Lofi, Johanna; Voelker, Antje H L; Ducassou, Emmanuelle; Hernandéz-Molina, Francisco Javier; Sierro, Francisco Javier; Bahr, André; Galvani, Aurélie; Lourens, Lucas Joost; Pardo-Igúzquiza, Eulogio; Pezard, Philippe A; Rodríguez-Tovar, Francisco Javier; Williams, Trevor J (2017): (Table 2) Main lithologies from different Sites of IODP Exp339 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.870924, In supplement to: Lofi, J et al. (2016): Quaternary chronostratigraphic framework and sedimentary processes for the Gulf of Cadiz and Portuguese Contourite Depositional Systems derived from Natural Gamma Ray records. Marine Geology, 377, 40-57, https://doi.org/10.1016/j.margeo.2015.12.005
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Further details:
Stow, Dorrik A V; Hernandéz-Molina, Francisco Javier; Alvarez Zarikian, Carlos A; Expedition 339 Scientists (2013): Proceedings of the Integrated Ocean Drilling Program. Washington, DC (Integrated Ocean Drilling Program Management International, Inc.), 339, https://doi.org/10.2204/iodp.proc.339.2013
Project(s):
Coverage:
Median Latitude: 36.907354 * Median Longitude: -8.219007 * South-bound Latitude: 36.425000 * West-bound Longitude: -10.126027 * North-bound Latitude: 37.571416 * East-bound Longitude: -7.277000
Date/Time Start: 2011-11-25T00:00:00 * Date/Time End: 2011-11-25T00:00:00
Minimum DEPTH, sediment/rock: 55.0 m * Maximum DEPTH, sediment/rock: 348.5 m
Event(s):
339-U1385 * Latitude: 37.571416 * Longitude: -10.126027 * Date/Time: 2011-11-25T00:00:00 * Elevation: -2587.0 m * Campaign: Exp339 (Mediterranean Outflow) * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE)
339-U1386 * Latitude: 36.828000 * Longitude: -7.755000 * Elevation: -561.0 m * Campaign: Exp339 (Mediterranean Outflow) * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE)
339-U1387 * Latitude: 36.805000 * Longitude: -7.718000 * Elevation: -558.0 m * Campaign: Exp339 (Mediterranean Outflow) * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE)
Comment:
Compilation based on the shipboard descriptions (Stow et al., 2013; doi:10.2204/iodp.proc.339.2013.).
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | Lofi, Johanna | |||
2 | Lithologic unit/sequence | Unit | Lofi, Johanna | |||
3 | DEPTH, sediment/rock | Depth sed | m | Lofi, Johanna | Geocode | |
4 | Depth, top/min | Depth top | m | Lofi, Johanna | ||
5 | Depth, bottom/max | Depth bot | m | Lofi, Johanna | ||
6 | Age, comment | Comm | Lofi, Johanna | |||
7 | Main Lithology | Main lith | Lofi, Johanna |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
35 data points
Data
1 Event | 2 Unit | 3 Depth sed [m] | 4 Depth top [m] | 5 Depth bot [m] | 6 Comm | 7 Main lith |
---|---|---|---|---|---|---|
339-U1385 | Unit I | 76.0 | 0 | 152 | Holocene - Pleistocene | Bioturbated nannofossil muds and nannofossil clays. Hemipelagic succession. |
339-U1386 | Subunit IA | 55.0 | 0 | 110 | Holocene - Pleistocene | Nannofossil mud, calcareous silty mud, and silty sand with biogenic carbonate. Mixed sandy and muddy contourite succession. |
339-U1386 | Subunit IB | 162.5 | 110 | 215 | Pleistocene | Nannofossil mud and calcareous silty mud. Reduced abundance of coarser grained lithologies compared to subunit IA. Muddy/silty contourite succession. |
339-U1386 | Subunit IC | 317.5 | 215 | 420 | Pleistocene | Nannofossil mud, calcareous silty mud, and silty sand with biogenic carbonate. Mixed sandy and muddy contourite succession with increased abundance of coarser lithologies downhole and appearance of silty turbidites in the lowermost 30 m. |
339-U1387 | Unit I | 227.0 | 0 | 454 | Holocene - Pleistocene | Nannofossil mud, silty mud with biogenic carbonate, and silty sand with biogenic carbonate. Mixed sandy/muddy contourite succession with few turbidites. |
339-U1389 | Subunit IA | 155.0 | 0 | 310 | Holocene - Pleistocene | Calcareous mud (63%), silty and sandy mud with biogenic carbonate. Little evidence of a direct turbidity current input. Contourite-dominated depositional system. |
339-U1389 | Subunit IB | 348.5 | 310 | 387 | Pleistocene | Calcareous mud (82%), silty and sandy mud with biogenic carbonate. Coarser grained lithologies in non recovered intervals? Contourite-dominated depositional system. |