Temporal dynamics in coral bioindicators for water quality on coastal coral reefs of the Great Barrier Reef
Timothy F. Cooper A B F G , Peter V. Ridd C , Karin E. Ulstrup A D , Craig Humphrey A , Matthew Slivkoff E and Katharina E. Fabricius AA Australian Institute of Marine Science, PMB No. 3, Townsville MC, Townsville Qld 4810, Australia.
B School of Marine and Tropical Biology, and ARC Centre of Excellence for Coral Reef Studies, James Cook University, Townsville Qld 4811, Australia.
C School of Mathematics, Physics and IT, James Cook University, Townsville Qld 4811, Australia.
D Marine Biological Laboratory, Department of Biology, University of Copenhagen, Strandpromenaden 5, DK-3000 Helsingør, Denmark.
E School of Imaging and Applied Physics, Curtin University of Technology, Kent St, Bentley WA 6102, Australia.
F Current address: Australian Institute of Marine Science, Botany Building (M096), University of Western Australia, 35 Stirling Highway, Crawley WA 6009, Australia.
G Corresponding author. Email: t.cooper@aims.gov.au
Marine and Freshwater Research 59(8) 703-716 https://doi.org/10.1071/MF08016
Submitted: 26 January 2008 Accepted: 2 June 2008 Published: 22 August 2008
Abstract
There is a need to identify effective coral bioindicators that provide quantifiable links between changes in water quality and the condition of coastal coral reefs. Temporal variation in a range of coral bioindicators including symbiont density, concentration of chlorophyll a, skeletal density and colony brightness of Pocillopora damicornis, as well as colony brightness and density of macro-bioeroders of massive Porites spp. was examined for 2 years on a coastal coral reef of the Great Barrier Reef. The specificity to changes in water quality varied among bioindicators. For example, a 2.5-fold variation in symbiont density of P. damicornis was related strongly to mean 14-day sea surface temperature and seasonal changes in water quality, suggesting medium specificity to changes in water quality. In contrast, the density of macro-bioeroders in Porites did not vary seasonally but there were consistently more macro-bioeroders at the coastal than mid-shelf reference locations, suggesting high specificity of spatial differences in water quality. In situ measurements of benthic irradiance and turbidity allowed the quantification of potential stress thresholds for coastal corals. Our data suggest long-term turbidity >3 NTU leads to sublethal stress, whereas long-term turbidity >5 NTU corresponds to severe stress effects on corals at shallow depths.
Additional keywords: benthic irradiance, bioerosion, sea surface temperature, specificity, symbiont density, turbidity.
Acknowledgements
This study was supported by the Reef and Rainforest Research Centre through the Marine and Tropical Sciences Research Facility (MTSRF), joint contributions from the Co-operative Research Centre (CRC) for Coral Reefs and Rainforest CRC to the Catchment to Reef Program, and the Australian Institute of Marine Science. The research was undertaken in accordance with Marine Parks Permit G05/13484.1 (PVR) and G06/15571.1 (AIMS). We gratefully acknowledge the support provided in the field and laboratory from Ray Berkelmans, Joe Goiffre, Tim Hyndes, David McKinnon, Tim Phillips, Sven Uthicke, Jake van Oosterom and Madeleine van Oppen. We also thank two anonymous referees for comments that improved the manuscript.
Akaike, H. (1974). A new look at the statistical model identification. IEEE Transactions on Automatic Control 19, 716–723.
| Crossref | GoogleScholarGoogle Scholar |
Barnes, D. J. , and Lough, J. M. (1992). Systematic variations in the depth of skeleton occupied by coral tissue in massive colonies of Porites from the Great Barrier Reef. Journal of Experimental Marine Biology and Ecology 159, 113–128.
| Crossref | GoogleScholarGoogle Scholar |
Cooper, T. F. , Uthicke, S. , Humphrey, C. , and Fabricius, K. E. (2007). Gradients in water column nutrients, sediment parameters, irradiance and coral reef development in the Whitsunday Region, central Great Barrier Reef. Estuarine, Coastal and Shelf Science 74, 458–470.
| Crossref | GoogleScholarGoogle Scholar |
Fitt, W. K. , McFarland, F. K. , Warner, M. E. , and Chilcoat, G. C. (2000). Seasonal patterns of tissue biomass and densities of symbiotic dinoflagellates in reef corals and relation to coral bleaching. Limnology and Oceanography 45, 677–685.
Hill, R. , and Ralph, P. J. (2005). Diel and seasonal changes in fluorescence rise kinetics of three scleractinian corals. Functional Plant Biology 32, 549–559.
| Crossref | GoogleScholarGoogle Scholar |
Larcombe, P. , Ridd, P. V. , Prytz, A. , and Wilson, B. (1995). Factors controlling suspended sediment on inner-shelf coral reefs, Townsville, Australia. Coral Reefs 14, 163–171.
| Crossref | GoogleScholarGoogle Scholar |
Muscatine, L. , Falkowski, P. G. , Dubinsky, Z. , Cook, P. A. , and McCloskey, L. R. (1989). The effect of external nutrient resources on the population dynamics of zooxanthellae in a reef coral. Proceedings of the Royal Society of London. Series B. Biological Sciences 236, 311–324.
Ridd, P. V. , and Larcombe, P. (1994). Biofouling control for optical backscatter suspended sediment sensors. Marine Geology 116, 255–258.
| Crossref | GoogleScholarGoogle Scholar |
Warner, M. E. , Chilcoat, G. C. , McFarland, F. K. , and Fitt, W. K. (2002). Seasonal fluctuations in the photosynthetic capacity of photosystem II in symbiotic dinoflagellates in the Caribbean reef-building coral Montastraea. Marine Biology 141, 31–38.
| Crossref | GoogleScholarGoogle Scholar |
Winters, G. , Loya, Y. , and Beer, S. (2006). In situ measured seasonal variations in F-v/F-m of two common Red Sea corals. Coral Reefs 25, 593–598.
| Crossref | GoogleScholarGoogle Scholar |
Wolanski, E. , Fabricius, K. E. , Cooper, T. F. , and Humphrey, C. (2008). Wet season fine sediment dynamics on the inner shelf of the Great Barrier Reef. Estuarine, Coastal and Shelf Science 77, 755–762.
| Crossref | GoogleScholarGoogle Scholar |