Weinelt, Mara; Sarnthein, Michael (2003): Age model of sediment core GIK23055-3 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.97123
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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: 68.423333 * Longitude: 4.021660
Date/Time Start: 1986-07-04T00:00:00 * Date/Time End: 1986-07-04T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 6.16 m
Event(s):
GIK23055-3 * Latitude: 68.423333 * Longitude: 4.021660 * Date/Time: 1986-07-04T00:00:00 * Elevation: -2311.0 m * Penetration: 6.77 m * Location: Norwegian Sea * Campaign: M2/2 * Basis: Meteor (1986) * Method/Device: Kasten corer (KAL)
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:
44 data points
Data
1 Depth sed [m] | 2 Age model [ka] | 3 Comment |
---|---|---|
0.00 | 0.70 | extrapolated |
0.14 | 9.80 | deduced from C14 analog age of 9.0 ka; after Bard et al. (1990) |
0.18 | 12.40 | deduced from C14 analog age of 10.4 ka; after Bard et al. (1990) |
0.33 | 17.10 | deduced from C14 analog age of 13.6 ka; after Bard et al. (1990) |
0.35 | 18.30 | deduced from C14 analog age of 14.8 ka; after Bard et al. (1990) |
0.89 | 29.60 | deduced from C14 analog age of 26.1 ka; after Bard et al. (1990) |
1.90 | 55.45 | d18O event 3.33; after Martinson et al. (1987) |
1.97 | 65.22 | d18O event 4.2; after Martinson et al. (1987) |
2.21 | 79.46 | d18O event 5.1; after Martinson et al. (1987) |
2.27 | 90.53 | d18O event 5.2; after Martinson et al. (1987) |
2.50 | 103.55 | d18O event 5.3; after Martinson et al. (1987) |
2.53 | 110.79 | d18O event 5.4; after Martinson et al. (1987) |
2.73 | 122.38 | d18O event 5.51; after Martinson et al. (1987) |
2.85 | 125.00 | d18O event 5.53; after Martinson et al. (1987) |
3.58 | 135.10 | d18O event 6.2; after Martinson et al. (1987) |
3.68 | 141.33 | d18O event 6.3; after Martinson et al. (1987) |
3.76 | 157.10 | d18O event 6.4; after Martinson et al. (1987) |
4.50 | 171.37 | d18O event 6.5; after Martinson et al. (1987) |
4.61 | 179.73 | d18O event 6.62; after Martinson et al. (1987) |
5.90 | 185.19 | d18O event 6.64; after Martinson et al. (1987) |
6.00 | 193.07 | d18O event 7.1; after Martinson et al. (1987) |
6.16 | 215.54 | d18O event 7.2; after Martinson et al. (1987) |