Molluscan assemblages on coral reefs and associated hard substrata in the northern Red Sea

Citation
M. Zuschin et al., Molluscan assemblages on coral reefs and associated hard substrata in the northern Red Sea, CORAL REEF, 20(2), 2001, pp. 107-116
Citations number
71
Categorie Soggetti
Aquatic Sciences
Journal title
CORAL REEFS
ISSN journal
07224028 → ACNP
Volume
20
Issue
2
Year of publication
2001
Pages
107 - 116
Database
ISI
SICI code
0722-4028(200109)20:2<107:MAOCRA>2.0.ZU;2-F
Abstract
Information on spatial variability and distribution patterns of organisms i n coral reef environments is necessary to evaluate the increasing anthropog enic disturbance of marine environments (Richmond 1993; Wilkinson 1993; Day ton 1994). Therefore different types of subtidal, reef-associated hard subs trata (reef flats, reef slopes, coral carpets, coral patches, rock grounds) , each with different coral associations, were investigated to determine th e distribution pattern of molluscs and their life habits (feeding strategie s and substrate relations). The molluscs were strongly dominated by taxa wi th distinct relations to corals, and five assemblages were differentiated. The Dendropoma maxima assemblage on reef fiats is a discrete entity, strong ly dominated by this encrusting and suspension-feeding gastropod. All other assemblages are arranged along a substrate gradient of changing coral asso ciations and potential molluscan habitats. The Coralliophila neritoidea Bar batia foliata assemblage depends on the presence of Porites and shows a dom inance of gastropods feeding on corals and of bivalves associated with livi ng corals. The Chamoidea-Cerithium spp. assemblage on rock grounds is stron gly dominated by encrusting bivalves. The Drupella cormus-Pteriidae assembl age occurs on Millepora-Acropora reef slopes and is strongly dominated by b ivalves associated with living corals. The Barbatia setigera-Ctenoides annu lata assemblage includes a broad variety of taxa, molluscan life habits and bottom types, but occurs mainly on faviid carpets and is transitional amon g the other three assemblages. A predicted degradation of coral coverage to rock bottoms due to increasing eutrophication and physical damage in the s tudy area (Riegl and Piller 2000) will result in a loss of coral-associated molluscs in favor of bivalve crevice dwellers in dead coral heads and of e ncrusters on dead hard substrata.