Holbourn, Ann E; Kuhnt, Wolfgang; James, Noel P (2002): Age model of ODP Hole 182-1132B [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.95058, In supplement to: Holbourn, AE et al. (2002): Late Pleistocene bryozoan reef mounds of the Great Australian Bight: isotope stratigraphy and benthic foraminiferal record. Paleoceanography, 17(3), 1042, https://doi.org/10.1029/2001PA000643
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Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -33.316180 * Longitude: 127.602200
Date/Time Start: 1998-11-21T01:15:00 * Date/Time End: 1998-11-22T04:25:00
Minimum DEPTH, sediment/rock: 28.85 m * Maximum DEPTH, sediment/rock: 144.04 m
Event(s):
182-1132B * Latitude: -33.316180 * Longitude: 127.602200 * Date/Time Start: 1998-11-21T01:15:00 * Date/Time End: 1998-11-22T04:25:00 * Elevation: -218.5 m * Penetration: 284.6 m * Recovery: 217.35 m * Location: Great Australian Bight * Campaign: Leg182 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 32 cores; 284.6 m cored; 0 m drilled; 76.4 % 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 | Holbourn, Ann E | Age model, SPECMAP chronology, Imbrie et al. (1984) | |
| 3 | Age model, optional | Age model opt | ka | Holbourn, Ann E | Age model, Martinson et al (1987) | |
| 4 | Marine isotopic stage | MIS | Holbourn, Ann E | 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] | 3 Age model opt [ka] | 4 MIS |
|---|---|---|---|
| 28.85 | 65 | 64.09 | 4.2 |
| 40.09 | 80 | 79.25 | 5.1 |
| 41.78 | 128 | 129.84 | 6.0 |
| 44.44 | 151 | 152.58 | 6.4 |
| 61.54 | 171 | 175.05 | 6.5 |
| 66.43 | 183 | 183.30 | 6.6 |
| 68.08 | 194 | 193.07 | 7.1 |
| 76.76 | 228 | 224.89 | 7.4 |
| 81.88 | 238 | 240.19 | 7.5 |
| 84.59 | 249 | 247.60 | 8.2 |
| 90.93 | 303 | 9.0 | |
| 100.65 | 310 | 9.1 | |
| 103.58 | 320 | 9.2 | |
| 105.17 | 331 | 9.3 | |
| 108.28 | 339 | 10.0 | |
| 110.00 | 341 | 10.2 | |
| 119.17 | 368 | 11.1 | |
| 128.65 | 375 | 11.2 | |
| 132.16 | 405 | 11.3 | |
| 134.21 | 423 | 12.0 | |
| 135.95 | 434 | 12.2 | |
| 142.18 | 451 | 12.3 | |
| 144.04 | 471 | 12.4 |