The relationship between seawater temperature and the average Mg/Ca ratios in planktic
foraminifera is well established, providing an essential tool for reconstructing past ocean …

Abstract The Mg/Ca ratio of foraminiferal calcite is a widely used empirical proxy for ocean
temperature. Foraminiferal Mg/Ca‐temperature relationships are based on extant species …

As calcareous foraminifera precipitate their shells from the surrounding water mass, they are
the basis of most marine radiocarbon chronologies and paleo-proxies. Nevertheless, post …

The composition of planktonic foraminiferal (PF) calcite is routinely used to reconstruct
climate variability. However, PF ecology leaves a large imprint on the proxy signal: seasonal …

Most climate proxies of sea surface temperatures suffer from severe limitations when applied
to cold temperatures that characterize Arctic environments. These limitations prevent us from …

Trace and minor elements incorporated in foraminiferal shells are among the most used
proxies for reconstructing past environmental conditions. A prominent issue concerning …

Mg/Ca ratio paleothermometry in foraminifera is an important tool for the reconstruction and
interpretation of past environments. However, existing Mg/Ca: temperature relationships for …

The chemical composition of fossil foraminiferal shells (tests) is widely used as tracers for
past ocean chemistry. It is, therefore, important to understand how different (trace) elements …

The trace element (TE) and isotopic composition of calcareous foraminifera has been
invaluable in advancing our understanding of environmental change throughout the …

Neogloboquadrina pachyderma is the dominant species of planktonic foraminifera found in
polar waters and is therefore invaluable for paleoceanographic studies of the high latitudes …