Large δ 13 C Gradients in the Preindustrial North Atlantic Revealed

Lost Details Changes in ocean circulation are commonly inferred by differences between the distribution of carbon isotopes in the past and now, but making such comparisons neglects the fact that modern fossil fuel burning has modified the carbon isotopic composition of the ocean. This in turn obscur...

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Published in:Science
Main Authors: Olsen, Are, Ninnemann, Ulysses
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 2010
Subjects:
Online Access:http://dx.doi.org/10.1126/science.1193769
https://www.science.org/doi/pdf/10.1126/science.1193769
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spelling craaas:10.1126/science.1193769 2024-06-09T07:48:02+00:00 Large δ 13 C Gradients in the Preindustrial North Atlantic Revealed Olsen, Are Ninnemann, Ulysses 2010 http://dx.doi.org/10.1126/science.1193769 https://www.science.org/doi/pdf/10.1126/science.1193769 en eng American Association for the Advancement of Science (AAAS) Science volume 330, issue 6004, page 658-659 ISSN 0036-8075 1095-9203 journal-article 2010 craaas https://doi.org/10.1126/science.1193769 2024-05-16T12:54:45Z Lost Details Changes in ocean circulation are commonly inferred by differences between the distribution of carbon isotopes in the past and now, but making such comparisons neglects the fact that modern fossil fuel burning has modified the carbon isotopic composition of the ocean. This in turn obscures details about recent mass movement of water. Olsen and Ninnemann (p. 658 ) correct for this effect in the North Atlantic and show that the natural distribution of carbon isotopes has more detail and is clearly related to water mass distributions. The results change some important ideas about glacial-interglacial ocean variations within the context of modern climate variability. Article in Journal/Newspaper North Atlantic AAAS Resource Center (American Association for the Advancement of Science) Science 330 6004 658 659
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description Lost Details Changes in ocean circulation are commonly inferred by differences between the distribution of carbon isotopes in the past and now, but making such comparisons neglects the fact that modern fossil fuel burning has modified the carbon isotopic composition of the ocean. This in turn obscures details about recent mass movement of water. Olsen and Ninnemann (p. 658 ) correct for this effect in the North Atlantic and show that the natural distribution of carbon isotopes has more detail and is clearly related to water mass distributions. The results change some important ideas about glacial-interglacial ocean variations within the context of modern climate variability.
format Article in Journal/Newspaper
author Olsen, Are
Ninnemann, Ulysses
spellingShingle Olsen, Are
Ninnemann, Ulysses
Large δ 13 C Gradients in the Preindustrial North Atlantic Revealed
author_facet Olsen, Are
Ninnemann, Ulysses
author_sort Olsen, Are
title Large δ 13 C Gradients in the Preindustrial North Atlantic Revealed
title_short Large δ 13 C Gradients in the Preindustrial North Atlantic Revealed
title_full Large δ 13 C Gradients in the Preindustrial North Atlantic Revealed
title_fullStr Large δ 13 C Gradients in the Preindustrial North Atlantic Revealed
title_full_unstemmed Large δ 13 C Gradients in the Preindustrial North Atlantic Revealed
title_sort large δ 13 c gradients in the preindustrial north atlantic revealed
publisher American Association for the Advancement of Science (AAAS)
publishDate 2010
url http://dx.doi.org/10.1126/science.1193769
https://www.science.org/doi/pdf/10.1126/science.1193769
genre North Atlantic
genre_facet North Atlantic
op_source Science
volume 330, issue 6004, page 658-659
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.1193769
container_title Science
container_volume 330
container_issue 6004
container_start_page 658
op_container_end_page 659
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