Enhanced sensitivity of DNA- and rRNA-based stable isotope probing by fractionation and quantitative analysis of isopycnic centrifugation gradients

Stable isotope probing (SIP) of nucleic acids allows the detection and identification of active members of natural microbial populations that are involved in the assimilation of an isotopically labelled compound into nucleic acids. SIP is based on the separation of isotopically labelled DNA or rRNA by isopycnic density gradient centrifugation. We have developed a highly sensitive protocol for the detection of 'light' and 'heavy' nucleic acids in fractions of centrifugation gradients. It involves the fluorometric quantification of total DNA or rRNA, and the quantification of either 16S rRNA genes or 16S rRNA in gradient fractions by real-time PCR with domain-specific primers. Using this approach, we found that fully 13C-labelled DNA or rRNA of Methylobacterium extorquens was quantitatively resolved from unlabelled DNA or rRNA of Methanosarcina barkeri by cesium chloride or cesium trifluoroacetate density gradient centrifugation respectively. However, a constant low background of unspecific nucleic acids was detected in all DNA or rRNA gradient fractions, which is important for the interpretation of environmental SIP results. Consequently, quantitative analysis of gradient fractions provides a higher precision and finer resolution for retrieval of isotopically enriched nucleic acids than possible using ethidium bromide or gradient fractionation combined with fingerprinting analyses. This is a prerequisite for the fine-scale tracing of microbial populations metabolizing 13C-labelled compounds in natural ecosystems.     

Isolation and characterization of new strains of methanogens from cold terrestrial habitats

Five strains of methanogenic archaea (MT, MS, MM, MSP, ZB) were isolated from permanently and periodically cold terrestrial habitats. Physiological and morphological studies, as well as phylogenetic analyses of the new isolates were performed. Based on sequences of the 16S rRNA and methyl-coenzyme M reductase a-subunit (mcrA) genes all new isolates are closely related to known mesophilic and psychrotolerant methanogens. Both, phylogenetic analyses and phenotypic properties allow to classify strains MT, MS, and MM as members of the genus Methanosarcina. Strain MT is a new ecotype of Methanosarcina mazei, whereas strains MM and MS are very similar to each other and can be assigned to the recently described psychrotolerant species Methanosarcina lacustris. The hydrogenotrophic strain MSP is a new ecotype of the genus Methanocorpusculum. The obligately methylotrophic strain ZB is closely related to Methanomethylovorans hollandica and can be classified as new ecotype of this species. All new isolates, including the strains from permanently cold environments, are not true psychrophiles according to their growth temperature characteristics. In spite of the ability of all isolates to grow at temperatures as low as 1-5 degrees C, all of them have their growth optima in the range of moderate temperatures (25-35 degrees C). Thus, they can be regarded as psychrotolerant organisms. Psychrotolerant methanogens are thought to play an important role in methane production in both, habitats under seasonal temperature variations or from permanently cold areas.     

Effects of Amendment with Ferrihydrite and Gypsum on the Structure and Activity of Methanogenic Populations in Rice Field Soil

Methane emission from paddy fields may be reduced by the addition of electron acceptors to stimulate microbial populations competitive to methanogens. We have studied the effects of ferrihydrite and gypsum (CaSO₄·2H₂O) amendment on methanogenesis and population dynamics of methanogens after flooding of Italian rice field soil slurries. Changes in methanogen community structure were followed by archaeal small subunit (SSU) ribosomal DNA (rDNA)- and rRNA-based terminal restriction fragment length polymorphism analysis and by quantitative SSU rRNA hybridization probing. Under ferrihydrite amendment, acetate was consumed efficiently (<60 μM) and a rapid but incomplete inhibition of methanogenesis occurred after 3 days. In contrast to unamended controls, the dynamics of Methanosarcina populations were largely suppressed as indicated by rDNA and rRNA analysis. However, the low acetate availability was still sufficient for activation of Methanosaeta spp., as indicated by a strong increase of SSU rRNA but not of relative rDNA frequencies. Unexpectedly, rRNA amounts of the novel rice cluster I (RC-I) methanogens increased significantly, while methanogenesis was low, which may be indicative of transient energy conservation coupled to Fe(III) reduction by these methanogens. Under gypsum addition, hydrogen was rapidly consumed to low levels (~0.4 Pa), indicating the presence of a competitive population of hydrogenotrophic sulfate-reducing bacteria (SRB). This was paralleled by a suppressed activity of the hydrogenotrophic RC-I methanogens as indicated by the lowest SSU rRNA quantities detected in all experiments. Full inhibition of methanogenesis only became apparent when acetate was depleted to nonpermissive thresholds (<5 μM) after 10 days. Apparently, a competitive, acetotrophic population of SRB was not present initially, and hence, acetotrophic methanosarcinal populations were less suppressed than under ferrihydrite amendment. In conclusion, although methane production was inhibited effectively under both mitigation regimens, different methanogenic populations were either suppressed or stimulated, which demonstrates that functionally similar disturbances of an ecosystem may result in distinct responses of the populations involved.     

