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The major breakdown product of microbial decomposition is carbon dioxide, which is formed by respiring aerobic organisms.
Permafrost thaw and microbial decomposition is considered one of the most likely positive climate feedbacks from terrestrial ecosystems to the atmosphere in a warmer world, but the rate of carbon release from permafrost soil remains highly uncertain.
Carbon (C) and nitrogen (N) cycling in soil during microbial decomposition is well studied, yet the mechanism underlying the response of microbial C utilization to the presence of N still remains an open question.
The protection of organic material within aggregates against microbial decomposition is regarded as an important process in soil organic carbon stabilization but detailed knowledge about this process is still lacking.
This is because of the fact that microbial decomposition is one of the major factors that caused a significant decrease in the C/N ratio (Nath and Singh 2009; Chauhan and Singh 2012a, b).
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Rates of microbial decomposition are much lower under anaerobic conditions, which release CH4, than under aerobic conditions, which produce CO2; however, CH4 has roughly 25 times the greenhouse warming potential of CO2.
In the present study, we detected that some metabolic pathways related to microbial decomposition were significantly more abundant in the stomach than in the small intestine and large intestine.
Microbial decomposition process is important for wastewater treatment.
Litter decomposition is driven by saprotrophic microbial communities.
Lignocellulose decomposition is influenced by the structure and function of microbial communities [2, 3] and terrestrial carbon cycling models increasingly parameterize these properties [4, 5].
The process of decomposition is complex and includes, for example, ingrowth of microbial biomass and nutrient accumulation in addition to leaching and respiration.
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