Dynamics of North Atlantic Deep Water masses during the Holocene

High resolution flow speed reconstructions of two core sites located on Gardar Drift in the northeast Atlantic Basin and Orphan Knoll in the northwest Atlantic Basin reveal a long-term decrease in flow speed of Northeast Atlantic Deep Water (NEADW) after 6,500 years. Benthic foraminiferal oxygen iso...

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Bibliographic Details
Published in:Paleoceanography
Main Authors: Hoogakker, B. A. A., Chapman, M. R., McCave, I. N., Hillaire-Marcel, C., Ellison, C. R. W., Hall, Ian Robert, Telford, R. J.
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2011
Subjects:
Online Access:https://orca.cardiff.ac.uk/id/eprint/30488/
http://www.agu.org/pubs/crossref/2011/2011PA002155.shtml
https://orca.cardiff.ac.uk/id/eprint/30488/1/Hoogakker%202011.pdf
https://doi.org/10.1029/2011PA002155