4.6 Article

Succession of internal sulfur cycles and sulfur-oxidizing bacterial communities in microaerophilic wastewater biofilms

Journal

APPLIED AND ENVIRONMENTAL MICROBIOLOGY
Volume 71, Issue 5, Pages 2520-2529

Publisher

AMER SOC MICROBIOLOGY
DOI: 10.1128/AEM.71.5.2520-2529.2005

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The succession of sulfur-oxidizing bacterial (SOB) community structure and the complex internal sulfur cycle occurring in wastewater biofilms growing under microaerophillic conditions was analyzed by using a polyphasic approach that employed 16S rRNA gene-cloning analysis combined with fluorescence in situ hybridization, microelectrode measurements, and standard batch and reactor experiments. A complete sulfur cycle was established via So accumulation within 80 days in the biofilms in replicate. This development was generally split into two phases, (i) a sulfur-accumulating phase and (ii) a sulfate-producing phase. In the first phase (until about 40 days), since the sulfide production rate (sulfate-reducing activity) exceeded the maximum sulfide-oxidizing capacity of SOB in the biofilms, H2S was only partially oxidized to S-0 by mainly Thiomicrospira denitirificans with NO3- as an electron acceptor, leading to significant accumulation of So in the biofilms. In the second phase, the SOB populations developed further and diversified with time. In particular, S-0 accumulation promoted the growth of a novel strain, strain SO07, which predominantly carried out the oxidation of S-0 to SO42- under oxic conditions, and Thiothrix sp. strain CT3. In situ hybridization analysis revealed that the dense populations of Thiothrix (ca. 10(9) cells cm(-3)) and strain SO07 (ca. 10(8) cells cm(-3)) were found at the sulfur-rich surface (100 mu m), while the population of Thiomicrospira denitirificans was distributed throughout the biofilms with a density of ca. 10(7) to 10(8) cells cm(-3). Microelectrode measurements revealed that active sulfide-oxidizing zones overlapped the spatial distributions of different phylogenetic SOB groups in the biofilms. As a consequence, the sulfide-oxidizing capacities of the biofilms became high enough to completely oxidize all H,S produced by SRB to SO42- in the second phase, indicating establishment of the complete sulfur cycle in the biofilms.

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