Extended Data Fig. 7. Influence of paleo-precipitation scenarios on spatial distribution of denudation rates.

Differences in annual mean precipitation between the Phanerozoic paleo-climate model of Li et al.⁹³ and the one from Valdes et al.¹⁵ using the CO₂ curve from Foster et al.⁶⁸ are presented on the left (drier predictions in Li et al.⁹³ range from yellow to red and wetter ones from cyan to dark blue). Simulated differences in erosion and deposition rates between the two scenarios using goSPL¹² show higher erosion with the Li et al.⁹³ simulation in blue and higher deposition in red.