渤海湾西岸CZ01钻孔沉积物粒度端元分析及其气候—海平面变化响应<sup>*</sup>

doi:10.7605/gdlxb.2022.06.083

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Abstract

Located on the west coast of the Bohai Bay where land and sea interact,the Cangzhou region is vulnerable to sea level changes and extreme weather events and is very sensitive to the response to global climate change. A non-parametric end-member analysis model was applied to classify the sediment grain size of CZ01 borehole in Cangzhou region into six end-members since the late Mid-Pleistocene and analyze their sources,and to reveal the response of each end-members to climate and sea-level changes at different time scales in conjunction with the existing geological record. The results show that: (1)EM1(5.01 μm)is mainly a remote wind-dust input,EM2(13.18 μm)and EM3(39.81 μm)are sediments carried by the ancient Yellow River,EM4(69.18 μm)and EM5(138.04 μm)are marine sediments,EM6(275.42 μm)may indicate extreme climate events such as paleofloods. (2)During the Marine Oxygen Isotope Stages(MIS)Ⅰ,the climate is warm and humid,and the EM4+5 indicates that the sea-level of the Bohai Sea is wavelike rising and gradually reaches the modern sea level. During this period,the Bohai Sea level stagnates or decreases slightly after a steady state of rise due to the Younger Dryas impact hypothesis around 11.5 ka BP and a dry-cold climate event around 5.1 ka BP,while around 9.5 ka BP,7.5 ka BP,5.8 ka BP and 1.7 ka BP,the Bohai Sea level rises due to increased precipitation caused by strengthening East Asian summer monsoon. (3)The cold and dry climate in the Northern Hemisphere in MIS Ⅵ stage,and the regional subsidence center transfer caused by the weakening of Himalayaorogeny around 150~132 ka BP resulted in the increase of Bohai Sea surface. In MIS Ⅴ stage,the climate fluctuated dramatically: during the warm period of interglacial period(5a,5c and 5e),the climate was warm and humid,and the sea-level of Bohai Sea rose, and the sea level height of the Bohai Sea during MIS5b and 5d is lower. Compared with the end of MIS5a,the sea-level in MIS Ⅳ decreased suddenly and then tended to be stable. Several small-scale transgression events occurred during the period,which may be related to the frequent changes of East Asian summer monsoon. From the MIS Ⅲ stage to the Last Glacial Maximum,the sea-level decreased significantly with periodic fluctuations,and a large-scale transgression occurred at about 46 ka BP. MIS Ⅱ stage showed a slight decreased sea-level compared with MIS Ⅲ stage,which was a low sea-level period. Due the termination of the glacier period around 15 ka BP,and the strengthened East Asian summer monsoon, sea-level began to rise again. The sedimentary records of the Bohai Sea since 180 ka BP are consistent with the geological records in the northern hemisphere and even worldwide,which are closely related to the glacier melts caused by solar radiation fluctuation and the change of East Asian summer monsoon.

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	WANG Ting
	ZOU Chunhui
	MAO Longjiang
	ZHOU Yulong
	MO Duowen

Key words： grain size end-member analysis provenance climate and sea-level west coast of Bohai Bay

Received: 23 May 2022

ZTFLH:	P532
	P563
	P941.78

Fund:

Co-funded by the National Natural Science Foundation of China(No.41771218),the National Key Research and Development Program of China(No.2020YFC1521605)and the National Social Science Major Foundation of China(No.19ZDA231)

Corresponding Authors: ZOU Chunhui,born in 1992,is a doctoral candidate. He majors in environmental archaeology. E-mail: 991899875@qq.com. MAO Longjiang,born in 1976,professor,is mainly engaged in environmental evolution and environmental archaeology,marine sedimentation process and environment. E-mail: mlj1214@163.com.

About author: WANG Ting,born in 1997,is a master degree candidate. She majors in marine science. E-mail: 17864261091@163.com.

Cite this article:

WANG Ting,ZOU Chunhui,MAO Longjiang et al. Sediment grain size end-member analysis and its response to climate and sea-level changes in CZ01 borehole on west coast of Bohai Bay[J]. JOPC, 2022, 24(6): 1224-1237.

URL:

http://journal09.magtechjournal.com/gdlxb/EN/10.7605/gdlxb.2022.06.083 OR http://journal09.magtechjournal.com/gdlxb/EN/Y2022/V24/I6/1224

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