•A sedimentological analysis of 3-billion-years old Mesoarchaean carbonates is presented.•Carbonates formed along a tide-influenced clastic–carbonate shoreline of an epicontinental sea.•Sedimentary cyclicity of diverse tidal facies is recognized.•A diverse assemblage of microbialites is recorded.•Bacteria participated in both in situ carbonate precipitation and trapping and binding of sediment.
Precambrian Research – Elsevier
Published: Jun 1, 2016
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