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9 - The impact of weather and climate extremes on coral growth

Published online by Cambridge University Press:  14 September 2009

By
M. James C. Crabbe ,
Emma L. L. Walker  and
David B. Stephenson
Edited by
Henry F. Diaz  and
Richard J. Murnane
M. James C. Crabbe
Affiliation:
Luton Institute of Research in the Applied Natural Sciences, Faculty of Creative Arts, Technologies and Science, University of Bedfordshire, Park Square, Luton LU1 3JU, UK
Emma L. L. Walker
Affiliation:
Department of Meteorology, University of Reading, Early Gate, Reading RG6 6BB, UK
David B. Stephenson
Affiliation:
Department of Meteorology, University of Reading, Early Gate, Reading RG6 6BB, UK
Henry F. Diaz
Affiliation:
National Oceanic and Atmospheric Administration, District of Columbia
Richard J. Murnane
Affiliation:
Bermuda Biological Station for Research, Garrett Park, Maryland
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Summary

Condensed summary

Coral reefs are complex underwater ecosystems that are particularly vulnerable to climate extremes. In this chapter, we review the meteorological processes that influence corals and their growth, illustrate a number of methods for growth rate modeling, and show how climate extremes can affect growth rates. We then provide two examples of detailed modeling of coral colony growth as a function of climate in the Caribbean, for reefs off the coasts of Jamaica and Curaçao. For the Jamaican reefs, non-branching coral recruitment was inversely correlated with storm severity. For the reefs off Curaçao, the only significant correlation, which was negative, was the maximum daily temperature with a 30-day moving average applied (p-value of 0.002), suggesting that during the measurement period, temperatures rose to values higher than optimum for growth, but not sufficiently high to cause bleaching.

Our results show that hurricanes and severe storms can limit the recruitment and survival of massive coral colonies, and that small changes in temperature can significantly influence branching coral growth rates. Even for the simple exponential growth models, it is possible to introduce parameters for climate variables and climate change that should be useful predictively. Future studies will link climate modeling with environmental genetics and studies on symbiont diversity.

Introduction

The deeps have music soft and low

When winds awake the airy spry,

It lures me, lures me on to go

And see the land where corals lie.

The land, the land where corals lie.

(Text by Richard Garnett (1835–1906). Set by Sir Edward Elgar (1857–1934), Op. 37, first performance 1899, from Sea Pictures, no. 4.)
Type
Chapter
Information
Climate Extremes and Society , pp. 165 - 188
Publisher: Cambridge University Press
Print publication year: 2008

