Dissolved iron in the North Atlantic Ocean and Labrador Sea along the GEOVIDE section (GEOTRACES section GA01)
Dissolved Fe (DFe) samples from the GEOVIDE voyage (GEOTRACES GA01, MayJune2014) in the North Atlantic Ocean were analyzed using asea FAST -pico coupled to an Element XR sector fieldinductively coupled plasma mass spectrometer (SF-ICP-MS) and provided interestinginsights into the Fe sources in this...
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2020
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Online Access: | https://doi.org/10.5194/bg-17-917-2020 http://ecite.utas.edu.au/137715 |
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ftunivtasecite:oai:ecite.utas.edu.au:137715 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, M Planquette, H Bowie, AR van der Merwe, P Gallinari, M de Gesincourt, FD Germain, Y Gourain, A Benetti, M Reverdin, G Treguer, P Boutorh, J Cheize, M Lacan, F Barraqueta, J-LM Pereira-Contreira, L Shelley, R Lherminier, P Sarthou, G 2020 application/pdf https://doi.org/10.5194/bg-17-917-2020 http://ecite.utas.edu.au/137715 en eng Copernicus GmbH http://ecite.utas.edu.au/137715/1/137715 - Dissolved iron in the North Atlantic Ocean and Labrador Sea.pdf http://dx.doi.org/10.5194/bg-17-917-2020 Tonnard, M and Planquette, H and Bowie, AR and van der Merwe, P and Gallinari, M and de Gesincourt, FD and Germain, Y and Gourain, A and Benetti, M and Reverdin, G and Treguer, P and Boutorh, J and Cheize, M and Lacan, F and Barraqueta, J-LM and Pereira-Contreira, L and Shelley, R and Lherminier, P and Sarthou, G, Dissolved iron in the North Atlantic Ocean and Labrador Sea along the GEOVIDE section (GEOTRACES section GA01), Biogeosciences, 17 pp. 917-943. ISSN 1726-4170 (2020) [Refereed Article] http://ecite.utas.edu.au/137715 Earth Sciences Oceanography Chemical oceanography Refereed Article PeerReviewed 2020 ftunivtasecite https://doi.org/10.5194/bg-17-917-2020 2022-08-29T22:17:53Z Dissolved Fe (DFe) samples from the GEOVIDE voyage (GEOTRACES GA01, MayJune2014) in the North Atlantic Ocean were analyzed using asea FAST -pico coupled to an Element XR sector fieldinductively coupled plasma mass spectrometer (SF-ICP-MS) and provided interestinginsights into the Fe sources in this area. Overall, DFe concentrations rangedfrom 0.090.01 to 7.80.5 nmol L −1 .Elevated DFe concentrations were observed above the Iberian, Greenland, andNewfoundland margins likely due to riverine inputs from the Tagus River,meteoric water inputs, and sedimentary inputs. Deep winter convectionoccurring the previous winter provided iron-to-nitrate ratios sufficient tosustain phytoplankton growth and lead to relatively elevated DFeconcentrations within subsurface waters of the Irminger Sea. Increasing DFeconcentrations along the flow path of the Labrador Sea Water were attributedto sedimentary inputs from the Newfoundland Margin. Bottom waters from theIrminger Sea displayed high DFe concentrations likely due to the dissolutionof Fe-rich particles in the Denmark Strait Overflow Water and the PolarIntermediate Water. Finally, the nepheloid layers located in the differentbasins and at the Iberian Margin were found to act as either a source or asink of DFe depending on the nature of particles, with organic particleslikely releasing DFe and Mn particle scavenging DFe. Article in Journal/Newspaper Denmark Strait Greenland Labrador Sea Newfoundland North Atlantic eCite UTAS (University of Tasmania) Newfoundland Greenland Irminger Sea ENVELOPE(-34.041,-34.041,63.054,63.054) Biogeosciences 17 4 917 943 |
institution |
Open Polar |
collection |
eCite UTAS (University of Tasmania) |
op_collection_id |
ftunivtasecite |
language |
English |
topic |
Earth Sciences Oceanography Chemical oceanography |
spellingShingle |
