Changes
On October 22, 2024, 9:41:31 AM UTC,
ckan_admin:
-
Changed the version of Suppl. Info - Alkenone distributions and hydrogen isotope ratios show changes in haptophyte species and source water in the Holo to 3 (previously 2)
-
Changed value of field
geographic_coverage
to[{"place":"Arkona Basin, Baltic Sea","latitude_1":"","longitude_1":"","latitude_2":"","longitude_2":""}]
in Suppl. Info - Alkenone distributions and hydrogen isotope ratios show changes in haptophyte species and source water in the Holo
| f | 1 | { | f | 1 | { |
| 2 | "author": null, | 2 | "author": null, | ||
| 3 | "author_email": null, | 3 | "author_email": null, | ||
| 4 | "code": "7b.b.x", | 4 | "code": "7b.b.x", | ||
| 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | ||
| 6 | "creator_user_id": "e2280cf1-9542-4dea-a4bb-4d572f59536f", | 6 | "creator_user_id": "e2280cf1-9542-4dea-a4bb-4d572f59536f", | ||
| 7 | "creators": "[{\"firstname\":\"Gabriella | 7 | "creators": "[{\"firstname\":\"Gabriella | ||
| 8 | M.\",\"lastname\":\"Weiss\",\"affiliation\":\"Royal Netherlands | 8 | M.\",\"lastname\":\"Weiss\",\"affiliation\":\"Royal Netherlands | ||
| 9 | Institute for Sea | 9 | Institute for Sea | ||
| 10 | \":\"Barbara\",\"lastname\":\"Massalska\",\"affiliation\":\"University | 10 | \":\"Barbara\",\"lastname\":\"Massalska\",\"affiliation\":\"University | ||
| 11 | of Warsaw, | 11 | of Warsaw, | ||
| 12 | firstname\":\"Rick\",\"lastname\":\"Hennekam\",\"affiliation\":\"Royal | 12 | firstname\":\"Rick\",\"lastname\":\"Hennekam\",\"affiliation\":\"Royal | ||
| 13 | Netherlands Institute for Sea | 13 | Netherlands Institute for Sea | ||
| 14 | tname\":\"Gert-Jan\",\"lastname\":\"Reichart\",\"affiliation\":\"Royal | 14 | tname\":\"Gert-Jan\",\"lastname\":\"Reichart\",\"affiliation\":\"Royal | ||
| 15 | Netherlands Institute for Sea | 15 | Netherlands Institute for Sea | ||
| 16 | rstname\":\"Stefan\",\"lastname\":\"Schouten\",\"affiliation\":\"Royal | 16 | rstname\":\"Stefan\",\"lastname\":\"Schouten\",\"affiliation\":\"Royal | ||
| 17 | Netherlands Institute for Sea | 17 | Netherlands Institute for Sea | ||
| 18 | ondingauthor\":false},{\"firstname\":\"Jaap\",\"lastname\":\"Sinninghe | 18 | ondingauthor\":false},{\"firstname\":\"Jaap\",\"lastname\":\"Sinninghe | ||
| 19 | Damste\",\"affiliation\":\"Royal Netjerlands Institute for Sea | 19 | Damste\",\"affiliation\":\"Royal Netjerlands Institute for Sea | ||
| 20 | ddress\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Marcel | 20 | ddress\":\"\",\"iscorrespondingauthor\":false},{\"firstname\":\"Marcel | ||
| 21 | T. J.\",\"lastname\":\"van der Meer\",\"affiliation\":\"Royal | 21 | T. J.\",\"lastname\":\"van der Meer\",\"affiliation\":\"Royal | ||
| 22 | Netherlands Institute for Sea | 22 | Netherlands Institute for Sea | ||
| 23 | 752\",\"contactemailaddress\":\"\",\"iscorrespondingauthor\":false}]", | 23 | 752\",\"contactemailaddress\":\"\",\"iscorrespondingauthor\":false}]", | ||
| 24 | "dataset_persistent_id": "DOI:10.33591/nioz/7b.b.x", | 24 | "dataset_persistent_id": "DOI:10.33591/nioz/7b.b.x", | ||
| 25 | "dates": "", | 25 | "dates": "", | ||
| 26 | "deposit_date": "2020-02-01", | 26 | "deposit_date": "2020-02-01", | ||
| 27 | "depositor": "Gabriella Weiss", | 27 | "depositor": "Gabriella Weiss", | ||
| 28 | "distribution_date": "2020-02-01", | 28 | "distribution_date": "2020-02-01", | ||
| 29 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 29 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 30 | Institute for Sea Research)", | 30 | Institute for Sea Research)", | ||
| 31 | "doi_date_published": "2020-02-05", | 31 | "doi_date_published": "2020-02-05", | ||
| 32 | "funding_references": | 32 | "funding_references": | ||
| 33 | SC\",\"awardnumber\":\"\",\"awardtitle\":\"\"},{\"name\":\"Gravitation | 33 | SC\",\"awardnumber\":\"\",\"awardtitle\":\"\"},{\"name\":\"Gravitation | ||
| 34 | Grant\",\"awardnumber\":\"024.002.001\",\"awardtitle\":\"\"}]", | 34 | Grant\",\"awardnumber\":\"024.002.001\",\"awardtitle\":\"\"}]", | ||
