Massive bioturbated coralline limestone with low diverse, medium isolated corals heads of Favites, Heliastraea, Tarbellastraea, Porites, Thegioastraea spp. Coralline red algae occur as free-rolling or partly attatched rhodoliths and debris of Lithothamnium and Mesophyllum spp. Red algae play a significant role in construction of
the reef facies, where they bind and connect coral colonies and other skeletal and non  skeletal constituents into a coherent mass. The bivalves, gastropods and echinoids act as essential rock forming constituents in this lithofacies. Fore-reef sediments mainly gave bioclastic wackestone, algal wackestone, bioclastic packstones, coralline framestone, coralline rudstone and grainstones. Most of these sediments are driven from the reef-core framework. Thin sections show fragments of corals, red algae, benthic foraminifera (miliolids) and ostracods. Most of these fragments were recrystallized due to diagenesis.