Fig. 2: Benthic foraminiferal trace-metal temperature calibrations used in this study.
From: Relatively warm deep-water formation persisted in the Last Glacial Maximum
a–c, Trace metal versus estimated growth temperature for multiple species of benthic foraminifera that all show similar temperature sensitivities (a; Methods, Extended Data Fig. 2 and references therein), G. affinis20 (b) and H. elegans21 (c). The shading and dashed lines represent 95% confidence (CI) and 95% prediction (PI) intervals, respectively.
