Impact of temperature on in planta expression of genes involved in synthesis of the Pseudomonas syringae phytotoxin coronatine.

Coronatine (COR) is a chlorosis-inducing phytotoxin produced by the plant-pathogenic bacterium Pseudomonas syringae. Confocal laser scanning microscopy was used to investigate in vitro and in planta expression of COR genes by two model organisms, P. syringae pv. glycinea PG4180, a pathogen of soybean, and P syringae pv. tomato DC3000, a pathogen of tomato and crucifers. Previously, it was shown in vitro that the cma operon involved in COR synthesis in PG4180 is expressed in a temperature-dependent manner, with maximal rates at 18 degrees C and low activity at 28 degrees C. However, nothing was known about the influence of temperature on the expression of COR biosynthetic genes in planta. Therefore, transcriptional fusions of the PG4180 and DC3000 cma promoter regions to a promoterless egfp gene were constructed and expressed in both P. syringae strains. The fluorescence patterns in response to temperature during growth of a strain in vitro were consistent with its COR production and the cma transcript abundance as revealed by RNA dot blot hybridization. Quantification of fluorescence indicated that cma promoter activity was dependent on the genetic background of the host strain. Expression of cma::egfp in PG4180 was temperature-dependent in minimal medium as well as inside the plant tissue. In contrast, transcription of the cma operon was not significantly affected by temperature in DC3000. However, cells of DC3000 harboring the cma::egfp fusions showed higher levels of fluorescence when recovered from infected host plants compared with cells grown in minimal medium. These results indicate that the signals for induction of COR biosynthesis differ significantly in PG4180 and DC3000.

Acetoclastic and hydrogenotrophic methane production and methanogenic populations in an acidic West-Siberian peat bog.

Sites in the West Siberian peat bog 'Bakchar' were acidic (pH 4.2-4.8), low in nutrients, and emitted CH4 at rates of 0.2-1.5 mmol m(-2) h(-1). The vertical profile of delta13CH4 and delta13CO2 dissolved in the porewater indicated increasing isotope fractionation and thus increasing contribution of H2/CO2-dependent methanogenesis with depth. The anaerobic microbial community at 30-50 cm below the water table produced CH4 with optimum activity at 20-25 degrees C and pH 5.0-5.5 respectively. Inhibition of methanogenesis with 2-bromo-ethane sulphonate showed that acetate, phenyl acetate, phenyl propionate and caproate were important intermediates in the degradation pathway of organic matter to CH4. Further degradation of these intermediates indicated that 62-72% of the CH4 was ultimately derived from acetate, the remainder from H2/CO2. Turnover times of [2-14C]acetate were on the order of 2 days (15, 25 degrees C) and accounted for 60-65% of total CH4 production. Conversion of 14CO2 to 14CH4 accounted for 35-43% of total CH4 production. These results showed that acetoclastic and hydrogenotrophic methanogenesis operated closely at a ratio of approximately 2 : 1 irrespective of the incubation temperature (4, 15 and 25 degrees C). The composition of the archaeal community was determined in the peat samples by terminal restriction fragment length polymorphism (T-RFLP) analysis and sequencing of amplified SSU rRNA gene fragments, and showed that members of Methanomicrobiaceae, Methanosarcinaceae and Rice cluster II (RC-II) were present. Other, presumably non-methanogenic archaeal clusters (group III, RC-IV, RC-V, RC-VI) were also detected. Fluorescent in situ hybridization (FISH) showed that the number of Bacteria decreased (from 24 x 10(7) to 4 x 10(7) cells per gram peat) with depth (from 5 to 55 cm below the water table), whereas the numbers of Archaea slightly increased (from 1 x 10(7) to 2 x 10(7) cells per gram peat). Methanosarcina spp. accounted for about half of the archaeal cells. Our results show that both hydrogenotrophic and acetoclastic methanogenesis are an integral part of the CH4-producing pathway in acidic peat and were represented by appropriate methanogenic populations.

Development and steroid regulation of RFamide immunoreactivity in antennal-lobe neurons of the sphinx moth Manduca sexta.

