Lackschewitz, Klas Sven (2009): Stable isotope analysis on planktic foraminifera on sediment core PS1855-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.712827
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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: 70.600700 * Longitude: -14.609800
Date/Time Start: 1990-06-17T21:45:00 * Date/Time End: 1990-06-17T21:45:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 0.33 m
Event(s):
PS1855-1 (GIK21855-1 PS17/022) * Latitude: 70.600700 * Longitude: -14.609800 * Date/Time: 1990-06-17T21:45:00 * Elevation: -1851.0 m * Penetration: 0.39 m * Recovery: 0.39 m * Location: Kolbeinsey Ridge * Campaign: ARK-VII/1 (PS17) * Basis: Polarstern * 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:
36 data points
Data
| 1 Depth sed [m] | 2 N. pachyderma s δ18O [‰ PDB] | 3 N. pachyderma s δ13C [‰ PDB] |
|---|---|---|
| 0.00 | 3.62 | 0.53 |
| 0.01 | 3.48 | 0.60 |
| 0.03 | 3.78 | 0.55 |
| 0.05 | 3.48 | 0.66 |
| 0.07 | 3.54 | 0.71 |
| 0.09 | 3.50 | 0.76 |
| 0.11 | 3.46 | 0.72 |
| 0.13 | 3.65 | 0.69 |
| 0.15 | 3.54 | 0.84 |
| 0.17 | 3.53 | 0.69 |
| 0.19 | 3.51 | 0.81 |
| 0.21 | 3.53 | 0.87 |
| 0.23 | 3.57 | 0.81 |
| 0.25 | 3.49 | 0.81 |
| 0.27 | 3.65 | 0.85 |
| 0.29 | 3.63 | 0.79 |
| 0.31 | 3.60 | 0.64 |
| 0.33 | 3.63 | 0.76 |