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| f | 1 | { | f | 1 | { |
| 2 | "alternate_identifier": "https://doi.org/10.1594/PANGAEA.932797", | 2 | "alternate_identifier": "https://doi.org/10.1594/PANGAEA.932797", | ||
| 3 | "author": "Rob Middag (Royal Netherlands Institute for Sea | 3 | "author": "Rob Middag (Royal Netherlands Institute for Sea | ||
| 4 | Research)", | 4 | Research)", | ||
| 5 | "author_email": "rob.middag@nioz.nl", | 5 | "author_email": "rob.middag@nioz.nl", | ||
| 6 | "code": "7b.b.jc", | 6 | "code": "7b.b.jc", | ||
| 7 | "contributor": "Royal Netherlands Institute for Sea Research | 7 | "contributor": "Royal Netherlands Institute for Sea Research | ||
| 8 | (NIOZ)", | 8 | (NIOZ)", | ||
| 9 | "creator_user_id": "b0e3b75f-a36a-4f96-b150-d3cc47a607cb", | 9 | "creator_user_id": "b0e3b75f-a36a-4f96-b150-d3cc47a607cb", | ||
| 10 | "creators": | 10 | "creators": | ||
| 11 | firstname\":\"Loes\",\"lastname\":\"Gerringa\",\"affiliation\":\"Royal | 11 | firstname\":\"Loes\",\"lastname\":\"Gerringa\",\"affiliation\":\"Royal | ||
| 12 | Netherlands Institute for Sea | 12 | Netherlands Institute for Sea | ||
| 13 | {\"firstname\":\"Rob\",\"lastname\":\"Middag\",\"affiliation\":\"Royal | 13 | {\"firstname\":\"Rob\",\"lastname\":\"Middag\",\"affiliation\":\"Royal | ||
| 14 | Netherlands Institute for Sea | 14 | Netherlands Institute for Sea | ||
| 15 | stname\":\"Micha\",\"lastname\":\"Rijkenberg\",\"affiliation\":\"Royal | 15 | stname\":\"Micha\",\"lastname\":\"Rijkenberg\",\"affiliation\":\"Royal | ||
| 16 | Netherlands Institute for Sea | 16 | Netherlands Institute for Sea | ||
| 17 | "firstname\":\"Hans\",\"lastname\":\"Slagter\",\"affiliation\":\"Royal | 17 | "firstname\":\"Hans\",\"lastname\":\"Slagter\",\"affiliation\":\"Royal | ||
| 18 | Netherlands Institute for Sea | 18 | Netherlands Institute for Sea | ||
| 19 | "firstname\":\"Patrick\",\"lastname\":\"Laan\",\"affiliation\":\"Royal | 19 | "firstname\":\"Patrick\",\"lastname\":\"Laan\",\"affiliation\":\"Royal | ||
| 20 | Netherlands Institute for Sea | 20 | Netherlands Institute for Sea | ||
| 21 | address\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Ronja | 21 | address\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Ronja | ||
| 22 | \",\"lastname\":\"Paffrath\",\"affiliation\":\"3.\\tMarine Isotope | 22 | \",\"lastname\":\"Paffrath\",\"affiliation\":\"3.\\tMarine Isotope | ||
| 23 | Geochemistry, Institute for Chemistry and Biology of the Marine | 23 | Geochemistry, Institute for Chemistry and Biology of the Marine | ||
| 24 | Environment (ICBM), University of Oldenburg, Oldenburg, GermanyRoyal | 24 | Environment (ICBM), University of Oldenburg, Oldenburg, GermanyRoyal | ||
| 25 | Netherlands Institute for Sea | 25 | Netherlands Institute for Sea | ||
| 26 | ress\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Dorothea | 26 | ress\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Dorothea | ||
| 27 | \",\"lastname\":\"Bauch\",\"affiliation\":\"4.\\tLeibniz Laboratory | 27 | \",\"lastname\":\"Bauch\",\"affiliation\":\"4.\\tLeibniz Laboratory | ||
| 28 | for Radiometric Dating and Stable Isotope Research, Kiel University, | 28 | for Radiometric Dating and Stable Isotope Research, Kiel University, | ||
