Rhizobium strains expressing uptake hydrogenase in different host species of cowpea miscellany

Uptake hydrogenase activity in nodules of green gram (Vigna radiata (L.) (Wilczek)), black gram (Vigna mungo (L.) (Hepper)), cowpea (Vigna unguiculata (L.) and cluster bean (Cyamopsis tetragonoloba (L.) (Taub.)), formed with two Hup⁺ (S24 and CT2014) and one Hup⁻ (M11)Rhizobium strains, was determined at different levels of external H2 in air atmosphere. Nodules of all the 4 host species formed by inoculation with strains S24 and CT2014, showed H2 uptake but not those formed with strain M11. H₂ uptake rates were higher in 1 and 2% H₂ in air atmosphere (v/v) than at 5 or 10% levels in all the host species. Variations in the relative rates of H₂ uptake were observed both, due to host species as well as due toRhizobium strains. However, no host dependent complete repression of the expression of H₂ uptake activity was observed in nodules of any of the host species formed with Hup⁺ strains.     

High Photobiological Hydrogen Production Activity of a <Emphasis Type="Italic">Nostoc</Emphasis> sp. PCC 7422 Uptake Hydrogenase-Deficient Mutant with High Nitrogenase Activity

We describe a strategy to establish cyanobacterial strains with high levels of H₂ production that involves the identification of promising wild-type strains followed by optimization of the selected strains using genetic engineering. Nostoc sp. PCC 7422 was chosen from 12 other heterocystous strains, because it has the highest nitrogenase activity. We sequenced the uptake hydrogenase (Hup) gene cluster as well as the bidirectional hydrogenase gene cluster from the strain, and constructed a mutant (ΔhupL) by insertional disruption of the hupL gene. The ΔhupL mutant produced H₂ at 100 μmoles mg chlorophyll a ^-1 h^-1, a rate three times that of the wild-type. The ΔhupL cells could accumulate H₂ to about 29% (v/v) accompanied by O₂ evolution in 6 days, under a starting gas phase of Ar + 5% CO₂. The presence of 20% O₂ in the initial gas phase inhibited H₂ accumulation of the ΔhupL cells by less than 20% until day 7.     

Effect of oxygen partial pressure on nitrogen fixation and acetylene reduction in a sandy loam soil amended with glucose

Summary Small samples of soil amended with 2% (w/w) of glucose were preincubated either aerobically or anaerobically and then assayed (N₂ ¹⁵ and C₂H₂-C₂H₄) either aerobically or anaerobically for different time periods. One-hour C₂H₂-C₂H₄ assays showed greatest activity when anaerobic assay followed anaerobic preincubation. During the anaerobic preincubation a lag of 12–24 h occurred before rapid increase in one-hour assay activity was observed. When aerobic assay followed aerobic preincubation a longer lag was observed and lower activities were obtained. When anaerobic assay followed aerobic preincubation (orvice versa) negligible activities were observed in short assays, and longer assays showed increasing activity related to changes in atmosphere and/or microbial population in the closed system. Preincubation of soil on a diffusion gradient at a series of different partial pressures of oxygen confirmed the above pattern and showed that as preincubation pO₂ increased, the anaerobic assay activity rapidly decreased. As preincubation pO₂ decreased from 0.2 atm the aerobic assay activity decreased but less rapidly. The activities observed were related to the sizes of the Azotobacter and Clostridium populations. There was no evidence of aerobic or anaerobic C₂H₂ reduction in any cultures of ‘oligonitrophiles’ isolated. Incorporation of N₂ ¹⁵ was related to C₂H₂ reduction activity in the soil system studied. However, observed C₂H₄/N₂ molar ratios ranged from 10 to 22 and appeared to be highest in samples which were preincubated anaerobically. Issued as Macdonald College Journal Series No.618 and as Canadian IBP contribution No.84.     

