Jung, Simon J A (2004): Age model of sediment core GIK23419-8 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.186497
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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: 54.961667 * Longitude: -19.755000
Date/Time Start: 1991-08-28T00:00:00 * Date/Time End: 1991-08-28T00:00:00
Minimum DEPTH, sediment/rock: 0.050 m * Maximum DEPTH, sediment/rock: 7.200 m
Event(s):
GIK23419-8 * Latitude: 54.961667 * Longitude: -19.755000 * Date/Time: 1991-08-28T00:00:00 * Elevation: -1487.0 m * Penetration: 94.55 m * Recovery: 7.47 m * Location: Norwegian Sea * Campaign: M17/2 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL)
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 | ||
| 3 | Age, comment | Comm | Sarnthein, Michael |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
40 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] | 3 Comm |
|---|---|---|
| 0.050 | 0.00 | extrapolated |
| 0.235 | 9.80 | deduced from C14 analog age of 9.1 ka; after Bard et al. (1990) |
| 0.389 | 17.10 | deduced from C14 analog age of 13.6 ka; after Bard et al. (1990) |
| 0.400 | 18.30 | deduced from C14 analog age of 14.8 ka; after Bard et al. (1990) |
| 0.689 | 29.50 | deduced from C14 analog age of 26.0 ka; after Bard et al. (1990) |
| 1.550 | 55.46 | d18O event 3.3; after Martinson et al. (1987) |
| 1.615 | 60.40 | end of stage 4; after Martinson et al. (1987) |
| 1.665 | 64.23 | d18O event 4.22; after Martinson et al. (1987) |
| 1.900 | 79.25 | d18O event 5.1; after Martinson et al. (1987) |
| 2.500 | 125.00 | d18O event 5.53; after Martinson et al. (1987) |
| 2.700 | 135.34 | d18O event 6.2; after Martinson et al. (1987) |
| 3.700 | 215.54 | d18O event 7.3; after Martinson et al. (1987) |
| 4.200 | 241.19 | d18O event 7.5; after Martinson et al. (1987) |
| 5.200 | 288.54 | d18O event 8.5; after Martinson et al. (1987) |
| 5.600 | 331.00 | d18O event 9.3; after Imbrie et al. (1984) |
| 5.800 | 341.00 | d18O event 10.2; after Imbrie et al. (1984) |
| 6.400 | 368.00 | d18O event 11.1; after Imbrie et al. (1984) |
| 6.500 | 375.00 | d18O event 11.2; after Imbrie et al. (1984) |
| 6.800 | 405.00 | d18O event 11.3; after Imbrie et al. (1984) |
| 7.200 | 434.00 | d18O event 12.2; after Imbrie et al. (1984) |