsonia type locality (UCMP V-2843) (L 4706),US,New Mexico,Rio Arriba,stated in text,6,small collection,See map on page 289 of Lucas et al. (2005),gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,,,,,,,,NA,Chama Basin,"""The VanderHoof quarry is in green and brown micaceous clay and siltstone that progressively becomes lighter colored towards its top. These clays and siltstones are capped by a medium-grained crossbedded sandstone and underlain by a layer of marl and spherical carbonate concretions."" Lucas et al. (2005)",claystone,"brown,green",,,,siltstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"CM,NMMNH",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Ecolsonia,n. gen.,NA,NA,vertebrate,P. P. Vaughn. 1969. Further evidence of a close relationship of the trematopsid and dissorophid labyrinthodont amphibians with a description of a new genus and a new species. Bulletin of the Southern California Academy of Sciences 68:121-130,327,697,0,R. Butler,E. Dunne,,07/07/2016 08:53,07/07/2016 08:53,NA,cutlerensis,Ecolsonia,59745,n. sp.,296.4,268,Wolfcamp,,NA,US,Ecolsonia cutlerensis
1335610,occ,NA,,180106,members,Chenoprosopus milleri,species,139020,,Chenoprosopus milleri,NA,species,139020,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Cochleosauridae,36999,37000,NA,NA,NA,,-106.621315,36.139988,Van der Hoof Quarry,NA,Ecolsonia type locality (UCMP V-2843) (L 4706),US,New Mexico,Rio Arriba,stated in text,6,small collection,See map on page 289 of Lucas et al. (2005),gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,,,,,,,,NA,Chama Basin,"""The VanderHoof quarry is in green and brown micaceous clay and siltstone that progressively becomes lighter colored towards its top. These clays and siltstones are capped by a medium-grained crossbedded sandstone and underlain by a layer of marl and spherical carbonate concretions."" Lucas et al. (2005)",claystone,"brown,green",,,,siltstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"CM,NMMNH",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Chenoprosopus,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,07/07/2016 09:04,07/07/2016 09:04,NA,milleri,Chenoprosopus,59746,,296.4,268,Wolfcamp,,NA,US,Chenoprosopus milleri
1335611,occ,NA,,180106,members,Eryops grandis,species,345659,,Eryops grandis,NA,species,345657,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-106.621315,36.139988,Van der Hoof Quarry,NA,Ecolsonia type locality (UCMP V-2843) (L 4706),US,New Mexico,Rio Arriba,stated in text,6,small collection,See map on page 289 of Lucas et al. (2005),gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,,,,,,,,NA,Chama Basin,"""The VanderHoof quarry is in green and brown micaceous clay and siltstone that progressively becomes lighter colored towards its top. These clays and siltstones are capped by a medium-grained crossbedded sandstone and underlain by a layer of marl and spherical carbonate concretions."" Lucas et al. (2005)",claystone,"brown,green",,,,siltstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"CM,NMMNH",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,07/07/2016 09:04,07/07/2016 09:04,NA,grandis,Eryops,59746,,296.4,268,Wolfcamp,,NA,US,Eryops grandis
1335612,occ,NA,,180106,members,Zatrachys serratus,species,255221,,Zatrachys serratus,NA,species,255221,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,,-106.621315,36.139988,Van der Hoof Quarry,NA,Ecolsonia type locality (UCMP V-2843) (L 4706),US,New Mexico,Rio Arriba,stated in text,6,small collection,See map on page 289 of Lucas et al. (2005),gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,,,,,,,,NA,Chama Basin,"""The VanderHoof quarry is in green and brown micaceous clay and siltstone that progressively becomes lighter colored towards its top. These clays and siltstones are capped by a medium-grained crossbedded sandstone and underlain by a layer of marl and spherical carbonate concretions."" Lucas et al. (2005)",claystone,"brown,green",,,,siltstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"CM,NMMNH",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,07/07/2016 09:04,07/07/2016 09:04,NA,serratus,Zatrachys,59746,,296.4,268,Wolfcamp,,NA,US,Zatrachys serratus
1335613,occ,NA,,180106,members,Platyhystrix rugosus,species,345923,,Platyhystrix rugosus,NA,species,194929,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37034,NA,NA,NA,,-106.621315,36.139988,Van der Hoof Quarry,NA,Ecolsonia type locality (UCMP V-2843) (L 4706),US,New Mexico,Rio Arriba,stated in text,6,small collection,See map on page 289 of Lucas et al. (2005),gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,,,,,,,,NA,Chama Basin,"""The VanderHoof quarry is in green and brown micaceous clay and siltstone that progressively becomes lighter colored towards its top. These clays and siltstones are capped by a medium-grained crossbedded sandstone and underlain by a layer of marl and spherical carbonate concretions."" Lucas et al. (2005)",claystone,"brown,green",,,,siltstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"CM,NMMNH",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Platyhystrix,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,07/07/2016 09:04,07/07/2016 09:04,NA,rugosus,Platyhystrix,59746,,296.4,268,Wolfcamp,,NA,US,Platyhystrix rugosus
1335614,occ,NA,,180106,members,Diadectes lentus,species,346261,,Diadectes lentus,NA,species,120884,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-106.621315,36.139988,Van der Hoof Quarry,NA,Ecolsonia type locality (UCMP V-2843) (L 4706),US,New Mexico,Rio Arriba,stated in text,6,small collection,See map on page 289 of Lucas et al. (2005),gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,,,,,,,,NA,Chama Basin,"""The VanderHoof quarry is in green and brown micaceous clay and siltstone that progressively becomes lighter colored towards its top. These clays and siltstones are capped by a medium-grained crossbedded sandstone and underlain by a layer of marl and spherical carbonate concretions."" Lucas et al. (2005)",claystone,"brown,green",,,,siltstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"CM,NMMNH",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,07/07/2016 09:04,07/07/2016 09:04,NA,lentus,Diadectes,59746,,296.4,268,Wolfcamp,,NA,US,Diadectes lentus
1335615,occ,NA,,180106,members,Ophiacodon mirus,species,123418,,Ophiacodon mirus,NA,species,123418,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-106.621315,36.139988,Van der Hoof Quarry,NA,Ecolsonia type locality (UCMP V-2843) (L 4706),US,New Mexico,Rio Arriba,stated in text,6,small collection,See map on page 289 of Lucas et al. (2005),gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,,,,,,,,NA,Chama Basin,"""The VanderHoof quarry is in green and brown micaceous clay and siltstone that progressively becomes lighter colored towards its top. These clays and siltstones are capped by a medium-grained crossbedded sandstone and underlain by a layer of marl and spherical carbonate concretions."" Lucas et al. (2005)",claystone,"brown,green",,,,siltstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"CM,NMMNH",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,07/07/2016 09:04,07/07/2016 09:04,NA,mirus,Ophiacodon,59746,,296.4,268,Wolfcamp,,NA,US,Ophiacodon mirus
1335616,occ,NA,,180106,members,Sphenacodon ferox,species,122487,,Sphenacodon ferox,NA,species,122487,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,,-106.621315,36.139988,Van der Hoof Quarry,NA,Ecolsonia type locality (UCMP V-2843) (L 4706),US,New Mexico,Rio Arriba,stated in text,6,small collection,See map on page 289 of Lucas et al. (2005),gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,,,,,,,,NA,Chama Basin,"""The VanderHoof quarry is in green and brown micaceous clay and siltstone that progressively becomes lighter colored towards its top. These clays and siltstones are capped by a medium-grained crossbedded sandstone and underlain by a layer of marl and spherical carbonate concretions."" Lucas et al. (2005)",claystone,"brown,green",,,,siltstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"CM,NMMNH",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,07/07/2016 09:04,07/07/2016 09:04,NA,ferox,Sphenacodon,59746,,296.4,268,Wolfcamp,,NA,US,Sphenacodon ferox
1335617,occ,NA,,180107,members,Ecolsonia cutlerensis,species,229320,,Ecolsonia cutlerensis,NA,species,229320,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,37028,NA,NA,NA,,-106.75193,36.233521,Morfin Bonebed,NA,,US,New Mexico,Rio Arriba,stated in text,6,small collection,See page 289 of Lucas et al. (2005) for detailed map. The Morfin bonebed lies geographically near the Baldwin and Miller bonebeds.,gp_mid,-34.1,4.64,101,US,FED,El Cobre Canyon,Cutler,,bed,,,,,,,NA,,"""Lithologically, the bonebed exhibits a sequence of sandstone lenses and sheets with interbedded siltstones and mudstones. This is indicative of repeated cycles of shallow, ephemeral flow and deposition from suspension characteristic of a crevasse-splay deposit. Most elements recovered from this quarry are isolated, especially those from the underlying limestone-pebble conglomerate."" Lucas et al. (2005)",sandstone,,,,,siltstone,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Ecolsonia,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,07/07/2016 09:14,07/07/2016 09:14,NA,cutlerensis,Ecolsonia,59746,,296.4,268,Wolfcamp,,NA,US,Ecolsonia cutlerensis
1335618,occ,NA,,80784,,n. gen. Actiobates n. sp. peabodyi,species,344750,,Actiobates peabodyi,NA,species,344750,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,37049,NA,NA,NA,,-95.259048,38.378502,Garnett Quarry,NA,"Garnett Vertebrate Fauna, Charles Hardesty farm",US,Kansas,Anderson,estimated from map,6,outcrop,"""6 miles northwest of Garnett"" (Reisz, 1986); ""NW 1/4, NE 1/4, sec. 5, tp. 20 S, rge. 19 E, Putnam Township, Anderson County, Kansas"" (Reisz & Berman, 1986)\r\n""Charles A. Hardest farm, NW/4 NE/4 sec. 5 T20S R19E, Putnam Township, Anderson County, Kansas. The Universal Transverse Mercantor (UTM) coordinates of the quarry are 15STN963466. Locality is close to Garnett, Kansas."" (Laurin 1993). ",gp_mid,-27.44,-2.3,101,US,,Stanton,Lansing,Rock Lake Shale,group of beds,,,,,,,NA,"""Rock Lake Member, Stanton Formation, Lansing Group, Missourian Series, Upper Pennsylvanian"" (Reisz & Berman, 1996)\r\nall vertebrate remains seem to come exclusively from the basal part of the Rock Lake Shale (see Reisz et al., 1982)","""dark greyishbrown, moderately well bedded, very carbonaceous, calcareous mudstone"" (Reisz et al., 1982)",mudstone,brown,,"calcareous,carbonaceous",Y,,,,,,fine channel fill,foreland basin,"""The Rock Lake Shale is a rather thin but otherwise typical ۪outside۪ shale of a ۪Kansas Megacyclothem۪ sequence formed as a change from regressive to transgressive conditions occurred [...] The site is located along the western edge of what was, during the Late Pennsylvanian, a shallow, forested stream valley or channel that was eroded into a limestone coastal plain during the latter stages of a major eustatic fall in sea level. As the succeeding rise in sea level occurred, the valley was gradually flooded by estuarine waters"" (Reisz et al., 1982).\r\nSequence stratigraphy is interpreted from the description given by Reisz et al. (1982). The surface of the underlying limestone is the sequence boundary merged with the transgressive surface and the Lake Rock Shale is the basalmost deposit of the transgressive systems tract.",macrofossils,some,some,,,,NA,,body,good,,snapshot,,,,,,,NA,,,taxonomic,"bulk,mechanical",ROM,,,,"F. E. Peabody, R. Camp, R. L. Carroll, R. R. Reisz, M. J. Heaton, B. R. Pynn, G. MacDonald","1953-1956, 1965, 1980, 1981",,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Actiobates,n. gen.,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,07/07/2016 09:20,07/07/2016 09:20,28862,peabodyi,Actiobates,57795,n. sp.,305.9,303.4,Missourian,,NA,US,Actiobates peabodyi
1335676,occ,NA,,80833,,Chenoprosopus milleri,species,139020,,Chenoprosopus milleri,NA,species,139020,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Cochleosauridae,36999,37000,NA,NA,NA,,-106.671387,36.184723,Baldwin bonebed,85339,"type horizon of Sphenacodon ferox & Ophiacodon mirus, Arroya de Agua",US,New Mexico,Rio Arriba,estimated from map,seconds,small collection,"""about a mile and a half above the confluence of the Poleo creek with the Puerco, and near the Mexican village of Arroya de Agua."" (Williston, 1916)\r\nApparently is what Williston (1916) calls the Poleo Creek a northwestern headstream of the Rio Puerco (see Williston & Case, 1913 p. 1 fig. 1, Inst. Washington Publ. 181), however, in modern maps a southwestern headstream is designated as Poleo Creek. ",gp_mid,-34.08,4.56,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,D. A. Baldwin,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Chenoprosopus,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,08/07/2016 10:29,08/07/2016 10:29,27105,milleri,Chenoprosopus,59746,,296.4,268,Wolfcamp,,NA,US,Chenoprosopus milleri
1335677,occ,NA,,80833,,Eryops grandis,species,345659,,Eryops grandis,NA,species,345657,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-106.671387,36.184723,Baldwin bonebed,85339,"type horizon of Sphenacodon ferox & Ophiacodon mirus, Arroya de Agua",US,New Mexico,Rio Arriba,estimated from map,seconds,small collection,"""about a mile and a half above the confluence of the Poleo creek with the Puerco, and near the Mexican village of Arroya de Agua."" (Williston, 1916)\r\nApparently is what Williston (1916) calls the Poleo Creek a northwestern headstream of the Rio Puerco (see Williston & Case, 1913 p. 1 fig. 1, Inst. Washington Publ. 181), however, in modern maps a southwestern headstream is designated as Poleo Creek. ",gp_mid,-34.08,4.56,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,D. A. Baldwin,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,08/07/2016 10:29,08/07/2016 10:29,27105,grandis,Eryops,59746,,296.4,268,Wolfcamp,,NA,US,Eryops grandis
1335678,occ,NA,,80833,,Zatrachys serratus,species,255221,,Zatrachys serratus,NA,species,255221,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,,-106.671387,36.184723,Baldwin bonebed,85339,"type horizon of Sphenacodon ferox & Ophiacodon mirus, Arroya de Agua",US,New Mexico,Rio Arriba,estimated from map,seconds,small collection,"""about a mile and a half above the confluence of the Poleo creek with the Puerco, and near the Mexican village of Arroya de Agua."" (Williston, 1916)\r\nApparently is what Williston (1916) calls the Poleo Creek a northwestern headstream of the Rio Puerco (see Williston & Case, 1913 p. 1 fig. 1, Inst. Washington Publ. 181), however, in modern maps a southwestern headstream is designated as Poleo Creek. ",gp_mid,-34.08,4.56,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,D. A. Baldwin,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,08/07/2016 10:29,08/07/2016 10:29,27105,serratus,Zatrachys,59746,,296.4,268,Wolfcamp,,NA,US,Zatrachys serratus
1335679,occ,NA,,80833,,Platyhystrix rugosus,species,345923,,Platyhystrix rugosus,NA,species,194929,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37034,NA,NA,NA,,-106.671387,36.184723,Baldwin bonebed,85339,"type horizon of Sphenacodon ferox & Ophiacodon mirus, Arroya de Agua",US,New Mexico,Rio Arriba,estimated from map,seconds,small collection,"""about a mile and a half above the confluence of the Poleo creek with the Puerco, and near the Mexican village of Arroya de Agua."" (Williston, 1916)\r\nApparently is what Williston (1916) calls the Poleo Creek a northwestern headstream of the Rio Puerco (see Williston & Case, 1913 p. 1 fig. 1, Inst. Washington Publ. 181), however, in modern maps a southwestern headstream is designated as Poleo Creek. ",gp_mid,-34.08,4.56,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,D. A. Baldwin,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Platyhystrix,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,08/07/2016 10:29,08/07/2016 10:29,27105,rugosus,Platyhystrix,59746,,296.4,268,Wolfcamp,,NA,US,Platyhystrix rugosus
1335680,occ,NA,,80833,,Diadectes lentus,species,346261,,Diadectes lentus,NA,species,120884,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-106.671387,36.184723,Baldwin bonebed,85339,"type horizon of Sphenacodon ferox & Ophiacodon mirus, Arroya de Agua",US,New Mexico,Rio Arriba,estimated from map,seconds,small collection,"""about a mile and a half above the confluence of the Poleo creek with the Puerco, and near the Mexican village of Arroya de Agua."" (Williston, 1916)\r\nApparently is what Williston (1916) calls the Poleo Creek a northwestern headstream of the Rio Puerco (see Williston & Case, 1913 p. 1 fig. 1, Inst. Washington Publ. 181), however, in modern maps a southwestern headstream is designated as Poleo Creek. ",gp_mid,-34.08,4.56,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,D. A. Baldwin,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,08/07/2016 10:29,08/07/2016 10:29,27105,lentus,Diadectes,59746,,296.4,268,Wolfcamp,,NA,US,Diadectes lentus
1335681,occ,NA,,80833,,Rhiodenticulatus heatoni,species,135851,,Rhiodenticulatus heatoni,NA,species,135851,Lucas et al.,2005,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37503,NA,NA,NA,,-106.671387,36.184723,Baldwin bonebed,85339,"type horizon of Sphenacodon ferox & Ophiacodon mirus, Arroya de Agua",US,New Mexico,Rio Arriba,estimated from map,seconds,small collection,"""about a mile and a half above the confluence of the Poleo creek with the Puerco, and near the Mexican village of Arroya de Agua."" (Williston, 1916)\r\nApparently is what Williston (1916) calls the Poleo Creek a northwestern headstream of the Rio Puerco (see Williston & Case, 1913 p. 1 fig. 1, Inst. Washington Publ. 181), however, in modern maps a southwestern headstream is designated as Poleo Creek. ",gp_mid,-34.08,4.56,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,D. A. Baldwin,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Rhiodenticulatus,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,08/07/2016 10:29,08/07/2016 10:29,27105,heatoni,Rhiodenticulatus,59746,,296.4,268,Wolfcamp,,NA,US,Rhiodenticulatus heatoni
1335995,occ,NA,,67862,,Colobomycter n. sp. vaughni,species,345089,,Colobomycter vaughni,NA,species,345089,MacDougall et al.,2016,Chordata,33815,Reptilia,36322,,NA,Acleistorhinidae,37514,38921,NA,NA,NA,,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Colobomycter,,NA,NA,"paleoentomology,vertebrate","M. J. MacDougall, S. P. Modesto, and R. R. Reisz. 2016. A new reptile from the Richards Spur Locality, Oklahoma, USA, and patterns of Early Permian parareptile diversification. Journal of Vertebrate Paleontology 36(5):e1179641",327,697,0,R. Butler,E. Dunne,,11/07/2016 06:33,11/07/2016 06:33,19393,vaughni,Colobomycter,59809,n. sp.,290.1,268,Leonard,,NA,US,Colobomycter vaughni
1336075,occ,NA,,155305,,Dawsonerpeton polydens,species,336807,,Dawsonerpeton polydens,NA,species,336780,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,336806,NA,NA,NA,,14.075,50.23,"Zabor, near Schlan",NA,Zbor,CZ,,,based on nearby landmark,2,outcrop,Coordinates based on Slan_ (=Schlan),gp_mid,21.97,4.74,305,CZ,,Slany,,Kounov,group of beds,,,,,,,NA,,,"""siliciclastic""",,lithified,,,,,,,,terrestrial indet.,rift,"Central-West Bohemian basin; extensional basin developed within Variscan zone along simple asymmetric mega-graben formed on the Central Bohemian and Litomerice fault zones, with some contribution from transtensional wrench faults.",macrofossils,,,,,,NA,,mold/impression,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Repository: National Museum, Prague (CGH)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Dawsonerpeton,,NA,NA,paleoentomology,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,11/07/2016 12:53,11/07/2016 12:53,50655,polydens,Dawsonerpeton,57795,,304.8,303.4,Stephanian B,,NA,CZ,Dawsonerpeton polydens
1336733,occ,NA,,84835,,n. gen. Branchiosaurus n. sp. salamandroides,species,255222,,Branchiosaurus salamandroides,NA,species,255222,Fritsch,1876,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37039,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchiosaurus,n. gen.,NA,NA,vertebrate,A. Fritsch. 1876. ber die Fauna der Gaskohle des Pilsner und Rakonitzer Beckens. Sitzungs-Berichte der koniglichen bohmischen Gellschaft der Wissenschaften Prag 1875:70-78,327,697,0,R. Butler,E. Dunne,,12/07/2016 10:11,12/07/2016 10:11,28608,salamandroides,Branchiosaurus,58031,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Branchiosaurus salamandroides
1336734,occ,NA,,125662,,Branchiosaurus salamandroides,species,255222,,Branchiosaurus salamandroides,NA,species,255222,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37039,NA,NA,NA,,13.395,49.814999,Tremosna,NA,"Temon̩, Temon",CZ,,,based on nearby landmark,3,outcrop,,gp_mid,19.75,0.69,305,CZ,,Kladno,,Nyrany,,,,,,,,NA,Tremosna in B̦hmen. Mittleres Obercarbon.,,not reported,,,,,coal,,,,,terrestrial indet.,rift,"Central-West Bohemian basin; extensional basin developed within Variscan zone along simple asymmetric mega-graben formed on the Central Bohemian and Litomerice fault zones, with some contribution from transtensional wrench faults.",macrofossils,,,,,,NA,,mold/impression,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchiosaurus,,NA,NA,"paleoentomology,vertebrate",R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,12/07/2016 10:12,12/07/2016 10:12,50906,salamandroides,Branchiosaurus,57795,,311.45,306.95,Westphalian D,,NA,CZ,Branchiosaurus salamandroides
1336742,occ,NA,,176090,members,Branchiosaurus sp.,genus,37039,,Branchiosaurus,NA,genus,37039,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37039,NA,NA,NA,,4.387342,46.696396,"Montceau-les-Mines, Saone et Loire",NA,"Blanzy, Sa̫ne-et-Loire",FR,Bourgogne,,based on nearby landmark,6,,"Coordinates based on Blanzy, a commune in the Sa̫ne-et-Loire department in the region of Bourgogne in eastern France",gp_mid,17.13,0.02,305,FR,,,,,bed,,,,,,,NA,Locatity situated in the Montceau Basin,,not reported,,,,,,,,,,terrestrial indet.,,"No further information available on stratigraphy aside from that presented in Carroll et al. (1998, Handbuch der Palaoherpetologie 1)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MNHN,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchiosaurus,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,697,R. Butler,E. Dunne,E. Dunne,12/07/2016 10:34,12/07/2016 10:34,NA,sp.,Branchiosaurus,57795,,304.8,301.2,Stephanian B,Stephanian C,NA,FR,Branchiosaurus sp.
1336743,occ,NA,,180284,members,Leptorophus n. sp. raischi,species,345146,,Leptorophus raischi,NA,species,345146,Schoch,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,229328,NA,NA,NA,,7.767154,49.72987,Obermoschel ,NA,,DE,Rheinland-Pfalz,,estimated from map,6,,"Coordinates based on the centre of Obermoschel, a town in the district Donnersbergkreis, in Rhineland-Palatinate, Germany, 15km SW of Bad Kreuznach",gp_mid,19.8,5.15,315,DE,,Meisenheim,,,,,,,,,,NA,"The outcrop belongs to the Jeckenbach Subformation of the Meisenheim Formation, informal Unit M5.",The outcrop falls into a fining-upward sequence reaching from fluviatile sandy sediments to lacustrine laminated claystones. The lake horizon has a thickness of 250 cm. ,sandstone,,,sandy,,claystone,,,,,lacustrine indet.,,"Location represents a locally restricted lake deposit near Obermoschel (Rheinland-Pfalz, Germany, Geoskop locality number UGKU L-27).",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Leptorophus,,NA,NA,vertebrate,R. R. Schoch. 2014. First evidence of the branchiosaurid temnospondyl Leptorophus in the Early Permian of the Saar-Nahe Basin (SW Germany). Neues Jahrbuch f_r Geologie und Pal_ontologie Abhandlungen 272(2):225-236,327,697,0,R. Butler,E. Dunne,,12/07/2016 10:59,12/07/2016 10:59,NA,raischi,Leptorophus,59833,n. sp.,298.9,295,Autunian,,NA,DE,Leptorophus raischi
1336891,occ,NA,,28145,,Acheloma n. sp. whitei,species,345161,recombined as,Phonerpeton whitei,NA,species,345161,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,230700,NA,NA,NA,,-99.022781,33.687222,"South of Fulda, 19 (Belle Plains)",NA,"Locality 19 (Romer 1928), Locality Vb (Romer & Price 1940), S. of Fulda, Hackberry Creek, North Side Little Wichita, South Side Little Wichita, North Side of Godwin Creek, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""Numerous exposures occur in the valley of the Little Wichita south and southeast of Fulda."" Specimens are labeled with various locality names, see aka above. See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 2 mi north of locality.",gp_mid,-30.3,-1.05,101,US,,Petrolia,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,Cope,1908,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Acheloma,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,13/07/2016 05:27,13/07/2016 05:27,28729,whitei,Phonerpeton,57795,n. sp.,290.1,279.3,Artinskian,,NA,US,Phonerpeton whitei
1336900,occ,NA,,67862,,Cacops n. sp. woehri,species,37025,species not entered,Cacops,NA,genus,37025,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37025,NA,NA,NA,,-98.403893,34.770557,Richards Spur,NA,Fort Sill; OMNH locality V51; Dolese Bros. limestone quarry; FEP 60A,US,Oklahoma,Comanche,estimated from map,seconds,outcrop,"""situated just west of the Anadarko-Lawton highway (U.S. routes 62 and 281), 10 1/2 miles south of Apache, about 1 1/2 miles south of the junction of this route and highway 277 (from Chickasha). It is about 6 miles north of Fort Sill, in sec. 31, T. 4 N. R. 11 W., Indian Meridian and Baseline, in Comanche County, Oklahoma"" (Gregory et al., 1956 p. 2)",gp_mid,-28.89,0.32,101,US,,Garber,Sumner,,member,,,,,,,NA,"no younger than the Leondardian Arroyo Formation (which underlies the Vale) based on biostratigraphy, see Sullivan and Reisz (1999 p. 1265) for discussion;\r\n""The locality [...] is assigned to the surrounding Garber Formation (Sumner Group). The Fort Sill locality has been correlated (Heaton, 1979; Olson, 1991) with the lowermost horizons of the Clear Fork Group of Texas (beds recognized formerly as the 'Arroyo Formation')"" (Modesto, 1998)","primarily ""fine grey clay... However, sheets of coarse conglomerate occur near the irregular fissure walls, providing evidence for occasional floods... Tetrapod remains occur within both conglomerate and clay""; clay is ""largely unlithified"" (Sullivan & Reisz, 1999 pp. 1258/59)",claystone,"fine,gray",poorly lithified,,Y,conglomerate,coarse,,,Y,fissure fill,non-subsiding area,,macrofossils,,,,,,NA,,body,variable,,,,,,abundant,,,NA,,"remains are ""occasionally partly articulated but more commonly disarticulated"" (Sullivan & Reisz, 1999 p. 1259)\r\nfissure fill deposits contain ""myriads of bones of small reptiles and amphibians"" (Gregory et al., 1956 p. 2)",taxonomic,"selective quarrying,surface (float),sieve,field collection,survey of museum collection","FMNH,MCZ,OU,YPM",,,,"F. E. Peabody, W. Langston, J. Bolt, E. C. Olson, among others",,"The fossils are prepared by ""washing the largely unlithified fossiliferous clays and sorting in the laboratory"" (Sullivan & Reisz, 1999 p. 1259)\r\napparently, the material comes from spoil piles produced during commercial quarrying.\r\nAdditonal institutions storing material from Richards Spur:\r\nKU(MNH)= KUVP = University of Kansas, Museum of Natural History, Lawrence\r\nROM = Royal Ontario Musuem, Toronto, Canada\r\nUCLA = University of California Los Angeles\r\nUCMP = University of California Museum of Paleontology, Berkeley\r\nUMMP = University of Michigan Museum of Paleontology, Detroit\r\nUSNM = Smithsonian National Museum of Natural History, Washington, DC\r\nUWBM = University of Washington, Burke Museum, Seattle","Bolt (1969) notes that the clay mound (the ""D-concentrate"") in the spoil heap of the quarry that contained the type material of Doleserpeton annectens bears the ""remains of many thousands of individuals but virtually no genera other than Doleserpeton"".\r\nThe type specimen of Sillerpeton permianum is said to be UCMP 62480 by Lund (1978 p. 65). This specimen number, however, does not appear among the specimens of Phlegethontia cf. longissima listed by McGinnis (1967 p. 2) but one of these specimens bears the catalogue number UCMP 62580. The latter is listed as referred specimen of S. permianum in Lund (1978 p. 66). Anderson (2002, J. Paleont. 76(6) p. 1031) lists both UCMP 62480 and 62580 as type of S. permianum. Since UCMP 62480 is a braincase according to Lund (1978) and UCMP 62580 is a braincase as well (McGinnis, 1967; Lund, 1978) and since there is only one aistopod braincase present in the Fort Sill material (Anderson, 2002) the type of S. permianum is very likely to be UCMP 62580.\r\nAnderson & Reisz (2003) do not explicitly say when the type of Bolterpeton carrolli was collected but it is improbable that this specimen was known to Bolt in 1980. OMNH 71111 and OMNH 71112, although not explicitly mentioned by Bolt (1980), well may belong to the material that was originally assigned to ""species x"". Furthermore, Anderson & Reisz (2003) do not explicitly assign the remainder of ""species x"" to Bolterpeton. Nevertheless they say that these specimens are ""closely related"" to Bolterpeton, but ""because of the size difference between Bolterpeton and Species X, it cannot be said whether Species X is a different species or an ontogenetic variant."" Thus, these specimens are re-identified here as ? Bolterpeton sp.","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Cacops,,NA,NA,"paleoentomology,vertebrate",R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,697,R. Butler,E. Dunne,E. Dunne,13/07/2016 07:37,03/08/2016 10:40,19393,woehri,Cacops,57795,n. sp.,290.1,268,Leonard,,NA,US,Cacops woehri
1336908,occ,NA,,79162,,Parioxys n. sp. bolli,species,345163,,Parioxys bolli,NA,species,345163,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37052,NA,NA,NA,specimens,-98.650002,33.583332,Archer City Bonebed 1 (Putnam Fm.),NA,"Locality IIIf (Romer & Price, 1940)",US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Parioxys,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,697,R. Butler,E. Dunne,E. Dunne,13/07/2016 08:30,24/08/2016 05:22,43845,bolli,Parioxys,57795,n. sp.,296.4,268,Wolfcamp,,1,US,Parioxys bolli
1337191,occ,NA,,171346,,Ecolsonia cutlerensis,species,229320,,Ecolsonia cutlerensis,NA,species,229320,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,37028,NA,NA,NA,,-106.652222,36.159443,Valley floor of east Camp Quarry,NA,1 km SE Arroyo del Agua,US,New Mexico,Rio Arriba,based on nearby landmark,seconds,small collection,"Coordinates are for the area 1 km southeast of the small village of Arroyo del Agua, Rio Arriba County, New Mexico. See Lucas et al. (2005) for detailed map of other fossil-bearing locations in the area.",gp_mid,-34.08,4.53,101,US,FED,Cutler,,,bed,,,,,,,NA,,,"""siliciclastic""",,,,,,,,,,fine channel fill,,,macrofossils,,some,,partial skeletons,,NA,,"mold/impression,adpression",,,,,,,,,,NA,,,taxonomic,field collection,CM,,,,,1982,,"""Numerous articulated specimens have been collected from the valley floor immediately east of the Camp quarry."" Lucas et a. (2005)","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Ecolsonia,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 06:11,14/07/2016 06:11,NA,cutlerensis,Ecolsonia,59746,,296.4,268,Wolfcamp,,NA,US,Ecolsonia cutlerensis
1337192,occ,NA,,171346,,Tseajaia cf. campi,species,120742,,Tseajaia campi,NA,species,120742,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Tseajaiidae,37239,37240,NA,NA,NA,,-106.652222,36.159443,Valley floor of east Camp Quarry,NA,1 km SE Arroyo del Agua,US,New Mexico,Rio Arriba,based on nearby landmark,seconds,small collection,"Coordinates are for the area 1 km southeast of the small village of Arroyo del Agua, Rio Arriba County, New Mexico. See Lucas et al. (2005) for detailed map of other fossil-bearing locations in the area.",gp_mid,-34.08,4.53,101,US,FED,Cutler,,,bed,,,,,,,NA,,,"""siliciclastic""",,,,,,,,,,fine channel fill,,,macrofossils,,some,,partial skeletons,,NA,,"mold/impression,adpression",,,,,,,,,,NA,,,taxonomic,field collection,CM,,,,,1982,,"""Numerous articulated specimens have been collected from the valley floor immediately east of the Camp quarry."" Lucas et a. (2005)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tseajaia,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 06:11,14/07/2016 06:11,NA,campi,Tseajaia,59746,cf.,296.4,268,Wolfcamp,,NA,US,Tseajaia campi
1337193,occ,NA,,180382,members,Eryops grandis,species,345659,,Eryops grandis,NA,species,345657,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-106.659729,36.123783,Anderson Quarry,NA,(UCMP locality V3431) (NMMNH locality L 4991),US,New Mexico,Rio Arriba,stated in text,6,outcrop,"Loaction lies approximately 4km south of Arroyo del Agua village in Rio Arriba county, New Mexico.",gp_mid,-34.1,4.51,101,US,FED,Arroyo del Agua,Cutler,,,,,,,,,NA,,"""The Anderson quarry consists of light gray shale with lenses of crossbedded sandstone capped by numerous, light-colored marl layers. "" Lucas et al. (2005)","""shale""",gray,,,,sandstone,,,,,lacustrine indet.,,"Langston (1953) interpreted this deposit as belonging to a nearshore lake deposit, but Eberth (1985) interpreted it as a crevasse-channel deposit similar to the VanderHoof, Quarry Butte and Welles quarries.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 06:44,14/07/2016 06:44,NA,grandis,Eryops,59746,,296.4,268,Wolfcamp,,NA,US,Eryops grandis
1337195,occ,NA,,180382,members,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-106.659729,36.123783,Anderson Quarry,NA,(UCMP locality V3431) (NMMNH locality L 4991),US,New Mexico,Rio Arriba,stated in text,6,outcrop,"Loaction lies approximately 4km south of Arroyo del Agua village in Rio Arriba county, New Mexico.",gp_mid,-34.1,4.51,101,US,FED,Arroyo del Agua,Cutler,,,,,,,,,NA,,"""The Anderson quarry consists of light gray shale with lenses of crossbedded sandstone capped by numerous, light-colored marl layers. "" Lucas et al. (2005)","""shale""",gray,,,,sandstone,,,,,lacustrine indet.,,"Langston (1953) interpreted this deposit as belonging to a nearshore lake deposit, but Eberth (1985) interpreted it as a crevasse-channel deposit similar to the VanderHoof, Quarry Butte and Welles quarries.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 06:44,14/07/2016 06:44,NA,sp.,Diadectes,59746,,296.4,268,Wolfcamp,,NA,US,Diadectes sp.
1337196,occ,NA,,180382,members,Bolosaurus sp.,genus,37511,,Bolosaurus,NA,genus,37511,Lucas et al.,2005,Chordata,33815,Reptilia,36322,,NA,Bolosauridae,37510,37511,NA,NA,NA,,-106.659729,36.123783,Anderson Quarry,NA,(UCMP locality V3431) (NMMNH locality L 4991),US,New Mexico,Rio Arriba,stated in text,6,outcrop,"Loaction lies approximately 4km south of Arroyo del Agua village in Rio Arriba county, New Mexico.",gp_mid,-34.1,4.51,101,US,FED,Arroyo del Agua,Cutler,,,,,,,,,NA,,"""The Anderson quarry consists of light gray shale with lenses of crossbedded sandstone capped by numerous, light-colored marl layers. "" Lucas et al. (2005)","""shale""",gray,,,,sandstone,,,,,lacustrine indet.,,"Langston (1953) interpreted this deposit as belonging to a nearshore lake deposit, but Eberth (1985) interpreted it as a crevasse-channel deposit similar to the VanderHoof, Quarry Butte and Welles quarries.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Bolosaurus,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 06:44,14/07/2016 06:44,NA,sp.,Bolosaurus,59746,,296.4,268,Wolfcamp,,NA,US,Bolosaurus sp.
1337197,occ,NA,,180382,members,Ophiacodon sp.,genus,38888,,Ophiacodon,NA,genus,38888,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-106.659729,36.123783,Anderson Quarry,NA,(UCMP locality V3431) (NMMNH locality L 4991),US,New Mexico,Rio Arriba,stated in text,6,outcrop,"Loaction lies approximately 4km south of Arroyo del Agua village in Rio Arriba county, New Mexico.",gp_mid,-34.1,4.51,101,US,FED,Arroyo del Agua,Cutler,,,,,,,,,NA,,"""The Anderson quarry consists of light gray shale with lenses of crossbedded sandstone capped by numerous, light-colored marl layers. "" Lucas et al. (2005)","""shale""",gray,,,,sandstone,,,,,lacustrine indet.,,"Langston (1953) interpreted this deposit as belonging to a nearshore lake deposit, but Eberth (1985) interpreted it as a crevasse-channel deposit similar to the VanderHoof, Quarry Butte and Welles quarries.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 06:44,14/07/2016 06:44,NA,sp.,Ophiacodon,59746,,296.4,268,Wolfcamp,,NA,US,Ophiacodon sp.
1337198,occ,NA,,180382,members,cf. Sphenacodon ferocior,species,122488,,Sphenacodon ferocior,NA,species,122488,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,,-106.659729,36.123783,Anderson Quarry,NA,(UCMP locality V3431) (NMMNH locality L 4991),US,New Mexico,Rio Arriba,stated in text,6,outcrop,"Loaction lies approximately 4km south of Arroyo del Agua village in Rio Arriba county, New Mexico.",gp_mid,-34.1,4.51,101,US,FED,Arroyo del Agua,Cutler,,,,,,,,,NA,,"""The Anderson quarry consists of light gray shale with lenses of crossbedded sandstone capped by numerous, light-colored marl layers. "" Lucas et al. (2005)","""shale""",gray,,,,sandstone,,,,,lacustrine indet.,,"Langston (1953) interpreted this deposit as belonging to a nearshore lake deposit, but Eberth (1985) interpreted it as a crevasse-channel deposit similar to the VanderHoof, Quarry Butte and Welles quarries.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,cf.,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,697,R. Butler,E. Dunne,E. Dunne,14/07/2016 06:44,10/08/2016 11:06,NA,ferocior,Sphenacodon,59746,,296.4,268,Wolfcamp,,NA,US,Sphenacodon ferocior
1337201,occ,NA,,180383,members,Chenoprosopus milleri,species,139020,,Chenoprosopus milleri,NA,species,139020,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Cochleosauridae,36999,37000,NA,NA,NA,,-106.621315,36.139988,Quarry butte,NA,"UCMP locality V3529, NMMNH locality L 4707",US,New Mexico,Rio Arriba,stated in text,6,small collection,"Locality lies SSE of the village of Arroyo del Agua, between the Welles and Van der Hoof quarries. See map on page 289 of Lucas et al. (2005)",gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,group of beds,,,,,,,NA,Chama Basin,"""Lithologically, the Quarry Butte locality consists of shale similar to those of the two nearby quarries, which are capped by crossbedded sandstones and underlain by marls. The only lithologically distinct characteristic of the site is a series of hard, lenticular, calcareous lenses in the shale."" Lucas et al. (2005)",claystone,"brown,green",,,,siltstone,,,,,lacustrine indet.,,"The Welles quarry, VanderHoof quarry and Quarry Butte locality were interpreted by Langston (1953) as belonging to a single large lake deposit, due to their similar lithologies and verte- brate assemblages. However, Berman et al. (1988) interpreted the quarries as ephemeral crevasse channels that were temporary sites of standing water within a locally anastomosed river system.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"NMMNH,UCMP",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Chenoprosopus,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 06:56,14/07/2016 06:56,NA,milleri,Chenoprosopus,59746,,296.4,268,Wolfcamp,,NA,US,Chenoprosopus milleri
1337202,occ,NA,,180383,members,Eryops grandis,species,345659,,Eryops grandis,NA,species,345657,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-106.621315,36.139988,Quarry butte,NA,"UCMP locality V3529, NMMNH locality L 4707",US,New Mexico,Rio Arriba,stated in text,6,small collection,"Locality lies SSE of the village of Arroyo del Agua, between the Welles and Van der Hoof quarries. See map on page 289 of Lucas et al. (2005)",gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,group of beds,,,,,,,NA,Chama Basin,"""Lithologically, the Quarry Butte locality consists of shale similar to those of the two nearby quarries, which are capped by crossbedded sandstones and underlain by marls. The only lithologically distinct characteristic of the site is a series of hard, lenticular, calcareous lenses in the shale."" Lucas et al. (2005)",claystone,"brown,green",,,,siltstone,,,,,lacustrine indet.,,"The Welles quarry, VanderHoof quarry and Quarry Butte locality were interpreted by Langston (1953) as belonging to a single large lake deposit, due to their similar lithologies and verte- brate assemblages. However, Berman et al. (1988) interpreted the quarries as ephemeral crevasse channels that were temporary sites of standing water within a locally anastomosed river system.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"NMMNH,UCMP",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 06:56,14/07/2016 06:56,NA,grandis,Eryops,59746,,296.4,268,Wolfcamp,,NA,US,Eryops grandis
1337203,occ,NA,,180383,members,Platyhystrix rugosus,species,345923,,Platyhystrix rugosus,NA,species,194929,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37034,NA,NA,NA,,-106.621315,36.139988,Quarry butte,NA,"UCMP locality V3529, NMMNH locality L 4707",US,New Mexico,Rio Arriba,stated in text,6,small collection,"Locality lies SSE of the village of Arroyo del Agua, between the Welles and Van der Hoof quarries. See map on page 289 of Lucas et al. (2005)",gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,group of beds,,,,,,,NA,Chama Basin,"""Lithologically, the Quarry Butte locality consists of shale similar to those of the two nearby quarries, which are capped by crossbedded sandstones and underlain by marls. The only lithologically distinct characteristic of the site is a series of hard, lenticular, calcareous lenses in the shale."" Lucas et al. (2005)",claystone,"brown,green",,,,siltstone,,,,,lacustrine indet.,,"The Welles quarry, VanderHoof quarry and Quarry Butte locality were interpreted by Langston (1953) as belonging to a single large lake deposit, due to their similar lithologies and verte- brate assemblages. However, Berman et al. (1988) interpreted the quarries as ephemeral crevasse channels that were temporary sites of standing water within a locally anastomosed river system.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"NMMNH,UCMP",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Platyhystrix,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 06:56,14/07/2016 06:56,NA,rugosus,Platyhystrix,59746,,296.4,268,Wolfcamp,,NA,US,Platyhystrix rugosus
1337204,occ,NA,,180383,members,Diadectes lentus,species,346261,,Diadectes lentus,NA,species,120884,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-106.621315,36.139988,Quarry butte,NA,"UCMP locality V3529, NMMNH locality L 4707",US,New Mexico,Rio Arriba,stated in text,6,small collection,"Locality lies SSE of the village of Arroyo del Agua, between the Welles and Van der Hoof quarries. See map on page 289 of Lucas et al. (2005)",gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,group of beds,,,,,,,NA,Chama Basin,"""Lithologically, the Quarry Butte locality consists of shale similar to those of the two nearby quarries, which are capped by crossbedded sandstones and underlain by marls. The only lithologically distinct characteristic of the site is a series of hard, lenticular, calcareous lenses in the shale."" Lucas et al. (2005)",claystone,"brown,green",,,,siltstone,,,,,lacustrine indet.,,"The Welles quarry, VanderHoof quarry and Quarry Butte locality were interpreted by Langston (1953) as belonging to a single large lake deposit, due to their similar lithologies and verte- brate assemblages. However, Berman et al. (1988) interpreted the quarries as ephemeral crevasse channels that were temporary sites of standing water within a locally anastomosed river system.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"NMMNH,UCMP",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 06:56,14/07/2016 06:56,NA,lentus,Diadectes,59746,,296.4,268,Wolfcamp,,NA,US,Diadectes lentus
1337205,occ,NA,,180383,members,Ophiacodon mirus,species,123418,,Ophiacodon mirus,NA,species,123418,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-106.621315,36.139988,Quarry butte,NA,"UCMP locality V3529, NMMNH locality L 4707",US,New Mexico,Rio Arriba,stated in text,6,small collection,"Locality lies SSE of the village of Arroyo del Agua, between the Welles and Van der Hoof quarries. See map on page 289 of Lucas et al. (2005)",gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,group of beds,,,,,,,NA,Chama Basin,"""Lithologically, the Quarry Butte locality consists of shale similar to those of the two nearby quarries, which are capped by crossbedded sandstones and underlain by marls. The only lithologically distinct characteristic of the site is a series of hard, lenticular, calcareous lenses in the shale."" Lucas et al. (2005)",claystone,"brown,green",,,,siltstone,,,,,lacustrine indet.,,"The Welles quarry, VanderHoof quarry and Quarry Butte locality were interpreted by Langston (1953) as belonging to a single large lake deposit, due to their similar lithologies and verte- brate assemblages. However, Berman et al. (1988) interpreted the quarries as ephemeral crevasse channels that were temporary sites of standing water within a locally anastomosed river system.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"NMMNH,UCMP",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 06:56,14/07/2016 06:56,NA,mirus,Ophiacodon,59746,,296.4,268,Wolfcamp,,NA,US,Ophiacodon mirus
1337206,occ,NA,,180383,members,Sphenacodon ferox,species,122487,,Sphenacodon ferox,NA,species,122487,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,,-106.621315,36.139988,Quarry butte,NA,"UCMP locality V3529, NMMNH locality L 4707",US,New Mexico,Rio Arriba,stated in text,6,small collection,"Locality lies SSE of the village of Arroyo del Agua, between the Welles and Van der Hoof quarries. See map on page 289 of Lucas et al. (2005)",gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,group of beds,,,,,,,NA,Chama Basin,"""Lithologically, the Quarry Butte locality consists of shale similar to those of the two nearby quarries, which are capped by crossbedded sandstones and underlain by marls. The only lithologically distinct characteristic of the site is a series of hard, lenticular, calcareous lenses in the shale."" Lucas et al. (2005)",claystone,"brown,green",,,,siltstone,,,,,lacustrine indet.,,"The Welles quarry, VanderHoof quarry and Quarry Butte locality were interpreted by Langston (1953) as belonging to a single large lake deposit, due to their similar lithologies and verte- brate assemblages. However, Berman et al. (1988) interpreted the quarries as ephemeral crevasse channels that were temporary sites of standing water within a locally anastomosed river system.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"NMMNH,UCMP",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 06:56,14/07/2016 06:56,NA,ferox,Sphenacodon,59746,,296.4,268,Wolfcamp,,NA,US,Sphenacodon ferox
1337209,occ,NA,,180384,members,Chenoprosopus milleri,species,139020,,Chenoprosopus milleri,NA,species,139020,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Cochleosauridae,36999,37000,NA,NA,NA,,-106.621315,36.139988,Welles Quarry (Arroyo del Agua),NA,"UCMP locality 3528, NMMNH locality L 4825",US,New Mexico,Rio Arriba,stated in text,6,small collection,"Locality lies SSE of the village of Arroyo del Agua, between the Quarry Butte and Van der Hoof quarry. See map on page 289 of Lucas et al. (2005)",gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,group of beds,,,,,,,NA,Chama Basin,"""The Welles quarry is similar lithologically to the VanderHoof quarry [The VanderHoof quarry is in green and brown micaceous clay and siltstone that progressively becomes lighter colored towards its top. These clays and siltstones are capped by a medium-grained crossbedded sandstone and underlain by a layer of marl and spherical carbonate concretions.]."" Lucas et al. (2005)",siltstone,"brown,green",,,,claystone,,,,,lacustrine indet.,,"The Welles quarry, VanderHoof quarry and Quarry Butte locality were interpreted by Langston (1953) as belonging to a single large lake deposit, due to their similar lithologies and verte- brate assemblages. However, Berman et al. (1988) interpreted the quarries as ephemeral crevasse channels that were temporary sites of standing water within a locally anastomosed river system.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"NMMNH,UCMP",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Chenoprosopus,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 07:01,14/07/2016 07:01,NA,milleri,Chenoprosopus,59746,,296.4,268,Wolfcamp,,NA,US,Chenoprosopus milleri
1337210,occ,NA,,180384,members,Eryops grandis,species,345659,,Eryops grandis,NA,species,345657,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-106.621315,36.139988,Welles Quarry (Arroyo del Agua),NA,"UCMP locality 3528, NMMNH locality L 4825",US,New Mexico,Rio Arriba,stated in text,6,small collection,"Locality lies SSE of the village of Arroyo del Agua, between the Quarry Butte and Van der Hoof quarry. See map on page 289 of Lucas et al. (2005)",gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,group of beds,,,,,,,NA,Chama Basin,"""The Welles quarry is similar lithologically to the VanderHoof quarry [The VanderHoof quarry is in green and brown micaceous clay and siltstone that progressively becomes lighter colored towards its top. These clays and siltstones are capped by a medium-grained crossbedded sandstone and underlain by a layer of marl and spherical carbonate concretions.]."" Lucas et al. (2005)",siltstone,"brown,green",,,,claystone,,,,,lacustrine indet.,,"The Welles quarry, VanderHoof quarry and Quarry Butte locality were interpreted by Langston (1953) as belonging to a single large lake deposit, due to their similar lithologies and verte- brate assemblages. However, Berman et al. (1988) interpreted the quarries as ephemeral crevasse channels that were temporary sites of standing water within a locally anastomosed river system.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"NMMNH,UCMP",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 07:01,14/07/2016 07:01,NA,grandis,Eryops,59746,,296.4,268,Wolfcamp,,NA,US,Eryops grandis
1337211,occ,NA,,180384,members,Zatrachys serratus,species,255221,,Zatrachys serratus,NA,species,255221,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,,-106.621315,36.139988,Welles Quarry (Arroyo del Agua),NA,"UCMP locality 3528, NMMNH locality L 4825",US,New Mexico,Rio Arriba,stated in text,6,small collection,"Locality lies SSE of the village of Arroyo del Agua, between the Quarry Butte and Van der Hoof quarry. See map on page 289 of Lucas et al. (2005)",gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,group of beds,,,,,,,NA,Chama Basin,"""The Welles quarry is similar lithologically to the VanderHoof quarry [The VanderHoof quarry is in green and brown micaceous clay and siltstone that progressively becomes lighter colored towards its top. These clays and siltstones are capped by a medium-grained crossbedded sandstone and underlain by a layer of marl and spherical carbonate concretions.]."" Lucas et al. (2005)",siltstone,"brown,green",,,,claystone,,,,,lacustrine indet.,,"The Welles quarry, VanderHoof quarry and Quarry Butte locality were interpreted by Langston (1953) as belonging to a single large lake deposit, due to their similar lithologies and verte- brate assemblages. However, Berman et al. (1988) interpreted the quarries as ephemeral crevasse channels that were temporary sites of standing water within a locally anastomosed river system.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"NMMNH,UCMP",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 07:01,14/07/2016 07:01,NA,serratus,Zatrachys,59746,,296.4,268,Wolfcamp,,NA,US,Zatrachys serratus
1337212,occ,NA,,180384,members,Platyhystrix rugosus,species,345923,,Platyhystrix rugosus,NA,species,194929,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37034,NA,NA,NA,,-106.621315,36.139988,Welles Quarry (Arroyo del Agua),NA,"UCMP locality 3528, NMMNH locality L 4825",US,New Mexico,Rio Arriba,stated in text,6,small collection,"Locality lies SSE of the village of Arroyo del Agua, between the Quarry Butte and Van der Hoof quarry. See map on page 289 of Lucas et al. (2005)",gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,group of beds,,,,,,,NA,Chama Basin,"""The Welles quarry is similar lithologically to the VanderHoof quarry [The VanderHoof quarry is in green and brown micaceous clay and siltstone that progressively becomes lighter colored towards its top. These clays and siltstones are capped by a medium-grained crossbedded sandstone and underlain by a layer of marl and spherical carbonate concretions.]."" Lucas et al. (2005)",siltstone,"brown,green",,,,claystone,,,,,lacustrine indet.,,"The Welles quarry, VanderHoof quarry and Quarry Butte locality were interpreted by Langston (1953) as belonging to a single large lake deposit, due to their similar lithologies and verte- brate assemblages. However, Berman et al. (1988) interpreted the quarries as ephemeral crevasse channels that were temporary sites of standing water within a locally anastomosed river system.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"NMMNH,UCMP",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Platyhystrix,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 07:01,14/07/2016 07:01,NA,rugosus,Platyhystrix,59746,,296.4,268,Wolfcamp,,NA,US,Platyhystrix rugosus
1337213,occ,NA,,180384,members,Diadectes lentus,species,346261,,Diadectes lentus,NA,species,120884,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-106.621315,36.139988,Welles Quarry (Arroyo del Agua),NA,"UCMP locality 3528, NMMNH locality L 4825",US,New Mexico,Rio Arriba,stated in text,6,small collection,"Locality lies SSE of the village of Arroyo del Agua, between the Quarry Butte and Van der Hoof quarry. See map on page 289 of Lucas et al. (2005)",gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,group of beds,,,,,,,NA,Chama Basin,"""The Welles quarry is similar lithologically to the VanderHoof quarry [The VanderHoof quarry is in green and brown micaceous clay and siltstone that progressively becomes lighter colored towards its top. These clays and siltstones are capped by a medium-grained crossbedded sandstone and underlain by a layer of marl and spherical carbonate concretions.]."" Lucas et al. (2005)",siltstone,"brown,green",,,,claystone,,,,,lacustrine indet.,,"The Welles quarry, VanderHoof quarry and Quarry Butte locality were interpreted by Langston (1953) as belonging to a single large lake deposit, due to their similar lithologies and verte- brate assemblages. However, Berman et al. (1988) interpreted the quarries as ephemeral crevasse channels that were temporary sites of standing water within a locally anastomosed river system.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"NMMNH,UCMP",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 07:01,14/07/2016 07:01,NA,lentus,Diadectes,59746,,296.4,268,Wolfcamp,,NA,US,Diadectes lentus
1337214,occ,NA,,180384,members,Ophiacodon mirus,species,123418,,Ophiacodon mirus,NA,species,123418,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-106.621315,36.139988,Welles Quarry (Arroyo del Agua),NA,"UCMP locality 3528, NMMNH locality L 4825",US,New Mexico,Rio Arriba,stated in text,6,small collection,"Locality lies SSE of the village of Arroyo del Agua, between the Quarry Butte and Van der Hoof quarry. See map on page 289 of Lucas et al. (2005)",gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,group of beds,,,,,,,NA,Chama Basin,"""The Welles quarry is similar lithologically to the VanderHoof quarry [The VanderHoof quarry is in green and brown micaceous clay and siltstone that progressively becomes lighter colored towards its top. These clays and siltstones are capped by a medium-grained crossbedded sandstone and underlain by a layer of marl and spherical carbonate concretions.]."" Lucas et al. (2005)",siltstone,"brown,green",,,,claystone,,,,,lacustrine indet.,,"The Welles quarry, VanderHoof quarry and Quarry Butte locality were interpreted by Langston (1953) as belonging to a single large lake deposit, due to their similar lithologies and verte- brate assemblages. However, Berman et al. (1988) interpreted the quarries as ephemeral crevasse channels that were temporary sites of standing water within a locally anastomosed river system.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"NMMNH,UCMP",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 07:01,14/07/2016 07:01,NA,mirus,Ophiacodon,59746,,296.4,268,Wolfcamp,,NA,US,Ophiacodon mirus
1337215,occ,NA,,180384,members,Sphenacodon ferox,species,122487,,Sphenacodon ferox,NA,species,122487,Lucas et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,,-106.621315,36.139988,Welles Quarry (Arroyo del Agua),NA,"UCMP locality 3528, NMMNH locality L 4825",US,New Mexico,Rio Arriba,stated in text,6,small collection,"Locality lies SSE of the village of Arroyo del Agua, between the Quarry Butte and Van der Hoof quarry. See map on page 289 of Lucas et al. (2005)",gp_mid,-34.07,4.5,101,US,FED,El Cobre Canyon,Cutler,,group of beds,,,,,,,NA,Chama Basin,"""The Welles quarry is similar lithologically to the VanderHoof quarry [The VanderHoof quarry is in green and brown micaceous clay and siltstone that progressively becomes lighter colored towards its top. These clays and siltstones are capped by a medium-grained crossbedded sandstone and underlain by a layer of marl and spherical carbonate concretions.]."" Lucas et al. (2005)",siltstone,"brown,green",,,,claystone,,,,,lacustrine indet.,,"The Welles quarry, VanderHoof quarry and Quarry Butte locality were interpreted by Langston (1953) as belonging to a single large lake deposit, due to their similar lithologies and verte- brate assemblages. However, Berman et al. (1988) interpreted the quarries as ephemeral crevasse channels that were temporary sites of standing water within a locally anastomosed river system.",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,"NMMNH,UCMP",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,vertebrate,"S. G. Lucas, S. K. Harris, and J. A. Spielmann, D. S. Berman, A. C. Henrici, A. B. Heckert, K. E. Zeigler, L. F. Rinehart. 2005. Early Permian Vertebrate Assemblage and its Biostratigraphic Significance, Arroyo del Agua, Rio Arriba County, New Mexico. New Mexico Geological Society, 56th Field Conference Guidebook, Geology of the Chama Basin ",327,697,0,R. Butler,E. Dunne,,14/07/2016 07:01,14/07/2016 07:01,NA,ferox,Sphenacodon,59746,,296.4,268,Wolfcamp,,NA,US,Sphenacodon ferox
1337246,occ,NA,,179964,members,Lafonius lehmani,species,336709,,Lafonius lehmani,NA,species,336709,Hunt et al.,1992,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36987,NA,NA,NA,,-106.33754,35.001019,Kinney Brick Company Quarry,NA,,US,New Mexico,Bernalillo,stated in text,6,outcrop,"SE1/4 sec. 18, T9N, R6E, Bernalillo County, New Mexico, USA",gp_mid,-35.39,2.01,101,US,FED,Wild Cow,, Pine Shadow,,,,,,,,NA,"In Schoch & Milner (2014; Palaeoherpetology Handbook) the formation is noted to be the Atrasado Formation, but in original paper it is recorded as the Wild Cow Formation. ""The vertebrate fossils of the Kinney Brick locality are recovered from the Pine Shadow Member of the Wild Cow Formation in Bernalillo County, New Mexico. Based on fusulinids, the Pine Shadow Member is assigned an early Virgilian age, and approximately 28 m of the upper part of the member are exposed in the quarry."" Kissel (2010)",The fossils are produced from the lowermost 0.5 m of shale and shaly limestone above the micritic limestone that floors the quarry.,"""shale""",,,,Y,"""limestone""",,,,Y,lagoonal,,"""Excavations in the Kinney Brick Company Quarry expose about 27 m of the Pine Shadow Member of the Wild Cow Formation (LUCAS & HUBER 1991; KUES & LUCAS 1992). There is broad consensus that this sequence represents a prograding delta complex (KUES & LUCAS 1992; LORENZ et al. 1992). However, there is some disagreement as to the origin of the laminated shale that yielded the amphibian specimens. Most authors, including ourselves, interpret this cyclically-bedded sequence to represent tidal rhythmites (FELDMAN et al. 1992; ARCHER & CLARK 1992), but others (e. g., HUBER 1992) prefer a deeper water, varve model. "" Hunt et al. (1996)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,NMMNH,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Lafonius,,NA,NA,vertebrate,"A. P. Hunt, S. G. Lucas, and D. S. Berman. 1992. The Late Pennsylvanian amphibian fauna of the Kinney Quarry, central New Mexico. New Mexico Bureau of Mines and Mineral Resources Bulletin 138:211-220",327,697,0,R. Butler,E. Dunne,,14/07/2016 09:00,14/07/2016 09:00,NA,lehmani,Lafonius,59862,,303.4,298.9,Virgilian,,NA,US,Lafonius lehmani
1337280,occ,NA,,180393,members,n. gen. Brevidorsum n. sp. profundum,species,345263,,Brevidorsum profundum,NA,species,345263,Carroll,1964,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37023,NA,NA,NA,,-98.462326,33.529819,North of the west fork of the Trinity River,NA,"Trinity River West Fork, Archer County",US,Texas,Archer,based on nearby landmark,6,,"Coordinates based on location north of the West Fork of the Trinity River located in Archer County. \r\n""Texan Emigration and Land Co. section 1834"", Carroll (1964)",gp_mid,-30.28,-1.92,101,US,,,Wichita,,bed,,,,,,,NA,"""Near Pueblo-Moran Boundary""\r\nStratography determined using Wellstead (1991)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,Romer,1948,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Brevidorsum,n. gen.,NA,NA,vertebrate,R. L. Carroll. 1964. Early evolution of the dissorophid amphibians. Bulletin of the Museum of Comparative Zoology 131:161-250,327,697,0,R. Butler,E. Dunne,,15/07/2016 06:07,15/07/2016 06:07,NA,profundum,Brevidorsum,59694,n. sp.,298.9,290.1,Asselian,Sakmarian,NA,US,Brevidorsum profundum
1337284,occ,NA,,11152,,Parioxys ferricolus,species,345270,,Parioxys ferricolus,NA,species,345270,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37052,NA,NA,NA,,-98.949997,33.633331,Fulda,NA,USGS locality number 8877,US,Texas,Baylor,based on nearby landmark,minutes,small collection,"The bank of the stream at the crossing of the old road, one fourth mile south of the ford of Little Wichita River, 4 miles southeast of Fulda, a station in Baylor County. ",gp_mid,-30.27,-1.12,101,US,,Belle Plains,,,group of beds,,,,,,,NA,,the plant-bearing shale is easily eroded and the original deposit probably has been totally destroyed or obscured,"""shale""",,poorly lithified,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,adpression,,,,,,,,,,NA,,,taxonomic,"surface (in situ),field collection",USNM,,,,,,"These specimens were among the collections made by David White in 1910. Material from this area was the source of White's paper (White, D. The characters of the fossil plant Gigantopteris Schenk and its occurence in North America. Proc. U.S. Nat. Mus. 41:493-516. 1912.) dealing with Gigantopteris americana.\r\n\r\nHowever, the material discussed in Mamay 1954, 1976 is a mixture of newly collected material and White's material. Mamay (1976) states that he was unable to exactly relocate White's localities, although the name of one of White's localities (Castle Hollow) may correspond to the description of Mamay (1976) of a broad depression with fossiliferous shale outcropping around its rim.",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Parioxys,,NA,NA,paleobotany,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,15/07/2016 06:34,15/07/2016 06:34,4100,ferricolus,Parioxys,57795,,295.5,272.3,Sakmarian,Kungurian,NA,US,Parioxys ferricolus
1337285,occ,NA,,28238,,Parioxys ferricolus,species,345270,,Parioxys ferricolus,NA,species,345270,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37052,NA,NA,NA,,-98.901947,33.740276,"Tit Mountain, 21 (Belle Plains Formation)",NA,"Locality 21 (Romer 1928), Locality Vd (Romer & Price 1940), Corn Mountain, Corn Hill, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Tit Mountain or Corn Hill, an elevation just northeast of Dundee"" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 500 feet above the Coleman Junction."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Not the same as ""South side of Tit Mountain butte, TMM 40031"" locality (Langston 1986); that collection was obviously made much later than the Tit Mountain collection of Romer (1928), which has less detailed locality data.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Parioxys,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,15/07/2016 06:34,15/07/2016 06:34,26948,ferricolus,Parioxys,57795,,290.1,279.3,Artinskian,,NA,US,Parioxys ferricolus
1337320,occ,NA,,84835,,Limnerpeton n. sp. elegans,species,336864,recombined as,Limnogyrinus elegans,NA,species,336864,Fritsch,1881,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Micromelerpetontidae,37041,255223,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Limnerpeton,,NA,NA,vertebrate,A. Fritsch. 1881. Fauna der Gaskohle und der Kalksteine der Permaformations Bohmens. Band 1. Heft 3. 1(3),327,327,327,R. Butler,R. Butler,R. Butler,15/07/2016 10:06,15/07/2016 10:07,28608,elegans,Limnogyrinus,58152,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Limnogyrinus elegans
1337325,occ,NA,,86946,,Baphetes minor,species,320862,nomen dubium,Baphetes,NA,genus,36970,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,,NA,Baphetidae,227378,36970,NA,NA,NA,,-64.451385,45.698612,"Joggins; Divison 4, Section XII, coal-group 26",NA,Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Division 4 ""of the section extends from McCairn's Cove to the end of the high cliff beyond 'Coal-mine Point'."" (Dawson, 1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173 p. 162); Lat long is approx. for Coal Mine Point",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XII",coal-group 26,,,,NA,"Coal-group 26 has a total thickness of 118 ft (including a 4 inch coaly shale). (Dawson, 1878 p. 170). Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","""Gray sandstone and shale, with erect Sigillaria; at four or five levels, and two Stigmarian underclays"" (Dawson, 1878 p. 170)",sandstone,gray,,,,claystone,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",,,snapshot,,,,,,,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" (Lyell, 1853, Quart. J. Geol. Soc. 9)",taxonomic,"field collection,survey of museum collection,observed (not collected)",,,,,"J. W. Dawson, P. W. McNaughton, among others",,,"Dawson (1878, Acadian Geology, 3rd ed.) reports Stigmaria sp. from this site","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Baphetes,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,15/07/2016 10:44,15/07/2016 10:44,28956,minor,Baphetes,57795,,318.1,314.6,Westphalian A,,NA,CA,Baphetes minor
1337414,occ,NA,,86946,,Trachystegos n. sp. megalodon,species,320816,,Trachystegos megalodon,NA,species,320816,Carroll and Gaskill,1978,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Pantylidae,37290,37292,NA,NA,NA,,-64.451385,45.698612,"Joggins; Divison 4, Section XII, coal-group 26",NA,Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Division 4 ""of the section extends from McCairn's Cove to the end of the high cliff beyond 'Coal-mine Point'."" (Dawson, 1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173 p. 162); Lat long is approx. for Coal Mine Point",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XII",coal-group 26,,,,NA,"Coal-group 26 has a total thickness of 118 ft (including a 4 inch coaly shale). (Dawson, 1878 p. 170). Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","""Gray sandstone and shale, with erect Sigillaria; at four or five levels, and two Stigmarian underclays"" (Dawson, 1878 p. 170)",sandstone,gray,,,,claystone,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",,,snapshot,,,,,,,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" (Lyell, 1853, Quart. J. Geol. Soc. 9)",taxonomic,"field collection,survey of museum collection,observed (not collected)",,,,,"J. W. Dawson, P. W. McNaughton, among others",,,"Dawson (1878, Acadian Geology, 3rd ed.) reports Stigmaria sp. from this site","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Trachystegos,,NA,NA,vertebrate,R. L. Carroll and P. Gaskill. 1978. The Order Microsauria. Memoirs of the American Philosophical Society 126:1-211,327,697,697,R. Butler,E. Dunne,E. Dunne,18/07/2016 05:34,18/07/2016 05:35,28956,megalodon,Trachystegos,28692,n. sp.,318.1,314.6,Westphalian A,,NA,CA,Trachystegos megalodon
1337415,occ,NA,,86946,,Asaphestera n. sp. intermedia,species,338119,,Asaphestera intermedia,NA,species,227002,Carroll and Gaskill,1978,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Tuditanidae,37280,37281,NA,NA,NA,,-64.451385,45.698612,"Joggins; Divison 4, Section XII, coal-group 26",NA,Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Division 4 ""of the section extends from McCairn's Cove to the end of the high cliff beyond 'Coal-mine Point'."" (Dawson, 1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173 p. 162); Lat long is approx. for Coal Mine Point",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XII",coal-group 26,,,,NA,"Coal-group 26 has a total thickness of 118 ft (including a 4 inch coaly shale). (Dawson, 1878 p. 170). Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","""Gray sandstone and shale, with erect Sigillaria; at four or five levels, and two Stigmarian underclays"" (Dawson, 1878 p. 170)",sandstone,gray,,,,claystone,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",,,snapshot,,,,,,,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" (Lyell, 1853, Quart. J. Geol. Soc. 9)",taxonomic,"field collection,survey of museum collection,observed (not collected)",,,,,"J. W. Dawson, P. W. McNaughton, among others",,,"Dawson (1878, Acadian Geology, 3rd ed.) reports Stigmaria sp. from this site","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Asaphestera,,NA,NA,vertebrate,R. L. Carroll and P. Gaskill. 1978. The Order Microsauria. Memoirs of the American Philosophical Society 126:1-211,327,697,697,R. Butler,E. Dunne,E. Dunne,18/07/2016 05:34,18/07/2016 05:35,28956,intermedia,Asaphestera,28692,n. sp.,318.1,314.6,Westphalian A,,NA,CA,Asaphestera intermedia
1337416,occ,NA,,86946,,Dendrerpeton n. sp. confusum,species,256961,,Dendrerpeton confusum,NA,species,256961,Clack and Milner,2015,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dendrerpetonidae,36994,36995,NA,NA,NA,,-64.451385,45.698612,"Joggins; Divison 4, Section XII, coal-group 26",NA,Coal Measures; Head of Bay of Fundy,CA,Nova Scotia,Cumberland,estimated from map,seconds,outcrop,"Division 4 ""of the section extends from McCairn's Cove to the end of the high cliff beyond 'Coal-mine Point'."" (Dawson, 1878, Acadian Geology, 3rd edn.; 1882, Phil. Trans. R. Soc. Lond., 173 p. 162); Lat long is approx. for Coal Mine Point",gp_mid,-10.29,-13.31,108,CA,,Joggins,Cumberland,,group of beds,,"Division 4, Section XII",coal-group 26,,,,NA,"Coal-group 26 has a total thickness of 118 ft (including a 4 inch coaly shale). (Dawson, 1878 p. 170). Currently, the Cumberland Group is considered eqivalent to Westphalian A (Langsettian) (see e. g. Holmes et al., 1989, J. Vert. Paleont. 19; or Falcon-Lang et al. 2006, J. Geol. Soc. Lond. 163).(TL)\r\n","""Gray sandstone and shale, with erect Sigillaria; at four or five levels, and two Stigmarian underclays"" (Dawson, 1878 p. 170)",sandstone,gray,,,,claystone,,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,"body,coalified",,,snapshot,,,,,,,NA,,"Vertebrate fossils are contained within a sandstone cast of the trunk within a ""cylinder of bark now turned to coal."" (Lyell, 1853, Quart. J. Geol. Soc. 9)",taxonomic,"field collection,survey of museum collection,observed (not collected)",,,,,"J. W. Dawson, P. W. McNaughton, among others",,,"Dawson (1878, Acadian Geology, 3rd ed.) reports Stigmaria sp. from this site","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Dendrerpeton,,NA,NA,vertebrate,"J. A. Clack and A. R. Milner. 2015. Handbook of Paleoherpetology, Part 3A1: Basal Tetrapoda. ",327,697,697,R. Butler,E. Dunne,E. Dunne,18/07/2016 05:34,18/07/2016 05:35,28956,confusum,Dendrerpeton,57666,n. sp.,318.1,314.6,Westphalian A,,NA,CA,Dendrerpeton confusum
1337443,occ,NA,,34761,,Aspidosaurus n. sp. novomexicanus,species,136991,,Aspidosaurus novomexicanus,NA,species,136991,Williston,1911,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37021,NA,NA,NA,,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Aspidosaurus,,NA,NA,vertebrate,S. W. Williston. 1911. American Permian Vertebrates ,327,697,697,R. Butler,E. Dunne,E. Dunne,18/07/2016 09:17,09/08/2016 06:23,43845,novomexicanus,Aspidosaurus,9228,n. sp.,303.4,298.9,Virgilian,,NA,US,Aspidosaurus novomexicanus
1337444,occ,NA,,173721,,Conjunctio sp.,genus,37026,,Conjunctio,NA,genus,37026,Carroll,1964,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37026,NA,NA,NA,,-98.201385,33.760277,Halsell Hill,NA,,US,Texas,Clay County,based on political unit,seconds,small collection,"Precise coordinates not available, coordinates based on the centre of the County",gp_mid,-30.08,-2.01,101,US,,Nocona,Wichita,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,some,some,,,,NA,,body,medium,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,A. S. Romer,April 18 1950,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Conjunctio,,NA,NA,,R. L. Carroll. 1964. Early evolution of the dissorophid amphibians. Bulletin of the Museum of Comparative Zoology 131:161-250,327,697,0,R. Butler,E. Dunne,,18/07/2016 09:22,18/07/2016 09:22,56628,sp.,Conjunctio,59694,,298.9,295.5,Asselian,,NA,US,Conjunctio sp.