Hydrogen oxidation and nitrogen fixation in rhizobia,with special attention focused on strain ORS 571

In this survey we describe the influence of hydrogen oxidation on the physiology ofRhizobium ORS 571. The presence of hydrogen is required for the synthesis of hydrogenase. Carbon substrates do not repress the synthesis of hydrogenase. The respiratory system contains cytrochromes of theb- andc-type. Cytochromea ₆₀₀ is present after growth at high oxygen tensions. The nature of the terminal oxidases functioning at low oxygen tensions has not been established yet. → H⁺/O values with endogenous substrates are between 6 and 7. The results show the presence of two phosphorylation sites: site 1 (ATP/2e=1.0) and site 2(ATP/2e=1.33). By measuring molar growth yields it has been demonstrated that carbon-limited, nitrogen-fixing cultures obtain additional ATP from hydrogen oxidation, and that site 2 of oxidative phosphorylation is passed during hydrogen oxidation. A method is described to calculate ATP/N₂ values (the total amount of ATP used by nitrogenase during the fixation of 1 mol N₂) and H₂/N₂ ratios (mol hydrogen formed per mol N₂ fixed) in aerobic organisms. ForRhizobium ORS 571 the ATP/N₂ value is about 40 and the H₂/N₂ ratio is between 5 and 7.5. Cells obtained from oxygen-limited nitrogen-fixing cultures contain 30–40% poly-β-hydroxybutyrate, which explains the high molar growth yields found. Hydrogen has not been detected in the effluent gas of these cultures, which may point to reoxidation of the hydrogen formed at nitrogen fixation. Calculations show that the effect of hydrogen reoxidation on the efficiency of nitrogen fixation (g N fixed × mol⁻¹ substrate converted) is not very large and that the actual H₂/N₂ ratio is of much more importance. After addition of hydrogen to succinate-limited, ammonia-assimilating cultures, an initial increase of the Y_succinate value (g dry wt × mol⁻¹ succinate) is followed by a gradual decrease. This is accompanied by a large decrease of the value, and an increased permeability of the cytoplasmic membrane to protons. The results may be explained by a transition of the culture from an energy-limited state to a carbon-limited state.     

Seasonal variation in the nitrogenase activity of aPanicum maximum var.trichoglume pasture and identification of associated bacteria

Summary The influence of seasonal variation on nitrogenase (N₂-ase) activity of undisturbed soil-plant cores ofPanicum maximum var.trichoglume was measured using the C₂H₂ reduction assay. The largest N₂-ase activity in the field, 14.7 g N ha⁻¹ day⁻¹, occurred in spring when soil moisture was high, soil temperature was low and nitrogenous fertiliser influence was at a minimum. The potential N₂-ase activity of the cores, measured under controlled conditions, reached a maximum of 27.2 g N ha⁻¹ day⁻¹ and averaged 26.3 g N ha⁻¹ day⁻¹ over the 14 month sampling period. N₂-ase activity was positively correlated (P=0.05) with field soil moisture and negatively correlated with field soil temperature (r=0.59 and −0.78 respectively). Multiple regression showed that 69% of the variation of N₂-ase activity in the field was associated with the combined effects of soil moisture and soil temperature. Nitrogen fixing bacteria were isolated from the roots ofP. maximum and based upon morphology, biochemical tests and fluorescent antibody reaction, were found to be closely related toAzospirillum lipoferum.     

Soil H2-uptake in relation to soil properties and rhizobial H2-production

Summary The biological nature of soil H₂-consumption has been investigated. Soil microorganisms were capable to remove H₂ present in the gas phase at concentrations in the range of 200 ppm at rates varying between 0.2 and 1.0 l.min^–1. 100 g^–1. Free soil enzymes did not contribute significantly at the H₂ concentrations tested. Oxygen seemed to be the predominant electron acceptor. The influence of microbiological and physical soil properties on the H₂-uptake activity was examined for 38 soils.A highly significant correlation between biomass-C and H₂-uptake rate of the soil was noted, suggesting that the latter parameter might be useful as an indirect estimation of soil microbial biomass. The correlation was however not applicable for soils recently grown with legumes. Indeed, soya plants nodulated with aRhizobium strain with a weak hydrogen uptake capability, strongly increased the hydrogen oxidizing capability of the surrounding soil.     

