Coral growth rates and environmental control of density banding

Abstract

Linear and mass growth rates are compared for the massive coral species Favia pallida (Dana), Goniastrea retiformis (Lamarck), and Porites lutea Milne Edwards & Haime at Enewetak Atoll. Marshall Islands. Goniastrea retiformis is the densest of the three species and has an intermediate growth rate; Porites lutea grows more rapidly. All three grow indeterminately at a declining rate with increasing depth. The high-density portion of annual band couplets is produced during the late summer and fall when water temperatures are highest and possibly the availability of light is reduced, and the low density portion is formed during periods of seasonally lower water temperatures and possibly higher availability of light. A similar pattern is found in three massive coral species from Belize. The high density portions of annual bands account for a greater proportion of linear and mass growth in deeper water and in corals with relatively slow growth rates. I predict that linear growth rates will be highest where conditions are most favorable for deposition of the low density portion. Geographical patterns of coral density banding based on the literature are discussed and a model is proposed relating the interplay of light availability and water temperature to the production of high and low density skeletal bands.