Venz, Kathryn A; Hodell, David A (2002): (Table 3) Plio-Pleistocene age-depth points of ODP Site 162-982 in the Southern Ocean [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.696101, In supplement to: Venz, KA; Hodell, DA (2002): New evidence for changes in Plio-Pleistocene deep water circulation from Southern Ocean ODP Leg 177 Site 1090. Palaeogeography, Palaeoclimatology, Palaeoecology, 182(3-4), 197-220, https://doi.org/10.1016/S0031-0182(01)00496-5
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: 57.512667 * Longitude: -15.854183
Date/Time Start: 1995-07-15T00:00:00 * Date/Time End: 1995-07-19T00:00:00
Minimum DEPTH, sediment/rock: 0.02 m * Maximum DEPTH, sediment/rock: 73.08 m
Event(s):
162-982 * Latitude: 57.512667 * Longitude: -15.854183 * Date/Time Start: 1995-07-15T00:00:00 * Date/Time End: 1995-07-19T00:00:00 * Elevation: -1134.2 m * Penetration: 1143.9 m * Recovery: 1008 m * Location: South Atlantic Ocean * Campaign: Leg162 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 120 cores; 1123.9 m cored; 0 m drilled; 89.7% recovery
Comment:
Depth is composite depth (mcd). The chronology was derived by correlation of the benthic foraminiferal oxygen isotopic signals with DSDP Site 94-607 (Raymo et al., 1990 doi:10.1016/0012-821X(90)90051-X) using the program Analyseries (Paillard et al., 1996 doi:10.1029/96EO00259)
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 | Venz, Kathryn A | Age model, stable isotope stratigraphy |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
63 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.02 | 0.0000 |
| 0.57 | 5.8474 |
| 3.02 | 131.4000 |
| 3.62 | 183.5800 |
| 4.97 | 245.5600 |
| 6.92 | 339.5500 |
| 10.09 | 422.9800 |
| 11.64 | 476.6700 |
| 14.14 | 528.9500 |
| 16.10 | 629.2000 |
| 17.63 | 682.8000 |
| 18.73 | 707.4000 |
| 20.03 | 782.9000 |
| 20.63 | 810.0400 |
| 22.48 | 862.1800 |
| 23.53 | 926.3700 |
| 24.58 | 959.1500 |
| 25.28 | 1005.4000 |
| 26.13 | 1037.3000 |
| 29.15 | 1128.9000 |
| 30.00 | 1194.8000 |
| 30.05 | 1208.9000 |
| 30.45 | 1249.0000 |
| 31.10 | 1288.6000 |
| 31.90 | 1336.9000 |
| 32.35 | 1367.1000 |
| 33.45 | 1413.1000 |
| 33.60 | 1430.5000 |
| 34.10 | 1464.8000 |
| 34.55 | 1501.2000 |
| 35.25 | 1541.4000 |
| 37.73 | 1662.4000 |
| 39.08 | 1756.7000 |
| 39.70 | 1758.9000 |
| 40.40 | 1782.9000 |
| 40.50 | 1795.7000 |
| 41.10 | 1839.8000 |
| 42.45 | 1919.2000 |
| 43.25 | 1948.4000 |
| 44.15 | 1993.0000 |
| 45.75 | 2065.7000 |
| 47.80 | 2147.6000 |
| 49.45 | 2242.3000 |
| 49.50 | 2284.6000 |
| 50.03 | 2310.7000 |
| 50.78 | 2370.5000 |
| 51.43 | 2410.0000 |
| 52.23 | 2436.7000 |
| 53.28 | 2481.8000 |
| 54.53 | 2521.5000 |
| 56.18 | 2577.1000 |
| 57.48 | 2603.0000 |
| 57.50 | 2604.6000 |
| 57.55 | 2618.0000 |
| 58.15 | 2650.0000 |
| 59.69 | 2701.6000 |
| 61.14 | 2736.4000 |
| 62.39 | 2770.5000 |
| 63.39 | 2817.8000 |
| 64.64 | 2879.8000 |
| 65.79 | 2983.5000 |
| 68.17 | 3150.2000 |
| 73.08 | 3299.8000 |