Changes
On May 22, 2025, 1:27:39 PM UTC,
-
Added resource Data_PS117_Cd_Zn_iso.csv to Trace Metals Amundsen Sea Araon ANA08B and Weddell Sea PS117
| f | 1 | { | f | 1 | { |
| 2 | "author": "Rob Middag (Royal Netherlands Institute for Sea | 2 | "author": "Rob Middag (Royal Netherlands Institute for Sea | ||
| 3 | Research)", | 3 | Research)", | ||
| 4 | "author_email": "rob.middag@nioz.nl", | 4 | "author_email": "rob.middag@nioz.nl", | ||
| 5 | "code": "7b.b.bd", | 5 | "code": "7b.b.bd", | ||
| 6 | "contributor": "Royal Netherlands Institute for Sea Research | 6 | "contributor": "Royal Netherlands Institute for Sea Research | ||
| 7 | (NIOZ)", | 7 | (NIOZ)", | ||
| 8 | "creator_user_id": "880d6d71-36e9-4ad8-b385-61c0f365121c", | 8 | "creator_user_id": "880d6d71-36e9-4ad8-b385-61c0f365121c", | ||
| 9 | "creators": | 9 | "creators": | ||
| 10 | ":\"Middag\",\"orcid\":\"0000-0002-3326-530X\",\"affiliation\":\"Royal | 10 | ":\"Middag\",\"orcid\":\"0000-0002-3326-530X\",\"affiliation\":\"Royal | ||
| 11 | Netherlands Institute for Sea | 11 | Netherlands Institute for Sea | ||
| 12 | rue,\"contactemailaddress\":\"rob.middag@nioz.nl\",\"formatted\":\"Rob | 12 | rue,\"contactemailaddress\":\"rob.middag@nioz.nl\",\"formatted\":\"Rob | ||
| 13 | Middag - Royal Netherlands Institute for Sea Research - ORCID: | 13 | Middag - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 14 | 0000-0002-3326-530X - Corresponding Author - | 14 | 0000-0002-3326-530X - Corresponding Author - | ||
| 15 | rob.middag@nioz.nl\"},{\"firstname\":\"Mathijs\",\"lastname\":\"van | 15 | rob.middag@nioz.nl\"},{\"firstname\":\"Mathijs\",\"lastname\":\"van | ||
| 16 | Manen\",\"orcid\":\"0000-0002-6016-9161\",\"affiliation\":\"Royal | 16 | Manen\",\"orcid\":\"0000-0002-6016-9161\",\"affiliation\":\"Royal | ||
| 17 | Netherlands Institute for Sea | 17 | Netherlands Institute for Sea | ||
| 18 | dingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Mathijs | 18 | dingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Mathijs | ||
| 19 | van Manen - Royal Netherlands Institute for Sea Research - ORCID: | 19 | van Manen - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 20 | e\":\"Tian\",\"orcid\":\"0000-0001-5778-5273\",\"affiliation\":\"Royal | 20 | e\":\"Tian\",\"orcid\":\"0000-0001-5778-5273\",\"affiliation\":\"Royal | ||
| 21 | Netherlands Institute for Sea | 21 | Netherlands Institute for Sea | ||
| 22 | dingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Hung-An | 22 | dingauthor\":null,\"contactemailaddress\":null,\"formatted\":\"Hung-An | ||
| 23 | Tian - Royal Netherlands Institute for Sea Research - ORCID: | 23 | Tian - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 24 | e\":\"Laan\",\"orcid\":\"0000-0001-5115-6070\",\"affiliation\":\"Royal | 24 | e\":\"Laan\",\"orcid\":\"0000-0001-5115-6070\",\"affiliation\":\"Royal | ||
| 25 | Netherlands Institute for Sea | 25 | Netherlands Institute for Sea | ||
| 26 | arch\",\"iscorrespondingauthor\":null,\"contactemailaddress\":null}]", | 26 | arch\",\"iscorrespondingauthor\":null,\"contactemailaddress\":null}]", | ||
| 27 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.bd", | 27 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.bd", | ||
| 28 | "dates": "[{\"datefrom\":\"2017-12-27 | 28 | "dates": "[{\"datefrom\":\"2017-12-27 | ||
| 29 | 00:00:00.000\",\"dateto\":\"2018-02-02 | 29 | 00:00:00.000\",\"dateto\":\"2018-02-02 | ||
| 30 | 00:00:00.000\",\"type\":\"collected\",\"information\":\"Sampling | 30 | 00:00:00.000\",\"type\":\"collected\",\"information\":\"Sampling | ||
| 31 | during expedition ANA08B\",\"formatted\":\"collected from: 27/12/2017 | 31 | during expedition ANA08B\",\"formatted\":\"collected from: 27/12/2017 | ||
