Iron in sea ice: Review and new insights
International audience The discovery that melting sea ice can fertilize iron (Fe)-depleted polar waters has recently fostered trace metal research efforts in sea ice. The aim of this review is to summarize and synthesize the current understanding of Fe biogeochemistry in sea ice. To do so, we compil...
Published in: | Elementa: Science of the Anthropocene |
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Main Authors: | , , , , , , , |
Other Authors: | , , , , , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2016
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Subjects: | |
Online Access: | https://hal.science/hal-01836470 https://doi.org/10.12952/journal.elementa.000130 |
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ftunivnantes:oai:HAL:hal-01836470v1 |
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Open Polar |
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Université de Nantes: HAL-UNIV-NANTES |
op_collection_id |
ftunivnantes |
language |
English |
topic |
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] |
spellingShingle |
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] Lannuzel, Delphine Vancoppenolle, Martin van Der Merwe, Pier de Jong, J. Meiners, Klaus M. Grotti, M. Nishioka, Jun Schoemann, Véronique Iron in sea ice: Review and new insights |
topic_facet |
[PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] |
description |
International audience The discovery that melting sea ice can fertilize iron (Fe)-depleted polar waters has recently fostered trace metal research efforts in sea ice. The aim of this review is to summarize and synthesize the current understanding of Fe biogeochemistry in sea ice. To do so, we compiled available data on particulate, dissolved, and total dissolvable Fe (PFe, DFe and TDFe, respectively) from sea-ice studies from both polar regions and from sub-Arctic and northern Hemisphere temperate areas. Data analysis focused on a circum-Antarctic Fe dataset derived from 61 ice cores collected during 10 field expeditions carried out between 1997 and 2012 in the Southern Ocean. Our key findings are that 1) concentrations of all forms of Fe (PFe, DFe, TDFe) are at least a magnitude larger in fast ice and pack ice than in typical Antarctic surface waters; 2) DFe, PFe and TDFe behave differently when plotted against sea-ice salinity, suggesting that their distributions in sea ice are driven by distinct, spatially and temporally decoupled processes; 3) DFe is actively extracted from seawater into growing sea ice; 4) fast ice generally has more Fe-bearing particles, a finding supported by the significant negative correlation observed between both PFe and TDFe concentrations in sea ice and water depth; 5) the Fe pool in sea ice is coupled to biota, as indicated by the positive correlations of PFe and TDFe with chlorophyll a and particulate organic carbon; and 6) the vast majority of DFe appears to be adsorbed onto something in sea ice. This review also addresses the role of sea ice as a reservoir of Fe and its role in seeding seasonally ice-covered waters. We discuss the pivotal role of organic ligands in controlling DFe concentrations in sea ice and highlight the uncertainties that remain regarding the mechanisms of Fe incorporation in sea ice. |
author2 |
Institute for Marine and Antarctic Studies Hobart (IMAS) University of Tasmania Hobart, Australia (UTAS) Nucleus for European Modeling of the Ocean (NEMO R&D ) Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) Antarctic Climate and Ecosystems Cooperative Research Centre (ACE-CRC) Department of Geosciences, Environment and Society Université libre de Bruxelles (ULB) Department of Chemistry and Industrial Chemistry, Genova University Università degli studi di Genova = University of Genoa (UniGe) Institute of Low Temperature Science Sapporo Hokkaido University Sapporo, Japan SCOR WG 140-BEPSII European Project: 321938,EC:FP7:PEOPLE,FP7-PEOPLE-2012-CIG,BISICLO(2012) |
format |
Article in Journal/Newspaper |
author |
Lannuzel, Delphine Vancoppenolle, Martin van Der Merwe, Pier de Jong, J. Meiners, Klaus M. Grotti, M. Nishioka, Jun Schoemann, Véronique |
author_facet |
Lannuzel, Delphine Vancoppenolle, Martin van Der Merwe, Pier de Jong, J. Meiners, Klaus M. Grotti, M. Nishioka, Jun Schoemann, Véronique |
author_sort |
Lannuzel, Delphine |
title |
Iron in sea ice: Review and new insights |
title_short |
Iron in sea ice: Review and new insights |
title_full |
Iron in sea ice: Review and new insights |
title_fullStr |
Iron in sea ice: Review and new insights |
title_full_unstemmed |
Iron in sea ice: Review and new insights |
title_sort |
iron in sea ice: review and new insights |
publisher |
HAL CCSD |
publishDate |
2016 |
url |
https://hal.science/hal-01836470 https://doi.org/10.12952/journal.elementa.000130 |
geographic |
Antarctic Arctic Southern Ocean |
geographic_facet |
Antarctic Arctic Southern Ocean |
genre |
