Seasonal fluctuations in the photosynthetic capacity of photosystem II in symbiotic dinoflagellates in the Caribbean reef-building coral <Emphasis Type="Italic">Montastraea</Emphasis>

The photosynthetic capacity of photosystem II (PS II) in symbiotic dinoflagellates (Symbiodinium sp.), as measured by analysis of chlorophyll fluorescence, was investigated in the primary Caribbean reef-building corals, Montastraea annularis and Montastraea faveolata, for 5 years and Montastraea franksi over 2 years in the Bahamas. Significant seasonal fluctuations in the quantum yield of charge separation (F_v/F_m) of PS II were found in all species at all depths, with the highest photosynthetic capacity consistently recorded between mid-winter and early spring and the lowest photosynthetic capacity occurring in the mid to late summer. Corals residing in shallow depths of 1-2 m showed the greatest fluctuations in F_v/F_m, whereas deeper corals (3-4 and 14 m depths) had consistently higher values of F_v/F_m. Densities of symbiotic dinoflagellates and photosynthetic pigments followed a similar pattern. Fluctuations of photosynthetic capacity showed a strong correlation with seasonal patterns of water temperature and light. Such seasonal shifts in photosynthetic capacity are most likely due to several biochemical processes in the algae that lead to alterations of both photoprotection and photodamage. While symbiont density changed significantly on a seasonal basis, visual signs of coral bleaching were noted only in the fall of 1995 and the spring and summer of 1998. Comparisons of photosynthetic capacity and the decrease in the number of symbionts and their subsequent recovery indicated that symbiont populations in this study had the ability to recover quickly following bleaching events, as long as continued physical perturbation (e.g. thermal stress) did not shorten the recovery phase. Large-scale bleaching events are best viewed as the end points of seasonal physiological variation in which photosynthetic capacity and density of symbiotic dinoflagellates are reduced to a lower level than during "non-bleaching" years.