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| 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | 5 | "contributor": "NIOZ Royal Netherlands Institute for Sea Research", | ||
| 6 | "creator_user_id": "24237d57-222e-49f2-be7e-bb15bf87c977", | 6 | "creator_user_id": "24237d57-222e-49f2-be7e-bb15bf87c977", | ||
| 7 | "creators": "[{\"firstname\":\"Jaap\",\"lastname\":\"Sinninghe | 7 | "creators": "[{\"firstname\":\"Jaap\",\"lastname\":\"Sinninghe | ||
| 8 | Damste\",\"orcid\":\"0000-0002-8683-1854\",\"affiliation\":\"Royal | 8 | Damste\",\"orcid\":\"0000-0002-8683-1854\",\"affiliation\":\"Royal | ||
| 9 | Netherlands Institute for Sea | 9 | Netherlands Institute for Sea | ||
| 10 | ndingauthor\":true,\"contactemailaddress\":\"jaap.damste@nioz.nl\"}]", | 10 | ndingauthor\":true,\"contactemailaddress\":\"jaap.damste@nioz.nl\"}]", | ||
| 11 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.hd", | 11 | "dataset_persistent_id": "DOI:10.25850/nioz/7b.b.hd", | ||
| 12 | "deposit_date": "2022-09-24", | 12 | "deposit_date": "2022-09-24", | ||
| 13 | "depositor": "Jaap Damste", | 13 | "depositor": "Jaap Damste", | ||
| 14 | "distribution_date": "2022-09-24", | 14 | "distribution_date": "2022-09-24", | ||
| 15 | "distributor": "Research Data Management(NIOZ Royal Netherlands | 15 | "distributor": "Research Data Management(NIOZ Royal Netherlands | ||
| 16 | Institute for Sea Research)", | 16 | Institute for Sea Research)", | ||
| 17 | "doi_date_published": "2022-09-24", | 17 | "doi_date_published": "2022-09-24", | ||
| 18 | "funding_references": | 18 | "funding_references": | ||
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| 23 | (Netherlands Earth System Science Centre)\",\"formatted\":\"Dutch | 23 | (Netherlands Earth System Science Centre)\",\"formatted\":\"Dutch | ||
| 24 | Ministry for Education, Culture and Science - 024.002.001 - NESSC | 24 | Ministry for Education, Culture and Science - 024.002.001 - NESSC | ||
| 25 | (Netherlands Earth System Science Centre)\"},{\"name\":\"European | 25 | (Netherlands Earth System Science Centre)\"},{\"name\":\"European | ||
| 26 | Union\u02b9s 7th Framework Programme (FP/2007\u20132013) | 26 | Union\u02b9s 7th Framework Programme (FP/2007\u20132013) | ||
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| 33 | "license_id": "CC0-1.0", | 33 | "license_id": "CC0-1.0", | ||
| 34 | "license_title": "CC0 1.0", | 34 | "license_title": "CC0 1.0", | ||
| 35 | "license_url": "https://creativecommons.org/publicdomain/zero/1.0/", | 35 | "license_url": "https://creativecommons.org/publicdomain/zero/1.0/", | ||
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| 38 | "metadata_created": "2024-10-22T11:47:32.678753", | 38 | "metadata_created": "2024-10-22T11:47:32.678753", | ||
| n | 39 | "metadata_modified": "2024-10-22T20:51:24.223579", | n | 39 | "metadata_modified": "2026-09-14T12:25:13.356460", |
| 40 | "name": "7bbhd", | 40 | "name": "7bbhd", | ||
| 41 | "notes": "Hydroxylated glycerol dibiphytanyl glycerol tetraethers | 41 | "notes": "Hydroxylated glycerol dibiphytanyl glycerol tetraethers | ||
| 42 | (OH-GDGTs) produced by both marine and freshwater thaumarchaea are | 42 | (OH-GDGTs) produced by both marine and freshwater thaumarchaea are | ||
| 43 | increasingly used for the reconstruction of past sea surface | 43 | increasingly used for the reconstruction of past sea surface | ||
| 44 | temperature (SST). They occur throughout the modern Baltic Sea, but it | 44 | temperature (SST). They occur throughout the modern Baltic Sea, but it | ||
| 45 | is unknown if their OH-GDGTs can be used for assessing past SST in | 45 | is unknown if their OH-GDGTs can be used for assessing past SST in | ||
| 46 | this area, where salinity has changed considerably over the Holocene. | 46 | this area, where salinity has changed considerably over the Holocene. | ||
| 47 | Three commonly applied OH-GDGT proxies for SST reconstruction, i.e., | 47 | Three commonly applied OH-GDGT proxies for SST reconstruction, i.e., | ||
