Cultivation-independent detection of autotrophic hydrogen-oxidizing bacteria by DNA stable-isotope probing.

Knallgas bacteria are a physiologically defined group that is primarily studied using cultivation-dependent techniques. Given that current cultivation techniques fail to grow most bacteria, cultivation-independent techniques that selectively detect and identify knallgas bacteria will improve our ability to study their diversity and distribution. We used stable-isotope probing (SIP) to identify knallgas bacteria in rhizosphere soil of legumes and in a microbial mat from Obsidian Pool in Yellowstone National Park. When samples were incubated in the dark, incorporation of (13)CO(2) was H(2) dependent. SIP enabled the detection of knallgas bacteria that were not detected by cultivation, and the majority of bacteria identified in the rhizosphere soils were betaproteobacteria predominantly related to genera previously known to oxidize hydrogen. Bacteria in soil grew on hydrogen at concentrations as low as 100 ppm. A hydB homolog encoding a putative high-affinity NiFe hydrogenase was amplified from (13)C-labeled DNA from both vetch and clover rhizosphere soil. The results indicate that knallgas bacteria can be detected by SIP and populations that respond to different H(2) concentrations can be distinguished. The methods described here should be applicable to a variety of ecosystems and will enable the discovery of additional knallgas bacteria that are resistant to cultivation.

Dynamic secondary ion mass spectrometry imaging of microbial populations utilizing C-labelled substrates in pure culture and in soil.

We demonstrate that dynamic secondary ion mass spectrometry (SIMS)-based ion microscopy can provide a means of measuring (13)C assimilation into individual bacterial cells grown on (13)C-labelled organic compounds in the laboratory and in field soil. We grew pure cultures of Pseudomonas putida NCIB 9816-4 in minimal media with known mixtures of (12)C- and (13)C-glucose and analysed individual cells via SIMS imaging. Individual cells yielded signals of masses 12, 13, 24, 25, 26 and 27 as negative secondary ions indicating the presence of (12)C(-), (13)C(-), (24)((12)C(2))(-), (25)((12)C(13)C)(-), (26)((12)C(14)N)(-) and (27)((13)C(14)N)(-) ions respectively. We verified that ratios of signals taken from the same cells only changed minimally during a approximately 4.5 min period of primary O(2)(+) beam sputtering by the dynamic SIMS instrument in microscope detection mode. There was a clear relationship between mass 27 and mass 26 signals in Pseudomonas putida cells grown in media containing varying proportions of (12)C- to (13)C-glucose: a standard curve was generated to predict (13)C-enrichment in unknown samples. We then used two strains of Pseudomonas putida able to grow on either all or only a part of a mixture of (13)C-labelled and unlabelled carbon sources to verify that differential (13)C signals measured by SIMS were due to (13)C assimilation into cell biomass. Finally, we made three key observations after applying SIMS ion microscopy to soil samples from a field experiment receiving (12)C- or (13)C-phenol: (i) cells enriched in (13)C were heterogeneously distributed among soil populations; (ii) (13)C-labelled cells were detected in soil that was dosed a single time with (13)C-phenol; and (iii) in soil that received 12 doses of (13)C-phenol, 27% of the cells in the total community were more than 90% (13)C-labelled.

Field-based stable isotope probing reveals the identities of benzoic acid-metabolizing microorganisms and their in situ growth in agricultural soil.

We used a combination of stable isotope probing (SIP), gas chromatography-mass spectrometry-based respiration, isolation/cultivation, and quantitative PCR procedures to discover the identity and in situ growth of soil microorganisms that metabolize benzoic acid. We added [(13)C]benzoic acid or [(12)C]benzoic acid (100 microg) once, four times, or five times at 2-day intervals to agricultural field plots. After monitoring (13)CO(2) evolution from the benzoic acid-dosed soil, field soils were harvested and used for nucleic acid extraction and for cultivation of benzoate-degrading bacteria. Exposure of soil to benzoate increased the number of culturable benzoate degraders compared to unamended soil, and exposure to benzoate shifted the dominant culturable benzoate degraders from Pseudomonas species to Burkholderia species. Isopycnic separation of heavy [(13)C]DNA from the unlabeled fraction allowed terminal restriction fragment length polymorphism (T-RFLP) analyses to confirm that distinct 16S rRNA genes were localized in the heavy fraction. Phylogenetic analysis of sequenced 16S rRNA genes revealed a predominance (15 of 58 clones) of Burkholderia species in the heavy fraction. Burkholderia sp. strain EBA09 shared 99.5% 16S rRNA sequence similarity with a group of clones representing the dominant RFLP pattern, and the T-RFLP fragment for strain EBA09 and a clone from that cluster matched the fragment enriched in the [(13)C]DNA fraction. Growth of the population represented by EBA09 during the field-dosing experiment was demonstrated by using most-probable-number-PCR and primers targeting EBA09 and the closely related species Burkholderia hospita. Thus, the target population identified by SIP not only actively metabolized benzoic acid but reproduced in the field upon the addition of the substrate.

