Traditional stable isotope geochemistry involves isotopes of light elements such as H, C, N,
O, and S, which are measured predominantly by gas-source mass spectrometry (Valley et al …

Different approaches are used to study wood provenance, but most of them are based on
tracers in wood that are generally controlled by climatic factors. The strontium isotopic ratio …

Since the early 1950s, the number of international measurement standards for anchoring
stable isotope delta scales has mushroomed from 3 to more than 30, expanding to more …

Geochemical data for H 2 O and other volatiles, as well as major and trace elements, are
reported for 377 samples of lunar volcanic glass from three chemical groups (A15 green …

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 …

Mass-dependent Mo isotope fractionation has been investigated for a wide range of
meteorites including chondrites (enstatite, ordinary and carbonaceous chondrites), iron …

The stable strontium isotope system (δ 88/86 Sr) has recently been suggested to be a
suitable proxy for determining variations in the strength of the marine carbonate system, the …

Transhumance and palaeodiet are two central themes in archaeology and using chemical
analysis of bones and teeth to reconstruct trends and patterns in diet and mobility has …

Nutrient biolifting is an important pedogenic process in which plant roots obtain inorganic
nutrients such as phosphorus (P) and calcium (Ca) from minerals at depth and concentrate …

The isotopic composition of Phanerozoic marine sediments provides important information
about changes in seawater chemistry. In particular, the radiogenic strontium isotope (87 …