Vogt, Christoph (2004): Clay mineralogy of sediment core PS2198-4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.137767, 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: 85.564700 * Longitude: -9.057500
Date/Time Start: 1991-09-15T00:00:00 * Date/Time End: 1991-09-15T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 0.10 m
Event(s):
PS2198-4 (PS19/214) * Latitude: 85.564700 * Longitude: -9.057500 * Date/Time: 1991-09-15T00:00:00 * Elevation: -3820.0 m * Penetration: 0.3 m * Recovery: 0.3 m * Location: Morris Jesup Rise * Campaign: ARK-VIII/3 (PS19 ARCTIC91) * Basis: Polarstern * Method/Device: MultiCorer (MUC)
Parameter(s):
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
77 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 | 9 | 49 | 16 | 25 | 1.32 | 1.00 | 0.30 | 0.60 | 0.17 | 5.95 | 0.31 |
0.01 | 11 | 54 | 15 | 20 | 1.16 | 1.13 | 0.31 | 0.49 | 0.20 | 7.10 | 0.42 |
0.04 | 12 | 41 | 26 | 22 | 1.32 | 1.24 | 0.30 | 0.59 | 0.11 | 6.72 | 0.26 |
0.04 | 14 | 36 | 28 | 22 | 1.35 | 1.38 | 0.32 | 0.61 | 0.08 | 6.98 | 0.15 |
0.07 | 17 | 37 | 26 | 21 | 1.54 | 1.45 | 0.33 | 0.57 | 0.22 | 7.30 | 0.33 |
0.07 | 19 | 33 | 27 | 21 | 1.59 | 1.65 | 0.32 | 0.68 | 0.07 | 8.19 | 0.13 |
0.10 | 23 | 32 | 25 | 20 | 1.56 | 1.61 | 0.32 | 0.56 | 0.13 | 7.04 | 0.19 |