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	eventRemarks	occurrenceRemarks
8878B758BA799F394E542450FAD4F80C.mc.B0B90C13BA679F394CEE2569FDA1F91D	8878B758BA799F394E542450FAD4F80C.taxon				lectotype	The Morris types are found in a belemnite rostrum (broken in two parts) from the Upper Cretaceous Norfolk Chalk near Norwich, Great Britain. The type stratum was not further specified by Morris, but the Upper Cretaceous at Norfolk comprises the Turonian to lower Maastrichtian and the belemnite genus Belemnitella d’Orbigny, 1840 narrows down the stratigraphical range to the upper Campanian to lower Maastrichtian. The type material is deposited at the Natural History Museum in London (PI A 559). The belemnite contains, apart from many other bioerosion trace fossils, about ten specimens of D. dendrina. Morris did not designate a holotype, but one of the specimens (Fig. 2 E – G) is encircled with ink and corresponds to the position of trace 6 b on figure 6 on the original plate (Morris 1851: pl. IV, fig. 6). Based on this circumstance, and due to this specimen clearly exhibiting the diagnostic inlet tunnel, it is hereby designated as the lectotype, rendering the other specimens (e. g., Fig. 2 H – I) on the same belemnite paralectotypes.		1										United Kingdom	Norwich		Norfolk Chalk	https://treatment.plazi.org/id/8878B758BA799F394E542450FAD4F80C#B0B90C13BA679F394CEE2569FDA1F91D				MaterialCitation		
8878B758BA629F3E4E1F25B0FB24FDBB.mc.B0B90C13BA639F3D4CEE2380FA8EFC08	8878B758BA629F3E4E1F25B0FB24FDBB.taxon				holotype	The holotype (Fig. 4 A) is preserved in an epoxy resin cast of a Belemnitella mucronata rostrum from the upper Campanian stobaei / basiplana Zone, sampled in the Germania IV quarry near Misburg, Germany.		1										Germany		Misburg	Germany	https://treatment.plazi.org/id/8878B758BA629F3E4E1F25B0FB24FDBB#B0B90C13BA639F3D4CEE2380FA8EFC08				MaterialCitation		
8878B758BA629F3E4E1F25B0FB24FDBB.mc.B0B90C13BA609F3E4CEE2106FA8DFE8A	8878B758BA629F3E4E1F25B0FB24FDBB.taxon				holotype	One paratype (Fig. 4 B) is found on the same and further paratypes (e. g., Fig. 4 C) on three other epoxy casts from belemnite rostra sampled at the type locality and from an outcrop near Lägerdorf, Germany.		1										Germany		Misburg	Lagerdorf	https://treatment.plazi.org/id/8878B758BA629F3E4E1F25B0FB24FDBB#B0B90C13BA609F3E4CEE2106FA8DFE8A				MaterialCitation		
8878B758BA6C9F334E15229AFCF0FC61.mc.B0B90C13BA6D9F334CEE213BFA8EFD85	8878B758BA6C9F334E15229AFCF0FC61.taxon	NYSM 6697		NYSM	lectotype	Clarke (1908) depicted two drawings (syntypes; Fig. 6 A, C), none of which designated as the holotype. Clarke (1921) reproduced both of his original illustrations and again did not explicitly indicate a holotype. Plewes (1996) re-illustrated both of the specimens Clarke based his drawings upon (1908: pl. 12, figs 1 – 2) and both appear to be damaged. The less damaged specimen (Clarke 1908: pl. 12, fig. 2) was considered as the holotype, whereas the other specimen was qualified as “ damaged beyond recognition ”. However, since her illustration as well as new images of this specimen indicate that this is not the case, and since the trace depicted by Clarke (1908: pl. 12, fig. 1) does match his original description much more closely, it his herein formally selected as the lectotype (Fig. 6 A – B), rendering the other specimen		1										United States of America	New York		Portage Beds	https://treatment.plazi.org/id/8878B758BA6C9F334E15229AFCF0FC61#B0B90C13BA6D9F334CEE213BFA8EFD85				MaterialCitation		
