Kirsten Küsel

Hydrogenotrophic Methanogenesis by Moderately Acid-Tolerant Methanogens of a Methane-Emitting Acidic Peat

ABSTRACT The emission of methane (1.3 mmol of CH4 m−2 day−1), precursors of methanogenesis, and the methanogenic microorganisms of acidic bog peat (pH 4.4) from a moderately reduced forest site were investigated by in situ measurements, microcosm incubations, and cultivation methods, respectively. Bog peat produced CH4 (0.4 to 1.7 μmol g [dry wt] of soil−1 day−1) under anoxic conditions. At in situ pH, supplemental H2-CO2, ethanol, and 1-propanol all increased CH4 production rates while formate, acetate, propionate, and butyrate inhibited the production of CH4; methanol had no effect. H2-dependent acetogenesis occurred in H2-CO2-supplemented bog peat only after extended incubation periods. Nonsupplemented bog peat initially produced small amounts of H2 that were subsequently consumed. The accumulation of H2 was stimulated by ethanol and 1-propanol or by inhibiting methanogenesis with bromoethanesulfonate, and the consumption of ethanol was inhibited by large amounts of H2; these results collectively indicated that ethanol- or 1-propanol-utilizing bacteria were trophically associated with H2-utilizing methanogens. A total of 109 anaerobes and 107 hydrogenotrophic methanogens per g (dry weight) of bog peat were enumerated by cultivation techniques. A stable methanogenic enrichment was obtained with an acidic, H2-CO2-supplemented, fatty acid-enriched defined medium. CH4 production rates by the enrichment were similar at pH 4.5 and 6.5, and acetate inhibited methanogenesis at pH 4.5 but not at pH 6.5. A total of 27 different archaeal 16S rRNA gene sequences indicative of Methanobacteriaceae, Methanomicrobiales, and Methanosarcinaceae were retrieved from the highest CH4-positive serial dilutions of bog peat and methanogenic enrichments. A total of 10 bacterial 16S rRNA gene sequences were also retrieved from the same dilutions and enrichments and were indicative of bacteria that might be responsible for the production of H2 that could be used by hydrogenotrophic methanogens. These results indicated that in this acidic bog peat, (i) H2 is an important substrate for acid-tolerant methanogens, (ii) interspecies hydrogen transfer is involved in the degradation of organic carbon, (iii) the accumulation of protonated volatile fatty acids inhibits methanogenesis, and (iv) methanogenesis might be due to the activities of methanogens that are phylogenetic members of the Methanobacteriaceae, Methanomicrobiales, and Methanosarcinaceae.

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

ABSTRACT 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.

Ecological consequences of the phylogenetic and physiological diversities of acetogens

Acetogens reduce CO2 to acetate via the acetyl-CoA pathway and have been classically thought of as obligately anaerobic bacteria. Nearly 100 acetogenic species from 20 different genera have been isolated to date. These isolates are able to use very diverse electron donors and acceptors, and it is thus very likely that the in situ activities of acetogens are very diverse and not restricted to acetogenesis. Since acetogens constitute a very phylogenetically diverse bacteriological group, it should be anticipated that they can inhabit, and have impact on, diverse habitats. Indeed, they have been isolated from a broad range of habitats, including oxic soils and other habitats not generally regarded as suitable for acetogens. Although the ecological impact of acetogens is determined by the in situ manifestation of their physiological potentials, assessing their in situ activities is difficult due to their physiological and phylogenetic diversities. This mini-review will highlight a few of the physiological and ecological realities of acetogens, and will focus on: (i) metabolic diversities and regulation, (ii) phylogenetic diversity and molecular ecology, and (iii) the capacity of acetogens to cope with oxic conditions under both laboratory and in situ conditions.

