1985
DOI: 10.1111/j.1574-6968.1985.tb01153.x
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Sulphate reduction in oxic and sub-oxic North-East Atlantic sediments

Abstract: Oxic and sub‐oxic N.‐E. Atlantic sediments were examined for sulphate‐reducing activity. Oxygen and/or nitrate reduction are probably the dominant mineralisation processes in the abyssal plain sediment studied. A low rate of sulphate reduction (0.1 nmol SO2−4/ml/day) was recorded in the surface 5 cm of the continental slope sediment, together with the presence of a range of sulphate‐reducing bacteria (SRB). A higher activity of sulphate reduction (2.2 nmol SO2−4/ml/day) occurred in the continental shelf sedime… Show more

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Cited by 34 publications
(8 citation statements)
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“…Although growth of SRB requires anaerobic conditions, SRB are active in or near oxic-anoxic transition zones in marine and fresh water sediments (Battersby et al, 1985) and in microbial mats (Canfield and Desmarais, 1991), where sulfate may be regenerated by the oxidation of hydrogen sulfide (Widdel and Hansen, 1992;Johnson et al, 1997). Oxygen inhibits central redox proteins (Stams and Hansen, 1982;Cammack et al, 1994;Dolla et al, 2006) and cell division (Sass et al, 1998;Cypionka, 2000) in the SRB and generates reactive oxygen species (ROS) (Imlay, 2003;Dolla et al, 2006).…”
Section: Introductionmentioning
confidence: 99%
“…Although growth of SRB requires anaerobic conditions, SRB are active in or near oxic-anoxic transition zones in marine and fresh water sediments (Battersby et al, 1985) and in microbial mats (Canfield and Desmarais, 1991), where sulfate may be regenerated by the oxidation of hydrogen sulfide (Widdel and Hansen, 1992;Johnson et al, 1997). Oxygen inhibits central redox proteins (Stams and Hansen, 1982;Cammack et al, 1994;Dolla et al, 2006) and cell division (Sass et al, 1998;Cypionka, 2000) in the SRB and generates reactive oxygen species (ROS) (Imlay, 2003;Dolla et al, 2006).…”
Section: Introductionmentioning
confidence: 99%
“…In particular, sulfate‐reducers were isolated from oxic environments close to anoxic or periodically anoxic zones (e.g. [4–6]). Also, these bacteria were shown to produce ATP in the presence of oxygen (e.g.…”
Section: Introductionmentioning
confidence: 99%
“…A number of sulfate-reducing bacteria (SRB) have been detected in oxic surface sediments of various aquatic environments where the E h values were higher than those for sulfate reduction; e.g. marine coastal sediments [1,2], oceanic sediments [3] and freshwater sediments [4][5][6]. Also, some types of SRB were enriched and isolated from strongly oxidized open sea [7] and from well aerated activated sludge and oxic marine muds [8].…”
Section: Introductionmentioning
confidence: 99%