Definition
Microbial mats are benthic small-scale ecosystems that generally develop under environmental conditions that exclude fauna, often referred to as “extreme environments.” The biogeochemical cycles in microbial mats are usually largely closed, although small fluxes of elements are exchanged with the geo-, bio-, and atmosphere. An important feature of microbial mats is their carbon and nitrogen autotrophy, i.e., the fixation of inorganic carbon and atmospheric nitrogen are key processes. In illuminated environments, therefore, the photoautotrophic cyanobacteria are the mat-building organisms while in the deep sea or in some caves, chemosynthetic bacteria and archaea are the primary producers.
Overview
The term microbial matoriginates from the macroscopic structure that these...
References and Further Reading
Des Marais DJ (2003) Biogeochemistry of hypersaline microbial mats illustrates the dynamics of modern microbial ecosystems and the early evolution of the biosphere. Biol Bull 204:160–167
Dupraz C, Reid RP, Braissant O, Decho AW, Norman RS, Visscher PT (2009) Processes of carbonate precipitation in modern microbial mats. Earth Sci Rev 96:141–162
Noffke N, Gerdes G, Klenke T (2003) Benthic cyanobacteria and their influence on the sedimentary dynamics of peritidal depositional systems (siliciclastic, evaporitic salty, and evaporitic carbonatic). Earth Sci Rev 62:163–176
Schopf JW (2000) Solution to Darwin’s dilemma: discovery of the missing Precambrian record of life. Proc Natl Acad Sci U S A 97:6947–6953
Stal LJ (1995) Physiological ecology of cyanobacteria in microbial mats and other communities. New Phytol 131:1–32
Stal LJ (2001) Coastal microbial mats: the physiology of a small-scale ecosystem. S Afr J Bot 67:399–410
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Stal, L.J. (2014). Microbial Mats. In: Amils, R., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_5085-1
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DOI: https://doi.org/10.1007/978-3-642-27833-4_5085-1
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