Morphological analysis of viral communities in the floodwater of a Japanese paddy field

Capsid size distributions of viral communities in the floodwater of a Japanese paddy field under a long-term fertilizer trial were surveyed during the rice cultivation period by using transmission electron microscopy. The capsid size distributions were monophasic, and the median values fell within the range of 50-70 nm. The quartile intervals were narrow from either 40-50 nm or 50-60 nm to either 60-70 nm or 70-80 nm for most samples. There was no clear seasonal variation in the capsid size distribution of viral communities. The difference in size distributions among different fertilizer plots was also not found. Viral communities in the floodwater were predominated by isometric icosahedral forms. Viruses with octahedral capsids and elongated ones were rare and sporadic in the floodwater.     

The distribution characteristics of the major capsid gene (g23) of T4-type phages in paddy floodwater in Northeast China

Our previous study revealed the high diversity of the major capsid gene (g23) of T4-type phages that existed in the paddy field soils in Northeast China. In this study, the phylogeny and genetic diversity of the g23 gene in the paddy floodwater samples collected from five sampling sites at three sampling times during the rice (Oryza sativa L.) growth season in Northeast China are reported. In total, 104 different g23 clones were isolated, among which 50% of the clones exhibited the highest identities with the clones retrieved in paddy soils and upland black soils. The remaining clones had the highest identities with lake origins. Phylogenetic analysis revealed that 43% of the g23 clones grouped into three novel subgroups which included the clones unique to paddy floodwater, and no g23 sequences obtained in paddy floodwater fell into the paddy soil groups II, III, IV, V, VI, VII and NPC-A. UniFrac analysis of g23 clone assemblages demonstrated that T4-type phage communities in paddy floodwater were changed spatially and temporally, and the communities were different from those in paddy soils. Further comparison of the g23 clone assemblages from different environments demonstrated that T4-type phages were biogeographically distributed, and the distribution was both affected by geographical separation and ecological processes across the biomes.     

Frequency of phage-infected bacterial cells in the floodwater of a Japanese paddy field

In aquatic environments, viruses play an important role in the microbial food web through microbial mortality from viral lysis. Bacteriophages (phages) compose the majority of viral communities in the floodwater of paddy fields. The present study evaluated bacterial mortality from phage lysis in the floodwater of a Japanese paddy field based on the frequency of phage-infected bacterial cells by transmission electron microscopy. Floodwater was sampled five times during the rice cultivation period from two plots of NPK plus lime (no-compost plot) and NPK plus lime and compost (compost plot) under a long-term and ongoing fertilizer trial that began in 1925. The frequency of visibly infected cells in the compost plot was larger, ranging from 2.4 to 3.6% (average 3.0%), than that in the no-compost plot, which ranged from 1.6 to 2.9% (average 2.0%). The fractions of bacterial mortality from phage lysis in the floodwater samples were estimated to range from 12.8 to 27.3% (average 17.2%) and from 21.7 to 35.0% (average 27.9%) for the samples collected from the no-compost plot and the compost plot, respectively. This is the first study to estimate bacterial mortality from phage lysis in the paddy field ecosystem, and the frequency of phage lysis in floodwater was found to be within the frequency ranges observed in other aquatic environments.     

Seasonal variations in the abundance of virus-like particles and bacteria in the floodwater of a Japanese paddy field

Abstract

Viruses are the most abundant biological entities in marine and freshwater environments. Many studies have shown the ecological importance of viruses in the primary production and microbial food web in aquatic environments. However, no studies have examined viral abundance in the floodwater of paddy fields. The present study surveyed the abundance of virus-like particles (VLPs) and bacteria in the floodwater of a Japanese paddy field under a long-term fertilizer trial since 1925 during the rice cultivation period. Virus-like particles and bacterial abundances in the floodwater ranged from 5.6 × 10⁶ to 1.2 × 10⁹ VLPs mL^?1 and from 9.2 × 10⁵ to 4.3 × 10⁸ cells mL^?1 with mean abundances of 1.5 × 10⁸ VLPs mL^?1 and 5.1 × 10⁷ cells mL^?1, respectively, and increased with an increase in the turbidity of the floodwater with suspended particles. The magnitude of seasonal variation was more than 50-fold for VLP abundance and 100-fold for bacterial abundance. The virus-to-bacterium ratios fluctuated over the rice cultivation period, ranging from 0.11 to 72 and their increase correlated with the decrease in bacterial abundance. Our results suggest that viral abundance in the floodwater of paddy fields is larger than in natural marine and freshwater environments.     

