Consumption of NO by methanotrophic bacteria in pure culture and in soil

Abstract The methanotrophs Methylomonas angile (type I) and Methylosinus trichosporium (type II) produced nitrite, nitrate and N₂O during growth on methane, apparently by heterotrophic nitrification of ammonium. The methanotrophs were also able to consume NO but did not produce it. After incubation of soil from a drained paddy field in the presence of CH₄ the numbers of methanotrophs increased from 10⁵ to 10⁷ per gram dry weigth. The thus enriched soil showed increased rates of NO consumption while rates of NO production did not change.     

Selective grazing of methanotrophs by protozoa in a rice field soil

Biological methane oxidation is a key process in the methane cycle of wetland ecosystems. The methanotrophic biomass may be grazed by protozoa, thus linking the methane cycle to the soil microbial food web. In the present study, the edibility of different methanotrophs for soil protozoa was compared. The number of methanotroph-feeding protozoa in a rice field soil was estimated by determining the most-probable number (MPN) using methanotrophs as food bacteria; naked amoebae and flagellates were the dominant protozoa. Among ten methanotrophic strains examined as a food source, seven yielded a number of protozoa comparable with the yield with Escherichia coli [10⁴ MPN (g soil dry weight)⁻¹], and three out of four Methylocystis spp. yielded significantly fewer numbers [10²–10³ MPN (g soil dry weight)⁻¹]. The lower edibility of the Methylocystis spp. was not explained either by their growth phase or by harmful effects on protozoa. Incubation of the soil under methane resulted in a higher number of protozoa actively grazing on methanotrophs, especially on the less-edible group. Protozoa isolated from the soil demonstrated a grazing preference on the different methanotrophs consistent with the results of MPN counts. The results indicate that selective grazing by protozoa may be a biological factor affecting the methanotrophic community in a wetland soil.     

Diversity and activity of methanotrophs in alkaline soil from a Chinese coal mine

Culture-independent molecular biological techniques, including 16S rRNA gene and functional gene clone libraries and microarray analyses using pmoA (encoding a key subunit of particulate methane monooxygenase), were applied to investigate the methanotroph community structure in alkaline soil from a Chinese coal mine. This environment contained a high diversity of methanotrophs, including the type II methanotrophs Methylosinus / Methylocystis , type I methanotrophs related to Methylobacter / Methylosoma and Methylococcus , and a number of as yet uncultivated methanotrophs. In order to identify the metabolically active methane-oxidizing bacteria from this alkaline environment, DNA stable isotope probing (DNA-SIP) experiments using ¹³CH₄ were carried out. This showed that both type I and type II methanotrophs were active, together with methanotrophs related to Methylocella , which had previously been found only in acidic environments. Methylotrophs, including Methylopila and Hyphomicrobium , were also detected in soil DNA and after DNA-SIP experiments. DNA sequence information on the most abundant, active methanotrophs in this alkaline soil will facilitate the design of oligonucleotide probes to monitor enrichment cultures when isolating key alkaliphilic methanotrophs from such environments.     

Monitoring impact of in situ biostimulation treatment on groundwater bacterial community by DGGE

Changes in bacterial diversity during the field experiment on biostimulation were monitored by denaturing gradient gel electrophoresis (DGGE) analysis of PCR-amplified 16S rDNA fragments. The results revealed that the bacterial community was disturbed after the start of treatment, continued to change for 45 days or 60 days and then formed a relatively stable community different from the original community structure. DGGE analysis of soluble methane monooxygenase (sMMO) hydroxylase gene fragments, mmoX, was performed to monitor the shifts in the numerically dominant sMMO-containing methanotrophs during the field experiment. Sequence analysis on the mmoX gene fragments from the DGGE bands implied that the biostimulation treatment caused a shift of potential dominant sMMO-containing methanotrophs from type I methanotrophs to type II methanotrophs.     