During metamorphosis, the insect nervous system undergoes considerable remodeling: new neurons are integrated while larval neurons are remodeled or eliminated. To understand further the mechanisms involved in transforming larval to adult tissue we have mapped the metamorphic changes in a particularly well established brain area, the antennal lobe of the sphinx moth Manduca sexta, using an antiserum recognizing RFamide-related neuropeptides. Five types of RFamide-immunoreactive (ir) neurons could be distinguished in the antennal lobe, based on morphology and developmental appearance. Four cell types (types II-V, each consisting of one or two cells) showed RFamide immunostaining in the larva that persisted into metamorphosis. By contrast, the most prominent group (type I), a mixed population of local and projection neurons consisting of about 60 neurons in the adult antennal lobe, acquired immunostaining in a two-step process during metamorphosis. In a first step, from 5 to 7 days after pupal ecdysis, the number of labeled neurons reached about 25. In a second step, starting about 4 days later, the number of RFamide-ir neurons increased within 6 days to about 60. This two-step process parallels the rise and fall of the developmental hormone 20-hydroxyecdysone (20E) in the hemolymph. Artificially shifting the 20E peak to an earlier developmental time point resulted in the precocious appearance of RFamide immunostaining and led to premature formation of glomeruli. Prolonging high 20E concentrations to stages when the hormone titer starts to decline had no effect on the second increase of immunostained cell numbers. These results support the idea that the rise in 20E, which occurs after pupal ecdysis, plays a role in the first phase of RFamide expression and in glomeruli formation in the developing antennal lobes. The role of 20E in the second phase of RFamide expression is less clear, but increased cell numbers showing RFamide-ir do not appear to be a consequence of the declining levels in 20E that occur during adult development.

Quantification of Gram-negative sulphate-reducing bacteria in rice field soil by 16S rRNA gene-targeted real-time PCR.

For the quantification of Gram-negative sulphate reducers in rice fields, 11 real-time PCR assays were established targeting 16S rRNA genes combined with SybrGreen detection. Three of these assays were specific for the "main" groups, i.e. the Desulfovibrionaceae, the Desulfobacteraceae and Desulfobulbus sp., whereas eight assays were developed for subgroups within the first two main groups. The detection limits of the assays were between 2 x 10(5) and 4 x 10(3) targets g(-1) (wet weight) or less than 0.02% of the eubacterial 16S rDNA targets in bulk soil, rhizosphere soil and rice root DNA extracts. Analysis of soil spiked with defined cell numbers of sulphate-reducing bacteria showed good correlation of measured target numbers to amended cells. In rice field bulk and rhizosphere soil, the Desulfobacteraceae were the predominant main group with target numbers of 6.4 x 10(7) (+/-1.0 x 10(7)) and 7.5 x 10(7) (+/-1.7 x 10(7)), respectively. Within this group the Desulforhabdus/Synthrophobacter assemblage and Desulfobacterium sp. were predominant. At the rice roots, the three main groups were abundant in similar numbers (approx. 1.0 x 10(8)) indicating that the relative abundance of the Desulfovibrionaceae and also of Desulfobulbus sp. was increased, relatively to the Desulfobacteraceae. Within the Desulfovibrionaceae the subgroup was predominant that was detected by assay DSV-II. This assay detects many from rice field soil isolated Desulfovibrio-strains and molecular retrieved sequences. Therefore these organisms that were already detected in the rice field environment by isolation and by molecular techniques are indeed best adapted to the conditions provided by the rice roots.

Identification of rice root associated nitrate, sulfate and ferric iron reducing bacteria during root decomposition.

