| Homo erectus pekinensis's age and environment——with discussion on the relationship among Homo erectus from Beijing,Nanjing and Chenjiawo |
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| 作者姓名： | LIU Jinling & WANG Weiming
Nanjing Institute of Geology and Palaeontology Chinese Academy of Sciences Nanjing China Correspondence should be addressed to Liu Jinling and Wang Weiming |
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| 作者单位： | LIU Jinling & WANG Weiming
Nanjing Institute of Geology and Palaeontology，Chinese Academy of Sciences，Nanjing 210008，China Correspondence should be addressed to Liu Jinling and Wang Weiming |
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| 基金项目： | 国家自然科学基金，国家重点基础研究发展计划(973计划) |
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| 摘 要： | This paper inspects the relationship between Homo erectus from Beijing, Nanjing and Chenjiawo on the viewpoint of environmental variations. Pieces of evidence show that Nanjing and Chenjiawo Homo erectus lived in glacial age at the Marine Oxygen Isotope Stage (MIS) 16, while Homo erectus pekinensis in major interglacial age at MISs 15-13. It is also recovered that the cave deposits in Tangshan, Nanjing, and Zhoukoudian, Beijing, as well as the deposits at the Homo erectus site in Chenjiawo, have undergone some similar development process. All of them originated from early-middle Middle Pleistocene, and have gone through the test of the major glacial age at MIS 16 and the major interglacial period at the paleosol stage S5. At the same time, they were also closely connected with some environment events, such as the uplift of the Qinghai-Xizang Plateau, the formation of glaciations and the loess accumulations.
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Homo erectus pekinensis's age and environment--with discussion on the relationship among Homo erectus from Beijing, Nanjing and Chenjiawo |
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| LIU Jinling & WANG Weiming
Nanjing Institute of Geology and Palaeontology,Chinese Academy of Sciences,Nanjing ,China Correspondence should be addressed to Liu Jinling and Wang Weiming.Homo erectus pekinensis''''s age and environment--with discussion on the relationship among Homo erectus from Beijing, Nanjing and Chenjiawo[J].Science in China(Earth Sciences),2004,47(1). |
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| Authors: | Liu Jinling WANG Weiming |
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| Institution: | Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China |
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| Abstract: | This paper inspects the relationship between Homo erectus from Beijing, Nanjing and Chenjiawo on the viewpoint of environmental variations. Pieces of evidence show that Nanjing and Chenjiawo Homo erectus lived in glacial age at the Marine Oxygen Isotope Stage (MIS) 16, while Homo erectus pekinensis in major interglacial age at MlSs 15-13. It is also recovered that the cave deposits in Tangshan, Nanjing, and Zhoukoudian, Beijing, as well as the deposits at the Homo erectus site in Chenjiawo, have undergone some similar development process. All of them originated from early-middle Middle Pleistocene, and have gone through the test of the major glacial age at MIS 16 and the major interglacial period at the paleosol stage S5. At the same time, they were also closely connected with some environment events, such as the uplift of the Qinghai-Xizang Plateau, the formation of glaciations and the loess accumulations. |
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| Keywords: | Homo erectus from Beijing Nanjing and Chenjiawo climate and environment comprehensive comparisons |
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