Changes
On November 30, 2024 at 9:22:18 AM UTC, admin:
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Removed tag Mg-Ca from Mg/Ca and isotopic data of sediment core PS75/059-2
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Added the following tags to Mg/Ca and isotopic data of sediment core PS75/059-2
f | 1 | { | f | 1 | { |
2 | "author": "Tapia, Ra\u00fal", | 2 | "author": "Tapia, Ra\u00fal", | ||
3 | "author_email": "", | 3 | "author_email": "", | ||
4 | "citation": [], | 4 | "citation": [], | ||
5 | "creator_user_id": "17755db4-395a-4b3b-ac09-e8e3484ca700", | 5 | "creator_user_id": "17755db4-395a-4b3b-ac09-e8e3484ca700", | ||
6 | "doi": "10.1594/PANGAEA.899276", | 6 | "doi": "10.1594/PANGAEA.899276", | ||
7 | "doi_date_published": "2019", | 7 | "doi_date_published": "2019", | ||
8 | "doi_publisher": "", | 8 | "doi_publisher": "", | ||
9 | "doi_status": "True", | 9 | "doi_status": "True", | ||
10 | "extra_authors": [ | 10 | "extra_authors": [ | ||
11 | { | 11 | { | ||
12 | "extra_author": "N\u00fcrnberg, Dirk", | 12 | "extra_author": "N\u00fcrnberg, Dirk", | ||
13 | "familyName": "N\u00fcrnberg", | 13 | "familyName": "N\u00fcrnberg", | ||
14 | "givenName": "Dirk", | 14 | "givenName": "Dirk", | ||
15 | "orcid": "" | 15 | "orcid": "" | ||
16 | }, | 16 | }, | ||
17 | { | 17 | { | ||
18 | "extra_author": "Ho, Sze Ling", | 18 | "extra_author": "Ho, Sze Ling", | ||
19 | "familyName": "Ho", | 19 | "familyName": "Ho", | ||
20 | "givenName": "Sze Ling", | 20 | "givenName": "Sze Ling", | ||
21 | "orcid": "0000-0002-4898-9036" | 21 | "orcid": "0000-0002-4898-9036" | ||
22 | }, | 22 | }, | ||
23 | { | 23 | { | ||
24 | "extra_author": "Lamy, Frank", | 24 | "extra_author": "Lamy, Frank", | ||
25 | "familyName": "Lamy", | 25 | "familyName": "Lamy", | ||
26 | "givenName": "Frank", | 26 | "givenName": "Frank", | ||
27 | "orcid": "0000-0001-5952-1765" | 27 | "orcid": "0000-0001-5952-1765" | ||
28 | }, | 28 | }, | ||
29 | { | 29 | { | ||
30 | "extra_author": "Ullermann, Johannes", | 30 | "extra_author": "Ullermann, Johannes", | ||
31 | "familyName": "Ullermann", | 31 | "familyName": "Ullermann", | ||
32 | "givenName": "Johannes", | 32 | "givenName": "Johannes", | ||
33 | "orcid": "" | 33 | "orcid": "" | ||
34 | }, | 34 | }, | ||
35 | { | 35 | { | ||
36 | "extra_author": "Gersonde, Rainer", | 36 | "extra_author": "Gersonde, Rainer", | ||
37 | "familyName": "Gersonde", | 37 | "familyName": "Gersonde", | ||
38 | "givenName": "Rainer", | 38 | "givenName": "Rainer", | ||
39 | "orcid": "0000-0002-7340-6269" | 39 | "orcid": "0000-0002-7340-6269" | ||
40 | }, | 40 | }, | ||
41 | { | 41 | { | ||
42 | "extra_author": "Tiedemann, Ralf", | 42 | "extra_author": "Tiedemann, Ralf", | ||
43 | "familyName": "Tiedemann", | 43 | "familyName": "Tiedemann", | ||
44 | "givenName": "Ralf", | 44 | "givenName": "Ralf", | ||
45 | "orcid": "0000-0001-7211-8049" | 45 | "orcid": "0000-0001-7211-8049" | ||
46 | } | 46 | } | ||
47 | ], | 47 | ], | ||
48 | "familyName": "Tapia", | 48 | "familyName": "Tapia", | ||
49 | "givenName": "Ra\u00fal", | 49 | "givenName": "Ra\u00fal", | ||
50 | "groups": [], | 50 | "groups": [], | ||
51 | "id": "2713a559-aa24-458d-b049-d2705818d544", | 51 | "id": "2713a559-aa24-458d-b049-d2705818d544", | ||
52 | "isopen": false, | 52 | "isopen": false, | ||
53 | "license_id": "CC-BY-4.0", | 53 | "license_id": "CC-BY-4.0", | ||
54 | "license_title": "CC-BY-4.0", | 54 | "license_title": "CC-BY-4.0", | ||
55 | "metadata_created": "2024-11-30T08:50:45.743980", | 55 | "metadata_created": "2024-11-30T08:50:45.743980", | ||
n | 56 | "metadata_modified": "2024-11-30T08:50:45.743985", | n | 56 | "metadata_modified": "2024-11-30T09:22:18.345218", |