8878B758BA6C9F334E15229AFCF0FC61.mc.B0B90C13BA6D9F334CEE225DFEF0FD17	8878B758BA6C9F334E15229AFCF0FC61.taxon	NYSM 6698		NYSM	paralectotype	a paralectotype (Fig. 6 C – D). The lectotype, a natural cast in a Loxopteria dispar shell from the Portage Beds, Upper Devonian, from Correll’s Point, New York, USA, is housed in the New York State Museum (NYSM 6697). The paralectotype is a natural cast in a Loxonema danai from the type locality (NYSM 6698).		1										United States of America	New York		Portage Beds	https://treatment.plazi.org/id/8878B758BA6C9F334E15229AFCF0FC61#B0B90C13BA6D9F334CEE225DFEF0FD17				MaterialCitation		
8878B758BA6A9F354DAD2106FE5FF9C9.mc.B0B90C13BA6B9F354CEE241FFC1CFB55	8878B758BA6A9F354DAD2106FE5FF9C9.taxon			XXVI	holotype	The holotype (Fig. 7 A – C) is preserved as a natural cast in a brachiopod shell from the Flaser-Schiefer, Kondel-Gruppe, Oberkoblenz, Devonian, from Brodenbach Valley near the river Mosel in a small quarry opposite the Teufelslei near Münstermaifeld, Germany. Deposited in the brachiopod collection at the Senckenberg Institute in Frankfurt, Germany (SMF XXVI 166 a).		1										Germany			Brodenbach Valley near the river Mosel	https://treatment.plazi.org/id/8878B758BA6A9F354DAD2106FE5FF9C9#B0B90C13BA6B9F354CEE241FFC1CFB55				MaterialCitation		
8878B758BA6B9F374D9C2653FDCDFC81.mc.B0B90C13BA699F374CEE2134FD53FE7E	8878B758BA6B9F374D9C2653FDCDFC81.taxon				holotype	The holotype (Fig. 8 A) was epoxy cast in a shell of the brachiopod Athyris McCoy, 1844 from the Otisco Member, Middle Devonian, sampled at a cliff exposure along a railroad cut 300 m E of Portland Point, Cayuga County, New York, USA. It is deposited at the Institut für Geowissenschaften, Goethe-Universität, Frankfurt, Germany (Bo 1 / 4).		1						300				United States of America	New York		cliff exposure along a railroad cut	https://treatment.plazi.org/id/8878B758BA6B9F374D9C2653FDCDFC81#B0B90C13BA699F374CEE2134FD53FE7E				MaterialCitation		
8878B758BA699F094DC12383FD90FD86.mc.B0B90C13BA569F084CEE22EEFC03FCA4	8878B758BA699F094DC12383FD90FD86.taxon				holotype	The holotype (Fig. 9 A – B) was epoxy cast in a Mediospirifer brachiopod shell from the Windom Member, Middle Devonian, sampled at Barnum Creek quarry just W of NY highway 89 and 0.2 km S of the Ovid / Romulus town line, Seneca County, New York, USA. It is deposited at the Institut für Geowissenschaften, Goethe-Universität, Frankfurt, Germany (Bo 1 / 8).		1										United States of America	New York	It	Seneca County	https://treatment.plazi.org/id/8878B758BA699F094DC12383FD90FD86#B0B90C13BA569F084CEE22EEFC03FCA4				MaterialCitation		
8878B758BA579F0A4DB4229FFD48FB0F.mc.B0B90C13BA549F0A4CEE2325FB90FC6F	8878B758BA579F0A4DB4229FFD48FB0F.taxon				holotype	The type material comprises various specimens in several epoxy resin casts of Ostrea oyster shells sampled in an old quarry near the northern limit of the Swedish lake island Ivö; lower Campanian, Cretaceous. Of the two specimens on the cast indicated as “ holotype ”, the one illustrated on Hofmann’s plate 9, figure 5 – 6 is hereby designated as the lectotype (Fig. 10 A – C), rendering the		3													near the northern limit of the Swedish lake island Ivo	https://treatment.plazi.org/id/8878B758BA579F0A4DB4229FFD48FB0F#B0B90C13BA549F0A4CEE2325FB90FC6F				MaterialCitation		