| 29 | Kiel, Germany and GEOMAR Hemholtz Centre for Ocean Research, Kiel, | 29 | Kiel, Germany and GEOMAR Hemholtz Centre for Ocean Research, Kiel, | ||
| 30 | ndingauthor\":false},{\"firstname\":\"Michiel\",\"lastname\":\"Rutgers | 30 | ndingauthor\":false},{\"firstname\":\"Michiel\",\"lastname\":\"Rutgers | ||
| 31 | van der Loeff\",\"affiliation\":\"5.\\tHelmholtz Centre for Polar and | 31 | van der Loeff\",\"affiliation\":\"5.\\tHelmholtz Centre for Polar and | ||
| 32 | Marine Research, Alfred Wegener Institute, Bremerhaven, | 32 | Marine Research, Alfred Wegener Institute, Bremerhaven, | ||
| 33 | 742\",\"contactemailaddress\":\"\",\"iscorrespondingauthor\":false}]", | 33 | 742\",\"contactemailaddress\":\"\",\"iscorrespondingauthor\":false}]", | ||
| 34 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.jc", | 34 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.jc", | ||
| 35 | "dates": | 35 | "dates": | ||
| 36 | -10-14T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"\"}]", | 36 | -10-14T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"\"}]", | ||
| 37 | "deposit_date": "2021-05-20", | 37 | "deposit_date": "2021-05-20", | ||
| 38 | "depositor": "loes gerringa (loes.gerringa@nioz.nl)", | 38 | "depositor": "loes gerringa (loes.gerringa@nioz.nl)", | ||
| 39 | "distribution_date": "2021-05-20", | 39 | "distribution_date": "2021-05-20", | ||
| 40 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 40 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 41 | Institute for Sea Research)", | 41 | Institute for Sea Research)", | ||
| 42 | "doi_date_published": "2021-07-20T08:31:06.0874969", | 42 | "doi_date_published": "2021-07-20T08:31:06.0874969", | ||
| 43 | "funding_references": "[{\"name\":\"NWO\",\"awardnumber\":\" | 43 | "funding_references": "[{\"name\":\"NWO\",\"awardnumber\":\" | ||
| 44 | 822.01.018 \",\"awardtitle\":\"origin and fate of | 44 | 822.01.018 \",\"awardtitle\":\"origin and fate of | ||
| 45 | "name\":\"DFG\",\"awardnumber\":\"BA1689/2-2\",\"awardtitle\":\"\"}]", | 45 | "name\":\"DFG\",\"awardnumber\":\"BA1689/2-2\",\"awardtitle\":\"\"}]", | ||
| 46 | "geographic_coverage": "[{\"place\":\"Arctic | 46 | "geographic_coverage": "[{\"place\":\"Arctic | ||
| 47 | ":\"21.192830\",\"longitude_1\":\"-116.679830\",\"formatted\":\"Arctic | 47 | ":\"21.192830\",\"longitude_1\":\"-116.679830\",\"formatted\":\"Arctic | ||
| 48 | Ocean N: 89.930170 S: 70.999330 E: -116.679830 W: 21.192830\"}]", | 48 | Ocean N: 89.930170 S: 70.999330 E: -116.679830 W: 21.192830\"}]", | ||
| 49 | "groups": [], | 49 | "groups": [], | ||
| 50 | "id": "3a291f18-0efc-440e-9ce9-92e83fd374d8", | 50 | "id": "3a291f18-0efc-440e-9ce9-92e83fd374d8", | ||
| 51 | "isopen": true, | 51 | "isopen": true, | ||
| 52 | "license_id": "CC0-1.0", | 52 | "license_id": "CC0-1.0", | ||
| 53 | "license_title": "CC0 1.0", | 53 | "license_title": "CC0 1.0", | ||
| 54 | "license_url": "https://creativecommons.org/publicdomain/zero/1.0/", | 54 | "license_url": "https://creativecommons.org/publicdomain/zero/1.0/", | ||
| 55 | "maintainer": "loes", | 55 | "maintainer": "loes", | ||
| 56 | "maintainer_email": "loes.gerringa@nioz.nl", | 56 | "maintainer_email": "loes.gerringa@nioz.nl", | ||