57 | "name": "png-doi-10-1594-pangaea-899276", | 57 | "name": "png-doi-10-1594-pangaea-899276", | ||
58 | "notes": "Southern Ocean Intermediate Waters (SOIWs), such as | 58 | "notes": "Southern Ocean Intermediate Waters (SOIWs), such as | ||
59 | Antarctic Intermediate Water and Subantarctic Mode Water, play a key | 59 | Antarctic Intermediate Water and Subantarctic Mode Water, play a key | ||
60 | role in modulating the global climate on glacial-interglacial time | 60 | role in modulating the global climate on glacial-interglacial time | ||
61 | scales. They link the Southern Ocean and the tropics via mechanisms | 61 | scales. They link the Southern Ocean and the tropics via mechanisms | ||
62 | such as \"oceanic tunneling\" that transport climatic signals across | 62 | such as \"oceanic tunneling\" that transport climatic signals across | ||
63 | latitudes. Despite their importance, the past evolution of the SOIWs | 63 | latitudes. Despite their importance, the past evolution of the SOIWs | ||
64 | in the Central South Pacific is largely unknown. Here we compare | 64 | in the Central South Pacific is largely unknown. Here we compare | ||
65 | paired Mg/Ca-temperature, stable carbon (\u03b413C) and oxygen | 65 | paired Mg/Ca-temperature, stable carbon (\u03b413C) and oxygen | ||
66 | (\u03b418O) isotope records from surface-dwelling and deep-dwelling | 66 | (\u03b418O) isotope records from surface-dwelling and deep-dwelling | ||
67 | planktic foraminifera to infer changes in the water column structure | 67 | planktic foraminifera to infer changes in the water column structure | ||
68 | for the last 260 ka in the Central South Pacific (54\u00b0 S). Our | 68 | for the last 260 ka in the Central South Pacific (54\u00b0 S). Our | ||
69 | study focuses on the subsurface oceanographic variability controlled | 69 | study focuses on the subsurface oceanographic variability controlled | ||
70 | by SOIWs, which are subducted at the Subantarctic Front.\n\nOur data | 70 | by SOIWs, which are subducted at the Subantarctic Front.\n\nOur data | ||
71 | show that the subsurface ocean in the Central South Pacific was colder | 71 | show that the subsurface ocean in the Central South Pacific was colder | ||
72 | and fresher during glacial stages than during the Holocene (0-10 ka | 72 | and fresher during glacial stages than during the Holocene (0-10 ka | ||
73 | BP), suggesting a general glacial enhanced presence of Antarctic | 73 | BP), suggesting a general glacial enhanced presence of Antarctic | ||
74 | Intermediate Water, in agreement with previous studies from the | 74 | Intermediate Water, in agreement with previous studies from the | ||
75 | Eastern Equatorial Pacific and the Southeast Pacific. However, the | 75 | Eastern Equatorial Pacific and the Southeast Pacific. However, the | ||
76 | subsurface ocean salinity differs for both glacial stages, with | 76 | subsurface ocean salinity differs for both glacial stages, with | ||
77 | fresher condition during the Last Glacial Maximum (LGM; \u223c26.5-19 | 77 | fresher condition during the Last Glacial Maximum (LGM; \u223c26.5-19 | ||
78 | ka BP) and more saline condition during the Penultimate Glacial | 78 | ka BP) and more saline condition during the Penultimate Glacial | ||
79 | Maximum (PGM; \u223c155-140 ka BP). The \u03b413C data also show | 79 | Maximum (PGM; \u223c155-140 ka BP). The \u03b413C data also show | ||
80 | contrasting conditions for both glacial time windows in the upper | 80 | contrasting conditions for both glacial time windows in the upper | ||
