Curry, William B; Lohmann, G P (1982): (Table 2) Stable carbon and oxygen isotope ratios of Planulina wuellerstorfi from sediment core CHN115-88PC [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.726249, In supplement to: Curry, WB; Lohmann, GP (1982): Carbon isotopic changes in benthic foraminifera from the Western South Atlantic: Reconstruction of glacial abyssal circulation patterns. Quaternary Research, 18(2), 218-235, https://doi.org/10.1016/0033-5894(82)90071-0
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Coverage:
Latitude: -30.916667 * Longitude: -36.080000
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 0.90 m
Event(s):
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 | Mass spectrometer VG Micromass 602 | > 250 µm |
| 4 | Planulina wuellerstorfi, δ13C | P. wuellerstorfi δ13C | ‰ PDB | Curry, William B | Mass spectrometer VG Micromass 602 | > 250 µm |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
60 data points
Data
| 1 Depth sed [m] | 2 Age [ka BP] | 3 P. wuellerstorfi δ18O [‰ PDB] | 4 P. wuellerstorfi δ13C [‰ PDB] |
|---|---|---|---|
| 0.00 | 0 | 2.62 | 0.68 |
| 0.06 | 11 | 2.82 | 0.43 |
| 0.06 | 11 | 3.43 | 0.63 |
| 0.06 | 11 | 3.04 | 0.74 |
| 0.10 | 20 | 4.17 | 0.27 |
| 0.10 | 20 | 2.96 | 0.41 |
| 0.16 | 33 | 3.61 | 0.57 |
| 0.16 | 33 | 3.92 | 0.29 |
| 0.16 | 33 | 3.87 | 0.57 |
| 0.20 | 42 | 3.80 | 0.52 |
| 0.20 | 42 | 3.73 | 0.70 |
| 0.20 | 42 | 4.18 | 0.65 |
| 0.20 | 42 | 3.44 | 0.64 |
| 0.26 | 55 | 3.85 | 0.60 |
| 0.26 | 55 | 3.54 | 0.41 |
| 0.26 | 55 | 3.55 | 0.83 |
| 0.30 | 64 | 3.80 | 0.57 |
| 0.30 | 64 | 3.61 | 0.32 |
| 0.30 | 64 | 3.90 | 0.55 |
| 0.36 | 77 | 3.75 | 0.62 |
| 0.36 | 77 | 3.80 | 0.47 |
| 0.40 | 84 | 2.92 | -0.11 |
| 0.40 | 84 | 3.39 | 0.99 |
| 0.46 | 95 | 3.29 | 0.35 |
| 0.56 | 112 | 2.90 | 0.22 |
| 0.60 | 120 | 2.89 | 0.58 |
| 0.70 | 132 | 3.68 | 0.26 |
| 0.76 | 138 | 3.60 | 0.04 |
| 0.86 | 146 | 3.37 | 0.02 |
| 0.90 | 150 | 3.56 | -0.39 |