Kosintsev P.A., Tiunov M.P., Gimranov D.O., Panov V.S.
В журнале Doklady Biological Sciences
Год: 2016 Том: 471 Номер: 1 Страницы: 266-268
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.