Functional Diversity and Electron Donor Dependence of Microbial Populations Capable of U(VI) Reduction in Radionuclide-Contaminated Subsurface Sediments

ABSTRACT In order to elucidate the potential mechanisms of U(VI) reduction for the optimization of bioremediation strategies, the structure-function relationships of microbial communities were investigated in microcosms of subsurface materials cocontaminated with radionuclides and nitrate. A polyphasic approach was used to assess the functional diversity of microbial populations likely to catalyze electron flow under conditions proposed for in situ uranium bioremediation. The addition of ethanol and glucose as supplemental electron donors stimulated microbial nitrate and Fe(III) reduction as the predominant terminal electron-accepting processes (TEAPs). U(VI), Fe(III), and sulfate reduction overlapped in the glucose treatment, whereas U(VI) reduction was concurrent with sulfate reduction but preceded Fe(III) reduction in the ethanol treatments. Phyllosilicate clays were shown to be the major source of Fe(III) for microbial respiration by using variable-temperature Mössbauer spectroscopy. Nitrate- and Fe(III)-reducing bacteria (FeRB) were abundant throughout the shifts in TEAPs observed in biostimulated microcosms and were affiliated with the genera Geobacter, Tolumonas, Clostridium, Arthrobacter, Dechloromonas, and Pseudomonas. Up to two orders of magnitude higher counts of FeRB and enhanced U(VI) removal were observed in ethanol-amended treatments compared to the results in glucose-amended treatments. Quantification of citrate synthase (gltA) levels demonstrated a stimulation of Geobacteraceae activity during metal reduction in carbon-amended microcosms, with the highest expression observed in the glucose treatment. Phylogenetic analysis indicated that the active FeRB share high sequence identity with Geobacteraceae members cultivated from contaminated subsurface environments. Our results show that the functional diversity of populations capable of U(VI) reduction is dependent upon the choice of electron donor.

Tolerance and Metabolic Response of Acetogenic Bacteria toward Oxygen

ABSTRACT The acetogens Sporomusa silvacetica, Moorella thermoacetica, Clostridium magnum, Acetobacterium woodii, and Thermoanaerobacter kivui (i) grew in both semisolid and liquid cultivation media containing O2 and (ii) consumed small amounts of O2. Low concentrations of O2 caused a lag phase in growth but did not alter the ability of these acetogens to synthesize acetate via the acetyl coenzyme A pathway. Cell extracts of S. silvacetica, M. thermoacetica, and C. magnum contained peroxidase and NADH oxidase activities; catalase and superoxide dismutase activities were not detected.

Competition of Fe(III) reduction and methanogenesis in an acidic fen

Peatlands are sources of relevant greenhouse gases such as CH4, but the temporal presence of Fe(III) may inhibit methanogenesis. Because excess of carbon during the vegetation period might allow concomitant electron-accepting processes, Fe(III) reduction and methanogenesis were studied during an annual season in an acidic fen. The upper peat layer displayed the highest Fe(II)- and CH4-forming activities. The rates of Fe(II) formation did not change during the year and methanogenesis started mostly when Fe(II) formation reached a plateau. Most of the Fe(III) pool seemed to be bioavailable, and addition of nitrilotriacetic acid stimulated only light Fe(II) formation, whereas EDTA and anthraquinone-2,6-disulfonate had no effect. In the presence of an inhibitor for methanogenesis (sodium 2-bromoethanesulfonate), Fe(II) formation was inhibited to 45%. Addition of Fe(III) during ongoing methanogenesis led only to a partial inhibition of CH4 formation. The proportion of acetoclastic methanogenesis varied between 42% and 90%, but no trend with time was observed. The number of acetate-, ethanol- or lactate-utilizing Fe(III) reducers approximated 10(5)-10(6) cells g (fresh wt peat)(-1). Fermentative glucose-utilizing Fe(III)-reducers were most abundant. Our results suggest that (1) methanogens used Fe(III) as an electron acceptor and (2) fermenting bacteria, which do not compete with methanogens for common electron donors, dominated the reduction of Fe(III) in this fen.

