The evaluation of FHB resistance QTLs introgressed into elite Canadian spring wheat germplasm

FHB resistance QTL alleles from Nyuubai, Sumai-3, and Wuhan-1 were evaluated for their effect on Fusarium head blight (FHB) index, Fusarium damaged kernels (FDK), deoxynivalenol (DON) accumulation, plant height, anthesis date, and numerous grain quality traits in three elite Canadian spring wheat backgrounds. The three FHB resistance parameters were negatively correlated with plant height in the three populations. The Wuhan-1 4B resistance allele was the most effective resistance allele but was associated with a 9.3 cm increase in plant height. The Wuhan-1 2D, Nyuubai 3BSc, Sumai-3 3BSc, Nyuubai 5AS, and Sumai-3 5AS alleles were also effective FHB resistance alleles in these populations. The Nyuubai and Sumai-3 3BS alleles were the least effective of the FHB resistance alleles in the FHB nursery tests. The Sumai-3 5AS resistance allele was significantly associated with reduced grain protein content, while the same trend was observed for the Nyuubai 5AS resistance allele but was not significant. FHB resistance tended to increase with more FHB resistance alleles introgressed into the elite genetic background, which suggested that marker-assisted selection (MAS) will prove useful for improving FHB resistance in Canadian germplasm.     

Effect of temperature on structure and function of the methanogenic archaeal community in an anoxic rice field soil.

Soil temperatures in Italian rice fields typically range between about 15 and 30 degrees C. A change in the incubation temperature of anoxic methanogenic soil slurry from 30 degrees C to 15 degrees C typically resulted in a decrease in the CH4 production rate, a decrease in the steady-state H2 partial pressure, and a transient accumulation of acetate. Previous experiments have shown that these changes were due to an alteration of the carbon and electron flow in the methanogenic degradation pathway of organic matter caused by the temperature shift (K. J. Chin and R. Conrad, FEMS Microbiol. Ecol. 18:85-102, 1995). To investigate how temperature affects the structure of the methanogenic archaeal community, total DNA was extracted from soil slurries incubated at 30 and 15 degrees C. The archaeal small-subunit (SSU) rRNA-encoding genes (rDNA) of these environmental DNA samples were amplified by PCR with an archaeal-specific primer system and used for the generation of clone libraries. Representative rDNA clones (n = 90) were characterized by terminal restriction fragment length polymorphism (T-RFLP) and sequence analysis. T-RFLP analysis produced for the clones terminally labeled fragments with a characteristic length of mostly 185, 284, or 392 bp. Sequence analysis allowed determination of the phylogenetic affiliation of the individual clones with their characteristic T-RFLP fragment lengths and showed that the archaeal community of the anoxic rice soil slurry was dominated by members of the families Methanosarcinaceae (185 bp) and Methanosaetaceae (284 bp), the kingdom Crenarchaeota (185 or 284 bp), and a novel, deeply branching lineage of the (probably methanogenic) kingdom Euryarchaeota (392 bp) that has recently been detected on rice roots (R. Grosskopf, S. Stubner, and W. Liesack, Appl. Environ. Microbiol. 64:4983-4989, 1998). The structure of the archaeal community changed when the temperature was shifted from 30 degrees C to 15 degrees C. Before the temperature shift, the clones (n = 30) retrieved from the community were dominated by Crenarchaeota (70%), "novel Euryarchaeota" (23%), and Methanosarcinacaeae (7%). Further incubation at 30 degrees C (n = 30 clones) resulted in a relative increase in members of the Methanosarcinaceae (77%), whereas further incubation at 15 degrees C (n = 30 clones) resulted in a much more diverse community consisting of 33% Methanosarcinaceae, 23% Crenarchaeota, 20% Methanosaetaceae, and 17% novel Euryarchaeota. The appearance of Methanosaetaceae at 15 degrees C was conspicuous. These results demonstrate that the structure of the archaeal community in anoxic rice field soil changed with time and incubation temperature.     

Aerobic denitrification by a newly isolated heterotrophic bacterium strain TL1

A bacterial strain which eliminates NH 3 by aerobic nitrification/heterotrophic denitrification below a pO of 30 % saturation was enriched in continuous culture from the nitrification step of a leachate-treatment plant and isolated as pure culture. The strain uses acetate, propionate, butyrate, and ethanol as carbon sources and belongs to the -subgroup of proteobacteria. Reaction parameters for deammonification and substrate utilization were determined.     