Genomic organization and mapping of the human and mouse neuronal β2-nicotinic acetylcholine receptor genes

As a first step in determining whether there are polymorphisms in the nicotinic acetylcholine receptor (nAChR) genes that are associated with nicotine addiction, we isolated genomic clones of the β2-nAChR genes from human and mouse BAC libraries. Although cDNA sequences were available for the human gene, only the promoter sequence had been reported for the mouse gene. We determined the genomic structures by sequencing 12 kb of the human gene and over 7 kb of the mouse gene. While the sizes of exons in the mouse and human genes are the same, the introns differ in size. Both promoters have a high GC content (60–80%) proximal to the AUG and share a neural-restrictive silencer element (NRSE), but overall sequence identity is only 72%. Using a 6-Mb YAC contig of Chr 1, we mapped the human β2-nAChR gene, CHRNB2, to 1q21.3 with the order of markers cen, FLG, IVL, LOR, CHRNB2, tel. The mouse gene, Acrb2, had previously been mapped to Chr 3 in a region orthologous to human Chr 1. We refined mapping of the mouse gene and other markers on a radiation hybrid panel of Chr 3 and found the order cen, Acrb2, Lor, Iv1, Flg, tel. Our results indicate that this cluster of markers on human Chr 1 is inverted with respect to its orientation on the chromosome compared with markers in the orthologous region of mouse Chr 3. Received: 26 January 1999 / Accepted: 10 May 1999     

Identification of Bacterial Micropredators Distinctively Active in a Soil Microbial Food Web

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.     

Functional characterization of an anaerobic benzene‐degrading enrichment culture by DNA stable isotope probing

The flow of carbon under sulfate‐reducing conditions within a benzene‐mineralizing enrichment culture was analysed using fully labelled [¹³C₆]‐benzene. Over 180 days of incubation, 95% of added ¹³C‐benzene was released as ¹³C‐carbon dioxide. DNA extracted from cultures that had degraded different amounts of unlabelled or ¹³C‐labelled benzene was centrifuged in CsCl density gradients to identify ¹³C‐benzene‐assimilating organisms by density‐resolved terminal restriction fragment length polymorphism analysis and cloning of 16S rRNA gene fragments. Two phylotypes showed significantly increased relative abundance of their terminal restriction fragments in ‘heavy’ fractions of ¹³C‐benzene‐incubated microcosms compared with a ¹²C‐benzene‐incubated control: a member of the Cryptanaerobacter/Pelotomaculum group within the Peptococcaceae, and a phylotype belonging to the Epsilonproteobacteria. The Cryptanaerobacter/Pelotomaculum phylotype was the most frequent sequence type. A small amount of ¹³C‐methane was aceticlastically produced, as concluded from the linear relationship between methane production and benzene degradation and the detection of Methanosaetaceae as the only methanogens present. Other phylotypes detected but not ¹³C‐labelled belong to several genera of sulfate‐reducing bacteria, that may act as hydrogen scavengers for benzene oxidation. Our results strongly support the hypothesis that benzene is mineralized by a consortium consisting of syntrophs, hydrogenotrophic sulfate reducers and to a minor extent of aceticlastic methanogens.     

