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Article Navigation >  Acta Sedimentologica Sinica  > 2002  >  20(2): 307-313

ZHANG Qiang, ZHU Cheng, FANG Ying san. Sedimentological Record of Environmental Evolution in the Mid-Pleistocene in Ningzheng Area[J]. Acta Sedimentologica Sinica, 2002, 20(2): 307-313.
Citation: ZHANG Qiang, ZHU Cheng, FANG Ying san. Sedimentological Record of Environmental Evolution in the Mid-Pleistocene in Ningzheng Area[J]. Acta Sedimentologica Sinica, 2002, 20(2): 307-313.
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Sedimentological Record of Environmental Evolution in the Mid-Pleistocene in Ningzheng Area

  • 1.

    Department of Urban & Resources Sciences,Nanjing 210093;

  • 2.

    Nanjing Museum,Nanjing 210000

  • Received Date: 2001-05-18
  • Rev Recd Date: 2001-08-29
  • Publish Date: 2002-04-10
  • ESR dating, grain size and magnetic susceptibility measurements indicated that there exists a great difference in properties between the Xiashu loess, a kind of aeolian sediments, and the loess in the north China.The evidence showed that there are more clay particles in the Xiashu loess. Kd, frequency-dependent susceptibility and other environmental indicators suggested 5 relatively warm and humid climatic periods in the mid-Pleistocene: 159～163ka,192ka,195～198ka,203～230ka and 311～350ka. The first warmer climatic period was corresponding to the slightly relative warmer climatic period shawed in the deep-sea oxygen isotope (V21-146 hole) stages 6 and the 2~ nd , 3~ rd and 4~ th warmer climatic periods were corresponding to the warmer climatic event reflected by S2 and to the marine oxygen isotope stage 7. There existed a good relation between the four buried palaeosol layers of Laohushan Xiashu loess section and the four warm, humid climatic periods of the Jurong section. Paleolithic excavation shows a certain amount of stone implements in the 6 and 7 layer, indicating human activities at that time. Magnetic susceptibility and grain-size records suggested a warm and humid environment at that time, which was suitable for the human activity. And, this was in good agreement with the research result from pithecanthrope cave of Tangshan in Nanjing. The stone implements of the Miaohoushan culture in North east China were similar in features to those from North China and Jurong Paleolithic site, probably suggesting that the channel of the Yangtze River used to lie in the south of Jurong, Ningzheng Region.
  • [1] 1. Steven A,Hovan,David K Rea,Nicklas G Pisias,et al.A direct link between the China loess and marine δ18O records: Aeolian flux to the north Pacific[J].Nature,1989,340: 296～300

    2. 杨达源。中国东部的第四纪风尘堆积与季风变迁[J].第四纪研究，1991,4: 354～358 [Yang D Y.Monsoon evolution and Quaternary aeolian sediment in the eastern part of China [J].Quaternary Science,1991,4: 354～358 ]

    3. 刘东生等。黄土与环境[M].北京:科学出版社，1985.191～208 [Liu T S.et al.Loess and Environment[M].Beijing: Science Press,1985.191～208 （in Chinese）]

    4. 安芷生，Porter S,Chappell J等。最近130ka洛川黄土堆积序列与格棱兰冰心记录[J].科学通报，1994,39: 2 254～2 256 [An Z S,Porter S,Chappell J,et al.Ice core record in the Greenland and the sediment sequence of Luochuan loess during the recent 130 ka [J].Chinese Science Bulletin,1994,39: 2 254～2 256]

    5. 丁仲礼，刘东生，刘秀铭等。250万年以来的37个气候旋回[J].科学通报，1994,39:1 494～1 496 [Ding Z L,Liu T S,Liu X M,et al.37 climatic sequences since 2,500,000 yrs [J].Chinese Science Bulletin,1994,39: 1 494～1 496 ]

    6. 黄姜侬，方家骅，邵家骥等。南京下蜀黄土沉积时代的研究[J].地质论评，1988,34: 240～247 [Huang J N,Fang J H,Shao J J,et al.Study on the sediment age of the Xiashu Loess of the Nanjing [J].Geological Review,1988,34: 240～247 ]

