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

OriginalPaper | Updated：2023-05-16

- Paleoclimatic change inferred from carbon isotope composition of organic matter in sediments of Dabusu Lake, Jilin Province, China
- Paleoclimatic change inferred from carbon isotope composition of organic matter in sediments of Dabusu Lake, Jilin Province, China
- 海洋湖沼学报（英文） 2004年22卷第2期页码：124-129
- Affiliations：
  
  1. Nanjing Institute of Geography & Limnology Chinese Academy of Sciences
  2. Geological Institute University of Tokyo
- Author bio：
- Funds：
  
  Project CXNIGLAS-A02-05 supported by Chinese Academy of Sciences, also supported by NSFC (40072056).
- DOI：10.1007/BF02842582
  中图分类号：
- 纸质出版：2004
- Accepted：
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Paleoclimatic change inferred from carbon isotope composition of organic matter in sediments of Dabusu Lake, Jilin Province, China[J]. 海洋湖沼学报（英文）, 2004,22(2):124-129.

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
Paleoclimatic change inferred from carbon isotope composition of organic matter in sediments of Dabusu Lake, Jilin Province, China[J]. 海洋湖沼学报（英文）, 2004,22(2):124-129. DOI： 10.1007/BF02842582.

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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