Dynamics of <Superscript>18</Superscript>O Incorporation from H <Subscript>2</Subscript><Superscript>18</Superscript>O into Soil Microbial DNA

Heavy water (H₂¹⁸O) has been used to label DNA of soil microorganisms in stable isotope probing experiments, yet no measurements have been reported for the ¹⁸O content of DNA from soil incubated with heavy water. Here we present the first measurements of atom% ¹⁸O for DNA extracted from soil incubated with the addition of H₂¹⁸O. Four experiments were conducted to test how the atom% ¹⁸O of DNA, extracted from Ponderosa Pine forest soil incubated with heavy water, was affected by the following variables: (1) time, (2) nutrients, (3) soil moisture, and (4) atom% ¹⁸O of added H₂O. In the time series experiment, the atom% ¹⁸O of DNA increased linearly (R ² = 0.994, p < 0.01) over the first 72 h of incubation. In the nutrient addition experiment, there was a positive correlation (R ² = 0.991, p = 0.006) between the log₁₀ of the amount of tryptic soy broth, a complex nutrient broth, added to soil and the log₁₀ of the atom% ¹⁸O of DNA. For the experiment where soil moisture was manipulated, the atom% ¹⁸O of DNA increased with higher soil moisture until soil moisture reached 30%, above which ¹⁸O enrichment of DNA declined as soils became more saturated. When the atom% ¹⁸O for H₂O added was varied, there was a positive linear relationship between the atom% ¹⁸O of the added water and the atom% ¹⁸O of the DNA. Results indicate that quantification of ¹⁸O incorporated into DNA from H₂¹⁸O has potential to be used as a proxy for microbial growth in soil.     

Growth and physiological activity in <Emphasis Type="Italic">Larix kaempferi</Emphasis> seedlings inoculated with ectomycorrhizae as affected by soil acidification

To evaluate the effect of ectomycorrhizal colonization on growth and physiological activity of Larix kaempferi seedlings grown under soil acidification, we grew L. kaempferi seedlings with three types of ectomycorrhizae for 180 days in acidified brown forest soil derived from granite. The soil had been treated with an acid solution (0 (control), 10, 30, 60, and 90 mmol H⁺ kg⁻¹). The water-soluble concentrations of Ca, Mg, K, Al, and Mn increased with increasing amounts of H⁺ added to the soil. Ectomycorrhizal development significantly increased in soil treated with 10 and 30 mmol H⁺ kg⁻¹ but was significantly reduced in soil treated with 60 and 90 mmol H⁺ kg⁻¹. The concentrations of Al and Mn in needles or roots increased with increasing H⁺ added to the soil. The total N in seedlings significantly increased with increasing H⁺ in soil and colonization with ectomycorrhiza. The maximum net photosynthetic rate at light and CO₂ saturation (P _max) was greater in soil treated with 10 mmol H⁺ kg⁻¹ than in controls, and was less is soils treated with greater than with 30 mmol H⁺ kg⁻¹, especially with 60 and 90 mmol H⁺ kg⁻¹. However, colonization with ectomycorrhiza significantly reduced the concentration of Al and Mn in needles or roots and increased the values of P _max and total dry mass (TDM). The relative TDM of L. kaempferi seedlings was approximately 40% at a (BC, base cation)/Al ratio of 1.0. However, ectomycorrhizal seedlings had a 100–120% greater TDM at a BC/Al ratio of 1.0 than non-ectomycorrhizal seedlings, even though the acid treatment reduced their overall growth.     

Moisture adsorption capacity and surface area as deduced from vapour pressure isotherms in relation to hygroscopic water of soils