1337445,occ,NA,,132657,,Archeria sp.,genus,37196,,Archeria,NA,genus,37196,Romer,1957,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,,-100.059998,32.5,Little Bitter Creek,NA,,US,Texas,Taylor,,2,,,gp_mid,-32.07,-2.24,101,US,,Moran,Wichita,,,,,,,,,NA,,,not reported,,,,,,,,,,marine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,,NA,NA,vertebrate,A. S. Romer. 1957. The Appendicular Skeleton of the Embolomerous Amphibian Archeria. Contributions from the Museum of Geology University of Michigan 13(5):103-159,327,697,0,R. Butler,E. Dunne,,18/07/2016 10:46,18/07/2016 10:46,42726,sp.,Archeria,59296,,298.9,295.5,Asselian,,NA,US,Archeria sp.
1337447,occ,NA,,28238,,Archeria sp.,genus,37196,,Archeria,NA,genus,37196,Romer,1957,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,,-98.901947,33.740276,"Tit Mountain, 21 (Belle Plains Formation)",NA,"Locality 21 (Romer 1928), Locality Vd (Romer & Price 1940), Corn Mountain, Corn Hill, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Tit Mountain or Corn Hill, an elevation just northeast of Dundee"" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 500 feet above the Coleman Junction."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Not the same as ""South side of Tit Mountain butte, TMM 40031"" locality (Langston 1986); that collection was obviously made much later than the Tit Mountain collection of Romer (1928), which has less detailed locality data.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,,NA,NA,vertebrate,A. S. Romer. 1957. The Appendicular Skeleton of the Embolomerous Amphibian Archeria. Contributions from the Museum of Geology University of Michigan 13(5):103-159,327,697,0,R. Butler,E. Dunne,,18/07/2016 10:50,18/07/2016 10:50,26948,sp.,Archeria,59296,,290.1,279.3,Artinskian,,NA,US,Archeria sp.
1337448,occ,NA,,28146,,Archeria sp.,genus,37196,,Archeria,NA,genus,37196,Romer,1957,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,,-98.901947,33.740276,"Slippery Creek, 20 (Belle Plains Formation)",NA,"Locality 20 (Romer 1928), Locality Vc (Romer & Price 1940), Lyle locality, Pearce locality, Young locality, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,local area,"""Slippery Creek is a tributary of the Little Wichita on the north side. Along it's course, nearly due south of Dundee, is a series of breaks. Lyle's, Pearce's, and Young's localities of Case were in this neighborhood."" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee, approx. 4 mi due north of locality.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,,NA,NA,vertebrate,A. S. Romer. 1957. The Appendicular Skeleton of the Embolomerous Amphibian Archeria. Contributions from the Museum of Geology University of Michigan 13(5):103-159,327,697,0,R. Butler,E. Dunne,,18/07/2016 10:51,18/07/2016 10:51,7693,sp.,Archeria,59296,,290.1,279.3,Artinskian,,NA,US,Archeria sp.
1337450,occ,NA,,28150,,Archeria sp.,genus,37196,,Archeria,NA,genus,37196,Romer,1957,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,,-98.92083,33.601391,"Godwin Creek, 14 (Admiral Formation)",NA,"Locality 14 (Romer 1928), Locality IVe (Romer & Price 1940), Southeast side of Godwin creek, faunal Zone 1, Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""specimens appear to come from the southeast side of this creek."" See detailed locality map in Romer 1928. ""Zone 1. Lat long is for Godwin Creek, USGS Dundee SW, Archer County.",gp_mid,-30.27,-1.17,101,US,,Admiral,Wichita,,group of beds,,,,,,,NA,"""The horizon is about 250-300 feet above the base of the formation."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\nthe Admiral Formation is entirely Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones.""\r\n\r\n","""shale""",red,,"argillaceous,sandy",,,,,,,terrestrial indet.,, terrestrial and near-shore deposition\n,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,"AMNH,FMNH,MCZ",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,,NA,NA,vertebrate,A. S. Romer. 1957. The Appendicular Skeleton of the Embolomerous Amphibian Archeria. Contributions from the Museum of Geology University of Michigan 13(5):103-159,327,697,0,R. Butler,E. Dunne,,18/07/2016 10:55,18/07/2016 10:55,7693,sp.,Archeria,59296,,290.1,279.3,Artinskian,,NA,US,Archeria sp.
1337451,occ,NA,,28145,,Archeria sp.,genus,37196,,Archeria,NA,genus,37196,Romer,1957,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,,-99.022781,33.687222,"South of Fulda, 19 (Belle Plains)",NA,"Locality 19 (Romer 1928), Locality Vb (Romer & Price 1940), S. of Fulda, Hackberry Creek, North Side Little Wichita, South Side Little Wichita, North Side of Godwin Creek, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""Numerous exposures occur in the valley of the Little Wichita south and southeast of Fulda."" Specimens are labeled with various locality names, see aka above. See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Fulda, approx. 2 mi north of locality.",gp_mid,-30.3,-1.05,101,US,,Petrolia,Wichita,,group of beds,,,,,,,NA,"""about 450-500 feet above the Coleman Junction Limestone, and not far below the Beaverburk."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,Cope,1908,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,,NA,NA,vertebrate,A. S. Romer. 1957. The Appendicular Skeleton of the Embolomerous Amphibian Archeria. Contributions from the Museum of Geology University of Michigan 13(5):103-159,327,697,0,R. Butler,E. Dunne,,18/07/2016 10:56,18/07/2016 10:56,28729,sp.,Archeria,59296,,290.1,279.3,Artinskian,,NA,US,Archeria sp.
1337465,occ,NA,,28267,,Trimerorhachis n. sp. greggi,species,345367,,Trimerorhachis greggi,NA,species,345367,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-99.26667,33.700001,"Craddock Bonebed, Brush Creek, 38 (Arroyo Formation)",NA,"Locality 38 (Romer 1928), Craddock's ranch, Craddock bone bed, Brushy Creek, Bushy Creek, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,minutes,local area,"""About seven miles north and somewhat west of Seymour lies Craddock's ranch, an area of 6 square miles, drained by Gray's Creek on the east and Brush Creek on the west. Numerous ""breaks"" are present in this region.."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for area south of Kemp Lake between Brushy Creek and Gray Creek. ",gp_mid,-29,1.73,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The beds average about 150 feet above the base of the Clear Fork."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,good,,,,#NAME?,,,,,NA,,"A large proportion of the remains recorded under entry 38 are from Craddock bone bed. (Romer 1928). \n""The material secured includes two or three hundred bones, none of them associated save those of Araeoscelis."" (Williston 1911)",taxonomic,"field collection,survey of museum collection","AMNH,BSP,FMNH,USNM",,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated but previously unpublished locality data.,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,19/07/2016 05:03,19/07/2016 05:03,9228,greggi,Trimerorhachis,57795,n. sp.,279.3,272.3,Kungurian,,NA,US,Trimerorhachis greggi
1337466,occ,NA,,180465,members,Trimerorhachis n. sp. sandovalensis,species,345366,,Trimerorhachis sandovalensis,NA,species,345366,Berman and Reisz,1980,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-106.744904,35.66658,Jemez River,NA,west side of Canyon de San Diego,US,New Mexico,Sandoval,stated in text,6,small collection,"Located on west side of Canyon de San Diego, west of State Highway 4 and along western edge of Jemez River, about 11.5km south of Jemez Springs, approximately lat 3540'N and long 10645'W, Sandoval County, New Mexico.",gp_mid,-34.43,4.18,101,US,FED,Abo/Cutler,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)",siltstone,"coarse,gray",poorly lithified,,Y,sandstone,red,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,"D. S. Berman and R. Reisz. 1980. A new species of Trimerorhachis (Amphibia, Temnospondyli) from the Lower Permian Abo Formation of New Mexico, with discussion of Permian faunal distributions in that state. Annals of Carnegie Museum 49(24):455-485",327,697,0,R. Butler,E. Dunne,,19/07/2016 05:23,19/07/2016 05:23,NA,sandovalensis,Trimerorhachis,59887,n. sp.,296.4,268,Wolfcamp,,NA,US,Trimerorhachis sandovalensis
1337581,occ,NA,,85292,,Tuditanus n. sp. tabulatus,species,192951,subjective synonym of,Isodectes obtusus,NA,species,137370,Moodie,1909,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Saurerpetontidae,36980,36983,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Tuditanus,,NA,NA,vertebrate,R. L. Moodie. 1909. A contribution to a monograph of the extinct Amphibia of North America. New forms from the Carboniferous. Journal of Geology 17(1):38-82,327,697,0,R. Butler,E. Dunne,,20/07/2016 05:50,20/07/2016 05:50,28831,tabulatus,Isodectes,28743,n. sp.,311.45,306.95,Westphalian D,,NA,US,Isodectes tabulatus
1337582,occ,NA,,165526,,Tuditanus n. sp. sculptilis,species,192953,subjective synonym of,Isodectes obtusus,NA,species,137370,Moodie,1909,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Saurerpetontidae,36980,36983,NA,NA,NA,,-80.474998,40.798,Cannelton,NA,,US,Pennsylvania,Beaver,based on nearby landmark,3,small collection,Coordinates based on the location of Cannelton,gp_mid,-21.08,-11.59,101,US,,Upper Kittanning Coal,Allegheny,,group of beds,,,,,,,NA,"""Coal Measures""",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,many,,,,,NA,,"body,adpression",,,snapshot,,dispersed,,,,,NA,,,taxonomic,survey of museum collection,,,,,R. D. Lacoe,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Tuditanus,,NA,NA,vertebrate,R. L. Moodie. 1909. A contribution to a monograph of the extinct Amphibia of North America. New forms from the Carboniferous. Journal of Geology 17(1):38-82,327,697,0,R. Butler,E. Dunne,,20/07/2016 05:57,20/07/2016 05:57,28740,sculptilis,Isodectes,28743,n. sp.,318.1,306.95,Westphalian,,NA,US,Isodectes sculptilis
1337583,occ,NA,,165526,,Tuditanus n. sp. minimus,species,192952,subjective synonym of,Isodectes obtusus,NA,species,137370,Moodie,1909,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Saurerpetontidae,36980,36983,NA,NA,NA,,-80.474998,40.798,Cannelton,NA,,US,Pennsylvania,Beaver,based on nearby landmark,3,small collection,Coordinates based on the location of Cannelton,gp_mid,-21.08,-11.59,101,US,,Upper Kittanning Coal,Allegheny,,group of beds,,,,,,,NA,"""Coal Measures""",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,many,,,,,NA,,"body,adpression",,,snapshot,,dispersed,,,,,NA,,,taxonomic,survey of museum collection,,,,,R. D. Lacoe,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Tuditanus,,NA,NA,vertebrate,R. L. Moodie. 1909. A contribution to a monograph of the extinct Amphibia of North America. New forms from the Carboniferous. Journal of Geology 17(1):38-82,327,697,0,R. Butler,E. Dunne,,20/07/2016 05:57,20/07/2016 05:57,28740,minimus,Isodectes,28743,n. sp.,318.1,306.95,Westphalian,,NA,US,Isodectes minimus
1337584,occ,NA,,85292,,Colosteus n. sp. foveatus,species,345382,subjective synonym of,Isodectes obtusus,NA,species,137370,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Saurerpetontidae,36980,36983,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Colosteus,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,20/07/2016 06:09,20/07/2016 06:09,28831,foveatus,Isodectes,57795,n. sp.,311.45,306.95,Westphalian D,,NA,US,Isodectes foveatus
1337585,occ,NA,,176092,members,Isodectes obtusus,species,137434,,Isodectes obtusus,NA,species,137370,Hook and Baird,1994,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Saurerpetontidae,36980,36983,NA,NA,NA,,-80.612236,40.989132,Five Points Coal Mine,NA,,US,Ohio,Mahoning County,based on nearby landmark,6,outcrop,"""Five Points, south of Youngstown, Mahoning County, Ohio"" Sues et al. (2013) Atl Geol.",gp_mid,-18.98,-8.63,101,US,,,Allegheny,,,,,,,,,NA,,,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Isodectes,,NA,NA,vertebrate,"R. W. Hook and D. Baird. 1994. A new fish and tetrapod assemblage from the Allegheny Group (late Westphalian, Upper Carboniferous) of eastern Ohio, USA. In U. Heidtke (ed.), New Research on Permo-Carboniferous Faunas ",327,697,697,R. Butler,E. Dunne,E. Dunne,20/07/2016 06:16,20/07/2016 06:16,NA,obtusus,Isodectes,57803,,313.8,305.9,Desmoinesian,,NA,US,Isodectes obtusus
1337586,occ,NA,,79598,,Isodectes obtusus,species,137434,,Isodectes obtusus,NA,species,137370,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Saurerpetontidae,36980,36983,NA,NA,NA,,-88.139999,41.267223,Mazon Creek,NA,"Mazon Creek Vertebrate Fauna, Braidwood Fauna, pit 11",US,Illinois,Grundy/Will,based on political unit,seconds,local area,"Lat Long is for SW Will Co., Illinois",gp_mid,-23.34,-5.09,101,US,,Carbondale,,Francis Creek Shale,,,,,,,,NA,"""Francis Creek Shale above Morris (no. 2) Coal, Carbondale Formation, Westphalian D, Middle Pennsylvanian"" (Carroll & Baird, 1972)\r\nBaird et al. (1985) refer to the no. 2 coal as Colchester or Croweburg Coal Member.","""Concretions occur typically in laminated to weakly rippled, silty mudstone deposits which typically show little or no evidence of bioturbation. Small-scale sedimentary structures in nodule-bearing sequences include climbing ripple drift, and soft-sediment load-failure..."" (Baird et al., 1985 p.90). Note that this is a general description of the fossil bearing strata of the Francis Creek Shale Member which does not refer specifically to the occurences in the Mazon Creek area proper.",mudstone,"current ripples,deformed bedding",,silty,,siderite,nodular,,,Y,deltaic indet.,foreland basin,"""...these indicate rapid and often episodic mud deposition in interdistributary bay and prodelta settings."" (Baird et al., 1985 p.90)",macrofossils,,,,,,NA,,"mold/impression,concretion,soft parts,replaced with other",good,parautochthonous,,,,,,,,NA,,"""Outlines of the limbs can be seen in the matrix, indicating the extent of the soft tissue and the texture of the skin. The bone itself was represented by a very soft, claylike material that had been removed from the hard, ironstone matrix."" (Carroll, & Baird, 1972 p. 323)\r\nBones are replaced by clay minerals such as Kaolinite (Gregory, 1948 p. 637).",taxonomic,"mechanical,survey of museum collection","FMNH,MCZ,USNM,YPM","species names,ichnofossils",,,"R. L. Moodie, P. Turnbull, among others","1871, 1953",,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Isodectes,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,20/07/2016 06:22,20/07/2016 06:22,28608,obtusus,Isodectes,57795,,311.45,306.95,Westphalian D,,NA,US,Isodectes obtusus
1337587,occ,NA,,28264,,Trimerorhachis n. sp. conangulus,species,345389,subjective synonym of,Isodectes obtusus,NA,species,137370,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Saurerpetontidae,36980,36983,NA,NA,NA,,-99.23333,33.755833,"Indian Creek, 35 (Arroyo Formation)",NA,"Locality 35 (Romer 1928), Cacops bone bed, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Baylor,based on nearby landmark,seconds,local area,"""about 5 miles west of the Vernon road in the valley of the Wichita, not far from Indian Creek."" (Williston 1911) \n\n""collections are mainly from the region near its mouth [Lower Clear Fork]."" See detailed locality map in Romer 1928. "" Zone 4. Lower Clear Fork. Lat long is for Kemp Lake near today's mouth of Indian Creek. Numbered ""35"" with taxonomic list and on map, but is incorrectly numbered ""35"" in Romer text.",gp_mid,-28.95,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""The localities are about 100 to 150 feet above the Lueders limestone."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,occasional,"Thickness of the bone bed is about 2 feet. Many skeletons and partial associated elements. Those at the top are less concentrated, i.e., fewer skeletons that are more isolated, and less thickly encrusted by matrix. Lower skeletons lie closely packed together and are often cemented into large blocks. Skeletons are typically prone, though some are found in the supine position.",taxonomic,"bulk,field collection",,,,,,,"Chicago University Collections among others.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities. Based on the following statement, ""A large proportion of the specimens recorded from here are from the Cacops bone bed"" some of the specimens listed by Romer 1928 may be from farther afield than the specific gulley mentioned by Williston.","Romer (1928) provides a list of genotypes and holotypes (without authority data) with associated, previously unpublished locality data.","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,20/07/2016 06:42,20/07/2016 06:42,9228,conangulus,Isodectes,57795,n. sp.,279.3,272.3,Kungurian,,NA,US,Isodectes conangulus
1337590,occ,NA,,28256,,Isodectes obtusus,species,137434,,Isodectes obtusus,NA,species,137370,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Saurerpetontidae,36980,36983,NA,NA,NA,,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Isodectes,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,20/07/2016 07:01,20/07/2016 07:01,17702,obtusus,Isodectes,57795,,279.3,272.3,Kungurian,,NA,US,Isodectes obtusus
1337758,occ,NA,,84835,,Limnerpeton n. sp. laticeps,species,345448,recombined as,Mordex laticeps,NA,species,345448,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,345449,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Limnerpeton,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,22/07/2016 06:03,22/07/2016 06:03,28608,laticeps,Mordex,57795,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Mordex laticeps
1337765,occ,NA,,125662,,Mordex laticeps,species,345450,,Mordex laticeps,NA,species,345448,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trematopidae,37047,345449,NA,NA,NA,,13.395,49.814999,Tremosna,NA,"Temon̩, Temon",CZ,,,based on nearby landmark,3,outcrop,,gp_mid,19.75,0.69,305,CZ,,Kladno,,Nyrany,,,,,,,,NA,Tremosna in B̦hmen. Mittleres Obercarbon.,,not reported,,,,,coal,,,,,terrestrial indet.,rift,"Central-West Bohemian basin; extensional basin developed within Variscan zone along simple asymmetric mega-graben formed on the Central Bohemian and Litomerice fault zones, with some contribution from transtensional wrench faults.",macrofossils,,,,,,NA,,mold/impression,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Mordex,,NA,NA,"paleoentomology,vertebrate",R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,22/07/2016 06:06,22/07/2016 06:06,50906,laticeps,Mordex,57795,,311.45,306.95,Westphalian D,,NA,CZ,Mordex laticeps
1337842,occ,NA,,79598,,Mazonerpeton n. sp. longicaudatum,species,345452,subjective synonym of,Amphibamus grandiceps,NA,species,229305,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,37019,NA,NA,NA,,-88.139999,41.267223,Mazon Creek,NA,"Mazon Creek Vertebrate Fauna, Braidwood Fauna, pit 11",US,Illinois,Grundy/Will,based on political unit,seconds,local area,"Lat Long is for SW Will Co., Illinois",gp_mid,-23.34,-5.09,101,US,,Carbondale,,Francis Creek Shale,,,,,,,,NA,"""Francis Creek Shale above Morris (no. 2) Coal, Carbondale Formation, Westphalian D, Middle Pennsylvanian"" (Carroll & Baird, 1972)\r\nBaird et al. (1985) refer to the no. 2 coal as Colchester or Croweburg Coal Member.","""Concretions occur typically in laminated to weakly rippled, silty mudstone deposits which typically show little or no evidence of bioturbation. Small-scale sedimentary structures in nodule-bearing sequences include climbing ripple drift, and soft-sediment load-failure..."" (Baird et al., 1985 p.90). Note that this is a general description of the fossil bearing strata of the Francis Creek Shale Member which does not refer specifically to the occurences in the Mazon Creek area proper.",mudstone,"current ripples,deformed bedding",,silty,,siderite,nodular,,,Y,deltaic indet.,foreland basin,"""...these indicate rapid and often episodic mud deposition in interdistributary bay and prodelta settings."" (Baird et al., 1985 p.90)",macrofossils,,,,,,NA,,"mold/impression,concretion,soft parts,replaced with other",good,parautochthonous,,,,,,,,NA,,"""Outlines of the limbs can be seen in the matrix, indicating the extent of the soft tissue and the texture of the skin. The bone itself was represented by a very soft, claylike material that had been removed from the hard, ironstone matrix."" (Carroll, & Baird, 1972 p. 323)\r\nBones are replaced by clay minerals such as Kaolinite (Gregory, 1948 p. 637).",taxonomic,"mechanical,survey of museum collection","FMNH,MCZ,USNM,YPM","species names,ichnofossils",,,"R. L. Moodie, P. Turnbull, among others","1871, 1953",,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Mazonerpeton,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,22/07/2016 06:47,22/07/2016 06:47,28608,longicaudatum,Amphibamus,57795,n. sp.,311.45,306.95,Westphalian D,,NA,US,Amphibamus longicaudatum
1338117,occ,NA,,85300,,Aspidosaurus n. sp. binasser,species,345459,,Aspidosaurus binasser,NA,species,345459,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37021,NA,NA,NA,,-99.145836,33.751389,Lueders Fm. Locality 2,NA,Lake Kemp dam,US,Texas,Baylor,estimated from map,seconds,small collection,"""a bluff along the shore of Lake Kemp, beginning close to the southern end of the Lake Kemp dam.""\r\nfor details see map on p. 5 in Berman (1970)",gp_mid,-30.32,-0.89,101,US,,Lueders,Wichita,Maybelle limestone,bed,,,,,,,NA,8 feet below the Aa2 submember of the Maybelle limestone,"""The fossiliferous layer found at site 2 is a gray, clay-pebble conglomerate. The pebbles are generally under 0.5 inch in diameter and are surrounded by a gray argillaceous matrix.""",conglomerate,"pebbly,gray",,argillaceous,Y,,,,,,shallow subtidal indet.,foreland basin,"""This layer is hesistantly suspected of having been deposited in a near-shore, marine situation""","macrofossils,mesofossils",,,,,,NA,,body,variable,,snapshot,,,,common,,,NA,,,taxonomic,"surface (in situ),acetic,field collection",,some macrofossils,,,,,,"UCLA VP 2030 was originally identified as Captorhinus aguti by Berman (1970), based on Seltin's (1959, Field. Geol.) conclusion that Captorhinus is a monospecific genus. Given that currently there are three recognized species of Captorhinus, the specimen is left without assignment to a species in the taxonomic list. ","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Aspidosaurus,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,22/07/2016 09:50,22/07/2016 09:50,28758,binasser,Aspidosaurus,57795,n. sp.,290.1,272.3,Artinskian,Kungurian,NA,US,Aspidosaurus binasser
1338135,occ,NA,,13947,,cf. Aspidosaurus sp.,genus,37021,,Aspidosaurus,NA,genus,37021,May et al.,2011,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37021,NA,NA,NA,,-96.699997,34.933334,OMNH V1005,NA,,US,Oklahoma,Seminole,based on nearby landmark,minutes,small collection,"""just north of the Canadian River""; shown on map as due north of Ada, in the southermost part of Seminole County; this is just north of the town of Tyrola",gp_mid,-28.89,-2.47,101,US,,Ada,,,bed,,,,,,,NA,"from a ""single stratigraphic horizon... 22.4 m above the contact"" with the ""underlying Vamoosa Formation""",,mudstone,gray,,,,,,,,,coarse channel fill,,"bone horizon is from ""tributary channel fill deposits"" immediately below a layer of ""pedogenic carbonate nodules""",macrofossils,,,,,,NA,,body,,allochthonous,time-averaged,,,preferred,,,occasional,NA,,,taxonomic,"selective quarrying,surface (float),sieve,field collection",,,250 specimens,,,,"All of the in situ specimens recovered from the locality were found within a single stratigraphic horizon stretching approximately 11 m along the face of the outcrop. Screenwashing of 40 kg of sediment recovered ""very little additional material""","authors report minimum number of individuals, but material is transported and allochthonous, so specimen counts are recorded instead","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Aspidosaurus,cf.,NA,NA,vertebrate,"W. May, A. K. Huttenlocker, and J. D. Pardo , J. Benca, B. J. Small. 2011. New Upper Pennsylvanian armored dissorophid records (Temnospondyli, Dissorophoidea) from the U.S. midcontinent and the stratigraphic distributions of dissorophids. Journal of Vertebrate Paleontology 31(4):907-912",327,697,697,R. Butler,E. Dunne,E. Dunne,22/07/2016 10:01,22/07/2016 10:04,6174,sp.,Aspidosaurus,59928,,303.4,298.9,Virgilian,,NA,US,Aspidosaurus sp.
1338152,occ,NA,,180631,members,cf. Aspidosaurus sp.,genus,37021,,Aspidosaurus,NA,genus,37021,May et al.,2011,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37021,NA,NA,NA,,-95.730003,40.48,Peru Locality,NA,Indian Cave Sandstone exposures,US,Nebraska,Nemaha,based on nearby landmark,2,outcrop,"""The exposures are preserved as shear sandstone cliffs along an abandoned railroad right-of-way and hiking trail, facing the Missouri River floodplain to the northeast of Peru"" May et al. 2011",gp_mid,-25.38,1.9,101,US,,Onaga,,Indian Cave Sandstone,group of beds,,,,,,,NA,"The Indian Cave Sandstone, an informal unit, has been recently reinterpreted\r\nas a series of disjunct incised valley fills from the upper Pennsylvanian of southeastern Nebraska and Kansas (Fischbein et al., 2009); the Peru exposures represent an incised valley fill in the uppermost Pennsylvanian Towle Shale Member of the Onaga Formation (Admire Group).","The sediments include fine- to coarse-grained large-scale trough cross-bedded sandstones with silty and carbonaceous lenses bearing plant, invertebrate, and vertebrate remains, representing a transitional or estuarine paleoenvironment.",sandstone,,lithified,,,,,,,,estuary/bay,,"The highly disarticulated nature of the tetrapod fossils indicates some transport within the basin. The vertebrate fauna was surveyed by Ossian (1974), who interpreted the fauna as a largely autochthonous estuarine or nearshore marine assemblage dominated by actinopterygians and chondrichthyans, with frequent occurrences of disarticulated (probably transported) terrestrial material preserving isolated remains of lungfish as well as temnospondyls, lepospondyls, and amniotes, including Phlegethontia, Ophiderpeton, Diploceraspis, Diplocaulus, Dendrerpeton, Captorhinus, and indeterminate material dubiously attributed to dissorophids and microsaurs.۪",macrofossils,,,,,,NA,,body,medium,,,,,,,,frequent,NA,,,taxonomic,,,all macrofossils,,,May et al.,2009,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Aspidosaurus,cf.,NA,NA,vertebrate,"W. May, A. K. Huttenlocker, and J. D. Pardo , J. Benca, B. J. Small. 2011. New Upper Pennsylvanian armored dissorophid records (Temnospondyli, Dissorophoidea) from the U.S. midcontinent and the stratigraphic distributions of dissorophids. Journal of Vertebrate Paleontology 31(4):907-912",327,697,0,R. Butler,E. Dunne,,22/07/2016 10:18,22/07/2016 10:18,NA,sp.,Aspidosaurus,59928,,303.7,298.9,Gzhelian,,NA,US,Aspidosaurus sp.
1338164,occ,NA,,180632,members,Branchiosaurus salamandroides,species,255222,,Branchiosaurus salamandroides,NA,species,255222,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37039,NA,NA,NA,,2.742165,46.286964,Commentry,NA,,FR,Allier,,based on nearby landmark,6,small collection,"Location is ambiguous in text, therefore coordinates are base on the location of Commentary, a commune in the department of Allier in central France.",gp_mid,16.43,-0.13,305,FR,,,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,NHMUK and MNHN,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchiosaurus,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,22/07/2016 10:47,22/07/2016 10:47,NA,salamandroides,Branchiosaurus,57795,,303.4,301.2,Stephanian C,,NA,FR,Branchiosaurus salamandroides
1338165,occ,NA,,84835,,Platyrhinops n. sp. fritschi,species,345466,,Platyrhinops fritschi,NA,species,345466,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,123089,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Platyrhinops,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,22/07/2016 10:52,22/07/2016 10:52,28608,fritschi,Platyrhinops,57795,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Platyrhinops fritschi
1338177,occ,NA,,85292,,Raniceps n. sp. lyelli,species,229338,recombined as,Platyrhinops lyelli,NA,species,229338,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,123089,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Raniceps,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,25/07/2016 04:15,25/07/2016 04:15,28831,lyelli,Platyrhinops,57795,n. sp.,311.45,306.95,Westphalian D,,NA,US,Platyrhinops lyelli
1338178,occ,NA,,85292,,Tuditanus n. sp. mordex,species,345483,subjective synonym of,Platyrhinops lyelli,NA,species,229338,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,123089,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Tuditanus,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,25/07/2016 04:16,25/07/2016 04:16,28831,mordex,Platyrhinops,57795,n. sp.,311.45,306.95,Westphalian D,,NA,US,Platyrhinops mordex
1338179,occ,NA,,85292,,n. gen. Ichthycanthus n. sp. platypus,species,320864,subjective synonym of,Platyrhinops lyelli,NA,species,229338,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Amphibamidae,123081,123089,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Ichthycanthus,n. gen.,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,25/07/2016 04:20,25/07/2016 04:20,28831,platypus,Platyrhinops,57795,n. sp.,311.45,306.95,Westphalian D,,NA,US,Platyrhinops platypus
1338180,occ,NA,,84716,,cf. Platyhystrix sp.,genus,37034,,Platyhystrix,NA,genus,37034,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37034,NA,NA,NA,,-98.900002,33.641666,Rattlesnake Canyon (Admiral Fm.),NA,Locality IVc (Romer & Price 1940); Cummins' Headquarters; Lyles Place,US,Texas,Archer,estimated from map,seconds,outcrop,"Rattlesnake Canyon, Archer County, Texas. Lat long is estimated from map on p. 397 in Clark & Carroll (1973).",gp_mid,-30.23,-1.14,101,US,,Petrolia,Wichita,,,,,,,,,NA,"""Uppermost Admiral Formation"" (Clark & Carroll, 1973); the uppermost part of the traditional Admiral Fm. today is considered the lowermost part of the Petrolia Fm. (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Platyhystrix,cf.,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,25/07/2016 04:42,25/07/2016 04:42,28415,sp.,Platyhystrix,57795,,290.1,279.3,Artinskian,,NA,US,Platyhystrix sp.
1338181,occ,NA,,28238,,cf. Platyhystrix sp.,genus,37034,,Platyhystrix,NA,genus,37034,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37034,NA,NA,NA,,-98.901947,33.740276,"Tit Mountain, 21 (Belle Plains Formation)",NA,"Locality 21 (Romer 1928), Locality Vd (Romer & Price 1940), Corn Mountain, Corn Hill, faunal Zone 2, Middle Wichita Group, Texas red-beds, redbeds",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""Tit Mountain or Corn Hill, an elevation just northeast of Dundee"" See detailed locality map in Romer 1928. ""Zone 2. Middle Wichita; to the Beaverburk Limestone; Belle Plains Formation?"" Lat long is for Dundee.",gp_mid,-30.18,-1.06,101,US,,Belle Plains,Wichita,,group of beds,,,,,,,NA,"""about 500 feet above the Coleman Junction."" Details for Faunal Zone 2 of Romer 1928: ""Beyond the horizon of Godwin Creek is found a series of beds about 200 feet in thickness, of a transitional character, in which thin and impure limestones are occasionally present.""\r\nthe base of the Artinskian is just above Coleman Junction Formation (Wardlaw 2005, Permophiles), and the ""Belle Plains"" = Petrolia Formation is below the Waggoner Ranch Formation, whose base equals the base of the Bead Mountain Formation (Tabor et al. 2002), which is in the middle of the Artinskian (Wardlaw 2005)","red-beds and ""6-inch limestone""\r\n\r\n",claystone,red,,,,"""limestone""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Not the same as ""South side of Tit Mountain butte, TMM 40031"" locality (Langston 1986); that collection was obviously made much later than the Tit Mountain collection of Romer (1928), which has less detailed locality data.\r\nRomer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Platyhystrix,cf.,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,25/07/2016 04:43,25/07/2016 04:43,26948,sp.,Platyhystrix,57795,,290.1,279.3,Artinskian,,NA,US,Platyhystrix sp.
1338182,occ,NA,,180633,members,cf. Platyhystrix sp.,genus,37034,,Platyhystrix,NA,genus,37034,Foreman and Martin,1989,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37034,NA,NA,NA,individuals,-95.41037,39.817047,"Robinson Locality, Brown County",NA,Bern Limestone,US,Kansas,Brown,based on nearby landmark,6,small collection,"Coordinates are for the centre of Robinson, a city in Brown County, Kansas, United States. Locality lies just northeast of the town of Robinson.",gp_mid,-25.51,1.2,101,US,,Bern Limestone,Wabaunsee,Soldier Creek Shale,group of beds,,,,,,,NA,Bern Limestone,The fossiliferous horizon is composed almost entirely of densely packed stromatolites that lie between two shales.,"""shale""",,,,Y,,,,,,lagoonal,,"Although it has been suggested that shallow marine conditions existed at the site during time of deposition, it has also been argued that the cyanobacteria of the stromatolites grew in an environment of mixed fresh and marine water, either a lagoon or a bay (Foreman and Martin, 1988)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,"Like the Middle Virgilian Hamilton fauna, the Robinson fauna is dominated by aquatic taxa, with only a few specimens of terrestrial forms present.","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Platyhystrix,cf.,NA,NA,vertebrate,"B. C. Foreman and L. D. Martin. 1989. A review of Paleozoic tetrapod localities of Nebraska and Kansas. In: Regional Geology and Palaeontology of Upper Paleozoic Hamilton Quarry Area in Southeastern Kansas. In G. Mapes, P. H. Mapes (eds.), Kansas Geological Survey Guidebook 6 ",327,697,697,R. Butler,E. Dunne,E. Dunne,25/07/2016 04:57,07/09/2016 03:45,NA,sp.,Platyhystrix,59937,,303.4,298.9,Virgilian,,1,US,Platyhystrix sp.
1338183,occ,NA,,85292,,Ceraterpeton n. sp. divaricatum,species,192965,subjective synonym of,Stegops newberryi,NA,species,345484,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37055,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Ceraterpeton,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,25/07/2016 05:11,25/07/2016 05:11,28831,divaricatum,Stegops,57795,n. sp.,311.45,306.95,Westphalian D,,NA,US,Stegops divaricatum
1338184,occ,NA,,85292,,Erpetosaurus n. sp. tuberculatus,species,345486,subjective synonym of,Stegops newberryi,NA,species,345484,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37055,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Erpetosaurus,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,25/07/2016 05:20,25/07/2016 05:20,28831,tuberculatus,Stegops,57795,n. sp.,311.45,306.95,Westphalian D,,NA,US,Stegops tuberculatus
1338185,occ,NA,,176092,members,Stegops newberryi,species,345485,,Stegops newberryi,NA,species,345484,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37055,NA,NA,NA,,-80.612236,40.989132,Five Points Coal Mine,NA,,US,Ohio,Mahoning County,based on nearby landmark,6,outcrop,"""Five Points, south of Youngstown, Mahoning County, Ohio"" Sues et al. (2013) Atl Geol.",gp_mid,-18.98,-8.63,101,US,,,Allegheny,,,,,,,,,NA,,,coal,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Stegops,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,25/07/2016 05:22,25/07/2016 05:22,NA,newberryi,Stegops,57795,,313.8,305.9,Desmoinesian,,NA,US,Stegops newberryi
1338187,occ,NA,,85292,,Tuditanus n. sp. huxleyi,species,192958,recombined as,Macrerpeton huxleyi,NA,species,192958,Gubin,1980,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37003,NA,NA,NA,,-80.673332,40.56778,Linton,NA,Diamond Coal Mine,US,Ohio,Jefferson,estimated from map,seconds,outcrop,"""located at the mouth of Yellow Creek in northeastern Saline Township, Jefferson County"" (Hook & Baird, 1988)",gp_mid,-18.48,-8.09,101,US,,,Allegheny,Upper Freeport Coal,group of beds,,,,,,,NA,"""immediately [... below ...] a locally thick bituminous seam, known as the Upper Freeport coal, at the top of the Allegheny Group. The Upper Freeport is the No. 6 coal of Newberry (1871, 1874, 1878) or the No. 7 coal of subsequent Ohio Geological Survey reports, and is taken to be correlative to the top of the Westphalian D Series of Europe"" (Hook & Baird, 1988)","""Linton fossils are preserved in a thin deposit of cannel coal [...]. The cannel is composed primarily of miospores and other resistant plant parts dispersed within a very fine-grained, pyrite-rich matrix of organic detritus"" which are enclosed in an ""erosive-based, fining-upward, sandstone-dominated\r\nsediment body"" (Hook & Baird, 1988)",coal,,,,,,,,,,mire/swamp,foreland basin,"""the cannel [...] originated as a subaqueous sapropelic peat that formed under neutral to moderately alkaline, anoxic conditions [...] at the bottom of an approximately 15-m-deep abandoned river meander [...] the Linton meander was closed rapidly by neck cutoff . In the absence of significant clastic influx, plant debris derived from the surrounding levees formed a peaty muck in the bottom of the oxbow and, after a brief period of aerobic decomposition, degenerated into an anoxic, scavenger-free sapropelic peat.\r\nThe oxbow was situated in the meander belt on a large, contemporaneously active river. As sediment supply within this system diminished, peat-forming mires expanded over floodplain deposits, and where no clastic sediments intervened, humic peat accumulated directly above sapropel-filled abandoned channel segments."" (Hook & Baird, 1988)",macrofossils,,,,,,NA,,body,good,autochthonous,snapshot,,,,common,,,NA,,"""Although the predominance of aquatic taxa has led workers to conclude that amphibious to terrestrial forms are 'wash ins' or 'erratics', the petrography of the cannel and the high degree of completeness exhibited by most specimens demonstrate that animal remains were derived from the oxbow lake and its immediate surroundings. Post-mortem transport was essentially downward into the sapropelic milieu, not laterally across an environmental transect that supposedly ranged from 'upland' and 'open water' to 'swamp lake', as depicted by Milner (1980) and suggested by others. In short, the assemblage is autochthonous at the scale of the oxbow lake and its margins. [...]\r\nfor all intents and purposes, the Linton vertebrate assemblage is a biocoenose, and recognition of discrete terrestrial and lacustrine communities within it is largely artificial."" (Hook & Baird, 1988)",taxonomic,"selective quarrying,survey of museum collection","AMNH,CM,MCZ,USNM",all microfossils,,,"J. S. Newberry, T. Stock, S. Houston, D. Baird, D. Mullenaux, among others",,"""thousands of fossils [...] obtained within the mine, from the mine dump, and from local collectors"" (Hook & Baird, 1988)\r\nPU = Princeton University Fossil Vertebrate Collection (should now be reposited in the Yale Peabody Museum)","Anderson (2002) states that AMNH 6966 (incl. 6886) is the ""only known specimen"" of Phlegethontia linearis. Hence, all other specimens referred to P. linearis by earlier authors (i.e. Lund, 1978) are listed as P. longissima in the taxonomic list. However, since some of this material is neither listed as Phlegethontia nor even mentioned at all by Anderson (2002), there is no information on the current whereabouts and taxonomic status of these specimens (marked by an asterisk in the taxonomic list).","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Tuditanus,,NA,NA,vertebrate,Y. M. Gubin. 1980. [New Permian dissorophids of the Ural forelands]. In Russian. Paleontologicheskii Zhurnal 3:82-90,327,697,0,R. Butler,E. Dunne,,25/07/2016 05:34,25/07/2016 05:34,28831,huxleyi,Macrerpeton,59938,n. sp.,311.45,306.95,Westphalian D,,NA,US,Macrerpeton huxleyi
1338188,occ,NA,,180634,members,Dasyceps sp.,genus,37054,,Dasyceps,NA,genus,37054,Milner et al.,2007,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37054,NA,NA,NA,,13.413596,49.897076,Obora,NA,1km North of Obora,CZ,Plze Region,Plze-North District,based on nearby landmark,6,small collection,"Coordinates are for 1km north of Obora, a village and municipality in Plze-North District in the Plze Region of the Czech Republic. Location lies ""3 km south of Skalice nad Svitavou, Moravia.""",gp_mid,23.27,6.31,305,CZ,,Middle Letovice,,,,,,,,,,NA,"""Middle Letovice Formation, Autunian, Lower Permian""",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Dasyceps,,NA,NA,vertebrate,"A. R. Milner, J. Klembara, and O. Dostl. 2007. A zatrachydid temnospondyl from the Lower Permian of the Boskovice Furrow in Moravia (Czech Republic). Journal of Vertebrate Paleontology 27(3):711-715",327,697,0,R. Butler,E. Dunne,,25/07/2016 07:06,25/07/2016 07:06,NA,sp.,Dasyceps,59939,,298.9,295,Autunian,,NA,CZ,Dasyceps sp.
