The quantitative reconstruction of past seawater salinity has yet to be achieved, and the
search for a direct and independent salinity proxy is ongoing. Recent culture and field …

Boron isotope systematics of planktonic foraminifera from core-top sediments and culture
experiments have been studied to investigate the sensitivity of δ 11 B of calcite tests to …

Seawater chemistry exerts an important control on the incorporation of trace elements into
the shells of marine calcifying organisms. Variability in the major ion chemistry of seawater is …

In this study we analyzed the impact of seawater carbonate chemistry on the incorporation of
elements in both hyaline and porcelaneous larger benthic foraminifera. We observed a …

Mg/Ca palaeothermometry in foraminiferal calcite is a widely applied tool in
palaeoceanography. However, our understanding of the effects of planktic foraminiferal …

We present modern B/Ca core-top calibrations for the epifaunal benthic foraminifer
Nuttallides umbonifera and the infaunal Oridorsalis umbonatus to test whether B/Ca values …

Measurement of elemental ratios (E/Ca) has been performed in two symbiont‐bearing
species of high‐Mg calcite benthic foraminifers (hyaline, Baculogypsina sphaerulata and …

Sulfur (S) incorporation in foraminiferal shells is hypothesized to change with carbonate ion
concentration [CO 3 2−], due to substitution of sulfate for carbonate ions in the calcite crystal …

We present the first trace metal partition coefficients obtained from reproducing cultures of
deep-sea benthic foraminifera. Paleoceanographically important species, including juvenile …

The trace elemental composition of foraminiferal shell calcite is known to reflect the
environment in which the shell was precipitated. Whereas conservative elements …