Distribution of copper-binding ligands in Fram Strait and influences from the Greenland Shelf (GEOTRACES GN05)
The Fram Strait represents the major gateway of Arctic Ocean waters towards the Nordic Seas and North Atlantic Ocean and is a key region to study the impact of climate change on biogeochemical cycles. In the region, information about trace metal speciation, such as copper, is scarce. This manuscript...
| Autores: | , , , , , , , |
|---|---|
| Tipo de recurso: | artículo |
| Estado: | Versión publicada |
| Fecha de publicación: | 2024 |
| País: | España |
| Institución: | Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya) |
| Repositorio: | Recercat. Dipósit de la Recerca de Catalunya |
| OAI Identifier: | oai:recercat.cat:10459.1/464750 |
| Acceso en línea: | https://doi.org/10.1016/j.scitotenv.2023.168162 https://hdl.handle.net/10459.1/464750 |
| Access Level: | acceso abierto |
| Palabra clave: | Copper Fram Strait Northeast Greenland shelf Compostos bioactius Canvis climàtics Ferroelectricitat |
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Distribution of copper-binding ligands in Fram Strait and influences from the Greenland Shelf (GEOTRACES GN05)Arnone, VeronicaSantana-Casiano, J. MagdalenaGonzález-Dávila, MelchorSarthou, GéraldineKrisch, StephanLodeiro, PabloAchterberg, Eric P.González, Aridane G.CopperFram StraitNortheast Greenland shelfCompostos bioactiusCanvis climàticsFerroelectricitatThe Fram Strait represents the major gateway of Arctic Ocean waters towards the Nordic Seas and North Atlantic Ocean and is a key region to study the impact of climate change on biogeochemical cycles. In the region, information about trace metal speciation, such as copper, is scarce. This manuscript presents the concentrations and conditional stability constants of copper-binding ligands (LCu and log KcondCu2+L) in the water column of Fram Strait and the Greenland shelf (GEOTRACES cruise GN05). Cu-binding ligands were analysed by Competitive Ligand Exchange-Adsorptive Cathodic Stripping Voltammetry (CLE-ACSV) using salicylaldoxime (SA) as competitive ligand. Based on water masses and the hydrodynamic influences, three provinces were considered (coast, shelf, and Fram Strait) and differences were observed between regions and water masses. The strongest variability was observed in surface waters, with increasing LCu concentrations (mean values: Fram Strait = 2.6 ± 1.0 nM; shelf = 5.2 ± 1.3 nM; coast = 6.4 ± 0.8 nM) and decreasing log KcondCu2+L values (mean values: Fram Strait = 15.7 ± 0.3; shelf = 15.2 ± 0.3; coast = 14.8 ± 0.3) towards the west. The surface LCu concentrations obtained above the Greenland shelf indicate a supply from the coastal environment to the Polar Surface Water (PSW) which is an addition to the ligand exported from the central Arctic to Fram Strait. The significant differences (in terms of LCu and log KcondCu2+L) between shelf and coastal samples were explained considering the processes which modify ligand concentrations and binding strengths, such as biological activity in sea-ice, phytoplankton bloom in surface waters, bacterial degradation, and meltwater discharge from 79NG glacier terminus. Overall, the ligand concentration exceeded those of dissolved Cu (dCu) and kept the free copper (Cu2+) concentrations at femtomolar levels (0.13–21.13 fM). This indicates that Cu2+ toxicity limits were not reached and dCu levels were stabilized in surface waters by organic complexes, which favoured its transport to the Nordic Seas and North Atlantic Ocean and the development of microorganism.The authors would like to thank captain Schwarze and his crew of the RV Polarstern, the chief scientist Torsten Kanzow and all other participants, for their effort and support during sample collection. We also acknowledge the financial support for the ATOPFe project (CTM2017-83476-P) from the Ministerio de Ciencia e Innovación (Spain). VA participation was funded by the PhD grant (PRE 2018-084476). AGG participation was partially funded by LabexMER International Postdoctoral Program for providing fellowship and Laboratoire d'Excellence LabexMer (ANR-10-LABX-19). PL also thank the support from the Ministerio de Ciencia, Innovación y Universidades of Spain and University of Lleida (Beatriz Galindo Senior award number BG20/00104).Elsevier2024info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttps://doi.org/10.1016/j.scitotenv.2023.168162https://hdl.handle.net/10459.1/464750reponame:Recercat. Dipósit de la Recerca de Catalunyainstname:Varias* (Consorci de Biblioteques Universitáries de Catalunya, Centre de Serveis Científics i Acadèmics de Catalunya)Inglésinfo:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CTM2017-83476-PReproducció del document publicat a https://doi.org/10.1016/j.scitotenv.2023.168162Science of the Total Environment, 2024, vol. 909, núm. 168162, p. 1-14cc- by-nc (c) Arnone et al., 2024Attribution-NonCommercial 4.0 Internationalinfo:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc/4.0/oai:recercat.cat:10459.1/4647502026-05-29T05:05:01Z |
| dc.title.none.fl_str_mv |
Distribution of copper-binding ligands in Fram Strait and influences from the Greenland Shelf (GEOTRACES GN05) |
| title |
Distribution of copper-binding ligands in Fram Strait and influences from the Greenland Shelf (GEOTRACES GN05) |
| spellingShingle |
