Corals are like greenhouses growing millions of symbiont algae inside their cells which provide the coral with more than 90% of its daily energy requirement. The coral can be viewed as an intricate optical machine and its interaction with visible light is one of the key factors in the coral life cycle and bleaching episodes. The coral consists of two compartments: 1) the living tissue where the host photoprotective pigments and the symbiont algae with all its photosynthetic pigments are contained, and 2) the skeleton, a highly reflective limestone structure secreted by the coral polyp in a species-specific manner and affected by local environmental factors.
Coral skeletons are highly scattering in the upper ~200 μm of the skeleton layer (measured as ‘microscopic’ reduced coefficient, µSʹ,m ) and effectively amplify and homogenize the ambient light-field of their endosymbiotic dinoflagellates. This effect enhances productivity of the symbiosis, but also contributes to the likelihood of catastrophic dissociation as densities of light-absorbing symbionts decrease and light levels for the remaining symbionts rapidly increase.
We are studying light transport and scattering in coral to better understand its role on coral physiology and coral bleaching susceptibility. We are using photophysiological techniques, light scattering models and experiments, and non-invasive imaging techniques such as Inverse Spectroscopic Optical Coherence Tomography (ISOCT).