Weinelt, Mara; Sarnthein, Michael (2003): Age model of sediment core GIK17730-4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.97122
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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: 72.111667 * Longitude: 7.388333
Date/Time Start: 1990-08-11T00:00:00 * Date/Time End: 1990-08-11T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 4.85 m
Event(s):
GIK17730-4 * Latitude: 72.111667 * Longitude: 7.388333 * Date/Time: 1990-08-11T00:00:00 * Elevation: -2749.0 m * Penetration: 8.15 m * Recovery: 7.31 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:
58 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] | 3 Comment |
|---|---|---|
| 0.00 | 0.00 | assumption of no sediment loss |
| 0.20 | 2.72 | deduced from mesured C14 age of 2.93 ka; after Bard et al. (1990) |
| 0.40 | 5.58 | deduced from mesured C14 age of 5.21 ka; after Bard et al. (1990) |
| 0.50 | 6.86 | deduced from mesured C14 age of 6.40 ka; after Bard et al. (1990) |
| 0.68 | 9.80 | deduced from C14 analog age of 8.9 ka; after Bard et al. (1990) |
| 0.70 | 8.47 | deduced from mesured C14 age of 8.07 ka; after Bard et al. (1990) |
| 0.80 | 12.40 | deduced from C14 analog age of 10.4 ka; after Bard et al. (1990) |
| 1.00 | 9.82 | deduced from mesured C14 age of 9.12 ka; after Bard et al. (1990) |
| 1.12 | 12.72 | deduced from mesured C14 age of 11.19 ka; after Bard et al. (1990) |
| 1.23 | 14.25 | deduced from mesured C14 age of 12.63 ka; after Bard et al. (1990) |
| 1.25 | 17.10 | deduced from C14 analog age of 13.6 ka; after Bard et al. (1990) |
| 1.27 | 17.10 | deduced from C14 analog age of 13.6 ka; after Bard et al. (1990) |
| 1.33 | 18.30 | deduced from C14 analog age of 14.8 ka; after Bard et al. (1990) |
| 1.38 | 18.30 | deduced from C14 analog age of 14.9 ka; after Bard et al. (1990) |
| 1.45 | 21.27 | deduced from mesured C14 age of 17.77 ka; after Bard et al. (1990) |
| 1.60 | 22.77 | deduced from mesured C14 age of 19.27 ka; after Bard et al. (1990) |
| 1.60 | 29.50 | deduced from C14 analog age of 26.0 ka; after Bard et al. (1990) |
| 1.80 | 25.99 | deduced from mesured C14 age of 22.49 ka; after Bard et al. (1990) |
| 1.98 | 29.50 | deduced from C14 analog age of 26.0 ka; after Bard et al. (1990) |
| 2.20 | 33.36 | deduced from mesured C14 age of 29.86 ka; after Bard et al. (1990) |
| 2.40 | 39.90 | deduced from mesured C14 age of 35.40 ka; after Bard et al. (1990) |
| 2.45 | 55.45 | d18O event 3.33; after Martinson et al. (1987) |
| 2.55 | 65.22 | d18O event 4.2; after Martinson et al. (1987) |
| 2.75 | 79.46 | d18O event 5.1; after Martinson et al. (1987) |
| 3.30 | 55.45 | d18O event 3.33; after Martinson et al. (1987) |
| 3.50 | 65.22 | d18O event 4.2; after Martinson et al. (1987) |
| 3.65 | 125.00 | d18O event 5.5; after Martinson et al. (1987) |
| 3.85 | 79.46 | d18O event 5.1; after Martinson et al. (1987) |
| 4.85 | 125.00 | d18O event 5.5; after Martinson et al. (1987) |