Vergnaud-Grazzini, Colette; Pierre, Catherine (1991): (Table 3) Stable isotopes measured on Uvigerina peregrina from sediment core KS82-30 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.358376, 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: 36.452100 * Longitude: -3.897820
Date/Time Start: 1982-11-29T00:00:00 * Date/Time End: 1982-11-29T00:00:00
Minimum DEPTH, sediment/rock: 0.0 m * Maximum DEPTH, sediment/rock: 2.4 m
Event(s):
KS82-30 (KS030) * Latitude: 36.452100 * Longitude: -3.897820 * Date/Time: 1982-11-29T00:00:00 * Elevation: -795.0 m * Recovery: 7.45 m * Location: Mediterranean Sea * Campaign: FAEGAS_IV * Basis: Le Noroit * Method/Device: Piston corer (PC) * Comment: No: KS82-30
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 | Uvigerina peregrina, δ18O | U. peregrina δ18O | ‰ PDB | Vergnaud-Grazzini, Colette | Mass spectrometer VG SIRA 9 | |
4 | Uvigerina peregrina, δ13C | U. peregrina δ13C | ‰ PDB | Vergnaud-Grazzini, Colette | Mass spectrometer VG SIRA 9 |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
66 data points
Data
1 Depth sed [m] | 2 Age model [ka] | 3 U. peregrina δ18O [‰ PDB] | 4 U. peregrina δ13C [‰ PDB] |
---|---|---|---|
0.0 | 1.5 | 2.99 | -0.55 |
0.2 | 1.9 | 2.07 | -0.56 |
0.4 | 2.5 | 2.01 | -0.51 |
0.5 | 2.7 | 1.69 | -0.67 |
0.6 | 3.0 | 2.05 | -0.53 |
0.7 | 3.6 | 1.92 | -0.59 |
0.8 | 4.3 | 1.91 | -0.61 |
1.0 | 5.8 | 2.13 | -0.51 |
1.1 | 6.6 | 2.04 | -0.65 |
1.2 | 7.3 | 2.09 | -0.55 |
1.3 | 8.1 | 1.63 | -0.56 |
1.4 | 8.8 | 1.59 | -0.75 |
1.5 | 9.2 | 2.19 | -0.45 |
1.6 | 9.6 | 2.10 | -0.50 |
1.7 | 10.0 | 2.49 | -0.42 |
1.8 | 10.4 | 3.50 | -0.26 |
1.9 | 11.0 | 3.06 | -0.34 |
2.0 | 11.6 | 3.36 | -0.09 |
2.1 | 12.3 | 3.55 | -0.11 |
2.2 | 12.5 | 1.02 | -0.06 |
2.3 | 12.8 | 4.02 | -0.06 |
2.4 | 13.1 | 4.67 | -0.22 |