MARINE ECOLOGY PROGRESS SERIES
Mar Ecol Prog Ser
Vol. 411: 73–87, 2010
doi: 10.3354/meps08640
Published July 29
INTRODUCTION
Coral-population dynamics are influenced by popu-
lation processes that act on individual colonies at all
life history stages from differential recruitment and
survival (Birkeland 1977, Vermeij & Sandin 2008)
through to senescence (Rinkevich & Loya 1986, Bak &
Meesters 1999). Still, we know little about population
processes and how they vary spatially, seasonally and
under different environmental conditions. We under-
stand even less about differential weightings and sen-
sitivities of populations to slight process changes and
the repercussions of those changes on subsequent pop-
ulation trajectories. In a time of rapid climate change
(IPCC 2007), it is pertinent to quantify population pro-
cesses to determine which of them are most sensitive to
environmental shifts and examine those processes
within the context of population vulnerability to phase
shifts (Scheffer & Carpenter 2003, van Nes & Scheffer
2007, Guttal & Jayaprakash 2008).
This study investigated 5 coral-population processes:
(1) recruitment (newly settled juveniles), (2) postsettle-
ment mortality (death of newly settled recruits),
(3) colony growth (transition into a larger size class),
© Inter-Research 2010 · www.int-res.com *Email: lynnette.roth@gmail.com
Effects of thermal stress on key processes driving
coral-population dynamics
Lynnette Roth
1,
*
, Semen Koksal
2
, Robert van Woesik
1
1
Department of Biological Sciences, and
2
Department of Mathematical Sciences; Florida Institute of Technology,
150 West University Boulevard, Melbourne, Florida 32901, USA
ABSTRACT: A primary goal of ecology is to understand population dynamics by quantifying key pro-
cesses that regulate population densities through time. Change to any one process may alter the pop-
ulation trajectory, its genetic constitution, and its size-frequency distribution. This study sought to
quantify which of the 5 processes — (1) recruitment, (2) post-settlement mortality, (3) growth, (4) par-
tial mortality and (5) total colony mortality — most influenced corymbose Acropora coral-population
dynamics on reefs in southern Japan. Here we tracked coral reef colonies at a windward site and a
leeward site from 1996 to 2001 through a thermal anomaly (+1.8°C in 1998). We were particularly
interested in examining which of those processes had the largest effect on population dynamics. To
predict size-frequency distributions, we constructed a system of nonlinear differential equations that
included those 5 processes. Recruitment at the windward site remained consistent through time,
whereas the leeward site had more variable recruitment rates at all depths, and showed a consider-
able decrease after the 1998 thermal anomaly that remained suppressed for many years. At all
depths, the proportion of colonies transitioning to a larger size class was higher during the thermal
anomaly than in other years. Partial mortality was generally highest on 20 to 30 cm length colonies,
but was not a good indicator of thermal stress. Total colony mortality was most evident for the small-
est and largest corymbose Acropora colonies during the thermal anomaly, effectively narrowing the
size-frequency distributions. Sensitivity analyses revealed that total colony mortality had the largest
effect on coral-population growth rate (λ), followed by post-settlement mortality and recruitment.
Quantifying the population processes that lead to state changes is a prerequisite for understanding
reef dynamics in a rapidly warming ocean.
KEY WORDS: Sensitivity · Size-frequency distribution · Modeling · Bleaching · Temperature
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