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V Torsvik

Publications and source records attributed to V Torsvik.

14 recordsLinked to original sources

Characterization of microbial diversity in hypersaline environments by melting profiles and reassociation kinetics in combination with terminal restriction fragment length polymorphism (T-RFLP).

The diversity of prokaryotes inhabiting solar saltern ponds was determined by thermal melting and reassociation of community DNA. These measurements were compared with fingerprinting techniques such as terminal restriction fragment length polymorphisms (T-RFLP) analysis, denaturant gradient gel electrophoresis (DGGE), and cloning and sequencing approaches. Three ponds with salinities of 22, 32, and 37% (NaCl saturation) were studied. The combination of independent molecular techniques to estimate the total genetic diversity provided a realistic assessment to reveal the microbial diversity in these environments. The changes in the prokaryotic communities at different salinity (22, 32, and 37% salt) were significant and revealed that the total genetic diversity increased from 22% to 32% salinity. At 37% salinity the diversity was reduced again to nearly half that at 22% salinity. Our results revealed that the community "genome" had a DNA complexity that was 7 (in 22% salinity pond), 13 (in 32% salinity pond), and 4 (in 37% salinity pond) times the complexity of an Escherichia coli genome. The base composition profiles showed two abundant populations, which changed in relative amount between the three ponds. They indicated an uneven taxon distribution at 22% and 37% salinity and a more even distribution at 32% salinity. The results indicated a large predominating population at 37% salinity, which might correspond to the abundance of square archaea (SPhT) observed by transmission electron microscopy (TEM) and also indicated by the same T-RFLP fragment as the SPhT. The SPhT phylotype has also been reported to be the most frequently retrieved phylotype from this environment by culture independent techniques. In addition, two different operational taxonomic units (OTU) were detected at 37% salinity based on PCR with bacterial specific primers and T-RFLP. One of these predominant phylotypes is the extreme halophilic bacterium belonging to the bacteroidetes group, Salinibacter ruber.

Bacteria↗

Microenvironments and microbial community structure in sediments.

The aim of this study was to explore the potential of a combined chemical and microbiological approach as part of a study of organic carbon oxidation processes in sediments. An assessment of microbiological diversity using molecular techniques was carried out in combination with high resolution chemical measurements at the sediment-water interface of a coastal lagoon affected by eutrophication in autumn 2000. There was a 0.2 mm overlap between the O2 and H2S profiles. pH showed a maximum just above the sediment-water interface coinciding with an oxygen maximum, suggesting photosynthetic activity, and a minimum coinciding with the O2-H2S interface. The redox potential was high in bottom water and surface sediment, reflecting the presence of oxygen and oxides, and reached low values after a step-wise decrease at -18 mm. Reduction of Fe occurred within the biofilm at the O2-H2S interface and was mostly due to reduction by H2S. The elevated concentrations of dissolved Mn in the oxic water may have been caused either by in situ production within organic aggregates or lateral water flow from sites nearby at which Mn2+ diffuses out of the sediment. Sequences related to sulphur chemolitotrophs were retrieved from the biofilm samples, which is consistent with the small overlap between O2 and H2S observed in this biofilm. Although the resolution of techniques used was different, sequencing results were consistent with chemical data in delineating the same horizons according to redox, pH or ecological properties.

Bacteria↗

Methanotrophic diversity in an agricultural soil as evaluated by denaturing gradient gel electrophoresis profiles of pmoA, mxaF and 16S rDNA sequences.

Molecular methods were used to characterize the diversity of a methanotrophic population in an agricultural soil. For this purpose we have used DGGE analysis of functional and phylogenetic markers. Functional markers utilised comprised the pmoA-gene coding for the alpha-subunit of the particulate methane monooxygenase (pMMO) present in all known methanotrophs and the mxaF-gene coding for the alpha-subunit of methanol dehydrogenase (MDH) present in all gram-negative methylotrophs. In addition, we have used 16S rDNA as a phylogenetic marker. DGGE patterns of an enrichment culture, and sequencing of major DGGE bands obtained with the bacterial specific primers showed that the community structure was dominated by methanotrophic populations related to Methylobacter sp. and Methylomicrobium sp. The PCR products amplified with the functional primer sets were related to both type I and type II methanotrophs. We also designed a new pmoA-targeting primer set which could be used in a nested protocol to amplify PCR-products from DNA extracted directly from the soil.

