Changes
On October 22, 2024, 9:40:20 AM UTC,
-
Changed the version of Sediment pore water nutrient profiles in Portuguese marine canyons to 4 (previously 3)
| f | 1 | { | f | 1 | { |
| 2 | "author": null, | 2 | "author": null, | ||
| 3 | "author_email": null, | 3 | "author_email": null, | ||
| 4 | "code": "7b.b.p", | 4 | "code": "7b.b.p", | ||
| 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | ||
| 6 | "creator_user_id": "75e1c58d-86c0-45e7-9ed1-17838cc9f463", | 6 | "creator_user_id": "75e1c58d-86c0-45e7-9ed1-17838cc9f463", | ||
| 7 | "creators": | 7 | "creators": | ||
| 8 | \"firstname\":\"Eric\",\"lastname\":\"Epping\",\"affiliation\":\"Royal | 8 | \"firstname\":\"Eric\",\"lastname\":\"Epping\",\"affiliation\":\"Royal | ||
| 9 | Netherlands Institute for Sea | 9 | Netherlands Institute for Sea | ||
| 10 | iladdress\":\"eric.epping@nioz.nl\",\"iscorrespondingauthor\":true}]", | 10 | iladdress\":\"eric.epping@nioz.nl\",\"iscorrespondingauthor\":true}]", | ||
| 11 | "dataset_persistent_id": "DOI:10.33591/nioz/7b.b.p", | 11 | "dataset_persistent_id": "DOI:10.33591/nioz/7b.b.p", | ||
| 12 | "dates": | 12 | "dates": | ||
| 13 | 004-05-13T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"Leg | 13 | 004-05-13T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"Leg | ||
| 14 | period 1\"}]", | 14 | period 1\"}]", | ||
| 15 | "deposit_date": "2019-07-19", | 15 | "deposit_date": "2019-07-19", | ||
| 16 | "depositor": "Wim Pool", | 16 | "depositor": "Wim Pool", | ||
| 17 | "distribution_date": "2019-07-19", | 17 | "distribution_date": "2019-07-19", | ||
| 18 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 18 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 19 | Institute for Sea Research)", | 19 | Institute for Sea Research)", | ||
| n | n | 20 | "doi_date_published": "2019-07-19", | ||
| 20 | "funding_references": | 21 | "funding_references": | ||
| 21 | "[{\"name\":\"EU\",\"awardnumber\":\"\",\"awardtitle\":\"Canyons | 22 | "[{\"name\":\"EU\",\"awardnumber\":\"\",\"awardtitle\":\"Canyons | ||
| 22 | 2004\"}]", | 23 | 2004\"}]", | ||
| 23 | "geographic_coverage": "[{\"place\":\"Mediterranean and Atlantic | 24 | "geographic_coverage": "[{\"place\":\"Mediterranean and Atlantic | ||
| 24 | Iberian | 25 | Iberian | ||
| 25 | \"\",\"longitude_1\":\"\",\"latitude_2\":\"\",\"longitude_2\":\"\"}]", | 26 | \"\",\"longitude_1\":\"\",\"latitude_2\":\"\",\"longitude_2\":\"\"}]", | ||
| 26 | "groups": [], | 27 | "groups": [], | ||
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| 28 | "isopen": false, | 29 | "isopen": false, | ||
| 29 | "license_title": null, | 30 | "license_title": null, | ||
| 30 | "maintainer": null, | 31 | "maintainer": null, | ||
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| 32 | "metadata_created": "2024-10-22T09:40:16.034981", | 33 | "metadata_created": "2024-10-22T09:40:16.034981", | ||
| n | 33 | "metadata_modified": "2024-10-22T09:40:19.677851", | n | 34 | "metadata_modified": "2024-10-22T09:40:20.019052", |
| 34 | "name": "7bbp", | 35 | "name": "7bbp", | ||
| 35 | "notes": "Shelf morphology and local hydrodynamical conditions may | 36 | "notes": "Shelf morphology and local hydrodynamical conditions may | ||
| 36 | significantly influence the partitioning of material (terrestrial or | 37 | significantly influence the partitioning of material (terrestrial or | ||
