ISSN 1006-3021 CN11-3474/P
Published bimonthly started in 1979
同步变化的东亚季风和印度季风:来自年层石笋氧同位素的证据
  
关键词:Indian monsoon  East Asian monsoon  speleothem  oxygen isotope
基金项目:国家自然科学基金重点项目(编号:40531004)
作者单位E-mail
周翀 中国地质大学生物地质与环境地质教育部重点实验室湖北武汉430074 chyhu@cug.edu.cn 
胡超涌 中国地质大学生物地质与环境地质教育部重点实验室湖北武汉430074  
黄俊华 中国地质大学生物地质与环境地质教育部重点实验室湖北武汉430074  
谢树成 中国地质大学生物地质与环境地质教育部重点实验室湖北武汉430074  
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摘要:
Asynchronous Variation of Indian Monsoon and East Asian Monsoon:Evidence from High-Resolution Oxygen Isotope Records of Laminated Speleothems
      Indian Monsoon and East Asian Monsoon are two sub-systems of Asian Monsoon.A common pattern between the two monsoons at the seasonal and orbital time scales was formulated from the meteorological data and geological records.However,the relationship of the two sub-systems on the inter-annual and inter-decadal scales remains quite obscure.In this study,high-resolution oxygen isotope compositions of two laminated speoleothems from the Defore Cave of Oman and the Heshang Cave of China were compared with each other to detect the link between the Indian Monsoon and the East Asian Monsoon. δ18O of Defore stalagmite is characteristic of the India Monsoon while δ18O of Heshang stalagmite is an indicator of the East Asian Monsoon. Two stalagmite records show similar structures for the last 780 years on the decadal scale, implying the asynchronous variation of the Indian Monsoon and the East Asian Monsoon.
ZHOU Chong,HU Chao-yong,HUANG Jun-hua,XIE Shu-cheng.2008.Asynchronous Variation of Indian Monsoon and East Asian Monsoon:Evidence from High-Resolution Oxygen Isotope Records of Laminated Speleothems[J].Acta Geoscientica Sinica,29(6):761-764.
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