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Microbialite

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thumb|right|Microbialites in Lake Salda rocks thumb|Emerged microbialite formation at Lake Van, East Anatolia alt=|thumb|right|Classification of microbialites (redrawn and simplified from Schmid, 1996).alt=|thumb|right|Stromatolites – laminated microbialites (Precambrian silicified stromatolite, Strelley Pool Chert, (Pilbara Craton), Western Australia|W. Australia)

~8 min read

Encyclopedic overview

8 sections
Contents
  • Classification
  • Evolution
  • Formation of microbialites
  • Modern microbialites distribution
  • Composition
  • Microbes that produce microbialites
  • Interest in studying microbialites
  • References

thumb|right|Microbialites in Lake Salda rocks thumb|Emerged microbialite formation at Lake Van, East Anatolia alt=|thumb|right|Classification of microbialites (redrawn and simplified from Schmid, 1996).alt=|thumb|right|Stromatolites – laminated microbialites (Precambrian silicified stromatolite, Strelley Pool Chert, (Pilbara Craton), Western Australia|W. Australia)

Microbialite is a benthic sedimentary deposit made of carbonate mud (particle diameter less than 5 μm) that is formed with the mediation of microbes. The constituent carbonate mud is a type of automicrite (or authigenic carbonate mud); therefore, it precipitates in situ instead of being transported and deposited. Being formed in situ, a microbialite can be seen as a type of boundstone where reef builders are microbes, and precipitation of carbonate is biotically induced instead of forming tests, shells or skeletons.

Excerpted from Wikipedia’s “Microbialite” article, available under the CC BY-SA 4.0 licence.

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