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Titlebook: Microbial Sediments; Robert E. Riding,Stanley M. Awramik Book 2000 Springer-Verlag Berlin Heidelberg 2000 Geomikrobiologie.Karst.Mikroben.

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Microbial Phosphate Sediment,l in phosphate formation and that in many cases their activity is imprinted in the framework of these rocks. The microbiota involved in this activity include bacterial, fungal and cyanobacterial mat-forming microphytes bearing in their extracellular structures a large part of the phosphate phase of
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Subaerial Microbial Mats and Their Effects on Soil and Rock,heric environments can be regarded as the maximum biomass maintaining metabolic potential in the presence of the minimum amount of water. Rock or other subaerial biofilms are made up primarily of poikilotroph micro-or-ganisms which thrive on the lowest water activity possible. Biofilms on and in roc
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Cyanobacteria: Architects of Sedimentary Structures, at the sediment-water interface, coupled with rapid bacterial oxidation of this organic product, maintains steep redox gradients, creating additional metabolic niches. The consequent changes in mineral solubility promote biogeochemical cycling of elements and may lead to recrystallization and rearr
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