1338190,occ,NA,,84835,,n. gen. Capetus n. sp. palustris,species,256954,,Capetus palustris,NA,species,256954,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,256952,NA,NA,NA,,13.207222,49.713055,Nyrany,NA,"Humboldt Mine, Krimice Mine, N_any, Nyrschan, N_rschan",CZ,Pilsen,Pilsen-North,based on nearby landmark,seconds,local area,"Lat Long is for the town of N_any, WSW of Pilsen, Czech Republic",gp_mid,19.67,0.55,305,CZ,,Kladno,,N_any,group of beds,,,,,,,NA,,,coal,,,,,,,,,,lacustrine indet.,foreland basin,,macrofossils,,,,,,NA,,"body,cast,mold/impression",good,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"GH = Nrodni Muzeum (National Musuem), Prague, Czech Republic\r\nMP = Natural History Musuem, Pilzen\r\nNMW = Naturhistorisches Museum Wien (Natural Histroy Museum, Vienna), Austria",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Capetus,n. gen.,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,25/07/2016 09:00,25/07/2016 09:00,28608,palustris,Capetus,28828,n. sp.,311.45,306.95,Westphalian D,,NA,CZ,Capetus palustris
1338212,occ,NA,,180643,members,n. gen. Clamorosaurus n. sp. nocturnus,species,345531,,Clamorosaurus nocturnus,NA,species,345531,Gubin,1983,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37010,NA,NA,NA,,57.185925,65.130753,Pechora River,NA,,RU,Komi Republic,,estimated from map,6,small collection,"Coordinates based on the location of Pechora, a town in the Komi Republic, Russia, located on the Pechora River, west of and near the northern Ural Mountains. ",gp_mid,37.99,34.29,302,RU,,,,,,,,,,,,NA,Pechora Basin,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,PIN,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Clamorosaurus,n. gen.,NA,NA,vertebrate,Y. M. Gubin. 1983. [The first eryopids from the Permian of the Eastern European platform]. In Russian. Paleontologicheskii Zhurnal 1983(4):110-115,327,697,0,R. Butler,E. Dunne,,26/07/2016 04:15,26/07/2016 04:15,NA,nocturnus,Clamorosaurus,59952,n. sp.,279.5,272.5,Ufimian,,NA,RU,Clamorosaurus nocturnus
1338213,occ,NA,,84719,,Clamorosaurus n. sp. borealis,species,345532,,Clamorosaurus borealis,NA,species,345532,Gubin,1983,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37010,NA,NA,NA,,60.049999,66.033333,Inta city,NA,,RU,Komi,Inta,stated in text,minutes,small collection,Pechora Basin; Lat Long is from Olson (1957),gp_mid,35.28,33.63,302,RU,,Inta,,,,,,,,,,NA,"Locality biostratigraphically lies within the Inta Assemblage Zone (Inta Kompleks) (Ivakhnenko, 1990; Modesto & Rybczynski, 2000), which is Asselian to Ufimian in age (Modesto & Rybczynski, 2000). Ivakhnenko (1990, fig. 1) and Shishkin et al. (2000) say that the locality is of Ufimian age; Ivakhnenko (2008 p. 87) states that the locality is Artinskian in age (""same age"" as type locality of Riabininus uralensis, see collection (84718)).","""Carbonaceous shales and channel sandstone"" (Olson, 1957)","""shale""",,,carbonaceous,,sandstone,,,,Y,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,PIN,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Clamorosaurus,,NA,NA,vertebrate,Y. M. Gubin. 1983. [The first eryopids from the Permian of the Eastern European platform]. In Russian. Paleontologicheskii Zhurnal 1983(4):110-115,327,697,0,R. Butler,E. Dunne,,26/07/2016 04:19,26/07/2016 04:19,28378,borealis,Clamorosaurus,59952,n. sp.,290.1,272.5,Artinskian,Ufimian,NA,RU,Clamorosaurus borealis
1338223,occ,NA,,180649,members,n. gen. Osteophorus n. sp. roemeri,species,345534,,Osteophorus roemeri,NA,species,345534,Meyer,1856,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37014,NA,NA,NA,,15.590299,51.111996,"Mala Dolna Weiz, near Lw_wek lski",NA,formerly Klien-Neunforf,PL,,,based on nearby landmark,6,small collection,"Coorindates are for the centre of Lw_wek lski, a town in the Lower Silesian Voivodeship in Poland.",gp_mid,26.35,11.26,305,PL,,,,,,,,,,,,NA,Lower Rotliegend; ?Lower Permian,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Osteophorus,n. gen.,NA,NA,vertebrate,H. v. Meyer. 1856. ber Osteophorus roemeri aus dem Rothliegenden von Klien-Neundorf in Schlesien. Palaeontographica 7:99-104,327,697,0,R. Butler,E. Dunne,,26/07/2016 05:22,26/07/2016 05:22,NA,roemeri,Osteophorus,59955,n. sp.,298.9,254,Rotliegendes,,NA,PL,Osteophorus roemeri
1338234,occ,NA,,154179,,Porierpeton nitens,species,345542,nomen dubium,Porierpeton,NA,genus,345541,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,345541,NA,NA,NA,,13.675,50.209999,"Kounov, Rakovnik District",NA,Kounova,CZ,,,based on nearby landmark,2,outcrop,"""Kounova lies some 35 miles northwest of Prague in the Rakonitz coal basin"" Romer (1945)\r\nPreviously in area known as Bohemia",gp_mid,21.74,4.64,305,CZ,,Slany,,Kounov,group of beds,,,,,,,NA,,,"""siliciclastic""",,lithified,,,,,,,,terrestrial indet.,rift,"Central-West Bohemian basin; extensional basin developed within Variscan zone along simple asymmetric mega-graben formed on the Central Bohemian and Litomerice fault zones, with some contribution from transtensional wrench faults.\r\nThe sediments at Kounova suggest deposition in the bottom of a quiet pool, and the environment seems to have been that of a coal-swamp region. (Kissel, 2010)\r\n",macrofossils,,,,,,NA,,mold/impression,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Repository: National Museum, Prague (CGH)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Porierpeton,,NA,NA,"paleoentomology,vertebrate",R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,26/07/2016 06:24,26/07/2016 06:24,37199,nitens,Porierpeton,57795,,304.8,303.4,Stephanian B,,NA,CZ,Porierpeton nitens
1338235,occ,NA,,154179,,Macromerion n. sp. schwartzenbergii,species,334675,,Macromerion schwartzenbergii,NA,species,334675,Romer,1945,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38906,NA,NA,NA,,13.675,50.209999,"Kounov, Rakovnik District",NA,Kounova,CZ,,,based on nearby landmark,2,outcrop,"""Kounova lies some 35 miles northwest of Prague in the Rakonitz coal basin"" Romer (1945)\r\nPreviously in area known as Bohemia",gp_mid,21.74,4.64,305,CZ,,Slany,,Kounov,group of beds,,,,,,,NA,,,"""siliciclastic""",,lithified,,,,,,,,terrestrial indet.,rift,"Central-West Bohemian basin; extensional basin developed within Variscan zone along simple asymmetric mega-graben formed on the Central Bohemian and Litomerice fault zones, with some contribution from transtensional wrench faults.\r\nThe sediments at Kounova suggest deposition in the bottom of a quiet pool, and the environment seems to have been that of a coal-swamp region. (Kissel, 2010)\r\n",macrofossils,,,,,,NA,,mold/impression,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Repository: National Museum, Prague (CGH)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Macromerion,,NA,NA,"paleoentomology,vertebrate",A. S. Romer. 1945. The Late Carboniferous Vertebrate Fauna of Kounova (Bohemia) compared with that of the Texas Redbeds. American Journal of Science 243:417-442,327,697,697,R. Butler,E. Dunne,E. Dunne,26/07/2016 06:30,26/07/2016 06:30,37199,schwartzenbergii,Macromerion,57665,n. sp.,304.8,303.4,Stephanian B,,NA,CZ,Macromerion schwartzenbergii
1338236,occ,NA,,154179,,n. gen. Batrachocephalus n. sp. crassidens,species,320815,recombined as,Boii crassidens,NA,species,320815,Fritsch,1876,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Tuditanidae,37280,37282,NA,NA,NA,,13.675,50.209999,"Kounov, Rakovnik District",NA,Kounova,CZ,,,based on nearby landmark,2,outcrop,"""Kounova lies some 35 miles northwest of Prague in the Rakonitz coal basin"" Romer (1945)\r\nPreviously in area known as Bohemia",gp_mid,21.74,4.64,305,CZ,,Slany,,Kounov,group of beds,,,,,,,NA,,,"""siliciclastic""",,lithified,,,,,,,,terrestrial indet.,rift,"Central-West Bohemian basin; extensional basin developed within Variscan zone along simple asymmetric mega-graben formed on the Central Bohemian and Litomerice fault zones, with some contribution from transtensional wrench faults.\r\nThe sediments at Kounova suggest deposition in the bottom of a quiet pool, and the environment seems to have been that of a coal-swamp region. (Kissel, 2010)\r\n",macrofossils,,,,,,NA,,mold/impression,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Repository: National Museum, Prague (CGH)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Batrachocephalus,n. gen.,NA,NA,"paleoentomology,vertebrate",A. Fritsch. 1876. ber die Fauna der Gaskohle des Pilsner und Rakonitzer Beckens. Sitzungs-Berichte der koniglichen bohmischen Gellschaft der Wissenschaften Prag 1875:70-78,327,697,697,R. Butler,E. Dunne,E. Dunne,26/07/2016 06:30,26/07/2016 06:30,37199,crassidens,Boii,58031,n. sp.,304.8,303.4,Stephanian B,,NA,CZ,Boii crassidens
1338237,occ,NA,,154179,,Ophiderpeton n. sp. vicinum,species,320838,recombined as,Oestocephalus vicinum,NA,species,320838,Fritsch,1880,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Oestocephalidae,230698,230697,NA,NA,NA,,13.675,50.209999,"Kounov, Rakovnik District",NA,Kounova,CZ,,,based on nearby landmark,2,outcrop,"""Kounova lies some 35 miles northwest of Prague in the Rakonitz coal basin"" Romer (1945)\r\nPreviously in area known as Bohemia",gp_mid,21.74,4.64,305,CZ,,Slany,,Kounov,group of beds,,,,,,,NA,,,"""siliciclastic""",,lithified,,,,,,,,terrestrial indet.,rift,"Central-West Bohemian basin; extensional basin developed within Variscan zone along simple asymmetric mega-graben formed on the Central Bohemian and Litomerice fault zones, with some contribution from transtensional wrench faults.\r\nThe sediments at Kounova suggest deposition in the bottom of a quiet pool, and the environment seems to have been that of a coal-swamp region. (Kissel, 2010)\r\n",macrofossils,,,,,,NA,,mold/impression,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Repository: National Museum, Prague (CGH)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Ophiderpeton,,NA,NA,"paleoentomology,vertebrate",A. Fritsch. 1880. Fauna der Gaskohle und der Kalksteine der Permformation Bohmens. 1(2),327,697,697,R. Butler,E. Dunne,E. Dunne,26/07/2016 06:30,26/07/2016 06:30,37199,vicinum,Oestocephalus,58421,n. sp.,304.8,303.4,Stephanian B,,NA,CZ,Oestocephalus vicinum
1338240,occ,NA,,176500,members,Pleuronoura pellati,species,345544,nomen dubium,Pleuronoura,NA,genus,345543,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,345543,NA,NA,NA,,-4.279287,46.99017,"Millery, near Autun",NA,,FR,Saone et Loire,,based on nearby landmark,6,small collection,"Coordinates are for Millery, Saone et Loire, near Autun, France",gp_mid,12.36,1.11,305,FR,,Millery Series,,,group of beds,,,,,,,NA,Lower Permian,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,M. Pellat,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Pleuronoura,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,26/07/2016 07:09,26/07/2016 07:09,NA,pellati,Pleuronoura,57795,,298.9,295,Autunian,,NA,FR,Pleuronoura pellati
1338314,occ,NA,,180674,members,n. gen. Actinodon n. sp. frossardi,species,345642,,Actinodon frossardi,NA,species,345642,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37008,NA,NA,NA,,4.382756,47.025478,Dracy Saint Loup,NA,"Muse, north of Autun",FR,Saone et Laoire,,based on nearby landmark,6,small collection,"Coordinates based on Muse, 10km NE of Autun, Departement Saone et Loire, France",gp_mid,18.2,2.01,305,FR,,Muse,,,,,,,,,,NA,"""Autunian"", Lower Permian - Schoch & Milner, 2014",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,skulls,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MNHN,all macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Actinodon,n. gen.,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,27/07/2016 04:38,27/07/2016 04:38,NA,frossardi,Actinodon,57795,n. sp.,298.9,295,Autunian,,NA,FR,Actinodon frossardi
1338315,occ,NA,,180674,members,Actinodon n. sp. brevis,species,345643,subjective synonym of,Actinodon frossardi,NA,species,345642,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37008,NA,NA,NA,,4.382756,47.025478,Dracy Saint Loup,NA,"Muse, north of Autun",FR,Saone et Laoire,,based on nearby landmark,6,small collection,"Coordinates based on Muse, 10km NE of Autun, Departement Saone et Loire, France",gp_mid,18.2,2.01,305,FR,,Muse,,,,,,,,,,NA,"""Autunian"", Lower Permian - Schoch & Milner, 2014",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,skulls,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MNHN,all macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Actinodon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,27/07/2016 04:38,27/07/2016 04:38,NA,brevis,Actinodon,57795,n. sp.,298.9,295,Autunian,,NA,FR,Actinodon brevis
1338316,occ,NA,,176500,members,Actinodon frossardi,species,345642,,Actinodon frossardi,NA,species,345642,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37008,NA,NA,NA,,-4.279287,46.99017,"Millery, near Autun",NA,,FR,Saone et Loire,,based on nearby landmark,6,small collection,"Coordinates are for Millery, Saone et Loire, near Autun, France",gp_mid,12.36,1.11,305,FR,,Millery Series,,,group of beds,,,,,,,NA,Lower Permian,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,M. Pellat,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Actinodon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,27/07/2016 04:52,27/07/2016 04:52,NA,frossardi,Actinodon,57795,,298.9,295,Autunian,,NA,FR,Actinodon frossardi
1338317,occ,NA,,180675,members,Apateon n. sp. intermedius,species,345645,,Apateon intermedius,NA,species,345645,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,10.724043,50.638474,Silbergrund near St_tzerbach,NA,,DE,Thuringia,Suhl,based on nearby landmark,6,small collection,"Coordinates based on the location of Silbergrund, Suhl, Thuringia, Germany.",gp_mid,20.87,5.82,305,DE,,Mohrenbach,,,group of beds,,,,,,,NA,M̦hrenbach Formation,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,all macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,27/07/2016 05:08,27/07/2016 05:08,NA,intermedius,Apateon,57795,n. sp.,303.7,298.9,Gzhelian,,NA,DE,Apateon intermedius
1338318,occ,NA,,79163,,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-98.777496,33.449722,Cottonwood Creek (Moran Fm.),NA,Locality IIb (Romer & Price),US,Texas,Archer,estimated from map,seconds,outcrop,"Cottonwood Creek is a tributary of the south fork of the Little Wichita River (about 10 miles south of Archer City). Locality is ""near the head of Cottonwood Creek, close to the southern border of Archer Co."" (Romer & Price, 1940) ",gp_mid,-30.65,-2.02,101,US,,Archer City,Wichita,,group of beds,,,,,,,NA,"""about 50 feet below the Sedwick limestone equivalent"" (Clark & Carroll, 1973)\r\nThe former Moran Formation comprises the lower part of the Archer City Formation (Hentz, 1988, The University of Texas at Austin, Bureau of Economic Geology, Report of Investigations, 170).",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,observed (not collected),MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,27/07/2016 06:24,27/07/2016 06:24,28415,sp.,Eryops,57795,,298.9,295.5,Asselian,,NA,US,Eryops sp.
1338507,occ,NA,,176543,members,Onchiodon n. sp. langenhani,species,345774,,Onchiodon langenhani,NA,species,345774,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37013,NA,NA,NA,,10.453702,50.877323,Sembachtal near Winterstein,NA,,DE,Thuringia,Emsetal,based on nearby landmark,6,small collection,,gp_mid,20.64,6,305,DE,,Ilmenau,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Onchiodon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,31/07/2016 14:52,31/07/2016 14:52,NA,langenhani,Onchiodon,57795,n. sp.,303.7,298.9,Gzhelian,,NA,DE,Onchiodon langenhani
1338510,occ,NA,,180757,members,Onchiodon n. sp. manebachensis,species,345775,,Onchiodon manebachensis,NA,species,345775,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37013,NA,NA,NA,,10.85653,50.666248,"Cliff at Ilm River, Moosbach",NA,,DE,Thuringia,,based on nearby landmark,6,small collection,"Coorinates based on Moosbach, near Manebach in Thuringia, Germany",gp_mid,20.94,5.87,305,DE,,Mohrenbach,,,,,,,,,,NA,,"The Georgenthal and M̦hrenbach Formations unconformably overlie the folded Variscan basement, which consists of Proterozoic to Lower Palaeozoic formations of the Saxothuringian zone in the SE, a deeply-weathered granitic massif in the middle part (Th_ringer Hauptgranit, Vis̩), and metamorphic rocks of the Ruhla Crystalline Complex in the NW. The Georgenthal and M̦hrenbach formations mainly consist of trachyticlatitic volcanics, pyroclastics and intrusives. In addition, the M̦hrenbach Formation contains acid volcanics that become increasingly acid upwards.",not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,PSUL Langehan collection,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Onchiodon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,31/07/2016 15:01,31/07/2016 15:01,NA,manebachensis,Onchiodon,57795,n. sp.,303.7,298.9,Gzhelian,,NA,DE,Onchiodon manebachensis
1338514,occ,NA,,180761,members,Onchiodon n. sp. thuringiensis,species,345776,,Onchiodon thuringiensis,NA,species,345776,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37013,NA,NA,NA,,11.517153,48.371948,Kammerberg near Manebach,NA,,DE,Thuringia,,based on nearby landmark,6,small collection,"Coordinates based on the village of Kammerberg, near Manebach, Thuringia, Germany.",gp_mid,22.37,4.25,305,DE,,Manebach,,,,,,,,,,NA,Pennsylvanian-Permian Boundary,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Onchiodon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,31/07/2016 15:14,31/07/2016 15:14,NA,thuringiensis,Onchiodon,57795,n. sp.,303.7,295.5,Gzhelian,Asselian,NA,DE,Onchiodon thuringiensis
1338517,occ,NA,,58139,,Melanerpeton n. sp. pusillum,species,345777,,Melanerpeton pusillum,NA,species,345777,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,260059,NA,NA,NA,,16.335833,50.583889,"Olivt_n, Broumov City, Boheme",NA,"Olivetin, Oelberg bei Branau",CZ,Boheme,,based on nearby landmark,seconds,,"Olivet_n, close to the City Broumov, Boheme\r\nGerman name of Olivetin (Oelberg) given by Estes 1970, J Paleont",gp_mid,26.98,10.91,305,CZ,,,,,,,,,,,,NA,"Lower Permian (i.e., Rotliegendes: JA)",,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"Geologic-paleontological department of the National-Museum, Prag",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Melanerpeton,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,31/07/2016 15:25,31/07/2016 15:25,15696,pusillum,Melanerpeton,57795,n. sp.,298.9,254,Rotliegendes,,NA,CZ,Melanerpeton pusillum
1338519,occ,NA,,176543,members,Melanerpeton n. sp. sembachense,species,345779,,Melanerpeton sembachense,NA,species,345779,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,260059,NA,NA,NA,,10.453702,50.877323,Sembachtal near Winterstein,NA,,DE,Thuringia,Emsetal,based on nearby landmark,6,small collection,,gp_mid,20.64,6,305,DE,,Ilmenau,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Melanerpeton,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,31/07/2016 15:50,31/07/2016 15:50,NA,sembachense,Melanerpeton,57795,n. sp.,303.7,298.9,Gzhelian,,NA,DE,Melanerpeton sembachense
1338520,occ,NA,,180765,members,Melanerpeton n. sp. eisfeldi,species,345780,,Melanerpeton eisfeldi,NA,species,345780,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,260059,NA,NA,NA,,10.565278,50.856945,"Gottlob quarry, Friedrichroda",NA,,DE,Thuringia,,based on nearby landmark,seconds,small collection,"Coordinates based on the town of Friedrichroda, Suhl district, Thuringia, Germany",gp_mid,21.24,6.7,305,DE,,Goldlauterer,,Upper Goldlauterer,,,,,,,,NA,"Lower Rotliegenden, upper Autun",,not reported,gray,lithified,,,,,,,,fluvial-lacustrine indet.,rift,Thuringian Forest basin; extensional basin with dextral strike-slip transtension component following the Variscan orogeny.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,"Material from this locality are housed at NHMUK, SMF, and MNG.","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Melanerpeton,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,31/07/2016 15:57,31/07/2016 15:57,NA,eisfeldi,Melanerpeton,57795,n. sp.,298.9,295.5,Asselian,,NA,DE,Melanerpeton eisfeldi
1338551,occ,NA,,160735,,Melanerpeton n. sp. arnhardti,species,345778,,Melanerpeton arnhardti,NA,species,345778,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,260059,NA,NA,NA,,10.717,50.707001,"Lochbrunnen, near Oberhof",NA,,DE,Th_ringer Wald,,based on nearby landmark,3,outcrop,Road from Oberhof to Schwarzwald,gp_mid,21.49,6.74,305,DE,,Oberh̦fer,,,group of beds,,,,,,,NA,,,"""shale""",,,,,,,,,,lacustrine indet.,rift,"Thuringian Forest basin; extensional basin with dextral strike-slip transtension component following the Variscan orogeny. After a relief reactivation, red-brown alluvial fan conglomerates and fluvial sandstones grade into brownish to greenish fluvio-lacustrine and very finely laminated (varved) black shales of the depocentres intercalated by basin-wide tuff marker-beds."" Roscher & Schneider, 2006",macrofossils,,,,,,NA,,mold/impression,,,,,,,,,,NA,,,taxonomic,,,,,,,,Repository: Zentralen Geologischen Instituts Berlin (ZGI) and Bergakademie Freiberg (FG),,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Melanerpeton,,NA,NA,paleoentomology,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,02/08/2016 10:58,02/08/2016 10:58,52735,arnhardti,Melanerpeton,57795,n. sp.,298.9,290.1,Asselian,Sakmarian,NA,DE,Melanerpeton arnhardti
1338552,occ,NA,,160735,,Onchiodon labyrinthicus,species,66913,,Onchiodon labyrinthicus,NA,species,66913,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37013,NA,NA,NA,,10.717,50.707001,"Lochbrunnen, near Oberhof",NA,,DE,Th_ringer Wald,,based on nearby landmark,3,outcrop,Road from Oberhof to Schwarzwald,gp_mid,21.49,6.74,305,DE,,Oberh̦fer,,,group of beds,,,,,,,NA,,,"""shale""",,,,,,,,,,lacustrine indet.,rift,"Thuringian Forest basin; extensional basin with dextral strike-slip transtension component following the Variscan orogeny. After a relief reactivation, red-brown alluvial fan conglomerates and fluvial sandstones grade into brownish to greenish fluvio-lacustrine and very finely laminated (varved) black shales of the depocentres intercalated by basin-wide tuff marker-beds."" Roscher & Schneider, 2006",macrofossils,,,,,,NA,,mold/impression,,,,,,,,,,NA,,,taxonomic,,,,,,,,Repository: Zentralen Geologischen Instituts Berlin (ZGI) and Bergakademie Freiberg (FG),,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Onchiodon,,NA,NA,paleoentomology,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,02/08/2016 10:58,02/08/2016 10:58,52735,labyrinthicus,Onchiodon,57795,,298.9,290.1,Asselian,Sakmarian,NA,DE,Onchiodon labyrinthicus
1338553,occ,NA,,180778,members,Onchiodon labyrinthicus,species,66913,,Onchiodon labyrinthicus,NA,species,66913,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37013,NA,NA,NA,,10.585,50.821667,"Wintersbrunnen, near Friedrichroda",NA,,DE,Thuringia,,based on nearby landmark,seconds,small collection,Coordinates based on the location of a geocache at the same location.,gp_mid,21.26,6.67,305,DE,,Oberhof,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,Werneburg,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Onchiodon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,02/08/2016 11:14,02/08/2016 11:14,NA,labyrinthicus,Onchiodon,57795,,298.9,295.5,Asselian,,NA,DE,Onchiodon labyrinthicus
1338554,occ,NA,,180779,members,Onchiodon labyrinthicus,species,66913,,Onchiodon labyrinthicus,NA,species,66913,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37013,NA,NA,NA,,10.565278,50.856945,Friedrichroda,NA,,DE,Thuringia,,based on nearby landmark,seconds,small collection,"Coordinates based on the centre of the town of Friedrichroda, Suhl district, Thuringia, Germany",gp_mid,21.35,6.86,305,DE,,Goldlauterer,,,group of beds,,,,,,,NA,Stratigraphy here is based on Koniger at al. (2002),,not reported,gray,lithified,,,,,,,,fluvial-lacustrine indet.,rift,Thuringian Forest basin; extensional basin with dextral strike-slip transtension component following the Variscan orogeny.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Onchiodon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,02/08/2016 11:19,02/08/2016 11:19,NA,labyrinthicus,Onchiodon,57795,,298.9,290.1,Asselian,Sakmarian,NA,DE,Onchiodon labyrinthicus
1338555,occ,NA,,58139,,Onchiodon credneri,species,345806,,Onchiodon credneri,NA,species,345806,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37013,NA,NA,NA,,16.335833,50.583889,"Olivt_n, Broumov City, Boheme",NA,"Olivetin, Oelberg bei Branau",CZ,Boheme,,based on nearby landmark,seconds,,"Olivet_n, close to the City Broumov, Boheme\r\nGerman name of Olivetin (Oelberg) given by Estes 1970, J Paleont",gp_mid,26.98,10.91,305,CZ,,,,,,,,,,,,NA,"Lower Permian (i.e., Rotliegendes: JA)",,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"Geologic-paleontological department of the National-Museum, Prag",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Onchiodon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,02/08/2016 11:25,02/08/2016 11:25,15696,credneri,Onchiodon,57795,,298.9,254,Rotliegendes,,NA,CZ,Onchiodon credneri
1338556,occ,NA,,180780,members,Onchiodon n. sp. credneri,species,345806,,Onchiodon credneri,NA,species,345806,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37013,NA,NA,NA,,15.06758,50.79026,"Ruprechtice, Liberecky kraj",NA,,CZ,,,based on nearby landmark,6,small collection,"Lat and long based on the location of Ruprechtice in the city of Liberec, Czech Republic.",gp_mid,23.99,7.5,305,CZ,,Broumov,,,group of beds,,,,,,,NA,The Broumov Formation (after the town of Broumov) is Upper Autunian in age.,The Broumov Formation is formed of red mudstones and grey and variegated pelitic rocks with carbonates and cherts. - Falke (1972),mudstone,red,lithified,,,"""carbonate""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Onchiodon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,02/08/2016 11:37,02/08/2016 11:37,NA,credneri,Onchiodon,57795,n. sp.,298.9,295,Autunian,,NA,CZ,Onchiodon credneri
1338557,occ,NA,,180781,members,cf. Onchiodon sp.,genus,37013,,Onchiodon,NA,genus,37013,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37013,NA,NA,NA,,12.880819,50.837048,Chemnitz-Altendorf,NA,"Chemnitz Altendorf, Saxony",DE,Saxony,,based on nearby landmark,6,small collection,"Lat Long based on the centre of Chemnitz-Altendorf, in Chemnitz, Saxony, Germany",gp_mid,23.07,7.81,305,DE,,Luekersdorf,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Onchiodon,cf.,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,02/08/2016 11:48,02/08/2016 11:48,NA,sp.,Onchiodon,57795,,298.9,272.3,Cisuralian,,NA,DE,Onchiodon sp.
1338558,occ,NA,,178736,members,Branchiosaurus humbergensis,species,345807,recombined as,Melanerpeton humbergense,NA,species,345807,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,260059,NA,NA,NA,,7.602687,49.711227,"Jeckenbach, near Meisenheim",NA,,DE,Rhineland-Palatine,Bad Kreuznach,based on nearby landmark,6,small collection,"""Jeckenbach, Saar-Nahe Basin"" (Glienke, 2015). Coordinates based on the location of Jeckenbach.",gp_mid,19.7,5.1,315,DE,,Meisenheim,Rotliegend,,bed,,,,,,,NA,"Jecken- bach Bank (M6), Rotliegend",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Repository: MNHM (Museum National d۪Histoire Naturelle, Paris, France)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchiosaurus,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,02/08/2016 11:59,02/08/2016 11:59,NA,humbergensis,Melanerpeton,57795,,298.9,295,Autunian,,NA,DE,Melanerpeton humbergensis
1338559,occ,NA,,85451,,Melanerpeton humbergense,species,345808,,Melanerpeton humbergense,NA,species,345807,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,260059,NA,NA,NA,,7.696111,49.578056,Niederkirchen/Westpfalz,NA,Gemeindeburg near Niederkirchen,DE,Rhineland-Palatinate,Kaiserslautern,based on nearby landmark,seconds,small collection,"Niederkirchen (Westpfalz), 16 km north of the city of Kaiserslautern; Lat long is for Niederkirchen. Locality lies in the Saar-Nahe district. Location described by Glienke (2013) as ""Gemeindeburg near Niederkirchen/Westpfalz, Saar-Nahe Basin)",gp_mid,19.79,4.99,315,DE,,Meisenheim,Rotliegend,,member,,M6,M6,,,,NA,"""Biostratigraphically, the find can be attributed to Boy's Leptorophus humbergensis-Apateon caducus association. This association is part of the Apateon caducus group and has an upper 'Autunian' age. This corresponds to the lower Sakmarian of international stratigraphy""\r\nThe Jeckenbach Subformation, however, is of Asselian age according to ""Stratigraphische Tabelle von Deutschland 2002""","""laminated silty grey shale""","""shale""","planar lamination,gray",,silty,Y,,,,,,lacustrine - large,intermontane basin,"""deposited in a large, shallow, eutrophic lake"" - Carroll (1991)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Melanerpeton,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,02/08/2016 12:02,02/08/2016 12:02,28837,humbergense,Melanerpeton,57795,,298.9,295.5,Asselian,,NA,DE,Melanerpeton humbergense
1338565,occ,NA,,179047,members,Melanerpeton sp.,genus,260059,,Melanerpeton,NA,genus,260059,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,260059,NA,NA,NA,,15.406135,50.576557,"Kostalov, near Trutnov",NA,Kolov,CZ,Liberec Region,Semily District,based on nearby landmark,6,small collection,,gp_mid,24.27,7.36,305,CZ,,Lower Rotliegendes,,,,,,,,,,NA,"Higher Coal-bearing zone, 'Upper Red beds'.",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Melanerpeton,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,02/08/2016 12:18,02/08/2016 12:18,NA,sp.,Melanerpeton,57795,,298.9,295.5,Asselian,,NA,CZ,Melanerpeton sp.
1338566,occ,NA,,180765,members,Apateon n. sp. kontheri,species,345812,,Apateon kontheri,NA,species,345812,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,10.565278,50.856945,"Gottlob quarry, Friedrichroda",NA,,DE,Thuringia,,based on nearby landmark,seconds,small collection,"Coordinates based on the town of Friedrichroda, Suhl district, Thuringia, Germany",gp_mid,21.24,6.7,305,DE,,Goldlauterer,,Upper Goldlauterer,,,,,,,,NA,"Lower Rotliegenden, upper Autun",,not reported,gray,lithified,,,,,,,,fluvial-lacustrine indet.,rift,Thuringian Forest basin; extensional basin with dextral strike-slip transtension component following the Variscan orogeny.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,"Material from this locality are housed at NHMUK, SMF, and MNG.","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,02/08/2016 12:43,02/08/2016 12:43,NA,kontheri,Apateon,57795,n. sp.,298.9,295.5,Asselian,,NA,DE,Apateon kontheri
1338570,occ,NA,,34797,,Apateon gracilis,species,37038,species not entered,Apateon,NA,genus,37038,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,2.966667,46.466667,Buxieres-les-Mines (Autunian shales),NA,"Buxieres les Mines, Allier, Autunien ",FR,,Allier,based on nearby landmark,minutes,outcrop,"Buxieres-les-Mines (near Moulins North of the Massif Central), Department of Allier",gp_mid,17.46,1.45,305,FR,,,,,,,,,,Buxieres,,NA,"middle Autunien, Autunien encompasses the Asselian and Sakmarian stages = lower Permian",,"""shale""",,lithified,,,,,,,,terrestrial indet.,,Autunian shales,macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,"surface (in situ),field collection",MNHN,,,,,,Museum d'Histoire Naturelle d'Autun (France),,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,02/08/2016 12:58,02/08/2016 12:58,9281,gracilis,Apateon,57795,,298.9,290.1,Asselian,Sakmarian,NA,FR,Apateon gracilis
1338612,occ,NA,,180794,members,Apateon sp.,genus,37038,,Apateon,NA,genus,37038,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,15.617567,50.566929,Horni Kalna,NA,"Horn_ Kaln, Vrchlabi",CZ,,,based on nearby landmark,6,small collection,"Lat long based on the centre of Horn_ Kaln, a village and municipality in Trutnov District in the Hradec Krlov̩ Region of the Czech Republic",gp_mid,24.82,8.1,305,CZ,,Prosecne,,,group of beds,,Kalna,Kalna,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 04:54,03/08/2016 04:54,NA,sp.,Apateon,57795,,298.9,272.3,Cisuralian,,NA,CZ,Apateon sp.
1338613,occ,NA,,180765,members,Branchiosaurus n. sp. flagrifer,species,345820,recombined as,Apateon flagrifer,NA,species,345820,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,10.565278,50.856945,"Gottlob quarry, Friedrichroda",NA,,DE,Thuringia,,based on nearby landmark,seconds,small collection,"Coordinates based on the town of Friedrichroda, Suhl district, Thuringia, Germany",gp_mid,21.24,6.7,305,DE,,Goldlauterer,,Upper Goldlauterer,,,,,,,,NA,"Lower Rotliegenden, upper Autun",,not reported,gray,lithified,,,,,,,,fluvial-lacustrine indet.,rift,Thuringian Forest basin; extensional basin with dextral strike-slip transtension component following the Variscan orogeny.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,"Material from this locality are housed at NHMUK, SMF, and MNG.","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchiosaurus,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 05:12,03/08/2016 05:12,NA,flagrifer,Apateon,57795,n. sp.,298.9,295.5,Asselian,,NA,DE,Apateon flagrifer
1338614,occ,NA,,180674,members,Branchiosaurus n. sp. dracyi,species,345822,recombined as,Apateon dracyi,NA,species,345822,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,4.382756,47.025478,Dracy Saint Loup,NA,"Muse, north of Autun",FR,Saone et Laoire,,based on nearby landmark,6,small collection,"Coordinates based on Muse, 10km NE of Autun, Departement Saone et Loire, France",gp_mid,18.2,2.01,305,FR,,Muse,,,,,,,,,,NA,"""Autunian"", Lower Permian - Schoch & Milner, 2014",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,skulls,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MNHN,all macrofossils,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchiosaurus,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 05:55,03/08/2016 05:55,NA,dracyi,Apateon,57795,n. sp.,298.9,295,Autunian,,NA,FR,Apateon dracyi
1338615,occ,NA,,176543,members,Apateon dracyi,species,345823,,Apateon dracyi,NA,species,345822,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,10.453702,50.877323,Sembachtal near Winterstein,NA,,DE,Thuringia,Emsetal,based on nearby landmark,6,small collection,,gp_mid,20.64,6,305,DE,,Ilmenau,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,697,R. Butler,E. Dunne,E. Dunne,03/08/2016 05:57,22/08/2016 09:18,NA,dracyi,Apateon,57795,,303.7,298.9,Gzhelian,,NA,DE,Apateon dracyi
1338616,occ,NA,,176535,members,Apateon dracyi,species,345823,,Apateon dracyi,NA,species,345822,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,12.925204,51.199074,"Clennen, Saxony",NA,,DE,Mittelsachsen,Bockelwitz,based on nearby landmark,6,small collection,"Coordinates based on the location of Clennen, a small populated area in Saxony, Germany.",gp_mid,22.57,7.46,305,DE,,Bortewitz,,,group of beds,,Clennen tuffite,Clennen tuffite,,,,NA,B̦rtewitz Formation,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,697,R. Butler,E. Dunne,E. Dunne,03/08/2016 05:59,22/08/2016 09:18,NA,dracyi,Apateon,57795,,298.9,295,Autunian,,NA,DE,Apateon dracyi
1338617,occ,NA,,180764,members,Apateon flagrifer,species,345821,,Apateon flagrifer,NA,species,345820,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,10.753,50.639,Pochwerksgrund,NA,,DE,Thuringia,,based on nearby landmark,3,small collection,"Pochwerksgrund near Goldlauter, Th_ringer Wald",gp_mid,21.64,6.85,305,DE,,Goldlauterer,,Lower Goldlauterer,,,,,,,,NA,In German: Unteres Goldlauterer Schichten,,not reported,,,,,,,,,,fluvial-lacustrine indet.,rift,"Thuringian Forest basin; extensional basin with dextral strike-slip transtension component following the Variscan orogeny. After a relief reactivation, red-brown alluvial fan conglomerates and fluvial sandstones grade into brownish to greenish fluvio-lacustrine and very finely laminated (varved) black shales of the depocentres intercalated by basin-wide tuff marker-beds."" Roscher & Schneider, 2006",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 06:11,03/08/2016 06:11,NA,flagrifer,Apateon,57795,,295.5,290.1,Sakmarian,,NA,DE,Apateon flagrifer
1338618,occ,NA,,180795,members,Apateon flagrifer,species,345821,,Apateon flagrifer,NA,species,345820,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,10.86,50.677776,"Sperbersbach, near Oberhof",NA,,DE,Th_ringia,,based on nearby landmark,seconds,outcrop,Coordinates based on centre of Manebach,gp_mid,21.69,6.9,305,DE,,Goldlauterer,,Lower Goldlauterer,,,,,,,,NA,"In German: Untere Goldlauterer Schichten, Acanthodeshorizont, Unterrotliegendes","""Gold mudstone""",not reported,,,,,,,,,,fluvial-lacustrine indet.,rift,"Thuringian Forest basin; extensional basin with dextral strike-slip transtension component following the Variscan orogeny. After a relief reactivation, red-brown alluvial fan conglomerates and fluvial sandstones grade into brownish to greenish fluvio-lacustrine and very finely laminated (varved) black shales of the depocentres intercalated by basin-wide tuff marker-beds."" Roscher & Schneider, 2006",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 06:15,03/08/2016 06:15,NA,flagrifer,Apateon,57795,,295.5,290.1,Sakmarian,,NA,DE,Apateon flagrifer
1338619,occ,NA,,178736,members,Apateon caducus,species,345825,,Apateon caducus,NA,species,345824,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,7.602687,49.711227,"Jeckenbach, near Meisenheim",NA,,DE,Rhineland-Palatine,Bad Kreuznach,based on nearby landmark,6,small collection,"""Jeckenbach, Saar-Nahe Basin"" (Glienke, 2015). Coordinates based on the location of Jeckenbach.",gp_mid,19.7,5.1,315,DE,,Meisenheim,Rotliegend,,bed,,,,,,,NA,"Jecken- bach Bank (M6), Rotliegend",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Repository: MNHM (Museum National d۪Histoire Naturelle, Paris, France)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,697,R. Butler,E. Dunne,E. Dunne,03/08/2016 06:37,03/08/2016 06:38,NA,caducus,Apateon,57795,,298.9,295,Autunian,,NA,DE,Apateon caducus
1338620,occ,NA,,85451,,Apateon caducus,species,345825,,Apateon caducus,NA,species,345824,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,7.696111,49.578056,Niederkirchen/Westpfalz,NA,Gemeindeburg near Niederkirchen,DE,Rhineland-Palatinate,Kaiserslautern,based on nearby landmark,seconds,small collection,"Niederkirchen (Westpfalz), 16 km north of the city of Kaiserslautern; Lat long is for Niederkirchen. Locality lies in the Saar-Nahe district. Location described by Glienke (2013) as ""Gemeindeburg near Niederkirchen/Westpfalz, Saar-Nahe Basin)",gp_mid,19.79,4.99,315,DE,,Meisenheim,Rotliegend,,member,,M6,M6,,,,NA,"""Biostratigraphically, the find can be attributed to Boy's Leptorophus humbergensis-Apateon caducus association. This association is part of the Apateon caducus group and has an upper 'Autunian' age. This corresponds to the lower Sakmarian of international stratigraphy""\r\nThe Jeckenbach Subformation, however, is of Asselian age according to ""Stratigraphische Tabelle von Deutschland 2002""","""laminated silty grey shale""","""shale""","planar lamination,gray",,silty,Y,,,,,,lacustrine - large,intermontane basin,"""deposited in a large, shallow, eutrophic lake"" - Carroll (1991)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 06:37,03/08/2016 06:37,28837,caducus,Apateon,57795,,298.9,295.5,Asselian,,NA,DE,Apateon caducus
1338621,occ,NA,,180796,members,Apateon caducus,species,345825,,Apateon caducus,NA,species,345824,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,7.442166,49.573666,Erdesbach (H̦lle),NA,Holle near Erdesbach,DE,Rhineland-Palatinate,Kusel district,based on nearby landmark,6,small collection,"Cooridnates based on the centre of Erdesbach, a municipality in the Kusel district in Rhineland-Palatinate, Germany.",gp_mid,19.63,4.95,315,DE,,Meisenheim,,M7,group of beds,,,,,Saar Nahe,Saar Nahe,NA,,,not reported,,,,,,,,,,lacustrine - small,,"""Small lake deposit""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,all macrofossils,,,,,,GPIM Collection,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 06:50,03/08/2016 06:50,NA,caducus,Apateon,57795,,298.9,295.5,Asselian,,NA,DE,Apateon caducus
1338622,occ,NA,,180797,members,Branchiosaurus n. sp. caducus,species,345824,recombined as,Apateon caducus,NA,species,345824,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,7.709929,49.573929,Pfarrwald at Heimkirchen,NA,"Heimkirchen, near Niderkirchen",DE,Rhineland-Palatine,,,6,,"Coordinates are for Heimkirchen, a small residential area, approximately 500m east of Niederkirchen, Rhineland-Palatine, Germany.",gp_mid,19.91,5.15,315,DE,,Meisenheim,,,group of beds,,M9,Kappeln Bank,,,,NA,Startigraphy here is based on Koniger at al. (2002),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Branchiosaurus,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 07:04,03/08/2016 07:04,NA,caducus,Apateon,57795,n. sp.,298.9,290.1,Asselian,Sakmarian,NA,DE,Apateon caducus
1338623,occ,NA,,180798,members,n. gen. Apateon n. sp. pedestris,species,229308,,Apateon pedestris,NA,species,229308,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,7.766667,49.783333,Munsterappel,NA,M_nsterappel,DE,Rhineland-Palatine,,estimated from map,minutes,small collection,"Lat long is based on the location of the Munsterappel P1 locality of Kerp et. al. (1990); The Munsterappel P 1 locality is located a few kilometres north of the Gutenbacherhof locality and the Oberhausen locality. Area around Oberhausen, a small village approximately 6 km east of Alsenz, in the eastern part of the Saar-Nahe Basin (SW Germany). ",gp_mid,19.62,4.95,315,DE,,Meisenheim,,,bed,,M8,Odernheim,,Saar-Nahe Basin,Odernheimer Kalkbank,NA,Possibly Late Carboniferous (Pennsylvanian) but Kerp et al. 1990 think Asselian-Sakmarian age may be more correct. Bed is assignable to the upper sub-unit of the Lauterecken-Odernheim Schichten (L-0 10) subunit of Boy and Fichter 1982.,,sandstone,"brown,gray",,,,siltstone,,,,,fluvial-lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"surface (in situ),field collection",,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,n. gen.,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 08:08,03/08/2016 08:08,NA,pedestris,Apateon,57795,n. sp.,303.7,295.5,Gzhelian,Asselian,NA,DE,Apateon pedestris
1338624,occ,NA,,180797,members,Apateon pedestris,species,229308,,Apateon pedestris,NA,species,229308,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,7.709929,49.573929,Pfarrwald at Heimkirchen,NA,"Heimkirchen, near Niderkirchen",DE,Rhineland-Palatine,,,6,,"Coordinates are for Heimkirchen, a small residential area, approximately 500m east of Niederkirchen, Rhineland-Palatine, Germany.",gp_mid,19.91,5.15,315,DE,,Meisenheim,,,group of beds,,M9,Kappeln Bank,,,,NA,Startigraphy here is based on Koniger at al. (2002),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 08:10,03/08/2016 08:10,NA,pedestris,Apateon,57795,,298.9,290.1,Asselian,Sakmarian,NA,DE,Apateon pedestris
1338625,occ,NA,,85451,,Apateon pedestris,species,229308,,Apateon pedestris,NA,species,229308,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,7.696111,49.578056,Niederkirchen/Westpfalz,NA,Gemeindeburg near Niederkirchen,DE,Rhineland-Palatinate,Kaiserslautern,based on nearby landmark,seconds,small collection,"Niederkirchen (Westpfalz), 16 km north of the city of Kaiserslautern; Lat long is for Niederkirchen. Locality lies in the Saar-Nahe district. Location described by Glienke (2013) as ""Gemeindeburg near Niederkirchen/Westpfalz, Saar-Nahe Basin)",gp_mid,19.79,4.99,315,DE,,Meisenheim,Rotliegend,,member,,M6,M6,,,,NA,"""Biostratigraphically, the find can be attributed to Boy's Leptorophus humbergensis-Apateon caducus association. This association is part of the Apateon caducus group and has an upper 'Autunian' age. This corresponds to the lower Sakmarian of international stratigraphy""\r\nThe Jeckenbach Subformation, however, is of Asselian age according to ""Stratigraphische Tabelle von Deutschland 2002""","""laminated silty grey shale""","""shale""","planar lamination,gray",,silty,Y,,,,,,lacustrine - large,intermontane basin,"""deposited in a large, shallow, eutrophic lake"" - Carroll (1991)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 08:11,03/08/2016 08:11,28837,pedestris,Apateon,57795,,298.9,295.5,Asselian,,NA,DE,Apateon pedestris
1338626,occ,NA,,178736,members,Apateon pedestris,species,229308,,Apateon pedestris,NA,species,229308,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,7.602687,49.711227,"Jeckenbach, near Meisenheim",NA,,DE,Rhineland-Palatine,Bad Kreuznach,based on nearby landmark,6,small collection,"""Jeckenbach, Saar-Nahe Basin"" (Glienke, 2015). Coordinates based on the location of Jeckenbach.",gp_mid,19.7,5.1,315,DE,,Meisenheim,Rotliegend,,bed,,,,,,,NA,"Jecken- bach Bank (M6), Rotliegend",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Repository: MNHM (Museum National d۪Histoire Naturelle, Paris, France)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 08:11,03/08/2016 08:11,NA,pedestris,Apateon,57795,,298.9,295,Autunian,,NA,DE,Apateon pedestris
1338627,occ,NA,,180796,members,Apateon pedestris,species,229308,,Apateon pedestris,NA,species,229308,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,7.442166,49.573666,Erdesbach (H̦lle),NA,Holle near Erdesbach,DE,Rhineland-Palatinate,Kusel district,based on nearby landmark,6,small collection,"Cooridnates based on the centre of Erdesbach, a municipality in the Kusel district in Rhineland-Palatinate, Germany.",gp_mid,19.63,4.95,315,DE,,Meisenheim,,M7,group of beds,,,,,Saar Nahe,Saar Nahe,NA,,,not reported,,,,,,,,,,lacustrine - small,,"""Small lake deposit""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,all macrofossils,,,,,,GPIM Collection,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 08:12,03/08/2016 08:12,NA,pedestris,Apateon,57795,,298.9,295.5,Asselian,,NA,DE,Apateon pedestris
1338628,occ,NA,,180800,members,Apateon pedestris,species,229308,,Apateon pedestris,NA,species,229308,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,7.701944,49.761665,Odernheim,NA,Odernheimer Kalkbank,DE,Rhineland-Palatine,Bad Kreuznach,based on nearby landmark,seconds,small collection,"Coordinates based on location south of Obernheim am Glan, a town in Rhineland-Palatine, Germany.",gp_mid,19.86,5.33,315,DE,,Meisenheim,,,group of beds,,Obernheim beds,Obernheimer Kalkbank,,,,NA,"Meisenheim Formation (M8), Saar-Nahe Basin, Germany\r\nObernheimer Kalkbank (""limestone bank"")",,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 08:16,03/08/2016 08:16,NA,pedestris,Apateon,57795,,298.9,290.1,Asselian,Sakmarian,NA,DE,Apateon pedestris
1338629,occ,NA,,176500,members,Apateon pedestris,species,229308,,Apateon pedestris,NA,species,229308,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,-4.279287,46.99017,"Millery, near Autun",NA,,FR,Saone et Loire,,based on nearby landmark,6,small collection,"Coordinates are for Millery, Saone et Loire, near Autun, France",gp_mid,12.36,1.11,305,FR,,Millery Series,,,group of beds,,,,,,,NA,Lower Permian,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,M. Pellat,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 08:21,03/08/2016 08:21,NA,pedestris,Apateon,57795,,298.9,295,Autunian,,NA,FR,Apateon pedestris
1338630,occ,NA,,180801,members,Apateon pedestris,species,229308,,Apateon pedestris,NA,species,229308,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,4.297222,46.949165,"Autun, Saone et Loire",NA,"Autun, Sa̫ne-et-Loire",FR,Burgundy,Sa̫ne-et-Loire,based on nearby landmark,seconds,small collection,"Coordinates based on the centre of Autun, a commune in the Sa̫ne-et-Loire department in Burgundy in eastern France.",gp_mid,18.16,1.93,305,FR,,Autun,,,group of beds,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,adpression,,,,,,,,,,NA,,,taxonomic,,MNHN,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 08:27,03/08/2016 08:27,NA,pedestris,Apateon,57795,,298.9,295,Autunian,,NA,FR,Apateon pedestris
1338631,occ,NA,,180802,members,Apateon pedestris,species,229308,,Apateon pedestris,NA,species,229308,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,7.689722,49.734436,Rehborn,NA,,DE,Rhineland-Palatine,Bad Kreuznach,,6,,"Lat long based on the residential area of Rehborn, 1km north of Meisenheim in the Bad Kreuznach district in Rhineland-Palatinate, Germany.",gp_mid,19.75,5.14,315,DE,,Meisenheim,,,group of beds,,M6,M6,,,,NA,"""Lower Rotliegend"". Stratgraphy here based on K̦niger et al. (2002)",,not reported,,,,,,,,,,fluvial-lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 08:55,03/08/2016 08:55,NA,pedestris,Apateon,57795,,298.9,295.5,Asselian,,NA,DE,Apateon pedestris
1338632,occ,NA,,180803,members,Apateon pedestris,species,229308,,Apateon pedestris,NA,species,229308,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,7.405251,49.480812,Quirnbach,NA,near Kusel,DE,Rhineland-Palatinate,Kusel,based on nearby landmark,6,small collection,"Lat long based on centre of Quirnbach/Pfalz in the Kusel district in Rhineland-Palatinate, Germany.",gp_mid,19.46,4.6,315,DE,,Quirnbach,,,,,Lauterecken Oernheim,Lauterecken Oernheim,,Saar-Nahe,Lauterecken Oernheim,NA,"Saar-Nahe Basin, Lower Rotliegend. Time interval based on K̦niger et al. (2002: Fig 2).",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 09:01,03/08/2016 09:01,NA,pedestris,Apateon,57795,,301.2,298.9,Kuzel,,NA,DE,Apateon pedestris
1338633,occ,NA,,180804,members,Apateon pedestris,species,229308,,Apateon pedestris,NA,species,229308,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,7.555727,49.65683,Grumbach,NA,,DE,Rhineland-Palatine,Kusel,based on nearby landmark,6,small collection,"Lat long is for the centre of Grumbach, in the Kusel district in Rhineland-Palatinate, Germany.",gp_mid,19.68,5.04,315,DE,,Meisenheim,,,group of beds,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 09:14,03/08/2016 09:14,NA,pedestris,Apateon,57795,,298.9,295.5,Asselian,,NA,DE,Apateon pedestris
1338634,occ,NA,,180805,members,Apateon pedestris,species,229308,,Apateon pedestris,NA,species,229308,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,7.76075,49.585155,Messersbacherhof,NA,,DE,Rhineland-Palatine,,based on nearby landmark,6,small collection,"Lat long is for the centre of Messersbacherhof, a residential area near the Kreuzbach river, approximately 20km north of Kaiserslautern, in Rhineland-Palatinate, Germany.",gp_mid,19.83,5.01,315,DE,,Meisenheim,,,group of beds,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,03/08/2016 09:17,03/08/2016 09:17,NA,pedestris,Apateon,57795,,298.9,295.5,Asselian,,NA,DE,Apateon pedestris
1338643,occ,NA,,180809,members,n. gen. Timonya n. sp. anneae,species,345832,,Timonya anneae,NA,species,345832,Cisneros et al.,2015,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,345831,NA,NA,NA,,-42.839375,-5.104057,"Timon, Maranhao",NA,Maranḥo,BR,Maranhao,Timon,based on nearby landmark,6,small collection,"Lat long corresponds with the centre of Timon Municipality, Maranḥo State, a municipality in Brazil",gp_mid,-11.13,-27.66,201,BR,,Lower Pedra de Fogo,,,group of beds,,,,,Parnaiba,Parnaiba,NA,"""Lower Pedra de Fogo Formation (Parna ba Basin)""","""The rocks exposed at the Timon quarry are massive, tabular strata of red siltstone interbedded with fine-grained sandstone and mudstone intervals. The fossil-bearing strata in this quarry are an B3 m thick succession of fissile dark reddish-brown mudstone overlying a finely laminated light-purple calcareous fine-grained sandstone with greenish grey mottles (36 m on Fig. 4). "" Cisneros et al. (2015)",siltstone,"massive,tabular,red",,,,sandstone,,,,,fluvial-lacustrine indet.,,"""The fossil-bearing interval is interpreted as fluvio-lacustrine in origin, deposited in a range of terrestrial and aquatic sub-environments on the margins and nearshore of large continental lakes, on seasonally wet floodplains and channels, and within small ponds "" Cisneros et al. (2015)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,Collections at UFPI,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Timonya,n. gen.,NA,NA,vertebrate,"J. C. Cisneros, C. Marsicano, and K. D. Angielczyk, R. M. H. Smith, M. Richter, J. Frobisch, C. F. Kammerer, R. W. Sadleir. 2015. New Permian fauna from tropical Gondwana. Nature Communications 6(8676)",327,697,0,R. Butler,E. Dunne,,03/08/2016 12:08,03/08/2016 12:08,NA,anneae,Timonya,60045,n. sp.,279.3,272.3,Kungurian,,NA,BR,Timonya anneae
1338644,occ,NA,,180810,members,Timonya anneae,species,345832,,Timonya anneae,NA,species,345832,Cisneros et al.,2015,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,345831,NA,NA,NA,,-42.811382,-5.364122,"Nazaria, Piaui State",NA,Nazaria Municipality,BR,Piaui,Nazaria,based on nearby landmark,6,small collection,"Lat long corresponds with the centre of Nazria Municipality, Piau_ State, a municipality in Brazil",gp_mid,-11.18,-27.92,201,BR,,Lower Pedra de Fogo,,,group of beds,,,,,Parnaiba,Parnaiba,NA,"""Lower Pedra de Fogo Formation (Parna ba Basin)""",,not reported,,,,,,,,,,fluvial-lacustrine indet.,,"""The fossil-bearing interval is interpreted as fluvio-lacustrine in origin, deposited in a range of terrestrial and aquatic sub-environments on the margins and nearshore of large continental lakes, on seasonally wet floodplains and channels, and within small ponds "" Cisneros et al. (2015)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,Collections at UFPI,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Timonya,,NA,NA,vertebrate,"J. C. Cisneros, C. Marsicano, and K. D. Angielczyk, R. M. H. Smith, M. Richter, J. Frobisch, C. F. Kammerer, R. W. Sadleir. 2015. New Permian fauna from tropical Gondwana. Nature Communications 6(8676)",327,697,0,R. Butler,E. Dunne,,03/08/2016 12:12,03/08/2016 12:12,NA,anneae,Timonya,60045,,279.3,272.3,Kungurian,,NA,BR,Timonya anneae
1338645,occ,NA,,180810,members,Procuhy n. sp. nazariensis,species,345834,,Procuhy nazariensis,NA,species,345834,Cisneros et al.,2015,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,345833,NA,NA,NA,,-42.811382,-5.364122,"Nazaria, Piaui State",NA,Nazaria Municipality,BR,Piaui,Nazaria,based on nearby landmark,6,small collection,"Lat long corresponds with the centre of Nazria Municipality, Piau_ State, a municipality in Brazil",gp_mid,-11.18,-27.92,201,BR,,Lower Pedra de Fogo,,,group of beds,,,,,Parnaiba,Parnaiba,NA,"""Lower Pedra de Fogo Formation (Parna ba Basin)""",,not reported,,,,,,,,,,fluvial-lacustrine indet.,,"""The fossil-bearing interval is interpreted as fluvio-lacustrine in origin, deposited in a range of terrestrial and aquatic sub-environments on the margins and nearshore of large continental lakes, on seasonally wet floodplains and channels, and within small ponds "" Cisneros et al. (2015)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,Collections at UFPI,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Procuhy,,NA,NA,vertebrate,"J. C. Cisneros, C. Marsicano, and K. D. Angielczyk, R. M. H. Smith, M. Richter, J. Frobisch, C. F. Kammerer, R. W. Sadleir. 2015. New Permian fauna from tropical Gondwana. Nature Communications 6(8676)",327,697,0,R. Butler,E. Dunne,,03/08/2016 12:14,03/08/2016 12:14,NA,nazariensis,Procuhy,60045,n. sp.,279.3,272.3,Kungurian,,NA,BR,Procuhy nazariensis
1338755,occ,NA,,180810,members,Captorhinus aguti,species,90718,,Captorhinus aguti,NA,species,134887,Cisneros et al.,2015,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,,-42.811382,-5.364122,"Nazaria, Piaui State",NA,Nazaria Municipality,BR,Piaui,Nazaria,based on nearby landmark,6,small collection,"Lat long corresponds with the centre of Nazria Municipality, Piau_ State, a municipality in Brazil",gp_mid,-11.18,-27.92,201,BR,,Lower Pedra de Fogo,,,group of beds,,,,,Parnaiba,Parnaiba,NA,"""Lower Pedra de Fogo Formation (Parna ba Basin)""",,not reported,,,,,,,,,,fluvial-lacustrine indet.,,"""The fossil-bearing interval is interpreted as fluvio-lacustrine in origin, deposited in a range of terrestrial and aquatic sub-environments on the margins and nearshore of large continental lakes, on seasonally wet floodplains and channels, and within small ponds "" Cisneros et al. (2015)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,Collections at UFPI,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,"J. C. Cisneros, C. Marsicano, and K. D. Angielczyk, R. M. H. Smith, M. Richter, J. Frobisch, C. F. Kammerer, R. W. Sadleir. 2015. New Permian fauna from tropical Gondwana. Nature Communications 6(8676)",327,697,0,R. Butler,E. Dunne,,04/08/2016 04:07,04/08/2016 04:07,NA,aguti,Captorhinus,60045,,279.3,272.3,Kungurian,,NA,BR,Captorhinus aguti
1338756,occ,NA,,180814,members,Rhinesuchidae indet.,family,37065,,Rhinesuchidae,NA,family,37065,Cisneros et al.,2015,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Rhinesuchidae,37065,NA,NA,NA,NA,,-42.602898,-5.593595,"Monsenhor Gil, Piaui State",NA,Monsenhor Gil Municipality,BR,Piaui,Monsenhor Gil,based on nearby landmark,6,small collection,"Lat long corresponds with the centre of Monsenhor Gil Municipality, Piau_ State, Brazil",gp_mid,-11.02,-28.19,201,BR,,Lower Pedra de Fogo,,,group of beds,,,,,Parnaiba,Parnaiba,NA,"""Lower Pedra de Fogo Formation (Parna ba Basin)""",,not reported,,,,,,,,,,fluvial-lacustrine indet.,,"""The fossil-bearing interval is interpreted as fluvio-lacustrine in origin, deposited in a range of terrestrial and aquatic sub-environments on the margins and nearshore of large continental lakes, on seasonally wet floodplains and channels, and within small ponds "" Cisneros et al. (2015)",macrofossils,,,,,,NA,,"body,mold/impression",,,,,,,,,,NA,,,taxonomic,,,,,,,,,Collections at UFPI,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Rhinesuchidae,,NA,NA,vertebrate,"J. C. Cisneros, C. Marsicano, and K. D. Angielczyk, R. M. H. Smith, M. Richter, J. Frobisch, C. F. Kammerer, R. W. Sadleir. 2015. New Permian fauna from tropical Gondwana. Nature Communications 6(8676)",327,697,0,R. Butler,E. Dunne,,04/08/2016 04:10,04/08/2016 04:10,NA,indet.,,60045,,279.3,272.3,Kungurian,,NA,BR, indet.
