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《Acta Palaeontologica Sinica》 2006-03
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LIU Jin-Ling and WANG Wei-Ming(Nanjing Institute of Geology and Palaeontology, the Chinese Academy of Sciences, Nanjing 210008, )  
Taking the regulation of the Pleistocene global climate change as the basis, combined with progress on the demarcation of the marine oxygen isotope stage (MIS), and the comparison between the glacier epoch in China and MIS, etc., this paper carries on an examination to the correlation between some Pleistocene events in China and MIS put forward by some scholars. The result demonstrates that Homo erectus in Nanjing most probably lived in the main glacier epoch of Kunlun, about 642ka—620ka before present, most comparable with MIS16. It is also evident that Homo erectus pekinensis was living in the initial stage of the great interglacial epoch (MIS15—13), and the earliest Homo erectus pekinensis might occur about 620 ka ago.
【Fund】: 国家自然科学基金(No.49971076)资助课题。
【CateGory Index】: Q981
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