Seasonal and local spatial patterns in the upper thermal limits of corals on the inshore Central Great Barrier Reef

Abstract Experimental studies of the upper thermal limits of corals from Orpheus Island, an inshore reef in the central Great Barrier Reef, show that Acropora formosa has a 5-day 50%-bleaching threshold of between 31 and 32 °C in summer, only 2 to 3 °C higher than local mean summer temperatures (29 °C). Summer bleaching thresholds for Pocillopora damicornis and A. elseyi were 1 °C higher (between 32 and 33 °C). The winter bleaching threshold of Pocillopora damicornis was 1 °C lower than its summer threshold, indicating that seasonal acclimatisation may take place. This seasonal difference raises the possibility that at least some corals may be capable of short-term thermal acclimatisation. Neither P. damicornis nor A. elseyi showed habitat-specific (reef flat versus reef slope) differences in bleaching thresholds. Further, colonies of P. damicornis collected from sites 3 km apart also showed no difference in bleaching threshold despite populations of this species responding differently at these two sites during a natural bleaching event. The bleaching thresholds determined in this study are best considered as the maximum tolerable temperatures for local populations of these species because they were determined in the absence of additional stressors (e.g. high light) which often co-occur during natural bleaching events. We consider the 5-day 50% bleaching thresholds determined in these experiments to be fair indicators of upper thermal limits, because >50% of a sample population died when allowed to recover in situ. We found a delay of up to a month in the bleaching response of corals following thermal stress, a result that has implications for identifying the timing of stressful conditions in natural bleaching events.

[1]  S. Coles,et al.  Effects of temperature on the mortality and growth of Hawaiian reef corals , 1977 .

[2]  B. Brown,et al.  Coral bleaching: causes and consequences , 1997, Coral Reefs.

[3]  R. Bak,et al.  Effects of coral bleaching on tissue regeneration potential and colony survival , 1993 .

[4]  G. Ostrander,et al.  Coral bleaching: a potential biomarker of environmental stress. , 1997, Journal of toxicology and environmental health.

[5]  S. Coles,et al.  Thermal Tolerance in Tropical Versus Subtropical Pacific Reef Corals , 1976 .

[6]  R. Berkelmans,et al.  Large-scale bleaching of corals on the Great Barrier Reef , 1999, Coral Reefs.

[7]  D. Gleason,et al.  Ultraviolet radiation and coral bleaching , 1993, Nature.

[8]  C. H. Edmondson,et al.  The ecology of an Hawaiian coral reef , 1974 .

[9]  S. Coles,et al.  Synergistic effects of temperature, salinity and light on the hermatypic coral Montipora verrucosa , 1978 .

[10]  C. Yonge,et al.  STUDIES ON THE PHYSIOLOGY OF CORALS: IV. THE STRUCTURE, DISTRIBUTION AND PHYSIOLOGY OF THE ZOOXANTHELLAE , 1931 .

[11]  Knut Schmidt-Nielsen,et al.  Animal Physiology: Adaptation and Environment , 1985 .

[12]  S. Maritorena,et al.  A survey of environmental physico-chemical parameters during a minor coral mass bleaching event in Tahiti in 1993 , 1994 .

[13]  N. Knowlton,et al.  New taxonomy and niche partitioning on coral reefs: jack of all trades or master of some? , 1994, Trends in ecology & evolution.

[14]  N. Knowlton,et al.  Intraspecific diversity and ecological zonation in coral-algal symbiosis. , 1995, Proceedings of the National Academy of Sciences of the United States of America.

[15]  B. Hoeksema Control of bleaching in mushroom coral populations (Scleractinia: Fungiidae) in the Java Sea: stress tolerance and interference by life history strategy , 1991 .

[16]  O. Hoegh‐Guldberg,et al.  Periodic mass-bleaching and elevated sea temperatures: bleaching of outer reef slope communities in Moorea, French Polynesia , 1995 .

[17]  R. Buddemeier,et al.  CORAL BLEACHING AS AN ADAPTIVE MECHANISM : A TESTABLE HYPOTHESIS , 1993 .

[18]  T. Goreau Coral bleaching in Jamaica , 1990, Nature.