1338757,occ,NA,,180814,members,Rhinesuchidae indet.,family,37065,,Rhinesuchidae,NA,family,37065,Cisneros et al.,2015,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Rhinesuchidae,37065,NA,NA,NA,NA,,-42.602898,-5.593595,"Monsenhor Gil, Piaui State",NA,Monsenhor Gil Municipality,BR,Piaui,Monsenhor Gil,based on nearby landmark,6,small collection,"Lat long corresponds with the centre of Monsenhor Gil Municipality, Piau_ State, Brazil",gp_mid,-11.02,-28.19,201,BR,,Lower Pedra de Fogo,,,group of beds,,,,,Parnaiba,Parnaiba,NA,"""Lower Pedra de Fogo Formation (Parna ba Basin)""",,not reported,,,,,,,,,,fluvial-lacustrine indet.,,"""The fossil-bearing interval is interpreted as fluvio-lacustrine in origin, deposited in a range of terrestrial and aquatic sub-environments on the margins and nearshore of large continental lakes, on seasonally wet floodplains and channels, and within small ponds "" Cisneros et al. (2015)",macrofossils,,,,,,NA,,"body,mold/impression",,,,,,,,,,NA,,,taxonomic,,,,,,,,,Collections at UFPI,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Rhinesuchidae,,NA,NA,vertebrate,"J. C. Cisneros, C. Marsicano, and K. D. Angielczyk, R. M. H. Smith, M. Richter, J. Frobisch, C. F. Kammerer, R. W. Sadleir. 2015. New Permian fauna from tropical Gondwana. Nature Communications 6(8676)",327,697,0,R. Butler,E. Dunne,,04/08/2016 04:10,04/08/2016 04:10,NA,indet.,,60045,,279.3,272.3,Kungurian,,NA,BR, indet.
1338758,occ,NA,,180815,members,Rhinesuchidae indet.,family,37065,,Rhinesuchidae,NA,family,37065,Cisneros et al.,2015,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Rhinesuchidae,37065,NA,NA,NA,NA,,-42.077934,-5.602332,"Pastos Bons, Maranhao",NA,Pedra de Fogo type-section,BR,Maranhao,,based on nearby landmark,6,small collection,"Lat long corresponds with the centre of Pastos Bons, Maranḥo State, Brazil.",gp_mid,-10.45,-28.33,201,BR,,Lower Pedra de Fogo,,,group of beds,,,,,Parnaiba,Parnaiba,NA,"""Lower Pedra de Fogo Formation (Parna ba Basin)""",,not reported,,,,,,,,,,fluvial-lacustrine indet.,,"""The fossil-bearing interval is interpreted as fluvio-lacustrine in origin, deposited in a range of terrestrial and aquatic sub-environments on the margins and nearshore of large continental lakes, on seasonally wet floodplains and channels, and within small ponds "" Cisneros et al. (2015)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,Collections at UFPI,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Rhinesuchidae,,NA,NA,vertebrate,"J. C. Cisneros, C. Marsicano, and K. D. Angielczyk, R. M. H. Smith, M. Richter, J. Frobisch, C. F. Kammerer, R. W. Sadleir. 2015. New Permian fauna from tropical Gondwana. Nature Communications 6(8676)",327,697,0,R. Butler,E. Dunne,,04/08/2016 04:15,04/08/2016 04:15,NA,indet.,,60045,,279.3,272.3,Kungurian,,NA,BR, indet.
1338759,occ,NA,,180816,members,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Witzmann and Voigt,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,7.825868,49.630356,"UGKU Locality 6, Rockenhausen",NA,Saar Nahe Basin,DE,Rhineland-Palatine,Donnersbergkreis,stated in text,6,small collection,"Lat long based on the location of Rockenhausen, a town in the Donnersbergkreis, in Rhineland-Palatinate, Germany. Rockenhausen is situated near to the southeastern margin of the Saar-Nahe Basin, which is one of the largest continuous outcrops of Late Carboniferous and Early Permian continental deposits in Central Europe (Schafer 1989; Schindler 2007b).",gp_mid,19.97,5.23,315,DE,,Meisenheim,Glan,,,,,,,,,NA,"The Permian part of the basin filling, largely equivalent with the local Rotliegend Group, attains a cumulative thickness of about 3,000 m (Boy et al. 2012). It is divided into two subgroups with nine and four formations, respectively. Lithostratigraphically, the fossil horizon is referred to the lower member of the Meisenheim Formation (middle part of the Jeckenbach Subformation, M5 or M6 sensu Boy et al. 2012). Radiometric data from intercalated volcanic ashes point to an early Early Permian (Asselian-Sakmarian) age of the Meisenheim Formation (Koniger 2000; Koniger and Lorenz 2002; von Seckendorff 2012).","The Glan Subgroup is a succession of predominantly grey-coloured, fluviolacustrine sediments, whereas alluvio-fluvial to playa-like red beds and volcanites characterize the Nahe Subgroup.",mudstone,"planar lamination,black,gray",,,,,,,,,fluvial-lacustrine indet.,,"The fossil-bearing beds at UGKU locality 6 can be interpreted as deeper lacustrine deposits, which is in agreement with finds of an articulated paramblypterid fish, isolated acanthodian fin spines, and fish or amphibian coprolites in the same strata (personal communication by Thomas Schindler and authors۪ own observations). Fossil bone from this site is always of black colour indicating that thermal overprinting by overlaying basaltic to andesitic subvolcanic rocks was below the critical threshold for the degradation of bitumen (Poschmann and Schindler 2004; Montenari and Uhl 2005).",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,UGKU,,"Fossils were found by a private collector, Bernd Graumann, Mehlingen, in 1978.",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"F. Witzmann and S. Voigt. 2014. An Eryops-like interclavicle from the Early Permian of the Saar-Nahe Basin, and a discussion of temnospondyl interclavicle characters. Palaeontologische Zeitschrift ",327,697,0,R. Butler,E. Dunne,,04/08/2016 04:36,04/08/2016 04:36,NA,sp.,Eryops,60048,,298.9,290.1,Asselian,Sakmarian,NA,DE,Eryops sp.
1338761,occ,NA,,180817,members,n. gen. Palatinerpeton n. sp. kraetschmeri,species,344538,,Palatinerpeton kraetschmeri,NA,species,344538,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,344539,NA,NA,NA,,7.814231,49.692101,"Morsbacher hof, near Mannweiler-Colln",NA,Mannweiler C̦lln,DE,Rhineland-Palatine,Donnersbergkreis ,based on nearby landmark,6,small collection,"Lat long is for Morsbacherstrae, on the east side of the town of Mannweiler-C̦lln in the Donnersbergkreis district, in Rhineland-Palatinate, Germany.",gp_mid,19.95,5.28,315,DE,,Lauterecken-Odernehim,,,group of beds,,Morsbacher-Bank,Morsbacher Bank,,,,NA,"""Lower Rotliegend, Autunian"" Schoch & Milner, 2000. Dating here is based on Koniger et al. (2002)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Palatinerpeton,n. gen.,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 05:03,04/08/2016 05:03,NA,kraetschmeri,Palatinerpeton,28828,n. sp.,298.9,290.1,Asselian,Sakmarian,NA,DE,Palatinerpeton kraetschmeri
1338762,occ,NA,,27263,,Actinodon n. sp. risinensis,species,345843,recombined as,Lysipterygium risinense,NA,species,345843,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Lysipterygiidae,345842,345841,NA,NA,NA,,74.908333,34.041668,Risin Spur (Gangamopteris Shales),NA,Lower Gondwanan series,IN,Kashmir,,based on nearby landmark,seconds,,"specimens were collected ""..on Risin Spur near Zewan Village..""",gp_mid,61.41,-55.08,501,IN,,,,,,,,,,,,NA,"""collected from the Lower Permian Gangamopteris shales (glassy volcanic tuff) of the Lower Gondwana series"". Age previously given as Rotliegendes but Gangamopteris shales correlated with Eurydesma-bearing beds at Manendragarh and the Salt Range, suggesting an Asselian-Sakmarian age.","""shales (glassy volcanic tuff)""","""shale""",tuffaceous,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,mold/impression",medium,,,,,,,,,NA,,"Specimen is in a slab. Much of the specimen is preserved as an impression. Bones, where preserved, are of ""a reddish crumbly material, mixed with matrix.""",taxonomic,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Actinodon,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 05:32,04/08/2016 05:32,7535,risinensis,Lysipterygium,28828,n. sp.,298.9,290.1,Asselian,Sakmarian,NA,IN,Lysipterygium risinensis
1338763,occ,NA,,156530,,Chelydosaurus n. sp. marahomensis,species,345846,,Chelydosaurus marahomensis,NA,species,345846,Verma,1962,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Actinodontidae,66914,296857,NA,NA,NA,,75.089996,33.875,"Baliarpatti spur, Marahom (Verma collection)",NA,,IN,,,estimated from map,3,small collection,,gp_mid,61.08,-54.27,501,IN,,Mamal,,,bed,,,,,,,NA,"Collected from a float block lying on the Marahom Member, but that could have come from the Marahom or Risin members",,"""shale""","tuffaceous,gray",lithified,,,,,,,,lacustrine indet.,rift,Rift basins associated with opening of Neotethys,macrofossils,,,,,,NA,,adpression,,,,,,,,,,NA,,,taxonomic,,,,,,K.K. Verma,,Repository: Geological Survey of India,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Chelydosaurus,,NA,NA,paleoentomology,"K. K. Verma. 1962. Chelydosaurus marahomensis n.sp. a new fossil labyrinthodont from the Lower Gondwanas near Marahom, Anantnag District, Kashmir. Indian Minerals 16:180-182",327,697,0,R. Butler,E. Dunne,,04/08/2016 05:43,04/08/2016 05:43,51296,marahomensis,Chelydosaurus,60049,n. sp.,290.1,279.3,Artinskian,,NA,IN,Chelydosaurus marahomensis
1338764,occ,NA,,180797,members,n. gen. Sclerocephalus n. sp. haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.709929,49.573929,Pfarrwald at Heimkirchen,NA,"Heimkirchen, near Niderkirchen",DE,Rhineland-Palatine,,,6,,"Coordinates are for Heimkirchen, a small residential area, approximately 500m east of Niederkirchen, Rhineland-Palatine, Germany.",gp_mid,19.91,5.15,315,DE,,Meisenheim,,,group of beds,,M9,Kappeln Bank,,,,NA,Startigraphy here is based on Koniger at al. (2002),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,n. gen.,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 06:10,04/08/2016 06:10,NA,haeuseri,Sclerocephalus,28828,n. sp.,298.9,290.1,Asselian,Sakmarian,NA,DE,Sclerocephalus haeuseri
1338765,occ,NA,,178736,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.602687,49.711227,"Jeckenbach, near Meisenheim",NA,,DE,Rhineland-Palatine,Bad Kreuznach,based on nearby landmark,6,small collection,"""Jeckenbach, Saar-Nahe Basin"" (Glienke, 2015). Coordinates based on the location of Jeckenbach.",gp_mid,19.7,5.1,315,DE,,Meisenheim,Rotliegend,,bed,,,,,,,NA,"Jecken- bach Bank (M6), Rotliegend",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Repository: MNHM (Museum National d۪Histoire Naturelle, Paris, France)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 06:31,04/08/2016 06:31,NA,haeuseri,Sclerocephalus,28828,,298.9,295,Autunian,,NA,DE,Sclerocephalus haeuseri
1338766,occ,NA,,180805,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.76075,49.585155,Messersbacherhof,NA,,DE,Rhineland-Palatine,,based on nearby landmark,6,small collection,"Lat long is for the centre of Messersbacherhof, a residential area near the Kreuzbach river, approximately 20km north of Kaiserslautern, in Rhineland-Palatinate, Germany.",gp_mid,19.83,5.01,315,DE,,Meisenheim,,,group of beds,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 06:32,04/08/2016 06:32,NA,haeuseri,Sclerocephalus,28828,,298.9,295.5,Asselian,,NA,DE,Sclerocephalus haeuseri
1338767,occ,NA,,180804,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.555727,49.65683,Grumbach,NA,,DE,Rhineland-Palatine,Kusel,based on nearby landmark,6,small collection,"Lat long is for the centre of Grumbach, in the Kusel district in Rhineland-Palatinate, Germany.",gp_mid,19.68,5.04,315,DE,,Meisenheim,,,group of beds,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 06:32,04/08/2016 06:32,NA,haeuseri,Sclerocephalus,28828,,298.9,295.5,Asselian,,NA,DE,Sclerocephalus haeuseri
1338768,occ,NA,,180806,members,Apateon pedestris,species,229308,,Apateon pedestris,NA,species,229308,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,7.359738,49.001251,Kappeln,NA,"Kappeln, Rhineland Palatine",DE,Rhineland-Palatine,,based on nearby landmark,6,small collection,"Lat long is for the centre of Kappel in the Rhein-Hunsr_ck-Kreis in Rhineland-Palatinate, Germany.",gp_mid,19.82,4.54,305,DE,,Meisenheim,,,group of beds,,M8,M8,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 06:34,04/08/2016 06:34,NA,pedestris,Apateon,28828,,298.9,290.1,Asselian,Sakmarian,NA,DE,Apateon pedestris
1338769,occ,NA,,180806,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.359738,49.001251,Kappeln,NA,"Kappeln, Rhineland Palatine",DE,Rhineland-Palatine,,based on nearby landmark,6,small collection,"Lat long is for the centre of Kappel in the Rhein-Hunsr_ck-Kreis in Rhineland-Palatinate, Germany.",gp_mid,19.82,4.54,305,DE,,Meisenheim,,,group of beds,,M8,M8,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 06:34,04/08/2016 06:34,NA,haeuseri,Sclerocephalus,28828,,298.9,290.1,Asselian,Sakmarian,NA,DE,Sclerocephalus haeuseri
1338770,occ,NA,,85451,,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.696111,49.578056,Niederkirchen/Westpfalz,NA,Gemeindeburg near Niederkirchen,DE,Rhineland-Palatinate,Kaiserslautern,based on nearby landmark,seconds,small collection,"Niederkirchen (Westpfalz), 16 km north of the city of Kaiserslautern; Lat long is for Niederkirchen. Locality lies in the Saar-Nahe district. Location described by Glienke (2013) as ""Gemeindeburg near Niederkirchen/Westpfalz, Saar-Nahe Basin)",gp_mid,19.79,4.99,315,DE,,Meisenheim,Rotliegend,,member,,M6,M6,,,,NA,"""Biostratigraphically, the find can be attributed to Boy's Leptorophus humbergensis-Apateon caducus association. This association is part of the Apateon caducus group and has an upper 'Autunian' age. This corresponds to the lower Sakmarian of international stratigraphy""\r\nThe Jeckenbach Subformation, however, is of Asselian age according to ""Stratigraphische Tabelle von Deutschland 2002""","""laminated silty grey shale""","""shale""","planar lamination,gray",,silty,Y,,,,,,lacustrine - large,intermontane basin,"""deposited in a large, shallow, eutrophic lake"" - Carroll (1991)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 06:34,04/08/2016 06:34,28837,haeuseri,Sclerocephalus,28828,,298.9,295.5,Asselian,,NA,DE,Sclerocephalus haeuseri
1338771,occ,NA,,180800,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.701944,49.761665,Odernheim,NA,Odernheimer Kalkbank,DE,Rhineland-Palatine,Bad Kreuznach,based on nearby landmark,seconds,small collection,"Coordinates based on location south of Obernheim am Glan, a town in Rhineland-Palatine, Germany.",gp_mid,19.86,5.33,315,DE,,Meisenheim,,,group of beds,,Obernheim beds,Obernheimer Kalkbank,,,,NA,"Meisenheim Formation (M8), Saar-Nahe Basin, Germany\r\nObernheimer Kalkbank (""limestone bank"")",,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,697,R. Butler,E. Dunne,E. Dunne,04/08/2016 06:37,04/08/2016 06:43,NA,haeuseri,Sclerocephalus,28828,,298.9,290.1,Asselian,Sakmarian,NA,DE,Sclerocephalus haeuseri
1338793,occ,NA,,180780,members,Sclerocephalus n. sp. credneri,species,345849,,Sclerocephalus credneri,NA,species,345849,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,15.06758,50.79026,"Ruprechtice, Liberecky kraj",NA,,CZ,,,based on nearby landmark,6,small collection,"Lat and long based on the location of Ruprechtice in the city of Liberec, Czech Republic.",gp_mid,23.99,7.5,305,CZ,,Broumov,,,group of beds,,,,,,,NA,The Broumov Formation (after the town of Broumov) is Upper Autunian in age.,The Broumov Formation is formed of red mudstones and grey and variegated pelitic rocks with carbonates and cherts. - Falke (1972),mudstone,red,lithified,,,"""carbonate""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 08:20,04/08/2016 08:20,NA,credneri,Sclerocephalus,28828,n. sp.,298.9,295,Autunian,,NA,CZ,Sclerocephalus credneri
1338794,occ,NA,,180847,members,Sclerocephalus jogischneideri,species,345848,,Sclerocephalus jogischneideri,NA,species,345848,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,10.615278,50.787498,Tambach,NA,,DE,Thuringia,Gotha,based on nearby landmark,seconds,hand sample,"Coordinates are for the centre of Tambach-Dietharz, in Thuringia, Germany",gp_mid,21.29,6.64,305,DE,,Oberhof,Rotliegend,,bed,,Oberhof Beds,Upper Oberhof Beds,,Tambach Basin,Tambach Basin,NA,,,"""siliciclastic""",,,,Y,,,,,,fluvial-lacustrine indet.,intramontane basin,"The Tambach Basin generally is regarded as an intramontane basin (for details see Eberth et al., 2000, Palaios 15(4) pp. 293-313).",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,MNG (Museum der Natur Gotha),,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 08:28,04/08/2016 08:28,NA,jogischneideri,Sclerocephalus,28828,,298.9,295,Autunian,,NA,DE,Sclerocephalus jogischneideri
1338795,occ,NA,,180799,members,Sclerocephalus jogischneideri,species,345848,,Sclerocephalus jogischneideri,NA,species,345848,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,10.58887,50.834412,"Finsterbergen, near Friedrichroda",NA,,DE,Thuringia,,based on nearby landmark,6,small collection,"Coordinates based on the centre of Finsterbergen, a town approximately 2km south of Friedrichroda, Thuringia, Germany",gp_mid,21.26,6.68,305,DE,,Oberhof,,,bed,,Oberhof Beds,Upper Oberhof Beds,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,FG collection,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 08:32,04/08/2016 08:32,NA,jogischneideri,Sclerocephalus,28828,,298.9,295,Autunian,,NA,DE,Sclerocephalus jogischneideri
1338796,occ,NA,,175918,members,n. gen. Weissia n. sp. bavarica,species,345851,recombined as,Sclerocephalus bavaricus,NA,species,345851,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.34937,49.449932,"Ohmbach, near Altenglan",NA,,DE,Rhineland-Palatine,Kusel,based on nearby landmark,6,small collection,"Lat long is for the town of Ohmbach in the Kusel district of Rhineland-Palatine, Germany.",gp_mid,19.6,4.81,315,DE,,Altenglan,,,group of beds,,Ohmbach Carbonate Unit,Ohmbach Carbonate Unit,,Saar Nahe,Saar Nahe,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Weissia,n. gen.,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 08:53,04/08/2016 08:53,NA,bavarica,Sclerocephalus,28828,n. sp.,298.9,295,Autunian,,NA,DE,Sclerocephalus bavarica
1338809,occ,NA,,180848,members,Sclerocephalus n. sp. jogischneideri,species,345848,,Sclerocephalus jogischneideri,NA,species,345848,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,10.565278,50.856945,Road-cut uphill of Gottlob quarry,NA,,DE,Thuringia,Suhl,based on nearby landmark,seconds,small collection,"Coordinates based on the town of Friedrichroda, Suhl district, Thuringia, Germany",gp_mid,21.24,6.7,305,DE,,Oberhof,,,bed,,Upper Oberhof Beds,Upper Oberhof Beds,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,"FG collection (Pal_ontologische Sammlung, Bergakademie Freiberg)","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. Osteology and relationships of the temnospondyl genus Sclerocephalus. Zoological Journal of the Linnean Society 157:135-168,327,697,697,R. Butler,E. Dunne,E. Dunne,04/08/2016 09:11,04/08/2016 09:12,NA,jogischneideri,Sclerocephalus,60052,n. sp.,298.9,295.5,Asselian,,NA,DE,Sclerocephalus jogischneideri
1338861,occ,NA,,180851,members,Sclerocephalus n. sp. nobilis,species,345860,,Sclerocephalus nobilis,NA,species,345860,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.707693,49.766941,Klauswald at Odernheim,NA,,DE,Rhineland-Palatine,Bad Kreuznach,based on nearby landmark,6,small collection,"Coordinates based on the centre of Odernheim am Glan, a town in Rhineland-Palatine, Germany.",gp_mid,19.75,5.17,315,DE,,Meisenheim,,,bed,,Kappeln Black Shale,Kappeln Unit,,Saar-Nahe Basin,Saar Nahe Basin,NA,Obernheim Subformation (M9),,"""shale""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. Osteology and relationships of the temnospondyl genus Sclerocephalus. Zoological Journal of the Linnean Society 157:135-168,327,697,0,R. Butler,E. Dunne,,04/08/2016 10:04,04/08/2016 10:04,NA,nobilis,Sclerocephalus,60052,n. sp.,298.9,295,Autunian,,NA,DE,Sclerocephalus nobilis
1338862,occ,NA,,180851,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.707693,49.766941,Klauswald at Odernheim,NA,,DE,Rhineland-Palatine,Bad Kreuznach,based on nearby landmark,6,small collection,"Coordinates based on the centre of Odernheim am Glan, a town in Rhineland-Palatine, Germany.",gp_mid,19.75,5.17,315,DE,,Meisenheim,,,bed,,Kappeln Black Shale,Kappeln Unit,,Saar-Nahe Basin,Saar Nahe Basin,NA,Obernheim Subformation (M9),,"""shale""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. Osteology and relationships of the temnospondyl genus Sclerocephalus. Zoological Journal of the Linnean Society 157:135-168,327,697,0,R. Butler,E. Dunne,,04/08/2016 10:09,04/08/2016 10:09,NA,haeuseri,Sclerocephalus,60052,,298.9,295,Autunian,,NA,DE,Sclerocephalus haeuseri
1338863,occ,NA,,180851,members,Cheliderpeton n. sp. lellbachae,species,345862,,Cheliderpeton lellbachae,NA,species,345862,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Intasuchidae,137935,37009,NA,NA,NA,,7.707693,49.766941,Klauswald at Odernheim,NA,,DE,Rhineland-Palatine,Bad Kreuznach,based on nearby landmark,6,small collection,"Coordinates based on the centre of Odernheim am Glan, a town in Rhineland-Palatine, Germany.",gp_mid,19.75,5.17,315,DE,,Meisenheim,,,bed,,Kappeln Black Shale,Kappeln Unit,,Saar-Nahe Basin,Saar Nahe Basin,NA,Obernheim Subformation (M9),,"""shale""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Cheliderpeton,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. Osteology and relationships of the temnospondyl genus Sclerocephalus. Zoological Journal of the Linnean Society 157:135-168,327,697,697,R. Butler,E. Dunne,E. Dunne,04/08/2016 10:09,04/08/2016 10:13,NA,lellbachae,Cheliderpeton,60052,n. sp.,298.9,295,Autunian,,NA,DE,Cheliderpeton lellbachae
1338871,occ,NA,,180796,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.442166,49.573666,Erdesbach (H̦lle),NA,Holle near Erdesbach,DE,Rhineland-Palatinate,Kusel district,based on nearby landmark,6,small collection,"Cooridnates based on the centre of Erdesbach, a municipality in the Kusel district in Rhineland-Palatinate, Germany.",gp_mid,19.63,4.95,315,DE,,Meisenheim,,M7,group of beds,,,,,Saar Nahe,Saar Nahe,NA,,,not reported,,,,,,,,,,lacustrine - small,,"""Small lake deposit""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,all macrofossils,,,,,,GPIM Collection,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. Osteology and relationships of the temnospondyl genus Sclerocephalus. Zoological Journal of the Linnean Society 157:135-168,327,697,0,R. Butler,E. Dunne,,04/08/2016 10:45,04/08/2016 10:45,NA,haeuseri,Sclerocephalus,60052,,298.9,295.5,Asselian,,NA,DE,Sclerocephalus haeuseri
1338872,occ,NA,,180783,members,Melanerpeton humbergense,species,345808,,Melanerpeton humbergense,NA,species,345807,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,260059,NA,NA,NA,,7.778611,49.413334,"Humberg, near Obernheim",NA,,DE,Rhineland-Pfalz,,based on nearby landmark,seconds,small collection,"Lat long based on the location of Humberg, approximately 1.5km south of the city of Kaiserslautern, Rhineland-Palatine, Germany",gp_mid,19.88,4.84,305,DE,,Meisenheim,Glan,M10,group of beds,,,,,,,NA,"M10, Odernheim Subformation.\r\n""The Pappelberg-Tuff in the Meisenheim Formation (Glan Group) has been dated by U/Pb zircon SHRIMP technique at 297.03.2 Ma. Taking the Carboniferous/Permian boundary at 296 Ma, the Meisenheim Formation coincides approximately with this boundary."" K̦niger et al. (2002)\r\n","In the informal units M5 to M10 the base of each unit is developed as mostly reddish, coarse-grained channel deposits of a braided river system. - Boy et al. (2012)",sandstone,red,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Melanerpeton,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,697,R. Butler,E. Dunne,E. Dunne,04/08/2016 10:47,04/08/2016 10:47,NA,humbergense,Melanerpeton,57795,,298.9,295.5,Asselian,,NA,DE,Melanerpeton humbergense
1338873,occ,NA,,180783,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.778611,49.413334,"Humberg, near Obernheim",NA,,DE,Rhineland-Pfalz,,based on nearby landmark,seconds,small collection,"Lat long based on the location of Humberg, approximately 1.5km south of the city of Kaiserslautern, Rhineland-Palatine, Germany",gp_mid,19.88,4.84,305,DE,,Meisenheim,Glan,M10,group of beds,,,,,,,NA,"M10, Odernheim Subformation.\r\n""The Pappelberg-Tuff in the Meisenheim Formation (Glan Group) has been dated by U/Pb zircon SHRIMP technique at 297.03.2 Ma. Taking the Carboniferous/Permian boundary at 296 Ma, the Meisenheim Formation coincides approximately with this boundary."" K̦niger et al. (2002)\r\n","In the informal units M5 to M10 the base of each unit is developed as mostly reddish, coarse-grained channel deposits of a braided river system. - Boy et al. (2012)",sandstone,red,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. Osteology and relationships of the temnospondyl genus Sclerocephalus. Zoological Journal of the Linnean Society 157:135-168,327,697,0,R. Butler,E. Dunne,,04/08/2016 10:47,04/08/2016 10:47,NA,haeuseri,Sclerocephalus,60052,,298.9,295.5,Asselian,,NA,DE,Sclerocephalus haeuseri
1338874,occ,NA,,180802,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.689722,49.734436,Rehborn,NA,,DE,Rhineland-Palatine,Bad Kreuznach,,6,,"Lat long based on the residential area of Rehborn, 1km north of Meisenheim in the Bad Kreuznach district in Rhineland-Palatinate, Germany.",gp_mid,19.75,5.14,315,DE,,Meisenheim,,,group of beds,,M6,M6,,,,NA,"""Lower Rotliegend"". Stratgraphy here based on K̦niger et al. (2002)",,not reported,,,,,,,,,,fluvial-lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. Osteology and relationships of the temnospondyl genus Sclerocephalus. Zoological Journal of the Linnean Society 157:135-168,327,697,0,R. Butler,E. Dunne,,04/08/2016 10:51,04/08/2016 10:51,NA,haeuseri,Sclerocephalus,60052,,298.9,295.5,Asselian,,NA,DE,Sclerocephalus haeuseri
1338875,occ,NA,,180853,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.689722,49.734436,Rehborn (Hasenkopf),NA,,DE,Rhineland-Palatine,Bad Kreuznach,,6,,"Lat long based on the residential area of Rehborn, 1km north of Meisenheim in the Bad Kreuznach district in Rhineland-Palatinate, Germany.",gp_mid,19.75,5.14,315,DE,,Meisenheim,,,group of beds,,M8,M8,,,,NA,Stratigraphy here based on K̦niger et al. (2002),,not reported,,,,,,,,,,fluvial-lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. Osteology and relationships of the temnospondyl genus Sclerocephalus. Zoological Journal of the Linnean Society 157:135-168,327,697,0,R. Butler,E. Dunne,,04/08/2016 10:53,04/08/2016 10:53,NA,haeuseri,Sclerocephalus,60052,,298.9,295.5,Asselian,,NA,DE,Sclerocephalus haeuseri
1338876,occ,NA,,180854,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.590683,49.652191,Lauterecken (Windhof),NA,,DE,Rhineland-Palatine,Kusel,based on nearby landmark,6,small collection,"Lat long is for the centre of Lauterecken, in the Kusel district in Rhineland-Palatinate, Germany.",gp_mid,19.7,5.05,315,DE,,Meisenheim,,,bed,,M6,M6,,Saar Nahe Basin,Saar Nahe Basin,NA,Stratigraphy based on that of Koniger et al. (2002),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. Osteology and relationships of the temnospondyl genus Sclerocephalus. Zoological Journal of the Linnean Society 157:135-168,327,697,0,R. Butler,E. Dunne,,04/08/2016 10:55,04/08/2016 10:55,NA,haeuseri,Sclerocephalus,60052,,298.9,295.5,Asselian,,NA,DE,Sclerocephalus haeuseri
1338878,occ,NA,,180855,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.627551,49.719891,Desloch,NA,,DE,Rhineland-Palatine,Kusel,based on nearby landmark,6,small collection,"Lat long is for the centre of Desloch, in the Kusel district in Rhineland-Palatinate, Germany.",gp_mid,19.71,5.12,315,DE,,Meisenheim,,,bed,,M6,M6,,Saar Nahe Basin,Saar Nahe Basin,NA,Stratigraphy based on that of Koniger et al. (2002),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. Osteology and relationships of the temnospondyl genus Sclerocephalus. Zoological Journal of the Linnean Society 157:135-168,327,697,0,R. Butler,E. Dunne,,04/08/2016 11:29,04/08/2016 11:29,NA,haeuseri,Sclerocephalus,60052,,298.9,295.5,Asselian,,NA,DE,Sclerocephalus haeuseri
1338879,occ,NA,,180857,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.653571,49.728008,Raumbach,NA,,DE,Rhineland-Palatine,Bad Kreuznach,based on nearby landmark,6,small collection,"Lat long is for the centre of Raumbach, in the Bad Kreuznach district in Rhineland-Palatinate, Germany.",gp_mid,19.73,5.13,315,DE,,Meisenheim,,,bed,,M6,M6,,Saar Nahe Basin,Saar Nahe Basin,NA,Stratigraphy based on that of Koniger et al. (2002),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. Osteology and relationships of the temnospondyl genus Sclerocephalus. Zoological Journal of the Linnean Society 157:135-168,327,697,0,R. Butler,E. Dunne,,04/08/2016 11:31,04/08/2016 11:31,NA,haeuseri,Sclerocephalus,60052,,298.9,295.5,Asselian,,NA,DE,Sclerocephalus haeuseri
1338880,occ,NA,,180858,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.573897,49.829369,Langenthal,NA,,DE,Rhineland-Palatine,Bad Kreuznach,based on nearby landmark,6,small collection,"Lat long is for the centre of Langenthal, in the Bad Kreuznach district in Rhineland-Palatinate, Germany.",gp_mid,19.65,5.21,315,DE,,Meisenheim,,,bed,,M8,M8,,Saar Nahe Basin,Saar Nahe Basin,NA,Stratigraphy based on that of Koniger et al. (2002),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. Osteology and relationships of the temnospondyl genus Sclerocephalus. Zoological Journal of the Linnean Society 157:135-168,327,697,0,R. Butler,E. Dunne,,04/08/2016 11:33,04/08/2016 11:33,NA,haeuseri,Sclerocephalus,60052,,298.9,295.5,Asselian,,NA,DE,Sclerocephalus haeuseri
1338881,occ,NA,,180859,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.33006,49.516792,Albessen,NA,,DE,Rhineland-Palatine,Kusel,based on nearby landmark,6,small collection,"Lat long is for the centre of Albessen, in the Kusel district in Rhineland-Palatinate, Germany.",gp_mid,19.57,4.87,315,DE,,Meisenheim,,,bed,,M8,M8,,Saar Nahe Basin,Saar Nahe Basin,NA,Stratigraphy based on that of Koniger et al. (2002),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. Osteology and relationships of the temnospondyl genus Sclerocephalus. Zoological Journal of the Linnean Society 157:135-168,327,697,0,R. Butler,E. Dunne,,04/08/2016 11:35,04/08/2016 11:35,NA,haeuseri,Sclerocephalus,60052,,298.9,295.5,Asselian,,NA,DE,Sclerocephalus haeuseri
1338882,occ,NA,,178735,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.778986,49.802879,Niederhausen/Appel,NA,,DE,Rhineland-Palatinate,Bad Kreuznach,based on nearby landmark,6,small collection,"""Niederhausen/Appel, Saar-Nahe Basin"" (Glienke, 2015). Coordinates based on the location of Niederhausen.",gp_mid,19.79,5.22,315,DE,,Meisenheim,Rotliegend,,bed,,,,,,,NA,"Saar-Nahe Basin, Kappeln Bank, Meisenheim Formation (M9)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Repository: MNHM (Museum National d۪Histoire Naturelle, Paris, France)",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. Osteology and relationships of the temnospondyl genus Sclerocephalus. Zoological Journal of the Linnean Society 157:135-168,327,697,0,R. Butler,E. Dunne,,04/08/2016 11:35,04/08/2016 11:35,NA,haeuseri,Sclerocephalus,60052,,298.9,295.5,Asselian,,NA,DE,Sclerocephalus haeuseri
1338883,occ,NA,,180860,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.689722,49.734436,Gresaubach,NA,,DE,Saarland,,based on nearby landmark,6,small collection,"Lat long based on the residential area of Gresaubach, in Saarland, Germany.",gp_mid,19.75,5.14,315,DE,,Meisenheim,,M10,group of beds,,,,,,,NA,Stratgraphy here based on K̦niger et al. (2002),,not reported,,,,,,,,,,fluvial-lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. Osteology and relationships of the temnospondyl genus Sclerocephalus. Zoological Journal of the Linnean Society 157:135-168,327,697,0,R. Butler,E. Dunne,,04/08/2016 11:38,04/08/2016 11:38,NA,haeuseri,Sclerocephalus,60052,,298.9,295.5,Asselian,,NA,DE,Sclerocephalus haeuseri
1338885,occ,NA,,180862,members,Sclerocephalus haeuseri,species,255233,,Sclerocephalus haeuseri,NA,species,255233,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37015,NA,NA,NA,,7.555727,49.65683,St Wendel,NA,Sankt Wendel,DE,Saarland,,based on nearby landmark,6,small collection,"Lat long is for the centre of Sankt Wendel (St. Wendel), as town in the northeast of Saarland, Germany.",gp_mid,19.68,5.04,315,DE,,Meisenheim,,,bed,,M3,M3,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Sclerocephalus,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. Osteology and relationships of the temnospondyl genus Sclerocephalus. Zoological Journal of the Linnean Society 157:135-168,327,697,0,R. Butler,E. Dunne,,04/08/2016 11:41,04/08/2016 11:41,NA,haeuseri,Sclerocephalus,60052,,298.9,295.5,Asselian,,NA,DE,Sclerocephalus haeuseri
1338886,occ,NA,,58139,,n. gen. Cheliderpeton n. sp. vranyi,species,345866,,Cheliderpeton vranyi,NA,species,345866,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Intasuchidae,137935,37009,NA,NA,NA,,16.335833,50.583889,"Olivt_n, Broumov City, Boheme",NA,"Olivetin, Oelberg bei Branau",CZ,Boheme,,based on nearby landmark,seconds,,"Olivet_n, close to the City Broumov, Boheme\r\nGerman name of Olivetin (Oelberg) given by Estes 1970, J Paleont",gp_mid,26.98,10.91,305,CZ,,,,,,,,,,,,NA,"Lower Permian (i.e., Rotliegendes: JA)",,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,"Geologic-paleontological department of the National-Museum, Prag",,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Cheliderpeton,n. gen.,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 11:54,04/08/2016 11:54,15696,vranyi,Cheliderpeton,28828,n. sp.,298.9,254,Rotliegendes,,NA,CZ,Cheliderpeton vranyi
1338887,occ,NA,,180780,members,Cheliderpeton vranyi,species,345866,,Cheliderpeton vranyi,NA,species,345866,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Intasuchidae,137935,37009,NA,NA,NA,,15.06758,50.79026,"Ruprechtice, Liberecky kraj",NA,,CZ,,,based on nearby landmark,6,small collection,"Lat and long based on the location of Ruprechtice in the city of Liberec, Czech Republic.",gp_mid,23.99,7.5,305,CZ,,Broumov,,,group of beds,,,,,,,NA,The Broumov Formation (after the town of Broumov) is Upper Autunian in age.,The Broumov Formation is formed of red mudstones and grey and variegated pelitic rocks with carbonates and cherts. - Falke (1972),mudstone,red,lithified,,,"""carbonate""",,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Cheliderpeton,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 11:54,04/08/2016 11:54,NA,vranyi,Cheliderpeton,28828,,298.9,295,Autunian,,NA,CZ,Cheliderpeton vranyi
1338890,occ,NA,,180864,members,n. gen. Archegosaurus n. sp. decheni,species,255841,,Archegosaurus decheni,NA,species,255841,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37058,NA,NA,NA,,6.906613,49.408798,Lebach,NA,,DE,Saarland,Saarlouis,based on nearby landmark,6,small collection,"Lat long based on the residential area of Lebach, in the district of Saarlouis, Saarland, Germany.",gp_mid,19.33,4.7,315,DE,,Meisenheim,,,group of beds,,M10,Odernheim Beds,,Saar Nahe,Saar Nahe Basin,NA,Stratgraphy here based on K̦niger et al. (2002),,not reported,,,,,,,,,,fluvial-lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Archegosaurus,n. gen.,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 12:13,04/08/2016 12:13,NA,decheni,Archegosaurus,28828,n. sp.,298.9,295.5,Asselian,,NA,DE,Archegosaurus decheni
1338891,occ,NA,,180861,members,Archegosaurus decheni,species,255841,,Archegosaurus decheni,NA,species,255841,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37058,NA,NA,NA,,7.746577,49.44294,Kaiserslautern,NA,,DE,Rhineland-Palatinate,,based on nearby landmark,6,small collection,"Lat long based on the centre of Kaiserslautern, Rhineland-Palatinate, Germany",gp_mid,19.85,4.87,305,DE,,Mesienheim,,,bed,,Odernheim beds,Odernheim beds,,Saar Nahe Basin,Saar Nahe Basin,NA,,,not reported,,,,,,,,,,fluvial-lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Archegosaurus,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 12:24,04/08/2016 12:24,NA,decheni,Archegosaurus,28828,,298.9,295,Autunian,,NA,DE,Archegosaurus decheni
1338892,occ,NA,,180865,members,cf. Archegosaurus decheni,species,255841,,Archegosaurus decheni,NA,species,255841,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37058,NA,NA,NA,,7.390728,49.496632,Huffler,NA,H_fer,DE,Rhineland-Palatinate,Kusel,based on nearby landmark,6,small collection,"Lat long based on the centre of H_fer, Rhineland-Palatinate, Germany",gp_mid,19.61,4.86,315,DE,,Mesienheim,,,bed,,Odernheim beds,Odernheim beds,,Saar Nahe Basin,Saar Nahe Basin,NA,,,not reported,,,,,,,,,,fluvial-lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Archegosaurus,cf.,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,04/08/2016 12:26,04/08/2016 12:26,NA,decheni,Archegosaurus,28828,,298.9,295,Autunian,,NA,DE,Archegosaurus decheni
1338897,occ,NA,,27263,,Kashmirosaurus ornatus,species,345882,,Kashmirosaurus ornatus,NA,species,345879,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Archegosauridae,37057,345877,NA,NA,NA,,74.908333,34.041668,Risin Spur (Gangamopteris Shales),NA,Lower Gondwanan series,IN,Kashmir,,based on nearby landmark,seconds,,"specimens were collected ""..on Risin Spur near Zewan Village..""",gp_mid,61.41,-55.08,501,IN,,,,,,,,,,,,NA,"""collected from the Lower Permian Gangamopteris shales (glassy volcanic tuff) of the Lower Gondwana series"". Age previously given as Rotliegendes but Gangamopteris shales correlated with Eurydesma-bearing beds at Manendragarh and the Salt Range, suggesting an Asselian-Sakmarian age.","""shales (glassy volcanic tuff)""","""shale""",tuffaceous,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,mold/impression",medium,,,,,,,,,NA,,"Specimen is in a slab. Much of the specimen is preserved as an impression. Bones, where preserved, are of ""a reddish crumbly material, mixed with matrix.""",taxonomic,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Kashmirosaurus,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,05/08/2016 04:24,05/08/2016 04:24,7535,ornatus,Kashmirosaurus,28828,,298.9,290.1,Asselian,Sakmarian,NA,IN,Kashmirosaurus ornatus
1338898,occ,NA,,27263,,Archegosaurus n. sp. kashmiriensis,species,345883,subjective synonym of,Kashmirosaurus ornatus,NA,species,345879,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Archegosauridae,37057,345877,NA,NA,NA,,74.908333,34.041668,Risin Spur (Gangamopteris Shales),NA,Lower Gondwanan series,IN,Kashmir,,based on nearby landmark,seconds,,"specimens were collected ""..on Risin Spur near Zewan Village..""",gp_mid,61.41,-55.08,501,IN,,,,,,,,,,,,NA,"""collected from the Lower Permian Gangamopteris shales (glassy volcanic tuff) of the Lower Gondwana series"". Age previously given as Rotliegendes but Gangamopteris shales correlated with Eurydesma-bearing beds at Manendragarh and the Salt Range, suggesting an Asselian-Sakmarian age.","""shales (glassy volcanic tuff)""","""shale""",tuffaceous,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,mold/impression",medium,,,,,,,,,NA,,"Specimen is in a slab. Much of the specimen is preserved as an impression. Bones, where preserved, are of ""a reddish crumbly material, mixed with matrix.""",taxonomic,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Archegosaurus,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,05/08/2016 04:33,05/08/2016 04:33,7535,kashmiriensis,Kashmirosaurus,28828,n. sp.,298.9,290.1,Asselian,Sakmarian,NA,IN,Kashmirosaurus kashmiriensis
1338900,occ,NA,R,180796,members,Cheliderpeton latirostre,species,345886,recombined as,Glanochthon latirostris,NA,species,345885,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,255230,NA,NA,NA,,7.442166,49.573666,Erdesbach (H̦lle),NA,Holle near Erdesbach,DE,Rhineland-Palatinate,Kusel district,based on nearby landmark,6,small collection,"Cooridnates based on the centre of Erdesbach, a municipality in the Kusel district in Rhineland-Palatinate, Germany.",gp_mid,19.63,4.95,315,DE,,Meisenheim,,M7,group of beds,,,,,Saar Nahe,Saar Nahe,NA,,,not reported,,,,,,,,,,lacustrine - small,,"""Small lake deposit""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,all macrofossils,,,,,,GPIM Collection,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Cheliderpeton,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,327,R. Butler,E. Dunne,R. Butler,05/08/2016 05:27,08/08/2016 10:05,NA,latirostre,Glanochthon,28828,,298.9,295.5,Asselian,,NA,DE,Glanochthon latirostre
1338900,occ,32669,,180796,members,Glanochthon angusta,species,255231,,Glanochthon angusta,NA,species,255231,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,255230,NA,NA,NA,,7.442166,49.573666,Erdesbach (H̦lle),NA,Holle near Erdesbach,DE,Rhineland-Palatinate,Kusel district,based on nearby landmark,6,small collection,"Cooridnates based on the centre of Erdesbach, a municipality in the Kusel district in Rhineland-Palatinate, Germany.",gp_mid,19.63,4.95,315,DE,,Meisenheim,,M7,group of beds,,,,,Saar Nahe,Saar Nahe,NA,,,not reported,,,,,,,,,,lacustrine - small,,"""Small lake deposit""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,all macrofossils,,,,,,GPIM Collection,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Glanochthon,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. The temnospondyl Glanochthon from the Lower Permian Meisenheim Formation of Germany. Special Papers in Palaeontology 81:121-136,327,327,0,R. Butler,R. Butler,,05/08/2016 06:35,05/08/2016 06:35,NA,angusta,Glanochthon,60064,,298.9,295.5,Asselian,,NA,DE,Glanochthon angusta
1338901,occ,NA,,180869,members,Archegosaurus n. sp. latirostris,species,345885,recombined as,Glanochthon latirostris,NA,species,345885,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,255230,NA,NA,NA,,7.689722,49.734436,"Quarry at Rummelbach, Gresaubach",NA,,DE,Saarland,,based on nearby landmark,6,small collection,"Lat long based on the residential area of Gresaubach, in Saarland, Germany.",gp_mid,19.75,5.14,315,DE,,Lauterecken-Odernheim,,L10,group of beds,,,,,Saar Nahe,Saar Nahe,NA,Humberg-Schwarzschiefer Bank,,not reported,,,,,,,,,,fluvial-lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Archegosaurus,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,327,R. Butler,E. Dunne,R. Butler,05/08/2016 05:36,12/08/2016 05:39,NA,latirostris,Glanochthon,28828,n. sp.,298.9,295,Autunian,,NA,DE,Glanochthon latirostris
1338902,occ,NA,R,180870,members,Cheliderpeton latirostre,species,345886,recombined as,Glanochthon latirostris,NA,species,345885,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,255230,NA,NA,NA,,7.453431,49.597427,Rathsweiler,NA,,DE,Rhineland-Palatinate,Kusel district,based on nearby landmark,6,small collection,"Cooridnates based on the centre of Rathsweiler, a municipality in the Kusel district in Rhineland-Palatinate, Germany.",gp_mid,19.63,4.97,315,DE,,Meisenheim,,M7,bed,,,,,Saar Nahe,Saar Nahe,NA,,,not reported,,,,,,,,,,lacustrine - small,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,all macrofossils,,,,,,GPIM Collection,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Cheliderpeton,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,05/08/2016 05:40,05/08/2016 05:40,NA,latirostre,Glanochthon,28828,,298.9,295,Autunian,,NA,DE,Glanochthon latirostre
1338902,occ,32668,,180870,members,Glanochthon angusta,species,255231,,Glanochthon angusta,NA,species,255231,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,255230,NA,NA,NA,,7.453431,49.597427,Rathsweiler,NA,,DE,Rhineland-Palatinate,Kusel district,based on nearby landmark,6,small collection,"Cooridnates based on the centre of Rathsweiler, a municipality in the Kusel district in Rhineland-Palatinate, Germany.",gp_mid,19.63,4.97,315,DE,,Meisenheim,,M7,bed,,,,,Saar Nahe,Saar Nahe,NA,,,not reported,,,,,,,,,,lacustrine - small,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,all macrofossils,,,,,,GPIM Collection,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Glanochthon,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. The temnospondyl Glanochthon from the Lower Permian Meisenheim Formation of Germany. Special Papers in Palaeontology 81:121-136,327,327,0,R. Butler,R. Butler,,05/08/2016 06:32,05/08/2016 06:32,NA,angusta,Glanochthon,60064,,298.9,295,Autunian,,NA,DE,Glanochthon angusta
1338909,occ,NA,,180800,members,Glanochthon n. sp. angusta,species,255231,,Glanochthon angusta,NA,species,255231,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,255230,NA,NA,NA,,7.701944,49.761665,Odernheim,NA,Odernheimer Kalkbank,DE,Rhineland-Palatine,Bad Kreuznach,based on nearby landmark,seconds,small collection,"Coordinates based on location south of Obernheim am Glan, a town in Rhineland-Palatine, Germany.",gp_mid,19.86,5.33,315,DE,,Meisenheim,,,group of beds,,Obernheim beds,Obernheimer Kalkbank,,,,NA,"Meisenheim Formation (M8), Saar-Nahe Basin, Germany\r\nObernheimer Kalkbank (""limestone bank"")",,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Glanochthon,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. The temnospondyl Glanochthon from the Lower Permian Meisenheim Formation of Germany. Special Papers in Palaeontology 81:121-136,327,697,0,R. Butler,E. Dunne,,05/08/2016 06:43,05/08/2016 06:43,NA,angusta,Glanochthon,60064,n. sp.,298.9,290.1,Asselian,Sakmarian,NA,DE,Glanochthon angusta
1338910,occ,NA,,180860,members,Glanochthon angusta,species,255231,,Glanochthon angusta,NA,species,255231,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,255230,NA,NA,NA,,7.689722,49.734436,Gresaubach,NA,,DE,Saarland,,based on nearby landmark,6,small collection,"Lat long based on the residential area of Gresaubach, in Saarland, Germany.",gp_mid,19.75,5.14,315,DE,,Meisenheim,,M10,group of beds,,,,,,,NA,Stratgraphy here based on K̦niger et al. (2002),,not reported,,,,,,,,,,fluvial-lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Glanochthon,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. The temnospondyl Glanochthon from the Lower Permian Meisenheim Formation of Germany. Special Papers in Palaeontology 81:121-136,327,697,0,R. Butler,E. Dunne,,05/08/2016 06:43,05/08/2016 06:43,NA,angusta,Glanochthon,60064,,298.9,295.5,Asselian,,NA,DE,Glanochthon angusta
1338912,occ,NA,,180872,members,Glanochthon angusta,species,255231,,Glanochthon angusta,NA,species,255231,Schoch and Witzmann,2009,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,255230,NA,NA,NA,,7.67016,49.556805,Worsbach,NA,W̦rsbach,DE,Rhineland-Palatinate,,based on nearby landmark,6,small collection,"Locality lies in the Saar-Nahe district, south of Niederkirchen.",gp_mid,19.78,4.97,315,DE,,Meisenheim,Rotliegend,M6,member,,,,,,,NA,,"""laminated silty grey shale""","""shale""",,,,Y,,,,,,lacustrine - large,,"""deposited in a large, shallow, eutrophic lake"" - Carroll (1991)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Glanochthon,,NA,NA,vertebrate,R. R. Schoch and F. Witzmann. 2009. The temnospondyl Glanochthon from the Lower Permian Meisenheim Formation of Germany. Special Papers in Palaeontology 81:121-136,327,697,697,R. Butler,E. Dunne,E. Dunne,05/08/2016 06:59,05/08/2016 07:00,NA,angusta,Glanochthon,60064,,298.9,295.5,Asselian,,NA,DE,Glanochthon angusta
1339743,occ,NA,,80877,,n. gen. Ambedus n. sp. pusilus,species,345909,,Ambedus pusilus,NA,species,345909,Kissel and Reisz,2004,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,345908,NA,NA,NA,,-80.900002,39.724998,Clark Hill,NA,,US,Ohio,Monroe,based on political unit,seconds,,"""from Clark Hill on County Route 43 near junction with State Route, Salem Township""\r\nPolar coordinates approx. mark center of Salem Township.",gp_mid,-14.82,-2.52,101,US,,Greene,Dunkard,Niniveh Limestone,bed,,,,,,,NA,"Note: The age of the Greene Fm., wich is not well constrained, here is based on correlation chart (fig. 4) in Wellstead (1991, Bull. AMNH 209).",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ambedus,n. gen.,NA,NA,vertebrate,"R. A. Kissel and R. R. Reisz. 2004. Ambedus pusillus, new genus, new species, a small diadectid (Tetrapoda: Diadectomorpha) from the Lower Permian of Ohio, with a consideration of diadectomorph phylogeny. Annals of Carnegie Museum 73:197-212",327,697,0,R. Butler,E. Dunne,,08/08/2016 03:48,08/08/2016 03:48,27105,pusilus,Ambedus,60076,n. sp.,295.5,290.1,Sakmarian,,NA,US,Ambedus pusilus
1339744,occ,NA,,180937,members,n. gen. Desmatodon n. sp. hollandi,species,321002,,Desmatodon hollandi,NA,species,321002,Moran,1952,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37248,NA,NA,NA,,-79.77639,40.405834,Pitcairn Locailty,NA,"Locality C (Moran, 1952)",US,Pennsylvania,Allegheny,based on nearby landmark,seconds,small collection,"Lat long is for Pitcairn, Pennsylvania, US",gp_mid,-15.75,-5.63,101,US,,Red Knob,Conemaugh,,bed,,,,,,,NA,"The Pitcairn locality in Pennsylvania (Locality C of Moran, 1952) is located within the Red Knob Formation, approximately 100 m below the base of the Pittsburgh coal, near the middle of the Conemaugh Group. ",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Desmatodon,n. gen.,NA,NA,vertebrate,"W. E. Moran. 1952. Location and Stratigraphy of Known Occurrences of Fossil Tetrapods in the Upper Pennsylvanian and Permian of Pennsylvania, West Virginia, and Ohio. Annals of Carnegie Museum 33:1-45",327,697,0,R. Butler,E. Dunne,,08/08/2016 04:24,08/08/2016 04:24,NA,hollandi,Desmatodon,28677,n. sp.,305.9,303.4,Missourian,,NA,US,Desmatodon hollandi
1339745,occ,NA,,34761,,Desmatodon hollandi,species,321002,,Desmatodon hollandi,NA,species,321002,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37248,NA,NA,NA,,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Desmatodon,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,08/08/2016 04:27,08/08/2016 04:27,43845,hollandi,Desmatodon,60077,,303.4,298.9,Virgilian,,NA,US,Desmatodon hollandi
1339746,occ,NA,,34761,,Chenoprosopus milleri,species,139020,,Chenoprosopus milleri,NA,species,139020,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Cochleosauridae,36999,37000,NA,NA,NA,,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Chenoprosopus,,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,08/08/2016 04:32,08/08/2016 04:32,43845,milleri,Chenoprosopus,57795,,303.4,298.9,Virgilian,,NA,US,Chenoprosopus milleri
1339747,occ,NA,,180938,members,Desmatodon n. sp. hesperis,species,335335,,Desmatodon hesperis,NA,species,335335,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37248,NA,NA,NA,,-105.859726,38.471809,"Badger Creek, Fremont County",NA,,US,Colorado,Fremont,based on nearby landmark,6,small collection,"Lat long is for Badger Creek just outside Howard, Fremont County, Colorado, United States",gp_mid,-34.25,2.44,101,US,FED,Sangre de Cristo,,,bed,,,,,,,NA,"The recognized age of the Badger Creek locality is based on the vertebrate assemblage that it produces (Vaughn, 1969a)","The Sangre de Cristo Formation is approximately 2933 m thick (Vaughn, 1972), with the fossil-bearing site located approximately 442 m above the base of the formation, as defined by Brill (1952). ","""shale""",,,,Y,,,,,,fluvial-lacustrine indet.,,"The vertebrate remains are produced from a meter-thick, lens-shaped black shale unitdesignated as part of Interval 300۪ by Brill (1952)that is thought to represent a pond deposit, perhaps an oxbow lake that was present within the general system of the stream channels preserved within this part of the formation; in addition to the lenticular shape of the bed, the presence of palaeoniscoid fish scales and small pelecypods further suggests an aquatic origin of the deposit (Vaughn, 1972)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"With the exception of some aistopod vertebrae and osteoderms and some palatal and anterior limb elements of a small temnospondyls, the vertebrate remains are disarticulated, although they are found in close association (Vaughn, 1969a)",taxonomic,survey of museum collection,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Desmatodon,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,697,R. Butler,E. Dunne,E. Dunne,08/08/2016 04:44,08/08/2016 04:52,NA,hesperis,Desmatodon,60077,n. sp.,305.9,303.4,Missourian,,NA,US,Desmatodon hesperis
1339749,occ,NA,,180937,members,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-79.77639,40.405834,Pitcairn Locailty,NA,"Locality C (Moran, 1952)",US,Pennsylvania,Allegheny,based on nearby landmark,seconds,small collection,"Lat long is for Pitcairn, Pennsylvania, US",gp_mid,-15.75,-5.63,101,US,,Red Knob,Conemaugh,,bed,,,,,,,NA,"The Pitcairn locality in Pennsylvania (Locality C of Moran, 1952) is located within the Red Knob Formation, approximately 100 m below the base of the Pittsburgh coal, near the middle of the Conemaugh Group. ",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,08/08/2016 08:31,08/08/2016 08:31,NA,sp.,Eryops,60077,,305.9,303.4,Missourian,,NA,US,Eryops sp.