Activity and composition of methanotrophic bacterial communities in planted rice soil studied by flux measurements, analyses of pmoA gene and stable isotope probing of phospholipid fatty acids

Methanotrophs in the rhizosphere of rice field ecosystems attenuate the emissions of CH₄ into the atmosphere and thus play an important role for the global cycle of this greenhouse gas. Therefore, we measured the activity and composition of the methanotrophic community in the rhizosphere of rice microcosms. Methane oxidation was determined by measuring the CH₄ flux in the presence and absence of difluoromethane as a specific inhibitor for methane oxidation. Methane oxidation started on day 24 and reached the maximum on day 32 after transplantation. The total methanotrophic community was analysed by terminal restriction fragment length polymorphism (T-RFLP) and cloning/sequencing of the pmoA gene, which encodes a subunit of particulate methane monooxygenase. The metabolically active methanotrophic community was analysed by stable isotope probing of microbial phospholipid fatty acids (PLFA-SIP) using ¹³C-labelled CH₄ directly added to the rhizospheric region. Rhizospheric soil and root samples were collected after exposure to ¹³CH₄ for 8 and 18 days. Both T-RFLP/cloning and PLFA-SIP approaches showed that type I and type II methanotrophic populations changed over time with respect to activity and population size in the rhizospheric soil and on the rice roots. However, type I methanotrophs were more active than type II methanotrophs at both time points indicating they were of particular importance in the rhizosphere. PLFA-SIP showed that the active methanotrophic populations exhibit a pronounced spatial and temporal variation in rice microcosms.     

Monitoring the fate of genetically engineered bacteria sprayed on the phylloplane of bush beans and grass

Abstract The fate of a Bacillus amyloliquefaciens with the recombinant plasmid pSB20 sprayed on the phyllosphere of grass, and of a Tn 5 marked Pseudomonas syringae sprayed on the phyllosphere of bush beans was studied in planted soil microcosms. B. amyloliquefaciens showed a decline from 1.5×10⁸ to 3.1×10² cfu g⁻¹ on the phylloplane of grass in the course of the experiment. B. amyloliquefaciens was easy to follow by selective cultivation due to the complete absence of bacterial background growth. Southern blot hybridization of Hin dIII digested genomic DNA showed plasmid restriction patterns identical with pSB20 indicating high plasmid stability. In total DNA extracts from phyllosphere bacteria the recombinant plasmid was detectable by Southern blot hybridization up to 6×10⁴ cfu g⁻¹ (wet weight). Counts of hybridizing colonies showed that P. syringae established on the phyllosphere of bush beans at between 5×10³ and 4×10⁶ cfu g⁻¹ fresh weight. During senescence of the bean plants the strain was no longer detectable by selective cultivation and subsequent colony hybridization. In contrast, Tn5 marked DNA was detected after PCR amplification over the whole period of the experiment.     

Survival of κ-carrageenan-encapsulated and unencapsulated Pseudomonas aeruginosa UG2Lr cells in forest soil monitored by polymerase chain reaction and spread plating

Abstract A method was developed for direct extraction, purification and amplification of DNA from forest soil. Eighty-two % of the DNA in Pseudomonas aeruginosa UG2Lr introduced into soil was recovered. The detection limit for the strain was approximately 800 cfu g⁻¹ of dry soil based on the polymerase chain reaction (PCR). Survival of κ-carrageenan-encapsulated and unencapsulated UG2Lr was monitored by antibiotic selective and bioluminescence-based nonselective plating and PCR-amplification of a tnsA fragment. After freeze-thaw treatment of soil samples, the unencapsulated UG2Lr declined from an initial population density of 1 × 10⁹ cfu g⁻¹ of dry soil to below the detection threshold of both selective (14 cfu g⁻¹ of dry soil) and nonselective (1 × 10³ cfu g⁻¹ of dry soil) plating. However, presence of nonculturable UG2Lr cells in the soil was revealed by PCR and resuscitation of the bacteria. Population density of the encapsulated UG2Lr increased from 2.7 × 10⁶ to 2.9 × 10⁸ cfu g⁻¹ of dry soil after a 3-week incubation at 22°C and declined to 6.3 × 10⁶ cfu g⁻¹ of dry soil after the freeze-thaw treatment.     

