Abstract
The reconstruction of past temperatures is often
achieved through measuring the Mg/Ca value of
foraminiferal test carbonate. The diversity in foraminiferal
Mg/Ca–temperature calibrations suggests that there is
also a biological control on this proxy. This study
presents a new Mg/Ca–temperature calibration for the
benthic foraminifer Bulimina marginata, based on cultures
under a range of temperatures (4–14
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