The first finding of Asian black bear (Carnivora, Ursidae, Ursus (Euarctos) thibetanus G. Cuvier, 1823) in the Late Pleistocene of northern Eurasia

An M1 tooth of Asian black bear ( Ursus ( Euarctos ) thibetanus G. Cuvier, 1823) was found in deposits of the Tetyukhinskaya cave (Middle Sikhote-Alin, 44°35′N, 135°36′E). This finding is the first reliable evidence of Asian black bear’s presence in Pleistocene of Primorye. Its morphological and mor...

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Published inDoklady. Biological sciences Vol. 471; no. 1; pp. 266 - 268
Main Authors Kosintsev, P. A., Tiunov, M. P., Gimranov, D. O., Panov, V. S.
Format Journal Article
LanguageEnglish
Published Moscow Pleiades Publishing 01.11.2016
Springer Nature B.V
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Summary:An M1 tooth of Asian black bear ( Ursus ( Euarctos ) thibetanus G. Cuvier, 1823) was found in deposits of the Tetyukhinskaya cave (Middle Sikhote-Alin, 44°35′N, 135°36′E). This finding is the first reliable evidence of Asian black bear’s presence in Pleistocene of Primorye. Its morphological and morphometric descriptions are given. The period of inhabitation of U. (E.) thibetanus determined based on the radiocarbon date obtained during the study of the tooth, is 39 874 ± 133 BP (NSK-850, UGAMS-21786), which corresponds to the middle of Marine Isotope Stage 3 (MIS 3) of Late Pleistocene. The composition of ancient theriofauna indicates the existence of wide variety of landscapes in Primorye in the middle of Late Pleistocene. A refugium of forest fauna, in which species of taiga, nemoral, and Central Asian mountain–forest theriocomplexes were present, was located in southern Primorye in Late Pleistocene.
Bibliography:ObjectType-Article-1
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ISSN:0012-4966
1608-3105
DOI:10.1134/S0012496616060041