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On November 30, 2024 at 9:21:39 AM UTC, admin:
f | 1 | { | f | 1 | { |
2 | "author": "Perner, Kerstin", | 2 | "author": "Perner, Kerstin", | ||
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.898319", | 6 | "doi": "10.1594/PANGAEA.898319", | ||
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": "Moros, Matthias", | 12 | "extra_author": "Moros, Matthias", | ||
13 | "familyName": "Moros", | 13 | "familyName": "Moros", | ||
14 | "givenName": "Matthias", | 14 | "givenName": "Matthias", | ||
15 | "orcid": "" | 15 | "orcid": "" | ||
16 | }, | 16 | }, | ||
17 | { | 17 | { | ||
18 | "extra_author": "Jennings, Anne E", | 18 | "extra_author": "Jennings, Anne E", | ||
19 | "familyName": "Jennings", | 19 | "familyName": "Jennings", | ||
20 | "givenName": "Anne E", | 20 | "givenName": "Anne E", | ||
21 | "orcid": "0000-0003-3176-2916" | 21 | "orcid": "0000-0003-3176-2916" | ||
22 | }, | 22 | }, | ||
23 | { | 23 | { | ||
24 | "extra_author": "Lloyd, Jeremy M", | 24 | "extra_author": "Lloyd, Jeremy M", | ||
25 | "familyName": "Lloyd", | 25 | "familyName": "Lloyd", | ||
26 | "givenName": "Jeremy M", | 26 | "givenName": "Jeremy M", | ||
27 | "orcid": "" | 27 | "orcid": "" | ||
28 | }, | 28 | }, | ||
29 | { | 29 | { | ||
30 | "extra_author": "Knudsen, Karen Luise", | 30 | "extra_author": "Knudsen, Karen Luise", | ||
31 | "familyName": "Knudsen", | 31 | "familyName": "Knudsen", | ||
32 | "givenName": "Karen Luise", | 32 | "givenName": "Karen Luise", | ||
33 | "orcid": "" | 33 | "orcid": "" | ||
34 | } | 34 | } | ||
35 | ], | 35 | ], | ||
36 | "familyName": "Perner", | 36 | "familyName": "Perner", | ||
37 | "givenName": "Kerstin", | 37 | "givenName": "Kerstin", | ||
38 | "groups": [], | 38 | "groups": [], | ||
39 | "id": "0e28f8c9-bc22-4843-847a-9b1061bdadd9", | 39 | "id": "0e28f8c9-bc22-4843-847a-9b1061bdadd9", | ||
40 | "isopen": false, | 40 | "isopen": false, | ||
41 | "license_id": "CC-BY-4.0", | 41 | "license_id": "CC-BY-4.0", | ||
42 | "license_title": "CC-BY-4.0", | 42 | "license_title": "CC-BY-4.0", | ||
43 | "metadata_created": "2024-11-30T08:47:24.950954", | 43 | "metadata_created": "2024-11-30T08:47:24.950954", | ||
n | 44 | "metadata_modified": "2024-11-30T08:47:24.950959", | n | 44 | "metadata_modified": "2024-11-30T09:21:39.444134", |
45 | "name": "png-doi-10-1594-pangaea-898319", | 45 | "name": "png-doi-10-1594-pangaea-898319", | ||
46 | "notes": "Benthic foraminiferal assemblages from a core southwest of | 46 | "notes": "Benthic foraminiferal assemblages from a core southwest of | ||
47 | Disko Bugt provide a Holocene perspective (last ~7 ka BP) on | 47 | Disko Bugt provide a Holocene perspective (last ~7 ka BP) on | ||
48 | ice-sheet/ocean interactions between the West Greenland Current (WGC) | 48 | ice-sheet/ocean interactions between the West Greenland Current (WGC) | ||
49 | and the West Greenland ice sheet. Changes in the fauna reveal | 49 | and the West Greenland ice sheet. Changes in the fauna reveal | ||
50 | significant variations in the water mass properties (temperature and | 50 | significant variations in the water mass properties (temperature and | ||
51 | salinity) of the WGC through time. From 7.3 to 6.2 ka BP, a relatively | 51 | salinity) of the WGC through time. From 7.3 to 6.2 ka BP, a relatively | ||
52 | warm/strong WGC influences ice-sheet melt in Disko Bugt and causes | 52 | warm/strong WGC influences ice-sheet melt in Disko Bugt and causes | ||
53 | enhanced meltwater production, resulting in low surface-water | 53 | enhanced meltwater production, resulting in low surface-water | ||
54 | productivity. The most favourable oceanographic conditions occur from | 54 | productivity. The most favourable oceanographic conditions occur from | ||
55 | 5.5 to 3.5 ka BP, associated with 'thermal optimum-like' conditions, | 55 | 5.5 to 3.5 ka BP, associated with 'thermal optimum-like' conditions, | ||
