Wiers, Steffen; Snowball, Ian; O'Regan, Matthew; Almqvist, Bjarne (2019): Stable oxygen isotopes measured on planktonic foraminifera Neogloboquadrina pachyderma of sediment core PS92/045-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.899376, In supplement to: Wiers, S et al. (2019): Late Pleistocene chronology of sediments from the Yermak Plateau and uncertainty in dating based on geomagnetic excursions. Geochemistry, Geophysics, Geosystems, 20(7), 3289-3310, https://doi.org/10.1029/2018GC007920
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Abstract:
Stable oxygen isotopes measured on planktonic foraminifera Neogloboquadrina pachyderma.
Coverage:
Latitude: 81.893330 * Longitude: 9.768830
Date/Time Start: 2015-06-17T14:04:00 * Date/Time End: 2015-06-17T14:04:00
Minimum DEPTH, sediment/rock: 0.03 m * Maximum DEPTH, sediment/rock: 4.74 m
Event(s):
PS92/045-2 * Latitude: 81.893330 * Longitude: 9.768830 * Date/Time: 2015-06-17T14:04:00 * Elevation: -915.2 m * Location: Arctic Ocean * Campaign: PS92 (ARK-XXIX/1, TRANSSIZ) * Basis: Polarstern * Method/Device: Gravity corer (GC)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Wiers, Steffen | Geocode | |
| 2 | Neogloboquadrina pachyderma, δ18O | N. pachyderma δ18O | ‰ PDB | Wiers, Steffen | vs VPDB; norm |
License:
Creative Commons Attribution 4.0 International (CC-BY-4.0)
Size:
37 data points
Data
| 1 Depth sed [m] | 2 N. pachyderma δ18O [‰ PDB] |
|---|---|
| 0.03 | 3.63 |
| 0.07 | 3.56 |
| 1.02 | 3.66 |
| 1.06 | 3.84 |
| 1.18 | 4.61 |
| 1.22 | 4.60 |
| 1.25 | 4.78 |
| 1.29 | 4.68 |
| 1.33 | 4.76 |
| 1.37 | 4.73 |
| 1.41 | 4.62 |
| 1.45 | 4.53 |
| 1.57 | 4.39 |
| 1.61 | 4.31 |
| 1.65 | 4.55 |
| 1.69 | 4.33 |
| 1.73 | 4.12 |
| 1.77 | 4.03 |
| 1.81 | 3.89 |
| 2.82 | 3.96 |
| 2.86 | 4.30 |
| 2.90 | 4.36 |
| 3.10 | 3.67 |
| 3.14 | 3.90 |
| 3.18 | 3.37 |
| 3.65 | 3.58 |
| 4.05 | 3.31 |
| 4.13 | 4.77 |
| 4.17 | 4.71 |
| 4.21 | 3.79 |
| 4.34 | 4.44 |
| 4.38 | 4.47 |
| 4.46 | 4.52 |
| 4.50 | 4.10 |
| 4.58 | 4.33 |
| 4.70 | 4.14 |
| 4.74 | 4.42 |