Naphthalene metabolism and growth inhibition by naphthalene in Polaromonas naphthalenivorans strain CJ2.

This study was designed to characterize naphthalene metabolism in Polaromonas naphthalenivorans CJ2. Comparisons were completed using two archetypal naphthalene-degrading bacteria: Pseudomonas putida NCIB 9816-4 and Ralstonia sp. strain U2, representative of the catechol and gentisate pathways, respectively. Strain CJ2 carries naphthalene catabolic genes that are homologous to those in Ralstonia sp. strain U2. Here we show that strain CJ2 metabolizes naphthalene via gentisate using respirometry, metabolite detection by GC-MS and cell-free enzyme assays. Unlike P. putida NCIB 9816-4 or Ralstonia sp. strain U2, strain CJ2 did not grow in minimal medium saturated with naphthalene. Growth assays revealed that strain CJ2 is inhibited by naphthalene concentrations of 78 microM (10 p.p.m.) and higher, and the inhibition of growth is accompanied by the accumulation of orange-coloured, putative naphthalene metabolites in the culture medium. Loss of cell viability coincided with the appearance of the coloured metabolites, and analysis by HPLC suggested that the accumulated metabolites were 1,2-naphthoquinone and its unstable auto-oxidation products. The naphthoquinone breakdown products accumulated in inhibited, but not uninhibited, cultures of strain CJ2. Furthermore, naphthalene itself was shown to directly inhibit growth of a regulatory mutant of strain CJ2 that is unable to metabolize naphthalene. These results suggest that, despite being able to use naphthalene as a carbon and energy source, strain CJ2 must balance naphthalene utilization against two types of toxicity.

Use of field-based stable isotope probing to identify adapted populations and track carbon flow through a phenol-degrading soil microbial community.

The goal of this field study was to provide insight into three distinct populations of microorganisms involved in in situ metabolism of phenol. Our approach measured 13CO2 respired from [13C]phenol and stable isotope probing (SIP) of soil DNA at an agricultural field site. Traditionally, SIP-based investigations have been subject to the uncertainties posed by carbon cross-feeding. By altering our field-based, substrate-dosing methodologies, experiments were designed to look beyond primary degraders to detect trophically related populations in the food chain. Using gas chromatography-mass spectrometry (GC/MS), it was shown that (13)C-labeled biomass, derived from primary phenol degraders in soil, was a suitable growth substrate for other members of the soil microbial community. Next, three dosing regimes were designed to examine active members of the microbial community involved in phenol metabolism in situ: (i) 1 dose of [13C]phenol, (ii) 11 daily doses of unlabeled phenol followed by 1 dose of [13C]phenol, and (iii) 12 daily doses of [13C]phenol. GC/MS analysis demonstrated that prior exposure to phenol boosted 13CO2 evolution by a factor of 10. Furthermore, imaging of 13C-treated soil using secondary ion mass spectrometry (SIMS) verified that individual bacteria incorporated 13C into their biomass. PCR amplification and 16S rRNA gene sequencing of 13C-labeled soil DNA from the 3 dosing regimes revealed three distinct clone libraries: (i) unenriched, primary phenol degraders were most diverse, consisting of alpha-, beta-, and gamma-proteobacteria and high-G+C-content gram-positive bacteria, (ii) enriched primary phenol degraders were dominated by members of the genera Kocuria and Staphylococcus, and (iii) trophically related (carbon cross-feeders) were dominated by members of the genus Pseudomonas. These data show that SIP has the potential to document population shifts caused by substrate preexposure and to follow the flow of carbon through terrestrial microbial food chains.