Curry, William B; Lohmann, G P (1983): (Table 1) Stable carbon and oxygen isotope ratios of Planulina wuellerstorfi from sediment core EN066-38PG [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.726019, In supplement to: Curry, WB; Lohmann, GP (1983): Reduced advection into Atlantic Ocean deep eastern basins during last glaciation maximum. Nature, 306, 577-580, https://doi.org/10.1038/306577a0
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Coverage:
Latitude: 4.918000 * Longitude: -20.498000
Date/Time Start: 1981-05-31T00:00:00 * Date/Time End: 1981-05-31T00:00:00
Minimum DEPTH, sediment/rock: 0.03 m * Maximum DEPTH, sediment/rock: 0.69 m
Event(s):
EN066-38PG (0038PG) * Latitude: 4.918000 * Longitude: -20.498000 * Date/Time: 1981-05-31T00:00:00 * Elevation: -2937.0 m * Campaign: EN06601 * Basis: Endeavor * Method/Device: Gravity corer (GC)
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | AGE | Age | ka BP | Geocode | ||
| 3 | Planulina wuellerstorfi, δ18O | P. wuellerstorfi δ18O | ‰ PDB | Curry, William B | Isotope ratio mass spectrometry | |
| 4 | Planulina wuellerstorfi, δ13C | P. wuellerstorfi δ13C | ‰ PDB | Curry, William B | Isotope ratio mass spectrometry |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
38 data points
Data
| 1 Depth sed [m] | 2 Age [ka BP] | 3 P. wuellerstorfi δ18O [‰ PDB] | 4 P. wuellerstorfi δ13C [‰ PDB] |
|---|---|---|---|
| 0.03 | 2.2 | 2.52 | 0.98 |
| 0.03 | 2.2 | 2.75 | 1.11 |
| 0.06 | 4.3 | 2.69 | 1.24 |
| 0.09 | 6.5 | 3.17 | 0.93 |
| 0.09 | 6.5 | 2.82 | 0.85 |
| 0.12 | 8.7 | 2.96 | 1.09 |
| 0.16 | 11.6 | 3.17 | 0.69 |
| 0.19 | 14.0 | 3.99 | 0.41 |
| 0.22 | 17.0 | 4.05 | 0.50 |
| 0.26 | 21.0 | 4.23 | 0.69 |
| 0.29 | 24.0 | 3.98 | 0.59 |
| 0.32 | 27.0 | 3.93 | 0.41 |
| 0.35 | 30.0 | 4.00 | 0.52 |
| 0.39 | 33.3 | 3.94 | 0.55 |
| 0.39 | 33.3 | 3.90 | 0.60 |
| 0.42 | 35.1 | 3.85 | 0.62 |
| 0.46 | 37.6 | 3.89 | 0.70 |
| 0.49 | 39.5 | 3.92 | 0.53 |
| 0.69 | 52.1 | 3.70 | 0.79 |