Weber, Michael E; Kuhn, Gerhard; Sprenk, Daniela; Rolf, Christian; Ohlwein, Christian; Ricken, Werner (2012): (Table 3) Age model of sediment core MD07-3133 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.771902, 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: -57.444000 * Longitude: -43.457800
Date/Time Start: 2007-03-05T17:30:00 * Date/Time End: 2007-03-05T17:30:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 32.76 m
Event(s):
MD07-3133 * Latitude: -57.444000 * Longitude: -43.457800 * Date/Time: 2007-03-05T17:30:00 * Elevation: -3103.0 m * Recovery: 32.8 m * Campaign: MD160 (OOMPH, SUBCLIMATE) * Basis: Marion Dufresne (1995) * Method/Device: Calypso Corer II (CALYPSO2) * Comment: 2 core catcher samples; top 20-30 cm missing
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 | Age, calculated calendar years |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
42 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.00 | 0.000 |
| 15.56 | 8.510 |
| 19.00 | 11.420 |
| 23.04 | 14.770 |
| 24.00 | 16.539 |
| 24.29 | 17.030 |
| 24.68 | 17.785 |
| 25.02 | 18.848 |
| 25.13 | 19.104 |
| 25.33 | 20.090 |
| 25.65 | 21.189 |
| 25.75 | 21.507 |
| 25.84 | 21.928 |
| 26.00 | 23.290 |
| 26.10 | 23.834 |
| 26.29 | 24.230 |
| 26.42 | 24.708 |
| 26.70 | 25.605 |
| 27.06 | 26.570 |
| 27.33 | 27.957 |
| 27.52 | 28.383 |
| 27.85 | 28.827 |
| 28.00 | 29.340 |
| 28.05 | 29.587 |
| 28.11 | 29.842 |
| 28.25 | 30.052 |
| 28.50 | 30.375 |
| 28.65 | 30.495 |
| 28.79 | 30.632 |
| 28.92 | 30.730 |
| 29.20 | 30.958 |
| 29.36 | 31.132 |
| 29.58 | 31.510 |
| 29.95 | 31.870 |
| 30.78 | 32.808 |
| 31.03 | 32.992 |
| 31.15 | 33.330 |
| 31.37 | 33.576 |
| 31.58 | 33.952 |
| 32.38 | 35.075 |
| 32.67 | 35.575 |
| 32.76 | 35.752 |