Environmental magnetic characteristics and provenance significance of sediments in NW South China Sea since the past 16 ka

XIAO Chunfeng; SUN Qishun; CHEN Liang; YIN Zhengxin; CHEN Long; GUAN Yulong; ZHANG Yuzhen; JIANG Zhaoxia

doi:10.16562/j.cnki.0256-1492.2022091301

2023 Vol. 43, No. 1

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Article navigation > Marine Geology & Quaternary Geology > 2023 > 43(1): 13-26

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XIAO Chunfeng, SUN Qishun, CHEN Liang, YIN Zhengxin, CHEN Long, GUAN Yulong, ZHANG Yuzhen, JIANG Zhaoxia. Environmental magnetic characteristics and provenance significance of sediments in NW South China Sea since the past 16 ka[J]. Marine Geology & Quaternary Geology, 2023, 43(1): 13-26. doi: 10.16562/j.cnki.0256-1492.2022091301

Citation:

XIAO Chunfeng, SUN Qishun, CHEN Liang, YIN Zhengxin, CHEN Long, GUAN Yulong, ZHANG Yuzhen, JIANG Zhaoxia. Environmental magnetic characteristics and provenance significance of sediments in NW South China Sea since the past 16 ka[J]. Marine Geology & Quaternary Geology, 2023, 43(1): 13-26. doi: 10.16562/j.cnki.0256-1492.2022091301

Environmental magnetic characteristics and provenance significance of sediments in NW South China Sea since the past 16 ka

1.
Frontiers Science Center for Deep Ocean Multispheres and Earth System, Key Lab of Submarine Geosciences and Prospecting Techniques, MOE, College of Marine Geosciences, Ocean University of China, Qingdao 266100, China
2.
Laboratory for Marine Geology, Laoshan Laboratory, Qingdao 266237, China
3.
Chongben Honors College, Ocean University of China, Qingdao 266100, China
4.
South China Sea Marine Survey and Technology Center, State Oceanic Administration,Guangzhou 510300, China
5.
Key Laboratory of Marine Environmental Survey Technology and Application, Ministry of Natural Resources, Guangzhou 510300, China

More Information

Corresponding author: JIANG Zhaoxia, jiangzhaoxia@ouc.edu.cn

Received Date: 13 September 2022

Revised Date: 28 November 2022

Accepted Date: 28 November 2022

Publish Date: 28 February 2023

Abstract

Abstract

As the largest marginal sea in the western Pacific Ocean, South China Sea (SCS) is sensitive to the East Asian monsoon and global climate change. The provenance of SCS sediments remains controversial. We carried out a systematic magnetic analysis on Core SCS-02 from the Qiongdongnan Basin, to trace the origin of sediments. Results show that the magnetic carriers of Core SCS-02 sediment are mainly magnetite and hematite. Since 16 kaBP, the particle size and magnetic mineralogy have shown systematic changes, indicating the change of the sedimentary source-sink process. During 15.5～16 kaBP, the sediments were with higher magnetic susceptibility, coarser grain size, and higher coercivity. The sea level was 100 m below the modern one, and the Yingge Sea was above the ancient sea level. The ancient Red River estuary was closer to the study area, leading to more material transported from the old Red River to the depositional area. During 7.5～15.5 kaBP, sea level rose rapidly, the total content of magnetic minerals decreased, but the relative content of magnetite gradually increased, and the magnetic particles became finer, indicating that the contribution of ancient Pearl River and Taiwan increased with the rise of sea level. Since 7.5 kaBP, the modern land and sea pattern had been formed fundamentally, changes in magnetic mineral composition and particle size stabilized relatively, and the sediments were mainly from the modern Red River and the Pearl River. Therefore, the environmental magnetic parameters are good proxies for the source-sink changes of sediments in the South China Sea, and provide an effective reference for the studies of sea level change and climate evolution.
- environmental magnetism /
- magnetic minerals /
- source-sink information /
- South China Sea

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References

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