The influence of Antarctic subglacial volcanism on the global iron cycle during the Last Glacial Maximum

Contributions of iron sources to Southern Ocean CO2sequestration during the last glacial period remain uncertain. Here, based on the biogeochemical analysis of subglacial calcites, the authors propose Antarctic volcanism, via subglacial drainage of Fe-rich waters, as a key contributor.

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Autores principales: Silvia Frisia, Laura S. Weyrich, John Hellstrom, Andrea Borsato, Nicholas R. Golledge, Alexandre M. Anesio, Petra Bajo, Russell N. Drysdale, Paul C. Augustinus, Camille Rivard, Alan Cooper
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Publicado: Nature Portfolio 2017
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Acceso en línea:https://doaj.org/article/86ce22f85bef4743829e3dc7dbbe6fd6
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spelling oai:doaj.org-article:86ce22f85bef4743829e3dc7dbbe6fd62021-12-02T15:38:56ZThe influence of Antarctic subglacial volcanism on the global iron cycle during the Last Glacial Maximum10.1038/ncomms154252041-1723https://doaj.org/article/86ce22f85bef4743829e3dc7dbbe6fd62017-06-01T00:00:00Zhttps://doi.org/10.1038/ncomms15425https://doaj.org/toc/2041-1723Contributions of iron sources to Southern Ocean CO2sequestration during the last glacial period remain uncertain. Here, based on the biogeochemical analysis of subglacial calcites, the authors propose Antarctic volcanism, via subglacial drainage of Fe-rich waters, as a key contributor.Silvia FrisiaLaura S. WeyrichJohn HellstromAndrea BorsatoNicholas R. GolledgeAlexandre M. AnesioPetra BajoRussell N. DrysdalePaul C. AugustinusCamille RivardAlan CooperNature PortfolioarticleScienceQENNature Communications, Vol 8, Iss 1, Pp 1-9 (2017)
institution DOAJ
collection DOAJ
language EN
topic Science
Q
spellingShingle Science
Q
Silvia Frisia
Laura S. Weyrich
John Hellstrom
Andrea Borsato
Nicholas R. Golledge
Alexandre M. Anesio
Petra Bajo
Russell N. Drysdale
Paul C. Augustinus
Camille Rivard
Alan Cooper
The influence of Antarctic subglacial volcanism on the global iron cycle during the Last Glacial Maximum
description Contributions of iron sources to Southern Ocean CO2sequestration during the last glacial period remain uncertain. Here, based on the biogeochemical analysis of subglacial calcites, the authors propose Antarctic volcanism, via subglacial drainage of Fe-rich waters, as a key contributor.
format article
author Silvia Frisia
Laura S. Weyrich
John Hellstrom
Andrea Borsato
Nicholas R. Golledge
Alexandre M. Anesio
Petra Bajo
Russell N. Drysdale
Paul C. Augustinus
Camille Rivard
Alan Cooper
author_facet Silvia Frisia
Laura S. Weyrich
John Hellstrom
Andrea Borsato
Nicholas R. Golledge
Alexandre M. Anesio
Petra Bajo
Russell N. Drysdale
Paul C. Augustinus
Camille Rivard
Alan Cooper
author_sort Silvia Frisia
title The influence of Antarctic subglacial volcanism on the global iron cycle during the Last Glacial Maximum
title_short The influence of Antarctic subglacial volcanism on the global iron cycle during the Last Glacial Maximum
title_full The influence of Antarctic subglacial volcanism on the global iron cycle during the Last Glacial Maximum
title_fullStr The influence of Antarctic subglacial volcanism on the global iron cycle during the Last Glacial Maximum
title_full_unstemmed The influence of Antarctic subglacial volcanism on the global iron cycle during the Last Glacial Maximum
title_sort influence of antarctic subglacial volcanism on the global iron cycle during the last glacial maximum
publisher Nature Portfolio
publishDate 2017
url https://doaj.org/article/86ce22f85bef4743829e3dc7dbbe6fd6
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