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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Published in:Science
Main Authors: Bard, Edouard, Rostek, Frauke, Turon, Jean-Louis, Gendreau, Sandra
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 2000
Subjects:
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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spelling 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
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id 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
container_title Science
container_volume 289
container_issue 5483
container_start_page 1321
op_container_end_page 1324
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