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Holocene coastal morphologies and shoreline reconstruction for the southwestern coast of the Bohai Sea, China

Published online by Cambridge University Press:  20 January 2017

Yanxia Liu ,
Haijun Huang ,
Yali Qi ,
Xiao Liu  and
Xiguang Yang
Yanxia Liu
Affiliation:
Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266061, China
Haijun Huang*
Affiliation:
Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
Yali Qi
Affiliation:
Guangdong Ocean University, Zhanjiang 52400, China
Xiao Liu
Affiliation:
Shandong University of Technology, Zibo 255049, China
Xiguang Yang
Affiliation:
Northeast Forestry University, Harbin 150040, China
*
*Corresponding author. E-mail address:[email protected](H. Huang)
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Abstract

Ground-penetrating radar (GPR) reflection profiles were interpreted and combined with sedimentological data to highlight the morpho-evolutionary history of the southwestern sector of the Bohai Sea. The internal structures in GPR images obtained near the Holocene maximum transgression boundary revealed concave-upward and onlap types of transgressive paleotopography. The relationship between historical courses of the Yellow River and the distribution of shell ridges at three periods (6 ka, 2 ka, and recent times) showed that the concave-upward types derived from the marine sediments overlap the fluvial sediments, and the onlap types from the marine sediments cover the coastal lagoon sediments. Based on the above paleogeographical setting, previous sea-level markers were corrected, taking into account uncertainties of their relationship to former water levels. The rates of vertical tectonic displacement, evaluated through comparison of the relative sea level (RSL) data from the GPR images and the Holocene predicted sea-level elevation, markedly affected RSL changes. The fitted RSL curves from the corrected sea-level indicators showed that the accuracy of former sea-level determinations can be improved by comparing with the maximum transgressive position of GPR detection. A topographic digital elevation model (DEM) for 6 ka is reconstructed based on the corrected data.

Keywords

GPRPaleogeographical evolutionPaleoshoreline reconstructionRelative sea levelBohai Sea
Type
Research Article
Information
Quaternary Research , Volume 86 , Issue 2 , September 2016 , pp. 144 - 161
Copyright
Copyright © American Quaternary Association 2016

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