Dissolved iron in the North Atlantic Ocean and Labrador Sea along the GEOVIDE section (GEOTRACES section GA01)
Publisher's version (útgefin grein) Dissolved Fe (DFe) samples from the GEOVIDE voyage (GEOTRACES GA01, May-June 2014) in the North Atlantic Ocean were analyzed using a seaFAST-pico™ coupled to an Element XR sector field inductively coupled plasma mass spectrometer (SF-ICP-MS) and provided inte...
Published in: | Biogeosciences |
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Language: | English |
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2020
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Online Access: | https://hdl.handle.net/20.500.11815/2413 https://doi.org/10.5194/bg-17-917-2020 |
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ftopinvisindi:oai:opinvisindi.is:20.500.11815/2413 2023-05-15T16:00:40+02:00 Dissolved iron in the North Atlantic Ocean and Labrador Sea along the GEOVIDE section (GEOTRACES section GA01) Tonnard, Manon Planquette, Hélène Bowie, Andrew R. van der Merwe, Pier Gallinari, Morgane Desprez de Gésincourt, Floriane Germain, Yoan Gourain, Arthur Benetti, Marion Reverdin, Gilles Tréguer, Paul Boutorh, Julia Cheize, Marie Lacan, François Menzel Barraqueta, Jan-Lukas Pereira-Contreira, Leonardo Shelley, Rachel Lherminier, Pascale Sarthou, Géraldine Jarðvísindastofnun (HÍ) Institute of Earth Sciences (UI) Verkfræði- og náttúruvísindasvið (HÍ) School of Engineering and Natural Sciences (UI) Háskóli Íslands University of Iceland 2020-02-21 917-943 https://hdl.handle.net/20.500.11815/2413 https://doi.org/10.5194/bg-17-917-2020 en eng Copernicus GmbH Biogeosciences;17(4) https://bg.copernicus.org/articles/17/917/2020/bg-17-917-2020.pdf Tonnard, M., Planquette, H., Bowie, A. R., van der Merwe, P., Gallinari, M., Desprez de Gésincourt, F., Germain, Y., Gourain, A., Benetti, M., Reverdin, G., Tréguer, P., Boutorh, J., Cheize, M., Lacan, F., Menzel Barraqueta, J.-L., Pereira-Contreira, L., Shelley, R., Lherminier, P., and Sarthou, G.: Dissolved iron in the North Atlantic Ocean and Labrador Sea along the GEOVIDE section (GEOTRACES section GA01), Biogeosciences, 17, 917–943, https://doi.org/10.5194/bg-17-917-2020, 2020. 1726-4189 https://hdl.handle.net/20.500.11815/2413 Biogeosciences doi:10.5194/bg-17-917-2020 info:eu-repo/semantics/openAccess GEOVIDE voyage North Atlantic Ocean Norður-Atlantshaf info:eu-repo/semantics/article 2020 ftopinvisindi https://doi.org/20.500.11815/2413 https://doi.org/10.5194/bg-17-917-2020 2022-11-18T06:52:06Z Publisher's version (útgefin grein) Dissolved Fe (DFe) samples from the GEOVIDE voyage (GEOTRACES GA01, May-June 2014) in the North Atlantic Ocean were analyzed using a seaFAST-pico™ coupled to an Element XR sector field inductively coupled plasma mass spectrometer (SF-ICP-MS) and provided interesting insights into the Fe sources in this area. Overall, DFe concentrations ranged from 0:09 ± 0:01 to 7:8 ± 0:5 nmol L-1. Elevated DFe concentrations were observed above the Iberian, Greenland, and Newfoundland margins likely due to riverine inputs from the Tagus River, meteoric water inputs, and sedimentary inputs. Deep winter convection occurring the previous winter provided iron-to-nitrate ratios sufficient to sustain phytoplankton growth and lead to relatively elevated DFe concentrations within subsurface waters of the Irminger Sea. Increasing DFe concentrations along the flow path of the Labrador Sea Water were attributed to sedimentary inputs from the Newfoundland