Morphology, host range and phylogenetic diversity of Sphingomonas phages in the floodwater of a Japanese paddy field

Members of the Sphingomonas -related genera ( Sphingomonas , Sphingobium , Novosphingobium and Sphingopyxis ) are dominant in bacterial isolates from the floodwater of Japanese paddy fields. Fifty-eight Sphingomonas / Novosphingobium bacteriophages (phages) were isolated to elucidate their morphology, host range and phylogenetic diversity based on the capsid gene ( g23 ) sequence. All of the phages were siphoviruses with isometric or elongated, icosahedral capsids and a long, non-contractile tail. The genomes were double-stranded DNA measuring either 40, 60, 100 or 160 kb. The host range of the phages was examined by infecting 16 bacterial isolates from the floodwater, belonging to Sphingomonas , Novosphingobium , Sphingopyxis and Porphyrobacter . The host range was widely different and varied between infection of only the host used for isolation and infection of hosts belonging to the three genera of Sphingomonas , Novosphingobium and Porphyrobacter . All phages had g23 , indicating the ubiquity of the g23 gene among Myoviridae and Siphoviridae members. Every g23 sequence of the phages belonged to one of the six uncharacterized Paddy Groups proposed by Fujii et al . (2008 ). The g23 sequences were identical at the nucleotide level for several phages with isometric and elongated capsids with 60 and 160 kb genomes, and between some phages and the clones that were retrieved from distant paddy fields. This indicates the common occurrence of horizontal transfer of g23 in the paddy fields. The g23 sequence does not correlate with the host range of those phages. In addition, a larger degree of divergence of g23 from coliphage T4 in paddy fields compared to marine environments was estimated from the present study.     

Novel capsid genes (g23) of T4-type bacteriophages in a Japanese paddy field

Viruses exist everywhere on the planet. Recent development in viral genomics confirmed that genomic information is preserved among viral subsets and can be used for phylogenetic classification of viruses and for evaluation of viral diversity in the environment. The capsid gene of T4-type bacteriophages, g23, is the most widely applied gene for evaluating the diversity of the T4-type bacteriophage family. In this study, we applied denaturing gradient gel electrophoresis to PCR products of DNA with g23-specific primers that were extracted from a Japanese paddy field under long-term fertilizer trial and obtained 39 different g23 clones at the DNA level. They showed identities of 27–99% with the clones within the NCBI database at the amino acid level. They were quite distinctive from those obtained in marine environments and most of them formed six phylogenetically novel groups in the T4-type bacteriophage family with the clones obtained from another paddy field. The existence of six novel groups was confirmed from molecular analysis of all the amino acid sequences between the primers, of the amino acid sequences excluding hypervariable region, and of those of conserved regions. These findings indicate that T4-type bacteriophage communities in paddy fields consist of previously uncharacterized members phylogenetically distant from those in marine environments. The type of fertilizers and the stage during rice cultivation were not the major factors in determining T4-type bacteriophage communities in the paddy field.     

T4-type bacteriophage communities estimated from the major capsid genes (g23) in manganese nodules in Japanese paddy fields

The present study compared the capsid gene ( g23 ) of T4-type bacteriophages (phages) in Mn nodules with those in the plow layer soil and subsoils of two Japanese paddy fields by applying the primers MZIA1bis and MZIA6 to DNA extracts from the nodules and soils. The deduced amino acid sequences of the g23 genes in the Mn nodules were similar to those in the plow layer soil and in the subsoils. This result indicated that similar T4-type phage communities developed at these sites and that the diversity of T4-type phage communities was wide enough to cover those in the plow layer soil and in the subsoils. The majority of g23 clones formed several clusters with the clones and phages obtained from far-apart paddy fields, and the sequences of two clones were completely identical to a phage and a clone from other paddy fields at the nucleotide or amino acid level, indicating horizontal transfer of g23 genes between those paddy fields. A clone with a long nucleotide residue (686 bp) and a distribution remote from the other clones in the phylogenetic tree indicated that there were many uncharacterized, novel g23 genes in the paddy fields.     