Combined Genomic and Proteomic Approaches Identify Gene Clusters Involved in Anaerobic 2-Methylnaphthalene Degradation in the Sulfate-Reducing Enrichment Culture N47

The highly enriched deltaproteobacterial culture N47 anaerobically oxidizes the polycyclic aromatic hydrocarbons naphthalene and 2-methylnaphthalene, with sulfate as the electron acceptor. Combined genome sequencing and liquid chromatography-tandem mass spectrometry-based shotgun proteome analyses were performed to identify genes and proteins involved in anaerobic aromatic catabolism. Proteome analysis of 2-methylnaphthalene-grown N47 cells resulted in the identification of putative enzymes catalyzing the anaerobic conversion of 2-methylnaphthalene to 2-naphthoyl coenzyme A (2-naphthoyl-CoA), as well as the reductive ring cleavage of 2-naphthoyl-CoA, leading to the formation of acetyl-CoA and CO₂. The glycyl radical-catalyzed fumarate addition to the methyl group of 2-methylnaphthalene is catalyzed by naphthyl-2-methyl-succinate synthase (Nms), composed of α-, β-, and γ-subunits that are encoded by the genes nmsABC. Located upstream of nmsABC is nmsD, encoding the Nms-activating enzyme, which harbors the characteristic [Fe₄S₄] cluster sequence motifs of S-adenosylmethionine radical enzymes. The bns gene cluster, coding for enzymes involved in beta-oxidation reactions converting naphthyl-2-methyl-succinate to 2-naphthoyl-CoA, was found four intervening open reading frames further downstream. This cluster consists of eight genes (bnsABCDEFGH) corresponding to 8.1 kb, which are closely related to genes for enzymes involved in anaerobic toluene degradation within the denitrifiers “Aromatoleum aromaticum” EbN1, Azoarcus sp. strain T, and Thauera aromatica. Another contiguous DNA sequence harbors the gene for 2-naphthoyl-CoA reductase (ncr) and 16 additional genes that were found to be expressed in 2-methylnaphthalene-grown cells. These genes code for enzymes that were supposed to catalyze the dearomatization and ring cleavage reactions converting 2-naphthoyl-CoA to acetyl-CoA and CO₂. Comparative sequence analysis of the four encoding subunits (ncrABCD) showed the gene product to have the closest similarity to the Azoarcus type of benzoyl-CoA reductase. The present work provides the first insight into the genetic basis of anaerobic 2-methylnaphthalene metabolism and delivers implications for understanding contaminant degradation.Polycyclic aromatic hydrocarbons (PAHs) are constantly released into the environment by anthropogenic activities such as industrial use or by accidental contamination. Due to the low chemical reactivity caused by the resonance energy of the aromatic ring structure and the low bioavailability of PAHs, they are persistent in the environment (15). The understanding of microbial metabolic capabilities in terms of anaerobic PAH degradation is in its infancy. However, natural amelioration of contaminated sites relies on the degradation capacities of microorganisms, and therefore, it is an essential prerequisite to broaden knowledge about the microorganisms involved and their potentials concerning PAH breakdown.Numerous microorganisms that can degrade PAHs under aerobic conditions have already been identified, but only a small number of anaerobic cultures that degrade PAHs like naphthalene, 2-methylnaphthalene, and phenanthrene have been isolated so far (17, 20, 24, 31, 46-48, 50, 52, 66). It has been shown that these anaerobic degraders activate aromatic hydrocarbons by very unusual biochemical reactions which differ completely from those of aerobic degradation. The peripheral pathway of 2-methylnaphthalene degradation occurs in analogy to anaerobic toluene degradation by the addition of fumarate to the methyl group, catalyzed by the glycyl radical enzyme naphthyl-2-methyl-succinate synthase (Nms) (Fig. ​(Fig.1)1) (3). In subsequent reactions, naphthyl-2-methyl-succinate is activated to yield the coenzyme A (CoA) ester and oxidized to form naphthyl-2-methylene-succinyl-CoA. The following beta-oxidation of the side chain results in the formation of 2-naphthoyl-CoA and succinate (3, 53). The first three enzyme reactions of this pathway have been