The past decade has seen a remarkable expansion of studies that use mass-dependent
variations of triple oxygen isotopes (16 O, 17 O, 18 O) in isotope hydrology and isotope …

The usefulness of triple isotope studies of natural systems is contingent on the existence of
resolvable differences in mass-dependent fractionation exponents θ [where θ= ln (17/16α)/ln …

Abstract Characterization of moisture origins is crucial to understanding hydroclimatic
processes. Nevertheless, documenting past atmospheric moisture contents and their …

The new excess term of the triple oxygen isotope composition in meteoric water, expressed
as∆′ 17 O, is conceived to track the component of kinetic fractionation in the water cycle …

Evaporation can increase the δ 18 O values of lake waters and carbonates by several per
mil. If not accounted for in geological studies, this can lead to substantial misinterpretation of …

The stable isotopic composition of pedogenic carbonates is central to many studies of past
climate and topography, providing a basis for our understanding of Earth's terrestrial history …

The analysis of hydrogen (δD) and oxygen (δ18O) isotope ratios of H2O are widely used
tools for studies of the hydrological cycle (Friedman 1953; Dansgaard 1954; Gonfiantini …

This study investigates the combined hydrogen deuterium and triple oxygen isotope
hydrology of the Salar del Huasco, an endorheic salt flat with shallow lakes at its centre that …

It has long been recognized that the stable oxygen isotope 18 O/16 O ratios of chemical
sediments show a systematic decrease with increasing age. This continuous, 3.8 Ga long …

The isotopic composition of precipitation is used to trace water cycling and climate change,
but interpretations of the environmental information recorded in central Andean precipitation …