FN Archimer Export Format
PT J
TI Dissolved iron in the North Atlantic Ocean and Labrador Sea along the GEOVIDE section (GEOTRACES section GA01)
BT 
AF 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
   Menzel Barraqueta, Jan-Lukas
   Pereira-Contreira, Leonardo
   Shelley, Rachel
   Lherminier, Pascale
   Sarthou, Géraldine
AS 1:1,2,3;2:1;3:2,3;4:2;5:1;6:1;7:4;8:5;9:6,7;10:7;11:1;12:1;13:4;14:8;15:9;16:4,10,11;17:12;18:1;
FF 1:;2:;3:;4:;5:;6:;7:PDG-REM-GM-LCG;8:;9:;10:;11:;12:;13:PDG-REM-GM-LCG;14:;15:;16:;17:PDG-ODE-LOPS-OH;18:;
C1 Laboratoire des sciences de l'Environnement MARin – CNRS UMR 6539 – Institut Universitaire Européen de la Mer, Plouzané, 29280, France
   Antarctic Climate and Ecosystems – Cooperative Research Centre, Hobart, TAS 7001, Australia
   Institute for Marine and Antarctic Studies, University of Tasmania, Hobart, TAS 7001, Australia
   Laboratoire Cycles Géochimiques et ressources – Ifremer, Plouzané, 29280, France
   Ocean Sciences Department, School of Environmental Sciences, University of Liverpool, L69 3GP, UK
   Institute of Earth Sciences, University of Iceland, Reykjavik, Iceland
   LOCEAN, Sorbonne Universités, UPMC/CNRS/IRD/MNHN, Paris, France
   GEOMAR Helmholtz-Zentrum für Ozeanforschung Kiel Wischhofstraße 1–3, Geb. 12 24148 Kiel, Germany
   Fundação Universidade Federal do Rio Grande (FURG), R. Luis Loréa, Rio Grande – RS, 96200-350, Brazil
   Dept. 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
   Ifremer, Université de Bretagne Occidentale (UBO), CNRS, IRD, Laboratoire d'Océanographie Physique et Spatiale (LOPS), IUEM, 29280, Plouzané, France
C2 UBO, FRANCE
   ACE CRC, AUSTRALIA
   UNIV TASMANIA, AUSTRALIA
   IFREMER, FRANCE
   UNIV LIVERPOOL, UK
   UNIV ICELAND, ICELAND
   UNIV PARIS 06, FRANCE
   IFM GEOMAR, GERMANY
   UNIV FED RIO GRANDE, BRAZIL
   UNIV FLORIDA STATE, USA
   UNIV PLYMOUTH, UK
   IFREMER, FRANCE
SI BREST
SE PDG-REM-GM-LCG
   PDG-ODE-LOPS-OH
UM LOPS
   LEMAR
IN WOS Ifremer UPR
   WOS Ifremer UMR
   WOS Cotutelle UMR
   DOAJ
   copubli-france
   copubli-europe
   copubli-univ-france
   copubli-int-hors-europe
   copubli-sud
IF 4.295
TC 22
UR https://archimer.ifremer.fr/doc/00441/55233/56714.pdf
   https://archimer.ifremer.fr/doc/00441/55233/56715.pdf
   https://archimer.ifremer.fr/doc/00441/55233/70966.pdf
   https://archimer.ifremer.fr/doc/00441/55233/70967.pdf
LA English
DT Article
CR GEOVIDE
BO Pourquoi pas ?
AB Dissolved Fe (DFe) samples from the GEOVIDE voyage (GEOTRACES GA01, May–June 2014) in the North Atlantic Ocean were analysed using a SeaFAST-picoTM coupled to an Element XR HR-ICP-MS and provided interesting insights on the Fe sources in this area. Overall, DFe concentrations ranged from 0.09 ± 0.01 nmol L−1 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. Air-sea interactions were suspected to be responsible for the increase in DFe concentrations within subsurface waters of the Irminger Sea due to deep convection occurring the previous winter, that provided iron-to-nitrate ratios sufficient to sustain phytoplankton growth. 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 from the Denmark Strait Overflow Water and the Polar Intermediate Water. Finally, the nepheloid layers were found to act as either a source or a sink of DFe depending on the nature of particles. 
PY 2020
PD FEB
SO Biogeosciences
SN 1726-4170
PU Copernicus GmbH
VL 17
IS 4
UT 000516719200003
BP 917
EP 943
DI 10.5194/bg-17-917-2020
ID 55233
ER

EF