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《SCIENTIA GEOGRAPHICA SINICA》 1999-06
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Mid Holocene Climatic Transition and Rapid Interruption in Neolithic Cultures in the Eastern Plain of Taihu Lake

YU Shi yong 1 ZHU Cheng 1 QU Wei zheng (1.Department of Geo. & Ocean Sciences, Nanjing University, Nanjing Jiangsu 210093; 2.Department of Oceanography, Qingdao University of Oceanography, Qingdao Shandong 266003)  
The Eastern Plain of Taihu Lake, located at west part of the Changjiang River Delta, could cater us exceptional information both about Holocene climate changes and human activity. Most of the Neolithic culture sites in the area could be successful to serve as the proxy profiles that contain both evidence for Holocene climatic variation and vestige of human settlement. Among them, Caoxieshan cultural site, 120°45′E, 31°22′N, is most typical and could enact as a unique paradigm. High resolution and continual records of pollen, grain size and magnetic susceptibility that span 5620 years from Caoxieshan cultural site, Suzhou provide a climatic context for Neolithic culture history. The origin and flourishing of Songze cultures overlapped the Holocene Hypsithermal Interval. Prior to 5365 a B.P., the climates were sustainably humid and warm, nevertheless, at the end of Songze cultures, a serious arid event centered at about 5?365 a B.P. rendered the civilization degenerate. Ultimately, a harsh cold wet event during the transition from the warm humid Atlantic Phase to the warm dry Subboreal Phase uppered the lake level of Yangcheng lake group significantly, made the Songze cultures vanish and left a 200 year regional hiatus of human occupation. After 5?160 a B.P., climates conversed as dry and warm, the lake retreated, Liangzhu cultures, a relatively well developed civilization emerged.
【Fund】: 国家自然科学基金!“长江三角洲全新世初至商周时期灾变事件对人类生存的影响( 批准号:49771075)”;;南京大学海岸海岛开发实
【CateGory Index】: P532
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