Coral reefs cover less than one percent of the ocean floor but support approximately 25 percent of all marine species. They are among the most biodiverse ecosystems on Earth, providing habitat, nursery grounds, and food sources for fish, molluscs, crustaceans, and thousands of other organisms. Beyond their ecological role, reefs protect coastlines from wave erosion, support fishing and tourism industries, and are the source of compounds used in medical research.
Coral reefs are under severe stress from multiple pressures: ocean warming causes bleaching, in which corals expel the symbiotic algae (zooxanthellae) that provide their colour and much of their nutrition; ocean acidification from dissolved CO2 weakens the calcium carbonate skeletons of corals; sedimentation from land-based activities smothers reefs; and overfishing removes the fish species that keep reef-damaging organisms (such as crown-of-thorns starfish and algae) in check.
The interaction of these stressors is cumulative: a reef weakened by bleaching is less able to recover from a disease outbreak or a cyclone. Restoration efforts — including coral farming and transplantation — have shown promise at small scales but face the same pressures that caused the degradation in the first place. Without addressing the underlying drivers, particularly ocean warming, restoration cannot reverse the trend.