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DOI10.1126/science.289.5483.1321
Hydrological impact of Heinrich events in the subtropical Northeast Atlantic
Bard E.; Rostek F.; Turon J.-L.; Gendreau S.
发表日期2000
ISSN0036-8075
起始页码1321
结束页码1324
卷号289期号:5483
英文摘要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.
英文关键词advection; cooling; Heinrich event; hydrological response; paleoclimate; water mass; arctic climate; article; priority journal; salinity; sea; sediment; tropic climate; water pollutant; water pollution; Atlantic Ocean
语种英语
来源期刊Science
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/242954
作者单位CEREGE, UMR 6635, CNRS/Universite d'Aix-Marseille III, Europole de l'Arbois, 13545 Aix-en-Provence Cedex 4, France
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Bard E.,Rostek F.,Turon J.-L.,et al. Hydrological impact of Heinrich events in the subtropical Northeast Atlantic[J],2000,289(5483).
APA Bard E.,Rostek F.,Turon J.-L.,&Gendreau S..(2000).Hydrological impact of Heinrich events in the subtropical Northeast Atlantic.Science,289(5483).
MLA Bard E.,et al."Hydrological impact of Heinrich events in the subtropical Northeast Atlantic".Science 289.5483(2000).
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