Carbonate laminae recorded in a siliciclastic tidalflat colonized bymicrobial mats

MAISANO, L.; QUIJADA, I.E.; CUADRADO, D.G.; PERILLO, V.L.; PAN, J.; MARTINEZ, A.M.

SEDIMENTARY GEOLOGY

ELSEVIER SCIENCE BV

Año: 2020 vol. 405

0037-0738

Microbial mats in siliciclastic coastal environments are considered as non-lithifying systems that lack the poten-tial for calcification. This work documents precipitation and preservation of well-defined, laterally continuouscarbonate laminae in low-relief microbial mats from a siliciclastic supratidalflat in northern Patagonia (PasoSeco, Argentina). Petrographic, epifluorescence, and SEM-EDS studies of surficial and buried microbial mats show that they are composed of repeated sediment sequences comprised of four different types of laminae,which are, from base to top: (A) a sand and silt lamina, (B) a lamina largely composed of organic matterdisplaying moulds of subvertical cyanobacteria filaments, (C) a lamina composed of dense micritic carbonate,which is cut by moulds of vertical cyanobacteria filaments, and (D) a lamina composed of organic matter contain-ing abundant horizontal cyanobacteria filaments. The formation of each different lamina is strongly controlled bythe environmental conditions, characterized by episodic seawater flooding, followed by several days to weeks in which water remains covering the sediment and gradually evaporates producing a salinity increase and the precipitation of calcite, gypsum and halite. Thus, the basal sand and silt lamina forms as the result of the transport of siliciclastic grains and particles during seawater flooding. The overlying lamina B, composed of organic matter with moulds of subvertical cyanobacteria filaments, is formed when calm water conditions are recovered and organic material is produced by photosynthetic microbial activity. The following lamina C, composed of dense micritic carbonate, precipitates when the salinity of stagnant water reaches CaCO3supersaturation. Finally, the uppermost lamina D, composed of organic matter with horizontal cyanobacteria filaments, is developed while the sediment surface is drying and gypsum and halite precipitate, although these minerals are not preserved in the sediment because they dissolve during subsequent inundations. All these observations show that well-developed, laterally-continuous carbonate laminae may be formed and preserved in a siliciclastic tidal environment if biotic and abiotic sedimentary processes closely interact to create the required conditions. The studied microbial mats increase sediment impermeability, which favours water retention in theflat and, thus, subse-quent evaporation of the retained seawater. Moreover, microbial cells and EPS (extracellular polymeric sub-stance) suspended in seawater might act as nuclei for CaCO3precipitation, which will later settle down on themicrobial mat. In addition, EPS of the microbial mats may also serve as nucleus forin situcarbonate precipitation.