The anaerobic degradation of gaseous, nonmethane alkanes — From in situ processes to microorganisms

The short chain, gaseous alkanes ethane, propane, n- and iso-butane are released in significant amounts into the atmosphere, where they contribute to tropospheric chemistry and ozone formation. Biodegradation of gaseous alkanes by aerobic microorganisms, mostly bacteria and fungi isolated from terre...

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Published in:Computational and Structural Biotechnology Journal
Main Author: Florin Musat
Format: Article
Language:English
Published: Elsevier 2015-01-01
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2001037015000112
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author Florin Musat
author_facet Florin Musat
author_sort Florin Musat
collection DOAJ
container_title Computational and Structural Biotechnology Journal
description The short chain, gaseous alkanes ethane, propane, n- and iso-butane are released in significant amounts into the atmosphere, where they contribute to tropospheric chemistry and ozone formation. Biodegradation of gaseous alkanes by aerobic microorganisms, mostly bacteria and fungi isolated from terrestrial environments, has been known for several decades. The first indications for short chain alkane anaerobic degradation were provided by geochemical studies of deep-sea environments around hydrocarbon seeps, and included the uncoupling of the sulfate-reduction and anaerobic oxidation of methane rates, the consumption of gaseous alkanes in anoxic sediments, or the enrichment in 13C of gases in interstitial water vs. the source gas. Microorganisms able to degrade gaseous alkanes were recently obtained from deep-sea and terrestrial sediments around hydrocarbon seeps. Up to date, only sulfate-reducing pure or enriched cultures with ethane, propane and n-butane have been reported. The only pure culture presently available, strain BuS5, is affiliated to the Desulfosarcina–Desulfococcus cluster of the Deltaproteobacteria. Other phylotypes involved in gaseous alkane degradation have been identified based on stable-isotope labeling and whole-cell hybridization. Under anoxic conditions, propane and n-butane are activated similar to the higher alkanes, by homolytic cleavage of the CH bond of a subterminal carbon atom, and addition of the ensuing radical to fumarate, yielding methylalkylsuccinates. An additional mechanism of activation at the terminal carbon atoms was demonstrated for propane, which could in principle be employed also for the activation of ethane.
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spelling doaj-art-c58ff83d4e0946e1b53229baadf200dc2025-08-19T19:46:22ZengElsevierComputational and Structural Biotechnology Journal2001-03702015-01-0113C22222810.1016/j.csbj.2015.03.002The anaerobic degradation of gaseous, nonmethane alkanes — From in situ processes to microorganismsFlorin MusatThe short chain, gaseous alkanes ethane, propane, n- and iso-butane are released in significant amounts into the atmosphere, where they contribute to tropospheric chemistry and ozone formation. Biodegradation of gaseous alkanes by aerobic microorganisms, mostly bacteria and fungi isolated from terrestrial environments, has been known for several decades. The first indications for short chain alkane anaerobic degradation were provided by geochemical studies of deep-sea environments around hydrocarbon seeps, and included the uncoupling of the sulfate-reduction and anaerobic oxidation of methane rates, the consumption of gaseous alkanes in anoxic sediments, or the enrichment in 13C of gases in interstitial water vs. the source gas. Microorganisms able to degrade gaseous alkanes were recently obtained from deep-sea and terrestrial sediments around hydrocarbon seeps. Up to date, only sulfate-reducing pure or enriched cultures with ethane, propane and n-butane have been reported. The only pure culture presently available, strain BuS5, is affiliated to the Desulfosarcina–Desulfococcus cluster of the Deltaproteobacteria. Other phylotypes involved in gaseous alkane degradation have been identified based on stable-isotope labeling and whole-cell hybridization. Under anoxic conditions, propane and n-butane are activated similar to the higher alkanes, by homolytic cleavage of the CH bond of a subterminal carbon atom, and addition of the ensuing radical to fumarate, yielding methylalkylsuccinates. An additional mechanism of activation at the terminal carbon atoms was demonstrated for propane, which could in principle be employed also for the activation of ethane.http://www.sciencedirect.com/science/article/pii/S2001037015000112Gaseous alkanesMicrobial degradationAnaerobicMarineSedimentsSulfate
spellingShingle Florin Musat
The anaerobic degradation of gaseous, nonmethane alkanes — From in situ processes to microorganisms
Gaseous alkanes
Microbial degradation
Anaerobic
Marine
Sediments
Sulfate
title The anaerobic degradation of gaseous, nonmethane alkanes — From in situ processes to microorganisms
title_full The anaerobic degradation of gaseous, nonmethane alkanes — From in situ processes to microorganisms
title_fullStr The anaerobic degradation of gaseous, nonmethane alkanes — From in situ processes to microorganisms
title_full_unstemmed The anaerobic degradation of gaseous, nonmethane alkanes — From in situ processes to microorganisms
title_short The anaerobic degradation of gaseous, nonmethane alkanes — From in situ processes to microorganisms
title_sort anaerobic degradation of gaseous nonmethane alkanes from in situ processes to microorganisms
topic Gaseous alkanes
Microbial degradation
Anaerobic
Marine
Sediments
Sulfate
url http://www.sciencedirect.com/science/article/pii/S2001037015000112
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