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Data Description |
| Citation: | Vogelsang, Elke; Sarnthein, Michael (2001): Age control of sediment core RC13-229. doi:10.1594/PANGAEA.59733
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| Reference(s): | Vogelsang, Elke; Sarnthein, Michael; Pflaumann, Uwe (2001): d18O Stratigraphy, chronology, and sea surface temperatures of Atlantic sediment records (GLAMAP-2000 Kiel). Berichte-Reports, Geologisch-Paläontologisches Institut und Museum, Christian-Albrechts-Universität, Kiel, 13, 13+244 pp
 Sarnthein, Michael; Winn, Kyaw; Jung, Simon J A; Duplessy, Jean-Claude; Labeyrie, Laurent; Erlenkeuser, Helmut; Ganssen, Gerald M (1994): Changes in east Atlantic deepwater circulation over the last 30,000 years: Eight time slice reconstructions. Paleoceanography, 9(2), 209-267, doi:10.1029/93PA03301
Curry, William B; Duplessy, Jean-Claude; Labeyrie, Laurent; Shackleton, Nicholas J (1988): Changes in the distribution of d13C of deep water SumCO2 between the last glaciation and the Holocene. Paleoceanography, 3(3), 317-341, doi:10.1029/PA003i003p00317
Oppo, Delia W; Fairbanks, Richard G (1987): Variability in the deep and intermediate water circulation of the Atlantic Ocean during the past 25.000 years: Northern Hemisphere modulation of the Southern Ocean. Earth and Planetary Science Letters, 86(1), 1-15, doi:10.1016/0012-821X(87)90183-X
CLIMAP Project Members (1984): The last interglacial ocean. Quaternary Research, 21(2), 123-224, doi:10.1016/0033-5894(84)90098-X
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| Project(s): |
Glacial Atlantic Mapping and Prediction (GLAMAP2000)
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| Coverage: | West: 11.3070 * East: 11.3070 * South: -25.4900 * North: -25.4900
Date/Time Start: 1970-10-10T00:00:00 * Date/Time End: 1970-10-10T00:00:00
Minimum DEPTH, sediment: 0.0 m * Maximum DEPTH, sediment: 0.9 m
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| Event(s): | RC13-229
* Latitude: -25.4900 * Longitude: 11.3070 * Elevation: -4191.0 m * Date/Time: 1970-10-10T00:00:00 * Recovery: 16.37 m * Campaign: RC13 * Basis: Robert Conrad * Device: Piston corer | ||||||||||||||||||||||||||||||||||||||||||
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| Comment: | Stratigraphy is different from Curry et al. (1988); Medium sedimentation rates allow for high resolution across Termination I; Core from deeper waters of the Cape Basin (AABW) produces cold d18O signal?
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| Parameter(s): |
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| Size: | 14 data points
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