Millennial scale persistence of organic carbon bound to iron in Arctic marine sediments

Burial of organic material in marine sediments can sequester massive amounts of carbon, but the dynamics of this carbon sink are poorly understood. Here the authors investigate the so-called rusty carbon sink in Arctic shelf sediments, finding that organic carbon-iron associations are stable for 100...

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Main Authors: Johan C. Faust, Allyson Tessin, Ben J. Fisher, Mark Zindorf, Sonia Papadaki, Katharine R. Hendry, Katherine A. Doyle, Christian März
Format: Article
Language:English
Published: Nature Portfolio 2021-01-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/s41467-020-20550-0
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author Johan C. Faust
Allyson Tessin
Ben J. Fisher
Mark Zindorf
Sonia Papadaki
Katharine R. Hendry
Katherine A. Doyle
Christian März
author_facet Johan C. Faust
Allyson Tessin
Ben J. Fisher
Mark Zindorf
Sonia Papadaki
Katharine R. Hendry
Katherine A. Doyle
Christian März
author_sort Johan C. Faust
collection DOAJ
description Burial of organic material in marine sediments can sequester massive amounts of carbon, but the dynamics of this carbon sink are poorly understood. Here the authors investigate the so-called rusty carbon sink in Arctic shelf sediments, finding that organic carbon-iron associations are stable for 1000 s of years.
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spelling doaj.art-e4b94dd70b4c459c89c568de4135f5c92022-12-21T21:35:30ZengNature PortfolioNature Communications2041-17232021-01-011211910.1038/s41467-020-20550-0Millennial scale persistence of organic carbon bound to iron in Arctic marine sedimentsJohan C. Faust0Allyson Tessin1Ben J. Fisher2Mark Zindorf3Sonia Papadaki4Katharine R. Hendry5Katherine A. Doyle6Christian März7School of Earth and Environment, The University of LeedsDepartment of Geology, Kent State UniversitySchool of Earth and Environment, The University of LeedsLaboratoire Environnement Profond, Ifremer - Centre de BretagneSchool of Earth Sciences, University of BristolSchool of Earth Sciences, University of BristolSchool of Earth and Environment, The University of LeedsSchool of Earth and Environment, The University of LeedsBurial of organic material in marine sediments can sequester massive amounts of carbon, but the dynamics of this carbon sink are poorly understood. Here the authors investigate the so-called rusty carbon sink in Arctic shelf sediments, finding that organic carbon-iron associations are stable for 1000 s of years.https://doi.org/10.1038/s41467-020-20550-0
spellingShingle Johan C. Faust
Allyson Tessin
Ben J. Fisher
Mark Zindorf
Sonia Papadaki
Katharine R. Hendry
Katherine A. Doyle
Christian März
Millennial scale persistence of organic carbon bound to iron in Arctic marine sediments
Nature Communications
title Millennial scale persistence of organic carbon bound to iron in Arctic marine sediments
title_full Millennial scale persistence of organic carbon bound to iron in Arctic marine sediments
title_fullStr Millennial scale persistence of organic carbon bound to iron in Arctic marine sediments
title_full_unstemmed Millennial scale persistence of organic carbon bound to iron in Arctic marine sediments
title_short Millennial scale persistence of organic carbon bound to iron in Arctic marine sediments
title_sort millennial scale persistence of organic carbon bound to iron in arctic marine sediments
url https://doi.org/10.1038/s41467-020-20550-0
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