| 48 | the OH-GDGT%, RI-OH, and RI-OH\u00b4 indices, were tested using a | 48 | the OH-GDGT%, RI-OH, and RI-OH\u00b4 indices, were tested using a | ||
| 49 | Thaumarchaeotal culture enriched from the Baltic Sea grown at 4 and | 49 | Thaumarchaeotal culture enriched from the Baltic Sea grown at 4 and | ||
| 50 | 22\u00b0C, and 12 surface sediments from the Baltic Sea and the | 50 | 22\u00b0C, and 12 surface sediments from the Baltic Sea and the | ||
| 51 | adjacent Skagerrak. In the culture experiments all three proxies | 51 | adjacent Skagerrak. In the culture experiments all three proxies | ||
| 52 | showed the expected response with the rise of temperature, but their | 52 | showed the expected response with the rise of temperature, but their | ||
| 53 | absolute values were not always in line with existing marine core top | 53 | absolute values were not always in line with existing marine core top | ||
| 54 | calibrations, especially for the OH-GDGT% index. Of the two proxies | 54 | calibrations, especially for the OH-GDGT% index. Of the two proxies | ||
| 55 | based on the distribution of OH-GDGTs, the RI-OH index shows no | 55 | based on the distribution of OH-GDGTs, the RI-OH index shows no | ||
| 56 | increase with increasing mean annual SST, whilst the RI-OH\u00b4 index | 56 | increase with increasing mean annual SST, whilst the RI-OH\u00b4 index | ||
| 57 | shows only a linear correlation with SST when the sediments from the | 57 | shows only a linear correlation with SST when the sediments from the | ||
| 58 | Bothnian Sea and Bay area, with a reduced salinity and increased | 58 | Bothnian Sea and Bay area, with a reduced salinity and increased | ||
| 59 | lateral sediment influx, are omitted from the dataset. Two sedimentary | 59 | lateral sediment influx, are omitted from the dataset. Two sedimentary | ||
| 60 | Holocene records from the Arkona and Gotland basins were studied, the | 60 | Holocene records from the Arkona and Gotland basins were studied, the | ||
| 61 | latter in high resolution. In the brackish phase of the Baltic Sea | 61 | latter in high resolution. In the brackish phase of the Baltic Sea | ||
| 62 | (the Littorina Sea stage), the RI-OH\u00b4 index shows a good | 62 | (the Littorina Sea stage), the RI-OH\u00b4 index shows a good | ||
| 63 | correlation with the TEX_86^( L), an established temperature proxy in | 63 | correlation with the TEX_86^( L), an established temperature proxy in | ||
| 64 | the Baltic Sea, and can be used to identify important climatic events. | 64 | the Baltic Sea, and can be used to identify important climatic events. | ||
| 65 | However, during the preceding Ancylus Lake phase the RI-OH\u00b4 (and | 65 | However, during the preceding Ancylus Lake phase the RI-OH\u00b4 (and | ||
| 66 | RI-OH) index records far too high values, resulting in anomalously | 66 | RI-OH) index records far too high values, resulting in anomalously | ||
| 67 | high SST estimates. This is probably because freshwater thaumarchaea | 67 | high SST estimates. This is probably because freshwater thaumarchaea | ||
| 68 | adjust their OH-GDGTs differently, as has been shown for thaumarchaea | 68 | adjust their OH-GDGTs differently, as has been shown for thaumarchaea | ||
| 69 | in Lake Lugano\u2019s water column. In the Littorina Sea, the Ancylus | 69 | in Lake Lugano\u2019s water column. In the Littorina Sea, the Ancylus | ||
| 70 | Lake and the Yoldia Lake phases of the Baltic basin, the record of the | 70 | Lake and the Yoldia Lake phases of the Baltic basin, the record of the | ||
| 71 | RI-OH\u00b4 index, thus, most likely reflects both changes in | 71 | RI-OH\u00b4 index, thus, most likely reflects both changes in | ||
| 72 | temperature and salinity. Overall, our study indicates that a reduced | 72 | temperature and salinity. Overall, our study indicates that a reduced | ||
