Changes
On November 30, 2024 at 3:50:29 PM UTC, admin:
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Moved Sediment elemental chemistry, magnetic susceptibility, isothermal remanent magnetization, and age model from NGHP-01 Sites 10 and 16 (offshore Krishna-Godavari Basin, Bay of Bengal) from organization PANGAEA (Geophysics) to organization PANGAEA (Lithosphere)
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Removed the following tags from Sediment elemental chemistry, magnetic susceptibility, isothermal remanent magnetization, and age model from NGHP-01 Sites 10 and 16 (offshore Krishna-Godavari Basin, Bay of Bengal)
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Added the following tags to Sediment elemental chemistry, magnetic susceptibility, isothermal remanent magnetization, and age model from NGHP-01 Sites 10 and 16 (offshore Krishna-Godavari Basin, Bay of Bengal)
f | 1 | { | f | 1 | { |
2 | "author": "Phillips, Stephen C", | 2 | "author": "Phillips, Stephen C", | ||
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.933230", | 6 | "doi": "10.1594/PANGAEA.933230", | ||
7 | "doi_date_published": "2021", | 7 | "doi_date_published": "2021", | ||
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": "Johnson, Joel", | 12 | "extra_author": "Johnson, Joel", | ||
13 | "familyName": "Johnson", | 13 | "familyName": "Johnson", | ||
14 | "givenName": "Joel", | 14 | "givenName": "Joel", | ||
15 | "orcid": "" | 15 | "orcid": "" | ||
16 | } | 16 | } | ||
17 | ], | 17 | ], | ||
18 | "familyName": "Phillips", | 18 | "familyName": "Phillips", | ||
19 | "givenName": "Stephen C", | 19 | "givenName": "Stephen C", | ||
20 | "groups": [], | 20 | "groups": [], | ||
21 | "id": "86eb52c1-652b-41a9-8128-81a58d71d954", | 21 | "id": "86eb52c1-652b-41a9-8128-81a58d71d954", | ||
22 | "isopen": false, | 22 | "isopen": false, | ||
23 | "license_id": "CC-BY-4.0", | 23 | "license_id": "CC-BY-4.0", | ||
24 | "license_title": "CC-BY-4.0", | 24 | "license_title": "CC-BY-4.0", | ||
25 | "metadata_created": "2024-11-29T10:31:03.121781", | 25 | "metadata_created": "2024-11-29T10:31:03.121781", | ||
n | 26 | "metadata_modified": "2024-11-29T10:31:03.121787", | n | 26 | "metadata_modified": "2024-11-30T15:50:29.400514", |
27 | "name": "png-doi-10-1594-pangaea-933230", | 27 | "name": "png-doi-10-1594-pangaea-933230", | ||
28 | "notes": "We present datasets associated with an approach to | 28 | "notes": "We present datasets associated with an approach to | ||
29 | disentangle detrital and diagenetic influences on magnetic | 29 | disentangle detrital and diagenetic influences on magnetic | ||
30 | susceptibility in marine sediments in the Bay of Bengal. The goal of | 30 | susceptibility in marine sediments in the Bay of Bengal. The goal of | ||
31 | the approach is to identify zones in which titanomagnetite has been | 31 | the approach is to identify zones in which titanomagnetite has been | ||
32 | subject to dissolution and resulting in pyrite precipitation at paleo | 32 | subject to dissolution and resulting in pyrite precipitation at paleo | ||
33 | depths of the sulfate-methane transition zone (SMTZ) or paleo-seep | 33 | depths of the sulfate-methane transition zone (SMTZ) or paleo-seep | ||
34 | activity. These data are from two sites with cores recovered during | 34 | activity. These data are from two sites with cores recovered during | ||
