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O'Reilly, Luke (2022): Radiocarbon dating in sediment core CE18011_VC1 and RH17002_VC7 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.945397, In: O'Reilly, L (2022): Coral content, radiocarbon dating, geochemistry, benthic foraminifera and grain size distribution in sediment cores CE18011_VC1 and RH17002_VC7 [dataset bundled publication]. PANGAEA, https://doi.org/10.1594/PANGAEA.945476

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Published: 2022-06-14DOI registered: 2022-07-29

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Abstract:
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.
Keyword(s):
Benthic foraminifera; cold-water coral mound; grainsize; NE Atlantic; stable isotope analysis
Related to:
Lim, Aaron; O'Reilly, Luke; Harris, Kimberley; Conti, Luis (2020): CE19008 Cruise Report: Monitoring Changes in Submarine Canyon Coral Habitats - Leg 1 (MoCha_SCan). Zenodo, https://doi.org/10.5281/ZENODO.3699111
O'Reilly, Luke; Fentimen, Robin; Butschek, Felix; Titschack, Jürgen; Lim, Aaron; Moore, Niamh; O'Connor, O J; Appah, John; Harris, Kimberley; Vennemann, Torsten W; Wheeler, Andrew J (2022): Environmental forcing by submarine canyons: Evidence between two closely situated cold-water coral mounds (Porcupine Bank Canyon and Western Porcupine Bank, NE Atlantic). Marine Geology, 454, 106930, https://doi.org/10.1016/j.margeo.2022.106930
Further details:
Blaauw, Maarten; Christen, Andrés (2011): Flexible paleoclimate age-depth models using an autoregressive gamma process. Bayesian Analysis, 6(3), 457-474, https://doi.org/10.1214/11-BA618
Langner, Michael; Mulitza, Stefan (2019): Technical note: PaleoDataView – a software toolbox for the collection, homogenization and visualization of marine proxy data. Climate of the Past, 15(6), 2067-2072, https://doi.org/10.5194/cp-15-2067-2019
Funding:
Horizon 2020 (H2020), grant/award no. 818123: Integrated Assessment of Atlantic Marine Ecosystems in Space and Time
Science Foundation Ireland (SFI), grant/award no. SFI 16/IA/4528: MMMonKey_Pro
Coverage:
Median Latitude: 51.986050 * Median Longitude: -15.006200 * South-bound Latitude: 51.982900 * West-bound Longitude: -15.012900 * North-bound Latitude: 51.989200 * East-bound Longitude: -14.999500
Date/Time Start: 2018-08-05T15:28:00 * Date/Time End: 2018-08-05T15:28:00
Minimum DEPTH, sediment/rock: 0.10 m * Maximum DEPTH, sediment/rock: 1.22 m
Event(s):
CE18011_VC1 * Latitude: 51.982900 * Longitude: -14.999500 * Date/Time: 2018-08-05T15:28:00 * Elevation: -660.0 m * Location: Porcupine Bank * Campaign: CE19008 (MoCha_SCan_Leg1) * Basis: Celtic Explorer * Method/Device: Vibro corer (VC) * Comment: Sample taken by remotely operated vehicle mounted (ROV) vibrocorer.
RH17002_VC7 * Latitude: 51.989200 * Longitude: -15.012900 * Date/Time: 2018-08-05T15:28:00 * Elevation: -651.0 m * Location: Porcupine Bank * Campaign: RH17002 (CoCoHaCa) * Basis: Granuaile * Method/Device: Vibro corer (VC) * Comment: Sample was taken by remotely operated vehicle mounted (ROV) vibrocorer rig.
Comment:
AMS 14C dates obtained from benthic and planktic foraminifera and CWC fragments collected from cores RH17002_VC7 and CE18011_VC1. Reservoir (res.) ages and error, calibrated (cal.) age determined from Paleo Data View (Langner and Mulitza, 2019). Age model (AM) age was determined using BACON (Blaauw and Christen, 2011). Aggradation rates (AR) are calculated through linear interpolation of acquired ages.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEventO'Reilly, Luke
2DEPTH, sediment/rockDepth sedmO'Reilly, LukeGeocode
3Laboratory code/labelLab labelO'Reilly, Luke
4Age, dated materialDated materialO'Reilly, Luke
5Age, datedAge datedkaO'Reilly, LukeAccelerator mass spectrometry (AMS), radiocarbon ages
6Age, dated standard errorAge std e±O'Reilly, LukeAccelerator mass spectrometry (AMS), radiocarbon ages
7Reservoir ageRes agekaO'Reilly, LukeAge, 14C milieu/reservoir corrected
8Reservoir age, standard errorRes age e±O'Reilly, LukeAge, 14C milieu/reservoir corrected
9Calendar age, minimum/youngCal age minka BPO'Reilly, LukeAge, calculated calendar yearsμ-2σ
10Calendar age, maximum/oldCal age maxka BPO'Reilly, LukeAge, calculated calendar yearsμ+2σ
11Calendar age, medianCal age medianka BPO'Reilly, LukeAge, calculated calendar years
12Aggradation rateAgg ratecm/kaO'Reilly, LukeAge, 14C AMS, linear interpolation
Status:
Curation Level: Enhanced curation (CurationLevelC) * Processing Level: PANGAEA data processing level 3 (ProcLevel3)
Size:
88 data points

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