Foraminiferal tests are a common component of many marine sediments. The oxygen
isotope ratio (δ18O) of test calcite is frequently used to reconstruct aspects of their life …

Recent paleoclimatic work on terrestrial and marine deposits from Asia and the Indian
Ocean has indicated abrupt changes in the strength of the Asian monsoon during the last …

Paleoclimatic records from the Bay of Bengal are rare. We reconstruct the sea-surface
temperature (SST) and salinity from paired δ18O and Mg/Ca measurements in planktonic …

Differential carbon and oxygen stable isotope (δ13C and δ18O) fractionation between
planktonic foraminifera test calcite and sea water related to ecology and life stage confound …

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

In order to consistently approximate the thermal vertical structure of past upper water
columns, Mg/Ca ratios of eight planktonic foraminiferal species with different preferential …

The reconstruction of past ocean temperatures is fundamental to the study of past climate
changes, therefore considerable effort has been invested in developing proxies for seawater …

δ18O values of nine tropical–subtropical planktonic foraminiferal species with different
preferential habitat depths collected from 62 core–top samples along an east–west transect …

Processes and causes of biotic and environmental change at the Triassic–Jurassic transition
remain controversial, partly because of a scarcity of Triassic–Jurassic boundary sections …

Past variability in upper ocean thermocline depth is commonly estimated from the
abundance of different species of planktonic organisms or the difference in oxygen isotopic …