35 | the Indian National Gas Hydrate Program Expedition 01 (NGHP-01). We | 35 | the Indian National Gas Hydrate Program Expedition 01 (NGHP-01). We | ||
36 | characterize the upper 27 meters below seafloor (mbsf) at Hole | 36 | characterize the upper 27 meters below seafloor (mbsf) at Hole | ||
37 | NGHP-01-10D (15\u00b0 51.8609'N, 81\u00b0 50.0749' E, 1035 m water | 37 | NGHP-01-10D (15\u00b0 51.8609'N, 81\u00b0 50.0749' E, 1035 m water | ||
38 | depth) and the upper 73 mbsf at Hole NGHP-01-16A (16\u00b0 35.5986' N, | 38 | depth) and the upper 73 mbsf at Hole NGHP-01-16A (16\u00b0 35.5986' N, | ||
39 | 082\u00b0 41.0070' E, 1252 m water depth). These sediments were | 39 | 082\u00b0 41.0070' E, 1252 m water depth). These sediments were | ||
40 | collected using piston coring and extended core barrel coring during | 40 | collected using piston coring and extended core barrel coring during | ||
41 | drilling on the JOIDES Resolution in June and July of 2006. We | 41 | drilling on the JOIDES Resolution in June and July of 2006. We | ||
42 | present high-resolution measurements of magnetic susceptibility | 42 | present high-resolution measurements of magnetic susceptibility | ||
43 | (onboard Geotek multi-sensor core logging) and X-ray fluorescence (Cox | 43 | (onboard Geotek multi-sensor core logging) and X-ray fluorescence (Cox | ||
44 | Analytical core scanner at Woods Hole Oceanographic Institution, WHOI) | 44 | Analytical core scanner at Woods Hole Oceanographic Institution, WHOI) | ||
45 | for the elements Zr, Rb, Fe, Ti, Ca, and K. Discrete measurements of | 45 | for the elements Zr, Rb, Fe, Ti, Ca, and K. Discrete measurements of | ||
46 | total organic carbon (TOC) and total sulfur (TS) were measured on | 46 | total organic carbon (TOC) and total sulfur (TS) were measured on | ||
47 | powdered sediment samples using a Perkin Elmer CHNS/O 2400 Series II | 47 | powdered sediment samples using a Perkin Elmer CHNS/O 2400 Series II | ||
48 | elemental analyzer at the University of New Hampshire (UNH). Grain | 48 | elemental analyzer at the University of New Hampshire (UNH). Grain | ||
49 | size was measured using a Beckman Coulter LS 13320 Laser Diffraction | 49 | size was measured using a Beckman Coulter LS 13320 Laser Diffraction | ||
50 | Particle Size Analyzer at WHOI. We also present acquisition curves of | 50 | Particle Size Analyzer at WHOI. We also present acquisition curves of | ||
51 | isothermal remanent magnetization (IRM) from 0 to 1.1T and thermal | 51 | isothermal remanent magnetization (IRM) from 0 to 1.1T and thermal | ||
52 | demagnetization (20 to 580 degrees C) measured across three axes using | 52 | demagnetization (20 to 580 degrees C) measured across three axes using | ||
53 | an HSM2 SQUID spinner magnetometer at UNH. Authigenic carbonate | 53 | an HSM2 SQUID spinner magnetometer at UNH. Authigenic carbonate | ||
54 | nodules at Site 16 were pulverized and measured by X-ray diffraction | 54 | nodules at Site 16 were pulverized and measured by X-ray diffraction | ||
55 | at UNH to determine mineralogy. These carbonate powders at Site 16 | 55 | at UNH to determine mineralogy. These carbonate powders at Site 16 | ||
56 | were analyzed for oxygen and carbon isotopic signature using a | 56 | were analyzed for oxygen and carbon isotopic signature using a | ||
57 | Finnegan MAT 253 mass spectrometer with a Kiel IV carbonate | 57 | Finnegan MAT 253 mass spectrometer with a Kiel IV carbonate | ||
