SUN Chengcheng, ZHOU Limin, ZHENG Xiangmin, NIU Rui, MENG Qinghao, WANG Lin, DU Dandan, XU Hongyang, WANG Zhen, CHU Huimin. PEAT RECORD OF HOLOCENE CLIMATE CHANGE IN THE YANGBAJING BASIN, TIBET PLATEAU[J]. Marine Geology & Quaternary Geology, 2016, 36(5): 149-155. DOI: 10.16562/j.cnki.0256-1492.2016.05.015
Citation: SUN Chengcheng, ZHOU Limin, ZHENG Xiangmin, NIU Rui, MENG Qinghao, WANG Lin, DU Dandan, XU Hongyang, WANG Zhen, CHU Huimin. PEAT RECORD OF HOLOCENE CLIMATE CHANGE IN THE YANGBAJING BASIN, TIBET PLATEAU[J]. Marine Geology & Quaternary Geology, 2016, 36(5): 149-155. DOI: 10.16562/j.cnki.0256-1492.2016.05.015
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PEAT RECORD OF HOLOCENE CLIMATE CHANGE IN THE YANGBAJING BASIN, TIBET PLATEAU

  • Faculty of Earth Sciences, East China Normal University, Shanghai 201100, China

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  • Received Date: March 04, 2016
  • Revised Date: June 20, 2016
    Graphical Abstract
    • Abstract
  • There is a vast peat land in the Qinonggou(QNG) of the Yangbajing Basin next to the southern margin of the Nianqing Tanggula Mountain, Tibet Plateau. By extracting the humification and total organic carbon(TOC)data from the peat in QNG, combined with the 14C dating control, we have reconstructed the Holocene palaeoclimatic variation from 9.1 to 3.5 cal.kaBP at the Yangbajing Basin. On stage I, during 9.1~7.4 cal.kaBP,the temperature showed a fluctuating upward trend. Two obvious cold events occurred in 9.1 cal.kaBP and 8.0 cal.kaBP. On stage Ⅱ, of 7.4~4.7 cal.kaBP, the temperature fluctuation was frequent and intense. Two obvious cold events occurred in 6.0 cal.kaBP and 5.8 cal.kaBP respectively. On stage Ⅲ, during 4.7~3.5 cal.kaBP, the temperature showed a fluctuating downward trend. But the frequency and amplitude of the changes were much tender than those of the second stage. There only occurred a relative significant cold event at 4.0 cal.kaBP.
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