Lackschewitz, Klas Sven (2000): Stable isotope analysis on planktic foraminifera on sediment core POS158/1_0003/1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.57336
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Related to:
Lackschewitz, Klas Sven (1991): Sedimentationsprozesse am aktiven mittelozeanischen Kolbeinsey Rücken (nördlich von Island). GEOMAR Report, GEOMAR Research Center for Marine Geosciences, Christian Albrechts University in Kiel, 9, 133 pp
Project(s):
Funding:
Fourth Framework Programme (FP4), grant/award no. MAS3980185: Quaternary Environment of the Eurasian North
Coverage:
Latitude: 69.032000 * Longitude: -18.362000
Date/Time Start: 1989-01-01T00:00:00 * Date/Time End: 1989-01-01T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 0.41 m
Event(s):
POS158/1_0003/1 (414) * Latitude: 69.032000 * Longitude: -18.362000 * Date/Time: 1989-01-01T00:00:00 * Elevation: -1250.0 m * Recovery: 0.4 m * Campaign: POS158/1 (PO158/A) * Basis: Poseidon * Method/Device: Giant box corer (GKG)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Neogloboquadrina pachyderma sinistral, δ18O | N. pachyderma s δ18O | ‰ PDB | Lackschewitz, Klas Sven | Mass spectrometer Finnigan MAT 251 | |
| 3 | Neogloboquadrina pachyderma sinistral, δ13C | N. pachyderma s δ13C | ‰ PDB | Lackschewitz, Klas Sven | Mass spectrometer Finnigan MAT 251 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
42 data points
Data
| 1 Depth sed [m] | 2 N. pachyderma s δ18O [‰ PDB] | 3 N. pachyderma s δ13C [‰ PDB] |
|---|---|---|
| 0.01 | 3.50 | 0.64 |
| 0.03 | 3.32 | 0.58 |
| 0.05 | 3.45 | 0.57 |
| 0.07 | 3.40 | 0.64 |
| 0.09 | 3.54 | 0.32 |
| 0.11 | 3.54 | -0.01 |
| 0.13 | 3.60 | 0.04 |
| 0.15 | 3.77 | 0.07 |
| 0.17 | 3.57 | -0.11 |
| 0.19 | 3.99 | 0.14 |
| 0.21 | 3.91 | 0.11 |
| 0.23 | 4.23 | 0.19 |
| 0.25 | 3.98 | 0.04 |
| 0.27 | 3.96 | 0.08 |
| 0.29 | 3.91 | 0.25 |
| 0.31 | 3.62 | 0.18 |
| 0.33 | 3.69 | 0.10 |
| 0.35 | 3.81 | 0.19 |
| 0.37 | 3.94 | 0.19 |
| 0.39 | 3.93 | 0.29 |
| 0.41 | 3.70 | 0.66 |