Nowaczyk, Norbert R; Antonow, Martin (1997): (Table 3) Age model of sediment core PS1882-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.351556, In supplement to: Nowaczyk, NR; Antonow, M (1997): High-resolution magnetostratigraphy of four sediment cores from the Greenland Sea - I. Identification of the Mono Lake excursion, Laschamp and Biwa I/Jamaica geomagnetic polarity events. Geophysical Journal International, 131(2), 310-324, https://doi.org/10.1111/j.1365-246X.1997.tb01224.x
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Project(s):
Coverage:
Latitude: 73.593200 * Longitude: -8.371300
Date/Time Start: 1990-06-25T12:51:00 * Date/Time End: 1990-06-25T12:51:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 6.30 m
Event(s):
PS1882-2 (GIK21882-2 PS17/056) * Latitude: 73.593200 * Longitude: -8.371300 * Date/Time: 1990-06-25T12:51:00 * Elevation: -3173.0 m * Penetration: 7.55 m * Recovery: 6.5 m * Location: Vesteris Banken * Campaign: ARK-VII/1 (PS17) * Basis: Polarstern * Method/Device: Kasten corer (KAL)
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 | Nowaczyk, Norbert R | Age model, composite | from AMS-14C, stable isotope stratigratigraphy and biostratigraphy |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
38 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] |
|---|---|
| 0.00 | 0.0 |
| 0.07 | 6.5 |
| 0.21 | 9.0 |
| 0.35 | 12.5 |
| 0.45 | 15.0 |
| 0.52 | 17.0 |
| 0.65 | 17.5 |
| 0.75 | 18.2 |
| 0.93 | 21.5 |
| 0.98 | 22.5 |
| 1.04 | 23.4 |
| 1.10 | 24.1 |
| 1.45 | 27.0 |
| 1.55 | 28.0 |
| 1.60 | 28.1 |
| 1.63 | 28.8 |
| 1.68 | 29.5 |
| 1.72 | 30.0 |
| 1.78 | 30.8 |
| 1.82 | 32.5 |
| 1.98 | 35.0 |
| 2.09 | 36.5 |
| 2.15 | 37.5 |
| 2.32 | 38.4 |
| 2.42 | 39.7 |
| 2.55 | 42.8 |
| 2.60 | 43.8 |
| 2.70 | 45.0 |
| 3.55 | 59.0 |
| 3.75 | 68.0 |
| 4.00 | 73.9 |
| 4.10 | 79.2 |
| 4.35 | 91.0 |
| 4.65 | 99.4 |
| 5.70 | 129.8 |
| 5.90 | 135.1 |
| 6.07 | 139.0 |
| 6.30 | 152.6 |