58 | preparation device (phosphoric acid at 77 \u00b0C) at the University | 58 | preparation device (phosphoric acid at 77 \u00b0C) at the University | ||
59 | of Michigan. Carbonate powders from Site 10 were analyzed by Finnegan | 59 | of Michigan. Carbonate powders from Site 10 were analyzed by Finnegan | ||
60 | MAT 252 mass spectrometer with a Kiel III carbonate preparation device | 60 | MAT 252 mass spectrometer with a Kiel III carbonate preparation device | ||
61 | (phosphoric acid at 70 \u00b0C) at Oregon State University (OSU) for | 61 | (phosphoric acid at 70 \u00b0C) at Oregon State University (OSU) for | ||
62 | oxygen and carbon isotopic signature. We picked mixed planktonic | 62 | oxygen and carbon isotopic signature. We picked mixed planktonic | ||
63 | foraminifers (primarily Globigerinoides ruber and Globigerinoides | 63 | foraminifers (primarily Globigerinoides ruber and Globigerinoides | ||
64 | sacculifer) from Site 16 sent them for radiocarbon analysis at | 64 | sacculifer) from Site 16 sent them for radiocarbon analysis at | ||
65 | National Ocean Sciences Accelerator Mass Spectrometry (NOSAMS) | 65 | National Ocean Sciences Accelerator Mass Spectrometry (NOSAMS) | ||
66 | facility at WHOI. The radiocarbon ages were then calibrated using | 66 | facility at WHOI. The radiocarbon ages were then calibrated using | ||
67 | Calib 8.2 and the Marine20 calibration curve. We also picked benthic | 67 | Calib 8.2 and the Marine20 calibration curve. We also picked benthic | ||
68 | foraminifers from Site 16 (Hoeglundina elegans and Uvigerina | 68 | foraminifers from Site 16 (Hoeglundina elegans and Uvigerina | ||
69 | peregrina) for analysis of oxygen and carbon isotopes at the | 69 | peregrina) for analysis of oxygen and carbon isotopes at the | ||
70 | University of Michigan.", | 70 | University of Michigan.", | ||
71 | "num_resources": 0, | 71 | "num_resources": 0, | ||
72 | "num_tags": 11, | 72 | "num_tags": 11, | ||
73 | "orcid": "0000-0003-0858-4701", | 73 | "orcid": "0000-0003-0858-4701", | ||
74 | "organization": { | 74 | "organization": { | ||
75 | "approval_status": "approved", | 75 | "approval_status": "approved", | ||
n | 76 | "created": "2024-11-29T10:29:57.814346", | n | 76 | "created": "2024-11-30T15:47:13.444138", |
77 | "description": "PANGAEA (Data Publisher for Earth & Environmental | 77 | "description": "PANGAEA (Data Publisher for Earth & Environmental | ||
78 | Science): The information system PANGAEA is operated as an Open Access | 78 | Science): The information system PANGAEA is operated as an Open Access | ||
79 | library aimed at archiving, publishing and distributing georeferenced | 79 | library aimed at archiving, publishing and distributing georeferenced | ||
80 | data from earth system research. PANGAEA guarantees long-term | 80 | data from earth system research. PANGAEA guarantees long-term | ||
81 | availability (greater than 10 years) of its content. PANGAEA is open | 81 | availability (greater than 10 years) of its content. PANGAEA is open | ||
82 | to any project, institution, or individual scientist to use or to | 82 | to any project, institution, or individual scientist to use or to | ||
83 | archive and publish data. PANGAEA focuses on georeferenced | 83 | archive and publish data. PANGAEA focuses on georeferenced | ||
84 | observational data, experimental data, and models/simulations. | 84 | observational data, experimental data, and models/simulations. | ||
