Nam, Seung-Il (2003): Age model of sediment core PS1730-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.129516, In supplement to: Nam, S-I (1997): Late Quaternary glacial history and paleoceanographic reconstructions along the East Greenland continental margin: Evidence from high-resolution records of stable isotopes and ice-rafted debris (Spätquartäre Vereisungsgeschichte und paläozeanographische Rekonstruktionen am ostgrönlandischen Kontinentalrand). Berichte zur Polarforschung = Reports on Polar Research, 241, 257 pp, https://doi.org/10.2312/BzP_0241_1997
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Project(s):
Funding:
Fourth Framework Programme (FP4), grant/award no. MAS3980185: Quaternary Environment of the Eurasian North
Coverage:
Latitude: 70.116500 * Longitude: -17.694300
Date/Time Start: 1988-08-18T00:00:00 * Date/Time End: 1988-08-18T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 7.76 m
Event(s):
PS1730-2 (GIK21730-2 PS13/224) * Latitude: 70.116500 * Longitude: -17.694300 * Date/Time: 1988-08-18T00:00:00 * Elevation: -1622.0 m * Penetration: 13 m * Recovery: 7.79 m * Location: Greenland Sea * Campaign: ARK-V/3b (PS13 GRÖKORT) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 5 core sections: 2.82-3.82, 3.82-4.82, 4.82-5.86, 5.86-6.86, 6.86-7.79 m
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Age model | Age model | ka | Nam, Seung-Il |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
27 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.01 | 4.41 |
| 0.20 | 7.91 |
| 0.35 | 10.60 |
| 0.70 | 14.32 |
| 0.80 | 16.27 |
| 0.90 | 18.60 |
| 1.40 | 23.00 |
| 1.60 | 24.90 |
| 2.00 | 27.95 |
| 4.00 | 55.45 |
| 4.25 | 58.96 |
| 4.40 | 65.22 |
| 4.60 | 73.91 |
| 4.70 | 79.25 |
| 5.10 | 103.29 |
| 5.50 | 125.19 |
| 5.60 | 129.84 |
| 5.90 | 135.10 |
| 6.10 | 142.28 |
| 6.20 | 152.58 |
| 6.40 | 175.05 |
| 6.70 | 183.30 |
| 6.98 | 189.61 |
| 7.20 | 193.07 |
| 7.40 | 200.57 |
| 7.60 | 215.54 |
| 7.76 | 224.89 |