Vogt, Christoph (2004): Clay mineralogy of sediment core PS2204-3 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.137774, 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: 85.054700 * Longitude: -13.021700
Date/Time Start: 1991-09-20T00:00:00 * Date/Time End: 1991-09-20T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 0.17 m
Event(s):
PS2204-3 (PS19/224) * Latitude: 85.054700 * Longitude: -13.021700 * Date/Time: 1991-09-20T00:00:00 * Elevation: -3899.0 m * Penetration: 0.35 m * Recovery: 0.35 m * Location: Morris Jesup Rise * 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:
132 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 | 8 | 61 | 10 | 21 | 0.75 | 0.79 | 0.29 | 0.50 | 0.24 | 7.42 | 0.46 |
0.01 | 15 | 58 | 8 | 19 | 1.25 | 1.32 | 0.28 | 0.47 | 0.23 | 6.53 | 0.43 |
0.03 | 13 | 62 | 6 | 19 | 0.80 | 0.90 | 0.29 | 0.51 | 0.17 | 5.18 | 0.27 |
0.04 | 10 | 60 | 10 | 20 | 1.07 | 1.16 | 0.38 | 0.70 | 0.08 | 4.86 | 0.16 |
0.04 | 11 | 63 | 6 | 19 | 1.28 | 1.20 | 0.28 | 0.50 | 0.24 | 7.36 | 0.43 |
0.07 | 12 | 63 | 7 | 19 | 0.81 | 1.00 | 0.28 | 0.48 | 0.28 | 6.98 | 0.48 |
0.09 | 6 | 57 | 16 | 20 | 1.26 | 1.32 | 0.33 | 0.45 | 0.29 | 8.64 | 0.29 |
0.10 | 2 | 62 | 16 | 21 | 0.47 | 0.67 | 0.33 | 0.51 | 0.27 | 9.73 | 0.21 |
0.12 | 3 | 59 | 17 | 21 | 0.79 | 0.91 | 0.34 | 0.50 | 0.26 | 8.70 | 0.22 |
0.14 | 3 | 58 | 17 | 21 | 0.75 | 0.91 | 0.39 | 0.77 | 0.18 | 8.58 | 0.19 |
0.15 | 1 | 61 | 17 | 21 | 0.64 | 0.45 | 0.35 | 0.62 | 0.25 | 7.62 | 0.32 |
0.17 | 3 | 55 | 19 | 23 | 0.81 | 0.95 | 0.35 | 0.67 | 0.16 | 5.28 | 0.14 |