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dc.contributor.authorYuan, D. X.zh_CN
dc.contributor.authorCheng, H.zh_CN
dc.contributor.authorEdwards, R. L.zh_CN
dc.contributor.authorDykoski, C. A.zh_CN
dc.contributor.authorKelly, M. J.zh_CN
dc.contributor.authorZhang, M. L.zh_CN
dc.contributor.authorQing, J. M.zh_CN
dc.contributor.authorLin, Y. S.zh_CN
dc.contributor.authorWang, Y. J.zh_CN
dc.contributor.authorWu, J. Y.zh_CN
dc.contributor.authorDorale, J. A.zh_CN
dc.contributor.authorAn, Z. S.zh_CN
dc.contributor.authorCai, Y. J.zh_CN
dc.contributor.author袁东星zh_CN
dc.date.accessioned2013-12-12T02:08:44Z
dc.date.available2013-12-12T02:08:44Z
dc.date.issued2004zh_CN
dc.identifier.citationScience,304(5670):575-578zh_CN
dc.identifier.issn0036-8075zh_CN
dc.identifier.otherISI:000220975100045zh_CN
dc.identifier.urihttps://dspace.xmu.edu.cn/handle/2288/60765
dc.description.abstractThorium-230 ages and oxygen isotope ratios of stalagmites from Dongge Cave, China, characterize the Asian Monsoon and low-latitude precipitation over the past 160,000 years. Numerous abrupt changes in O-18/O-16 values result from changes in tropical and subtropical precipitation driven by insolation and millennial-scale circulation shifts. The Last Interglacial Monsoon lasted 9.7+/-1.1 thousand years, beginning with an abrupt (less than 200 years) drop in O-18/O-16 values 129.3+/-0.9 thousand years ago and ending with an abrupt (less than 300 years) rise in O-18/O-16 values 119.6+/-0.6 thousand years ago. The start coincides with insolation rise and measures of full interglacial conditions, indicating that insolation triggered the final rise to full interglacial conditions.zh_CN
dc.language.isoen_USzh_CN
dc.subjectICE-CORE RECORDzh_CN
dc.subjectSTABLE ISOTOPESzh_CN
dc.subjectTERMINATION IIzh_CN
dc.subjectCLIMATEzh_CN
dc.subjectPERIODzh_CN
dc.subjectPRECIPITATIONzh_CN
dc.subjectSPELEOTHEMSzh_CN
dc.subjectHOLOCENEzh_CN
dc.subjectEVENTzh_CN
dc.titleTiming, duration, and transitions of the Last Interglacial Asian Monsoonzh_CN
dc.typeArticlezh_CN


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