Volume 4 Issue 4
Dec.  1998
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FAN Shuxian, TONG Guobang, ZHENG Hongrui, 1998. EVOLUTION OF PALEOCLIMATE AND PLANT COMMUNITY IN THE LAST 800 ka B P IN DATONG AREA. Journal of Geomechanics, 4 (4): 64-68.
Citation: FAN Shuxian, TONG Guobang, ZHENG Hongrui, 1998. EVOLUTION OF PALEOCLIMATE AND PLANT COMMUNITY IN THE LAST 800 ka B P IN DATONG AREA. Journal of Geomechanics, 4 (4): 64-68.

EVOLUTION OF PALEOCLIMATE AND PLANT COMMUNITY IN THE LAST 800 ka B P IN DATONG AREA

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  • Received: 1998-03-29
  • Published: 1998-12-28
  • A sporopollen analysis of the Dongshuitou section, Xiaobeizhuang section and Nansigou section of the Heishan hill, Datong, Shanxi, shows that the vegetation since 800 ka B P has gone through four stages developing from forest through sylvosteppe and steppe to desertsteppe, Corresponding to the changes of paleoclimate, i.e. three climatic cycles, including nine subcycles, each beginning with a cold and dry climate, and ending in a warm and humid one.

     

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