Changes
On October 22, 2024, 8:43:25 PM UTC,
ckan_admin:
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Changed the version of Co-evolution of the terrestrial and aquatic ecosystem in the Holocene Baltic Sea to 2 (previously 1)
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Changed value of field
funding_references
to[{"name":"NWO Rubicon","awardnumber":"019.183EN.002","awardtitle":null}]
in Co-evolution of the terrestrial and aquatic ecosystem in the Holocene Baltic Sea
| f | 1 | { | f | 1 | { |
| 2 | "author": null, | 2 | "author": null, | ||
| 3 | "author_email": null, | 3 | "author_email": null, | ||
| 4 | "code": "7b.b.2c", | 4 | "code": "7b.b.2c", | ||
| 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | ||
| 6 | "creator_user_id": "ba352652-fd7a-4620-b8c9-6d53fcf8c654", | 6 | "creator_user_id": "ba352652-fd7a-4620-b8c9-6d53fcf8c654", | ||
| 7 | "creators": "[{\"firstname\":\"Gabriella | 7 | "creators": "[{\"firstname\":\"Gabriella | ||
| 8 | M.\",\"lastname\":\"Weiss\",\"orcid\":null,\"affiliation\":\"Royal | 8 | M.\",\"lastname\":\"Weiss\",\"orcid\":null,\"affiliation\":\"Royal | ||
| 9 | Netherlands Institute for Sea | 9 | Netherlands Institute for Sea | ||
| 10 | ulie\",\"lastname\":\"Lattaud\",\"orcid\":null,\"affiliation\":\"Royal | 10 | ulie\",\"lastname\":\"Lattaud\",\"orcid\":null,\"affiliation\":\"Royal | ||
| 11 | Netherlands Institute for Sea | 11 | Netherlands Institute for Sea | ||
| 12 | ingauthor\":null,\"contactemailaddress\":null},{\"firstname\":\"Marcel | 12 | ingauthor\":null,\"contactemailaddress\":null},{\"firstname\":\"Marcel | ||
| 13 | T.J.\",\"lastname\":\"van der | 13 | T.J.\",\"lastname\":\"van der | ||
| 14 | Meer\",\"orcid\":null,\"affiliation\":\"Royal Netherlands Institute | 14 | Meer\",\"orcid\":null,\"affiliation\":\"Royal Netherlands Institute | ||
| 15 | for Sea | 15 | for Sea | ||
| 16 | ngauthor\":null,\"contactemailaddress\":null},{\"firstname\":\"Timothy | 16 | ngauthor\":null,\"contactemailaddress\":null},{\"firstname\":\"Timothy | ||
| 17 | I.\",\"lastname\":\"Eglinton\",\"orcid\":null,\"affiliation\":\"Swiss | 17 | I.\",\"lastname\":\"Eglinton\",\"orcid\":null,\"affiliation\":\"Swiss | ||
| 18 | Federal Institute of Technology of Zurich | 18 | Federal Institute of Technology of Zurich | ||
| 19 | THZ)\",\"iscorrespondingauthor\":null,\"contactemailaddress\":null}]", | 19 | THZ)\",\"iscorrespondingauthor\":null,\"contactemailaddress\":null}]", | ||
| 20 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.2c", | 20 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.2c", | ||
| 21 | "deposit_date": "2021-12-03", | 21 | "deposit_date": "2021-12-03", | ||
| 22 | "depositor": "Eric Epping", | 22 | "depositor": "Eric Epping", | ||
| 23 | "distribution_date": "2021-12-03", | 23 | "distribution_date": "2021-12-03", | ||
| 24 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 24 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 25 | Institute for Sea Research)", | 25 | Institute for Sea Research)", | ||
| 26 | "doi_date_published": "2021-12-08", | 26 | "doi_date_published": "2021-12-08", | ||
| n | 27 | "funding_references": "", | n | 27 | "funding_references": "[{\"name\":\"NWO |
| 28 | Rubicon\",\"awardnumber\":\"019.183EN.002\",\"awardtitle\":null}]", | ||||
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| 32 | "license_title": "CC0 1.0", | 33 | "license_title": "CC0 1.0", | ||
| 33 | "license_url": "https://creativecommons.org/publicdomain/zero/1.0/", | 34 | "license_url": "https://creativecommons.org/publicdomain/zero/1.0/", | ||
| 34 | "maintainer": null, | 35 | "maintainer": null, | ||
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| 36 | "metadata_created": "2024-10-22T11:45:38.230306", | 37 | "metadata_created": "2024-10-22T11:45:38.230306", | ||
| n | 37 | "metadata_modified": "2024-10-22T20:43:24.583697", | n | 38 | "metadata_modified": "2024-10-22T20:43:24.857897", |
| 38 | "name": "7bb2c", | 39 | "name": "7bb2c", | ||
| 39 | "notes": "The Baltic Sea experienced changes in marine input | 40 | "notes": "The Baltic Sea experienced changes in marine input | ||
| 40 | throughout the Holocene as substantial regional ice retreat led to | 41 | throughout the Holocene as substantial regional ice retreat led to | ||
| 41 | isostatic adjustment, eustatic sea level change, and periodic | 42 | isostatic adjustment, eustatic sea level change, and periodic | ||
| 42 | isolation from the North Sea. Here, we determine the distributions and | 43 | isolation from the North Sea. Here, we determine the distributions and | ||
| 43 | isotopic signatures of organic compounds preserved in a sediment | 44 | isotopic signatures of organic compounds preserved in a sediment | ||
| 44 | record spanning the last ~ 11 ka to reconstruct environmental change | 45 | record spanning the last ~ 11 ka to reconstruct environmental change | ||
| 45 | under these dynamic conditions. Carbon and hydrogen isotope ratios of | 46 | under these dynamic conditions. Carbon and hydrogen isotope ratios of | ||
| 46 | short-, mid-, and long-chain n-alkanes, along with long-chain diol and | 47 | short-, mid-, and long-chain n-alkanes, along with long-chain diol and | ||
