Jung, Simon J A (2004): Age model of sediment core GIK17051-3 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.186498
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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: 56.163333 * Longitude: -31.990000
Date/Time Start: 1989-10-13T00:00:00 * Date/Time End: 1989-10-13T00:00:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 8.100 m
Event(s):
GIK17051-3 * Latitude: 56.163333 * Longitude: -31.990000 * Date/Time: 1989-10-13T00:00:00 * Elevation: -2295.0 m * Penetration: 12 m * Recovery: 0.43 m * Location: Biscaya * Campaign: M11/1 * 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 | 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 |
| 0.300 | 3.20 | deduced from measured C14 age of 3.34 ka; after Bard et al. (1990) |
| 0.500 | 5.16 | deduced from measured C14 age of 4.86 ka; after Bard et al. (1990) |
| 0.900 | 7.18 | deduced from measured C14 age of 6.69 ka; after Bard et al. (1990) |
| 1.275 | 9.80 | deduced from C14 analog age of 9.10 ka; after Bard et al. (1990) |
| 1.425 | 12.40 | deduced from C14 analog age of 10.40 ka; after Bard et al. (1990) |
| 1.500 | 10.90 | deduced from measured C14 age of 9.98 ka; after Bard et al. (1990) |
| 1.500 | 12.80 | deduced from measured C14 age of 11.26 ka; after Bard et al. (1990) |
| 1.800 | 14.70 | deduced from measured C14 age of 12.93 ka; after Bard et al. (1990) |
| 1.800 | 14.40 | deduced from measured C14 age of 12.69 ka; after Bard et al. (1990) |
| 1.900 | 17.10 | deduced from C14 analog age of 13.60 ka; after Bard et al. (1990) |
| 2.100 | 21.81 | deduced from measured C14 age of 18.31 ka; after Bard et al. (1990) |
| 2.120 | 18.30 | deduced from C14 analog age of 14.80 ka; after Bard et al. (1990) |
| 2.950 | 29.50 | deduced from C14 analog age of 26.00 ka; after Bard et al. (1990) |
| 4.920 | 55.45 | d18O event 3.3; after Martinson et al. (1987) |
| 5.300 | 62.62 | d18O event 4.22; after Martinson et al. (1987) |
| 6.050 | 79.25 | d18O event 5.1; after Martinson et al. (1987) |
| 8.100 | 125.00 | d18O event 5.52; after Martinson et al. (1987) |