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 …

Abstract The Weddell Gyre (WG) is one of the main oceanographic features of the Southern
Ocean south of the Antarctic Circumpolar Current which plays an influential role in global …

Dissolved stable isotope ratios of the transition metals provide useful information, both for
understanding the cycling of these bioactive trace elements through the oceans, and tracing …

Isotopic data collected to date as part of the GEOTRACES and other programmes show that
the oceanic dissolved pool is isotopically heavy relative to the inputs for zinc (Zn) and nickel …

Cadmium (Cd) isotopes are known to fractionate during complexation with various
environmentally relevant surfaces and ligands. Our results, which were obtained using (i) …

Cadmium (Cd) is a micronutrient and a tracer of biological productivity and circulation in the
ocean. The correlation between dissolved Cd and the major algal nutrients in seawater has …

This study presents a high‐precision Cd isotope measurement method for soil and rock
reference materials using MC‐ICP‐MS with double spike correction. The effects of molecular …

Trace elements and their isotopes are being actively studied as powerful tracers in the
modern ocean and as proxies for the palaeocean. Although distributions and fractionations …

The distribution of Zn and Cd and their stable isotope ratios (δ 66 Zn and δ 114 Cd) were
measured on samples from the Eastern Subtropical South Pacific Zonal Transect (EPZT), US …

The biogeochemical cycling of cadmium (Cd) and its isotopes in the surface ocean is
dominated by biological uptake into phytoplankton, while regeneration of the sinking …