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On October 22, 2024, 11:45:38 AM UTC,
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Added resource WeissLattaud et al Table 1.csv to 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:10.33591/nioz/7b.b.2c", | 20 | "dataset_persistent_id": "DOI:10.33591/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", | ||
| 27 | "funding_references": "", | 27 | "funding_references": "", | ||
| 28 | "groups": [], | 28 | "groups": [], | ||
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| 34 | "metadata_created": "2024-10-22T11:45:38.230306", | 34 | "metadata_created": "2024-10-22T11:45:38.230306", | ||
| n | 35 | "metadata_modified": "2024-10-22T11:45:38.230313", | n | 35 | "metadata_modified": "2024-10-22T11:45:38.587664", |
| 36 | "name": "7bb2c", | 36 | "name": "7bb2c", | ||
| 37 | "notes": "The Baltic Sea experienced changes in marine input | 37 | "notes": "The Baltic Sea experienced changes in marine input | ||
| 38 | throughout the Holocene as substantial regional ice retreat led to | 38 | throughout the Holocene as substantial regional ice retreat led to | ||
| 39 | isostatic adjustment, eustatic sea level change, and periodic | 39 | isostatic adjustment, eustatic sea level change, and periodic | ||
| 40 | isolation from the North Sea. Here, we determine the distributions and | 40 | isolation from the North Sea. Here, we determine the distributions and | ||
| 41 | isotopic signatures of organic compounds preserved in a sediment | 41 | isotopic signatures of organic compounds preserved in a sediment | ||
| 42 | record spanning the last ~ 11 ka to reconstruct environmental change | 42 | record spanning the last ~ 11 ka to reconstruct environmental change | ||
| 43 | under these dynamic conditions. Carbon and hydrogen isotope ratios of | 43 | under these dynamic conditions. Carbon and hydrogen isotope ratios of | ||
| 44 | short-, mid-, and long-chain n-alkanes, along with long-chain diol and | 44 | short-, mid-, and long-chain n-alkanes, along with long-chain diol and | ||
| 45 | glycerol dialkyl glycerol tetraether abundances, were analyzed in | 45 | glycerol dialkyl glycerol tetraether abundances, were analyzed in | ||
| 46 | sediments sampled from the Arkona Basin in the southwestern Baltic | 46 | sediments sampled from the Arkona Basin in the southwestern Baltic | ||
| 47 | Sea. In the earlier part of the record (specifically 10 \u2013 8.2 | 47 | Sea. In the earlier part of the record (specifically 10 \u2013 8.2 | ||
| 48 | ka), hydrogen isotope values of higher plant-derived n-alkanes | 48 | ka), hydrogen isotope values of higher plant-derived n-alkanes | ||
| 49 | revealed a change in dominant water source from an ice melt-derived to | 49 | revealed a change in dominant water source from an ice melt-derived to | ||
| 50 | a precipitation-dominated hydrological regime. Following this shift in | 50 | a precipitation-dominated hydrological regime. Following this shift in | ||
| 51 | water source, carbon isotope values of n-alkanes suggest | 51 | water source, carbon isotope values of n-alkanes suggest | ||
| 52 | diversification of vegetation. Shifts in hydrology and vegetation did | 52 | diversification of vegetation. Shifts in hydrology and vegetation did | ||
| 53 | not coincide with established phase boundaries, but instead occurred | 53 | not coincide with established phase boundaries, but instead occurred | ||
| 54 | mid-phase or spanned phase transitions. For this reason, we suggest | 54 | mid-phase or spanned phase transitions. For this reason, we suggest | ||
| 55 | describing the Ancylus Lake in two phases: a meltwater phase (10.6 to | 55 | describing the Ancylus Lake in two phases: a meltwater phase (10.6 to | ||
| 56 | 9.2 ka) and a precipitation phase (9.2 to 7.7 ka). Our results | 56 | 9.2 ka) and a precipitation phase (9.2 to 7.7 ka). Our results | ||
| 57 | highlight the utility of using C and H isotope ratios in conjunction | 57 | highlight the utility of using C and H isotope ratios in conjunction | ||
| 58 | with other compound abundance proxies to better understand the complex | 58 | with other compound abundance proxies to better understand the complex | ||
| 59 | environmental change recorded in paleo archives.", | 59 | environmental change recorded in paleo archives.", | ||
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| 63 | "approval_status": "approved", | 63 | "approval_status": "approved", | ||
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| 72 | "title": "Royal Netherlands Institute for Sea Research", | 72 | "title": "Royal Netherlands Institute for Sea Research", | ||
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| 81 | "state": "active", | 104 | "state": "active", | ||
| 82 | "subject": "Earth and Environmental Sciences", | 105 | "subject": "Earth and Environmental Sciences", | ||
| 83 | "tags": [ | 106 | "tags": [ | ||
| 84 | { | 107 | { | ||
| 85 | "display_name": "Baltic Sea", | 108 | "display_name": "Baltic Sea", | ||
| 86 | "id": "6590bb10-f51d-4c1c-a338-8552211eb811", | 109 | "id": "6590bb10-f51d-4c1c-a338-8552211eb811", | ||
| 87 | "name": "Baltic Sea", | 110 | "name": "Baltic Sea", | ||
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| 97 | }, | 120 | }, | ||
| 98 | { | 121 | { | ||
| 99 | "display_name": "Holocene", | 122 | "display_name": "Holocene", | ||
| 100 | "id": "5483c3f3-deb1-4929-971b-a253b6f90517", | 123 | "id": "5483c3f3-deb1-4929-971b-a253b6f90517", | ||
| 101 | "name": "Holocene", | 124 | "name": "Holocene", | ||
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| 104 | }, | 127 | }, | ||
| 105 | { | 128 | { | ||
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| 108 | "name": "Hydrogen isotopes", | 131 | "name": "Hydrogen isotopes", | ||
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| 111 | }, | 134 | }, | ||
| 112 | { | 135 | { | ||
| 113 | "display_name": "biomarkers", | 136 | "display_name": "biomarkers", | ||
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| 115 | "name": "biomarkers", | 138 | "name": "biomarkers", | ||
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| 117 | "vocabulary_id": null | 140 | "vocabulary_id": null | ||
| 118 | }, | 141 | }, | ||
| 119 | { | 142 | { | ||
| 120 | "display_name": "n-alkanes", | 143 | "display_name": "n-alkanes", | ||
| 121 | "id": "3d10fddf-8de9-4d5e-9421-b441f8e90a69", | 144 | "id": "3d10fddf-8de9-4d5e-9421-b441f8e90a69", | ||
| 122 | "name": "n-alkanes", | 145 | "name": "n-alkanes", | ||
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| 124 | "vocabulary_id": null | 147 | "vocabulary_id": null | ||
| 125 | } | 148 | } | ||
| 126 | ], | 149 | ], | ||
| 127 | "title": "Co-evolution of the terrestrial and aquatic ecosystem in | 150 | "title": "Co-evolution of the terrestrial and aquatic ecosystem in | ||
| 128 | the Holocene Baltic Sea", | 151 | the Holocene Baltic Sea", | ||
| 129 | "type": "dataset", | 152 | "type": "dataset", | ||
| 130 | "url": "https://dataportal.nioz.nl/doi/10.33591/nioz/7b.b.2c", | 153 | "url": "https://dataportal.nioz.nl/doi/10.33591/nioz/7b.b.2c", | ||
| 131 | "version": "1" | 154 | "version": "1" | ||
| 132 | } | 155 | } |