81 | water column, with a large depletion of 0.37\u2030 in \u03b413C from | 81 | water column, with a large depletion of 0.37\u2030 in \u03b413C from | ||
82 | the LGM values, suggests a larger contribution of \"old\" low | 82 | the LGM values, suggests a larger contribution of \"old\" low | ||
83 | \u03b413C deep waters at intermediate depths at the study site during | 83 | \u03b413C deep waters at intermediate depths at the study site during | ||
84 | the PGM, plausibly due to stronger upwelling in high southern | 84 | the PGM, plausibly due to stronger upwelling in high southern | ||
85 | latitudes. The dissimilar scenarios between the LGM and the PGM may | 85 | latitudes. The dissimilar scenarios between the LGM and the PGM may | ||
86 | have been caused by processes that are analogous to the phase-switch | 86 | have been caused by processes that are analogous to the phase-switch | ||
87 | in modern day Southern Annular Mode.", | 87 | in modern day Southern Annular Mode.", | ||
88 | "num_resources": 0, | 88 | "num_resources": 0, | ||
n | 89 | "num_tags": 7, | n | 89 | "num_tags": 8, |
90 | "orcid": "0000-0002-2620-7355", | 90 | "orcid": "0000-0002-2620-7355", | ||
91 | "organization": { | 91 | "organization": { | ||
92 | "approval_status": "approved", | 92 | "approval_status": "approved", | ||
93 | "created": "2024-11-30T08:45:56.114425", | 93 | "created": "2024-11-30T08:45:56.114425", | ||
94 | "description": "PANGAEA (Data Publisher for Earth & Environmental | 94 | "description": "PANGAEA (Data Publisher for Earth & Environmental | ||
95 | Science): The information system PANGAEA is operated as an Open Access | 95 | Science): The information system PANGAEA is operated as an Open Access | ||
96 | library aimed at archiving, publishing and distributing georeferenced | 96 | library aimed at archiving, publishing and distributing georeferenced | ||
97 | data from earth system research. PANGAEA guarantees long-term | 97 | data from earth system research. PANGAEA guarantees long-term | ||
98 | availability (greater than 10 years) of its content. PANGAEA is open | 98 | availability (greater than 10 years) of its content. PANGAEA is open | ||
99 | to any project, institution, or individual scientist to use or to | 99 | to any project, institution, or individual scientist to use or to | ||
100 | archive and publish data. PANGAEA focuses on georeferenced | 100 | archive and publish data. PANGAEA focuses on georeferenced | ||
101 | observational data, experimental data, and models/simulations. | 101 | observational data, experimental data, and models/simulations. | ||
102 | Citability, comprehensive metadata descriptions, interoperability of | 102 | Citability, comprehensive metadata descriptions, interoperability of | ||
103 | data and metadata, a high degree of structural and semantic | 103 | data and metadata, a high degree of structural and semantic | ||
104 | harmonization of the data inventory as well as the commitment of the | 104 | harmonization of the data inventory as well as the commitment of the | ||
105 | hosting institutions ensures FAIRness of archived data.", | 105 | hosting institutions ensures FAIRness of archived data.", | ||
106 | "id": "c4bc8467-02a4-44bb-8114-5fa3b31fd7d4", | 106 | "id": "c4bc8467-02a4-44bb-8114-5fa3b31fd7d4", | ||
107 | "image_url": "pangaea_topiclandsurface.png", | 107 | "image_url": "pangaea_topiclandsurface.png", | ||
108 | "is_organization": true, | 108 | "is_organization": true, | ||
109 | "name": "pangaea_landsurface", | 109 | "name": "pangaea_landsurface", | ||
110 | "state": "active", | 110 | "state": "active", | ||
111 | "title": "PANGAEA (Land Surface)", | 111 | "title": "PANGAEA (Land Surface)", | ||
