Jung, Simon J A (2004): Age model of sediment core GIK17049-6 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.186493
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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: 55.260000 * Longitude: -26.725000
Date/Time Start: 1989-10-11T00:00:00 * Date/Time End: 1989-10-11T00:00:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 12.600 m
Event(s):
GIK17049-6 * Latitude: 55.260000 * Longitude: -26.725000 * Date/Time: 1989-10-11T00:00:00 * Elevation: -3331.0 m * Penetration: 17 m * Location: Biscaya * Campaign: M11/1 * Basis: Meteor (1986) * Method/Device: Piston corer (Kiel type) (KOL)
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:
40 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] | 3 Comm |
|---|---|---|
| 0.000 | 0.00 | assumption of no sediment loss |
| 0.125 | 1.44 | deduced from measured C14 age of 1.91 ka; after Bard et al. (1990) |
| 0.475 | 5.30 | deduced from measured C14 age of 5.01 ka; after Bard et al. (1990) |
| 0.575 | 6.87 | deduced from measured C14 age of 6.42 ka; after Bard et al. (1990) |
| 0.950 | 6.88 | deduced from measured C14 age of 6.43 ka; after Bard et al. (1990) |
| 1.200 | 11.00 | deduced from measured C14 age of 10.15 ka; after Bard et al. (1990) |
| 1.200 | 13.33 | deduced from measured C14 age of 11.82 ka; after Bard et al. (1990) |
| 1.300 | 13.70 | deduced from measured C14 age of 12.14 ka; after Bard et al. (1990) |
| 1.450 | 18.25 | deduced from measured C14 age of 14.75 ka; after Bard et al. (1990) |
| 2.100 | 31.30 | deduced from measured C14 age of 27.80 ka; after Bard et al. (1990) |
| 2.725 | 32.10 | deduced from measured C14 age of 28.60 ka; after Bard et al. (1990) |
| 3.700 | 71.00 | d18O event 4.2; after Martinson et al. (1987) |
| 4.200 | 91.00 | d18O event 5.2; after Martinson et al. (1987) |
| 4.900 | 111.00 | d18O event 5.4; after Martinson et al. (1987) |
| 5.600 | 122.00 | d18O event 5.52; after Martinson et al. (1987) |
| 6.000 | 135.00 | d18O event 6.2; after Martinson et al. (1987) |
| 6.300 | 141.00 | d18O event 6.3; after Martinson et al. (1987) |
| 8.300 | 193.00 | d18O event 7.0; after Martinson et al. (1987) |
| 10.000 | 241.00 | d18O event 7.5; after Martinson et al. (1987) |
| 12.600 | 331.00 | d18O event 9.3; after Martinson et al. (1987) |