Natural copper-binding ligands in the Arctic Ocean. The influence of the Transpolar Drift (GEOTRACES GN04)
The Arctic Ocean is a unique biogeochemical environment characterized by low salinity surface waters, extensive sea-ice coverage, high riverine inputs, large shelf extension and the long residence time of deep waters. These characteristics determine the distribution of dissolved bio-essential trace...
Published in: | Frontiers in Marine Science |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Frontiers Media SA
2023
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Online Access: | https://archimer.ifremer.fr/doc/00869/98126/107415.pdf https://archimer.ifremer.fr/doc/00869/98126/107416.docx https://doi.org/10.3389/fmars.2023.1306278 https://archimer.ifremer.fr/doc/00869/98126/ |
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ftarchimer:oai:archimer.ifremer.fr:98126 2024-05-19T07:28:16+00:00 Natural copper-binding ligands in the Arctic Ocean. The influence of the Transpolar Drift (GEOTRACES GN04) Arnone, Veronica Santana-casiano, J. Magdalena González-dávila, Melchor Planquette, Helene Sarthou, Geraldine Gerringa, Loes J. A. González, Aridane G. 2023-12 application/pdf https://archimer.ifremer.fr/doc/00869/98126/107415.pdf https://archimer.ifremer.fr/doc/00869/98126/107416.docx https://doi.org/10.3389/fmars.2023.1306278 https://archimer.ifremer.fr/doc/00869/98126/ eng eng Frontiers Media SA https://archimer.ifremer.fr/doc/00869/98126/107415.pdf https://archimer.ifremer.fr/doc/00869/98126/107416.docx doi:10.3389/fmars.2023.1306278 https://archimer.ifremer.fr/doc/00869/98126/ info:eu-repo/semantics/openAccess restricted use Frontiers In Marine Science (2296-7745) (Frontiers Media SA), 2023-12 , Vol. 10 , P. 1306278 (20p.) copper copper-binding ligands voltammetric method Arctic Ocean Transpolar Drift text Article info:eu-repo/semantics/article 2023 ftarchimer https://doi.org/10.3389/fmars.2023.1306278 2024-04-30T23:30:28Z The Arctic Ocean is a unique biogeochemical environment characterized by low salinity surface waters, extensive sea-ice coverage, high riverine inputs, large shelf extension and the long residence time of deep waters. These characteristics determine the distribution of dissolved bio-essential trace metals, such as copper (Cu), and the dissolved organic-binding ligands capable of complexing it. This work reports the concentrations and conditional stability constants of dissolved Cu-binding ligands (LCu and log KcondCu2+L) measured in samples from the Polarstern (PS94) expedition, as part of the international GEOTRACES program (cruise GN04). Full-depth profile stations from the Barents Sea, Nansen Basin, Amundsen Basin and Makarov Basin were analysed by competitive ligand exchange-adsorptive cathodic stripping voltammetry (CLE-AdCSV). The basins and water masses presented a wide range of LCu concentrations (range: 1.40 – 7.91 nM) and log KcondCu2+L values (range: 13.83 – 16.01). The highest variability of Cu-binding ligand concentrations was observed in surface waters (≤200 m), and mean concentrations increased from the Barents Sea and Nansen Basin (2.15 ± 0.31 nM and 1.93 ± 0.35 nM, respectively) to the Amundsen (3.84 ± 1.69 nM) and Makarov Basins (4.40± 2.03 nM). The influence of the Transpolar Drift (TDP) flow path was observed in the Amundsen and Makarov Basins, especially on Cu-binding ligand concentrations (LCu range: 3.96 – 7.91 nM). In contrast, deep waters (>200 m) showed no significant differences between basins and water masses in terms of LCu concentrations (range: 1.45 – 2.78 nM) and log KcondCu2+L (range: 14.02 – 15.46). The presence of strong Cu-binding ligands (log KcondCu2+L>13) in surface waters stabilises the excess of dissolved copper (dCu) transported in the TPD and favours its export to the Fram Strait and Nordic Seas. Article in Journal/Newspaper amundsen basin Arctic Arctic Ocean Barents Sea Fram Strait makarov basin Nansen Basin Nordic Seas Sea ice Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) Frontiers in Marine Science 10 |
institution |
Open Polar |
collection |
Archimer (Archive Institutionnelle de l'Ifremer - Institut français de recherche pour l'exploitation de la mer) |
op_collection_id |
ftarchimer |
language |
English |
topic |
copper copper-binding ligands voltammetric method Arctic Ocean Transpolar Drift |
spellingShingle |