Margin. Bottom waters from the Irminger Sea displayed high DFe concentrations likely due to the dissolution of Fe-rich particles in the Denmark Strait Overflow Water and the Polar Intermediate Water. Finally, the nepheloid layers located in the different basins and at the Iberian Margin were found to act as either a source or a sink of DFe depending on the nature of particles, with organic particles likely releasing DFe and Mn particle scavenging DFe. This research has been supported by the French National Research Agency ANR GEOVIDE (grant no. ANR-13-BS06-0014), the RPDOC BITMAP (grant no. ANR-12-PDOC-0025-01), the French National Center for Scientific Research (grant no. CNRS-LEFE-CYBER), the LabexMER (grant no. ANR-10-LABX-19), and Ifremer (Institut français de recherche pour l'exploitation de la mer). Peer Reviewed Article in Journal/Newspaper Denmark Strait Greenland Labrador Sea Newfoundland North Atlantic Opin vísindi (Iceland) Greenland Irminger Sea ENVELOPE(-34.041,-34.041,63.054,63.054) Newfoundland Biogeosciences 17 4 917 943 |
institution |
Open Polar |
collection |
Opin vísindi (Iceland) |
op_collection_id |
ftopinvisindi |
language |
English |
topic |
GEOVIDE voyage North Atlantic Ocean Norður-Atlantshaf |
spellingShingle |
GEOVIDE voyage North Atlantic Ocean Norður-Atlantshaf Tonnard, Manon Planquette, Hélène Bowie, Andrew R. van der Merwe, Pier Gallinari, Morgane Desprez de Gésincourt, Floriane Germain, Yoan Gourain, Arthur Benetti, Marion Reverdin, Gilles Tréguer, Paul Boutorh, Julia Cheize, Marie Lacan, François Menzel Barraqueta, Jan-Lukas Pereira-Contreira, Leonardo Shelley, Rachel Lherminier, Pascale Sarthou, Géraldine Dissolved iron in the North Atlantic Ocean and Labrador Sea along the GEOVIDE section (GEOTRACES section GA01) |
topic_facet |
GEOVIDE voyage North Atlantic Ocean Norður-Atlantshaf |
description |
Publisher's version (útgefin grein) Dissolved Fe (DFe) samples from the GEOVIDE voyage (GEOTRACES GA01, May-June 2014) in the North Atlantic Ocean were analyzed using a seaFAST-pico™ coupled to an Element XR sector field inductively coupled plasma mass spectrometer (SF-ICP-MS) and provided interesting insights into the Fe sources in this area. Overall, DFe concentrations ranged from 0:09 ± 0:01 to 7:8 ± 0:5 nmol L-1. Elevated DFe concentrations were observed above the Iberian, Greenland, and Newfoundland margins likely due to riverine inputs from the Tagus River, meteoric water inputs, and sedimentary inputs. Deep winter convection occurring the previous winter provided iron-to-nitrate ratios sufficient to sustain phytoplankton growth and lead to relatively elevated DFe concentrations within subsurface waters of the Irminger Sea. Increasing DFe concentrations along the flow path of the Labrador Sea Water were attributed to sedimentary inputs from the Newfoundland Margin. Bottom waters from the Irminger Sea displayed high DFe concentrations likely due to the dissolution of Fe-rich particles in the Denmark Strait Overflow Water and the Polar Intermediate Water. Finally, the nepheloid layers located in the different basins and at the Iberian Margin were found to act as either a source or a sink of DFe depending on the nature of particles, with organic particles likely releasing DFe and Mn particle scavenging DFe. This research has been supported by the French National Research Agency ANR GEOVIDE (grant no. ANR-13-BS06-0014), the RPDOC BITMAP (grant no. ANR-12-PDOC-0025-01), the French National Center for Scientific Research (grant no. CNRS-LEFE-CYBER), the LabexMER (grant no. ANR-10-LABX-19), and Ifremer (Institut français de recherche pour l'exploitation de la mer). Peer Reviewed |
