occurrenceID	taxonID	catalogNumber	collectionCode	institutionCode	typeStatus	verbatimLabel	sex	individualCount	eventDate	recordedBy	recordNumber	decimalLatitude	decimalLongitude	minimumElevationInMeters	maximumElevationInMeters	minimumDepthInMeters	maximumDepthInMeters	country	stateProvince	municipality	locality	references	associatedOccurrences	associatedReferences	associatedSequences	basisOfRecord
F160A367717DFFBEFE087324FAED2433.mc.C9A1182C717DFFB9FF4A7214FCF225AB	F160A367717DFFBEFE087324FAED2433.taxon	UCMP A-5018		UCMP		UCMP A- 5018 (holotype no. 10675) is the type and only specimen; it exposes a partly disarticulated abactinal surface showing the disc and proximal portions of four arms. Large marginal spines and smaller abactinal ones are visible. Marginals, adambulacrals, ambulacrals and abactinal ossicles of the holotype were figured individually by Blake (1973).		1														https://treatment.plazi.org/id/F160A367717DFFBEFE087324FAED2433#C9A1182C717DFFB9FF4A7214FCF225AB				MaterialCitation
F160A367717BFFBFFD86760FFB7723FA.mc.C9A1182C717BFFBFFF4A75A8FAF72309	F160A367717BFFBFFD86760FFB7723FA.taxon	NHMUK EE 13594		NHMUK		The type specimen, NHMUK EE 13594, consists of a set of associated ossicles from the upper Oxfordian (Couches d’Effingen, bifurcatus ammonite Zone, stenocycloides ammonite Subzone) at Savigna, near Orgelet (Département du Jura, France; see Gale 2011 a, 2011 b). Additional material comprises several hundred ossicles and groups of associated ossicles from the type locality (NHMUK collections).		1														https://treatment.plazi.org/id/F160A367717BFFBFFD86760FFB7723FA#C9A1182C717BFFBFFF4A75A8FAF72309				MaterialCitation
F160A367717BFFBDFDA474F9FEE524A6.mc.C9A1182C7179FFBDFF4A76AFFAC5226C	F160A367717BFFBDFDA474F9FEE524A6.taxon	NHMUK PI EE 17989, NHMUK PI EE 17990-17995		NHMUK		The ambulacral illustrated here (Fig. 6 J) is the holotype (NHMUK PI EE 17989); paratypes are NHMUK PI EE 17990 – 17995. All specimens are from middle Toarcian strata at Le Clapier (Département d’Aveyron, 62 km WNW of Montpellier, southern France; see Thuy 2012). Additional paratypes are fifteen ossicles (SNSB-BGSP 2020 XLV 16 – 30) from the upper Toarcian – lower Aalenian (possibly aalensis ammonite Zone) at Quedlinburg (Landkreis Harz, northern Germany; see Hess 2014).		1														https://treatment.plazi.org/id/F160A367717BFFBDFDA474F9FEE524A6#C9A1182C7179FFBDFF4A76AFFAC5226C				MaterialCitation
F160A3677167FFA1FD9E760FFBBB227A.mc.C9A1182C7167FFA3FF4A7443FAE623F1	F160A3677167FFA1FD9E760FFBBB227A.taxon	NHMM JJ 10490a, NHMM JJ 9591		NHMM		The inferomarginal illustrated here (Fig. 8 F) is the holotype (NHMM JJ 10490 a), while the other figured ossicles in lot NHMM JJ 10490 are paratypes. Additional material includes around 50 isolated ossicles (lot NHMM JJ 9591). All material is from the upper Maastrichtian (Maastricht Formation, Emael Member, Lava Horizon) at the CBR-Romontbos Quarry, Eben Emael (Liège, northeast Belgium).		1														https://treatment.plazi.org/id/F160A3677167FFA1FD9E760FFBBB227A#C9A1182C7167FFA3FF4A7443FAE623F1				MaterialCitation
F160A3677165FFA5FDB071FEFC98256E.mc.C9A1182C7160FFA4FF4A753CFA8B2356	F160A3677165FFA5FDB071FEFC98256E.taxon	NHMM JJ 11736		NHMM		A set of> 100 associated ossicles (marginals, a single terminal, abactinals, actinals, orals, circumorals, odontophores, adambulacrals, ambulacrals, marginal spines, adambulacral spines and oral spines) from ca 12 metres below the Cretaceous-Paleogene (K / Pg) boundary in the upper Maastrichtian Højerup Member (Tor Formation; Surlyk et al. 2006) at Kulsti Rende, Stevns Klint, eastern Denmark, is the holotype (NHMM JJ 11736). Additional material includes disarticulated, yet associated, ossicles of another individual from the same locality and stratigraphical unit, as well as isolated marginal ossicles from several localities exposing Cenomanian – Maastrichtian rocks in the United Kingdom (Kent, Hampshire), Belgium, Germany (Rügen, SNSB-BGSP collections; Aachen area) and the Czech Republic, including ossicles from the lower Campanian Chalk of Downend, Hampshire (Gale 1980).		1														https://treatment.plazi.org/id/F160A3677165FFA5FDB071FEFC98256E#C9A1182C7160FFA4FF4A753CFA8B2356				MaterialCitation
F160A3677161FFABFDC37293FCA7230E.mc.C9A1182C7161FFA5FF4A7059FB5A27D0	F160A3677161FFABFDC37293FCA7230E.taxon	SNSB-BGSP 2020 XLV 31, SNSB-BGSP 2020 XLV 32-39, SNSB-BGSP 2020 XLV 32				The interradial marginal pair (Fig. 12 A) is the holotype (SNSB-BGSP 2020 XLV 31); the other eight ossicles illustrated here are paratypes (SNSB-BGSP 2020 XLV 32 – 39), all from the upper lower Maastrichtian Chalk of Rügen, northeast Germany. Additional material includes over 30 marginal ossicles and other ossicles from the same locality (lot SNSB-BGSP 2020 XLV 32).		1														https://treatment.plazi.org/id/F160A3677161FFABFDC37293FCA7230E#C9A1182C7161FFA5FF4A7059FB5A27D0				MaterialCitation
