南海北部ZHS-176孔古海洋学记录：氧同位素和有机碳

葛倩; 孟宪伟; 初凤友; 薛佐; 雷吉江

doi:10.3724/SP.J.1140.2012.05073

南海北部ZHS-176孔古海洋学记录：氧同位素和有机碳

1 国家海洋局海底科学重点实验室, 国家海洋局第二海洋研究所, 杭州 310012;

2 国家海洋局第一海洋研究所, 青岛 266061;

3 Department of Marine, Earth and Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695, USA

基金项目:
国家自然科学基金青年基金项目(41106045)

国家海洋局第二海洋研究所基本科研业务费专项(JT1102)

详细信息

作者简介: 葛倩(1983-),男,助理研究员,主要从事古海洋学方面的研究,E-mail:gq980447@hotmail.com

中图分类号: P736.2

收稿日期: 2012-06-13

修回日期: 2012-07-16

PALEOCEANOGRAPHIC RECORDS OF CORE ZHS-176 FROM THE NORTHERN SOUTH CHINA SEA: OXYGEN ISOTOPE AND ORGANIC CARBON

1 Key Laboratory of Submarine Geosciences, State Oceanic Administration, Second Institute of Oceanography, State Oceanic Administration, Hangzhou, 310012, China;

2 First Institute of Oceanography, State Oceanic Administration, Qingdao, 266061, China;

3 Department of Marine, Earth and Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695, USA

Received Date: 13 June 2012

Revised Date: 16 July 2012

摘要

摘要: 对南海北部陆坡ZHS-176孔进行浮游有孔虫氧同位素和有机碳的研究,重建了末次冰期以来的古气候演化历史。ZHS-176孔浮游有孔虫氧同位素分析揭示了末次冰期期间的气候波动,如末次盛冰期、Heinrich事件1、Bølling-Allerød暖期与新仙女木事件在南海北部陆坡均有响应。同时,在全新世阶段存在3个强降水期和3个弱降水期。ZHS-176孔有机碳以生物成因为主,随着夏季风的增强,陆源物质含量增加,但在3 kaBP以后由于华南地区夏季风减弱而导致陆源输入减少。
- 全新世 /
- 氧同位素 /
- 有机碳 /
- 南海 /
- 末次冰期
Abstract: A coupled approach based on planktonic foraminiferal oxygen isotope and organic carbon from core ZHS-176 in the northern South China Sea slope is adopted to reconstruct the history of paleoclimatic evolution since the last glacial stage. The planktonic foraminiferal oxygen isotopic oscillations in core ZHS-176 during the last glacial period are coeval with climatic variations recorded in the Greenland ice core and Western Pacific sediment. These variations include the Last Glacial Maximum, Heinrich event 1, Bølling-Allerød, and Younger Dryas. During the Holocene, we also find three periods of strong precipitation stages and three periods of weak precipitation stages. The oxygen isotopic record exhibits correlation with climate records from distant regions, including the high-latitude area of North Atlantic, providing evidence for global tele-connection among regional climates. The biogenic organic carbon is dominated in core ZHS-176, and the content of terrigenous one increases while the East Asian summer monsoon strengthens. But after 3 kaBP, the terrigenous input decreases because of the weakened East Asian summer monsoon in the South China region.
- South China Sea /
- last glacial /
- Holocene /
- oxygen isotope /
- organic carbon

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参考文献(62)

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南海北部ZHS-176孔古海洋学记录：氧同位素和有机碳

1 国家海洋局海底科学重点实验室, 国家海洋局第二海洋研究所, 杭州 310012; 2 国家海洋局 第一海洋研究所, 青岛 266061; 3 Department of Marine, Earth and Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695, USA

作者简介: 葛倩(1983-),男,助理研究员,主要从事古海洋学方面的研究,E-mail:gq980447@hotmail.com

PALEOCEANOGRAPHIC RECORDS OF CORE ZHS-176 FROM THE NORTHERN SOUTH CHINA SEA: OXYGEN ISOTOPE AND ORGANIC CARBON

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1 国家海洋局海底科学重点实验室, 国家海洋局第二海洋研究所, 杭州 310012;

2 国家海洋局第一海洋研究所, 青岛 266061;

3 Department of Marine, Earth and Atmospheric Sciences, North Carolina State University, Raleigh, NC 27695, USA