Anderson, David M; Prell, Warren L; Barratt, N J (1989): (Table 2) Stable isotope analysis on planktonic foraminifer G. sacculifer from sediment core RC10-131 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.263950, In supplement to: Anderson, DM et al. (1989): Estimates of sea surface temperature in the Coral Sea at the last glacial Maximum. Paleoceanography, 4(6), 615-627, https://doi.org/10.1029/PA004i006p00615
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Project(s):
Coverage:
Latitude: -14.530000 * Longitude: 157.970000
Date/Time Start: 1966-04-20T00:00:00 * Date/Time End: 1966-04-20T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 2.40 m
Event(s):
RC10-131 * Latitude: -14.530000 * Longitude: 157.970000 * Date/Time: 1966-04-20T00:00:00 * Elevation: -2933.0 m * Recovery: 9.37 m * Campaign: RC10 * Basis: Robert Conrad * 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 sacculifer, δ13C | G. sacculifer δ13C | ‰ PDB | Anderson, David M | Mass spectrometer VG SIRA 24 | |
| 3 | Globigerinoides sacculifer, δ18O | G. sacculifer δ18O | ‰ PDB | Anderson, David M | Mass spectrometer VG SIRA 24 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
56 data points
Data
| 1 Depth sed [m] | 2 G. sacculifer δ13C [‰ PDB] | 3 G. sacculifer δ18O [‰ PDB] |
|---|---|---|
| 0.01 | 0.97 | -1.96 |
| 0.10 | 0.98 | -1.62 |
| 0.20 | 0.86 | -1.37 |
| 0.30 | 1.05 | -0.82 |
| 0.30 | 0.75 | -0.55 |
| 0.40 | 0.98 | -0.64 |
| 0.50 | 1.01 | -0.32 |
| 0.60 | 1.32 | -0.47 |
| 0.70 | 0.92 | -1.03 |
| 0.70 | 0.91 | -0.66 |
| 0.80 | 1.06 | -0.91 |
| 0.90 | 0.87 | -1.03 |
| 1.00 | 1.18 | -1.06 |
| 1.10 | 1.02 | -0.88 |
| 1.10 | 0.96 | -1.05 |
| 1.20 | 0.95 | -0.97 |
| 1.30 | 1.09 | -0.74 |
| 1.40 | 1.16 | -1.36 |
| 1.50 | 1.09 | -1.66 |
| 1.60 | 1.13 | -1.23 |
| 1.70 | 1.29 | -1.49 |
| 1.80 | 0.98 | -1.44 |
| 1.90 | 0.75 | -1.62 |
| 2.00 | 0.78 | -1.39 |
| 2.10 | 0.32 | -1.39 |
| 2.20 | 0.76 | -0.73 |
| 2.30 | 0.78 | -0.31 |
| 2.40 | 0.71 | -0.62 |