Reef-building stony corals live in a mutually beneficial partnership with photosynthetic algae that is the core energetic driver of coral reefs. Stressful conditions such as high temperature lead to the disruption of this symbiosis known as coral bleaching, and eventual coral death (Brown, 1997). Climate change-related mass bleaching events have become increasingly common, affecting about 75% of coral reefs in Hawaiʻi and 93% of surveyed corals in the Great Barrier Reef, with over 50% mortality in some regions (Couch et al., 2017;Hoegh-Guldberg et al., 2015). Current climate-change mitigation measures (e.g., the Paris agreement), aiming to limit global warming to 2℃ are unlikely to effectively moderate impacts on coral reefs. As temperature stress events become more frequent and severe, most reefs are projected to face near-annual bleaching by mid-century, leaving these ecosystems under an imminent threat of collapse and