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Advances in the aquatic sciences
RESEARCH ARTICLE

Coral mucus release and following particle trapping contribute to rapid nutrient recycling in a Northern Red Sea fringing reef

Florian W. Mayer A and Christian Wild A B
+ Author Affiliations
- Author Affiliations

A Coral Reef Ecology Work Group (CORE), Center of Geobiology and Biodiversity Research & Department of Earth and Environmental Sciences, Ludwig-Maximilians-University, 80333 Munich, Germany.

B Corresponding author. Email: c.wild@lrz.uni-muenchen.de

Marine and Freshwater Research 61(9) 1006-1014 https://doi.org/10.1071/MF09250
Submitted: 2 October 2009  Accepted: 19 February 2010   Published: 23 September 2010

Abstract

Mucus released by corals can function as an important energy carrier and particle trap in reef ecosystems with strong tidal currents. In fringing reefs with calm conditions, these processes may occur on smaller spatial scales. Observations of coral mucus dynamics in the Northern Red Sea revealed highly particle-enriched and negatively buoyant mucus strings attached to ∼27% of coral colonies for up to 79 min. Mucus strings of the scleractinian coral genus Acropora exhibited three orders of magnitude higher particulate organic carbon and nitrogen concentrations when compared with freshly released coral mucus, which confirms efficient particle trapping. After detachment from the coral surface, more than 95% of mucus strings rapidly descended to the reef sea floor within less than 1 m. Such mucus-induced transport may account for 21–25% of the total sedimentary particulate organic matter supply. In situ and laboratory analyses of planktonic and benthic microbial degradation of mucus strings showed high rates of up to 16 and 26% particulate organic carbon h–1, respectively. These findings suggest a newly discovered, tight sediment–water coupling mechanism via coral mucus that may contribute to rapid nutrient recycling in oligotrophic fringing coral reefs.

Additional keywords: coral reef ecosystem, microbial degradation, sediment–water coupling.


Acknowledgements

We would like to thank Carin Jantzen, Malik Naumann and Andreas Haas of the Coral Reef Ecology Work Group (CORE) in Munich for sampling assistance and Chris Williams for language counselling. Christoph Mayr (GeoBio-Center Munich) is acknowledged for POM analysis, as are the staff of Marine Science Station in Aqaba, Jordan, for welcoming us during the two expeditions. Editor Professor Andrew Boulton and two anonymous referees are acknowledged for their help in improving the manuscript. This work was funded by German Research Foundation (DFG) grant Wi 2677/2-1 and supported by a PhD stipend to Florian Mayer from FAZIT Foundation, Frankfurt, Germany.


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