Mapping quantitative trait loci controlling agronomic traits in the spring wheat cross RL4452x'AC Domain'.

Relatively little is known about the genetic control of agronomic traits in common wheat (Triticum aestivum L.) compared with traits that follow Mendelian segregation patterns. A doubled-haploid population was generated from the cross RL4452x'AC Domain' to study the inheritance of the agronomic traits: plant height, time to maturity, lodging, grain yield, test weight, and 1000-grain weight. This cross includes the genetics of 2 western Canadian wheat marketing classes. Composite interval mapping was conducted with a microsatellite linkage map, incorporating 369 loci, and phenotypic data from multiple Manitoba environments. The plant height quantitative trait loci (QTLs), QHt.crc-4B and QHt.crc-4D, mapped to the expected locations of Rht-B1 and Rht-D1. These QTLs were responsible for most of the variation in plant height and were associated with other agronomic traits. An additional 25 agronomic QTLs were detected in the RL4452x'AC Domain' population beyond those associated with QHt.crc-4B and QHt.crc-4D. 'AC Domain' contributed 4 alleles for early maturity, including a major time to maturity QTL on 7D. RL4452 contributed 2 major alleles for increased grain yield at QYld.crc-2B and QYld.crc-4A, which are potential targets for marker-assisted selection. A key test weight QTL was detected on 3B and prominent 1000-grain weight QTLs were identified on 3D and 4A.     

Identification of major subgroups of ammonia-oxidizing bacteria in environmental samples by T-RFLP analysis of amoA PCR products

A cloning-independent method based on T-RFLP (terminal restriction fragment length polymorphism) analysis of amoA PCR products was developed to identify major subgroups of autotrophic ammonia oxidizers of the beta-subclass of the class Proteobacteria in total community DNA. Based on a database of 28 partial gene sequences encoding the active-site polypeptide of ammonia monooxygenase (amoA), defined lengths of terminal restriction fragments (= operational taxonomic units, OTUs) of amoA were predicted to correlate in TaqI-based T-RFLP analysis with phylogenetically defined subgroups of ammonia oxidizers. Members of the genus Nitrosospira showed a specific OTU of 283 bp in length, while a fragment size of 219 bp was indicative of Nitrosomonas-like sequence types including N. europaea, N. eutropha, and N. halophila. Two amoA sequence clusters designated previously as the lineages 'PluBsee' and 'Sch?hsee' [Rotthauwe, J.-H., Witzel, K.-P., Liesack, W., 1997. Appl. Environ. Microbiol. 63, 4704-4712] shared a TaqI-based OTU with a fragment size of 48 bp, but sequence types of these two lineages could be differentiated by AluI-based T-RFLP analysis. A survey of various environmental samples and enrichment cultures by T-RFLP analysis and by comparative analysis of cloned amoA sequences confirmed the predicted correlations between distinct OTUs and phylogenetic information. Our data suggest that amoA-based T-RFLP analysis is a reliable tool to rapidly assess the complexity of ammonia-oxidizing communities in environmental samples with respect to the presence of major subgroups, i.e. nitrosospiras versus nitrosomonads.     

Effect of Temperature on Structure and Function of the Methanogenic Archaeal Community in an Anoxic Rice Field Soil

