Beveridge, N; Elderfield, Henry; Shackleton, Nicholas J (1995): (TAble 3d) Stable isotope analysis on sediment core BOFS28/3M [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.59503, In supplement to: Beveridge, N et al. (1995): Deep thermohaline circulation in the low-latitude Atlantic during the last glacial. Paleoceanography, 10(3), 643-660, https://doi.org/10.1029/94PA03353
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Project(s):
Coverage:
Latitude: 24.615000 * Longitude: -22.762000
Date/Time Start: 1990-10-11T00:00:00 * Date/Time End: 1990-10-11T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 0.50 m
Event(s):
BOFS28/3K (BOFS28#3) * Latitude: 24.615000 * Longitude: -22.762000 * Date/Time: 1990-10-11T00:00:00 * Elevation: -4900.0 m * Location: Northeast Atlantic * Campaign: CD53 * Basis: Charles Darwin * Method/Device: Kasten corer (KAL) * Comment: BOFS-ID 18295
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 | Cibicidoides wuellerstorfi, δ18O | C. wuellerstorfi δ18O | ‰ PDB | Elderfield, Henry | Mass spectrometer VG Isogas Prism | |
| 4 | Cibicidoides wuellerstorfi, δ13C | C. wuellerstorfi δ13C | ‰ PDB | Elderfield, Henry | Mass spectrometer VG Isogas Prism |
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 C. wuellerstorfi δ18O [‰ PDB] | 4 C. wuellerstorfi δ13C [‰ PDB] |
|---|---|---|---|
| 0.01 | 1.52000 | 2.21 | 1.08 |
| 0.03 | 2.56000 | 2.43 | 0.97 |
| 0.07 | 4.89000 | 2.37 | 0.89 |
| 0.18 | 10.92000 | 3.04 | 0.59 |
| 0.20 | 12.31000 | 3.56 | 0.34 |
| 0.22 | 13.61000 | 3.12 | 0.38 |
| 0.24 | 14.90000 | 3.46 | 0.38 |
| 0.26 | 16.08000 | 3.32 | 0.21 |
| 0.28 | 17.19000 | 3.40 | 0.28 |
| 0.29 | 17.70000 | 3.79 | 0.01 |
| 0.31 | 19.43000 | 3.68 | 0.01 |
| 0.40 | 24.03000 | 3.67 | 0.23 |
| 0.41 | 25.11000 | 3.58 | 0.20 |
| 0.42 | 26.16000 | 3.79 | 0.20 |
| 0.43 | 27.23000 | 3.63 | 0.42 |
| 0.44 | 28.33000 | 3.75 | 0.26 |
| 0.45 | 29.58000 | 3.74 | 0.36 |
| 0.47 | 31.43000 | 3.54 | 0.51 |
| 0.48 | 32.43000 | 3.59 | 0.47 |
| 0.50 | 34.40000 | 3.50 | 0.54 |