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 PG1900 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.787751, 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: 35.260130 * Longitude: 98.602740
Date/Time Start: 2008-03-08T00:00:00 * Date/Time End: 2008-03-08T00:00:00
Minimum DEPTH, sediment/rock: 0.130 m * Maximum DEPTH, sediment/rock: 4.170 m
Event(s):
PG1900 * Latitude: 35.260130 * Longitude: 98.602740 * Date/Time: 2008-03-08T00:00:00 * Elevation: 4095.0 m * Lake water depth: 37 m * Recovery: 4.23 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 [%] |
|---|---|
| 0.130 | 1.5 |
| 0.230 | 1.3 |
| 0.330 | 3.2 |
| 0.430 | 5.1 |
| 0.520 | 3.4 |
| 0.620 | 0.8 |
| 0.780 | 0.9 |
| 0.880 | 1.5 |
| 0.970 | 0.7 |
| 1.070 | 1.8 |
| 1.170 | 2.3 |
| 1.270 | 1.2 |
| 1.380 | 2.3 |
| 1.480 | 2.1 |
| 1.580 | 4.4 |
| 1.700 | 5.0 |
| 1.800 | 2.4 |
| 1.900 | 4.4 |
| 2.000 | 2.1 |
| 2.100 | 1.2 |
| 2.200 | 1.2 |
| 2.300 | 3.4 |
| 2.400 | 3.0 |
| 2.510 | 1.5 |
| 2.600 | 4.6 |
| 2.700 | 1.1 |
| 2.800 | 1.2 |
| 2.900 | 1.2 |
| 3.050 | 2.7 |
| 3.150 | 2.0 |
| 3.250 | 2.7 |
| 3.350 | 1.8 |
| 3.450 | 4.3 |
| 3.560 | 4.2 |
| 3.660 | 4.5 |
| 3.770 | 5.5 |
| 3.870 | 8.0 |
| 3.970 | 7.9 |
| 4.070 | 13.9 |
| 4.170 | 15.2 |