Viruses have been shown to be responsible for considerable bacterial mortality and nutrient cycling in aquatic systems. As yet no detailed studies have been published on the role of viruses in natural soil bacterial communities despite common knowledge that viruses exist in the soil. This thesis sought to address some key questions on the ecology of soil bacterial viruses and their hosts. Disturbance through soil desiccation, nutrient inputs, rhizosphere effects and protozoan predation pressure were investigated. The first study of lysogeny in natural soil systems was also undertaken. The work presented here utilised tools and techniques commonplace in aquatic systems research and applied them to soil. A novel protocol was developed based on physical extraction of bacteria and viruses from soil and direct counting with epifluorescence microscopy. Physical extraction was achieved using shaking, ultrasound sonication and low speed centrifugation. The fluorochrome SYBR Gold was used to stain nucleic acid of extracted bacteria and viruses, and image analysis software used to determine bacterial cell volumes. Bacterial and viral abundances were in the region of 107-109 per gram of soil over a range of soil types. Significant fluctuations in viral and bacterial abundances were recorded at timescales of less than 24 h. Glucose and nitrogen addition led to substantial increases in bacterial and viral abundance. Loss of soil moisture resulted in peaks of viral abundance in sandy soils but not in a clay soil. A six-week microcosm study demonstrated that phage were not a significant regulator of bacterial abundance. Low levels of lysogeny were recorded over a range of soils when measured explicitly with Mitomycin C. The implication from that study was that viruses in soil behave differently to those in aquatic systems. Bacterial and viral abundances were highly coupled in most instances, irrespective of the potential activity of bacteria. Further fundamental studies are recommended.

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Stable carbon isotope fractionation during methanogenesis is affected by the availability of substrates. The effects of different substrates on methanogen biomass, total lipid extract, biomarkers and methane under both abundant and limiting substrate conditions were studied. Methanosarcina barkeri was grown with methanol, acetate, trimethylamine (TMA) and H2/CO2, and carbon isotope fractionation in methane production was greatest with methanol, followed by H2/CO2, TMA and acetate. In contrast, biomass was isotopically lightest in M.barkeri grown on methanol, followed by TMA, H2/CO2 and acetate. Generally, fractionation was greater in cultures grown with abundant substrate availability as compared to those supplied with limiting substrate. During autotrophic growth, fractionation was greatest during slower growth for both methane and biomass production. The results of these fractionation studies under controlled laboratory conditions can be applied to the interpretation of isotopic signatures for methane and methanogen biomarkers, and ecological processes, in marine environments. Several hypersaline springs off the western shore of Lake Winnipegosis, MB support unique microbial mat communities. These low temperature springs contain water with a mean salinity as high as 6.1%. Studies were undertaken to contrast the anaerobic microbial communities of these springs, specifically the methanogens and sulphate-reducing bacteria (SRB), and their contributions to biogeochemical cycling in these mats. Comparisons of lipid profiles revealed changes in the proportions of the dominant fatty acids related to the amount of mat growth. Cultures of SRB and methanogens were established with six different substrates. Methanogenic cultures grew best on TMA and methanol, but could use formate, H2/CO2 and glycine betaine as well. In contrast, H2/CO2 was the preferred substrate of the SRB enrichment cultures, which were also able to use formate, but not TMA, the breakdown product of the compatible solute glycine betaine. Maximum methane production occurred at 5% salinity. The lipid composition of the mats, including methanogen biomarkers, and the results of the enrichments on different substrates and at different salinities, suggest that methanogenesis in these springs is supported by compatible solutes whereas sulphate reduction is linked to availability of hydrogen and formate.

Thesis (Ph. D.)--University of Hawaii at Manoa, 1995. / Includes bibliographical references (leaves 215-245). / Microfiche. / xii, 245 leaves, bound ill. (some col.) 29 cm

Wetlands account for approximately 20% of annual global methane emissions. Many wetlands receive inputs of organic matter, nutrients, metals and various toxic compounds from adjacent agricultural and industrial areas. The present study aimed to investigate the microbial composition of a natural methanogenic consortium. A consortium-based molecular approach to study diversity of methanogenic microbial communities in a natural wetland at the primary inflow was used. Key microorganisms of a nethane producing consortium were identified. Extracted high molecular mss DNA ws analysed by PCR combined with denaturing gradient gel electrophoresis and subsequent sequencing of 16S rDNA. This study was also aimed to identify syntrophic microorganisms in the wetland system. The data obtained suggest a well established syntrophic relationship within the wetland.

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Erratum pasted inside back end paper. / Bibliography: leaves 174-201. / xvii, 202, [77] leaves, [8] leaves of plates : ill. (chiefly col.) ; 30 cm. / Title page, contents and abstract only. The complete thesis in print form is available from the University Library. / Establishes that the herbicide carbetamide degrades rapidly upon repeated application to soil, when compared to a previously untreated soil. / Thesis (Ph.D.)--University of Adelaide, Dept. of Crop Protection, 1997

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