A coral reef, ring- or horseshoe-shaped, enclosing a tropical lagoon. Most of the world’s atolls are found in the Indian and Pacific oceans, and are said to be sensitive to fluctuations in relative sea level—although Woodruffe et al. (1999) Marine Geol. 160, 1, in a study of West Island, Cocos, dispute this assumption. Single colony, semicircular corals (microatolls) grow to a level constrained by exposure at low spring tides (Spencer and Viles (2002) Geomorph. 48, 1–3).