Oppo, Delia W; Fairbanks, Richard G; Gordon, Arnold L; Shackleton, Nicholas J (1990): (Table 2) Age model of sediment core RC13-229 in the Cape Basin, Atlantic Ocean [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.264558, In supplement to: Oppo, DW et al. (1990): Late Pleistocene Southern Ocean d13C variability. Paleoceanography, 5(1), 43-54, https://doi.org/10.1029/PA005i001p00043
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Coverage:
Latitude: -25.490000 * Longitude: 11.307000
Date/Time Start: 1970-10-10T00:00:00 * Date/Time End: 1970-10-10T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 16.14 m
Event(s):
RC13-229 * Latitude: -25.490000 * Longitude: 11.307000 * Date/Time: 1970-10-10T00:00:00 * Elevation: -4191.0 m * Recovery: 16.37 m * Campaign: RC13 * Basis: Robert Conrad * Method/Device: Piston corer (PC)
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 | Oppo, Delia W | Age model, SPECMAP chronology, Imbrie et al. (1984) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
56 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.00 | 2.5 |
| 0.60 | 17.9 |
| 1.10 | 25.4 |
| 1.55 | 50.2 |
| 1.70 | 55.5 |
| 1.80 | 64.1 |
| 1.90 | 70.8 |
| 2.00 | 73.9 |
| 2.15 | 79.3 |
| 2.40 | 91.0 |
| 2.50 | 103.0 |
| 2.66 | 110.8 |
| 2.90 | 122.6 |
| 3.25 | 129.8 |
| 3.35 | 135.1 |
| 3.76 | 161.3 |
| 4.15 | 183.3 |
| 4.22 | 189.6 |
| 4.30 | 193.1 |
| 4.50 | 215.5 |
| 4.56 | 224.9 |
| 4.68 | 240.2 |
| 4.80 | 247.6 |
| 4.99 | 265.7 |
| 5.35 | 288.5 |
| 5.60 | 298.0 |
| 5.91 | 310.0 |
| 6.10 | 320.0 |
| 6.30 | 330.0 |
| 6.50 | 337.0 |
| 6.65 | 342.0 |
| 7.55 | 361.0 |
| 7.85 | 368.0 |
| 8.67 | 405.0 |
| 9.14 | 423.0 |
| 9.46 | 434.0 |
| 9.54 | 444.0 |
| 10.35 | 471.0 |
| 10.86 | 481.0 |
| 11.24 | 502.0 |
| 11.54 | 513.0 |
| 11.74 | 524.0 |
| 12.01 | 538.0 |
| 12.35 | 552.0 |
| 12.44 | 563.0 |
| 12.62 | 574.0 |
| 12.71 | 585.0 |
| 12.96 | 596.0 |
| 13.22 | 607.0 |
| 13.71 | 617.0 |
| 13.81 | 628.0 |
| 14.41 | 643.0 |
| 14.85 | 668.0 |
| 15.45 | 683.0 |
| 15.76 | 711.0 |
| 16.14 | 730.0 |