Hald, Morten; Vorren, Tore O (1987): (Table 3) Stable isotope ratios of Cassidulina reniforme from sediment core NOR56-1 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.52322, In supplement to: Hald, M; Vorren, TO (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: 69.850000 * Longitude: 17.250000
Minimum DEPTH, sediment/rock: 1.340 m * Maximum DEPTH, sediment/rock: 3.885 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 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
84 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] |
|---|---|---|---|---|
| 1.340 | 1.28 | 1.4 | -0.821 | 3.115 |
| 1.540 | 1.48 | 1.6 | -0.900 | 3.701 |
| 1.740 | 1.68 | 1.8 | -1.218 | 3.498 |
| 1.940 | 1.88 | 2.0 | -1.509 | 3.653 |
| 2.145 | 2.07 | 2.2 | -1.325 | 3.586 |
| 2.285 | 2.27 | 2.3 | -1.283 | 3.873 |
| 2.385 | 2.37 | 2.4 | -1.369 | 3.554 |
| 2.485 | 2.47 | 2.5 | -1.227 | 3.197 |
| 2.585 | 2.57 | 2.6 | -1.433 | 3.159 |
| 2.685 | 2.67 | 2.7 | -1.285 | 3.240 |
| 2.785 | 2.77 | 2.8 | -1.370 | 3.570 |
| 2.885 | 2.87 | 2.9 | -1.414 | 3.862 |
| 2.985 | 2.97 | 3.0 | -1.324 | 3.868 |
| 3.085 | 3.07 | 3.1 | -1.320 | 3.800 |
| 3.185 | 3.17 | 3.2 | -1.212 | 3.474 |
| 3.285 | 3.27 | 3.3 | -1.260 | 3.570 |
| 3.385 | 3.37 | 3.4 | -1.132 | 3.354 |
| 3.485 | 3.47 | 3.5 | -1.168 | 3.741 |
| 3.585 | 3.57 | 3.6 | -1.086 | 3.622 |
| 3.685 | 3.67 | 3.7 | -1.037 | 4.087 |
| 3.885 | 3.87 | 3.9 | 1.232 | 3.250 |