Geochemistry of sediment cores CE18011_VC1 and RH17002_VC7
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| Format: | Dataset Open Access |
| Sprache: | en |
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PANGAEA
2022
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| _version_ | 1867170407886356480 |
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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. Grain size analysis of the siliclastic fraction of the sediment were used to infer changes in hydrodynamic regime (i.e. mean grain size and mean sortable silt size). δ13C and δ18O were determined from planktic foraminifera (Globigerina bulloides) and benthic foraminifera (Cibicidoides pachyderma) to infer watermass variation. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_945475 |
| institution | PANGAEA |
| language | en |
| publishDate | 2022 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Geochemistry of sediment cores CE18011_VC1 and RH17002_VC7 O'Reilly, Luke Benthic foraminifera; CE18011_VC1; CE19008; Celtic Explorer; CoCoHaCa; cold-water coral mound; DEPTH, sediment/rock; Event label; Foraminifera, benthic δ13C; Foraminifera, benthic δ18O; Foraminifera, planktic δ13C; Foraminifera, planktic δ18O; grainsize; Grain size, mean; Granuaile; iAtlantic; Integrated Assessment of Atlantic Marine Ecosystems in Space and Time; MoCha_SCan_Leg1; NE Atlantic; Porcupine Bank; RH17002; RH17002_VC7; Sortable-silt mean size, average; stable isotope analysis; 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. Grain size analysis of the siliclastic fraction of the sediment were used to infer changes in hydrodynamic regime (i.e. mean grain size and mean sortable silt size). δ13C and δ18O were determined from planktic foraminifera (Globigerina bulloides) and benthic foraminifera (Cibicidoides pachyderma) to infer watermass variation. |
| title | Geochemistry of sediment cores CE18011_VC1 and RH17002_VC7 |
| topic | Benthic foraminifera; CE18011_VC1; CE19008; Celtic Explorer; CoCoHaCa; cold-water coral mound; DEPTH, sediment/rock; Event label; Foraminifera, benthic δ13C; Foraminifera, benthic δ18O; Foraminifera, planktic δ13C; Foraminifera, planktic δ18O; grainsize; Grain size, mean; Granuaile; iAtlantic; Integrated Assessment of Atlantic Marine Ecosystems in Space and Time; MoCha_SCan_Leg1; NE Atlantic; Porcupine Bank; RH17002; RH17002_VC7; Sortable-silt mean size, average; stable isotope analysis; Stable isotope analysis; VC; Vibro corer |
| url | https://doi.org/10.1594/PANGAEA.945475 |