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《Geological Review》 2005-04
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Climatic and Environmental Change in North China Plain during the Last Glacial Maximum

GUO Shengqiao, WANG Sumin, YANG Lijuan Geological Survey of Jiangsu Province, Nanjing, 210018 Open Lab. of Lacustrine Sediment and Environment, Najing Institute of Geography and Lake, Chinese Academy, 210008  
Based on the carbon-14 and TL dating of the Longrao-Nanwang profile in the North China Plain, a continuous lake sediment is attributed to the Last Glacial Maximum (LGM) (20-16 ka BP) in Ningjin Lake. Our pollen and geochemical data indicate that the LGM was not a single cold and dry condition, but an oscillatory process from cool-humid through cold-humid to cold-dry climate. The Ningjin lacustrine record further shows a simultaneous global cold event. In combination with previous records we suggest that, under a global cold background during the LGM, winter monsoons became stronger while summer monsoons became weaker.
【Fund】: 本文为国家自然科学基金资助项目(编号49402033)的成果。
【CateGory Index】: P532
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