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 …

At the Earth's surface, calcium (Ca) is a critical element at a variety of scales: it is soluble in
natural waters, a biological nutrient, and a major constituent of the dominant mineral sink for …

Several studies have measured riverine fluxes of Ca and carbonate alkalinity in Iceland with
the aim of quantifying the role of basalt weathering in the long-term carbon cycle. A major …

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 …

We report mass‐independent and mass‐dependent Ca isotopic compositions for thirteen
geological reference materials, including carbonates (NIST SRM 915a and 915b), Atlantic …

Carbonatites are igneous rocks composed of over 50% modal carbonate minerals and their
exact origin and possible mode (s) of formation are still debated. We report stable Ca …

Li, B, Mg and Ca isotopes became of increasing interest during the last decade due to their
potential for better constraining the carbon cycle and nutrient cycling. At the soil-water-plant …

Calcium is an essential element in the biogeochemical cycles that regulate the long-term
climate state of Earth. The removal of CO 2 from the ocean-atmosphere system is controlled …

In order to investigate Ca isotope fractionation during crustal melting and magma
differentiation, we report high-precision Ca isotopic data of 17 well-characterized granitoids …

Mountain uplift is frequently invoked as a mechanism that accelerates atmospheric CO2
consumption by chemical weathering, thereby cooling climate over geological timescales …