Resupply of mesopelagic dissolved iron controlled by particulate iron composition
International audience The dissolved iron supply controls half of the oceans’ primary productivity. Resupply by the remineralization of sinking particles, and subsequent vertical mixing, largely sustains this productivity. However, our understanding of the drivers of dissolved iron resupply, and the...
Published in: | Nature Geoscience |
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Main Authors: | , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2019
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Subjects: | |
Online Access: | https://hal.science/hal-02366981 https://hal.science/hal-02366981/document https://hal.science/hal-02366981/file/Bressac_et_al_2019_NATgeoscience_preprint.pdf https://doi.org/10.1038/s41561-019-0476-6 |
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English |
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EXPORT ACL POLAR FRONTAL ZONES DUST-DEPOSITION SOUTHERN-OCEAN MEDITERRANEAN SEA SEDIMENT TRAP CARBON SEQUESTRATION REMINERALIZATION BIOGEOCHEMISTRY FLUXES [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDE.BE]Environmental Sciences/Biodiversity and Ecology |
spellingShingle |
EXPORT ACL POLAR FRONTAL ZONES DUST-DEPOSITION SOUTHERN-OCEAN MEDITERRANEAN SEA SEDIMENT TRAP CARBON SEQUESTRATION REMINERALIZATION BIOGEOCHEMISTRY FLUXES [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDE.BE]Environmental Sciences/Biodiversity and Ecology Bressac, M. Guieu, Cécile Ellwood, M. Tagliabue, A. Wagener, T. Laurenceau-Cornec, E. Whitby, H. Sarthou, Géraldine Boyd, P. Resupply of mesopelagic dissolved iron controlled by particulate iron composition |
topic_facet |
EXPORT ACL POLAR FRONTAL ZONES DUST-DEPOSITION SOUTHERN-OCEAN MEDITERRANEAN SEA SEDIMENT TRAP CARBON SEQUESTRATION REMINERALIZATION BIOGEOCHEMISTRY FLUXES [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDE.BE]Environmental Sciences/Biodiversity and Ecology |
description |
International audience The dissolved iron supply controls half of the oceans’ primary productivity. Resupply by the remineralization of sinking particles, and subsequent vertical mixing, largely sustains this productivity. However, our understanding of the drivers of dissolved iron resupply, and their influence on its vertical distribution across the oceans, is still limited due to sparse observations. There is a lack of empirical evidence as to what controls the subsurface iron remineralization due to difficulties in studying mesopelagic biogeochemistry. Here we present estimates of particulate transformations to dissolved iron, concurrent oxygen consumption and iron-binding ligand replenishment based on in situ mesopelagic experiments. Dissolved iron regeneration efficiencies (that is, replenishment over oxygen consumption) were 10- to 100-fold higher in low-dust subantarctic waters relative to higher-dust Mediterranean sites. Regeneration efficiencies are heavily influenced by particle composition. Their make-up dictates ligand release, controls scavenging, modulates ballasting and may lead to the differential remineralization of biogenic versus lithogenic iron. At high-dust sites, these processes together increase the iron remineralization length scale. Modelling reveals that in oceanic regions near deserts, enhanced lithogenic fluxes deepen the ferricline, which alter the vertical patterns of dissolved iron replenishment, and set its redistribution at the global scale. Such wide-ranging regeneration efficiencies drive different vertical patterns in dissolved iron replenishment across oceanic provinces. |
author2 |
Institute for Marine and Antarctic Studies Hobart (IMAS) University of Tasmania Hobart, Australia (UTAS) Laboratoire d'océanographie de Villefranche (LOV) Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut de la Mer de Villefranche (IMEV) Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) Australian National University (ANU) Department of Earth Ocean and Ecological Sciences Liverpool University of Liverpool Institut méditerranéen d'océanologie (MIO) Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS) Laboratoire des Sciences de l'Environnement Marin (LEMAR) (LEMAR) Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Institut Universitaire Européen de la Mer (IUEM) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Antarctic Climate and Ecosystems Cooperative Research Centre (ACE-CRC) European Project: 626734,EC:FP7:PEOPLE,FP7-PEOPLE-2013-IOF,IRON-IC(2014) |
format |
Article in Journal/Newspaper |
author |
Bressac, M. Guieu, Cécile Ellwood, M. Tagliabue, A. Wagener, T. Laurenceau-Cornec, E. Whitby, H. Sarthou, Géraldine Boyd, P. |
author_facet |
Bressac, M. Guieu, Cécile Ellwood, M. Tagliabue, A. Wagener, T. Laurenceau-Cornec, E. Whitby, H. Sarthou, Géraldine Boyd, P. |
author_sort |
Bressac, M. |
title |
Resupply of mesopelagic dissolved iron controlled by particulate iron composition |
title_short |
Resupply of mesopelagic dissolved iron controlled by particulate iron composition |
title_full |
Resupply of mesopelagic dissolved iron controlled by particulate iron composition |
title_fullStr |
Resupply of mesopelagic dissolved iron controlled by particulate iron composition |
title_full_unstemmed |
Resupply of mesopelagic dissolved iron controlled by particulate iron composition |
title_sort |
resupply of mesopelagic dissolved iron controlled by particulate iron composition |