85 | Citability, comprehensive metadata descriptions, interoperability of | 85 | Citability, comprehensive metadata descriptions, interoperability of | ||
86 | data and metadata, a high degree of structural and semantic | 86 | data and metadata, a high degree of structural and semantic | ||
87 | harmonization of the data inventory as well as the commitment of the | 87 | harmonization of the data inventory as well as the commitment of the | ||
88 | hosting institutions ensures FAIRness of archived data.", | 88 | hosting institutions ensures FAIRness of archived data.", | ||
n | 89 | "id": "76c25ab7-8ae1-4fcb-8c3a-3d90943a65be", | n | 89 | "id": "6012878a-1da5-4a37-b3af-fb4949ca1642", |
90 | "image_url": "pangaea_topicgeophysics.png", | 90 | "image_url": "pangaea_topiclithosphere.png", | ||
91 | "is_organization": true, | 91 | "is_organization": true, | ||
n | 92 | "name": "pangaea_geophysics", | n | 92 | "name": "pangaea_lithosphere", |
93 | "state": "active", | 93 | "state": "active", | ||
n | 94 | "title": "PANGAEA (Geophysics)", | n | 94 | "title": "PANGAEA (Lithosphere)", |
95 | "type": "organization" | 95 | "type": "organization" | ||
96 | }, | 96 | }, | ||
n | 97 | "owner_org": "76c25ab7-8ae1-4fcb-8c3a-3d90943a65be", | n | 97 | "owner_org": "6012878a-1da5-4a37-b3af-fb4949ca1642", |
98 | "private": false, | 98 | "private": false, | ||
99 | "publication_year": "2021", | 99 | "publication_year": "2021", | ||
100 | "related_identifiers": [ | 100 | "related_identifiers": [ | ||
101 | { | 101 | { | ||
102 | "authors": "Johnson Joel E,Phillips Stephen C,Clyde William | 102 | "authors": "Johnson Joel E,Phillips Stephen C,Clyde William | ||
103 | C,Giosan Liviu,Torres Marta E", | 103 | C,Giosan Liviu,Torres Marta E", | ||
104 | "email_authors": | 104 | "email_authors": | ||
105 | s.stephen.c@gmail.com,,lgiosan@whoi.edu,Marta.Torres@oregonstate.edu", | 105 | s.stephen.c@gmail.com,,lgiosan@whoi.edu,Marta.Torres@oregonstate.edu", | ||
106 | "identifier": "https://doi.org/10.1029/2021GC009867", | 106 | "identifier": "https://doi.org/10.1029/2021GC009867", | ||
107 | "identifier_type": "DOI", | 107 | "identifier_type": "DOI", | ||
108 | "orcid_authors": | 108 | "orcid_authors": | ||
109 | 858-4701,0000-0001-8814-3409,0000-0001-6769-5204,0000-0001-7284-733X", | 109 | 858-4701,0000-0001-8814-3409,0000-0001-6769-5204,0000-0001-7284-733X", | ||
110 | "relation_type": "References", | 110 | "relation_type": "References", | ||
111 | "source": "Geochemistry, Geophysics, Geosystems", | 111 | "source": "Geochemistry, Geophysics, Geosystems", | ||
112 | "title": "Isolating Detrital and Diagenetic Signals in Magnetic | 112 | "title": "Isolating Detrital and Diagenetic Signals in Magnetic | ||
113 | Susceptibility Records From Methane\u2010Bearing Marine Sediments", | 113 | Susceptibility Records From Methane\u2010Bearing Marine Sediments", | ||
114 | "year": "2021" | 114 | "year": "2021" | ||
115 | } | 115 | } | ||
116 | ], | 116 | ], | ||
117 | "relationships_as_object": [], | 117 | "relationships_as_object": [], | ||
118 | "relationships_as_subject": [], | 118 | "relationships_as_subject": [], | ||
119 | "repository_name": "PANGAEA (Data Publisher for Earth & | 119 | "repository_name": "PANGAEA (Data Publisher for Earth & | ||
120 | Environmental Science)", | 120 | Environmental Science)", | ||
121 | "resource_type": "application/zip - filename: Phillips-etal_2021", | 121 | "resource_type": "application/zip - filename: Phillips-etal_2021", | ||
