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No change in the neodymium isotope composition of deep water exported from the North Atlantic on glacial-interglacial time scales

Abstract:

Quantifying past circulation is a vital part of testing our understanding of the modern and future climate system. The isotopic composition of neodymium (Nd) in marine precipitates has considerable promise as a recorder of past circulation patterns, but its robust application requires knowledge of the end-member compositions in order to correctly deconvolute a downstream signal. We show here, using in situ, high temporal resolution analyses of ferromanganese crusts from the North Atlantic, th...

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Publication status:
Published

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Publisher copy:
10.1130/G23204A.1

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Institution:
University of Oxford
Department:
Oxford, MPLS, Earth Sciences
Role:
Author
Journal:
GEOLOGY
Volume:
35
Issue:
1
Pages:
37-40
Publication date:
2007-01-05
DOI:
EISSN:
0091-7613
ISSN:
0091-7613
URN:
uuid:4de43b33-6f67-4b84-8efe-e14d9c23ff60
Source identifiers:
184844
Local pid:
pubs:184844

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