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A raised OIS 3 sea level recorded in coastal sediments, southern Changjiang delta plain, China

Published online by Cambridge University Press:  20 January 2017

Zhanghua Wang ,
Brian G. Jones ,
Ting Chen ,
Baocheng Zhao  and
Qing Zhan
Zhanghua Wang*
Affiliation:
State Key Laboratory for Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China
Brian G. Jones
Affiliation:
School of Earth and Environmental Sciences, University of Wollongong, NSW 2522, Australia
Ting Chen
Affiliation:
State Key Laboratory for Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China
Baocheng Zhao
Affiliation:
Shanghai Geological Survey, Shanghai 200072, China
Qing Zhan
Affiliation:
Shanghai Geological Survey, Shanghai 200072, China
*
*Corresponding author. Fax: + 86 21 62546441. E-mail address:[email protected] (Z. Wang).
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Abstract

The distribution of marine-influenced oxygen isotope stage (OIS) 5 to OIS 1 sediments was examined in several late Quaternary boreholes from the southern Changjiang (Yangtze) delta plain, China, using different dating methods including OSL, U-series, AMS 14C and paleomagnetism. Results demonstrate that coastal and estuarine deposition during OIS 5 and OIS 3 occurred throughout the study area. However, Holocene transgressive sediments were absent on the Taihu block. The burial depth of intertidal to subtidal sediment deposited during OIS 5e records 30–80 m subsidence caused by sediment compaction and tectonic movement since that time. However, coastal sediments formed during the late phase of OIS 3 were buried to a depth of ca. 6–15 m in the Taihu Lake area, while the burial depth increased eastward to ca. 45–60 m on the coastal plain. This phenomenon, combined with the distribution of Holocene marine strata, indicates at least 25–30 m uplift of the Taihu block since the end of OIS 3. We suggest that this uplift was mainly caused by the differential subsidence due to substantial amount of post-glacial deposition by the Changjiang and Huanghe Rivers on the continental shelf of east China marginal sea.

Keywords

OIS 3 sea levelDifferential subsidenceUplift of Taihu blockChangjiang coast
Type
Research Article
Information
Quaternary Research , Volume 79 , Issue 3 , May 2013 , pp. 424 - 438
Copyright
University of Washington

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