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Miocene mammalian faunas from Wushan,China and their evolutionary,biochronological, and biogeographic significances
Authors:Bo-Yang Sun  Xiu-Xi Wang  Min-Xiao Ji  Li-Bo Pang  Qin-Qin Shi  Su-Kuan Hou  Dan-Hui Sun  Shi-Qi Wang
Institution:1. Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China;2. University of Chinese Academy of Sciences, Beijing 100039, China;3. Laboratory of Evolutionary Biology, Department of Anatomy, College of Medicine, Howard University, Washington D.C. 20059, USA;4. Key Laboratory of Western China’s Environmental Systems (Ministry of Education), College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000, China;5. China Three Gorges Museum, Chongqing 400013, China;6. CAS Center for Excellence in Tibetan Plateau Earth Sciences, Beijing 100101, China
Abstract:We report Miocene mammalian faunas from three nearby localities: Kangping, Nanyu, and Yangping, in the Wushan Subbasin, Gansu Province, China. From the Kangping locality, we identified four species, Platybelodon grangeri, Hispanotherium wushanense n. sp., Kubanochoerus sp., and Turcocerus cf. kekemaidengensis, which indicate that this fauna can be correlated with MN7/8. From the Nanyu locality, we identified Platybelodon aff. tongxinensis, which, together with the previously reported specimens of Gomphotherium wimani and Micromeryx cf. flourensianus, enables us to correlate this fauna with MN6. The Yangping locality is found to be early Miocene in age based on the presence of cf. Gomphotherium sp. This occurrence is the earliest record of proboscideans in China, and thus represents the “Proboscidean Datum Event”. Evolutionary trends of Platybelodon and Hispanotherium are figured and discussed. The possibility of a geographic boundary associated with the eastern and western differentiation of species of Turcocerus and bunodont listriodonts in China is also evaluated. This boundary was consistent with the major division of the eastern and western mammalian faunas of the middle Miocene in China. The localities in Inner Mongolia suggest a large area with transitional habitats.
Keywords:Wushan Subbasin  Miocene  Fauna  Age  Evolution  Paleozoogeography
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