Weinelt, Mara; Sarnthein, Michael (2003): Age model of sediment core GIK23259-2. PANGAEA, https://doi.org/10.1594/PANGAEA.97129
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Related to:
Weinelt, Mara (1993): Veränderungen der Oberflächenzirkulation im Europäischen Nordmeer während der letzten 60.000 Jahre - Hinweise aus stabilen Isotopen. Berichte aus dem Sonderforschungsbereich 313, Christian-Albrechts-Universität, Kiel, 41, 106 pp, https://doi.org/10.2312/reports-sfb313.1993.41
Project(s):
Coverage:
Latitude: 72.030000 * Longitude: 9.265000
Date/Time Start: 1988-07-21T00:00:00 * Date/Time End: 1988-07-21T00:00:00
Minimum DEPTH, sediment/rock: 0.20 m * Maximum DEPTH, sediment/rock: 6.00 m
Event(s):
GIK23259-2 * Latitude: 72.030000 * Longitude: 9.265000 * Date/Time: 1988-07-21T00:00:00 * Elevation: -2518.0 m * Penetration: 14.75 m * Recovery: 7.51 m * Location: Arctic Ocean * Campaign: M7/2 * Basis: Meteor (1986) * Method/Device: Piston corer (Kiel type) (KOL)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Age model | Age model | ka | Sarnthein, Michael | see age model comment | |
3 | Comment | Comment | Sarnthein, Michael |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
50 data points
Data
1 Depth sed [m] | 2 Age model [ka] | 3 Comment |
---|---|---|
0.20 | 3.30 | deduced from mesured C14 age of 3.42 ka; after Bard et al. (1990) |
0.30 | 5.92 | deduced from mesured C14 age of 5.56 ka; after Bard et al. (1990) |
0.55 | 9.00 | deduced from mesured C14 age of 8.46 ka; after Bard et al. (1990) |
0.64 | 12.40 | deduced from C14 analog age of 10.4 ka; after Bard et al. (1990) |
0.99 | 13.45 | deduced from mesured C14 age of 11.92 ka; after Bard et al. (1990) |
1.20 | 14.95 | deduced from mesured C14 age of 13.11 ka; after Bard et al. (1990) |
1.25 | 17.10 | deduced from C14 analog age of 13.6 ka; after Bard et al. (1990) |
1.35 | 15.67 | deduced from mesured C14 age of 13.55 ka; after Bard et al. (1990) |
1.40 | 18.30 | deduced from C14 analog age of 14.8 ka; after Bard et al. (1990) |
1.70 | 21.22 | deduced from mesured C14 age of 17.72 ka; after Bard et al. (1990) |
1.90 | 21.89 | deduced from mesured C14 age of 18.39 ka; after Bard et al. (1990) |
2.40 | 28.09 | deduced from mesured C14 age of 24.59 ka; after Bard et al. (1990) |
2.53 | 29.50 | deduced from C14 analog age of 26.0 ka; after Bard et al. (1990) |
2.70 | 33.22 | deduced from mesured C14 age of 29.72 ka; after Bard et al. (1990) |
2.90 | 36.37 | deduced from mesured C14 age of 32.87 ka; after Bard et al. (1990) |
3.00 | 36.69 | deduced from mesured C14 age of 33.19 ka; after Bard et al. (1990) |
3.10 | 43.10 | deduced from mesured C14 age of 39.6 ka; after Bard et al. (1990) |
3.85 | 55.45 | d18O event 3.3; after Martinson et al. (1987) |
4.05 | 65.22 | d18O event 4.22; after Martinson et al. (1987) |
4.30 | 79.46 | d18O event 5.1; after Martinson et al. (1987) |
4.70 | 103.55 | d18O event 5.3; after Martinson et al. (1987) |
4.80 | 110.79 | d18O event 5.4; after Martinson et al. (1987) |
5.20 | 125.00 | d18O event 5.5; after Martinson et al. (1987) |
5.80 | 135.10 | d18O event 6.2; after Martinson et al. (1987) |
6.00 | 141.00 | d18O event 6.3; after Martinson et al. (1987) |