Anaerobic respiration
Anaerobic respiration is respiration using electron acceptors other than molecular oxygen (O2). Although oxygen is not the final electron acceptor, the process still uses a respiratory electron transport chain.[1]
In
4H
2O2−
4), sulfate (SO2−
4), or elemental sulfur (S). These terminal electron acceptors have smaller reduction potentials
As compared with fermentation
Anaerobic cellular respiration and
There are two important anaerobic microbial methane formation pathways, through carbon dioxide / bicarbonate (HCO−
3) reduction (respiration) or acetate fermentation.[2]
Ecological importance
Anaerobic respiration is a critical component of the global
An example of the ecological importance of anaerobic respiration is the use of nitrate as a
Economic relevance
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.[7]
Specific types of anaerobic respiration are also critical in
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.[9]
Examples of electron acceptors in respiration
Type | Lifestyle | Electron acceptor | Products | Eo′ (V) | Example organisms |
---|---|---|---|---|---|
Aerobic respiration
|
facultative anaerobes
|
O2 | H2O, CO2 | +0.82 | prokaryotes
|
Perchlorate respiration | Facultative anaerobes
|
ClO− 4, ClO− 3 |
H2O, O2, Cl− | +0.797 | prokaryotes[10]
|
Iodate respiration | Facultative anaerobes
|
IO− 3 |
H2O, H2O2, I− | +0.72 | prokaryotes[12]
|
Iron reduction
|
Facultative anaerobes and obligate anaerobes
|
Fe(III) | Fe(II) | +0.75 | Organisms within the order Desulfuromonadales (such as Geobacter, Geothermobacter, Geopsychrobacter, Pelobacter) and Shewanella species [13] |
Manganese | Facultative anaerobes and obligate anaerobes
|
Mn(IV) | Mn(II) | Desulfuromonadales and Shewanella species [13] | |
Cobalt reduction | Facultative anaerobes and obligate anaerobes
|
Co(III) | Co(II) | Geobacter sulfurreducens | |
Uranium reduction | Facultative anaerobes and obligate anaerobes
|
U(VI) | U(IV) | Geobacter metallireducens, Shewanella oneidensis[14] | |
Nitrate reduction (denitrification) | Facultative anaerobes
|
Nitrate NO− 3 |
(Ultimately) N2 | +0.40 | Paracoccus denitrificans, Escherichia coli |
Fumarate respiration | Facultative anaerobes
|
Fumarate
|
Succinate
|
+0.03 | Escherichia coli |
Sulfate respiration
|
Obligate anaerobes | Sulfate SO2− 4 |
Sulfide HS− | −0.22 | Many Deltaproteobacteria species in the orders Desulfobacterales, Desulfovibrionales, and Syntrophobacterales
|
Methanogenesis (carbon dioxide reduction) | Methanogens
|
Carbon dioxide CO2 | Methane CH4 | −0.25 | Methanosarcina barkeri |
Sulfur respiration (sulfur reduction) | Facultative anaerobes and obligate anaerobes
|
Sulfur S0 | Sulfide HS− | −0.27 | Desulfuromonadales |
Acetogenesis (carbon dioxide reduction) | Obligate anaerobes | Carbon dioxide CO2 | Acetate | −0.30 | Acetobacterium woodii |
Dehalorespiration | Facultative anaerobes and obligate anaerobes
|
Halogenated organic compounds R–X | Halide ions and dehalogenated compound X− + R–H | +0.25 – +0.60[15] | Dehalococcoides and Dehalobacter species |
See also
- Hydrogenosomes and mitosomes
- Anaerobic digestion
- Microbial fuel cell
- Standard electrode potential (data page)
- Table of standard reduction potentials for half-reactions important in biochemistry
- Lithotrophs
Further reading
- Gregory, Kelvin B.; Bond, Daniel R.; Lovley, Derek R. (June 2004). "Graphite electrodes as electron donors for anaerobic respiration". Environmental Microbiology. 6 (6): 596–604. PMID 15142248.