The Holocene Asian monsoon: Links to solar changes and North Atlantic climate

被引:2069
作者
Wang, YJ
Cheng, H [1 ]
Edwards, RL
He, YQ
Kong, XG
An, ZS
Wu, JY
Kelly, MJ
Dykoski, CA
Li, XD
机构
[1] Nanjing Normal Univ, Coll Geog Sci, Nanjing 210097, Peoples R China
[2] Univ Minnesota, Dept Geol & Geophys, Minneapolis, MN 55455 USA
[3] Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 71005, Peoples R China
[4] Hong Kong Polytech Univ, Dept Civil & Struct Engn, Kowloon, Hong Kong, Peoples R China
关键词
D O I
10.1126/science.1106296
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
A 5-year-resolution absolute-dated oxygen isotope record from Dongge Cave, southern China, provides a continuous history of the Asian monsoon over the past 9000 years. Although the record broadly follows summer insolation, it is punctuated by eight weak monsoon events tasting similar to 1 to 5 centuries. One correlates with the "8200-year" event, another with the collapse of the Chinese Neolithic culture, and most with North Atlantic ice-rafting events. Cross-correlation of the decadal- to centennial-scale monsoon record with the atmospheric carbon-14 record shows that some, but not all, of the monsoon variability at these frequencies results from changes in solar output.
引用
收藏
页码:854 / 857
页数:4
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