| 32 | to: 02/02/2018 Sampling during expedition | 32 | to: 02/02/2018 Sampling during expedition | ||
| 33 | ANA08B\"},{\"datefrom\":\"2018-12-26 | 33 | ANA08B\"},{\"datefrom\":\"2018-12-26 | ||
| 34 | 00:00:00.000\",\"dateto\":\"2019-02-01 | 34 | 00:00:00.000\",\"dateto\":\"2019-02-01 | ||
| 35 | 00:00:00.000\",\"type\":\"collected\",\"information\":\"Sampling | 35 | 00:00:00.000\",\"type\":\"collected\",\"information\":\"Sampling | ||
| 36 | during expedition PS117\",\"formatted\":\"collected from: 26/12/2018 | 36 | during expedition PS117\",\"formatted\":\"collected from: 26/12/2018 | ||
| 37 | to: 01/02/2019 Sampling during expedition PS117\"}]", | 37 | to: 01/02/2019 Sampling during expedition PS117\"}]", | ||
| 38 | "deposit_date": "2022-09-07", | 38 | "deposit_date": "2022-09-07", | ||
| 39 | "depositor": "Rob Middag (rob.middag@nioz.nl)", | 39 | "depositor": "Rob Middag (rob.middag@nioz.nl)", | ||
| 40 | "distribution_date": "2022-09-07", | 40 | "distribution_date": "2022-09-07", | ||
| 41 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 41 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 42 | Institute for Sea Research)", | 42 | Institute for Sea Research)", | ||
| 43 | "doi_date_published": "2022-09-15T11:29:11.1587333", | 43 | "doi_date_published": "2022-09-15T11:29:11.1587333", | ||
| 44 | "funding_references": "[{\"name\":\"NWO\",\"awardnumber\":\" | 44 | "funding_references": "[{\"name\":\"NWO\",\"awardnumber\":\" | ||
| 45 | ALWPP.2016.020\",\"awardtitle\":\"Iron limitation and viral lysis, | 45 | ALWPP.2016.020\",\"awardtitle\":\"Iron limitation and viral lysis, | ||
| 46 | phytoplankton caught between a rock and a hard | 46 | phytoplankton caught between a rock and a hard | ||
| 47 | place\",\"formatted\":\"NWO - ALWPP.2016.020 - Iron limitation and | 47 | place\",\"formatted\":\"NWO - ALWPP.2016.020 - Iron limitation and | ||
| 48 | viral lysis, phytoplankton caught between a rock and a hard | 48 | viral lysis, phytoplankton caught between a rock and a hard | ||
| 49 | awardnumber\":\"AWI_PS117_02\",\"awardtitle\":null,\"formatted\":\"AWI | 49 | awardnumber\":\"AWI_PS117_02\",\"awardtitle\":null,\"formatted\":\"AWI | ||
| 50 | - AWI_PS117_02 -\"}]", | 50 | - AWI_PS117_02 -\"}]", | ||
| 51 | "geographic_coverage": "[{\"place\":\"Amundsen | 51 | "geographic_coverage": "[{\"place\":\"Amundsen | ||
| 52 | null,\"longitude_2\":null,\"latitude_1\":null,\"formatted\":\"Amundsen | 52 | null,\"longitude_2\":null,\"latitude_1\":null,\"formatted\":\"Amundsen | ||
| 53 | Sea N: S: E: W:\"},{\"place\":\"Weddell | 53 | Sea N: S: E: W:\"},{\"place\":\"Weddell | ||
| 54 | "longitude_2\":\"-55\",\"longitude_1\":\"0.5\",\"formatted\":\"Weddell | 54 | "longitude_2\":\"-55\",\"longitude_1\":\"0.5\",\"formatted\":\"Weddell | ||
| 55 | Sea N: -59 S: -70.5 E: 0.5 W: -55\"}]", | 55 | Sea N: -59 S: -70.5 E: 0.5 W: -55\"}]", | ||
| 56 | "groups": [], | 56 | "groups": [], | ||
| 57 | "id": "19b81cc4-2d8e-431c-90a5-678b8b93d4da", | 57 | "id": "19b81cc4-2d8e-431c-90a5-678b8b93d4da", | ||
| 58 | "isopen": true, | 58 | "isopen": true, | ||
| 59 | "license_id": "CC-BY-4.0", | 59 | "license_id": "CC-BY-4.0", | ||
| 60 | "license_title": "Creative Commons Attribution 4.0", | 60 | "license_title": "Creative Commons Attribution 4.0", | ||
| 61 | "license_url": "https://creativecommons.org/licenses/by/4.0/", | 61 | "license_url": "https://creativecommons.org/licenses/by/4.0/", | ||
| 62 | "maintainer": "Rob", | 62 | "maintainer": "Rob", | ||
| 63 | "maintainer_email": "rob.middag@nioz.nl", | 63 | "maintainer_email": "rob.middag@nioz.nl", | ||
| 64 | "metadata_created": "2024-10-22T11:46:43.174734", | 64 | "metadata_created": "2024-10-22T11:46:43.174734", | ||