Physiological ecology of Clostridium glycolicum RD-1, an aerotolerant acetogen isolated from sea grass roots

ABSTRACT An anaerobic, H2-utilizing bacterium, strain RD-1, was isolated from the highest growth-positive dilution series of a root homogenate prepared from the sea grass Halodule wrightii. Cells of RD-1 were gram-positive, spore-forming, motile rods that were linked by connecting filaments. Acetate was produced in stoichiometries indicative of an acetyl coenzyme A (acetyl-CoA) pathway-dependent metabolism when RD-1 utilized H2-CO2, formate, lactate, or pyruvate. Growth on sugars or ethylene glycol yielded acetate and ethanol as end products. RD-1 grew at the expense of glucose in the presence of low initial concentrations (up to 6% [vol/vol]) of O2 in the headspace of static, horizontally incubated culture tubes; the concentration of O2 decreased during growth in such cultures. Peroxidase, NADH oxidase, and superoxide dismutase activities were detected in the cytoplasmic fraction of cells grown in the presence of O2. In comparison to cultures incubated under strictly anoxic conditions, acetate production decreased, higher amounts of ethanol were produced, and lactate and H2 became significant end products when RD-1 was grown on glucose in the presence of O2. Similarly, when RD-1 was grown on fructose in the presence of elevated salt concentrations, lower amounts of acetate and higher amounts of ethanol and H2 were produced. When the concentration of O2 in the headspace exceeded 1% (vol/vol), supplemental H2 was not utilized. The 16S rRNA gene of RD-1 had a 99.7% sequence similarity to that ofClostridium glycolicum DSM 1288T, an organism characterized as a fermentative anaerobe. Comparative experiments with C. glycolicum DSM 1288T demonstrated that it had negligible H2- and formate-utilizing capacities. However, carbon monoxide dehydrogenase was detected in both RD-1 and C.glycolicum DSM 1288T. A 91.4% DNA-DNA hybridization between the genomic DNA of RD-1 and that ofC. glycolicum DSM 1288Tconfirmed that RD-1 was a strain of C.glycolicum. These results indicate that (i) RD-1 metabolizes certain substrates via the acetyl-CoA pathway, (ii) RD-1 can tolerate and consume limited amounts of O2, (iii) oxic conditions favor the production of ethanol, lactate, and H2by RD-1, and (iv) the ability of RD-1 to cope with limited amounts of O2 might contribute to its survival in a habitat subject to daily gradients of photosynthesis-derived O2.

Clostridium scatologenes strain SL1 isolated as an acetogenic bacterium from acidic sediments

A strictly anaerobic, H2-utilizing bacterium, strain SL1, was isolated from the sediment of an acidic coal mine pond. Cells of strain SL1 were sporulating, motile, long rods with a multilayer cell wall. Growth was observed at 5-35 degrees C and pH 3.9-7.0. Acetate was the sole end product of H2 utilization and was produced in stoichiometries indicative of an acetyl-CoA-pathway-dependent metabolism. Growth and substrate utilization also occurred with CO/CO2, vanillate, syringate, ferulate, ethanol, propanol, 1-butanol, glycerine, cellobiose, glucose, fructose, mannose, xylose, formate, lactate, pyruvate and gluconate. With most substrates, acetate was the main or sole product formed. Growth in the presence of H2/CO2 or CO/CO2 was difficult to maintain in laboratory cultures. Methoxyl, carboxyl and acrylate groups of various aromatic compounds were O-demethylated, decarboxylated and reduced, respectively. Small amounts of butyrate were produced during the fermentation of sugars. The acrylate group of ferulate was reduced. Nitrate, sulfate, thiosulfate, dimethylsulfoxide and Fe(III) were not utilized as electron acceptors. Analysis of the 16S rRNA gene sequence of strain SL1 demonstrated that it is closely related to Clostridium scatologenes (99.6% sequence similarity), an organism characterized as a fermentative anaerobe but not previously shown to be capable of acetogenic growth. Comparative experiments with C. scatologenes DSM 757T demonstrated that it utilized H2/CO2 (negligible growth), CO/CO2 (negligible growth), formate, ethanol and aromatic compounds according to stoichiometries indicative of the acetyl-CoA pathway. CO dehydrogenase, formate dehydrogenase and hydrogenase activities were present in both strain SL1 and C. scatologenes DSM 757T. These results indicate that (i) sediments of acidic coal mine ponds harbour acetogens and (ii) C. scatologenes is an acetogen that tends to lose its capacity to grow acetogenically under H2/CO2 or CO/CO2 after prolonged laboratory cultivation.