author2 |
Jarðvísindastofnun (HÍ) Institute of Earth Sciences (UI) Verkfræði- og náttúruvísindasvið (HÍ) School of Engineering and Natural Sciences (UI) Háskóli Íslands University of Iceland |
format |
Article in Journal/Newspaper |
author |
Tonnard, Manon Planquette, Hélène Bowie, Andrew R. van der Merwe, Pier Gallinari, Morgane Desprez de Gésincourt, Floriane Germain, Yoan Gourain, Arthur Benetti, Marion Reverdin, Gilles Tréguer, Paul Boutorh, Julia Cheize, Marie Lacan, François Menzel Barraqueta, Jan-Lukas Pereira-Contreira, Leonardo Shelley, Rachel Lherminier, Pascale Sarthou, Géraldine |
author_facet |
Tonnard, Manon Planquette, Hélène Bowie, Andrew R. van der Merwe, Pier Gallinari, Morgane Desprez de Gésincourt, Floriane Germain, Yoan Gourain, Arthur Benetti, Marion Reverdin, Gilles Tréguer, Paul Boutorh, Julia Cheize, Marie Lacan, François Menzel Barraqueta, Jan-Lukas Pereira-Contreira, Leonardo Shelley, Rachel Lherminier, Pascale Sarthou, Géraldine |
author_sort |
Tonnard, Manon |
title |
Dissolved iron in the North Atlantic Ocean and Labrador Sea along the GEOVIDE section (GEOTRACES section GA01) |
title_short |
Dissolved iron in the North Atlantic Ocean and Labrador Sea along the GEOVIDE section (GEOTRACES section GA01) |
title_full |
Dissolved iron in the North Atlantic Ocean and Labrador Sea along the GEOVIDE section (GEOTRACES section GA01) |
title_fullStr |
Dissolved iron in the North Atlantic Ocean and Labrador Sea along the GEOVIDE section (GEOTRACES section GA01) |
title_full_unstemmed |
Dissolved iron in the North Atlantic Ocean and Labrador Sea along the GEOVIDE section (GEOTRACES section GA01) |
title_sort |
dissolved iron in the north atlantic ocean and labrador sea along the geovide section (geotraces section ga01) |
publisher |
Copernicus GmbH |
publishDate |
2020 |
url |
https://hdl.handle.net/20.500.11815/2413 https://doi.org/10.5194/bg-17-917-2020 |
long_lat |
ENVELOPE(-34.041,-34.041,63.054,63.054) |
geographic |
Greenland Irminger Sea Newfoundland |
geographic_facet |
Greenland Irminger Sea Newfoundland |
genre |
Denmark Strait Greenland Labrador Sea Newfoundland North Atlantic |
genre_facet |
Denmark Strait Greenland Labrador Sea Newfoundland North Atlantic |
op_relation |
Biogeosciences;17(4) https://bg.copernicus.org/articles/17/917/2020/bg-17-917-2020.pdf Tonnard, M., Planquette, H., Bowie, A. R., van der Merwe, P., Gallinari, M., Desprez de Gésincourt, F., Germain, Y., Gourain, A., Benetti, M., Reverdin, G., Tréguer, P., Boutorh, J., Cheize, M., Lacan, F., Menzel Barraqueta, J.-L., Pereira-Contreira, L., Shelley, R., Lherminier, P., and Sarthou, G.: Dissolved iron in the North Atlantic Ocean and Labrador Sea along the GEOVIDE section (GEOTRACES section GA01), Biogeosciences, 17, 917–943, https://doi.org/10.5194/bg-17-917-2020, 2020. 1726-4189 https://hdl.handle.net/20.500.11815/2413 Biogeosciences doi:10.5194/bg-17-917-2020 |
op_rights |
info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/20.500.11815/2413 https://doi.org/10.5194/bg-17-917-2020 |
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Biogeosciences |
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17 |
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4 |
container_start_page |
917 |
op_container_end_page |
943 |
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1766396686364573696 |