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

Shen Ji; Zhang Enlou; Yang Xiangdong; Ryo Matsumoto

doi:10.1007/BF02842582

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

Updated：2023-05-16

- Paleoclimatic change inferred from carbon isotope composition of organic matter in sediments of Dabusu Lake, Jilin Province, China
- Journal of Oceanology and Limnology Vol. 22, Issue 2, Pages: 124-129(2004)
- Affiliations：
  
  1. Nanjing Institute of Geography & Limnology Chinese Academy of Sciences
  2. Geological Institute University of Tokyo
- Author bio：
- Funds：
- DOI：10.1007/BF02842582
  CLC：
- Published：2004
- Accepted：
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Ji, S., Enlou, Z., Xiangdong, Y. et al. Paleoclimatic change inferred from carbon isotope composition of organic matter in sediments of Dabusu Lake, Jilin Province, China., Chin. J. Ocean. Limnol. 22, 124–129 (2004). https://doi.org/10.1007/BF02842582
DOI：

Ji, S., Enlou, Z., Xiangdong, Y. et al. Paleoclimatic change inferred from carbon isotope composition of organic matter in sediments of Dabusu Lake, Jilin Province, China., Chin. J. Ocean. Limnol. 22, 124–129 (2004). https://doi.org/10.1007/BF02842582 DOI：

摘要

Abstract

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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references

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