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When the spatio-temporal dynamics of microbial groups are accounted for, our simulations show the importance of reaction energetics and nutrient limitations such as microbial nitrogen demands.
Two major microbial groups are now believed to be involved in ammonia oxidation: chemolithotrophic ammonia-oxidizing bacteria (AOB) and ammonia-oxidizing archaea (AOA).
The three most common microbial groups are bacterial epsilonproteobacteria, archaeon thermophilics of the Methanococcus family, and archaeons of the Euryarchaeota family.
Our data show that cells from representative microbial groups are not killed even when exposed to much more blue light than is actually used in the system.
It is not known how the different microbial groups are represented within this important subgroup [ 35].
Since these microbial groups are uncultured, this association as well as many others uniquely identified by eLSA provides new insight into their ecological role in the ocean surface waters.
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Five microbial groups were considered in the model: facultatively aerobic bacteria or denitrifiers, fermenters, and sulfate-, mandanese-, and iron-reducers.
However, no dissimilarities in cell population densities or population ratios of the microbial groups were detected in the rhizosphere of the two plant lines.
Three microbial groups were defined: (A) A-group: wild-type bacteria strains treated with adequat antibiotherapy; (B) B-group: antibiotic resistant bacteria treated with adequat antibiotherapy; (C) C-group: multi-drug resistant bacteria treated with inadequat antibiotherapy.
Understanding the impacts of spilled oil on indigenous microbial communities and identification of oil-degrading microbial groups were prerequisites for the clean-up efforts of oil-contaminated marine benthic ecosystems.
Furthermore, soil microbial groups were highly correlated with soil SOC (P < 0.001), C/N ratio (P < 0.001), pH (P < 0.01), total nitrogen (P < 0.01), and the proportion of aggregates with a >0.25 mm diameter (P < 0.05).
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