| 57 | "metadata_created": "2024-10-22T11:43:27.446667", | 57 | "metadata_created": "2024-10-22T11:43:27.446667", | ||
| t | 58 | "metadata_modified": "2025-05-29T10:47:05.853159", | t | 58 | "metadata_modified": "2025-05-29T10:47:06.655649", |
| 59 | "name": "dissolved-cd", | 59 | "name": "dissolved-cd", | ||
| 60 | "notes": "During the Polarstern (PS94) expedition in summer 2015, | 60 | "notes": "During the Polarstern (PS94) expedition in summer 2015, | ||
| 61 | part of the international GEOTRACES program sources and sinks of | 61 | part of the international GEOTRACES program sources and sinks of | ||
| 62 | dissolved (D) Cd, Co, Cu, Fe, Mn, Ni, Zn and Pb were studied in the | 62 | dissolved (D) Cd, Co, Cu, Fe, Mn, Ni, Zn and Pb were studied in the | ||
| 63 | central Arctic Ocean (with the exception of Pb, described by Gerringa | 63 | central Arctic Ocean (with the exception of Pb, described by Gerringa | ||
| 64 | et al., 2021). In the Polar Surface Water in which the TransPolar | 64 | et al., 2021). In the Polar Surface Water in which the TransPolar | ||
| 65 | Drift (TPD) is situated, salinity and d18O derived fractions indicated | 65 | Drift (TPD) is situated, salinity and d18O derived fractions indicated | ||
| 66 | a distinct riverine source for silicate DCo, DCu, DFe, DMn and DNi. | 66 | a distinct riverine source for silicate DCo, DCu, DFe, DMn and DNi. | ||
| 67 | Linear relationships between DMn and the meteoric fraction depended on | 67 | Linear relationships between DMn and the meteoric fraction depended on | ||
| 68 | the source distance, likely due to Mn-precipitation with transport | 68 | the source distance, likely due to Mn-precipitation with transport | ||
| 69 | time. In the upper 50 m of the Makarov Basin, outside the TPD core, | 69 | time. In the upper 50 m of the Makarov Basin, outside the TPD core, | ||
| 70 | DCo, DMn, DNi, DCd and DCu were enriched by Pacific waters, whereas | 70 | DCo, DMn, DNi, DCd and DCu were enriched by Pacific waters, whereas | ||
| 71 | DFe seemed diluted. DCo, DFe, DMn and DZn were relatively high in the | 71 | DFe seemed diluted. DCo, DFe, DMn and DZn were relatively high in the | ||
| 72 | Barents Sea and enriched Atlantic water going into the Nansen Basin. | 72 | Barents Sea and enriched Atlantic water going into the Nansen Basin. | ||
| 73 | Deep concentrations of all metals were significantly lower in the | 73 | Deep concentrations of all metals were significantly lower in the | ||
| 74 | Makarov Basin compared to the Nansen and Amundsen, the Eurasian, | 74 | Makarov Basin compared to the Nansen and Amundsen, the Eurasian, | ||
| 75 | Basins. The Gakkel Ridge hydrothermal input and higher continental | 75 | Basins. The Gakkel Ridge hydrothermal input and higher continental | ||
| 76 | slope convection are explanations of higher metal concentrations in | 76 | slope convection are explanations of higher metal concentrations in | ||
| 77 | the Eurasian Basins. Although scavenging rates are lower in the | 77 | the Eurasian Basins. Although scavenging rates are lower in the | ||
| 78 | Makarov Basin compared to the Eurasian Basins, the residence time is | 78 | Makarov Basin compared to the Eurasian Basins, the residence time is | ||
| 79 | longer and therefore we suggest that scavenging can decrease the | 79 | longer and therefore we suggest that scavenging can decrease the | ||
