A Heinrich-like event, H-0 (DC-0): Source(s) for detrital carbonate in the North Atlantic during the Younger Dryas Chronozone

• Published in: Paleoceanography
• Main Authors: Andrews, J. T., Jennings, Anne E., Kerwin, M., Kirby, M., Manley, W., Miller, G. H., Bond, G., MacLean, B.
• Format: Article in Journal/Newspaper
• Language: English
• Published: AGU (American Geophysical Union) 1995
• Subjects: Baffin Bay; Cumberland Sound; Hudson; Hudson Bay; Hudson Strait; Newfoundland; Baffin; Davis Strait; Ice Sheet; Labrador Sea; North Atlantic
• Online Access: https://oceanrep.geomar.de/id/eprint/32852/; https://oceanrep.geomar.de/id/eprint/32852/1/Andrews.pdf; https://doi.org/10.1029/95PA01426

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...