Duplessy, Jean-Claude (1982): (Table 2) Stable carbon and oxygen isotope ratios of Globigerinoides ruber from sediment core MD77-171 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.726203, 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: 11.460000 * Longitude: 94.090000
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: 4.2 m
Event(s):
MD77-171 * Latitude: 11.460000 * Longitude: 94.090000 * Date/Time: 1977-01-01T00:00:00 * Elevation: -1760.0 m * Recovery: 14.1 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 | Globigerinoides ruber, δ18O | G. ruber δ18O | ‰ PDB | Duplessy, Jean-Claude | Isotope ratio mass spectrometry | |
| 3 | Globigerinoides ruber, δ13C | G. ruber δ13C | ‰ PDB | Duplessy, Jean-Claude | Isotope ratio mass spectrometry |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
86 data points
Data
| 1 Depth sed [m] | 2 G. ruber δ18O [‰ PDB] | 3 G. ruber δ13C [‰ PDB] |
|---|---|---|
| 0.0 | -3.00 | 1.01 |
| 0.1 | -3.11 | 0.96 |
| 0.2 | -3.31 | 1.01 |
| 0.3 | -2.98 | 0.93 |
| 0.4 | -3.31 | 1.01 |
| 0.5 | -3.34 | 0.86 |
| 0.6 | -3.34 | 0.78 |
| 0.7 | -3.25 | 1.15 |
| 0.8 | -3.41 | 0.79 |
| 0.9 | -3.31 | 0.69 |
| 1.0 | -3.31 | 0.73 |
| 1.1 | -3.40 | 0.98 |
| 1.2 | -3.29 | 0.73 |
| 1.3 | -3.20 | 0.68 |
| 1.4 | -3.20 | 0.58 |
| 1.5 | -3.08 | 0.51 |
| 1.6 | -2.68 | 0.83 |
| 1.7 | -2.30 | 0.79 |
| 1.8 | -1.94 | 0.84 |
| 1.9 | -1.57 | 0.97 |
| 2.0 | -2.05 | 1.09 |
| 2.1 | -2.04 | 0.87 |
| 2.2 | -2.12 | 0.79 |
| 2.3 | -1.94 | 0.95 |
| 2.4 | -1.45 | 0.77 |
| 2.5 | -0.98 | 0.86 |
| 2.6 | -0.96 | 0.93 |
| 2.7 | -1.04 | 0.80 |
| 2.8 | -1.05 | 0.84 |
| 2.9 | -1.34 | 1.03 |
| 3.0 | -0.91 | 1.08 |
| 3.1 | -1.32 | 0.82 |
| 3.2 | -1.22 | 1.06 |
| 3.3 | -1.14 | 1.12 |
| 3.4 | -1.06 | 1.18 |
| 3.5 | -0.99 | 1.11 |
| 3.6 | -1.39 | 0.86 |
| 3.7 | -1.06 | 0.86 |
| 3.8 | -1.27 | 0.79 |
| 3.9 | -1.41 | 0.72 |
| 4.0 | -1.40 | 1.17 |
| 4.1 | -1.21 | 1.19 |
| 4.2 | -1.20 | 1.11 |