The first Asian skeleton of Diaceratherium from the early Miocene Shanwang Basin (Shandong, China), and implications for its migration route

• Published in: Journal of Asian Earth Sciences: X Vol. 6; p. 100074
• Main Authors: Lu, Xiaokang, Cerdeño, Esperanza, Zheng, Xiaoting, Wang, Shiqi, Deng, Tao
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.12.2021; Elsevier
• Subjects: Diaceratherium; Eastern Asia; Migration route; Oligocene–Miocene transition; Shanwang Basin; Shanwang Basin; Eastern Asia; Migration route; Diaceratherium; Oligocene–Miocene transition
• ISSN: 2590-0560; 2590-0560
• DOI: 10.1016/j.jaesx.2021.100074

[Display omitted] •To report first Asian skeleton of Diaceratherium from early Miocene Shanwang Basin in China.•To revalidate “Plesiaceratherium” shanwangensis and revise it to Diaceratherium as D. shanwangense.•To suggest alternative route from Europe to East Asia via northern margin of Tibetan Plateau. Owing to the scarcity of records, the Asian evolution and migration of Diaceratherium, a large extinct genus of rhinoceros of the Teleoceratini, remain unclear. The skeleton described herein, from the early Miocene Shanwang Basin in China, is identified as Diaceratherium shanwangense, a species originally defined based on upper cheek teeth. This skeleton features a large body, short horn-bearing nasal bones, moderately retracted nasal notch at the P3 level, and the metapodials that are less massive than those in other previously identified species of Diaceratherium. Mammalian fossils reported from the Oligocene–Miocene transition of the Old World, such as Dorcatherium and Amphicyon, have indicated a migration route between Europe and Eastern Asia via Southern and South-eastern Asia, namely along the southern margins of the Tibetan Plateau. However, the fossil remains of Diaceratherium reported in this study were discovered in eastern China, which represents the second accurate record of the genus in Asia (together with its presence in Kazakhstan). Consequently, given the temporal range and geological distribution of Diaceratherium, we propose that the expansion of this genus to the eastern part of the continent occurred via a route following the northern margins of the Tibetan Plateau, which if verified, represents an alternative expansion route differing from the established routes of other mammals.