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Shackleton, Nicholas J (1977): (Table 4) Stable carbon and oxygen isotope ratios of planktic and benthic foraminifera from sediment core V22-174 in the Atlantic Ocean [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.106778, In supplement to: Shackleton, NJ (1977): Carbon-13 in Uvigerina: Tropical rain forest history and the equatorial Pacific carbonate dissolution cycle. In: Andersen, N R & Malahoff, A (eds.), The Fate of Fossil Fuel in the Oceans. New York (Plenum), 401-427

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Keyword(s):
GLAMAP
Related to:
Vogelsang, Elke; Sarnthein, Michael; Pflaumann, Uwe (2001): d18O Stratigraphy, chronology, and sea surface temperatures of Atlantic sediment records (GLAMAP-2000 Kiel). Berichte-Reports, Institut für Geowissenschaften, Universität Kiel, 13, 13+244 pp., https://doi.org/10.2312/reports-ifg.2001.13
Further details:
Vogelsang, Elke (2001): Age control of sediment cores V22-174. Berichte-Reports, Geologisch-Paläontologisches Institut und Museum, Christian-Albrechts-Universität, Kiel, 13+244 pp, 13, hdl:10013/epic.33133.d001
Coverage:
Latitude: -10.070000 * Longitude: -12.820000
Date/Time Start: 1966-05-13T00:00:00 * Date/Time End: 1966-05-13T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 0.90 m
Event(s):
V22-174 * Latitude: -10.070000 * Longitude: -12.820000 * Date/Time: 1966-05-13T00:00:00 * Elevation: -2630.0 m * Recovery: 15.66 m * Campaign: V22 * Basis: Vema * Method/Device: Piston corer (PC)
Parameter(s):
Size:
94 data points

Data

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Depth sed [m]

G. ruber δ18O [‰ PDB]

G. ruber δ13C [‰ PDB]

G. sacculifer δ18O [‰ PDB]

G. sacculifer δ13C [‰ PDB]

U. auberiana δ18O [‰ PDB]

U. auberiana δ13C [‰ PDB]
0.00-1.231.62-0.922.183.070.48
0.10-1.211.25-0.742.033.230.56
0.20-1.011.30-0.591.903.090.28
0.30-0.731.16-0.141.733.440.03
0.40-0.220.980.221.653.990.09
0.43-0.181.090.411.74
0.470.011.000.531.904.740.11
0.500.120.890.641.694.730.14
0.530.281.090.491.904.740.04
0.570.311.180.812.044.710.24
0.600.290.960.731.894.500.24
0.630.321.000.661.824.580.15
0.670.080.880.661.874.610.06
0.700.080.930.531.824.600.28
0.800.021.100.511.394.520.17
0.900.020.920.311.814.310.26