Peregovich, Bernhard; Thiede, Jörn (2006): Age model, sedimentation and accumulation rate of sediment core IK9373-10 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.407274
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Related to:
Peregovich, Bernhard (1999): Die postglaziale Sedimentationsgeschichte der Laptewsee: schwermineralogische und sedimentpetrographische Untersuchungen (Postglacial Depositional History of the Laptev Sea: Mineralogy and Sedimentology). Berichte zur Polarforschung = Reports on Polar Research, 316, 85 pp, https://doi.org/10.2312/BzP_0316_1999
Project(s):
Funding:
Fourth Framework Programme (FP4), grant/award no. MAS3980185: Quaternary Environment of the Eurasian North
Coverage:
Latitude: 75.346667 * Longitude: 135.205000
Date/Time Start: 1993-09-09T00:00:00 * Date/Time End: 1993-09-09T00:00:00
Minimum DEPTH, sediment/rock: 0.000 m * Maximum DEPTH, sediment/rock: 1.090 m
Event(s):
IK9373-10 * Latitude: 75.346667 * Longitude: 135.205000 * Date/Time: 1993-09-09T00:00:00 * Elevation: -47.0 m * Recovery: 1.09 m * Location: Laptev Sea * Campaign: Transdrift-I * Basis: Ivan Kireyev * Method/Device: Kasten corer RUS (KAL_R)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Sedimentation rate | SR | cm/ka | Thiede, Jörn | Calculated | |
| 3 | Accumulation rate, mass | MAR | g/cm2/ka | Thiede, Jörn | Calculated |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
48 data points
Data
| 1 Depth sed [m] | 2 SR [cm/ka] | 3 MAR [g/cm2/ka] |
|---|---|---|
| 0.000 | 0.00 | 0.00 |
| 0.110 | 77.75 | 75.41 |
| 0.150 | 77.75 | 76.13 |
| 0.200 | 77.75 | 76.83 |
| 0.250 | 77.75 | 76.05 |
| 0.300 | 77.75 | 76.05 |
| 0.330 | 77.75 | |
| 0.350 | 77.78 | 75.06 |
| 0.400 | 77.78 | 68.88 |
| 0.450 | 77.78 | 71.31 |
| 0.500 | 77.78 | 75.92 |
| 0.540 | 77.78 | |
| 0.550 | 75.00 | 71.78 |
| 0.600 | 75.00 | 71.17 |
| 0.620 | 75.00 | |
| 0.650 | 70.31 | 68.27 |
| 0.700 | 70.31 | 67.15 |
| 0.760 | 70.31 | 67.78 |
| 0.800 | 60.54 | 56.16 |
| 0.850 | 60.54 | 58.90 |
| 0.900 | 60.54 | |
| 0.900 | 53.85 | 54.24 |
| 0.950 | 53.85 | 51.91 |
| 1.000 | 53.85 | 52.18 |
| 1.050 | 53.89 | 53.86 |
| 1.090 | 53.89 | 51.41 |