Distribution of copper-binding ligands in Fram Strait and influences from the Greenland Shelf (GEOTRACES GN05) Arnone, Veronica Copper Fram Strait Northeast Greenland shelf Compostos bioactius Canvis climàtics Ferroelectricitat |
| title_short |
Distribution of copper-binding ligands in Fram Strait and influences from the Greenland Shelf (GEOTRACES GN05) |
| title_full |
Distribution of copper-binding ligands in Fram Strait and influences from the Greenland Shelf (GEOTRACES GN05) |
| title_fullStr |
Distribution of copper-binding ligands in Fram Strait and influences from the Greenland Shelf (GEOTRACES GN05) |
| title_full_unstemmed |
Distribution of copper-binding ligands in Fram Strait and influences from the Greenland Shelf (GEOTRACES GN05) |
| title_sort |
Distribution of copper-binding ligands in Fram Strait and influences from the Greenland Shelf (GEOTRACES GN05) |
| dc.creator.none.fl_str_mv |
Arnone, Veronica Santana-Casiano, J. Magdalena González-Dávila, Melchor Sarthou, Géraldine Krisch, Stephan Lodeiro, Pablo Achterberg, Eric P. González, Aridane G. |
| author |
Arnone, Veronica |
| author_facet |
Arnone, Veronica Santana-Casiano, J. Magdalena González-Dávila, Melchor Sarthou, Géraldine Krisch, Stephan Lodeiro, Pablo Achterberg, Eric P. González, Aridane G. |
| author_role |
author |
| author2 |
Santana-Casiano, J. Magdalena González-Dávila, Melchor Sarthou, Géraldine Krisch, Stephan Lodeiro, Pablo Achterberg, Eric P. González, Aridane G. |
| author2_role |
author author author author author author author |
| dc.subject.none.fl_str_mv |
Copper Fram Strait Northeast Greenland shelf Compostos bioactius Canvis climàtics Ferroelectricitat |
| topic |
Copper Fram Strait Northeast Greenland shelf Compostos bioactius Canvis climàtics Ferroelectricitat |
| description |
The Fram Strait represents the major gateway of Arctic Ocean waters towards the Nordic Seas and North Atlantic Ocean and is a key region to study the impact of climate change on biogeochemical cycles. In the region, information about trace metal speciation, such as copper, is scarce. This manuscript presents the concentrations and conditional stability constants of copper-binding ligands (LCu and log KcondCu2+L) in the water column of Fram Strait and the Greenland shelf (GEOTRACES cruise GN05). Cu-binding ligands were analysed by Competitive Ligand Exchange-Adsorptive Cathodic Stripping Voltammetry (CLE-ACSV) using salicylaldoxime (SA) as competitive ligand. Based on water masses and the hydrodynamic influences, three provinces were considered (coast, shelf, and Fram Strait) and differences were observed between regions and water masses. The strongest variability was observed in surface waters, with increasing LCu concentrations (mean values: Fram Strait = 2.6 ± 1.0 nM; shelf = 5.2 ± 1.3 nM; coast = 6.4 ± 0.8 nM) and decreasing log KcondCu2+L values (mean values: Fram Strait = 15.7 ± 0.3; shelf = 15.2 ± 0.3; coast = 14.8 ± 0.3) towards the west. The surface LCu concentrations obtained above the Greenland shelf indicate a supply from the coastal environment to the Polar Surface Water (PSW) which is an addition to the ligand exported from the central Arctic to Fram Strait. The significant differences (in terms of LCu and log KcondCu2+L) between shelf and coastal samples were explained considering the processes which modify ligand concentrations and binding strengths, such as biological activity in sea-ice, phytoplankton bloom in surface waters, bacterial degradation, and meltwater discharge from 79NG glacier terminus. Overall, the ligand concentration exceeded those of dissolved Cu (dCu) and kept the free copper (Cu2+) concentrations at femtomolar levels (0.13–21.13 fM). This indicates that Cu2+ toxicity limits were not reached and dCu levels were stabilized in surface waters by organic complexes, which favoured its transport to the Nordic Seas and North Atlantic Ocean and the development of microorganism. |
| publishDate |
2024 |
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2024 |
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info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
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article |
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publishedVersion |
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https://doi.org/10.1016/j.scitotenv.2023.168162 https://hdl.handle.net/10459.1/464750 |
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https://doi.org/10.1016/j.scitotenv.2023.168162 https://hdl.handle.net/10459.1/464750 |
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Inglés |
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Inglés |
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info:eu-repo/grantAgreement/AEI/Plan Estatal de Investigación Científica y Técnica y de Innovación 2013-2016/CTM2017-83476-P Reproducció del document publicat a https://doi.org/10.1016/j.scitotenv.2023.168162 Science of the Total Environment, 2024, vol. 909, núm. 168162, p. 1-14 |
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cc- by-nc (c) Arnone et al., 2024 Attribution-NonCommercial 4.0 International info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc/4.0/ |
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cc- by-nc (c) Arnone et al., 2024 Attribution-NonCommercial 4.0 International http://creativecommons.org/licenses/by-nc/4.0/ |
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openAccess |
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