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Most microorganisms on earth live in aggregates such as films, flocs, mats, granules or sludge – this form of life is referred to as ‘biofilms’, and it is involved in the biogeochemical cycles of all major elements including metals. Encased in a highly hydrophilic matrix of extracellular polymeric substances, biofilm organisms can develop stable microconsortia and complex interactions, resulting in features of multicellular organisms.
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