LONG Hao, MA Hai-zhou, WANG Nai-ang, LI Yu, WANG Chen-hua. MID-HOLOCENE CLIMATE VARIATIONS FROM LAKE RECORDS OF NW TENGGER DESERT[J]. Marine Geology & Quaternary Geology, 2007, 27(3): 105-111.
Citation: LONG Hao, MA Hai-zhou, WANG Nai-ang, LI Yu, WANG Chen-hua. MID-HOLOCENE CLIMATE VARIATIONS FROM LAKE RECORDS OF NW TENGGER DESERT[J]. Marine Geology & Quaternary Geology, 2007, 27(3): 105-111.
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MID-HOLOCENE CLIMATE VARIATIONS FROM LAKE RECORDS OF NW TENGGER DESERT

  • 1 Qinghai Institute of Salt Lakes, Chinese Academy of Sciences, Xining 810008, China;

  • 2 School of Resources and Environment, Lanzhou University, Lanzhou 730000, China

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  • Received Date: November 19, 2006
  • Revised Date: January 21, 2007
    Graphical Abstract
    • Abstract
  • QTL section of 6.92 m depth is taken from Qingtu palaeolake, the terminal lake of Shiyang drainage located in NW Tengger Desert. Based on the detailed dating results, multi-proxy analysis of QTL section, including grain size, carbonate, TOC, C/N and δ13C of organic matter, was used to document regional climatic changes during 9~3 cal.kaBP. The climate evolution in the study area during 9~3 cal.kaBP is divided into four stages:①from cold and dry to warm and humid during the period of 9~7.8 cal.kaBP, ②a significant drought interval of multicentennial scale between 7.8~7.5 cal.kaBP, ③Holocene optimum characterized by a warm and moist climate during the period of 7.5~5 cal.kaBP, ④from humid to dry during 5~3 cal.kaBP.
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    • References (31)
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