Novel Lineages Cooccurrence of Recognized Genera and Low-Sulfate, Acidic Fens Reveal of Sulfate-Reducing Prokaryotes in Microarray and Functional Gene Analyses

Low-sulfate, acidic (approximately pH 4) fens in the Lehstenbach catchment in the Fichtelgebirge mountains in Germany are unusual habitats for sulfate-reducing prokaryotes (SRPs) that have been postulated to facilitate the retention of sulfur and protons in these ecosystems. Despite the low in situ availability of sulfate (concentration in the soil solution, 20 to 200 ␮M) and the acidic conditions (soil and soil solution pHs, approximately 4 and 5, respectively), the upper peat layers of the soils from two fens (Schlöppnerbrunnen I and II) of this catchment displayed significant sulfate-reducing capacities. 16S rRNA gene-based oligonucleotide mi-croarray analyses revealed stable diversity patterns for recognized SRPs in the upper 30 cm of both fens. Members of the family " Syntrophobacteraceae " were detected in both fens, while signals specific for the genus De-sulfomonile were observed only in soils from Schlöppnerbrunnen I. These results were confirmed and extended by comparative analyses of environmentally retrieved 16S rRNA and dissimilatory (bi)sulfite reductase (dsrAB) gene sequences; dsrAB sequences from Desulfobacca-like SRPs, which were not identified by microarray analysis , were obtained from both fens. Hypotheses concerning the ecophysiological role of these three SRP groups in the fens were formulated based on the known physiological properties of their cultured relatives. In addition to these recognized SRP lineages, six novel dsrAB types that were phylogenetically unrelated to all known SRPs were detected in the fens. These dsrAB sequences had no features indicative of pseudogenes and likely represent novel, deeply branching, sulfate-or sulfite-reducing prokaryotes that are specialized colonists of low-sulfate habitats. The dissimilatory reduction of sulfate is carried out exclusively by prokaryotic organisms and is one of the most important mineralization processes in anoxic aquatic environments, especially marine sediments (29, 30). In contrast to well-studied sulfate-reducing communities in marine little is known about the distribution, diversity, and in situ activities of sulfate-reducing prokaryotes (SRPs) in terrestrial ecosystems. The contribution of terrestrial SRPs to the overall turnover of organic matter is likely of minor importance on a global scale. However, SRPs contribute to the biodegradation of pollutants in soils and subsurface environments (1, 15, 49, 71) and are important to the geomicrobiology of specialized terrestrial habitats that are subject to flooding, such as rice fields (68, 76, 77) and fens (3, 5). ␦ 34 S values and 35 S-labeling patterns indicate that the dis-similatory reduction of sulfate is an ongoing process in the acidic fens of a forested catchment in northern …