Extended Data Fig. 4: Mixing of MIS 4-3 sediments required to lower 10Be concentrations to LGM values.
From: Nonlinear forcing of climate on mountain denudation during glaciations

Proportion of sediments previously stored in MIS 4–3 moraines required to lower the MIS 4–3 10Be concentration to the average LGM value. CB1 correspond to mixing moraine sediments with a null 10Be concentration. CB2 correspond to mixing moraine sediments with a 10Be concentrations of 2.53 × 103 at.g−145.