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Management Plan - Glover's Reef Marine Reserve

Management Plan - Glover's Reef Marine Reserve

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Patch <strong>Reef</strong>s<br />

Glovers <strong>Reef</strong> <strong>Marine</strong> <strong>Reserve</strong> – <strong>Management</strong> <strong>Plan</strong><br />

The majority of the more than 850 patch reefs within the Atoll’s lagoon are distributed randomly<br />

with the exception of those in the western and northeast portions of the Atoll where they are<br />

aligned along NNE-striking trends. They range in size from about 10 m to a few hundred<br />

meters (Wallace 1975). They consist of massive corals such as Montastrea, Diploria,<br />

Siderastrea and Porites, with occasional thickets of Agaricia and Acropora cervicornis; sea fans<br />

and brown algae are abundant on dead coral surfaces (McClanahan & Muthiga 1998).<br />

In the 1970s, three distinct coral assemblages were recognized along a north-south transect<br />

namely: Montastrea, Acropora and Algae-Porites. This distribution mimicked the zonation on<br />

the seaward reef tracts, and was believed to be a response to disturbances such as hurricanes<br />

(Wallace & Schafersmann 1977). A list of coral species of the patch reefs provided by Wallace<br />

(1975) is shown in Appendix 4.<br />

More recent studies have also focused on the composition of the Atoll’s patch reefs, and show<br />

that they have undergone a major change in their ecology. They have experienced a 75%<br />

reduction in coral cover (with M. annularis showing the least loss), a 99% loss in cover of<br />

Acropora spp., and a 315% increase in algae cover, particularly of the erect brown algae<br />

Lobophora (McClanahan & Muthiga 1998). The cause for this dramatic change over the past<br />

25 years is complex, and probably due to several inter-related factors, such as reduced<br />

herbivory, increased level of nutrients, and disease.<br />

The patch reefs no longer exhibit the zonation described earlier by Wallace and Schafersmann<br />

(1977). Furthermore, the phase change in community structure has resulted in the 80% hard<br />

coral cover and 20% algae cover reported by Wallace (1975) to be transformed to a 20% coral<br />

cover and 80% algae cover (McClanahan & Muthiga 1978).<br />

Lagoon Floor<br />

The lagoon floor, which ranges in depth from 6 to 18 m, is comprised of predominantly fine<br />

sand and mud sized carbonate sediment. It supports a sparse flora of Thalassia and algae,<br />

mainly Penicillus with some Halimeda (Wallace 1975).<br />

Some deeper areas of the lagoon are almost completely barren of vegetation, though<br />

echinoderms and other invertebrates are common.<br />

Wildtracks / Wildlife Conservation Society, 2007 32

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