Institute of Plant and Animal Ecology, Ural Branch, Russian Academy of Sciences, 620144, Yekaterinburg, Russia.
Federal Center of East Asian Terrestrial Biodiversity Research, Far East Branch, Russian Academy of Sciences, 620144, Vladivostok, Russia.
Dokl Biol Sci. 2020 Mar;491(1):47-49. doi: 10.1134/S0012496620010032. Epub 2020 Jun 1.
Enamel macro- and microstructure has been studied in the teeth of Merck's rhinoceros (Stephanorhinus kirchbergensis Jäger, 1839), woolly rhinoceros (Coelodonta antiquitatis Blumenbach, 1799), and rhinoceroses from the Tetyukhinskaya (44°35' N, 135°36' E) and Sukhaya (43°09' N, 131°28' E) caves in southern Primorye. The teeth from the caves were identified as the teeth of Merck's rhinoceros. Radiocarbon dating and accompanying animal species enabled the dating of Merck's rhinoceros remains to the Late Pleistocene (marine isotope stages 5-2). These finds mark the extreme eastern boundary of the Merck's rhinoceros species range in the Late Pleistocene. The living range reached the Pacific Ocean coast during a certain time interval within this epoch. This was due to the abundance of tree and shrub vegetation in the area during the Late Pleistocene.
对麦氏犀(Stephanorhinus kirchbergensis Jäger, 1839)、披毛犀(Coelodonta antiquitatis Blumenbach, 1799)以及来自外贝加尔边疆区捷丘欣斯基(北纬 44°35',东经 135°36')和苏哈亚(北纬 43°09',东经 131°28')洞穴的犀牛牙齿的宏观和微观结构进行了研究。洞穴中的牙齿被鉴定为麦氏犀的牙齿。放射性碳测年和伴随的动物物种使麦氏犀遗骸的年代确定为晚更新世(海洋同位素阶段 5-2)。这些发现标志着晚更新世麦氏犀物种范围的最东边界。在这个时期的某个时间间隔内,该物种的活动范围到达了太平洋海岸。这是由于晚更新世该地区树木和灌木植被丰富所致。