Changes
On October 22, 2024, 11:53:38 AM UTC,
-
Added resource Pigments Year.csv to Annual biogeochemical dynamics in the Western Scheldt
| f | 1 | { | f | 1 | { |
| 2 | "author": null, | 2 | "author": null, | ||
| 3 | "author_email": null, | 3 | "author_email": null, | ||
| 4 | "code": "7b.b.qf", | 4 | "code": "7b.b.qf", | ||
| 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | ||
| 6 | "creator_user_id": "f2bfd70d-fc03-4c01-bd7f-3d3276156f5d", | 6 | "creator_user_id": "f2bfd70d-fc03-4c01-bd7f-3d3276156f5d", | ||
| 7 | "creators": | 7 | "creators": | ||
| 8 | \"Soetaert\",\"orcid\":\"0000-0003-4603-7100\",\"affiliation\":\"Royal | 8 | \"Soetaert\",\"orcid\":\"0000-0003-4603-7100\",\"affiliation\":\"Royal | ||
| 9 | Netherlands Institute for Sea | 9 | Netherlands Institute for Sea | ||
| 10 | actemailaddress\":\"karline.soetaert@nioz.nl\",\"formatted\":\"Karline | 10 | actemailaddress\":\"karline.soetaert@nioz.nl\",\"formatted\":\"Karline | ||
| 11 | Soetaert - Royal Netherlands Institute for Sea Research - ORCID: | 11 | Soetaert - Royal Netherlands Institute for Sea Research - ORCID: | ||
| 12 | 0000-0003-4603-7100 - Corresponding Author - | 12 | 0000-0003-4603-7100 - Corresponding Author - | ||
| 13 | rline.soetaert@nioz.nl\"},{\"firstname\":\"Dunia\",\"lastname\":\"Rios | 13 | rline.soetaert@nioz.nl\"},{\"firstname\":\"Dunia\",\"lastname\":\"Rios | ||
| 14 | Yunes\",\"orcid\":\"0000-0002-1976-7186\",\"affiliation\":\"Royal | 14 | Yunes\",\"orcid\":\"0000-0002-1976-7186\",\"affiliation\":\"Royal | ||
| 15 | Netherlands Institute for Sea | 15 | Netherlands Institute for Sea | ||
| 16 | arch\",\"iscorrespondingauthor\":null,\"contactemailaddress\":null}]", | 16 | arch\",\"iscorrespondingauthor\":null,\"contactemailaddress\":null}]", | ||
| 17 | "dataset_persistent_id": "DOI:10.33591/nioz/7b.b.qf", | 17 | "dataset_persistent_id": "DOI:10.33591/nioz/7b.b.qf", | ||
| 18 | "dates": "[{\"datefrom\":\"2019-03-01 | 18 | "dates": "[{\"datefrom\":\"2019-03-01 | ||
| 19 | 00:00:00.000\",\"dateto\":\"2020-02-29 | 19 | 00:00:00.000\",\"dateto\":\"2020-02-29 | ||
| 20 | 00:00:00.000\",\"type\":\"collected\",\"information\":\"Monthly | 20 | 00:00:00.000\",\"type\":\"collected\",\"information\":\"Monthly | ||
| 21 | samples of sediment and water from three sites, Appels, Groot | 21 | samples of sediment and water from three sites, Appels, Groot | ||
| 22 | Buitenshoor and Paulina polder in the Western Scheldt\"}]", | 22 | Buitenshoor and Paulina polder in the Western Scheldt\"}]", | ||
| 23 | "deposit_date": "2023-08-04", | 23 | "deposit_date": "2023-08-04", | ||
| 24 | "depositor": "Dunia Rios Yunes", | 24 | "depositor": "Dunia Rios Yunes", | ||
| 25 | "distribution_date": "2023-08-04", | 25 | "distribution_date": "2023-08-04", | ||
| 26 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 26 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 27 | Institute for Sea Research)", | 27 | Institute for Sea Research)", | ||
| 28 | "doi_date_published": "2023-08-04", | 28 | "doi_date_published": "2023-08-04", | ||
| 29 | "funding_references": "[{\"name\":\"Royal Netherlands Academy of | 29 | "funding_references": "[{\"name\":\"Royal Netherlands Academy of | ||
| 30 | Arts and Sciences (KNAW)\",\"awardnumber\":\"PSA-SAE- | 30 | Arts and Sciences (KNAW)\",\"awardnumber\":\"PSA-SAE- | ||
