deMenocal, Peter B; Oppo, Delia W; Fairbanks, Richard G; Prell, Warren L (1992): (Table B1) Age model of DSDP Hole 68-502B in the Caribbean Sea [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.52482, In supplement to: deMenocal, PB et al. (1992): Pleistocene d13C variability of North Atlantic intermediate water. Paleoceanography, 7(2), 229-250, https://doi.org/10.1029/92PA00420
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Project(s):
Deep Sea Drilling Project (DSDP)
Coverage:
Latitude: 11.491800 * Longitude: -79.378200
Date/Time Start: 1979-08-16T00:00:00 * Date/Time End: 1979-08-16T00:00:00
Minimum DEPTH, sediment/rock: 0.20 m * Maximum DEPTH, sediment/rock: 24.93 m
Event(s):
68-502B * Latitude: 11.491800 * Longitude: -79.378200 * Date/Time: 1979-08-16T00:00:00 * Elevation: -3051.0 m * Penetration: 99.7 m * Recovery: 87.7 m * Location: Caribbean Sea/RIDGE * Campaign: Leg68 * Basis: Glomar Challenger * Method/Device: Drilling/drill rig (DRILL) * Comment: 23 cores; 99.7 m cored; 0 m drilled; 88 % recovery
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 | deMenocal, Peter B | Age model, stable isotope stratigraphy |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
56 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.20 | 4 |
| 0.59 | 18 |
| 1.10 | 36 |
| 1.66 | 64 |
| 2.01 | 116 |
| 2.20 | 125 |
| 2.30 | 136 |
| 2.80 | 161 |
| 3.20 | 179 |
| 3.40 | 196 |
| 3.90 | 220 |
| 4.10 | 230 |
| 4.70 | 252 |
| 5.40 | 274 |
| 6.20 | 297 |
| 6.46 | 327 |
| 6.71 | 339 |
| 7.02 | 363 |
| 7.31 | 385 |
| 7.61 | 408 |
| 8.11 | 435 |
| 8.31 | 450 |
| 8.40 | 471 |
| 8.61 | 480 |
| 9.51 | 500 |
| 10.31 | 520 |
| 10.95 | 586 |
| 11.50 | 616 |
| 11.76 | 630 |
| 12.15 | 650 |
| 12.80 | 667 |
| 13.55 | 679 |
| 13.95 | 690 |
| 14.25 | 700 |
| 14.81 | 707 |
| 15.39 | 718 |
| 16.21 | 735 |
| 16.70 | 744 |
| 16.95 | 760 |
| 17.42 | 814 |
| 17.74 | 840 |
| 18.24 | 864 |
| 18.52 | 876 |
| 18.64 | 908 |
| 19.36 | 927 |
| 19.96 | 950 |
| 20.30 | 962 |
| 20.86 | 981 |
| 21.55 | 1010 |
| 21.93 | 1046 |
| 22.55 | 1062 |
| 23.08 | 1080 |
| 23.40 | 1090 |
| 24.58 | 1105 |
| 24.73 | 1125 |
| 24.93 | 1135 |