| 80 | dissolved concentrations with time. This study provides a baseline to | 80 | dissolved concentrations with time. This study provides a baseline to | ||
| 81 | assess future change, and additionally identifies main processes | 81 | assess future change, and additionally identifies main processes | ||
| 82 | driving trace metal distributions. Our results underline the | 82 | driving trace metal distributions. Our results underline the | ||
| 83 | importance of fluvial input as well as shelf sources and internal | 83 | importance of fluvial input as well as shelf sources and internal | ||
| 84 | cycling, notably scavenging, for the distribution of bio-active metals | 84 | cycling, notably scavenging, for the distribution of bio-active metals | ||
| 85 | in the Arctic Ocean.", | 85 | in the Arctic Ocean.", | ||
| 86 | "num_resources": 2, | 86 | "num_resources": 2, | ||
| 87 | "num_tags": 22, | 87 | "num_tags": 22, | ||
| 88 | "organization": { | 88 | "organization": { | ||
| 89 | "approval_status": "approved", | 89 | "approval_status": "approved", | ||
| 90 | "created": "2024-10-22T06:06:56.074257", | 90 | "created": "2024-10-22T06:06:56.074257", | ||
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| 96 | "name": "nioz", | 96 | "name": "nioz", | ||
| 97 | "state": "active", | 97 | "state": "active", | ||
| 98 | "title": "Royal Netherlands Institute for Sea Research", | 98 | "title": "Royal Netherlands Institute for Sea Research", | ||
| 99 | "type": "organization" | 99 | "type": "organization" | ||
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| 103 | "production_date": "2021-07-20", | 103 | "production_date": "2021-07-20", | ||
| 104 | "related_identifier": "DOI: 10.1029/2021JC017323", | 104 | "related_identifier": "DOI: 10.1029/2021JC017323", | ||
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| 239 | }, | 239 | }, | ||
| 240 | { | 240 | { | ||
| 241 | "display_name": "cu", | 241 | "display_name": "cu", | ||
| 242 | "id": "5114f8d2-fb60-4c0a-bfc2-c06e4a0862a0", | 242 | "id": "5114f8d2-fb60-4c0a-bfc2-c06e4a0862a0", | ||
| 243 | "name": "cu", | 243 | "name": "cu", | ||
| 244 | "state": "active", | 244 | "state": "active", | ||
| 245 | "vocabulary_id": null | 245 | "vocabulary_id": null | ||
| 246 | }, | 246 | }, | ||
| 247 | { | 247 | { | ||
| 248 | "display_name": "dissolved", | 248 | "display_name": "dissolved", | ||
| 249 | "id": "dcc1d919-d84c-44f9-b5d1-145035cbeeee", | 249 | "id": "dcc1d919-d84c-44f9-b5d1-145035cbeeee", | ||
| 250 | "name": "dissolved", | 250 | "name": "dissolved", | ||
| 251 | "state": "active", | 251 | "state": "active", | ||
| 252 | "vocabulary_id": null | 252 | "vocabulary_id": null | ||
| 253 | }, | 253 | }, | ||
| 254 | { | 254 | { | ||
| 255 | "display_name": "fe", | 255 | "display_name": "fe", | ||
| 256 | "id": "21cbc5e9-20db-4efe-bc96-224407d8cfcb", | 256 | "id": "21cbc5e9-20db-4efe-bc96-224407d8cfcb", | ||
| 257 | "name": "fe", | 257 | "name": "fe", | ||
| 258 | "state": "active", | 258 | "state": "active", | ||
| 259 | "vocabulary_id": null | 259 | "vocabulary_id": null | ||
| 260 | }, | 260 | }, | ||
| 261 | { | 261 | { | ||
| 262 | "display_name": "geotraces", | 262 | "display_name": "geotraces", | ||
