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Institut für Geologie und Paläontologie, Karl-Franzens-Universität Graz, Heinrichstrasse 26, 8010 Graz, Austria
Bernhard.Riegl{at}kfunigraz.ac.at
Werner.Piller{at}kfunigraz.ac.at
Coral framework construction and resultant growth fabrics in response to environmental factors were studied in the northern Red Sea, and the Gulfs of Suez and Aqaba. The dependence of growth fabric types on sea-floor topography, oceanography and the ecology of constituent coral species was investigated. Five types of coral frameworks and their growth fabrics were differentiated: Acropora reef framework (platestone to mixstone facies); Porites reef framework (domestone facies); Porites carpet (columnar pillarstone facies); faviid carpet (mixstone facies); Stylophora carpet (thin pillarstone facies). Two non-framework community types were found: Stylophora-Acropora community and soft coral communities. Reef frameworks and resultant growth fabrics show a clear ecological zonation along depth and hydrodynamic exposure gradients. Coral carpets build a framework lacking a distinct internal zonation since they only grow in areas without pronounced gradients. In the northern Red Sea they show a gradual change with depth from Porites (pillarstone) to faviid (mixstone) dominance.
The initiation of frameworks was governed by bottom topography (reefs on steep slopes and highs, coral carpets in flat areas). According to environmental conditions, different coral communities produce different framework and growth fabric types. In step with framework growth the environment is modified. The modified environment in turn modifies the coral communities. Thus an environment-organism-environment feedback loop exists.
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