Radiocarbon dating in sediment core CE18011_VC1 and RH17002_VC7
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| Format: | Dataset Open Access |
| Langue: | en |
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PANGAEA
2022
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| _version_ | 1867168506636664832 |
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| author | O'Reilly, Luke |
| author_facet | O'Reilly, Luke |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | A remotely operated vehicle mounted (ROV) vibrocorer rig acquired the two cores from the Porcupine Bank Canyon (NE Atlantic) and western Porcupine Bank (NE Atlantic) during the RH17002 and CE18011 research cruises. RH17002_VC7 is a 0.81 m ROV-vibrocore and was acquired from a cold-water coral mound summit on lip of the Porcupine Bank Canyon. CE18011_VC1 is a 1.30 m ROV-vibrocore and was acquired from cold-water coral mound summit on the western Porcupine Bank. To construct a geochronological framework, mixed benthic foraminifera (Cibicides lobatulus, Cibicides refulgens and Discanomalina coronata), monospecific planktic foraminifera (Globigerina bulloides) and cold-water coral pieces (Madrepora oculata) were subjected to radiometric analysis. Results were standardized using PaleoDataView (Langner and Mulitza, 2019) to allow applicability and consistency across synthesis. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_945397 |
| institution | PANGAEA |
| language | en |
| publishDate | 2022 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Radiocarbon dating in sediment core CE18011_VC1 and RH17002_VC7 O'Reilly, Luke Accelerator mass spectrometry (AMS), radiocarbon ages; Age, 14C AMS, linear interpolation; Age, 14C milieu/reservoir corrected; Age, calculated calendar years; Age, dated; Age, dated material; Age, dated standard error; Aggradation rate; Benthic foraminifera; Calendar age, maximum/old; Calendar age, median; Calendar age, minimum/young; CE18011_VC1; CE19008; Celtic Explorer; CoCoHaCa; cold-water coral mound; DEPTH, sediment/rock; Event label; grainsize; Granuaile; iAtlantic; Integrated Assessment of Atlantic Marine Ecosystems in Space and Time; Laboratory code/label; MoCha_SCan_Leg1; NE Atlantic; Porcupine Bank; Reservoir age; Reservoir age, standard error; RH17002; RH17002_VC7; stable isotope analysis; VC; Vibro corer A remotely operated vehicle mounted (ROV) vibrocorer rig acquired the two cores from the Porcupine Bank Canyon (NE Atlantic) and western Porcupine Bank (NE Atlantic) during the RH17002 and CE18011 research cruises. RH17002_VC7 is a 0.81 m ROV-vibrocore and was acquired from a cold-water coral mound summit on lip of the Porcupine Bank Canyon. CE18011_VC1 is a 1.30 m ROV-vibrocore and was acquired from cold-water coral mound summit on the western Porcupine Bank. To construct a geochronological framework, mixed benthic foraminifera (Cibicides lobatulus, Cibicides refulgens and Discanomalina coronata), monospecific planktic foraminifera (Globigerina bulloides) and cold-water coral pieces (Madrepora oculata) were subjected to radiometric analysis. Results were standardized using PaleoDataView (Langner and Mulitza, 2019) to allow applicability and consistency across synthesis. |
| title | Radiocarbon dating in sediment core CE18011_VC1 and RH17002_VC7 |
| topic | Accelerator mass spectrometry (AMS), radiocarbon ages; Age, 14C AMS, linear interpolation; Age, 14C milieu/reservoir corrected; Age, calculated calendar years; Age, dated; Age, dated material; Age, dated standard error; Aggradation rate; Benthic foraminifera; Calendar age, maximum/old; Calendar age, median; Calendar age, minimum/young; CE18011_VC1; CE19008; Celtic Explorer; CoCoHaCa; cold-water coral mound; DEPTH, sediment/rock; Event label; grainsize; Granuaile; iAtlantic; Integrated Assessment of Atlantic Marine Ecosystems in Space and Time; Laboratory code/label; MoCha_SCan_Leg1; NE Atlantic; Porcupine Bank; Reservoir age; Reservoir age, standard error; RH17002; RH17002_VC7; stable isotope analysis; VC; Vibro corer |
| url | https://doi.org/10.1594/PANGAEA.945397 |