| 73 | salinity increases the values of the RI-OH\u00b4 (and RI-OH) indices | 73 | salinity increases the values of the RI-OH\u00b4 (and RI-OH) indices | ||
| 74 | substantially and this should be considered when applying these | 74 | substantially and this should be considered when applying these | ||
| 75 | proxies in other settings.", | 75 | proxies in other settings.", | ||
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| 209 | "subject": "Earth and Environmental Sciences", | 208 | "subject": "Earth and Environmental Sciences", | ||
| 210 | "tags": [ | 209 | "tags": [ | ||
| 211 | { | 210 | { | ||
| 212 | "display_name": "Baltic Sea", | 211 | "display_name": "Baltic Sea", | ||
| 213 | "id": "6590bb10-f51d-4c1c-a338-8552211eb811", | 212 | "id": "6590bb10-f51d-4c1c-a338-8552211eb811", | ||
| 214 | "name": "Baltic Sea", | 213 | "name": "Baltic Sea", | ||
| 215 | "state": "active", | 214 | "state": "active", | ||
| 216 | "vocabulary_id": null | 215 | "vocabulary_id": null | ||
| 217 | }, | 216 | }, | ||
| 218 | { | 217 | { | ||
| 219 | "display_name": "GDGTs", | 218 | "display_name": "GDGTs", | ||
| 220 | "id": "a2fd030f-578b-4d20-96a3-faa8bf659c75", | 219 | "id": "a2fd030f-578b-4d20-96a3-faa8bf659c75", | ||
| 221 | "name": "GDGTs", | 220 | "name": "GDGTs", | ||
| 222 | "state": "active", | 221 | "state": "active", | ||
| 223 | "vocabulary_id": null | 222 | "vocabulary_id": null | ||
| 224 | }, | 223 | }, | ||
| 225 | { | 224 | { | ||
| 226 | "display_name": "Holocene", | 225 | "display_name": "Holocene", | ||
| 227 | "id": "5483c3f3-deb1-4929-971b-a253b6f90517", | 226 | "id": "5483c3f3-deb1-4929-971b-a253b6f90517", | ||
| 228 | "name": "Holocene", | 227 | "name": "Holocene", | ||
| 229 | "state": "active", | 228 | "state": "active", | ||
| 230 | "vocabulary_id": null | 229 | "vocabulary_id": null | ||
| 231 | }, | 230 | }, | ||
| 232 | { | 231 | { | ||
| 233 | "display_name": "RI-OH", | 232 | "display_name": "RI-OH", | ||
| 234 | "id": "10ecc3bd-2193-4473-a62d-4fadb929ee15", | 233 | "id": "10ecc3bd-2193-4473-a62d-4fadb929ee15", | ||
| 235 | "name": "RI-OH", | 234 | "name": "RI-OH", | ||
| 236 | "state": "active", | 235 | "state": "active", | ||
| 237 | "vocabulary_id": null | 236 | "vocabulary_id": null | ||
| 238 | }, | 237 | }, | ||
| 239 | { | 238 | { | ||
| 240 | "display_name": "TEX86", | 239 | "display_name": "TEX86", | ||
| 241 | "id": "13ab29d0-137b-4dae-9b69-9c101d7715e8", | 240 | "id": "13ab29d0-137b-4dae-9b69-9c101d7715e8", | ||
| 242 | "name": "TEX86", | 241 | "name": "TEX86", | ||
| 243 | "state": "active", | 242 | "state": "active", | ||
| 244 | "vocabulary_id": null | 243 | "vocabulary_id": null | ||
| 245 | }, | 244 | }, | ||
| 246 | { | 245 | { | ||
| 247 | "display_name": "cultures", | 246 | "display_name": "cultures", | ||
| 248 | "id": "598ce3c2-83ec-41f4-a176-c4397f5199a1", | 247 | "id": "598ce3c2-83ec-41f4-a176-c4397f5199a1", | ||
| 249 | "name": "cultures", | 248 | "name": "cultures", | ||
| 250 | "state": "active", | 249 | "state": "active", | ||
| 251 | "vocabulary_id": null | 250 | "vocabulary_id": null | ||
| 252 | }, | 251 | }, | ||
| 253 | { | 252 | { | ||
| 254 | "display_name": "hydroxy GDGTs", | 253 | "display_name": "hydroxy GDGTs", | ||
| 255 | "id": "23743e15-1cd4-48c9-9938-e6e13ae8fd54", | 254 | "id": "23743e15-1cd4-48c9-9938-e6e13ae8fd54", | ||
| 256 | "name": "hydroxy GDGTs", | 255 | "name": "hydroxy GDGTs", | ||
| 257 | "state": "active", | 256 | "state": "active", | ||
| 258 | "vocabulary_id": null | 257 | "vocabulary_id": null | ||
| 259 | }, | 258 | }, | ||
| 260 | { | 259 | { | ||
| 261 | "display_name": "membrane lipids", | 260 | "display_name": "membrane lipids", | ||
| 262 | "id": "fc206870-ed79-4ab4-a628-9aeef7111050", | 261 | "id": "fc206870-ed79-4ab4-a628-9aeef7111050", | ||
| 263 | "name": "membrane lipids", | 262 | "name": "membrane lipids", | ||
| 264 | "state": "active", | 263 | "state": "active", | ||
| 265 | "vocabulary_id": null | 264 | "vocabulary_id": null | ||
