Vogt, Christoph (2003): Content of kalifeldspar in sediment core PS2445-4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.133426, 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: 82.766667 * Longitude: 40.226667
Date/Time Start: 1993-08-18T00:00:00 * Date/Time End: 1993-08-18T00:00:00
Minimum DEPTH, sediment/rock: 0.20 m * Maximum DEPTH, sediment/rock: 6.35 m
Event(s):
PS2445-4 (PS27/019) * Latitude: 82.766667 * Longitude: 40.226667 * Date/Time: 1993-08-18T00:00:00 * Elevation: -2999.0 m * Penetration: 7.5 m * Recovery: 7.25 m * Location: Barents Sea * Campaign: ARK-IX/4 (PS27) * Basis: Polarstern * Method/Device: Kasten corer (KAL)
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Kalifeldspar | Kfs | % | Vogt, Christoph | X-ray diffraction (XRD) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
46 data points
Data
1 Depth sed [m] | 2 Kfs [%] |
---|---|
0.20 | 0.0 |
0.40 | 0.0 |
0.50 | 0.0 |
0.65 | 14.8 |
0.70 | 7.4 |
0.75 | 6.2 |
0.80 | 6.8 |
0.85 | 0.0 |
0.90 | 7.6 |
0.95 | 0.0 |
1.00 | 5.8 |
1.05 | 0.0 |
1.10 | 10.5 |
1.20 | 6.7 |
1.25 | 0.0 |
1.30 | 25.4 |
1.35 | 9.5 |
1.40 | 8.1 |
1.50 | 0.0 |
1.55 | 0.0 |
1.60 | 12.3 |
1.65 | 0.0 |
1.70 | 0.0 |
1.75 | 5.3 |
1.80 | 0.0 |
1.85 | 7.8 |
1.90 | 7.0 |
2.00 | 55.3 |
2.05 | 73.1 |
2.10 | 0.0 |
2.15 | 24.6 |
2.20 | 0.0 |
2.25 | 8.3 |
2.30 | 0.0 |
2.35 | 11.5 |
2.40 | 13.1 |
2.45 | 0.0 |
2.50 | 0.0 |
2.70 | 0.0 |
3.00 | 0.0 |
3.40 | 9.6 |
3.80 | 10.4 |
4.60 | 8.4 |
5.20 | 0.0 |
5.80 | 0.0 |
6.35 | 11.5 |