Microarray and functional gene analyses of sulfate-reducing prokaryotes in low-sulfate, acidic fens reveal cooccurrence of recognized genera and novel lineages

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 μM) 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 microarray 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 Desulfomonile 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 (18, 19, 38, 41, 53, 56, 57, 72) and freshwater habitats (39, 40, 59, 60), relatively 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).δ³⁴S values and ³⁵S-labeling patterns indicate that the dissimilatory reduction of sulfate is an ongoing process in the acidic fens of a forested catchment in northern Bavaria, Germany (Lehstenbach, Fichtelgebirge) (3, 5). The deposition of sulfur that originated from the combustion of soft coal in Eastern Europe (10) led to accumulation of sulfur in the soils of this catchment (4). Although pollution controls have lessened the deposition in recent years, desorption of sulfate in aerated upland soils causes sulfate to enter fens at lower elevations. It was hypothesized that the dissimilatory reduction of sulfate in these mainly anoxic, waterlogged acidic fen soils (the pH of the fen soils is approximately 4) contributes to the retention of sulfur in this ecosystem (3, 4, 50). The reduction of sulfate in these fens is also a sink for protons and thus decreases the acidity of the soil solution and groundwater of this habitat.The acidity and low sulfate content of some of the fens in the Lehstenbach catchment provide an unusual habitat for SRPs, and the occurrence and activity of these organisms in such habitats have received little attention. The main objectives of this study were (i) to assess the capacity of the fen soils to reduce sulfate along vertical soil profiles in the upper peat layers, (ii) to determine the vertical community profiles for all known SRP lineages that inhabit the fens by the use of a 16S rRNA-based oligonucleotide microarray (SRP-PhyloChip) (44), (iii) to resolve the possible existence of novel SRP lineages in the fens by retrieval of dsrAB, which are genes that encode the alpha and beta subunits of the siroheme dissimilatory (bi)sulfite reductase (EC 1.8.99.3) (34, 66, 74), and (iv) to deduce the possible in situ functional relationships that can be inferred from this collective information.