Sarnthein, Michael (2006): Age model of sediment core GIK16772-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.358500
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: -1.350000 * Longitude: -11.961667
Date/Time Start: 1988-01-21T00:00:00 * Date/Time End: 1988-01-21T00:00:00
Minimum DEPTH, sediment/rock: 0.11 m * Maximum DEPTH, sediment/rock: 14.80 m
Event(s):
GIK16772-2 * Latitude: -1.350000 * Longitude: -11.961667 * Date/Time: 1988-01-21T00:00:00 * Elevation: -3912.0 m * Recovery: 15.05 m * Location: eastern Romanche Fracture Zone * Campaign: M6/5 * Basis: Meteor (1986) * Method/Device: Piston corer (Kiel type) (KOL) * Comment: offset to GIK16772-1 = 27.5 cm
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:
70 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] | 3 Comm |
|---|---|---|
| 0.11 | 17.10 | deduced from C14 analog age of 13.6 ka; after Bard et al. (1990) |
| 0.20 | 18.30 | deduced from C14 analog age of 14.8 ka; after Bard et al. (1990) |
| 0.50 | 24.20 | deduced from C14 analog age of 20.7 ka; after Bard et al. (1990) |
| 0.77 | 29.50 | deduced from C14 analog age of 26 ka; after Bard et al. (1990) |
| 1.90 | 55.45 | d18O;event 3.31; after Martinson et al. (1987) |
| 2.20 | 64.50 | d18O;event 4.2; after Martinson et al. (1987) |
| 2.80 | 71.10 | d18O;event 4.4; after Martinson et al. (1987) |
| 3.00 | 79.50 | d18O;event 5.1; after Martinson et al. (1987) |
| 3.30 | 90.50 | d18O;event 5.2; after Martinson et al. (1987) |
| 3.70 | 96.20 | d18O;event 5.31; after Martinson et al. (1987) |
| 3.90 | 103.50 | d18O;event 5.33; after Martinson et al. (1987) |
| 4.20 | 110.80 | d18O;event 5.4; after Martinson et al. (1987) |
| 4.90 | 122.50 | d18O;event 5.51; after Martinson et al. (1987) |
| 5.10 | 125.00 | d18O;event 5.53; after Martinson et al. (1987) |
| 5.60 | 135.30 | d18O;event 6.2; after Martinson et al. (1987) |
| 6.00 | 142.00 | d18O;event 6.3; after Martinson et al. (1987) |
| 6.60 | 149.30 | d18O;event 6.42; after Martinson et al. (1987) |
| 6.90 | 157.10 | d18O;event 6.44; after Martinson et al. (1987) |
| 7.00 | 162.80 | d18O;event 6.51; after Martinson et al. (1987) |
| 7.30 | 167.80 | d18O;event 6.53; after Martinson et al. (1987) |
| 7.70 | 172.50 | d18O;event 6.55; after Martinson et al. (1987) |
| 8.30 | 180.00 | d18O;event 6.6; after Martinson et al. (1987) |
| 9.10 | 193.10 | d18O event 7.1; after Martinson et al. (1987) |
| 9.30 | 200.60 | d18O event 7.2; after Martinson et al. (1987) |
| 9.50 | 208.00 | d18O event 7.31; after Martinson et al. (1987) |
| 10.00 | 215.50 | d18O event 7.33; after Martinson et al. (1987) |
| 10.60 | 226.00 | d18O event 7.40; after Martinson et al. (1987) |
| 11.10 | 241.00 | d18O event 7.5; after Martinson et al. (1987) |
| 11.60 | 247.60 | d18Oevent 8.02; after Martinson et al. (1987) |
| 12.00 | 253.40 | d18Oevent 8.2; after Martinson et al. (1987) |
| 12.90 | 267.50 | d18Oevent 8.44; after Martinson et al. (1987) |
| 13.20 | 288.20 | d18Oevent 8.5; after Martinson et al. (1987) |
| 13.70 | 299.00 | d18O event 8.6; after Imbrie et al. (1984) |
| 14.50 | 310.00 | d18O event 9.1; after Imbrie et al. (1984) |
| 14.80 | 328.00 | d18O event 9.2; after Imbrie et al. (1984) |