• 责任者：Wang Suming (State Key Laboratory of Lake Science and Environment ; Nanjing Institute of Geography and Limnology ; Nanjing 210008 ; China) ; Xue Bi
• 刊名：Geological Journal of China Universities
• 出版年：2009
• 卷期：15(2)
• 关键词：湖泊环境 ; lacustrine environment ; 中国 ; China
• 页码：p.141-148
• 图表：2 illus., 40 refs.
• 分类号：1400
• issnNo：ISSN1006-7493
• isbnNo：CN32-1440/P

All the information from the lake environment changes could be well archived in the lacustrine sediments. The changes in lake environment on the different time-scale are resulted from the tectonic movement, climatic change and human impact respectively. The major tectonic movement in China is the uplifting of Tibetan Plateau, and the climate system is the east Asian monsoon, however, the human impact seems to be more implicated, e.g.: the indirect impact such as the vegetation and land use changes in the catchment, or the direct impact such as the lake reclamation and the lake enclosure from large river system. Delineating the mechanism of the lake environment changes and distinguishing the human impact from the natural influence are presently highlighted by the paleolimnologists.