    7. 徐馨。宁镇地区第四纪古环境[J].南京大学学报，1987,8: 21～31 [Xu X.Quaternary paleoenvironment in the Ningzhen region [J].Journal of Nanjing University,1987,8: 21～31]

    8. 张建军，杨达源，陈曰友等。长江中下游地区下蜀黄土磁化率曲线与环境变迁[J].沉积学报，2000,18: 18～21 [Zhang J J,Yang D Y,Chen Y Y,et al.Magnetic curves of the Xiashu loess and the environment evolution in the middle and the lower reaches of the Yangtse River [J].Acta Sedimentologica Sinica,2000,18: 18～21]

    9. 徐馨，何才华，沈志达等编著。第四纪环境研究方法[M].贵阳:贵州科技出版社，1992.89～104 [Xu X,He C H,Shen Z D.Method of Study on the Quaternary environment[M].Guiyang: Science and Technology Press of Guizhou,1992.89～104]

    10. 孙东怀，鹿化煜，David Rea 等。中国黄土粒度的双峰分布及其古气候意义[J].沉积学报，2000,18（2）: 327～335 [Sun D H,Lu H Y,David R,et al.Double-peak grain-size distribution of the loess in China and its paleoclimatic meaning [J].Acta Sedimentologica Sinica,2000,18（2）: 327～335]

    11. 鹿化煜，安芷生。黄土高原黄土粒度组成的古气候意义[J].中国科学（D辑），1998,3: 278～283 [Lu H Y,An Z S.Paleoenvironment meaning in the grain size component in the Loess Plateau [J].Science in China （Series D），1998,3: 278～283]

    12. Xiao J L,An Z S,Liu T S,et al.East Asian monsoon variation during the last 130ka: evidence from the loess plateau of Central China and Lake Biwa of Japan[J].Quaternary Science Reviews,1999,18: 147～157

    13. 辽宁省地质局水文地质大队。辽宁第四纪[M].北京:地质出版社，1983.46～85 [Geology Group of Hydrology Geology in Liaoning Province.Quaternary Geology in Liaoning[M].Beijing:Geology Publishing House,1983.46～85]

    14. 郑祥民，严钦尚，郭蓄民。长江三角洲南部晚更世晚期风成黄土与地层[A].长江三角洲现代沉积研究[C].上海:华东师范大学出版社，1987.76～91 [Zheng X M,Yan Q S,Guo X M.Aeolian loess and stratigraphy of mid-Pleistocene in the south of the Yangtse Delta,Study on the present sediment of the Yangtze Delta [M].Shanghai:East-China Normal University Press,1987.76～91]

    15. 李徐生，杨达源，鹿化煜等。皖南第四纪风尘堆积序列粒度特征及其意义[J].海洋地质与第四纪地质，1997,17: 73～81 [Li X S,Yang D Y,Lu H Y,et al.Grain-size characteristics of the Quaternary Aeolian sequence in south Anhui province and its climate meaning [J].Marine Geology and Quaternary Geology,1997,17: 73～81]

    16. Oldfield F.Evironmental magnetism-Personal perspective[J].Quaternary Science Reviews,1991,10: 73～83

    17. Thompson R,Oldfield F.Environmental magnetism[M].London: Goerge Allen & Uniwin,1986

    18. Maher B A,Thompson R.Mineral magnetic record of the Chinese loess and palaeosol[J].Geology,1991,19: 3～6

    19. Heller F,Liu T.Palaeoclimate and sedimentary history from magnetic susceptibility of loess in China[J].Geophysics Research Letters,1986,13: 1169～1172

    20. 李峰宇。下蜀黄土的岩石磁学特征[J].南京师范大学学报，1993,16: 44～50 [Li F Y.Magnetism of the Xiashu Loess [J].Journal of Nanjing Normal University,1993,16: 44～50]

    21. Derbyshire E,Keen D H,Kemp R A,et al.Loess-Palaeosol sequence as records of palaeoclimatic variations during the last glacial-interglacial cycle: someproblems of correlation in north-central China[A].In: Derbyshire E,ed.Wind blown sediments in the Quaternary record,Quaternary Proceedings[C].Chichester,UK: Wiley,1995a,4:7～18

