2005
DOI: 10.1128/aem.71.10.6134-6141.2005
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Identification of Bacteria Potentially Responsible for Oxic and Anoxic Sulfide Oxidation in Biofilters of a Recirculating Mariculture System

Abstract: Bacteria presumably involved in oxygen-or nitrate-dependent sulfide oxidation in the biofilters of a recirculating marine aquaculture system were identified using a new application of reverse transcription-PCR denaturing gradient gel electrophoresis (DGGE) analysis termed differential-transcription (DT)-DGGE. Biofilter samples were incubated in various concentrations of sulfide or thiosulfate (0 to 5 mM) with either oxygen or nitrate as the sole electron acceptor. Before and after short-term incubations (10 to… Show more

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Cited by 71 publications
(41 citation statements)
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“…Evidence for sulfurdriven denitrification has been reported in marine ecosystems, including oceanic redoxclines (Brettar et al 2006, Grote et al 2008, near-coastal upwelling zones (Fossing et al 1995, Schulz et al 1999, and engineered mariculture systems (Cytryn et al 2005a, Sher et al 2008. The patterns of biogeochemical activity that we observed over depth are very similar to those documented in the Baltic Sea (Brettar & Rheinheimer 1991, Brettar et al 2006, albeit over a much smaller spatial scale (1 m vs. 10s of meters).…”
Section: Discussionsupporting
confidence: 73%
“…Evidence for sulfurdriven denitrification has been reported in marine ecosystems, including oceanic redoxclines (Brettar et al 2006, Grote et al 2008, near-coastal upwelling zones (Fossing et al 1995, Schulz et al 1999, and engineered mariculture systems (Cytryn et al 2005a, Sher et al 2008. The patterns of biogeochemical activity that we observed over depth are very similar to those documented in the Baltic Sea (Brettar & Rheinheimer 1991, Brettar et al 2006, albeit over a much smaller spatial scale (1 m vs. 10s of meters).…”
Section: Discussionsupporting
confidence: 73%
“…Samples taken in 2005 and in 2007 for this spring, however, had ␦ 13 C values of Ϫ6.1‰ and Ϫ12.4‰, respectively. Such pronounced isotopic enrichments are typical of methanotrophy, which enriches the residual methane pool in 13 C (resulting in a less negative ␦ 13 C value) due to preferential enzymatic breakage of 12 C-H bonds versus that of 13 C-H bonds (52). Similarly, GH-4 showed very enriched ␦ DIC ␦ 13 C values were Ϫ5.6‰ and Ϫ6.5‰ for GH-2 and GH-4, respectively.…”
Section: Vol 74 2008 Microbial Populations Of Cold Saline Arctic Spmentioning
confidence: 95%
“…Besides chemical oxidation, microorganisms are involved in the oxidation of sulfide at oxicanoxic interfaces; this reaction initiates the first step of the sulfur oxidation process (Cytryn et al, 2005;Jorgensen, 1982) and produces sulfate or sulfur as the major oxidation product (Friedrich, 1998;Ruepp et al, 2000;She et al, 2001;Theissen et al, 2003).…”
Section: Introductionmentioning
confidence: 99%