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Anaerobic respiration

From Wikipedia, the free encyclopedia
Respiration using electron acceptors other than oxygen
Not to be confused withFermentation.

Anaerobic respiration isrespiration usingelectron acceptors other thanmolecular oxygen (O2) in itselectron transport chain.[1]

Inaerobic organisms, electrons are shuttled to an electron transport chain, and the final electron acceptor isoxygen. Molecular oxygen is an excellent electron acceptor.Anaerobes instead use less-oxidizing substances such asnitrate (NO
3
),fumarate (C
4
H
2
O2−
4
),sulfate (SO2−
4
), or elementalsulfur (S). These terminal electron acceptors have smallerreduction potentials than O2. Less energy per oxidized molecule is released. Therefore, anaerobic respiration is less efficient than aerobic.[citation needed]

As compared with fermentation

[edit]
Further information:Fermentation

Anaerobic cellular respiration andfermentation generateATP in very different ways, and the terms should not be treated as synonyms. Cellular respiration (bothaerobic and anaerobic) uses highly reduced chemical compounds such asNADH andFADH2 (for example produced duringglycolysis and thecitric acid cycle) to establish anelectrochemical gradient (often a proton gradient) across a membrane. This results in anelectrical potential or ionconcentration difference across the membrane. The reduced chemical compounds are oxidized by a series of respiratoryintegral membrane proteins with sequentially increasingreduction potentials, with the final electron acceptor being oxygen (inaerobic respiration) or another chemical substance (in anaerobic respiration). Aproton motive force drivesprotons down the gradient (across the membrane) through the proton channel ofATP synthase. The resulting current drives ATP synthesis fromADP and inorganic phosphate.[citation needed]

Fermentation, in contrast, does not use an electrochemical gradient but instead uses onlysubstrate-level phosphorylation to produce ATP. The electron acceptorNAD+ is regenerated fromNADH 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 ofglyceraldehyde-3-phosphate is oxidized back to NAD+ by the reduction ofpyruvate tolactic acid at a later stage in the pathway. Inyeast,acetaldehyde is reduced toethanol to regenerate NAD+.[citation needed]

There are two important anaerobic microbial methane formation pathways, throughcarbon dioxide /bicarbonate (HCO
3
) reduction (respiration) or acetate fermentation.[2]

Ecological importance

[edit]

Anaerobic respiration is a critical component of the globalnitrogen,iron,sulfur, andcarbon cycles through the reduction of the oxyanions of nitrogen, sulfur, and carbon to more-reduced compounds. Thebiogeochemical cycling of these compounds, which depends upon anaerobic respiration, significantly impacts thecarbon cycle andglobal warming. 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 ofoxygen gas.[citation needed]

An example of the ecological importance of anaerobic respiration is the use of nitrate as aterminal electron acceptor, or dissimilatorydenitrification, which is the main route by which fixednitrogen is returned to the atmosphere as molecular nitrogen gas.[3] 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.[4] Another example ismethanogenesis, a form of carbon-dioxide respiration, that is used to producemethane gas byanaerobic 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 potentgreenhouse gas.[5]Sulfate respiration produceshydrogen 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 ofsulfidic metal ores.[6]

Economic relevance

[edit]
Anaerobic Denitrification (ETC System)

The model above shows the process of anaerobic respiration throughdenitrification, which uses nitrogen (in the form of nitrate,NO
3
) as the electron acceptor.NO
3
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 theaerobic electron transport chain.

Dissimilatorydenitrification is widely used in the removal ofnitrate andnitrite from municipal wastewater. An excess of nitrate can lead toeutrophication 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 inbioremediation, which uses microorganisms to convert toxic chemicals into less-harmful molecules to clean up contaminated beaches, aquifers, lakes, and oceans. For example, toxicarsenate orselenate can be reduced to less toxic compounds by various anaerobic bacteria via anaerobic respiration. The reduction ofchlorinated chemical pollutants, such asvinyl chloride andcarbon tetrachloride, also occurs through anaerobic respiration.[citation needed][8]

Anaerobic respiration is useful in generating electricity inmicrobial 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

