Vogt, Christoph (2004): Clay mineralogy of sediment core PS2208-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.137779, 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: 83.640300 * Longitude: 4.603700
Date/Time Start: 1991-09-24T00:00:00 * Date/Time End: 1991-09-24T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 0.29 m
Event(s):
PS2208-1 (PS19/234) * Latitude: 83.640300 * Longitude: 4.603700 * Date/Time: 1991-09-24T00:00:00 * Elevation: -3681.0 m * Penetration: 0.3 m * Recovery: 0.3 m * Location: Nansen Basin * Campaign: ARK-VIII/3 (PS19 ARCTIC91) * Basis: Polarstern * Method/Device: MultiCorer (MUC) * Comment: 11 Rohre
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
264 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 | 10 | 56 | 14 | 21 | 1.08 | 0.91 | 0.35 | 0.45 | 0.26 | 3.14 | 0.50 |
0.01 | 9 | 55 | 15 | 22 | 1.22 | 0.93 | 0.30 | 0.46 | 0.27 | 4.29 | 0.52 |
0.03 | 7 | 57 | 15 | 21 | 1.22 | 0.84 | 0.31 | 0.45 | 0.30 | 3.78 | 0.74 |
0.04 | 7 | 57 | 15 | 21 | 1.15 | 0.76 | 0.34 | 0.46 | 0.22 | 3.52 | 0.51 |
0.06 | 7 | 53 | 17 | 23 | 0.97 | 0.79 | 0.34 | 0.49 | 0.22 | 4.16 | 0.41 |
0.07 | 6 | 55 | 17 | 21 | 0.88 | 0.75 | 0.34 | 0.56 | 0.23 | 4.10 | 0.41 |
0.09 | 6 | 52 | 20 | 22 | 1.10 | 0.93 | 0.33 | 0.56 | 0.20 | 4.29 | 0.37 |
0.10 | 7 | 44 | 26 | 23 | 0.87 | 0.75 | 0.31 | 0.64 | 0.12 | 4.54 | 0.21 |
0.12 | 11 | 50 | 18 | 20 | 1.44 | 1.09 | 0.34 | 0.60 | 0.18 | 4.22 | 0.35 |
0.12 | 5 | 55 | 20 | 20 | 1.05 | 0.84 | 0.34 | 0.64 | 0.11 | 3.78 | 0.30 |
0.14 | 4 | 54 | 21 | 21 | 0.71 | 0.58 | 0.33 | 0.49 | 0.18 | 4.86 | 0.29 |
0.14 | 2 | 60 | 20 | 18 | 0.61 | 0.53 | 0.36 | 0.40 | 0.23 | 4.80 | 0.34 |
0.15 | 4 | 59 | 20 | 18 | 0.90 | 0.69 | 0.34 | 0.47 | 0.19 | 4.61 | 0.32 |
0.17 | 5 | 59 | 18 | 17 | 0.98 | 0.76 | 0.40 | 0.54 | 0.17 | 3.78 | 0.40 |
0.18 | 6 | 59 | 19 | 16 | 1.00 | 0.84 | 0.38 | 0.46 | 0.43 | 4.54 | 0.76 |
0.20 | 4 | 58 | 19 | 19 | 1.24 | 0.84 | 0.35 | 0.49 | 0.19 | 4.74 | 0.35 |
0.20 | 6 | 59 | 18 | 17 | 0.75 | 0.81 | 0.33 | 0.42 | 0.22 | 4.42 | 0.39 |
0.21 | 3 | 61 | 19 | 17 | 0.69 | 0.74 | 0.33 | 0.46 | 0.20 | 4.10 | 0.39 |
0.23 | 7 | 62 | 16 | 15 | 1.04 | 0.88 | 0.38 | 0.35 | 0.22 | 3.90 | 0.39 |
0.23 | 5 | 57 | 20 | 18 | 1.12 | 0.79 | 0.37 | 0.48 | 0.19 | 3.97 | 0.37 |
0.24 | 4 | 59 | 19 | 18 | 0.81 | 0.62 | 0.37 | 0.57 | 0.19 | 4.35 | 0.37 |
0.26 | 9 | 60 | 16 | 16 | 1.21 | 0.97 | 0.38 | 0.40 | 0.21 | 4.16 | 0.38 |
0.28 | 2 | 55 | 23 | 20 | 0.51 | 0.45 | 0.35 | 0.59 | 0.18 | 4.54 | 0.30 |
0.29 | 3 | 64 | 17 | 16 | 0.68 | 0.50 | 0.42 | 0.45 | 0.23 | 4.48 | 0.41 |