| n | 65 | "metadata_modified": "2025-05-22T13:27:23.727844", | n | 65 | "metadata_modified": "2025-05-22T13:27:38.962069", |
| 66 | "name": | 66 | "name": | ||
| 67 | "trace-metals-amundsen-sea-araon-ana08b-and-weddell-sea-ps117", | 67 | "trace-metals-amundsen-sea-araon-ana08b-and-weddell-sea-ps117", | ||
| 68 | "notes": "Amundsen ANA08B: Samples were collected onboard the South | 68 | "notes": "Amundsen ANA08B: Samples were collected onboard the South | ||
| 69 | Korean icebreaker RV Araon during the ANA08B research expedition to | 69 | Korean icebreaker RV Araon during the ANA08B research expedition to | ||
| 70 | the Amundsen Sea in the austral summer of 2017/2018. The sampling | 70 | the Amundsen Sea in the austral summer of 2017/2018. The sampling | ||
| 71 | period spanned from the 24th of January to the 2nd of February 2018. A | 71 | period spanned from the 24th of January to the 2nd of February 2018. A | ||
| 72 | total of 10 full depth stations were investigated with a maximum of 12 | 72 | total of 10 full depth stations were investigated with a maximum of 12 | ||
| 73 | sampling depths. The transect followed the in- and outflow of CDW in | 73 | sampling depths. The transect followed the in- and outflow of CDW in | ||
| 74 | the ASP through a trough near the Dotson ice shelf. The ASP was | 74 | the ASP through a trough near the Dotson ice shelf. The ASP was | ||
| 75 | surrounded by sea ice at the start of the sampling campaign, whereas | 75 | surrounded by sea ice at the start of the sampling campaign, whereas | ||
| 76 | the polynya had started to open to the open ocean on the northwest | 76 | the polynya had started to open to the open ocean on the northwest | ||
| 77 | side by the end of sampling. Along this transect, station 53 was | 77 | side by the end of sampling. Along this transect, station 53 was | ||
| 78 | located off the shelf and outside the polynya in the marginal sea ice | 78 | located off the shelf and outside the polynya in the marginal sea ice | ||
| 79 | zone, station 52 was located near the outermost edge of the polynya at | 79 | zone, station 52 was located near the outermost edge of the polynya at | ||
| 80 | the shelf break, stations 42 and 36 were located at the Dotson Ice | 80 | the shelf break, stations 42 and 36 were located at the Dotson Ice | ||
| 81 | Shelf front on the in -and outflow side respectively, and the | 81 | Shelf front on the in -and outflow side respectively, and the | ||
| 82 | remaining stations were located in the central open water body of the | 82 | remaining stations were located in the central open water body of the | ||
| 83 | ASP. Water was collected with the \u2018Titan\u2019 ultraclean CTD | 83 | ASP. Water was collected with the \u2018Titan\u2019 ultraclean CTD | ||
| 84 | sampling system for trace metals mounted with pristine large volume | 84 | sampling system for trace metals mounted with pristine large volume | ||
| 85 | samplers. To prevent light shock of phytoplankton, the original PVDF | 85 | samplers. To prevent light shock of phytoplankton, the original PVDF | ||
| 86 | samplers were replaced by a light-proof version of the Pristine | 86 | samplers were replaced by a light-proof version of the Pristine | ||
| 87 | samplers and were made from polypropylene. The salinity | 87 | samplers and were made from polypropylene. The salinity | ||
| 88 | (conductivity), temperature, fluorescence, depth (pressure) and oxygen | 88 | (conductivity), temperature, fluorescence, depth (pressure) and oxygen | ||
| 89 | were measured with a CTD (Seabird SBE 911+) mounted on the trace metal | 89 | were measured with a CTD (Seabird SBE 911+) mounted on the trace metal | ||
