Subaerial Meteoric Calcitization and Lithification of High-Magnesian Calcite Muds, Belize

MAZZULLO, S. J., and W. D. BISCHOFF, Wichita State University, Wichita, KS

Holocene (1000-1500 yrs old) high-magnesian calcite-dominated muddy sediments (1 m thick) on subaerially exposed cays in northern Belize are in the process of being converted to low-magnesian calcite micrite. Mineralogic stabilization and attendant lithification result from interaction of the sediments with meteoric fluids believed to be derived from seasonal upward discharge through subjacent Pleistocene limestones. The initial marine-derived sediments, composed of >85% HMC (and minor skeletal aragonite), consist of mud and associated soritid and miliolid foraminifera both with MgCO(3) content of 11-15 mol%, and isotopic compositions of -1.0 to -2.5% PDB (O), 0 to +1.5% PDB (C). With depth, lithified LMC crusts appear in the section, and the Mg concentration of the sediments and a sociated crusts decreases rapidly to 3 mol% or less, with a corresponding isotopic depletion to values approaching -7.0% (O) and -5.8% (C). Concomitantly there is progressive dissolution of skeletal aragonite in the sediments, reduction of porosity due to cementation by LMC, and in the muds, a decrease in Sr and increase in Mn contents.

The resultant petrofabric of these lithified LMC deposits, derived from the alteration of HMC-dominated muds, is characterized by micrite with patches of pore-filling micritic and microsparitic LMC cements. Such a fabric is similar to and can be confused easily with calcitized aragonite-dominated precursor muds, except for the relative rarity in the samples examined of aragonite relicts in component microspar and/or pseudospar.

AAPG Search and Discovery Article #91004 © 1991 AAPG Annual Convention Dallas, Texas, April 7-10, 1991 (2009)