Lackschewitz, Klas Sven (2009): Stable isotope analysis on planktic foraminifera on sediment core POS158/1_0020/2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.712822
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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: 67.997000 * Longitude: -18.532000
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: 2.71 m
Event(s):
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:
56 data points
Data
| 1 Depth sed [m] | 2 N. pachyderma s δ18O [‰ PDB] | 3 N. pachyderma s δ13C [‰ PDB] |
|---|---|---|
| 0.01 | 4.18 | 0.35 |
| 0.11 | 3.40 | -0.34 |
| 0.21 | 2.94 | -0.06 |
| 0.31 | 3.03 | -0.05 |
| 0.41 | 2.83 | -0.09 |
| 0.51 | 2.64 | -0.17 |
| 0.61 | 2.65 | -0.15 |
| 0.71 | 2.40 | -0.18 |
| 0.81 | 2.29 | -0.16 |
| 0.91 | 2.46 | -0.18 |
| 1.01 | 2.53 | -0.13 |
| 1.11 | 2.64 | -0.12 |
| 1.21 | 3.50 | 0.00 |
| 1.29 | 4.30 | 0.14 |
| 1.41 | 4.61 | -0.02 |
| 1.51 | 4.63 | 0.10 |
| 1.61 | 4.47 | 0.09 |
| 1.71 | 4.50 | -0.04 |
| 1.81 | 4.25 | 0.08 |
| 1.91 | 4.53 | 0.01 |
| 2.01 | 4.44 | -0.02 |
| 2.11 | 4.51 | -0.02 |
| 2.21 | 4.45 | -0.01 |
| 2.31 | 4.50 | -0.11 |
| 2.41 | 4.32 | 0.04 |
| 2.51 | 4.42 | 0.07 |
| 2.61 | 4.36 | -0.03 |
| 2.71 | 4.33 | 0.08 |