Succession of indigenous Pseudomonas spp. and actinomycetes on barley roots affected by the antagonistic strain Pseudomonas fluorescens DR54 and the fungicide imazalil.

In recent years, the interest in the use of bacteria for biological control of plant-pathogenic fungi has increased. We studied the possible side effects of coating barley seeds with the antagonistic strain Pseudomonas fluorescens DR54 or a commercial fungicide, imazalil. This was done by monitoring the number of indigenous Pseudomonas organisms and actinomycetes on barley roots during growth in soil, harvest after 50 days, and subsequent decomposition. Bacteria were enumerated by traditional plate spreading on Gould's S1 agar (Pseudomonas) and as filamentous colonies on Winogradsky agar (actinomycetes) and by two quantitative competitive PCR assays. For this we developed an assay targeting Streptomyces and closely related genera. DR54 constituted more than 75% of the Pseudomonas population at the root base during the first 21 days but decreased to less than 10% at day 50. DR54 was not successful in colonizing root tips. Initially, DR54 affected the number of indigenous Pseudomonas organisms negatively, whereas imazalil affected Pseudomonas numbers positively, but the effects were transient. Although plate counts were considerably lower than the number of DNA copies, the two methods correlated well for Pseudomonas during plant growth, but after plant harvest Pseudomonas-specific DNA copy numbers decreased while plate counts were in the same magnitude as before. Hence, Pseudomonas was 10-fold more culturable in a decomposition environment than in the rhizosphere. The abundance of actinomycetes was unaffected by DR54 or imazalil amendments, and CFU and quantitative PCR results correlated throughout the experiment. The abundance of actinomycetes increased gradually, mostly in numbers of DNA copies, confirming their role in colonizing old roots.

Community Dynamics of Free-living and Particle-associated Bacterial Assemblages during a Freshwater Phytoplankton Bloom.

Bacterial community dynamics were followed in a 19-day period during an induced diatom bloom in two freshwater mesocosms. The main goal was to compare diversity and succession among free-living (<10 mm) and particle-associated (>10 mm) bacteria. Denaturing gradient gel electrophoresis (DGGE) of PCR amplified 16S rDNA showed the highest number of bands among free-living bacteria, but with a significant phylogenetic overlap in the two size fractions indicating that free-living bacteria were also important members of the particle-associated bacterial assemblage. Whereas the number of bands in the free-living fraction decreased during the course of the bloom, several phylotypes unique to particles appeared towards the end of the experiment. Besides the primer set targeting Bacteria, a primer set targeting most members of the Cytophaga-Flavobacterium (CF)-cluster of the Cytophaga-Flavobacterium-Bacteroides group and a primer set mainly targeting a-Proteobacteria were applied. PCR-DGGE analyses revealed that a number of phylotypes targeted by those primer sets were found solely on particles. Almost all sequenced bands from the bacterial DGGE gel were related to phylogenetic groups commonly found in freshwater: a-Proteobacteria, CF, and Firmicutes. Despite the use of primers intended to be specific mainly for a-Proteobacteria most bands sequenced from the a-proteobacterial DGGE gel formed a cluster within the Verrucomicrobiales subdivision of the Verrucomicrobia division and were not related to a-Proteobacteria. Bands sequenced from the CF DGGE gel were related to members of the CF cluster. From the present study, we suggest that free-living and particle-associated bacterial communities should not be perceived as separate entities, but rather as interacting assemblages, where the extent of phylogenetic overlap is dependent on the nature of the particulate matter.

Community level physiological profile of soil bacteria unaffected by extraction method.

Extraction and purification of bacteria from soil by the Nycodenz gradient centrifugation procedure described by Bakken and Lindahl (1995; Recovery of bacterial cells from soil. In: van Elsas, J.D., Trevors, J.T. (Eds.), Nucleic Acids in the Environment: Methods and Applications. Springer Verlag, Berlin, pp. 9-27) were compared to soil slurry extractions. Bacterial communities from four different soils were described by the bacterial abundance, CTC-reducing capacity, culturability and the community level physiological profiles (CLPP) in BIOLOG GN plates. A significant loss of both total and culturable number of bacteria g(-1) soil dry weight were found after extraction and purification of cells. The origin of soil influenced the yield of cells and a difference between the four soils and an interaction between the soils and extraction procedure were found. The culturability and the CLPP were different between the four soils but were unaffected by the extraction procedure. The bacterial community obtained after extraction and purification thus represented the same fraction of the indigenous bacterial community.

Viability of indigenous soil bacteria assayed by respiratory activity and growth.

