Changes
On October 22, 2024, 8:28:49 PM UTC,
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Changed title to Suppl. Info - Alkenone distributions and hydrogen isotope ratios show changes in haptophyte species and source water in the Holocene Baltic Sea (previously Suppl. Info - Alkenone distributions and hydrogen isotope ratios show changes in haptophyte species and source water in the Holocene Baltic Sea.)
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Changed the version of Suppl. Info - Alkenone distributions and hydrogen isotope ratios show changes in haptophyte species and source water in the Holocene Baltic Sea to 6 (previously 5)
| 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:10.25850/nioz/7b.b.x", | 24 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.x", | ||
| 25 | "dates": | 25 | "dates": | ||
| 26 | -05-27T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"Cruise | 26 | -05-27T22:00:00.000Z\",\"type\":\"collected\",\"information\":\"Cruise | ||
| 27 | 64PE410 (RV Pelagia)\"}]", | 27 | 64PE410 (RV Pelagia)\"}]", | ||
| 28 | "deposit_date": "2020-02-01", | 28 | "deposit_date": "2020-02-01", | ||
| 29 | "depositor": "Gabriella Weiss", | 29 | "depositor": "Gabriella Weiss", | ||
| 30 | "distribution_date": "2020-02-01", | 30 | "distribution_date": "2020-02-01", | ||
| 31 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 31 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 32 | Institute for Sea Research)", | 32 | Institute for Sea Research)", | ||
| 33 | "doi_date_published": "2020-02-05", | 33 | "doi_date_published": "2020-02-05", | ||
| 34 | "funding_references": | 34 | "funding_references": | ||
| 35 | SC\",\"awardnumber\":\"\",\"awardtitle\":\"\"},{\"name\":\"Gravitation | 35 | SC\",\"awardnumber\":\"\",\"awardtitle\":\"\"},{\"name\":\"Gravitation | ||
| 36 | Grant\",\"awardnumber\":\"024.002.001\",\"awardtitle\":\"\"}]", | 36 | Grant\",\"awardnumber\":\"024.002.001\",\"awardtitle\":\"\"}]", | ||
| 37 | "geographic_coverage": "[{\"place\":\"Arkona Basin, Baltic | 37 | "geographic_coverage": "[{\"place\":\"Arkona Basin, Baltic | ||
| 38 | \"\",\"longitude_1\":\"\",\"latitude_2\":\"\",\"longitude_2\":\"\"}]", | 38 | \"\",\"longitude_1\":\"\",\"latitude_2\":\"\",\"longitude_2\":\"\"}]", | ||
| 39 | "groups": [], | 39 | "groups": [], | ||
| 40 | "id": "b9a50590-7903-4c01-b6ec-e9d4c347b535", | 40 | "id": "b9a50590-7903-4c01-b6ec-e9d4c347b535", | ||
| 41 | "isopen": true, | 41 | "isopen": true, | ||
| 42 | "license_id": "CC0-1.0", | 42 | "license_id": "CC0-1.0", | ||
| 43 | "license_title": "CC0 1.0", | 43 | "license_title": "CC0 1.0", | ||
| 44 | "license_url": "https://creativecommons.org/publicdomain/zero/1.0/", | 44 | "license_url": "https://creativecommons.org/publicdomain/zero/1.0/", | ||
| 45 | "maintainer": null, | 45 | "maintainer": null, | ||
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| 47 | "metadata_created": "2024-10-22T09:41:29.373546", | 47 | "metadata_created": "2024-10-22T09:41:29.373546", | ||
| n | 48 | "metadata_modified": "2024-10-22T20:28:49.145874", | n | 48 | "metadata_modified": "2024-10-22T20:28:49.613874", |
| 49 | "name": "7bbx", | 49 | "name": "7bbx", | ||
| 50 | "notes": "The Baltic Sea, a dynamic, marginal marine basin, | 50 | "notes": "The Baltic Sea, a dynamic, marginal marine basin, | ||
| 51 | experienced a number of large changes in\nsalinity during the Holocene | 51 | experienced a number of large changes in\nsalinity during the Holocene | ||
| 52 | as a result of fluctuations in global and local sea level related | 52 | as a result of fluctuations in global and local sea level related | ||
| 53 | to\nmelting of glacial ice sheets and subsequent isostatic rebound. | 53 | to\nmelting of glacial ice sheets and subsequent isostatic rebound. | ||
| 54 | These changes likely had\npronounced effects on the species | 54 | These changes likely had\npronounced effects on the species | ||
| 55 | composition of haptophytes, a common phytoplankton group\nfound in the | 55 | composition of haptophytes, a common phytoplankton group\nfound in the | ||
| 56 | Baltic Sea. This dynamic environment provides the ideal setting to | 56 | Baltic Sea. This dynamic environment provides the ideal setting to | ||
| 57 | study how\nspecies change impacts distribution and hydrogen isotope | 57 | study how\nspecies change impacts distribution and hydrogen isotope | ||
| 58 | ratios of long-chain alkenones\n(d2HC37), haptophyte-specific | 58 | ratios of long-chain alkenones\n(d2HC37), haptophyte-specific | ||
| 59 | biomarkers. Here we analyzed the aforementioned parameters | 59 | biomarkers. Here we analyzed the aforementioned parameters | ||