56 | encompassing minimum ice sheet extent in the Disko Bugt area. These | 56 | encompassing minimum ice sheet extent in the Disko Bugt area. These | ||
57 | conditions are attributed to: (1) reduced meltwater influence as the | 57 | conditions are attributed to: (1) reduced meltwater influence as the | ||
58 | ice sheet is land based and (2) enhanced contribution of warm/saline | 58 | ice sheet is land based and (2) enhanced contribution of warm/saline | ||
59 | water masses from the Irminger Current to the WGC. The transition into | 59 | water masses from the Irminger Current to the WGC. The transition into | ||
60 | the late Holocene (last ~3.5 ka BP) is characterized by a cooling of | 60 | the late Holocene (last ~3.5 ka BP) is characterized by a cooling of | ||
61 | oceanographic conditions, caused by increased advection of | 61 | oceanographic conditions, caused by increased advection of | ||
62 | cold/low-salinity water masses from the East Greenland Current. A | 62 | cold/low-salinity water masses from the East Greenland Current. A | ||
63 | longer-term late-Holocene cooling trend within the WGC is attributed | 63 | longer-term late-Holocene cooling trend within the WGC is attributed | ||
64 | to the onset of Neoglacial cooling within the North Atlantic region. | 64 | to the onset of Neoglacial cooling within the North Atlantic region. | ||
65 | Superimposed on this cooling trend, multicentennial-scale variability | 65 | Superimposed on this cooling trend, multicentennial-scale variability | ||
66 | within the WGC matches reconstructions from a nearby coring site in | 66 | within the WGC matches reconstructions from a nearby coring site in | ||
67 | Disko Bugt as follows: (1) cooling at ~2.5 ka BP, linked to the 2.7 ka | 67 | Disko Bugt as follows: (1) cooling at ~2.5 ka BP, linked to the 2.7 ka | ||
68 | BP 'cooling event'; (2) a warm phase centred at 1.8 ka BP, associated | 68 | BP 'cooling event'; (2) a warm phase centred at 1.8 ka BP, associated | ||
69 | with the 'Roman Warm Period'; (3) slight warming between 1.4 and 0.9 | 69 | with the 'Roman Warm Period'; (3) slight warming between 1.4 and 0.9 | ||
70 | ka BP, linked to the 'Medieval Climate Anomaly'; (4) severe cooling of | 70 | ka BP, linked to the 'Medieval Climate Anomaly'; (4) severe cooling of | ||
71 | the WGC after 0.9 ka BP, culminating at 0.3 ka BP during the 'Little | 71 | the WGC after 0.9 ka BP, culminating at 0.3 ka BP during the 'Little | ||
72 | Ice Age'. We show that multicentennial-scale palaeoceanography | 72 | Ice Age'. We show that multicentennial-scale palaeoceanography | ||
73 | variability along the West Greenland margin is driven by ocean | 73 | variability along the West Greenland margin is driven by ocean | ||
74 | forcing, i.e. variations in the relative contribution of Atlantic | 74 | forcing, i.e. variations in the relative contribution of Atlantic | ||
75 | (Irminger Current) and Polar (East Greenland Current) water masses to | 75 | (Irminger Current) and Polar (East Greenland Current) water masses to | ||
76 | the WGC during the last ~7 ka BP, influencing ice sheet dynamics.", | 76 | the WGC during the last ~7 ka BP, influencing ice sheet dynamics.", | ||
77 | "num_resources": 0, | 77 | "num_resources": 0, | ||
n | 78 | "num_tags": 6, | n | 78 | "num_tags": 7, |
79 | "orcid": "0000-0002-7464-2191", | 79 | "orcid": "0000-0002-7464-2191", | ||
80 | "organization": { | 80 | "organization": { | ||
81 | "approval_status": "approved", | 81 | "approval_status": "approved", | ||
82 | "created": "2024-11-30T08:45:56.114425", | 82 | "created": "2024-11-30T08:45:56.114425", | ||
83 | "description": "PANGAEA (Data Publisher for Earth & Environmental | 83 | "description": "PANGAEA (Data Publisher for Earth & Environmental | ||
84 | Science): The information system PANGAEA is operated as an Open Access | 84 | Science): The information system PANGAEA is operated as an Open Access | ||
85 | library aimed at archiving, publishing and distributing georeferenced | 85 | library aimed at archiving, publishing and distributing georeferenced | ||