| n | 35 | "geographic_coverage": "", | n | 35 | "geographic_coverage": "[{\"place\":\"Arkona Basin, Baltic |
| 36 | \"\",\"longitude_1\":\"\",\"latitude_2\":\"\",\"longitude_2\":\"\"}]", | ||||
| 36 | "groups": [], | 37 | "groups": [], | ||
| 37 | "id": "b9a50590-7903-4c01-b6ec-e9d4c347b535", | 38 | "id": "b9a50590-7903-4c01-b6ec-e9d4c347b535", | ||
| 38 | "isopen": false, | 39 | "isopen": false, | ||
| 39 | "license_title": null, | 40 | "license_title": null, | ||
| 40 | "maintainer": null, | 41 | "maintainer": null, | ||
| 41 | "maintainer_email": null, | 42 | "maintainer_email": null, | ||
| 42 | "metadata_created": "2024-10-22T09:41:29.373546", | 43 | "metadata_created": "2024-10-22T09:41:29.373546", | ||
| n | 43 | "metadata_modified": "2024-10-22T09:41:31.293097", | n | 44 | "metadata_modified": "2024-10-22T09:41:31.621133", |
| 44 | "name": "7bbx", | 45 | "name": "7bbx", | ||
| 45 | "notes": "The Baltic Sea, a dynamic, marginal marine basin, | 46 | "notes": "The Baltic Sea, a dynamic, marginal marine basin, | ||
| 46 | experienced a number of large changes in\nsalinity during the Holocene | 47 | experienced a number of large changes in\nsalinity during the Holocene | ||
| 47 | as a result of fluctuations in global and local sea level related | 48 | as a result of fluctuations in global and local sea level related | ||
| 48 | to\nmelting of glacial ice sheets and subsequent isostatic rebound. | 49 | to\nmelting of glacial ice sheets and subsequent isostatic rebound. | ||
| 49 | These changes likely had\npronounced effects on the species | 50 | These changes likely had\npronounced effects on the species | ||
| 50 | composition of haptophytes, a common phytoplankton group\nfound in the | 51 | composition of haptophytes, a common phytoplankton group\nfound in the | ||
| 51 | Baltic Sea. This dynamic environment provides the ideal setting to | 52 | Baltic Sea. This dynamic environment provides the ideal setting to | ||
| 52 | study how\nspecies change impacts distribution and hydrogen isotope | 53 | study how\nspecies change impacts distribution and hydrogen isotope | ||
| 53 | ratios of long-chain alkenones\n(d2HC37), haptophyte-specific | 54 | ratios of long-chain alkenones\n(d2HC37), haptophyte-specific | ||
| 54 | biomarkers. Here we analyzed the aforementioned parameters | 55 | biomarkers. Here we analyzed the aforementioned parameters | ||
| 55 | in\nHolocene sediments covering the contrasting hydrological phases of | 56 | in\nHolocene sediments covering the contrasting hydrological phases of | ||
| 56 | the Baltic Sea. Alkenone\ndistributions changed with different Baltic | 57 | the Baltic Sea. Alkenone\ndistributions changed with different Baltic | ||
| 57 | Sea salinity phases, suggesting that species shifts\ncoincide with | 58 | Sea salinity phases, suggesting that species shifts\ncoincide with | ||
| 58 | salinity change. d2HC37 values show two major shifts: one in the | 59 | salinity change. d2HC37 values show two major shifts: one in the | ||
| 59 | middle of the\nfreshwater Ancylus Lake phase (10.6 to 7.7 ka) and a | 60 | middle of the\nfreshwater Ancylus Lake phase (10.6 to 7.7 ka) and a | ||
| 60 | second at the transition from the brackish\nLittorina Sea phase (7.2 | 61 | second at the transition from the brackish\nLittorina Sea phase (7.2 | ||
| 61 | to 3 ka) into the fresher Modern Baltic (3 ka to the present). The | 62 | to 3 ka) into the fresher Modern Baltic (3 ka to the present). The | ||
| 62 | first\nshift represents a significant enrichment of 50 ???, which | 63 | first\nshift represents a significant enrichment of 50 ???, which | ||
| 63 | cannot be explained by salinity or\nspecies changes only. At this | 64 | cannot be explained by salinity or\nspecies changes only. At this | ||
| 64 | time, the isotopically depleted ice sheets had melted and only | 65 | time, the isotopically depleted ice sheets had melted and only | ||
| 65 | the\nrelatively enriched freshwater source remained. The second shift, | 66 | the\nrelatively enriched freshwater source remained. The second shift, | ||
