Carter, Robert M; Gammon, Paul (2004): (Table S1) Control points for the age model of ODP Site 181-1119 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.772061, In supplement to: Carter, RM; Gammon, P (2004): New Zealand Maritime Glaciation: Millennial-Scale Southern Climate Change Since 3.9 Ma. Science, 304(5677), 1659-1662, https://doi.org/10.1126/science.1093726
Always quote citation above when using data! You can download the citation in several formats below.
Related to:
Chen, Jiajie; Farrell, John W; Murray, David W; Prell, Warren L (1995): Timescale and paleoceanographic implications of a 3.6 m.y. oxygen isotope record from the northeast Indian Ocean (Ocean Drilling Program Site 758). Paleoceanography, 10(1), 21-48, https://doi.org/10.1029/94PA02290
Shackleton, Nicholas J (2000): The 100,000-year ice-age cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricity. Science, 289(5486), 1897-1902, https://doi.org/10.1126/science.289.5486.1897
Tian, Jun; Wang, Pinxian; Cheng, Xinrong; Li, Qianyu (2002): Astronomically tuned Plio- Pleistocene benthic d18O record from South-China Sea and Atlantic-Pacific comparison. Earth and Planetary Science Letters, 203(3-4), 1015-1029, https://doi.org/10.1016/S0012-821X(02)00923-8
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -44.755533 * Longitude: 172.393383
Date/Time Start: 1998-08-05T00:00:00 * Date/Time End: 1998-08-26T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 494.80 m
Event(s):
181-1119 * Latitude: -44.755533 * Longitude: 172.393383 * Date/Time Start: 1998-08-05T00:00:00 * Date/Time End: 1998-08-26T00:00:00 * Elevation: -396.2 m * Penetration: 656.6 m * Recovery: 612.8 m * Location: South Pacific Ocean * Campaign: Leg181 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 70 cores; 656.6 m cored; 0 m drilled; 93.3% recovery
Comment:
Sediment depth is given in mbsf. Age model generated by mapping from the tuned deuterium isotope record from Vostok (back to MIS 9.3; 0.35 Ma) (Shackleton, 2000) and the tuned oxygen isotope records from ODP Site 758, northern Indian Ocean (back to MIS Gi2; 3.64 Ma) (Chen et al., 1995), and Site 1143, South China Sea (back to MIS Gi11 at the base of the hole; 3.91 Ma) (Tian et al., 2002).
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Depth, composite revised | Depth comp r | rmcd | Carter, Robert M | ||
| 3 | Age model | Age model | ka | Carter, Robert M | ||
| 4 | Isotopic event | Isotopic event | Carter, Robert M | |||
| 5 | Age, comment | Comm | Carter, Robert M |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
195 data points
Data
| 1 Depth sed [m] | 2 Depth comp r [rmcd] | 3 Age model [ka] | 4 Isotopic event | 5 Comm |
|---|---|---|---|---|
| 0.00 | 0.00 | 0.000 | intra MIS 1 | Assumed |
| 0.28 | 0.44 | 9.000 | intra MIS 1 | Estimate (14C), Sub-Holocene diastem |
