Stock, Oliver; Melles, Martin (2006): Susceptibility of sediment core PG1125-1 from Lake Pjassino [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.399038
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Related to:
Stock, Oliver (1997): Rekonstruktion der holozänen Entwicklungsgeschichte des Pjassinosees mit Hilfe von Seesedimenten. Diploma Thesis, University Potsdam, 67 pp
Project(s):
Funding:
Fourth Framework Programme (FP4), grant/award no. MAS3980185: Quaternary Environment of the Eurasian North
Coverage:
Latitude: 70.028330 * Longitude: 87.948330
Minimum DEPTH, sediment/rock: 0.010 m * Maximum DEPTH, sediment/rock: 0.240 m
Event(s):
PG1125-1 * Latitude: 70.028330 * Longitude: 87.948330 * Lake water depth: 7.5 m * Penetration: 0.35 m * Recovery: 0.35 m * Campaign: RU-Land_1993_Norilsk_Taymyr (Norilsk/Taymyr93) * Basis: AWI Arctic Land Expedition * Method/Device: Gravity corer Potsdam (SL_P)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Magnetic susceptibility, volume | kappa | 10-6 SI | Melles, Martin | Bartington MS2C coil sensor |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
47 data points
Data
| 1 Depth sed [m] | 2 kappa [10-6 SI] |
|---|---|
| 0.010 | 2560.0 |
| 0.015 | 2980.0 |
| 0.020 | 3320.0 |
| 0.025 | 3640.0 |
| 0.030 | 3900.0 |
| 0.035 | 3840.0 |
| 0.040 | 3860.0 |
| 0.045 | 4120.0 |
| 0.050 | 4020.0 |
| 0.055 | 3880.0 |
| 0.060 | 3718.1 |
| 0.065 | 3776.7 |
| 0.070 | 3755.2 |
| 0.075 | 3733.8 |
| 0.080 | 3752.6 |
| 0.085 | 3751.2 |
| 0.090 | 3709.0 |
| 0.095 | 3687.7 |
| 0.100 | 3726.4 |
| 0.105 | 3805.1 |
| 0.110 | 3843.8 |
| 0.115 | 3922.5 |
| 0.120 | 3941.2 |
| 0.125 | 3662.9 |
| 0.130 | 3884.7 |
| 0.135 | 3927.2 |
| 0.140 | 3869.0 |
| 0.145 | 3911.1 |
| 0.150 | 3933.5 |
| 0.155 | 3955.4 |
| 0.160 | 3977.0 |
| 0.165 | 4019.0 |
| 0.170 | 3861.1 |
| 0.175 | 3644.4 |
| 0.180 | 3508.0 |
| 0.185 | 3170.1 |
| 0.190 | 3051.7 |
| 0.195 | 2954.1 |
| 0.200 | 2976.3 |
| 0.205 | 2998.3 |
| 0.210 | 2931.0 |
| 0.215 | 2923.4 |
| 0.220 | 2935.9 |
| 0.225 | 2906.7 |
| 0.230 | 2898.9 |
| 0.235 | 2752.1 |
| 0.240 | 2625.9 |