    22. 刘秀铭，刘东生，F Heller.黄土频率磁化率与古气候冷暖变换[J].第四纪研究，1990,1: 42～49 [Liu X M,Liu T S.Heller F.Palaeoclimatic changes and the frequency-dependent magnetic susceptibility of loess [J].Quaternary Science,1990,1: 42～49]

    23. Huayu Lu,Xiaodong Liu,Fuqing Zhang,et al.Astronomical calibration of loess-paleosol deposits at luochuan central Chinese Loess Plateau[J].Palaeogeography,Palaeoclimatology,Palaeoecology,1999,154: 237～246

    24. 汪永进，Hai Cheng,陆从伦。南京汤山猿人洞穴碳酸盐沉积物的电离质谱铀系年代[J].科学通报，1999,44: 1 548～1 551 [Wang Y J,Hai C,Lu C L.TIMS dating of carbonate sediment from the Tangshan pithecanthrope cave,Nanjing,China [J].Chinese Science Bulletin,1999,44: 1 548～1 551]

    25. 尤玉柱，于汇历。东北地区史前人类的生存环境[J].第四纪研究，1989,8: 142～159 [You Y Z,Yu H L.Prehistoric human living condition in the north-east of China[J].China Quaternary Science,1989,8:142～159]

    26. 朱诚，张建新，俞锦标。南京汤山猿人生存环境重建探讨[J].地理科学，1998,18: 433～441 [Zhu C,Zhang J X,Yu J B.Palaeoenvironmental reconstruction during the period of Nanjing ape man[J].Scientia Geographia Sinica,1998,18: 433～441]
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  • Received:  2001-05-18
  • Revised:  2001-08-29
  • Published:  2002-04-10

Sedimentological Record of Environmental Evolution in the Mid-Pleistocene in Ningzheng Area

  • 1. Department of Urban & Resources Sciences,Nanjing 210093;
  • 2. Nanjing Museum,Nanjing 210000
  • Received Date: 2001-05-18
  • Rev Recd Date: 2001-08-29
  • Publish Date: 2002-04-10

Abstract: ESR dating, grain size and magnetic susceptibility measurements indicated that there exists a great difference in properties between the Xiashu loess, a kind of aeolian sediments, and the loess in the north China.The evidence showed that there are more clay particles in the Xiashu loess. Kd, frequency-dependent susceptibility and other environmental indicators suggested 5 relatively warm and humid climatic periods in the mid-Pleistocene: 159～163ka,192ka,195～198ka,203～230ka and 311～350ka. The first warmer climatic period was corresponding to the slightly relative warmer climatic period shawed in the deep-sea oxygen isotope (V21-146 hole) stages 6 and the 2~ nd , 3~ rd and 4~ th warmer climatic periods were corresponding to the warmer climatic event reflected by S2 and to the marine oxygen isotope stage 7. There existed a good relation between the four buried palaeosol layers of Laohushan Xiashu loess section and the four warm, humid climatic periods of the Jurong section. Paleolithic excavation shows a certain amount of stone implements in the 6 and 7 layer, indicating human activities at that time. Magnetic susceptibility and grain-size records suggested a warm and humid environment at that time, which was suitable for the human activity. And, this was in good agreement with the research result from pithecanthrope cave of Tangshan in Nanjing. The stone implements of the Miaohoushan culture in North east China were similar in features to those from North China and Jurong Paleolithic site, probably suggesting that the channel of the Yangtze River used to lie in the south of Jurong, Ningzheng Region.

ZHANG Qiang, ZHU Cheng, FANG Ying san. Sedimentological Record of Environmental Evolution in the Mid-Pleistocene in Ningzheng Area[J]. Acta Sedimentologica Sinica, 2002, 20(2): 307-313.
Citation: ZHANG Qiang, ZHU Cheng, FANG Ying san. Sedimentological Record of Environmental Evolution in the Mid-Pleistocene in Ningzheng Area[J]. Acta Sedimentologica Sinica, 2002, 20(2): 307-313.
shu

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