8878B758BA579F0A4DB4229FFD48FB0F.mc.B0B90C13BA549F0A483E239FFF1EFC0C	8878B758BA579F0A4DB4229FFD48FB0F.taxon					other specimens on this and		1														https://treatment.plazi.org/id/8878B758BA579F0A4DB4229FFD48FB0F#B0B90C13BA549F0A483E239FFF1EFC0C				MaterialCitation		
8878B758BA579F0A4DB4229FFD48FB0F.mc.B0B90C13BA549F0A4CBE23B8FDC9FBD5	8878B758BA579F0A4DB4229FFD48FB0F.taxon				paralectotype	three other casts paralectotypes. The type material is deposited at the Institut für Geowissenschaften, Goethe Universität, Frankfurt, Germany (Bo 5 / 146: 146.1 = lectotype and one paralectotype, 146.2 to 146.4 = further paralectotypes).		1														https://treatment.plazi.org/id/8878B758BA579F0A4DB4229FFD48FB0F#B0B90C13BA549F0A4CBE23B8FDC9FBD5				MaterialCitation		
8878B758BA559F0D4E7E2429FC58FA41.mc.B0B90C13BA539F0D4CEE2428FCDDFB46	8878B758BA559F0D4E7E2429FC58FA41.taxon	(MLU.Mag1937.IV.4		MLU, IV	holotype	Holotype (Fig. 11 A – C) preserved in rostrum of Belemnitella mucronata from the Upper Cretaceous of Misburg near Hannover, Germany, deposited in the collection of the Institut für Geowissenschaften und Geographie, Halle, Germany (MLU. Mäg 1937. IV. 4).		1	1937-05									Germany		Geographie	Misburg near Hannover	https://treatment.plazi.org/id/8878B758BA559F0D4E7E2429FC58FA41#B0B90C13BA539F0D4CEE2428FCDDFB46				MaterialCitation		
8878B758BA539F0E4E4625DBFDA7FC22.mc.B0B90C13BA509F0E4CEE22ABFBB8FCC4	8878B758BA539F0E4E4625DBFDA7FC22.taxon	MLU.Mag1937.IV.9		MLU, IV	holotype	Holotype (Fig. 12 A – C) preserved in rostrum of an Actinocamax Miller, 1826 (belemnite) from the Upper Cretaceous of Misburg near Hannover, Germany, deposited in the collections of the Institut für Geowissenschaften und Geographie, Halle, Germany (MLU. Mäg 1937. IV. 9).		1	1937-05									Germany		Geographie	Misburg near Hannover	https://treatment.plazi.org/id/8878B758BA539F0E4E4625DBFDA7FC22#B0B90C13BA509F0E4CEE22ABFBB8FCC4				MaterialCitation		
8878B758BA509F004D8E2420FA8EFAE5.mc.B0B90C13BA5E9F004CEE2289FE49FCCB	8878B758BA509F004D8E2420FA8EFAE5.taxon	MLU.Mag1937.IV.5		MLU	holotype	The holotype is preserved in a rostrum of an Actinocamax from the Upper Cretaceous of Misburg near Hannover, Germany. It used to be deposited at the collections of the Institut für Geowissenschaften und Geographie, Halle, Germany, where only the original glass negative (MLU. Mäg 1937. IV. 5) presently remains (Fig. 13 A).		1										Germany		It	Misburg near Hannover	https://treatment.plazi.org/id/8878B758BA509F004D8E2420FA8EFAE5#B0B90C13BA5E9F004CEE2289FE49FCCB				MaterialCitation		
8878B758BA509F004D8E2420FA8EFAE5.mc.B0B90C13BA5E9F004DEE22E3FDBAFC57	8878B758BA509F004D8E2420FA8EFAE5.taxon	MLU.Mag1937.IV.10		MLU	neotype	Consequently, another specimen (Fig. 13 B – C) within the original material of Mägdefrau from the same type horizon and locality, on the same belemnite (MLU. Mäg 1937. IV. 10) that carries the holotype of Dictyoporus nodosus Mägdefrau, 1937, was selected as the neotype by Plewes (1996). Since the latter designation was not a valid nomenclatural act (unpublished thesis), this neotype designation is hereby formalised.		1										Germany		It	Misburg near Hannover	https://treatment.plazi.org/id/8878B758BA509F004D8E2420FA8EFAE5#B0B90C13BA5E9F004DEE22E3FDBAFC57				MaterialCitation		
