Curry, William B; Lohmann, G P (1983): (Table 1) Stable carbon and oxygen isotope ratios of Planulina wuellerstorfi from sediment core EN066-16PG [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.726013, 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: 5.453000 * Longitude: -21.143000
Date/Time Start: 1981-05-27T00:00:00 * Date/Time End: 1981-05-27T00:00:00
Minimum DEPTH, sediment/rock: 0.04 m * Maximum DEPTH, sediment/rock: 0.80 m
Event(s):
EN066-16PG (0016PG) * Latitude: 5.453000 * Longitude: -21.143000 * Date/Time: 1981-05-27T00:00:00 * Elevation: -3160.0 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:
42 data points
Data
1 Depth sed [m] | 2 Age [ka BP] | 3 P. wuellerstorfi δ18O [‰ PDB] | 4 P. wuellerstorfi δ13C [‰ PDB] |
---|---|---|---|
0.04 | 2.9 | 2.54 | 0.94 |
0.07 | 5.1 | 2.44 | 0.99 |
0.10 | 7.2 | 3.35 | 0.57 |
0.14 | 10.1 | 2.81 | 0.95 |
0.17 | 12.3 | 3.09 | 0.77 |
0.20 | 14.1 | 4.14 | 0.47 |
0.24 | 16.4 | 4.38 | 0.44 |
0.27 | 18.0 | 4.19 | 0.31 |
0.30 | 19.7 | 4.35 | 0.43 |
0.34 | 21.9 | 4.38 | 0.43 |
0.37 | 23.6 | 4.30 | 0.40 |
0.40 | 25.3 | 4.08 | 0.46 |
0.44 | 27.5 | 4.13 | 0.51 |
0.44 | 27.5 | 4.15 | 0.50 |
0.47 | 29.2 | 4.20 | 0.54 |
0.50 | 30.9 | 4.14 | 0.44 |
0.50 | 30.9 | 3.96 | 0.28 |
0.60 | 36.4 | 4.02 | 0.71 |
0.70 | 41.9 | 3.55 | 0.84 |
0.70 | 41.9 | 3.97 | 0.81 |
0.80 | 47.4 | 3.73 | 0.69 |