Soil bacteria respiration

NO,- Reduction Nitrate reductase NO,- Plants, animals, soil bacteria, yeasts (if undergoing "nitrate respiration Mo Mo... 

Wehrfritz J-M, Carter JP, Soiro S, Richardson DJ (1997) Hydroxylamine oxidation in heterotro-phic nitrate-reducing soil bacteria and purification of hydroxylamine cytochrome c oxidore-ductase from Pseudomonas species. Arch Microbiol 166 421 —424 Wehrfritz J-M, Reilly A, Spiro S, Richardson DJ (1993) Purification of hydroxylamine oxidase from Thiosphaera pantotropha. Identification of electron acceptors that couple heterotrophic nitrification to aerobic denitrification. FEBS Lett 335 246-250 Wetzstein H-G, Ferguson SJ (1985) Respiration-dependent proton translocation and the mechanism of proton motive force generation in Nitrobacter winogradskyi. FEMS Microbiol Lett 30 87-92... 

Carbon is released into the atmosphere as carbon dioxide as part of the process of respiration. The decomposition of the remains and wastes of living things by bacteria and other soil organisms also releases carbon dioxide into the atmosphere. In addition, carbon dioxide is released into the atmosphere by fires and other types of burning, including the burning of fossil fuels and erupting volcanoes. 

Aside from adding defined compounds, experimental additions of natural DOM mixtures suspected to vary in lability have helped test ideas about the contribution of various DOM sources to aquatic ecosystems. In a nice example using manipulation of natural DOM sources, Battin et al. (1999) used flowthrough microcosms to measure the relative uptake rates of allochthonous and autochthonous DOM by stream sediments. They documented greater than fivefold differences or more in uptake and respiration, depending on whether the DOM was extracted from soil or periphyton. Moreover, they were able to show, via transplant experiments, several cases where prior exposure to a particular source of DOM increased the ability of that community to metabolize the DOM supplied. There appears to be some preadaptation of microbial catabolic capacity when these stream biofilms were re-exposed to a familiar type of DOM. Similarly, the response of heterotrophic bacteria to carbon or nutrient addition was greatest when the source community was particularly active (Foreman et al., 1998). Kaplan et al. (1996) showed that fixed film bioreactors, colonized on one water source, were unable to rapidly metabolize DOC in water from another source. 

The main source of carbon monoxide, aside from the fossil fuel burning flux, is ffom oxidation of CH4 (Table 9.3). The remainder comes ffom decomposition of organic matter in soils, and bacteria and algae in the ocean that actively generate CO from respiration processes according to ... 

NPP is the net carbon gain by vegetation over a particular time period— typically a year. It is the balance between the carbon gained by photosynthesis and the carbon released by plant respiration. NPP includes the new biomass produced by plants, the soluble organic compounds that diffuse or are secreted by roots into the soil (root exudation), the carbon transfers to microbes that are symbiotically associated with roots (e.g., mycorrhizae and nitrogen-fixing bacteria), and the volatile emissions that are lost from leaves to the atmosphere (Clark et al., 2001). 

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