8878B758BA5E9F024DA62577FE2BFB76.mc.B0B90C13BA5F9F024CEE22DAFA8EFEE6	8878B758BA5E9F024DA62577FE2BFB76.taxon				holotype	The type material consists of a cast with many specimens, collectively addressed as “ holotype ” in the original publication, in a resin cast of a shell of Pecten O. F. Müller, 1776 from the Sophia Jakoba 8 II locality, Niederrheinische Bucht, Germany; Grafenberger Sand Member, Upper Oligocene.		1										Germany		Grafenberger Sand Member	Sophia Jakoba 8 II locality	https://treatment.plazi.org/id/8878B758BA5E9F024DA62577FE2BFB76#B0B90C13BA5F9F024CEE22DAFA8EFEE6				MaterialCitation		
8878B758BA5E9F024DA62577FE2BFB76.mc.B0B90C13BA5C9F024CEE2122FC1AFE4C	8878B758BA5E9F024DA62577FE2BFB76.taxon					Numerous further specimens collectively addressed as “ paratypes ” in several casts of another Pecten shell from the same locality, and in casts of an Ostrea shell from the Sophia Jakoba 6 locality, Lower Rhine Embayment; Germany, Ratheimer Beds, Lower Oligocene. Hereby		1														https://treatment.plazi.org/id/8878B758BA5E9F024DA62577FE2BFB76#B0B90C13BA5C9F024CEE2122FC1AFE4C				MaterialCitation		
8878B758BA5D9F064E6124C7FC4AFEAF.mc.B0B90C13BA5B9F054CEE24EDFB80FA83	8878B758BA5D9F064E6124C7FC4AFEAF.taxon	MLU.Mag1937.IV.10		MLU	holotype	The holotype (Fig. 15 A – B) is preserved in a Belemnitella mucronata (Schlotheim, 1813) rostrum from the Upper Cretaceous of Misburg near Hannover, Germany, deposited in the collections of the Institut für Geowissenschaften und Geographie, Halle, Germany (MLU. Mäg 1937. IV. 10).		1										Germany		Institut fur Geowissenschaften und Geographie	Misburg near Hannover	https://treatment.plazi.org/id/8878B758BA5D9F064E6124C7FC4AFEAF#B0B90C13BA5B9F054CEE24EDFB80FA83				MaterialCitation		
8878B758BA589F074D2521B4FDADFAAD.mc.B0B90C13BA599F074CEE2380FEC0FBD3	8878B758BA589F074D2521B4FDADFAAD.taxon	HU-62706		CA	holotype	Holotype (Fig. 16 A – B) in resin-cast of a Balanus fragment from the Purisima Formation, Pliocene, sampled at the base of a sea cliff at Capitola State Beach, Capitola, CA, USA. It is supposedly deposited in the Harvard University Paleobotanical Collection (HU- 62706), but is at present not traceable in this collection.		1										United States of America	CA	Harvard University Paleobotanical Collection	Purisima Formation	https://treatment.plazi.org/id/8878B758BA589F074D2521B4FDADFAAD#B0B90C13BA599F074CEE2380FEC0FBD3				MaterialCitation		
8878B758BA469F1A4E6D258AFC4AFB94.mc.B0B90C13BA449F1A4CEE23D9FC4AFB94	8878B758BA469F1A4E6D258AFC4AFB94.taxon	MLU.Mag1937.V.1		MLU	lectotype	Traces in fish scale from the Oligocene of Salbe, Germany, deposited in the collections of the Institut für Geowissenschaften und Geographie, Halle, Germany (MLU. Mäg 1937. V. 1). Because the fish scale contains numerous individuals of A. riccioides (syntypes), the complete and readily typical specimen shown in Fig. 17 D (arrow) is hereby designated as the lectotype.		1										Germany			Salbe	https://treatment.plazi.org/id/8878B758BA469F1A4E6D258AFC4AFB94#B0B90C13BA449F1A4CEE23D9FC4AFB94				MaterialCitation		
8878B758BA449F1B4E1A24A9FC22FC7E.mc.B0B90C13BA459F1B4CEE228EFEF3FCE9	8878B758BA449F1B4E1A24A9FC22FC7E.taxon	MLU.Mag1937.V.2		MLU	lectotype	Traces in fish scale from the Oligocene Septarienton of Eöthen, Germany, deposited in the collections of the Institut für Geowissenschaften und Geographie, Halle, Germany (MLU. Mäg 1937. V. 2). Because the scale contains several specimens of A. procera (syntypes), the most complete one (Fig. 18 B) is hereby designated as the lectotype, which is in accordance with the original figure (Mägdefrau 1937: pl. V, fig. 2).		1										Germany			Septarienton of Eothen	https://treatment.plazi.org/id/8878B758BA449F1B4E1A24A9FC22FC7E#B0B90C13BA459F1B4CEE228EFEF3FCE9				MaterialCitation		
