Sedimentary record of a late Holocene storm event in Laizhou Bay, Bohai Sea, China

Zhenqiao LIU; Liang ZHOU; Shu GAO; Longjiang MAO; Peng LU

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Sedimentary record of a late Holocene storm event in Laizhou Bay, Bohai Sea, China

Geology | Updated：2024-10-12

- Sedimentary record of a late Holocene storm event in Laizhou Bay, Bohai Sea, China
- Sedimentary record of a late Holocene storm event in Laizhou Bay, Bohai Sea, China
- 海洋湖沼学报(英文) 2023年41卷第3期页码：909-920
- Affiliations：
  
  1.State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200046, China
  2.Marine Geological Institute of Hainan Province, Haikou 570100, China
  3.School of Geography, Geomatics, and Planning, Jiangsu Normal University, Xuzhou 221116, China
  4.School of Marine Sciences, Nanjing University of Information Sciences & Technology, Nanjing 210044, China
  5.Institute of Geography, Henan Academy of Sciences, Zhengzhou 450052, China
- Author bio：
  
  sgao@sklec.ecnu.edu.cn
- Funds：
  
  the National Natural Science Foundation of China(41706096;41530962;41771218);the Research Start-up Project of Jiangsu Normal University (No.‍ 19XSRX006), and the Opening Foundation of Hainan Key Laboratory of Marine Geological Resources and Environment(HNHYDZZYHJKF005)
- DOI：
  中图分类号：
- 收稿：2021-07-13，
  
  纸质出版：2023-05-01
- Accepted：
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Sedimentary record of a late Holocene storm event in Laizhou Bay, Bohai Sea, China[J]. 海洋湖沼学报(英文), 2023,41(3):909-920.

LIU Zhenqiao,ZHOU Liang,GAO Shu,et al.Sedimentary record of a late Holocene storm event in Laizhou Bay, Bohai Sea, China[J].Journal of Oceanology and Limnology,2023,41(03):909-920.
Sedimentary record of a late Holocene storm event in Laizhou Bay, Bohai Sea, China[J]. 海洋湖沼学报(英文), 2023,41(3):909-920. DOI：

LIU Zhenqiao,ZHOU Liang,GAO Shu,et al.Sedimentary record of a late Holocene storm event in Laizhou Bay, Bohai Sea, China[J].Journal of Oceanology and Limnology,2023,41(03):909-920. DOI：

摘要

Abstract

The Bohai Sea is influenced by numerous extreme oceanic wave events in history. However

it is often difficult to determine the types of these events due to the lack of detailed historical records

causing uncertainty in the reconstruction of historical coastal disasters. We investigated an anomalous sand layer in the Xiliyu Village by the coast of Laizhou Bay

Shandong

from which an extreme event deposit was identified using a multi-proxy approach including grain size distribution

geochemistry

and magnetic susceptibility. This event was dated 2 700‍‍–‍3 100 a bp

and caused inundation of a large coastal area of Laizhou Bay. By comparing historical records with instrumental data

we believe that the event deposit was generated by a severe storm surge with wind speed of >34.9 m/s.

关键词

Keywords

references

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