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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 KET82-16. PANGAEA, https://doi.org/10.1594/PANGAEA.358892, 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: 41.310000 * Longitude: 17.590000
Date/Time Start: 1982-01-01T00:00:00 * Date/Time End: 1982-01-01T00:00:00
Minimum DEPTH, sediment/rock: 0.01 m * Maximum DEPTH, sediment/rock: 1.70 m
Event(s):
KET82-16 * Latitude: 41.310000 * Longitude: 17.590000 * Date/Time: 1982-01-01T00:00:00 * Elevation: -1166.0 m * Recovery: 5.98 m * Location: Mediterranean Sea * Campaign: ETNA82 * Method/Device: Piston corer (PC) * Comment: No: KET82-16
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepthmGeocode
2Globigerinoides ruber, δ18OG. ruber δ18O‰ PDBFontugne, Michel RIsotope ratio mass spectrometry
Size:
21 data points

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