The Middle and Late Holocene climate change in Bohai Bay revealed by diatom proxy

Zhiwen SHANG; Jianfen LI; Fu WANG; Hong WANG

doi:10.1007/s00343-024-3187-9

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The Middle and Late Holocene climate change in Bohai Bay revealed by diatom proxy

Geology | Updated：2024-11-19

- The Middle and Late Holocene climate change in Bohai Bay revealed by diatom proxy
- Journal of Oceanology and Limnology Vol. 42, Issue 5, Pages: 1493-1506(2024)
- Affiliations：
  
  1.TianjinCentre, China Geological Survey, Tianjin300170, China
  2.Key Laboratory of Coastal Geo-environment, China Geological Survey, Tianjin300170, China
  3.Tianjin Key Laboratory of Coast Geological Processes and Environmental Safety, Tianjin300170, China
- Author bio：
  
  shangzhiwen1007@126.com
- Funds：
- DOI：10.1007/s00343-024-3187-9
  CLC：
- Received：14 September 2023，
  
  Online First：03 February 2024，
  
  Published：01 September 2024
- Accepted：
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SHANG Zhiwen,LI Jianfen,WANG Fu,et al.The Middle and Late Holocene climate change in Bohai Bay revealed by diatom proxy[J].Journal of Oceanology and Limnology,2024,42(05):1493-1506.
DOI：

SHANG Zhiwen,LI Jianfen,WANG Fu,et al.The Middle and Late Holocene climate change in Bohai Bay revealed by diatom proxy[J].Journal of Oceanology and Limnology,2024,42(05):1493-1506. DOI： 10.1007/s00343-024-3187-9.

摘要

Abstract

A total of 98 samples from two boreholes in shallow sea area and two oyster reefs in adjacent coastal plain in the northwestern coast of Bohai Bay were collected for diatom analyses and species identification. The ratio of the marine species

Thalassionema

nitzschioides

to the intertidal-coastal species complex

Cyclotella

striata

stylorum

serves as a novel proxy for assessing the strength of marine influence. Chronological data

corrected for the local residence time effect

facilitated the construction of a diatom proxy-based marine influence curve for the study area. This curve delineates the dynamics of marine influence and their correlations with paleo-climate fluctuations and the East Asian monsoon variability

as well as their role in chenier formation. Results include: (1) eight periods of intensified marine influence have been documented since 7 000 a BP in the study area. The peak of each period

as determined by the diatom proxy

corresponds closely to the warm climatic phases and stronger East Asian summer monsoons

suggesting that the peaks marine influence indicate typically the periods of climatic warmth and monsoon activity intensification in the region; (2) a strong correlation exists between the development of cheniers and marine influence

and chenier formation began with the increasing marine influence and terminated at the end of warm periods as marine influence weakens. The climatic changes in the coastal area

as indicated by the diatom proxy

hold significant potential for future related research endeavors.

关键词

Keywords

references

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