Cold event at 5 500 a BP recorded in mud sediments on the inner shelf of the East China Sea

Fangjian Xu; Anchun Li; Kehui Xu; Tiegang Li; Shiyue Chen; Shiming Wan; Jianguo Liu

doi:10.1007/s00343-009-9273-1

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Cold event at 5 500 a BP recorded in mud sediments on the inner shelf of the East China Sea

OriginalPaper | Updated：2023-05-16

- Cold event at 5 500 a BP recorded in mud sediments on the inner shelf of the East China Sea
- Cold event at 5 500 a BP recorded in mud sediments on the inner shelf of the East China Sea
- 海洋湖沼学报（英文） 2009年27卷第4期页码：975-984
- Affiliations：
  
  1. Key Laboratory of Marine Geology and Environment Institute of Oceanology Chinese Academy of Sciences
  2. Faculty of Geo-Resources and Information China University of Petroleum
  3. Graduate University of Chinese Academy of Sciences
  4. Department of Marine Science Coastal Carolina University
- Author bio：
- Funds：
  
  Supported by the National Natural Science Foundation of China (Nos. 40576032 and 40776030), and Doctor Foundation of China University of Petroleum.
- DOI：10.1007/s00343-009-9273-1
  中图分类号：
- 网络首发：2009-12-04，
  
  纸质出版：2009
- Accepted：
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Cold event at 5 500 a BP recorded in mud sediments on the inner shelf of the East China Sea[J]. 海洋湖沼学报（英文）, 2009,27(4):975-984.

Xu, F., Li, A., Xu, K. et al. Cold event at 5 500 a BP recorded in mud sediments on the inner shelf of the East China Sea., Chin. J. Ocean. Limnol. 27, 975–984 (2009). https://doi.org/10.1007/s00343-009-9273-1
Cold event at 5 500 a BP recorded in mud sediments on the inner shelf of the East China Sea[J]. 海洋湖沼学报（英文）, 2009,27(4):975-984. DOI： 10.1007/s00343-009-9273-1.

Xu, F., Li, A., Xu, K. et al. Cold event at 5 500 a BP recorded in mud sediments on the inner shelf of the East China Sea., Chin. J. Ocean. Limnol. 27, 975–984 (2009). https://doi.org/10.1007/s00343-009-9273-1 DOI：

摘要

Abstract

A 700-year record (1.0–1.5 a resolution) of the East Asian winter monsoon (EAWM)

based on grain-size analysis and AMS14C dating of Core EC2005 from the inner-shelf mud wedge of the East China Sea (ECS)

was compared with the Dongge stalagmite δ18O record during the mid-Holocene. The upper muddy section of Core EC2005 has been formed mainly by suspended sediments derived from the Changjiang (Yangtze) River mouth since 7.3 ka BP. High precipitation and a strengthened EAWM might have played key roles in the high sedimentation rate (1 324–1 986 cm/ka) between 5.9–5.2 ka BP. The EAWM strengthened when the Asian summer monsoon weakened

especially around 5 500 a BP

which corresponded to a worldwide cold event. The EAWM during the mid-Holocene shows statistically significant solar periodicities at 62 and 11 a. The 5 500 a BP cold event might be resulted from orbital forcing and changes in solar activity.

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references

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