| 31 | 02\",\"awardtitle\":null}]", | 31 | 02\",\"awardtitle\":null}]", | ||
| 32 | "groups": [], | 32 | "groups": [], | ||
| 33 | "id": "24039fa5-46da-4f6b-ba99-ef18f147131c", | 33 | "id": "24039fa5-46da-4f6b-ba99-ef18f147131c", | ||
| 34 | "isopen": false, | 34 | "isopen": false, | ||
| 35 | "license_title": null, | 35 | "license_title": null, | ||
| 36 | "maintainer": null, | 36 | "maintainer": null, | ||
| 37 | "maintainer_email": null, | 37 | "maintainer_email": null, | ||
| 38 | "metadata_created": "2024-10-22T11:53:34.403671", | 38 | "metadata_created": "2024-10-22T11:53:34.403671", | ||
| n | 39 | "metadata_modified": "2024-10-22T11:53:37.620754", | n | 39 | "metadata_modified": "2024-10-22T11:53:37.967935", |
| 40 | "name": "7bbqf", | 40 | "name": "7bbqf", | ||
| 41 | "notes": "Estuarine intertidal sediments are important centres for | 41 | "notes": "Estuarine intertidal sediments are important centres for | ||
| 42 | organic matter remineralization and nutrients | 42 | organic matter remineralization and nutrients | ||
| 43 | recycling.\nNevertheless, there is limited understanding regarding how | 43 | recycling.\nNevertheless, there is limited understanding regarding how | ||
| 44 | these processes occur along the salinity gradient and\ntheir | 44 | these processes occur along the salinity gradient and\ntheir | ||
| 45 | seasonality. Here, we report on the seasonal biogeochemical cycles | 45 | seasonality. Here, we report on the seasonal biogeochemical cycles | ||
| 46 | from three types of intertidal sedimentary\nhabitats (freshwater, | 46 | from three types of intertidal sedimentary\nhabitats (freshwater, | ||
| 47 | brackish and marine) located in the Western Scheldt estuary (The | 47 | brackish and marine) located in the Western Scheldt estuary (The | ||
| 48 | Netherlands and\nBelgium). A full year of solute fluxes, porewater | 48 | Netherlands and\nBelgium). A full year of solute fluxes, porewater | ||
| 49 | nutrient and sediment pigment concentrations at a monthly\nresolution | 49 | nutrient and sediment pigment concentrations at a monthly\nresolution | ||
| 50 | revealed clear differences in the biogeochemistry of the three sites, | 50 | revealed clear differences in the biogeochemistry of the three sites, | ||
| 51 | indicating that environmental\nconditions determined the local | 51 | indicating that environmental\nconditions determined the local | ||
| 52 | nutrient dynamics. Temperature controlled sediment oxygen consumption | 52 | nutrient dynamics. Temperature controlled sediment oxygen consumption | ||
| 53 | rates\nand nutrient fluxes, but also affected pore water nutrient | 53 | rates\nand nutrient fluxes, but also affected pore water nutrient | ||
| 54 | concentrations up to 14 cm deep. Fresh and brackish\nsediments had a | 54 | concentrations up to 14 cm deep. Fresh and brackish\nsediments had a | ||
| 55 | net influx of dissolved inorganic nitrogen (DIN) (\udbc0\udc00 1.62 | 55 | net influx of dissolved inorganic nitrogen (DIN) (\udbc0\udc00 1.62 | ||
| 56 | mmol m\udbc0\udc00 2 d\udbc0\udc00 1 and -2.84 mmol m\udbc0\udc00 2 | 56 | mmol m\udbc0\udc00 2 d\udbc0\udc00 1 and -2.84 mmol m\udbc0\udc00 2 | ||
| 57 | d\udbc0\udc00 1,\nrespectively), while only the freshwater sediments | 57 | d\udbc0\udc00 1,\nrespectively), while only the freshwater sediments | ||
