10.7
Microbial mats are assemblies of microorganisms that grow on natural or artificial surfaces.
These assemblies typically begin as thin biofilms, only a few micrometers thick, and can develop into thicker layered structures.
Cyanobacterial mats in hot springs and saline environments show clear layered biological structures.
Daylight drives photosynthesis in the upper layers, dominated by cyanobacteria and other phototrophic bacteria, which produce oxygen.
Meanwhile, the deeper anoxic layers contain sulfate-reducing bacteria that generate hydrogen sulfide.
During the night, photosynthesis and oxygen production cease, allowing hydrogen sulfide to accumulate within the microbial mat.
On the other hand, chemolithotrophic mats found within deep, oxygen-deprived sediments are formed by sulfur-oxidizing Thioploca species.
These bacteria possess large internal vacuoles that store nitrate, which they absorb from the surrounding seawater.
They then glide into anoxic, sulfide-rich zones, utilizing the stored nitrate as an electron acceptor to oxidize hydrogen sulfide.
Microbiële gemeenschappen die biofilms en matten vormen, vertegenwoordigen complexe, ruimtelijk gestructureerde ecosystemen waarin metabolische proces…
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