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References

Baird, A. H., and Marshall, P. A. (2002). Mortality, growth and reproduction in Scleractinian corals following bleaching on the Great Barrier Reef. Marine Ecology Progress Series, 237, 133–41.CrossRefGoogle Scholar
Bak, R. P. M. (1976). The growth of coral colonies and the importance of crustose coralline algae and burrowing sponges in relation with carbonate accumulation. Netherlands Journal of Sea Research, 10, 285–337.CrossRefGoogle Scholar
Baker, A. C., Stargert, C. J., McClanahan, T. R., and Glynn, P. W. (2004). Corals' adaptive response to climate change. Nature, 430, 741.CrossRefGoogle ScholarPubMed
Bessat, F., and Buiges, D. (2001). Two centuries of variation in coral growth in a massive Porites colony from Moorea (French Polynesia): a response of ocean-atmosphere variability from south central Pacific. Palaeogeography, Palaeoclimatology, Palaeoecology, 175, 381–92.CrossRefGoogle Scholar
Birkeland, C. (1977). The importance of rate of biomass accumulation in early successional stages of benthic communities to the survival of coral recruits. Proceedings of the Third International Coral Reef Symposium, pp. 15–21.Google Scholar
Birkeland, C. (1997). Introduction. In Life and Death of Coral Reefs, ed. Birkeland, C.. New York: Chapman & Hall, pp. 1–12.CrossRefGoogle Scholar
Bosscher, H., and Schlager, W. (1992). Computer simulation of reef growth. Sedimentology, 39, 503–12.CrossRefGoogle Scholar
Brown, B. E. (1997). Adaptations of reef corals to physical environmental stress. Advances in Marine Biology, 31, 221–99.CrossRefGoogle Scholar
Buddemeier, R. W., Kleypas, J. A., and Aronson, R. B. (2004). Coral Reefs and Global Climate Change: Potential Contributions of Climate Change to Stresses on Coral Reef Ecosystems. Report, Pew Center on Global Climate Change, Arlington, VA.
Burke, L., and Maidens, J. (2004) Reefs at Risk in the Caribbean. Washington, D.C.: World Resources Institute.Google Scholar
Caldeira, K., and Wickett, M. E. (2003). Anthropogenic carbon and ocean pH. Nature, 425, 365.CrossRefGoogle ScholarPubMed
Carlin, J. P., Humphries, S., Crabbe, M. J. C., and Mazet, F. (2006). Zooxanthellae diversity in the Ningaloo Reef tract, western Australia. Abstracts of the 7th Reef Conservation UK Meeting, 6.Google Scholar
Chadwick-Furman, N. E. (1996). Reef coral diversity and global change. Global Change Biology, 2, 559–68.CrossRefGoogle Scholar
Chalker, B. E. (1981). Simulating light-saturation curves for photosynthesis and calcification by reef-building corals. Marine Biology, 63, 135–41.CrossRefGoogle Scholar
Chalker, B. E., Barnes, D. J., Dunlop, W. C., and Jokiel, P. L. (1988). Light and reef building corals. Interdisciplinary Science Review, 13, 222–37.CrossRefGoogle Scholar
Costanza, R., D'Arge, R., Groot, R., et al. (1997). The value of the world's ecosystem services and natural capital. Nature, 387, 253–60.CrossRefGoogle Scholar
Crabbe, M. J. C. (1988). Simple graphical methods for use with complex ligand binding and enzyme mechanisms. Federation of European Biochemical Societies Letters, 235, 183–8.CrossRefGoogle ScholarPubMed
Crabbe, M. J. C. (2003). A novel method for the transport and analysis of genetic material from polyps and zooxanthellae of Scleractinian corals. Journal of Biochemical and Biophysical Methods, 57, 171–6.CrossRefGoogle ScholarPubMed
Crabbe, M. J. C. (2006). Challenges for sustainability in cultures where regard for the future may not be present. Sustainability: Science, Practice and Policy, 2, http://ejournal.nbii.org/progress/2006fall/communityessay.crabbe.html.Google Scholar
