Evans, Jeff (2000): Stable isotope analysis on sediment core PS2629-4. PANGAEA, https://doi.org/10.1594/PANGAEA.57400
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Related to:
Evans, Jeff (2000): Late Weichselian and Holocene sedimentation in Kejser Franz Josephs Fjord and on the adjacent continental margin, East Greenland. PhD Thesis, Department of Earth Sciences, University of Cambridge, 150 pp
Project(s):
Funding:
Fourth Framework Programme (FP4), grant/award no. MAS3980185: Quaternary Environment of the Eurasian North
Coverage:
Latitude: 73.158330 * Longitude: -16.481660
Date/Time Start: 1994-09-03T16:31:00 * Date/Time End: 1994-09-03T16:31:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 2.00 m
Event(s):
PS2629-4 (PS31/137) * Latitude: 73.158330 * Longitude: -16.481660 * Date/Time: 1994-09-03T16:31:00 * Elevation: -847.0 m * Penetration: 5 m * Recovery: 2.14 m * Location: East Greenland Sea * Campaign: ARK-X/2 (PS31) * Basis: Polarstern * Method/Device: Gravity corer (Kiel type) (SL) * Comment: 2 core sections: 0.14-1.14, 1.14-2.14 m
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Neogloboquadrina pachyderma sinistral, δ13C | N. pachyderma s δ13C | ‰ PDB | Evans, Jeff | Mass spectrometer Finnigan MAT 251 | |
3 | Neogloboquadrina pachyderma sinistral, δ18O | N. pachyderma s δ18O | ‰ PDB | Evans, Jeff | Mass spectrometer Finnigan MAT 251 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
40 data points
Data
1 Depth sed [m] | 2 N. pachyderma s δ13C [‰ PDB] | 3 N. pachyderma s δ18O [‰ PDB] |
---|---|---|
0.01 | 0.289 | 3.097 |
0.10 | -0.154 | 3.473 |
0.30 | 0.017 | 4.434 |
0.40 | 0.062 | 4.398 |
0.50 | 0.059 | 4.422 |
0.60 | 0.118 | 4.454 |
0.70 | 0.010 | 4.410 |
0.80 | 0.117 | 4.540 |
0.90 | 0.053 | 4.169 |
1.00 | -0.074 | 3.856 |
1.10 | 0.019 | 4.171 |
1.20 | -0.115 | 3.415 |
1.30 | -0.044 | 3.777 |
1.40 | -0.017 | 3.748 |
1.50 | 0.000 | 3.903 |
1.60 | -0.232 | 3.819 |
1.70 | 0.088 | 3.597 |
1.80 | -0.108 | 3.699 |
1.90 | 0.113 | 3.281 |
2.00 | -0.100 | 2.949 |