“…However, we found no strong (unambiguous) evidence for such a potential link between inferred historical changes in CO 2 (or temperature) and diversification across the full tree, and not at all for subclade C (Table S5). However, the crown age of this subclade and its corresponding shifts towards CAM and into the Eastern Lowlands (c. 7.36 Ma) remarkably coincide with the strengthening of the Indian Summer monsoon (c. 7 Ma; Gupta et al, 2015), resulting in increased moisture levels throughout eastern Madagascar and, possibly, the establishment of the Northwest 'Sambirano' (Yoder & Nowak, 2006;Buerki et al, 2013;Andriananjamanantsoa et al, 2016). In addition, these changes in monsoon climate could have created environmental instability across the comparatively older sub-humid and humid forest biomes of the Central Highlands and Eastern Coast of Madagascar, respectively (Cornet, 1974;Buerki et al, 2013).…”