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 …

This work critically reviews stable isotope fractionation of essential (B, Mg, K, Ca, Fe, Ni, Cu,
Zn, Mo), beneficial (Si), and non-essential (Cd, Tl) metals and metalloids in plants. The …

Tracing pedogenic processes is fundamental for reconstructing climatic and environmental
changes using loess deposits. Lithium isotopes can serve as a sensitive tracer to unravel …

The feedback between CO 2 sources and sinks through chemical weathering is one of the
important reasons why Earth has maintained a habitable climate for over four billion years …

The oxygen isotope composition of carbonate minerals varies with temperature as well as
other environmental variables. For carbonates that precipitate slowly, under conditions that …

The marine biogeochemical cycle of Ba is thought to be controlled by particulate BaSO 4
(barite) precipitation associated with the microbial oxidation of organic carbon and its …

We report results of experiments conducted to quantify the sense and magnitude of
cadmium stable isotope fractionation during sorption to synthetic birnessite (Mn …

Oceanic crust and sediments are the primary K sinks for seawater, and they deliver
considerable amounts of K to the mantle via subduction. Historically, these crustal …

Natural variations in the isotopic composition of some 50 chemical elements are now being
used in geochemistry for studying transport processes, estimating temperature …

Significant uranium (U) isotope fractionation has been observed during abiotic reduction of
aqueous U, counter to the expectation that uranium isotopes are only fractionated by …