Paleoclimatic change inferred from carbon isotope composition of organic matter in sediments of Dabusu Lake, Jilin Province, China

被引:0
|
作者
Shen Ji
Zhang Enlou
Yang Xiangdong
Ryo Matsumoto
机构
[1] Chinese Academy of Sciences,Nanjing Institute of Geography & Limnology
[2] University of Tokyo,Geological Institute
来源
关键词
organic carbon isotope; paleoclimate; Dabusu Lake;
D O I
10.1007/BF02842582
中图分类号
学科分类号
摘要
Study on the organic compounds and stable isotope composition of a sediment section in Dabusu Lake revealed that the organic materials in the sediments came mainly from terrestrial plants brought into the lake by runoff. The δ13 C of the organic materials had high values during warm-dry climatic stages and decreased in cold-wet stages. Analysis of data on carbonate content and14C age showed that the lake basin had experienced several wet-cold and warm-dry climatic cycles since 15000 a BP. Since 6700 a BP, the climate reached a relatively stable warm-dry stage, so that the lake water was gradually condensed and finally a saline lake was formed.
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页码:124 / 129
页数:5
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