Sharamurunian
The Sharamurunian age is an Asian Land Mammal Age (~42.7[1]–39.9[2] Ma) within the Middle to Late Eocene epoch of the Paleogene. It follows the Irdinmanhan age and precedes the Ulangochuian age.[1] The Sharamurunian is named after the Shara Murun Formation.[3]
References
[edit]- 1 2 Bai, Bin; Wang, Yuan-Qing; Li, Qian; Wang, Hai-Bing; Mao, Fang-Yuan; Gong, Yan-Xin; Meng, Jin (2018). "Biostratigraphy and Diversity of Paleogene Perissodactyls from the Erlian Basin of Inner Mongolia, China". American Museum Novitates. 3914 (3914): 1–60. doi:10.1206/3914.1. ISSN 0003-0082.
- ↑ Bai, Bin; Meng, Jin; Janis, Christine M.; Zhang, Zhao-Qun; Wang, Yuan-Qing (2020). "Perissodactyl diversities and responses to climate changes as reflected by dental homogeneity during the Cenozoic in Asia". Ecology and Evolution. 10 (13): 6333–6355. doi:10.1002/ece3.6363. ISSN 2045-7758. PMC 7381588. PMID 32724516.
- ↑ Lucas, Spencer G. (2002). Chinese Fossil Vertebrates. Columbia University Press. pp. 213–220. ISBN 978-0-231-50461-4.
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