Sparse isopachus rim cements are probably related to initial freshwater cements that originated from dissolution of original aragonite and calcite. The radial calcite ooids accumulated adjacent to a high energy setting. Note radial character of the crystals in the ooid layering is somewhat obscure. Darkened spots within bioclastic layers are after cyanobacteria colonies that caused local micritization. Note the well developed large calcite spar overgrowths on echinoid fragments.