Curry, William B; Lohmann, G P (1982): (Table 2) Stable carbon and oxygen isotope ratios of Planulina wuellerstorfi from sediment core CHN115-89PC [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.726250, 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
Always quote citation above when using data! You can download the citation in several formats below.
Coverage:
Latitude: -30.880000 * Longitude: -38.196667
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 1.10 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:
54 data points
Data
| 1 Depth sed [m] | 2 Age [ka BP] | 3 P. wuellerstorfi δ18O [‰ PDB] | 4 P. wuellerstorfi δ13C [‰ PDB] |
|---|---|---|---|
| 0.00 | 11.0 | 3.28 | 0.38 |
| 0.10 | 13.0 | 3.36 | 0.29 |
| 0.10 | 13.0 | 3.44 | 0.61 |
| 0.20 | 16.0 | 3.47 | 0.68 |
| 0.20 | 16.0 | 3.82 | 0.04 |
| 0.28 | 17.5 | 3.65 | 0.56 |
| 0.30 | 18.0 | 3.89 | 0.16 |
| 0.30 | 18.0 | 4.15 | 0.23 |
| 0.30 | 18.0 | 3.51 | 0.69 |
| 0.36 | 35.0 | 3.64 | 0.25 |
| 0.40 | 47.0 | 3.90 | 0.45 |
| 0.45 | 61.0 | 3.84 | 0.81 |
| 0.45 | 61.0 | 3.68 | 0.55 |
| 0.56 | 82.0 | 3.16 | 0.56 |
| 0.60 | 86.0 | 3.52 | 0.64 |
| 0.67 | 94.0 | 2.76 | 0.37 |
| 0.70 | 98.0 | 3.41 | 0.89 |
| 0.77 | 105.0 | 2.89 | 0.83 |
| 0.80 | 109.0 | 3.12 | 0.70 |
| 0.84 | 113.0 | 3.13 | 0.94 |
| 0.90 | 120.0 | 2.93 | 0.82 |
| 0.90 | 120.0 | 2.96 | 0.22 |
| 0.95 | 128.0 | 3.54 | 0.46 |
| 1.00 | 141.0 | 4.19 | -0.05 |
| 1.07 | 159.0 | 3.95 | 0.21 |
| 1.10 | 167.0 | 3.41 | -0.02 |
| 1.10 | 167.0 | 3.83 | -0.13 |