Crabbe, M. J. C. (2007). Global warming and coral reefs: modeling the effect of temperature on Acropora palmata colony growth. Computational Biology and Chemistry, 31, 294–7.CrossRefGoogle Scholar
Crabbe, M. J. C., and Carlin, J. P. (2004). Zooxanthellae clade populations in corals. Abstracts of the 38th Population Genetics Group, 6.Google Scholar
Crabbe, M. J. C., and Carlin, J. P. (2007). Industrial sedimentation lowers coral growth rates in a turbid lagoon environment, Discovery Bay, Jamaica, International Journal of Integrative Biology, 1, 37–40.Google Scholar
Crabbe, M. J. C., and Smith, D. J. (2002). Comparison of two reef sites in the Wakatobi Marine National Park (SE Sulawesi, Indonesia) using digital image analysis. Coral Reefs, 21, 242–4.CrossRefGoogle Scholar
Crabbe, M. J. C., and Smith, D. J. (2003). Computer modeling and estimation of recruitment patterns of non-branching coral colonies at three sites in the Wakatobi Marine Park, SE Sulawesi, Indonesia: implications for coral reef conservation. Computational Biology and Chemistry, 27, 17–27.CrossRefGoogle Scholar
Crabbe, M. J. C., and Smith, D. J. (2005). Sediment impacts on growth rates of Acropora and Porites corals from fringing reefs of Sulawesi, Indonesia. Coral Reefs, 24, 437–41.CrossRefGoogle Scholar
Crabbe, M. J. C., and Smith, D. J. (2006). Modelling variations in corallite morphology of Galaxea fascicularis coral colonies with depth and light on coastal fringing reefs in the Wakatobi Marine National Park (SE Sulawesi, Indonesia). Computational Biology and Chemistry, 30, 155–9.CrossRefGoogle Scholar
Crabbe, M. J. C., Karaviotis, S., and Smith, D. J. (2004). Preliminary comparison of three coral reef sites in the Wakatobi Marine National Park (SE Sulawesi, Indonesia): estimated recruitment dates compared with Discovery Bay, Jamaica. Bulletin of Marine Science, 74, 469–76.Google Scholar
Crabbe, M. J. C., Mendes, J. M., and Warner, G. F. (2002). Lack of recruitment of non-branching corals in Discovery Bay is linked to severe storms. Bulletin of Marine Science, 70, 939–45.Google Scholar
Crabbe, M. J. C., Wilson, M. E. J., and Smith, D. J. (2006). Quaternary corals from reefs in the Wakatobi Marine National Park, SE Sulawesi, Indonesia, show similar growth rates to modern corals from the same area. Journal of Quaternary Science, 21, published online: 12 May 2006. doi:10.1002/jqs.1011.CrossRefGoogle Scholar
Crabbe, M. J. C., Martinez, E., Garcia, C., Chub, J., Castro, L., and Guy, J. (2008). Growth modeling indicates hurricanes and severe storms are linked to low coral recruitment in the Caribbean. Marine Environmental Research (in press).CrossRefGoogle Scholar
Dodge, R. E., and Lang, J. C. (1983). Environmental correlates of hermatypic coral (Montastrea annularis) growth on the East Flower Gardens Bank, northwest Gulf of Mexico. Limnology and Oceanography, 28, 228–40.CrossRefGoogle Scholar
Dodge, R. E., and Vaisnys, J. R. (1975). Hermatypic coral growth banding as an environmental recorder. Nature, 258, 706–8.CrossRefGoogle Scholar
Done, T. J. (1999). Coral communities adaptability to environmental change at the scales of regions, reefs and reef zones. American Zoologist, 39, 66–79.CrossRefGoogle Scholar
Feely, R. A., Sabine, C. L., Lee, K., Berelson, W., Kleypas, J., Fabry, V. J., and Millero, F. J. (2004). Impact of anthropogenic CO2 on the CaCO3 system in the oceans. Science, 305, 362–6.CrossRefGoogle ScholarPubMed
Gleason, M. G., and Wellington, G. M. (1993). Ultraviolet radiation and coral bleaching. Nature, 365, 836–8.CrossRefGoogle Scholar
Goulet, T. L. (2006) Most corals may not change their symbionts. Marine Ecology Progress Series, 321, 1–7.CrossRefGoogle Scholar
