YANG Sheng-li, FANG Xiao-min, SHI Zheng-tao, SONG Chun-hui. DRYING EVENT AT 500 kaBP RECORDED BY THE CHENGDU CLAY GRAIN SIZE AT THE EASTERN MARGIN OF THE TIBETAN PLATEAU[J]. Marine Geology & Quaternary Geology, 2008, 28(2): 105-114.
Citation: YANG Sheng-li, FANG Xiao-min, SHI Zheng-tao, SONG Chun-hui. DRYING EVENT AT 500 kaBP RECORDED BY THE CHENGDU CLAY GRAIN SIZE AT THE EASTERN MARGIN OF THE TIBETAN PLATEAU[J]. Marine Geology & Quaternary Geology, 2008, 28(2): 105-114.
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DRYING EVENT AT 500 kaBP RECORDED BY THE CHENGDU CLAY GRAIN SIZE AT THE EASTERN MARGIN OF THE TIBETAN PLATEAU

  • 1 Institute of Tibetan Plateau Research, CAS, Beijing 100085, China;

  • 2 Key Laboratory of Western China's Environmental Systems MOE and College of Resources and Environment, Lanzhou University, Lanzhou 730000, China;

  • 3 School of Tourism and Geography, Yunnan Normal University, Kunming 648092, China

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  • Received Date: November 26, 2007
  • Revised Date: March 11, 2008
    Graphical Abstract
    • Abstract
  • Asian aridification is a reflection of the combination of the uplift of the Tibetan Plateau and global cooling. Comparison of the grain size of the Chengdu Clay from the eastern edge of the Tibetan Plateau and that of the Chinese Loess Plateau reveals a significant arid intensification event at about 500 ka. We estimate that the rapid uplift of the Tibetan Plateau during the middle Pleistocene and its entering cryosphere have caused this event.
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