Changes
On November 30, 2024 at 9:21:44 AM UTC, admin:
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Removed tag mid-Pleistocene transition from A 1.3 million-year benthic foraminiferal record at IODP Site U1391, Portuguese margin
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Added the following tags to A 1.3 million-year benthic foraminiferal record at IODP Site U1391, Portuguese margin
f | 1 | { | f | 1 | { |
2 | "author": "Guo, Qimei", | 2 | "author": "Guo, Qimei", | ||
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.923308", | 6 | "doi": "10.1594/PANGAEA.923308", | ||
7 | "doi_date_published": "2020", | 7 | "doi_date_published": "2020", | ||
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": "Li, Baohua", | 12 | "extra_author": "Li, Baohua", | ||
13 | "familyName": "Li", | 13 | "familyName": "Li", | ||
14 | "givenName": "Baohua", | 14 | "givenName": "Baohua", | ||
15 | "orcid": "" | 15 | "orcid": "" | ||
16 | }, | 16 | }, | ||
17 | { | 17 | { | ||
18 | "extra_author": "Voelker, Antje H L", | 18 | "extra_author": "Voelker, Antje H L", | ||
19 | "familyName": "Voelker", | 19 | "familyName": "Voelker", | ||
20 | "givenName": "Antje H L", | 20 | "givenName": "Antje H L", | ||
21 | "orcid": "0000-0001-6465-6023" | 21 | "orcid": "0000-0001-6465-6023" | ||
22 | }, | 22 | }, | ||
23 | { | 23 | { | ||
24 | "extra_author": "Kim, Jin Kyoung", | 24 | "extra_author": "Kim, Jin Kyoung", | ||
25 | "familyName": "Kim", | 25 | "familyName": "Kim", | ||
26 | "givenName": "Jin Kyoung", | 26 | "givenName": "Jin Kyoung", | ||
27 | "orcid": "" | 27 | "orcid": "" | ||
28 | } | 28 | } | ||
29 | ], | 29 | ], | ||
30 | "familyName": "Guo", | 30 | "familyName": "Guo", | ||
31 | "givenName": "Qimei", | 31 | "givenName": "Qimei", | ||
32 | "groups": [], | 32 | "groups": [], | ||
33 | "id": "e1804f53-54ae-4a89-b628-99c1590b02d4", | 33 | "id": "e1804f53-54ae-4a89-b628-99c1590b02d4", | ||
34 | "isopen": false, | 34 | "isopen": false, | ||
35 | "license_id": "CC-BY-4.0", | 35 | "license_id": "CC-BY-4.0", | ||
36 | "license_title": "CC-BY-4.0", | 36 | "license_title": "CC-BY-4.0", | ||
37 | "metadata_created": "2024-11-30T08:47:38.319774", | 37 | "metadata_created": "2024-11-30T08:47:38.319774", | ||
n | 38 | "metadata_modified": "2024-11-30T08:47:38.319780", | n | 38 | "metadata_modified": "2024-11-30T09:21:44.571819", |
39 | "name": "png-doi-10-1594-pangaea-923308", | 39 | "name": "png-doi-10-1594-pangaea-923308", | ||
40 | "notes": "Reconstruction of the Mediterranean Outflow Water (MOW) | 40 | "notes": "Reconstruction of the Mediterranean Outflow Water (MOW) | ||
41 | dynamics in the geologic past contributes to exploring its influence | 41 | dynamics in the geologic past contributes to exploring its influence | ||
42 | on the North Atlantic Ocean circulation and the climate. The middle | 42 | on the North Atlantic Ocean circulation and the climate. The middle | ||
43 | Pleistocene transition (MPT) is one of the most important | 43 | Pleistocene transition (MPT) is one of the most important | ||
44 | characteristics of Quaternary climate change, but until now, research | 44 | characteristics of Quaternary climate change, but until now, research | ||
45 | on the MOW variability during this time interval has been limited. | 45 | on the MOW variability during this time interval has been limited. | ||
46 | This work presents the first continuous and high-resolution (~2 kyr) | 46 | This work presents the first continuous and high-resolution (~2 kyr) | ||
