/* DATA DESCRIPTION: Citation: 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 MD84-658. PANGAEA, https://doi.org/10.1594/PANGAEA.358893, 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 Coverage: LATITUDE: 35.033333 * LONGITUDE: 17.050000 MINIMUM DEPTH, sediment/rock: 0.02 m * MAXIMUM DEPTH, sediment/rock: 0.42 m Event(s): MD84-658 * LATITUDE: 35.033333 * LONGITUDE: 17.050000 * ELEVATION: -2020.0 m * LOCATION: Mediterranean Sea * CAMPAIGN: NOE * BASIS: Marion Dufresne (1972) (URI: https://fr.wikipedia.org/wiki/Marion_Dufresne_(1972)) * METHOD/DEVICE: Piston corer (PC) * COMMENT: No: MD84-658 Parameter(s): DEPTH, sediment/rock [m] (Depth sed) * GEOCODE Globigerinoides ruber, δ18O [‰ PDB] (G. ruber δ18O) * PI: Fontugne, Michel R * METHOD/DEVICE: Isotope ratio mass spectrometry (URI: https://en.wikipedia.org/wiki/Isotope_ratio_mass_spectrometry) License: Creative Commons Attribution 3.0 Unported (CC-BY-3.0) (URI: https://creativecommons.org/licenses/by/3.0/) Size: 9 data points */ Depth sed [m] G. ruber δ18O [‰ PDB] 0.02 0.58 0.06 -0.21 0.09 -0.45 0.14 2.83 0.17 3.10 0.22 3.26 0.28 3.00 0.36 2.72 0.42 2.40