Determination of substrate utilization patterns of soil microbial communities: An approach to assess population changes after hydrocarbon pollution

Abstract: Changes in hydrocarbon content in soils resulted in characteristic shifts of the substrate utilization patterns as tested with the Biolog system. The altered patterns of substrate utilization corresponded to similar changes in abundance of hydrocarbon-utilizing bacteria and the occurrence of specific bacterial groups in the soils. Substrate utilization patterns as recorded with the Biolog system are suitable for rapidly assessing dynamics of autochthonous soil communities and evaluating their biodegradative potential.     

Microbial mineralization of organic phosphate in soil

Summary Phosphate-dissolving microorganisms were isolated from non-rhizosphere and rhizosphere of plants. These isolates included bacteria, fungi and actinomycetes. In broth cultures, Gram-negative short rod,Bacillus andStreptomyces species were found to be more active in solubilizing phosphate thanAspergillus, Penicillium, Proteus, Serratia, Pseudomonas andMicrococcus spp. The sterile soils mixed with isolated pure culture showed slower mineralization of organic phosphate than that of non-sterile soil samples at all incubation periods. Maximum amount of phosphate mineralization by isolated microorganisms were obtained at the 60th and the 75th day of incubation in sterile and non-sterile soils respectively. The mixed cultures were most effective in mineralizing organic phosphate and individuallyBacillus sp. could be ranked next to mixed cultures. Species ofPseudomonas andMicrococcus were almost the same as that of the control under both sterile and non-sterile conditions.     

Dynamics of soil microbial biomass N under zero and shallow tillage for spring wheat,using15N urea

Summary Field studies to determine the effect of zero and shallow (10 cm) cultivation on microbial biomass were conducted on several Chernozemic soils in western Canada. Using the CHCl₃ fumigation method, the distribution of microbial biomass N and the immobilization and subsequent release of added¹⁵N (¹⁵N-urea) from the microbial biomass were determined in the A horizon, at the 0 to 5 and 5 to 10 cm depth, during the growing season for spring wheat.Temporal variation in microbial biomass N, associated with the development of the rhizosphere, was characterized by an increase between Feekes stage 1 and 5 or 10 and decrease at Feekes stage 11.4. Over the long term, the variation in biomass N between tillage systems corresponded with crop residue distribution. Immobilization of fertilizer N was related to the increase in biomass N from Feekes stage 1, which in turn, was associated with the incorporation of recent crop residues or levels of labile organic matter in the surface soil. The study demonstrated the relatively rapid remineralization of immobilized fertilizer N under field conditions and emphasized the role of the microbial biomass N as both a sink and source of mineral N.     

The biological transformation of P in soil

Summary Organic forms of soil phosphorus (P_o) are an important source of available P for plants following mineralisation. The rates and pathways of P through soil organic matter are, however, poorly understood when compared to physco-chemical aspects of the P cycle. The essential role of soil microorganisms as a labile resercoir of P, confirmed experimentally and in modelling studies, has recently led to the development of methods for measuring thier P content. Incorporation in a new P fractionation scheme of these measurements with estimates of P_i and P_o fractions that vary in the exten toftheir availability to plants has enabled the dynamics of short-term soil P transformations to be investigated in relation to long-term changes observed in the field.Different types of soil P compounds that minearlise at different rates can now be measured directly in extracts by³¹P-nuclear magnetic resonance. Orthophosphate diesters, including phospholipids and nucleic acids, are the most readily mineralised group of these compounds. However, mineralisation rates rather than the amounts of types of P_o in soil ultimately control P availability to plants. These rates are influenced by a number of soil and site factors, as a sensitive new technique using [³²P] RNA has recently shown.These recent developments reflect a more holistic approach to investigation of the soil P cycle than in the past, which should lead to improved fertilizer management practices.Introductory lecture     

Effect of topsoil storage on microbial activity,primary production and decomposition potential

