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Fontugne, Michel R; Paterne, Martine; Calvert, Stephen E; Murat, Anne; Guichard, Francois; Arnold, Maurice (1989): (Table 1b) Stable oxgen isotope ratio measured on G. ruber from sediment core KET82-22 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.726980, In supplement to: Fontugne, MR et al. (1989): Adriatic deep water formation during the Holocene: implication for the reoxygenation of the deep eastern Mediterranean Sea. Paleoceanography, 4(2), 199-206, https://doi.org/10.1029/PA004i002p00199

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Coverage:
Latitude: 37.560000 * Longitude: 16.530000
Date/Time Start: 1982-01-01T00:00:00 * Date/Time End: 1982-01-01T00:00:00
Minimum DEPTH, sediment/rock: 0.0 m * Maximum DEPTH, sediment/rock: 1.6 m
Event(s):
KET82-22 * Latitude: 37.560000 * Longitude: 16.530000 * Date/Time: 1982-01-01T00:00:00 * Elevation: -1691.0 m * Recovery: 11.8 m * Location: Mediterranean Sea * Campaign: ETNA82 * Method/Device: Piston corer (PC) * Comment: No: KET82-22/close to Italy. Messina Strait
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
DEPTH, sediment/rockDepth sedmGeocode
Globigerinoides ruber, δ18OG. ruber δ18O‰ PDBFontugne, Michel RIsotope ratio mass spectrometry
Size:
17 data points

Data

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Depth sed [m]

G. ruber δ18O [‰ PDB]
0.00.03
0.1-0.59
0.2-0.05
0.3-0.05
0.4-0.78
0.5-0.47
0.60.55
0.70.89
0.81.19
0.91.14
1.01.59
1.12.56
1.22.40
1.32.87
1.42.61
1.52.26
1.62.55