The early Eocene (56 to 48 million years ago) is inferred to have been the most recent time
that Earth's atmospheric CO 2 concentrations exceeded 1000 ppm. Global mean …

Planktonic foraminifera preserved in marine sediments archive the physical and chemical
conditions under which they built their shells. To interpret the paleoceanographic …

Boron isotope systematics indicate that boron incorporation into foraminiferal CaCO3 is
determined by the partition coefficient, KD (=), and [B (OH) 4−/HCO3−] seawater, providing …

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

Reliable temperature estimates from both surface and subsurface ocean waters are needed
to reconstruct past upper water column temperature gradients and past oceanic heat …

Oxygen isotopes are widely used in palaeoenvironmental and palaeoclimatic studies as
they record variations in the precipitation temperature of biogenic carbonates and …

Stable carbon isotopic (δ 13 C) minimum events have been widely described in marine
archives recording the properties of thermocline and intermediate waters during glacial …

We measured the oxygen isotopic composition of the deep‐dwelling foraminiferal species G.
inflata, G. truncatulinoides dextral and sinistral, and P. obliquiloculata in 29 modern core …

The intratest variation in the chemical composition of Globorotalia scitula and G. inflata
recovered from a sediment trap sample collected at 3000 m in the North Atlantic in early …

We present a species‐specific Mg/Ca‐calcification temperature calibration for Globorotalia
inflata from a suite of 38 core top samples from the South Atlantic (from 8° S to 49° S). G …