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Figure 2. Coral condition by location.<br />
100%<br />
80%<br />
60%<br />
40%<br />
20%<br />
0%<br />
Alphonse St Pierre Providence<br />
Recently Dead<br />
Bleached<br />
Unbleached<br />
Figure 3. Coral condition over time at Alphonse Atoll at a) 10 m and<br />
b) 15 m water depth for March and May 1998 survey periods.<br />
100%<br />
80%<br />
60%<br />
40%<br />
20%<br />
0%<br />
March 10m May 10m March 15m May 15m<br />
appeared to be a common occurrence creating a temperature<br />
differentiation of approximately 3º C - 6º C. This<br />
phenomenon could have mitigated the impact of the<br />
anomalous 1998 sea-surface temperatures which caused<br />
the widespread coral bleaching.<br />
A year after the bleaching event (February - March<br />
1999) the shallow (8-15m) outer slope, was dominated<br />
by dead coral and coral rubble composed of substantial<br />
quantities of dead branching coral. The dead coral surfaces<br />
on the NW and SW slopes were dominated by the<br />
reticulate, foliaceous, green alga Microdictyon. Observations<br />
in November 1999 showed that this cover has persisted<br />
although the alga has been substantially grazed.<br />
Pocilloporid and acroporid recruits (3-5 cm diameter)<br />
were observed in November 1999 but these were very<br />
few. The largest cover percentage of live coral was<br />
found in the NE and SE spur and groove zone (