Duplessy, Jean-Claude (1982): (Table 5) Stable carbon and oxygen isotope ratios of Uvigerina spp. from sediment core MD77-191 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.726213, In supplement to: Duplessy, J-C (1982): North Atlantic deep water circulation during the last climate cycle. Bulletin de l'Institut de Geologie du Bassin d'Aquitaine, 31, 379-391
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Coverage:
Latitude: 7.300000 * Longitude: 76.430000
Date/Time Start: 1977-01-01T00:00:00 * Date/Time End: 1977-01-01T00:00:00
Minimum DEPTH, sediment/rock: 0.0 m * Maximum DEPTH, sediment/rock: 7.5 m
Event(s):
MD77-191 * Latitude: 7.300000 * Longitude: 76.430000 * Date/Time: 1977-01-01T00:00:00 * Elevation: -1254.0 m * Recovery: 13.4 m * Location: Indian Ocean * Campaign: MD13 (OSIRIS III) * Basis: Marion Dufresne (1972) * Method/Device: Piston corer (PC)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Uvigerina spp., δ18O | Uvigerina spp. δ18O | ‰ PDB | Duplessy, Jean-Claude | Isotope ratio mass spectrometry | |
| 3 | Uvigerina spp., δ13C | Uvigerina spp. δ13C | ‰ PDB | Duplessy, Jean-Claude | Isotope ratio mass spectrometry |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
151 data points
Data
| 1 Depth sed [m] | 2 Uvigerina spp. δ18O [‰ PDB] | 3 Uvigerina spp. δ13C [‰ PDB] |
|---|---|---|
| 0.0 | 2.78 | -0.63 |
| 0.1 | 2.64 | -0.54 |
| 0.2 | 2.71 | -0.58 |
| 0.3 | 2.65 | -0.76 |
| 0.4 | 2.54 | -0.66 |
| 0.5 | 2.43 | -0.69 |
| 0.6 | 2.36 | -0.86 |
| 0.7 | 2.41 | -0.67 |
| 0.8 | 2.50 | -0.64 |
| 0.9 | 2.47 | -0.56 |
| 1.0 | 2.61 | -0.63 |
| 1.1 | 2.56 | -0.81 |
| 1.2 | 2.77 | -0.71 |
| 1.3 | 2.77 | -0.75 |
| 1.4 | 2.84 | -0.78 |
| 1.5 | 2.71 | -0.78 |
| 1.6 | 2.52 | -0.61 |
| 1.7 | 2.73 | -0.62 |
| 1.8 | 2.62 | -0.60 |
| 1.9 | 2.90 | -0.61 |
| 2.0 | 2.70 | -0.65 |
| 2.1 | 2.88 | -0.56 |
| 2.2 | 2.78 | -0.81 |
| 2.3 | 2.55 | -0.85 |
| 2.4 | 2.60 | -1.04 |
| 2.5 | 2.83 | -0.71 |
| 2.6 | 2.95 | -0.60 |
| 2.7 | 2.99 | -0.50 |
| 2.8 | 2.88 | -0.95 |
| 2.9 | 2.85 | -0.99 |
| 3.0 | 2.77 | -0.92 |
| 3.1 | 2.53 | -0.75 |
| 3.2 | 2.70 | -0.65 |
| 3.3 | 2.78 | -0.72 |
| 3.4 | 2.91 | -0.74 |
| 3.5 | 2.87 | -0.68 |
| 3.6 | 2.65 | -0.61 |
| 3.7 | 2.77 | -0.75 |
| 3.8 | 2.94 | -0.62 |
| 3.9 | 2.82 | -0.83 |
| 4.0 | 2.87 | -8.00 |
| 4.1 | 2.98 | -0.92 |
| 4.2 | 2.98 | -0.83 |
| 4.3 | 3.09 | -0.68 |
| 4.4 | 3.10 | -0.87 |
| 4.5 | 3.12 | -0.96 |
| 4.6 | 3.06 | |
| 4.7 | 3.00 | -0.45 |
| 4.8 | 2.51 | -0.37 |
| 4.9 | 2.55 | -0.67 |
| 5.0 | 2.64 | -0.68 |
| 5.1 | 3.07 | -1.05 |
| 5.2 | 3.30 | -0.86 |
| 5.3 | 3.00 | -0.83 |
| 5.4 | 3.16 | -0.84 |
| 5.5 | 2.88 | -0.80 |
| 5.6 | 3.06 | -0.79 |
| 5.7 | 3.31 | -0.48 |
| 5.8 | 2.64 | -0.34 |
| 5.9 | 2.84 | -0.80 |
| 6.0 | 2.88 | -0.70 |
| 6.1 | 3.10 | -0.86 |
| 6.2 | 3.00 | -0.49 |
| 6.3 | 2.77 | -0.36 |
| 6.4 | 3.11 | -0.57 |
| 6.5 | 3.04 | -0.55 |
| 6.6 | 3.34 | -0.28 |
| 6.7 | 3.58 | -0.48 |
| 6.8 | 3.33 | -0.64 |
| 6.9 | 3.89 | -0.63 |
| 7.0 | 4.25 | -0.55 |
| 7.1 | 4.23 | -0.56 |
| 7.2 | 4.08 | -0.78 |
| 7.3 | 4.02 | -0.80 |
| 7.4 | 3.20 | -0.35 |
| 7.5 | 3.20 | -0.40 |