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In most soil substrates, microorganisms play an important role in the production or consumption of N2O, CH4, and CO2.
Microorganisms play an important role in the breakdown and transformation of organic matter in fertile soils with many species contributing to different aspects of soil fertility.
These sulfate-reducing microorganisms play an important role in energy production as well as the maintenance of the microbial community (Elshahed et al. 2003; Douglas and Douglas 2001).
Microorganisms play an essential role in remediation of most organic contaminants in soil and water resources due to their metabolic versatility and their capacity to adapt to changing environmental conditions (Meckenstock et al. 2015).
When plants die, the silica is reincorporated into the soil where microorganisms play an important role in the degradation of organic matter and in the release of minerals nutrients [28, 29], other important source that raises mineralization rate is earthworms producing biohumus.
Proteases produced by pathogenic microorganisms play an important role in virulence [1].
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Microorganisms play a fundamental role in the cycling of nutrients and energy on our planet.
Soil microorganisms play a crucial role in mineralization and breakdown of complex organic compounds in soil.
Microorganisms play a significant role in bioremediation of heavy metal contaminated soil and wastewater.
Microorganisms play a central role in litter decomposition and partitioning C between CO2 evolution and sequestration of C into semi-permanent pools in soils.
Experimental results also suggest that iron-reducing bacteria, which are robust and well-adapted microorganisms, play a key role in these interfacial processes.
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