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OXYGEN ISOTOPE STRATIGRAPHY OF WESTERN EQUATORIAL PACIFIC CORE L2011

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【Author】 WU SHIYING FANG ZECHENG (First Institute of Oceanography, National Bureau of Oceanography, Qingdao) CHEN CHENGYE ZHENG SHUHUI (Department of Geology, Peking University)

【机构】 First Institute of Oceanography； National Bureau of Oceanography； Qingdao； Department of Geology； Peking University； Peking University；

【摘要】 <正> The oxygen isotope composition of foraminifera in deep-sea sediments has provided so far the most accurate record for the Pleistocene Epoch. It revises the traditional concepts about the glacial-interglacial (cold-warm) stages in the Quaternary climate and has become the basic stratigraphic tool as compared with other methods. Since the evolution of the Quaternary climate has great influence on the life of human beings and the geological environment, oxygen isotope stratigraphy has been established and used extensively in investigations of the history of events in the deep-sea core.更多还原

【关键词】 stratigraphic； isotope； Quaternary； stratigraphy； glacial； sedimentation； dissolution； Pleistocene； buried； record；

【文献出处】 A Monthly Journal of Science ,科学通报(英文版) , 编辑部邮箱 ,1983年02期

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