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Dryad

Late Pleistocene cave bear from Niedźwiedzia Cave (Poland): its fate and preservation inferred from taphonomy, pathology, and geochemistry

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Aug 01, 2024 version files 31.50 KB

Abstract

This comprehensive study examines bone remains from Niedźwiedzia Cave in the Eastern Sudetes, offering detailed insights into the palaeobiology and adversities encountered by the Pleistocene cave bear Ursus spelaeus ingressus in the Śnieżnik Massif. Emphasising habitual cave use for hibernation and a primarily herbivorous diet, the findings attribute mortality to resource scarcity during hibernation and habitat fragmentation amid climate shifts. Taphonomic analysis identifies prolonged cave use by successive generations without predation impact yet underscores alkaline cave conditions influencing post-depositional processes. Mortality patterns, notably among juveniles, imply dwindling resources, indicative of environmental instability. Skeletal examination reveals a high incidence of forelimb fractures, indicating risks during activities like digging or confrontations. Palaeopathological evidence unveils vulnerabilities to tuberculosis, abscesses, rickets, and injuries, elucidating mobility challenges. The cave’s silts exhibit an unusual zinc concentration, potentially derived from successive bear generations consuming zinc-rich plants. This study illuminates the lives of late cave bears, elucidating unique environmental hurdles faced near their species’ end.