The equant spar cements are probably freshwater cements dissolved from original aragonite and calcite. The radial calcite ooids accumulated on high energy shoals. Note ooid nulceae of quartz and seletal material. There appear to be a few botryoidal grains enclosed by radial ooid coating. Darkened spots within bioclastic layers are remanents of colonies of cyanobacteria that caused local micritization.