Rare earth elements in the North Atlantic, part I: Non-conservative behavior reveals margin inputs and deep waters scavenging

International audience Dissolved concentrations of 14 Rare Earth Elements (dREE) were measured in seawater samples collected during the GEOVIDE cruise (GEOTRACES GA01, May-June 2014) in the North Atlantic. This is the first dREE dataset produced using the manually operated self-built preconcentratio...

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Published in:Chemical Geology
Main Authors: Lagarde, Marion, Pham, Viet, Quoc, Lherminier, Pascale, Belhadj, Moustafa, Jeandel, Catherine
Other Authors: Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS), Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP), Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS), 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)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-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)-École polytechnique (X), Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-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)-École polytechnique (X), Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)), Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Institute of Environmental Technology Hanoi (IET), Vietnam Academy of Science and Technology (VAST), This research has been supported by the French National Research Agency (grant ANR-13-BS06-0014, ANR-12-PDOC-0025-01), the French National Centre for Scientific Research (grant CNRS-LEFE-CYBER), the LabexMER (grant ANR-10-LABX-19), and Ifremer. It was supported in the logistics by DT-INSU and GENAVIR. The International GEOTRACES Programme is possible in part thanks to the support from the U.S. National Science Foundation (Grant OCE-2140395) to the Scientific Committee on Oceanic Research (SCOR)., ANR-17-EURE-0015,ISBlue,Interdisciplinary Graduate School for the Blue planet(2017)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2024
Subjects:
Online Access:https://hal.univ-brest.fr/hal-04690693
https://hal.univ-brest.fr/hal-04690693v1/document
https://hal.univ-brest.fr/hal-04690693v1/file/1-s2.0-S0009254124003103-main.pdf
https://doi.org/10.1016/j.chemgeo.2024.122230
id ftuniparissaclay:oai:HAL:hal-04690693v1
record_format openpolar
institution Open Polar
collection Archives ouvertes de Paris-Saclay
op_collection_id ftuniparissaclay
language English
topic Boundary exchange
dREE
GEOTRACES
GEOVIDE
Iberian margin
Margin inputs
Nepheloid layers
Non-conservative behavior
[SDE]Environmental Sciences
spellingShingle Boundary exchange
dREE
GEOTRACES
GEOVIDE
Iberian margin
Margin inputs
Nepheloid layers
Non-conservative behavior
[SDE]Environmental Sciences
Lagarde, Marion
Pham, Viet, Quoc
Lherminier, Pascale
Belhadj, Moustafa
Jeandel, Catherine
Rare earth elements in the North Atlantic, part I: Non-conservative behavior reveals margin inputs and deep waters scavenging
topic_facet Boundary exchange
dREE
GEOTRACES
GEOVIDE
Iberian margin
Margin inputs
Nepheloid layers
Non-conservative behavior
[SDE]Environmental Sciences
description International audience Dissolved concentrations of 14 Rare Earth Elements (dREE) were measured in seawater samples collected during the GEOVIDE cruise (GEOTRACES GA01, May-June 2014) in the North Atlantic. This is the first dREE dataset produced using the manually operated self-built preconcentration system, made of eight columns of Nobias chelate PA-1® resin (Hitachi High-Technologies) in parallel. Concentration profiles differ from the typical "nutrient-like" dREE vertical distributions. Instead, we observe surface enrichment, especially close to the Iberian margin, and constant or decreasing concentrations below 500 m. An extended Optimum Multiparameter Analysis applied to the GEOVIDE section allowed disentangling the conservative signal brought by water masses from the non-conservative signal produced by inputs or subtractions along the water pathways. Results show i) strong dissolved inputs from the Iberian margin from resuspended particle dissolution, ii) that surprisingly, rather than mixing, scavenging in deep water masses is responsible for the decreasing concentrations at depth, especially in the lower North East Atlantic Deep Water and the Iceland Scotland Overflow Water, and iii) that in the Irminger and Labrador Seas, biological uptake is compensated by external inputs. The combination of lithogenic inputs from the Iberian margin, due to partial dissolution, with scavenging in deep water masses supports that mechanisms occurring at the land-ocean interface explain part of the observations of boundary exchange.