1339751,occ,NA,,180940,members,Diadectes lentus,species,346261,,Diadectes lentus,NA,species,120884,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-106.652222,36.159443,UCMP V-2844,NA,valley floor east of Loma Salazar,US,New Mexico,Rio Arriba,based on nearby landmark,seconds,small collection,See Lucas et al. (2005) for detailed map of other fossil-bearing locations in the area.,gp_mid,-34.08,4.53,101,US,FED,Cutler,,,bed,,,,,,,NA,,,"""siliciclastic""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,08/08/2016 08:46,08/08/2016 08:46,NA,lentus,Diadectes,60077,,296.4,268,Wolfcamp,,NA,US,Diadectes lentus
1339752,occ,NA,,180940,members,Chenoprosopus milleri,species,139020,,Chenoprosopus milleri,NA,species,139020,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Cochleosauridae,36999,37000,NA,NA,NA,,-106.652222,36.159443,UCMP V-2844,NA,valley floor east of Loma Salazar,US,New Mexico,Rio Arriba,based on nearby landmark,seconds,small collection,See Lucas et al. (2005) for detailed map of other fossil-bearing locations in the area.,gp_mid,-34.08,4.53,101,US,FED,Cutler,,,bed,,,,,,,NA,,,"""siliciclastic""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Chenoprosopus,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,08/08/2016 08:46,08/08/2016 08:46,NA,milleri,Chenoprosopus,60077,,296.4,268,Wolfcamp,,NA,US,Chenoprosopus milleri
1339753,occ,NA,,180940,members,Zatrachys serratus,species,255221,,Zatrachys serratus,NA,species,255221,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,,-106.652222,36.159443,UCMP V-2844,NA,valley floor east of Loma Salazar,US,New Mexico,Rio Arriba,based on nearby landmark,seconds,small collection,See Lucas et al. (2005) for detailed map of other fossil-bearing locations in the area.,gp_mid,-34.08,4.53,101,US,FED,Cutler,,,bed,,,,,,,NA,,,"""siliciclastic""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,08/08/2016 08:46,08/08/2016 08:46,NA,serratus,Zatrachys,60077,,296.4,268,Wolfcamp,,NA,US,Zatrachys serratus
1339754,occ,NA,,180940,members,Sphenacodon ferox,species,122487,,Sphenacodon ferox,NA,species,122487,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,,-106.652222,36.159443,UCMP V-2844,NA,valley floor east of Loma Salazar,US,New Mexico,Rio Arriba,based on nearby landmark,seconds,small collection,See Lucas et al. (2005) for detailed map of other fossil-bearing locations in the area.,gp_mid,-34.08,4.53,101,US,FED,Cutler,,,bed,,,,,,,NA,,,"""siliciclastic""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,CM,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,08/08/2016 08:46,08/08/2016 08:46,NA,ferox,Sphenacodon,60077,,296.4,268,Wolfcamp,,NA,US,Sphenacodon ferox
1339755,occ,NA,,180940,members,Ophiacodon mirus,species,123418,,Ophiacodon mirus,NA,species,123418,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-106.652222,36.159443,UCMP V-2844,NA,valley floor east of Loma Salazar,US,New Mexico,Rio Arriba,based on nearby landmark,seconds,small collection,See Lucas et al. (2005) for detailed map of other fossil-bearing locations in the area.,gp_mid,-34.08,4.53,101,US,FED,Cutler,,,bed,,,,,,,NA,,,"""siliciclastic""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,CM,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,08/08/2016 08:46,08/08/2016 08:46,NA,mirus,Ophiacodon,60077,,296.4,268,Wolfcamp,,NA,US,Ophiacodon mirus
1339757,occ,NA,,180940,members,Platyhystrix rugosus,species,345923,,Platyhystrix rugosus,NA,species,194929,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37034,NA,NA,NA,,-106.652222,36.159443,UCMP V-2844,NA,valley floor east of Loma Salazar,US,New Mexico,Rio Arriba,based on nearby landmark,seconds,small collection,See Lucas et al. (2005) for detailed map of other fossil-bearing locations in the area.,gp_mid,-34.08,4.53,101,US,FED,Cutler,,,bed,,,,,,,NA,,,"""siliciclastic""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Platyhystrix,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,08/08/2016 08:46,08/08/2016 08:46,NA,rugosus,Platyhystrix,60077,,296.4,268,Wolfcamp,,NA,US,Platyhystrix rugosus
1339758,occ,NA,,180940,members,Eryops grandis,species,345659,,Eryops grandis,NA,species,345657,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-106.652222,36.159443,UCMP V-2844,NA,valley floor east of Loma Salazar,US,New Mexico,Rio Arriba,based on nearby landmark,seconds,small collection,See Lucas et al. (2005) for detailed map of other fossil-bearing locations in the area.,gp_mid,-34.08,4.53,101,US,FED,Cutler,,,bed,,,,,,,NA,,,"""siliciclastic""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,08/08/2016 08:46,08/08/2016 08:46,NA,grandis,Eryops,60077,,296.4,268,Wolfcamp,,NA,US,Eryops grandis
1339765,occ,NA,,180944,members,Ctenosaurus n. sp. rugosus,species,194929,recombined as,Platyhystrix rugosus,NA,species,194929,Case,1910,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37034,NA,NA,NA,,-106.616386,36.1175,Arroyo del Agua (Cope Collection AMNH),NA,,US,New Mexico,Rio Arriba,based on nearby landmark,seconds,small collection," Lat long is for village of Arroyo del Agua, Rio Arriba County, New Mexico.",gp_mid,-34.08,4.48,101,US,FED,Cutler,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,AMNH,,,,E. D. Cope,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Ctenosaurus,,NA,NA,vertebrate,E. C. Case. 1910. New or little known reptiles and amphibians from the Permian (?) of Texas. Bulletin of the American Museum of Natural History 28:163-181,327,697,0,R. Butler,E. Dunne,,09/08/2016 05:16,09/08/2016 05:16,NA,rugosus,Platyhystrix,28729,n. sp.,296.4,268,Wolfcamp,,NA,US,Platyhystrix rugosus
1339766,occ,NA,,180945,members,n. gen. Dissorophus n. sp. multicinctus,species,255227,,Dissorophus multicinctus,NA,species,255227,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37027,NA,NA,NA,,-99.251389,33.601112,Baylor County,NA,Type locality of Dissorophus multicinctus,US,Texas,,based on nearby landmark,seconds,small collection,"Lat long is for Seymour, capital of and close to the geographical centre of Baylor County Texas. The exact location of the original site is unknown.",gp_mid,-30.51,-1.04,101,US,,,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,"""Lower Permian redbed sequence""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,AMNH,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Dissorophus,n. gen.,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,09/08/2016 05:29,09/08/2016 05:29,NA,multicinctus,Dissorophus,57795,n. sp.,298.9,272.3,Cisuralian,,NA,US,Dissorophus multicinctus
1339767,occ,NA,,28256,,cf. Zatrachys sp.,genus,37056,,Zatrachys,NA,genus,37056,Schoch and Milner,2014,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,,-99.216667,33.766666,"Coffee Creek, 34 (Arroyo Formation)",NA,"Locality 34 (Romer 1928), faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds; Locality VIIa (Romer & Price 1940); ""Labidosaurus pocket""; Coffee Creek Bonebed; West Coffee Creek; Middle Coffee Creek; East Coffee Creek",US,Texas,Baylor/Willbarger,based on nearby landmark,minutes,local area,"Collection comprises outcrops that today are at the bottom of Lake Kemp and outcrops in the northern vicinity of Lake Kemp. See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork"". Lat long is for Kemp Lake near the today's mouths of West, Middle, and East Coffee Creek.",gp_mid,-28.93,1.77,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""probably not much over 100 feet above the Lueders limestone; the lowest portion may have lain below it.."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\r\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,USNM",,,,"J. W. Kitching, P. C. Miller, E. C. Olson, C. H. Sternberg, S. W. Williston, among others","1895, 1897, 1909, 1965, 1972","Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.\r\nAdditional institutions storing material from Coffee Creek:\r\nBP (Bernard Price Institute, University of the Witwatersrand, Johannesburg, South Africa)\r\nBSP (Bayerische Staatssammlung f_r Pal_ontologie und Geologie, Munich, Germany)\r\nUMMP (University of Michigan Museum of Paleontology, Ann Arbor, MI)",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,cf.,NA,NA,vertebrate,R. R. Schoch and A. R. Milner. 2014. Handbook of Paleoherpetology Part 3A2 Temnospondyli I. ,327,697,0,R. Butler,E. Dunne,,09/08/2016 07:59,09/08/2016 07:59,17702,sp.,Zatrachys,57795,,279.3,272.3,Kungurian,,NA,US,Zatrachys sp.
1339768,occ,NA,,180946,members,Zatrachys serratus,species,255221,,Zatrachys serratus,NA,species,255221,Urban and Berman,2007,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,,-80.569092,40.064594,Road cut at intersection of Dallas Pike and Interstate 70,NA,Urban & Berman Locality 2,US,West Virginia,Ohio,estimated from map,6,small collection,"Lat long is for the intersection of Dallas Pike and Interstate 70, Ohio County, West Virginia. ",gp_mid,-14.25,-1.84,101,US,,Greene,Dunkard,,,,,,,,,NA,,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,"M. Urban and D. S. Berman. 2007. First occurrence of the late Paleozoic amphibian Zatrachys serratus (Temnospondyli, Zatrachydidae) in the Eastern United States. Annals of Carnegie Museum 76(3):157-164",327,697,0,R. Butler,E. Dunne,,09/08/2016 08:13,09/08/2016 08:13,NA,serratus,Zatrachys,40605,,296.4,268,Wolfcamp,,NA,US,Zatrachys serratus
1339769,occ,NA,,180947,members,Zatrachys serratus,species,255221,,Zatrachys serratus,NA,species,255221,Urban and Berman,2007,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,,-80.569092,40.064594,Road cut on County Highway 41/8,NA,Urban & Berman Locality 3,US,West Virginia,Ohio,estimated from map,6,small collection,"Lat long is for the area , 0.1 mi east of the intersection of Dallas Pike and Interstate 70, Ohio County, West Virginia. ",gp_mid,-14.25,-1.84,101,US,,Greene,Dunkard,Upper Dallas,,,,,,,,NA,,,"""limestone""",,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,"M. Urban and D. S. Berman. 2007. First occurrence of the late Paleozoic amphibian Zatrachys serratus (Temnospondyli, Zatrachydidae) in the Eastern United States. Annals of Carnegie Museum 76(3):157-164",327,697,0,R. Butler,E. Dunne,,09/08/2016 08:16,09/08/2016 08:16,NA,serratus,Zatrachys,40605,,296.4,268,Wolfcamp,,NA,US,Zatrachys serratus
1339770,occ,NA,,77786,,Limnoscelis n. sp. dynatis,species,115315,,Limnoscelis dynatis,NA,species,115315,Wideman et al.,2005,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Limnoscelidae,37231,37232,NA,NA,NA,,-105.852776,38.486942,Howard Quarry,NA,,US,Colorado,Fremont,,seconds,,,gp_mid,-34.24,2.45,101,US,FED,Sangre de Cristo,,,,,,,,,,NA,"""Late Pennsylvanian, probably Missourian, in age"" Berman & Sumida (1990)","""Quarry in a 2-3 ft thick black shale in the Sangre de Cristo Formation, near the town of Howard in the Arkansas River avalley, Freemont, Colorado (see Vaughn 1969, 1972)"" (Berman and Sumida 1990)","""shale""",black,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,biostratigraphic,"selective quarrying,mechanical,survey of museum collection",CM,,1 individuals,,Peter P. Vaughn,"1969, 1972",,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Limnoscelis,,NA,NA,vertebrate,"N. K. Wideman, S. S. Sumida, and M. O.'Neil. 2005. A Reassessment of the Taxonomic Status of the Materials Assigned to the Early Permian Tetrapod Genera Limnosceloides and Limnoscelops. In S. G. Lucas & K. E. Zeigler (ed.), The Nonmarine Permian. New Mexico Museum of Natural History and Science Bulletin 30:358-362",327,697,0,R. Butler,E. Dunne,,09/08/2016 10:44,09/08/2016 10:44,26271,dynatis,Limnoscelis,29241,n. sp.,305.9,303.4,Missourian,,NA,US,Limnoscelis dynatis
1339782,occ,NA,,180950,members,n. gen. Phanerosaurus n. sp. naumanni,species,321004,,Phanerosaurus naumanni,NA,species,321004,Meyer,1860,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,321003,NA,NA,NA,,12.495,50.71611,"Ergebirge Basin, near Zwickau",NA,,DE,Saxony,,based on nearby landmark,seconds,small collection,"Lat long is for the town of Zwickau, in Saxony, Germany.",gp_mid,22.46,6.91,305,DE,,Leukersdorf,,,,,,,,,,NA,Stratigraphy for Leukersdorf Formation obtained from R̦ler & Noll (2006) Rev. Palaeobot. Palynol.: 140,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Phanerosaurus,n. gen.,NA,NA,vertebrate,H. v. Meyer. 1860. Phanerosaurus naumanni aus dem Sandstein des Rothliegenden in Deutschland. Paleontographica 7:248-252,327,697,0,R. Butler,E. Dunne,,10/08/2016 06:28,10/08/2016 06:28,NA,naumanni,Phanerosaurus,60082,n. sp.,298.9,295.5,Asselian,,NA,DE,Phanerosaurus naumanni
1339786,occ,NA,,52522,,Phanerosaurus n. sp. pugnax,species,321005,recombined as,Stephanospondylus pugnax,NA,species,321005,Geinitz and Deichm_ller,1882,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37249,NA,NA,NA,,13.650278,50.999722,Niederhaslich,NA,Niederh_sslich; Niederh_slich; Nieder-H_sslich; Plauenscher Grund; D̦hlen Basin,DE,Saxony,Weieritzkreis,based on nearby landmark,seconds,outcrop,"Niederh_slich in the D̦hlen basin, today it is one part of the City of Freital, SW of Dresden in Sachsen; the outcrop does not exist anymore.",gp_mid,23.3,7.73,305,DE,,Niederh_slich-Schweinsdorf,Rotliegend,Niederh_slich limestone,member,,,,,,,NA,"""The Niederh_slich Formation belongs stratigraphically [...] to the Melanerpeton gracile-M. pulcherimus Zone, i. e. uppermost Unterrotliegend"" (U. Hoffman, 2002, Workshop _Oberkarbon - Untertrias in Zentraleuropa: Prozesse und ihr Timing [online] http://www.geo.tu-freiberg.de/palaeo/GeoTage-2002.pdf) (TL);\r\nthe Niederh_slich limestone is Asselian according to assorted references, e.g., Gebhardt and Schneider 1993 (JA)\r\nAccording to Roscher & Schneider (2006, in Lucas et al. (eds), Geol. Soc. Spec. Publ. 265) the Niederh_slich Fm. is Sakmarian in age (TL).",,"""limestone""",,,,,,,,,,lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Museum: Staatliches Museum f_r Mineralogie und Geologie, Dresden (SMMGD)",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Phanerosaurus,,NA,NA,vertebrate,H. B. Geinitz and J. V. Deichm_ller. 1882. Die Saurier der unteren Dyas von Sachsen [Saurians from the Lower Dyas of Saxony]. Palaeontographica 9:1-46,327,697,0,R. Butler,E. Dunne,,10/08/2016 06:52,10/08/2016 06:52,14125,pugnax,Stephanospondylus,60084,n. sp.,295.5,290.1,Sakmarian,,NA,DE,Stephanospondylus pugnax
1339822,occ,NA,,180957,members,Diadectes sideropelicus,species,320982,,Diadectes sideropelicus,NA,species,320982,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-98.650002,33.583332,Archer City Bonebed 2,NA,,US,Texas,Archer,estimated from map,minutes,local area,About one mile southwest of Archer City.,gp_mid,-30.06,-1.27,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 08:26,10/08/2016 08:26,NA,sideropelicus,Diadectes,60077,,296.4,268,Wolfcamp,,NA,US,Diadectes sideropelicus
1339828,occ,NA,,180938,members,Trihecaton howardinus,species,320818,,Trihecaton howardinus,NA,species,320818,Kissel,2010,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Trihecatontidae,37305,37306,NA,NA,NA,,-105.859726,38.471809,"Badger Creek, Fremont County",NA,,US,Colorado,Fremont,based on nearby landmark,6,small collection,"Lat long is for Badger Creek just outside Howard, Fremont County, Colorado, United States",gp_mid,-34.25,2.44,101,US,FED,Sangre de Cristo,,,bed,,,,,,,NA,"The recognized age of the Badger Creek locality is based on the vertebrate assemblage that it produces (Vaughn, 1969a)","The Sangre de Cristo Formation is approximately 2933 m thick (Vaughn, 1972), with the fossil-bearing site located approximately 442 m above the base of the formation, as defined by Brill (1952). ","""shale""",,,,Y,,,,,,fluvial-lacustrine indet.,,"The vertebrate remains are produced from a meter-thick, lens-shaped black shale unitdesignated as part of Interval 300۪ by Brill (1952)that is thought to represent a pond deposit, perhaps an oxbow lake that was present within the general system of the stream channels preserved within this part of the formation; in addition to the lenticular shape of the bed, the presence of palaeoniscoid fish scales and small pelecypods further suggests an aquatic origin of the deposit (Vaughn, 1972)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"With the exception of some aistopod vertebrae and osteoderms and some palatal and anterior limb elements of a small temnospondyls, the vertebrate remains are disarticulated, although they are found in close association (Vaughn, 1969a)",taxonomic,survey of museum collection,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Trihecaton,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,697,R. Butler,E. Dunne,E. Dunne,10/08/2016 08:37,10/08/2016 08:38,NA,howardinus,Trihecaton,60077,,305.9,303.4,Missourian,,NA,US,Trihecaton howardinus
1339829,occ,NA,,180938,members,Limnoscelis dynatis,species,115315,,Limnoscelis dynatis,NA,species,115315,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Limnoscelidae,37231,37232,NA,NA,NA,,-105.859726,38.471809,"Badger Creek, Fremont County",NA,,US,Colorado,Fremont,based on nearby landmark,6,small collection,"Lat long is for Badger Creek just outside Howard, Fremont County, Colorado, United States",gp_mid,-34.25,2.44,101,US,FED,Sangre de Cristo,,,bed,,,,,,,NA,"The recognized age of the Badger Creek locality is based on the vertebrate assemblage that it produces (Vaughn, 1969a)","The Sangre de Cristo Formation is approximately 2933 m thick (Vaughn, 1972), with the fossil-bearing site located approximately 442 m above the base of the formation, as defined by Brill (1952). ","""shale""",,,,Y,,,,,,fluvial-lacustrine indet.,,"The vertebrate remains are produced from a meter-thick, lens-shaped black shale unitdesignated as part of Interval 300۪ by Brill (1952)that is thought to represent a pond deposit, perhaps an oxbow lake that was present within the general system of the stream channels preserved within this part of the formation; in addition to the lenticular shape of the bed, the presence of palaeoniscoid fish scales and small pelecypods further suggests an aquatic origin of the deposit (Vaughn, 1972)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"With the exception of some aistopod vertebrae and osteoderms and some palatal and anterior limb elements of a small temnospondyls, the vertebrate remains are disarticulated, although they are found in close association (Vaughn, 1969a)",taxonomic,survey of museum collection,CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Limnoscelis,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,697,R. Butler,E. Dunne,E. Dunne,10/08/2016 08:37,10/08/2016 08:38,NA,dynatis,Limnoscelis,60077,,305.9,303.4,Missourian,,NA,US,Limnoscelis dynatis
1339830,occ,NA,,180938,members,Ianthasaurus sp.,genus,38912,,Ianthasaurus,NA,genus,38912,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38912,NA,NA,NA,,-105.859726,38.471809,"Badger Creek, Fremont County",NA,,US,Colorado,Fremont,based on nearby landmark,6,small collection,"Lat long is for Badger Creek just outside Howard, Fremont County, Colorado, United States",gp_mid,-34.25,2.44,101,US,FED,Sangre de Cristo,,,bed,,,,,,,NA,"The recognized age of the Badger Creek locality is based on the vertebrate assemblage that it produces (Vaughn, 1969a)","The Sangre de Cristo Formation is approximately 2933 m thick (Vaughn, 1972), with the fossil-bearing site located approximately 442 m above the base of the formation, as defined by Brill (1952). ","""shale""",,,,Y,,,,,,fluvial-lacustrine indet.,,"The vertebrate remains are produced from a meter-thick, lens-shaped black shale unitdesignated as part of Interval 300۪ by Brill (1952)that is thought to represent a pond deposit, perhaps an oxbow lake that was present within the general system of the stream channels preserved within this part of the formation; in addition to the lenticular shape of the bed, the presence of palaeoniscoid fish scales and small pelecypods further suggests an aquatic origin of the deposit (Vaughn, 1972)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,"With the exception of some aistopod vertebrae and osteoderms and some palatal and anterior limb elements of a small temnospondyls, the vertebrate remains are disarticulated, although they are found in close association (Vaughn, 1969a)",taxonomic,survey of museum collection,CM,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ianthasaurus,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 08:37,10/08/2016 08:37,NA,sp.,Ianthasaurus,60077,,305.9,303.4,Missourian,,NA,US,Ianthasaurus sp.
1339837,occ,NA,,80784,,Xyrospondylus ecordi,species,138230,,Xyrospondylus ecordi,NA,species,138229,Kissel,2010,Chordata,33815,Osteichthyes,34881,Pelycosauria,38883,,NA,38934,NA,NA,NA,,-95.259048,38.378502,Garnett Quarry,NA,"Garnett Vertebrate Fauna, Charles Hardesty farm",US,Kansas,Anderson,estimated from map,6,outcrop,"""6 miles northwest of Garnett"" (Reisz, 1986); ""NW 1/4, NE 1/4, sec. 5, tp. 20 S, rge. 19 E, Putnam Township, Anderson County, Kansas"" (Reisz & Berman, 1986)\r\n""Charles A. Hardest farm, NW/4 NE/4 sec. 5 T20S R19E, Putnam Township, Anderson County, Kansas. The Universal Transverse Mercantor (UTM) coordinates of the quarry are 15STN963466. Locality is close to Garnett, Kansas."" (Laurin 1993). ",gp_mid,-27.44,-2.3,101,US,,Stanton,Lansing,Rock Lake Shale,group of beds,,,,,,,NA,"""Rock Lake Member, Stanton Formation, Lansing Group, Missourian Series, Upper Pennsylvanian"" (Reisz & Berman, 1996)\r\nall vertebrate remains seem to come exclusively from the basal part of the Rock Lake Shale (see Reisz et al., 1982)","""dark greyishbrown, moderately well bedded, very carbonaceous, calcareous mudstone"" (Reisz et al., 1982)",mudstone,brown,,"calcareous,carbonaceous",Y,,,,,,fine channel fill,foreland basin,"""The Rock Lake Shale is a rather thin but otherwise typical ۪outside۪ shale of a ۪Kansas Megacyclothem۪ sequence formed as a change from regressive to transgressive conditions occurred [...] The site is located along the western edge of what was, during the Late Pennsylvanian, a shallow, forested stream valley or channel that was eroded into a limestone coastal plain during the latter stages of a major eustatic fall in sea level. As the succeeding rise in sea level occurred, the valley was gradually flooded by estuarine waters"" (Reisz et al., 1982).\r\nSequence stratigraphy is interpreted from the description given by Reisz et al. (1982). The surface of the underlying limestone is the sequence boundary merged with the transgressive surface and the Lake Rock Shale is the basalmost deposit of the transgressive systems tract.",macrofossils,some,some,,,,NA,,body,good,,snapshot,,,,,,,NA,,,taxonomic,"bulk,mechanical",ROM,,,,"F. E. Peabody, R. Camp, R. L. Carroll, R. R. Reisz, M. J. Heaton, B. R. Pynn, G. MacDonald","1953-1956, 1965, 1980, 1981",,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Xyrospondylus,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 08:43,10/08/2016 08:43,28862,ecordi,Xyrospondylus,60077,,305.9,303.4,Missourian,,NA,US,Xyrospondylus ecordi
1339841,occ,NA,,126535,,cf. Saurerpeton obtusum,species,137431,recombined as,Isodectes obtusus,NA,species,137370,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Saurerpetontidae,36980,36983,NA,NA,NA,,-79.966667,40.444443,Soho Street Quarry,NA,Locality 1 of Moran (1952),US,Pennsylvania,Allegheny,estimated from map,seconds,,"Location details given by Wellstead (1991): ""a quarry on east side of Soho Street, approximately 0.25km north of Fifth Avenue, Pittsburgh, Allegheny County Pennsylvania. The site is now covered by a housing development.""",gp_mid,-15.23,-4.42,101,US,,,Conemaugh,,bed,,,,,,,NA,"""Freshwater limestone bed within the Pittsburgh Limestone, lying 12m below the base of the Conemaugh Group, Upper Pennsylvanian (=Stephanian)"" (Wellstead, 1991)",,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,"CM,MCZ",,,,Burke party,1936,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Saurerpeton,cf.,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 08:47,10/08/2016 08:47,41027,obtusum,Isodectes,60077,,306.95,298.9,Stephanian,,NA,US,Isodectes obtusum
1339842,occ,NA,,126535,,Eryops avinoffi,species,37011,species not entered,Eryops,NA,genus,37011,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-79.966667,40.444443,Soho Street Quarry,NA,Locality 1 of Moran (1952),US,Pennsylvania,Allegheny,estimated from map,seconds,,"Location details given by Wellstead (1991): ""a quarry on east side of Soho Street, approximately 0.25km north of Fifth Avenue, Pittsburgh, Allegheny County Pennsylvania. The site is now covered by a housing development.""",gp_mid,-15.23,-4.42,101,US,,,Conemaugh,,bed,,,,,,,NA,"""Freshwater limestone bed within the Pittsburgh Limestone, lying 12m below the base of the Conemaugh Group, Upper Pennsylvanian (=Stephanian)"" (Wellstead, 1991)",,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,"CM,MCZ",,,,Burke party,1936,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 08:47,10/08/2016 08:47,41027,avinoffi,Eryops,60077,,306.95,298.9,Stephanian,,NA,US,Eryops avinoffi
1339843,occ,NA,,126535,,Megamolgophis agostinii,species,37323,species not entered,Megamolgophis,NA,genus,37323,Kissel,2010,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37323,NA,NA,NA,,-79.966667,40.444443,Soho Street Quarry,NA,Locality 1 of Moran (1952),US,Pennsylvania,Allegheny,estimated from map,seconds,,"Location details given by Wellstead (1991): ""a quarry on east side of Soho Street, approximately 0.25km north of Fifth Avenue, Pittsburgh, Allegheny County Pennsylvania. The site is now covered by a housing development.""",gp_mid,-15.23,-4.42,101,US,,,Conemaugh,,bed,,,,,,,NA,"""Freshwater limestone bed within the Pittsburgh Limestone, lying 12m below the base of the Conemaugh Group, Upper Pennsylvanian (=Stephanian)"" (Wellstead, 1991)",,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,"CM,MCZ",,,,Burke party,1936,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Megamolgophis,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 08:47,10/08/2016 08:47,41027,agostinii,Megamolgophis,60077,,306.95,298.9,Stephanian,,NA,US,Megamolgophis agostinii
1339844,occ,NA,,126535,,cf. Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Kissel,2010,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-79.966667,40.444443,Soho Street Quarry,NA,Locality 1 of Moran (1952),US,Pennsylvania,Allegheny,estimated from map,seconds,,"Location details given by Wellstead (1991): ""a quarry on east side of Soho Street, approximately 0.25km north of Fifth Avenue, Pittsburgh, Allegheny County Pennsylvania. The site is now covered by a housing development.""",gp_mid,-15.23,-4.42,101,US,,,Conemaugh,,bed,,,,,,,NA,"""Freshwater limestone bed within the Pittsburgh Limestone, lying 12m below the base of the Conemaugh Group, Upper Pennsylvanian (=Stephanian)"" (Wellstead, 1991)",,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,"CM,MCZ",,,,Burke party,1936,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,cf.,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 08:47,10/08/2016 08:47,41027,sp.,Diplocaulus,60077,,306.95,298.9,Stephanian,,NA,US,Diplocaulus sp.
1339856,occ,NA,,180633,members,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Kissel,2010,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,individuals,-95.41037,39.817047,"Robinson Locality, Brown County",NA,Bern Limestone,US,Kansas,Brown,based on nearby landmark,6,small collection,"Coordinates are for the centre of Robinson, a city in Brown County, Kansas, United States. Locality lies just northeast of the town of Robinson.",gp_mid,-25.51,1.2,101,US,,Bern Limestone,Wabaunsee,Soldier Creek Shale,group of beds,,,,,,,NA,Bern Limestone,The fossiliferous horizon is composed almost entirely of densely packed stromatolites that lie between two shales.,"""shale""",,,,Y,,,,,,lagoonal,,"Although it has been suggested that shallow marine conditions existed at the site during time of deposition, it has also been argued that the cyanobacteria of the stromatolites grew in an environment of mixed fresh and marine water, either a lagoon or a bay (Foreman and Martin, 1988)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,"Like the Middle Virgilian Hamilton fauna, the Robinson fauna is dominated by aquatic taxa, with only a few specimens of terrestrial forms present.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,697,R. Butler,E. Dunne,E. Dunne,10/08/2016 09:28,07/09/2016 03:45,NA,sp.,Diplocaulus,60077,,303.4,298.9,Virgilian,,1,US,Diplocaulus sp.
1339893,occ,NA,,34761,,Platyhystrix rugosus,species,345923,,Platyhystrix rugosus,NA,species,194929,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37034,NA,NA,NA,,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Platyhystrix,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 09:43,10/08/2016 09:43,43845,rugosus,Platyhystrix,60077,,303.4,298.9,Virgilian,,NA,US,Platyhystrix rugosus
1339894,occ,NA,,34761,,aff. Desmatodon hollandi ?,species,321002,,Desmatodon hollandi,NA,species,321002,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37248,NA,NA,NA,,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Desmatodon,aff.,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 09:43,10/08/2016 09:43,43845,hollandi,Desmatodon,60077,?,303.4,298.9,Virgilian,,NA,US,Desmatodon hollandi
1339895,occ,NA,,34761,,Ophiacodon navajovicus,species,122334,,Ophiacodon navajovicus,NA,species,54987,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 09:43,10/08/2016 09:43,43845,navajovicus,Ophiacodon,60077,,303.4,298.9,Virgilian,,NA,US,Ophiacodon navajovicus
1339896,occ,NA,,34761,,Aerosaurus greenlorum,species,38893,species not entered,Aerosaurus,NA,genus,38893,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Varanopidae,95329,38893,NA,NA,NA,,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Aerosaurus,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 09:43,10/08/2016 09:43,43845,greenlorum,Aerosaurus,60077,,303.4,298.9,Virgilian,,NA,US,Aerosaurus greenlorum
1339897,occ,NA,,34761,,cf. Edaphosaurus novomexicanus,species,122351,,Edaphosaurus novomexicanus,NA,species,122351,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,cf.,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 09:43,10/08/2016 09:43,43845,novomexicanus,Edaphosaurus,60077,,303.4,298.9,Virgilian,,NA,US,Edaphosaurus novomexicanus
1339898,occ,NA,,34761,,Sphenacodon ferox,species,122487,,Sphenacodon ferox,NA,species,122487,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 09:43,10/08/2016 09:43,43845,ferox,Sphenacodon,60077,,303.4,298.9,Virgilian,,NA,US,Sphenacodon ferox
1339901,occ,NA,,177058,members,Edops sp.,genus,37005,,Edops,NA,genus,37005,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Edopidae,37004,37005,NA,NA,NA,,-80.657288,40.04414,Elm Grove,NA,,US,West Virginia,Ohio,estimated from map,6,small collection,"Coordinates based on Elm Grove, within Wheeling city limits in Ohio County, West Virginia, United States. The Elm Grove locality is found along a road cut on Interstate Highway 70, near the town of Elm Grove.",gp_mid,-15.22,-3.49,101,US,,Pittsburgh,Monongahela,"Monongahela ""B"" freshwater Limestone",bed,,,,,,,NA,"Stratigraphy originally recorded as ""Stephanian"" (Carroll et al., 1998). Update: The Pittsburgh Fm. is the lower unit of the Monongahela Group and is entirely within the Virgilian (see, e.g. Eble et al., 2006, pp. 197-222 in GSA Spec. Pap. 399) . \r\n""The fossiliferous horizon is Limestone B of the Pittsburgh Formation of the Monongahela Group (Berman, 1979), which is considered Virgilian in age (Berman et al., 1997)."" Kissel (2010)",,"""limestone""",,,,,,,,,,fluvial indet.,foreland basin,"The deposit preserved at the Elm Grove locality is interpreted as a meander cutoff channel that filled very slowly (Lund, 1972).",macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,"selective quarrying,surface (in situ),mechanical,field collection,survey of museum collection",CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Edops,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 09:57,10/08/2016 09:57,NA,sp.,Edops,60077,,303.4,298.9,Virgilian,,NA,US,Edops sp.
1339902,occ,NA,,177058,members,Diploceraspis burkei,species,227035,,Diploceraspis burkei,NA,species,227035,Kissel,2010,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37265,NA,NA,NA,,-80.657288,40.04414,Elm Grove,NA,,US,West Virginia,Ohio,estimated from map,6,small collection,"Coordinates based on Elm Grove, within Wheeling city limits in Ohio County, West Virginia, United States. The Elm Grove locality is found along a road cut on Interstate Highway 70, near the town of Elm Grove.",gp_mid,-15.22,-3.49,101,US,,Pittsburgh,Monongahela,"Monongahela ""B"" freshwater Limestone",bed,,,,,,,NA,"Stratigraphy originally recorded as ""Stephanian"" (Carroll et al., 1998). Update: The Pittsburgh Fm. is the lower unit of the Monongahela Group and is entirely within the Virgilian (see, e.g. Eble et al., 2006, pp. 197-222 in GSA Spec. Pap. 399) . \r\n""The fossiliferous horizon is Limestone B of the Pittsburgh Formation of the Monongahela Group (Berman, 1979), which is considered Virgilian in age (Berman et al., 1997)."" Kissel (2010)",,"""limestone""",,,,,,,,,,fluvial indet.,foreland basin,"The deposit preserved at the Elm Grove locality is interpreted as a meander cutoff channel that filled very slowly (Lund, 1972).",macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,"selective quarrying,surface (in situ),mechanical,field collection,survey of museum collection",CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diploceraspis,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 09:57,10/08/2016 09:57,NA,burkei,Diploceraspis,60077,,303.4,298.9,Virgilian,,NA,US,Diploceraspis burkei
1339903,occ,NA,,177058,members,Lysorophus dunkardensis,species,320833,,Lysorophus dunkardensis,NA,species,320833,Kissel,2010,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-80.657288,40.04414,Elm Grove,NA,,US,West Virginia,Ohio,estimated from map,6,small collection,"Coordinates based on Elm Grove, within Wheeling city limits in Ohio County, West Virginia, United States. The Elm Grove locality is found along a road cut on Interstate Highway 70, near the town of Elm Grove.",gp_mid,-15.22,-3.49,101,US,,Pittsburgh,Monongahela,"Monongahela ""B"" freshwater Limestone",bed,,,,,,,NA,"Stratigraphy originally recorded as ""Stephanian"" (Carroll et al., 1998). Update: The Pittsburgh Fm. is the lower unit of the Monongahela Group and is entirely within the Virgilian (see, e.g. Eble et al., 2006, pp. 197-222 in GSA Spec. Pap. 399) . \r\n""The fossiliferous horizon is Limestone B of the Pittsburgh Formation of the Monongahela Group (Berman, 1979), which is considered Virgilian in age (Berman et al., 1997)."" Kissel (2010)",,"""limestone""",,,,,,,,,,fluvial indet.,foreland basin,"The deposit preserved at the Elm Grove locality is interpreted as a meander cutoff channel that filled very slowly (Lund, 1972).",macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,"selective quarrying,surface (in situ),mechanical,field collection,survey of museum collection",CM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 09:57,10/08/2016 09:57,NA,dunkardensis,Lysorophus,60077,,303.4,298.9,Virgilian,,NA,US,Lysorophus dunkardensis
1339904,occ,NA,,177058,members,Edaphosaurus colohistion,species,122353,,Edaphosaurus colohistion,NA,species,122353,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,,-80.657288,40.04414,Elm Grove,NA,,US,West Virginia,Ohio,estimated from map,6,small collection,"Coordinates based on Elm Grove, within Wheeling city limits in Ohio County, West Virginia, United States. The Elm Grove locality is found along a road cut on Interstate Highway 70, near the town of Elm Grove.",gp_mid,-15.22,-3.49,101,US,,Pittsburgh,Monongahela,"Monongahela ""B"" freshwater Limestone",bed,,,,,,,NA,"Stratigraphy originally recorded as ""Stephanian"" (Carroll et al., 1998). Update: The Pittsburgh Fm. is the lower unit of the Monongahela Group and is entirely within the Virgilian (see, e.g. Eble et al., 2006, pp. 197-222 in GSA Spec. Pap. 399) . \r\n""The fossiliferous horizon is Limestone B of the Pittsburgh Formation of the Monongahela Group (Berman, 1979), which is considered Virgilian in age (Berman et al., 1997)."" Kissel (2010)",,"""limestone""",,,,,,,,,,fluvial indet.,foreland basin,"The deposit preserved at the Elm Grove locality is interpreted as a meander cutoff channel that filled very slowly (Lund, 1972).",macrofossils,,,,,,NA,,body,good,,,,,,,,,NA,,,taxonomic,"selective quarrying,surface (in situ),mechanical,field collection,survey of museum collection",CM,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 09:57,10/08/2016 09:57,NA,colohistion,Edaphosaurus,60077,,303.4,298.9,Virgilian,,NA,US,Edaphosaurus colohistion
1339909,occ,NA,,154179,,Naosaurus n. sp. mirabilis,species,346037,recombined as,Edaphosaurus mirabilis,NA,species,346037,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,,13.675,50.209999,"Kounov, Rakovnik District",NA,Kounova,CZ,,,based on nearby landmark,2,outcrop,"""Kounova lies some 35 miles northwest of Prague in the Rakonitz coal basin"" Romer (1945)\r\nPreviously in area known as Bohemia",gp_mid,21.74,4.64,305,CZ,,Slany,,Kounov,group of beds,,,,,,,NA,,,"""siliciclastic""",,lithified,,,,,,,,terrestrial indet.,rift,"Central-West Bohemian basin; extensional basin developed within Variscan zone along simple asymmetric mega-graben formed on the Central Bohemian and Litomerice fault zones, with some contribution from transtensional wrench faults.\r\nThe sediments at Kounova suggest deposition in the bottom of a quiet pool, and the environment seems to have been that of a coal-swamp region. (Kissel, 2010)\r\n",macrofossils,,,,,,NA,,mold/impression,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Repository: National Museum, Prague (CGH)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Naosaurus,,NA,NA,"paleoentomology,vertebrate",R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,327,697,697,R. Butler,E. Dunne,E. Dunne,10/08/2016 10:07,15/08/2016 11:32,37199,mirabilis,Edaphosaurus,27105,n. sp.,304.8,303.4,Stephanian B,,NA,CZ,Edaphosaurus mirabilis
1339910,occ,NA,,154179,,cf. Macromerion schwarzenbergii,species,38906,species not entered,Macromerion,NA,genus,38906,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38906,NA,NA,NA,,13.675,50.209999,"Kounov, Rakovnik District",NA,Kounova,CZ,,,based on nearby landmark,2,outcrop,"""Kounova lies some 35 miles northwest of Prague in the Rakonitz coal basin"" Romer (1945)\r\nPreviously in area known as Bohemia",gp_mid,21.74,4.64,305,CZ,,Slany,,Kounov,group of beds,,,,,,,NA,,,"""siliciclastic""",,lithified,,,,,,,,terrestrial indet.,rift,"Central-West Bohemian basin; extensional basin developed within Variscan zone along simple asymmetric mega-graben formed on the Central Bohemian and Litomerice fault zones, with some contribution from transtensional wrench faults.\r\nThe sediments at Kounova suggest deposition in the bottom of a quiet pool, and the environment seems to have been that of a coal-swamp region. (Kissel, 2010)\r\n",macrofossils,,,,,,NA,,mold/impression,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Repository: National Museum, Prague (CGH)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Macromerion,cf.,NA,NA,"paleoentomology,vertebrate","R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 10:07,10/08/2016 10:07,37199,schwarzenbergii,Macromerion,60077,,304.8,303.4,Stephanian B,,NA,CZ,Macromerion schwarzenbergii
1339928,occ,NA,,180974,members,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Kissel,2010,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-106.691673,35.772633,Jemez Springs,NA,,US,New Mexico,Sandoval,based on nearby landmark,6,small collection,"Lat long is for the centre of Jemez Springs, Sandoval County, New Mexico.",gp_mid,-34.33,4.24,101,US,FED,Abo,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)",siltstone,"coarse,gray",poorly lithified,,Y,sandstone,red,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 11:00,10/08/2016 11:00,NA,sp.,Diplocaulus,60077,,296.4,268,Wolfcamp,,NA,US,Diplocaulus sp.
1339929,occ,NA,,180974,members,cf. Archeria sp.,genus,37196,,Archeria,NA,genus,37196,Kissel,2010,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,,-106.691673,35.772633,Jemez Springs,NA,,US,New Mexico,Sandoval,based on nearby landmark,6,small collection,"Lat long is for the centre of Jemez Springs, Sandoval County, New Mexico.",gp_mid,-34.33,4.24,101,US,FED,Abo,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)",siltstone,"coarse,gray",poorly lithified,,Y,sandstone,red,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,cf.,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 11:00,10/08/2016 11:00,NA,sp.,Archeria,60077,,296.4,268,Wolfcamp,,NA,US,Archeria sp.
1339930,occ,NA,,180974,members,Trimerorhachis sandovalensis,species,345366,,Trimerorhachis sandovalensis,NA,species,345366,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-106.691673,35.772633,Jemez Springs,NA,,US,New Mexico,Sandoval,based on nearby landmark,6,small collection,"Lat long is for the centre of Jemez Springs, Sandoval County, New Mexico.",gp_mid,-34.33,4.24,101,US,FED,Abo,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)",siltstone,"coarse,gray",poorly lithified,,Y,sandstone,red,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 11:00,10/08/2016 11:00,NA,sandovalensis,Trimerorhachis,60077,,296.4,268,Wolfcamp,,NA,US,Trimerorhachis sandovalensis
1339931,occ,NA,,180974,members,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-106.691673,35.772633,Jemez Springs,NA,,US,New Mexico,Sandoval,based on nearby landmark,6,small collection,"Lat long is for the centre of Jemez Springs, Sandoval County, New Mexico.",gp_mid,-34.33,4.24,101,US,FED,Abo,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)",siltstone,"coarse,gray",poorly lithified,,Y,sandstone,red,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 11:00,10/08/2016 11:00,NA,sp.,Trimerorhachis,60077,,296.4,268,Wolfcamp,,NA,US,Trimerorhachis sp.
1339932,occ,NA,,180974,members,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-106.691673,35.772633,Jemez Springs,NA,,US,New Mexico,Sandoval,based on nearby landmark,6,small collection,"Lat long is for the centre of Jemez Springs, Sandoval County, New Mexico.",gp_mid,-34.33,4.24,101,US,FED,Abo,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)",siltstone,"coarse,gray",poorly lithified,,Y,sandstone,red,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 11:00,10/08/2016 11:00,NA,sp.,Eryops,60077,,296.4,268,Wolfcamp,,NA,US,Eryops sp.
1339933,occ,NA,,180974,members,Platyhystrix sp.,genus,37034,,Platyhystrix,NA,genus,37034,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37034,NA,NA,NA,,-106.691673,35.772633,Jemez Springs,NA,,US,New Mexico,Sandoval,based on nearby landmark,6,small collection,"Lat long is for the centre of Jemez Springs, Sandoval County, New Mexico.",gp_mid,-34.33,4.24,101,US,FED,Abo,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)",siltstone,"coarse,gray",poorly lithified,,Y,sandstone,red,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Platyhystrix,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 11:00,10/08/2016 11:00,NA,sp.,Platyhystrix,60077,,296.4,268,Wolfcamp,,NA,US,Platyhystrix sp.
1339934,occ,NA,,180974,members,Zatrachys sp.,genus,37056,,Zatrachys,NA,genus,37056,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,,-106.691673,35.772633,Jemez Springs,NA,,US,New Mexico,Sandoval,based on nearby landmark,6,small collection,"Lat long is for the centre of Jemez Springs, Sandoval County, New Mexico.",gp_mid,-34.33,4.24,101,US,FED,Abo,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)",siltstone,"coarse,gray",poorly lithified,,Y,sandstone,red,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 11:00,10/08/2016 11:00,NA,sp.,Zatrachys,60077,,296.4,268,Wolfcamp,,NA,US,Zatrachys sp.
1339935,occ,NA,,180974,members,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-106.691673,35.772633,Jemez Springs,NA,,US,New Mexico,Sandoval,based on nearby landmark,6,small collection,"Lat long is for the centre of Jemez Springs, Sandoval County, New Mexico.",gp_mid,-34.33,4.24,101,US,FED,Abo,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)",siltstone,"coarse,gray",poorly lithified,,Y,sandstone,red,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 11:00,10/08/2016 11:00,NA,sp.,Diadectes,60077,,296.4,268,Wolfcamp,,NA,US,Diadectes sp.
1339938,occ,NA,,180974,members,Sphenacodon sp.,genus,38909,,Sphenacodon,NA,genus,38909,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,,-106.691673,35.772633,Jemez Springs,NA,,US,New Mexico,Sandoval,based on nearby landmark,6,small collection,"Lat long is for the centre of Jemez Springs, Sandoval County, New Mexico.",gp_mid,-34.33,4.24,101,US,FED,Abo,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)",siltstone,"coarse,gray",poorly lithified,,Y,sandstone,red,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 11:01,10/08/2016 11:01,NA,sp.,Sphenacodon,60077,,296.4,268,Wolfcamp,,NA,US,Sphenacodon sp.
1339943,occ,NA,,77412,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-106.639442,36.157223,UCMP V-2814,NA,Camp Quarry,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"""southeast slope of a small butte, 410 yards south of New Mexico State Highway 96, about 940 yards southeast of the Rio Puerco bridge at Arroyo del Agua, section 8, T.22N., R.3E., Rio Arriba County, New Mexico"" (Langston, 1965 p. 6; 1966 p.691)",gp_mid,-34.09,4.48,101,US,FED,Abo/Cutler,,,group of beds,,,,,,,NA,All specimens appear to come from about the same stratigraphic level (38-36 m below top of the butte). Whether these beds are uppermost Carboniferous or lower Permian is a subject of controversy.\r\n,"""soft brick-red clayey siltstone"" (Langston, 1965 p. 6; 1966 p.691; Langston & Reisz, 1981 p. 74)",siltstone,red,,argillaceous,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,general faunal/floral,"bulk,surface (float),survey of museum collection",UCMP,all macrofossils,,,"C. L. Camp, among others","1928, 1934, 1935","""Berman & Reisz reopened this quarry in 1979, but despite extensive digging by a team of five people, only a few scattered bone fragments were recovered. It appears that the site has been completeley exhausted"" (Langston & Reisz, 1981 p. 74).\r\nType of Rhiodenticulatus heatoni was ""probably not found in the main bone level of the quarry, but rather as float on the slope of Loma Salazar a few feet away and presumably at or just above the quarry bone level."" (Berman & Reisz, 1986).","""Captorhinomorphs and Diadectomorphs"" (Langston 1966 p.690)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 11:03,10/08/2016 11:03,26206,sp.,Diadectes,60077,,303.4,268,Virgilian,Wolfcamp,NA,US,Diadectes sp.