| 90 | clean sampling system of NIOZ. The sampling system was deployed on a | 90 | clean sampling system of NIOZ. The sampling system was deployed on a | ||
| 91 | 11 mm Dyneema cable without internal conductive wires and therefore an | 91 | 11 mm Dyneema cable without internal conductive wires and therefore an | ||
| 92 | SBE 17 plus V2 Searam in a titanium housing provided power, saved the | 92 | SBE 17 plus V2 Searam in a titanium housing provided power, saved the | ||
| 93 | CTD data and closed the sampling bottles at pre-programmed depths. | 93 | CTD data and closed the sampling bottles at pre-programmed depths. | ||
| 94 | After deployment, the complete CTD sampling system was placed in a | 94 | After deployment, the complete CTD sampling system was placed in a | ||
| 95 | cleanroom environment inside a modified high cube shipping container | 95 | cleanroom environment inside a modified high cube shipping container | ||
| 96 | and subsamples were collected.\n\nWeddell Sea PS117: Samples were | 96 | and subsamples were collected.\n\nWeddell Sea PS117: Samples were | ||
| 97 | collected on board the German icebreaker RV Polarstern during the | 97 | collected on board the German icebreaker RV Polarstern during the | ||
| 98 | PS117 research expedition to the Weddell Sea in the austral summer of | 98 | PS117 research expedition to the Weddell Sea in the austral summer of | ||
| 99 | 2018/2019. The sampling period spanned from the 26th of January to the | 99 | 2018/2019. The sampling period spanned from the 26th of January to the | ||
| 100 | 1st of February 2019. A total of 23 (semi)full depth stations were | 100 | 1st of February 2019. A total of 23 (semi)full depth stations were | ||
| 101 | taken with a maximum of 20 sampling depths. Samples for trace metals | 101 | taken with a maximum of 20 sampling depths. Samples for trace metals | ||
| 102 | were collected along the prime meridian (0\u00b0 W) transect in | 102 | were collected along the prime meridian (0\u00b0 W) transect in | ||
| 103 | December/January 2018-2019 at 8 stations. Northernmost station 22 is | 103 | December/January 2018-2019 at 8 stations. Northernmost station 22 is | ||
| 104 | located at 59\u00b0S and southernmost station 30 at 69.37\u00b0 S. | 104 | located at 59\u00b0S and southernmost station 30 at 69.37\u00b0 S. | ||
| 105 | Additionally, 4 stations were samples near the ice sheet and in the | 105 | Additionally, 4 stations were samples near the ice sheet and in the | ||
| 106 | Weddell Basin that were not along a transect. Due to the | 106 | Weddell Basin that were not along a transect. Due to the | ||
| 107 | malfunctioning sampling system, deepest depths were not sampled | 107 | malfunctioning sampling system, deepest depths were not sampled | ||
| 108 | correctly and can therefore not be used in the analysis. Along the | 108 | correctly and can therefore not be used in the analysis. Along the | ||
| 109 | Weddell Sea transect a total of 11 trace metal stations, of which 6 | 109 | Weddell Sea transect a total of 11 trace metal stations, of which 6 | ||
| 110 | full depth, were sampled in January/February 2019. The transect starts | 110 | full depth, were sampled in January/February 2019. The transect starts | ||
| 111 | in the Weddell Sea basin at station 61 (45.8\u00b0W) and followed the | 111 | in the Weddell Sea basin at station 61 (45.8\u00b0W) and followed the | ||
| 112 | continental slope towards the West-Antarctic peninsula where the shelf | 112 | continental slope towards the West-Antarctic peninsula where the shelf | ||
| 113 | station 95 was closest to the continent (54.5\u00b0 W).\nWater was | 113 | station 95 was closest to the continent (54.5\u00b0 W).\nWater was | ||