Summary The effects of disturbing (cultivating) and stockpiling prairie grassland topsoil on microbial activity, microbial biomass C, plant production and decomposition potentials were studied by measuring CO₂ efflux from unamended and glucose amended soil in the laboratory and by conducting a pot and litter bag study in the greenhouse. Stockpiling appeared to have very little effect on soil respiratory activity, but did reduce the microbial biomass C levels. Throughout the 3 year study the microbial biomass C in the surface soil of the stockpile was less than that in the undisturbed soil, while the biomass C in soil at the bottom of the stockpile was at no time significantly different from that in the undisturbed soil. The reduction in microbial biomass C in the surface soil immediately after stockpiling was attributed to a decrease in the soil organic C levels caused by a slight dilution of the topsoil with subsurface mineral soil, and the exposure of the stockpile surface to extreme environmental conditions. Soils from all depths of the stockpile responded more slowly to the addition of glucose than soil from the undisturbed and cultivated treatments even when no differences in biomass were detected between the undisturbed and stockpiled soils. It is postulated that the rapidity with which the soil microbial biomass responds to glucose additions may be a sensitive indicator of stress on the soil biological components. The reduction in biomass after storage for 1 year had no adverse effects on the decomposition or primary production potential of the stored soil. Rather, shoot production by fall rye was stimulated in the stored topsoil, presumably a result of better N nutrition.     

Antagonistic effects of soil bacteria onFusarium oxysporum Schlecht f.sp.dianthii (Prill and Del.) Snyd. and Hans.

Summary Thirty two bacteria antagonistic to a number of phytopathogenic fungi were isolated from soil samples. One bacterial strain, designated as M 51, appeared to be particularly active towardsF. oxysporum f. sp.dianthii, in vitro andin vivo and it was inhibitoryin vitro to three otherFusarium spp. used. Tests to find if there was protection against fusarium wilt were carried out by three different methods of inoculation of the cuttings: a) dipping of cuttings for ten minutes in bacterial suspension; b) spraying of suspension on perlite where the rooted cuttings were planted; c) spraying the greenhouse bench rooting boxes, where the non-rooted cuttings were planted, with bacterial suspension. Following this all the cuttings were transplanted into soil naturally highly infested withFusarium oxysporum f. sp.dianthii (3000 units/g). Good protection against fusarium wilt was obtained for cuttings inoculated by method (b). However protection decreased gradually about 60 days after they were transplanted; both control and inoculated cuttings showed a comparable mortality rate. Method of inoculation and the development of the protective effect are discussed.     

Mineralization dynamics in fallow dryland wheat plots,Colorado

Summary There was a flush of mineralization in fallow wheat plots in the wet and warm summer of 1982 at Akron, Colorado. Peak mineralization rates and concentrations of N and P coincided with a 2.5-fold increase in protozoan biomass. No-till contained considerably more activity than stubble mulch plots, especially in the surface 2.5 cm and there was more water storage in no-till on all dates. Differential management of agricultural residues and the resultant effects upon the microbial community significantly altered patterns of nutrient cycling.     

Regulation of carbon and electron flow in Propionispira arboris: physiological function of hydrogenase and its role in homopropionate formation

Abstract Hydrogenase activity was characterized in cell extracts of Propionispira arboris that consumed or produced H₂, coupled to methyl viologen reduction, and displayed highest levels (2.6 μmol/min/mg protein) in extracts prepared from fumarate-grown cells. Reversible hydrogenase activity in cell extracts correlated with the production of low levels of hydrogen during the growth phase and its subsequent consumption during the stationary phase of cells grown on glucose or lactate as the carbon and energy source. The addition of exogenous hydrogen to glucose, lactate or fumarate-grown cells dramatically increased propionate production at the expense of acetate formation. This accounted for the formation of propionate as nearly the sole end product of glucose fermentation under two atmospheres of hydrogen. The physiological function of hydrogenase in regulation of carbon and electron flow, and the significance of the results in applied and environmental microbiology are discussed.     

Separation of algal mixtures and bacterial mixtures with flow-microfluorometer using chlorophyll and ethidium bromide fluorescence

The applicability of flow-microfluorometer to separate microbial cells was demonstrated with algal and bacterial cells. Algal mixtures were sorted according to the natural chlorophyll fluorescence and the bacterial mixtures were sorted according to the fluorescence of ethidium bromide-stained nucleic acid.Abbreviation FMF Flow-microfluorometer