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Root exudates shape microbial communities at the plant-soil interface. Here we compared bacterial communities that utilize plant-derived carbon in the rhizosphere of wheat in different soil depths, including topsoil, as well as two subsoil layers up to 1 m depth. The experiment was performed in a greenhouse using soil monoliths with intact soil structure taken from an agricultural field. To identify bacteria utilizing plant-derived carbon, 13C-CO2 labelling of plants was performed for two weeks at the EC50 stage, followed by isopycnic density gradient centrifugation of extracted DNA from the rhizosphere combined with 16S rRNA gene-based amplicon sequencing. Our findings suggest substantially different bacterial key players and interaction mechanisms between plants and bacteria utilizing plant-derived carbon in the rhizosphere of subsoils and topsoil. Among the three soil depths, clear differences were found in 13C enrichment pattern across abundant operational taxonomic units (OTUs). Whereas, OTUs linked to Proteobacteria were enriched in 13C mainly in the topsoil, in both subsoil layers OTUs related to Cohnella, Paenibacillus, Flavobacterium showed a clear 13C signal, indicating an important, so far overseen role of Firmicutes and Bacteriodetes in the subsoil rhizosphere. [ABSTRACT FROM AUTHOR]

Stable isotope probing (SIP) techniques have become stateof- the-art in microbial ecology over the last 10 years, allowing for the targeted detection and identification of organisms, metabolic pathways and elemental fluxes active in specific processes within complex microbial communities. For studying anaerobic hydrocarbon-degrading microbial communities, four stable isotope techniques have been used so far: DNA/RNA-SIP, PLFA (phospholipid-derived fatty acids)-SIP, protein-SIP, and single-cell-SIP by nanoSIMS (nanoscale secondary ion mass spectrometry) or confocal Raman microscopy. DNA/RNA-SIP techniques are most frequently applied due to their most meaningful phylogenetic resolution. Especially using 13 C-labeled benzene and toluene as model substrates, many new hydrocarbon degraders have been identified by SIP under various electron acceptor conditions. This has extended the current perspective of the true diversity of anaerobic hydrocarbon degraders relevant in the environment. Syntrophic hydrocarbon degradation was found to be a common mechanism for various electron acceptors. Fundamental concepts and recent advances in SIP are reflected here. A discussion is presented concerning how these techniques generate direct insights into intrinsic hydrocarbon degrader populations in environmental systems and how useful they are for more integrated approaches in the monitoring of contaminated sites and for bioremediation. [ABSTRACT FROM AUTHOR]

Hydrocarbon contaminants in groundwater can be degraded by microbes under different redox settings, forming hot spots of degradation especially at the fringes of contaminant plumes. At a tar-oil-contaminated aquifer in Germany, it was previously shown that the distribution of anaerobic toluene degraders as traced via catabolic and ribosomal marker genes is highly correlated to zones of increased anaerobic degradation at the lower fringe of the plume. Here, we trace the respective distribution of aerobic toluene degraders over a fine-scale depth transect of sediments taken at the upper fringe of the plume and below, based on the analysis of 16 S rRNA genes as well as catabolic markers in intervals of 3-10 cm. Well-defined small-scale distribution maxima of typical aerobic degrader lineages within the Pseudomonadaceae, Comamonadaceae and Burkholderiaceae are revealed over the redox gradient. An unexpected maximal abundance of 9.2 × 106 toluene monooxygenase ( tmoA) genes per g of sediment was detected in the strongly reduced plume core, and gene counts did not increase towards the more oxidized upper plume fringe. This may point towards unusual ecological controls of these yet unidentified aerobic degraders, and indicates that competitive niche partitioning between aerobic and anaerobic hydrocarbon degraders in the field is not yet fully understood. These findings demonstrate the potential of catabolic marker gene assays in elaborating the ecology of contaminant plumes, which is a prerequisite for developing integrated monitoring strategies for natural attenuation. [ABSTRACT FROM AUTHOR]

Abstract: Hyporheic substrates play a key role in aquatic ecosystems, and increasing loads of fine sediment are considered one of the major threats to stream ecosystems. Knowledge concerning the interaction of stream substratum properties with habitat quality and microbial community structure is essential for a comprehensive understanding of the functionality of the hyporheic zone. To date, there is a lack of optimal field sampling methods for hyporheic microbial communities in streams. We systematically tested the effects of defined substratum textures on the physicochemical properties of interstitial water and on bacterial communities utilising T-RFLP fingerprinting. We also tested the representativeness of different methodological approaches of investigating bacterial diversity comparing sampling of substratum, interstitial water, and exposed coupons made of granite, carbonate and glass. The temporal development of physicochemical habitat characteristics in the interstitial zone, especially of fish-toxic nitrogen compounds and oxygen supply, significantly depended on substratum texture and was strongly correlated with bacterial community composition. Multivariate analyses of bacterial community data indicated strong differences in community composition between direct (substratum samples) and indirect (interstitial water samples, coupons) sampling strategies. Substratum samples yielded highest richness of operational taxonomic units (OTUs) and the most pronounced temporal dynamics of bacterial community composition. Consequently, this technique appears most representative for assessing bacterial community structure and diversity in hyporheic habitats. The observed couplings between substratum texture, physicochemical habitat conditions and bacterial community structure expand current knowledge of previously described negative effects of fine sediments on taxa from higher levels of biological organization. [Copyright &y& Elsevier]

