Vogt, Christoph (2004): Mineralogy of sediment core PS2174-4 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.138267, 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
Always quote citation above when using data! You can download the citation in several formats below.
Project(s):
Funding:
Fourth Framework Programme (FP4), grant/award no. MAS3980185: Quaternary Environment of the Eurasian North
Coverage:
Latitude: 87.494700 * Longitude: 90.500200
Date/Time Start: 1991-08-22T00:00:00 * Date/Time End: 1991-08-22T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 0.47 m
Event(s):
PS2174-4 (PS19/171) * Latitude: 87.494700 * Longitude: 90.500200 * Date/Time: 1991-08-22T00:00:00 * Elevation: -4427.0 m * Penetration: 0.43 m * Recovery: 0.48 m * Location: Amundsen Basin * Campaign: ARK-VIII/3 (PS19 ARCTIC91) * Basis: Polarstern * Method/Device: Giant box corer (GKG)
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 | Dolomite | Dol | % | Vogt, Christoph | X-ray diffraction (XRD) | |
| 6 | Calcium carbonate | CaCO3 | % | Vogt, Christoph | X-ray diffraction (XRD) |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
235 data points
Data
| 1 Depth sed [m] | 2 Qz [%] | 3 Qz/Fsp | 4 Pl [%] | 5 Dol [%] | 6 CaCO3 [%] |
|---|---|---|---|---|---|
| 0.00 | 26.7 | 0.43 | 40.0 | 0.55 | 2.5 |
| 0.01 | 26.7 | 0.38 | 36.6 | 0.25 | 0.8 |
| 0.02 | 28.3 | 0.35 | 35.2 | 0.53 | 0.0 |
| 0.04 | 28.5 | 0.33 | 26.9 | 0.40 | 0.0 |
| 0.05 | 27.5 | 0.31 | 28.5 | 0.76 | 0.0 |
| 0.06 | 27.8 | 0.30 | 30.1 | 0.51 | 0.0 |
| 0.07 | 25.8 | 0.30 | 21.1 | 0.43 | 0.0 |
| 0.08 | 28.7 | 0.32 | 40.1 | 0.76 | 0.2 |
| 0.09 | 29.8 | 0.36 | 29.0 | 0.61 | 0.0 |
| 0.10 | 27.8 | 0.38 | 25.4 | 0.00 | 0.0 |
| 0.11 | 24.8 | 0.37 | 41.1 | 0.69 | 0.0 |
| 0.12 | 27.5 | 0.38 | 25.6 | 1.58 | 0.0 |
| 0.13 | 26.9 | 0.34 | 30.8 | 1.59 | 0.0 |
| 0.14 | 19.6 | 0.29 | 28.6 | 0.58 | 0.0 |
| 0.15 | 27.6 | 0.40 | 29.2 | 0.95 | 0.0 |
| 0.16 | 22.1 | 0.38 | 20.6 | 1.71 | 0.0 |
| 0.17 | 24.9 | 0.37 | 33.8 | 0.78 | 0.0 |
| 0.18 | 23.4 | 0.43 | 33.1 | 0.82 | 0.0 |
| 0.19 | 23.0 | 0.40 | 29.1 | 0.87 | 0.0 |
| 0.20 | 23.0 | 0.41 | 23.6 | 1.29 | 0.0 |
| 0.21 | 20.4 | 0.33 | 27.0 | 0.30 | 0.0 |
| 0.22 | 17.9 | 0.37 | 31.3 | 0.30 | 0.0 |
| 0.23 | 20.0 | 0.38 | 26.7 | 0.27 | 0.0 |
| 0.24 | 19.3 | 0.34 | 32.1 | 0.00 | 0.0 |
| 0.25 | 21.7 | 0.25 | 0.0 | 0.00 | 0.0 |
| 0.26 | 20.1 | 0.30 | 31.1 | 0.00 | 0.0 |
| 0.27 | 21.1 | 0.29 | 26.5 | 0.00 | 0.0 |
| 0.28 | 18.6 | 0.30 | 33.4 | 0.23 | 0.0 |
| 0.29 | 19.2 | 0.32 | 38.9 | 0.00 | 0.0 |
| 0.30 | 18.2 | 0.33 | 20.4 | 0.00 | 0.0 |
| 0.31 | 19.8 | 0.36 | 27.4 | 0.00 | 0.0 |
| 0.32 | 16.9 | 0.29 | 30.9 | 0.00 | 0.0 |
| 0.33 | 19.2 | 0.27 | 28.5 | 0.00 | 0.0 |
| 0.34 | 17.6 | 0.34 | 17.5 | 0.24 | 0.0 |
| 0.35 | 18.6 | 0.41 | 20.6 | 0.63 | 0.0 |
| 0.36 | 19.9 | 0.32 | 21.4 | 0.00 | 0.0 |
| 0.37 | 20.0 | 0.28 | 27.6 | 0.00 | 0.0 |
| 0.38 | 18.3 | 0.34 | 23.7 | 0.00 | 0.0 |
| 0.39 | 17.5 | 0.34 | 20.8 | 0.00 | 0.0 |
| 0.40 | 19.8 | 0.31 | 20.9 | 0.28 | 0.0 |
| 0.41 | 20.3 | 0.34 | 21.4 | 0.00 | 0.0 |
| 0.42 | 17.8 | 0.32 | 22.9 | 0.00 | 0.0 |
| 0.43 | 18.5 | 0.29 | 27.0 | 0.00 | 0.0 |
| 0.44 | 18.6 | 0.30 | 30.5 | 0.00 | 0.0 |
| 0.45 | 16.0 | 0.36 | 17.2 | 0.00 | 0.0 |
| 0.46 | 19.3 | 0.32 | 27.8 | 0.59 | 0.0 |
| 0.47 | 19.8 | 0.28 | 28.5 | 0.00 | 0.0 |