Members of many invertebrate groups live symbiotically with unicellular algae, but the symbiosis between corals amid dinoflagellate algae (zooxanthelhae) is espe cially interesting because it occurs in all species of tropical reef-buildimig corals ( see reviews by Droop, 1963 ; Yonge, 1963 ; McLaughlin and Zahl, 1966) . Moreover, a significant effect of the algae om-m time physiology of corals has been clearly demon strated and quantified : Corals with symbiotic algae calcify n-many timies faster iii light than in darkness, while corals which have lost their zooxanthelhae calcify at rates which are slower and unaffected by light (Kawaguti and Sakumoto, 1948; Goreau, 1959 ; Goreau and Goreau, 1959) . In the light, photosynthesis by zoo xanthellae must soniehow lead to higher rates of calcification by corals. Three mechanism-mishave been proposed to explain how zooxamithehlae imifluemice coral calcification : ( 1) removal of carbon dioxide in photosymithiesis directly favors chemical equilibria leading to the precipitation of calcium-micarbonate (Goreau, 1959) ; (2) algal removal of phosphates, which n-mayact as crystal poisomis, enhances crystallization of calcium carbonate (Simkiss, 1964a, 1964b) ; and (3) orgamiic products of photosynthesis, either specific mi-materialsrequired for skeletogenesis, or nutrients or general energy sources supplied to the coral, ierm-m-mit faster calcifica tion (Goreau, 1959 ; Wainwright, 1963) . So far, there has been i-moexperimental evidence which conclusively supports or eliminates one hypothesis or another. One observation appears to be inconsistent with current ideas about the inti nate relationship between algal photosynthesis and coral calcification. In tFmestag horn coral, Acropora cervicornis ( Fig. 1) , as in other bramiching forms, calcification rates are highest in the tips, decreasing progressively towards the base (Goreau and Goreau, 1959) . However, very few symbiotic algae are found iii the tips, their numbers increasing towards the base. Where abumidanit, they give the coral a deep brown color, contrasting sharply' with the whiteness of the almost algae-free tips (Figs. 1 and 2). We undertook a study of ti-merapidly calcifying tips in order to clarify the problem of how the algae stimulate coral calcification rates.