Lynch-Stieglitz, Jean; Fairbanks, Richard G; Charles, Christopher D (1994): (Table B1) Stable isotope ratios of benthic foraminifera from sediment core SO36-7SL [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.386608, In supplement to: Lynch-Stieglitz, J et al. (1994): Glacial-interglacial history of Antarctic Intermediate Water: Relative strengths of Antarctic versus Indian Ocean sources. Paleoceanography, 9(1), 7-30, https://doi.org/10.1029/93PA02446
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Project(s):
Coverage:
Latitude: -42.308667 * Longitude: 144.670717
Date/Time Start: 1985-04-16T00:00:00 * Date/Time End: 1985-04-16T00:00:00
Minimum DEPTH, sediment/rock: 0.00 m * Maximum DEPTH, sediment/rock: 4.15 m
Event(s):
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Planulina wuellerstorfi, δ18O | P. wuellerstorfi δ18O | ‰ PDB | Lynch-Stieglitz, Jean | Mass spectrometer Finnigan MAT 251 | |
| 3 | Planulina wuellerstorfi, δ13C | P. wuellerstorfi δ13C | ‰ PDB | Lynch-Stieglitz, Jean | Mass spectrometer Finnigan MAT 251 | |
| 4 | Uvigerina sp., δ18O | Uvigerina sp. δ18O | ‰ PDB | Lynch-Stieglitz, Jean | Mass spectrometer Finnigan MAT 251 | |
| 5 | Uvigerina sp., δ13C | Uvigerina sp. δ13C | ‰ PDB | Lynch-Stieglitz, Jean | Mass spectrometer Finnigan MAT 251 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
93 data points
Data
| 1 Depth sed [m] | 2 P. wuellerstorfi δ18O [‰ PDB] | 3 P. wuellerstorfi δ13C [‰ PDB] | 4 Uvigerina sp. δ18O [‰ PDB] | 5 Uvigerina sp. δ13C [‰ PDB] |
|---|---|---|---|---|
| 0.00 | 3.00 | 0.11 | ||
| 0.05 | 2.33 | 0.07 | ||
| 0.10 | 2.47 | 0.36 | ||
| 0.15 | 2.58 | -0.06 | ||
| 0.20 | 3.44 | 0.48 | ||
| 0.30 | 3.50 | -0.40 | ||
| 0.35 | 3.37 | -0.36 | ||
| 0.40 | 3.90 | -0.46 | ||
| 0.45 | 3.78 | -0.36 | ||
| 0.50 | 4.25 | -0.48 | ||
| 0.60 | 4.41 | -0.51 | ||
| 0.66 | 3.48 | 0.66 | ||
| 0.70 | 4.28 | -0.54 | ||
| 0.80 | 4.18 | -0.58 | ||
| 0.90 | 4.20 | -0.70 | ||
| 1.00 | 3.98 | -0.60 | ||
| 1.10 | 4.02 | -0.62 | ||
| 1.20 | 4.03 | -0.58 | ||
| 1.30 | 3.96 | -0.56 | ||
| 1.40 | 3.85 | -0.57 | ||
| 1.50 | 3.57 | -0.36 | ||
| 1.60 | 3.59 | -0.31 | ||
| 1.80 | 3.77 | -0.50 | ||
| 1.90 | 3.67 | -0.44 | ||
| 2.00 | 3.70 | -0.58 | ||
| 2.10 | 3.58 | -0.42 | ||
| 2.20 | 3.61 | -0.68 | ||
| 2.30 | 3.70 | -0.75 | ||
| 2.40 | 3.35 | -0.41 | ||
| 2.50 | 3.70 | -0.60 | ||
| 2.60 | 3.61 | -0.63 | ||
| 2.70 | 3.79 | -0.68 | ||
| 2.80 | 3.75 | -0.58 | ||
| 3.00 | 3.51 | -0.58 | ||
| 3.10 | 3.57 | -0.63 | ||
| 3.20 | 3.63 | -0.71 | ||
| 3.30 | 3.53 | -0.92 | ||
| 3.40 | 3.74 | -0.67 | ||
| 3.50 | 3.51 | 0.56 | ||
| 3.60 | 3.74 | 0.86 | ||
| 3.70 | 3.54 | -0.74 | ||
| 3.80 | 3.67 | -0.60 | ||
| 3.90 | 3.60 | -0.71 | ||
| 4.00 | 3.58 | |||
| 4.05 | 3.40 | -0.62 | ||
| 4.10 | 3.42 | -0.36 | ||
| 4.15 | 2.78 | -1.06 |