8878B758BA429F1F4DB52269FBC4FB6A.mc.B0B90C13BA439F1F4CEE2794FD2FFE8A	8878B758BA429F1F4DB52269FBC4FB6A.taxon	Bo 13/159			neotype	The hereby designated neotype (= former holotype of junior synonym Semidendrina pulchra; Fig. 19 C – E) is cast in epoxy from a Lopha sp. bivalve shell from Villers-sur-Mer, France; Argiles à Fig. 19. Nododendrina europaea (Fischer, 1875). A – B. Original illustrations of the trace as observed in a transparent shell of the bivalve Pecten opercularis (Linnaeus, 1758) from the Gulf of Gascogne, France (reproduced from Fischer 1875: pl. XVI, figs 5 – 6; no scale). C – E. SEM overview and close-up of the neotype (= holotype of the junior synonym Semidendrina pulchra Bromley et al., 2007) in an epoxy cast of an Upper Jurassic Lopha shell from Villers-sur-Mer, France. F. SEM of an ontogenetic series as recorded in an epoxy cast of a bivalve shell that was exposed for two years at a depth of 15 m in the Kosterfjord, Sweden (modified from Wisshak 2006). Lopha gregarea, Oxfordian, Upper Jurassic. Deposited at the Institut für Geowissenschaften, Goethe-Universität, Frankfurt, Germany (Bo 13 / 159).		1										France			Villers-sur-Mer	https://treatment.plazi.org/id/8878B758BA429F1F4DB52269FBC4FB6A#B0B90C13BA439F1F4CEE2794FD2FFE8A				MaterialCitation		
8878B758BA419F114DEC24F0FDCBFAE9.mc.B0B90C13BA4F9F114CEE21E8FA8FFDAB	8878B758BA419F114DEC24F0FDCBFAE9.taxon	MLU.Mag1937.IV.2		MLU	lectotype	Several dozen type specimens (Fig. 20 A) of N. incomposita are preserved in a brachiopod shell from the Lower Maastrichtian (Upper Cretaceous) of Rügen, Germany, deposited in the collections of the Institut für Geowissenschaften und Geographie, Halle, Germany (MLU. Mäg 1937. IV. 2). One of these specimens (indicated by an arrow in Fig. 20 A) is hereby selected as the lectotype, rendering the other		1										Germany			Rugen	https://treatment.plazi.org/id/8878B758BA419F114DEC24F0FDCBFAE9#B0B90C13BA4F9F114CEE21E8FA8FFDAB				MaterialCitation		
8878B758BA419F114DEC24F0FDCBFAE9.mc.B0B90C13BA4F9F114CEE227FFD31FD4F	8878B758BA419F114DEC24F0FDCBFAE9.taxon	MLU.Mag1937.IV.2		MLU	paralectotype	specimens in the brachiopod paralectotypes.		1										Germany			Rugen	https://treatment.plazi.org/id/8878B758BA419F114DEC24F0FDCBFAE9#B0B90C13BA4F9F114CEE227FFD31FD4F				MaterialCitation		
8878B758BA4F9F134D85257AFC44FE70.mc.B0B90C13BA4C9F124CEE2365FDBBFBF0	8878B758BA4F9F134D85257AFC44FE70.taxon				syntype	Various syntypes (Fig. 21 A) are preserved in a natural cast of a dorsal valve of a Buxtonia semicircularis brachiopod from the Late Mississippian Redoak Hollow Formation, exposed in the vicinity of the village of Milo, Carter County, Oklahoma, USA. The type material used to be deposited in the collections of the Geological Survey of Nebraska, but the empty drawer contains a note only, with the information that the collection was “ scrutinised ” in the 1990 s; the current whereabouts of the material is unknown (Robert Diffendal, pers. comm.).		1										United States of America	Oklahoma		Late Mississippian Redoak Hollow Formation	https://treatment.plazi.org/id/8878B758BA4F9F134D85257AFC44FE70#B0B90C13BA4C9F124CEE2365FDBBFBF0				MaterialCitation		
