Marine Biology

, Volume 151, Issue 5, pp 1623–1631 | Cite as

Coral mortality following extreme low tides and high solar radiation

  • K. R. N. AnthonyEmail author
  • A. P. Kerswell
Research Article


Extreme tidal events are one of the most predictable natural disturbances in marine benthic habitats and are important determinants of zonation patterns in intertidal benthic communities. On coral reefs, spring low tides are recurrent disturbances, but are rarely reported to cause mass mortality. However, in years when extremely low tides coincide with high noon irradiances, they have the potential to cause widespread damage. Here, we report on such an event on a fringing coral reef in the central Great Barrier Reef (Australia) in September 2005. Visual surveys of colony mortality and bleaching status of more than 13,000 corals at 14 reef sites indicated that most coral taxa at wave-protected sites were severely affected by the event. Between 40 and 75% of colonies in the major coral taxa (Acropora, Porites, Faviidae, Mussidae and Pocilloporidae) were either bleached or suffered partial mortality. In contrast, corals at wave-exposed sites were largely unaffected (<1% of the corals were bleached), as periodic washing by waves prevented desiccation. Surveys along a 1–9 m depth gradient indicated that high coral mortality was confined to the tidal zone. However, 20–30% of faviid colonies were bleached throughout the depth range, suggesting that the increase in benthic irradiances during extreme low tides caused light stress in deeper water. Analyses of an 8-year dataset of tidal records for the area indicated that the combination of extended periods of aerial exposure and high irradiances occurs during May–September in most years, but that the event in September 2005 was the most severe. We argue that extreme low-tide, high-irradiance events are important structuring forces of intertidal coral reef communities, and can be as damaging as thermal stress events. Importantly, they occur at a time of year when risks from thermal stress, cyclones and monsoon-associated river run-off are minimal.


Coral Reef Great Barrier Reef Coral Community Coral Bleaching Coral Coloni 
These keywords were added by machine and not by the authors. This process is experimental and the keywords may be updated as the learning algorithm improves.



We thank D. Everett, A. Cole, J. Livingstone and J. Smith for assistance in the field and R. Pedersen and J. Broadbent (Maritime Safety Queensland) for providing the tidal data and A. Baird, M. Kosnik, W. Robbins and an anonymous reviewer for comments on the manuscript. The study was funded by the Australian Research Council through a Linkage grant. This is a contribution from the ARC Centre of Excellence for Coral Reef Studies.


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Copyright information

© Springer-Verlag 2007

Authors and Affiliations

  1. 1.School of Marine Biology and AquacultureJames Cook UniversityTownsvilleAustralia
  2. 2.Centre for Marine StudiesThe University of QueenslandBrisbaneAustralia

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