112 | "type": "organization" | 112 | "type": "organization" | ||
113 | }, | 113 | }, | ||
114 | "owner_org": "c4bc8467-02a4-44bb-8114-5fa3b31fd7d4", | 114 | "owner_org": "c4bc8467-02a4-44bb-8114-5fa3b31fd7d4", | ||
115 | "private": false, | 115 | "private": false, | ||
116 | "publication_year": "2019", | 116 | "publication_year": "2019", | ||
117 | "related_identifiers": [ | 117 | "related_identifiers": [ | ||
118 | { | 118 | { | ||
119 | "authors": "Tapia Ra\u00fal,N\u00fcrnberg Dirk,Ho Sze Ling,Lamy | 119 | "authors": "Tapia Ra\u00fal,N\u00fcrnberg Dirk,Ho Sze Ling,Lamy | ||
120 | Frank,Ullermann Johannes,Gersonde Rainer,Tiedemann Ralf", | 120 | Frank,Ullermann Johannes,Gersonde Rainer,Tiedemann Ralf", | ||
121 | "email_authors": | 121 | "email_authors": | ||
122 | hannes.ullermann@awi.de,rainer.gersonde@awi.de,ralf.tiedemann@awi.de", | 122 | hannes.ullermann@awi.de,rainer.gersonde@awi.de,ralf.tiedemann@awi.de", | ||
123 | "identifier": "https://doi.org/10.1016/j.quascirev.2019.01.016", | 123 | "identifier": "https://doi.org/10.1016/j.quascirev.2019.01.016", | ||
124 | "identifier_type": "DOI", | 124 | "identifier_type": "DOI", | ||
125 | "orcid_authors": | 125 | "orcid_authors": | ||
126 | 98-9036,0000-0001-5952-1765,,0000-0002-7340-6269,0000-0001-7211-8049", | 126 | 98-9036,0000-0001-5952-1765,,0000-0002-7340-6269,0000-0001-7211-8049", | ||
127 | "relation_type": "IsSupplementTo", | 127 | "relation_type": "IsSupplementTo", | ||
128 | "source": "Quaternary Science Reviews", | 128 | "source": "Quaternary Science Reviews", | ||
129 | "title": "Glacial differences of Southern Ocean Intermediate | 129 | "title": "Glacial differences of Southern Ocean Intermediate | ||
130 | Waters in the Central South Pacific", | 130 | Waters in the Central South Pacific", | ||
131 | "year": "2019" | 131 | "year": "2019" | ||
132 | } | 132 | } | ||
133 | ], | 133 | ], | ||
134 | "relationships_as_object": [], | 134 | "relationships_as_object": [], | ||
135 | "relationships_as_subject": [], | 135 | "relationships_as_subject": [], | ||
136 | "repository_name": "PANGAEA (Data Publisher for Earth & | 136 | "repository_name": "PANGAEA (Data Publisher for Earth & | ||
137 | Environmental Science)", | 137 | Environmental Science)", | ||
138 | "resource_type": "text/tab-separated-values - filename: | 138 | "resource_type": "text/tab-separated-values - filename: | ||
139 | PS75_059-2_Mg-Ca", | 139 | PS75_059-2_Mg-Ca", | ||
140 | "resources": [], | 140 | "resources": [], | ||
141 | "source_metadata_created": "2019", | 141 | "source_metadata_created": "2019", | ||
142 | "source_metadata_modified": "", | 142 | "source_metadata_modified": "", | ||
143 | "state": "active", | 143 | "state": "active", | ||
144 | "subject_areas": [ | 144 | "subject_areas": [ | ||
145 | { | 145 | { | ||
146 | "subject_area_additional": "", | 146 | "subject_area_additional": "", | ||
147 | "subject_area_name": "BiologicalClassification" | 147 | "subject_area_name": "BiologicalClassification" | ||
148 | }, | 148 | }, | ||
149 | { | 149 | { | ||
150 | "subject_area_additional": "", | 150 | "subject_area_additional": "", | ||
151 | "subject_area_name": "LandSurface" | 151 | "subject_area_name": "LandSurface" | ||
152 | }, | 152 | }, | ||
153 | { | 153 | { | ||
154 | "subject_area_additional": "", | 154 | "subject_area_additional": "", | ||
155 | "subject_area_name": "Lithosphere" | 155 | "subject_area_name": "Lithosphere" | ||
156 | } | 156 | } | ||
157 | ], | 157 | ], | ||
158 | "tags": [ | 158 | "tags": [ | ||
159 | { | 159 | { | ||
n | n | 160 | "display_name": "Ca", | ||
161 | "id": "9a302f64-db48-41ee-9239-6fffffd8a770", | ||||