47 | foraminiferal stable oxygen and carbon isotopes and benthic | 47 | foraminiferal stable oxygen and carbon isotopes and benthic | ||
48 | foraminiferal records from Integrated Ocean Drilling Program (IODP) | 48 | foraminiferal records from Integrated Ocean Drilling Program (IODP) | ||
49 | Site U1391, drilled off the Portuguese margin in the Northeast | 49 | Site U1391, drilled off the Portuguese margin in the Northeast | ||
50 | Atlantic Ocean, to decipher the MOW variability over the last 1.3 | 50 | Atlantic Ocean, to decipher the MOW variability over the last 1.3 | ||
51 | myr.", | 51 | myr.", | ||
52 | "num_resources": 0, | 52 | "num_resources": 0, | ||
n | 53 | "num_tags": 4, | n | 53 | "num_tags": 5, |
54 | "orcid": "", | 54 | "orcid": "", | ||
55 | "organization": { | 55 | "organization": { | ||
56 | "approval_status": "approved", | 56 | "approval_status": "approved", | ||
57 | "created": "2024-11-30T08:45:56.114425", | 57 | "created": "2024-11-30T08:45:56.114425", | ||
58 | "description": "PANGAEA (Data Publisher for Earth & Environmental | 58 | "description": "PANGAEA (Data Publisher for Earth & Environmental | ||
59 | Science): The information system PANGAEA is operated as an Open Access | 59 | Science): The information system PANGAEA is operated as an Open Access | ||
60 | library aimed at archiving, publishing and distributing georeferenced | 60 | library aimed at archiving, publishing and distributing georeferenced | ||
61 | data from earth system research. PANGAEA guarantees long-term | 61 | data from earth system research. PANGAEA guarantees long-term | ||
62 | availability (greater than 10 years) of its content. PANGAEA is open | 62 | availability (greater than 10 years) of its content. PANGAEA is open | ||
63 | to any project, institution, or individual scientist to use or to | 63 | to any project, institution, or individual scientist to use or to | ||
64 | archive and publish data. PANGAEA focuses on georeferenced | 64 | archive and publish data. PANGAEA focuses on georeferenced | ||
65 | observational data, experimental data, and models/simulations. | 65 | observational data, experimental data, and models/simulations. | ||
66 | Citability, comprehensive metadata descriptions, interoperability of | 66 | Citability, comprehensive metadata descriptions, interoperability of | ||
67 | data and metadata, a high degree of structural and semantic | 67 | data and metadata, a high degree of structural and semantic | ||
68 | harmonization of the data inventory as well as the commitment of the | 68 | harmonization of the data inventory as well as the commitment of the | ||
69 | hosting institutions ensures FAIRness of archived data.", | 69 | hosting institutions ensures FAIRness of archived data.", | ||
70 | "id": "c4bc8467-02a4-44bb-8114-5fa3b31fd7d4", | 70 | "id": "c4bc8467-02a4-44bb-8114-5fa3b31fd7d4", | ||
71 | "image_url": "pangaea_topiclandsurface.png", | 71 | "image_url": "pangaea_topiclandsurface.png", | ||
72 | "is_organization": true, | 72 | "is_organization": true, | ||
73 | "name": "pangaea_landsurface", | 73 | "name": "pangaea_landsurface", | ||
74 | "state": "active", | 74 | "state": "active", | ||
75 | "title": "PANGAEA (Land Surface)", | 75 | "title": "PANGAEA (Land Surface)", | ||
76 | "type": "organization" | 76 | "type": "organization" | ||
77 | }, | 77 | }, | ||
78 | "owner_org": "c4bc8467-02a4-44bb-8114-5fa3b31fd7d4", | 78 | "owner_org": "c4bc8467-02a4-44bb-8114-5fa3b31fd7d4", | ||