Agriculture↗

Analysis of bacterial communities in heavy metal-contaminated soils at different levels of resolution.

The impact of heavy metal contamination on soil bacterial communities was studied in soils amended for many years with sewage sludge contaminated with heavy metals to varying extents. At the broad level of resolution, DNA reassociation analysis indicated a dramatic decrease in bacterial diversity from 16{ omitted}000 bacterial genomes (g soil [wet wt])(-1) in the non-contaminated soil to 6400 bacterial genomes (g soil [wet wt])(-1) in soil with low metal amendments and only 2000 bacterial genomes (g soil [wet wt])(-1) in soil with high metal amendments. No differences between bacterial communities of these soils, however, were displayed in the %G+C profiles analysed by thermal denaturation. At a coarse level of characterisation, in situ hybridisation analysing larger phylogenetic groups of bacteria revealed a general decrease in the percentage of cells detected with probes ARCH915, BET42a, GAM42a, SRB385, CF319a, LGCb and HGC69a with increasing metal amendment. Only cells detected with probe ALF1b increased significantly from 3.1+/-0.8% of the cells detected by the domain-specific probe EUB338 in the non-contaminated soil to 6.5+/-1.3% in soil with high metal amendments. These shifts in populations of larger phylogenetic groups were largely confirmed by dot blot analysis of 16S and 23S rDNA clone libraries from bacteria in soil with low metal and high metal amendments, respectively. For a fine-level characterisation, 72 clones of 16S rDNA libraries were identified by comparative sequence analysis. A few sequences could not be assigned to the major taxa described. Most of the sequences were assigned to the Gram-positive bacteria with a high DNA G+C content (45%) and the alpha-subdivision of Proteobacteria (24%). However, only minor differences were seen between bacterial communities from the low and high metal soils. In the soil with high metal amendment, more sequences clustered to the alpha-subdivision of Proteobacteria, while in the low metal soil, more sequences clustered to the Gram-positive bacteria with a high DNA G+C content.

Journal Article↗

Quantitative selective PCR of 16S ribosomal DNA correlates well with selective agar plating in describing population dynamics of indigenous Pseudomonas spp. in soil hot spots.

We used a quantitative PCR method targeting 16S ribosomal DNA using competitive PCR for specific detection of indigenous Pseudomonas DNA in soil hot spots. The amount of Pseudomonas DNA corresponded to the number of culturable Pseudomonas bacteria on Gould's S1 agar. This represents the first use of PCR for quantification of indigenous bacteria in more than one sample of soil.

Culture Media↗

Abundance and diversity of Archaea in heavy-metal-contaminated soils.

The impact of heavy-metal contamination on archaean communities was studied in soils amended with sewage sludge contaminated with heavy metals to varying extents. Fluorescent in situ hybridization showed a decrease in the percentage of Archaea from 1.3% +/- 0.3% of 4', 6-diamidino-2-phenylindole-stained cells in untreated soil to below the detection limit in soils amended with heavy metals. A comparison of the archaean communities of the different plots by denaturing gradient gel electrophoresis revealed differences in the structure of the archaean communities in soils with increasing heavy-metal contamination. Analysis of cloned 16S ribosomal DNA showed close similarities to a unique and globally distributed lineage of the kingdom Crenarchaeota that is phylogenetically distinct from currently characterized crenarchaeotal species.

Archaea↗

Novel techniques for analysing microbial diversity in natural and perturbed environments.

Molecular techniques were applied for analysing the entire bacterial community, including both the cultivated and non-cultivated part of the community. DNA was extracted from samples of soils and sediments, and a combination of different molecular methods were used to investigate community structure and diversity in these environments. Reassociation of sheared and thermally denatured DNA in solution was used to measure the total genetical diversity. PCR-denaturing gradient gel electrophoresis (DGGE) analysis of rRNA genes gave information about changes in the numerically dominating bacterial populations. Hybridisation with phylogenetic group specific probes, and sequencing provided information about the affiliation of the bacterial populations. Using DNA reassociation analysis we demonstrated that bacterial communities in pristine soil and sediments may contain more than 10,000 different bacterial types. The diversity of the total soil community was at least 200 times higher than the diversity of bacterial isolates from the same soil. This indicates that the culturing conditions select for a distinct subpopulation of the bacteria present in the environment. Molecular methods were applied to monitor the effects of perturbations due to antropogenic activities and pollution on microbial communities. Our investigations show that agricultural management, fish farming and pollution may lead to profound changes in the community structure and a reduction in the bacterial diversity.