Antarc* Antarctic Arctic Sea ice Southern Ocean ice covered waters |
genre_facet |
Antarc* Antarctic Arctic Sea ice Southern Ocean ice covered waters |
op_source |
EISSN: 2325-1026 Elementa: Science of the Anthropocene https://hal.science/hal-01836470 Elementa: Science of the Anthropocene, 2016, 4, ⟨10.12952/journal.elementa.000130⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.12952/journal.elementa.000130 info:eu-repo/grantAgreement/EC/FP7/321938/EU/BIogeochemical cycles, Sea Ice and CLimate in the Polar Oceans/BISICLO hal-01836470 https://hal.science/hal-01836470 doi:10.12952/journal.elementa.000130 |
op_doi |
https://doi.org/10.12952/journal.elementa.000130 |
container_title |
Elementa: Science of the Anthropocene |
container_volume |
4 |
_version_ |
1766028480821067776 |
spelling |
ftunivnantes:oai:HAL:hal-01836470v1 2023-05-15T13:32:35+02:00 Iron in sea ice: Review and new insights Lannuzel, Delphine Vancoppenolle, Martin van Der Merwe, Pier de Jong, J. Meiners, Klaus M. Grotti, M. Nishioka, Jun Schoemann, Véronique Institute for Marine and Antarctic Studies Hobart (IMAS) University of Tasmania Hobart, Australia (UTAS) Nucleus for European Modeling of the Ocean (NEMO R&D ) Laboratoire d'Océanographie et du Climat : Expérimentations et Approches Numériques (LOCEAN) Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) École normale supérieure - Paris (ENS-PSL) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-École normale supérieure - Paris (ENS-PSL) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université Paris Diderot - Paris 7 (UPD7)-École polytechnique (X)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) Antarctic Climate and Ecosystems Cooperative Research Centre (ACE-CRC) Department of Geosciences, Environment and Society Université libre de Bruxelles (ULB) Department of Chemistry and Industrial Chemistry, Genova University Università degli studi di Genova = University of Genoa (UniGe) Institute of Low Temperature Science Sapporo Hokkaido University Sapporo, Japan SCOR WG 140-BEPSII European Project: 321938,EC:FP7:PEOPLE,FP7-PEOPLE-2012-CIG,BISICLO(2012) 2016-10-27 https://hal.science/hal-01836470 https://doi.org/10.12952/journal.elementa.000130 en eng HAL CCSD University of California Press info:eu-repo/semantics/altIdentifier/doi/10.12952/journal.elementa.000130 info:eu-repo/grantAgreement/EC/FP7/321938/EU/BIogeochemical cycles, Sea Ice and CLimate in the Polar Oceans/BISICLO hal-01836470 https://hal.science/hal-01836470 doi:10.12952/journal.elementa.000130 EISSN: 2325-1026 Elementa: Science of the Anthropocene https://hal.science/hal-01836470 Elementa: Science of the Anthropocene, 2016, 4, ⟨10.12952/journal.elementa.000130⟩ [PHYS.PHYS.PHYS-GEO-PH]Physics [physics]/Physics [physics]/Geophysics [physics.geo-ph] info:eu-repo/semantics/article Journal articles 2016 ftunivnantes https://doi.org/10.12952/journal.elementa.000130 2023-01-18T01:03:18Z International audience The discovery that melting sea ice can fertilize iron (Fe)-depleted polar waters has recently fostered trace metal research efforts in sea ice. The aim of this review is to summarize and synthesize the current understanding of Fe biogeochemistry in sea ice. To do so, we compiled available data on particulate, dissolved, and total dissolvable Fe (PFe, DFe and TDFe, respectively) from sea-ice studies from both polar regions and from sub-Arctic and northern Hemisphere temperate areas. Data analysis focused on a circum-Antarctic Fe dataset derived from 61 ice cores collected during 10 field expeditions carried out between 1997 and 2012 in the Southern Ocean. Our key findings are that 1) concentrations of all forms of Fe (PFe, DFe, TDFe) are at least a magnitude larger in fast ice and pack ice than in typical Antarctic surface waters; 2) DFe, PFe and TDFe behave differently when plotted against sea-ice salinity, suggesting that their distributions in sea ice are driven by distinct, spatially and temporally decoupled processes; 3) DFe is actively extracted from seawater into growing sea ice; 4) fast ice generally has more Fe-bearing particles, a finding supported by the significant negative correlation observed between both PFe and TDFe concentrations in sea ice and water depth; 5) the Fe pool in sea ice is coupled to biota, as indicated by the positive correlations of PFe and TDFe with chlorophyll a and particulate organic carbon; and 6) the vast majority of DFe appears to be adsorbed onto something in sea ice. This review also addresses the role of sea ice as a reservoir of Fe and its role in seeding seasonally ice-covered waters. We discuss the pivotal role of organic ligands in controlling DFe concentrations in sea ice and highlight the uncertainties that remain regarding the mechanisms of Fe incorporation in sea ice. Article in Journal/Newspaper Antarc* Antarctic Arctic Sea ice Southern Ocean ice covered waters Université de Nantes: HAL-UNIV-NANTES Antarctic Arctic Southern Ocean Elementa: Science of the Anthropocene 4 |