Melles, Martin (1991): Grain size fraction analysis of sediment core PS1011-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.626389, 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: -77.283000 * Longitude: -35.395000
Date/Time Start: 1983-02-13T00:00:00 * Date/Time End: 1983-02-13T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 0.32 m
Event(s):
PS1011-1 (PS01/155) * Latitude: -77.283000 * Longitude: -35.395000 * Date/Time: 1983-02-13T00:00:00 * Elevation: -721.0 m * Penetration: 0.34 m * Recovery: 0.33 m * Location: Filchner Trough * 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 | 20.01 | 2.71 | 2.25 | 3.45 | 9.91 | 9.61 | 13.30 | 16.23 | 12.91 | 5.72 | 1.16 | 0.67 | 0.36 | 1.70 |
0.04 | 15.50 | 2.29 | 1.88 | 2.98 | 5.87 | 5.28 | 19.36 | 15.88 | 7.64 | 3.51 | 1.84 | 3.38 | 4.35 | 10.25 |
0.07 | 8.54 | 1.63 | 1.82 | 2.63 | 5.90 | 4.72 | 12.07 | 11.05 | 6.70 | 5.56 | 3.69 | 6.76 | 10.29 | 18.64 |
0.11 | 14.54 | 2.22 | 2.22 | 4.60 | 10.39 | 8.17 | 15.43 | 12.92 | 7.02 | 4.46 | 4.05 | 3.83 | 3.77 | 6.37 |
0.21 | 14.00 | 1.99 | 2.45 | 4.43 | 10.87 | 8.88 | 14.15 | 12.27 | 6.64 | 3.74 | 3.65 | 3.32 | 4.05 | 9.63 |
0.32 | 13.48 | 2.20 | 2.07 | 3.88 | 8.92 | 7.11 | 13.14 | 11.75 | 6.21 | 3.58 | 3.58 | 3.24 | 5.33 | 15.50 |