| 263 | "id": "be5c4b60-9551-425f-82b0-b1e952ba6d7d", | 263 | "id": "be5c4b60-9551-425f-82b0-b1e952ba6d7d", | ||
| 264 | "name": "geotraces", | 264 | "name": "geotraces", | ||
| 265 | "state": "active", | 265 | "state": "active", | ||
| 266 | "vocabulary_id": null | 266 | "vocabulary_id": null | ||
| 267 | }, | 267 | }, | ||
| 268 | { | 268 | { | ||
| 269 | "display_name": "mn", | 269 | "display_name": "mn", | ||
| 270 | "id": "d0f4bcd7-6687-4707-bd6a-e8be961ce764", | 270 | "id": "d0f4bcd7-6687-4707-bd6a-e8be961ce764", | ||
| 271 | "name": "mn", | 271 | "name": "mn", | ||
| 272 | "state": "active", | 272 | "state": "active", | ||
| 273 | "vocabulary_id": null | 273 | "vocabulary_id": null | ||
| 274 | }, | 274 | }, | ||
| 275 | { | 275 | { | ||
| 276 | "display_name": "ni", | 276 | "display_name": "ni", | ||
| 277 | "id": "3462881b-661e-431a-ac21-66dd155082a4", | 277 | "id": "3462881b-661e-431a-ac21-66dd155082a4", | ||
| 278 | "name": "ni", | 278 | "name": "ni", | ||
| 279 | "state": "active", | 279 | "state": "active", | ||
| 280 | "vocabulary_id": null | 280 | "vocabulary_id": null | ||
| 281 | }, | 281 | }, | ||
| 282 | { | 282 | { | ||
| 283 | "display_name": "pb", | 283 | "display_name": "pb", | ||
| 284 | "id": "eb4f07e7-fc10-4651-95e2-dde2890b14d3", | 284 | "id": "eb4f07e7-fc10-4651-95e2-dde2890b14d3", | ||
| 285 | "name": "pb", | 285 | "name": "pb", | ||
| 286 | "state": "active", | 286 | "state": "active", | ||
| 287 | "vocabulary_id": null | 287 | "vocabulary_id": null | ||
| 288 | }, | 288 | }, | ||
| 289 | { | 289 | { | ||
| 290 | "display_name": "ps94", | 290 | "display_name": "ps94", | ||
| 291 | "id": "6394f414-e9f2-4141-a422-a451b5869ed4", | 291 | "id": "6394f414-e9f2-4141-a422-a451b5869ed4", | ||
| 292 | "name": "ps94", | 292 | "name": "ps94", | ||
| 293 | "state": "active", | 293 | "state": "active", | ||
| 294 | "vocabulary_id": null | 294 | "vocabulary_id": null | ||
| 295 | }, | 295 | }, | ||
| 296 | { | 296 | { | ||
| 297 | "display_name": "trace metals", | 297 | "display_name": "trace metals", | ||
| 298 | "id": "e8e69e11-d555-4cc7-8c04-f582de3e5c23", | 298 | "id": "e8e69e11-d555-4cc7-8c04-f582de3e5c23", | ||
| 299 | "name": "trace metals", | 299 | "name": "trace metals", | ||
| 300 | "state": "active", | 300 | "state": "active", | ||
| 301 | "vocabulary_id": null | 301 | "vocabulary_id": null | ||
| 302 | }, | 302 | }, | ||
| 303 | { | 303 | { | ||
| 304 | "display_name": "zn", | 304 | "display_name": "zn", | ||
| 305 | "id": "2c06263a-ec16-4341-befc-d9b6b506264e", | 305 | "id": "2c06263a-ec16-4341-befc-d9b6b506264e", | ||
| 306 | "name": "zn", | 306 | "name": "zn", | ||
| 307 | "state": "active", | 307 | "state": "active", | ||
| 308 | "vocabulary_id": null | 308 | "vocabulary_id": null | ||
| 309 | } | 309 | } | ||
| 310 | ], | 310 | ], | ||
| 311 | "title": "Dissolved Cd, Co, Cu, Fe, Mn, Ni, Pb and Zn in the Arctic | 311 | "title": "Dissolved Cd, Co, Cu, Fe, Mn, Ni, Pb and Zn in the Arctic | ||
| 312 | Ocean", | 312 | Ocean", | ||
| 313 | "type": "dataset", | 313 | "type": "dataset", | ||
| 314 | "url": "https://doi.org/10.25850/nioz/7b.b.jc", | 314 | "url": "https://doi.org/10.25850/nioz/7b.b.jc", | ||
| 315 | "version": "1" | 315 | "version": "1" | ||
| 316 | } | 316 | } |