• 责任者：Li Jun (Laboratory of Earth Surface Processes ; MOE ; College of Urban and Environmental Sciences ; Peking University ; Beijing 100871 ; China) ; Wang Shuyun
• 刊名：Acta Scientiarum Naturalium Universitatis Pekinensis
• 出版年：2011
• 卷期：47(6)
• 关键词：晚更新世 ; Upper Pleistocene ; 全新世 ; Holocene ; 湖泊环境 ; lacustrine environment ; 洞庭湖 ; Dongting Lake
• 页码：p.1041-1048
• 图表：6 illus., 1 table, 30 refs.
• 分类号：1400
• issnNo：ISSN0479-8023
• isbnNo：CN11-2442/N

 A continuous record from the Dongtinghu Lake is presented in this work. The authors provide detailed evidence of particle size, magnetic capacity and pollen analysis of ZK01 core that reveals the changes of lake’s environment and climate since 6 000 a B.P.. The results reveal that hydrological environment and climate change evidently affected the process of regional ancient culture and history. Particularly, the changes of hydrological environment and climate maybe were the main fading reason of prehistoric civilization in Dongtinghu area. Since 1 000 a B.P., human activities such as embankment and reclamation in the banks of Yangtze River affected obviously the evolution history of flow and sediment process and river-lake environment in Dongtinghu region.