Melles, Martin (1991): Grain size fraction analysis of sediment core PS1219-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.626400, 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: -76.606000 * Longitude: -36.891300
Date/Time Start: 1984-02-21T00:00:00 * Date/Time End: 1984-02-21T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 0.35 m
Event(s):
PS1219-1 (PS04/495) * Latitude: -76.606000 * Longitude: -36.891300 * Date/Time: 1984-02-21T00:00:00 * Elevation: -875.0 m * Penetration: 0.36 m * Recovery: 0.36 m * Location: Weddell Sea * Campaign: ANT-II/4 (PS04) * 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 | 58.53 | 8.20 | 8.05 | 5.74 | 4.17 | 1.54 | 4.74 | 3.88 | 2.67 | 1.72 | 0.46 | 0.29 | 0.00 | 0.00 |
0.11 | 57.75 | 7.56 | 7.41 | 4.94 | 4.52 | 1.90 | 7.21 | 5.43 | 1.72 | 0.62 | 0.36 | 0.57 | 0.00 | 0.00 |
0.20 | 41.45 | 8.77 | 8.56 | 8.36 | 8.16 | 2.45 | 8.10 | 6.78 | 3.01 | 1.12 | 0.37 | 0.43 | 2.43 | 0.00 |
0.25 | 40.35 | 8.99 | 9.21 | 8.55 | 8.12 | 4.16 | 5.37 | 6.06 | 4.40 | 2.03 | 1.05 | 0.70 | 1.04 | 0.00 |
0.30 | 40.28 | 10.43 | 11.23 | 10.95 | 11.76 | 3.75 | 2.69 | 3.35 | 2.44 | 1.02 | 0.40 | 0.47 | 1.26 | 0.00 |
0.35 | 48.31 | 9.45 | 8.79 | 7.90 | 7.25 | 3.51 | 4.00 | 4.69 | 3.41 | 1.44 | 0.83 | 0.41 | 0.00 | 0.00 |