| 66 | coincident with a change in\ndistribution, is likely caused by a | 67 | coincident with a change in\ndistribution, is likely caused by a | ||
| 67 | change in species composition alone. These findings show | 68 | change in species composition alone. These findings show | ||
| 68 | that\nhydrogen isotope ratios of long-chain alkenones, combined with | 69 | that\nhydrogen isotope ratios of long-chain alkenones, combined with | ||
| 69 | their relative distribution, can be\nused to reconstruct changes in | 70 | their relative distribution, can be\nused to reconstruct changes in | ||
| 70 | source water.", | 71 | source water.", | ||
| 71 | "num_resources": 4, | 72 | "num_resources": 4, | ||
| 72 | "num_tags": 5, | 73 | "num_tags": 5, | ||
| 73 | "organization": { | 74 | "organization": { | ||
| 74 | "approval_status": "approved", | 75 | "approval_status": "approved", | ||
| 75 | "created": "2024-10-22T06:06:56.074257", | 76 | "created": "2024-10-22T06:06:56.074257", | ||
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| 81 | "name": "nioz", | 82 | "name": "nioz", | ||
| 82 | "state": "active", | 83 | "state": "active", | ||
| 83 | "title": "Royal Netherlands Institute for Sea Research", | 84 | "title": "Royal Netherlands Institute for Sea Research", | ||
| 84 | "type": "organization" | 85 | "type": "organization" | ||
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| 181 | "state": "active", | 182 | "state": "active", | ||
| 182 | "subject": "Earth and Environmental Sciences", | 183 | "subject": "Earth and Environmental Sciences", | ||
| 183 | "tags": [ | 184 | "tags": [ | ||
| 184 | { | 185 | { | ||
| 185 | "display_name": "Alkenones", | 186 | "display_name": "Alkenones", | ||
| 186 | "id": "b3e0ca32-dc1f-4f37-80fa-6817b60184ff", | 187 | "id": "b3e0ca32-dc1f-4f37-80fa-6817b60184ff", | ||
| 187 | "name": "Alkenones", | 188 | "name": "Alkenones", | ||
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| 191 | { | 192 | { | ||
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| 193 | "id": "6590bb10-f51d-4c1c-a338-8552211eb811", | 194 | "id": "6590bb10-f51d-4c1c-a338-8552211eb811", | ||
| 194 | "name": "Baltic Sea", | 195 | "name": "Baltic Sea", | ||
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| 202 | "state": "active", | 203 | "state": "active", | ||
| 203 | "vocabulary_id": null | 204 | "vocabulary_id": null | ||
| 204 | }, | 205 | }, | ||
| 205 | { | 206 | { | ||
| 206 | "display_name": "Haptophytes", | 207 | "display_name": "Haptophytes", | ||
| 207 | "id": "b9497b61-cc04-4262-af6a-e925b79297b1", | 208 | "id": "b9497b61-cc04-4262-af6a-e925b79297b1", | ||
| 208 | "name": "Haptophytes", | 209 | "name": "Haptophytes", | ||
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| 210 | "vocabulary_id": null | 211 | "vocabulary_id": null | ||
| 211 | }, | 212 | }, | ||
| 212 | { | 213 | { | ||
| 213 | "display_name": "Hydrogen isotope ratios", | 214 | "display_name": "Hydrogen isotope ratios", | ||
| 214 | "id": "60e5d148-2783-42e3-b368-a1a726a459c0", | 215 | "id": "60e5d148-2783-42e3-b368-a1a726a459c0", | ||
| 215 | "name": "Hydrogen isotope ratios", | 216 | "name": "Hydrogen isotope ratios", | ||
| 216 | "state": "active", | 217 | "state": "active", | ||
| 217 | "vocabulary_id": null | 218 | "vocabulary_id": null | ||
| 218 | } | 219 | } | ||
| 219 | ], | 220 | ], | ||
| 220 | "title": "Suppl. Info - Alkenone distributions and hydrogen isotope | 221 | "title": "Suppl. Info - Alkenone distributions and hydrogen isotope | ||
| 221 | ratios show changes in haptophyte species and source water in the | 222 | ratios show changes in haptophyte species and source water in the | ||
| 222 | Holo", | 223 | Holo", | ||
| 223 | "type": "dataset", | 224 | "type": "dataset", | ||
| 224 | "url": "https://dataportal.nioz.nl/doi/10.33591/nioz/7b.b.x", | 225 | "url": "https://dataportal.nioz.nl/doi/10.33591/nioz/7b.b.x", | ||
| t | 225 | "version": "2" | t | 226 | "version": "3" |
| 226 | } | 227 | } |