| 47 | glycerol dialkyl glycerol tetraether abundances, were analyzed in | 48 | glycerol dialkyl glycerol tetraether abundances, were analyzed in | ||
| 48 | sediments sampled from the Arkona Basin in the southwestern Baltic | 49 | sediments sampled from the Arkona Basin in the southwestern Baltic | ||
| 49 | Sea. In the earlier part of the record (specifically 10 \u2013 8.2 | 50 | Sea. In the earlier part of the record (specifically 10 \u2013 8.2 | ||
| 50 | ka), hydrogen isotope values of higher plant-derived n-alkanes | 51 | ka), hydrogen isotope values of higher plant-derived n-alkanes | ||
| 51 | revealed a change in dominant water source from an ice melt-derived to | 52 | revealed a change in dominant water source from an ice melt-derived to | ||
| 52 | a precipitation-dominated hydrological regime. Following this shift in | 53 | a precipitation-dominated hydrological regime. Following this shift in | ||
| 53 | water source, carbon isotope values of n-alkanes suggest | 54 | water source, carbon isotope values of n-alkanes suggest | ||
| 54 | diversification of vegetation. Shifts in hydrology and vegetation did | 55 | diversification of vegetation. Shifts in hydrology and vegetation did | ||
| 55 | not coincide with established phase boundaries, but instead occurred | 56 | not coincide with established phase boundaries, but instead occurred | ||
| 56 | mid-phase or spanned phase transitions. For this reason, we suggest | 57 | mid-phase or spanned phase transitions. For this reason, we suggest | ||
| 57 | describing the Ancylus Lake in two phases: a meltwater phase (10.6 to | 58 | describing the Ancylus Lake in two phases: a meltwater phase (10.6 to | ||
| 58 | 9.2 ka) and a precipitation phase (9.2 to 7.7 ka). Our results | 59 | 9.2 ka) and a precipitation phase (9.2 to 7.7 ka). Our results | ||
| 59 | highlight the utility of using C and H isotope ratios in conjunction | 60 | highlight the utility of using C and H isotope ratios in conjunction | ||
| 60 | with other compound abundance proxies to better understand the complex | 61 | with other compound abundance proxies to better understand the complex | ||
| 61 | environmental change recorded in paleo archives.", | 62 | environmental change recorded in paleo archives.", | ||
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| 65 | "approval_status": "approved", | 66 | "approval_status": "approved", | ||
| 66 | "created": "2024-10-22T06:06:56.074257", | 67 | "created": "2024-10-22T06:06:56.074257", | ||
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| 74 | "title": "Royal Netherlands Institute for Sea Research", | 75 | "title": "Royal Netherlands Institute for Sea Research", | ||
| 75 | "type": "organization" | 76 | "type": "organization" | ||
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| 172 | "state": "active", | 173 | "state": "active", | ||
| 173 | "subject": "Earth and Environmental Sciences", | 174 | "subject": "Earth and Environmental Sciences", | ||
| 174 | "tags": [ | 175 | "tags": [ | ||
| 175 | { | 176 | { | ||
| 176 | "display_name": "Baltic Sea", | 177 | "display_name": "Baltic Sea", | ||
| 177 | "id": "6590bb10-f51d-4c1c-a338-8552211eb811", | 178 | "id": "6590bb10-f51d-4c1c-a338-8552211eb811", | ||
| 178 | "name": "Baltic Sea", | 179 | "name": "Baltic Sea", | ||
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| 185 | "name": "Carbon isotopes", | 186 | "name": "Carbon isotopes", | ||
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| 190 | "display_name": "Holocene", | 191 | "display_name": "Holocene", | ||
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| 195 | }, | 196 | }, | ||
| 196 | { | 197 | { | ||
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| 199 | "name": "Hydrogen isotopes", | 200 | "name": "Hydrogen isotopes", | ||
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| 201 | "vocabulary_id": null | 202 | "vocabulary_id": null | ||
| 202 | }, | 203 | }, | ||
| 203 | { | 204 | { | ||
| 204 | "display_name": "biomarkers", | 205 | "display_name": "biomarkers", | ||
| 205 | "id": "102b4608-b092-45e6-a420-376a10fe89c6", | 206 | "id": "102b4608-b092-45e6-a420-376a10fe89c6", | ||
| 206 | "name": "biomarkers", | 207 | "name": "biomarkers", | ||
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| 209 | }, | 210 | }, | ||
| 210 | { | 211 | { | ||
| 211 | "display_name": "n-alkanes", | 212 | "display_name": "n-alkanes", | ||
| 212 | "id": "3d10fddf-8de9-4d5e-9421-b441f8e90a69", | 213 | "id": "3d10fddf-8de9-4d5e-9421-b441f8e90a69", | ||
| 213 | "name": "n-alkanes", | 214 | "name": "n-alkanes", | ||
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| 216 | } | 217 | } | ||
| 217 | ], | 218 | ], | ||
| 218 | "title": "Co-evolution of the terrestrial and aquatic ecosystem in | 219 | "title": "Co-evolution of the terrestrial and aquatic ecosystem in | ||
| 219 | the Holocene Baltic Sea", | 220 | the Holocene Baltic Sea", | ||
| 220 | "type": "dataset", | 221 | "type": "dataset", | ||
| 221 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.2c", | 222 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.2c", | ||
| t | 222 | "version": "1" | t | 223 | "version": "2" |
| 223 | } | 224 | } |