Weber, Michael E; Kuhn, Gerhard; Sprenk, Daniela; Rolf, Christian; Ohlwein, Christian; Ricken, Werner (2012): (Table 1) Age model of sediment core MD07-3134 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.771900, In supplement to: Weber, ME et al. (2012): Dust transport from Patagonia to Antarctica - a new stratigraphic approach from the Scotia Sea and its implications for the last glacial cycle. Quaternary Science Reviews, 36, 177-188, https://doi.org/10.1016/j.quascirev.2012.01.016
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Project(s):
Coverage:
Latitude: -59.410800 * Longitude: -41.473000
Date/Time Start: 2007-03-06T16:10:00 * Date/Time End: 2007-03-06T16:10:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 58.06 m
Event(s):
MD07-3134 * Latitude: -59.410800 * Longitude: -41.473000 * Date/Time: 2007-03-06T16:10:00 * Elevation: -3663.0 m * Recovery: 58.08 m * Campaign: MD160 (OOMPH, SUBCLIMATE) * Basis: Marion Dufresne (1995) * Method/Device: Calypso Corer II (CALYPSO2) * Comment: 1 core catcher sample
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 | Weber, Michael E |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
48 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.00 | 0.000 |
| 8.93 | 8.500 |
| 11.98 | 12.805 |
| 13.42 | 14.798 |
| 14.69 | 16.540 |
| 15.26 | 17.641 |
| 15.43 | 18.182 |
| 15.52 | 18.386 |
| 15.77 | 19.120 |
| 16.00 | 20.064 |
| 16.37 | 21.189 |
| 16.86 | 23.110 |
| 16.97 | 23.572 |
| 17.05 | 23.845 |
| 17.38 | 24.731 |
| 17.78 | 25.710 |
| 18.30 | 27.984 |
| 18.56 | 28.834 |
| 18.80 | 29.970 |
| 19.84 | 31.140 |
| 20.40 | 32.201 |
| 22.59 | 35.760 |
| 24.70 | 38.459 |
| 25.08 | 39.230 |
| 26.19 | 41.646 |
| 26.31 | 42.050 |
| 26.65 | 42.980 |
| 26.97 | 44.270 |
| 27.49 | 46.390 |
| 28.38 | 47.657 |
| 29.35 | 48.670 |
| 33.38 | 54.170 |
| 33.95 | 55.690 |
| 34.86 | 56.526 |
| 38.66 | 60.500 |
| 40.06 | 62.071 |
| 40.66 | 62.810 |
| 41.52 | 63.626 |
| 43.20 | 65.520 |
| 44.05 | 66.349 |
| 44.92 | 67.061 |
| 45.41 | 67.740 |
| 46.49 | 70.700 |
| 46.95 | 72.110 |
| 50.37 | 75.756 |
| 54.18 | 87.409 |
| 55.23 | 89.876 |
| 58.06 | 92.490 |