Vergnaud-Grazzini, Colette; Pierre, Catherine (1991): (Table 3) Stable isotopes measured on Uvigerina peregrina from sediment core KC82-41 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.52456, In supplement to: Vergnaud-Grazzini, C; Pierre, C (1991): High fertility in the Alboran Sea since the last glacial maximum. Paleoceanography, 6(4), 519-536, https://doi.org/10.1029/91PA00501
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Coverage:
Latitude: 35.985000 * Longitude: -4.400000
Date/Time Start: 1982-11-28T00:00:00 * Date/Time End: 1982-11-28T00:00:00
Minimum DEPTH, sediment/rock: 0.0 m * Maximum DEPTH, sediment/rock: 3.3 m
Event(s):
KC82-41 (KC041) * Latitude: 35.985000 * Longitude: -4.400000 * Date/Time: 1982-11-28T00:00:00 * Elevation: -1288.0 m * Recovery: 3.3 m * Campaign: FAEGAS_IV * Basis: Le Noroit * Method/Device: Piston corer (PC) * Comment: No: KC82-41
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 2 | Age model | Age model | ka | Vergnaud-Grazzini, Colette | Age model, stable isotope stratigraphy | calculated ages |
| 3 | Globigerina bulloides, δ18O | G. bulloides δ18O | ‰ PDB | Vergnaud-Grazzini, Colette | Mass spectrometer VG SIRA 9 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
62 data points
Data
| 1 Depth sed [m] | 2 Age model [ka] | 3 G. bulloides δ18O [‰ PDB] |
|---|---|---|
| 0.0 | 0.0 | 0.04 |
| 0.1 | 1.5 | 0.01 |
| 0.2 | 2.0 | 0.53 |
| 0.3 | 2.5 | 0.19 |
| 0.4 | 3.0 | 0.00 |
| 0.5 | 3.5 | 0.00 |
| 0.7 | 4.5 | 0.32 |
| 0.8 | 5.0 | 0.49 |
| 0.9 | 5.6 | 0.25 |
| 1.1 | 6.7 | 0.43 |
| 1.3 | 8.8 | 0.09 |
| 1.4 | 9.1 | 0.66 |
| 1.5 | 9.3 | 0.46 |
| 1.6 | 9.6 | 0.41 |
| 1.7 | 9.8 | 0.46 |
| 1.8 | 10.1 | 1.05 |
| 1.9 | 10.4 | 1.62 |
| 2.0 | 10.8 | 1.17 |
| 2.1 | 11.1 | 0.72 |
| 2.2 | 11.5 | 1.02 |
| 2.3 | 11.9 | 1.17 |
| 2.4 | 12.3 | 0.97 |
| 2.5 | 13.1 | 1.80 |
| 2.6 | 13.9 | 2.45 |
| 2.7 | 14.0 | 2.24 |
| 2.8 | 14.2 | 1.24 |
| 2.9 | 14.3 | 1.99 |
| 3.0 | 14.4 | 2.19 |
| 3.1 | 14.6 | 2.51 |
| 3.2 | 15.0 | 2.38 |
| 3.3 | 15.5 | 2.42 |