Ice Age Terminations

被引:774
作者
Cheng, Hai [1 ]
Edwards, R. Lawrence [1 ]
Broecker, Wallace S. [2 ]
Denton, George H. [3 ]
Kong, Xinggong [4 ]
Wang, Yongjin [4 ]
Zhang, Rong [5 ]
Wang, Xianfeng [1 ]
机构
[1] Univ Minnesota, Dept Geol & Geophys, Minneapolis, MN 55455 USA
[2] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA
[3] Univ Maine, Climate Change Inst, Bryand Global Sci Ctr, Dept Earth Sci, Orono, ME 04469 USA
[4] Nanjing Normal Univ, Coll Geog Sci, Nanjing 210097, Peoples R China
[5] NOAA, Geophys Fluid Dynam Lab, Princeton, NJ 08540 USA
基金
美国国家科学基金会; 中国国家自然科学基金;
关键词
ABRUPT CLIMATE-CHANGE; MILLENNIAL-SCALE; ASIAN MONSOON; HIGH-RESOLUTION; DONGGE CAVE; HULU CAVE; ATLANTIC; RECORD; VARIABILITY; HOLOCENE;
D O I
10.1126/science.1177840
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
Th-230-dated oxygen isotope records of stalagmites from Sanbao Cave, China, characterize Asian Monsoon (AM) precipitation through the ends of the third-and fourthmost recent ice ages. As a result, AM records for the past four glacial terminations can now be precisely correlated with those from ice cores and marine sediments, establishing the timing and sequence of major events. In all four cases, observations are consistent with a classic Northern Hemisphere summer insolation intensity trigger for an initial retreat of northern ice sheets. Meltwater and icebergs entering the North Atlantic alter oceanic and atmospheric circulation and associated fluxes of heat and carbon, causing increases in atmospheric CO2 and Antarctic temperatures that drive the termination in the Southern Hemisphere. Increasing CO2 and summer insolation drive recession of northern ice sheets, with probable positive feedbacks between sea level and CO2.
引用
收藏
页码:248 / 252
页数:5
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