Venz, Kathryn A; Hodell, David A (2002): (Table 3) Plio-Pleistocene age-depth points of ODP Site 177-1090 in the Southern Ocean [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.696102, 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: -42.913617 * Longitude: 8.899817
Date/Time Start: 1997-12-25T00:00:00 * Date/Time End: 1997-12-25T00:00:00
Minimum DEPTH, sediment/rock: 0.0300 m * Maximum DEPTH, sediment/rock: 57.3300 m
Event(s):
177-1090 * Latitude: -42.913617 * Longitude: 8.899817 * Date/Time: 1997-12-25T00:00:00 * Elevation: -3701.6 m * Penetration: 936.4 m * Recovery: 874.9 m * Location: South Atlantic Ocean * Campaign: Leg177 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 101 cores; 936.4 m cored; 0 m drilled; 93.4% 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] |
|---|---|
| 0.0300 | 0.00 |
| 0.7500 | 20.00 |
| 2.5690 | 64.00 |
| 3.1390 | 80.00 |
| 3.5890 | 100.00 |
| 4.2890 | 122.00 |
| 4.5290 | 128.00 |
| 6.3290 | 188.00 |
| 6.8690 | 228.00 |
| 7.0860 | 238.00 |
| 7.9060 | 270.00 |
| 8.3560 | 296.00 |
| 8.8800 | 329.61 |
| 9.0031 | 338.71 |
| 13.2270 | 425.23 |
| 16.2100 | 522.97 |
| 17.1600 | 560.84 |
| 18.1100 | 616.08 |
| 21.8100 | 682.80 |
| 24.9600 | 782.90 |
| 27.0100 | 811.30 |
| 28.0500 | 864.39 |
| 31.3800 | 986.60 |
| 33.2300 | 1048.80 |
| 34.5800 | 1088.50 |
| 35.3900 | 1123.20 |
| 36.3300 | 1192.80 |
| 36.9700 | 1249.00 |
| 37.7200 | 1288.60 |
| 38.4700 | 1336.60 |
| 39.1200 | 1372.70 |
| 39.5200 | 1419.70 |
| 40.3700 | 1457.90 |
| 40.7700 | 1490.00 |
| 41.0200 | 1525.70 |
| 41.4700 | 1566.90 |
| 42.4700 | 1662.40 |
| 43.1200 | 1722.10 |
| 43.4200 | 1758.90 |
| 43.6700 | 1791.80 |
| 44.3700 | 1835.10 |
| 44.4200 | 1866.50 |
| 45.1200 | 1915.10 |
| 45.7700 | 1948.40 |
| 46.5200 | 1988.40 |
| 47.5400 | 2031.50 |
| 47.6900 | 2059.20 |
| 47.9900 | 2084.40 |
| 48.9400 | 2147.60 |
| 50.2400 | 2193.00 |
| 50.7400 | 2242.30 |
| 50.9400 | 2295.10 |
| 51.8400 | 2361.40 |
| 51.8900 | 2391.20 |
| 52.5800 | 2436.70 |
| 53.0800 | 2487.90 |
| 53.6800 | 2543.60 |
| 53.7300 | 2577.10 |
| 55.0300 | 2650.00 |
| 56.0800 | 2720.20 |
| 56.1300 | 2817.80 |
| 56.5300 | 2879.80 |
| 57.3300 | 2903.50 |