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In less than 10 years, subaerially-exposed Holocene oolitic sand on Eleuthera Island, Bahamas was completely case-hardened by freshwater vadose calcite cementation. This phenomenon demonstrates the rapidity of freshwater carbonate diagenesis and explains, in part, why carbonate platforms preferentially shed unconsolidated sediment during highstands and not during lowstands when they are subaerially...
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