Patterns of isotopic disequilibria in azooxanthellate coral skeletons

A specimen of Desmophyllum cristagalli, an azooxanthellate (non-photosynthetic) coral was intensively and systematically sampled on all interior and exterior coeval surfaces. Even though the coral grew at an almost-constant temperature of about 2.5 °C, δ18O varied by almost 3‰ and was up to 3.25‰ depleted with respect to aragonite–seawater oxygen isotope equilibrium. Contour maps of δ18O show that, although portions of the skeleton approached equilibrium, the location of those areas were unpredictable and were not associated with any readily identifiable characteristics, such as colour, texture or crystalline structure changes. The use of regression lines and intercepts will give the mean temperature experienced by individual corals (Smith et al., 2000, Palaios 15: 25), but the prospect of documenting temperature changes over the lifetime of an individual coral remains problematical. Because of the large and seemingly random degree of isotopic disequilibrium, several isotopic values from coeval skeletal material must be obtained for the determination of a single temperature. Although azooxanthellate corals have been shown to have growth banding, analogous to reef corals, the layers are thin and difficult to see with the naked eye, uneven and often discontinuous, rendering sampling for a `time series' impossible at present. Reasons for the degree of variation in the isotopic patterns remain unclear.