Stock, Oliver; Melles, Martin (2006): Susceptibility of sediment core PG1129-1 from Lake Pjassino [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.399042
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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: 70.036660 * Longitude: 87.848330
Minimum DEPTH, sediment/rock: 0.010 m * Maximum DEPTH, sediment/rock: 0.330 m
Event(s):
PG1129-1 * Latitude: 70.036660 * Longitude: 87.848330 * Lake water depth: 8.5 m * Penetration: 0.45 m * Recovery: 0.45 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:
65 data points
Data
1 Depth sed [m] | 2 kappa [10-6 SI] |
---|---|
0.010 | 2720.00 |
0.015 | 3060.00 |
0.020 | 3560.00 |
0.025 | 3860.00 |
0.030 | 3940.00 |
0.035 | 4100.00 |
0.040 | 3860.00 |
0.045 | 3880.00 |
0.050 | 3880.00 |
0.055 | 3918.04 |
0.060 | 3855.62 |
0.065 | 3954.51 |
0.070 | 4053.12 |
0.075 | 3991.89 |
0.080 | 3910.73 |
0.085 | 3909.65 |
0.090 | 3888.62 |
0.095 | 3907.49 |
0.100 | 3846.47 |
0.105 | 3825.34 |
0.110 | 3763.98 |
0.115 | 3842.68 |
0.120 | 3881.53 |
0.125 | 3820.00 |
0.130 | 3900.00 |
0.135 | 3820.00 |
0.140 | 3820.00 |
0.145 | 3860.00 |
0.150 | 3800.00 |
0.155 | 3880.00 |
0.160 | 3940.00 |
0.165 | 3840.00 |
0.170 | 3920.00 |
0.175 | 3900.00 |
0.180 | 3980.00 |
0.185 | 4000.00 |
0.190 | 4080.00 |
0.195 | 3960.00 |
0.200 | 4080.00 |
0.205 | 4040.00 |
0.210 | 4120.00 |
0.215 | 4140.00 |
0.220 | 4180.00 |
0.225 | 4118.25 |
0.230 | 4076.89 |
0.235 | 4035.55 |
0.240 | 4094.45 |
0.245 | 3973.47 |
0.250 | 4032.37 |
0.255 | 4031.23 |
0.260 | 4170.10 |
0.265 | 4108.95 |
0.270 | 3946.88 |
0.275 | 3765.75 |
0.280 | 3744.54 |
0.285 | 3783.19 |
0.290 | 3942.08 |
0.295 | 4001.11 |
0.300 | 4065.67 |
0.305 | 4109.92 |
0.310 | 4013.55 |
0.315 | 3878.37 |
0.320 | 3862.34 |
0.325 | 3826.59 |
0.330 | 3874.71 |