79 | "private": false, | 79 | "private": false, | ||
80 | "publication_year": "2020", | 80 | "publication_year": "2020", | ||
81 | "related_identifiers": [ | 81 | "related_identifiers": [ | ||
82 | { | 82 | { | ||
83 | "authors": "Guo Qimei,Li Baohua,Voelker Antje H L,Kim Jin | 83 | "authors": "Guo Qimei,Li Baohua,Voelker Antje H L,Kim Jin | ||
84 | Kyoung,Guo Qimei,Li Baohua,Kim Jin Kyoung,Expedition 339 Scientists ", | 84 | Kyoung,Guo Qimei,Li Baohua,Kim Jin Kyoung,Expedition 339 Scientists ", | ||
85 | "email_authors": | 85 | "email_authors": | ||
86 | r@ipma.pt,jink92@kordi.re.kr,qmguo@nigpas.ac.cn,,jink92@kordi.re.kr,", | 86 | r@ipma.pt,jink92@kordi.re.kr,qmguo@nigpas.ac.cn,,jink92@kordi.re.kr,", | ||
87 | "identifier": "https://doi.org/10.1016/j.quascirev.2020.106567", | 87 | "identifier": "https://doi.org/10.1016/j.quascirev.2020.106567", | ||
88 | "identifier_type": "DOI", | 88 | "identifier_type": "DOI", | ||
89 | "orcid_authors": ",,0000-0001-6465-6023,,,,,", | 89 | "orcid_authors": ",,0000-0001-6465-6023,,,,,", | ||
90 | "relation_type": "References", | 90 | "relation_type": "References", | ||
91 | "source": "Quaternary Science Reviews", | 91 | "source": "Quaternary Science Reviews", | ||
92 | "title": "Mediterranean Outflow Water dynamics across the middle | 92 | "title": "Mediterranean Outflow Water dynamics across the middle | ||
93 | Pleistocene transition based on a 1.3 million-year benthic | 93 | Pleistocene transition based on a 1.3 million-year benthic | ||
94 | foraminiferal record off the Portuguese margin", | 94 | foraminiferal record off the Portuguese margin", | ||
95 | "year": "2020" | 95 | "year": "2020" | ||
96 | }, | 96 | }, | ||
97 | { | 97 | { | ||
98 | "authors": "Guo Qimei,Li Baohua,Voelker Antje H L,Kim Jin | 98 | "authors": "Guo Qimei,Li Baohua,Voelker Antje H L,Kim Jin | ||
99 | Kyoung,Guo Qimei,Li Baohua,Kim Jin Kyoung,Expedition 339 Scientists ", | 99 | Kyoung,Guo Qimei,Li Baohua,Kim Jin Kyoung,Expedition 339 Scientists ", | ||
100 | "email_authors": | 100 | "email_authors": | ||
101 | r@ipma.pt,jink92@kordi.re.kr,qmguo@nigpas.ac.cn,,jink92@kordi.re.kr,", | 101 | r@ipma.pt,jink92@kordi.re.kr,qmguo@nigpas.ac.cn,,jink92@kordi.re.kr,", | ||
102 | "identifier": "https://doi.org/10.1016/j.gloplacha.2016.11.004", | 102 | "identifier": "https://doi.org/10.1016/j.gloplacha.2016.11.004", | ||
103 | "identifier_type": "DOI", | 103 | "identifier_type": "DOI", | ||
104 | "orcid_authors": ",,0000-0001-6465-6023,,,,,", | 104 | "orcid_authors": ",,0000-0001-6465-6023,,,,,", | ||
105 | "relation_type": "References", | 105 | "relation_type": "References", | ||
106 | "source": "Global and Planetary Change", | 106 | "source": "Global and Planetary Change", | ||
107 | "title": "Benthic foraminiferal assemblages and bottom water | 107 | "title": "Benthic foraminiferal assemblages and bottom water | ||
108 | evolution off the Portuguese margin since the Middle Pleistocene", | 108 | evolution off the Portuguese margin since the Middle Pleistocene", | ||
109 | "year": "2017" | 109 | "year": "2017" | ||
110 | } | 110 | } | ||
111 | ], | 111 | ], | ||
112 | "relationships_as_object": [], | 112 | "relationships_as_object": [], | ||
113 | "relationships_as_subject": [], | 113 | "relationships_as_subject": [], | ||
114 | "repository_name": "PANGAEA (Data Publisher for Earth & | 114 | "repository_name": "PANGAEA (Data Publisher for Earth & | ||
115 | Environmental Science)", | 115 | Environmental Science)", | ||
