Shallow‐marine carbonate cementation in Holocene segments of the calcifying green alga Halimeda
نویسندگان
چکیده
Early-diagenetic cementation of tropical carbonates results from the combination numerous physico-chemical and biological processes. In marine phreatic environment it represents an essential mechanism for development stabilization carbonate platforms. However, diagenetic cements that developed early in are likely to become obliterated during later stages meteoric or burial diagenesis. When lithified sediment samples studied, this complicates recognition processes involved cementation, their geological implications. contribution, a petrographic microfacies analysis Holocene Halimeda segments collected on coral island Spermonde Archipelago, Indonesia, is presented. Through electron microscopical analyses polished samples, study shows characterized by intragranular fibrous aragonite, equant High-Mg calcite (3.9 7.2 Mol% Mg), bladed Low-Mg (0.4 1.0 Mg) mini-micritic (3.2 3.3 Mg). The co-existence consecutive aragonite initially flow oversaturated seawater along template skeleton, followed adjustment cement mineralogy towards as result reduced permeability fluid rates pores. Growth top etched substrates explained shifts pore water pH alkalinity through microbial sulphate reduction. Microbial activity appears be main trigger precipitation well, based presumable detection extracellular polymeric matrix stage mini-micrite precipitation. Radiocarbon five furthermore indicate virtually complete with thermodynamically/kinetically controlled takes place about 100 years. Collectively, early-diagenetic highly diverse provides new quantitative constraints rate factories.
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ژورنال
عنوان ژورنال: Sedimentology
سال: 2021
ISSN: ['1365-3091', '0037-0746']
DOI: https://doi.org/10.1111/sed.12927