Coherent high- and low-latitude climate variability during the holocene warm period

被引：525
|
作者：
deMenocal, P [1 ]
Ortiz, J
Guilderson, T
Sarnthein, M
机构：
[1] Columbia Univ, Lamont Doherty Earth Observ, Palisades, NY 10964 USA
[2] Lawrence Livermore Natl Lab, Ctr Accelerator Mass Spectrometry, Livermore, CA 94551 USA
[3] Univ Kiel, Inst Geowissensch, Kiel, Germany
来源：
SCIENCE | 2000年 / 288卷 / 5474期
关键词：
D O I：
10.1126/science.288.5474.2198
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 faunal record of sea-surface temperature (SST) variations off West Africa documents a series of abrupt, millennial-scale cooling events, which punctuated the Holocene warm period. These events evidently resulted from increased southward advection of cooler temperate or subpolar waters to this subtropical location or from enhanced regional upwelling. The most recent of these events was the Little Ice Age, which occurred between 1300 to 1850 A.D., when subtropical SSTs were reduced by 3 degrees to 4 degrees C. These events were synchronous with Holocene changes in subpolar North Atlantic SSTs, documenting a strong, in-phase link between millennial-scale variations in high- and Low-latitude climate during the Holocene.
引用
收藏
页码：2198 / 2202
页数：5
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