measured in vitro (3, 53). Recently, Musat et al. (48) identified the gene coding for the α-subunit of a putative naphthyl-2-methyl-succinate synthase (nmsA) in 2-methylnaphthalene-grown bacterial cultures. The molecular composition of the nmsA gene is analogous to that of the benzylsuccinate synthase α-subunit gene (bssA). The Bss enzyme is a well-investigated close homolog of Nms, catalyzing fumarate addition in the initial reaction of anaerobic toluene degradation (34, 40). Based on findings from comparative sequence studies, glycine radical-catalyzed fumarate addition has been shown to be a widely distributed initial reaction mechanism for anaerobic hydrocarbon degradation involving toluene and 2-methylnaphthalene, n-alkanes (12, 13, 25, 51), m-xylene (33), m- and p-cresols (9), and ethylbenzene (32).Open in a separate windowFIG. 1.Proposed pathway for anaerobic 2-methylnaphthalene degradation and reductive dearomatization of 2-naphthoyl-CoA (3, 4, 53). Genes found in the N47 genome encode the following enzymes (shown in gray boxes): NmsABC, naphthyl-2-methyl-succinate synthase; BnsEF, naphthyl-2-methyl-succinate CoA transferase; BnsG, naphthyl-2-methyl-succinyl-CoA dehydrogenase; BnsH, naphthyl-2-methylene-succinyl-CoA hydratase; BnsCD, naphthyl-2-hydroxymethyl-succinyl-CoA dehydrogenase; BnsAB, naphthyl-2-oxomethyl-succinyl-CoA thiolase; and NcrABCD, 2-naphthoyl-CoA reductase. The position of the double bond is not known for octahydro-2-naphthoyl-CoA. COSCoA, thioester of CoA and the respective carboxyl group.In a process analogous to the anaerobic benzoyl-CoA degradation pathway (7), 2-naphthoyl-CoA is subjected to aromatic ring reduction by a putative naphthoyl-CoA reductase, probably generating 5,6,7,8-tetrahydro-naphthoyl-CoA and further octahydro-2-naphthoic acid (4, 46). In the subsequent reactions, the ring system should be thiolytically cleaved and subjected to beta-oxidation, leading to the formation of acetyl-CoA and CO₂.In contrast to the first enzymatic reaction in the degradation of methylated aromatics, the first enzymatic reaction in anaerobic degradation of unsubstituted aromatic compounds such as naphthalene is still unresolved. In order to determine the initial activation reaction of anaerobic naphthalene degradation, studies based on the analysis of metabolites have been performed. Zhang and Young (66) observed the incorporation of ¹³C-labeled bicarbonate from the buffer into the carboxyl group of 2-naphthoic acid, hypothesizing that carboxylation is the initial activation reaction of anaerobic naphthalene degradation in the culture studied. Recently, Safinowski and Meckenstock (54) identified the deuterated metabolites naphthyl-2-methyl-succinate and naphthyl-2-methylene-succinate, which are exclusive intermediates of anaerobic 2-methylnaphthalene degradation, in the enrichment culture N47 when the culture was cultivated on fully deuterated naphthalene. Moreover, specific enzyme activities of the anaerobic 2-methylnaphtahlene degradation pathway have been detected in naphthalene-grown cells (54). Therefore, methylation of naphthalene to yield 2-methylnaphthalene as the initial activation reaction and subsequent degradation via the 2-methylnaphthalene pathway were proposed for this bacterial culture. The elucidation of 2-methylnaphthalene degradation may therefore reveal an important part of the naphthalene degradation pathway. However, Musat et al. (48) questioned methylation as the first reaction in naphthalene degradation for their marine naphthalene-degrading deltaproteobacterial NaphS strains.Whereas molecular components involved in anaerobic degradation of monoaromatic hydrocarbons are well known, knowledge about genes and enzymes involved in anaerobic PAH degradation is still missing (14). Here, we provide the first results of a whole-proteome- and whole-genome-based investigation of the sulfate-reducing enrichment culture N47 degrading naphthalene and 2-methylnaphtalene. We have identified some gene clusters encoding enzymes involved in 2-methylnaphthalene degradation, 2-naphthoyl-CoA dearomatization, and subsequent ring cleavage reactions in 2-methylnaphthalene-grown N47 cells.     

