H2 is a central intermediate of the complex anaerobic microbioal degradation of plant biomass and in situ concentrations of the gas are generally low because of its ongoing consumption. In contrast, high H2 concentrations were determined in the gut of the earthworm Lumbricus terrestris. These observations raised the question why the anaerobic microbial community in peatlands is poised to effectively scavenge H2 whereas H2 production by ingested soil anaerobes exceeds H2 consumption in the gut of L. terrestris. To address this question, H2-producing and H2-consuming processes were analyzed in peat soil slurries (soil microcosms) and diluted L. terrestris gut contents (gut content microcosms). In order to identify active H2 metabolizing taxa, gene marker analyses were intended. Hydrogenases are the key enzymes of the H2 metabolism and therefore represent suitable gene marker for H2-metabolizing microorgansims. Thus, PCR-primers for the amplification of hydrogenase gene sequences from environmental samples were designed. Furthermore, a sequence similarity cut-off of 80% for the clustering of environmental hydrogenase gene sequences on the family level was established by comparative 16S rRNA-hydrogenase gene analyses. Cellulose is a major constituent of sedges, which is the dominant vegetation and the major source of organic carbon in the investigated peatland. The polymer was readily degraded mainly to propionate, acetate, and CO2, whereas an accumulation of H2 was not observed in peat soil microcosms. Based on process data and thermodynamic calculations, methano¬genesis and acetogenesis could be excluded as abundant sinks for cellulose-derived H2. Propionate fermenters might have cometabolized H2 and cellulose hydrolysis products. Fibrobacter-related unclassified Bacteria, Prolixibacteraceae, Porphyro¬monanda¬ceae, Clostridiaceae, Ruminococcaceae, Acidobacteriaceae, Holo¬phagaceae, and Spiro-chaetaceae were identified as active assimilators of cellulose-derived carbon by 16S rRNA SIP (stable isotope probing). However, the H2 metabolism and the hydrolytic capabilities especially of the novel taxa remain unresolved. In contrast to the cellulose-supplemented soil microcosms, considerably higher concentrations of H2 were observed in microcosms with washed roots of Carex rostrata (an abundant sedge in the investigated peatland). Hydrogenase gene analyses revealed that several families within the Firmicutes (e.g., Clostridiaceae, Ruminococcaceae, and Lachnospiraceae) dominated H2 production in unsupplemented root microcosms. Formate, which can be excreted by roots, was converted into H2 and CO2 by formate hydrogenlyase-containing taxa (e.g., Betaproteobacteria and Acidobacteria). H2, derived from the fermentation of endogenous sources or supplemented formate, was primarily consumed by acetogens (e.g., Clostridiaceae und Veillonellaceae). These finding reinforced the assumption that the rhizosphere of sedges is a hotspot for H2-evolving fermenters and H2-consuming acetogens. In addition to primary fermenters, secondary syntrophic fermenters (syntrophs) are considered as major H2 producers in peatlands. 16S rRNA transcript analyses identified (i) a novel strain of Pelobacter propionicus as syntrophic ethanol oxidizer, (ii) Syntrophomonas and Telmatospirillum-related taxa as syntrophic butyrate oxidizers, and (iii) Syntrophobacter, Smithella, unclassified Bacteroidetes, and unclassified Fibrobacteres as potential syntrophic propionate oxidizers in soil microcosms. CH4 and CO2 were the only accumulating endproducts of the propionate, butyrate, and ethanol degradation, suggesting that H2, formate, and acetate (the fermentation products of the syntrophs) were effectively scavenged by methanogens. Aceticlastic methanogens (Methanosarcina and Methano¬saeta) outnumbered hydrogenotrophic methanogens (Methanoregula and Methanocella). This might indicate that acetogens were active and competed with hydrogenotrophic methanogens for available H2. In a previous study, in which L. terrestris gut content microcosms were supplemented with glucose, Clostridiaceae and Enterobacteriaceae were identified as important primary fermenters and potential producers of H2 whereas syntrophs, methanogens, and acetogens were not crucial for the H2 turnover. Hydrogenase transcript analyses corroborated these findings. Aeromonadaceae and Peptostreptococcaceae were determined as abundant H2-evolving taxa in addition to Clostridiaceae and Enterobacteriaceae. However, the former two families were not involved in the degradation of glucose and might have fermented endogenous carbon compounds. Proteins, nucleic acids, and carbohydrates derived from disrupted microbial cells represent potential endogenous substrates that are available in the earthworm gut. Aeromonas sp. and Clostridium bifermentans (phylogenetically belongs to the Peptostreptococcaceae) were indeed stimulated within a few hours after the supplementation of yeast cell lysates to gut content microcosms. Subsequently, proteolytic Clostridiaceae, saccharolytic Enterobacteriaceae, and unclassified Lachnospiraceae partially replaced the initially dominating fermenters. The acetogens Clostridium glycolicum and Clostridium magnum were also abundant. They probably utilized formate rather than H2, underscoring the assumption that acetogens are not an important sink for H2 in the gut of L. terrestris. The collective data indicated that at the oligotrophic conditions prevailing in peatlands (i) H2, is produced by primary and secondary fermenters and is effectively scavenged by methanogens, acetognes, and propionate fermenters, (ii) the rhizosphere of sedges is a hotspot for H2 metabolizers, and (iii) novel microbial taxa are involved in the complex anaerobic degradation of plant biomass. In contrast to the oligotrophic peatland soils, huge amounts of readily degradable carbon sources are available for the anaerobic microorganisms in the gut of earthworms. Because of the short gut passage, the anaerobes do not form an interwoven foodweb and consequently, primary and secondary fermentation products are not completely scavenged. Thus, fermentation-derived organic acids can be absorbed by the earthworm whereas H2 diffuses out of the worm and becomes available for H2 oxidizers in the soil.