Images of Δ18O
Image showing a marine coring vessel and the new CENOGRID climate curve, overlain on hot/cold colour bands to indicate the different climate states. Temperature is inferred from the concentration of the stable oxygen isotope δ18O of the marine sediments which is an indicator of global ice volume. Image credit Thomas Westerhold / Adam Kutz.
Stable-isotopic composition of precipitation over the northern slope of the central HimalayaCited bySave article to KindleSave article to DropboxSave article to Google Drive
Article An improved estimate for the δ13C and δ18O signatures of carbon monoxide produced from atmospheric oxidation of volatile organic compounds
Article Evidence from giant-clam δ18O of intense El Ninõ–Southern Oscillation-related variability but reduced frequency 3700 years ago
High-sensitivity Thermo Delta V Advantage Isotope Ratio Mass Spectrometer (IRMS) configured for δ13C, δ15N, δ2H, and δ18O analysis*
Acquisition of Post-Depositional Effects on Stable Isotopes (δ18O and δD) of Snow and Firn at Dome A, East Antarctica
Disentangle Kinetic From Equilibrium Fractionation Using Primary (δ17O, δ18O, δD) and Secondary (Δ17O, dex) Stable Isotope Parameters on Samples From the Swiss Precipitation Network
Article The Δ17O and δ18O values of atmospheric nitrates simultaneously collected downwind of anthropogenic sources – implications for polluted air masses