taxonID	type	format	identifier	references	title	description	created	creator	contributor	publisher	audience	source	license	rightsHolder	datasetID
15297C4EFFFE387F6BC6C86BFD14C68D.taxon	http://purl.org/dc/dcmitype/StillImage	image/png	https://zenodo.org/record/10272172/files/figure.png	https://doi.org/10.5281/zenodo.10272172	Fig. 2. Holotype and only specimen of Ferussina petofiana Páll-Gergely, sp. n.: A–D, F = various views of the shell; E = aperture; G: protoconch and first teleoconch whorls; H = Arrows	Fig. 2. Holotype and only specimen of Ferussina petofiana Páll-Gergely, sp. n.: A–D, F = various views of the shell; E = aperture; G: protoconch and first teleoconch whorls; H = Arrows	2023-10-06	Tang, Jin;Zhang, Gongaote;Guo, Junqi;Luo, Lingxuan;Jiang, Jiamei;Pan, Hongbo		Zenodo	biologists	Tang, Jin;Zhang, Gongaote;Guo, Junqi;Luo, Lingxuan;Jiang, Jiamei;Pan, Hongbo			
15297C4EFFFE387F6BC6C86BFD14C68D.taxon	http://purl.org/dc/dcmitype/StillImage	image/png	https://zenodo.org/record/10272176/files/figure.png	https://doi.org/10.5281/zenodo.10272176	Fig. 3. Artistic reconstruction of Ferussina petofiana Páll-Gergely, sp. n. (artwork by Márton Zsoldos)	Fig. 3. Artistic reconstruction of Ferussina petofiana Páll-Gergely, sp. n. (artwork by Márton Zsoldos)	2023-10-06	Tang, Jin;Zhang, Gongaote;Guo, Junqi;Luo, Lingxuan;Jiang, Jiamei;Pan, Hongbo		Zenodo	biologists	Tang, Jin;Zhang, Gongaote;Guo, Junqi;Luo, Lingxuan;Jiang, Jiamei;Pan, Hongbo			
15297C4EFFFE387F6BC6C86BFD14C68D.taxon	http://purl.org/dc/dcmitype/StillImage	image/png	https://zenodo.org/record/10272170/files/figure.png	https://doi.org/10.5281/zenodo.10272170	Fig. 1. Geological setting of the type locality of Ferussina petofiana. A = Position of the Hațeg Basin (rectangle; HB) within Romania.B = Simplified geological map of the Hațeg Basin, highlighting the distribution of the uppermost Cretaceous continental deposits (shades of green). Legend: 1 – surrounding metamorphic basement, 2 – units of the sedimentary basin infill (mostly marine), 3-5 – fossiliferous Maastrichtian continental deposits, with 3 – Sînpetru Formation, 4 – Densuș-Ciula Formation (v – volcaniclastic beds), and 5 – Sînpetru Formation-correlative units (see CSIKI-SAVA et al. 2016), 6 – Quaternary cover, 7 – sites with gastropod assemblages (a –SCHAFARZIK 1909,b –RĂDULESCU et al. 1976, c –ANTONESCU et al. 1983, d –GRIGORESCU et al. 1985, e – PANĂ et al. 2002, f – CSIKI et al. 2008, g – VASILE et al. 2011; see text for details), 8 – site K3 of Vălioara, the type locality of Ferussina petofiana (from BOTFALVAI et al. 2021). C = Synthetic lithological column near site K3 (marked by red arrow), modified from BOTFALVAI et al. (2021). Lithofacies abbreviations: BChD – braided channel deposits, mainly conglomerates, ChL – sandstone channel lag, SSp – sandstone sheet-splay, PdFP – poorly drained floodplain deposits, mainly grey-greenish silts and muds, WdFP – well-drained floodplain deposits, mainly red silts and muds. For more details, see BOTFALVAI et al. (2021). D. View of site K3 in the Pârâul Neagului ravine, located in grey-greenish fine-grained floodplain deposits (near handle of hammer). E. The Retezat Mountains overlooking the Hațeg Basin from the south (photo by Gergő Konecsni), mentioned by the Petőfi poem written during his 1849 visit in the	Fig. 1. Geological setting of the type locality of Ferussina petofiana. A = Position of the Hațeg Basin (rectangle; HB) within Romania.B = Simplified geological map of the Hațeg Basin, highlighting the distribution of the uppermost Cretaceous continental deposits (shades of green). Legend: 1 – surrounding metamorphic basement, 2 – units of the sedimentary basin infill (mostly marine), 3-5 – fossiliferous Maastrichtian continental deposits, with 3 – Sînpetru Formation, 4 – Densuș-Ciula Formation (v – volcaniclastic beds), and 5 – Sînpetru Formation-correlative units (see CSIKI-SAVA et al. 2016), 6 – Quaternary cover, 7 – sites with gastropod assemblages (a –SCHAFARZIK 1909,b –RĂDULESCU et al. 1976, c –ANTONESCU et al. 1983, d –GRIGORESCU et al. 1985, e – PANĂ et al. 2002, f – CSIKI et al. 2008, g – VASILE et al. 2011; see text for details), 8 – site K3 of Vălioara, the type locality of Ferussina petofiana (from BOTFALVAI et al. 2021). C = Synthetic lithological column near site K3 (marked by red arrow), modified from BOTFALVAI et al. (2021). Lithofacies abbreviations: BChD – braided channel deposits, mainly conglomerates, ChL – sandstone channel lag, SSp – sandstone sheet-splay, PdFP – poorly drained floodplain deposits, mainly grey-greenish silts and muds, WdFP – well-drained floodplain deposits, mainly red silts and muds. For more details, see BOTFALVAI et al. (2021). D. View of site K3 in the Pârâul Neagului ravine, located in grey-greenish fine-grained floodplain deposits (near handle of hammer). E. The Retezat Mountains overlooking the Hațeg Basin from the south (photo by Gergő Konecsni), mentioned by the Petőfi poem written during his 1849 visit in the	2023-10-06	Tang, Jin;Zhang, Gongaote;Guo, Junqi;Luo, Lingxuan;Jiang, Jiamei;Pan, Hongbo		Zenodo	biologists	Tang, Jin;Zhang, Gongaote;Guo, Junqi;Luo, Lingxuan;Jiang, Jiamei;Pan, Hongbo			