Activity of methanotrophic bacteria in Green Bay sediments

Abstract Sediment pore water samples obtained from a 19 m station in Green Bay in Lake Michigan were examined for levels of ambient dissolved methane and copper, and for the potential for in situ methane oxidation by methanotrophs found within surface sediments. The in situ methane concentration in the upper oxic sediment layer ranged from 20–150 μmol · 1⁻¹ at this station. The activity of methanotrophs and the kinetics of methane oxidation in these sediments were demonstrated by the uptake of radiolabeled methane. K_s values varied between 4.1–9.6 nmol · cm³ of sediment slurry. High V_max values (12.7–35.2 nmol · cm⁻³ · h⁻¹) suggest a large population of methanotrophs in the sediments. An average methane flux to the oxic sediments of 0.24 mol · m⁻² · year⁻¹ was calculated from the pore water methane gradients. Pore water concentrations of copper in the upper sediment layer ranged from 10–120 nmol · 1⁻¹. Based upon the copper concentration, other measured parameters, and equilibrium conditions defined by WATEQF4, an estimate for dissolved free Cu²⁺ concentration of 5–38 nmol · 1⁻¹ pore water was obtained. Several factors control the rate of methane oxidation, including oxygen, methane, and the bioavailability of free Cu²⁺.     

Molecular detection of marine bacterial populations on beaches contaminated by the Nakhodka tanker oil-spill accident

In January 1997, the tanker Nakhodka sank in the Japan Sea, and more than 5000 tons of heavy oil leaked. The released oil contaminated more than 500 km of the coastline, and some still remained even by June 1999. To investigate the long-term influence of the Nakhodka oil spill on marine bacterial populations, sea water and residual oil were sampled from the oil-contaminated zones 10, 18, 22 and 29 months after the accident, and the bacterial populations in these samples were analysed by denaturing gradient gel electrophoresis (DGGE) of PCR-amplified 16S rDNA fragments. The dominant DGGE bands were sequenced, and the sequences were compared with those in DNA sequence libraries. Most of the bacteria in the sea water samples were classified as the  Cytophaga – Flavobacterium – Bacteroides phylum, α- Proteobacteria or cyanobacteria. The bacteria detected in the oil paste samples were different from those detected in the sea water samples; they were types related to hydrocarbon degraders, exemplified by strains closely related to Sphingomonas subarctica and Alcanivorax borkumensis . The sizes of the major bacterial populations in the oil paste samples ranged from 3.4 × 10⁵ to 1.6 × 10⁶ bacteria per gram of oil paste, these low numbers explaining the slow rate of natural attenuation.     

Microbial communities in iron-silica-rich microbial mats at deep-sea hydrothermal fields of the Southern Mariana Trough

The abundance, diversity and composition of bacterial and archaeal communities in the microbial mats at deep-sea hydrothermal fields were investigated, using culture-independent 16S rRNA and functional gene analyses combined with mineralogical analysis. Microbial mats were collected at two hydrothermal areas on the ridge of the back-arc spreading centre in the Southern Mariana Trough. Scanning electron microscope and energy dispersive X-ray spectroscopic (SEM-EDS) analyses revealed that the mats were mainly composed of amorphous silica and contained numerous filamentous structures of iron hydroxides. Direct cell counting with SYBR Green I staining showed that the prokaryotic cell densities were more than 10⁸ cells g⁻¹. Quantitative polymerase chain reaction (Q-PCR) analysis revealed that Bacteria are more abundant than Archaea in the microbial communities. Furthermore, zetaproteobacterial cells accounted for 6% and 22% of the prokaryotic cells in each mat estimated by Q-PCR with newly designed primers and TaqMan probe. Phylotypes related to iron-oxidizers, methanotrophs/methylotrophs, ammonia-oxidizers and sulfate-reducers were found in the 16S rRNA gene clone libraries constructed from each mat sample. A variety of unique archaeal 16S rRNA gene phylotypes, several pmoA , dsrAB and archaeal amoA gene phylotypes were also recovered from the microbial mats. Our results provide insights into the diversity and abundance of microbial communities within microbial mats in deep-sea hydrothermal fields.     

The planktonic and benthic bacterial populations of Lough Neagh

The planktonic and benthic bacterial populations of Lough Neagh, Northern Ireland, were studied over a one-year period. Direct counts of bacteria in the water column averaged 6 times 10⁷/ml with limited spatial or temporal variation; viable counts, however, showed a pronounced late spring maximum of 1.7 times 10⁶/ml and were consistently higher at a littoral sampling station. Direct counts of bacteria in the profundal sediments averaged 8 times 10⁹/ml whilst viable benthic counts rose steeply during spring to reach a June maximum of 1 times 10⁸/ml. Direct: viable count ratios were much greater in the more sandy littoral zone. The predominant benthic isolate was an Aeromonas sp. which was also common in samples from the water column. These results confirm the eutrophic status of Lough Neagh indicated by other biological and chemical surveys.     