1339947,occ,NA,,77412,,Eryops grandis,species,345659,,Eryops grandis,NA,species,345657,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-106.639442,36.157223,UCMP V-2814,NA,Camp Quarry,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"""southeast slope of a small butte, 410 yards south of New Mexico State Highway 96, about 940 yards southeast of the Rio Puerco bridge at Arroyo del Agua, section 8, T.22N., R.3E., Rio Arriba County, New Mexico"" (Langston, 1965 p. 6; 1966 p.691)",gp_mid,-34.09,4.48,101,US,FED,Abo/Cutler,,,group of beds,,,,,,,NA,All specimens appear to come from about the same stratigraphic level (38-36 m below top of the butte). Whether these beds are uppermost Carboniferous or lower Permian is a subject of controversy.\r\n,"""soft brick-red clayey siltstone"" (Langston, 1965 p. 6; 1966 p.691; Langston & Reisz, 1981 p. 74)",siltstone,red,,argillaceous,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,general faunal/floral,"bulk,surface (float),survey of museum collection",UCMP,all macrofossils,,,"C. L. Camp, among others","1928, 1934, 1935","""Berman & Reisz reopened this quarry in 1979, but despite extensive digging by a team of five people, only a few scattered bone fragments were recovered. It appears that the site has been completeley exhausted"" (Langston & Reisz, 1981 p. 74).\r\nType of Rhiodenticulatus heatoni was ""probably not found in the main bone level of the quarry, but rather as float on the slope of Loma Salazar a few feet away and presumably at or just above the quarry bone level."" (Berman & Reisz, 1986).","""Captorhinomorphs and Diadectomorphs"" (Langston 1966 p.690)","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 11:09,10/08/2016 11:09,26206,grandis,Eryops,60077,,303.4,268,Virgilian,Wolfcamp,NA,US,Eryops grandis
1339948,occ,NA,,77412,,Zatrachys serratus,species,255221,,Zatrachys serratus,NA,species,255221,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,,-106.639442,36.157223,UCMP V-2814,NA,Camp Quarry,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"""southeast slope of a small butte, 410 yards south of New Mexico State Highway 96, about 940 yards southeast of the Rio Puerco bridge at Arroyo del Agua, section 8, T.22N., R.3E., Rio Arriba County, New Mexico"" (Langston, 1965 p. 6; 1966 p.691)",gp_mid,-34.09,4.48,101,US,FED,Abo/Cutler,,,group of beds,,,,,,,NA,All specimens appear to come from about the same stratigraphic level (38-36 m below top of the butte). Whether these beds are uppermost Carboniferous or lower Permian is a subject of controversy.\r\n,"""soft brick-red clayey siltstone"" (Langston, 1965 p. 6; 1966 p.691; Langston & Reisz, 1981 p. 74)",siltstone,red,,argillaceous,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,general faunal/floral,"bulk,surface (float),survey of museum collection",UCMP,all macrofossils,,,"C. L. Camp, among others","1928, 1934, 1935","""Berman & Reisz reopened this quarry in 1979, but despite extensive digging by a team of five people, only a few scattered bone fragments were recovered. It appears that the site has been completeley exhausted"" (Langston & Reisz, 1981 p. 74).\r\nType of Rhiodenticulatus heatoni was ""probably not found in the main bone level of the quarry, but rather as float on the slope of Loma Salazar a few feet away and presumably at or just above the quarry bone level."" (Berman & Reisz, 1986).","""Captorhinomorphs and Diadectomorphs"" (Langston 1966 p.690)","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 11:09,10/08/2016 11:09,26206,serratus,Zatrachys,60077,,303.4,268,Virgilian,Wolfcamp,NA,US,Zatrachys serratus
1339949,occ,NA,,77412,,Broiliellus novomexicanus,species,136992,recombined as,Aspidosaurus novomexicanus,NA,species,136991,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37021,NA,NA,NA,,-106.639442,36.157223,UCMP V-2814,NA,Camp Quarry,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"""southeast slope of a small butte, 410 yards south of New Mexico State Highway 96, about 940 yards southeast of the Rio Puerco bridge at Arroyo del Agua, section 8, T.22N., R.3E., Rio Arriba County, New Mexico"" (Langston, 1965 p. 6; 1966 p.691)",gp_mid,-34.09,4.48,101,US,FED,Abo/Cutler,,,group of beds,,,,,,,NA,All specimens appear to come from about the same stratigraphic level (38-36 m below top of the butte). Whether these beds are uppermost Carboniferous or lower Permian is a subject of controversy.\r\n,"""soft brick-red clayey siltstone"" (Langston, 1965 p. 6; 1966 p.691; Langston & Reisz, 1981 p. 74)",siltstone,red,,argillaceous,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,general faunal/floral,"bulk,surface (float),survey of museum collection",UCMP,all macrofossils,,,"C. L. Camp, among others","1928, 1934, 1935","""Berman & Reisz reopened this quarry in 1979, but despite extensive digging by a team of five people, only a few scattered bone fragments were recovered. It appears that the site has been completeley exhausted"" (Langston & Reisz, 1981 p. 74).\r\nType of Rhiodenticulatus heatoni was ""probably not found in the main bone level of the quarry, but rather as float on the slope of Loma Salazar a few feet away and presumably at or just above the quarry bone level."" (Berman & Reisz, 1986).","""Captorhinomorphs and Diadectomorphs"" (Langston 1966 p.690)","brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Broiliellus,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 11:09,10/08/2016 11:09,26206,novomexicanus,Aspidosaurus,60077,,303.4,268,Virgilian,Wolfcamp,NA,US,Aspidosaurus novomexicanus
1339950,occ,NA,,77412,,Limnoscelis sp.,genus,37232,,Limnoscelis,NA,genus,37232,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Limnoscelidae,37231,37232,NA,NA,NA,,-106.639442,36.157223,UCMP V-2814,NA,Camp Quarry,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"""southeast slope of a small butte, 410 yards south of New Mexico State Highway 96, about 940 yards southeast of the Rio Puerco bridge at Arroyo del Agua, section 8, T.22N., R.3E., Rio Arriba County, New Mexico"" (Langston, 1965 p. 6; 1966 p.691)",gp_mid,-34.09,4.48,101,US,FED,Abo/Cutler,,,group of beds,,,,,,,NA,All specimens appear to come from about the same stratigraphic level (38-36 m below top of the butte). Whether these beds are uppermost Carboniferous or lower Permian is a subject of controversy.\r\n,"""soft brick-red clayey siltstone"" (Langston, 1965 p. 6; 1966 p.691; Langston & Reisz, 1981 p. 74)",siltstone,red,,argillaceous,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,general faunal/floral,"bulk,surface (float),survey of museum collection",UCMP,all macrofossils,,,"C. L. Camp, among others","1928, 1934, 1935","""Berman & Reisz reopened this quarry in 1979, but despite extensive digging by a team of five people, only a few scattered bone fragments were recovered. It appears that the site has been completeley exhausted"" (Langston & Reisz, 1981 p. 74).\r\nType of Rhiodenticulatus heatoni was ""probably not found in the main bone level of the quarry, but rather as float on the slope of Loma Salazar a few feet away and presumably at or just above the quarry bone level."" (Berman & Reisz, 1986).","""Captorhinomorphs and Diadectomorphs"" (Langston 1966 p.690)","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Limnoscelis,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 11:09,10/08/2016 11:09,26206,sp.,Limnoscelis,60077,,303.4,268,Virgilian,Wolfcamp,NA,US,Limnoscelis sp.
1339951,occ,NA,,77412,,Ophiacodon mirus,species,123418,,Ophiacodon mirus,NA,species,123418,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-106.639442,36.157223,UCMP V-2814,NA,Camp Quarry,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"""southeast slope of a small butte, 410 yards south of New Mexico State Highway 96, about 940 yards southeast of the Rio Puerco bridge at Arroyo del Agua, section 8, T.22N., R.3E., Rio Arriba County, New Mexico"" (Langston, 1965 p. 6; 1966 p.691)",gp_mid,-34.09,4.48,101,US,FED,Abo/Cutler,,,group of beds,,,,,,,NA,All specimens appear to come from about the same stratigraphic level (38-36 m below top of the butte). Whether these beds are uppermost Carboniferous or lower Permian is a subject of controversy.\r\n,"""soft brick-red clayey siltstone"" (Langston, 1965 p. 6; 1966 p.691; Langston & Reisz, 1981 p. 74)",siltstone,red,,argillaceous,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,general faunal/floral,"bulk,surface (float),survey of museum collection",UCMP,all macrofossils,,,"C. L. Camp, among others","1928, 1934, 1935","""Berman & Reisz reopened this quarry in 1979, but despite extensive digging by a team of five people, only a few scattered bone fragments were recovered. It appears that the site has been completeley exhausted"" (Langston & Reisz, 1981 p. 74).\r\nType of Rhiodenticulatus heatoni was ""probably not found in the main bone level of the quarry, but rather as float on the slope of Loma Salazar a few feet away and presumably at or just above the quarry bone level."" (Berman & Reisz, 1986).","""Captorhinomorphs and Diadectomorphs"" (Langston 1966 p.690)",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 11:09,10/08/2016 11:09,26206,mirus,Ophiacodon,60077,,303.4,268,Virgilian,Wolfcamp,NA,US,Ophiacodon mirus
1339952,occ,NA,,77412,,Edaphosaurus novomexicanus,species,122351,,Edaphosaurus novomexicanus,NA,species,122351,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,,-106.639442,36.157223,UCMP V-2814,NA,Camp Quarry,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"""southeast slope of a small butte, 410 yards south of New Mexico State Highway 96, about 940 yards southeast of the Rio Puerco bridge at Arroyo del Agua, section 8, T.22N., R.3E., Rio Arriba County, New Mexico"" (Langston, 1965 p. 6; 1966 p.691)",gp_mid,-34.09,4.48,101,US,FED,Abo/Cutler,,,group of beds,,,,,,,NA,All specimens appear to come from about the same stratigraphic level (38-36 m below top of the butte). Whether these beds are uppermost Carboniferous or lower Permian is a subject of controversy.\r\n,"""soft brick-red clayey siltstone"" (Langston, 1965 p. 6; 1966 p.691; Langston & Reisz, 1981 p. 74)",siltstone,red,,argillaceous,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,general faunal/floral,"bulk,surface (float),survey of museum collection",UCMP,all macrofossils,,,"C. L. Camp, among others","1928, 1934, 1935","""Berman & Reisz reopened this quarry in 1979, but despite extensive digging by a team of five people, only a few scattered bone fragments were recovered. It appears that the site has been completeley exhausted"" (Langston & Reisz, 1981 p. 74).\r\nType of Rhiodenticulatus heatoni was ""probably not found in the main bone level of the quarry, but rather as float on the slope of Loma Salazar a few feet away and presumably at or just above the quarry bone level."" (Berman & Reisz, 1986).","""Captorhinomorphs and Diadectomorphs"" (Langston 1966 p.690)",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 11:09,10/08/2016 11:09,26206,novomexicanus,Edaphosaurus,60077,,303.4,268,Virgilian,Wolfcamp,NA,US,Edaphosaurus novomexicanus
1339953,occ,NA,,77412,,Sphenacodon ferox,species,122487,,Sphenacodon ferox,NA,species,122487,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,,-106.639442,36.157223,UCMP V-2814,NA,Camp Quarry,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"""southeast slope of a small butte, 410 yards south of New Mexico State Highway 96, about 940 yards southeast of the Rio Puerco bridge at Arroyo del Agua, section 8, T.22N., R.3E., Rio Arriba County, New Mexico"" (Langston, 1965 p. 6; 1966 p.691)",gp_mid,-34.09,4.48,101,US,FED,Abo/Cutler,,,group of beds,,,,,,,NA,All specimens appear to come from about the same stratigraphic level (38-36 m below top of the butte). Whether these beds are uppermost Carboniferous or lower Permian is a subject of controversy.\r\n,"""soft brick-red clayey siltstone"" (Langston, 1965 p. 6; 1966 p.691; Langston & Reisz, 1981 p. 74)",siltstone,red,,argillaceous,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,variable,,,,,,,,,NA,,,general faunal/floral,"bulk,surface (float),survey of museum collection",UCMP,all macrofossils,,,"C. L. Camp, among others","1928, 1934, 1935","""Berman & Reisz reopened this quarry in 1979, but despite extensive digging by a team of five people, only a few scattered bone fragments were recovered. It appears that the site has been completeley exhausted"" (Langston & Reisz, 1981 p. 74).\r\nType of Rhiodenticulatus heatoni was ""probably not found in the main bone level of the quarry, but rather as float on the slope of Loma Salazar a few feet away and presumably at or just above the quarry bone level."" (Berman & Reisz, 1986).","""Captorhinomorphs and Diadectomorphs"" (Langston 1966 p.690)",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 11:09,10/08/2016 11:09,26206,ferox,Sphenacodon,60077,,303.4,268,Virgilian,Wolfcamp,NA,US,Sphenacodon ferox
1339955,occ,NA,,85733,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-98.59861,34.295834,Deep Red Run,NA,"Deep Red Creek; Cope's ""Indian Territory""",US,Oklahoma,Cotton,estimated from map,seconds,outcrop,"""There was at one time a small fort called Fort Auger on the north side of Red River about opposite where the town of Iowa Park is now located. There was a road leading from Fort Auger to Fort Sill. Near the crossing of Deep Red Creek by this old road is the locality at which I collected the vertebrates in Cope's collection labelled 'Indian Territory.' "" (Cummins, 1908).\r\n""This site is in Cotton County [...]. The site is several miles northwest of Randlett, but we were not able to locate it more precisely."" (Olson, 1967, Oklahoma Geol. Surv. Circ. 74).\r\nLat long is for Deep Red Creek immediately east of Tillman-Cotton County line (sec. 18, T.3S. R.13W., Whites Lake 7.5' quadrangle).",gp_mid,-29.65,-0.67,101,US,,Garber,Sumner,,member,,,,,,,NA,"""The trend of the strike of the texas beds suggests that the locality lies in the Clyde formation. [...] The presence of a large Dimetrodon [...] suggests a higher position; of Cricotus a lower one; of Ophiacodon major the Clyde itself. The somewhat conflicting evidence is thus on the whole agreeable to an approximate Clyde determination."" (Romer & Price, 1940).\r\nIn the chart (fig. 2) of Olson (1967, Oklahoma Geol. Surv. Circ. 74) the relevant stratigraphic unit is given as ""Hennessey Shale"" but is correlated with the Garber Sandstone of other parts of Oklahoma.\r\nIn the stratigraphic chart (table 1) of Heaton (1979, Oklahoma Geol. Surv. Bull. 127) the Deep Red Run locality is assigned to the middle part of the Garber Sandstone, the latter being correlated with the Lueders Fm. of Texas.",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,snapshot,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,W. F. Cummins,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 12:20,10/08/2016 12:20,30068,sp.,Diadectes,60077,,290.1,272.3,Artinskian,Kungurian,NA,US,Diadectes sp.
1339956,occ,NA,,84716,,Archeria crassidisca,species,345353,,Archeria crassidisca,NA,species,229309,Kissel,2010,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,,-98.900002,33.641666,Rattlesnake Canyon (Admiral Fm.),NA,Locality IVc (Romer & Price 1940); Cummins' Headquarters; Lyles Place,US,Texas,Archer,estimated from map,seconds,outcrop,"Rattlesnake Canyon, Archer County, Texas. Lat long is estimated from map on p. 397 in Clark & Carroll (1973).",gp_mid,-30.23,-1.14,101,US,,Petrolia,Wichita,,,,,,,,,NA,"""Uppermost Admiral Formation"" (Clark & Carroll, 1973); the uppermost part of the traditional Admiral Fm. today is considered the lowermost part of the Petrolia Fm. (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 12:47,10/08/2016 12:47,28415,crassidisca,Archeria,60077,,290.1,279.3,Artinskian,,NA,US,Archeria crassidisca
1339957,occ,NA,,84716,,Eryops megacephalus,species,70397,,Eryops megacephalus,NA,species,70397,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-98.900002,33.641666,Rattlesnake Canyon (Admiral Fm.),NA,Locality IVc (Romer & Price 1940); Cummins' Headquarters; Lyles Place,US,Texas,Archer,estimated from map,seconds,outcrop,"Rattlesnake Canyon, Archer County, Texas. Lat long is estimated from map on p. 397 in Clark & Carroll (1973).",gp_mid,-30.23,-1.14,101,US,,Petrolia,Wichita,,,,,,,,,NA,"""Uppermost Admiral Formation"" (Clark & Carroll, 1973); the uppermost part of the traditional Admiral Fm. today is considered the lowermost part of the Petrolia Fm. (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 12:47,10/08/2016 12:47,28415,megacephalus,Eryops,60077,,290.1,279.3,Artinskian,,NA,US,Eryops megacephalus
1339958,occ,NA,,84716,,Zatrachys serratus,species,255221,,Zatrachys serratus,NA,species,255221,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,,-98.900002,33.641666,Rattlesnake Canyon (Admiral Fm.),NA,Locality IVc (Romer & Price 1940); Cummins' Headquarters; Lyles Place,US,Texas,Archer,estimated from map,seconds,outcrop,"Rattlesnake Canyon, Archer County, Texas. Lat long is estimated from map on p. 397 in Clark & Carroll (1973).",gp_mid,-30.23,-1.14,101,US,,Petrolia,Wichita,,,,,,,,,NA,"""Uppermost Admiral Formation"" (Clark & Carroll, 1973); the uppermost part of the traditional Admiral Fm. today is considered the lowermost part of the Petrolia Fm. (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 12:47,10/08/2016 12:47,28415,serratus,Zatrachys,60077,,290.1,279.3,Artinskian,,NA,US,Zatrachys serratus
1339959,occ,NA,,84716,,Trimerorhachis insignis,species,90711,,Trimerorhachis insignis,NA,species,90711,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-98.900002,33.641666,Rattlesnake Canyon (Admiral Fm.),NA,Locality IVc (Romer & Price 1940); Cummins' Headquarters; Lyles Place,US,Texas,Archer,estimated from map,seconds,outcrop,"Rattlesnake Canyon, Archer County, Texas. Lat long is estimated from map on p. 397 in Clark & Carroll (1973).",gp_mid,-30.23,-1.14,101,US,,Petrolia,Wichita,,,,,,,,,NA,"""Uppermost Admiral Formation"" (Clark & Carroll, 1973); the uppermost part of the traditional Admiral Fm. today is considered the lowermost part of the Petrolia Fm. (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 12:47,10/08/2016 12:47,28415,insignis,Trimerorhachis,60077,,290.1,279.3,Artinskian,,NA,US,Trimerorhachis insignis
1339960,occ,NA,,84716,,Diadectes sideropelicus,species,320982,,Diadectes sideropelicus,NA,species,320982,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-98.900002,33.641666,Rattlesnake Canyon (Admiral Fm.),NA,Locality IVc (Romer & Price 1940); Cummins' Headquarters; Lyles Place,US,Texas,Archer,estimated from map,seconds,outcrop,"Rattlesnake Canyon, Archer County, Texas. Lat long is estimated from map on p. 397 in Clark & Carroll (1973).",gp_mid,-30.23,-1.14,101,US,,Petrolia,Wichita,,,,,,,,,NA,"""Uppermost Admiral Formation"" (Clark & Carroll, 1973); the uppermost part of the traditional Admiral Fm. today is considered the lowermost part of the Petrolia Fm. (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 12:47,10/08/2016 12:47,28415,sideropelicus,Diadectes,60077,,290.1,279.3,Artinskian,,NA,US,Diadectes sideropelicus
1339961,occ,NA,,84716,,Dimetrodon milleri,species,122782,,Dimetrodon milleri,NA,species,122782,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-98.900002,33.641666,Rattlesnake Canyon (Admiral Fm.),NA,Locality IVc (Romer & Price 1940); Cummins' Headquarters; Lyles Place,US,Texas,Archer,estimated from map,seconds,outcrop,"Rattlesnake Canyon, Archer County, Texas. Lat long is estimated from map on p. 397 in Clark & Carroll (1973).",gp_mid,-30.23,-1.14,101,US,,Petrolia,Wichita,,,,,,,,,NA,"""Uppermost Admiral Formation"" (Clark & Carroll, 1973); the uppermost part of the traditional Admiral Fm. today is considered the lowermost part of the Petrolia Fm. (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 12:47,10/08/2016 12:47,28415,milleri,Dimetrodon,60077,,290.1,279.3,Artinskian,,NA,US,Dimetrodon milleri
1339962,occ,NA,,84716,,Edaphosaurus boanerges,species,122352,,Edaphosaurus boanerges,NA,species,122352,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,,-98.900002,33.641666,Rattlesnake Canyon (Admiral Fm.),NA,Locality IVc (Romer & Price 1940); Cummins' Headquarters; Lyles Place,US,Texas,Archer,estimated from map,seconds,outcrop,"Rattlesnake Canyon, Archer County, Texas. Lat long is estimated from map on p. 397 in Clark & Carroll (1973).",gp_mid,-30.23,-1.14,101,US,,Petrolia,Wichita,,,,,,,,,NA,"""Uppermost Admiral Formation"" (Clark & Carroll, 1973); the uppermost part of the traditional Admiral Fm. today is considered the lowermost part of the Petrolia Fm. (see Fig. 2 in Sander, 1989)",,not reported,,,,,,,,,,terrestrial indet.,foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,MCZ,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 12:47,10/08/2016 12:47,28415,boanerges,Edaphosaurus,60077,,290.1,279.3,Artinskian,,NA,US,Edaphosaurus boanerges
1339963,occ,NA,,180978,members,Eryops megacephalus,species,70397,,Eryops megacephalus,NA,species,70397,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-98.68528,33.672501,Coprolite Bonebed,NA,,US,Texas,Archer,estimated from map,seconds,outcrop,Locality lies northwest of Archer City,gp_mid,-30.04,-1.17,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,mudstone,red,,,,sandstone,,,,,"""floodplain""",foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 13:02,10/08/2016 13:02,NA,megacephalus,Eryops,60077,,296.4,268,Wolfcamp,,NA,US,Eryops megacephalus
1339964,occ,NA,,180978,members,Archeria crassidisca,species,345353,,Archeria crassidisca,NA,species,229309,Kissel,2010,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,,-98.68528,33.672501,Coprolite Bonebed,NA,,US,Texas,Archer,estimated from map,seconds,outcrop,Locality lies northwest of Archer City,gp_mid,-30.04,-1.17,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,mudstone,red,,,,sandstone,,,,,"""floodplain""",foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 13:02,10/08/2016 13:02,NA,crassidisca,Archeria,60077,,296.4,268,Wolfcamp,,NA,US,Archeria crassidisca
1339965,occ,NA,,180978,members,Diadectes sideropelicus,species,320982,,Diadectes sideropelicus,NA,species,320982,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-98.68528,33.672501,Coprolite Bonebed,NA,,US,Texas,Archer,estimated from map,seconds,outcrop,Locality lies northwest of Archer City,gp_mid,-30.04,-1.17,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,mudstone,red,,,,sandstone,,,,,"""floodplain""",foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 13:02,10/08/2016 13:02,NA,sideropelicus,Diadectes,60077,,296.4,268,Wolfcamp,,NA,US,Diadectes sideropelicus
1339966,occ,NA,,180978,members,Edaphosaurus boanerges,species,122352,,Edaphosaurus boanerges,NA,species,122352,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,,-98.68528,33.672501,Coprolite Bonebed,NA,,US,Texas,Archer,estimated from map,seconds,outcrop,Locality lies northwest of Archer City,gp_mid,-30.04,-1.17,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,mudstone,red,,,,sandstone,,,,,"""floodplain""",foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 13:02,10/08/2016 13:02,NA,boanerges,Edaphosaurus,60077,,296.4,268,Wolfcamp,,NA,US,Edaphosaurus boanerges
1339967,occ,NA,,180978,members,Dimetrodon limbatus,species,344229,,Dimetrodon limbatus,NA,species,70401,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-98.68528,33.672501,Coprolite Bonebed,NA,,US,Texas,Archer,estimated from map,seconds,outcrop,Locality lies northwest of Archer City,gp_mid,-30.04,-1.17,101,US,,Archer City,Wichita,,formation,,,,,,,NA,"The former Putnam Formation corresponds to the upper part of the Archer City Formation (see Fig. 2 in Sander, 1989)",,mudstone,red,,,,sandstone,,,,,"""floodplain""",foreland basin,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,10/08/2016 13:02,10/08/2016 13:02,NA,limbatus,Dimetrodon,60077,,296.4,268,Wolfcamp,,NA,US,Dimetrodon limbatus
1339968,occ,NA,,180979,,n. gen. Ductilodon n. sp. pruitti,species,345961,,Ductilodon pruitti,NA,species,345961,Gubin,1999,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,345960,NA,NA,NA,,-96.109444,38.863056,Eskridge locality,NA,,US,Kansas,Wabaunsee,based on nearby landmark,seconds,small collection,"Lat long is for the city of Eskridge, Wabaunsee County, Kansas.",gp_mid,-25.79,1.82,101,US,,Wreford,Council Grove,Speiser,,,,,,,,NA,"""Gearyan stage""",,"""mixed carbonate-siliciclastic""","gray,green",,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Ductilodon,n. gen.,NA,NA,vertebrate,"Y. M. Gubin. 1999. A New Diplocaulid (Nectridea, Amphibia) from the Early Permian of Kansas (USA). Paleontological Journal 33(6):630-637",327,697,0,R. Butler,E. Dunne,,11/08/2016 04:40,11/08/2016 04:40,NA,pruitti,Ductilodon,60089,n. sp.,295.5,290.1,Sakmarian,,NA,US,Ductilodon pruitti
1339969,occ,NA,,180979,,Acroplous vorax,species,255215,,Acroplous vorax,NA,species,255215,Foreman,1990,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eobrachyopidae,150302,36981,NA,NA,NA,,-96.109444,38.863056,Eskridge locality,NA,,US,Kansas,Wabaunsee,based on nearby landmark,seconds,small collection,"Lat long is for the city of Eskridge, Wabaunsee County, Kansas.",gp_mid,-25.79,1.82,101,US,,Wreford,Council Grove,Speiser,,,,,,,,NA,"""Gearyan stage""",,"""mixed carbonate-siliciclastic""","gray,green",,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Acroplous,,NA,NA,vertebrate,B. C. Foreman. 1990. A Revision of the Cranial Morphology of the Lower Permian Temnospondyl Amphibian Acroplous vorax Hotton. Journal of Vertebrate Paleontology 10(3):390-397,327,697,697,R. Butler,E. Dunne,E. Dunne,11/08/2016 04:43,11/08/2016 04:44,NA,vorax,Acroplous,59486,,295.5,290.1,Sakmarian,,NA,US,Acroplous vorax
1339970,occ,NA,,180979,,Lysorophus sp.,genus,37322,,Lysorophus,NA,genus,37322,Gubin,1999,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-96.109444,38.863056,Eskridge locality,NA,,US,Kansas,Wabaunsee,based on nearby landmark,seconds,small collection,"Lat long is for the city of Eskridge, Wabaunsee County, Kansas.",gp_mid,-25.79,1.82,101,US,,Wreford,Council Grove,Speiser,,,,,,,,NA,"""Gearyan stage""",,"""mixed carbonate-siliciclastic""","gray,green",,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,"Y. M. Gubin. 1999. A New Diplocaulid (Nectridea, Amphibia) from the Early Permian of Kansas (USA). Paleontological Journal 33(6):630-637",327,697,0,R. Butler,E. Dunne,,11/08/2016 04:43,11/08/2016 04:43,NA,sp.,Lysorophus,60089,,295.5,290.1,Sakmarian,,NA,US,Lysorophus sp.
1339972,occ,NA,,80784,,n. gen. Kenomagnathus n. sp. scotti,species,345967,,Kenomagnathus scotti,NA,species,345967,Spindler,2015,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,345966,NA,NA,NA,,-95.259048,38.378502,Garnett Quarry,NA,"Garnett Vertebrate Fauna, Charles Hardesty farm",US,Kansas,Anderson,estimated from map,6,outcrop,"""6 miles northwest of Garnett"" (Reisz, 1986); ""NW 1/4, NE 1/4, sec. 5, tp. 20 S, rge. 19 E, Putnam Township, Anderson County, Kansas"" (Reisz & Berman, 1986)\r\n""Charles A. Hardest farm, NW/4 NE/4 sec. 5 T20S R19E, Putnam Township, Anderson County, Kansas. The Universal Transverse Mercantor (UTM) coordinates of the quarry are 15STN963466. Locality is close to Garnett, Kansas."" (Laurin 1993). ",gp_mid,-27.44,-2.3,101,US,,Stanton,Lansing,Rock Lake Shale,group of beds,,,,,,,NA,"""Rock Lake Member, Stanton Formation, Lansing Group, Missourian Series, Upper Pennsylvanian"" (Reisz & Berman, 1996)\r\nall vertebrate remains seem to come exclusively from the basal part of the Rock Lake Shale (see Reisz et al., 1982)","""dark greyishbrown, moderately well bedded, very carbonaceous, calcareous mudstone"" (Reisz et al., 1982)",mudstone,brown,,"calcareous,carbonaceous",Y,,,,,,fine channel fill,foreland basin,"""The Rock Lake Shale is a rather thin but otherwise typical ۪outside۪ shale of a ۪Kansas Megacyclothem۪ sequence formed as a change from regressive to transgressive conditions occurred [...] The site is located along the western edge of what was, during the Late Pennsylvanian, a shallow, forested stream valley or channel that was eroded into a limestone coastal plain during the latter stages of a major eustatic fall in sea level. As the succeeding rise in sea level occurred, the valley was gradually flooded by estuarine waters"" (Reisz et al., 1982).\r\nSequence stratigraphy is interpreted from the description given by Reisz et al. (1982). The surface of the underlying limestone is the sequence boundary merged with the transgressive surface and the Lake Rock Shale is the basalmost deposit of the transgressive systems tract.",macrofossils,some,some,,,,NA,,body,good,,snapshot,,,,,,,NA,,,taxonomic,"bulk,mechanical",ROM,,,,"F. E. Peabody, R. Camp, R. L. Carroll, R. R. Reisz, M. J. Heaton, B. R. Pynn, G. MacDonald","1953-1956, 1965, 1980, 1981",,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Kenomagnathus,n. gen.,NA,NA,vertebrate,F. Spindler. 2015. The basal Sphenacodontia: Systematic revision and evolutionary implications. ,327,697,0,R. Butler,E. Dunne,,11/08/2016 06:15,11/08/2016 06:15,28862,scotti,Kenomagnathus,60090,n. sp.,305.9,303.4,Missourian,,NA,US,Kenomagnathus scotti
1339973,occ,NA,,80784,,n. gen. Tenuacaptor n. sp. reiszi,species,345969,,Tenuacaptor reiszi,NA,species,345969,Spindler,2015,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,345968,NA,NA,NA,,-95.259048,38.378502,Garnett Quarry,NA,"Garnett Vertebrate Fauna, Charles Hardesty farm",US,Kansas,Anderson,estimated from map,6,outcrop,"""6 miles northwest of Garnett"" (Reisz, 1986); ""NW 1/4, NE 1/4, sec. 5, tp. 20 S, rge. 19 E, Putnam Township, Anderson County, Kansas"" (Reisz & Berman, 1986)\r\n""Charles A. Hardest farm, NW/4 NE/4 sec. 5 T20S R19E, Putnam Township, Anderson County, Kansas. The Universal Transverse Mercantor (UTM) coordinates of the quarry are 15STN963466. Locality is close to Garnett, Kansas."" (Laurin 1993). ",gp_mid,-27.44,-2.3,101,US,,Stanton,Lansing,Rock Lake Shale,group of beds,,,,,,,NA,"""Rock Lake Member, Stanton Formation, Lansing Group, Missourian Series, Upper Pennsylvanian"" (Reisz & Berman, 1996)\r\nall vertebrate remains seem to come exclusively from the basal part of the Rock Lake Shale (see Reisz et al., 1982)","""dark greyishbrown, moderately well bedded, very carbonaceous, calcareous mudstone"" (Reisz et al., 1982)",mudstone,brown,,"calcareous,carbonaceous",Y,,,,,,fine channel fill,foreland basin,"""The Rock Lake Shale is a rather thin but otherwise typical ۪outside۪ shale of a ۪Kansas Megacyclothem۪ sequence formed as a change from regressive to transgressive conditions occurred [...] The site is located along the western edge of what was, during the Late Pennsylvanian, a shallow, forested stream valley or channel that was eroded into a limestone coastal plain during the latter stages of a major eustatic fall in sea level. As the succeeding rise in sea level occurred, the valley was gradually flooded by estuarine waters"" (Reisz et al., 1982).\r\nSequence stratigraphy is interpreted from the description given by Reisz et al. (1982). The surface of the underlying limestone is the sequence boundary merged with the transgressive surface and the Lake Rock Shale is the basalmost deposit of the transgressive systems tract.",macrofossils,some,some,,,,NA,,body,good,,snapshot,,,,,,,NA,,,taxonomic,"bulk,mechanical",ROM,,,,"F. E. Peabody, R. Camp, R. L. Carroll, R. R. Reisz, M. J. Heaton, B. R. Pynn, G. MacDonald","1953-1956, 1965, 1980, 1981",,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Tenuacaptor,n. gen.,NA,NA,vertebrate,F. Spindler. 2015. The basal Sphenacodontia: Systematic revision and evolutionary implications. ,327,697,0,R. Butler,E. Dunne,,11/08/2016 06:17,11/08/2016 06:17,28862,reiszi,Tenuacaptor,60090,n. sp.,305.9,303.4,Missourian,,NA,US,Tenuacaptor reiszi
1339974,occ,NA,,180761,members,Haptodus ? sp.,genus,38905,,Haptodus,NA,genus,38905,Spindler,2015,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,38905,NA,NA,NA,,11.517153,48.371948,Kammerberg near Manebach,NA,,DE,Thuringia,,based on nearby landmark,6,small collection,"Coordinates based on the village of Kammerberg, near Manebach, Thuringia, Germany.",gp_mid,22.37,4.25,305,DE,,Manebach,,,,,,,,,,NA,Pennsylvanian-Permian Boundary,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Haptodus,?,NA,NA,vertebrate,F. Spindler. 2015. The basal Sphenacodontia: Systematic revision and evolutionary implications. ,327,697,697,R. Butler,E. Dunne,E. Dunne,11/08/2016 06:20,11/08/2016 06:20,NA,sp.,Haptodus,60090,,303.7,295.5,Gzhelian,Asselian,NA,DE,Haptodus sp.
1339976,occ,NA,,180981,members,n. gen. Callibrachion n. sp. gaudryi,species,345972,,Callibrachion gaudryi,NA,species,345972,Spindler,2015,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,345971,NA,NA,NA,,4.297222,46.949165,"Black Shales of Autun, near Margenne",NA,"Autun, Saone et Loire",FR,Burgundy,Sa̫ne-et-Loire,based on nearby landmark,seconds,small collection,"Coordinates based Margenne, near Autun, in the Sa̫ne-et-Loire department in Burgundy in eastern France.",gp_mid,18.56,2.69,305,FR,,Millery,,,,,,,,,,NA,"According to modern stratigraphy (Werneburg & Schneider, 2006), the site [...] is part of the upper Millery Formation (Autunian, Rotliegend, Cisuralian), which was recently dated to the Artinskian (formerly Sakmarian, see Schneider et al., 2014). (Spindler, 2015)",,"""shale""",gray,,,,,,,,,lacustrine indet.,,"The dark grayish bituminous shale was deposited in a lacustrine environment (Marteau & Feys, 1989).",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MNHN,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Callibrachion,n. gen.,NA,NA,vertebrate,F. Spindler. 2015. The basal Sphenacodontia: Systematic revision and evolutionary implications. ,327,697,0,R. Butler,E. Dunne,,11/08/2016 08:59,11/08/2016 08:59,NA,gaudryi,Callibrachion,60090,n. sp.,290.1,279.3,Artinskian,,NA,FR,Callibrachion gaudryi
1340014,occ,NA,,180988,members,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Berman,1993,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-107.182503,34.639999,Sierra Lucero Locality,NA,,US,New Mexico,Cibola,stated in text,seconds,outcrop,"Vertebrate fossils were discovered and collected by the author in 1975 at numerous sites in a 10km long, narrow, north-south strip of Lower Permian Abo Formation exposure lying about 8km east of Sierra Lucero and 29km west of Interstate Highway 25 at Los Lunas in Valencia County.",gp_mid,-35.35,3.52,101,US,,Abo,,,,,,,,,,NA,"Abo Formation = Lower Permian (middle-upper Wolfcampian) (Lucas et al., 2015)",,not reported,,,,,,,,,,coastal indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,Berman,1975,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,12/08/2016 05:48,12/08/2016 05:48,NA,sp.,Trimerorhachis,60092,,295.5,279.3,Sakmarian,Artinskian,NA,US,Trimerorhachis sp.
1340015,occ,NA,,180988,members,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-107.182503,34.639999,Sierra Lucero Locality,NA,,US,New Mexico,Cibola,stated in text,seconds,outcrop,"Vertebrate fossils were discovered and collected by the author in 1975 at numerous sites in a 10km long, narrow, north-south strip of Lower Permian Abo Formation exposure lying about 8km east of Sierra Lucero and 29km west of Interstate Highway 25 at Los Lunas in Valencia County.",gp_mid,-35.35,3.52,101,US,,Abo,,,,,,,,,,NA,"Abo Formation = Lower Permian (middle-upper Wolfcampian) (Lucas et al., 2015)",,not reported,,,,,,,,,,coastal indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,Berman,1975,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,12/08/2016 05:48,12/08/2016 05:48,NA,sp.,Diadectes,60092,,295.5,279.3,Sakmarian,Artinskian,NA,US,Diadectes sp.
1340016,occ,NA,,180988,members,Sphenacodon sp.,genus,38909,,Sphenacodon,NA,genus,38909,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,,-107.182503,34.639999,Sierra Lucero Locality,NA,,US,New Mexico,Cibola,stated in text,seconds,outcrop,"Vertebrate fossils were discovered and collected by the author in 1975 at numerous sites in a 10km long, narrow, north-south strip of Lower Permian Abo Formation exposure lying about 8km east of Sierra Lucero and 29km west of Interstate Highway 25 at Los Lunas in Valencia County.",gp_mid,-35.35,3.52,101,US,,Abo,,,,,,,,,,NA,"Abo Formation = Lower Permian (middle-upper Wolfcampian) (Lucas et al., 2015)",,not reported,,,,,,,,,,coastal indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,Berman,1975,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,12/08/2016 05:48,12/08/2016 05:48,NA,sp.,Sphenacodon,60092,,295.5,279.3,Sakmarian,Artinskian,NA,US,Sphenacodon sp.
1340017,occ,NA,,180989,members,Sphenacodon sp.,genus,38909,,Sphenacodon,NA,genus,38909,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,,-107.182503,34.639999,Pecos River Valley Locality (Sangre de Cristo),NA,,US,New Mexico,San Miguel,estimated from map,seconds,outcrop,"The fossils were collected from scattered sites along the upper reaches of the Pecos River drainage from Glorieta Pass at Glorieta on the eastern border of Santa Fe County souteastward to about 8km south of Ribera in San Miguel County. The coordinates here are based on half way between these 2 points, close to Highway 25",gp_mid,-35.7,2.91,101,US,,Sangre de Cristo,,,,,,,,,,NA,Sangre de Cristo Formation = Gzhelian - Sakmarian (Wellstead 1991),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,12/08/2016 06:12,12/08/2016 06:12,NA,sp.,Sphenacodon,60092,,303.7,290.1,Gzhelian,Sakmarian,NA,US,Sphenacodon sp.
1340018,occ,NA,,180989,members,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-107.182503,34.639999,Pecos River Valley Locality (Sangre de Cristo),NA,,US,New Mexico,San Miguel,estimated from map,seconds,outcrop,"The fossils were collected from scattered sites along the upper reaches of the Pecos River drainage from Glorieta Pass at Glorieta on the eastern border of Santa Fe County souteastward to about 8km south of Ribera in San Miguel County. The coordinates here are based on half way between these 2 points, close to Highway 25",gp_mid,-35.7,2.91,101,US,,Sangre de Cristo,,,,,,,,,,NA,Sangre de Cristo Formation = Gzhelian - Sakmarian (Wellstead 1991),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,12/08/2016 06:12,12/08/2016 06:12,NA,sp.,Diadectes,60092,,303.7,290.1,Gzhelian,Sakmarian,NA,US,Diadectes sp.
1340026,occ,NA,,180990,members,Archeria sp.,genus,37196,,Archeria,NA,genus,37196,Olson,1967,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,,-97.69442,36.664398,Pond Creek,NA,,US,Oklahoma,Grant,stated in text,6,outcrop,"The Pond Creek site lies 5 miles east of the village of Pond Creek, Grant County, Oklahoma on the property of Price Shaeffer.",gp_mid,-27.43,1.65,101,US,,Garber,,,,,,,,,,NA,Cannot be accurately placed in either the Lucien or Hayward Members,"Also, red shales","""shale""",,,sandy,Y,conglomerate,,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:10,12/08/2016 10:10,NA,sp.,Archeria,28557,,290.1,268,Leonard,,NA,US,Archeria sp.
1340027,occ,NA,,180990,members,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Olson,1967,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-97.69442,36.664398,Pond Creek,NA,,US,Oklahoma,Grant,stated in text,6,outcrop,"The Pond Creek site lies 5 miles east of the village of Pond Creek, Grant County, Oklahoma on the property of Price Shaeffer.",gp_mid,-27.43,1.65,101,US,,Garber,,,,,,,,,,NA,Cannot be accurately placed in either the Lucien or Hayward Members,"Also, red shales","""shale""",,,sandy,Y,conglomerate,,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:10,12/08/2016 10:10,NA,sp.,Trimerorhachis,28557,,290.1,268,Leonard,,NA,US,Trimerorhachis sp.
1340028,occ,NA,,180990,members,Eryops megacephalus,species,70397,,Eryops megacephalus,NA,species,70397,Olson,1967,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-97.69442,36.664398,Pond Creek,NA,,US,Oklahoma,Grant,stated in text,6,outcrop,"The Pond Creek site lies 5 miles east of the village of Pond Creek, Grant County, Oklahoma on the property of Price Shaeffer.",gp_mid,-27.43,1.65,101,US,,Garber,,,,,,,,,,NA,Cannot be accurately placed in either the Lucien or Hayward Members,"Also, red shales","""shale""",,,sandy,Y,conglomerate,,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:10,12/08/2016 10:10,NA,megacephalus,Eryops,28557,,290.1,268,Leonard,,NA,US,Eryops megacephalus
1340029,occ,NA,,180990,members,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Olson,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-97.69442,36.664398,Pond Creek,NA,,US,Oklahoma,Grant,stated in text,6,outcrop,"The Pond Creek site lies 5 miles east of the village of Pond Creek, Grant County, Oklahoma on the property of Price Shaeffer.",gp_mid,-27.43,1.65,101,US,,Garber,,,,,,,,,,NA,Cannot be accurately placed in either the Lucien or Hayward Members,"Also, red shales","""shale""",,,sandy,Y,conglomerate,,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:10,12/08/2016 10:10,NA,sp.,Diadectes,28557,,290.1,268,Leonard,,NA,US,Diadectes sp.
1340030,occ,NA,,180990,members,Diplocaulus magnicornis,species,81712,,Diplocaulus magnicornis,NA,species,81712,Olson,1967,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-97.69442,36.664398,Pond Creek,NA,,US,Oklahoma,Grant,stated in text,6,outcrop,"The Pond Creek site lies 5 miles east of the village of Pond Creek, Grant County, Oklahoma on the property of Price Shaeffer.",gp_mid,-27.43,1.65,101,US,,Garber,,,,,,,,,,NA,Cannot be accurately placed in either the Lucien or Hayward Members,"Also, red shales","""shale""",,,sandy,Y,conglomerate,,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:12,12/08/2016 10:12,NA,magnicornis,Diplocaulus,28557,,290.1,268,Leonard,,NA,US,Diplocaulus magnicornis
1340031,occ,NA,,180990,members,Captorhinus cf. aguti,species,90718,,Captorhinus aguti,NA,species,134887,Olson,1967,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,,-97.69442,36.664398,Pond Creek,NA,,US,Oklahoma,Grant,stated in text,6,outcrop,"The Pond Creek site lies 5 miles east of the village of Pond Creek, Grant County, Oklahoma on the property of Price Shaeffer.",gp_mid,-27.43,1.65,101,US,,Garber,,,,,,,,,,NA,Cannot be accurately placed in either the Lucien or Hayward Members,"Also, red shales","""shale""",,,sandy,Y,conglomerate,,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:12,12/08/2016 10:12,NA,aguti,Captorhinus,28557,cf.,290.1,268,Leonard,,NA,US,Captorhinus aguti
1340032,occ,NA,,180990,members,Labidosaurus hamatus,species,134918,,Labidosaurus hamatus,NA,species,134856,Olson,1967,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37501,NA,NA,NA,,-97.69442,36.664398,Pond Creek,NA,,US,Oklahoma,Grant,stated in text,6,outcrop,"The Pond Creek site lies 5 miles east of the village of Pond Creek, Grant County, Oklahoma on the property of Price Shaeffer.",gp_mid,-27.43,1.65,101,US,,Garber,,,,,,,,,,NA,Cannot be accurately placed in either the Lucien or Hayward Members,"Also, red shales","""shale""",,,sandy,Y,conglomerate,,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Labidosaurus,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:12,12/08/2016 10:12,NA,hamatus,Labidosaurus,28557,,290.1,268,Leonard,,NA,US,Labidosaurus hamatus
1340033,occ,NA,,180990,members,Dimetrodon grandis,species,122786,,Dimetrodon grandis,NA,species,138059,Olson,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-97.69442,36.664398,Pond Creek,NA,,US,Oklahoma,Grant,stated in text,6,outcrop,"The Pond Creek site lies 5 miles east of the village of Pond Creek, Grant County, Oklahoma on the property of Price Shaeffer.",gp_mid,-27.43,1.65,101,US,,Garber,,,,,,,,,,NA,Cannot be accurately placed in either the Lucien or Hayward Members,"Also, red shales","""shale""",,,sandy,Y,conglomerate,,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:12,12/08/2016 10:12,NA,grandis,Dimetrodon,28557,,290.1,268,Leonard,,NA,US,Dimetrodon grandis
1340034,occ,NA,,180990,members,Dimetrodon giganhomogenes,species,38904,species not entered,Dimetrodon,NA,genus,38904,Olson,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-97.69442,36.664398,Pond Creek,NA,,US,Oklahoma,Grant,stated in text,6,outcrop,"The Pond Creek site lies 5 miles east of the village of Pond Creek, Grant County, Oklahoma on the property of Price Shaeffer.",gp_mid,-27.43,1.65,101,US,,Garber,,,,,,,,,,NA,Cannot be accurately placed in either the Lucien or Hayward Members,"Also, red shales","""shale""",,,sandy,Y,conglomerate,,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:12,12/08/2016 10:12,NA,giganhomogenes,Dimetrodon,28557,,290.1,268,Leonard,,NA,US,Dimetrodon giganhomogenes
1340035,occ,NA,,180990,members,Edaphosaurus sp.,genus,38911,,Edaphosaurus,NA,genus,38911,Olson,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,,-97.69442,36.664398,Pond Creek,NA,,US,Oklahoma,Grant,stated in text,6,outcrop,"The Pond Creek site lies 5 miles east of the village of Pond Creek, Grant County, Oklahoma on the property of Price Shaeffer.",gp_mid,-27.43,1.65,101,US,,Garber,,,,,,,,,,NA,Cannot be accurately placed in either the Lucien or Hayward Members,"Also, red shales","""shale""",,,sandy,Y,conglomerate,,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:12,12/08/2016 10:12,NA,sp.,Edaphosaurus,28557,,290.1,268,Leonard,,NA,US,Edaphosaurus sp.
1340037,occ,NA,,180991,members,Archeria sp.,genus,37196,,Archeria,NA,genus,37196,Olson,1967,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,,-98.092766,34.164795,Waurika Site 1,NA,Waurika Locality,US,Oklahoma,Jefferson,based on nearby landmark,6,outcrop,"The site lies 6 miles west of the Waurika, Jefferson County, Oklahoma on the property of Price Shaeffer. Coordinates used here are approximate.",gp_mid,-28.99,-0.33,101,US,,,,,,,,,,,,NA,,Ryan-Aspaltum Sandstone lies 40 feet above the shale,"""shale""",gray,,,Y,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:41,12/08/2016 10:41,NA,sp.,Archeria,28557,,290.1,268,Leonard,,NA,US,Archeria sp.
1340038,occ,NA,,180991,members,Trimerorhachis cf. insignis,species,90711,,Trimerorhachis insignis,NA,species,90711,Olson,1967,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-98.092766,34.164795,Waurika Site 1,NA,Waurika Locality,US,Oklahoma,Jefferson,based on nearby landmark,6,outcrop,"The site lies 6 miles west of the Waurika, Jefferson County, Oklahoma on the property of Price Shaeffer. Coordinates used here are approximate.",gp_mid,-28.99,-0.33,101,US,,,,,,,,,,,,NA,,Ryan-Aspaltum Sandstone lies 40 feet above the shale,"""shale""",gray,,,Y,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:41,12/08/2016 10:41,NA,insignis,Trimerorhachis,28557,cf.,290.1,268,Leonard,,NA,US,Trimerorhachis insignis
1340039,occ,NA,,180991,members,Eryops cf. megacephalus,species,70397,,Eryops megacephalus,NA,species,70397,Olson,1967,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-98.092766,34.164795,Waurika Site 1,NA,Waurika Locality,US,Oklahoma,Jefferson,based on nearby landmark,6,outcrop,"The site lies 6 miles west of the Waurika, Jefferson County, Oklahoma on the property of Price Shaeffer. Coordinates used here are approximate.",gp_mid,-28.99,-0.33,101,US,,,,,,,,,,,,NA,,Ryan-Aspaltum Sandstone lies 40 feet above the shale,"""shale""",gray,,,Y,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:41,12/08/2016 10:41,NA,megacephalus,Eryops,28557,cf.,290.1,268,Leonard,,NA,US,Eryops megacephalus
1340040,occ,NA,,180991,members,Diplocaulus cf. magnicornis,species,81712,,Diplocaulus magnicornis,NA,species,81712,Olson,1967,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-98.092766,34.164795,Waurika Site 1,NA,Waurika Locality,US,Oklahoma,Jefferson,based on nearby landmark,6,outcrop,"The site lies 6 miles west of the Waurika, Jefferson County, Oklahoma on the property of Price Shaeffer. Coordinates used here are approximate.",gp_mid,-28.99,-0.33,101,US,,,,,,,,,,,,NA,,Ryan-Aspaltum Sandstone lies 40 feet above the shale,"""shale""",gray,,,Y,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:41,12/08/2016 10:41,NA,magnicornis,Diplocaulus,28557,cf.,290.1,268,Leonard,,NA,US,Diplocaulus magnicornis
1340041,occ,NA,,180991,members,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Olson,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-98.092766,34.164795,Waurika Site 1,NA,Waurika Locality,US,Oklahoma,Jefferson,based on nearby landmark,6,outcrop,"The site lies 6 miles west of the Waurika, Jefferson County, Oklahoma on the property of Price Shaeffer. Coordinates used here are approximate.",gp_mid,-28.99,-0.33,101,US,,,,,,,,,,,,NA,,Ryan-Aspaltum Sandstone lies 40 feet above the shale,"""shale""",gray,,,Y,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:41,12/08/2016 10:41,NA,sp.,Diadectes,28557,,290.1,268,Leonard,,NA,US,Diadectes sp.
1340042,occ,NA,,180991,members,Ophiacodon retroversus,species,123420,,Ophiacodon retroversus,NA,species,138048,Olson,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-98.092766,34.164795,Waurika Site 1,NA,Waurika Locality,US,Oklahoma,Jefferson,based on nearby landmark,6,outcrop,"The site lies 6 miles west of the Waurika, Jefferson County, Oklahoma on the property of Price Shaeffer. Coordinates used here are approximate.",gp_mid,-28.99,-0.33,101,US,,,,,,,,,,,,NA,,Ryan-Aspaltum Sandstone lies 40 feet above the shale,"""shale""",gray,,,Y,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:41,12/08/2016 10:41,NA,retroversus,Ophiacodon,28557,,290.1,268,Leonard,,NA,US,Ophiacodon retroversus
1340043,occ,NA,,180991,members,Dimetrodon limbatus,species,344229,,Dimetrodon limbatus,NA,species,70401,Olson,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-98.092766,34.164795,Waurika Site 1,NA,Waurika Locality,US,Oklahoma,Jefferson,based on nearby landmark,6,outcrop,"The site lies 6 miles west of the Waurika, Jefferson County, Oklahoma on the property of Price Shaeffer. Coordinates used here are approximate.",gp_mid,-28.99,-0.33,101,US,,,,,,,,,,,,NA,,Ryan-Aspaltum Sandstone lies 40 feet above the shale,"""shale""",gray,,,Y,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:41,12/08/2016 10:41,NA,limbatus,Dimetrodon,28557,,290.1,268,Leonard,,NA,US,Dimetrodon limbatus
1340044,occ,NA,,180991,members,Edaphosaurus boanerges,species,122352,,Edaphosaurus boanerges,NA,species,122352,Olson,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,,-98.092766,34.164795,Waurika Site 1,NA,Waurika Locality,US,Oklahoma,Jefferson,based on nearby landmark,6,outcrop,"The site lies 6 miles west of the Waurika, Jefferson County, Oklahoma on the property of Price Shaeffer. Coordinates used here are approximate.",gp_mid,-28.99,-0.33,101,US,,,,,,,,,,,,NA,,Ryan-Aspaltum Sandstone lies 40 feet above the shale,"""shale""",gray,,,Y,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:41,12/08/2016 10:41,NA,boanerges,Edaphosaurus,28557,,290.1,268,Leonard,,NA,US,Edaphosaurus boanerges
1340045,occ,NA,,28275,,Cardiocephalus sternbergi,species,90715,,Cardiocephalus sternbergi,NA,species,90715,Olson,1967,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Gymnarthridae,37293,37294,NA,NA,NA,,-99.195557,33.973057,"Beaver Creek, 42 (Arroyo Formation)",NA,"Locality 42 (Romer 1928), Beaver Creek Wilbarger County, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Wilbarger,based on nearby landmark,seconds,outcrop,"""The upper reaches of the stream have yielded a few remains."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Beaver Creek.",gp_mid,-28.81,1.94,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""above the Lueders limestone, and quite probably correspond to the beds to the south of Coffee Creek."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Cardiocephalus,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:53,12/08/2016 10:53,7693,sternbergi,Cardiocephalus,28557,,279.3,272.3,Kungurian,,NA,US,Cardiocephalus sternbergi
1340046,occ,NA,,28275,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Olson,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-99.195557,33.973057,"Beaver Creek, 42 (Arroyo Formation)",NA,"Locality 42 (Romer 1928), Beaver Creek Wilbarger County, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Wilbarger,based on nearby landmark,seconds,outcrop,"""The upper reaches of the stream have yielded a few remains."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Beaver Creek.",gp_mid,-28.81,1.94,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""above the Lueders limestone, and quite probably correspond to the beds to the south of Coffee Creek."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:53,12/08/2016 10:53,7693,sp.,Diadectes,28557,,279.3,272.3,Kungurian,,NA,US,Diadectes sp.
1340047,occ,NA,,28275,,Dimetrodon grandis,species,122786,,Dimetrodon grandis,NA,species,138059,Olson,1967,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.195557,33.973057,"Beaver Creek, 42 (Arroyo Formation)",NA,"Locality 42 (Romer 1928), Beaver Creek Wilbarger County, faunal Zone 4, Lower Clear Fork Group, Texas red-beds, redbeds",US,Texas,Wilbarger,based on nearby landmark,seconds,outcrop,"""The upper reaches of the stream have yielded a few remains."" See detailed locality map in Romer 1928. ""Zone 4. Lower Clear Fork. Lat long is for Beaver Creek.",gp_mid,-28.81,1.94,101,US,,Arroyo,Clear Fork,,group of beds,,,,,,,NA,"""above the Lueders limestone, and quite probably correspond to the beds to the south of Coffee Creek."" Details for Faunal Zone 4 of Romer 1928: ""The vertebrate remains are confined to approximately the lowest 250 feet or so of the Clear Fork..""\nthe base and top of the Clear Fork Group (i.e., Arroyo, Vale, and Choza formations) are both within the Kungurian: see Wardlaw 2005 (Permophiles) for the base, and DiMichele et al. 2001 (J Paleont) for the top","""red beds... red clays, with small amounts of sandstone and conglomerates.""\r\n",claystone,red,,,Y,sandstone,,,conglomeratic,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,E. C. Olson. 1967. Early Permian Vertebrates. Oklahoma Geological Survey Circular 74:1-111,327,697,0,R. Butler,E. Dunne,,12/08/2016 10:53,12/08/2016 10:53,7693,grandis,Dimetrodon,28557,,279.3,272.3,Kungurian,,NA,US,Dimetrodon grandis
1340049,occ,NA,,180992,members,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Olson,1958,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-99.777496,33.669445,Locality BW (Lower Vale Fm.),NA,Alexander Ranch,US,Texas,Knox,based on nearby landmark,seconds,outcrop,For details see map in Olson (1958),gp_mid,-30.44,-0.02,101,US,,Vale,,Lower Vale,,,,,,,,NA,,for details see Olson (1958 p. 426),sandstone,,,,,conglomerate,,,,,"""floodplain""",,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,12/08/2016 11:09,12/08/2016 11:09,NA,sp.,Diplocaulus,58444,,290.1,268.8,Artinskian,Roadian,NA,US,Diplocaulus sp.
1340050,occ,NA,,180992,members,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Olson,1958,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-99.777496,33.669445,Locality BW (Lower Vale Fm.),NA,Alexander Ranch,US,Texas,Knox,based on nearby landmark,seconds,outcrop,For details see map in Olson (1958),gp_mid,-30.44,-0.02,101,US,,Vale,,Lower Vale,,,,,,,,NA,,for details see Olson (1958 p. 426),sandstone,,,,,conglomerate,,,,,"""floodplain""",,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,12/08/2016 11:09,12/08/2016 11:09,NA,sp.,Eryops,58444,,290.1,268.8,Artinskian,Roadian,NA,US,Eryops sp.