Ecophysiology of Fe-Cycling Bacteria in Acidic Sediments

ABSTRACT Using a combination of cultivation-dependent and -independent methods, this study aimed to elucidate the diversity of microorganisms involved in iron cycling and to resolve their in situ functional links in sediments of an acidic lignite mine lake. Using six different media with pH values ranging from 2.5 to 4.3, 117 isolates were obtained that grouped into 38 different strains, including 27 putative new species with respect to the closest characterized strains. Among the isolated strains, 22 strains were able to oxidize Fe(II), 34 were able to reduce Fe(III) in schwertmannite, the dominant iron oxide in this lake, and 21 could do both. All isolates falling into the Gammaproteobacteria (an unknown Dyella-like genus and Acidithiobacillus-related strains) were obtained from the top acidic sediment zones (pH 2.8). Firmicutes strains (related to Bacillus and Alicyclobacillus) were only isolated from deep, moderately acidic sediment zones (pH 4 to 5). Of the Alphaproteobacteria, Acidocella-related strains were only isolated from acidic zones, whereas Acidiphilium-related strains were isolated from all sediment depths. Bacterial clone libraries generally supported and complemented these patterns. Geobacter-related clone sequences were only obtained from deep sediment zones, and Geobacter-specific quantitative PCR yielded 8 × 105 gene copy numbers. Isolates related to the Acidobacterium, Acidocella, and Alicyclobacillus genera and to the unknown Dyella-like genus showed a broad pH tolerance, ranging from 2.5 to 5.0, and preferred schwertmannite to goethite for Fe(III) reduction. This study highlighted the variety of acidophilic microorganisms that are responsible for iron cycling in acidic environments, extending the results of recent laboratory-based studies that showed this trait to be widespread among acidophiles.

Effect of pH on the anaerobic microbial cycling of sulfur in mining-impacted freshwater lake sediments

Lakes caused by coal strip-mining processes are characterized by low pH, low nutrient status, and high concentrations of Fe(II) and sulfate due to the oxidation of pyrite. Most microbiological studies of sulfidic mine tailings concentrate on processes in the oxic zone, and on the ability of acidophilic bacteria to promote the production of toxic leachates. Few studies have studied microbial processes in anoxic sediment zones, where the reduction of Fe(III) often is the dominant electron-accepting process in acidic sediments, and the reduction of sulfate occurs in sediments of elevated pH. In this study, microcosm experiments were performed with sediments of a coal mining-impacted lake to study the microbial turnover of sulfur under anoxic conditions. Microcosms with sediment of the zone of maximum sulfate-reducing activity indicated that sulfidic minerals subsequently formed due to the reduction of sulfate were not stable under anoxic conditions. Supplemental Na2S stimulated the formation of Fe(II) and sulfate, whereas supplemental S0 had no effect under pH 5 conditions. Low numbers of S0-utilizing Fe(III)-reducing bacteria were enumerated in this sediment zone. In contrast, sediment microcosms of the upper acidic sediment zone demonstrated that supplemental elemental S0 stimulated the formation of Fe(II) and sulfate, whereas supplemental Na2S had no effect. Most probable number estimates demonstrated that S0-utilizing Fe(III)-reducing bacteria cultivated at pH 3 approximated to 1% of the total direct counts of bacteria in the upper acidic sediment zone. Sulfate reducers cultured at pH 5.2 were more abundant than sulfate reducers cultured at pH 6.4 in both sediment zones. A sulfate-reducing bacterium, Lau III, was isolated at the in situ pH of 5.2 from the highest growth positive dilution series from the zone of maximum sulfate-reducing activity. Analysis of the 16S rRNA gene sequence (1498 base pairs) of Lau III demonstrated that it was a member of the Clostridium–Bacillus subphylum of gram-positive bacteria related to Desulfosporosinus orientis Y11571 (96.4% 16S rRNA gene sequence similarity). Lau III was a spore-forming, lactate-utilizing sulfate reducer capable of growing at a pH range of 4.9–6.1 and a pH optimum of 5.5. These collective results indicate that, (i) acid-tolerant sulfate reducers are involved in the reduction of sulfate; (ii) sulfide or sulfidic minerals are reoxidized under anoxic conditions; and (iii) the anaerobic turnover of sulfur is affected by the pH gradient in this impacted heterogeneous lake sediment.