Interactions Between Depositional Regime and Climate Proxies in the Northern South China Sea Since the Last Glacial Maximum

Wang, Xuesong1; Zhong, Yi2; Clift, Peter D.3; Feng, Yingci4; Wilson, David J.5; Kaboth-Bahr, Stefanie6; Bahr, Andre7; Gong, Xun1,8; Zhao, Debo9; Chen, Zhong4; Zhang, Yanan2; Tian, Yuhang4; Liu, Yuxing2; Liu, Xiaoyu2; Liu, Jiabo10; Xia, Wenyue2; Yang, Huihui2,11; Cao, Wei2; Liu, Qingsong2,12

2023-03-01

10.1029/2022PA004591

PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY   影响因子和分区

2572-4517

2572-4525

Sedimentary deposits from the northern South China Sea (SCS) can provide important constraints on past changes in ocean currents and the East Asian summer monsoon (EASM) in this region. However, the interpretation of such records spanning the last deglaciation is complicated because sea-level change may also have influenced the depositional processes and patterns. Here, we present new records of grain size, clay mineralogy, and magnetic mineralogy spanning the past 24 kyr from both shallow and deep-water sediment cores in the northern SCS. Our multi-proxy comparison among multiple cores helps constrain the influence of sea-level change, providing confidence in interpreting the regional climate-forced signals. After accounting for the influence of sea-level change, we find that these multi-proxy records reflect a combination of changes in (a) the strength of the North Pacific Intermediate Water inflow, (b) the EASM strength, and (c) the Kuroshio Current extent. Overall, this study provides new insights into the roles of varying terrestrial weathering and oceanographic processes in controlling the depositional record on the northern SCS margin in response to climate and sea-level fluctuations.

SCI

英语

通讯

National Natural Science Foundation of China["42274094","92158208","42261144739","41976065"] ; Natural Science Foundation of Guangdong Province[2021A1515011370] ; State Key Laboratory of Marine Geology, Tongji University[MGK202209] ; State Key Laboratory of Marine Geology, Shenzhen Science and Technology Program[2019YFE0125000] ; Ministry of Science and Technology of the People's Republic of China[GKZ22Y656] ; State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences[NE/T011440/1] ; NERC independent research fellowship[SSKP202101] ; null[KQTD20170810111725321]

Geology ; Oceanography ; Paleontology

Geosciences, Multidisciplinary ; Oceanography ; Paleontology

WOS:000948941900001

AMER GEOPHYSICAL UNION

Web of Science

1.China Univ Geosci, Inst Adv Marine Res, Guangzhou, Peoples R China
2.Southern Univ Sci & Technol, Dept Ocean Sci & Engn, Shenzhen, Peoples R China
3.Louisiana State Univ, Dept Geol & Geophys, Baton Rough, LA USA
4.South China Sea Inst Oceanol, Innovat Acad South China Sea Ecol & Environm Engn, Chinese Acad Sci, Key Lab Ocean, Guangzhou, Peoples R China
5.UCL, Dept Earth Sci, London, England
6.Univ Potsdam, Inst Geosci, Potsdam Golm, Germany
7.Heidelberg Univ, Inst Earth Sci, Heidelberg, Germany
8.China Univ Geosci, State Key Lab Biogeol & Environm Geol, Hubei Key Lab Marine Geol Resources, Wuhan, Peoples R China
9.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Peoples R China
10.China Univ Geosci, Sch Geophys & Geomat, Paleomagnetism & Planetary Magnetism Lab, Wuhan, Peoples R China
11.Harbin Inst Technol, Scholl Environm, Harbin, Peoples R China
12.Shanghai Sheshan Natl Geophys Observ, Shanghai, Peoples R China

Wang, Xuesong,Zhong, Yi,Clift, Peter D.,et al. Interactions Between Depositional Regime and Climate Proxies in the Northern South China Sea Since the Last Glacial Maximum[J]. PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY,2023,38(3).

Wang, Xuesong.,Zhong, Yi.,Clift, Peter D..,Feng, Yingci.,Wilson, David J..,...&Liu, Qingsong.(2023).Interactions Between Depositional Regime and Climate Proxies in the Northern South China Sea Since the Last Glacial Maximum.PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY,38(3).

Wang, Xuesong,et al."Interactions Between Depositional Regime and Climate Proxies in the Northern South China Sea Since the Last Glacial Maximum".PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY 38.3(2023).