Hydrological impact of Heinrich events in the subtropical northeast Atlantic

被引：503
作者：
Bard, E
Rostek, F
Turon, JL
Gendreau, S
机构：
[1] CEREGE, CNRS, UMR 6635, F-13545 Aix En Provence 4, France
[2] Univ Aix Marseille 3, F-13545 Aix En Provence, France
[3] Univ Bordeaux 1, F-33405 Talence, France
[4] Dept Geol & Oceanog, CNRS, UMR EPOC 5805, F-33405 Talence, France
来源：
SCIENCE | 2000年 / 289卷 / 5483期
关键词：
D O I：
10.1126/science.289.5483.1321
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：
Reconstructing the impact of Heinrich events outside the main belt of ice rafting is crucial to understanding the underlying causes of these abrupt climatic events. A high-resolution study of a marine sediment core from the Iberian margin demonstrates that this midlatitude area was strongly affected both by cooling and advection of low-salinity arctic water masses during the Last three Heinrich events. These paleoclimatic time series reveal the internal complexity of each of the last three Heinrich events and illustrate the value of parallel studies of the organic and inorganic fractions of the sediments.
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收藏
页码：1321 / 1324
页数：4
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