甲烷及三氯乙烯驯化对垃圾填埋场覆盖土细菌群落结构的影响

对典型垃圾填埋覆盖土进行CH₄原位富集和三氯乙烯(TCE)驯化,研究了其生物氧化能力和微生物群落结构变化.覆盖土CH₄氧化速率为0.20～0.87 μmol·g^-1 soil·h^-1,TCE降解速率为0.009～0.013 mg·L^-1·h^-1,其中山东垃圾填埋场覆盖土土样甲烷氧化活性高于广东、上海和重庆地区土样.通过Illumina MiSeq测序技术分析了α多样性和驯化前后微生物菌群结构变化规律.结果表明: 在所有被注释的操作分类单元聚类结果中,细菌OTUs分配为39个门,85个纲,562个属,富集驯化后变形杆菌门、拟杆菌门、绿弯菌门和酸杆菌门仍为各土样的优势菌群,所占比例之和高于77.4%;γ-变形杆菌纲、β--变形杆菌纲、α-变形杆菌纲、放线菌纲和酸杆菌纲所占比例之和高于26.5%.嗜甲基菌属、厌氧绳菌属、节杆菌属和假单胞菌属经TCE驯化后,其相对丰度呈增加趋势.表明在覆盖土氯代烃生物降解过程中,除了被广泛认可的甲烷氧化菌异养共代谢机制以外,还存在非甲烷共代谢机制和氯代烃自养降解机制.     

Post-processing microflora and the shelf stability of gari marketed in Port Harcourt

Gari was examined for its post-processing microbial content. Aerobic mesophilic bacteria and fungi were isolated from all samples. The total viable bacterial counts ranged from 2.0 × 10² to 8.0 × 10⁴ cfu/g. Fungal counts ranged from 1.0 × 10² to 1.5 × 10⁴ cfu/g. The total viable counts of fresh samples were much lower than those of market and packaged samples. Bacillus, Micrococcus and Proteus spp. were the bacteria isolated, Aspergillus niger, Aspergillus flavus and Penicillium spp. the fungi. Food borne parasites and pathogens such as Staph. aureus and Clostridium perfringens were not found. The gari samples were quite stable, having a shelf life of 3–6 months. The water activities of the samples ranged from 0.52 to 0.68. Based on the microbial counts of the samples, the critical upper limit for the safety of gari was set at 10⁴ cfu/g dry sample.     

Rapid and sensitive detection by PCR of mpcI gene in the rhizosphere

Abstract: A simple and sensitive detection system, using polymerase chain reaction (PCR) and a soil microcosm, was developed to detect a bacterial catabolic gene in the rhizosphere. The inoculated population of Alcaligenes eutrophus JMP134, a phenol and 2,4-dichlorophenoxy acetic acid utilizer, was readily detected by this technique, which permitted taking of samples from specific locations of root (including rhizosphere) and soil. The number of JMP134 viable cells (10²–10³ cells), typically picked up by the nitrocellulose filter strip method, yielded sufficient amount of the target DNA to be detected by PCR. Primers encoding metapyrocatechase I (MPC I; catechol 2,3-dioxygenase) enabled the discrimination of at least five viable cells of JMP134 among the indigenous microorganisms inhabiting bush bean roots. This simplified PCR detection procedure facilitated monitoring of the specific degradative gene in the rhizosphere in only 5 h.     

Survival of Ralstonia solanacearum in Soil under Irrigated Rice Culture and Aquatic Weeds

The survival of Ralstonia solanacearum in naturally infested sandy loam soil under irrigated rice culture was investigated in Sankhu village (1400 m above sea level) in central Nepal. The experimental plot had a previous history of bacterial wilt and a range of 1.5 × 10⁴–3 × 10⁴ colony-forming units (CFU) per g soil was present. The survival of R. solanacearum was monitored in roots of naturally growing aquatic weeds in the rice plot and in soil before and after rice harvest. The incidence of the bacterial infection in the weeds, Dopatrium sp. and Monochoria vaginalis , were 57.5 and 10%, respectively. The bacterial population detected in soil before rice harvest was 1.5 × 10⁴ CFU per g soil whereas a range of 7.5 × 10²–1.5 × 10³ CFU per g was detected after the rice harvest. Biovar typing of R. solanacearum isolated from potato plants, potato tubers, aquatic weeds, and the soil from the experimental plot yielded the diverse biovars 2 A, 3 and 4. This is the first report of the survival of these biovars in soil, which was under continuous flow of irrigation water for 3 months during rice culture.     

