Jung, Simon J A (2004): Age model of sediment core GIK23414-9 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.186495
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Related to:
Jung, Simon J A (1996): Wassermassenaustausch zwischen NE-Atlantik und Nordmeer während der letzten 300 000/80 000 Jahre im Abbild stabiler O- und C- Isotope. Berichte aus dem Sonderforschungsbereich 313, Christian-Albrechts-Universität, Kiel, 61, 104 pp, https://doi.org/10.2312/reports-sfb313.1996.61
Project(s):
Coverage:
Latitude: 53.536660 * Longitude: -20.288330
Date/Time Start: 1991-08-22T00:00:00 * Date/Time End: 1991-08-22T00:00:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 8.550 m
Event(s):
GIK23414-9 (M23414) * Latitude: 53.536660 * Longitude: -20.288330 * Date/Time: 1991-08-22T00:00:00 * Elevation: -2196.0 m * Penetration: 10.5 m * Recovery: 9.08 m * Location: Northeast Atlantic * Campaign: M17/2 * 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 | Age, comment | Comm | Sarnthein, Michael |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
36 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] | 3 Comm |
|---|---|---|
| 0.000 | 0.00 | assumption of no sediment loss |
| 0.375 | 9.80 | deduced from C14 analog age of 9.1 ka; after Bard et al. (1990) |
| 0.415 | 12.40 | deduced from C14 analog age of 10.4 ka; after Bard et al. (1990) |
| 0.525 | 17.10 | deduced from C14 analog age of 13.6 ka; after Bard et al. (1990) |
| 0.600 | 18.30 | deduced from C14 analog age of 14.8 ka; after Bard et al. (1990) |
| 0.975 | 29.50 | deduced from C14 analog age of 26.0 ka; after Bard et al. (1990) |
| 2.525 | 55.46 | d18O event 3.3; after Martinson et al. (1987) |
| 2.700 | 60.40 | end of stage 4; after Martinson et al. (1987) |
| 3.650 | 103.80 | d18O event 5.3; after Martinson et al. (1987) |
| 4.025 | 122.19 | d18O event 5.51; after Martinson et al. (1987) |
| 4.250 | 125.00 | d18O event 5.53; after Martinson et al. (1987) |
| 4.600 | 135.34 | d18O event 6.2; after Martinson et al. (1987) |
| 5.200 | 141.33 | d18O event 6.3; after Martinson et al. (1987) |
| 6.100 | 185.19 | d18O event 6.64; after Martinson et al. (1987) |
| 6.450 | 193.18 | d18O event 7.1; after Martinson et al. (1987) |
| 6.900 | 215.54 | d18O event 7.3; after Martinson et al. (1987) |
| 7.700 | 241.19 | d18O event 7.5; after Martinson et al. (1987) |
| 8.550 | 267.48 | d18O event 8.4; after Martinson et al. (1987) |