Melles, Martin (1991): Grain size fraction analysis of sediment core PS1016-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.626393, In supplement to: Melles, M (1991): Paläoglaziologie und Paläozeanographie im Spätquartär am Kontinentalrand des südlichen Weddellmeeres, Antarktis (Late Quaternary paleoglaciology and paleoceanography at the continental margin of the southern Weddell Sea, Antarctica). Berichte zur Polarforschung = Reports on Polar Research, 81, 190 pp, https://doi.org/10.2312/BzP_0081_1991
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Project(s):
Coverage:
Latitude: -77.284790 * Longitude: -40.832690
Date/Time Start: 1983-02-18T00:00:00 * Date/Time End: 1983-02-18T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 0.39 m
Event(s):
PS1016-1 (PS01/177) * Latitude: -77.284790 * Longitude: -40.832690 * Date/Time: 1983-02-18T00:00:00 * Elevation: -701.0 m * Penetration: 0.41 m * Recovery: 0.4 m * Location: Filchner Shelf * Campaign: ANT-I/2 (PS01) * Basis: Polarstern * Method/Device: Giant box corer (GKG)
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
84 data points
Data
1 Depth sed [m] | 2 <2 µm [%] | 3 4-2 µm [%] | 4 8-4 µm [%] | 5 16-8 µm [%] | 6 32-16 µm [%] | 7 63-32 µm [%] | 8 125-63 µm [%] | 9 250-125 µm [%] | 10 500-250 µm [%] | 11 1-0.5 mm [%] | 12 2-1 mm [%] | 13 4-2 mm [%] | 14 8-4 mm [%] | 15 >8 mm [%] |
---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
0.01 | 37.19 | 5.97 | 4.27 | 4.98 | 6.82 | 3.55 | 6.38 | 12.23 | 11.31 | 3.99 | 1.24 | 0.64 | 1.43 | 0.00 |
0.08 | 34.68 | 5.07 | 4.53 | 4.40 | 6.26 | 3.46 | 9.02 | 13.99 | 9.00 | 3.17 | 1.70 | 1.77 | 2.94 | 0.00 |
0.16 | 34.30 | 7.90 | 7.32 | 7.32 | 8.90 | 3.75 | 8.80 | 10.43 | 7.13 | 2.22 | 0.94 | 0.75 | 0.23 | 0.00 |
0.23 | 25.07 | 6.00 | 5.58 | 4.74 | 5.30 | 3.49 | 17.24 | 22.84 | 6.95 | 1.64 | 0.66 | 0.33 | 0.16 | 0.00 |
0.31 | 8.18 | 2.01 | 2.18 | 3.38 | 5.28 | 3.65 | 11.67 | 23.00 | 14.59 | 8.12 | 4.44 | 3.70 | 2.43 | 7.38 |
0.39 | 10.38 | 1.96 | 2.02 | 1.71 | 2.44 | 2.32 | 9.49 | 21.17 | 21.51 | 10.33 | 3.75 | 3.58 | 3.24 | 6.12 |