author2 Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS)
Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP)
Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS)
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)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-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)-École polytechnique (X)
Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-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)-École polytechnique (X)
Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636))
Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)
Institute of Environmental Technology Hanoi (IET)
Vietnam Academy of Science and Technology (VAST)
This research has been supported by the French National Research Agency (grant ANR-13-BS06-0014, ANR-12-PDOC-0025-01), the French National Centre for Scientific Research (grant CNRS-LEFE-CYBER), the LabexMER (grant ANR-10-LABX-19), and Ifremer. It was supported in the logistics by DT-INSU and GENAVIR. The International GEOTRACES Programme is possible in part thanks to the support from the U.S. National Science Foundation (Grant OCE-2140395) to the Scientific Committee on Oceanic Research (SCOR).
ANR-17-EURE-0015,ISBlue,Interdisciplinary Graduate School for the Blue planet(2017)
format Article in Journal/Newspaper
author Lagarde, Marion
Pham, Viet, Quoc
Lherminier, Pascale
Belhadj, Moustafa
Jeandel, Catherine
author_facet Lagarde, Marion
Pham, Viet, Quoc
Lherminier, Pascale
Belhadj, Moustafa
Jeandel, Catherine
author_sort Lagarde, Marion
title Rare earth elements in the North Atlantic, part I: Non-conservative behavior reveals margin inputs and deep waters scavenging
title_short Rare earth elements in the North Atlantic, part I: Non-conservative behavior reveals margin inputs and deep waters scavenging
title_full Rare earth elements in the North Atlantic, part I: Non-conservative behavior reveals margin inputs and deep waters scavenging
title_fullStr Rare earth elements in the North Atlantic, part I: Non-conservative behavior reveals margin inputs and deep waters scavenging
title_full_unstemmed Rare earth elements in the North Atlantic, part I: Non-conservative behavior reveals margin inputs and deep waters scavenging
title_sort rare earth elements in the north atlantic, part i: non-conservative behavior reveals margin inputs and deep waters scavenging
publisher HAL CCSD
publishDate 2024
url https://hal.univ-brest.fr/hal-04690693
https://hal.univ-brest.fr/hal-04690693v1/document
https://hal.univ-brest.fr/hal-04690693v1/file/1-s2.0-S0009254124003103-main.pdf
https://doi.org/10.1016/j.chemgeo.2024.122230
genre Iceland
North Atlantic
North East Atlantic
genre_facet Iceland
North Atlantic
North East Atlantic
op_source ISSN: 0009-2541
Chemical Geology
https://hal.univ-brest.fr/hal-04690693
Chemical Geology, 2024, 664, ⟨10.1016/j.chemgeo.2024.122230⟩
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hal-04690693
https://hal.univ-brest.fr/hal-04690693
https://hal.univ-brest.fr/hal-04690693v1/document
https://hal.univ-brest.fr/hal-04690693v1/file/1-s2.0-S0009254124003103-main.pdf
doi:10.1016/j.chemgeo.2024.122230
op_rights info:eu-repo/semantics/OpenAccess
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container_title Chemical Geology
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spelling ftuniparissaclay:oai:HAL:hal-04690693v1 2024-10-20T14:09:44+00:00 Rare earth elements in the North Atlantic, part I: Non-conservative behavior reveals margin inputs and deep waters scavenging Lagarde, Marion Pham, Viet, Quoc Lherminier, Pascale Belhadj, Moustafa Jeandel, Catherine Laboratoire d'études en Géophysique et océanographie spatiales (LEGOS) Institut de Recherche pour le Développement (IRD)-Université Toulouse III - Paul Sabatier (UT3) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Observatoire Midi-Pyrénées (OMP) Université de Toulouse (UT)-Université de Toulouse (UT)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National d'Études Spatiales Toulouse (CNES)-Centre National de la Recherche Scientifique (CNRS)-Météo-France-Centre