Survey of major capsid genes (g23) of T4-type bacteriophages in Japanese paddy field soils

Many studies have shown the ecological importance of viruses as the greatest genomic reservoirs on the planet. As bacteriophages (phages) comprise the majority of viruses in the environment, we surveyed the capsid genes (g23) of T4-type phages, Myoviridae, from DNA extracts of three paddy field soils located in northern, central and southern Japan using the degenerate primers MZIA1bis and MZIA6. Denaturing gradient gel electrophoresis (DGGE) was performed to separate PCR-amplified g23 products, and 56 DGGE bands were identified as g23 fragments. Only nine clones were grouped into T-evens, PseudoT-evens and ExoT-evens, and most of the other clones were classified into Paddy Groups I-VI. No significantly different distribution of g23 clones was observed among the paddy fields at the group level, indicating that phage communities estimated from the g23 composition were common on the nationwide level. Comparison of g23 sequences showed that g23 genes in paddy fields were different from those in marine environments, and more divergence of g23 genes was estimated in the paddy fields compared to the marine environment. Two novel g23 clones with very short amino acid residues were detected, suggesting the existence of uncharacterized, novel groups of g23 genes in paddy field soils.     

Comparison of g23 gene sequence diversity between Novosphingobium and Sphingomonas phages and phage communities in the floodwater of a Japanese paddy field

Our previous study indicated that the diversity of the major capsid gene (g23) of T4-type bacteriophages (phages) of Novosphingobium and Sphingomonas strains isolated from the floodwater of a Japanese paddy field is comparable to those of the clones obtained from other Japanese paddy fields. For more strict comparison of the diversity, this study examined g23 sequences between Novosphingobium and Sphingomonas phages and phage communities in the identical floodwater of a Japanese paddy field. The clones were obtained by applying g23-specific primers to DNA extracted from the floodwaters. Many 23 clones in the floodwater were grouped into the same clusters of Paddy Groups I-VI with g23 genes of Novosphingobium/Sphingomonas phages with some clones belonging to an additional cluster. In addition, the remaining clones belonged to the clusters of marine clones and T4-type enterophages. These findings indicate that the g23 genes in the floodwater are more diversified than those of Novosphingobium/Sphingomonas phages including g23 genes closely related to the genes of enterophages and marine origins.     

Phylogenetic study on a bacterial community in the floodwater of a Japanese paddy field estimated by sequencing 16S rDNA fragments after denaturing gradient gel electrophoresis

Phylogenetic positions of characteristic bands of 16S rDNA that were obtained from the floodwater of a Japanese paddy field by denaturing gradient gel electrophoresis (DGGE) analysis in a previous work (Biol Fertil Soils 36:306–312, 2002) were determined to identify dominant bacterial members in the floodwater. Sequences of DGGE bands were affiliated with the Cytophaga–Flavobacterium–Bacteroides group, β-Proteobacteria, and Actinobacteria and showed phylogenetically close relationships with species inhabiting other aquatic environments, although most of their closest relatives were uncultured bacterial clones.     

Community structure of the microbiota in the floodwater of a Japanese paddy field estimated by restriction fragment length polymorphism and denaturing gradient gel electrophoresis pattern analyses

The polymerase chain reaction-restriction fragment length polymorphism (PCR-RFLP) and PCR-denaturing gradient gel electrophoresis (DGGE) patterns of 16S rDNA were studied to elucidate the effects of the type of fertilization and the growth stage of rice plants on the community structure of the microbiota in the floodwater of a Japanese paddy field under a long-term fertilizer trial. From the mid tillering stage, a higher pH and temperature were observed in the plot without fertilization (NoF plot) than in the plots supplied with chemical fertilizers (CF plot) and with compost (CM plot). DNA fragments specific to the respective plots and common to every plot were detected after the digestion of PCR products by restriction enzymes. Cluster analysis separated the RFLP and DGGE patterns of the microbiota in the floodwater into four clusters; the microbiota in (1) the NoF plot, (2) the CF plot, (3) the CM plot, and (4) the CF and CM plots in the early growing stage. The effect of fertilizer application on the community structure was more conspicuous than that of seasonal variation.     

Comparison of phospholipid fatty acid composition in percolating water,floodwater, and the plow layer soil during the rice cultivation period in a Japanese paddy field

Azolla has been used as a green manure for rice in Vietnam and southern China (3). Recently it was adopted by farmers in the Koronadal area in South Cotabato Province, the Philippines (2). In that area Azolla pinnata grows reasonably well without phosphate fertilizer, which is generally used for stimulating Azolla growth (3, 5).     

