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PALEO-ENVIRONMENTAL RECONSTRUCTION DURING THE PERIOD OF NANJING HOMO ERECTUS

ZHU Cheng ZHANG Yun

ZHU Cheng, ZHANG Yun. PALEO-ENVIRONMENTAL RECONSTRUCTION DURING THE PERIOD OF NANJING HOMO ERECTUS[J]. 中国地理科学, 2000, 10(3): 209-217.
引用本文: ZHU Cheng, ZHANG Yun. PALEO-ENVIRONMENTAL RECONSTRUCTION DURING THE PERIOD OF NANJING HOMO ERECTUS[J]. 中国地理科学, 2000, 10(3): 209-217.
ZHU Cheng, ZHANG Yun. PALEO-ENVIRONMENTAL RECONSTRUCTION DURING THE PERIOD OF NANJING HOMO ERECTUS[J]. Chinese Geographical Science, 2000, 10(3): 209-217.
Citation: ZHU Cheng, ZHANG Yun. PALEO-ENVIRONMENTAL RECONSTRUCTION DURING THE PERIOD OF NANJING HOMO ERECTUS[J]. Chinese Geographical Science, 2000, 10(3): 209-217.

PALEO-ENVIRONMENTAL RECONSTRUCTION DURING THE PERIOD OF NANJING HOMO ERECTUS

基金项目: Under the auspices of the National Natural Science Foundation of China (49771075) and Testing Foundation by the Modern Analysis Center of Nanjing University.
详细信息
    作者简介:

    ZHU Cheng(1954- ),male,professor. His major research interests include environmental evolution and global changes.

  • 中图分类号: P534.63

PALEO-ENVIRONMENTAL RECONSTRUCTION DURING THE PERIOD OF NANJING HOMO ERECTUS

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出版历程
  • 收稿日期:  1999-05-26
  • 刊出日期:  2000-09-20

PALEO-ENVIRONMENTAL RECONSTRUCTION DURING THE PERIOD OF NANJING HOMO ERECTUS

    基金项目:  Under the auspices of the National Natural Science Foundation of China (49771075) and Testing Foundation by the Modern Analysis Center of Nanjing University.
    作者简介:

    ZHU Cheng(1954- ),male,professor. His major research interests include environmental evolution and global changes.

  • 中图分类号: P534.63

摘要: Using five group dating of the fossil by Uranium series age method shows that the age of Nanjing Homo Erectus is between 280-430 ka B. P. Combining with the analysis of fossil mammalian form Stegodon, Sus.Lydekkeri Zdansly, M.pachyosteus Young, P.grayi Zdansky and E.SanmeniensisTeilhard et Pive teau, which are located in the same stratum, the authors thinks that the Nanjing Homo Erectus may have lived in the late Mid Pleistocene (about 350 ka B.P.). Based upon the spores and pollen in the cave sediments of the area, we can find that most of spores and pollen are subtropical and warm temperature types. For instance, broad leaf trees which are fond of warm climate, including Cunning hamia, Jsuga and Pinus ,as well as Morus, Carpinus and Ptendium. Among the above spores and pollen, only Tsuga,Liquidambar, Betula,Ulmus and Salix are the remainders of Humid hot environment from the Tertiary period. Above evidences illustrate that the living environment of the Nanjing Homo Erectus not only was not cloder but also was not drier than the Peking Man's. It could be said that dry climate and the ice age of the Mid Pleistocene didn't undergo this area.As for the manner of the Homo Erectus's making stone artifact and using fire, because now we have not found the evidence of the stone artifact and the ash, the futher excavation to the talus of the Huludong cave should be needed.

English Abstract

ZHU Cheng, ZHANG Yun. PALEO-ENVIRONMENTAL RECONSTRUCTION DURING THE PERIOD OF NANJING HOMO ERECTUS[J]. 中国地理科学, 2000, 10(3): 209-217.
引用本文: ZHU Cheng, ZHANG Yun. PALEO-ENVIRONMENTAL RECONSTRUCTION DURING THE PERIOD OF NANJING HOMO ERECTUS[J]. 中国地理科学, 2000, 10(3): 209-217.
ZHU Cheng, ZHANG Yun. PALEO-ENVIRONMENTAL RECONSTRUCTION DURING THE PERIOD OF NANJING HOMO ERECTUS[J]. Chinese Geographical Science, 2000, 10(3): 209-217.
Citation: ZHU Cheng, ZHANG Yun. PALEO-ENVIRONMENTAL RECONSTRUCTION DURING THE PERIOD OF NANJING HOMO ERECTUS[J]. Chinese Geographical Science, 2000, 10(3): 209-217.

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