copper copper-binding ligands voltammetric method Arctic Ocean Transpolar Drift Arnone, Veronica Santana-casiano, J. Magdalena González-dávila, Melchor Planquette, Helene Sarthou, Geraldine Gerringa, Loes J. A. González, Aridane G. Natural copper-binding ligands in the Arctic Ocean. The influence of the Transpolar Drift (GEOTRACES GN04) |
topic_facet |
copper copper-binding ligands voltammetric method Arctic Ocean Transpolar Drift |
description |
The Arctic Ocean is a unique biogeochemical environment characterized by low salinity surface waters, extensive sea-ice coverage, high riverine inputs, large shelf extension and the long residence time of deep waters. These characteristics determine the distribution of dissolved bio-essential trace metals, such as copper (Cu), and the dissolved organic-binding ligands capable of complexing it. This work reports the concentrations and conditional stability constants of dissolved Cu-binding ligands (LCu and log KcondCu2+L) measured in samples from the Polarstern (PS94) expedition, as part of the international GEOTRACES program (cruise GN04). Full-depth profile stations from the Barents Sea, Nansen Basin, Amundsen Basin and Makarov Basin were analysed by competitive ligand exchange-adsorptive cathodic stripping voltammetry (CLE-AdCSV). The basins and water masses presented a wide range of LCu concentrations (range: 1.40 – 7.91 nM) and log KcondCu2+L values (range: 13.83 – 16.01). The highest variability of Cu-binding ligand concentrations was observed in surface waters (≤200 m), and mean concentrations increased from the Barents Sea and Nansen Basin (2.15 ± 0.31 nM and 1.93 ± 0.35 nM, respectively) to the Amundsen (3.84 ± 1.69 nM) and Makarov Basins (4.40± 2.03 nM). The influence of the Transpolar Drift (TDP) flow path was observed in the Amundsen and Makarov Basins, especially on Cu-binding ligand concentrations (LCu range: 3.96 – 7.91 nM). In contrast, deep waters (>200 m) showed no significant differences between basins and water masses in terms of LCu concentrations (range: 1.45 – 2.78 nM) and log KcondCu2+L (range: 14.02 – 15.46). The presence of strong Cu-binding ligands (log KcondCu2+L>13) in surface waters stabilises the excess of dissolved copper (dCu) transported in the TPD and favours its export to the Fram Strait and Nordic Seas. |
format |
Article in Journal/Newspaper |
author |
Arnone, Veronica Santana-casiano, J. Magdalena González-dávila, Melchor Planquette, Helene Sarthou, Geraldine Gerringa, Loes J. A. González, Aridane G. |
author_facet |
Arnone, Veronica Santana-casiano, J. Magdalena González-dávila, Melchor Planquette, Helene Sarthou, Geraldine Gerringa, Loes J. A. González, Aridane G. |
author_sort |
Arnone, Veronica |
title |
Natural copper-binding ligands in the Arctic Ocean. The influence of the Transpolar Drift (GEOTRACES GN04) |
title_short |
Natural copper-binding ligands in the Arctic Ocean. The influence of the Transpolar Drift (GEOTRACES GN04) |
title_full |
Natural copper-binding ligands in the Arctic Ocean. The influence of the Transpolar Drift (GEOTRACES GN04) |
title_fullStr |
Natural copper-binding ligands in the Arctic Ocean. The influence of the Transpolar Drift (GEOTRACES GN04) |
title_full_unstemmed |
Natural copper-binding ligands in the Arctic Ocean. The influence of the Transpolar Drift (GEOTRACES GN04) |
title_sort |
natural copper-binding ligands in the arctic ocean. the influence of the transpolar drift (geotraces gn04) |
publisher |
Frontiers Media SA |
publishDate |
2023 |
url |
https://archimer.ifremer.fr/doc/00869/98126/107415.pdf https://archimer.ifremer.fr/doc/00869/98126/107416.docx https://doi.org/10.3389/fmars.2023.1306278 https://archimer.ifremer.fr/doc/00869/98126/ |
genre |
amundsen basin Arctic Arctic Ocean Barents Sea Fram Strait makarov basin Nansen Basin Nordic Seas Sea ice |
genre_facet |
amundsen basin Arctic Arctic Ocean Barents Sea Fram Strait makarov basin Nansen Basin Nordic Seas Sea ice |
op_source |
Frontiers In Marine Science (2296-7745) (Frontiers Media SA), 2023-12 , Vol. 10 , P. 1306278 (20p.) |
op_relation |
https://archimer.ifremer.fr/doc/00869/98126/107415.pdf https://archimer.ifremer.fr/doc/00869/98126/107416.docx doi:10.3389/fmars.2023.1306278 https://archimer.ifremer.fr/doc/00869/98126/ |
op_rights |
info:eu-repo/semantics/openAccess restricted use |
op_doi |
https://doi.org/10.3389/fmars.2023.1306278 |
container_title |
Frontiers in Marine Science |
container_volume |
10 |
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1799472128096993280 |