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《Earth Science-Journal of China University of Geosciences》 2003-06
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Climate Variance Record of Aeolian Sand in Recent 2 ka, Alakehu Area, Eastern Kunlun Mountains

XIANG Shu-yuan, YU Jian-xin, WANG Guo-can, SHUANG Yan, WU Yan-ling(Faculty of Earth Sciences, China University of Geosciences, Wuhan430074, China)  
Sporopollen analysis to aeolian sand section at the east bank of the Alakehu, eastern Kunlun, shows a climate variance process in recent 2 000 a which happened 4 periods of warm and cold alternation. The warm periods occurred during 20-180, 330-410, 700-920 and 1 140-1 380 a respectively, and the cold periods during 180-330, 410-700, 920-1 140 and 1 380-1 920 a. The climates were warm-dry-slightly damp during warm periods and warm-slightly cold and dry during cold period. 700-920 a is the warmest and dampest period in recent 2 000 a, which is implied by the rich of rhus, that mainly distribute in semitropical zone and temperate zone and also rich of arbor sporopollen, and is accorded to the warm period of eastern China in Tang Dynasty which is recorded by the history documents. After 1 500 a, lacking of sporopollen shows that either arbor or herbage decreased sharply when the Little Ice Age came and became almost extinct nowadays. The authors suggest that cooling and drying in (about) 300 a the Little Ice Age is the main reason to the extinction of the arbor, not the people activity.
【Fund】: 中国地调局1∶25万阿拉克湖幅区域地质调查项目(No.19991300004021);; 国家自然科学基金项目(No.40072062);; 国土资源部科技司青藏高原新生代填图方法集成研究项目(No.2000201-2-2).
【CateGory Index】: P532
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