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Tracing the Nd isotope evolution of North Atlantic deep and intermediate waters in the Western North Atlantic since the Last Glacial Maximum from Blake Ridge sediments

Abstract:

A high-resolution authigenic Nd isotope record has been extracted from the Fe-Mn oxyhydroxide fraction of drift sediments along the Blake Ridge in the North Atlantic. These sediments facilitate reconstruction of the timing and extent of major hydrographic changes in the western North Atlantic since the Last Glacial Maximum (LGM). This is one of the few locations where sediments were deposited in the major flow path of the Western Boundary Undercurrent (WBUC), which transports North Atlantic D...

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Publication status:
Published

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Publisher copy:
10.1016/j.epsl.2007.10.037

Authors


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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
Journal:
EARTH AND PLANETARY SCIENCE LETTERS
Volume:
266
Issue:
1-2
Pages:
61-77
Publication date:
2008-02-01
DOI:
ISSN:
0012-821X
Language:
English
Keywords:
Pubs id:
pubs:82838
UUID:
uuid:3e24de0f-0ad2-48cc-9dfe-ec581b0ddfc8
Local pid:
pubs:82838
Source identifiers:
82838
Deposit date:
2012-12-19

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