Weinelt, Mara; Sarnthein, Michael (2003): Age model of sediment core GIK17719-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.97119
Always quote citation above when using data! You can download the citation in several formats below.
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: 72.150000 * Longitude: 12.586667
Date/Time Start: 1990-08-03T00:00:00 * Date/Time End: 1990-08-03T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 5.90 m
Event(s):
GIK17719-1 * Latitude: 72.150000 * Longitude: 12.586667 * Date/Time: 1990-08-03T00:00:00 * Elevation: -1823.0 m * Penetration: 9.86 m * Recovery: 8.78 m * Location: Norwegian Sea * Campaign: M13/2 * 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:
16 data points
Data
1 Depth sed [m] | 2 Age model [ka] | 3 Comment |
---|---|---|
0.00 | 7.9 | extrapolated |
0.30 | 9.8 | deduced from C14 analog age of 9.0 ka; after Bard et al. (1990) |
0.70 | 12.3 | deduced from C14 analog age of 10.3 ka; after Bard et al. (1990) |
1.50 | 14.4 | deduced from C14 analog age of 12.4 ka; after Bard et al. (1990) |
2.00 | 14.7 | deduced from C14 analog age of 12.7 ka; after Bard et al. (1990) |
2.20 | 17.1 | deduced from C14 analog age of 13.6 ka; after Bard et al. (1990) |
2.90 | 18.3 | deduced from C14 analog age of 14.9 ka; after Bard et al. (1990) |
5.90 | 29.5 | deduced from C14 analog age of 26.0 ka; after Bard et al. (1990) |