Graus, R. R., Macintyre, I. G., and Herchenroder, B. E. (1984). Computer simulation of the reef zonation at Discovery Bay, Jamaica: hurricane disruption and long-term physical oceanographic controls. Coral Reefs, 3, 59–68.CrossRefGoogle Scholar
Grigg, R. W. (1981). Coral reef development at high latitudes in Hawaii. Proceedings of the Fourth International Coral Reef Symposium, Manila, 1, 687–93.Google Scholar
Grigg, R. W. (1997). Paleoceanography of coral reefs in the Hawaiian-Emperor Chain – revisited. Coral Reefs, 16, S33–8.CrossRefGoogle Scholar
Guinotte, J. M., Buddemeier, R. W., and Kleypas, J. A. (2003). Future coral reef habitat marginality: temporal and spatial effects of climate change in the Pacific basin. Coral Reefs, 22, 551–8.CrossRefGoogle Scholar
Hoegh-Guldberg, O. (1999). Climate change, coral bleaching and the future of the world's coral reefs. Marine Freshwater Research, 50, 839–66.CrossRefGoogle Scholar
Hubbard, D. K. (1997). Reefs as dynamic systems. In Life and Death of Coral Reefs, ed. Birkeland, C.. New York: Chapman and Hall, pp. 43–67.CrossRefGoogle Scholar
Hubbard, D. K., and Scaturo, D. (1985). Growth rates of seven species of Scleractinian corals from Cane Bay and Salt River, St. Croix, U.S. Virgin Islands. Bulletin of Marine Science, 36, 325–38.Google Scholar
Hughes, T. P., Baird, A. H., Bellwood, D. R., et al. (2003). Climate change, human impacts, and the resilience of coral reefs. Science, 301, 929–33.CrossRefGoogle ScholarPubMed
Intergovernmental Panel on Climate Change (IPCC) (2001). Third Assessment Report of the Intergovernmental Panel on Climate Change, 2001: The Scientific Basis. Cambridge, UK: Cambridge University Press.
Intergovernmental Panel on Climate Change (IPCC) (2007). Summary for Policymakers from Working Group 1. http://www.ipcc.ch/SPM2 feb 07.pdf
Jiménez, C. and Cortés, J. (2003). Growth of seven species of Scleractinian corals in an upwelling environment of the eastern Pacific (Golfo De Papagayo, Costa Rica). Bulletin of Marine Science, 72, 187–98.Google Scholar
Jokiel, P. L. (2006). Impact of storm waves and storm floods on Hawaiian reefs. Proceedings of the 10th International Coral Reef Symposium, pp. 390–8.Google Scholar
Kleypas, J. A. (1997). Modelled estimates of global reef habitat and carbonate production since the last glacial maximum. Paleoceanography, 12, 533–45.CrossRefGoogle Scholar
Kleypas, J. A., Buddemeier, R. W., Archer, D., Gattuso, J.-P., Langdon, C., and Opdyke, B. N. (1999a). Geochemical consequences of increased atmospheric carbon dioxide on coral reefs. Science, 284, 118–20.CrossRefGoogle Scholar
Kleypas, J. A., McManus, J. W., Lambert, A. N., and Meñez, A. (1999b). Environmental limits to coral reef development: Where do we draw the line?American Zoologist, 39, 146–59.CrossRefGoogle Scholar
Knowlton, N., Lang, J. C., and Keller, B. D. (1988). Fates of staghorn coral isolates on hurricane-damaged reefs in Jamaica: the role of predators. Proceedings of the Sixth International Coral Reef Symposium, 2, 83–8.Google Scholar
Knowlton, N., Lang, J. C., Rooney, M. C., and Clifford, P. (1981). Evidence for delayed mortality in hurricane-damaged Jamaican staghorn corals. Nature, 294, 251–2.CrossRefGoogle Scholar
Leclerq, N., Gattuso, J.-P., and Jaubert, J. (2000). CO2 partial pressure controls and the calcification rate of a coral community. Global Change Biology, 6, 329–34.CrossRefGoogle Scholar
Lirman, D. (2003). A simulation of the population dynamics of the branching coral Acropora palmata: effects of storm intensity and frequency. Ecological Modelling, 161, 167–80.CrossRefGoogle Scholar
