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PALEOCLIMATIC CHANGES IN DABUSU LAKE
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作者 沈吉 曹建廷 +2 位作者 吴艳宏 ryomatsumoto 孙庆义 《Chinese Journal of Oceanology and Limnology》 SCIE CAS CSCD 2001年第1期91-96,共6页
Study on the carbonate content and oxygen isotope of a sediment section in Dabusu Lake revealed that this region has experienced several cold wet and warm dry climatic cycles since 15400 a BP. It was about 6740 a BP w... Study on the carbonate content and oxygen isotope of a sediment section in Dabusu Lake revealed that this region has experienced several cold wet and warm dry climatic cycles since 15400 a BP. It was about 6740 a BP when the climate in the region reached a relatively stable warm stage, so that the lake water was gradually condensed and finally a saline lake was formed. 展开更多
关键词 carbonate content oxygen isotope PALEOCLIMATE Dabusu Lake
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