Leakage of O(2) from roots of aquatic plants supports the oxidation of ammonia to nitrate and of sulfide to sulfate in the rhizosphere, so that these electron acceptors may become available to the root microbial communities and affect their activity. We studied the composition of the bacterial community active in anoxically incubated rice roots by analysis of terminal restriction fragment length polymorphism (T-RFLP) and by cloning and sequencing targeting bacterial 16S rRNA. The bacterial ribosomal abundance in unamended rice roots, which were naturally encrusted with ferric iron, were initially dominated (about 65% of total 16S rRNA) by Clostridium, Bacillus and Geobacter/Pelobacter, but after 5 d clostridia decreased and members of the Cytophaga-Flavobacterium-Bacteroides (CFB) phylum increased (up to 30% of total 16S rRNA). Addition of nitrate or sulfate to the root incubations resulted in bacterial growth detected by fluorescent in situ hybridization (FISH). It also affected the steady state concentrations of H(2), acetate, propionate and butyrate that were measured in the root incubations. Nitrate reducers were apparently involved in consumption of all of these compounds. Sulfate reducers, on the other hand, showed net production of acetate during utilization of propionate. Nitrate stimulated populations of Bacillus and Dechloromonas to become active, the latter temporarily increasing to 25% of total 16S rRNA, but suppressed the increase of CFB bacteria. Sulfate, on the other hand, stimulated Desulfosporosinus and Geobacter/Pelobacter, increasing to about 15% of total 16S rRNA, and suppressed CFB bacteria to become active. In conclusion, our study showed the potential effect of exogenous electron acceptors on the composition and activity of the bacterial community in rice root incubations, and identified the phylogenetic groups of the root microbial communities that respond to an increased availability of nitrate or sulfate.

Isolation and molecular characterization of thiosulfate-oxidizing bacteria from an Italian rice field soil.

In rice paddy soils an active cycling of sulfur compounds takes place. To elucidate the diversity of thiosulfate-oxidizing bacteria these organisms were enriched from bulk soil and rice roots by the most probable number method in liquid medium. From the MPN enrichment cultures 21 bacterial strains were isolated on solid mineral medium, and could be further shown to produce sulfate from thiosulfate. These strains were characterized by 16S rDNA analyses. The isolates were affiliated to seven different phylogenetic groups within the alpha- and beta-subclass of Proteobacteria. Two of these phylotypes were already described as S-oxidizers in this environment (Xanthobacter sp. and Bosea sp. related strains), but five groups represented new S-oxidizers in rice field soil. These isolates were closely related to Mesorhizobium loti, to Hydrogenophaga sp., to Delftia sp., to Pandoraea sp. or showed sequence similarity to a strain of Achromobacter sp.

Quantitative detection of methanotrophs in soil by novel pmoA-targeted real-time PCR assays.

Methane oxidation in soils is mostly accomplished by methanotrophic bacteria. Little is known about the abundance of methanotrophs in soils, since quantification by cultivation and microscopic techniques is cumbersome. Comparison of 16S ribosomal DNA and pmoA (alpha subunit of the particulate methane monooxygenase) phylogenetic trees showed good correlation and revealed five distinct groups of methanotrophs within the alpha and gamma subclasses of Proteobacteria: the Methylococcus group, the Methylobacter/Methylosarcina group, the Methylosinus group, the Methylocapsa group, and the forest clones group (a cluster of pmoA sequences retrieved from forest soils). We developed quantitative real-time PCR assays with SybrGreen for each of these five groups and for all methanotrophic bacteria by targeting the pmoA gene. Detection limits were between 10(1) and 10(2) target molecules per reaction for all assays. Real-time PCR analysis of soil samples spiked with cells of Methylococcus capsulatus, Methylomicrobium album, and Methylosinus trichosporium recovered almost all the added bacteria. Only the Methylosinus-specific assay recovered only 20% of added cells, possibly due to a lower lysis efficiency of type II methanotrophs. Analysis of the methanotrophic community structure in a flooded rice field soil showed (5.0 +/- 1.4) x 10(6) pmoA molecules g(-1) for all methanotrophs. The Methylosinus group was predominant (2.7 x 10(6) +/- 1.1 x 10(6) target molecules g(-1)). In addition, bacteria of the Methylobacter/Methylosarcina group were abundant (2.0 x 10(6) +/- 0.9 x 10(6) target molecules g of soil(-1)). On the other hand, pmoA affiliated with the forest clones and the Methylocapsa group was below the detection limit of 1.9 x 10(4) target molecules g of soil(-1). Our results showed that pmoA-targeted real-time PCR allowed fast and sensitive quantification of the five major groups of methanotrophs in soil. This approach will thus be useful for quantitative analysis of the community structure of methanotrophs in nature.

Differential detection of type II methanotrophic bacteria in acidic peatlands using newly developed 16S rRNA-targeted fluorescent oligonucleotide probes.

