1978
DOI: 10.1128/aem.36.2.306-313.1978
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Factors Related to the Oxygen Tolerance of Anaerobic Bacteria

Abstract: The effect of atmospheric oxygen on the viability of 13 strains of anaerobic bacteria, two strains of facultative bacteria, and one aerobic organism was examined. There were great variations in oxygen tolerance among the bacteria. All facultative bacteria survived more than 72 h of exposure to atmospheric oxygen. The survival time for anaerobes ranged from less than 45 min for Peptostreptococcus anaerobius to more than 72 h for two Clostridium perfringens strains… Show more

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Cited by 134 publications
(71 citation statements)
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References 32 publications
(32 reference statements)
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“…The frequent observation of detection level of (DO concentrations between 0.05 and 0.1 mg/L) DO concentrations suggests a flux of DO into the plume (Figure 2) , although the ongoing Fe(III)-reduction within the chloroethene plume between the USGS 4 and USGS 8 transects demonstrates that the supply of O 2 is not sufficient to prevent the onset and apparent predominance of anaerobic redox conditions Bradley 1998, 2007;Chapelle et al 2005). The comparable that periodic O 2 exposure is an important component of this redox variability in anaerobically active shallow groundwater environments (Rolfe et al 1978;Krieg and Hoffman 1986;Kato et al 1993;Marschall et al 1993;Fridovich 1998). Likewise, mineralization of DCE and VC at DO concentrations below the current field standard for nominally anoxic conditions (0.1 to 0.5 mg/L) can be substantial (Bradley and Chapelle 1996, 1997, 1999a, 1999b, 2000aBradley et al , 1998cSingh et al 2004;Gossett 2010) in groundwater and surface water systems.…”
Section: Implications For Natural Attenuation In Shallow Chloroethenementioning
confidence: 99%
“…The frequent observation of detection level of (DO concentrations between 0.05 and 0.1 mg/L) DO concentrations suggests a flux of DO into the plume (Figure 2) , although the ongoing Fe(III)-reduction within the chloroethene plume between the USGS 4 and USGS 8 transects demonstrates that the supply of O 2 is not sufficient to prevent the onset and apparent predominance of anaerobic redox conditions Bradley 1998, 2007;Chapelle et al 2005). The comparable that periodic O 2 exposure is an important component of this redox variability in anaerobically active shallow groundwater environments (Rolfe et al 1978;Krieg and Hoffman 1986;Kato et al 1993;Marschall et al 1993;Fridovich 1998). Likewise, mineralization of DCE and VC at DO concentrations below the current field standard for nominally anoxic conditions (0.1 to 0.5 mg/L) can be substantial (Bradley and Chapelle 1996, 1997, 1999a, 1999b, 2000aBradley et al , 1998cSingh et al 2004;Gossett 2010) in groundwater and surface water systems.…”
Section: Implications For Natural Attenuation In Shallow Chloroethenementioning
confidence: 99%
“…For example, in a microaerophile, Spirillum voltans, a mutant that had NADH peroxidase activity was much more resistant to H P O P than the parent strain, which had no NADH peroxidase activity [9]. In some anaerobic bacteria, only peroxidase activity but not catalase and superoxide dismutase activity showed correlation with oxygen tolerance [10]. Rhodobacter capsulatus produces catalase-peroxidase and peroxidase, and a catalase-peroxidase negative mutant showed only a slight di¡erence from the parent strain as to the resistance to oxidative stress, suggesting that the peroxidase has an important function in eliminating activated O P molecules in the bacterium [11].…”
Section: Discussionmentioning
confidence: 99%
“…They suggest that continuous anaerobiosis is not an urgent requirement during plaque processing, at least if the exposure to oxygen is of short duration as in this study. It has been shown that even strict anaerobes may tolerate some exposure to oxygen (16,27), When strict anaerobes were exposed to room atmosphere for as long as 20-40 min there was a 30-70% reduetion in the colony counts (16).…”
Section: Discussionmentioning
confidence: 99%