| 0.29 | 0.45 | 11.975 | intra MIS 2 | Estimate (14C), Sub-Holocene diastem |
| 1.98 | 2.14 | 15.157 | intra MIS 2 | AMS 14C |
| 3.92 | 4.08 | 16.419 | intra MIS 2 | AMS 14C |
| 4.84 | 5.00 | 17.278 | intra MIS 2 | AMS 14C |
| 6.36 | 6.52 | 18.180 | intra MIS 2 | AMS 14C |
| 11.12 | 10.88 | 21.531 | intra MIS 2 | AMS 14C |
| 14.54 | 14.30 | 24.059 | intra MIS 2 | AMS 14C |
| 18.62 | 18.34 | 39.330 | intra MIS 3 | AMS 14C |
| 41.78 | 42.78 | 113.000 | MIS 5.4 | Tuned Vostok, after Shackleton (2000) |
| 46.58 | 47.58 | 132.000 | MIS 5.5 | Tuned Vostok, MIS 5/6 diastem |
| 46.59 | 47.59 | 135.000 | intra-MIS 6 | Tuned Vostok, MIS 5/6 diastem |
| 48.52 | 50.78 | 151.000 | intra-MIS 6 | Tuned Vostok |
| 70.82 | 75.82 | 187.500 | MIS 6/7 | Tuned Vostok |
| 73.37 | 78.37 | 199.000 | MIS 7.1 | Tuned Vostok |
| 77.33 | 82.03 | 220.000 | MIS 7.5 | Tuned Vostok |
| 81.92 | 86.62 | 252.000 | intra-MIS 8 | Tuned Vostok, intra-MIS 8 downlap unconformity |
| 81.93 | 86.63 | 277.000 | intra-MIS 8 | Tuned Vostok, intra-MIS 8 downlap unconformity |
| 84.12 | 88.82 | 300.000 | MIS 8/9 | Tuned Vostok |
| 86.48 | 92.42 | 335.000 | MIS 9.3 | Tuned Vostok |
| 97.48 | 106.54 | 429.000 | MIS 12 | Tuned ODP 121-758, after Chen et al. (1995) |
| 122.07 | 132.65 | 572.000 | MIS 15.1 | Tuned ODP 121-758 |
| 168.25 | 187.00 | 688.000 | MIS 17 | Tuned ODP 121-758 |
| 182.27 | 201.02 | 783.000 | MIS 19 | Tuned ODP 121-758 |
| 204.52 | 223.27 | 952.000 | MIS 25 | Tuned ODP 121-758 |
| 216.71 | 235.46 | 1068.000 | MIS 31 | Tuned ODP 121-758 |
| 235.61 | 254.36 | 1238.000 | MIS 37 | Tuned ODP 121-758 |
| 241.55 | 260.30 | 1290.000 | MIS 40 | Tuned ODP 121-758 |
| 248.87 | 267.62 | 1398.000 | MIS 45 | Tuned ODP 121-758 |
| 267.61 | 286.36 | 1563.000 | MIS 53 | Tuned ODP 121-758 |
| 273.10 | 291.85 | 1642.000 | MIS 57 | Tuned ODP 121-758 |
| 279.96 | 298.71 | 1702.000 | MIS 60 | Tuned ODP 121-758 |
| 287.43 | 306.18 | 1788.000 | MIS 64 | Tuned ODP 121-758 |
| 296.26 | 315.01 | 1899.000 | MIS 69 | Tuned ODP 121-758 |
| 321.87 | 340.62 | 2146.000 | MIS 82 | Tuned ODP 121-758 |
| 327.36 | 346.11 | 2228.000 | MIS 85 | Tuned ODP 121-758 |
| 359.05 | 377.80 | 2528.000 | MIS 100 | Tuned ODP 121-758 |
| 370.94 | 389.69 | 2678.000 | MIS 107 | Tuned ODP 121-758 |
| 387.24 | 405.99 | 2872.000 | MIS 115 | Tuned ODP 121-758 |
| 397.61 | 416.36 | 2991.000 | MIS 121 | Tuned ODP 121-758 |
| 413.61 | 432.36 | 3130.000 | MIS 131 | Tuned ODP 121-758 |
| 432.51 | 451.26 | 3295.000 | MIS140 = M2 | Tuned ODP 121-758 |
| 441.96 | 460.71 | 3383.000 | MIS 146 | Tuned ODP 121-758 |
| 456.28 | 475.03 | 3585.000 | MIS 155 | Tuned ODP 121-758 |
| 462.68 | 481.43 | 3640.000 | MIS Gi-2 | Tuned ODP 184-1143A, after Tian et al. (2002) |
| 478.92 | 497.67 | 3770.000 | MIS Gi-8 | Tuned ODP 184-1143A |
| 491.52 | 510.27 | 3883.000 | MIS Gi-11 | Tuned ODP 184-1143A |
| 494.80 | 513.55 | 3912.300 | Estimated, total depth |