Lackschewitz, Klas Sven (2009): Stable isotope analysis on planktic foraminifera on sediment core PS1845-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.712823
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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: 69.461500 * Longitude: -15.782500
Date/Time Start: 1990-06-15T19:14:00 * Date/Time End: 1990-06-15T19:14:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 0.39 m
Event(s):
PS1845-2 (GIK21845-2 PS17/010) * Latitude: 69.461500 * Longitude: -15.782500 * Date/Time: 1990-06-15T19:14:00 * Elevation: -1749.0 m * Penetration: 0.4 m * Recovery: 0.4 m * Location: Kolbeinsey Ridge * Campaign: ARK-VII/1 (PS17) * Basis: Polarstern * Method/Device: Giant box corer (GKG) * Comment: 1 section 0-39
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] |
---|---|---|
0.00 | 3.37 | 0.53 |
0.01 | 3.34 | 0.60 |
0.03 | 3.31 | 0.51 |
0.05 | 3.46 | 0.46 |
0.07 | 3.55 | 0.47 |
0.09 | 3.27 | 0.47 |
0.11 | 3.63 | 0.05 |
0.13 | 3.63 | -0.20 |
0.15 | 3.77 | -0.08 |
0.17 | 3.62 | -0.03 |
0.19 | 4.42 | 0.12 |
0.21 | 4.03 | 0.11 |
0.23 | 4.14 | 0.06 |
0.25 | 4.25 | 0.19 |
0.27 | 4.29 | 0.01 |
0.29 | 4.40 | 0.14 |
0.31 | 3.85 | 0.06 |
0.33 | 4.12 | -0.02 |
0.35 | 4.14 | -0.02 |
0.37 | 3.82 | 0.08 |
0.39 | 4.10 | 0.15 |