Vogt, Christoph (2004): Clay mineralogy of sediment core PS2210-3 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.137781, 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: 83.045300 * Longitude: 10.124700
Date/Time Start: 1991-09-27T00:00:00 * Date/Time End: 1991-09-27T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 0.21 m
Event(s):
PS2210-3 (PS19/241) * Latitude: 83.045300 * Longitude: 10.124700 * Date/Time: 1991-09-27T00:00:00 * Elevation: -3949.0 m * Penetration: 0.35 m * Recovery: 0.35 m * Location: Nansen Basin * Campaign: ARK-VIII/3 (PS19 ARCTIC91) * Basis: Polarstern * Method/Device: MultiCorer (MUC) * Comment: 5 Rohre
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
154 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 | 15 | 51 | 15 | 18 | 1.51 | 1.19 | 0.38 | 0.41 | 0.19 | 2.88 | 0.33 |
0.01 | 9 | 54 | 17 | 20 | 0.87 | 0.78 | 0.35 | 0.48 | 0.13 | 3.33 | 0.32 |
0.04 | 8 | 47 | 23 | 22 | 1.05 | 0.87 | 0.35 | 0.53 | 0.12 | 3.97 | 0.21 |
0.06 | 13 | 42 | 24 | 22 | 1.52 | 1.26 | 0.34 | 0.56 | 0.09 | 4.48 | 0.13 |
0.07 | 8 | 50 | 19 | 23 | 1.09 | 0.84 | 0.34 | 0.55 | 0.08 | 3.78 | 0.17 |
0.09 | 9 | 56 | 17 | 18 | 1.14 | 0.89 | 0.40 | 0.35 | 0.16 | 3.39 | 0.27 |
0.10 | 6 | 50 | 23 | 21 | 1.28 | 0.98 | 0.35 | 0.63 | 0.08 | 4.22 | 0.16 |
0.10 | 4 | 60 | 20 | 17 | 0.73 | 0.66 | 0.41 | 0.47 | 0.12 | 4.35 | 0.22 |
0.12 | 1 | 50 | 28 | 21 | 0.72 | 0.62 | 0.36 | 0.71 | 0.06 | 3.97 | 0.09 |
0.14 | 1 | 57 | 22 | 20 | 0.47 | 0.40 | 0.39 | 0.70 | 0.08 | 4.99 | 0.12 |
0.17 | 5 | 61 | 18 | 16 | 1.06 | 0.89 | 0.37 | 0.47 | 0.13 | 4.03 | 0.28 |
0.18 | 12 | 52 | 18 | 18 | 1.66 | 1.15 | 0.40 | 0.39 | 0.16 | 2.88 | 0.22 |
0.20 | 11 | 48 | 21 | 20 | 1.16 | 1.08 | 0.41 | 0.42 | 0.15 | 3.33 | 0.19 |
0.21 | 3 | 55 | 20 | 22 | 0.99 | 0.77 | 0.39 | 0.70 | 0.10 | 4.74 | 0.18 |