The intracellular coral–dinoflagellate symbiosis is the engine that underpins the success of
coral reefs, one of the most diverse ecosystems on the planet. However, the breakdown of …

The Earth's oceans have absorbed more than 90% of the excess, climate change–induced
atmospheric heat. The resulting rise in oceanic temperatures affects all species and can …

Spatial and temporal patterns of future coral bleaching are uncertain, hampering global
conservation efforts to protect coral reefs against climate change. Our analysis of daily …

Increasingly frequent marine heatwaves are devastating coral reefs. Corals that survive
these extreme events must rapidly recover if they are to withstand subsequent events, and …

Anomalously high ocean temperatures have increased in frequency, intensity, and duration
over the last several decades because of greenhouse gas emissions that cause global …

Exposure to deoxygenation from climate warming and pollution is emerging as a
contributing factor of coral bleaching and mortality. However, the combined effects of heating …

Corals are being increasingly subjected to marine heatwaves. Theory suggests that
increasing the intensity of disturbances reduces recovery rates, which inspired us to …

The future of coral reefs in a warming world depends on corals' ability to recover from
bleaching, the loss of their symbiotic dinoflagellate algae (Symbiodiniaceae) during marine …

The Great Barrier Reef is the largest reef system in the modern ocean. To date, the influence
of temperature on the origin and long-term evolution of the Great Barrier Reef remains …

Selective breeding of resilient organisms is an emerging topic in marine conservation. It can
help us predict how species will adapt in the future and how we can help restore struggling …