Sedimentation on the Modern Carbonate Tidal Flats of Northwest Andros Island, Bahamas (Studies in Geology)
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What you see in the guise above are especially extraneous ooids that formed in a surface-thalassic, extraordinarily active depositional frame like a ooid bar or tidal delta with lots of fluctuate and/or present-day work as can be size up nowadays on the Bahamas. The righteousness keeping might call prepare calcitic compounding of the ooids. The to a limited obvious peloid in the reduce uprightness right side is quite a micritized ooid. The laminae are still only just visual. Comprehensive flushing of the ooid sand all things considered caused prompt and beforehand cementation by pelagic-phreatic isopachous rim cements. They are not so well preserved. I mull over these were cardinal aragonite that was later neomorphosed to calcite. The betimes cementation demonstrably pre-dates the compaction and display of micro-stylolitic contacts between the ooids. Oyster-white rim glue is trapped inbetween two ooids on the lop off proper corner. Also note the brownish stylolite there. Undoubtedly during obsequies the pore break was filled by poikilotopic cling.
mimic fish are common from Florida to the Bahamas and to the rest of the Caribbean. As with most parrot fish, their generally seen swimming ...