Vogt, Christoph (2004): Clay mineralogy of sediment core PS2213-4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.137786, 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: 80.473000 * Longitude: 8.205200
Date/Time Start: 1991-09-30T00:00:00 * Date/Time End: 1991-09-30T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 0.32 m
Event(s):
PS2213-4 (PS19/246) * Latitude: 80.473000 * Longitude: 8.205200 * Date/Time: 1991-09-30T00:00:00 * Elevation: -897.0 m * Penetration: 0.3 m * Recovery: 0.3 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:
176 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 |
---|---|---|---|---|---|---|---|---|---|---|---|
0.01 | 5 | 59 | 16 | 20 | 0.81 | 0.75 | 0.40 | 0.45 | 0.22 | 3.58 | 0.23 |
0.04 | 9 | 53 | 17 | 21 | 1.42 | 0.95 | 0.39 | 0.55 | 0.18 | 3.26 | 0.27 |
0.06 | 6 | 59 | 15 | 20 | 0.76 | 0.74 | 0.39 | 0.41 | 0.24 | 3.39 | 0.53 |
0.07 | 8 | 55 | 16 | 22 | 1.20 | 0.90 | 0.37 | 0.50 | 0.19 | 3.20 | 0.27 |
0.10 | 2 | 58 | 18 | 23 | 0.74 | 0.56 | 0.41 | 0.52 | 0.18 | 2.75 | 0.23 |
0.12 | 5 | 58 | 17 | 19 | 0.95 | 0.70 | 0.40 | 0.46 | 0.24 | 3.26 | 0.28 |
0.14 | 5 | 61 | 15 | 19 | 0.78 | 0.71 | 0.41 | 0.40 | 0.22 | 2.82 | 0.33 |
0.15 | 10 | 58 | 14 | 18 | 1.35 | 0.97 | 0.43 | 0.37 | 0.49 | 3.26 | 0.75 |
0.17 | 9 | 59 | 14 | 17 | 1.11 | 0.84 | 0.43 | 0.40 | 0.25 | 3.33 | 0.40 |
0.20 | 6 | 59 | 16 | 19 | 1.15 | 0.88 | 0.39 | 0.39 | 0.23 | 3.01 | 0.33 |
0.21 | 7 | 59 | 16 | 18 | 0.72 | 0.72 | 0.40 | 0.42 | 0.14 | 2.88 | 0.28 |
0.23 | 5 | 60 | 17 | 18 | 0.91 | 0.70 | 0.42 | 0.44 | 0.19 | 3.07 | 0.34 |
0.26 | 7 | 56 | 17 | 20 | 0.93 | 0.83 | 0.46 | 0.50 | 0.18 | 2.82 | 0.25 |
0.28 | 9 | 53 | 18 | 20 | 1.54 | 1.13 | 0.45 | 0.64 | 0.09 | 2.50 | 0.16 |
0.29 | 10 | 54 | 17 | 18 | 1.39 | 1.67 | 0.44 | 0.53 | 0.10 | 2.75 | 0.16 |
0.32 | 10 | 55 | 16 | 19 | 1.22 | 1.05 | 0.43 | 0.44 | 0.14 | 2.82 | 0.22 |