Extended Data Fig. 2: Core-top H. elegans Li/Ca, Mg/Ca, and Mg/Li vs. modern BWT.
From: Warmer shallow Atlantic during deglaciation and early Holocene due to weaker overturning circulation
Note that intra-lab Mg/Ca and Li/Ca offsets at WHOI have been corrected. To reconcile the Mg/Li inter-lab offset between WHOI and INSTAAR, a separate linear equation is fit to WHOI data and used for the down-core Mg/Li records generated at WHOI.