| 266 | }, | 265 | }, | ||
| 267 | { | 266 | { | ||
| 268 | "display_name": "proxies", | 267 | "display_name": "proxies", | ||
| 269 | "id": "fb4555e3-5993-44b7-9526-85dc35602f73", | 268 | "id": "fb4555e3-5993-44b7-9526-85dc35602f73", | ||
| 270 | "name": "proxies", | 269 | "name": "proxies", | ||
| 271 | "state": "active", | 270 | "state": "active", | ||
| 272 | "vocabulary_id": null | 271 | "vocabulary_id": null | ||
| 273 | }, | 272 | }, | ||
| 274 | { | 273 | { | ||
| 275 | "display_name": "salinity", | 274 | "display_name": "salinity", | ||
| 276 | "id": "1e285d08-e3be-4bdb-8ea4-8c7301ce7253", | 275 | "id": "1e285d08-e3be-4bdb-8ea4-8c7301ce7253", | ||
| 277 | "name": "salinity", | 276 | "name": "salinity", | ||
| 278 | "state": "active", | 277 | "state": "active", | ||
| 279 | "vocabulary_id": null | 278 | "vocabulary_id": null | ||
| 280 | }, | 279 | }, | ||
| 281 | { | 280 | { | ||
| 282 | "display_name": "sea surface temperature", | 281 | "display_name": "sea surface temperature", | ||
| 283 | "id": "92887644-ee99-48a2-8ef2-c79f09cfab56", | 282 | "id": "92887644-ee99-48a2-8ef2-c79f09cfab56", | ||
| 284 | "name": "sea surface temperature", | 283 | "name": "sea surface temperature", | ||
| 285 | "state": "active", | 284 | "state": "active", | ||
| 286 | "vocabulary_id": null | 285 | "vocabulary_id": null | ||
| 287 | }, | 286 | }, | ||
| 288 | { | 287 | { | ||
| 289 | "display_name": "sediments", | 288 | "display_name": "sediments", | ||
| 290 | "id": "3d6900ff-f286-47b2-95f0-ea74319e7899", | 289 | "id": "3d6900ff-f286-47b2-95f0-ea74319e7899", | ||
| 291 | "name": "sediments", | 290 | "name": "sediments", | ||
| 292 | "state": "active", | 291 | "state": "active", | ||
| 293 | "vocabulary_id": null | 292 | "vocabulary_id": null | ||
| 294 | }, | 293 | }, | ||
| 295 | { | 294 | { | ||
| 296 | "display_name": "temperature proxies", | 295 | "display_name": "temperature proxies", | ||
| 297 | "id": "f0dd9854-9024-4b49-a3cd-c0ff53636cf4", | 296 | "id": "f0dd9854-9024-4b49-a3cd-c0ff53636cf4", | ||
| 298 | "name": "temperature proxies", | 297 | "name": "temperature proxies", | ||
| 299 | "state": "active", | 298 | "state": "active", | ||
| 300 | "vocabulary_id": null | 299 | "vocabulary_id": null | ||
| 301 | }, | 300 | }, | ||
| 302 | { | 301 | { | ||
| 303 | "display_name": "temperature records", | 302 | "display_name": "temperature records", | ||
| 304 | "id": "5d1ba135-d0b1-452d-8e83-608a300bb2ed", | 303 | "id": "5d1ba135-d0b1-452d-8e83-608a300bb2ed", | ||
| 305 | "name": "temperature records", | 304 | "name": "temperature records", | ||
| 306 | "state": "active", | 305 | "state": "active", | ||
| 307 | "vocabulary_id": null | 306 | "vocabulary_id": null | ||
| 308 | }, | 307 | }, | ||
| 309 | { | 308 | { | ||
| 310 | "display_name": "thaumarchaeota", | 309 | "display_name": "thaumarchaeota", | ||
| 311 | "id": "b882e6c2-5980-4f27-85f1-99697f7c8477", | 310 | "id": "b882e6c2-5980-4f27-85f1-99697f7c8477", | ||
| 312 | "name": "thaumarchaeota", | 311 | "name": "thaumarchaeota", | ||
| 313 | "state": "active", | 312 | "state": "active", | ||
| 314 | "vocabulary_id": null | 313 | "vocabulary_id": null | ||
| 315 | } | 314 | } | ||
| 316 | ], | 315 | ], | ||
| 317 | "title": "Evaluation of the distributions of hydroxylated | 316 | "title": "Evaluation of the distributions of hydroxylated | ||
| 318 | isoprenoidal GDGTs in Holocene Baltic Sea sediments for reconstruction | 317 | isoprenoidal GDGTs in Holocene Baltic Sea sediments for reconstruction | ||
| 319 | of sea surface temperature: The effect of changing salinity", | 318 | of sea surface temperature: The effect of changing salinity", | ||
| 320 | "type": "dataset", | 319 | "type": "dataset", | ||
| 321 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.hd", | 320 | "url": "https://dataportal.nioz.nl/doi/10.25850/nioz/7b.b.hd", | ||
| t | 322 | "version": "2" | t | 321 | "version": "11" |
| 323 | } | 322 | } |