122 | "resources": [], | 122 | "resources": [], | ||
123 | "source_metadata_created": "2021", | 123 | "source_metadata_created": "2021", | ||
124 | "source_metadata_modified": "", | 124 | "source_metadata_modified": "", | ||
125 | "state": "active", | 125 | "state": "active", | ||
126 | "subject_areas": [ | 126 | "subject_areas": [ | ||
127 | { | 127 | { | ||
128 | "subject_area_additional": "", | 128 | "subject_area_additional": "", | ||
129 | "subject_area_name": "Chemistry" | 129 | "subject_area_name": "Chemistry" | ||
130 | }, | 130 | }, | ||
131 | { | 131 | { | ||
132 | "subject_area_additional": "", | 132 | "subject_area_additional": "", | ||
133 | "subject_area_name": "Geophysics" | 133 | "subject_area_name": "Geophysics" | ||
134 | }, | 134 | }, | ||
135 | { | 135 | { | ||
136 | "subject_area_additional": "", | 136 | "subject_area_additional": "", | ||
137 | "subject_area_name": "Lithosphere" | 137 | "subject_area_name": "Lithosphere" | ||
138 | } | 138 | } | ||
139 | ], | 139 | ], | ||
140 | "tags": [ | 140 | "tags": [ | ||
141 | { | 141 | { | ||
142 | "display_name": "Age model", | 142 | "display_name": "Age model", | ||
143 | "id": "f6e67202-673e-4b0b-89d2-a10386e4cba5", | 143 | "id": "f6e67202-673e-4b0b-89d2-a10386e4cba5", | ||
144 | "name": "Age model", | 144 | "name": "Age model", | ||
145 | "state": "active", | 145 | "state": "active", | ||
146 | "vocabulary_id": null | 146 | "vocabulary_id": null | ||
147 | }, | 147 | }, | ||
148 | { | 148 | { | ||
149 | "display_name": "Authigenic Carbonate", | 149 | "display_name": "Authigenic Carbonate", | ||
150 | "id": "c5f6dbdc-790d-4276-82fe-b4151477bbde", | 150 | "id": "c5f6dbdc-790d-4276-82fe-b4151477bbde", | ||
151 | "name": "Authigenic Carbonate", | 151 | "name": "Authigenic Carbonate", | ||
152 | "state": "active", | 152 | "state": "active", | ||
153 | "vocabulary_id": null | 153 | "vocabulary_id": null | ||
154 | }, | 154 | }, | ||
155 | { | 155 | { | ||
156 | "display_name": "CHNS", | 156 | "display_name": "CHNS", | ||
157 | "id": "2e76018c-4cb6-434c-98bb-e9e21c3293ff", | 157 | "id": "2e76018c-4cb6-434c-98bb-e9e21c3293ff", | ||
158 | "name": "CHNS", | 158 | "name": "CHNS", | ||
159 | "state": "active", | 159 | "state": "active", | ||
160 | "vocabulary_id": null | 160 | "vocabulary_id": null | ||
161 | }, | 161 | }, | ||
162 | { | 162 | { | ||
163 | "display_name": "Magnetic susceptibility", | 163 | "display_name": "Magnetic susceptibility", | ||
164 | "id": "53762724-6293-4c08-bdca-7b5801e9c5dd", | 164 | "id": "53762724-6293-4c08-bdca-7b5801e9c5dd", | ||
165 | "name": "Magnetic susceptibility", | 165 | "name": "Magnetic susceptibility", | ||
166 | "state": "active", | 166 | "state": "active", | ||
167 | "vocabulary_id": null | 167 | "vocabulary_id": null | ||
168 | }, | 168 | }, | ||
169 | { | 169 | { | ||
n | 170 | "display_name": "X-ray diffraction", | n | ||
171 | "id": "8389efe3-1049-423e-b405-fcd2186777af", | ||||
172 | "name": "X-ray diffraction", | ||||
173 | "state": "active", | ||||
174 | "vocabulary_id": null | ||||
175 | }, | ||||
176 | { | ||||
177 | "display_name": "X-ray fluorescence scanning", | ||||
178 | "id": "ff1bf086-d04d-4e1f-936c-8fa05f443bb8", | ||||
179 | "name": "X-ray fluorescence scanning", | ||||
180 | "state": "active", | ||||
181 | "vocabulary_id": null | ||||
182 | }, | ||||
183 | { | ||||
184 | "display_name": "benthic foraminifera isotopes", | 170 | "display_name": "benthic foraminifera isotopes", | ||