National de la Recherche Scientifique (CNRS) 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)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-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)-École polytechnique (X) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-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)-École polytechnique (X) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité)-Muséum national d'Histoire naturelle (MNHN)-Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Institut Pierre-Simon-Laplace (IPSL (FR_636)) Institut Polytechnique de Paris (IP Paris)-Institut Polytechnique de Paris (IP Paris)-Centre National d'Études Spatiales Toulouse (CNES)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité) Institute of Environmental Technology Hanoi (IET) Vietnam Academy of Science and Technology (VAST) This research has been supported by the French National Research Agency (grant ANR-13-BS06-0014, ANR-12-PDOC-0025-01), the French National Centre for Scientific Research (grant CNRS-LEFE-CYBER), the LabexMER (grant ANR-10-LABX-19), and Ifremer. It was supported in the logistics by DT-INSU and GENAVIR. The International GEOTRACES Programme is possible in part thanks to the support from the U.S. National Science Foundation (Grant OCE-2140395) to the Scientific Committee on Oceanic Research (SCOR). ANR-17-EURE-0015,ISBlue,Interdisciplinary Graduate School for the Blue planet(2017) 2024-06-16 https://hal.univ-brest.fr/hal-04690693 https://hal.univ-brest.fr/hal-04690693v1/document https://hal.univ-brest.fr/hal-04690693v1/file/1-s2.0-S0009254124003103-main.pdf https://doi.org/10.1016/j.chemgeo.2024.122230 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.chemgeo.2024.122230 hal-04690693 https://hal.univ-brest.fr/hal-04690693 https://hal.univ-brest.fr/hal-04690693v1/document https://hal.univ-brest.fr/hal-04690693v1/file/1-s2.0-S0009254124003103-main.pdf doi:10.1016/j.chemgeo.2024.122230 info:eu-repo/semantics/OpenAccess ISSN: 0009-2541 Chemical Geology https://hal.univ-brest.fr/hal-04690693 Chemical Geology, 2024, 664, ⟨10.1016/j.chemgeo.2024.122230⟩ Boundary exchange dREE GEOTRACES GEOVIDE Iberian margin Margin inputs Nepheloid layers Non-conservative behavior [SDE]Environmental Sciences info:eu-repo/semantics/article Journal articles 2024 ftuniparissaclay https://doi.org/10.1016/j.chemgeo.2024.122230 2024-09-20T00:21:16Z International audience Dissolved concentrations of 14 Rare Earth Elements (dREE) were measured in seawater samples collected during the GEOVIDE cruise (GEOTRACES GA01, May-June 2014) in the North Atlantic. This is the first dREE dataset produced using the manually operated self-built preconcentration system, made of eight columns of Nobias chelate PA-1® resin (Hitachi High-Technologies) in parallel. Concentration profiles differ from the typical "nutrient-like" dREE vertical distributions. Instead, we observe surface enrichment, especially close to the Iberian margin, and constant or decreasing concentrations below 500 m. An extended Optimum Multiparameter Analysis applied to the GEOVIDE section allowed disentangling the conservative signal brought by water masses from the non-conservative signal produced by inputs or subtractions along the water pathways. Results show i) strong dissolved inputs from the Iberian margin from resuspended particle dissolution, ii) that surprisingly, rather than mixing, scavenging in deep water masses is responsible for the decreasing concentrations at depth, especially in the lower North East Atlantic Deep Water and the Iceland Scotland Overflow Water, and iii) that in the Irminger and Labrador Seas, biological uptake is compensated by external inputs. The combination of lithogenic inputs from the Iberian margin, due to partial dissolution, with scavenging in deep water masses supports that mechanisms occurring at the land-ocean interface explain part of the observations of boundary exchange. Article in Journal/Newspaper Iceland North Atlantic North East Atlantic Archives ouvertes de Paris-Saclay Chemical Geology 664 122230