Depth-Resolved Quantification of Anaerobic Toluene Degraders and Aquifer Microbial Community Patterns in Distinct Redox Zones of a Tar Oil Contaminant Plume

Microbial degradation is the only sustainable component of natural attenuation in contaminated groundwater environments, yet its controls, especially in anaerobic aquifers, are still poorly understood. Hence, putative spatial correlations between specific populations of key microbial players and the occurrence of respective degradation processes remain to be unraveled. We therefore characterized microbial community distribution across a high-resolution depth profile of a tar oil-impacted aquifer where benzene, toluene, ethylbenzene, and xylene (BTEX) degradation depends mainly on sulfate reduction. We conducted depth-resolved terminal restriction fragment length polymorphism fingerprinting and quantitative PCR of bacterial 16S rRNA and benzylsuccinate synthase genes (bssA) to quantify the distribution of total microbiota and specific anaerobic toluene degraders. We show that a highly specialized degrader community of microbes related to known deltaproteobacterial iron and sulfate reducers (Geobacter and Desulfocapsa spp.), as well as clostridial fermenters (Sedimentibacter spp.), resides within the biogeochemical gradient zone underneath the highly contaminated plume core. This zone, where BTEX compounds and sulfate—an important electron acceptor—meet, also harbors a surprisingly high abundance of the yet-unidentified anaerobic toluene degraders carrying the previously detected F1-cluster bssA genes (C. Winderl, S. Schaefer, and T. Lueders, Environ. Microbiol. 9:1035-1046, 2007). Our data suggest that this biogeochemical gradient zone is a hot spot of anaerobic toluene degradation. These findings show that the distribution of specific aquifer microbiota and degradation processes in contaminated aquifers are tightly coupled, which may be of value for the assessment and prediction of natural attenuation based on intrinsic aquifer microbiota.     

Stable-Isotope Probing of Microorganisms Thriving at Thermodynamic Limits: Syntrophic Propionate Oxidation in Flooded Soil

Propionate is an important intermediate of the degradation of organic matter in many anoxic environments. In methanogenic environments, due to thermodynamic constraints, the oxidation of propionate requires syntrophic cooperation of propionate-fermenting proton-reducing bacteria and H₂-consuming methanogens. We have identified here microorganisms that were active in syntrophic propionate oxidation in anoxic paddy soil by rRNA-based stable-isotope probing (SIP). After 7 weeks of incubation with [¹³C]propionate (<10 mM) and the oxidation of ~30 μmol of ¹³C-labeled substrate per g dry weight of soil, we found that archaeal nucleic acids were ¹³C labeled to a larger extent than those of the bacterial partners. Nevertheless, both terminal restriction fragment length polymorphism and cloning analyses revealed Syntrophobacter spp., Smithella spp., and the novel Pelotomaculum spp. to predominate in “heavy” ¹³C-labeled bacterial rRNA, clearly showing that these were active in situ in syntrophic propionate oxidation. Among the Archaea, mostly Methanobacterium and Methanosarcina spp. and also members of the yet-uncultured “rice cluster I” lineage had incorporated substantial amounts of ¹³C label, suggesting that these methanogens were directly involved in syntrophic associations and/or thriving on the [¹³C]acetate released by the syntrophs. With this first application of SIP in an anoxic soil environment, we were able to clearly demonstrate that even guilds of microorganisms growing under thermodynamic constraints, as well as phylogenetically diverse syntrophic associations, can be identified by using SIP. This approach holds great promise for determining the structure and function relationships of further syntrophic or other nutritional associations in natural environments and for defining metabolic functions of yet-uncultivated microorganisms.