干旱气候变化与可持续发展

大洋钻探与全球变化(二)——从海洋角度研究第四纪古全球变化

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  • 同济大学海洋地质开放实验室  上海  200092
翦知泯,男,29岁,讲师(博士生),主要从事古海洋和微体古生物学研究.

收稿日期: 1995-02-21

  网络出版日期: 1995-06-01

基金资助

国家自然科学基金项目“西北太平洋晚第四纪三维空间的古水团研究尝试”(编:49406067)资助.

ODP AND GLOBAL CHANGE(II)—STUDYING QUATERNARY PAST GLOBAL CHANGE FROM THE VIEW OF SEA

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  • Laboratory of Marine Geology,Tongji University,Shanghai   200092

Received date: 1995-02-21

  Online published: 1995-06-01

摘要

海洋在第四纪全球气候和环境的变化中起着至关重要的作用。一方面,海洋沉积记录了大量第四纪古全球变化的信息,特别是可提供古全球变化中高分辨率的短期气候事件的记录;另一方面,无论是全球性大洋环流、生物和化学的变化,还是区域性西太平洋边缘海浅水陆架的出没,这些海洋事件都可能是许多第四纪古全球变化现象的原因之所在。因此,从海洋角度研究第四纪古全球变化,已成为当前古全球变化和国际古海洋学研究的重点。在这方面,深海钻探(DSDP)/大洋钻探(ODP)以及相关的海洋研究计划做出了巨大贡献。

本文引用格式

翦知泯 . 大洋钻探与全球变化(二)——从海洋角度研究第四纪古全球变化[J]. 地球科学进展, 1995 , 10(3) : 267 -272 . DOI: 10.11867/j.issn.1001-8166.1995.03.0267

Abstract

The sea which covers 71% of the Earth's surface plays a very important role in Quaternary changes of the Earth's climate and environment. Firstly,marine sediments contain a lot of information on Quaternary past global change,providing high-resolution records of short-term climatic events such as Younger Dryas event. Secondly, marine events, being changes in the circulation,biololgy and chemistry of the global ocean,or regional changes of the eustasy-induced emergence and submergence of shallow-water shelves in the western Pacific marginal seas, all can be causes of many phenomena of the Quaternary global changes. Therefore,Quaternry past global change studies from the marine aspect have become one of foci of the current international endeavor in global change science and paleoceanography. Great contribution to the field have been made by the Deep Sea Drilling (DSDP)/Ocean Drilling Program (ODP) and other related marine science programs.

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