Vogt, Christoph (2004): Mineralogy of sediment core PS2200-4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.138262, 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: 85.327700 * Longitude: -14.022000
Date/Time Start: 1991-09-16T00:00:00 * Date/Time End: 1991-09-16T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 0.19 m
Event(s):
PS2200-4 (PS19/218) * Latitude: 85.327700 * Longitude: -14.022000 * Date/Time: 1991-09-16T00:00:00 * Elevation: -1073.0 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:
84 data points
Data
1 Depth sed [m] | 2 Qz [%] | 3 Qz/Fsp | 4 Pl [%] | 5 Pl/std | 6 Dol [%] | 7 CaCO3 [%] |
---|---|---|---|---|---|---|
0.01 | 18.5 | 0.25 | 16.5 | 2.07 | 3.42 | 17.9 |
0.02 | 22.0 | 0.36 | 10.5 | 2.03 | 2.89 | 17.0 |
0.03 | 19.6 | 0.29 | 7.3 | 1.73 | 5.07 | 19.8 |
0.04 | 18.1 | 0.24 | 17.8 | 1.86 | 4.10 | 23.2 |
0.05 | 18.3 | 0.37 | 15.7 | 1.66 | 3.19 | 24.5 |
0.07 | 25.2 | 0.27 | 7.8 | 2.14 | 4.76 | 27.8 |
0.09 | 32.1 | 0.34 | 10.1 | 2.45 | 3.40 | 11.5 |
0.10 | 33.2 | 0.35 | 8.6 | 2.80 | 6.64 | 6.8 |
0.11 | 40.4 | 0.35 | 7.4 | 3.09 | 5.12 | 3.8 |
0.12 | 35.2 | 0.39 | 11.7 | 2.41 | 3.99 | 3.1 |
0.14 | 32.3 | 0.30 | 7.0 | 2.74 | 1.98 | 0.9 |
0.16 | 31.2 | 0.31 | 12.4 | 2.61 | 1.25 | 0.0 |
0.17 | 38.2 | 0.39 | 16.4 | 3.35 | 0.88 | 0.4 |
0.19 | 45.6 | 0.56 | 12.9 | 2.25 | 0.00 | 0.0 |