| 37 | in situ production) between shelf sediments (0-200 m) and the deeper | 38 | in situ production) between shelf sediments (0-200 m) and the deeper | ||
| 38 | ocean margin sediments (200-2000 m). Submarine canyons are typical | 39 | ocean margin sediments (200-2000 m). Submarine canyons are typical | ||
| 39 | morphological features of the rather narrow Iberian shelf. They have | 40 | morphological features of the rather narrow Iberian shelf. They have | ||
| 40 | been shown to trap and transport material from the shelf to the abyss. | 41 | been shown to trap and transport material from the shelf to the abyss. | ||
| 41 | During the OMEX cruise in 1999 the relative contribution of canyons in | 42 | During the OMEX cruise in 1999 the relative contribution of canyons in | ||
| 42 | off-shelf transport was studied by comparing sediment carbon budgets | 43 | off-shelf transport was studied by comparing sediment carbon budgets | ||
| 43 | for the Nazar?? Canyon and for ???normal??? shelf-slope-abyssal | 44 | for the Nazar?? Canyon and for ???normal??? shelf-slope-abyssal | ||
| 44 | transects. In this study, three different canyon-shelf systems were | 45 | transects. In this study, three different canyon-shelf systems were | ||
| 45 | compared, Setubal and Nazar?? Canyons on the Iberian Margin and Cap de | 46 | compared, Setubal and Nazar?? Canyons on the Iberian Margin and Cap de | ||
| 46 | Cr??us Canyon in the Gulf of Lyon.", | 47 | Cr??us Canyon in the Gulf of Lyon.", | ||
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| 50 | "approval_status": "approved", | 51 | "approval_status": "approved", | ||
| 51 | "created": "2024-10-22T06:06:56.074257", | 52 | "created": "2024-10-22T06:06:56.074257", | ||
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| 57 | "name": "nioz", | 58 | "name": "nioz", | ||
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| 59 | "title": "Royal Netherlands Institute for Sea Research", | 60 | "title": "Royal Netherlands Institute for Sea Research", | ||
| 60 | "type": "organization" | 61 | "type": "organization" | ||
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| 134 | "state": "active", | 136 | "state": "active", | ||
| 135 | "subject": "Earth and Environmental Sciences", | 137 | "subject": "Earth and Environmental Sciences", | ||
| 136 | "tags": [ | 138 | "tags": [ | ||
| 137 | { | 139 | { | ||
| 138 | "display_name": "Shelf - deep sea exchange", | 140 | "display_name": "Shelf - deep sea exchange", | ||
| 139 | "id": "5273d868-0e9c-446e-8201-132971e13c87", | 141 | "id": "5273d868-0e9c-446e-8201-132971e13c87", | ||
| 140 | "name": "Shelf - deep sea exchange", | 142 | "name": "Shelf - deep sea exchange", | ||
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| 142 | "vocabulary_id": null | 144 | "vocabulary_id": null | ||
| 143 | } | 145 | } | ||
| 144 | ], | 146 | ], | ||
| 145 | "title": "Sediment pore water nutrient profiles in Portuguese marine | 147 | "title": "Sediment pore water nutrient profiles in Portuguese marine | ||
| 146 | canyons", | 148 | canyons", | ||
| 147 | "type": "dataset", | 149 | "type": "dataset", | ||
| 148 | "url": "https://dataportal.nioz.nl/doi/10.33591/nioz/7b.b.p", | 150 | "url": "https://dataportal.nioz.nl/doi/10.33591/nioz/7b.b.p", | ||
| t | 149 | "version": "3" | t | 151 | "version": "4" |
| 150 | } | 152 | } |