162 | "name": "Ca", | ||||
163 | "state": "active", | ||||
164 | "vocabulary_id": null | ||||
165 | }, | ||||
166 | { | ||||
160 | "display_name": "Intermediate water masses", | 167 | "display_name": "Intermediate water masses", | ||
161 | "id": "050f0c6a-eaa5-478e-bde8-d65b817cdd17", | 168 | "id": "050f0c6a-eaa5-478e-bde8-d65b817cdd17", | ||
162 | "name": "Intermediate water masses", | 169 | "name": "Intermediate water masses", | ||
163 | "state": "active", | 170 | "state": "active", | ||
164 | "vocabulary_id": null | 171 | "vocabulary_id": null | ||
165 | }, | 172 | }, | ||
166 | { | 173 | { | ||
167 | "display_name": "Last Glacial Maximum", | 174 | "display_name": "Last Glacial Maximum", | ||
168 | "id": "c1848ede-39c9-498b-9d79-7d7921e93a62", | 175 | "id": "c1848ede-39c9-498b-9d79-7d7921e93a62", | ||
169 | "name": "Last Glacial Maximum", | 176 | "name": "Last Glacial Maximum", | ||
170 | "state": "active", | 177 | "state": "active", | ||
171 | "vocabulary_id": null | 178 | "vocabulary_id": null | ||
172 | }, | 179 | }, | ||
173 | { | 180 | { | ||
t | 174 | "display_name": "Mg-Ca", | t | 181 | "display_name": "Mg", |
175 | "id": "60e05160-1aac-4070-8ec0-e5b9c67bbc6b", | 182 | "id": "86cca393-27f6-4ad7-b493-9311da283302", | ||
176 | "name": "Mg-Ca", | 183 | "name": "Mg", | ||
177 | "state": "active", | 184 | "state": "active", | ||
178 | "vocabulary_id": null | 185 | "vocabulary_id": null | ||
179 | }, | 186 | }, | ||
180 | { | 187 | { | ||
181 | "display_name": "Penultimate Glacial Maximum", | 188 | "display_name": "Penultimate Glacial Maximum", | ||
182 | "id": "2495bfa5-7b54-44a7-b70d-b6c226b04dda", | 189 | "id": "2495bfa5-7b54-44a7-b70d-b6c226b04dda", | ||
183 | "name": "Penultimate Glacial Maximum", | 190 | "name": "Penultimate Glacial Maximum", | ||
184 | "state": "active", | 191 | "state": "active", | ||
185 | "vocabulary_id": null | 192 | "vocabulary_id": null | ||
186 | }, | 193 | }, | ||
187 | { | 194 | { | ||
188 | "display_name": "Southern Ocean", | 195 | "display_name": "Southern Ocean", | ||
189 | "id": "3d94acbb-99a0-41f0-8ee2-b94cf0a00597", | 196 | "id": "3d94acbb-99a0-41f0-8ee2-b94cf0a00597", | ||
190 | "name": "Southern Ocean", | 197 | "name": "Southern Ocean", | ||
191 | "state": "active", | 198 | "state": "active", | ||
192 | "vocabulary_id": null | 199 | "vocabulary_id": null | ||
193 | }, | 200 | }, | ||
194 | { | 201 | { | ||
195 | "display_name": "Stable isotopes", | 202 | "display_name": "Stable isotopes", | ||
196 | "id": "09acb6c0-191f-43f4-8056-58ea572067c0", | 203 | "id": "09acb6c0-191f-43f4-8056-58ea572067c0", | ||
197 | "name": "Stable isotopes", | 204 | "name": "Stable isotopes", | ||
198 | "state": "active", | 205 | "state": "active", | ||
199 | "vocabulary_id": null | 206 | "vocabulary_id": null | ||
200 | }, | 207 | }, | ||
201 | { | 208 | { | ||
202 | "display_name": "planktic foraminifera", | 209 | "display_name": "planktic foraminifera", | ||
203 | "id": "4b866205-149a-4101-ab3a-dda8e93d246e", | 210 | "id": "4b866205-149a-4101-ab3a-dda8e93d246e", | ||
204 | "name": "planktic foraminifera", | 211 | "name": "planktic foraminifera", | ||
205 | "state": "active", | 212 | "state": "active", | ||
206 | "vocabulary_id": null | 213 | "vocabulary_id": null | ||
207 | } | 214 | } | ||
208 | ], | 215 | ], | ||
209 | "title": "Mg/Ca and isotopic data of sediment core PS75/059-2", | 216 | "title": "Mg/Ca and isotopic data of sediment core PS75/059-2", | ||
210 | "type": "vdataset", | 217 | "type": "vdataset", | ||
211 | "url": "https://doi.org/10.1594/PANGAEA.899276" | 218 | "url": "https://doi.org/10.1594/PANGAEA.899276" | ||
212 | } | 219 | } |