Weinelt, Mara; Sarnthein, Michael (2003): Age model of sediment core GIK23059-3 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.97118
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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: 70.305000 * Longitude: -3.123333
Date/Time Start: 1986-07-06T00:00:00 * Date/Time End: 1986-07-06T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 1.30 m
Event(s):
GIK23059-3 * Latitude: 70.305000 * Longitude: -3.123333 * Date/Time: 1986-07-06T00:00:00 * Elevation: -2281.0 m * Penetration: 7.05 m * Recovery: 5.7 m * Location: Norwegian Sea * Campaign: M2/2 * Basis: Meteor (1986) * Method/Device: Kasten corer (KAL) * Comment: offset to GIK23059-2 = 10 cm
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Depth, composite | Depth comp | mcd | Sarnthein, Michael | Intercore correlation | Reference: GIK23059-2 |
| 3 | Age model | Age model | ka | Sarnthein, Michael | see age model comment | |
| 4 | Comment | Comment | Sarnthein, Michael |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
21 data points
Data
| 1 Depth sed [m] | 2 Depth comp [mcd] | 3 Age model [ka] | 4 Comment |
|---|---|---|---|
| 0.00 | 0.10 | 0.00 | assumption of no sediment loss |
| 0.04 | 0.14 | 9.80 | deduced from C14 analog age of 9.1 ka; after Stuiver et al. (1991) |
| 0.05 | 0.15 | 12.30 | deduced from C14 analog age of 10.3 ka; after Stuiver et al. (1991) |
| 0.18 | 0.28 | 17.10 | deduced from C14 analog age of 13.6 ka; after Bard et al. (1990) |
| 0.19 | 0.29 | 18.30 | deduced from C14 analog age of 14.8 ka; after Bard et al. (1990) |
| 0.60 | 0.70 | 29.50 | deduced from C14 analog age of 26.0 ka; after Bard et al. (1990) |
| 1.30 | 1.40 | 55.45 | d18O event 3.3; after Martinson et al. (1987) |