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 …

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 …

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 …

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 …

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 …

Increasing ocean temperatures threaten coral reefs globally, but corals residing in habitats
that experience high thermal variability are thought to be better adapted to survive climate …

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 …

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 …