publisher |
HAL CCSD |
publishDate |
2019 |
url |
https://hal.science/hal-02366981 https://hal.science/hal-02366981/document https://hal.science/hal-02366981/file/Bressac_et_al_2019_NATgeoscience_preprint.pdf https://doi.org/10.1038/s41561-019-0476-6 |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_source |
ISSN: 1752-0894 Nature Geoscience https://hal.science/hal-02366981 Nature Geoscience, 2019, 12 (12), pp.995-1003. ⟨10.1038/s41561-019-0476-6⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1038/s41561-019-0476-6 info:eu-repo/grantAgreement/EC/FP7/626734/EU/Implications of the mesopelagic Remineralization for the OceaN Iron Cycle/IRON-IC hal-02366981 https://hal.science/hal-02366981 https://hal.science/hal-02366981/document https://hal.science/hal-02366981/file/Bressac_et_al_2019_NATgeoscience_preprint.pdf doi:10.1038/s41561-019-0476-6 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1038/s41561-019-0476-6 |
container_title |
Nature Geoscience |
container_volume |
12 |
container_issue |
12 |
container_start_page |
995 |
op_container_end_page |
1000 |
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1810481664620494848 |
spelling |
ftunivtoulon:oai:HAL:hal-02366981v1 2024-09-15T18:37:18+00:00 Resupply of mesopelagic dissolved iron controlled by particulate iron composition Bressac, M. Guieu, Cécile Ellwood, M. Tagliabue, A. Wagener, T. Laurenceau-Cornec, E. Whitby, H. Sarthou, Géraldine Boyd, P. Institute for Marine and Antarctic Studies Hobart (IMAS) University of Tasmania Hobart, Australia (UTAS) Laboratoire d'océanographie de Villefranche (LOV) Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut de la Mer de Villefranche (IMEV) Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) Australian National University (ANU) Department of Earth Ocean and Ecological Sciences Liverpool University of Liverpool Institut méditerranéen d'océanologie (MIO) Institut de Recherche pour le Développement (IRD)-Aix Marseille Université (AMU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Toulon (UTLN)-Centre National de la Recherche Scientifique (CNRS) Laboratoire des Sciences de l'Environnement Marin (LEMAR) (LEMAR) Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Université de Brest (UBO)-Institut Universitaire Européen de la Mer (IUEM) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Antarctic Climate and Ecosystems Cooperative Research Centre (ACE-CRC) European Project: 626734,EC:FP7:PEOPLE,FP7-PEOPLE-2013-IOF,IRON-IC(2014) 2019-12 https://hal.science/hal-02366981 https://hal.science/hal-02366981/document https://hal.science/hal-02366981/file/Bressac_et_al_2019_NATgeoscience_preprint.pdf https://doi.org/10.1038/s41561-019-0476-6 en eng HAL CCSD Nature Publishing Group info:eu-repo/semantics/altIdentifier/doi/10.1038/s41561-019-0476-6 info:eu-repo/grantAgreement/EC/FP7/626734/EU/Implications of the mesopelagic Remineralization for the OceaN Iron Cycle/IRON-IC hal-02366981 https://hal.science/hal-02366981 https://hal.science/hal-02366981/document https://hal.science/hal-02366981/file/Bressac_et_al_2019_NATgeoscience_preprint.pdf doi:10.1038/s41561-019-0476-6 info:eu-repo/semantics/OpenAccess ISSN: 1752-0894 Nature Geoscience https://hal.science/hal-02366981 Nature Geoscience, 2019, 12 (12), pp.995-1003. ⟨10.1038/s41561-019-0476-6⟩ EXPORT ACL POLAR FRONTAL ZONES DUST-DEPOSITION SOUTHERN-OCEAN MEDITERRANEAN SEA SEDIMENT TRAP CARBON SEQUESTRATION REMINERALIZATION BIOGEOCHEMISTRY FLUXES [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDE.BE]Environmental Sciences/Biodiversity and Ecology info:eu-repo/semantics/article Journal articles 2019 ftunivtoulon https://doi.org/10.1038/s41561-019-0476-6 2024-08-12T23:37:03Z International audience The dissolved iron supply controls half of the oceans’ primary productivity. Resupply by the remineralization of sinking particles, and subsequent vertical mixing, largely sustains this productivity. However, our understanding of the drivers of dissolved iron resupply, and their influence on its vertical distribution across the oceans, is still limited due to sparse observations. There is a lack of empirical evidence as to what controls the subsurface iron remineralization due to difficulties in studying mesopelagic biogeochemistry. Here we present estimates of particulate transformations to dissolved iron, concurrent oxygen consumption and iron-binding ligand replenishment based on in situ mesopelagic experiments. Dissolved iron regeneration efficiencies (that is, replenishment over oxygen consumption) were 10- to 100-fold higher in low-dust subantarctic waters relative to higher-dust Mediterranean sites. Regeneration efficiencies are heavily influenced by particle composition. Their make-up dictates ligand release, controls scavenging, modulates ballasting and may lead to the differential remineralization of biogenic versus lithogenic iron. At high-dust sites, these processes together increase the iron remineralization length scale. Modelling reveals that in oceanic regions near deserts, enhanced lithogenic fluxes deepen the ferricline, which alter the vertical patterns of dissolved iron replenishment, and set its redistribution at the global scale. Such wide-ranging regeneration efficiencies drive different vertical patterns in dissolved iron replenishment across oceanic provinces. Article in Journal/Newspaper Southern Ocean Université de Toulon: HAL Nature Geoscience 12 12 995 1000 |