Hillenbrand, Claus-Dieter; Ehrmann, Werner; Larter, Robert D; Benetti, Sara; Dowdeswell, Julian A; Ó Cofaigh, Colm; Graham, Alastair G C; Grobe, Hannes (2009): (Supp. Fig.) Clay mineral content of sediment core PS2543-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.711170, In supplement to: Hillenbrand, C-D et al. (2009): Clay mineral provenance of sediments in the southern Bellingshausen Sea reveals drainage changes of the West Antarctic Ice Sheet during the Late Quaternary. Marine Geology, 265(1-2), 1-18, https://doi.org/10.1016/j.margeo.2009.06.009
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Project(s):
Coverage:
Latitude: -70.946660 * Longitude: -89.343330
Date/Time Start: 1994-02-18T00:00:00 * Date/Time End: 1994-02-18T00:00:00
Minimum DEPTH, sediment/rock: 0.270 m * Maximum DEPTH, sediment/rock: 1.570 m
Event(s):
PS2543-1 (PS29/051) * Latitude: -70.946660 * Longitude: -89.343330 * Date/Time: 1994-02-18T00:00:00 * Elevation: -547.0 m * Penetration: 3 m * Recovery: 1.7 m * Location: Bellingshausen Sea * Campaign: ANT-XI/3 (PS29) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 2 core sections: 0.25-0.7, 0.7-1.7 m
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Smectite | Sme | % | Hillenbrand, Claus-Dieter | X-ray diffraction (XRD) | |
3 | Illite | Ill | % | Hillenbrand, Claus-Dieter | X-ray diffraction (XRD) | |
4 | Chlorite | Chl | % | Hillenbrand, Claus-Dieter | X-ray diffraction (XRD) | |
5 | Kaolinite | Kln | % | Hillenbrand, Claus-Dieter | X-ray diffraction (XRD) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
52 data points
Data
1 Depth sed [m] | 2 Sme [%] | 3 Ill [%] | 4 Chl [%] | 5 Kln [%] |
---|---|---|---|---|
0.270 | 15.5 | 52.8 | 23.2 | 8.5 |
0.370 | 14.7 | 56.0 | 21.9 | 7.5 |
0.470 | 16.0 | 52.8 | 22.9 | 8.2 |
0.570 | 14.9 | 49.6 | 26.2 | 9.3 |
0.630 | 19.8 | 50.9 | 21.5 | 7.7 |
0.670 | 17.4 | 49.7 | 24.0 | 8.9 |
0.770 | 16.2 | 51.3 | 23.5 | 8.9 |
0.870 | 19.3 | 47.7 | 24.7 | 8.4 |
0.970 | 19.9 | 48.8 | 22.6 | 8.7 |
1.120 | 20.2 | 50.7 | 21.4 | 7.7 |
1.270 | 20.1 | 49.4 | 22.4 | 8.2 |
1.420 | 19.3 | 52.5 | 21.6 | 6.6 |
1.570 | 20.7 | 50.4 | 21.4 | 7.6 |