Opitz, Stephan; Wünnemann, Bernd; Aichner, Bernhard; Dietze, Elisabeth; Hartmann, Kai; Herzschuh, Ulrike; IJmker, Janneke; Lehmkuhl, Frank; Li, Shijie; Mischke, Steffen; Plotzki, Anna; Stauch, Georg; Diekmann, Bernhard (2012): Sand content of sediment core PG1904 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.787753, In supplement to: Opitz, S et al. (2012): Late Glacial and Holocene development of Lake Donggi Cona, north-eastern Tibetan Plateau, inferred from sedimentological analysis. Palaeogeography, Palaeoclimatology, Palaeoecology, 337-338, 159-176, https://doi.org/10.1016/j.palaeo.2012.04.013
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Project(s):
Permafrost Research (Periglacial Dynamics) @ AWI (AWI_PerDyn)
Coverage:
Latitude: 35.333630 * Longitude: 98.482390
Date/Time Start: 2008-03-12T00:00:00 * Date/Time End: 2008-03-12T00:00:00
Minimum DEPTH, sediment/rock: 0.030 m * Maximum DEPTH, sediment/rock: 4.350 m
Event(s):
PG1904 * Latitude: 35.333630 * Longitude: 98.482390 * Date/Time: 2008-03-12T00:00:00 * Elevation: 4095.0 m * Lake water depth: 39 m * Recovery: 4.46 m * Location: Lake Donggi Cona, Qinghai, China * Campaign: CN-Land_2008 (China2008) * Basis: AWI Arctic Land Expedition * Method/Device: Composite Core (COMPCORE)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Sand | Sand | % | Diekmann, Bernhard | Grain size, sieving/settling tube |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
40 data points
Data
| 1 Depth sed [m] | 2 Sand [%] |
|---|---|
| 0.030 | 4.1 |
| 0.130 | 1.9 |
| 0.230 | 2.2 |
| 0.330 | 3.2 |
| 0.430 | 2.3 |
| 0.540 | 1.3 |
| 0.640 | 0.8 |
| 0.740 | 2.3 |
| 0.840 | 2.1 |
| 0.940 | 1.5 |
| 1.030 | 1.4 |
| 1.470 | 4.3 |
| 1.580 | 3.9 |
| 1.680 | 3.7 |
| 1.780 | 4.3 |
| 1.880 | 4.8 |
| 1.980 | 5.2 |
| 2.080 | 5.9 |
| 2.180 | 2.7 |
| 2.280 | 3.3 |
| 2.490 | 3.7 |
| 2.590 | 2.9 |
| 2.690 | 2.9 |
| 2.790 | 4.9 |
| 2.890 | 2.0 |
| 2.990 | 1.1 |
| 3.090 | 2.4 |
| 3.200 | 2.8 |
| 3.290 | 2.6 |
| 3.390 | 2.5 |
| 3.450 | 2.9 |
| 3.550 | 4.5 |
| 3.650 | 5.0 |
| 3.750 | 4.7 |
| 3.850 | 5.6 |
| 3.950 | 14.2 |
| 4.050 | 17.1 |
| 4.150 | 10.7 |
| 4.240 | 12.0 |
| 4.350 | 12.7 |