Changes
On October 22, 2024, 9:40:17 AM UTC,
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Added resource pore water nutrients.xls to Nutrient pore water profiles in Portuguese marine canyons
| 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)", | ||
| 20 | "funding_references": | 20 | "funding_references": | ||
| 21 | "[{\"name\":\"EU\",\"awardnumber\":\"\",\"awardtitle\":\"Canyons | 21 | "[{\"name\":\"EU\",\"awardnumber\":\"\",\"awardtitle\":\"Canyons | ||
| 22 | 2004\"}]", | 22 | 2004\"}]", | ||
| 23 | "geographic_coverage": "[{\"place\":\"Mediterranean and Atlantic | 23 | "geographic_coverage": "[{\"place\":\"Mediterranean and Atlantic | ||
| 24 | Iberian | 24 | Iberian | ||
| 25 | \"\",\"longitude_1\":\"\",\"latitude_2\":\"\",\"longitude_2\":\"\"}]", | 25 | \"\",\"longitude_1\":\"\",\"latitude_2\":\"\",\"longitude_2\":\"\"}]", | ||
| 26 | "groups": [], | 26 | "groups": [], | ||
| 27 | "id": "4eaf6522-f548-4abf-b84e-42d63aa2ecc5", | 27 | "id": "4eaf6522-f548-4abf-b84e-42d63aa2ecc5", | ||
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| 29 | "license_title": null, | 29 | "license_title": null, | ||
| 30 | "maintainer": null, | 30 | "maintainer": null, | ||
| 31 | "maintainer_email": null, | 31 | "maintainer_email": null, | ||
| 32 | "metadata_created": "2024-10-22T09:40:16.034981", | 32 | "metadata_created": "2024-10-22T09:40:16.034981", | ||
| n | 33 | "metadata_modified": "2024-10-22T09:40:17.492954", | n | 33 | "metadata_modified": "2024-10-22T09:40:17.882037", |
| 34 | "name": "7bbp", | 34 | "name": "7bbp", | ||
| 35 | "notes": "Shelf morphology and local hydrodynamical conditions may | 35 | "notes": "Shelf morphology and local hydrodynamical conditions may | ||
| 36 | significantly influence the partitioning of material (terrestrial or | 36 | significantly influence the partitioning of material (terrestrial or | ||
| 37 | in situ production) between shelf sediments (0-200 m) and the deeper | 37 | in situ production) between shelf sediments (0-200 m) and the deeper | ||
| 38 | ocean margin sediments (200-2000 m). Submarine canyons are typical | 38 | ocean margin sediments (200-2000 m). Submarine canyons are typical | ||
| 39 | morphological features of the rather narrow Iberian shelf. They have | 39 | morphological features of the rather narrow Iberian shelf. They have | ||
| 40 | been shown to trap and transport material from the shelf to the abyss. | 40 | 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 | 41 | During the OMEX cruise in 1999 the relative contribution of canyons in | ||
| 42 | off-shelf transport was studied by comparing sediment carbon budgets | 42 | off-shelf transport was studied by comparing sediment carbon budgets | ||
| 43 | for the Nazar\u00e9 Canyon and for \u2018normal\u2019 | 43 | for the Nazar\u00e9 Canyon and for \u2018normal\u2019 | ||
| 44 | shelf-slope-abyssal transects. In this study, three different | 44 | shelf-slope-abyssal transects. In this study, three different | ||
| 45 | canyon-shelf systems were compared, Setubal and Nazar\u00e9 Canyons on | 45 | canyon-shelf systems were compared, Setubal and Nazar\u00e9 Canyons on | ||
| 46 | the Iberian Margin and Cap de Cr\u00e9us Canyon in the Gulf of Lyon.", | 46 | the Iberian Margin and Cap de Cr\u00e9us Canyon in the Gulf of Lyon.", | ||
| n | 47 | "num_resources": 1, | n | 47 | "num_resources": 2, |