116 | "resource_type": "application/zip - filename: Guo-etal_2020", | 116 | "resource_type": "application/zip - filename: Guo-etal_2020", | ||
117 | "resources": [], | 117 | "resources": [], | ||
118 | "source_metadata_created": "2020", | 118 | "source_metadata_created": "2020", | ||
119 | "source_metadata_modified": "", | 119 | "source_metadata_modified": "", | ||
120 | "state": "active", | 120 | "state": "active", | ||
121 | "subject_areas": [ | 121 | "subject_areas": [ | ||
122 | { | 122 | { | ||
123 | "subject_area_additional": "", | 123 | "subject_area_additional": "", | ||
124 | "subject_area_name": "LandSurface" | 124 | "subject_area_name": "LandSurface" | ||
125 | }, | 125 | }, | ||
126 | { | 126 | { | ||
127 | "subject_area_additional": "", | 127 | "subject_area_additional": "", | ||
128 | "subject_area_name": "Lithosphere" | 128 | "subject_area_name": "Lithosphere" | ||
129 | } | 129 | } | ||
130 | ], | 130 | ], | ||
131 | "tags": [ | 131 | "tags": [ | ||
132 | { | 132 | { | ||
133 | "display_name": "Benthic foraminifera", | 133 | "display_name": "Benthic foraminifera", | ||
134 | "id": "71eb9196-bb01-47ad-94b8-6c61104f66b5", | 134 | "id": "71eb9196-bb01-47ad-94b8-6c61104f66b5", | ||
135 | "name": "Benthic foraminifera", | 135 | "name": "Benthic foraminifera", | ||
136 | "state": "active", | 136 | "state": "active", | ||
137 | "vocabulary_id": null | 137 | "vocabulary_id": null | ||
138 | }, | 138 | }, | ||
139 | { | 139 | { | ||
140 | "display_name": "IODP Site U1391", | 140 | "display_name": "IODP Site U1391", | ||
141 | "id": "02baf401-88d1-48d8-901b-21966d8ea665", | 141 | "id": "02baf401-88d1-48d8-901b-21966d8ea665", | ||
142 | "name": "IODP Site U1391", | 142 | "name": "IODP Site U1391", | ||
143 | "state": "active", | 143 | "state": "active", | ||
144 | "vocabulary_id": null | 144 | "vocabulary_id": null | ||
145 | }, | 145 | }, | ||
146 | { | 146 | { | ||
n | n | 147 | "display_name": "Pleistocene transition", | ||
148 | "id": "82246b19-a04c-4eb6-8200-d68664c2f3f2", | ||||
149 | "name": "Pleistocene transition", | ||||
150 | "state": "active", | ||||
151 | "vocabulary_id": null | ||||
152 | }, | ||||
153 | { | ||||
147 | "display_name": "Stable isotopes", | 154 | "display_name": "Stable isotopes", | ||
148 | "id": "09acb6c0-191f-43f4-8056-58ea572067c0", | 155 | "id": "09acb6c0-191f-43f4-8056-58ea572067c0", | ||
149 | "name": "Stable isotopes", | 156 | "name": "Stable isotopes", | ||
150 | "state": "active", | 157 | "state": "active", | ||
151 | "vocabulary_id": null | 158 | "vocabulary_id": null | ||
152 | }, | 159 | }, | ||
153 | { | 160 | { | ||
t | 154 | "display_name": "mid-Pleistocene transition", | t | 161 | "display_name": "mid", |
155 | "id": "55fe70a1-9b94-4b5a-a7f1-256a81e8cd01", | 162 | "id": "c29e00ed-dfdb-4acf-9d4a-0a4a115dce53", | ||
156 | "name": "mid-Pleistocene transition", | 163 | "name": "mid", | ||
157 | "state": "active", | 164 | "state": "active", | ||
158 | "vocabulary_id": null | 165 | "vocabulary_id": null | ||
159 | } | 166 | } | ||
160 | ], | 167 | ], | ||
161 | "title": "A 1.3 million-year benthic foraminiferal record at IODP | 168 | "title": "A 1.3 million-year benthic foraminiferal record at IODP | ||
162 | Site U1391, Portuguese margin", | 169 | Site U1391, Portuguese margin", | ||
163 | "type": "vdataset", | 170 | "type": "vdataset", | ||
164 | "url": "https://doi.org/10.1594/PANGAEA.923308" | 171 | "url": "https://doi.org/10.1594/PANGAEA.923308" | ||
165 | } | 172 | } |