[edit]
TypeLifestyleElectron acceptorProductsEo′ (V)Example organisms
Aerobic respirationObligate aerobes andfacultative anaerobesO2H2O+0.82Aerobic organisms such asEscherichia coli
(Per)chlorate respirationFacultative anaerobesClO4,ClO3H2O,O2,Cl+0.797Azospira suillum,Sedimenticola selenatireducens,Sedimenticola thiotaurini, and othergram negativeprokaryotes[10]
Iodate respirationFacultative anaerobesIO3H2O,H2O2,I+0.72Denitromonas,[11]Azoarcus,Pseudomonas, and otherprokaryotes[12]
Iron reduction
(Dissimilatory iron reducing bacteria)
Facultative anaerobes andobligate anaerobesFe3+Fe2++0.75Organisms within the orderDesulfuromonadales (such asGeobacter,Geothermobacter,Geopsychrobacter,Pelobacter) andShewanella species[13]
Manganese reduction
(dissimilatory metal-reducing microorganisms)
Facultative anaerobes andobligate anaerobesMn4+Mn2+Desulfuromonadales andShewanella species[13]
Cobalt reduction
(dissimilatory metal-reducing microorganisms)
Facultative anaerobes andobligate anaerobesCo3+Co2+Geobacter sulfurreducens
Uranium reduction
(dissimilatory metal-reducing microorganisms)
Facultative anaerobes andobligate anaerobesU6+U4+Geobacter metallireducens,Shewanella oneidensis[14]
Denitrification
(nitrate reduction)
Facultative anaerobesNO3(Ultimately) N2+0.40Paracoccus denitrificans,Escherichia coli
Fumarate respirationFacultative anaerobesFumarateSuccinate+0.03Escherichia coli
Sulfate respirationObligate anaerobesSO2−4H2O,HS−0.22ManyDeltaproteobacteria species in the ordersDesulfobacterales,Desulfovibrionales, andSyntrophobacterales
Methanogenesis (carbon dioxide reduction)MethanogensCO2CH4−0.25Methanosarcina barkeri
Sulfur respiration (sulfur reduction)Facultative anaerobes andobligate anaerobesS0HS−0.27Desulfuromonadales
Acetogenesis (carbon dioxide reduction)Obligate anaerobesCO2Acetate−0.30Acetobacterium woodii
HalorespirationFacultative anaerobes andobligate anaerobesHalogenated organic compounds
(RX)
Halide ions, dehalogenated compounds
(X +RH)
+0.25 – +0.60[15]Dehalococcoides andDehalobacter species

See also

[edit]

Further reading

[edit]

