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Historical Biology
An International Journal of Paleobiology
Volume 30, 2018 - Issue 5
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Articles

Hipparion material from Gaojiashan locality in the Late Miocene of Linxia Basin, Gansu, China and associated mammalian fossil assemblage

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Pages 677-693 | Received 02 Jan 2017, Accepted 02 Apr 2017, Published online: 19 Apr 2017
 

Abstract

Two Hipparion species, H. forstenae and H. hippidiodus from Gaojiashan locality in the Linxia Basin, Gansu, China are described in this paper, with the first presence of the former in the Linxia Basin. The lower cheek teeth of Hipparion from Gaojiashan bear deep ectoflexids, and after comparisons to other Chinese Hipparion fossils with deep ectoflexids, the mandibles with deep ectoflexids on the lower premolars suggest their attributions to H. forstenae. The presence of a deep ectoflexid on p2 may be interpretable as an intraspecifically variable feature in H. forstenae, and can also be found in H. dermatorhinum. Besides the Hipparion material, at least 8 species of large mammals occur at the Gaojiashan locality, including Adcrocuta eximia, Chilotherium wimani, Shansirhinus ringstroemi, Eucladoceros cf. proboulei, Palaeotragus cf. coelophrys, Giraffidae gen. et sp. indet., and the previously studied Promephitis hootoni and Eostyloceros hezhengensis. Although the sample from Gaojiashan shares five species with the Yangjiashan fauna, the Gaojiashan fossil assemblage may date to the Baodean because of the presence of H. forstenae. The overall taxonomic composition of the Gaojiashan assemblage at least suggests an approximate Baodean age, which would imply survival of C. wimani into the Baodean of the Linxia Basin.

Acknowledgements

We thank Dr Deng Tao for providing the material and guiding the research. We thank Dr Corwin Sullivan for English improving and comments. We thank Dr Shi Qinqin for her assistance in the field. We thank Gao Wei for his photographs and Hou Yemao for his CT scans.

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