| 60 | in\nHolocene sediments covering the contrasting hydrological phases of | 60 | in\nHolocene sediments covering the contrasting hydrological phases of | ||
| 61 | the Baltic Sea. Alkenone\ndistributions changed with different Baltic | 61 | the Baltic Sea. Alkenone\ndistributions changed with different Baltic | ||
| 62 | Sea salinity phases, suggesting that species shifts\ncoincide with | 62 | Sea salinity phases, suggesting that species shifts\ncoincide with | ||
| 63 | salinity change. d2HC37 values show two major shifts: one in the | 63 | salinity change. d2HC37 values show two major shifts: one in the | ||
| 64 | middle of the\nfreshwater Ancylus Lake phase (10.6 to 7.7 ka) and a | 64 | middle of the\nfreshwater Ancylus Lake phase (10.6 to 7.7 ka) and a | ||
| 65 | second at the transition from the brackish\nLittorina Sea phase (7.2 | 65 | second at the transition from the brackish\nLittorina Sea phase (7.2 | ||
| 66 | to 3 ka) into the fresher Modern Baltic (3 ka to the present). The | 66 | to 3 ka) into the fresher Modern Baltic (3 ka to the present). The | ||
| 67 | first\nshift represents a significant enrichment of 50 ???, which | 67 | first\nshift represents a significant enrichment of 50 ???, which | ||
| 68 | cannot be explained by salinity or\nspecies changes only. At this | 68 | cannot be explained by salinity or\nspecies changes only. At this | ||
| 69 | time, the isotopically depleted ice sheets had melted and only | 69 | time, the isotopically depleted ice sheets had melted and only | ||
| 70 | the\nrelatively enriched freshwater source remained. The second shift, | 70 | the\nrelatively enriched freshwater source remained. The second shift, | ||
| 71 | coincident with a change in\ndistribution, is likely caused by a | 71 | coincident with a change in\ndistribution, is likely caused by a | ||
| 72 | change in species composition alone. These findings show | 72 | change in species composition alone. These findings show | ||
| 73 | that\nhydrogen isotope ratios of long-chain alkenones, combined with | 73 | that\nhydrogen isotope ratios of long-chain alkenones, combined with | ||
| 74 | their relative distribution, can be\nused to reconstruct changes in | 74 | their relative distribution, can be\nused to reconstruct changes in | ||
| 75 | source water.", | 75 | source water.", | ||
| 76 | "num_resources": 4, | 76 | "num_resources": 4, | ||
| 77 | "num_tags": 5, | 77 | "num_tags": 5, | ||
| 78 | "organization": { | 78 | "organization": { | ||
| 79 | "approval_status": "approved", | 79 | "approval_status": "approved", | ||
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| 186 | "state": "active", | 186 | "state": "active", | ||
| 187 | "subject": "Earth and Environmental Sciences", | 187 | "subject": "Earth and Environmental Sciences", | ||
| 188 | "tags": [ | 188 | "tags": [ | ||
| 189 | { | 189 | { | ||
| 190 | "display_name": "Alkenones", | 190 | "display_name": "Alkenones", | ||
| 191 | "id": "b3e0ca32-dc1f-4f37-80fa-6817b60184ff", | 191 | "id": "b3e0ca32-dc1f-4f37-80fa-6817b60184ff", | ||
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| 208 | "vocabulary_id": null | 208 | "vocabulary_id": null | ||
| 209 | }, | 209 | }, | ||
| 210 | { | 210 | { | ||
| 211 | "display_name": "Haptophytes", | 211 | "display_name": "Haptophytes", | ||
| 212 | "id": "b9497b61-cc04-4262-af6a-e925b79297b1", | 212 | "id": "b9497b61-cc04-4262-af6a-e925b79297b1", | ||
| 213 | "name": "Haptophytes", | 213 | "name": "Haptophytes", | ||
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| 216 | }, | 216 | }, | ||
| 217 | { | 217 | { | ||
| 218 | "display_name": "Hydrogen isotope ratios", | 218 | "display_name": "Hydrogen isotope ratios", | ||
| 219 | "id": "60e5d148-2783-42e3-b368-a1a726a459c0", | 219 | "id": "60e5d148-2783-42e3-b368-a1a726a459c0", | ||
| 220 | "name": "Hydrogen isotope ratios", | 220 | "name": "Hydrogen isotope ratios", | ||
| 221 | "state": "active", | 221 | "state": "active", | ||
| 222 | "vocabulary_id": null | 222 | "vocabulary_id": null | ||
| 223 | } | 223 | } | ||
| 224 | ], | 224 | ], | ||
| 225 | "title": "Suppl. Info - Alkenone distributions and hydrogen isotope | 225 | "title": "Suppl. Info - Alkenone distributions and hydrogen isotope | ||
| 226 | ratios show changes in haptophyte species and source water in the | 226 | ratios show changes in haptophyte species and source water in the | ||
| n | 227 | Holocene Baltic Sea.", | n | 227 | Holocene Baltic Sea", |
| 228 | "type": "dataset", | 228 | "type": "dataset", | ||
| 229 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.x", | 229 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.x", | ||
| t | 230 | "version": "5" | t | 230 | "version": "6" |
| 231 | } | 231 | } |