Vogt, Christoph (2004): Clay mineralogy of sediment core PS2212-6 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.137784, In supplement to: Vogt, C (1997): Zeitliche und räumliche Verteilung von Mineralvergesellschaftungen in spätquartären Sedimenten des Arktische Ozeans und ihre Nützlichkeit als Klimaindikatoren während der Glazial/Interglazial-Wechsel (Regional and temporal variations of mineral assemblages in Arctic Ocean sediments as climate indicator during glacial/interglacial changes). Berichte zur Polarforschung = Reports on Polar Research, 251, 309 pp, https://doi.org/10.2312/BzP_0251_1997
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Project(s):
Funding:
Fourth Framework Programme (FP4), grant/award no. MAS3980185: Quaternary Environment of the Eurasian North
Coverage:
Latitude: 82.023700 * Longitude: 15.672300
Date/Time Start: 1991-09-29T00:00:00 * Date/Time End: 1991-09-29T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 0.35 m
Event(s):
PS2212-6 (PS19/245) * Latitude: 82.023700 * Longitude: 15.672300 * Date/Time: 1991-09-29T00:00:00 * Elevation: -2531.0 m * Penetration: 0.4 m * Recovery: 0.4 m * Location: Yermak Plateau * Campaign: ARK-VIII/3 (PS19 ARCTIC91) * Basis: Polarstern * Method/Device: MultiCorer (MUC) * Comment: 8 Rohre
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
209 data points
Data
1 Depth sed [m] | 2 Sme [%] | 3 Ill [%] | 4 Kln [%] | 5 Chl [%] | 6 Sme HHW [d2Theta] | 7 Smec IW [d2Theta] | 8 Ill HHW glyc [d2Theta] | 9 Ill EI | 10 Qz/std | 11 Qz [%] | 12 Fsp/std |
---|---|---|---|---|---|---|---|---|---|---|---|
0.00 | 5 | 61 | 16 | 19 | 0.89 | 0.68 | 0.42 | 0.42 | 0.15 | 2.56 | 0.25 |
0.01 | 7 | 56 | 17 | 20 | 1.18 | 0.89 | 0.40 | 0.42 | 0.17 | 2.94 | 0.19 |
0.06 | 7 | 58 | 17 | 18 | 1.32 | 1.04 | 0.40 | 0.43 | 0.15 | 2.69 | 0.21 |
0.07 | 5 | 57 | 18 | 21 | 0.68 | 0.58 | 0.41 | 0.40 | 0.17 | 3.01 | 0.21 |
0.10 | 6 | 58 | 17 | 19 | 1.19 | 0.85 | 0.39 | 0.39 | 0.15 | 2.69 | 0.20 |
0.12 | 8 | 57 | 16 | 19 | 1.32 | 0.94 | 0.40 | 0.44 | 0.13 | 2.75 | 0.20 |
0.14 | 6 | 59 | 16 | 18 | 1.15 | 0.94 | 0.41 | 0.41 | 0.15 | 2.94 | 0.19 |
0.15 | 5 | 55 | 19 | 21 | 0.91 | 0.64 | 0.37 | 0.48 | 0.12 | 2.88 | 0.22 |
0.17 | 7 | 59 | 16 | 18 | 1.07 | 0.92 | 0.42 | 0.45 | 0.13 | 2.62 | 0.21 |
0.18 | 6 | 59 | 16 | 20 | 1.11 | 0.90 | 0.41 | 0.46 | 0.13 | 2.82 | 0.24 |
0.20 | 7 | 59 | 16 | 18 | 1.33 | 1.02 | 0.41 | 0.44 | 0.13 | 3.07 | 0.22 |
0.23 | 7 | 60 | 16 | 17 | 1.18 | 0.94 | 0.45 | 0.55 | 0.13 | 3.33 | 0.19 |
0.24 | 10 | 62 | 13 | 14 | 1.43 | 1.13 | 0.44 | 0.36 | 0.16 | 2.88 | 0.24 |
0.27 | 8 | 53 | 19 | 20 | 1.06 | 0.87 | 0.42 | 0.54 | 0.11 | 3.26 | 0.21 |
0.28 | 9 | 54 | 18 | 19 | 1.17 | 0.97 | 0.41 | 0.60 | 0.09 | 3.46 | 0.18 |
0.29 | 6 | 54 | 20 | 20 | 1.05 | 0.95 | 0.40 | 0.59 | 0.09 | 3.33 | 0.15 |
0.32 | 14 | 47 | 19 | 20 | 1.06 | 0.93 | 0.38 | 0.43 | 0.18 | 3.26 | 0.25 |
0.34 | 19 | 41 | 20 | 20 | 1.09 | 1.04 | 0.40 | 0.39 | 0.16 | 3.14 | 0.37 |
0.35 | 16 | 47 | 19 | 18 | 1.42 | 1.23 | 0.42 | 0.58 | 0.06 | 3.58 | 0.09 |