185 | "id": "1634edf2-5fa1-4c76-8d7f-9ae601e355ca", | 171 | "id": "1634edf2-5fa1-4c76-8d7f-9ae601e355ca", | ||
186 | "name": "benthic foraminifera isotopes", | 172 | "name": "benthic foraminifera isotopes", | ||
187 | "state": "active", | 173 | "state": "active", | ||
188 | "vocabulary_id": null | 174 | "vocabulary_id": null | ||
189 | }, | 175 | }, | ||
190 | { | 176 | { | ||
191 | "display_name": "elemental composition", | 177 | "display_name": "elemental composition", | ||
192 | "id": "b07d6585-b76f-44d2-bb4a-f7df5cd76058", | 178 | "id": "b07d6585-b76f-44d2-bb4a-f7df5cd76058", | ||
193 | "name": "elemental composition", | 179 | "name": "elemental composition", | ||
194 | "state": "active", | 180 | "state": "active", | ||
195 | "vocabulary_id": null | 181 | "vocabulary_id": null | ||
196 | }, | 182 | }, | ||
197 | { | 183 | { | ||
198 | "display_name": "isothermal remanent magnetization", | 184 | "display_name": "isothermal remanent magnetization", | ||
199 | "id": "923b9a2e-c5c3-4ecc-9bb9-4ce8ff6d4059", | 185 | "id": "923b9a2e-c5c3-4ecc-9bb9-4ce8ff6d4059", | ||
200 | "name": "isothermal remanent magnetization", | 186 | "name": "isothermal remanent magnetization", | ||
201 | "state": "active", | 187 | "state": "active", | ||
202 | "vocabulary_id": null | 188 | "vocabulary_id": null | ||
203 | }, | 189 | }, | ||
204 | { | 190 | { | ||
205 | "display_name": "magnetic mineralogy", | 191 | "display_name": "magnetic mineralogy", | ||
206 | "id": "e3c09baf-68a9-4346-9b4f-b01a5db7cf6e", | 192 | "id": "e3c09baf-68a9-4346-9b4f-b01a5db7cf6e", | ||
207 | "name": "magnetic mineralogy", | 193 | "name": "magnetic mineralogy", | ||
208 | "state": "active", | 194 | "state": "active", | ||
209 | "vocabulary_id": null | 195 | "vocabulary_id": null | ||
210 | }, | 196 | }, | ||
211 | { | 197 | { | ||
212 | "display_name": "radiocarbon age", | 198 | "display_name": "radiocarbon age", | ||
213 | "id": "de06c3b4-1676-43a3-931a-5f83fc603054", | 199 | "id": "de06c3b4-1676-43a3-931a-5f83fc603054", | ||
214 | "name": "radiocarbon age", | 200 | "name": "radiocarbon age", | ||
t | t | 201 | "state": "active", | ||
202 | "vocabulary_id": null | ||||
203 | }, | ||||
204 | { | ||||
205 | "display_name": "ray diffraction", | ||||
206 | "id": "389b46e2-e8a1-48fe-8bc1-f806664d403b", | ||||
207 | "name": "ray diffraction", | ||||
208 | "state": "active", | ||||
209 | "vocabulary_id": null | ||||
210 | }, | ||||
211 | { | ||||
212 | "display_name": "ray fluorescence scanning", | ||||
213 | "id": "c4dfeba6-3cf9-4189-a423-0ad3da07cc8b", | ||||
214 | "name": "ray fluorescence scanning", | ||||
215 | "state": "active", | 215 | "state": "active", | ||
216 | "vocabulary_id": null | 216 | "vocabulary_id": null | ||
217 | } | 217 | } | ||
218 | ], | 218 | ], | ||
219 | "title": "Sediment elemental chemistry, magnetic susceptibility, | 219 | "title": "Sediment elemental chemistry, magnetic susceptibility, | ||
220 | isothermal remanent magnetization, and age model from NGHP-01 Sites 10 | 220 | isothermal remanent magnetization, and age model from NGHP-01 Sites 10 | ||
221 | and 16 (offshore Krishna-Godavari Basin, Bay of Bengal)", | 221 | and 16 (offshore Krishna-Godavari Basin, Bay of Bengal)", | ||
222 | "type": "vdataset", | 222 | "type": "vdataset", | ||
223 | "url": "https://doi.org/10.1594/PANGAEA.933230" | 223 | "url": "https://doi.org/10.1594/PANGAEA.933230" | ||
224 | } | 224 | } |