8878B758BA4D9F144DB021F2FC5FFB79.mc.B0B90C13BA4A9F144CEE22BCFB50FCF6	8878B758BA4D9F144DB021F2FC5FFB79.taxon	Bo 1/1		Bo	holotype	Holotype (Fig. 22 A) is cast in epoxy from a Mediospirifer brachiopod shell from the Erie lakeshore bluffs S of the mouth of Eighteenmile Creek 4.0 – 5.5 km SW of Wanakah, New York, USA. Wanakah Member, Ludlowville Formation, Hamilton Group, Givetian, Devonian. The holotype is deposited in the Institut für Geowissenschaften, Goethe-Universität, Frankfurt, Germany (Bo 1 / 1).		1										United States of America	New York	Goethe-Universitat	Erie lakeshore bluffs S of the mouth of Eighteenmile Creek	https://treatment.plazi.org/id/8878B758BA4D9F144DB021F2FC5FFB79#B0B90C13BA4A9F144CEE22BCFB50FCF6				MaterialCitation		
8878B758BA4B9F164E152106FE7AFA22.mc.B0B90C13BA489F164CEE238AFDF4FC62	8878B758BA4B9F164E152106FE7AFA22.taxon	GSC 10854		UTM, GSC	holotype	Holotype (Fig. 23 A – B) and		1										Canada	Quebec	Geological Survey	southern Anticosti Island	https://treatment.plazi.org/id/8878B758BA4B9F164E152106FE7AFA22#B0B90C13BA489F164CEE238AFDF4FC62				MaterialCitation		
8878B758BA4B9F164E152106FE7AFA22.mc.B0B90C13BA489F164E4A2385FC0FFBCF	8878B758BA4B9F164E152106FE7AFA22.taxon	GSC 10854		UTM, GSC	paratype	paratype are cast in epoxy from a shell of the brachiopod Pentamerus palaformis Jin & Copper, 2000 from locality A 1187 (UTM: 12 E / 1 544400 / 5454300), southern Anticosti Island, Québec, Canada. Goéland Member, Jupiter Formation, Early Silurian. They are deposited at the Geological Survey of Canada, Ottawa, Ontario, Canada (GSC 10854).		1										Canada	Quebec	Geological Survey	southern Anticosti Island	https://treatment.plazi.org/id/8878B758BA4B9F164E152106FE7AFA22#B0B90C13BA489F164E4A2385FC0FFBCF				MaterialCitation		
8878B758BA489F684E362623FC03FC4C.mc.B0B90C13BA499F174CEE21E5FD94FDC0	8878B758BA489F684E362623FC03FC4C.taxon	SMF XXX 864			holotype	The holotype (Fig. 24 A – B) and one		1				76.38333	15.95	80				Svalbard and Jan Mayen		Shelf	Expedition	https://treatment.plazi.org/id/8878B758BA489F684E362623FC03FC4C#B0B90C13BA499F174CEE21E5FD94FDC0				MaterialCitation		
8878B758BA489F684E362623FC03FC4C.mc.B0B90C13BA499F174E2421E4FCA8FD53	8878B758BA489F684E362623FC03FC4C.taxon	SMF XXX 865		SMF	paratype	paratype (Fig. 24 C – D), together with several further specimens, are cast in epoxy resin from a subfossil (possibly Late Pleistocene to probably Holocene) shell of the bivalve Chlamys islandica (O. F. Müller, 1776), sampled in 75 to 85 m water depth at Sørkappbanken, SW Svalbard Shelf (76 ° 23 ′ N, 15 ° 57 ′ E; station 15 / 161 - AGT of the ARK VI / 1 - 4 Expedition of the RV Polarstern in 1989; see Krause et al. 1991 for details).		1				76.38333	15.95	80				Svalbard Shelf		Shelf	Sorkappbanken	https://treatment.plazi.org/id/8878B758BA489F684E362623FC03FC4C#B0B90C13BA499F174E2421E4FCA8FD53				MaterialCitation		
8878B758BA369F694E3E23EEFCB9FD05.mc.B0B90C13BA369F684CEE2631FD07F920	8878B758BA369F694E3E23EEFCB9FD05.taxon	BSPG 2007 XII 12		BSPG	holotype	The holotype (Fig. 25 A – E) is cast in epoxy of a bivalve shell from the Buckhorn Asphalt, Boggy Formation, Deese group, Desmoinesian, middle Pennsylvanian, sampled at the Buckhorn Asphalt Quarry, Oklahoma, USA. The epoxy cast is stored in the Bayerische Staatssammlung für Paläontologie und Geologie München, Germany (BSPG 2007 XII 12 d). For further details about the type locality and its ichnological record, see Wisshak et al. (2008)		1										United States of America	Oklahoma	The	Boggy Formation	https://treatment.plazi.org/id/8878B758BA369F694E3E23EEFCB9FD05#B0B90C13BA369F684CEE2631FD07F920				MaterialCitation		
