南海南部普林虫与“中更新世革命”

徐建; 汪品先; 黄宝琦; 翦知湣

Volume 29 Issue 1

Jan. 2004

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Article Navigation > Earth Science > 2004 > 29(1): 7-14

XU Jian, WANG Pin-xian, HUANG Bao-qi, JIAN Zhi-min, 2004. Mid-Pleistocene Revolution Recorded by Pulleniatina obliquiloculata in the Southern South China Sea. Earth Science, 29(1): 7-14.

Citation:

XU Jian, WANG Pin-xian, HUANG Bao-qi, JIAN Zhi-min, 2004. Mid-Pleistocene Revolution Recorded by Pulleniatina obliquiloculata in the Southern South China Sea. Earth Science, 29(1): 7-14.

XU Jian, WANG Pin-xian, HUANG Bao-qi, JIAN Zhi-min, 2004. Mid-Pleistocene Revolution Recorded by Pulleniatina obliquiloculata in the Southern South China Sea. Earth Science, 29(1): 7-14.

Citation:

XU Jian, WANG Pin-xian, HUANG Bao-qi, JIAN Zhi-min, 2004. Mid-Pleistocene Revolution Recorded by Pulleniatina obliquiloculata in the Southern South China Sea. Earth Science, 29(1): 7-14.

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Mid-Pleistocene Revolution Recorded by Pulleniatina obliquiloculata in the Southern South China Sea

1.
Laboratory of Marine Geology, Tongji University, Shanghai 200092, China
2.
College of En vironmental Sciences, Peking Un iversity, Beijing 100871, China

Received Date: 2003-07-11
Publish Date: 2004-01-25

Abstract

Abstract

Planktonic foraminifers from ODP Site 1143, southern South China Sea (SCS), were analyzed to reveal their response to glacial cycles in the past 2.1 Ma. Pulleniatina obliquiloculata, a widely-accepted indicator of the Kuroshio, shows completely reverse fluctuations, with high abundance in glacials, in southern SCS to those in the Okinawa trough and northern SCS since the Mid-Pleistocene Revolution (MPR). Before the MPR, P.obliquiloculata is abundant in interglacial intervals. Cross-spectral and phase analyses between P.obliquiloculata and δ¹⁸O confirmed the observations depicted above. The authors ascribed the transition of P.obliquiloculata's response to glacial cycles in southern SCS to a profound change in the regional upper ocean structure, probably related to glacial separation of the southern SCS from the Indian water and to higher surface salinity during glacial times after the MPR.
- Pulleniatina obliquiloculata,
- glacial cycle,
- the Mid-Pleistocene Revolution (MPR),
- southern South China Sea (SCS)

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References(43)

References

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Mid-Pleistocene Revolution Recorded by Pulleniatina obliquiloculata in the Southern South China Sea

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