A Heinrich-like event, H-0 (DC-0): Source(s) for detrital carbonate in the North Atlantic during the Younger Dryas Chronozone
In the North Atlantic we define H-0 as a Heinrich-like event which occurred during the Younger Dryas chron. On the SE Baffin shelf prior to 11 ka, surface water productivity was reasonably high, as measured by the numbers of diatom and planktic foraminifera per gram, but an abrupt increase in detrit...
Published in: | Paleoceanography |
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Main Authors: | , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
American Geophysical Union
2010
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Subjects: | |
Online Access: | https://oceanrep.geomar.de/id/eprint/37690/ https://oceanrep.geomar.de/id/eprint/37690/1/Andrews.pdf https://doi.org/10.1029/95PA01426 |