The understanding of microbial interactions and trophic networks is a prerequisite for the elucidation of the turnover and transformation of organic materials in soils. To elucidate the incorporation of biomass carbon into a soil microbial food web, we added 13C-labeled Escherichia coli biomass to an agricultural soil and identified those indigenous microbes that were specifically active in its mineralization and carbon sequestration. rRNA stable isotope probing (SIP) revealed that uncultivated relatives of distinct groups of gliding bacterial micropredators (Lysobacter spp., Myxococcales, and the Bacteroidetes) lead carbon sequestration and mineralization from the added biomass. In addition, fungal populations within the Microascaceae were shown to respond to the added biomass after only 1 h of incubation and were thus surprisingly reactive to degradable labile carbon. This RNA-SIP study identifies indigenous microbes specifically active in the transformation of a nondefined complex carbon source, bacterial biomass, directly in a soil ecosystem. [ABSTRACT FROM AUTHOR]

Detailed studies on the relation of structure and function of microbial communities in a sediment depth profile scarcely exist. We determined as functional aspect the vertical distribution of the acetotrophic and hydrogenotrophic CH4 production activity by measuring production rates and stable 13C/12C-isotopic signatures of CH4 in the profundal sediment of Lake Dagow. The structural aspect was determined by the composition of the methanogenic community by quantifying the abundance of different archaeal groups using ‘real-time’ polymerase chain reaction and analysis of terminal restriction fragment length polymorphism (T-RFLP). Methane production rates in the surface sediment (0–3 cm depth) were higher in August than in May, but strongly decreased with depth (down to 20 cm). The δ13C of the produced CH4 and CO2 indicated an increase in isotopic fractionation with sediment depth. The relative contribution of hydrogenotrophic to total methanogenesis, which was calculated from the isotopic signatures, increased with depth from about 22% to 38%. Total numbers of microorganisms were higher in August than in May, but strongly decreased with depth. The increase of microorganisms from May to August mainly resulted from Bacteria. The Archaea, on the other hand, exhibited a rather constant abundance, but also decreased with depth from about 1 × 108 copies of the archaeal 16S rRNA gene per gram of dry sediment at the surface to 4 × 107 copies per gram at 15–20 cm depth. T-RFLP analysis combined with phylogenetic analysis of cloned sequences of the archaeal 16S rRNA genes showed that the methanogenic community consisted mainly of Methanomicrobiales and Methanosaetaceae. The relative abundance of Methanosaetaceae decreased with depth, whereas that of Methanomicrobiales slightly increased. Hence, the vertical distribution of the functional characteristics (CH4 production from acetate versus H2/CO2) was reflected in the structure of the community consisting of acetotrophic ( Methanosaetaceae) versus hydrogenotrophic ( Methanomicrobiales) phenotypes. [ABSTRACT FROM AUTHOR]

Methane is formed on rice roots mainly by CO2 reduction. The present study aimed to identify the active methanogenic populations responsible for this process. Soil-free rice roots were incubated anaerobically under an atmosphere of H2/13CO2 or N2/13CO2 with phosphate or carbonate (marble) as buffer medium. Nucleic acids were extracted and fractionated by caesium trifluoroacetate equilibrium density gradient centrifugation after 16-day incubation. Community analyses were performed for gradient fractions using terminal restriction fragment polymorphism analysis (T-RFLP) and sequencing of the 16S rRNA genes. In addition, rRNA was extracted and analysed at different time points to trace the community change during the 16-day incubation. TheMethanosarcinaceaeand the yet-uncultured archaeal lineage Rice Cluster-I (RC-I) were predominant in the root incubations when carbonate buffer and N2 headspace were used. The analysis of[13C]DNA showed that the relative 16S rRNA gene abundance of RC-I increased whereas that of theMethanosarcinaceaedecreased with increasing DNA buoyant density, indicating that members of RC-I were more active than theMethanosarcinaceae. However, an unexpected finding was that RC-I was suppressed in the presence of high H2 concentrations (80%, v/v), which during the early incubation period caused a lower CH4 production compared with that with N2 in the headspace. Eventually, however, CH4 production increased, probably because of the activity ofMethanosarcinaceae,which became prevalent. Phosphate buffer appeared to inhibit the activity of theMethanosarcinaceae, resulting in lower CH4 production as compared with carbonate buffer. Under these conditions,Methanobacteriaceaewere the prevalent methanogens. Our study suggests that the active methanogenic populations on rice roots change in correspondence to the presence of H2 (80%, v/v) and the type of buffer used in the system. [ABSTRACT FROM AUTHOR]

Stable isotope probing (SIP) is a novel technique to characterize structure and in situ function of active microbial populations, which is based on the incorporation of 13C-labelled substrates into nucleic acids. Here, we have traced methylotrophic members of a rice field soil microbial community, which became active upon continuous addition of 13C-methanol (<22 mM) as studied in microcosms. By combining rRNA- and DNA-based SIP, as well as domain-specific real-time PCR detection of templates in fractions of centrifugation gradients, we were able to detect 13C-labelled bacterial rRNA after 6 days of incubation. Fingerprinting and comparative sequence analysis of ‘heavy’ bacterial rRNA showed that mostly members of the Methylobacteriaceae and a novel clade within the Methylophilaceae formed part of the indigenous methylotrophic community. Over time, however, the Methylophilaceae were enriched. Unexpectedly, nucleic acids of eukaryotic origin were detected, mostly in intermediately 13C-labelled gradient fractions. These eukaryotes were identified as fungi mostly related to Fusarium and Aspergillus spp., and also Cercozoa, known as predatory soil flagellates. The detection of fungi and protozoa in 13C-enriched nucleic acid fractions suggests a possible involvement in either direct assimilation of label by the fungi, or a food web, i.e. that primary 13C-methanol consuming methylotrophs were decomposed by fungi and grazed by protozoa. [ABSTRACT FROM AUTHOR]