Paleotempestology evidence recorded by eolian deposition in the Bohai Sea coastal zone during the last interglacial period

• Published in: Marine geology Vol. 379; pp. 78 - 83
• Main Authors: Du, Shuhuan, Li, Baosheng, Chen, Muhong, Xiang, Rong, Niu, Donefeng, Si, Yuejun
• Format: Journal Article
• Language: English
• Published: Elsevier B.V 01.09.2016
• Subjects: Bohai Sea coastal zone; Brackish; Deposition; Eolian sediments; Evolution; Fossils; Grain size; Last interglacial period; Latitude; Marine; Marine geology; Marine micropaleontology; Paleotempestology record; Sediments; Storms; INW, Huanghai Sea; China, People's Rep; INW, Bohai Sea; Marine micropaleontology; Last interglacial period; Paleotempestology record; Bohai Sea coastal zone; Eolian sediments
• ISSN: 0025-3227; 1872-6151
• DOI: 10.1016/j.margeo.2016.05.013

Reconstruction of the generation, development, and evolution of modern storms through paleotempestology is used to understand the regularity of storm activity and the relationship between storm activity and global climate change. Existing paleotempestology research in China is concentrated mainly on the low latitude sediments deposited since the Holocene (about 7000a). In this study, we examine the storm deposits in the eolian sediments of the Bohai Sea coastal zone at middle latitudes, choosing the Miaodao stratigraphic section (MDS) as the target area. This area is located in the Bohai Sea strait and shows evidence of storms since the last interglacial period using an analysis of the grain size parameter, element ratios, and marine micropaleontology foraminifera fossils in the sediment during the last 130ka that can be used in our paleotempestology research. The results include three main findings: (1) the marine micropaleontology foraminifer fossils appear in the eolian sediment of the MDS and, in combination with grain size parameter and element ratios of the sediments, serve as evidence of the paleotempestology record on the Bohai Sea coastal zone; (2) planktonic foraminifera fossils appear in the MDS, indicating that the Yellow Sea warm current affected the Bohai Sea during the last interglacial period; and (3) storm activity in the marine isotope stage (MIS) 5a has been recorded in the MDS 15 times. The findings of this study expand the paleotempestology record from 7000a to 90ka and serve as a reference for research for middle latitude storm activity. •Foraminifer fossils as evidence of paleotempestology record on the eolian sediment•Yellow Sea warm current affected the Bohai Sea during the last interglacial period.•Storm activity frequency in the MIS5a representing millennial-scale periodicity