Iron from a submarine source impacts the productive layer of the Western Tropical South Pacific (WTSP)

Abstract In the Western Tropical South Pacific, patches of high chlorophyll concentrations linked to the occurrence of N2-fixing organisms are found in the vicinity of volcanic islands. The survival of these organisms relies on a high bioavailable iron supply whose origin and fluxes remain unknown....

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Autores principales: Cécile Guieu, Sophie Bonnet, Anne Petrenko, Christophe Menkes, Valérie Chavagnac, Karine Desboeufs, Christophe Maes, Thierry Moutin
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Publicado: Nature Portfolio 2018
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Acceso en línea:https://doaj.org/article/8d047e9d0eda47d29fff4a0cb420ff7a
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spelling oai:doaj.org-article:8d047e9d0eda47d29fff4a0cb420ff7a2021-12-02T15:08:17ZIron from a submarine source impacts the productive layer of the Western Tropical South Pacific (WTSP)10.1038/s41598-018-27407-z2045-2322https://doaj.org/article/8d047e9d0eda47d29fff4a0cb420ff7a2018-06-01T00:00:00Zhttps://doi.org/10.1038/s41598-018-27407-zhttps://doaj.org/toc/2045-2322Abstract In the Western Tropical South Pacific, patches of high chlorophyll concentrations linked to the occurrence of N2-fixing organisms are found in the vicinity of volcanic islands. The survival of these organisms relies on a high bioavailable iron supply whose origin and fluxes remain unknown. Here, we measured high dissolved iron (DFe) concentrations (up to 66 nM) in the euphotic layer, extending zonally over 10 degrees longitude (174 E−175 W) at ∼20°S latitude. DFe atmospheric fluxes were at the lower end of reported values of the remote ocean and could not explain the high DFe concentrations measured in the water column in the vicinity of Tonga. We argue that the high DFe concentrations may be sustained by a submarine source, also characterized by freshwater input and recorded as salinity anomalies by Argo float in situ measurements and atlas data. The observed negative salinity anomalies are reproduced by simulations from a general ocean circulation model. Submarine iron sources reaching the euphotic layer may impact nitrogen fixation across the whole region.Cécile GuieuSophie BonnetAnne PetrenkoChristophe MenkesValérie ChavagnacKarine DesboeufsChristophe MaesThierry MoutinNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 8, Iss 1, Pp 1-9 (2018)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Cécile Guieu
Sophie Bonnet
Anne Petrenko
Christophe Menkes
Valérie Chavagnac
Karine Desboeufs
Christophe Maes
Thierry Moutin
Iron from a submarine source impacts the productive layer of the Western Tropical South Pacific (WTSP)
description Abstract In the Western Tropical South Pacific, patches of high chlorophyll concentrations linked to the occurrence of N2-fixing organisms are found in the vicinity of volcanic islands. The survival of these organisms relies on a high bioavailable iron supply whose origin and fluxes remain unknown. Here, we measured high dissolved iron (DFe) concentrations (up to 66 nM) in the euphotic layer, extending zonally over 10 degrees longitude (174 E−175 W) at ∼20°S latitude. DFe atmospheric fluxes were at the lower end of reported values of the remote ocean and could not explain the high DFe concentrations measured in the water column in the vicinity of Tonga. We argue that the high DFe concentrations may be sustained by a submarine source, also characterized by freshwater input and recorded as salinity anomalies by Argo float in situ measurements and atlas data. The observed negative salinity anomalies are reproduced by simulations from a general ocean circulation model. Submarine iron sources reaching the euphotic layer may impact nitrogen fixation across the whole region.
format article
author Cécile Guieu
Sophie Bonnet
Anne Petrenko
Christophe Menkes
Valérie Chavagnac
Karine Desboeufs
Christophe Maes
Thierry Moutin
author_facet Cécile Guieu
Sophie Bonnet
Anne Petrenko
Christophe Menkes
Valérie Chavagnac
Karine Desboeufs
Christophe Maes
Thierry Moutin
author_sort Cécile Guieu
title Iron from a submarine source impacts the productive layer of the Western Tropical South Pacific (WTSP)
title_short Iron from a submarine source impacts the productive layer of the Western Tropical South Pacific (WTSP)
title_full Iron from a submarine source impacts the productive layer of the Western Tropical South Pacific (WTSP)
title_fullStr Iron from a submarine source impacts the productive layer of the Western Tropical South Pacific (WTSP)
title_full_unstemmed Iron from a submarine source impacts the productive layer of the Western Tropical South Pacific (WTSP)
title_sort iron from a submarine source impacts the productive layer of the western tropical south pacific (wtsp)
publisher Nature Portfolio
publishDate 2018
url https://doaj.org/article/8d047e9d0eda47d29fff4a0cb420ff7a
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