Abstract Based on an extensive 16S rRNA sequence database for type II methanotrophic bacteria, a set of 16S rRNA-targeted oligonucleotide probes was developed for differential detection of specific phylogenetic groups of these bacteria by fluorescence in situ hybridisation (FISH). This set of oligonucleotides included a genus-specific probe for Methylocystis (Mcyst-1432) and three species-specific probes for Methylosinus sporium (Msins-647), Methylosinus trichosporium (Msint-1268) and the recently described acidophilic methanotroph Methylocapsa acidiphila (Mcaps-1032). These novel probes were applied to further characterise the type II methanotroph community that was detected in an acidic Sphagnum peat from West Siberia in a previous study (Dedysh et al. (2001) Appl. Environ. Microbiol. 67, 4850-4857). The largest detectable population of indigenous methanotrophs simultaneously hybridised with a group-specific probe targeting all currently known Methylosinus/Methylocystis spp. (M-450), with a genus-specific probe for Methylocystis spp. (Mcyst-1432), and with an additional probe (Mcyst-1261) that had been designed to target a defined phylogenetic subgroup of Methylocystis spp. The same subgroup of Methylocystis was also detected in acidic peat sampled from Sphagnum-dominated wetland in northern Germany. The population size of this peat-inhabiting Methylocystis subgroup was 2.0+/-0.1x10(6) cells g(-1) (wet weight) of peat from Siberia and 5.5+/-0.5x10(6) cells g(-1) of peat from northern Germany. This represented 60 and 95%, respectively, of the total number of methanotroph cells detected by FISH in these two wetland sites. Other major methanotroph populations were M. acidiphila and Methylocella palustris. Type I methanotrophs accounted for not more than 1% of total methanotroph cells. Neither M. trichosporium nor M. sporium were detected in acidic Sphagnum peat.

Effects of nitrate- and sulfate-amendment on the methanogenic populations in rice root incubations.

Abstract Potential interactions between methanogenic archaea and nitrate- and sulfate-reducing bacteria were studied in anoxic incubations of excised rice roots as a model system, by following changes in the concentrations of electron donors and acceptors and in the methanogenic community structure. The relative abundances of methanogenic groups were determined by analyses of terminal restriction fragment length polymorphism targeting archaeal SSU rRNA. Nitrate and sulfate amendment both resulted in suppression of CH(4) production. Suppression by nitrate was initially due to substrate competition for H(2) but eventually also resulted in the suppression of rRNA synthesis of methanogens, in particular of Methanosarcina spp., which was most probably caused by toxic N-compounds (e.g. nitrite). Sulfate-reducing bacteria also successfully competed with methanogens for H(2) and retarded the growth (and/or rRNA synthesis) of the methanogenic populations belonging to the hydrogenotrophic Rice cluster I/Methanomicrobiaceae-group. Our results thus show the potential effect of competition and substrate toxicity on growth and/or synthesis of ribosomes in the two major functional groups of methanogens in a natural habitat.

Enumeration of 16S rDNA of Desulfotomaculum lineage 1 in rice field soil by real-time PCR with SybrGreen detection.

Real-time PCR is a new and highly sensitive method for the quantification of microbial organisms in environmental samples. This work was conducted to evaluate real-time PCR with SybrGreen (SG) detection as quantification method for Desulfotomaculum lineage 1 organisms in samples of rice field soil. The method was optimized in several parameters like SG concentration. These allowed quantitative PCR with different primer combinations yielding PCR products with lengths up to 1066 bp and with sensitivities of 10(2) targets for all assays. The detection limit in environmental DNA extracts (rice bulk soil and rice roots) was 10(6) targets per gram dry weight according to the dilution of the DNA extracts necessary to overcome PCR inhibition of humic substances. A verification, that the fluorescence increase was due to specific PCR products, was done by agarose gel electrophoresis since melting curve analysis of the PCR products did not show a distinct peak in the first derivative, when the environmental DNA extracts were used in PCR. Amplification with a primer combination specific for Desulfotomaculum lineage 1 organisms showed an abundance of this group of approximately 2% and 0.5% of the eubacterial 16S rDNA targets in rice bulk soil and rice root samples, respectively. Approximately half of this number was obtained in both habitats with a PCR assay specific for a Desulfotomaculum sequence cluster obtained previously from rice field soil.