Sarnthein, Michael (2004): Age model of sediment core GeoB1113-4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.134327
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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: -5.745000 * Longitude: -11.036660
Date/Time Start: 1989-03-02T00:00:00 * Date/Time End: 1989-03-02T00:00:00
Minimum DEPTH, sediment/rock: 0.330 m * Maximum DEPTH, sediment/rock: 10.430 m
Event(s):
GeoB1113-4 * Latitude: -5.745000 * Longitude: -11.036660 * Date/Time: 1989-03-02T00:00:00 * Elevation: -2374.0 m * Recovery: 10.7 m * Location: Equatorial Atlantic * Campaign: M9/4 * Basis: Meteor (1986) * Method/Device: Gravity corer (Kiel type) (SL) * Comment: offset to GeoB1113-5 = 12 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 | ||
| 3 | Age, comment | Comm | Sarnthein, Michael | |||
| 4 | Depth, composite | Depth comp | mcd | Sarnthein, Michael | Intercore correlation | Reference: GeoB1113-7 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
96 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] | 3 Comm | 4 Depth comp [mcd] |
|---|---|---|---|
| 0.330 | 16.40 | deduced from C14 analog age of 13.6 ka; after Bard et al. (1990) | 0.45 |
| 0.380 | 18.00 | deduced from C14 analog age of 15.0 ka; after Bard et al. (1990) | 0.50 |
| 0.730 | 29.50 | deduced from C14 analog age of 25.5 ka; after Bard et al. (1990) | 0.85 |
| 1.380 | 50.21 | d18O;event 3.3; after Martinson et al. (1987) | 1.50 |
| 1.580 | 55.45 | d18O;event 3.31; after Martinson et al. (1987) | 1.70 |
| 1.680 | 61.00 | d18O;event 4.0; after Martinson et al. (1987) | 1.80 |
| 1.880 | 69.19 | d18O;event 4.3; after Martinson et al. (1987) | 2.00 |
| 2.080 | 79.25 | d18O;event 5.1; after Martinson et al. (1987) | 2.20 |
| 2.230 | 90.50 | d18O;event 5.2; after Martinson et al. (1987) | 2.35 |
| 2.480 | 96.21 | d18O;event 5.31; after Martinson et al. (1987) | 2.60 |
| 2.680 | 107.55 | d18O;event 5.4; after Martinson et al. (1987) | 2.80 |
| 3.080 | 122.19 | d18O;event 5.51; after Martinson et al. (1987) | 3.20 |
| 3.280 | 131.70 | d18O;event 5.53; after Martinson et al. (1987) | 3.40 |
| 3.330 | 134.23 | d18O;event 6.22; after Martinson et al. (1987) | 3.45 |
| 3.630 | 141.33 | d18O;event 6.3; after Martinson et al. (1987) | 3.75 |
| 3.830 | 149.34 | d18O;event 6.4; after Martinson et al. (1987) | 3.95 |
| 4.280 | 171.37 | d18O;event 6.42; after Martinson et al. (1987) | 4.40 |
| 4.780 | 185.19 | d18O;event 6.6; after Martinson et al. (1987) | 4.90 |
| 5.030 | 193.18 | d18O event 7.1; after Martinson et al. (1987) | 5.15 |
| 5.680 | 215.54 | d18O event 7.3; after Martinson et al. (1987) | 5.80 |
| 6.030 | 225.16 | d18O;event 7.4; after Martinson et al. (1987) | 6.15 |
| 6.405 | 241.19 | d18O;event 7.5; after Martinson et al. (1987) | 6.52 |
| 6.730 | 247.60 | d18Oevent 8.2; after Martinson et al. (1987) | 6.85 |
| 6.830 | 253.43 | d18Oevent 8.21; after Martinson et al. (1987) | 6.95 |
| 7.355 | 267.48 | d18Oevent 8.4; after Martinson et al. (1987) | 7.48 |
| 7.730 | 288.17 | d18Oevent 8.5; after Martinson et al. (1987) | 7.85 |
| 8.030 | 299.00 | d18Oevent 8.6; after Martinson et al. (1987) | 8.15 |
| 8.380 | 310.00 | d18Oevent 9.1; after Martinson et al. (1987) | 8.50 |
| 8.780 | 331.00 | d18Oevent 9.3; after Martinson et al. (1987) | 8.90 |
| 9.080 | 342.00 | d18Oevent 10.2; after Martinson et al. (1987) | 9.20 |
| 9.930 | 368.00 | d18Oevent 11.1; after Martinson et al. (1987) | 10.05 |
| 10.430 | 405.00 | d18Oevent 11.3; after Martinson et al. (1987) | 10.55 |