Early anthozoan ancestors emerge in Precambrian seas, laying groundwork for reef-building life.
Scleractinian and tabulate corals begin forming the earliest true reef structures in tropical seas.
Massive reef systems built by tabulate and rugose corals dominate warm shallow seas worldwide.
The Great Dying wipes out most reef-building corals and countless marine species.
Stony corals radiate across Triassic and Jurassic seas, forming the ancestors of today's reefs.
The world's largest coral reef system starts developing off the coast of northeastern Australia.
The Coral Triangle region becomes the richest marine biodiversity hotspot on Earth.
Early modern scientists debate whether coral is plant, mineral, or animal.
Darwin proposes his influential theory explaining atoll, barrier, and fringing reef formation through subsidence.
Rising ocean temperatures trigger unprecedented worldwide coral bleaching, devastating reef ecosystems.
Fish, mollusks, crustaceans, echinoderms and marine reptiles evolve alongside corals, turning reefs into some of the richest habitats on Earth.
Long before humans existed, coral reefs became bustling underwater cities. Ancient armored fish and trilobites moved among Paleozoic reefs, while later, brightly colored reef fish, giant clams, sea turtles, sharks, and countless invertebrates such as starfish, sea urchins, and crustaceans made reefs their home. Marine reptiles like ichthyosaurs and later marine mammals such as dugongs also frequented reef-adjacent waters. This immense biodiversity developed gradually over hundreds of millions of years, with different animal groups appearing, adapting, and sometimes vanishing as reef ecosystems rose and fell through mass extinctions and recoveries. The image of a coral reef teeming with fish schools, camouflaged octopuses, and grazing sea turtles reflects this long co-evolution of coral structures and the animals that depend on them.