86 | data from earth system research. PANGAEA guarantees long-term | 86 | data from earth system research. PANGAEA guarantees long-term | ||
87 | availability (greater than 10 years) of its content. PANGAEA is open | 87 | availability (greater than 10 years) of its content. PANGAEA is open | ||
88 | to any project, institution, or individual scientist to use or to | 88 | to any project, institution, or individual scientist to use or to | ||
89 | archive and publish data. PANGAEA focuses on georeferenced | 89 | archive and publish data. PANGAEA focuses on georeferenced | ||
90 | observational data, experimental data, and models/simulations. | 90 | observational data, experimental data, and models/simulations. | ||
91 | Citability, comprehensive metadata descriptions, interoperability of | 91 | Citability, comprehensive metadata descriptions, interoperability of | ||
92 | data and metadata, a high degree of structural and semantic | 92 | data and metadata, a high degree of structural and semantic | ||
93 | harmonization of the data inventory as well as the commitment of the | 93 | harmonization of the data inventory as well as the commitment of the | ||
94 | hosting institutions ensures FAIRness of archived data.", | 94 | hosting institutions ensures FAIRness of archived data.", | ||
95 | "id": "c4bc8467-02a4-44bb-8114-5fa3b31fd7d4", | 95 | "id": "c4bc8467-02a4-44bb-8114-5fa3b31fd7d4", | ||
96 | "image_url": "pangaea_topiclandsurface.png", | 96 | "image_url": "pangaea_topiclandsurface.png", | ||
97 | "is_organization": true, | 97 | "is_organization": true, | ||
98 | "name": "pangaea_landsurface", | 98 | "name": "pangaea_landsurface", | ||
99 | "state": "active", | 99 | "state": "active", | ||
100 | "title": "PANGAEA (Land Surface)", | 100 | "title": "PANGAEA (Land Surface)", | ||
101 | "type": "organization" | 101 | "type": "organization" | ||
102 | }, | 102 | }, | ||
103 | "owner_org": "c4bc8467-02a4-44bb-8114-5fa3b31fd7d4", | 103 | "owner_org": "c4bc8467-02a4-44bb-8114-5fa3b31fd7d4", | ||
104 | "private": false, | 104 | "private": false, | ||
105 | "publication_year": "2019", | 105 | "publication_year": "2019", | ||
106 | "related_identifiers": [ | 106 | "related_identifiers": [ | ||
107 | { | 107 | { | ||
108 | "authors": "Perner Kerstin,Moros Matthias,Jennings Anne E,Lloyd | 108 | "authors": "Perner Kerstin,Moros Matthias,Jennings Anne E,Lloyd | ||
109 | Jeremy M,Knudsen Karen Luise", | 109 | Jeremy M,Knudsen Karen Luise", | ||
110 | "email_authors": | 110 | "email_authors": | ||
111 | ngs@colorado.edu,j.m.lloyd@durham.ac.uk,karenluise.knudsen@geo.au.dk", | 111 | ngs@colorado.edu,j.m.lloyd@durham.ac.uk,karenluise.knudsen@geo.au.dk", | ||
112 | "identifier": "https://doi.org/10.1177/0959683612460785", | 112 | "identifier": "https://doi.org/10.1177/0959683612460785", | ||
113 | "identifier_type": "DOI", | 113 | "identifier_type": "DOI", | ||
114 | "orcid_authors": "0000-0002-7464-2191,,0000-0003-3176-2916,,", | 114 | "orcid_authors": "0000-0002-7464-2191,,0000-0003-3176-2916,,", | ||
115 | "relation_type": "IsSupplementTo", | 115 | "relation_type": "IsSupplementTo", | ||
116 | "source": "The Holocene", | 116 | "source": "The Holocene", | ||
117 | "title": "Holocene palaeoceanographic evolution off West | 117 | "title": "Holocene palaeoceanographic evolution off West | ||
118 | Greenland", | 118 | Greenland", | ||
119 | "year": "2013" | 119 | "year": "2013" | ||
120 | } | 120 | } | ||
121 | ], | 121 | ], | ||
122 | "relationships_as_object": [], | 122 | "relationships_as_object": [], | ||
123 | "relationships_as_subject": [], | 123 | "relationships_as_subject": [], | ||
124 | "repository_name": "PANGAEA (Data Publisher for Earth & | 124 | "repository_name": "PANGAEA (Data Publisher for Earth & | ||
125 | Environmental Science)", | 125 | Environmental Science)", | ||
126 | "resource_type": "application/zip - filename: Perner-etal_2013", | 126 | "resource_type": "application/zip - filename: Perner-etal_2013", | ||
