Vogt, Christoph (2004): Mineralogy of sediment core PS2202-4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.138273, 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: 85.108500 * Longitude: -14.368700
Date/Time Start: 1991-09-18T00:00:00 * Date/Time End: 1991-09-18T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 0.19 m
Event(s):
PS2202-4 (PS19/222) * Latitude: 85.108500 * Longitude: -14.368700 * Date/Time: 1991-09-18T00:00:00 * Elevation: -1081.0 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):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Quartz | Qz | % | Vogt, Christoph | X-ray diffraction (XRD) | |
3 | Quartz/Feldspar ratio | Qz/Fsp | Vogt, Christoph | X-ray diffraction (XRD) | ||
4 | Plagioclase | Pl | % | Vogt, Christoph | X-ray diffraction (XRD) | |
5 | Plagioclase/standard ratio | Pl/std | Vogt, Christoph | X-ray diffraction (XRD) | ||
6 | Dolomite | Dol | % | Vogt, Christoph | X-ray diffraction (XRD) | |
7 | Calcium carbonate | CaCO3 | % | Vogt, Christoph | X-ray diffraction (XRD) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
66 data points
Data
1 Depth sed [m] | 2 Qz [%] | 3 Qz/Fsp | 4 Pl [%] | 5 Pl/std | 6 Dol [%] | 7 CaCO3 [%] |
---|---|---|---|---|---|---|
0.01 | 15.7 | 0.18 | 8.8 | 1.89 | 4.30 | 19.4 |
0.02 | 21.4 | 0.24 | 10.0 | 1.96 | 8.49 | 17.4 |
0.04 | 18.8 | 0.24 | 9.0 | 1.79 | 6.37 | 30.1 |
0.06 | 19.4 | 0.28 | 9.8 | 2.02 | 12.36 | 22.6 |
0.08 | 34.1 | 0.43 | 11.7 | 2.45 | 7.52 | 7.7 |
0.09 | 29.5 | 0.37 | 6.5 | 2.21 | 6.52 | 8.2 |
0.11 | 36.2 | 0.38 | 15.3 | 2.65 | 2.90 | 3.8 |
0.13 | 34.7 | 0.35 | 15.0 | 2.54 | 0.00 | 0.0 |
0.15 | 47.1 | 0.35 | 13.3 | 3.59 | 0.10 | 0.1 |
0.17 | 29.5 | 0.27 | 10.2 | 2.71 | 0.00 | 0.0 |
0.19 | 38.2 | 0.30 | 12.7 | 3.74 | 0.00 | 0.0 |