Characterization of ammonia oxidizing bacteria associated with weeds in a Japanese paddy field using amoA gene fragments

Abstract

Ammonia oxidizing bacteria (AOB) are important microorganisms in rice paddy field ecosystems because they play a key role in the nitrogen (N) cycle by converting ammonia (NH₃) to nitrite (NO^? ₂). In this study, we investigated AOB associated with three types of weeds in a Japanese paddy field (semi-aquatic Echinochloa oryzicola Vasing, floating Lemna paucicostata Hegelm and submerged Najas graminea Delile) using molecular techniques polymerase chain reaction-denaturing gradient gel electrophoresis (PCR-DGGE) and DNA sequencing targeting ammonia monooxygenase (amoA) gene. This work confirmed that rice paddy weeds harbor AOB and that the community composition is different for each type of weed. However, all AOB sequences associated with the tested weeds were closely related to known species of Nitrosospira-like AOB isolated from soil, suggesting that AOB associated with weeds were not specific to weeds and can also be found in the soil. Nitosomanas-like AOB were not detected on any of the weeds tested. In addition, the most dominant AOB strains present in the tested weeds were closely related to Nitrosospira sp. Ka3 and Nitrosospira sp. CT2F. The phylogenetic tree revealed that most of the AOB detected in the present study belonged to amoA cluster 1.     

Community structure of microaerophilic iron-oxidizing bacteria in Japanese paddy field soils

ABSTRACT

Redox cycle of iron (Fe) is the central process in the biogeochemistry of paddy field soil. Although Fe(II)-oxidizing process is mediated by both abiotic and biotic reactions, microorganisms involved in the process have not been well studied in paddy field soil. The present study investigated the community structure of microaerophilic Fe(II)-oxidizing bacteria (FeOB) in the family Gallionellaceae in the plow layer of paddy fields located in the central (Anjo) and northeastern (Omagari) Japan since the members in the family are the typical FeOB in circumneutral freshwater environments and possibly have the significant role for Fe(II) oxidation in paddy field soils. A primer set targeting 16S rRNA gene of Gallionella-related FeOB was newly designed for the polymerase chain reaction-denaturing gradient gel electrophoresis (PCR-DGGE) and quantitative PCR (qPCR) analyses. DGGE analysis showed significant differences in the band patterns between the field sites. Besides, minor differences were observed in the patterns between the soil depths (0–1 cm and below 1 cm) in the Anjo field, while the patterns were relatively stable in the Omagari field during the annual rice cultivation practices. In total 54 bands were sequenced and clustered into 20 operational taxonomic units (OTUs) on the basis of the 97% similarity. Eighteen out of twenty OTUs (50 of 54 bands) were affiliated within the FeOB cluster of Gallionellaceae, some of which were clustered with known microaerophilic FeOB, Ferrigenium kumadai, Ferriphaselus amnicola, ‘Sideroxydans lithotrophicus’ and ‘S. paludicola’. The number of the 16S rRNA gene copies was 10⁵–10⁷ and 10⁶–10⁸ copies g^?1 dried soil in the two paddy fields and negatively correlated to the contents of acetate-extractable Fe(II) in the soils during the rice cultivation period. These results suggested inhabitance of considerable number of diverse Gallionella-related FeOB and their potential involvement in the Fe(II)-oxidizing process of soil, especially during the rice cultivation period in the paddy field soils.     

Dynamics of dissolved oxygen (DO) in ponded water of a paddy field

The transfer of heat and dissolved oxygen (DO) through water is important to understand the phenomenon of ponded water in a paddy soil. The heat from solar radiation is absorbed at the soil surface and transferred into the ponded water by convection. This study clarified the dynamics of DO, as well as the role of convection in water in DO transfer in the ponded water of a paddy field. DO concentration in the ponded water of a paddy field was measured in situ in the daytime and during the night. The results were confirmed in lab-scale model experiments. The DO concentration and temperature profiles in the ponded water of a lab-scale paddy field model were investigated under convective and non-convective conditions using solar radiation and infrared radiation, respectively. Under the ponded condition, solar radiation was absorbed at the soil surface whereas infrared radiation was absorbed at the water surface and thereby convective and non-convective conditions were generated, respectively. The diurnal variation in DO concentration was closely related to the intensity of solar radiation. Oxygen generation by micro-algae and its subsequent circulation by convection resulted in uniform DO concentration profiles, with super-saturated values in the ponded water in the daytime. Eventually oxygen was released to the atmosphere by deaeration until DO in water was depleted to the saturated level. During the night the oxygen moved from the atmosphere into the water surface by reaeration which depends on the oxygen deficit related to saturation. The oxygen deficit is caused by the respiration of microorganisms. The oxygen, that moved from the atmosphere to the water surface, was transferred to the soil surface by convection in the water layer. Thus convection plays an important role in the DO transfer in the ponded water of a paddy field. The DO dynamics is correlated with biological processes in the ponded paddy soil.