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| "author_email": null, | | "author": "Rob Middag (Royal Netherlands Institute for Sea |
| | | Research)", |
| | | "author_email": "rob.middag@nioz.nl", |
| "code": "7b.b.jc", | | "code": "7b.b.jc", |
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| Netherlands Institute for Sea | | Netherlands Institute for Sea |
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| Netherlands Institute for Sea | | Netherlands Institute for Sea |
| "firstname\":\"Hans\",\"lastname\":\"Slagter\",\"affiliation\":\"Royal | | "firstname\":\"Hans\",\"lastname\":\"Slagter\",\"affiliation\":\"Royal |
| Netherlands Institute for Sea | | Netherlands Institute for Sea |
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| Geochemistry, Institute for Chemistry and Biology of the Marine | | Geochemistry, Institute for Chemistry and Biology of the Marine |
| Environment (ICBM), University of Oldenburg, Oldenburg, GermanyRoyal | | Environment (ICBM), University of Oldenburg, Oldenburg, GermanyRoyal |
| Netherlands Institute for Sea | | Netherlands Institute for Sea |
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| for Radiometric Dating and Stable Isotope Research, Kiel University, | | for Radiometric Dating and Stable Isotope Research, Kiel University, |
| Kiel, Germany and GEOMAR Hemholtz Centre for Ocean Research, Kiel, | | Kiel, Germany and GEOMAR Hemholtz Centre for Ocean Research, Kiel, |
| ndingauthor\":false},{\"firstname\":\"Michiel\",\"lastname\":\"Rutgers | | ndingauthor\":false},{\"firstname\":\"Michiel\",\"lastname\":\"Rutgers |
| van der Loeff\",\"affiliation\":\"5.\\tHelmholtz Centre for Polar and | | van der Loeff\",\"affiliation\":\"5.\\tHelmholtz Centre for Polar and |
| Marine Research, Alfred Wegener Institute, Bremerhaven, | | Marine Research, Alfred Wegener Institute, Bremerhaven, |
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| "deposit_date": "2021-05-20", | | "deposit_date": "2021-05-20", |
| n | "depositor": "loes gerringa", | n | "depositor": "loes gerringa (loes.gerringa@nioz.nl)", |
| "distribution_date": "2021-05-20", | | "distribution_date": "2021-05-20", |
| "distributor": "Research Data Management(NIOZ Royal Netherlands | | "distributor": "Research Data Management(NIOZ Royal Netherlands |
| Institute for Sea Research)", | | Institute for Sea Research)", |
| n | "doi_date_published": "2021-07-20", | n | "doi_date_published": "2021-07-20T08:31:06.0874969", |
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| n | "metadata_modified": "2024-10-22T20:41:06.992874", | n | "metadata_modified": "2025-03-11T12:21:26.415591", |
| "name": "7bbjc", | | "name": "dissolved-cd", |
| "notes": "During the Polarstern (PS94) expedition in summer 2015, | | "notes": "During the Polarstern (PS94) expedition in summer 2015, |
| part of the international GEOTRACES program sources and sinks of | | part of the international GEOTRACES program sources and sinks of |
| n | dissolved (D) Cd, Co, Cu, Fe, Mn, Ni and Zn were studied in the | n | dissolved (D) Cd, Co, Cu, Fe, Mn, Ni, Pb and Zn were studied in the |
| central Arctic Ocean. In the Polar Surface Water in which the | | central Arctic Ocean. In the Polar Surface Water in which the |
| TransPolar Drift (TPD) is situated, salinity and d18O derived | | TransPolar Drift (TPD) is situated, salinity and d18O derived |
| fractions indicated a distinct riverine source for silicate DCo, DCu, | | fractions indicated a distinct riverine source for silicate DCo, DCu, |
| DFe, DMn and DNi. Linear relationships between DMn and the meteoric | | DFe, DMn and DNi. Linear relationships between DMn and the meteoric |
| fraction depended on the source distance, likely due to | | fraction depended on the source distance, likely due to |
| Mn-precipitation with transport time. In the upper 50 m of the Makarov | | Mn-precipitation with transport time. In the upper 50 m of the Makarov |
| Basin, outside the TPD core, DCo, DMn, DNi, DCd and DCu were enriched | | Basin, outside the TPD core, DCo, DMn, DNi, DCd and DCu were enriched |
| by Pacific waters, whereas DFe seemed diluted. DCo, DFe, DMn and DZn | | by Pacific waters, whereas DFe seemed diluted. DCo, DFe, DMn and DZn |
| were relatively high in the Barents Sea and enriched Atlantic water | | were relatively high in the Barents Sea and enriched Atlantic water |
| going into the Nansen Basin. Deep concentrations of all metals were | | going into the Nansen Basin. Deep concentrations of all metals were |
| significantly lower in the Makarov Basin compared to the Nansen and | | significantly lower in the Makarov Basin compared to the Nansen and |
| Amundsen, the Eurasian, Basins. The Gakkel Ridge hydrothermal input | | Amundsen, the Eurasian, Basins. The Gakkel Ridge hydrothermal input |
| and higher continental slope convection are explanations of higher | | and higher continental slope convection are explanations of higher |
| metal concentrations in the Eurasian Basins. Although scavenging rates | | metal concentrations in the Eurasian Basins. Although scavenging rates |
| are lower in the Makarov Basin compared to the Eurasian Basins, the | | are lower in the Makarov Basin compared to the Eurasian Basins, the |
| residence time is longer and therefore we suggest that scavenging can | | residence time is longer and therefore we suggest that scavenging can |
| decrease the dissolved concentrations with time. This study provides a | | decrease the dissolved concentrations with time. This study provides a |
| baseline to assess future change, and additionally identifies main | | baseline to assess future change, and additionally identifies main |
| processes driving trace metal distributions. Our results underline the | | processes driving trace metal distributions. Our results underline the |
| importance of fluvial input as well as shelf sources and internal | | importance of fluvial input as well as shelf sources and internal |
| cycling, notably scavenging, for the distribution of bio-active metals | | cycling, notably scavenging, for the distribution of bio-active metals |
| in the Arctic Ocean.", | | in the Arctic Ocean.", |
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| } | | } |
| ], | | ], |
| n | "title": "Dissolved Cd, Co, Cu, Fe, Mn, Ni and Zn in the Arctic | n | "title": "Dissolved Cd, Co, Cu, Fe, Mn, Ni, Pb and Zn in the Arctic |
| Ocean", | | Ocean", |
| "type": "dataset", | | "type": "dataset", |
| t | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.jc", | t | "url": "https://doi.org/10.25850/nioz/7b.b.jc", |
| "version": "2" | | "version": "1" |
| } | | } |