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The Late Neogene mammal biochronology in the Loess Plateau,China
Institution:1. State Key Laboratory of Mineral Deposit Research, School of Earth Sciences and Engineering, Nanjing University, Nanjing 210023, China;2. Department of Earth and Environmental Sciences, Università di Milano-Bicocca, 20126 Milano, Italy;1. Institut de Paléoprimatologie, Paléontologie Humaine: Evolution et Paléoenvironnements, UMR 7262 CNRS, Université de Poitiers, 86000 France;2. Centre de Recherches Pétrologiques et Géochimiques, UMR CNRS 7358, Vandoeuvre-lès-Nancy 54500 France;3. Université Pierre et Marie Curie—UPMC, CR2P—UMR 7207 CNRS, MNHN, UPMC—57 rue Cuvier, CP 48, F-75005 Paris, France;4. Muséum national d''Histoire naturelle, CR2P—UMR 7207 CNRS, MNHN, UPMC, 57 rue Cuvier, CP 38, F-75005, Paris, France;5. Department of Geology, Defence Services Academy, Pyin Oo Lwin, Myanmar
Abstract:For lacking of absolute dating, and because of the strong mammalian faunal endemism, the Chinese late Neogene has long been subdivided into mammalian ages mostly based on isolated local faunas by evolutionary stages of fossil taxa. The correlation with European stages and or mammalian units remains unsatisfied. We report the recent advances of the land mammal biochronology of late Neogene based on fossils found from continuous sections located at Lantian, Shaanxi Province and Lingtai, Gansu Province. There recognized three biozones for the late Miocene by fossils from the Bahe and Lantian formations, and three biozones for Pliocene on the data from Lingtai. The detailed biochronology work in combination with paleomagnetic data may improve the precision of correlation in the continental scale.
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