The bacterial population in barley field soil was estimated by determining the numbers of (i) cells reducing the artificial electron acceptor 5-cyano-2,3-ditolyl tetrazolium chloride (CTC) to CTC-formazan (respiratory activity), (ii) cells dividing a limited number of times (microcolony formation) on nutrient-poor media, (iii) cells dividing many times (colony formation) on nutrient-poor agar media, and (iv) cells stained with acridine orange (total counts). The CTC reduction assay was used for the first time for populations of indigenous soil bacteria and was further developed for use in this environment. The number of viable cells was highest when estimated by the number of microcolonies developing during 2 months of incubation on filters placed on the surface of nutrient-poor media. The number of bacteria reducing CTC to formazan was slightly lower than the number of bacteria forming microcolonies. Traditional plate counts of CFU (culturable cells) yielded the lowest estimate of viable cell numbers. The microcolony assay gave an estimate of both (i) cells forming true microcolonies (in which growth ceases after a few cell divisions) representing viable but nonculturable cells and (ii) cells forming larger microcolonies (in which growth continues) representing viable, culturable cells. The microcolony assay, allowing single-cell observations, thus seemed to be best suited for estimation of viable cell numbers in soil. The effect on viable and culturable cell numbers of a temperature increase from 4 to 17 degrees C for 5 days was investigated in combination with drying or wetting of the soil. Drying or wetting prior to the temperature increase, rather than the temperature increase per se, affected both the viable and culturable numbers of bacteria; both numbers were reduced in predried soil, while they increased slightly in the prewetted soil.

[H]thymidine incorporation to estimate growth rates of anaerobic bacterial strains.

The incorporation of [H]thymidine by axenic cultures of anaerobic bacteria was investigated as a means to measure growth. The three fermentative strains and one of the methanogenic strains tested incorporated [H]thymidine, whereas the sulfate-reducing bacterium and two of the methanogenic bacteria were unable to incorporate [H]thymidine during growth. It is concluded that the [H]thymidine incorporation method underestimates bacterial growth in anaerobic environments.

Microbial biomass and activity in subsurface sediments from Vejen, Denmark.

Subsurface sediment samples were collected from 4 to 31 m below landsurface in glacio-fluvial sediments from the Quaternary period. The samples were described in terms of pH, electrical conductivity, chloride concentration, organic matter content, and grain size distribution. Viable counts of bacteria varied from 0.5 to 1,203 x 103 colony forming units/g dry weight (gdw); total numbers of bacteria acridine orange direct counts (AODC) varied from 1.7 to 147 × 10(7) cells/gdw; growth rates (incorporation of [(3)H]-thymidine) varied from 1.4 to 60.7 × 10(4) cells/(gdw · day); and rate constants for mineralization of (14)C-labelled compounds varied from 0.2 to 2.3 × 10(-3) ml/(dpm · day) for acetate, and from 0 to 2.0 × 10(-3) ml/(dpm · day) for phenol. Sediment texture influenced the total number of bacteria and potential for mineralization; with increasing content of clay and silt and decreasing content of sand, AODC increased and the mineralization rate declined. Intrinsic permeability calculated from grain size correlated positively with mineralization rate for acetate. Statistical correlation analysis showed high correlations between some of the abiotic parameters, but it was not possible to point out a single abiotic parameter that could explain the variation of size and activity of the microbial population. The microbial data obtained in these geologically young sediments were compared to literature data from older sediments, and this comparison showed that age and type of geological formation might be important for the size and activity of the microbial populations.

Contrasts between subsurface microbial communities and their metabolic adaptation to polycyclic aromatic hydrocarbons at a forested and an urban coal-tar disposal site.

The abundance and distribution of microorganisms and their potential for mineralizing polycyclic aromatic hydrocarbons (PAHs) were measured in subsurface sediment samples at two geographically separate buried coal-tar sites. At a relatively undisturbed forested site in the northeastern United States, metabolic adaptation to the PAHs was evident: Radiolabeled naphthalene and phenanthrene were converted to (14)CO2 in core material from inside but not outside a plume of groundwater contamination. However, at the urban site in the midwestern United States these PAHs were mineralized in sediments from both contaminated and uncontaminated boreholes. Thus, clear qualitative evidence showing an adaptational response by the subsurface microbial community was not obtained at the urban site. Instead, subtler clues suggesting metabolic adaptation by subsurface microorganisms from the urban site were discerned by comparing lag periods and extents of (14)CO2 production from radiolabeled PAHs added to samples from contaminated and uncontaminated boreholes. Despite slightly higher PAH mineralization activity in contaminated borehole samples, p-hydroxybenzoate was mineralized equally in all samples from the urban site regardless of location. No striking trends in the abundances of actinomycetes, fungi, and either viable or total bacteria were encountered. However, colonies of the soil bacterium, Bacillus mycoides, were detected on enumeration plates of several samples from unsaturated and saturated zones in both urban boreholes. Furthermore, other common soil bacteria, Myxococcus xanthus and Chromobacterium violaceum, were identified in samples from the uncontaminated urban borehole. The occurrence of bacteria usually restricted to surface soil, combined with the observation of fragments of building materials in many of the core samples, suggested that past excavation and backfilling operations may have caused mixing of surface soil with subsurface materials at the urban site. We speculate that this mixing, as well as non-coal-tar-derived sources of PAHs, contributed to the PAH-mineralizing activity present in the sediment samples from the uncontaminated urban borehole.