Shown are comparisons for four ocean drilling sites for which surface ocean pH has been reconstructed across the PETM (Fig. 2) – 401, 865, 1209, and 1263 (this study and ref. 20). Their paleo locations in the cGENIE Earth system model are shown to the side (panel q). Model-data comparisons are made for: (i) wt% CaCO3 (far LH panel for each site), (ii) δ13C of bulk carbonate (second-from-left series of panels), and (iii) surface ocean pH (third-from-left series of panels). To provide an orientation in time with regard to the evolution across the PETM event, the farthest-right series of panels shows the projected evolution of atmospheric δ13C of CO2 in the model. For wt% CaCO3 and δ13C of bulk carbonate, model points (resolved at 1 cm resolution) are plotted as filled yellow circles. Model-projected pH (global and annual mean, as per shown in Fig. 3j and Extended Data Fig. 6a) and atmospheric δ13C of CO2 are shown as continuous red lines. In all cases, observed data values are shown as stars (*). The age models for Sites 865, 1209 and 1263 employing original relative age model constraints20 used to convert from model-simulated sediment depth (resolved at 1 cm intervals) at each location in the cGENIE Earth system model, are calculated using a constant detrital flux accumulation rate. The observed data are plotting on their respective site 690-derived age models25. Both model and data age scales are synchronized to age zero at PETM onset (horizontal line). See SI for details.