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Examples of the following habitats may often be included
incidentally in MPAs. However, if reefs are to flourish, they
should be deliberately identified and protected within MPA
boundaries.
Reef flats. Corals on reef flats and upper
reef crests that are exposed at low tides often exhibit
stress tolerance and may resist or recover rapidly from
bleaching. They will be important providers of larvae that
may settle in dead areas and aid their recovery.
These reef flats often provide vital nurseries
for reef fishes that will move onto the reef and help
reestablish communities affected by bleaching.
Nitrogen and organic material produced on the reef
flats, or transported from there in the form of feces
of herbivorous fishes and other organisms, all contribute
valuable nutrients to the reef community and aid in its
functioning and recovery.
Back-reef lagoons. Coral assemblages in
back-reef lagoons, especially shallow lagoons behind fringing
reefs, are routinely exposed to wide temperature fluctuations
(the ponding effect) and consequently may exhibit some acclimatization
to temperature stress and resistance to bleaching.
Back-reef lagoons are also important nurseries
for fishes.
Corals in naturally turbid, deeper lagoons may
show higher resistance to bleaching than corals of the
same species in clear waters over barrier reefs.
Seagrass beds and sand flats. Seagrass beds
and sand flats surrounding coral reefs are important feeding
grounds for nocturnal feeding fishes, such as snappers and
grunts, which shelter on reefs by day. When they return
to the reef, these fishes deposit nutrients in the form
of feces that are introduced to the reef food web and contribute
to the growth and recovery of reef communities.
Mangroves. The generally turbid waters and
shading effect of mangroves may reduce the susceptibility
of corals in that area to bleaching.
Mangroves also provide nurseries for juveniles
of certain reef fishes (e.g., groupers, parrotfishes,
and snappers)
Where they are close enough to reefs, mangroves
provide feeding grounds to fishes that shelter on the
reefs.
Mangroves introduce fixed nitrogen and organic
detritus into the food chain of reefs, as do reef flats
and seagrass beds.
Beaches and dunes. Coastlines are dynamic
zones. Disturbances to them may cause beach erosion and
alteration of the natural cycle of accumulation and erosion
of sand along the shore, increase turbidity of inshore waters,
or even smother living reefs with excessive sediment.
This is especially true of sand cays, which have
been known to move across reefs, fall off into deeper
water and disappear for good, as occurred at Maziwi Island,
Tanzania. Before its disappearance, Maziwi Island was
the most important green sea turtle nesting beach off
mainland Tanzania.
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