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Data Publisher for Earth & Environmental Science

Sarnthein, Michael; Duplessy, Jean-Claude (2004): Age model of sediment core NA87-22 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.134590

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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: 55.500000 * Longitude: -14.583333
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 6.40 m
Event(s):
NA87-22 * Latitude: 55.500000 * Longitude: -14.583333 * Elevation: -2161.0 m * Location: North Atlantic * Method/Device: Gravity corer (GC)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
Age modelAge modelkaDuplessy, Jean-Claude
Age, commentCommDuplessy, Jean-Claude
Size:
27 data points

Data

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


Depth sed [m]

Age model [ka]

Comm
0.000.00assumption of no sediment loss
0.953.33deduced from mesured C14 age of 3.12 ka; after Bard et al. (1990)
2.008.63deduced from mesured C14 age of 7.88 ka; after Bard et al. (1990)
2.5010.82deduced from mesured C14 age of 9.61 ka; after Bard et al. (1990)
2.7012.47deduced from mesured C14 age of 10.47 ka; after Bard et al. (1990)
2.8512.92deduced from mesured C14 age of 10.92 ka; after Bard et al. (1990)
3.0513.29deduced from mesured C14 age of 11.29 ka; after Bard et al. (1990)
3.2513.98deduced from mesured C14 age of 11.98 ka; after Bard et al. (1990)
3.5518.76deduced from mesured C14 age of 15.26 ka; after Bard et al. (1990)
3.8019.80deduced from mesured C14 age of 16.30 ka; after Bard et al. (1990)
4.0020.69deduced from mesured C14 age of 17.19 ka; after Bard et al. (1990)
4.4022.41deduced from mesured C14 age of 18.91 ka; after Bard et al. (1990)
5.1029.50deduced from C14 analog age of 26.00 ka; after Bard et al. (1990)
6.4042.67