Vorren, Tore O; Hald, Morten (1987): (Table 2) Stable isotope ratios of foraminifera from sediment core NOR9-2 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.52311, In supplement to: Hald, Morten; Vorren, Tore O (1987): Stable isotope stratigraphy and paleoceanography during the last deglaciation on the continental shelf off Troms, Northern Norway. Paleoceanography, 2(6), 583-599, https://doi.org/10.1029/PA002i006p00583
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Project(s):
Funding:
Fourth Framework Programme (FP4), grant/award no. MAS3980185: Quaternary Environment of the Eurasian North
Coverage:
Latitude: 69.550000 * Longitude: 16.166667
Minimum DEPTH, sediment/rock: 0.220 m * Maximum DEPTH, sediment/rock: 2.790 m
Event(s):
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
2 | Depth, top/min | Depth top | m | Hald, Morten | ||
3 | Depth, bottom/max | Depth bot | m | Hald, Morten | ||
4 | Cassidulina reniforme, δ13C | C. reniforme δ13C | ‰ PDB | Hald, Morten | Mass spectrometer Finnigan MAT 251 | |
5 | Cassidulina reniforme, δ18O | C. reniforme δ18O | ‰ PDB | Hald, Morten | Mass spectrometer Finnigan MAT 251 | |
6 | Neogloboquadrina pachyderma sinistral, δ13C | N. pachyderma s δ13C | ‰ PDB | Hald, Morten | Mass spectrometer Finnigan MAT 251 | |
7 | Neogloboquadrina pachyderma sinistral, δ18O | N. pachyderma s δ18O | ‰ PDB | Hald, Morten | Mass spectrometer Finnigan MAT 251 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
30 data points
Data
1 Depth sed [m] | 2 Depth top [m] | 3 Depth bot [m] | 4 C. reniforme δ13C [‰ PDB] | 5 C. reniforme δ18O [‰ PDB] | 6 N. pachyderma s δ13C [‰ PDB] | 7 N. pachyderma s δ18O [‰ PDB] |
---|---|---|---|---|---|---|
0.220 | 0.21 | 0.23 | -0.92 | 3.18 | -0.66 | 2.76 |
0.485 | 0.47 | 0.50 | -1.01 | 3.38 | -0.53 | 2.82 |
0.685 | 0.67 | 0.70 | -1.27 | 3.17 | -0.68 | 2.52 |
0.870 | 0.85 | 0.89 | -1.81 | 3.04 | ||
1.330 | 1.31 | 1.35 | -1.28 | 3.56 | ||
2.790 | 2.00 | 3.58 | -1.34 | 3.27 |