Soil temperatures in Italian rice fields typically range between about 15 and 30°C. A change in the incubation temperature of anoxic methanogenic soil slurry from 30°C to 15°C typically resulted in a decrease in the CH₄ production rate, a decrease in the steady-state H₂ partial pressure, and a transient accumulation of acetate. Previous experiments have shown that these changes were due to an alteration of the carbon and electron flow in the methanogenic degradation pathway of organic matter caused by the temperature shift (K. J. Chin and R. Conrad, FEMS Microbiol. Ecol. 18:85–102, 1995). To investigate how temperature affects the structure of the methanogenic archaeal community, total DNA was extracted from soil slurries incubated at 30 and 15°C. The archaeal small-subunit (SSU) rRNA-encoding genes (rDNA) of these environmental DNA samples were amplified by PCR with an archaeal-specific primer system and used for the generation of clone libraries. Representative rDNA clones (n = 90) were characterized by terminal restriction fragment length polymorphism (T-RFLP) and sequence analysis. T-RFLP analysis produced for the clones terminally labeled fragments with a characteristic length of mostly 185, 284, or 392 bp. Sequence analysis allowed determination of the phylogenetic affiliation of the individual clones with their characteristic T-RFLP fragment lengths and showed that the archaeal community of the anoxic rice soil slurry was dominated by members of the families Methanosarcinaceae (185 bp) and Methanosaetaceae (284 bp), the kingdom Crenarchaeota (185 or 284 bp), and a novel, deeply branching lineage of the (probably methanogenic) kingdom Euryarchaeota (392 bp) that has recently been detected on rice roots (R. Großkopf, S. Stubner, and W. Liesack, Appl. Environ. Microbiol. 64:4983–4989, 1998). The structure of the archaeal community changed when the temperature was shifted from 30°C to 15°C. Before the temperature shift, the clones (n = 30) retrieved from the community were dominated by Crenarchaeota (70%), “novel Euryarchaeota” (23%), and Methanosarcinacaeae (7%). Further incubation at 30°C (n = 30 clones) resulted in a relative increase in members of the Methanosarcinaceae (77%), whereas further incubation at 15°C (n = 30 clones) resulted in a much more diverse community consisting of 33% Methanosarcinaceae, 23% Crenarchaeota, 20% Methanosaetaceae, and 17% novel Euryarchaeota. The appearance of Methanosaetaceae at 15°C was conspicuous. These results demonstrate that the structure of the archaeal community in anoxic rice field soil changed with time and incubation temperature.     

Novel bacterial lineages at the (sub)division level as detected by signature nucleotide-targeted recovery of 16S rRNA genes from bulk soil and rice roots of flooded rice microcosms

Using a newly developed 16S rRNA gene (rDNA)-targeted PCR assay with proposed group specificity for planctomycetes, we examined anoxic bulk soil of flooded rice microcosms for the presence of novel planctomycete-like diversity. For comparison, oxic rice roots were included as an additional sample in this investigation. The bacterial diversity detectable by this PCR assay was assessed by using a combined approach that included terminal restriction fragment length polymorphism (T-RFLP) analysis and comparative sequence analysis of cloned 16S rDNA. T-RFLP fingerprint patterns generated from rice roots contained 12 distinct terminal restriction fragments (T-RFs). In contrast, the T-RFLP fingerprint patterns obtained from the anoxic bulk soil contained 33 distinct T-RFs, a clearly higher level of complexity. A survey of 176 bulk soil 16S rDNA clone sequences permitted correlation of 20 T-RFs with phylogenetic information. The other 13 T-RFs remained unidentified. The predominant T-RFs obtained from rice roots could be assigned to members of the genus Pirellula within the Planctomycetales, while most of the T-RFs obtained from the bulk soil corresponded to novel lines of bacterial descent. Using a level of 16S rDNA sequence dissimilarity to cultured microorganisms of approximately 20% as a threshold value, we detected 11 distinct bacterial lineages for which pure-culture representatives are not known. Four of these lineages could be assigned to the order Planctomycetales, while one lineage was affiliated with the division Verrucomicrobia and one lineage was affiliated with the spirochetes. The other five lineages either could not be assigned to any of the main lines of bacterial descent or clearly expanded the known diversity of division level lineages WS3 and OP3. Our results indicate the presence of bacterial diversity at a subdivision and/or division level that has not been detected previously by the so-called universal 16S rDNA PCR assays.     

Structure and function of the methanogenic archaeal community in stable cellulose-degrading enrichment cultures at two different temperatures (15 and 30 degrees C)

Methanogenic cultures were enriched from an air-dried rice field soil and incubated under anaerobic conditions at 30 degrees C with cellulose as substrate (ET1). The culture was then transferred and further incubated at either 15 degrees C (E15) or 30 degrees C (E30), to establish stable cultures that methanogenically degrade cellulose. After five transfers, the rates of CH(4) production became reproducible. At 30 degrees C, CH(4) production rates were (mean+/-S.D.) 15.2+/-0.7 nmol h(-1) ml(-1) culture for the next 16 transfers and at 15 degrees C, they were 0.38+/-0.07 nmol h(-1) ml(-1) for the next six transfers. When E30 was assayed at temperatures between 5-50 degrees C, CH(4) production rates increased with the temperature, reached a maximum at 40 degrees C and then decreased. The same temperature optimum was observed in E15, but with a lower maximum CH(4) production rate. The apparent activation energies of CH(4) production were similar (about 120 kJ mol(-1)4 mM at the beginning of the assay. The structure of the archaeal community was analyzed by molecular techniques. Total DNA was extracted from the microbial cultures before the transfer to different temperatures (ET1) and afterwards (E15, E30). The archaeal small subunit (SSU) ribosomal RNA-encoding genes (rDNA) of these DNA samples were amplified by PCR with archaeal-specific primers and characterized by terminal restriction fragment length polymorphism (T-RFLP). After obtaining a constant T-RFLP pattern in the cultural transfers at 15 and 30 degrees C, the PCR amplicons were used for the generation of clone libraries. Representative rDNA clones (n=10 for each type of culture) were characterized by T-RFLP and sequence analysis. In the primary culture (ET1), the archaeal community was dominated by clones representing 'rice cluster I', a novel lineage of methanogenic Euryarchaeota. However, further transfers resulted in the dominance of Methanosarcinaceae and Methanosaetaceae at 30 and 15 degrees C, respectively. This dominance was confirmed by fluorescence in situ hybridization (FISH) of archaeal cells. Obviously, different archaeal communities were established at the two different temperatures, but their activities nevertheless exhibited similar temperature optima.     