Lough, J. M. (2000). Unprecedented thermal stress to coral reefs?Geophysical Research Letters, 27, 3901–4.CrossRefGoogle Scholar
Lough, J. M., and Barnes, D. J. (2000). Environmental controls on growth of the massive coral Porites. Journal of Experimental Marine Biology, 245, 225–43.CrossRefGoogle ScholarPubMed
McFarlane, S. A., and Evans, K. F. (2004). Clouds and shortwave fluxes at Nauru. Part II: Shortwave flux closure. Journal of Atmospheric Sciences, 61, 2602–15.CrossRefGoogle Scholar
Mieog, J. C., Oppen, M. J. H., Cantin, N. E., Stam, W. T., and Olsen, J. L. (2007). Real-time PCR reveals a high incidence of Symbiodinium clade D at low levels in four scleractinian corals across the Great Barrier Reef: implications for symbiont shuffling. Coral Reefs, 26, 449–57.CrossRefGoogle Scholar
Muller-Parker, G, and D'Elia, C. F. (1997). Interactions between corals and their symbiotic alga. In Life and Death of Coral Reefs, ed. Birkeland, C.. New York: Chapman and Hall, pp. 96–112.CrossRefGoogle Scholar
Nie, B., Chen, T., Liang, M., Wang, Y., Zhong, J., and Zhu, Y. (1997). Relationship between coral growth rate and sea surface temperature in the northern part of the South China Sea during the past 100 years. Science in China (Series D), 40, 173–82.CrossRefGoogle Scholar
Rowan, R. (2004). Thermal adaptation in reef coral symbionts. Nature, 430, 742.CrossRefGoogle ScholarPubMed
Scoffin, T. P., Tudhope, A. W., Brown, B. E., Chansang, H., and Cheeney, R. F. (1992). Patterns and possible environmental controls of skeletogenesis of Porites lutea, South Thailand. Coral Reefs, 11, 1–11.CrossRefGoogle Scholar
Sheppard, C. R. C. (2003). Predicted recurrences of mass coral mortality in the Indian Ocean. Nature, 425, 294–297.CrossRefGoogle ScholarPubMed
Slowey, N. C., and Crowley, T. J. (1995). Interdecadal variability of Northern Hemisphere circulation recorded by Gulf of Mexico corals. Geophysical Research Letters, 22, 2345–8.CrossRefGoogle Scholar
Stat, M., Carter, D. and Hoegh-Guldberg, O. (2006). The evolutionary history of Symbiodinium and Scleractinian hosts: symbiosis, diversity, and the effect of climate change. Perspectives in Plant Ecology Evolution and Systematics, 8, 23–43.CrossRefGoogle Scholar
UNISYS (2006). http://weather.unisys.com/hurricane/index.html.
Oppen, M. J. H., and Gates, R. D. (2006). Conservation genetics and the resilience of reef-building corals. Molecular Ecology, 15, 3863–83.CrossRefGoogle ScholarPubMed
Walker, E. L. L. (2005). The role of weather and climate processes in coral growth. M.S. thesis, University of Reading.
Ward, S. (1995). The effect of damage on the growth, reproduction and storage of lipids in the Scleractinian coral Pocillopora damicornis (Linnaeus). Journal of Experimental Marine Biology and Ecology, 187, 193–206.CrossRefGoogle Scholar
Wilkinson, C., Souter, D., and Goldberg, J., eds. (2006). Status of Coral Reefs in Tsunami Affected Countries: 2005. Townsville, Queensland: Australia Institute of Marine Sciences.Google Scholar
Winter, A., Appledorn, R. S., Bruckner, A., Williams, E. H. Jr., and Goenaga, C. (1998). Sea surface temperatures and coral reef bleaching off La Parguera, Puerto Rico (northeastern Caribbean Sea). Coral Reefs, 17, 377–82.CrossRefGoogle Scholar
Woodley, J. D. (1992). The incidence of hurricanes on the north coast of Jamaica since 1870: are the classic reef descriptions atypical?Hydrobiologia, 247, 133–38.CrossRefGoogle Scholar
Woodley, J. D., Chornesky, E. A., Clifford, P. A., et al. (1981). Hurricane Allen's impact on Jamaican coral reefs. Science, 214, 749–55.CrossRefGoogle ScholarPubMed

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