F160A367716FFFABFDA27470FB8C2699.mc.C9A1182C716FFFABFF4A7357FC25248D	F160A367716FFFABFDA27470FB8C2699.taxon					Seventeen marginal ossicles; the inferomarginal figured (Fig. 6 A) is MHI 2183 / 7; the other inferomarginal and oral ossicle illustrated here are MHI 2183 / 8 and 9. All are from the Maantang Formation (Carnian, Upper Triassic; sample C 30) at Jiancougou, Sechuan Province, China.		1														https://treatment.plazi.org/id/F160A367716FFFABFDA27470FB8C2699#C9A1182C716FFFABFF4A7357FC25248D				MaterialCitation
F160A367716CFFA8FDA174D1FEE727D0.mc.C9A1182C716CFFA8FF4A72F1FAEA2666	F160A367716CFFA8FDA174D1FEE727D0.taxon	NHMUK PI EE 17997		NHMUK		The arm fragment (NHMUK PI EE 17997) from the Albian Red Chalk (Hunstanton Formation) at Speeton, Yorkshire (United Kingdom) is the holotype and single specimen known to date. The specimen was originally articulated; it was subsequently reconstructed on plasticene by the Wright brothers.		1														https://treatment.plazi.org/id/F160A367716CFFA8FDA174D1FEE727D0#C9A1182C716CFFA8FF4A72F1FAEA2666				MaterialCitation
F160A367716DFFA9FD87760EFEAE263A.mc.C9A1182C716DFFA9FF4A75E8FD032390	F160A367716DFFA9FD87760EFEAE263A.taxon	Nds LH 105.107, NHMUK PI EE 17998-18004		NHMUK		A distal arm fragment (Nds LH 105.107), comprising five marginal pairs, with articulating spines preserved, is the holotype; it is from the lower Hauterivian (Endemoceras amblygonium ammonite Zone) at Engelbostel near Hannover (northern Germany). Paratypes (NHMUK PI EE 17998 – 18004) are 35 marginal ossicles and a single oral ossicle from the upper 3 metres of the Tealby Clay (Hauterivian) at Nettleton, Lincolnshire (United Kingdom).		1														https://treatment.plazi.org/id/F160A367716DFFA9FD87760EFEAE263A#C9A1182C716DFFA9FF4A75E8FD032390				MaterialCitation
F160A367716BFFACFDD0724BFB7727D1.mc.C9A1182C716BFFAFFF4A71D0FCB327D0	F160A367716BFFACFDD0724BFB7727D1.taxon	MZA L13a		MZA		The holotype (MZA L 13 a) is a complete asteroid in a claystone matrix, comprising part and counterpart, from the Lower Jurassic (Hettangian, liasicus ammonite Zone) of Hallau, Canton Schaffhausen, Switzerland (Peyer 1944). It is contained in the collections of the Museum zu Aller Heiligen, Schaffhausen, and has suffered from considerable over-preparation. Additional material includes a suite of specimens from the same locality and horizon, most notably, specimen MZA L 13 b / 32 a-e, which is a partially dissociated individual of which one arm is well preserved (Blake 1984: fig. 1 a – g). This specimen is coated with a glue-like substance which obscures much detail and requires specialist preparation. The present description is based on these two individuals.		1														https://treatment.plazi.org/id/F160A367716BFFACFDD0724BFB7727D1#C9A1182C716BFFAFFF4A71D0FCB327D0				MaterialCitation
F160A3677156FF93FDA2764FFB442614.mc.C9A1182C7156FF92FF4A751AFA9222A6	F160A3677156FF93FDA2764FFB442614.taxon	NMB M9683		NMB		The single specimen available (NMB M 9683) comprises fragments of three arms and dissociated ossicles, intimately entwined with an isocrinid crinoid on a single slab, from the Bajocian of Reigoldswil (Canton Baselland, Switzerland). The specimen is very fragmentary and is not easy to interpret, because pressure solution has welded scraps of calcite onto most ossicles, making discrimination of features difficult.		1														https://treatment.plazi.org/id/F160A3677156FF93FDA2764FFB442614#C9A1182C7156FF92FF4A751AFA9222A6				MaterialCitation
F160A3677154FF97FDC073B3FBB52299.mc.C9A1182C7154FF90FF4A7165FAB02734	F160A3677154FF97FDC073B3FBB52299.taxon	NHMUK PI EE 15225, NHMUK PI EE 18005-18007, 18009		NHMUK		The holotype (Texas Memorial Museum, number 1786 TX 1) is from the Grayson Formation (lower Cenomanian) at the Waco shale pit (Waco, Mclennan County, Texas, USA). Additional material comprises a magnificent individual (NHMUK PI EE 15225), collected by Frank Holterhoff from the Grayson Formation (lower Cenomanian) of Dottie Lynn, Fort Worth, Texas and illustrated here (Fig. 16 A – C), as well as numerous dissociated ossicles from the same locality (NHMUK PI EE 18005 – 18007, 18009)		1														https://treatment.plazi.org/id/F160A3677154FF97FDC073B3FBB52299#C9A1182C7154FF90FF4A7165FAB02734				MaterialCitation
