Iron fertilization enhanced net community production but not downward particle flux during the Southern Ocean iron fertilization experiment LOHAFEX

International audience A closed eddy core in the Subantarctic Atlantic Ocean was fertilized twice with two tons of iron (as FeSO4), and the 300 km2 fertilized patch was studied for 39 days to test whether fertilization enhances downward particle flux into the deep ocean. Chlorophyll a and primary pr...

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Published in:Global Biogeochemical Cycles
Main Authors: Martin, Patrick, van Der Loeff, Michiel M. Rutgers, Cassar, Nicolas, Vandromme, Pieter, d'Ovidio, Francesco, Stemmann, Lars, Rengarajan, R., Soares, Melena, González, Humberto, E., Ebersbach, Friederike, E, Lampitt, Richard S., Sanders, Richard, Barnett, Bruce A., Smetacek, Victor, Naqvi, S. Wajih A.
Other Authors: Earth Observatory of Singapore (EOS), Nanyang Technological University Singapour, National Oceanography Centre Southampton (NOC), University of Southampton, Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung = Alfred Wegener Institute for Polar and Marine Research = Institut Alfred-Wegener pour la recherche polaire et marine (AWI), Helmholtz-Gemeinschaft = Helmholtz Association, Division of Earth and Ocean Sciences, Duke University Durham, Laboratoire d'océanographie de Villefranche (LOV), Observatoire océanologique de Villefranche-sur-mer (OOVM), Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS), Processus de couplage à Petite Echelle, Ecosystèmes et Prédateurs Supérieurs (PEPS), 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), Physical Research Laboratory Ahmedabad (PRL), Indian Space Research Organisation (ISRO), CSIR National Institute of Oceanography India (NIO), Instituto de Ciencias Marinas y Limnológicas, Universidad Austral de Chile
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2013
Subjects:
Online Access:https://hal.science/hal-01445819
https://hal.science/hal-01445819/document
https://hal.science/hal-01445819/file/Martin_et_al-2013-Global_Biogeochemical_Cycles.pdf
https://doi.org/10.1002/gbc.20077
id ftmuseumnhn:oai:HAL:hal-01445819v1
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institution Open Polar
collection Muséum National d'Histoire Naturelle (MNHM): HAL
op_collection_id ftmuseumnhn
language English
topic [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[SDE.BE]Environmental Sciences/Biodiversity and Ecology
[SDE.IE]Environmental Sciences/Environmental Engineering
spellingShingle [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[SDE.BE]Environmental Sciences/Biodiversity and Ecology
[SDE.IE]Environmental Sciences/Environmental Engineering
Martin, Patrick
van Der Loeff, Michiel M. Rutgers
Cassar, Nicolas
Vandromme, Pieter
d'Ovidio, Francesco
Stemmann, Lars
Rengarajan, R.
Soares, Melena
González, Humberto, E.
Ebersbach, Friederike, E
Lampitt, Richard S.
Sanders, Richard
Barnett, Bruce A.
Smetacek, Victor
Naqvi, S. Wajih A.
Iron fertilization enhanced net community production but not downward particle flux during the Southern Ocean iron fertilization experiment LOHAFEX
topic_facet [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography
[SDE.BE]Environmental Sciences/Biodiversity and Ecology
[SDE.IE]Environmental Sciences/Environmental Engineering
description International audience A closed eddy core in the Subantarctic Atlantic Ocean was fertilized twice with two tons of iron (as FeSO4), and the 300 km2 fertilized patch was studied for 39 days to test whether fertilization enhances downward particle flux into the deep ocean. Chlorophyll a and primary productivity doubled after fertilization, and photosynthetic quantum yield (FV/FM) increased from 0.33 to ≥0.40. Silicic acid (<2 µmol L −1 ) limited diatoms, which contributed <10% of phytoplankton biomass. Copepods exerted high grazing pressure. This is the first study of particle flux out of an artificially fertilized bloom with very low diatom biomass. Net community production (NCP) inside the patch, estimated from O2:Ar ratios, averaged 21 mmol POC m−2 d−1, probably ±20%. 234 Th profiles implied constant export of ~6.3 mmol POC m −2 d −1 in the patch, similar to unfertilized waters. The difference between NCP and 234 Th-derived export partly accumulated in the mixed layer and was partly remineralized between the mixed layer and 100 m. Neutrally buoyant sediment traps at 200 and 450 m inside and outside the patch caught mostly <1.1 mmol POC m −2 d −1 , predominantly of fecal origin; flux did not increase upon fertilization. Our data thus indicate intense flux attenuation between 100 and 200 m, and probably between the mixed layer and 100 m. We attribute the lack of fertilization-induced export to silicon limitation of diatoms and reprocessing of sinking particles by detritus feeders. Our data are consistent with the view that nitrate-rich but silicate-deficient waters are not poised for enhanced particle export upon iron addition.