The effect of procaine on the partitioning of plasmid pSC101

Abstract An examination of samples obtained from a commercial fish smoker, using seawater agar with incubation at 4°, 15° and 37°C for up to 28 days, revealed the presence of large bacterial populations in smoked fish. However, initially only low bacterial numbers, i.e., 2 × 10³/g, were present in the muscle of fresh, whole haddock ( Melanogrammus aeglefinus ). With filleting, there was a sudden increase in numbers to 9.2 × 10⁵/g. Yet immediately after smoking, the bacterial populations decreased (5 × 10⁵/g), followed by a gradual increase with storage (e.g., 2 × 10⁶/g after 24 h). Representative colonies were presumptively identified as Acinetobacter, Alcaligenes , coryneforms, Pseudomonas and Vibrio spp.     

Microbial load in poultry feed and detection of aflatoxin B1 using monoclonal antibody-based enzyme linked immunosorbent assay

Feed samples collected from different poultry farms and feed mills situated in Andaman and Nicobar islands in India were assessed for microflora and aflatoxin B₁ contamination. The bacterial counts ranged from 1.0 times 10⁷ to 8.8 times 10⁷ cfu/g of the feeds, while counts of fungi ranged from 1.0 times 10³ to 8.7 times 10³ cfu/g. The mycoflora comprised mainly of Aspergillus spp., A. flavus being most dominant. Aflatoxin B₁ was detected by monoclonal antibody-based enzyme linked immunosorbent assay technique and the content in different feed samples ranged from 5.5 to 90 ng/g.     

The distribution of some freshwater planktonic bacteria in two stratified eutrophic lakes

SUMMARY. Changes in bacterial populations and certain physical and chemical variables in Esthwaite Water between June and September 1975 were studied and compared with results obtained from 1972 to 1974 in the hypolimnia of Blelham Tarn and the Lund tubes. The counts of total bacteria ranged between 1 and 7 × 10⁶ml⁻¹ and were highest in the anoxic hypolimnion. The bacterial genera examined in more detail constituted only a small percentage of this count and included Ochrobium (10⁴ml⁻¹), Naumanniella (10³ml⁻¹), Leptothrix (10²ml⁻¹), Planctomyces (10³ml⁻¹), and Metallogenium (10²ml⁻¹). The iron bacteria appear to grow best in the oxycline where there was not only sufficient oxygen for aerobic growth but also a plentiful supply of reduced iron. Planctomyces numbers increased as the thermocline became depressed in September. The results from Blelham Tarn might be interpreted as further evidence of growth by iron bacteria in the absence of dissolved oxygen, but other explanations are possible. Examination of the results by multiple regression analysis showed that it was possible to explain a significant proportion of the bacterial variation (with the notable exception of the Planctomyces counts) in spite of considerable intercorrelation of the regressor variables.     

Influence of PCBs on the predator-prey relation between bacteria and protozoa in soil

Abstract This work deals with the impact of a possible accidental pollutant, pyralene (Prodelec, France; PCBs in trichlorobenzene), intoduced into the soil. Its influence on the predator-prey relation between bacteria and amoebae was studied by comparing the population dynamics of (i) an inoculated bacterial population ( A. lipoferum ) chosen as a biological tracer, (ii) the indigenous bacterial microflora, (iii) the infigenous amoebae. In the absence of pyralene the inoculated bacterial population decreased from 10⁷ to 10⁴ bacteria g⁻¹ soil (dw), grazed by the infigenous amoebae whose numbers increased 3-fold. In contrast, in presence of 2500 ppm of pyralene the introduced bacteria survived at a higher level (3·10⁶ bacteria g⁻¹ soil (dw)) while the number of amoebae diminished slightly. No predation occurred with PCB contamination. The indigenous bacterial microflora was not affected quantitatively by pyralene. In pure liquid culture with 500 ppm of pyralene added, bacterial growth was inhibited and an amoebal strain isolated from an inoculated uncontaminated soil was killed. We conclude that the active form of the amoebae were killed, and encystement was inhibited by pyralene in the soil. Hence the protozoa were unable to regulate the introduced A. lipoferum strain as they did in the absence of the pollutant.