Secular Variation of Iron Isotopes in North Atlantic Deep Water

A high-precision iron isotope time series for a ferromanganese crust demonstrates that the iron isotope composition in North Atlantic Deep Water has changed substantially over the past 6 million years and that iron isotope variations in the crust are closely correlated to those of lead isotopes. The...

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Published in:Science
Main Authors: Zhu, Xiang-Kun, O'Nions, R. Keith, Guo, Yueling, Reynolds, Ben C.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 2000
Subjects:
Online Access:http://dx.doi.org/10.1126/science.287.5460.2000
https://www.science.org/doi/pdf/10.1126/science.287.5460.2000
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spelling craaas:10.1126/science.287.5460.2000 2024-09-15T18:20:41+00:00 Secular Variation of Iron Isotopes in North Atlantic Deep Water Zhu, Xiang-Kun O'Nions, R. Keith Guo, Yueling Reynolds, Ben C. 2000 http://dx.doi.org/10.1126/science.287.5460.2000 https://www.science.org/doi/pdf/10.1126/science.287.5460.2000 en eng American Association for the Advancement of Science (AAAS) Science volume 287, issue 5460, page 2000-2002 ISSN 0036-8075 1095-9203 journal-article 2000 craaas https://doi.org/10.1126/science.287.5460.2000 2024-07-04T04:01:37Z A high-precision iron isotope time series for a ferromanganese crust demonstrates that the iron isotope composition in North Atlantic Deep Water has changed substantially over the past 6 million years and that iron isotope variations in the crust are closely correlated to those of lead isotopes. The close correlation between the two isotope series indicates that the observed iron isotope variations predominantly reflect those of iron input from terrigenous sources and provides no evidence for biologically induced mass fractionation within North Atlantic Deep Water. Article in Journal/Newspaper North Atlantic Deep Water North Atlantic AAAS Resource Center (American Association for the Advancement of Science) Science 287 5460 2000 2002
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description A high-precision iron isotope time series for a ferromanganese crust demonstrates that the iron isotope composition in North Atlantic Deep Water has changed substantially over the past 6 million years and that iron isotope variations in the crust are closely correlated to those of lead isotopes. The close correlation between the two isotope series indicates that the observed iron isotope variations predominantly reflect those of iron input from terrigenous sources and provides no evidence for biologically induced mass fractionation within North Atlantic Deep Water.
format Article in Journal/Newspaper
author Zhu, Xiang-Kun
O'Nions, R. Keith
Guo, Yueling
Reynolds, Ben C.
spellingShingle Zhu, Xiang-Kun
O'Nions, R. Keith
Guo, Yueling
Reynolds, Ben C.
Secular Variation of Iron Isotopes in North Atlantic Deep Water
author_facet Zhu, Xiang-Kun
O'Nions, R. Keith
Guo, Yueling
Reynolds, Ben C.
author_sort Zhu, Xiang-Kun
title Secular Variation of Iron Isotopes in North Atlantic Deep Water
title_short Secular Variation of Iron Isotopes in North Atlantic Deep Water
title_full Secular Variation of Iron Isotopes in North Atlantic Deep Water
title_fullStr Secular Variation of Iron Isotopes in North Atlantic Deep Water
title_full_unstemmed Secular Variation of Iron Isotopes in North Atlantic Deep Water
title_sort secular variation of iron isotopes in north atlantic deep water
publisher American Association for the Advancement of Science (AAAS)
publishDate 2000
url http://dx.doi.org/10.1126/science.287.5460.2000
https://www.science.org/doi/pdf/10.1126/science.287.5460.2000
genre North Atlantic Deep Water
North Atlantic
genre_facet North Atlantic Deep Water
North Atlantic
op_source Science
volume 287, issue 5460, page 2000-2002
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.287.5460.2000
container_title Science
container_volume 287
container_issue 5460
container_start_page 2000
op_container_end_page 2002
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