Holbourn, Ann E; Kuhnt, Wolfgang; James, Noel P (2002): Age model of ODP Hole 182-1129C [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.95057, 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: -33.296560 * Longitude: 128.481300
Date/Time Start: 1998-11-24T23:24:00 * Date/Time End: 1998-11-26T18:30:00
Minimum DEPTH, sediment/rock: 5.44 m * Maximum DEPTH, sediment/rock: 137.46 m
Event(s):
182-1129C * Latitude: -33.296560 * Longitude: 128.481300 * Date/Time Start: 1998-11-24T23:24:00 * Date/Time End: 1998-11-26T18:30:00 * Elevation: -202.4 m * Penetration: 451.6 m * Recovery: 322.89 m * Location: Great Australian Bight * Campaign: Leg182 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 48 cores; 451.6 m cored; 0 m drilled; 71.5 % 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:
54 data points
Data
1 Depth sed [m] | 2 Age model [ka] | 3 Age model opt [ka] | 4 MIS |
---|---|---|---|
5.44 | 12 | 12.05 | 2.0 |
6.12 | 19 | 17.85 | 2.2 |
34.51 | 65 | 64.09 | 4.2 |
37.88 | 80 | 79.25 | 5.1 |
40.83 | 128 | 129.84 | 6.0 |
43.12 | 151 | 152.58 | 6.4 |
58.74 | 171 | 175.05 | 6.5 |
61.70 | 183 | 183.30 | 6.6 |
70.97 | 194 | 193.07 | 7.1 |
78.70 | 228 | 224.89 | 7.4 |
79.97 | 238 | 240.19 | 7.5 |
84.45 | 249 | 247.60 | 8.2 |
94.97 | 310 | 9.1 | |
97.15 | 339 | 10.0 | |
97.70 | 341 | 10.2 | |
113.61 | 368 | 11.1 | |
123.38 | 405 | 11.3 | |
127.52 | 423 | 12.0 | |
128.08 | 434 | 12.2 | |
134.45 | 451 | 12.3 | |
137.46 | 471 | 12.4 |