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Sarnthein, Michael (2003): Age model of sediment core GIK15637-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.134245

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Related to:
Sarnthein, Michael; Winn, Kyaw; Jung, Simon J A; Duplessy, Jean-Claude; Labeyrie, Laurent D; 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, https://doi.org/10.1029/93PA03301
Coverage:
Latitude: 27.005000 * Longitude: -18.986667
Date/Time Start: 1980-03-10T00:00:00 * Date/Time End: 1980-03-10T00:00:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 8.250 m
Event(s):
GIK15637-1 * Latitude: 27.005000 * Longitude: -18.986667 * Date/Time: 1980-03-10T00:00:00 * Elevation: -3849.0 m * Recovery: 8.68 m * Location: Northeast Atlantic * Campaign: M53 * Basis: Meteor (1964) * Method/Device: Piston corer (Kiel type) (KOL)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
Age modelAge modelkaSarnthein, Michael
Age, commentCommSarnthein, Michael
Size:
30 data points

Data

Download dataset as tab-delimited text — use the following character encoding:


Depth sed [m]

Age model [ka]

Comm
0.0007.00extrapolated
0.1059.80deduced from C14 analog age of 9.1 ka; after Bard et al. (1990)
0.23511.60deduced from C14 analog age of 10.4 ka; after GISP2 ice warve chronology
0.50517.10deduced from C14 analog age of 13.6 ka; after Bard et al. (1990)
0.55518.30deduced from C14 analog age of 14.8 ka; after Bard et al. (1990)
0.70529.50deduced from C14 analog age of 26 ka; after Bard et al. (1990)
1.20555.45d18O event 3.31; after Martinson et al. (1987)
2.000122.20d18O event 5.51; after Martinson et al. (1987)
2.335135.10d18O event 6.2; after Martinson et al. (1987)
3.420189.61d18O event 7; after Martinson et al. (1987)
4.400244.18d18O event 8; after Martinson et al. (1987)
5.650303.00d18O event 9; after Imbrie et al. (1984)
6.400339.00d18O event 10; after Imbrie et al. (1984)
7.220362.00d18O event 11; after Imbrie et al. (1984)
8.250423.00d18O event 12; after Imbrie et al. (1984)