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The trace fossil Lepidenteron lewesiensis: a taphonomic window on diversity of Late Cretaceous fishes

dc.contributor.authorŚwierczewska-Gładysz, Ewa
dc.contributor.authorBieńkowska-Wasiluk, Małgorzata
dc.contributor.authorUchman, Alfred
dc.contributor.authorJurkowska, Agata
dc.date.accessioned2021-09-13T10:24:40Z
dc.date.available2021-09-13T10:24:40Z
dc.date.issued2015
dc.identifier.citationBieńkowska-Wasiluk, M., Uchman, A., Jurkowska, A. et al. The trace fossil Lepidenteron lewesiensis: a taphonomic window on diversity of Late Cretaceous fishes. Paläontol Z 89, 795–806 (2015). https://doi.org/10.1007/s12542-015-0260-xpl_PL
dc.identifier.issn0031-0220
dc.identifier.urihttp://hdl.handle.net/11089/39025
dc.description.abstractThe trace fossil Lepidenteron lewesiensis (Mantell 1822) provides an exceptional taphonomic window to diversity of fishes as shown for the Upper Cretaceous of Poland, in the Middle Turonian–Lower Maastrichtian deposits of the Opole Trough, Miechów Trough, Mazury-Podlasie Homocline, and SE part of the Border Synclinorium. Lepidenteron lewesiensis is an unbranched burrow lined with small fish scales and bones, without a constructed wall. It contains scales, vertebrae, and bones of the head belonging to ten taxa of teleostean fishes: two undetermined teleosteans, six undetermined Clupeocephala, one Dercetidae, and one undetermined euteleostean. The preservation of fish remains suggests that fishes were pulled down into the burrow by an animal, probably by eunicid polychaetes.pl_PL
dc.description.abstractDas Spurenfossil Lepidenteron lewesiensis (Mantell 1822) ermöglicht einen biostratinomischen Einblick in die Diversität von Fischen, wie Fossilmaterial aus der Oberkreide von Polen zeigt. Es stammt aus dem Mittelturonium bis Untermaastrichtium des südöstlichen Abschnittes der Grenz-Synklinale, dem Opolen-Trog, dem Miechów-Trog und der Masuren-Podlachien-Homoklinale. L. lewesiensis ist ein unverzweigter Grabgang ohne ausgekleidete Wände, dessen Ränder von kleinen Fischschuppen und—knochen gebildet werden. Diese setzen sich aus Schuppen, Wirbel und Schädelknochen von zehn Teleostei-Taxa zusammen und zwar aus zwei unbestimmte Teleosteer, sechs unbestimmten Clupeocephala, einem Dercetidae und einem unbestimmten Euteleostei. Die Erhaltung der Fischüberreste deutet darauf hin, dass die Fische von einem Tier, wahrscheinlich einem Polychaeten der Familie Eunicidae, in den Bau gezogen wurden.pl_PL
dc.description.sponsorshipWe are very grateful to Dr. Lionel Cavin (Geneva) and the anonymous reviewer for constructive comments on an earlier version of the manuscript. Additional support was provided by the Jagiellonian University (DS funds), National Science Center (Grant Number: PRO-2011/01/N/ST10/07717), and the Laboratory of Geology (University of Lodz) BSt Grant No. 560/844. We are grateful to Dr. Johann Egger (Wien) and Kilian Eichenseer M.Sc. (Erlangen) for help with translating the abstract into German. We are grateful to Dr. Ursula Göhlich (Wien) for access to the Dercetis specimen.pl_PL
dc.language.isoenpl_PL
dc.publisherSpringerpl_PL
dc.relation.ispartofseriesPaläontologische Zeitschrift;89
dc.rightsUznanie autorstwa 4.0 Międzynarodowe*
dc.rights.urihttp://creativecommons.org/licenses/by/4.0/*
dc.subjectIchnofossilpl_PL
dc.subjectLepidenteron lewesiensispl_PL
dc.subjectUpper Cretaceouspl_PL
dc.subjectFishespl_PL
dc.subjectTaphonomypl_PL
dc.subjectPolandpl_PL
dc.subjectSpurenfossilpl_PL
dc.subjectOberkreidepl_PL
dc.subjectTaphonomiepl_PL
dc.subjectFischenpl_PL
dc.subjectTaphonomie Polenpl_PL
dc.titleThe trace fossil Lepidenteron lewesiensis: a taphonomic window on diversity of Late Cretaceous fishespl_PL
dc.typeArticlepl_PL
dc.page.number795–806pl_PL
dc.contributor.authorAffiliationInstitute of Earth Science, University of Lodz, Narutowicza 88, 90-139 Łódź, Polandpl_PL
dc.contributor.authorAffiliationFaculty of Geology, University of Warsaw, Żwirki i Wigury 93, 02-089, Warszawa, Polandpl_PL
dc.contributor.authorAffiliationInstitute of Geological Sciences, Jagiellonian University, Oleandry 2a, 30-063, Kraków, Polandpl_PL
dc.contributor.authorAffiliationInstitute of Geological Sciences, Jagiellonian University, Oleandry 2a, 30-063, Kraków, Polandpl_PL
dc.contributor.authorAffiliationFaculty of Geology, Geophysics and Environmental Protection, AGH University of Science and Technology, Mickiewicza 30, 30-059, Kraków, Polandpl_PL
dc.identifier.eissn1867-6812
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dc.identifier.doi10.1007/s12542-015-0260-x
dc.disciplinearcheologiapl_PL
dc.disciplinenauki biologicznepl_PL


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