Sarnthein, Michael (2006): Age model of sediment core GIK15637-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.358493
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Sarnthein, Michael; Winn, Kyaw; Jung, Simon J A; Duplessy, Jean-Claude; Labeyrie, Laurent D; Erlenkeuser, Helmut; Ganssen, Gerald M (1994): Changes in east Atlantic deepwater circulation over the last 30,000 years: Eight time slice reconstructions. Paleoceanography, 9(2), 209-267, https://doi.org/10.1029/93PA03301
Project(s):
Coverage:
Latitude: 27.005000 * Longitude: -18.986667
Date/Time Start: 1980-03-10T00:00:00 * Date/Time End: 1980-03-10T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 8.25 m
Event(s):
GIK15637-1 * Latitude: 27.005000 * Longitude: -18.986667 * Date/Time: 1980-03-10T00:00:00 * Elevation: -3849.0 m * Recovery: 8.68 m * Location: Northeast Atlantic * Campaign: M53 * Basis: Meteor (1964) * 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:
30 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] | 3 Comm |
|---|---|---|
| 0.00 | 7.00 | extrapolated |
| 0.10 | 9.80 | deduced from C14 analog age of 9.1 ka; after Bard et al. (1990) |
| 0.24 | 11.60 | deduced from C14 analog age of 10.4 ka; after GISP2 ice warve chronology |
| 0.50 | 17.10 | deduced from C14 analog age of 13.6 ka; after Bard et al. (1990) |
| 0.56 | 18.30 | deduced from C14 analog age of 14.8 ka; after Bard et al. (1990) |
| 0.70 | 29.50 | deduced from C14 analog age of 26 ka; after Bard et al. (1990) |
| 1.20 | 55.45 | d18O event 3.31; after Martinson et al. (1987) |
| 2.00 | 122.20 | d18O event 5.51; after Martinson et al. (1987) |
| 2.34 | 135.10 | d18O event 6.2; after Martinson et al. (1987) |
| 3.42 | 189.61 | d18O event 7; after Martinson et al. (1987) |
| 4.40 | 244.18 | d18O event 8; after Martinson et al. (1987) |
| 5.65 | 303.00 | d18O event 9; after Imbrie et al. (1984) |
| 6.40 | 339.00 | d18O event 10; after Imbrie et al. (1984) |
| 7.22 | 362.00 | d18O event 11; after Imbrie et al. (1984) |
| 8.25 | 423.00 | d18O event 12; after Imbrie et al. (1984) |