Carbonate fabrics include skeletal wackestones,
skeletal packstone, framestone, lime mudstone, and
bindstone in order of decreasing occurrences. The
skeletal grains are strongly modified by
dolomitisation, but were originally dominated by
corals and red algae, echinoderms, large and
planktonic foraminifera. Lime mud matrix has been
recrystallised. The widespread occurrence of corals
and red algae is strongly suggestive of deposition in
proximity to reefal buildups.