南海西北部过去~55 ka以来元素地球化学记录的古气候环境演变

田成静; 蔡观强; 李明坤; 李波; 赵利

doi:10.3799/dqkx.2020.276

Volume 46 Issue 3

Mar. 2021

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Tian Chengjing, Cai Guanqiang, Li Mingkun, Li Bo, Zhao Li, 2021. Paleoclimatic and Paleoenvironmental Changes Recorded by Elemental Geochemistry in the Northwestern South China Sea since the Past~55 ka. Earth Science, 46(3): 975-985. doi: 10.3799/dqkx.2020.276

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Tian Chengjing, Cai Guanqiang, Li Mingkun, Li Bo, Zhao Li, 2021. Paleoclimatic and Paleoenvironmental Changes Recorded by Elemental Geochemistry in the Northwestern South China Sea since the Past~55 ka. Earth Science, 46(3): 975-985. doi: 10.3799/dqkx.2020.276

Citation:

Tian Chengjing, Cai Guanqiang, Li Mingkun, Li Bo, Zhao Li, 2021. Paleoclimatic and Paleoenvironmental Changes Recorded by Elemental Geochemistry in the Northwestern South China Sea since the Past~55 ka. Earth Science, 46(3): 975-985. doi: 10.3799/dqkx.2020.276

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Paleoclimatic and Paleoenvironmental Changes Recorded by Elemental Geochemistry in the Northwestern South China Sea since the Past~55 ka

doi: 10.3799/dqkx.2020.276

1.
Key Laboratory of Marine Mineral Resources, MNR, Guangzhou Marine Geological Survey, Guangzhou 510075, China
2.
School of Geography, South China Normal University, Guangzhou 510631, China

Received Date: 2020-05-14
Publish Date: 2021-03-15

Abstract

Abstract

The north slope of Xisha carbonate platform in the northwestern South China Sea is supplied by land and marine biogenic materials, so the sediments contain abundant information on climate change. In order to explore the evolution history of paleoclimate and environment in this area, the 828 cm-long core SS7 was selected for elemental geochemical analysis in combination with the chronological framework established by the AMS¹⁴C and oxygen isotope of forams. The results show that the core age at bottom is~55 ka BP, and the elements within sediments are mainly controlled by the terrigenous clastic input, marine authigenesis, redox conditions, and marine chemical deposition. The K/Rb and K/Ti can be used to reflect the surface chemical weathering in the source area and the evolution of the East Asian summer monsoon (EASM) over the past 55 ka. The regional EASM apparently decreased at about 40 ka BP, and the decreases of K/Rb and K/Ti values responded to the rapidly cooling events in the northern hemisphere, including the Heinrich events and the Younger Drays. The EASM over the past 55 ka is not only controlled by the summer insolation in the low-latitude of the northern hemisphere, but also affected by the atmospheric dynamics in the equatorial Pacific (such as the Walker circulation in the Pacific).
- South China Sea,
- East Asian summer monsoon,
- elements,
- Xisha Islands,
- last glacial period,
- geochemistry

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Paleoclimatic and Paleoenvironmental Changes Recorded by Elemental Geochemistry in the Northwestern South China Sea since the Past~55 ka

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