Development of genetically modified wheat to assess its dough functional properties

End-use functionality of bread wheat depends mainly on the protein content, the presence of particular subunits of high and low molecular weight glutenin, the ratio of high molecular weight to low molecular weight glutenin subunits, and the ratio of glutenin to gliadin. The exact contribution of each of these factors to end-use functionality is still largely unknown. Transgenic plants can allow these factors to be studied within a particular background thus contributing to our understanding of end-use functionality. Two Canadian wheat lines, one of them containing high molecular weight glutenin subunits (HMW-GS) coded by all three Glu-1 loci and one line null at all three loci were assessed for dough rheological properties and bread and tortilla-making properties. Protein composition of the flours were characterized by sodium dodecyl sulfate polyacrylamide gel electrophoresis, size exclusion high performance liquid chromatography, and sedimentation test. Proteins in the samples were fractionated and the proportions of monomeric proteins, soluble glutenin, and insoluble glutenin were quantified. Functionality of the flours were characterized by small-scale methods such as the 2 g mixograph, 10 g farinograph, and micro-extension testing. End-use quality was evaluated by small-scale bread and tortilla production. Mixograph development time and mixograph peak height were much higher for the lines containing HMW-GS. The lines null for HMW-GS showed no resistance to extension. Lines null for HMW-GS produced 'brick'-like bread. Tortilla prepared from the null lines had poor rollability and lower puncture force. The results showed very strong dependencies of quality on the presence of HMW-GS.     

Novel Bacterial Lineages at the (Sub)Division Level as Detected by Signature Nucleotide-Targeted Recovery of 16S rRNA Genes from Bulk Soil and Rice Roots of Flooded Rice Microcosms

Using a newly developed 16S rRNA gene (rDNA)-targeted PCR assay with proposed group specificity for planctomycetes, we examined anoxic bulk soil of flooded rice microcosms for the presence of novel planctomycete-like diversity. For comparison, oxic rice roots were included as an additional sample in this investigation. The bacterial diversity detectable by this PCR assay was assessed by using a combined approach that included terminal restriction fragment length polymorphism (T-RFLP) analysis and comparative sequence analysis of cloned 16S rDNA. T-RFLP fingerprint patterns generated from rice roots contained 12 distinct terminal restriction fragments (T-RFs). In contrast, the T-RFLP fingerprint patterns obtained from the anoxic bulk soil contained 33 distinct T-RFs, a clearly higher level of complexity. A survey of 176 bulk soil 16S rDNA clone sequences permitted correlation of 20 T-RFs with phylogenetic information. The other 13 T-RFs remained unidentified. The predominant T-RFs obtained from rice roots could be assigned to members of the genus Pirellula within the Planctomycetales, while most of the T-RFs obtained from the bulk soil corresponded to novel lines of bacterial descent. Using a level of 16S rDNA sequence dissimilarity to cultured microorganisms of approximately 20% as a threshold value, we detected 11 distinct bacterial lineages for which pure-culture representatives are not known. Four of these lineages could be assigned to the order Planctomycetales, while one lineage was affiliated with the division Verrucomicrobia and one lineage was affiliated with the spirochetes. The other five lineages either could not be assigned to any of the main lines of bacterial descent or clearly expanded the known diversity of division level lineages WS3 and OP3. Our results indicate the presence of bacterial diversity at a subdivision and/or division level that has not been detected previously by the so-called universal 16S rDNA PCR assays.