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Bacterial oxygen production in the dark
Nitric oxide (NO) and nitrous oxide (N(2)O) are among nature’s most powerful electron acceptors. In recent years it became clear that microorganisms can take advantage of the oxidizing power of these compounds to degrade aliphatic and aromatic hydrocarbons. For two unrelated bacterial species, the “...
Autores principales: | , , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
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Frontiers Research Foundation
2012
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3413370/ https://www.ncbi.nlm.nih.gov/pubmed/22891064 http://dx.doi.org/10.3389/fmicb.2012.00273 |
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author | Ettwig, Katharina F. Speth, Daan R. Reimann, Joachim Wu, Ming L. Jetten, Mike S. M. Keltjens, Jan T. |
author_facet | Ettwig, Katharina F. Speth, Daan R. Reimann, Joachim Wu, Ming L. Jetten, Mike S. M. Keltjens, Jan T. |
author_sort | Ettwig, Katharina F. |
collection | PubMed |
description | Nitric oxide (NO) and nitrous oxide (N(2)O) are among nature’s most powerful electron acceptors. In recent years it became clear that microorganisms can take advantage of the oxidizing power of these compounds to degrade aliphatic and aromatic hydrocarbons. For two unrelated bacterial species, the “NC10” phylum bacterium “Candidatus Methylomirabilis oxyfera” and the γ-proteobacterial strain HdN1 it has been suggested that under anoxic conditions with nitrate and/or nitrite, monooxygenases are used for methane and hexadecane oxidation, respectively. No degradation was observed with nitrous oxide only. Similarly, “aerobic” pathways for hydrocarbon degradation are employed by (per)chlorate-reducing bacteria, which are known to produce oxygen from chlorite [Formula: see text]. In the anaerobic methanotroph M. oxyfera, which lacks identifiable enzymes for nitrogen formation, substrate activation in the presence of nitrite was directly associated with both oxygen and nitrogen formation. These findings strongly argue for the role of NO, or an oxygen species derived from it, in the activation reaction of methane. Although oxygen generation elegantly explains the utilization of “aerobic” pathways under anoxic conditions, the underlying mechanism is still elusive. In this perspective, we review the current knowledge about intra-aerobic pathways, their potential presence in other organisms, and identify candidate enzymes related to quinol-dependent NO reductases (qNORs) that might be involved in the formation of oxygen. |
format | Online Article Text |
id | pubmed-3413370 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2012 |
publisher | Frontiers Research Foundation |
record_format | MEDLINE/PubMed |
spelling | pubmed-34133702012-08-13 Bacterial oxygen production in the dark Ettwig, Katharina F. Speth, Daan R. Reimann, Joachim Wu, Ming L. Jetten, Mike S. M. Keltjens, Jan T. Front Microbiol Microbiology Nitric oxide (NO) and nitrous oxide (N(2)O) are among nature’s most powerful electron acceptors. In recent years it became clear that microorganisms can take advantage of the oxidizing power of these compounds to degrade aliphatic and aromatic hydrocarbons. For two unrelated bacterial species, the “NC10” phylum bacterium “Candidatus Methylomirabilis oxyfera” and the γ-proteobacterial strain HdN1 it has been suggested that under anoxic conditions with nitrate and/or nitrite, monooxygenases are used for methane and hexadecane oxidation, respectively. No degradation was observed with nitrous oxide only. Similarly, “aerobic” pathways for hydrocarbon degradation are employed by (per)chlorate-reducing bacteria, which are known to produce oxygen from chlorite [Formula: see text]. In the anaerobic methanotroph M. oxyfera, which lacks identifiable enzymes for nitrogen formation, substrate activation in the presence of nitrite was directly associated with both oxygen and nitrogen formation. These findings strongly argue for the role of NO, or an oxygen species derived from it, in the activation reaction of methane. Although oxygen generation elegantly explains the utilization of “aerobic” pathways under anoxic conditions, the underlying mechanism is still elusive. In this perspective, we review the current knowledge about intra-aerobic pathways, their potential presence in other organisms, and identify candidate enzymes related to quinol-dependent NO reductases (qNORs) that might be involved in the formation of oxygen. Frontiers Research Foundation 2012-08-07 /pmc/articles/PMC3413370/ /pubmed/22891064 http://dx.doi.org/10.3389/fmicb.2012.00273 Text en Copyright © Ettwig, Speth, Reimann, Wu, Jetten and Keltjens. http://www.frontiersin.org/licenseagreement This is an open-access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/3.0/) , which permits use, distribution and reproduction in other forums, provided the original authors and source are credited and subject to any copyright notices concerning any third-party graphics etc. |
spellingShingle | Microbiology Ettwig, Katharina F. Speth, Daan R. Reimann, Joachim Wu, Ming L. Jetten, Mike S. M. Keltjens, Jan T. Bacterial oxygen production in the dark |
title | Bacterial oxygen production in the dark |
title_full | Bacterial oxygen production in the dark |
title_fullStr | Bacterial oxygen production in the dark |
title_full_unstemmed | Bacterial oxygen production in the dark |
title_short | Bacterial oxygen production in the dark |
title_sort | bacterial oxygen production in the dark |
topic | Microbiology |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3413370/ https://www.ncbi.nlm.nih.gov/pubmed/22891064 http://dx.doi.org/10.3389/fmicb.2012.00273 |
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