author2 Earth Observatory of Singapore (EOS)
Nanyang Technological University Singapour
National Oceanography Centre Southampton (NOC)
University of Southampton
Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung = Alfred Wegener Institute for Polar and Marine Research = Institut Alfred-Wegener pour la recherche polaire et marine (AWI)
Helmholtz-Gemeinschaft = Helmholtz Association
Division of Earth and Ocean Sciences
Duke University Durham
Laboratoire d'océanographie de Villefranche (LOV)
Observatoire océanologique de Villefranche-sur-mer (OOVM)
Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)
Processus de couplage à Petite Echelle, Ecosystèmes et Prédateurs Supérieurs (PEPS)
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)
Physical Research Laboratory Ahmedabad (PRL)
Indian Space Research Organisation (ISRO)
CSIR National Institute of Oceanography India (NIO)
Instituto de Ciencias Marinas y Limnológicas
Universidad Austral de Chile
format Article in Journal/Newspaper
author Martin, Patrick
van Der Loeff, Michiel M. Rutgers
Cassar, Nicolas
Vandromme, Pieter
d'Ovidio, Francesco
Stemmann, Lars
Rengarajan, R.
Soares, Melena
González, Humberto, E.
Ebersbach, Friederike, E
Lampitt, Richard S.
Sanders, Richard
Barnett, Bruce A.
Smetacek, Victor
Naqvi, S. Wajih A.
author_facet Martin, Patrick
van Der Loeff, Michiel M. Rutgers
Cassar, Nicolas
Vandromme, Pieter
d'Ovidio, Francesco
Stemmann, Lars
Rengarajan, R.
Soares, Melena
González, Humberto, E.
Ebersbach, Friederike, E
Lampitt, Richard S.
Sanders, Richard
Barnett, Bruce A.
Smetacek, Victor
Naqvi, S. Wajih A.
author_sort Martin, Patrick
title Iron fertilization enhanced net community production but not downward particle flux during the Southern Ocean iron fertilization experiment LOHAFEX
title_short Iron fertilization enhanced net community production but not downward particle flux during the Southern Ocean iron fertilization experiment LOHAFEX
title_full Iron fertilization enhanced net community production but not downward particle flux during the Southern Ocean iron fertilization experiment LOHAFEX
title_fullStr Iron fertilization enhanced net community production but not downward particle flux during the Southern Ocean iron fertilization experiment LOHAFEX
title_full_unstemmed Iron fertilization enhanced net community production but not downward particle flux during the Southern Ocean iron fertilization experiment LOHAFEX
title_sort iron fertilization enhanced net community production but not downward particle flux during the southern ocean iron fertilization experiment lohafex
publisher HAL CCSD
publishDate 2013
url https://hal.science/hal-01445819
https://hal.science/hal-01445819/document
https://hal.science/hal-01445819/file/Martin_et_al-2013-Global_Biogeochemical_Cycles.pdf
https://doi.org/10.1002/gbc.20077
genre Southern Ocean
Copepods
genre_facet Southern Ocean
Copepods
op_source ISSN: 0886-6236
EISSN: 1944-8224
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spelling ftmuseumnhn:oai:HAL:hal-01445819v1 2024-05-19T07:48:59+00:00 Iron fertilization enhanced net community production but not downward particle flux during the Southern Ocean iron fertilization experiment LOHAFEX Martin, Patrick van Der Loeff, Michiel M. Rutgers Cassar, Nicolas Vandromme, Pieter d'Ovidio, Francesco Stemmann, Lars Rengarajan, R. Soares, Melena González, Humberto, E. Ebersbach, Friederike, E Lampitt, Richard S. Sanders, Richard Barnett, Bruce A. Smetacek, Victor Naqvi, S. Wajih A. Earth Observatory of Singapore (EOS) Nanyang Technological University Singapour National Oceanography Centre Southampton (NOC) University of