Labracherie, Monique; Labeyrie, Laurent D; Duprat, Josette M; Bard, Edouard; Arnold, Maurice; Pichon, Jean-Jacques; Duplessy, Jean-Claude (1989): (Table 3) Stable oxygen isotope ratios of Neogloboquadrina pachyderma from sediment core MD84-551 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.358399, In supplement to: Labracherie, M et al. (1989): The last deglaciation in the Southern Ocean. Paleoceanography, 4(6), 629-638, https://doi.org/10.1029/PA004i006p00629
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Coverage:
Latitude: -55.008300 * Longitude: 73.281700
Date/Time Start: 1984-01-01T00:00:00 * Date/Time End: 1984-01-01T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 3.50 m
Event(s):
MD84-551 * Latitude: -55.008300 * Longitude: 73.281700 * Date/Time: 1984-01-01T00:00:00 * Elevation: -2230.0 m * Recovery: 7.68 m * Location: South Indian Ocean * Campaign: MD38 (APSARA2) * 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 | Neogloboquadrina pachyderma sinistral, δ18O | N. pachyderma s δ18O | ‰ PDB | Labracherie, Monique | Mass spectrometer VG Micromass 602 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
43 data points
Data
| 1 Depth sed [m] | 2 N. pachyderma s δ18O [‰ PDB] |
|---|---|
| 0.00 | 3.15 |
| 0.10 | 3.31 |
| 0.20 | 3.00 |
| 0.30 | 3.15 |
| 0.40 | 3.14 |
| 0.50 | 3.27 |
| 0.60 | 3.13 |
| 0.70 | 3.21 |
| 0.80 | 3.09 |
| 0.90 | 3.40 |
| 1.00 | 3.20 |
| 1.10 | 3.18 |
| 1.12 | 3.49 |
| 1.22 | 3.85 |
| 1.30 | 3.84 |
| 1.40 | 3.04 |
| 1.42 | 3.53 |
| 1.50 | 4.08 |
| 1.55 | 4.74 |
| 1.60 | 4.78 |
| 1.62 | 4.45 |
| 1.72 | 4.10 |
| 1.82 | 4.25 |
| 1.92 | 4.29 |
| 2.00 | 4.11 |
| 2.02 | 4.17 |
| 2.10 | 4.06 |
| 2.20 | 4.05 |
| 2.30 | 3.82 |
| 2.40 | 3.68 |
| 2.50 | 4.00 |
| 2.60 | 3.51 |
| 2.70 | 3.78 |
| 2.80 | 3.83 |
| 2.90 | 3.86 |
| 3.00 | 3.81 |
| 3.10 | 3.55 |
| 3.16 | 3.85 |
| 3.20 | 3.48 |
| 3.26 | 3.80 |
| 3.40 | 3.83 |
| 3.46 | 3.80 |
| 3.50 | 3.67 |