Articles | Volume 17, issue 4
https://doi.org/10.5194/bg-17-917-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Special issue:
https://doi.org/10.5194/bg-17-917-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
21 Feb 2020
Research article |
| 21 Feb 2020
| 21 Feb 2020
Dissolved iron in the North Atlantic Ocean and Labrador Sea along the GEOVIDE section (GEOTRACES section GA01)
Manon Tonnard
Univ Brest, CNRS, IRD, Ifremer, LEMAR, 29280 Plouzane, France
Antarctic Climate and Ecosystems – Cooperative Research Centre,
University of Tasmania, Hobart, TAS 7001, Australia
Institute for Marine and Antarctic Studies, University of Tasmania,
Hobart, TAS 7001, Australia
Hélène Planquette
CORRESPONDING AUTHOR
Univ Brest, CNRS, IRD, Ifremer, LEMAR, 29280 Plouzane, France
Andrew R. Bowie
Antarctic Climate and Ecosystems – Cooperative Research Centre,
University of Tasmania, Hobart, TAS 7001, Australia
Institute for Marine and Antarctic Studies, University of Tasmania,
Hobart, TAS 7001, Australia
Pier van der Merwe
Antarctic Climate and Ecosystems – Cooperative Research Centre,
University of Tasmania, Hobart, TAS 7001, Australia
Morgane Gallinari
Univ Brest, CNRS, IRD, Ifremer, LEMAR, 29280 Plouzane, France
Floriane Desprez de Gésincourt
Univ Brest, CNRS, IRD, Ifremer, LEMAR, 29280 Plouzane, France
Yoan Germain
Laboratoire Cycles Géochimiques et ressources – Ifremer,
Plouzané, 29280, France
Arthur Gourain
Ocean Sciences Department, School of Environmental Sciences,
University of Liverpool, L69 3GP, UK
Marion Benetti
Institute of Earth Sciences, University of Iceland, Reykjavik, Iceland
LOCEAN, Sorbonne Universités, UPMC/CNRS/IRD/MNHN, Paris, France
Gilles Reverdin
LOCEAN, Sorbonne Universités, UPMC/CNRS/IRD/MNHN, Paris, France
Paul Tréguer
Univ Brest, CNRS, IRD, Ifremer, LEMAR, 29280 Plouzane, France
Julia Boutorh
Univ Brest, CNRS, IRD, Ifremer, LEMAR, 29280 Plouzane, France
Marie Cheize
Univ Brest, CNRS, IRD, Ifremer, LEMAR, 29280 Plouzane, France
François Lacan
LEGOS, Université de Toulouse – CNRS/IRD/CNES/UPS – Observatoire
Midi-Pyrénées, Toulouse, France
Jan-Lukas Menzel Barraqueta
GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel
Wischhofstraße 1–3, Geb. 12, 24148 Kiel, Germany
Department of Earth Sciences, Stellenbosch University, Stellenbosch,
7600, South Africa
Leonardo Pereira-Contreira
Fundação Universidade Federal do Rio Grande (FURG), R. Luis
Loréa, Rio Grande – RS, 96200-350, Brazil
Rachel Shelley
Fundação Universidade Federal do Rio Grande (FURG), R. Luis
Loréa, Rio Grande – RS, 96200-350, Brazil
Dept. of Earth, Ocean and Atmospheric Science, Florida State University,
117 N Woodward Ave, Tallahassee, Florida 32301, USA
School of Geography, Earth and Environmental Sciences, University of
Plymouth, Drake Circus, Plymouth, PL4 8AA, UK
Pascale Lherminier
Ifremer, Univ Brest, CNRS, IRD, Laboratoire d'Océanographie
Physique et Spatiale (LOPS), IUEM, 29280, Plouzané, France
Géraldine Sarthou
CORRESPONDING AUTHOR
Univ Brest, CNRS, IRD, Ifremer, LEMAR, 29280 Plouzane, France
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Latest update: 25 Nov 2025
Short summary
We investigated the spatial distribution of dissolved Fe during spring 2014, in order to understand the processes influencing the biogeochemical cycle in the North Atlantic. Our results highlighted elevated Fe close to riverine inputs at the Iberian Margin and glacial inputs at the Newfoundland and Greenland margins. Atmospheric deposition appeared to be a minor source of Fe. Convection was an important source of Fe in the Irminger Sea, which was depleted in Fe relative to nitrate.
We investigated the spatial distribution of dissolved Fe during spring 2014, in order to...
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