“…Because the ocean pH naturally changes throughout seasons, along depth gradients, with productivity and other biological factors, marine micro‐organisms may have the physiological plasticity required to cope with the predicted levels of OA over the next 100 years (Joint, Doney, & Karl, ). This notion is supported by several studies showing stable coral prokaryotic community when shifted from ambient to high CO 2 partial pressure ( p CO 2 ) and therefore reduced sea water pH conditions (Meron et al., ; Webster, Negri, Botte, Laffy, & Flores, ; Zhou, Yuan, Cai, Zhang, & Tian, ). However, other studies have demonstrated that a reduced sea water pH can lead to the loss of Symbiodinium (coral bleaching) and trigger shifts from a healthy microbiome composition to a microbial community typically associated with diseased corals (Anthony, Kline, Diaz‐Pulido, Dove, & Hoegh‐Guldberg, ; Vega Thurber, Willner‐Hall, Rodriguez‐Mueller, Desnues, & Edwards, ; Meron et al., ; Webster, Negri, Flores, Humphrey, & Soo, ; Morrow, Bourne, Humphrey, Botte, & Laffy, ).…”