南海北部晚第四纪高分辨率浮游氧同位素地层学及其古气候信息

葛黄敏; 李前裕; 成鑫荣; 郑洪波; 贺娟

doi:10.3799/dqkx.2010.067

Volume 35 Issue 4

Jul. 2010

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Article Navigation > Earth Science > 2010 > 35(4): 515-525

GE Huang-min, LI Qian-yu, CHENG Xin-rong, ZHENG Hong-bo, HE Juan, 2010. Late Quaternary High Resolution Monsoon Records in Planktonic Stable Isotopes from Northern South China Sea. Earth Science, 35(4): 515-525. doi: 10.3799/dqkx.2010.067

Citation:

GE Huang-min, LI Qian-yu, CHENG Xin-rong, ZHENG Hong-bo, HE Juan, 2010. Late Quaternary High Resolution Monsoon Records in Planktonic Stable Isotopes from Northern South China Sea. Earth Science, 35(4): 515-525. doi: 10.3799/dqkx.2010.067

Citation:

GE Huang-min, LI Qian-yu, CHENG Xin-rong, ZHENG Hong-bo, HE Juan, 2010. Late Quaternary High Resolution Monsoon Records in Planktonic Stable Isotopes from Northern South China Sea. Earth Science, 35(4): 515-525. doi: 10.3799/dqkx.2010.067

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Late Quaternary High Resolution Monsoon Records in Planktonic Stable Isotopes from Northern South China Sea

doi: 10.3799/dqkx.2010.067

1.
State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China
2.
School of Earth and Environment Science, University of Adelaide, Adelaide SA5005, Australia

Received Date: 2009-11-08
Publish Date: 2010-07-01

Abstract

Abstract

Oxygen and carbon stable isotope records (with an average time resolution of 228 a) were obtained from Core MD05-2904 (19°27.32', 116°15.15', water depth 2 066 m), using the mixed-layer dwelling planktonic foraminifer Globigerinoides ruber (white). The 45 m core spans from end of MIS 8 to the Holocene, representing the sediment record of the last 257 a. Strong precession periods (23.4 ka and 19.8 ka) were found from spectral analysis of both δ¹⁸O and δ¹³C records, following with semi-precession cycles (11.7 ka and 9.9 ka). The high resolution δ¹⁸O record of MD05-2904 reveals nearly all the Dansgaard/Oeschger and Heinrich events during MIS 2-4, as defined in the Greenland ice core record. A better correlation between MD05-2904 planktonic δ¹⁸O, the Hulu stalagmite δ¹⁸O record and previously published planktonic δ¹⁸O records from the SCS suggests that the planktonic δ¹⁸O record is influenced by monsoon-dominated regional factors, such as rainfall and river discharge related salinity changes. Lighter δ¹⁸O values in early MIS 3, early MIS 6 and MIS 7.4, and heavier values in MIS 5.5 are due to changes in precipitation and evaporation affected by monsoon. Sedimentation rates increased to 65-70 cm/ka in LGM, indicating more sediments when the site location was closer to the river mouth during glacial at lower sea level.
- oxygen isotope,
- stratigraphy,
- millennial scale climate change,
- East Asian monsoon,
- MD05-2904,
- northern South China Sea

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References(47)

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Late Quaternary High Resolution Monsoon Records in Planktonic Stable Isotopes from Northern South China Sea

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