Preliminary study on climatic signals of stable isotopes from Holocene speleothems under monsoon condition 被引量：4

Preliminary study on climatic signals of stable isotopes from Holocene speleothems under monsoon condition

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摘要 Within the East Asian monsoon zone the change in oxygen isotope of Holocene stalagmite is mainly related to monsoon rain rather than to temperature. And carbon isotope can be taken as a comprehensive signal which contains the natural information and the information of anthropogenic activity. Isotopic analysis is also compared with the annual layer records. Within the East Asian monsoon zone the change in oxygen isotope of Holocene stalagmite is mainly related to monsoon rain rather than to temperature. And carbon isotope can be taken as a comprehensive signal which contains the natural information and the information of anthropogenic activity. Isotopic analysis is also compared with the annual layer records.

作者 Ming Tan Dongsheng Liu Hua Zhong Xiaoguang Qin Hongchun Li Shusen Zhao Tieying Li Jinbo Lu Xiangyang Lu

机构地区 Chinese Acad Sci Univ So Calif Inst Geol Survey Beijing Peking Univ

出处《Chinese Science Bulletin》 SCIE EI CAS 1998年第6期506-509,共4页

基金 theChineseAcademyofSciencesandtheNationalNaturalScienceFoundationofChina (GrantNo .496 72134 )

关键词 SPELEOTHEM stable ISOTOPES monsoon. speleothem stable isotopes monsoon

分类号 P532 [天文地球—古生物学与地层学]

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Chinese Science Bulletin

1998年第6期

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