Response to Comment on "Mixed-Layer Deepening During Heinrich Events: A Multi-Planktonic Foraminiferal δ 18 O Approach"
Hillaire-Marcel and de Vernal question our hypothesis of the “homogenization of the upper water masses” of the North Atlantic during Heinrich events 0, 1, and 4. Here, we respond to their specific points and synthesize data from the southern Labrador Sea cores, the basic tenet of Hillaire-Marcel and...
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.1153646 https://www.science.org/doi/pdf/10.1126/science.1153646 |
Summary: | Hillaire-Marcel and de Vernal question our hypothesis of the “homogenization of the upper water masses” of the North Atlantic during Heinrich events 0, 1, and 4. Here, we respond to their specific points and synthesize data from the southern Labrador Sea cores, the basic tenet of Hillaire-Marcel and de Vernal's arguments. |
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