Hydrological Impact of Heinrich Events in the Subtropical Northeast Atlantic
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...
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2000
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Online Access: | http://dx.doi.org/10.1126/science.289.5483.1321 https://www.science.org/doi/pdf/10.1126/science.289.5483.1321 |
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craaas:10.1126/science.289.5483.1321 2024-09-15T18:25:20+00:00 Hydrological Impact of Heinrich Events in the Subtropical Northeast Atlantic Bard, Edouard Rostek, Frauke Turon, Jean-Louis Gendreau, Sandra 2000 http://dx.doi.org/10.1126/science.289.5483.1321 https://www.science.org/doi/pdf/10.1126/science.289.5483.1321 en eng American Association for the Advancement of Science (AAAS) Science volume 289, issue 5483, page 1321-1324 ISSN 0036-8075 1095-9203 journal-article 2000 craaas https://doi.org/10.1126/science.289.5483.1321 2024-08-29T04:01:04Z 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. Article in Journal/Newspaper Northeast Atlantic AAAS Resource Center (American Association for the Advancement of Science) Science 289 5483 1321 1324 |
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Open Polar |
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AAAS Resource Center (American Association for the Advancement of Science) |
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craaas |
language |
English |
description |
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. |
format |
Article in Journal/Newspaper |
author |
Bard, Edouard Rostek, Frauke Turon, Jean-Louis Gendreau, Sandra |
spellingShingle |
Bard, Edouard Rostek, Frauke Turon, Jean-Louis Gendreau, Sandra Hydrological Impact of Heinrich Events in the Subtropical Northeast Atlantic |
author_facet |
Bard, Edouard Rostek, Frauke Turon, Jean-Louis Gendreau, Sandra |
author_sort |
Bard, Edouard |
title |
Hydrological Impact of Heinrich Events in the Subtropical Northeast Atlantic |
title_short |
Hydrological Impact of Heinrich Events in the Subtropical Northeast Atlantic |
title_full |
Hydrological Impact of Heinrich Events in the Subtropical Northeast Atlantic |
title_fullStr |
Hydrological Impact of Heinrich Events in the Subtropical Northeast Atlantic |
title_full_unstemmed |
Hydrological Impact of Heinrich Events in the Subtropical Northeast Atlantic |
title_sort |
hydrological impact of heinrich events in the subtropical northeast atlantic |
publisher |
American Association for the Advancement of Science (AAAS) |
publishDate |
2000 |
url |
http://dx.doi.org/10.1126/science.289.5483.1321 https://www.science.org/doi/pdf/10.1126/science.289.5483.1321 |
genre |
Northeast Atlantic |
genre_facet |
Northeast Atlantic |
op_source |
Science volume 289, issue 5483, page 1321-1324 ISSN 0036-8075 1095-9203 |
op_doi |
https://doi.org/10.1126/science.289.5483.1321 |
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Science |
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289 |
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5483 |
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1321 |
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1324 |
_version_ |
1810465841850875904 |