ELSEVIER Ecological Modelling 84 (1996) 199-214
EI:OLOI;li'IIL
mODELLInl]
Patterns of coral bleaching: modeling the adaptive bleaching
hypothesis
John R. Ware a, *, Daphne Gail Fautin b, Robert W. Buddemeier c
a Computer Sciences Corporation, 1301 Piccard Drive, Rockville, MD 20850, USA
b Department of Systematics and Ecology, University of Kansas, Lawrence, KS 66045, USA
c Kansas Geological Survey, University of Kansas, Campus West, 1930 Constant Avenue, Lawrence, KS 66047, USA
Received 1 March 1994; accepted 24 August 1994
Abstract
Bleaching - the loss of symbiotic dinoflagellates (zooxanthellae) from animals normally possessing them - can be
induced by a variety of stresses, of which temperature has received the most attention. Bleaching is generally
considered detrimental, but Buddemeier and Fautin have proposed that bleaching is also adaptive, providing an
opportunity for recombining hosts with alternative algal types to form symbioses that might be better adapted to
altered circumstances. Our mathematical model of this "adaptive bleaching hypothesis" provides insight into how
animal-algae symbioses might react under various circumstances. It emulates many aspects of the coral bleaching
phenomenon including: corals bleaching in response to a temperature only slightly greater than their average local
maximum temperature; background bleaching; bleaching events being followed by bleaching of lesser magnitude in
the subsequent one to several years; higher thermal tolerance of corals subject to environmental variability compared
with those living under more constant conditions; patchiness in bleaching; and bleaching at temperatures that had
not previously resulted in bleaching.
Keywords: Adaptation; Coral bleaching; Marine ecosystems; Temperature
1. Introduction
Under normal conditions, most reef-building
corals are various shades of green or brown,
colors primarily due to the intracellular symbiotic
dinoflagellates known as zooxanthellae. These al-
gae of uncertain taxonomy (e.g., Taylor, 1974;
* Corresponding author. Fax: 301-670-2381.
Blank and Trench, 1985; Rowan and Powers,
1991) provide metabolic benefits to their hosts
(e.g., Land et al., 1975; Gattuso and Jaubert,
1990; Muscatine, 1990) and enhance coral calcifi-
cation (e.g., Goreau and Goreau, 1959; Yonge,
1973; Vandermeulen and Muscatine, 1974). A
coral is said to have bleached when the density of
zooxanthellae declines so the white coral skeleton
is visible through the coral tissue. (Reduced con-
centration of algal chlorophyll can also produce
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