Bacteria↗

Microbial Diversity and Community Structure in Two Different Agricultural Soil Communities.

Abstract In this study, two different agricultural soils were investigated: one organic soil and one sandy soil, from Stend (south of Bergen), Norway. The sandy soil was a field frequently tilled and subjected to crop rotations. The organic soil was permanent grazing land, infrequently tilled. Our objective was to compare the diversity of the cultivable bacteria with the diversity of the total bacterial population in soil. About 200 bacteria, randomly isolated by standard procedures, were investigated. The diversity of the cultivable bacteria was described at phenotypic, phylogenetic, and genetic levels by applying phenotypical testing (Biolog) and molecular methods, such as amplified rDNA restriction analysis (ARDRA); hybridization to oligonucleotide probes; and REP-PCR. The total bacterial diversity was determined by reassociation analysis of DNA isolated from the bacterial fraction of environmental samples, combined with ARDRA and DGGE analysis. The relationship between the diversity of cultivated bacteria and the total bacteria was elucidated. Organic soil exhibited a higher diversity for all analyses performed than the sandy soil. Analysis of cultivable bacteria resulted in different resolution levels and revealed a high biodiversity within the population of cultured isolates. The difference between the two agricultural soils was significantly higher when the total bacterial population was analyzed than when the cultivable population was. Thus, analysis of microbial diversity must ultimately embrace the entire microbial community DNA, rather than DNA from cultivable bacteria.

Journal Article↗

Analysis of broad-scale differences in microbial community composition of two pristine forest soils.

Broad-scale differences in soil microbial community composition were analyzed in two contrasting soils using DNA reassociation and % G + C profiles for analysis on the community-level, and filter- and whole cell hybridization techniques for a coarse-level characterization of larger phylogenetic groups of bacteria. Reassociation analysis of DNA from bacterial fractions extracted from the organic soil Seim and the mineral soil Hau revealed similar complexity of the communities with 5700 and 4900 different bacterial genomes (g soil [dry wt])-1, respectively. Thermal denaturation studies showed wide % G + C distributions in DNA from bacteria of both soils. Differences in the median % G + C with 55 to 61% for the bacterial community in soil Seim and 61 to 66% for that in soil Hau indicated a higher proportion of bacteria with a high DNA G + C content in soil Hau. In situ hybridization with fluorescent (Cy3-labeled) probes targeting larger phylogenetic groups showed minor differences between both soils, and between direct detection of bacteria in dispersed soil slurries and in bacterial fractions extracted from soils through about 90% of the total bacteria were lost during extraction. In dispersed slurries of both soils, only probes ALF1b, SRB385, and PLA46 hybridized to cells accounting for more than 1% of the DAPI-stained cells, while numbers obtained after hybridization with probes ARCH915, BET42a, GAM42a, HGC69a, and CF319a were below the detection limit set at < 1%. These results were confirmed by in situ hybridization with horseradish peroxidase (HRP)-labeled probes and subsequent Cy3-tyramide signal amplification. In contrast, dot blot hybridization with probe HGC69a indicated significant amounts of Gram-positive bacteria with a high DNA G + C content in both soils. These could subsequently be visualized in non-dispersed soil slurries by in situ hybridization with HRP-labeled probe HGC69a and Cy3-tyramide signal amplification. Filamentous Gram-positive bacteria with a high DNA G + C content, likely actinomycetes, which are present in soil Hau in significant numbers are obviously destroyed by procedures used for soil dispersion.

Actinomycetales↗

Distribution of bacterioplankton in meromictic Lake Saelenvannet, as determined by denaturing gradient gel electrophoresis of PCR-amplified gene fragments coding for 16S rRNA.

