Hillenbrand, Claus-Dieter; Kuhn, Gerhard; Frederichs, Thomas (2009): (Appendix) Age model of sediment profile PS2547-3 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.711068, In supplement to: Hillenbrand, C-D et al. (2009): Record of a Mid-Pleistocene depositional anomaly in West Antarctic continental margin sediments: An indicator for ice-sheet collapse? Quaternary Science Reviews, 28(13-14), 1147-1159, https://doi.org/10.1016/j.quascirev.2008.12.010
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Project(s):
Coverage:
Latitude: -71.150000 * Longitude: -119.918330
Date/Time Start: 1994-03-02T16:54:00 * Date/Time End: 1994-03-02T16:54:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 6.60 m
Event(s):
PS2547-3 (PS29/063) * Latitude: -71.150000 * Longitude: -119.918330 * Date/Time: 1994-03-02T16:54:00 * Elevation: -2096.0 m * Penetration: 13 m * Recovery: 8.76 m * Location: Amundsen Sea * Campaign: ANT-XI/3 (PS29) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 9 core sections: 0-0.76, 0.76-1.76, 1.76-2.76, 2.76-3.76, 3.76-4.76, 4.76-5.76, 5.76-6.76, 6.76-7.76, 7.76-8.76 m
Comment:
modified from Hillenbrand et al., 2002 data set: doi:10.1594/PANGAEA.55951
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 | Hillenbrand, Claus-Dieter | Age model according to Lisiecki & Raymo (2005) [LR04] | |
| 3 | Age, comment | Comm | Hillenbrand, Claus-Dieter | Marine Isotope Stage (MIS), paleomagnetic |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
47 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] | 3 Comm |
|---|---|---|
| 0.00 | 0 | |
| 0.07 | 14 | 1/2 |
| 0.17 | 71 | 4/5 |
| 0.45 | 130 | 5/6 |
| 0.83 | 191 | 6/7 |
| 1.06 | 243 | 7/8 |
| 1.13 | 300 | 8/9 |
| 1.27 | 337 | 9/10 |
| 1.44 | 374 | 10/11 |
| 1.60 | 424 | 11/12 |
| 1.74 | 478 | 12/13 |
| 1.87 | 533 | 13/14 |
| 1.93 | 563 | 14/15 |
| 2.07 | 621 | 15/16 |
| 2.43 | 676 | 16/17 |
| 2.64 | 712 | 17/18 |
| 2.73 | 761 | 18/19 |
| 2.90 | 780 | C1n (base) |
| 2.95 | 790 | 19/20 |
| 3.04 | 814 | 20/21 |
| 3.13 | 866 | 21/22 |
| 3.23 | 900 | 22/23 |
| 6.30 | 1770 | C2n (top) |
| 6.60 | 1950 | C2n (base) |