8878B758BA379F6B4E34231FFBB3FEAF.mc.B0B90C13BA349F6A4CEE23BDFCFCFB9B	8878B758BA379F6B4E34231FFBB3FEAF.taxon	SMF XXX 866		SMF	holotype	Holotype (Fig. 26 A – D) and a number of additional specimens cast in epoxy from a Lophelia pertusa coral skeleton from the Lindos Bay Formation, Middle Pleistocene, found at isolated hill one km SW of Lardos, Rhodes, Greece. For further details concerning the type locality and its ichnological record, see Titschack et al. (2013) and Wisshak (2008). Deposited in the trace fossil collection of the Senckenberg Institute in Frankfurt, Germany (SMF XXX 866).		1										Greece		Deposited	Lindos Bay Formation	https://treatment.plazi.org/id/8878B758BA379F6B4E34231FFBB3FEAF#B0B90C13BA349F6A4CEE23BDFCFCFB9B				MaterialCitation		
8878B758BA329F6E4E7A2447FC35F99E.mc.B0B90C13BA329F6E494327C2FE8BFEE6	8878B758BA329F6E4E7A2447FC35F99E.taxon	SMF XXX 867		E, F	holotype	holotype (Fig. 27 E) and		1										Germany			Germany	https://treatment.plazi.org/id/8878B758BA329F6E4E7A2447FC35F99E#B0B90C13BA329F6E494327C2FE8BFEE6				MaterialCitation		
8878B758BA329F6E4E7A2447FC35F99E.mc.B0B90C13BA309F6E4DD32106FD46FE4C	8878B758BA329F6E4E7A2447FC35F99E.taxon	SMF XXX 867		E, F	paratype	four paratypes (Fig. 27 A – D, F) are preserved in three epoxy resin casts, together with many other traces of the new ichnospecies, and are deposited in the trace fossil collection of the Senckenberg Institute in Frankfurt, Germany (SMF XXX 867, including the holotype, SMF XXX 868, including one paratype and SMF XXX 869,		1										Germany			Germany	https://treatment.plazi.org/id/8878B758BA329F6E4E7A2447FC35F99E#B0B90C13BA309F6E4DD32106FD46FE4C				MaterialCitation		
8878B758BA329F6E4E7A2447FC35F99E.mc.B0B90C13BA309F6E4E952178FBF8FE4C	8878B758BA329F6E4E7A2447FC35F99E.taxon	SMF XXX 869		E, F	paratype	including three paratypes).		1										Germany			Germany	https://treatment.plazi.org/id/8878B758BA329F6E4E7A2447FC35F99E#B0B90C13BA309F6E4E952178FBF8FE4C				MaterialCitation		
8878B758BA319F614E502106FCB1FD1E.mc.B0B90C13BA319F6F4CEE23EDFDBDFC39	8878B758BA319F614E502106FCB1FD1E.taxon	SMF XXX 870		SMF	holotype	The holotype (Fig. 28 A) and the		1										Greece		Marine Isotope Stage	Lindos Bay Formation	https://treatment.plazi.org/id/8878B758BA319F614E502106FCB1FD1E#B0B90C13BA319F6F4CEE23EDFDBDFC39				MaterialCitation		
8878B758BA319F614E502106FCB1FD1E.mc.B0B90C13BA319F6F4E1E23EDFB09FB69	8878B758BA319F614E502106FCB1FD1E.taxon	SMF XXX 870		SMF	paratype	paratype (Fig. 28 B – C) are found in the same epoxy resin cast from a shell of the bivalve Acanthocardia echinata (Linnaeus, 1758), sampled at the northern flank of an isolated hill one km SW of Lardos village, Rhodes, Greece, in a rhodolith bed determined as Marine Isotope Stage 12, Lindos Bay Formation, Middle Pleistocene. For further details on the type locality and its ichnological record see Titschack et al. (2013) and Wisshak (2008). The epoxy cast is deposited in the trace fossil collection of the Senckenberg Institute in Frankfurt, Germany (SMF XXX 870).		1										Greece		Marine Isotope Stage	northern flank of an isolated hill	https://treatment.plazi.org/id/8878B758BA319F614E502106FCB1FD1E#B0B90C13BA319F6F4E1E23EDFB09FB69				MaterialCitation		
