Anaerobic respiration is respiration using Oxidizing agent other than molecular oxygen (O2) in its electron transport chain.
In aerobic organisms, electrons are shuttled to an electron transport chain, and the final electron acceptor is oxygen. Molecular oxygen is an excellent electron acceptor. Anaerobes instead use less-oxidizing substances such as nitrate (), fumarate (), sulfate (), or elemental sulfur (S). These terminal electron acceptors have smaller reduction potentials than O2. Less energy per oxidized molecule is released. Therefore, anaerobic respiration is less efficient than aerobic.
Fermentation, in contrast, does not use an electrochemical gradient but instead uses only substrate-level phosphorylation to produce ATP. The electron acceptor NAD+ is regenerated from NADH formed in oxidative steps of the fermentation pathway by the reduction of oxidized compounds. These oxidized compounds are often formed during the fermentation pathway itself, but may also be external. For example, in homofermentative lactic acid bacteria, NADH formed during the oxidation of glyceraldehyde-3-phosphate is oxidized back to NAD+ by the reduction of pyruvate to lactic acid at a later stage in the pathway. In yeast, acetaldehyde is reduced to ethanol to regenerate NAD+.
There are two important anaerobic microbial methane formation pathways, through carbon dioxide / bicarbonate () reduction (respiration) or acetate fermentation.
An example of the ecological importance of anaerobic respiration is the use of nitrate as a terminal electron acceptor, or dissimilatory denitrification, which is the main route by which fixed nitrogen is returned to the atmosphere as molecular nitrogen gas. The denitrification process is also very important in host-microbe interactions. Like mitochondria in oxygen-respiring microorganisms, some single-cellular anaerobic ciliates use denitrifying endosymbionts to gain energy. Another example is methanogenesis, a form of carbon-dioxide respiration, that is used to produce methane gas by anaerobic digestion. Biogenic methane can be a sustainable alternative to fossil fuels. However, uncontrolled methanogenesis in landfill sites releases large amounts of methane into the atmosphere, acting as a potent greenhouse gas. Sulfate respiration produces hydrogen sulfide, which is responsible for the characteristic 'rotten egg' smell of coastal wetlands and has the capacity to precipitate heavy metal ions from solution, leading to the deposition of sulfide minerals.
Compare to the aerobic electron transport chain.]] Dissimilatory denitrification is widely used in the removal of nitrate and nitrite from municipal wastewater. An excess of nitrate can lead to eutrophication of waterways into which treated water is released. Elevated nitrite levels in drinking water can lead to problems due to its toxicity. Denitrification converts both compounds into harmless nitrogen gas.
Specific types of anaerobic respiration are also critical in bioremediation, which uses microorganisms to convert toxic chemicals into less-harmful molecules to clean up contaminated beaches, aquifers, lakes, and oceans. For example, toxic arsenate or selenate can be reduced to less toxic compounds by various anaerobic bacteria via anaerobic respiration. The reduction of Organochloride, such as vinyl chloride and carbon tetrachloride, also occurs through anaerobic respiration.
Anaerobic respiration is useful in generating electricity in microbial fuel cells, which employ bacteria that respire solid electron acceptors (such as oxidized iron) to transfer electrons from reduced compounds to an electrode. This process can simultaneously degrade organic carbon waste and generate electricity.
Aerobic respiration | and facultative anaerobes | +0.82 | such as Escherichia coli | ||
(Per)chlorate respiration | Facultative anaerobes | , , | +0.797 | Azospira suillum, Sedimenticola selenatireducens, Sedimenticola thiotaurini, and other gram negative prokaryotes | |
Iodate respiration | Facultative anaerobes | , | +0.72 | Denitromonas, Azoarcus, Pseudomonas, and other gram negative | |
Iron reduction(Dissimilatory iron reducing bacteria) | Facultative anaerobes and obligate anaerobes | +0.75 | Organisms within the order Desulfuromonadales (such as Geobacter, Geothermobacter, Geopsychrobacter, Pelobacter) and Shewanella species | ||
Manganese reduction(dissimilatory metal-reducing microorganisms) | Facultative anaerobes and obligate anaerobes | Desulfuromonadales and Shewanella species | |||
Cobalt reduction(dissimilatory metal-reducing microorganisms) | Facultative anaerobes and obligate anaerobes | Geobacter sulfurreducens | |||
Uranium reduction(dissimilatory metal-reducing microorganisms) | Facultative anaerobes and obligate anaerobes | Geobacter metallireducens, Shewanella oneidensis | |||
Denitrification(nitrate reduction) | Facultative anaerobes | (Ultimately) N2 | +0.40 | Paracoccus denitrificans, Escherichia coli | |
Fumarate respiration | Facultative anaerobes | Fumarate | Succinate | +0.03 | Escherichia coli |
Sulfate respiration | Obligate anaerobes | , | −0.22 | Many Deltaproteobacteria species in the orders Desulfobacterales, Desulfovibrionales, and Syntrophobacterales | |
Methanogenesis (carbon dioxide reduction) | Methanogens | −0.25 | Methanosarcina barkeri | ||
Sulfur respiration (sulfur reduction) | Facultative anaerobes and obligate anaerobes | Sulfur0 | −0.27 | Desulfuromonadales | |
Acetogenesis (carbon dioxide reduction) | Obligate anaerobes | Acetate | −0.30 | Acetobacterium woodii | |
Halorespiration | Facultative anaerobes and obligate anaerobes | Halocarbon() | Halide ions, dehalogenated compounds() | +0.25 – +0.60 | Dehalococcoides and Dehalobacter species |
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