Abstract
The growth of coral reefs has been a controversial subject ever since Darwin's1 subsidence theory. Scientists have argued over the major factors affecting growth2–4, but most have agreed that reefs grow dominantly along their windward margins5–7, a characteristic displayed in the Permian8 and Devonian9 reefs of New Mexico and Western Australia. Recently, however, Adey10 has indicated that the growth characteristics of windward margins are energy related, such that different growth characteristics are to be expected under different energy regimes. The Great Barrier Reef is a high-energy epicontinental shelf reef system on which it has been suggested11–13 that, in the prevailing conditions, windward growth has been subordinate to vertical and leeward growth. We present here results from drilling and monitoring studies demonstrating that reef growth in a transgressive epicontinental shelf environment is first vertical and then backwards, especially on the leeward margin, when the reef reaches the stillstand sea level position.
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References
Darwin, C. The Structure and Distribution of Coral Reefs (Smith, Elder, London, 1842).
Murray, J. Proc. R. Soc. Edinb. 10, 505–518 (1880).
Daly, R. A. Proc. Am. Acad. Arts Sci. 51, 157–251 (1915).
Davis, W. M. Am. geogr. Soc. Spec. Publ. 9 (1928).
Holmes, A. Principles of Physical Geology (Nelson, Sunbury-on-Thames, 1965).
Thornbury, W. D. Principles of Geomorphology (Wiley, New York, 1969).
Maxwell, W. G. H. Atlas of the Great Barrier Reef (Elsevier, Amsterdam, 1968).
Newell, N. D. et al. The Permian Reef Complex of the Guadalupe Mountains Region, Texas and New Mexico (W. H. Freeman, San Francisco, 1953).
Playford, P. E. Western Australia Geol. Surv. Rep. 1 (1969).
Adey, W. H. Science 202, 831–837 (1978).
Davies, P. J. Proc. 3rd int. Coral Reef Symp. 2, 325–330 (1977).
Davies, P. J. et al. Proc. 3rd int. Coral Reef Symp. 2, 331–338 (1977).
Stoddart, D. et al. Proc. R. Soc. B284, 149–159 (1978).
Davies, P. J., Radke, B. M. & Robison, C. R. BMR J. Aust. Geol. Geophys. 1, 231–240 (1976).
Davies, P. J. & Kinsey, D. W. Mar. Geol. 24, 1–11 (1977).
Harvey, H., Davies, P. J. & Marshall, J. F. BMR J. Aust. Geol. Geophys. 4, 141–147 (1979).
Davies, P. J. & Marshall, J. F. Search 10, 776–779 (1979).
Kinsey, D. W. Proc. 1st int. Coral Reef Symp. 13–32 (1972).
Kinsey, D. W. & Davies, P. J. in Biogeochemical Cycling of Mineral-forming Elements (eds Trudingar, P. & Swaine, D.) 131–162 (Elsevier, Amsterdam, 1979).
Kinsey, D. W. & Davies, P. J. Limnol. Oceanog. 24, 935–940 (1979).
Frankel, E. Proc. 3rd. int. Coral Reef Symp. 2, 201–208 (1977).
Davies, P. J. Reef Growth: A Review (Australian National University Press, in the press).
Davies, P. J. & West, B. (in preparation).
Orme, G. R., Flood, P. G. & Sargent, G. Proc. R. Soc. A291, 85–100 (1978).
Davies, P. J. Proc. 2nd int. Coral Reef Symp. 2, 573–578 (1974).
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Davies, P., Marshall, J. A model of epicontinental reef growth. Nature 287, 37–38 (1980). https://doi.org/10.1038/287037a0
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DOI: https://doi.org/10.1038/287037a0
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