Fossil Equidae in the Linxia Basin with Biostratigraphic and Paleozoogeographic SignificanceOACSTPCD
Fossil Equidae in the Linxia Basin with Biostratigraphic and Paleozoogeographic Significance
The Linxia Basin is characterized by an abundance of Cenozoic sediments,that contain exceptionally rich fossil resources.Equids are abundant in the Linxia Basin,the fossil record of equids in this region including 16 species that represent 10 genera.In comparison to other classic late Cenozoic areas in China,the Linxia Basin stands out,because the fauna and chronological data accompanying Linxia equids render them remarkably useful for biostratigraphy.The anchitheriines in the region,such as Anchitherium and Sinohippus,represent early equids that appeared in the late stages of the middle and late Miocene,respectively.Among the equines,most species of Chinese hipparions have been identified in the Linxia Basin and some species of the genera Hipparion and Hippotherium have FAD records for China.Furthermore,Equus eisenmannae is one of the earliest known species of Equus in the Old World and is well-represented at the Longdan locality.Some species with precise geohistorical distributions can serve as standards for high-resolution chronological units within this framework.Located at the eastern margin of the Tibetan Plateau and subject to considerable uplift,the Linxia Basin has served as a biogeographic transition area for equids throughout the late Cenozoic.
SUN Boyang
Key Laboratory of Vertebrate Evolution and Human Origins of the Chinese Academy of Sciences,Institute of Vertebrate Paleontology and Paleoanthropology,Chinese Academy of Sciences,Beijing 100044,China
EquidaeCenozoicbiostratigraphypaleozoogeographyLinxia Basin
《地质学报(英文版)》 2024 (001)
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The Editor-in-Chief Dr.Hou Zengqian,as well as two reviewers who greatly improved the manuscript,are thanked for promoting its publication.All members of the Linxia Basin project leaded by Prof.Qiu Zhanxiang contributed greatly in field work and discussion.Prof.Deng Tao and Dr.Liu Wenhui provided important data and files for research.Dr.Lawrence Flynn,Dr.Wang Xiaoming and Dr.Deng Chenglong are kindly acknowledged for their comments on the manuscript.We appreciate all of their efforts.This research was supported by National Key Research and Development Program of China(Grant No.2023YFF0804501),the Youth Innovation Promotion Association,Chinese Academy of Sciences(Grant No.2021069),the Strategic Priority Research Program of the Chinese Academy of Sciences(Grant Nos.XDB31000000),the Second Comprehensive Scientific Expedition on the Tibetan Plateau(Grant No.2019QZKK0705)and the All China Commission of Stratigraphy(Grant No.DD20221829).
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