1340051,occ,NA,,180992,members,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Olson,1958,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-99.777496,33.669445,Locality BW (Lower Vale Fm.),NA,Alexander Ranch,US,Texas,Knox,based on nearby landmark,seconds,outcrop,For details see map in Olson (1958),gp_mid,-30.44,-0.02,101,US,,Vale,,Lower Vale,,,,,,,,NA,,for details see Olson (1958 p. 426),sandstone,,,,,conglomerate,,,,,"""floodplain""",,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,12/08/2016 11:09,12/08/2016 11:09,NA,sp.,Diadectes,58444,,290.1,268.8,Artinskian,Roadian,NA,US,Diadectes sp.
1340052,occ,NA,,180992,members,Dimetrodon gigashomogenes,species,138123,,Dimetrodon gigashomogenes,NA,species,138123,Olson,1958,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-99.777496,33.669445,Locality BW (Lower Vale Fm.),NA,Alexander Ranch,US,Texas,Knox,based on nearby landmark,seconds,outcrop,For details see map in Olson (1958),gp_mid,-30.44,-0.02,101,US,,Vale,,Lower Vale,,,,,,,,NA,,for details see Olson (1958 p. 426),sandstone,,,,,conglomerate,,,,,"""floodplain""",,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,field collection,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"E. C. Olson. 1958. Fauna of the Vale and Choza: Summary, Review, and Integration of the Geology and the Faunas. Fieldiana Geology 10(32):397-448",327,697,0,R. Butler,E. Dunne,,12/08/2016 11:09,12/08/2016 11:09,NA,gigashomogenes,Dimetrodon,58444,,290.1,268.8,Artinskian,Roadian,NA,US,Dimetrodon gigashomogenes
1340065,occ,NA,,80576,,n. gen. Ruthenosaurus n. sp. russellorum,species,345994,,Ruthenosaurus russellorum,NA,species,345994,Reisz et al.,2011,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,345993,NA,NA,NA,,2.42849,44.470924,Saint-Christophe-Vallon,NA,1km east of Saint Christophe Vallon,FR,Aveyron,,stated in text,6,outcrop,"""1 km east to the village of SaintChristophe-Vallon, town of Valady, departement of Aveyron, Southern France"" Reisz et al. (2011)",gp_mid,19.6,3.43,305,FR,,,Gr̬s Rouge,,,,,,,Rodez,M1-M2,NA,"""Top of the red pelitic beds of the M1 Member, Gr̬s Rouge Group of the Rodez Basin, Saxo-Thuringian, upper Sakmarian to lower Lopingian (Lopez et al. 2005, 2008), middle Early-early Late Permian."" Reisz et al. (2011)",,sandstone,red,,,Y,conglomerate,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,MNHN,,,,,,"The specimen MNHN.F.MCL-2 (Casea rutena) comes from the pelitic beds on the top of the first member (M1), whereas MNHN.F.MCL-1, found 120 m above stratigraphically, comes from the upper part of the second member (M2) (Bourges 1987; Gand pers. comm. 2009) - Reisz et al. (2011)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ruthenosaurus,n. gen.,NA,NA,vertebrate,"R. R. Reisz, H. C. Maddin, and J. Fr̦bisch, J. Falconnet. 2011. A new large caseid (Synapsida, Caseasauria) from the Permian of Rodez (France), including a reappraisal of Casea rutena Sigogneau-Russell & Russell, 1974. Geodiversitas 33(2):227-246",327,697,0,R. Butler,E. Dunne,,13/08/2016 11:02,13/08/2016 11:02,27105,russellorum,Ruthenosaurus,60098,n. sp.,295.5,254.17,Sakmarian,Wuchiapingian,NA,FR,Ruthenosaurus russellorum
1340066,occ,NA,,180994,members,Cotylorhynchus sp.,genus,38917,,Cotylorhynchus,NA,genus,38917,Ronchi et al.,2011,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Caseidae,38913,38917,NA,NA,NA,,8.188649,40.642159,Torre del Porticciolo,NA,,IT,Sassari,Alghero,stated in text,6,,"Locality lies near Torre del Porticciolo (Alghero, Nurra, NW Sardinia, Italy). Coordinates here are for Torre del Porticciolo.",gp_mid,NA,NA,coordinates not computable using this model,IT,,Cala del Vino,,,,,,,,,,NA," Autunian is a traditional European term, previously considered an age, which now indicates a characteristic flora. In any case, as stated by Broutin et al. (1999) and by Ronchi et al. (2008b), referring to the International Stratigraphic Chart by IUGS, it spans from the latest Ghzelian to the early Sakmarian.",,mudstone,red,poorly lithified,,,sandstone,"gray,green",,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Cotylorhynchus,,NA,NA,vertebrate,"A. Ronchi, E. Sacchi, and M. Romano, U. Nicosia. 2011. A huge caseid pelycosaur from northwestern Sardinia and its bearing on European Permian stratigraphy and palaeobiogeography. Acta Palaeontologica Polonica 56(4):723-738",327,697,0,R. Butler,E. Dunne,,13/08/2016 11:50,13/08/2016 11:50,NA,sp.,Cotylorhynchus,60100,,303.7,290.1,Gzhelian,Sakmarian,NA,IT,Cotylorhynchus sp.
1340342,occ,NA,,181051,members,Geosaurus n. sp. cynodus,species,138140,recombined as,Neosaurus cynodus,NA,species,138140,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38907,NA,NA,NA,,5.526073,47.19632,"Moissey, Jura Dept.",NA,,FR,Jura,,based on nearby landmark,6,small collection,Moissey is a commune in the Jura department in Franche-Comt̩ in eastern France. Lat long is for the centre of Moissey.,gp_mid,18.93,2.34,305,FR,,,,,,,,,,,,NA,"""Walchia beds""",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Geosaurus,,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,327,697,0,R. Butler,E. Dunne,,16/08/2016 04:49,16/08/2016 04:49,NA,cynodus,Neosaurus,27105,n. sp.,298.9,295,Autunian,,NA,FR,Neosaurus cynodus
1340343,occ,NA,,13080,,Dimetrodon booneorum,species,122783,,Dimetrodon booneorum,NA,species,122783,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-98.856941,33.622501,Briar Creek,NA,"(Admiral Formation) Locality 13 (Romer 1928), Locality IVd (Romer & Price 1940), faunal Zone 1, Wichita Group, Texas red-beds, redbeds; Brier Creek",US,Texas,Archer,based on nearby landmark,seconds,outcrop,"""the collecting ground being mainly on the east side a few miles from the mouth, near and in the bone bed discovered by Case."" Lat long is for Dundee, approx. 9 mi south of locality, but see detailed locality map in Romer 1928. ""Zone 1. Lower Wichita; to Godwin Creek; Admiral Formation?""; DMS coordinates are for the mouth of Briar Creek into Lake Kickapoo",gp_mid,-30.21,-1.18,101,US,,Admiral,Wichita,,bed,,,,,,,NA,"""about 190 feet above the Coleman Junction."" Details for Faunal Zone 1 of Romer 1928: ""These beds [estimated thickness of 350 feet] occupy the middle portion of the Wichita as Cummins conceived of it; but they are now seen to occupy the lower part of this group. This zone is approximately equivalent to the Admiral Formation of Plummer and Moore (1921), although no definite correlation can be made at present."" Lower Permian stratigraphy for Texas was modified by Hentz (1988).\r\nthe Admiral Formation and middle Wichita Group are both Artinskian according to Wardlaw 2005, Permophiles (JA)","red-beds, ""a series of typical red beds, consisting of clays, sandstone and shales, mostly red in color, and devoid of limestones."" ",claystone,red,,,,sandstone,red,,,,terrestrial indet.,,terrestrial and near-shore deposition,macrofossils,,,,,,NA,,body,,,,,#NAME?,,,,,NA,,,taxonomic,survey of museum collection,,,,,,,Romer (1928) paper is a review of vertebrates from the Texas red-beds with previously unreported (or undetailed) localities.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,327,697,0,R. Butler,E. Dunne,,16/08/2016 05:30,16/08/2016 05:30,7693,booneorum,Dimetrodon,27105,,290.1,279.3,Artinskian,,NA,US,Dimetrodon booneorum
1340352,occ,NA,,181054,members,n. gen. Ctenorhachis n. sp. jacksoni,species,346070,,Ctenorhachis jacksoni,NA,species,346070,Hook and Hotton,1991,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,346069,NA,NA,NA,,-99.022781,33.687222,SE of Fulda,NA,,US,Texas,Baylor,based on nearby landmark,seconds,small collection,"Texas and New Orleans Railroad Company survey, abstract 1351, section 94. \r\nLat long is for Fulda, approx. 2 miles northwest of locality.",gp_mid,-30.3,-1.05,101,US,,Petrolia,Wichita,,,,,,,,,NA,Belle Plain Formation of Romer (1974),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ctenorhachis,n. gen.,NA,NA,vertebrate,"R. W. Hook and N. Hotton. 1991. A New Sphenacodontid Pelycosaur (Synapsida) from the Wichita Group, Lower Permian of North-Central Texas. Journal of Vertebrate Paleontology 11(1):37-44",327,697,0,R. Butler,E. Dunne,,16/08/2016 11:28,16/08/2016 11:28,NA,jacksoni,Ctenorhachis,60131,n. sp.,290.1,279.3,Artinskian,,NA,US,Ctenorhachis jacksoni
1340454,occ,NA,,52522,,Naosaurus n. sp. credneri,species,346040,recombined as,Edaphosaurus credneri,NA,species,346040,Reisz,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,,13.650278,50.999722,Niederhaslich,NA,Niederh_sslich; Niederh_slich; Nieder-H_sslich; Plauenscher Grund; D̦hlen Basin,DE,Saxony,Weieritzkreis,based on nearby landmark,seconds,outcrop,"Niederh_slich in the D̦hlen basin, today it is one part of the City of Freital, SW of Dresden in Sachsen; the outcrop does not exist anymore.",gp_mid,23.3,7.73,305,DE,,Niederh_slich-Schweinsdorf,Rotliegend,Niederh_slich limestone,member,,,,,,,NA,"""The Niederh_slich Formation belongs stratigraphically [...] to the Melanerpeton gracile-M. pulcherimus Zone, i. e. uppermost Unterrotliegend"" (U. Hoffman, 2002, Workshop _Oberkarbon - Untertrias in Zentraleuropa: Prozesse und ihr Timing [online] http://www.geo.tu-freiberg.de/palaeo/GeoTage-2002.pdf) (TL);\r\nthe Niederh_slich limestone is Asselian according to assorted references, e.g., Gebhardt and Schneider 1993 (JA)\r\nAccording to Roscher & Schneider (2006, in Lucas et al. (eds), Geol. Soc. Spec. Publ. 265) the Niederh_slich Fm. is Sakmarian in age (TL).",,"""limestone""",,,,,,,,,,lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,"Museum: Staatliches Museum f_r Mineralogie und Geologie, Dresden (SMMGD)",,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Naosaurus,,NA,NA,vertebrate,R. R. Reisz. 1986. Pelycosauria. Handbuch der Pal_oherpetologie / Encyclopedia of Paleoherpetology 17A:1-102,327,697,697,R. Butler,E. Dunne,E. Dunne,17/08/2016 09:38,17/08/2016 09:39,14125,credneri,Edaphosaurus,27105,n. sp.,295.5,290.1,Sakmarian,,NA,DE,Edaphosaurus credneri
1340518,occ,NA,,181075,members,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Berman,1993,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-106.636665,36.120834,Cardillo Quarry,NA,,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"Loaction lies approximately 41km due east of Anderson Quarry, south of Arroyo del Agua village in Rio Arriba county, New Mexico.",gp_mid,-34.09,4.49,101,US,FED,Arroyo del Agua,Cutler,,,,,,,,,NA,,"""The Anderson quarry consists of light gray shale with lenses of crossbedded sandstone capped by numerous, light-colored marl layers. "" Lucas et al. (2005)",mudstone,,,,,sandstone,,,,,crevasse splay,,"""The sediments quite likely represent some aspect of a crevasse-splay or channel deposit""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,CMNH,1979-80,Collecting parties at the CMNH and the University of Toronto. Specimens reposited in the CMNH.,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 05:45,18/08/2016 05:45,NA,sp.,Eryops,60092,,296.4,268,Wolfcamp,,NA,US,Eryops sp.
1340519,occ,NA,,181075,members,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-106.636665,36.120834,Cardillo Quarry,NA,,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"Loaction lies approximately 41km due east of Anderson Quarry, south of Arroyo del Agua village in Rio Arriba county, New Mexico.",gp_mid,-34.09,4.49,101,US,FED,Arroyo del Agua,Cutler,,,,,,,,,NA,,"""The Anderson quarry consists of light gray shale with lenses of crossbedded sandstone capped by numerous, light-colored marl layers. "" Lucas et al. (2005)",mudstone,,,,,sandstone,,,,,crevasse splay,,"""The sediments quite likely represent some aspect of a crevasse-splay or channel deposit""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,CMNH,1979-80,Collecting parties at the CMNH and the University of Toronto. Specimens reposited in the CMNH.,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 05:45,18/08/2016 05:45,NA,sp.,Diadectes,60092,,296.4,268,Wolfcamp,,NA,US,Diadectes sp.
1340520,occ,NA,,181075,members,Captorhinidae indet.,family,37495,,Captorhinidae,NA,family,37495,Berman,1993,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,NA,NA,NA,NA,,-106.636665,36.120834,Cardillo Quarry,NA,,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"Loaction lies approximately 41km due east of Anderson Quarry, south of Arroyo del Agua village in Rio Arriba county, New Mexico.",gp_mid,-34.09,4.49,101,US,FED,Arroyo del Agua,Cutler,,,,,,,,,NA,,"""The Anderson quarry consists of light gray shale with lenses of crossbedded sandstone capped by numerous, light-colored marl layers. "" Lucas et al. (2005)",mudstone,,,,,sandstone,,,,,crevasse splay,,"""The sediments quite likely represent some aspect of a crevasse-splay or channel deposit""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,CMNH,1979-80,Collecting parties at the CMNH and the University of Toronto. Specimens reposited in the CMNH.,,terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinidae,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 05:45,18/08/2016 05:45,NA,indet.,,60092,,296.4,268,Wolfcamp,,NA,US, indet.
1340521,occ,NA,,181075,members,Ophiacodon sp.,genus,38888,,Ophiacodon,NA,genus,38888,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-106.636665,36.120834,Cardillo Quarry,NA,,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"Loaction lies approximately 41km due east of Anderson Quarry, south of Arroyo del Agua village in Rio Arriba county, New Mexico.",gp_mid,-34.09,4.49,101,US,FED,Arroyo del Agua,Cutler,,,,,,,,,NA,,"""The Anderson quarry consists of light gray shale with lenses of crossbedded sandstone capped by numerous, light-colored marl layers. "" Lucas et al. (2005)",mudstone,,,,,sandstone,,,,,crevasse splay,,"""The sediments quite likely represent some aspect of a crevasse-splay or channel deposit""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,CMNH,1979-80,Collecting parties at the CMNH and the University of Toronto. Specimens reposited in the CMNH.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 05:45,18/08/2016 05:45,NA,sp.,Ophiacodon,60092,,296.4,268,Wolfcamp,,NA,US,Ophiacodon sp.
1340522,occ,NA,,181075,members,Sphenacodon sp.,genus,38909,,Sphenacodon,NA,genus,38909,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,,-106.636665,36.120834,Cardillo Quarry,NA,,US,New Mexico,Rio Arriba,stated in text,seconds,outcrop,"Loaction lies approximately 41km due east of Anderson Quarry, south of Arroyo del Agua village in Rio Arriba county, New Mexico.",gp_mid,-34.09,4.49,101,US,FED,Arroyo del Agua,Cutler,,,,,,,,,NA,,"""The Anderson quarry consists of light gray shale with lenses of crossbedded sandstone capped by numerous, light-colored marl layers. "" Lucas et al. (2005)",mudstone,,,,,sandstone,,,,,crevasse splay,,"""The sediments quite likely represent some aspect of a crevasse-splay or channel deposit""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,CMNH,1979-80,Collecting parties at the CMNH and the University of Toronto. Specimens reposited in the CMNH.,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 05:45,18/08/2016 05:45,NA,sp.,Sphenacodon,60092,,296.4,268,Wolfcamp,,NA,US,Sphenacodon sp.
1340524,occ,NA,,34761,,Embolomeri indet.,suborder,37178,,Embolomeri,NA,suborder,37178,Berman,1993,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Embolomeri,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 06:31,18/08/2016 06:31,43845,indet.,,60092,,303.4,298.9,Virgilian,,NA,US, indet.
1340525,occ,NA,,34761,,Diasparactus zenos,species,157286,recombined as,Diadectes zenos,NA,species,157286,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-106.345558,36.305557,El Cobre Canyon (Cutler Formation),NA,El Cabre (Cope Collection),US,New Mexico,Rio Arriba,estimated from map,seconds,local area,"El Cabre locality in Case 1907; ""El Cobre"" locality in AMNH Collections data.\r\n""There is in the Cope Collection a considerable quantity of material from New Mexico, El Cabre and Arroyo de Agua, names that do not appear on the maps."" (Case 1907)\r\nEl Cobre Canyon is located approximately 8 km northwest of the village of Abiquiu, Rio Arriba County, New Mexico (Berman, 1993). Lat Long is for center of canyon.",gp_mid,-34.62,3.06,101,US,FED,Cutler,,,,,,,,,,NA,"Based on the biostratigraphic information provided by two floral taxa, Alethopteris serlii and Neuropteris scheuchzeri, Fracasso (1980) argued for an Upper Pennsylvanian Missourian assignment, but Berman et al. (1997), while acknowledging a Late Pennsylvanian age, suggested that the beds of the canyon floor are latest Virgilian in age.",,"""siliciclastic""",,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,frequent,NA,,"""Only fragments of dissociated skeletons were found, individual elements for the most part"" (Vaughn, 1963)",taxonomic,"field collection,survey of museum collection","AMNH,FMNH,MCZ,YPM",,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diasparactus,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 06:31,18/08/2016 06:31,43845,zenos,Diadectes,60092,,303.4,298.9,Virgilian,,NA,US,Diadectes zenos
1340526,occ,NA,,180974,members,Dimetrodon occidentalis,species,123425,,Dimetrodon occidentalis,NA,species,123425,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-106.691673,35.772633,Jemez Springs,NA,,US,New Mexico,Sandoval,based on nearby landmark,6,small collection,"Lat long is for the centre of Jemez Springs, Sandoval County, New Mexico.",gp_mid,-34.33,4.24,101,US,FED,Abo,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)",siltstone,"coarse,gray",poorly lithified,,Y,sandstone,red,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 06:36,18/08/2016 06:36,NA,occidentalis,Dimetrodon,60092,,296.4,268,Wolfcamp,,NA,US,Dimetrodon occidentalis
1340527,occ,NA,,180974,members,Dimetrodon cf. occidentalis,species,123425,,Dimetrodon occidentalis,NA,species,123425,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-106.691673,35.772633,Jemez Springs,NA,,US,New Mexico,Sandoval,based on nearby landmark,6,small collection,"Lat long is for the centre of Jemez Springs, Sandoval County, New Mexico.",gp_mid,-34.33,4.24,101,US,FED,Abo,,,bed,,,,,,,NA,"""The fossiliferous levels of the Abo Formation in the vicinity of Jemez Springs are [...] probably latest Wolfcampian in age"" (Berman, 1977)","""red-mottled micaceous arkose""\r\n""red shale and coarse-grained stream channel sand"" (Berman, 1977)",siltstone,"coarse,gray",poorly lithified,,Y,sandstone,red,,,Y,fluvial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 06:36,18/08/2016 06:36,NA,occidentalis,Dimetrodon,60092,cf.,296.4,268,Wolfcamp,,NA,US,Dimetrodon occidentalis
1340528,occ,NA,,181076,members,Sphenacodon n. sp. ferocior,species,122488,,Sphenacodon ferocior,NA,species,122488,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,,-106.693993,35.750134,Spanish Queen mine locality,NA,Jemez Springs,US,New Mexico,Sandoval,based on nearby landmark,6,small collection,Locality lies about 6.5km south of Jemez Springs,gp_mid,-34.35,4.22,101,US,FED,Abo,,Lower,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,A. S. Romer,1931,Later the site was visited by a party from the University of California (Berkeley),,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,697,R. Butler,E. Dunne,E. Dunne,18/08/2016 06:45,18/08/2016 06:46,NA,ferocior,Sphenacodon,60092,n. sp.,296.4,268,Wolfcamp,,NA,US,Sphenacodon ferocior
1340529,occ,NA,,181076,members,cf. Archeria sp.,genus,37196,,Archeria,NA,genus,37196,Berman,1993,Chordata,33815,Osteichthyes,34881,,NA,Archeriidae,37195,37196,NA,NA,NA,,-106.693993,35.750134,Spanish Queen mine locality,NA,Jemez Springs,US,New Mexico,Sandoval,based on nearby landmark,6,small collection,Locality lies about 6.5km south of Jemez Springs,gp_mid,-34.35,4.22,101,US,FED,Abo,,Lower,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,A. S. Romer,1931,Later the site was visited by a party from the University of California (Berkeley),,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Archeria,cf.,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 06:45,18/08/2016 06:45,NA,sp.,Archeria,60092,,296.4,268,Wolfcamp,,NA,US,Archeria sp.
1340530,occ,NA,,85436,,Zatrachys sp.,genus,37056,,Zatrachys,NA,genus,37056,Berman,1993,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Zatracheidae,37053,37056,NA,NA,NA,,-106.748055,34.173889,NE Socorro,NA,Gallina Well,US,New Mexico,Socorro,estimated from map,seconds,small collection,"""about 20 (or 19.2km) km northeast of Socorro [...] in SE1/4 NE1/4 W1/4 of sec. 14, T. 2 S., R. 3 E""",gp_mid,-35.31,2.97,101,US,FED,Abo/Cutler,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""elements of the skull and postcranial skeleton of an individual that are randomly associated and densely concentrated in a small, strongly indurated, red concretion""",taxonomic,,,,,,"D. S. Berman, R. R. Reisz",,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Zatrachys,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 06:52,18/08/2016 06:52,28464,sp.,Zatrachys,60092,,296.4,268,Wolfcamp,,NA,US,Zatrachys sp.
1340531,occ,NA,,85436,,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Berman,1993,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-106.748055,34.173889,NE Socorro,NA,Gallina Well,US,New Mexico,Socorro,estimated from map,seconds,small collection,"""about 20 (or 19.2km) km northeast of Socorro [...] in SE1/4 NE1/4 W1/4 of sec. 14, T. 2 S., R. 3 E""",gp_mid,-35.31,2.97,101,US,FED,Abo/Cutler,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""elements of the skull and postcranial skeleton of an individual that are randomly associated and densely concentrated in a small, strongly indurated, red concretion""",taxonomic,,,,,,"D. S. Berman, R. R. Reisz",,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 06:52,18/08/2016 06:52,28464,sp.,Trimerorhachis,60092,,296.4,268,Wolfcamp,,NA,US,Trimerorhachis sp.
1340532,occ,NA,,85436,,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Berman,1993,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-106.748055,34.173889,NE Socorro,NA,Gallina Well,US,New Mexico,Socorro,estimated from map,seconds,small collection,"""about 20 (or 19.2km) km northeast of Socorro [...] in SE1/4 NE1/4 W1/4 of sec. 14, T. 2 S., R. 3 E""",gp_mid,-35.31,2.97,101,US,FED,Abo/Cutler,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""elements of the skull and postcranial skeleton of an individual that are randomly associated and densely concentrated in a small, strongly indurated, red concretion""",taxonomic,,,,,,"D. S. Berman, R. R. Reisz",,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 06:52,18/08/2016 06:52,28464,sp.,Diplocaulus,60092,,296.4,268,Wolfcamp,,NA,US,Diplocaulus sp.
1340533,occ,NA,,85436,,Diadectes sp.,genus,37247,,Diadectes,NA,genus,37247,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,,-106.748055,34.173889,NE Socorro,NA,Gallina Well,US,New Mexico,Socorro,estimated from map,seconds,small collection,"""about 20 (or 19.2km) km northeast of Socorro [...] in SE1/4 NE1/4 W1/4 of sec. 14, T. 2 S., R. 3 E""",gp_mid,-35.31,2.97,101,US,FED,Abo/Cutler,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""elements of the skull and postcranial skeleton of an individual that are randomly associated and densely concentrated in a small, strongly indurated, red concretion""",taxonomic,,,,,,"D. S. Berman, R. R. Reisz",,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diadectes,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 06:52,18/08/2016 06:52,28464,sp.,Diadectes,60092,,296.4,268,Wolfcamp,,NA,US,Diadectes sp.
1340534,occ,NA,,85436,,Sphenacodon sp.,genus,38909,,Sphenacodon,NA,genus,38909,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,,-106.748055,34.173889,NE Socorro,NA,Gallina Well,US,New Mexico,Socorro,estimated from map,seconds,small collection,"""about 20 (or 19.2km) km northeast of Socorro [...] in SE1/4 NE1/4 W1/4 of sec. 14, T. 2 S., R. 3 E""",gp_mid,-35.31,2.97,101,US,FED,Abo/Cutler,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""elements of the skull and postcranial skeleton of an individual that are randomly associated and densely concentrated in a small, strongly indurated, red concretion""",taxonomic,,,,,,"D. S. Berman, R. R. Reisz",,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 06:52,18/08/2016 06:52,28464,sp.,Sphenacodon,60092,,296.4,268,Wolfcamp,,NA,US,Sphenacodon sp.
1340535,occ,NA,,85436,,Onchiodon ? sp.,genus,37013,,Onchiodon,NA,genus,37013,Berman,1993,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37013,NA,NA,NA,,-106.748055,34.173889,NE Socorro,NA,Gallina Well,US,New Mexico,Socorro,estimated from map,seconds,small collection,"""about 20 (or 19.2km) km northeast of Socorro [...] in SE1/4 NE1/4 W1/4 of sec. 14, T. 2 S., R. 3 E""",gp_mid,-35.31,2.97,101,US,FED,Abo/Cutler,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,"body,concretion",,,,,,,,,,NA,,"""elements of the skull and postcranial skeleton of an individual that are randomly associated and densely concentrated in a small, strongly indurated, red concretion""",taxonomic,,,,,,"D. S. Berman, R. R. Reisz",,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Onchiodon,?,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 06:52,18/08/2016 06:52,28464,sp.,Onchiodon,60092,,296.4,268,Wolfcamp,,NA,US,Onchiodon sp.
1340538,occ,NA,,180989,members,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Berman,1993,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,,-107.182503,34.639999,Pecos River Valley Locality (Sangre de Cristo),NA,,US,New Mexico,San Miguel,estimated from map,seconds,outcrop,"The fossils were collected from scattered sites along the upper reaches of the Pecos River drainage from Glorieta Pass at Glorieta on the eastern border of Santa Fe County souteastward to about 8km south of Ribera in San Miguel County. The coordinates here are based on half way between these 2 points, close to Highway 25",gp_mid,-35.7,2.91,101,US,,Sangre de Cristo,,,,,,,,,,NA,Sangre de Cristo Formation = Gzhelian - Sakmarian (Wellstead 1991),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 08:26,18/08/2016 08:26,NA,sp.,Eryops,60092,,303.7,290.1,Gzhelian,Sakmarian,NA,US,Eryops sp.
1340539,occ,NA,,180989,members,cf. Platyhystrix rugosus,species,345923,,Platyhystrix rugosus,NA,species,194929,Berman,1993,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37034,NA,NA,NA,,-107.182503,34.639999,Pecos River Valley Locality (Sangre de Cristo),NA,,US,New Mexico,San Miguel,estimated from map,seconds,outcrop,"The fossils were collected from scattered sites along the upper reaches of the Pecos River drainage from Glorieta Pass at Glorieta on the eastern border of Santa Fe County souteastward to about 8km south of Ribera in San Miguel County. The coordinates here are based on half way between these 2 points, close to Highway 25",gp_mid,-35.7,2.91,101,US,,Sangre de Cristo,,,,,,,,,,NA,Sangre de Cristo Formation = Gzhelian - Sakmarian (Wellstead 1991),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Platyhystrix,cf.,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 08:26,18/08/2016 08:26,NA,rugosus,Platyhystrix,60092,,303.7,290.1,Gzhelian,Sakmarian,NA,US,Platyhystrix rugosus
1340540,occ,NA,,180989,members,Phlegethontia sp.,genus,37259,,Phlegethontia,NA,genus,37259,Berman,1993,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,37259,NA,NA,NA,,-107.182503,34.639999,Pecos River Valley Locality (Sangre de Cristo),NA,,US,New Mexico,San Miguel,estimated from map,seconds,outcrop,"The fossils were collected from scattered sites along the upper reaches of the Pecos River drainage from Glorieta Pass at Glorieta on the eastern border of Santa Fe County souteastward to about 8km south of Ribera in San Miguel County. The coordinates here are based on half way between these 2 points, close to Highway 25",gp_mid,-35.7,2.91,101,US,,Sangre de Cristo,,,,,,,,,,NA,Sangre de Cristo Formation = Gzhelian - Sakmarian (Wellstead 1991),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Phlegethontia,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 08:26,18/08/2016 08:26,NA,sp.,Phlegethontia,60092,,303.7,290.1,Gzhelian,Sakmarian,NA,US,Phlegethontia sp.
1340541,occ,NA,,180989,members,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Berman,1993,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-107.182503,34.639999,Pecos River Valley Locality (Sangre de Cristo),NA,,US,New Mexico,San Miguel,estimated from map,seconds,outcrop,"The fossils were collected from scattered sites along the upper reaches of the Pecos River drainage from Glorieta Pass at Glorieta on the eastern border of Santa Fe County souteastward to about 8km south of Ribera in San Miguel County. The coordinates here are based on half way between these 2 points, close to Highway 25",gp_mid,-35.7,2.91,101,US,,Sangre de Cristo,,,,,,,,,,NA,Sangre de Cristo Formation = Gzhelian - Sakmarian (Wellstead 1991),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 08:26,18/08/2016 08:26,NA,sp.,Diplocaulus,60092,,303.7,290.1,Gzhelian,Sakmarian,NA,US,Diplocaulus sp.
1340542,occ,NA,,180989,members,Lysorophus sp.,genus,37322,,Lysorophus,NA,genus,37322,Berman,1993,Chordata,33815,Osteichthyes,34881,Lysorophia,37319,,NA,37322,NA,NA,NA,,-107.182503,34.639999,Pecos River Valley Locality (Sangre de Cristo),NA,,US,New Mexico,San Miguel,estimated from map,seconds,outcrop,"The fossils were collected from scattered sites along the upper reaches of the Pecos River drainage from Glorieta Pass at Glorieta on the eastern border of Santa Fe County souteastward to about 8km south of Ribera in San Miguel County. The coordinates here are based on half way between these 2 points, close to Highway 25",gp_mid,-35.7,2.91,101,US,,Sangre de Cristo,,,,,,,,,,NA,Sangre de Cristo Formation = Gzhelian - Sakmarian (Wellstead 1991),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Lysorophus,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 08:26,18/08/2016 08:26,NA,sp.,Lysorophus,60092,,303.7,290.1,Gzhelian,Sakmarian,NA,US,Lysorophus sp.
1340543,occ,NA,,180989,members,Ophiacodon sp.,genus,38888,,Ophiacodon,NA,genus,38888,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-107.182503,34.639999,Pecos River Valley Locality (Sangre de Cristo),NA,,US,New Mexico,San Miguel,estimated from map,seconds,outcrop,"The fossils were collected from scattered sites along the upper reaches of the Pecos River drainage from Glorieta Pass at Glorieta on the eastern border of Santa Fe County souteastward to about 8km south of Ribera in San Miguel County. The coordinates here are based on half way between these 2 points, close to Highway 25",gp_mid,-35.7,2.91,101,US,,Sangre de Cristo,,,,,,,,,,NA,Sangre de Cristo Formation = Gzhelian - Sakmarian (Wellstead 1991),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 08:26,18/08/2016 08:26,NA,sp.,Ophiacodon,60092,,303.7,290.1,Gzhelian,Sakmarian,NA,US,Ophiacodon sp.
1340546,occ,NA,,181077,members,cf. Edops sp.,genus,37005,,Edops,NA,genus,37005,Berman,1993,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Edopidae,37004,37005,NA,NA,NA,,-106.082054,33.076641,Tularosa Locality,NA,,US,New Mexico,Otero,based on nearby landmark,6,small collection,"Locality lies 3.2km west of the town of Tularosa, Otero County. Sites from which fossils have been collected are scattered along a 20km NW-SE line at this point.",gp_mid,-35.51,1.76,101,US,,Laborcita,,,,,,,,,,NA,Stratigraphy determined by Vaughn (1969),,not reported,,,,,,,,,,"""floodplain""",,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Most specimens are housed at the CMNH,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Edops,cf.,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 08:41,18/08/2016 08:41,NA,sp.,Edops,60092,,296.4,268,Wolfcamp,,NA,US,Edops sp.
1340547,occ,NA,,181077,members,Platyhystrix cf. rugosus,species,345923,,Platyhystrix rugosus,NA,species,194929,Berman,1993,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37034,NA,NA,NA,,-106.082054,33.076641,Tularosa Locality,NA,,US,New Mexico,Otero,based on nearby landmark,6,small collection,"Locality lies 3.2km west of the town of Tularosa, Otero County. Sites from which fossils have been collected are scattered along a 20km NW-SE line at this point.",gp_mid,-35.51,1.76,101,US,,Laborcita,,,,,,,,,,NA,Stratigraphy determined by Vaughn (1969),,not reported,,,,,,,,,,"""floodplain""",,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Most specimens are housed at the CMNH,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Platyhystrix,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 08:41,18/08/2016 08:41,NA,rugosus,Platyhystrix,60092,cf.,296.4,268,Wolfcamp,,NA,US,Platyhystrix rugosus
1340548,occ,NA,,181077,members,Ophiacodon sp.,genus,38888,,Ophiacodon,NA,genus,38888,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-106.082054,33.076641,Tularosa Locality,NA,,US,New Mexico,Otero,based on nearby landmark,6,small collection,"Locality lies 3.2km west of the town of Tularosa, Otero County. Sites from which fossils have been collected are scattered along a 20km NW-SE line at this point.",gp_mid,-35.51,1.76,101,US,,Laborcita,,,,,,,,,,NA,Stratigraphy determined by Vaughn (1969),,not reported,,,,,,,,,,"""floodplain""",,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Most specimens are housed at the CMNH,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 08:41,18/08/2016 08:41,NA,sp.,Ophiacodon,60092,,296.4,268,Wolfcamp,,NA,US,Ophiacodon sp.
1340549,occ,NA,,181077,members,Sphenacodon cf. ferox,species,122487,,Sphenacodon ferox,NA,species,122487,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,,-106.082054,33.076641,Tularosa Locality,NA,,US,New Mexico,Otero,based on nearby landmark,6,small collection,"Locality lies 3.2km west of the town of Tularosa, Otero County. Sites from which fossils have been collected are scattered along a 20km NW-SE line at this point.",gp_mid,-35.51,1.76,101,US,,Laborcita,,,,,,,,,,NA,Stratigraphy determined by Vaughn (1969),,not reported,,,,,,,,,,"""floodplain""",,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Most specimens are housed at the CMNH,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 08:41,18/08/2016 08:41,NA,ferox,Sphenacodon,60092,cf.,296.4,268,Wolfcamp,,NA,US,Sphenacodon ferox
1340550,occ,NA,,181077,members,Sphenacodon sp.,genus,38909,,Sphenacodon,NA,genus,38909,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38909,NA,NA,NA,,-106.082054,33.076641,Tularosa Locality,NA,,US,New Mexico,Otero,based on nearby landmark,6,small collection,"Locality lies 3.2km west of the town of Tularosa, Otero County. Sites from which fossils have been collected are scattered along a 20km NW-SE line at this point.",gp_mid,-35.51,1.76,101,US,,Laborcita,,,,,,,,,,NA,Stratigraphy determined by Vaughn (1969),,not reported,,,,,,,,,,"""floodplain""",,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Most specimens are housed at the CMNH,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Sphenacodon,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 08:41,18/08/2016 08:41,NA,sp.,Sphenacodon,60092,,296.4,268,Wolfcamp,,NA,US,Sphenacodon sp.
1340551,occ,NA,,181077,members,Edaphosaurus cf. novomexicanus,species,122351,,Edaphosaurus novomexicanus,NA,species,122351,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,38911,NA,NA,NA,,-106.082054,33.076641,Tularosa Locality,NA,,US,New Mexico,Otero,based on nearby landmark,6,small collection,"Locality lies 3.2km west of the town of Tularosa, Otero County. Sites from which fossils have been collected are scattered along a 20km NW-SE line at this point.",gp_mid,-35.51,1.76,101,US,,Laborcita,,,,,,,,,,NA,Stratigraphy determined by Vaughn (1969),,not reported,,,,,,,,,,"""floodplain""",,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Most specimens are housed at the CMNH,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 08:41,18/08/2016 08:41,NA,novomexicanus,Edaphosaurus,60092,cf.,296.4,268,Wolfcamp,,NA,US,Edaphosaurus novomexicanus
1340552,occ,NA,,181037,members,Dimetrodon aff. limbatus,species,344229,,Dimetrodon limbatus,NA,species,70401,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Sphenacodontidae,38901,38904,NA,NA,NA,,-107.222656,33.068935,Caballo Mountains locality,NA,near Truth or Consequences,US,New Mexico,Sierra,stated in text,6,small collection,"The locality lies on the eastern flank of the Caballo Mountains in Sierra County, NM, close to the spa city of Truth or Consequences.",gp_mid,-36.29,2.32,101,US,FED,Abo,,,,,,,,,,NA,Stratigraphy comes from Vaughn (1969b),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Specimens are primarily housed at CMNH,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Dimetrodon,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 09:57,18/08/2016 09:57,NA,limbatus,Dimetrodon,60092,aff.,296.4,268,Wolfcamp,,NA,US,Dimetrodon limbatus
1340553,occ,NA,,181037,members,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Berman,1993,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-107.222656,33.068935,Caballo Mountains locality,NA,near Truth or Consequences,US,New Mexico,Sierra,stated in text,6,small collection,"The locality lies on the eastern flank of the Caballo Mountains in Sierra County, NM, close to the spa city of Truth or Consequences.",gp_mid,-36.29,2.32,101,US,FED,Abo,,,,,,,,,,NA,Stratigraphy comes from Vaughn (1969b),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Specimens are primarily housed at CMNH,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 09:57,18/08/2016 09:57,NA,sp.,Trimerorhachis,60092,,296.4,268,Wolfcamp,,NA,US,Trimerorhachis sp.
1340554,occ,NA,,181037,members,Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Berman,1993,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-107.222656,33.068935,Caballo Mountains locality,NA,near Truth or Consequences,US,New Mexico,Sierra,stated in text,6,small collection,"The locality lies on the eastern flank of the Caballo Mountains in Sierra County, NM, close to the spa city of Truth or Consequences.",gp_mid,-36.29,2.32,101,US,FED,Abo,,,,,,,,,,NA,Stratigraphy comes from Vaughn (1969b),,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Specimens are primarily housed at CMNH,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 09:57,18/08/2016 09:57,NA,sp.,Diplocaulus,60092,,296.4,268,Wolfcamp,,NA,US,Diplocaulus sp.
1340555,occ,NA,,180988,members,Embolomeri indet.,suborder,37178,,Embolomeri,NA,suborder,37178,Berman,1993,Chordata,33815,Osteichthyes,34881,,NA,,NA,NA,NA,NA,NA,,-107.182503,34.639999,Sierra Lucero Locality,NA,,US,New Mexico,Cibola,stated in text,seconds,outcrop,"Vertebrate fossils were discovered and collected by the author in 1975 at numerous sites in a 10km long, narrow, north-south strip of Lower Permian Abo Formation exposure lying about 8km east of Sierra Lucero and 29km west of Interstate Highway 25 at Los Lunas in Valencia County.",gp_mid,-35.35,3.52,101,US,,Abo,,,,,,,,,,NA,"Abo Formation = Lower Permian (middle-upper Wolfcampian) (Lucas et al., 2015)",,not reported,,,,,,,,,,coastal indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,Berman,1975,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Embolomeri,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 09:59,18/08/2016 09:59,NA,indet.,,60092,,295.5,279.3,Sakmarian,Artinskian,NA,US, indet.
1340557,occ,NA,,181078,members,Trimerorhachis sp.,genus,36991,,Trimerorhachis,NA,genus,36991,Berman,1993,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,36991,NA,NA,NA,,-106.536942,34.305,Los Pinos Mountains locality,NA,,US,New Mexico,Socorro,based on nearby landmark,seconds,small collection,Locality consists of 2 sites about 30km east of Interstate Highway and near the eastern margin of Los Pino Mountains.,gp_mid,-35.1,2.98,101,US,FED,Abo,,,,,,,,,,NA,Site lies close to the contact between the Abo and underlying Bursum Formation,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Specimens from both sites are reposited in the CMNH,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachis,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 10:04,18/08/2016 10:04,NA,sp.,Trimerorhachis,60092,,296.4,268,Wolfcamp,,NA,US,Trimerorhachis sp.
1340558,occ,NA,,181078,members,aff. Diplocaulus sp.,genus,37264,,Diplocaulus,NA,genus,37264,Berman,1993,Chordata,33815,Osteichthyes,34881,,NA,Diplocaulidae,142457,37264,NA,NA,NA,,-106.536942,34.305,Los Pinos Mountains locality,NA,,US,New Mexico,Socorro,based on nearby landmark,seconds,small collection,Locality consists of 2 sites about 30km east of Interstate Highway and near the eastern margin of Los Pino Mountains.,gp_mid,-35.1,2.98,101,US,FED,Abo,,,,,,,,,,NA,Site lies close to the contact between the Abo and underlying Bursum Formation,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Specimens from both sites are reposited in the CMNH,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Diplocaulus,aff.,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 10:04,18/08/2016 10:04,NA,sp.,Diplocaulus,60092,,296.4,268,Wolfcamp,,NA,US,Diplocaulus sp.
1340559,occ,NA,,181078,members,Platyhystrix sp.,genus,37034,,Platyhystrix,NA,genus,37034,Berman,1993,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37034,NA,NA,NA,,-106.536942,34.305,Los Pinos Mountains locality,NA,,US,New Mexico,Socorro,based on nearby landmark,seconds,small collection,Locality consists of 2 sites about 30km east of Interstate Highway and near the eastern margin of Los Pino Mountains.,gp_mid,-35.1,2.98,101,US,FED,Abo,,,,,,,,,,NA,Site lies close to the contact between the Abo and underlying Bursum Formation,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Specimens from both sites are reposited in the CMNH,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Platyhystrix,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 10:04,18/08/2016 10:04,NA,sp.,Platyhystrix,60092,,296.4,268,Wolfcamp,,NA,US,Platyhystrix sp.
1340560,occ,NA,,181078,members,Phlegethontia sp.,genus,37259,,Phlegethontia,NA,genus,37259,Berman,1993,Chordata,33815,Osteichthyes,34881,Aistopoda,37251,Phlegethontiidae,37257,37259,NA,NA,NA,,-106.536942,34.305,Los Pinos Mountains locality,NA,,US,New Mexico,Socorro,based on nearby landmark,seconds,small collection,Locality consists of 2 sites about 30km east of Interstate Highway and near the eastern margin of Los Pino Mountains.,gp_mid,-35.1,2.98,101,US,FED,Abo,,,,,,,,,,NA,Site lies close to the contact between the Abo and underlying Bursum Formation,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Specimens from both sites are reposited in the CMNH,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Phlegethontia,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 10:04,18/08/2016 10:04,NA,sp.,Phlegethontia,60092,,296.4,268,Wolfcamp,,NA,US,Phlegethontia sp.
1340561,occ,NA,,181078,members,Ophiacodon sp.,genus,38888,,Ophiacodon,NA,genus,38888,Berman,1993,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Ophiacodontidae,38884,38888,NA,NA,NA,,-106.536942,34.305,Los Pinos Mountains locality,NA,,US,New Mexico,Socorro,based on nearby landmark,seconds,small collection,Locality consists of 2 sites about 30km east of Interstate Highway and near the eastern margin of Los Pino Mountains.,gp_mid,-35.1,2.98,101,US,FED,Abo,,,,,,,,,,NA,Site lies close to the contact between the Abo and underlying Bursum Formation,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,Specimens from both sites are reposited in the CMNH,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ophiacodon,,NA,NA,vertebrate,"D. S. Berman. 1993. Lower Permian vertebrate localities of New Mexico and their assemblages. In S. G. Lucas, J. Zidek (eds.), Vertebrate Paleontology of New Mexico. New Mexico Museum of Natural History and Science Bulletin 2 ",327,697,0,R. Butler,E. Dunne,,18/08/2016 10:04,18/08/2016 10:04,NA,sp.,Ophiacodon,60092,,296.4,268,Wolfcamp,,NA,US,Ophiacodon sp.
1340562,occ,NA,,80720,,Broiliellus n. sp. hektotopos,species,346153,nomen dubium,Broiliellus,NA,genus,37024,Lucas,2013,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37024,NA,NA,NA,,-80.933334,39.766666,"Locality 6, near Cameron",NA,,US,Ohio,Monroe,based on nearby landmark,minutes,,"Locality 6, near Cameron",gp_mid,-14.93,-2.65,101,US,,,Washington,,,,,,,,,NA,"Dunkard series = Asselian - Sakmarian (Wellstead, 1991)",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Broiliellus,,NA,NA,vertebrate,"S. G. Lucas. 2013. Vertebrate biostratigraphy and biochronology of the upper Paleozoic Dunkard Group, PennsylvaniaWest VirginiaOhio, USA. International Journal of Coal geology 119:79-87",327,697,697,R. Butler,E. Dunne,E. Dunne,18/08/2016 10:13,18/08/2016 10:22,27105,hektotopos,Broiliellus,60155,n. sp.,298.9,290.1,Asselian,Sakmarian,NA,US,Broiliellus hektotopos
1340563,occ,NA,,22670,,Otocoelus testudineus,species,138239,subjective synonym of,Dissorophus multicinctus,NA,species,255227,Cummins,1908,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Dissorophidae,37017,37027,NA,NA,NA,,-99.233299,33.783298,Gray Creek,NA,"ETE Locality 1545, Gray Creek, ",US,Texas,,,4,,,gp_mid,-28.93,1.79,101,US,,,,,,,,,,,,NA,"ETE dating method: time_unit, ETE age comment: . radiometric intage_max, radiometric intage_min\r\noriginally entered as Asselian to Olenekian\r\n","ETE rock type adj: 0, ETE lithology comments: .",not reported,,,,,,,,,,terrestrial indet.,,"ETE sed env 1: ., ETE sed env 2: . ETE event: burrow, ETE env comment: burow collapse",,,,,,,NA,,,,,,,,,,,,NA,,"ETE Abrasion: ., ETE Assemblage formation: mass_death, ETE transport: ., ETE weathering/trampling: ., ETE part concentration: ., ETE time represented: . ,ETE vert pres: ., ETE invert pres: ., ETE plant pres: .",taxonomic,,,,4 specimens,,,,"ETE Size: .; ETE reference list: 478, ; ETE museum list: ",,"brackish,freshwater,terrestrial",NA,actively mobile,ground dwelling,NA,carnivore,,,hydroxyapatite,,NA,,Otocoelus,,NA,NA,,W. F. Cummins. 1908. The Localities and Horizons of Permian Vertebrate Fossils in Texas. Journal of Geology 16(8):737-745,327,697,0,R. Butler,E. Dunne,,18/08/2016 11:51,18/08/2016 11:51,5719,testudineus,Dissorophus,30068,,279.3,272.3,Kungurian,,NA,US,Dissorophus testudineus
1340589,occ,NA,,181085,members,n. gen. Utegenia n. sp. shpinari,species,346161,,Utegenia shpinari,NA,species,346161,Kuznetsov and Ivakhnenko,1981,Chordata,33815,Osteichthyes,34881,,NA,,NA,37212,NA,NA,NA,specimens,76.720001,44.259998,Kurty locality,NA,Zhal-Pak-Tas granite quarry,,Alma-Ata Region,Kaskelenskiy District,based on nearby landmark,2,small collection,"Kurty locality, 8 km NW of Zhal-Pak-Tas granite quarry, Almaty Province, southern Kazakhstan.",gp_mid,75.24,23.48,402,,,Kugaly,,,,,,,,,,NA,"Kugaly Formation, which is Late Pennsylvanian or Early Permian in age. All seymouriamorphs are Permian in age, including the Middle Permian Urumqia liudaowanensis from Xinjiang, China, which was synonymized under Utegenia shpinari by Ivakhnenko (1987). Therefore, the Permian age of Kurty seems more probable.",,siltstone,,lithified,,,,,,,,lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,PIN,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Utegenia,n. gen.,NA,NA,vertebrate,V. V. Kuznetsov and M. F. Ivakhnenko. 1981. Discosauriscids from the Upper Paleozoic in Southern Kazakhstan. Paleontological Journal 1981:101-108,327,697,697,R. Butler,E. Dunne,E. Dunne,19/08/2016 08:41,19/08/2016 08:44,NA,shpinari,Utegenia,60161,n. sp.,298.9,279.3,Asselian,Artinskian,42,,Utegenia shpinari
1340590,occ,NA,,181086,members,Seymouria n. sp. grandis,species,346166,,Seymouria grandis,NA,species,346166,Olson,1979,Chordata,33815,Osteichthyes,34881,,NA,Seymouriidae,37219,37223,NA,NA,NA,individuals,-97.5952,35.924335,South of Crescent,NA,,US,Oklahoma,Logan,estimated from map,6,small collection,"Site is ""in a gray-greenish dolomitic siltstone exposed in a road cut on the west side of US highway 77, about 0.2 km north of the Cimarron River and 9.6 km south of Crescent, Logan County, Oklahoma"". Coordintes are approximate.",gp_mid,-26.69,2.96,101,US,,,Hennessey,,,,,,,,,NA,Fairmont Shale,,siltstone,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,FMNH,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Seymouria,,NA,NA,vertebrate,E. C. Olson. 1979. Seymouria grandis n. sp. (Batrachosauria: Amphibia) from the Middle Clear Fork (Permian) of Oklahoma and Texas. Journal of Paleontology 53(3):720-728,327,697,0,R. Butler,E. Dunne,,19/08/2016 09:23,19/08/2016 09:23,NA,grandis,Seymouria,60165,n. sp.,279.3,272.3,Kungurian,,2,US,Seymouria grandis
1340592,occ,NA,,181087,members,Seymouria grandis,species,346166,,Seymouria grandis,NA,species,346166,Olson,1979,Chordata,33815,Osteichthyes,34881,,NA,Seymouriidae,37219,37223,NA,NA,NA,specimens,-97.563889,35.956944,East of Crescent,NA,,US,Oklahoma,Logan,estimated from map,seconds,small collection,"Site is ""2.4 km east of Crescent, Logan County"". Coordintes are approximate.",gp_mid,-26.65,2.98,101,US,,,Hennessey,,,,,,,,,NA,Basal Fairmont Shale,,siltstone,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Seymouria,,NA,NA,vertebrate,E. C. Olson. 1979. Seymouria grandis n. sp. (Batrachosauria: Amphibia) from the Middle Clear Fork (Permian) of Oklahoma and Texas. Journal of Paleontology 53(3):720-728,327,697,0,R. Butler,E. Dunne,,19/08/2016 09:29,19/08/2016 09:29,NA,grandis,Seymouria,60165,,279.3,272.3,Kungurian,,1,US,Seymouria grandis
1340709,occ,NA,,176531,members,Apateon dracyi,species,345823,,Apateon dracyi,NA,species,345822,Werneburg,2001,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,individuals,10.502759,50.866585,Tabarz,NA,Cabarz,DE,Thuringia,Gotha District,based on nearby landmark,6,small collection,"Coordinates are based on the centre of the municipality Tabarz in the district of Gotha, in Thuringia. Locality is in the Thuringian Forest. ",gp_mid,21.2,6.7,305,DE,,Goldlauter,,,group of beds,,Lower Goldlauter Beds,Lower Goldlauter Beds,,,,NA,Lower Goldlauter Beds,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. Werneburg. 2001. Apateon dracyiensis - eine fr_he Pionierform der Branchiosaurier aud dem Europ_ischen Rotliegend. Teil 1: Morphologie. Ver̦ffentlichungen Naturhist. Museum Schleusingen 16:17-36,327,697,0,R. Butler,E. Dunne,,22/08/2016 09:27,22/08/2016 09:27,NA,dracyi,Apateon,60187,,298.9,295.5,Asselian,,500,DE,Apateon dracyi
1340713,occ,NA,,181127,members,Apateon dracyi,species,345823,,Apateon dracyi,NA,species,345822,Werneburg,2001,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,10.476908,50.797466,Kniebreche at Kleinschmalkalden,NA,,DE,Thuringia,,based on nearby landmark,6,small collection,"Coordinates are based on the centre of the village of Kleinschmalkalden on the southern slope of the Thuringian Forest in Landkreis Schmalkalden-Meiningen of Thuringia, Germany",gp_mid,21.2,6.63,305,DE,,Goldlauter,,,,,,,,,,NA,Lower Goldlauter Beds,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,R. Werneburg. 2001. Apateon dracyiensis - eine fr_he Pionierform der Branchiosaurier aud dem Europ_ischen Rotliegend. Teil 1: Morphologie. Ver̦ffentlichungen Naturhist. Museum Schleusingen 16:17-36,327,697,0,R. Butler,E. Dunne,,22/08/2016 09:35,22/08/2016 09:35,NA,dracyi,Apateon,60187,,298.9,295.5,Asselian,,NA,DE,Apateon dracyi
1340714,occ,NA,,181128,members,Apateon flagrifer,species,345821,,Apateon flagrifer,NA,species,345820,Werneburg,1986,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,10.565278,50.856945,"Kesselgraben, Friedrichroda",NA,,DE,Thuringia,,based on nearby landmark,seconds,small collection,"Coordinates based on the location of Kesselgraben, near Friedrichroda, Suhl district, Thuringia, Germany",gp_mid,21.24,6.7,305,DE,,Goldlauterer,,Upper Goldlauterer,,,,,,,,NA,"Lower Rotliegenden, upper Autun",,not reported,,,,,,,,,,fluvial-lacustrine indet.,rift,Thuringian Forest basin; extensional basin with dextral strike-slip transtension component following the Variscan orogeny.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,"R. Werneburg. 1986. Die Stegocephalen (Amphibia) der Goldlauterer Schichten (Unterrotliegendes, Perm) des Th_ringer Waldes. Teil 1 Apateon flagrifer (Whittard). Freiberger Forschungschefte C 410:88-101",327,697,0,R. Butler,E. Dunne,,22/08/2016 10:16,22/08/2016 10:16,NA,flagrifer,Apateon,60188,,298.9,295,Autunian,,NA,DE,Apateon flagrifer
1340715,occ,NA,,181129,members,Apateon flagrifer,species,345821,,Apateon flagrifer,NA,species,345820,Werneburg,1986,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,10.638089,50.710541,Oberschonau,NA,Obersch̦nau,DE,Thuringia,,based on nearby landmark,6,small collection,"Coordinates based on the centre of Oberschonau, which is a municipality south of Friedrichroda",gp_mid,21.32,6.57,305,DE,,Goldlauterer,,Upper Goldlauterer,,,,,,,,NA,"Lower Rotliegenden, upper Autun",,not reported,gray,lithified,,,,,,,,fluvial-lacustrine indet.,rift,Thuringian Forest basin; extensional basin with dextral strike-slip transtension component following the Variscan orogeny.,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,"R. Werneburg. 1986. Die Stegocephalen (Amphibia) der Goldlauterer Schichten (Unterrotliegendes, Perm) des Th_ringer Waldes. Teil 1 Apateon flagrifer (Whittard). Freiberger Forschungschefte C 410:88-101",327,697,0,R. Butler,E. Dunne,,22/08/2016 10:19,22/08/2016 10:19,NA,flagrifer,Apateon,60188,,298.9,295.5,Asselian,,NA,DE,Apateon flagrifer
1340716,occ,NA,,181130,members,Apateon flagrifer,species,345821,,Apateon flagrifer,NA,species,345820,Werneburg,1986,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Branchiosauridae,37037,37038,NA,NA,NA,,10.510805,50.876282,"Strasse Grenzwiese, Cabarz",NA,"Tabarz, Strae Grenzwiese",DE,Thuringia,Gotha District,based on nearby landmark,6,small collection,"Coordinates are based on the location of Tabarz in the district of Gotha, in Thuringia. Locality is in the Thuringian Forest. ",gp_mid,21.2,6.71,305,DE,,Goldlauter,,,,,,,,,,NA,Lower Goldlauter Beds,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Apateon,,NA,NA,vertebrate,"R. Werneburg. 1986. Die Stegocephalen (Amphibia) der Goldlauterer Schichten (Unterrotliegendes, Perm) des Th_ringer Waldes. Teil 1 Apateon flagrifer (Whittard). Freiberger Forschungschefte C 410:88-101",327,697,0,R. Butler,E. Dunne,,22/08/2016 10:28,22/08/2016 10:28,NA,flagrifer,Apateon,60188,,298.9,295.5,Asselian,,NA,DE,Apateon flagrifer
1340717,occ,NA,,180761,members,Eryops sp.,genus,37011,,Eryops,NA,genus,37011,Werneburg,1986,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,37011,NA,NA,NA,specimens,11.517153,48.371948,Kammerberg near Manebach,NA,,DE,Thuringia,,based on nearby landmark,6,small collection,"Coordinates based on the village of Kammerberg, near Manebach, Thuringia, Germany.",gp_mid,22.37,4.25,305,DE,,Manebach,,,,,,,,,,NA,Pennsylvanian-Permian Boundary,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Eryops,,NA,NA,vertebrate,"R. Werneburg. 1986. Die Stegocephalen (Amphibia) der Goldlauterer Schichten (Unterrotliegendes, Perm) des Th_ringer Waldes. Teil 1 Apateon flagrifer (Whittard). Freiberger Forschungschefte C 410:88-101",327,697,0,R. Butler,E. Dunne,,22/08/2016 10:48,22/08/2016 10:48,NA,sp.,Eryops,60188,,303.7,295.5,Gzhelian,Asselian,1,DE,Eryops sp.