References

[edit]
  1. ^Slonczewski, Joan L.; Foster, John W. (2011).Microbiology: An Evolving Science (2nd ed.). New York: W.W. Norton. p. 166.ISBN 9780393934472.
  2. ^Sapart; et al. (2017)."The origin of methane in the East Siberian Arctic Shelf unraveled with triple isotope analysis".Biogeosciences.14 (9):2283–2292.Bibcode:2017BGeo...14.2283S.doi:10.5194/bg-14-2283-2017.hdl:2013/ULB-DIPOT:oai:dipot.ulb.ac.be:2013/253190.
  3. ^Simon, Jörg; Klotz, Martin G. (2013-02-01)."Diversity and evolution of bioenergetic systems involved in microbial nitrogen compound transformations".Biochimica et Biophysica Acta (BBA) - Bioenergetics.1827 (2):114–135.doi:10.1016/j.bbabio.2012.07.005.PMID 22842521.
  4. ^Graf, Jon S.; Schorn, Sina; Kitzinger, Katharina; Ahmerkamp, Soeren; Woehle, Christian; Huettel, Bruno; Schubert, Carsten J.; Kuypers, Marcel M. M.; Milucka, Jana (3 March 2021)."Anaerobic endosymbiont generates energy for ciliate host by denitrification".Nature.591 (7850):445–450.Bibcode:2021Natur.591..445G.doi:10.1038/s41586-021-03297-6.PMC 7969357.PMID 33658719.
  5. ^Bogner, Jean; Pipatti, Riitta; Hashimoto, Seiji; Diaz, Cristobal; Mareckova, Katarina; Diaz, Luis; Kjeldsen, Peter; Monni, Suvi; Faaij, Andre (2008-02-01). "Mitigation of global greenhouse gas emissions from waste: conclusions and strategies from the Intergovernmental Panel on Climate Change (IPCC) Fourth Assessment Report. Working Group III (Mitigation)".Waste Management & Research.26 (1):11–32.Bibcode:2008WMR....26...11B.doi:10.1177/0734242x07088433.ISSN 0734-242X.PMID 18338699.S2CID 29740189.
  6. ^Pester, Michael; Knorr, Klaus-Holger; Friedrich, Michael W.; Wagner, Michael; Loy, Alexander (2012-01-01)."Sulfate-reducing microorganisms in wetlands – fameless actors in carbon cycling and climate change".Frontiers in Microbiology.3: 72.doi:10.3389/fmicb.2012.00072.ISSN 1664-302X.PMC 3289269.PMID 22403575.
  7. ^Nancharaiah, Y. V.; Venkata Mohan, S.; Lens, P. N. L. (2016-09-01). "Recent advances in nutrient removal and recovery in biological and bioelectrochemical systems".Bioresource Technology.215:173–185.Bibcode:2016BiTec.215..173N.doi:10.1016/j.biortech.2016.03.129.ISSN 1873-2976.PMID 27053446.
  8. ^Polasko, Alexandra Lapat; Miao, Yu; Kwok, Ivy; Park, Keunseok; Park, Junyoung O.; Mahendra, Shaily (2021)."Vinyl chloride and 1,4-dioxane metabolism by Pseudonocardia dioxanivorans CB1190".Journal of Hazardous Materials Letters.2.Bibcode:2021JHzML...200039P.doi:10.1016/j.hazl.2021.100039.S2CID 239140980.
  9. ^Xu, Bojun; Ge, Zheng; He, Zhen (2015-05-15)."Sediment microbial fuel cells for wastewater treatment: challenges and opportunities".Environmental Science: Water Research & Technology.1 (3):279–284.doi:10.1039/c5ew00020c.hdl:10919/64969.ISSN 2053-1419.
  10. ^Melnyk, Ryan A.; Engelbrektson, Anna; Clark, Iain C.; Carlson, Hans K.; Byrne-Bailey, Kathy; Coates, John D. (2011)."Identification of a Perchlorate Reduction Genomic Island with Novel Regulatory and Metabolic Genes".Applied and Environmental Microbiology.77 (20):7401–7404.Bibcode:2011ApEnM..77.7401M.doi:10.1128/AEM.05758-11.PMC 3194888.PMID 21856823.
  11. ^Reyes-Umana, Victor; Henning, Zachary; Lee, Kristina; Barnum, Tyler P.; Coates, John D. (2021-07-02)."Genetic and phylogenetic analysis of dissimilatory iodate-reducing bacteria identifies potential niches across the world's oceans".The ISME Journal.16 (1):38–49.doi:10.1038/s41396-021-01034-5.ISSN 1751-7370.PMC 8692401.PMID 34215855.S2CID 235722250.
  12. ^Reyes-Umana, Victor; Henning, Zachary; Lee, Kristina; Barnum, Tyler; Coates, John (2020). "Genetic and phylogenetic analysis of dissimilatory iodate-reducing bacteria identifies potential niches across the world's oceans".bioRxiv 10.1101/2020.12.28.424624.
  13. ^abRichter, Katrin; Schicklberger, Marcus; Gescher, Johannes (2012-02-01)."Dissimilatory reduction of extracellular electron acceptors in anaerobic respiration".Applied and Environmental Microbiology.78 (4):913–921.Bibcode:2012ApEnM..78..913R.doi:10.1128/AEM.06803-11.ISSN 1098-5336.PMC 3273014.PMID 22179232.
  14. ^Wall, Judy D.; Krumholz, Lee R. (13 October 2006). "Uranium Reduction".Annual Review of Microbiology.60:149–166.doi:10.1146/annurev.micro.59.030804.121357.PMID 16704344.
  15. ^Holliger, C.; Wohlfarth, G.; Diekert, G. (1998)."Reductive dechlorination in the energy metabolism of anaerobic bacteria"(PDF).FEMS Microbiology Reviews.22 (5): 383.doi:10.1111/j.1574-6976.1998.tb00377.x.S2CID 85965965.
General
Energy
metabolism
Aerobic respiration
Anaerobic respiration
  • Electron acceptors other than oxygen
Fermentation
Specific
paths
Protein metabolism
Amino acid
Nucleotide
metabolism
Carbohydrate metabolism
(carbohydrate catabolism
andanabolism)
Human
Nonhuman
Lipid metabolism
(lipolysis,lipogenesis)
Fatty acid metabolism
Other
Other
Metro-style map of major metabolic pathways



The image above contains clickable links
Majormetabolic pathways inmetro-style map. Click any text (name of pathway or metabolites) to link to the corresponding article.
Single lines: pathways common to most lifeforms. Double lines: pathways not in humans (occurs in e.g. plants, fungi, prokaryotes). Orange nodes:carbohydrate metabolism. Violet nodes:photosynthesis. Red nodes:cellular respiration. Pink nodes:cell signaling. Blue nodes:amino acid metabolism. Grey nodes:vitamin andcofactor metabolism. Brown nodes:nucleotide andprotein metabolism. Green nodes:lipid metabolism.
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