| 58 | showed a net influx of phosphate (\udbc0\udc00 0.07 mmol m\udbc0\udc00 | 58 | showed a net influx of phosphate (\udbc0\udc00 0.07 mmol m\udbc0\udc00 | ||
| 59 | 2 d\udbc0\udc00 1). We\nestimated that intertidal sediments | 59 | 2 d\udbc0\udc00 1). We\nestimated that intertidal sediments | ||
| 60 | remineralized a total of 10,000 t C y\udbc0\udc00 1, with 97% of | 60 | remineralized a total of 10,000 t C y\udbc0\udc00 1, with 97% of | ||
| 61 | mineralization occurring\nin the brackish and marine parts. Overall, | 61 | mineralization occurring\nin the brackish and marine parts. Overall, | ||
| 62 | sediments removed 11% (1500 t N y\udbc0\udc00 1) and 15% (~200 t P | 62 | sediments removed 11% (1500 t N y\udbc0\udc00 1) and 15% (~200 t P | ||
| 63 | y\udbc0\udc00 1) of the\ntotal nitrogen and phosphorus entering the | 63 | y\udbc0\udc00 1) of the\ntotal nitrogen and phosphorus entering the | ||
| 64 | estuary from riverine input. Moreover, observations revealed | 64 | estuary from riverine input. Moreover, observations revealed | ||
| 65 | the\nhistorical improvement of water quality resulting from water | 65 | the\nhistorical improvement of water quality resulting from water | ||
| 66 | treatment policies. This spatiotemporal study of\nOM remineralization | 66 | treatment policies. This spatiotemporal study of\nOM remineralization | ||
| 67 | and early diagenesis in estuarine systems highlights the importance of | 67 | and early diagenesis in estuarine systems highlights the importance of | ||
| 68 | intertidal sediments\nfor estuarine systems. Our observations can be | 68 | intertidal sediments\nfor estuarine systems. Our observations can be | ||
| 69 | used in models to predict estuarine biogeochemistry or assess\nclimate | 69 | used in models to predict estuarine biogeochemistry or assess\nclimate | ||
| 70 | change scenarios.", | 70 | change scenarios.", | ||
| n | 71 | "num_resources": 10, | n | 71 | "num_resources": 11, |
| 72 | "num_tags": 5, | 72 | "num_tags": 5, | ||
| 73 | "organization": { | 73 | "organization": { | ||
| 74 | "approval_status": "approved", | 74 | "approval_status": "approved", | ||
| 75 | "created": "2024-10-22T06:06:56.074257", | 75 | "created": "2024-10-22T06:06:56.074257", | ||
| 76 | "description": "", | 76 | "description": "", | ||
| 77 | "id": "bed2a893-3895-450b-bf4b-c74318003b1b", | 77 | "id": "bed2a893-3895-450b-bf4b-c74318003b1b", | ||
| 78 | "image_url": | 78 | "image_url": | ||
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| 80 | "is_organization": true, | 80 | "is_organization": true, | ||
| 81 | "name": "nioz", | 81 | "name": "nioz", | ||
| 82 | "state": "active", | 82 | "state": "active", | ||
| 83 | "title": "Royal Netherlands Institute for Sea Research", | 83 | "title": "Royal Netherlands Institute for Sea Research", | ||
| 84 | "type": "organization" | 84 | "type": "organization" | ||
| 85 | }, | 85 | }, | ||
| 86 | "owner_org": "bed2a893-3895-450b-bf4b-c74318003b1b", | 86 | "owner_org": "bed2a893-3895-450b-bf4b-c74318003b1b", | ||
| 87 | "private": false, | 87 | "private": false, | ||
| 88 | "production_date": "2023-08-04T10:22:00.3812029", | 88 | "production_date": "2023-08-04T10:22:00.3812029", | ||
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