Earth Sciences Oceanography Chemical oceanography Tonnard, M Planquette, H Bowie, AR van der Merwe, P Gallinari, M de Gesincourt, FD Germain, Y Gourain, A Benetti, M Reverdin, G Treguer, P Boutorh, J Cheize, M Lacan, F Barraqueta, J-LM Pereira-Contreira, L Shelley, R Lherminier, P Sarthou, G Dissolved iron in the North Atlantic Ocean and Labrador Sea along the GEOVIDE section (GEOTRACES section GA01) |
topic_facet |
Earth Sciences Oceanography Chemical oceanography |
description |
Dissolved Fe (DFe) samples from the GEOVIDE voyage (GEOTRACES GA01, MayJune2014) in the North Atlantic Ocean were analyzed using asea FAST -pico coupled to an Element XR sector fieldinductively coupled plasma mass spectrometer (SF-ICP-MS) and provided interestinginsights into the Fe sources in this area. Overall, DFe concentrations rangedfrom 0.090.01 to 7.80.5 nmol L −1 .Elevated DFe concentrations were observed above the Iberian, Greenland, andNewfoundland margins likely due to riverine inputs from the Tagus River,meteoric water inputs, and sedimentary inputs. Deep winter convectionoccurring the previous winter provided iron-to-nitrate ratios sufficient tosustain phytoplankton growth and lead to relatively elevated DFeconcentrations within subsurface waters of the Irminger Sea. Increasing DFeconcentrations along the flow path of the Labrador Sea Water were attributedto sedimentary inputs from the Newfoundland Margin. Bottom waters from theIrminger Sea displayed high DFe concentrations likely due to the dissolutionof Fe-rich particles in the Denmark Strait Overflow Water and the PolarIntermediate Water. Finally, the nepheloid layers located in the differentbasins and at the Iberian Margin were found to act as either a source or asink of DFe depending on the nature of particles, with organic particleslikely releasing DFe and Mn particle scavenging DFe. |
format |
Article in Journal/Newspaper |
author |
Tonnard, M Planquette, H Bowie, AR van der Merwe, P Gallinari, M de Gesincourt, FD Germain, Y Gourain, A Benetti, M Reverdin, G Treguer, P Boutorh, J Cheize, M Lacan, F Barraqueta, J-LM Pereira-Contreira, L Shelley, R Lherminier, P Sarthou, G |
author_facet |
Tonnard, M Planquette, H Bowie, AR van der Merwe, P Gallinari, M de Gesincourt, FD Germain, Y Gourain, A Benetti, M Reverdin, G Treguer, P Boutorh, J Cheize, M Lacan, F Barraqueta, J-LM Pereira-Contreira, L Shelley, R Lherminier, P Sarthou, G |
author_sort |
Tonnard, M |
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://doi.org/10.5194/bg-17-917-2020 http://ecite.utas.edu.au/137715 |
long_lat |
ENVELOPE(-34.041,-34.041,63.054,63.054) |
geographic |
Newfoundland Greenland Irminger Sea |
geographic_facet |
Newfoundland Greenland Irminger Sea |
genre |
Denmark Strait Greenland Labrador Sea Newfoundland North Atlantic |
genre_facet |
Denmark Strait Greenland Labrador Sea Newfoundland North Atlantic |
op_relation |
http://ecite.utas.edu.au/137715/1/137715 - Dissolved iron in the North Atlantic Ocean and Labrador Sea.pdf http://dx.doi.org/10.5194/bg-17-917-2020 Tonnard, M and Planquette, H and Bowie, AR and van der Merwe, P and Gallinari, M and de Gesincourt, FD and Germain, Y and Gourain, A and Benetti, M and Reverdin, G and Treguer, P and Boutorh, J and Cheize, M and Lacan, F and Barraqueta, J-LM and Pereira-Contreira, L and Shelley, R and Lherminier, P and Sarthou, G, Dissolved iron in the North Atlantic Ocean and Labrador Sea along the GEOVIDE section (GEOTRACES section GA01), Biogeosciences, 17 pp. 917-943. ISSN 1726-4170 (2020) [Refereed Article] http://ecite.utas.edu.au/137715 |
op_doi |
https://doi.org/10.5194/bg-17-917-2020 |
container_title |
Biogeosciences |
container_volume |
17 |
container_issue |
4 |
container_start_page |
917 |
op_container_end_page |
943 |
_version_ |
1766396670892834816 |