Increased circumpolar deep water flow in the glacial South Atlantic: the cause of apparent North Atlantic deep water weakening
Increased circumpolar deep water flow in the glacial South Atlantic: the cause of apparent North Atlantic deep water weakening
NADW, CIRCUMPOLAR DEEP WATER, SEDIMENTS, NEODYMIUM ISOTOPES
F618-F619
Bayon, G.
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German, C.R.
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Nesbitt, R.W.
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Bertrand, P.
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Schneider, R.R.
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2001
Bayon, G.
ebd811fb-f5b9-4b3b-87b7-72b6c80cdfcf
German, C.R.
cd0eedd5-1377-4182-9c8a-b06aef8c1069
Nesbitt, R.W.
6a124ad1-4e6d-4407-b92f-592f7fd682e4
Bertrand, P.
a8b0e28a-4f44-4c8f-80b5-afd1a3648d53
Schneider, R.R.
28bfe7fa-4652-4528-a424-7c7cec7c5dd8
Bayon, G., German, C.R., Nesbitt, R.W., Bertrand, P. and Schneider, R.R.
(2001)
Increased circumpolar deep water flow in the glacial South Atlantic: the cause of apparent North Atlantic deep water weakening.
EOS: Transactions American Geophysical Union, 82 (47, Supplement), .
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More information
Published date: 2001
Keywords:
NADW, CIRCUMPOLAR DEEP WATER, SEDIMENTS, NEODYMIUM ISOTOPES
Identifiers
Local EPrints ID: 6046
URI: http://eprints.soton.ac.uk/id/eprint/6046
ISSN: 0096-3941
PURE UUID: 5604f50c-9076-45b7-8470-d35d2504734b
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Date deposited: 10 Jun 2004
Last modified: 11 Dec 2021 13:22
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Contributors
Author:
G. Bayon
Author:
C.R. German
Author:
R.W. Nesbitt
Author:
P. Bertrand
Author:
R.R. Schneider
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