综述与评述

中中新世气候转型期太平洋深层环流变化与碳循环

  • 何志 ,
  • 田军
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  • 同济大学海洋地质国家重点实验室,上海 200092
何志(1998-),男,湖北黄冈人,硕士研究生,主要从事古海洋学与古环境变化研究. E-mail:2031689@tongji.edu.cn
田军(1974-),男,湖北汉川人,教授,主要从事古海洋学与古环境变化研究. E-mail:tianjun@tongji.edu.cn

收稿日期: 2022-07-27

  修回日期: 2022-09-19

  网络出版日期: 2023-02-02

基金资助

国家自然科学基金重点项目“探索晚新生代太平洋中深层经向翻转流与气候演变冰期旋回的关系”(42030403)

Pacific Ocean Deep Circulation and Global Carbon Cycle During the Middle Miocene Climate Transition

  • Zhi HE ,
  • Jun TIAN
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  • State Key Laboratory of Marine Geology, Tongji University, Shanghai 200092, China
HE Zhi (1998-), male, Huanggang City, Hubei Province, Master student. Research areas include paleoceanography and paleoclimatology. E-mail: 2031689@tongji.edu.cn
TIAN Jun (1974-), male, Hanchuang City, Hubei Province, Professor. Research areas include paleoceanography and paleoclimatology. E-mail: tianjun@tongji.edu.cn

Received date: 2022-07-27

  Revised date: 2022-09-19

  Online published: 2023-02-02

Supported by

the National Natural Science Foundation of China “Probing the relationship of the Pacific Meridional overturning circulation with the glacial/interglacial variability of climate change during the late Cenozoic”(42030403)

摘要

中中新世气候转型(14.2~13.9 Ma)是全球联动的一个快速气候变化事件,冰盖、洋流和碳循环均发生显著变化,厘清其驱动机制对理解新生代全球变冷有重要意义。对此已有研究提出2种假说:一种重视洋流重组,另一种则突出碳循环的重要性,但二者都无法完美解释中中新世气候转型的种种现象。实际上,冰盖—洋流—碳循环三者形成耦合的系统,共同造成地球气候变化。综合已有的地质记录,两类机制均导致深部大洋碳储库增大,大气pCO2降低,并进一步促进气候变冷和冰盖增长,表明不同子系统之间的耦合作用引起气候突变。相较于碳循环过程和冰盖变化,学术界对中中新世气候转型期间洋流变化的了解较少,特别是南大洋和太平洋深部水团。未来的研究应聚焦于深部太平洋的洋流变化,以便更全面地完善对中中新世气候转型的理解。

本文引用格式

何志 , 田军 . 中中新世气候转型期太平洋深层环流变化与碳循环[J]. 地球科学进展, 2023 , 38(1) : 17 -31 . DOI: 10.11867/j.issn.1001-8166.2022.076

Abstract

The Middle Miocene Climate Transition (MMCT, 14.2~13.9 Ma) was a global climate change event characterized by significant changes in ice sheets, ocean currents, and carbon cycles. Clarifying the driving mechanism is important for understanding the global cooling during the Cenozoic. Two hypotheses have been proposed to explain the mechanism of MMCT, one emphasizing the reorganization of ocean circulation and the other highlighting the importance of the carbon cycle. However, neither hypothesis can explain the various phenomena of the MMCT. The ice sheets, ocean circulation, and carbon cycle are crucial in the mechanism of the MMCT, and form a coupled system that causes climate change on Earth. With the help of these three elements and combined with geological records, these two mechanisms lead to an increase in deep ocean carbon storage and a decrease in atmospheric pCO2, which further promotes climate cooling and ice sheet growth. In comparison with that on carbon cycle processes and ice sheet changes, existing research regarding ocean circulation, particularly in the deep Southern Ocean and Pacific Ocean, during the MMCT period is insufficient. Consequently, future research should focus on the changes in ocean circulation in these key regions to improve our understanding of the forcing mechanism of MMCT.

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