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How does biological weathering work in context of rock weathering? 


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Biological weathering in the context of rock weathering involves microbial activities that contribute significantly to the alteration of rock surfaces. Microorganisms, such as Actinobacteria and Proteobacteria , play crucial roles in mineral weathering processes. For instance, Actinobacteria have been found to leach minerals from granite, leading to the formation of secondary minerals like kaolinite and vermiculite . Additionally, chemolithotrophic bacteria like Fe(II) oxidizing bacteria (FeOB) are capable of oxidizing silicate-bound iron, accelerating weathering rates and influencing the overall biogeochemical cycling of elements in rock outcrops . Furthermore, fungi like Schizophyllum commune contribute to biophysical and biochemical weathering by exerting mechanical pressure, secreting organic acids, and enhancing dissolution of minerals like quartz, ultimately leading to rock degradation . These microbial activities highlight the diverse mechanisms through which biological weathering impacts rock surfaces.

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Biological weathering, driven by microorganisms like mosses and lichens, plays a key role in deteriorating rock cultural heritages by facilitating various bioweathering processes and interactions, intensifying weathering in specific microhabitats.
Biological weathering involves basidiomycete Schizophyllum commune secreting organic acids, siderophores, enzymes, and applying mechanical pressure to degrade black slate, releasing metals and forming new mineral phases like whewellite.
Biological weathering involves microorganisms, like chemolithotrophic Fe(II) oxidizing bacteria, oxidizing minerals like silicate-bound Fe(II) for energy, accelerating weathering and interacting with organotrophic microorganisms in rock weathering.
Biological weathering in rock surfaces involves microbial biofilms secreting extracellular polymeric substances that reduce water loss, limit salt transport, and stabilize the surface, mitigating geomorphic processes in arid environments.
Biological weathering involves microbial communities like Actinobacteria breaking down rock minerals, releasing nutrients, forming secondary minerals, and altering the rock's composition over time.

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