Coral Reefs

, Volume 24, Issue 3, pp 422–434 | Cite as

Cross-shelf differences in the pattern and pace of bioerosion of experimental carbonate substrates exposed for 3 years on the northern Great Barrier Reef, Australia

  • A. Tribollet
  • S. Golubic


Patterns of bioerosion of dead corals and rubbles on the northern Great Barrier Reef were studied by using blocks of the massive coral Porites experimentally exposed at six sites, located on an inshore–offshore profile, for 1 year and 3 years. Rates of microbioerosion by microborers, grazing by fish, and macrobioerosion by filter-feeding organisms were simultaneously evaluated using image analysis. Microbioerosion, grazing, and total bioerosion were lower at reefs near the Queensland coast than at the edge of the continental shelf (1.81 kg m−2 and 6.07 kg m−2 after 3 years of exposure respectively, for total bioerosion). The opposite pattern was observed for macrobioerosion. Bioaccretion was negligible. These patterns were evident after 1 year of exposure, and became enhanced after 3 years. Microborers were established and were the main agent of bioerosion after 1 year of exposure, and as the principal support for grazing, continued to be the main cause of carbonate loss after 3 years. Full grazing activity and establishment of a mature community of macroborers required more than 1 year of exposure. After 1 year, macroborers and grazers were the second most important agents of bioerosion on both inshore and offshore reefs. However, after 3 years, grazers became the main agents at all sites except at the inshore sites, where macroborers were the principal agents. Because the contribution of microborers, grazers, and macroborers to bioerosion varies in space and time, we suggest that the estimation of reef carbonate budgets need to take in account the activities of all bioerosion agents.


Total bioerosion Microbioerosion Cross-shelf patterns Great Barrier Reef Carbonate budget 



This study was made possible by grants from the French–Australian Cooperation in Marine Sciences and the French Program PNRCO about coral reefs, and by GBRMPA for allowing us to collect coral. We would like to thank M. Peyrot-Clausade, P. Hutchings and A.J. Underwood for having made this study possible and for their help. We also thank the following companies and persons for their assistance in the field or providing logistical support: Undersea Explorer company and its crew at Port Douglas, L. Vail and A. Hoggett of Lizard Island Marine Station, K. Atwood of the Australian Museum, Sydney, C. Marschal and C. Bezac of the Marine Station d’Endoume, Marseille. We thank also C. Langdon and Columbia University of the city of New York, E. Hochberg, J. Le Campion and T. Le Campion for their technical support, help and reviews.


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Copyright information

© Springer-Verlag 2005

Authors and Affiliations

  1. 1.Centre d’Océanologie de Marseille, UMR CNRS 6540Université de la MéditerranéeMarseilleFrance
  2. 2. St Cyr/LoireFrance
  3. 3.Department of BiologyBoston UniversityBostonUSA

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