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Anaerobic respiration is respiration using other than molecular oxygen (O2) in its electron transport chain.

(2025). 9780393934472, W.W. Norton.

In aerobic organisms, electrons are shuttled to an electron transport chain, and the final electron acceptor is . Molecular oxygen is an excellent electron acceptor. instead use less-oxidizing substances such as (), (), (), or elemental (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.


As compared with fermentation
Anaerobic cellular respiration and generate ATP in very different ways, and the terms should not be treated as synonyms. Cellular respiration (both aerobic and anaerobic) uses highly reduced chemical compounds such as and FADH2 (for example produced during and the citric acid cycle) to establish an electrochemical gradient (often a proton gradient) across a membrane. This results in an electrical potential or ion difference across the membrane. The reduced chemical compounds are oxidized by a series of respiratory integral membrane proteins with sequentially increasing reduction potentials, with the final electron acceptor being oxygen (in aerobic respiration) or another chemical substance (in anaerobic respiration). A proton motive force drives down the gradient (across the membrane) through the proton channel of . The resulting current drives ATP synthesis from ADP and inorganic phosphate.

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 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 to at a later stage in the pathway. In , is reduced to to regenerate NAD+.

There are two important anaerobic microbial methane formation pathways, through / () reduction (respiration) or acetate fermentation.


Ecological importance
Anaerobic respiration is a critical component of the global , , , and cycles through the reduction of the oxyanions of nitrogen, sulfur, and carbon to more-reduced compounds. The biogeochemical cycling of these compounds, which depends upon anaerobic respiration, significantly impacts the and . Anaerobic respiration occurs in many environments, including freshwater and marine sediments, soil, subsurface aquifers, deep subsurface environments, and biofilms. Even environments that contain oxygen, such as soil, have micro-environments that lack oxygen due to the slow diffusion characteristics of gas.

An example of the ecological importance of anaerobic respiration is the use of nitrate as a terminal electron acceptor, or dissimilatory , 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 , a form of carbon-dioxide respiration, that is used to produce 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 . Sulfate respiration produces , 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 .


Economic relevance
[[File:Anaerobic Denitrification (ETC System).svg|thumb|Anaerobic Denitrification (ETC System)

The model above shows the process of anaerobic respiration through , which uses nitrogen (in the form of nitrate, ) as the electron acceptor. goes through respiratory dehydrogenase and reduces through each step from the ubiquinose through the bc1 complex through the ATP synthase protein as well. Each reductase removes oxygen step by step so that the final product of anaerobic respiration is N2.

1. Cytoplasm
2. Periplasm

Compare to the aerobic electron transport chain.]] Dissimilatory is widely used in the removal of and from municipal wastewater. An excess of nitrate can lead to 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 , which uses microorganisms to convert toxic chemicals into less-harmful molecules to clean up contaminated beaches, aquifers, lakes, and oceans. For example, toxic or can be reduced to less toxic compounds by various anaerobic bacteria via anaerobic respiration. The reduction of , such as 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.


Examples of electron acceptors in respiration
Aerobic respiration and facultative anaerobes +0.82 such as
(Per)chlorate respirationFacultative anaerobes , ,+0.797, Sedimenticola selenatireducens, Sedimenticola thiotaurini, and other
Iodate respirationFacultative anaerobes ,+0.72, , , and other
Iron reduction(Dissimilatory iron reducing bacteria)Facultative anaerobes and obligate anaerobes +0.75Organisms within the order Desulfuromonadales (such as , , Geopsychrobacter, Pelobacter) and species
Manganese reduction(dissimilatory metal-reducing microorganisms)Facultative anaerobes and obligate anaerobes Desulfuromonadales and 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
(nitrate reduction)Facultative anaerobes (Ultimately) N2+0.40Paracoccus denitrificans,
Fumarate respirationFacultative anaerobes+0.03
Sulfate respirationObligate anaerobes ,−0.22Many Deltaproteobacteria species in the orders Desulfobacterales, Desulfovibrionales, and Syntrophobacterales
(carbon dioxide reduction) −0.25Methanosarcina barkeri
Sulfur respiration (sulfur reduction)Facultative anaerobes and obligate anaerobes0 −0.27Desulfuromonadales
(carbon dioxide reduction)Obligate anaerobes −0.30Acetobacterium woodii
Facultative anaerobes and obligate anaerobes() ions, dehalogenated compounds()+0.25 – +0.60 and species


See also
  • and – mitochondrion-related organelles (MROs)
  • Spinoloricus cinziae – an anaerobic microbial animal with hydrogenosome-like organelles
  • Monocercomonoides – genus of eukaryotes that lack mitochondria and MROs entirely
  • Anaerobic digestion
  • Microbial fuel cell
  • Standard electrode potential (data page)
  • Table of standard reduction potentials for half-reactions important in biochemistry


Further reading
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