Curry, William B; Lohmann, G P (1983): (Table 1) Stable carbon and oxygen isotope ratios of Planulina wuellerstorfi from sediment core EN066-36PG [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.726018, 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: 4.305000 * Longitude: -20.212000
Date/Time Start: 1981-05-30T00:00:00 * Date/Time End: 1981-05-30T00:00:00
Minimum DEPTH, sediment/rock: 0.04 m * Maximum DEPTH, sediment/rock: 0.80 m
Event(s):
EN066-36PG (0036PG) * Latitude: 4.305000 * Longitude: -20.212000 * Date/Time: 1981-05-30T00:00:00 * Elevation: -4095.0 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:
40 data points
Data
| 1 Depth sed [m] | 2 Age [ka BP] | 3 P. wuellerstorfi δ18O [‰ PDB] | 4 P. wuellerstorfi δ13C [‰ PDB] |
|---|---|---|---|
| 0.04 | 3.1 | 2.59 | 0.99 |
| 0.04 | 3.1 | 2.91 | 0.51 |
| 0.07 | 5.4 | 2.87 | 0.63 |
| 0.10 | 7.6 | 2.99 | 0.60 |
| 0.14 | 10.7 | 3.56 | 0.58 |
| 0.17 | 13.0 | 3.12 | 0.75 |
| 0.20 | 15.0 | 3.75 | 0.33 |
| 0.24 | 17.8 | 4.28 | 0.38 |
| 0.27 | 19.8 | 4.24 | 0.19 |
| 0.30 | 21.8 | 4.18 | 0.06 |
| 0.34 | 24.5 | 4.29 | 0.23 |
| 0.34 | 24.5 | 4.33 | 0.16 |
| 0.37 | 26.6 | 4.27 | 0.03 |
| 0.44 | 31.3 | 3.95 | 0.22 |
| 0.47 | 33.0 | 3.95 | 0.14 |
| 0.60 | 39.9 | 3.70 | 0.17 |
| 0.70 | 45.1 | 3.54 | 0.04 |
| 0.70 | 45.1 | 3.69 | 0.13 |
| 0.80 | 50.4 | 3.81 | 0.32 |
| 0.80 | 50.4 | 3.78 | 0.35 |