Multi‐disciplinary study of a late Pleistocene woolly rhinoceros found in the Pannonian Basin and implications for the contemporaneous palaeoenvironment

Author:

Gasparik Mihály1,Major István2ORCID,Lisztes‐Szabó Zsuzsa2ORCID,Magyari Enikő3,Szabó Bence34,Pandolfi Luca5,Borel Antony67ORCID,Futó István2,Horváth Anikó2,Kiss Gabriella Ilona2ORCID,Molnár Mihály2,Csík Attila8ORCID,Markó András9

Affiliation:

1. Hungarian Natural History Museum Department of Palaeontology and Geology Budapest Hungary

2. International Radiocarbon AMS Competence and Training Center (INTERACT), Institute for Nuclear Research Debrecen Hungary

3. MTA‐MTM‐ELTE Research Group for Palaeontology, Department of Environmental and Landscape Geography Eötvös Loránd University Budapest Hungary

4. Eötvös Loránd University, Department of Palaeontology Budapest Hungary

5. Dipartimento di Scienze, Università degli Studi della Basilicata, Campus di Macchia Romana Potenza Italy

6. Histoire Naturelle de l'Homme Préhistorique (HNHP UMR‐7194, MNHN, CNRS, UPVD), Alliance Sorbonne Université, Département Homme et Environnement, Muséum national d'histoire naturelle Paris France

7. Institute of Archeological Sciences, Eötvös Loránd University Budapest Hungary

8. Laboratory of Material Science, Institute for Nuclear Research Debrecen Hungary

9. Hungarian National Museum Budapest Hungary

Abstract

ABSTRACTExcavation campaigns conducted at the Pécel‐Kis hársas site (Hungary) between 2014 and 2017 yielded the remains of a mature female woolly rhinoceros (Coelodonta antiquitatis) and six lithic artefacts. Radiocarbon dating confirmed that the rhinoceros died ca. 20.4k cal a bp, at the very end of the Last Glacial Maximum and, considering the position of the artefacts when found, it was probably killed by Epigravettian hunters. Based on dental analyses of the specimen, a vigorous lichen‐ (and possibly moss‐)consuming diet could be inferred for the end of the animal's lifetime. Based on Sr results, we can exclude the possibility of long‐range migration. In accordance with the optimum environmental demands of the foraging lichen, the low δ18O value of osseous material implies a relatively cold contemporaneous climate with a calculated mean annual air temperature of around 0.7 °C. Meanwhile, the extremely low δ15N value may have resulted from the proximity of the discontinuous permafrost zone and some intensive soil dislocation. Consequently, poor vegetation and an open, tundra‐like habitat can be assumed to have been dominant at the site at that time, which is also supported by palaeoenvironmental modeling experiments.

Funder

European Regional Development Fund

Publisher

Wiley

Subject

Paleontology,Earth and Planetary Sciences (miscellaneous),Arts and Humanities (miscellaneous)

Cited by 1 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献

1. Mammalian palaeodiet;Reference Module in Earth Systems and Environmental Sciences;2024

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