“…As global seawater pH continues to decline, calcification by corals—the primary ecosystem providers—will become increasingly difficult (Albright et al., ; Andersson & Gledhill, ; Dove et al., ; Hoegh‐Guldberg et al., ; Shaw, Phinn, Tilbrook, & Steven, ). As shown in field (Albright et al., ; Shamberger et al., ; Shaw et al., ; Silverman et al., ) and mesocosm (Alsterberg, Eklöf, Gamfeldt, Havenhand, & Sundbäck, ; Dove et al., ; Page et al., ; Sarmento, Pinheiro, Montes, & Santos, ; Sarmento, Souza, Esteves, & Santos, ) studies, significant changes to reef chemistry, structure and benthic communities are already occurring with further negative prospects for reef resilience expected for the coming decades (Intergovernmental Panel on Climate Change [IPCC], ; Spalding & Brown, ). Predicting the impacts of changing ocean conditions on marine ecosystems requires a better understanding of community–habitat interactions, and the potential for compensatory mechanisms through ecological interactions to resist deleterious regime shifts in a future ocean (Alsterberg et al., ; Anthony, Diaz‐Pulido, Verlinden, Tilbrook, & Andersson, ; Dove et al., ; Ghedini, Russell, & Connell, ; Kleypas, Anthony, & Gattuso, ; Kroeker, Micheli, Gambi, & Martz, ; Nagelkerken & Munday, ; Page et al., ; Vinebrooke et al., ).…”