YIN Qian, ZHU Cheng, MA Chun-mei, WANG Fu-bao, ZHAO Zhi-ping, ZHENG Chao-gui, HUANG Lin-yan, TIAN Xiao-si. HOLOCENE CLIMATE CHANGE RECORDED IN PEAT HUMIFICATION IN TIANMU MOUNTAIN REGION[J]. Marine Geology & Quaternary Geology, 2006, 26(6): 117-122.
Citation: YIN Qian, ZHU Cheng, MA Chun-mei, WANG Fu-bao, ZHAO Zhi-ping, ZHENG Chao-gui, HUANG Lin-yan, TIAN Xiao-si. HOLOCENE CLIMATE CHANGE RECORDED IN PEAT HUMIFICATION IN TIANMU MOUNTAIN REGION[J]. Marine Geology & Quaternary Geology, 2006, 26(6): 117-122.
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HOLOCENE CLIMATE CHANGE RECORDED IN PEAT HUMIFICATION IN TIANMU MOUNTAIN REGION

  • 1 Department of Urban and Resources Sciences, Nanjing University, Nanjing 210093, China;

  • 2 Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China

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  • Received Date: May 24, 2006
  • Revised Date: July 31, 2006
    Graphical Abstract
    • Abstract
  • Age-depth curves have been constructed using radiocarbon dates for the Qian Mutian peat profile of Tianmu Mountain area, Zhejiang Province. According to the analysis of the peat humification and LOI for this region, we can find that both the proxy indices show good correlation and identify climatic shifts since 4 200 aBP. Mainly there are three phases:early phase (4 135±40~3 200 aBP)of low humification,indicating warm and moist climate;mid phase (3 200~630 aBP) of high humification,showing dry and cool climate;and late phase (since 630 aBP) of low humification,suggesting a cool and moist climate.
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    • References (20)
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