Reduced North Atlantic Deep Water Coeval with the Glacial Lake Agassiz Freshwater Outburst
An outstanding climate anomaly 8200 years before the present (B.P.) in the North Atlantic is commonly postulated to be the result of weakened overturning circulation triggered by a freshwater outburst. New stable isotopic and sedimentological records from a northwest Atlantic sediment core reveal th...
Published in: | Science |
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Main Authors: | , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Association for the Advancement of Science (AAAS)
2008
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Subjects: | |
Online Access: | http://dx.doi.org/10.1126/science.1148924 https://www.science.org/doi/pdf/10.1126/science.1148924 |