| 114 | collected with the \u2018Titan\u2019 ultraclean CTD sampling system | 114 | collected with the \u2018Titan\u2019 ultraclean CTD sampling system | ||
| 115 | for trace metals mounted with pristine large volume samplers. To | 115 | for trace metals mounted with pristine large volume samplers. To | ||
| 116 | prevent light shock of phytoplankton, the original PVDF samplers were | 116 | prevent light shock of phytoplankton, the original PVDF samplers were | ||
| 117 | replaced by a light-proof version of the Pristine samplers and were | 117 | replaced by a light-proof version of the Pristine samplers and were | ||
| 118 | made from polypropylene. The salinity (conductivity), temperature, | 118 | made from polypropylene. The salinity (conductivity), temperature, | ||
| 119 | fluorescence, depth (pressure) and oxygen were measured with a CTD | 119 | fluorescence, depth (pressure) and oxygen were measured with a CTD | ||
| 120 | (Seabird SBE 911+) mounted on the trace metal clean sampling system of | 120 | (Seabird SBE 911+) mounted on the trace metal clean sampling system of | ||
| 121 | NIOZ. The sampling system was deployed on a 11 mm Dyneema cable | 121 | NIOZ. The sampling system was deployed on a 11 mm Dyneema cable | ||
| 122 | without internal conductive wires and therefore an SBE 17 plus V2 | 122 | without internal conductive wires and therefore an SBE 17 plus V2 | ||
| 123 | Searam in a titanium housing provided power, saved the CTD data and | 123 | Searam in a titanium housing provided power, saved the CTD data and | ||
| 124 | closed the sampling bottles at pre-programmed depths. After | 124 | closed the sampling bottles at pre-programmed depths. After | ||
| 125 | deployment, the complete CTD sampling system was placed in a cleanroom | 125 | deployment, the complete CTD sampling system was placed in a cleanroom | ||
| 126 | environment inside a modified high cube shipping container and | 126 | environment inside a modified high cube shipping container and | ||
| 127 | subsamples were collected.", | 127 | subsamples were collected.", | ||
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| 147 | "https://doi.org/10.1016/j.marchem.2022.104161; | 147 | "https://doi.org/10.1016/j.marchem.2022.104161; | ||
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| 149 | https://doi.org/10.1016/j.gca.2023.10.029; | 149 | https://doi.org/10.1016/j.gca.2023.10.029; | ||
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| 177 | "state": "active", | 199 | "state": "active", | ||
| 178 | "subject": "Earth and Environmental Sciences", | 200 | "subject": "Earth and Environmental Sciences", | ||
| 179 | "tags": [ | 201 | "tags": [ | ||
| 180 | { | 202 | { | ||
| 181 | "display_name": "Trace Metals Amundsen Sea", | 203 | "display_name": "Trace Metals Amundsen Sea", | ||
| 182 | "id": "f172a774-5f58-430c-a1c4-783bb6db7548", | 204 | "id": "f172a774-5f58-430c-a1c4-783bb6db7548", | ||
| 183 | "name": "Trace Metals Amundsen Sea", | 205 | "name": "Trace Metals Amundsen Sea", | ||
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| 185 | "vocabulary_id": null | 207 | "vocabulary_id": null | ||
| 186 | } | 208 | } | ||
| 187 | ], | 209 | ], | ||
| 188 | "title": "Trace Metals Amundsen Sea Araon ANA08B and Weddell Sea | 210 | "title": "Trace Metals Amundsen Sea Araon ANA08B and Weddell Sea | ||
| 189 | PS117", | 211 | PS117", | ||
| 190 | "type": "dataset", | 212 | "type": "dataset", | ||
| 191 | "url": "https://doi.org/10.25850/nioz/7b.b.bd", | 213 | "url": "https://doi.org/10.25850/nioz/7b.b.bd", | ||
| 192 | "version": "1" | 214 | "version": "1" | ||
| 193 | } | 215 | } |