The biogeochemical cycling of metals in natural systems is often accompanied by stable
isotope fractionation which can now be measured due to recent analytical advances. In …

The isotopic compositions of natural materials are determined by their parent reservoirs, on
the one hand, and by fractionation mechanisms, on the other hand. Under the right …

Earth's water, intrinsic oxidation state and metal core density are fundamental chemical
features of our planet. Studies of exoplanets provide a useful context for elucidating the …

The nine editions of Stable Isotope Geochemistry have appeared over a time span of nearly
50 years. The first edition (1973) appeared as a slim book of 135 pages. Due to the rapid …

Zirconium is a commonly used elemental tracer of silicate differentiation, yet its stable
isotope systematics remain poorly known. Accessory phases rich in Zr4+ such as zircon and …

Estimates of the volume of the earliest crust based on zircon ages and radiogenic isotopes
remain equivocal. Stable isotope systems, such as molybdenum, have the potential to …

Iron is the only polyvalent major element, and controls reduction–oxidation (redox) reactions
in a host of geologic processes and reservoirs, from the mineral-to planetary-scale, on Earth …

Conflicting results exist regarding the mechanisms, direction, and magnitude of Zr isotope
fractionation in igneous systems. To better understand the origin of the fractionations …

Abstract Hydrothermal experiments at 220, 160, and 130° C were performed to calibrate the
Mg isotope fractionation factor between dolomite and aqueous Mg. Hydrothermal …

Fluids liberated from subducting slabs are critical in global geochemical cycles. We
investigate the behaviour of Mo during slab dehydration using two suites of exhumed …