Figure 1: Hydrologic cycle in relative flux units (100 units equals marine evaporation). Figures have been rounded up. (adapted from Chow 1964)
Oxygen and hydrogen isotope signatures of Northeast Atlantic water masses
MODELING CLIMATE AND VEGETATIONAL CHANGE SINCE THE LAST GLACIAL MAXIMUM USING STABLE ISOTOPES AND DIGITAL ANALYSIS Pennilyn Higgins Florida Museum of Natural.
Oxygen Isotope and Paleoclimatic Information. B. Oxygen Isotope studies of calcareous marine fauna A. Paleoclimatic information from biological material.
Trophic diversity and potential role of detritivorous crustaceans in Posidonia oceanica litter
Tracing Vegetation Changes through Carbon Isotopes