127 | "resources": [], | 127 | "resources": [], | ||
128 | "source_metadata_created": "2019", | 128 | "source_metadata_created": "2019", | ||
129 | "source_metadata_modified": "", | 129 | "source_metadata_modified": "", | ||
130 | "state": "active", | 130 | "state": "active", | ||
131 | "subject_areas": [ | 131 | "subject_areas": [ | ||
132 | { | 132 | { | ||
133 | "subject_area_additional": "", | 133 | "subject_area_additional": "", | ||
134 | "subject_area_name": "LandSurface" | 134 | "subject_area_name": "LandSurface" | ||
135 | }, | 135 | }, | ||
136 | { | 136 | { | ||
137 | "subject_area_additional": "", | 137 | "subject_area_additional": "", | ||
138 | "subject_area_name": "Lithosphere" | 138 | "subject_area_name": "Lithosphere" | ||
139 | } | 139 | } | ||
140 | ], | 140 | ], | ||
141 | "tags": [ | 141 | "tags": [ | ||
142 | { | 142 | { | ||
143 | "display_name": "Benthic foraminifera", | 143 | "display_name": "Benthic foraminifera", | ||
144 | "id": "71eb9196-bb01-47ad-94b8-6c61104f66b5", | 144 | "id": "71eb9196-bb01-47ad-94b8-6c61104f66b5", | ||
145 | "name": "Benthic foraminifera", | 145 | "name": "Benthic foraminifera", | ||
146 | "state": "active", | 146 | "state": "active", | ||
147 | "vocabulary_id": null | 147 | "vocabulary_id": null | ||
148 | }, | 148 | }, | ||
149 | { | 149 | { | ||
150 | "display_name": "EGC", | 150 | "display_name": "EGC", | ||
151 | "id": "5ea16960-be7a-421f-929d-e68cea2ae585", | 151 | "id": "5ea16960-be7a-421f-929d-e68cea2ae585", | ||
152 | "name": "EGC", | 152 | "name": "EGC", | ||
153 | "state": "active", | 153 | "state": "active", | ||
154 | "vocabulary_id": null | 154 | "vocabulary_id": null | ||
155 | }, | 155 | }, | ||
156 | { | 156 | { | ||
157 | "display_name": "GREENClim", | 157 | "display_name": "GREENClim", | ||
158 | "id": "4ed148e5-89b2-4d30-a984-f5b8a45080f0", | 158 | "id": "4ed148e5-89b2-4d30-a984-f5b8a45080f0", | ||
159 | "name": "GREENClim", | 159 | "name": "GREENClim", | ||
160 | "state": "active", | 160 | "state": "active", | ||
161 | "vocabulary_id": null | 161 | "vocabulary_id": null | ||
162 | }, | 162 | }, | ||
163 | { | 163 | { | ||
164 | "display_name": "Holocene", | 164 | "display_name": "Holocene", | ||
165 | "id": "aa687e2a-d753-48e6-a352-8d6aca6afce3", | 165 | "id": "aa687e2a-d753-48e6-a352-8d6aca6afce3", | ||
166 | "name": "Holocene", | 166 | "name": "Holocene", | ||
167 | "state": "active", | 167 | "state": "active", | ||
168 | "vocabulary_id": null | 168 | "vocabulary_id": null | ||
169 | }, | 169 | }, | ||
170 | { | 170 | { | ||
t | t | 171 | "display_name": "IC", | ||
172 | "id": "fd81975b-53ba-4bf5-8f4c-913a14313b21", | ||||
173 | "name": "IC", | ||||
174 | "state": "active", | ||||
175 | "vocabulary_id": null | ||||
176 | }, | ||||
177 | { | ||||
171 | "display_name": "WGC", | 178 | "display_name": "WGC", | ||
172 | "id": "d96b7f95-fb09-44b5-9b44-a4d53cb9e2f5", | 179 | "id": "d96b7f95-fb09-44b5-9b44-a4d53cb9e2f5", | ||
173 | "name": "WGC", | 180 | "name": "WGC", | ||
174 | "state": "active", | 181 | "state": "active", | ||
175 | "vocabulary_id": null | 182 | "vocabulary_id": null | ||
176 | }, | 183 | }, | ||
177 | { | 184 | { | ||
178 | "display_name": "ocean forcing", | 185 | "display_name": "ocean forcing", | ||
179 | "id": "37c6e4dd-ea45-487e-a564-c2a725ae2544", | 186 | "id": "37c6e4dd-ea45-487e-a564-c2a725ae2544", | ||
180 | "name": "ocean forcing", | 187 | "name": "ocean forcing", | ||
181 | "state": "active", | 188 | "state": "active", | ||
182 | "vocabulary_id": null | 189 | "vocabulary_id": null | ||
183 | } | 190 | } | ||
184 | ], | 191 | ], | ||
185 | "title": "Holocene palaeoceanographic evolution off West Greenland", | 192 | "title": "Holocene palaeoceanographic evolution off West Greenland", | ||
186 | "type": "vdataset", | 193 | "type": "vdataset", | ||
187 | "url": "https://doi.org/10.1594/PANGAEA.898319" | 194 | "url": "https://doi.org/10.1594/PANGAEA.898319" | ||
188 | } | 195 | } |