晚中新世西太平洋暖池的浮游有孔虫和氧同位素证据

李前裕; 李保华; 钟广法; 周祖翼; 成鑫荣; 王吉良; 汪品先

Volume 31 Issue 6

Jun. 2006

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Article Navigation > Earth Science > 2006 > 31(6): 754-764

LI Qian-yu, LI Bao-hua, ZHONG Guang-fa, ZHOU Zu-yi, CHENG Xin-rong, WANG Ji-liang, WANG Pin-xian, 2006. Planktonic Foraminifer and Oxygen Isotopic Evidence of a Late Miocene Western Pacific Warm Pool. Earth Science, 31(6): 754-764.

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Planktonic Foraminifer and Oxygen Isotopic Evidence of a Late Miocene Western Pacific Warm Pool

1.
State Key Laboratory of Marine Geology，Tongji University，Shanghai 200092，China
2.
School of Earth and Environmental Sciences，The University of Adelaide，Adelaide SA 5005，Australia
3.
Nanjing Institute of Geology and Paleontology，ChineseAcademy of Sciences，Nanjing 210008，China

Received Date: 2006-04-15
Publish Date: 2006-11-25

Abstract

Abstract

The disappearance at ~10 Ma of the deep dwelling planktonic foraminifer Globoquadrina dehiscens from the western Pacific including the South China Sea was about 3 Ma earlier than its final extinction elsewhere. Accompanying this event at ~10 Ma was a series of faunal turnover characterized by increase in mixed layer, warm-water species and decrease to a minimum in deepwater species. Paleobiological and isotopic evidences indicate sea surface warming and a deepened local thermocline that we interpret as related to the development of an early western Pacific warm pool. The stepwise decline of G. dehiscens and other deep dwelling species from the NW and SW Pacific suggests more intensive warm water pileup than equatorial localities where surface bypass flow through the narrowing Indonesia seaway appears to remain efficient during the Late Miocene. Planktonic ¹⁸O values from the South China Sea consistently lighter than the tropical western Pacific during the Miocene also suggest, similar to today, more variable hydrologic conditions along the periphery than in the core of the warm pool. Stronger hydrologic variability affected mainly by monsoons and increased thermal gradient along the western margin of the Late Miocene warm pool may have contributed to the decline of deep dwelling planktonic species including the early extinction of G. dehiscens from the South China Sea region.
- western Pacific warm pool (WPWP),
- South China Sea,
- Indonesian seaway,
- Miocene,
- planktonic foraminifer,
- oxygen isotope.

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References(63)

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