8878B758BA3F9F624E4A233FFB51FE3C.mc.B0B90C13BA3F9F614CEE258EFDF8FA5E	8878B758BA3F9F624E4A233FFB51FE3C.taxon	SMF XXX 871		SMF	holotype	The holotype (Fig. 29 A – E),		1										Australia	Victoria		Senckenberg Institute in Frankfurt	https://treatment.plazi.org/id/8878B758BA3F9F624E4A233FFB51FE3C#B0B90C13BA3F9F614CEE258EFDF8FA5E				MaterialCitation		
8878B758BA3F9F624E4A233FFB51FE3C.mc.B0B90C13BA3F9F614E5B258EFAE2F9C4	8878B758BA3F9F624E4A233FFB51FE3C.taxon	SMF XXX 871		SMF	paratype	two paratypes (Fig. 29 F – H) and several further specimens are cast in epoxy resin of a bivalve shell, sampled in the Balcome Clay, Fyansford Formation, Middle Miocene strata at Fossil Beach, Balcombe Bay, ~ 3 km S of Mornington, Victoria, Australia. The epoxy cast is deposited in the trace fossil collection of the Senckenberg Institute in Frankfurt, Germany (SMF XXX 871).		1										Australia	Victoria		Balcome Clay	https://treatment.plazi.org/id/8878B758BA3F9F624E4A233FFB51FE3C#B0B90C13BA3F9F614E5B258EFAE2F9C4				MaterialCitation		
8878B758BA3D9F644E722106FE07FA7D.mc.B0B90C13BA3D9F634CEE2360FDF3FC44	8878B758BA3D9F644E722106FE07FA7D.taxon	SMF XXX 872		SMF	holotype	The holotype (Fig. 30 D) and		1						15				Australia	Orpheus Island	The	Senckenberg Institute in Frankfurt	https://treatment.plazi.org/id/8878B758BA3D9F644E722106FE07FA7D#B0B90C13BA3D9F634CEE2360FDF3FC44				MaterialCitation		
8878B758BA3D9F644E722106FE07FA7D.mc.B0B90C13BA3D9F644E412363FAC0FE8A	8878B758BA3D9F644E722106FE07FA7D.taxon	SMF XXX 872		SMF	paratype	two paratypes (Fig. 30 C, E – F) are found in the same epoxy resin cast from an experimental bivalve shell (Callista) that was bioeroded at a water depth of 15 m in Pioneer Bay, Orpheus Island, Great Barrier Reef, Australia. The cast bearing the holotype and paratypes is deposited in the trace fossil collection of the Senckenberg Institute in Frankfurt, Germany (SMF XXX 872).		1						15				Australia	Orpheus Island	The	Pioneer Bay	https://treatment.plazi.org/id/8878B758BA3D9F644E722106FE07FA7D#B0B90C13BA3D9F644E412363FAC0FE8A				MaterialCitation		
8878B758BA3B9F664E6F21FFFB9EFE70.mc.B0B90C13BA3B9F654CEE23FCFD98FBC8	8878B758BA3B9F664E6F21FFFB9EFE70.taxon	SMF XXX 873		SMF	holotype	The holotype (Fig. 31 A – C) and the		1										Germany		The	Senckenberg Institute in Frankfurt	https://treatment.plazi.org/id/8878B758BA3B9F664E6F21FFFB9EFE70#B0B90C13BA3B9F654CEE23FCFD98FBC8				MaterialCitation		
8878B758BA3B9F664E6F21FFFB9EFE70.mc.B0B90C13BA3B9F654E3A23FFFADAFB5B	8878B758BA3B9F664E6F21FFFB9EFE70.taxon	SMF XXX 874		SMF	paratype	paratype (Fig. 31 D), together with numerous further specimens in all stages of ontogeny, are cast in epoxy resin from two fragments of Inoceramus sp. bivalve shells from the Upper Campanian (grimmensis / granulosus Zone), sampled in the Saturn Quarry near Kronsmoor, Germany. The casts are deposited in the trace fossil collection of the Senckenberg Institute in Frankfurt, Germany (SMF XXX 873, including the holotype, and SMF XXX 874, including the paratype).		1										Germany		The	Saturn Quarry near Kronsmoor	https://treatment.plazi.org/id/8878B758BA3B9F664E6F21FFFB9EFE70#B0B90C13BA3B9F654E3A23FFFADAFB5B				MaterialCitation		