1340718,occ,NA,,87877,,n. gen. Makowskia n. sp. laticephala,species,346269,,Makowskia laticephala,NA,species,346269,Klembara,2005,Chordata,33815,Osteichthyes,34881,,NA,Discosauriscidae,37207,346268,NA,NA,NA,individuals,16.612778,49.565277,"Kochov, Boskovice Furrow",NA,Boskovice Basin,CZ,Moravia,,based on nearby landmark,seconds,small collection,"Boskovice Furrow (or Boskovice Basin) in Moravia (Czech Republic); Kochov-L, about 500 m NE from Kochov (near Letovice).",gp_mid,25.35,6.67,305,CZ,,Middle Letovice,,,bed,Xenacanthus decheni,,,,,,NA,"Xenacanthus decheni (Goldfuss, 1847) biozone, Middle Letovice Formation, Autunian, Lower Permian","""laminated limestone""","""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,some,,,skeletons,,NA,,body,good,,snapshot,,,,,,,NA,,,taxonomic,chemical,,,,,,,"SNM: Slovak National Museum in Bratislava, Slovakia.",,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Makowskia,n. gen.,NA,NA,vertebrate,"J. Klembara. 2005. A new discosauriscid seymouriamorph tetrapod from the Lower Permian of Moravia, Czech Republic. Acta Palaeontologica Polonica 50(1):25-48",327,697,0,R. Butler,E. Dunne,,22/08/2016 11:08,22/08/2016 11:08,43843,laticephala,Makowskia,60189,n. sp.,298.9,295,Autunian,,1,CZ,Makowskia laticephala
1340782,occ,NA,,181134,,Discosauriscus n. sp. sigalovi,species,320957,recombined as,Ariekanerpeton sigalovi,NA,species,320957,Klembara and Ruta,2005,Chordata,33815,Osteichthyes,34881,,NA,Discosauriscidae,37207,37208,NA,NA,NA,specimens,69.638298,40.278896,"Sarytaypan locality, Leninabad",NA,,TJ,Leninabad,,based on nearby landmark,6,small collection,"Locality as stated in text: ""Sarytaypan locality, Leninabad province, Kuramin Ridge, Adrasman district, Tadzhikistan. [..] The present authors have not been able to identify the precise geographical locality from which the specimens were collected, hence the absence of a map."" (Klembara & Ruta, 2005). \r\nCoordinates here are based on the centre of Khujand (formerly Khodjend or Khodzhent until 1936 and Leninabad until 1991), the second-largest city of Tajikistan. ",gp_mid,71.94,19.48,402,TJ,,,,,,,,,,,,NA,"The beds are assumed to be coeval with the Lower Rotliegende of central Europe, although correlations are still largely uncertain (Laurin 1996b; Ivakhnenko 1981; Berman et al. 1997). ","Specimens were ""recovered from layers of tuffs within aleuritic (silt) shales.""","""shale""",,,,Y,,,,,,lacustrine indet.,,"""The depositional environment of the Ariekanerpeton-bearing sediments was presumably lacustrine and characterised by periodical water level oscillations.""",macrofossils,,,,,,NA,,body,poor,,,,,,common,,,NA,,"Skeletons ""were mostly destroyed by contact with hot volcanogenic material""",taxonomic,,PIN,,,,Kalakanaty geological group,1961,"The type locality (see below) was discovered by a team of geologists of the Kalakanaty geological group in 1961. In 1964, an expedition from the Palaeontological Institute of the Russian Academy of Sciences led by Tatarinov found 124 specimens. A second expedition to the type locality, led by Kalandadze in 1975, resulted in the collection of about 850 additional speci- mens of assorted size from a surface of about six square metres.","Specimens deposited in the Palaeontological Institute of the Russian Academy of Sciences, Moscow (PIN). Latex casts are deposited in the Department of Ecology, Comenius University, Bratislava, and bear the same registration numbers as the original specimens.","brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Discosauriscus,,NA,NA,vertebrate,J. Klembara and M. Ruta. 2005. The seymouriamorph tetrapod Ariekanerpeton sigalovi from the Lower Permian of Tadzhikistan. Part I: Cranial anatomy and ontogeny. Transactions of the Royal Society of Edinburgh: Earth Sciences 96(1):43-70,327,697,0,R. Butler,E. Dunne,,23/08/2016 06:23,23/08/2016 06:23,NA,sigalovi,Ariekanerpeton,60200,n. sp.,298.9,254,Rotliegendes,,974,TJ,Ariekanerpeton sigalovi
1340910,occ,NA,,181176,members,Hyloplesion n. sp. fritschia,species,137988,recombined as,Batropetes fritschia,NA,species,137988,Carroll,1968,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Brachystelechidae,37314,37513,NA,NA,NA,individuals,13.645523,50.006844,"Freital, near Dresden",NA,,DE,Saxony,,based on nearby landmark,6,outcrop,"The coordinates here are for the centre of the town of Freital, S_chsische Schweiz-Osterzgebirge, Saxony, Germany.",gp_mid,23.6,6.78,305,DE,,Niederhaslich-Schweinsdorf,Rotliegend,Niederhaslich limestone,member,,,,,,,NA,"""The Niederh_slich Formation belongs stratigraphically [...] to the Melanerpeton gracile-M. pulcherimus Zone, i. e. uppermost Unterrotliegend"" (U. Hoffman, 2002, Workshop _Oberkarbon - Untertrias in Zentraleuropa: Prozesse und ihr Timing [online] http://www.geo.tu-freiberg.de/palaeo/GeoTage-2002.pdf) (TL);\r\nthe Niederh_slich limestone is Asselian according to assorted references, e.g., Gebhardt and Schneider 1993 (JA)\r\nAccording to Roscher & Schneider (2006, in Lucas et al. (eds), Geol. Soc. Spec. Publ. 265) the Niederh_slich Fm. is Sakmarian in age (TL).",,"""limestone""",,,,,,,,,,lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Hyloplesion,,NA,NA,vertebrate,R. L. Carroll. 1968. The postcranial skeleton of the Permian microsaur Pantylus. Canadian Journal of Zoology 46:1175-1192,327,697,0,R. Butler,E. Dunne,,24/08/2016 09:08,24/08/2016 09:08,NA,fritschia,Batropetes,60212,n. sp.,295.5,290.1,Sakmarian,,1,DE,Batropetes fritschia
1340911,occ,NA,,181176,members,Hyloplesion n. sp. fritschia,species,137988,recombined as,Batropetes fritschia,NA,species,137988,Carroll,1968,Chordata,33815,Osteichthyes,34881,Microsauria,37278,Brachystelechidae,37314,37513,NA,NA,NA,individuals,13.645523,50.006844,"Freital, near Dresden",NA,,DE,Saxony,,based on nearby landmark,6,outcrop,"The coordinates here are for the centre of the town of Freital, S_chsische Schweiz-Osterzgebirge, Saxony, Germany.",gp_mid,23.6,6.78,305,DE,,Niederhaslich-Schweinsdorf,Rotliegend,Niederhaslich limestone,member,,,,,,,NA,"""The Niederh_slich Formation belongs stratigraphically [...] to the Melanerpeton gracile-M. pulcherimus Zone, i. e. uppermost Unterrotliegend"" (U. Hoffman, 2002, Workshop _Oberkarbon - Untertrias in Zentraleuropa: Prozesse und ihr Timing [online] http://www.geo.tu-freiberg.de/palaeo/GeoTage-2002.pdf) (TL);\r\nthe Niederh_slich limestone is Asselian according to assorted references, e.g., Gebhardt and Schneider 1993 (JA)\r\nAccording to Roscher & Schneider (2006, in Lucas et al. (eds), Geol. Soc. Spec. Publ. 265) the Niederh_slich Fm. is Sakmarian in age (TL).",,"""limestone""",,,,,,,,,,lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,dispersal=water,,hydroxyapatite,,NA,,Hyloplesion,,NA,NA,vertebrate,R. L. Carroll. 1968. The postcranial skeleton of the Permian microsaur Pantylus. Canadian Journal of Zoology 46:1175-1192,327,697,0,R. Butler,E. Dunne,,24/08/2016 09:08,24/08/2016 09:08,NA,fritschia,Batropetes,60212,n. sp.,295.5,290.1,Sakmarian,,1,DE,Batropetes fritschia
1340986,occ,NA,,180939,members,Animasaurus n. sp. carinatus,species,320997,recombined as,Diadectes carinatus,NA,species,320997,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Diadectidae,37246,37247,NA,NA,NA,individuals,-107.047775,38.763889,"Baldwin, near Animas",NA,,US,Colorado,,based on nearby landmark,seconds,small collection,,gp_mid,-32.78,6.82,101,US,FED,Abo,,,,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,YPM,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Animasaurus,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,24/08/2016 10:15,24/08/2016 10:15,NA,carinatus,Diadectes,28828,n. sp.,296.4,268,Wolfcamp,,1,US,Diadectes carinatus
1341058,occ,NA,,80111,,n. gen. Carbonoherpeton n. sp. carrolli,species,37187,species not entered,Carbonoherpeton,NA,genus,37187,Klembara,1985,Chordata,33815,Osteichthyes,34881,,NA,Eogyrinidae,37185,37187,NA,NA,NA,individuals,-60.266666,46.290001,Dominion Coal Co. strip mine No. 7,NA,"Sydney coal field; Florence, Cape Breton",CA,Nova Scotia,Cape Breton Island,estimated from map,seconds,small collection,"Dominion Coal Co. strip mine No. 7, about 2 miles north of the town of Florence",gp_mid,-3.96,-8.17,108,CA,,,Morien,,group of beds,,,,,,,NA,"""... above the Lloyd Cove (Lower Bonar) coal of the Morien group."" ",,coal,,,,Y,"""shale""",,,,,mire/swamp,intermontane basin,,macrofossils,,,,,,NA,,permineralized,,autochthonous,snapshot,,,,,,,NA,,the vertebrate remains come from the interior of fossilized tree stumps and are completely disarticulated,taxonomic,"selective quarrying,survey of museum collection",MCZ,,,,A.S. Romer,1956,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Carbonoherpeton,n. gen.,NA,NA,,"J. Klembara. 1985. A new embolomerous amphibian (Anthracosauria) from the Upper Carboniferous of Florence, Nova Scotia. Journal of Vertebrate Paleontology 5:293-302",327,697,0,R. Butler,E. Dunne,,25/08/2016 08:12,25/08/2016 08:12,26895,carrolli,Carbonoherpeton,60224,n. sp.,314.6,306.95,Westphalian C,Westphalian D,1,CA,Carbonoherpeton carrolli
1341681,occ,NA,,126535,,n. gen. Glaukerpeton n. sp. avinoffi,species,345493,,Glaukerpeton avinoffi,NA,species,345493,Werneburg and Berman,2012,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Eryopidae,37007,345492,NA,NA,NA,individuals,-79.966667,40.444443,Soho Street Quarry,NA,Locality 1 of Moran (1952),US,Pennsylvania,Allegheny,estimated from map,seconds,,"Location details given by Wellstead (1991): ""a quarry on east side of Soho Street, approximately 0.25km north of Fifth Avenue, Pittsburgh, Allegheny County Pennsylvania. The site is now covered by a housing development.""",gp_mid,-15.23,-4.42,101,US,,,Conemaugh,,bed,,,,,,,NA,"""Freshwater limestone bed within the Pittsburgh Limestone, lying 12m below the base of the Conemaugh Group, Upper Pennsylvanian (=Stephanian)"" (Wellstead, 1991)",,"""limestone""",,,,Y,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,general faunal/floral,,"CM,MCZ",,,,Burke party,1936,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Glaukerpeton,n. gen.,NA,NA,vertebrate,"R. Werneburg and D. S. Berman. 2012. Revision of the Aquatic Eryopid Temnospondyl Glaukerpeton avinoffi Romer, 1952, from the Upper Pennsyl Vanian of North America. Annals of Carnegie Museum 81(1):33-60",327,697,697,R. Butler,E. Dunne,E. Dunne,07/09/2016 03:34,07/09/2016 03:35,41027,avinoffi,Glaukerpeton,59940,n. sp.,306.95,298.9,Stephanian,,1,US,Glaukerpeton avinoffi
1341682,occ,NA,,180937,members,Edaphosaurus cf. raymondi,species,346039,nomen vanum,Edaphosauridae,NA,family,38910,Kissel,2010,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Edaphosauridae,38910,NA,NA,NA,NA,,-79.77639,40.405834,Pitcairn Locailty,NA,"Locality C (Moran, 1952)",US,Pennsylvania,Allegheny,based on nearby landmark,seconds,small collection,"Lat long is for Pitcairn, Pennsylvania, US",gp_mid,-15.75,-5.63,101,US,,Red Knob,Conemaugh,,bed,,,,,,,NA,"The Pitcairn locality in Pennsylvania (Locality C of Moran, 1952) is located within the Red Knob Formation, approximately 100 m below the base of the Pittsburgh coal, near the middle of the Conemaugh Group. ",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,survey of museum collection,CM,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Edaphosaurus,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,07/09/2016 03:40,07/09/2016 03:40,NA,raymondi,,60077,cf.,305.9,303.4,Missourian,,NA,US, raymondi
1341684,occ,NA,,180633,members,Trimerorhachidae indet.,family,36985,,Trimerorhachidae,NA,family,36985,Kissel,2010,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Trimerorhachidae,36985,NA,NA,NA,NA,individuals,-95.41037,39.817047,"Robinson Locality, Brown County",NA,Bern Limestone,US,Kansas,Brown,based on nearby landmark,6,small collection,"Coordinates are for the centre of Robinson, a city in Brown County, Kansas, United States. Locality lies just northeast of the town of Robinson.",gp_mid,-25.51,1.2,101,US,,Bern Limestone,Wabaunsee,Soldier Creek Shale,group of beds,,,,,,,NA,Bern Limestone,The fossiliferous horizon is composed almost entirely of densely packed stromatolites that lie between two shales.,"""shale""",,,,Y,,,,,,lagoonal,,"Although it has been suggested that shallow marine conditions existed at the site during time of deposition, it has also been argued that the cyanobacteria of the stromatolites grew in an environment of mixed fresh and marine water, either a lagoon or a bay (Foreman and Martin, 1988)",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,"Like the Middle Virgilian Hamilton fauna, the Robinson fauna is dominated by aquatic taxa, with only a few specimens of terrestrial forms present.","brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Trimerorhachidae,,NA,NA,vertebrate,"R. Kissel. 2010. Morphology, Phylogeny, and Evolution of Diadectidae (Cotylosauria: Diadectomorpha). University of Toronto ",327,697,0,R. Butler,E. Dunne,,07/09/2016 03:46,07/09/2016 03:46,NA,indet.,,60077,,303.4,298.9,Virgilian,,1,US, indet.
1342750,occ,NA,,179047,members,Cheliderpeton vranyi,species,345866,,Cheliderpeton vranyi,NA,species,345866,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,Intasuchidae,137935,37009,NA,NA,NA,,15.406135,50.576557,"Kostalov, near Trutnov",NA,Kolov,CZ,Liberec Region,Semily District,based on nearby landmark,6,small collection,,gp_mid,24.27,7.36,305,CZ,,Lower Rotliegendes,,,,,,,,,,NA,"Higher Coal-bearing zone, 'Upper Red beds'.",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Cheliderpeton,,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,22/09/2016 08:05,22/09/2016 08:05,NA,vranyi,Cheliderpeton,28828,,298.9,295.5,Asselian,,NA,CZ,Cheliderpeton vranyi
1342751,occ,NA,,179047,members,n. gen. Memonomenos n. sp. dyscriton,species,320850,recombined as,Archegosaurus dyscriton,NA,species,320850,Schoch and Milner,2000,Chordata,33815,Osteichthyes,34881,Temnospondyli,36320,,NA,37058,NA,NA,NA,,15.406135,50.576557,"Kostalov, near Trutnov",NA,Kolov,CZ,Liberec Region,Semily District,based on nearby landmark,6,small collection,,gp_mid,24.27,7.36,305,CZ,,Lower Rotliegendes,,,,,,,,,,NA,"Higher Coal-bearing zone, 'Upper Red beds'.",,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,amphibious,NA,carnivore,,,hydroxyapatite,,NA,,Memonomenos,n. gen.,NA,NA,vertebrate,R. Schoch and A. R. Milner. 2000. Stereospondyli. Handbuch der Pal_oherpetologie - Encyclopedia of Paleoherpetology 3B:1-203,327,697,0,R. Butler,E. Dunne,,22/09/2016 08:05,22/09/2016 08:05,NA,dyscriton,Archegosaurus,28828,n. sp.,298.9,295.5,Asselian,,NA,CZ,Archegosaurus dyscriton
1346304,occ,NA,IF,180863,,Saurichnites n. sp. salamandroides,species,347233,,Saurichnites salamandroides,NA,species,347233,Geinitz,1861,Chordata,33815,Reptilia,36322,Eosuchia,37795,Chirotheriidae,64084,64085,NA,NA,NA,,15.605044,50.643635,"Riesengebirges, Hohenelbe tracksite",NA,"Krkonose, Giant Mountains, Vrchlabi, Kalna",CZ,Hradec Kralove,Trutnov,based on nearby landmark,6,outcrop,"southern foot, Riesengebirges (= Krkonose, Giant Mountains), Hohenelbe (Vrchlabi) region, now Czech Republic",gp_mid,26.94,11.42,305,CZ,,,,,group of beds,,,,,,,NA,Rotliegende = Artinskian to Capitanian,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,some,footprints,,,NA,,trace,,autochthonous,snapshot,,,life position,,,,NA,,,taxonomic,"surface (in situ),field collection",,,,,J. Kablik,"1860, 1865",,,terrestrial,NA,actively mobile,,NA,carnivore,,,hydroxyapatite,,NA,,Saurichnites,,NA,NA,vertebrate,"H. B. Geinitz. 1861. Sauriern des Rothliegenden [Saurians from the Rothliegenden]. Neues Jahrbuch f_r Mineralogie, Geognosie, Geologie und Petrfakten-Kunde 1861:65-67",14,14,0,M. Carrano,M. Carrano,,19/10/2016 15:44,19/10/2016 15:44,NA,salamandroides,Chirotherium,60635,n. sp.,290.1,259.9,Artinskian,Capitanian,NA,CZ,Chirotherium salamandroides
1346305,occ,NA,IF,180863,,Saurichnites n. sp. lacertoides,species,347232,,Saurichnites lacertoides,NA,species,347232,Geinitz,1861,Chordata,33815,Reptilia,36322,Eosuchia,37795,Chirotheriidae,64084,64085,NA,NA,NA,,15.605044,50.643635,"Riesengebirges, Hohenelbe tracksite",NA,"Krkonose, Giant Mountains, Vrchlabi, Kalna",CZ,Hradec Kralove,Trutnov,based on nearby landmark,6,outcrop,"southern foot, Riesengebirges (= Krkonose, Giant Mountains), Hohenelbe (Vrchlabi) region, now Czech Republic",gp_mid,26.94,11.42,305,CZ,,,,,group of beds,,,,,,,NA,Rotliegende = Artinskian to Capitanian,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,some,footprints,,,NA,,trace,,autochthonous,snapshot,,,life position,,,,NA,,,taxonomic,"surface (in situ),field collection",,,,,J. Kablik,"1860, 1865",,,terrestrial,NA,actively mobile,,NA,carnivore,,,hydroxyapatite,,NA,,Saurichnites,,NA,NA,vertebrate,"H. B. Geinitz. 1861. Sauriern des Rothliegenden [Saurians from the Rothliegenden]. Neues Jahrbuch f_r Mineralogie, Geognosie, Geologie und Petrfakten-Kunde 1861:65-67",14,14,0,M. Carrano,M. Carrano,,19/10/2016 15:44,19/10/2016 15:44,NA,lacertoides,Chirotherium,60635,n. sp.,290.1,259.9,Artinskian,Capitanian,NA,CZ,Chirotherium lacertoides
1353002,occ,NA,,80691,,Captorhinus aguti,species,90718,,Captorhinus aguti,NA,species,134887,LeBlanc et al.,2015,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37497,NA,NA,NA,individuals,-98.64167,34.968056,South Carnegie Site,NA,"Roosevelt Company Quarry, Bally Mountain Locality, Bally Mountain Quarry",US,Oklahoma,Kiowa,estimated from map,seconds,small collection,"Olson (1967:36) originally describes the site as abandoned quarry of the Roosevelt Materials Company Carnegie plant; 11.2 miles south of the center of Carnegie, Caddo County, [...] NE 1/4 sec. 6, T. 5 N., R. 13 W. (Alden 7,5' quadrangle).\r\nLeBlanc et al. (2015) report captorhinid fossils from fissure fills in an abandoned limestone quarry on Bally Mountain in Kiowa County. They refer it to as Bally Mountain locality, but say that it is the same locality as Olsons South Carnegie site. Bally Mountain, however, is located 6 km WNW from the PLSS coordinates cited by Olson (1967). Bridges (1985:63, MSc thesis, Oklahoma State University) already has noted that Olsons description is wrong and gave the PLSS coordinates NE 1/4 sec. 26, T. 6 N., R. 14 W. (Bally Mountain 7,5' quadrangle) for the South Carnegie site. Although this is still about 2 km NE from the ridge that is labelled Bally Mountain on the maps, the originally entered DMS coordinates (3457'19"" N 9836'55"" W) are changed according to the PLSS coordinates given by Bridges (1985).",gp_mid,-28.96,0.59,101,US,,,,,,,,,,,,NA,"As far as can be determined, the deposits were formed in the same way and at the same time as were those at Richards Spur” (Olson, 1967; see collection 67862).","clay and conglomerates, much as at Richards Spur (Olson, 1967; see collection 67862)",claystone,,,,,conglomerate,,,,,fissure fill,non-subsiding area,,macrofossils,none,,"maxillae,mandibles",,,NA,,body,variable,,,concentrate,,,common,,frequent,NA,,"Olson (1967) states that preservation, however, is poor and only rather badly broken specimens have been found. [...] the prospects for finding significant amounts are poor, but subsequent collecting has brought many speciemens to light that are quite good preserved and determinable on species level (cf. LeBlanc et al., 2015).",taxonomic,field collection,"FMNH,ROM",,,,"E. C. Olson (FMNH), W. May (OMNH, ROM)",,OMNH = Sam Noble Oklahoma Museum of Natural History,"Simpson (1979; Oklahoma Geol. Notes 39(1)) in his table 1 (p. 7) lists the pelycosaur Basicranodon fortsilensis (sic) as the only known taxon from South Carnegie but in the text (p. 5) also mentions a large number of specimens of Captorhinus aguti from this site. LeBlanc et al. (2015) mention synapsids to be present but do not give a specific subtaxon. They, however, explicitly mention the anamniote Doleserpeton with regard to the similarity of the faunal composition of the Bally Mountain and Richards Spur localities. Since Doleserpeton is very abundant at Richards Spur and Olson (1967) says that the (then unnamed) amphibian taxa from South Carnegie and Richards Spur are the same, the Olson-based. taxon Amphibia indet. is re-identified as Doleserpeton sp..",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinus,,NA,NA,vertebrate,"A. R. H. LeBlanc, A. K. Brar, and W. May, R. R. Reisz. 2015. Multiple tooth-rowed captorhinids from the early Permian fissure fills of the Bally Mountain Locality of Oklahoma. Vertebrate Anatomy Morphology Palaeontology 1:35-49",315,334,0,J. Mueller,T. Liebrecht,,23/12/2016 08:55,23/12/2016 08:55,28557,aguti,Captorhinus,61256,,290.1,268,Leonard,,2,US,Captorhinus aguti
1353003,occ,NA,,80691,,Captorhinikos valensis,species,120855,,Captorhinikos valensis,NA,species,120855,LeBlanc et al.,2015,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,37496,NA,NA,NA,individuals,-98.64167,34.968056,South Carnegie Site,NA,"Roosevelt Company Quarry, Bally Mountain Locality, Bally Mountain Quarry",US,Oklahoma,Kiowa,estimated from map,seconds,small collection,"Olson (1967:36) originally describes the site as abandoned quarry of the Roosevelt Materials Company Carnegie plant; 11.2 miles south of the center of Carnegie, Caddo County, [...] NE 1/4 sec. 6, T. 5 N., R. 13 W. (Alden 7,5' quadrangle).\r\nLeBlanc et al. (2015) report captorhinid fossils from fissure fills in an abandoned limestone quarry on Bally Mountain in Kiowa County. They refer it to as Bally Mountain locality, but say that it is the same locality as Olsons South Carnegie site. Bally Mountain, however, is located 6 km WNW from the PLSS coordinates cited by Olson (1967). Bridges (1985:63, MSc thesis, Oklahoma State University) already has noted that Olsons description is wrong and gave the PLSS coordinates NE 1/4 sec. 26, T. 6 N., R. 14 W. (Bally Mountain 7,5' quadrangle) for the South Carnegie site. Although this is still about 2 km NE from the ridge that is labelled Bally Mountain on the maps, the originally entered DMS coordinates (3457'19"" N 9836'55"" W) are changed according to the PLSS coordinates given by Bridges (1985).",gp_mid,-28.96,0.59,101,US,,,,,,,,,,,,NA,"As far as can be determined, the deposits were formed in the same way and at the same time as were those at Richards Spur” (Olson, 1967; see collection 67862).","clay and conglomerates, much as at Richards Spur (Olson, 1967; see collection 67862)",claystone,,,,,conglomerate,,,,,fissure fill,non-subsiding area,,macrofossils,none,,"maxillae,mandibles",,,NA,,body,variable,,,concentrate,,,common,,frequent,NA,,"Olson (1967) states that preservation, however, is poor and only rather badly broken specimens have been found. [...] the prospects for finding significant amounts are poor, but subsequent collecting has brought many speciemens to light that are quite good preserved and determinable on species level (cf. LeBlanc et al., 2015).",taxonomic,field collection,"FMNH,ROM",,,,"E. C. Olson (FMNH), W. May (OMNH, ROM)",,OMNH = Sam Noble Oklahoma Museum of Natural History,"Simpson (1979; Oklahoma Geol. Notes 39(1)) in his table 1 (p. 7) lists the pelycosaur Basicranodon fortsilensis (sic) as the only known taxon from South Carnegie but in the text (p. 5) also mentions a large number of specimens of Captorhinus aguti from this site. LeBlanc et al. (2015) mention synapsids to be present but do not give a specific subtaxon. They, however, explicitly mention the anamniote Doleserpeton with regard to the similarity of the faunal composition of the Bally Mountain and Richards Spur localities. Since Doleserpeton is very abundant at Richards Spur and Olson (1967) says that the (then unnamed) amphibian taxa from South Carnegie and Richards Spur are the same, the Olson-based. taxon Amphibia indet. is re-identified as Doleserpeton sp..",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinikos,,NA,NA,vertebrate,"A. R. H. LeBlanc, A. K. Brar, and W. May, R. R. Reisz. 2015. Multiple tooth-rowed captorhinids from the early Permian fissure fills of the Bally Mountain Locality of Oklahoma. Vertebrate Anatomy Morphology Palaeontology 1:35-49",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,23/12/2016 08:55,23/12/2016 10:56,28557,valensis,Captorhinikos,61256,,290.1,268,Leonard,,4,US,Captorhinikos valensis
1353004,occ,NA,,80691,,Captorhinidae indet.,family,37495,,Captorhinidae,NA,family,37495,LeBlanc et al.,2015,Chordata,33815,Reptilia,36322,,NA,Captorhinidae,37495,NA,NA,NA,NA,individuals,-98.64167,34.968056,South Carnegie Site,NA,"Roosevelt Company Quarry, Bally Mountain Locality, Bally Mountain Quarry",US,Oklahoma,Kiowa,estimated from map,seconds,small collection,"Olson (1967:36) originally describes the site as abandoned quarry of the Roosevelt Materials Company Carnegie plant; 11.2 miles south of the center of Carnegie, Caddo County, [...] NE 1/4 sec. 6, T. 5 N., R. 13 W. (Alden 7,5' quadrangle).\r\nLeBlanc et al. (2015) report captorhinid fossils from fissure fills in an abandoned limestone quarry on Bally Mountain in Kiowa County. They refer it to as Bally Mountain locality, but say that it is the same locality as Olsons South Carnegie site. Bally Mountain, however, is located 6 km WNW from the PLSS coordinates cited by Olson (1967). Bridges (1985:63, MSc thesis, Oklahoma State University) already has noted that Olsons description is wrong and gave the PLSS coordinates NE 1/4 sec. 26, T. 6 N., R. 14 W. (Bally Mountain 7,5' quadrangle) for the South Carnegie site. Although this is still about 2 km NE from the ridge that is labelled Bally Mountain on the maps, the originally entered DMS coordinates (3457'19"" N 9836'55"" W) are changed according to the PLSS coordinates given by Bridges (1985).",gp_mid,-28.96,0.59,101,US,,,,,,,,,,,,NA,"As far as can be determined, the deposits were formed in the same way and at the same time as were those at Richards Spur” (Olson, 1967; see collection 67862).","clay and conglomerates, much as at Richards Spur (Olson, 1967; see collection 67862)",claystone,,,,,conglomerate,,,,,fissure fill,non-subsiding area,,macrofossils,none,,"maxillae,mandibles",,,NA,,body,variable,,,concentrate,,,common,,frequent,NA,,"Olson (1967) states that preservation, however, is poor and only rather badly broken specimens have been found. [...] the prospects for finding significant amounts are poor, but subsequent collecting has brought many speciemens to light that are quite good preserved and determinable on species level (cf. LeBlanc et al., 2015).",taxonomic,field collection,"FMNH,ROM",,,,"E. C. Olson (FMNH), W. May (OMNH, ROM)",,OMNH = Sam Noble Oklahoma Museum of Natural History,"Simpson (1979; Oklahoma Geol. Notes 39(1)) in his table 1 (p. 7) lists the pelycosaur Basicranodon fortsilensis (sic) as the only known taxon from South Carnegie but in the text (p. 5) also mentions a large number of specimens of Captorhinus aguti from this site. LeBlanc et al. (2015) mention synapsids to be present but do not give a specific subtaxon. They, however, explicitly mention the anamniote Doleserpeton with regard to the similarity of the faunal composition of the Bally Mountain and Richards Spur localities. Since Doleserpeton is very abundant at Richards Spur and Olson (1967) says that the (then unnamed) amphibian taxa from South Carnegie and Richards Spur are the same, the Olson-based. taxon Amphibia indet. is re-identified as Doleserpeton sp..",terrestrial,NA,actively mobile,ground dwelling,NA,"insectivore, herbivore","oviparous, dispersal=direct/internal,mobile",addition of parts,"phosphatic, ""sclero-protein""",compact or dense,NA,"minor folds, minor ribbing",Captorhinidae,,NA,NA,vertebrate,"A. R. H. LeBlanc, A. K. Brar, and W. May, R. R. Reisz. 2015. Multiple tooth-rowed captorhinids from the early Permian fissure fills of the Bally Mountain Locality of Oklahoma. Vertebrate Anatomy Morphology Palaeontology 1:35-49",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,23/12/2016 08:55,23/12/2016 09:04,28557,indet.,,61256,,290.1,268,Leonard,,2,US, indet.
1353005,occ,NA,,80691,,Synapsida indet.,unranked clade,99791,,Synapsida,NA,unranked clade,38882,LeBlanc et al.,2015,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,,NA,NA,NA,NA,NA,,-98.64167,34.968056,South Carnegie Site,NA,"Roosevelt Company Quarry, Bally Mountain Locality, Bally Mountain Quarry",US,Oklahoma,Kiowa,estimated from map,seconds,small collection,"Olson (1967:36) originally describes the site as abandoned quarry of the Roosevelt Materials Company Carnegie plant; 11.2 miles south of the center of Carnegie, Caddo County, [...] NE 1/4 sec. 6, T. 5 N., R. 13 W. (Alden 7,5' quadrangle).\r\nLeBlanc et al. (2015) report captorhinid fossils from fissure fills in an abandoned limestone quarry on Bally Mountain in Kiowa County. They refer it to as Bally Mountain locality, but say that it is the same locality as Olsons South Carnegie site. Bally Mountain, however, is located 6 km WNW from the PLSS coordinates cited by Olson (1967). Bridges (1985:63, MSc thesis, Oklahoma State University) already has noted that Olsons description is wrong and gave the PLSS coordinates NE 1/4 sec. 26, T. 6 N., R. 14 W. (Bally Mountain 7,5' quadrangle) for the South Carnegie site. Although this is still about 2 km NE from the ridge that is labelled Bally Mountain on the maps, the originally entered DMS coordinates (3457'19"" N 9836'55"" W) are changed according to the PLSS coordinates given by Bridges (1985).",gp_mid,-28.96,0.59,101,US,,,,,,,,,,,,NA,"As far as can be determined, the deposits were formed in the same way and at the same time as were those at Richards Spur” (Olson, 1967; see collection 67862).","clay and conglomerates, much as at Richards Spur (Olson, 1967; see collection 67862)",claystone,,,,,conglomerate,,,,,fissure fill,non-subsiding area,,macrofossils,none,,"maxillae,mandibles",,,NA,,body,variable,,,concentrate,,,common,,frequent,NA,,"Olson (1967) states that preservation, however, is poor and only rather badly broken specimens have been found. [...] the prospects for finding significant amounts are poor, but subsequent collecting has brought many speciemens to light that are quite good preserved and determinable on species level (cf. LeBlanc et al., 2015).",taxonomic,field collection,"FMNH,ROM",,,,"E. C. Olson (FMNH), W. May (OMNH, ROM)",,OMNH = Sam Noble Oklahoma Museum of Natural History,"Simpson (1979; Oklahoma Geol. Notes 39(1)) in his table 1 (p. 7) lists the pelycosaur Basicranodon fortsilensis (sic) as the only known taxon from South Carnegie but in the text (p. 5) also mentions a large number of specimens of Captorhinus aguti from this site. LeBlanc et al. (2015) mention synapsids to be present but do not give a specific subtaxon. They, however, explicitly mention the anamniote Doleserpeton with regard to the similarity of the faunal composition of the Bally Mountain and Richards Spur localities. Since Doleserpeton is very abundant at Richards Spur and Olson (1967) says that the (then unnamed) amphibian taxa from South Carnegie and Richards Spur are the same, the Olson-based. taxon Amphibia indet. is re-identified as Doleserpeton sp..",terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Synapsida,,NA,NA,vertebrate,"A. R. H. LeBlanc, A. K. Brar, and W. May, R. R. Reisz. 2015. Multiple tooth-rowed captorhinids from the early Permian fissure fills of the Bally Mountain Locality of Oklahoma. Vertebrate Anatomy Morphology Palaeontology 1:35-49",315,334,334,J. Mueller,T. Liebrecht,T. Liebrecht,23/12/2016 11:01,23/12/2016 11:02,28557,indet.,,61256,,290.1,268,Leonard,,NA,US, indet.
1353113,occ,NA,,183472,members,n. gen. Perittodus n. sp. apsconditus,species,348732,,Perittodus apsconditus,NA,species,348732,Clack et al.,2016,Chordata,33815,Osteichthyes,34881,,NA,,NA,348731,NA,NA,NA,specimens,-2.213471,55.792946,Willie۪s Hole,NA,Whiteadder Water near Chirnside,UK,Scotland,Berwickshire,based on nearby landmark,6,small collection,Coordinates based on the village of Chirnside.,gp_mid,-12.69,-32.69,313,UK,,Ballagan,,,,,,,,,,NA,"""Early mid_ Tournaisian""",,siltstone,,,,,claystone,,,,,"""floodplain""",,"""Perittodusapsconditus occurs within a 6cm thick laminated grey siltstone that contains a network of cracks filled with sandy siltstone identical to that of the overlying bed. Occurring within laminated siltstones, this may record an autochthonous lake dweller. Associated fossils comprise plants, actinopterygians, myriapods and ostracods. Koilops occurs within a unit comprising four beds of alternating black and green siltstone in which abundant palaeo_ sol clasts indicate erosion and transport of land_surface sediment during flooding events. ... An association between wetland palaeosols and tetrapod_ bearing facies has emerged from our studies, which is important because those horizons indicate a vegetated land surface.""",macrofossils,,,,,,NA,,"body,mold/impression",,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Perittodus,n. gen.,NA,NA,vertebrate,"J. A. Clack, C. E. Bennett, and D. K. Carpenter, S. J. Davies, N. C. Fraser, T. I. Kearsey, J. E. A. Marshall, D. Millward, B. K. A. Otoo, E. J. Reeves, A. J. Ross, M. Ruta, K. Z. Smithson, T. R. Smithson & S. A. Walsh. 2016. Phylogenetic and environmental context of a Tournaisian tetrapod fauna. Nature Ecology & Evolution 1(0002)",327,697,0,R. Butler,E. Dunne,,26/12/2016 10:51,26/12/2016 10:51,NA,apsconditus,Perittodus,61276,n. sp.,358.9,346.7,Tournaisian,,1,UK,Perittodus apsconditus
1353114,occ,NA,,183472,members,n. gen. Koilops n. sp. herma,species,348734,,Koilops herma,NA,species,348734,Clack et al.,2016,Chordata,33815,Osteichthyes,34881,,NA,,NA,348733,NA,NA,NA,specimens,-2.213471,55.792946,Willie۪s Hole,NA,Whiteadder Water near Chirnside,UK,Scotland,Berwickshire,based on nearby landmark,6,small collection,Coordinates based on the village of Chirnside.,gp_mid,-12.69,-32.69,313,UK,,Ballagan,,,,,,,,,,NA,"""Early mid_ Tournaisian""",,siltstone,,,,,claystone,,,,,"""floodplain""",,"""Perittodusapsconditus occurs within a 6cm thick laminated grey siltstone that contains a network of cracks filled with sandy siltstone identical to that of the overlying bed. Occurring within laminated siltstones, this may record an autochthonous lake dweller. Associated fossils comprise plants, actinopterygians, myriapods and ostracods. Koilops occurs within a unit comprising four beds of alternating black and green siltstone in which abundant palaeo_ sol clasts indicate erosion and transport of land_surface sediment during flooding events. ... An association between wetland palaeosols and tetrapod_ bearing facies has emerged from our studies, which is important because those horizons indicate a vegetated land surface.""",macrofossils,,,,,,NA,,"body,mold/impression",,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Koilops,n. gen.,NA,NA,vertebrate,"J. A. Clack, C. E. Bennett, and D. K. Carpenter, S. J. Davies, N. C. Fraser, T. I. Kearsey, J. E. A. Marshall, D. Millward, B. K. A. Otoo, E. J. Reeves, A. J. Ross, M. Ruta, K. Z. Smithson, T. R. Smithson & S. A. Walsh. 2016. Phylogenetic and environmental context of a Tournaisian tetrapod fauna. Nature Ecology & Evolution 1(0002)",327,697,0,R. Butler,E. Dunne,,26/12/2016 10:51,26/12/2016 10:51,NA,herma,Koilops,61276,n. sp.,358.9,346.7,Tournaisian,,1,UK,Koilops herma
1353115,occ,NA,,183473,members,n. gen. Diploradus n. sp. austiumensis,species,348738,,Diploradus austiumensis,NA,species,348738,Clack et al.,2016,Chordata,33815,Osteichthyes,34881,,NA,,NA,348737,NA,NA,NA,specimens,-2.068806,55.844093,Burnmouth Ross end cliffs,NA,,UK,Scotland,,stated in text,6,small collection,Coordinates based on the location of cliffs at Burnmouth.,gp_mid,-12.59,-32.64,313,UK,,Ballagan,,,,,,,,,,NA,"""Mid_ Tournaisian.""",,siltstone,,,,,claystone,,,,,"""floodplain""",,"""Diploradus occurs in a 40 cm thick, bedded, black sandy siltstone that lies between pedogenically modified grey siltstones. Associated fossils comprise fish scales, abundant plant fragments, megaspores and shrimp and scorpion cuticle. Ossirarus occurs within a complex 15 cm thick grey_black sandy siltstone that overlies a gleyed palaeosol and grades upwards into a laminated grey siltstone with brecciation cracks.""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Diploradus,n. gen.,NA,NA,vertebrate,"J. A. Clack, C. E. Bennett, and D. K. Carpenter, S. J. Davies, N. C. Fraser, T. I. Kearsey, J. E. A. Marshall, D. Millward, B. K. A. Otoo, E. J. Reeves, A. J. Ross, M. Ruta, K. Z. Smithson, T. R. Smithson & S. A. Walsh. 2016. Phylogenetic and environmental context of a Tournaisian tetrapod fauna. Nature Ecology & Evolution 1(0002)",327,697,697,R. Butler,E. Dunne,E. Dunne,26/12/2016 11:00,26/12/2016 11:05,NA,austiumensis,Diploradus,61276,n. sp.,358.9,346.7,Tournaisian,,2,UK,Diploradus austiumensis
1353116,occ,NA,,183473,members,n. gen. Ossirarus n. sp. kierani,species,348736,,Ossirarus kierani,NA,species,348736,Clack et al.,2016,Chordata,33815,Osteichthyes,34881,,NA,,NA,348735,NA,NA,NA,specimens,-2.068806,55.844093,Burnmouth Ross end cliffs,NA,,UK,Scotland,,stated in text,6,small collection,Coordinates based on the location of cliffs at Burnmouth.,gp_mid,-12.59,-32.64,313,UK,,Ballagan,,,,,,,,,,NA,"""Mid_ Tournaisian.""",,siltstone,,,,,claystone,,,,,"""floodplain""",,"""Diploradus occurs in a 40 cm thick, bedded, black sandy siltstone that lies between pedogenically modified grey siltstones. Associated fossils comprise fish scales, abundant plant fragments, megaspores and shrimp and scorpion cuticle. Ossirarus occurs within a complex 15 cm thick grey_black sandy siltstone that overlies a gleyed palaeosol and grades upwards into a laminated grey siltstone with brecciation cracks.""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Ossirarus,n. gen.,NA,NA,vertebrate,"J. A. Clack, C. E. Bennett, and D. K. Carpenter, S. J. Davies, N. C. Fraser, T. I. Kearsey, J. E. A. Marshall, D. Millward, B. K. A. Otoo, E. J. Reeves, A. J. Ross, M. Ruta, K. Z. Smithson, T. R. Smithson & S. A. Walsh. 2016. Phylogenetic and environmental context of a Tournaisian tetrapod fauna. Nature Ecology & Evolution 1(0002)",327,697,0,R. Butler,E. Dunne,,26/12/2016 11:00,26/12/2016 11:00,NA,kierani,Ossirarus,61276,n. sp.,358.9,346.7,Tournaisian,,1,UK,Ossirarus kierani
1353117,occ,NA,,183473,members,Perittodus apsconditus,species,348732,,Perittodus apsconditus,NA,species,348732,Clack et al.,2016,Chordata,33815,Osteichthyes,34881,,NA,,NA,348731,NA,NA,NA,specimens,-2.068806,55.844093,Burnmouth Ross end cliffs,NA,,UK,Scotland,,stated in text,6,small collection,Coordinates based on the location of cliffs at Burnmouth.,gp_mid,-12.59,-32.64,313,UK,,Ballagan,,,,,,,,,,NA,"""Mid_ Tournaisian.""",,siltstone,,,,,claystone,,,,,"""floodplain""",,"""Diploradus occurs in a 40 cm thick, bedded, black sandy siltstone that lies between pedogenically modified grey siltstones. Associated fossils comprise fish scales, abundant plant fragments, megaspores and shrimp and scorpion cuticle. Ossirarus occurs within a complex 15 cm thick grey_black sandy siltstone that overlies a gleyed palaeosol and grades upwards into a laminated grey siltstone with brecciation cracks.""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Perittodus,,NA,NA,vertebrate,"J. A. Clack, C. E. Bennett, and D. K. Carpenter, S. J. Davies, N. C. Fraser, T. I. Kearsey, J. E. A. Marshall, D. Millward, B. K. A. Otoo, E. J. Reeves, A. J. Ross, M. Ruta, K. Z. Smithson, T. R. Smithson & S. A. Walsh. 2016. Phylogenetic and environmental context of a Tournaisian tetrapod fauna. Nature Ecology & Evolution 1(0002)",327,697,0,R. Butler,E. Dunne,,26/12/2016 11:00,26/12/2016 11:00,NA,apsconditus,Perittodus,61276,,358.9,346.7,Tournaisian,,1,UK,Perittodus apsconditus
1353118,occ,NA,,183474,members,n. gen. Aytonerpeton n. sp. microps,species,348740,,Aytonerpeton microps,NA,species,348740,Clack et al.,2016,Chordata,33815,Osteichthyes,34881,,NA,,NA,348739,NA,NA,NA,specimens,-1.721389,55.954723,Burnmouth Ross end shore exposure,NA,,UK,Scotland,,stated in text,seconds,small collection,Coordinates based on the location of the shore exposure at Burnmouth.,gp_mid,-12.36,-32.53,313,UK,,Ballagan,,,,,,,,,,NA,"""340.6m above the base of the Ballagan Formation. Mid_-Tournaisian""",,siltstone,,,,,,,,,,"""floodplain""",,"""Aytonerpeton occurred within an overlying black sandy siltstone with abundant plant material.""",macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Aytonerpeton,n. gen.,NA,NA,vertebrate,"J. A. Clack, C. E. Bennett, and D. K. Carpenter, S. J. Davies, N. C. Fraser, T. I. Kearsey, J. E. A. Marshall, D. Millward, B. K. A. Otoo, E. J. Reeves, A. J. Ross, M. Ruta, K. Z. Smithson, T. R. Smithson & S. A. Walsh. 2016. Phylogenetic and environmental context of a Tournaisian tetrapod fauna. Nature Ecology & Evolution 1(0002)",327,697,0,R. Butler,E. Dunne,,26/12/2016 11:04,26/12/2016 11:04,NA,microps,Aytonerpeton,61276,n. sp.,358.9,346.7,Tournaisian,,1,UK,Aytonerpeton microps
1374837,occ,NA,,187716,,n. gen. Syodon n. sp. biarmicum,species,357010,,Syodon biarmicum,NA,species,357010,Ivakhnenko,2003,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Anteosauridae,38970,38959,NA,NA,NA,specimens,56.316666,58,"""Perm Region"" mines, Syodon biarmicum holotype site",NA,,RU,Perm Krai,,based on political unit,degrees,small collection,"Specimen collected historically from the ""mines of the Perm Region"" but no precise locality data availble. Coordinates based on city of Perm. ",gp_mid,43.81,29.15,302,RU,,Sheshmian,,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,PIN,,,,,,,,terrestrial,NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Syodon,n. gen.,NA,NA,vertebrate,M. F. Ivakhnenko. 2003. Eotherapsids from the East European Placket (Late Permian). Paleontological Journal 37(Suppl. 4):S339-S465,327,327,0,R. Butler,R. Butler,,08/08/2017 08:06,08/08/2017 08:06,NA,biarmicum,Syodon,63003,n. sp.,279.5,272.5,Ufimian,,1,RU,Syodon biarmicum
1375684,occ,NA,IF,180863,,Saurichnites n. sp. kablikae,species,358769,,Saurichnites kablikae,NA,species,358769,Geinitz and Deichm_ller,1882,Chordata,33815,Reptilia,36322,Eosuchia,37795,Chirotheriidae,64084,64085,NA,NA,NA,,15.605044,50.643635,"Riesengebirges, Hohenelbe tracksite",NA,"Krkonose, Giant Mountains, Vrchlabi, Kalna",CZ,Hradec Kralove,Trutnov,based on nearby landmark,6,outcrop,"southern foot, Riesengebirges (= Krkonose, Giant Mountains), Hohenelbe (Vrchlabi) region, now Czech Republic",gp_mid,26.94,11.42,305,CZ,,,,,group of beds,,,,,,,NA,Rotliegende = Artinskian to Capitanian,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,some,footprints,,,NA,,trace,,autochthonous,snapshot,,,life position,,,,NA,,,taxonomic,"surface (in situ),field collection",,,,,J. Kablik,"1860, 1865",,,terrestrial,NA,actively mobile,,NA,carnivore,,,hydroxyapatite,,NA,,Saurichnites,,NA,NA,vertebrate,H. B. Geinitz and J. V. Deichm_ller. 1882. Die Saurier der unteren Dyas von Sachsen [Saurians from the Lower Dyas of Saxony]. Palaeontographica 9:1-46,14,14,0,M. Carrano,M. Carrano,,17/08/2017 11:16,17/08/2017 11:16,NA,kablikae,Chirotherium,60084,n. sp.,290.1,259.9,Artinskian,Capitanian,NA,CZ,Chirotherium kablikae
1375685,occ,NA,IF,187930,,Saurichnites n. sp. leisnerianus,species,358767,,Saurichnites leisnerianus,NA,species,358767,Geinitz and Deichm_ller,1882,Chordata,33815,Reptilia,36322,Eosuchia,37795,Chirotheriidae,64084,64085,NA,NA,NA,,16.39727,50.504623,"Rathen, Radk_w tracksite",NA,W_nschelburg,PL,Lower Silesia,,based on nearby landmark,6,small collection,"from Rathen, near Radk_w (formerly W_nschelburg)",gp_mid,NA,NA,coordinates not computable using this model,PL,,,,,bed,,,,,,,NA,,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,footprints,,,NA,,trace,,autochthonous,snapshot,,,life position,,,,NA,,,general faunal/floral,"surface (in situ),field collection",,,,,E. Leisner,1863,,,terrestrial,NA,actively mobile,,NA,carnivore,,,hydroxyapatite,,NA,,Saurichnites,,NA,NA,vertebrate,H. B. Geinitz and J. V. Deichm_ller. 1882. Die Saurier der unteren Dyas von Sachsen [Saurians from the Lower Dyas of Saxony]. Palaeontographica 9:1-46,14,14,0,M. Carrano,M. Carrano,,17/08/2017 12:19,17/08/2017 12:19,NA,leisnerianus,Chirotherium,60084,n. sp.,290.1,279.3,Artinskian,,NA,PL,Chirotherium leisnerianus
1375693,occ,NA,,187932,,n. gen. Kamagorgon n. sp. ulanovi,species,358803,,Kamagorgon ulanovi,NA,species,358803,Ivakhnenko,2003,Chordata,33815,Osteichthyes,34881,Theriodontia,56648,Phthinosuchidae,38942,358802,NA,NA,NA,individuals,53.783611,56.858055,"Sidorovy Gory, PIN 4312/1",NA,,RU,Udmurt,Votkinskii,estimated from map,seconds,outcrop,,gp_mid,NA,NA,coordinates not computable using this model,RU,,,,,group of beds,,,,,,,NA,Upper part of the Ufimian stage to the bottom of the Upper Kazanian substage,,not reported,,,,,,,,,,terrestrial indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,PIN,,,,,,,,terrestrial,NA,actively mobile,,NA,carnivore,,,hydroxyapatite,,NA,,Kamagorgon,n. gen.,NA,NA,vertebrate,M. F. Ivakhnenko. 2003. Eotherapsids from the East European Placket (Late Permian). Paleontological Journal 37(Suppl. 4):S339-S465,327,327,0,R. Butler,R. Butler,,17/08/2017 16:43,17/08/2017 16:43,NA,ulanovi,Kamagorgon,63003,n. sp.,279.5,268,Ufimian,Kazanian,1,RU,Kamagorgon ulanovi
1377749,occ,NA,,188401,members,Spathicephalus n. sp. marsdeni,species,359291,,Spathicephalus marsdeni,NA,species,359291,Smithson et al.,2017,Chordata,33815,Osteichthyes,34881,,NA,Spathicephalidae,332447,36973,NA,NA,NA,specimens,-2.68503,56.320778,East Fife coast,NA,,UK,Scotland,Fife,based on nearby landmark,6,small collection,"East Fife coast, between St. Andrews and Fife Ness. Precise locality information is available from National Museums Scotland.",gp_mid,NA,NA,coordinates not computable using this model,UK,,Anstruther,,,,,,,,,,NA,"Anstruther Formation, Strathclyde Group; tessellatuscampyloptera(TC) palynozone (from the upper part of this zone); Asbian, Visean, Mississippian (336335 Ma).",,mudstone,,,,,,,,,,lacustrine indet.,,,macrofossils,,,,,,NA,,body,,,,,,,,,,NA,,,taxonomic,,,,,,,,,,"brackish,freshwater,terrestrial",NA,actively mobile,,NA,,,,hydroxyapatite,,NA,,Spathicephalus,,NA,NA,vertebrate,"T. R. Smithson, M. A. Browne, and S. J. Davies, J. E. Marshall, D. Millward, S. A. Walsh, J. A. Clack. 2017. A New Mississippian Tetrapod from Fife, Scotland and its Environmental Context. Papers in Palaeontology ",327,697,0,R. Butler,E. Dunne,,31/08/2017 04:46,31/08/2017 04:46,NA,marsdeni,Spathicephalus,63178,n. sp.,346.7,330.9,Visean,,2,UK,Spathicephalus marsdeni
1378806,occ,NA,,188672,,Diictodon sp.,genus,39075,,Diictodon,NA,genus,39075,Smith,1986,Chordata,33815,Osteichthyes,34881,Cotylosauria,56749,Pylaecephalidae,237785,39075,NA,NA,NA,,21.616667,-32.166668,Teekloof Pass cliff exposure,NA,,ZA,Karoo Basin,,,6,,,gp_mid,NA,NA,coordinates not computable using this model,ZA,,,,,,,,,,,,NA,,,mudstone,,,,,,,,,,fluvial indet.,,,macrofossils,,,,,,NA,,trace,,,,,,,,,,NA,,,general faunal/floral,,,,,,,,,,terrestrial,NA,actively mobile,,NA,herbivore,,,hydroxyapatite,,NA,,Diictodon,,NA,NA,,"R. M. H. Smith. 1986. Helical burrow casts of therapsid origin from the Beaufort Group (Permian) of South Africa. Palaeogeography, Palaeoclimatology, Palaeoecology 60:155-170",18,763,0,M. Uhen,K. Ziegler,,11/09/2017 18:19,11/09/2017 18:19,NA,sp.,Diictodon,63303,,298.9,252.17,Permian,,NA,ZA,Diictodon sp.