Southampton Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung = Alfred Wegener Institute for Polar and Marine Research = Institut Alfred-Wegener pour la recherche polaire et marine (AWI) Helmholtz-Gemeinschaft = Helmholtz Association Division of Earth and Ocean Sciences Duke University Durham Laboratoire d'océanographie de Villefranche (LOV) Observatoire océanologique de Villefranche-sur-mer (OOVM) Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Pierre et Marie Curie - Paris 6 (UPMC)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) Processus de couplage à Petite Echelle, Ecosystèmes et Prédateurs Supérieurs (PEPS) 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) Physical Research Laboratory Ahmedabad (PRL) Indian Space Research Organisation (ISRO) CSIR National Institute of Oceanography India (NIO) Instituto de Ciencias Marinas y Limnológicas Universidad Austral de Chile 2013 https://hal.science/hal-01445819 https://hal.science/hal-01445819/document https://hal.science/hal-01445819/file/Martin_et_al-2013-Global_Biogeochemical_Cycles.pdf https://doi.org/10.1002/gbc.20077 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1002/gbc.20077 hal-01445819 https://hal.science/hal-01445819 https://hal.science/hal-01445819/document https://hal.science/hal-01445819/file/Martin_et_al-2013-Global_Biogeochemical_Cycles.pdf doi:10.1002/gbc.20077 info:eu-repo/semantics/OpenAccess ISSN: 0886-6236 EISSN: 1944-8224 Global Biogeochemical Cycles https://hal.science/hal-01445819 Global Biogeochemical Cycles, 2013, 27, pp.871-881. &#x27E8;10.1002/gbc.20077&#x27E9; [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography [SDE.BE]Environmental Sciences/Biodiversity and Ecology [SDE.IE]Environmental Sciences/Environmental Engineering info:eu-repo/semantics/article Journal articles 2013 ftmuseumnhn https://doi.org/10.1002/gbc.20077 2024-04-25T00:54:19Z International audience A closed eddy core in the Subantarctic Atlantic Ocean was fertilized twice with two tons of iron (as FeSO4), and the 300 km2 fertilized patch was studied for 39 days to test whether fertilization enhances downward particle flux into the deep ocean. Chlorophyll a and primary productivity doubled after fertilization, and photosynthetic quantum yield (FV/FM) increased from 0.33 to ≥0.40. Silicic acid (<2 µmol L −1 ) limited diatoms, which contributed <10% of phytoplankton biomass. Copepods exerted high grazing pressure. This is the first study of particle flux out of an artificially fertilized bloom with very low diatom biomass. Net community production (NCP) inside the patch, estimated from O2:Ar ratios, averaged 21 mmol POC m−2 d−1, probably ±20%. 234 Th profiles implied constant export of ~6.3 mmol POC m −2 d −1 in the patch, similar to unfertilized waters. The difference between NCP and 234 Th-derived export partly accumulated in the mixed layer and was partly remineralized between the mixed layer and 100 m. Neutrally buoyant sediment traps at 200 and 450 m inside and outside the patch caught mostly <1.1 mmol POC m −2 d −1 , predominantly of fecal origin; flux did not increase upon fertilization. Our data thus indicate intense flux attenuation between 100 and 200 m, and probably between the mixed layer and 100 m. We attribute the lack of fertilization-induced export to silicon limitation of diatoms and reprocessing of sinking particles by detritus feeders. Our data are consistent with the view that nitrate-rich but silicate-deficient waters are not poised for enhanced particle export upon iron addition. Article in Journal/Newspaper Southern Ocean Copepods Muséum National d'Histoire Naturelle (MNHM): HAL Global Biogeochemical Cycles 27 3 871 881