The community structure of bacterioplankton in meromictic Lake Saelenvannet was examined by PCR amplification of the V3 region of 16S rRNA from microbial communities recovered from various depths in the water column. Two different primer sets were used, one for amplification of DNA from the domain Bacteria and another specific for DNA from the domain Archaea. Amplified DNA fragments were resolved by denaturing gradient gel electrophoresis (DGGE), and the resulting profiles were reproducible and specific for the communities from different depths. Bacterial diversity estimated from the number and intensity of specific fragments in DGGE profiles decreased with depth. The reverse was true for the Archaea, with the diversity increasing with depth. Hybridization of DGGE profiles with oligonucleotide probes specific for phylogenetic groups of microorganisms showed the presence of both sulfate-reducing bacteria and methanogens throughout the water column, but they appeared to be most abundant below the chemocline. Several dominant fragments in the DGGE profiles were excised and sequenced. Among the dominant populations were representatives related to Chlorobium phaeovibrioides, chloroplasts from eukaryotic algae, and unidentified Archaea.

Animals↗

Long-range changes in oxytetracycline concentration and bacterial resistance toward oxytetracycline in a fish farm sediment after medication.

Following 10 days medication with oxytetracycline, marine sediment was sampled beneath three selected cages (cages 1, 2 and 3) at a fish farm over a period of 18 mnd., in order to detect any change in the sediment oxytetracycline concentration, bacterial number and bacterial resistance towards the drug. The bulk of oxytetracycline disappeared during the first weeks, but it persisted in the sediment at lower concentrations for quite some time after the medication. Half-life (t(1/2)) of oxytetracycline in the sediment was measured as: 125, 144 and 87 days under cages 1, 2 and 3, respectively. At the end of the medication, all three sediments had greater than 100% oxytetracycline-resistant bacteria. This value dropped to 20% after 72 days and stabilised at levels of between 10 and 50%. The change in bacterial numbers, described as total and plate counts, was due to seasonal variations rather than to the medication.

Animals↗

Comparison of phenotypic diversity and DNA heterogeneity in a population of soil bacteria.

The phenotypic diversity of about 200 bacterial strains isolated from soil was compared with the genotypic diversity of the same population. The strains were phenotypically characterized by the API 20B test system. The results of these tests were subjected to cluster analysis, which revealed 41 biotypes at 80% similarity. The five dominating biotypes contained 43% of the strains. The phenotypic diversity as determined by the Shannon index, equitability, rarefaction, and cumulative differences was high, but indicated some dominant biotypes. The genetic diversity was measured by reassociation of mixtures of denatured DNA isolated from the bacterial strains (C0t plots). The observed genetic diversity was high. Reassociation of DNA from all bacterial strains together revealed that the population contained heterologous DNA equivalent to 20 totally different bacterial genomes (i.e., genomes that have no homology). This study showed that reassociation of DNA isolated from a collection of bacteria gave a good estimate of the diversity of the collection and that there was good agreement with different phenotypic diversity measures. The Shannon index in particular has features in common with the genetic diversity measure presented here.

Bacteria↗

High diversity in DNA of soil bacteria.

Soil bacterium DNA was isolated by minor modifications of previously described methods. After purification on hydroxyapatite and precipitation with cetylpyridinium bromide, the DNA was sheared in a French press to give fragments with an average molecular mass of 420,000 daltons. After repeated hydroxyapatite purification and precipitation with cetylpyridinium bromide, high-pressure liquid chromatography analysis showed the presence of 2.1% RNA or less, whereas 5-methylcytosine made up 2.9% of the total deoxycytidine content. No other unusual bases could be detected. The hyperchromicity was 31 to 36%, and the melting curve in 1 X SSC (0.15 M NaCl plus 0.015 M sodium citrate) corresponded to 58.3 mol% G+C. High-pressure liquid chromatography analysis of two DNA samples gave 58.6 and 60.8 mol% G+C. The heterogeneity of the DNA was determined by reassociation of single-stranded DNA, measured spectrophotometrically. Owing to the high complexity of the DNA, the reassociation had to be carried out in 6 X SSC with 30% dimethyl sulfoxide added. Cuvettes with a 1-mm light path were used, and the A275 was read. DNA concentrations as high as 950 micrograms ml-1 could be used, and the reassociation rate of Escherichia coli DNA was increased about 4.3-fold compared with standard conditions. C0t1/2 values were determined relative to that for E. coli DNA, whereas calf thymus DNA was reassociated for comparison. Our results show that the major part of DNA isolated from the bacterial fraction of soil is very heterogeneous, with a C0t1/2 about 4,600, corresponding to about 4,000 completely different genomes of standard soil bacteria.(ABSTRACT TRUNCATED AT 250 WORDS)

Bacteria↗