| 48 | "num_tags": 1, | 48 | "num_tags": 1, | ||
| 49 | "organization": { | 49 | "organization": { | ||
| 50 | "approval_status": "approved", | 50 | "approval_status": "approved", | ||
| 51 | "created": "2024-10-22T06:06:56.074257", | 51 | "created": "2024-10-22T06:06:56.074257", | ||
| 52 | "description": "", | 52 | "description": "", | ||
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| 54 | "image_url": | 54 | "image_url": | ||
| 55 | z.nl/application/files/1216/8924/5333/NIOZ-logo_witte_randi-2023.svg", | 55 | z.nl/application/files/1216/8924/5333/NIOZ-logo_witte_randi-2023.svg", | ||
| 56 | "is_organization": true, | 56 | "is_organization": true, | ||
| 57 | "name": "nioz", | 57 | "name": "nioz", | ||
| 58 | "state": "active", | 58 | "state": "active", | ||
| 59 | "title": "Royal Netherlands Institute for Sea Research", | 59 | "title": "Royal Netherlands Institute for Sea Research", | ||
| 60 | "type": "organization" | 60 | "type": "organization" | ||
| 61 | }, | 61 | }, | ||
| 62 | "owner_org": "bed2a893-3895-450b-bf4b-c74318003b1b", | 62 | "owner_org": "bed2a893-3895-450b-bf4b-c74318003b1b", | ||
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| 64 | "relationships_as_object": [], | 64 | "relationships_as_object": [], | ||
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| 67 | { | 67 | { | ||
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| 75 | "last_modified": "2024-10-22T09:40:17.471634", | 75 | "last_modified": "2024-10-22T09:40:17.471634", | ||
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| 79 | "name": "cruise report geochemie PE225.doc", | 79 | "name": "cruise report geochemie PE225.doc", | ||
| 80 | "package_id": "4eaf6522-f548-4abf-b84e-42d63aa2ecc5", | 80 | "package_id": "4eaf6522-f548-4abf-b84e-42d63aa2ecc5", | ||
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| 86 | c7-43b6-ac13-848106df01ba/download/cruise-report-geochemie-pe225.doc", | 86 | c7-43b6-ac13-848106df01ba/download/cruise-report-geochemie-pe225.doc", | ||
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| 101 | "name": "pore water nutrients.xls", | ||||
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| 88 | } | 110 | } | ||
| 89 | ], | 111 | ], | ||
| 90 | "state": "active", | 112 | "state": "active", | ||
| 91 | "subject": "Earth and Environmental Sciences", | 113 | "subject": "Earth and Environmental Sciences", | ||
| 92 | "tags": [ | 114 | "tags": [ | ||
| 93 | { | 115 | { | ||
| 94 | "display_name": "Shelf - deep sea exchange", | 116 | "display_name": "Shelf - deep sea exchange", | ||
| 95 | "id": "5273d868-0e9c-446e-8201-132971e13c87", | 117 | "id": "5273d868-0e9c-446e-8201-132971e13c87", | ||
| 96 | "name": "Shelf - deep sea exchange", | 118 | "name": "Shelf - deep sea exchange", | ||
| 97 | "state": "active", | 119 | "state": "active", | ||
| 98 | "vocabulary_id": null | 120 | "vocabulary_id": null | ||
| 99 | } | 121 | } | ||
| 100 | ], | 122 | ], | ||
| 101 | "title": "Nutrient pore water profiles in Portuguese marine | 123 | "title": "Nutrient pore water profiles in Portuguese marine | ||
| 102 | canyons", | 124 | canyons", | ||
| 103 | "type": "dataset", | 125 | "type": "dataset", | ||
| 104 | "url": "https://dataportal.nioz.nl/doi/10.33591/nioz/7b.b.p", | 126 | "url": "https://dataportal.nioz.nl/doi/10.33591/nioz/7b.b.p", | ||
| 105 | "version": "1" | 127 | "version": "1" | ||
| 106 | } | 128 | } |