Six calcareous and alluvial soil profiles differing in their texture, CaCO₃ and salinity were chosen from west and middle Nile Delta for the present study. The 1^st and 2^nd profiles from Borg El-Arab area were sandy loam in texture and > 30% CaCO₃, while the 3^rd and 4^th profiles (from Nubaria area) were sandy clay loam and < 30% CaCO₃. The 2^nd and 4^th profiles were taken from cultivated area with maize. The 5^th profile from Epshan area was non-saline clay alluvial soil and the 6^th from El-Khamsen was saline clay alluvial soil. The relation between soil moisture content (W%) and water vapour pressure (P/P _o) was established for the mentioned soils. Data showed that the specific surface area (S) values were 34–53 and 44–60 m²/g for calcareous soils of Borg El-Arab and Nubaria areas, 206–219 and 206–249 m²/g for non-saline and saline clay alluvial soils of Epshan and El-Khamsen areas, respectively. The corresponding values of the external specific surface area (S _e) were 16–21, 14–22, 72–86 and 92–112 m²/g. Submitting W _m+W _me as an adsorption boundary of moisture films (W _c) (where W _m is mono-adsorbed layer of water vapour on soil particles and W _me is the external mono-adsorbed layer), the maximum water adsorption capacity (W _a) was found to be W _c + W _me or W _m + 2W _me. It was ranged from 1.88 to 2.70%, 1.97 to 2.95%, 9.70–10.70% and 10.80 to 13.12% while the maximum hygroscopic water (M _H) values were 2.43–3.78%, 2.91–4.65%, 16–17% and 18.30–21.9% for the studied soil profiles respectively. The residual moisture content (θ _r) at pF 7 and P/P _o = 0 was ranged from 0.0005–0.0010%, 0.0007–0.0019% and 0.0043–0.0048% in Borg El-Arab, Nubaria and Epshan soil profiles, respectively. The inter-relations between the surface area and the hygroscopic moisture parameters of the soils under investigation were as follows Calcareous soils; W _m = 0.40 M _H, W _c = 0.55 M _H, W _a = 0.70 M _H, S = 14 M _H Non-saline soil; W _m = 0.35 M _H, W _c = 0.49 M _H, W _a = 0.63 M _H, S = 13 M _H Saline soil; W _m = 031 M _H, W _c = 0.45 M _H, W _a = 0.59 M _H, S = 12 M _H These relations give possibility to deduce the soil moisture adsorption capacities and specific surface area via maximum hygroscopic water, which can be obtained through the experimental determination of water vapor adsorption isotherms.     

Actual and potential rates of hydrogen photoproduction by continuous culture of the purple non-sulphur bacterium Rhodobacter capsulatus

The influence of (NH₄)₂SO₄ concentration and dilution rate (D) on actual and potential H₂ photoproduction has been studied in ammonium-limited chemostat cultures of Rhodobacter capsulatus B10. The actual H₂ production in a photobioreactor was maximal (approx. 80 ml h⁻¹l⁻¹) at D = 0.06 h⁻¹ and 4 mM (NH₄)₂SO₄. However, it was lower than the potential H₂ evolution (calculated from hydrogen evolution rates in incubation vials), which amounted to 100–120 ml h⁻¹ l⁻¹ at D = 0.03–0.08 h⁻¹. Taking into account the fact that H₂ production in the photobioreactor under these conditions was not limited by light or lactate, another limiting (inhibiting) factor should be sought. One possibility is an inhibition of H₂ production by the H₂ accumulated in the gas phase. This is apparent from the non-linear kinetics of H₂ evolution in the vials or from its inhibition by the addition of H₂; initial rates were restored in both cases after the vials had been refilled with argon. The actual H₂ production in the photobioreactor at D = 0.06 h⁻¹ was shown to increase from approximately 80 ml h⁻¹ l⁻¹ to approximately 100 ml h⁻¹ l⁻¹ under an argon flow at 100 ml min⁻¹. Under maximal H₂ production rates in the photobioreactor, up to 30% of the lactate feedstock was utilised for H₂ production and 50% for biomass synthesis. Received: 22 April 1997 / Received revision: 14 July 1997 / Accepted: 27 July 1997     

TheParasponia parviflora — Rhizobium symbiosis. Isotopic nitrogen fixation,hydrogen evolution and nitrogen-fixation efficiency,and oxygen relations

Summary Isotopic¹⁵N₂ experiments confirmed nitrogen fixation inParasponia parviflora. The conversion ratio C₂H₄/N₂ was 6.7 under the experimental conditions employed. Measurements of the δ¹⁵N in leaves of Parasponia and Trema showed on the basis of these determinations thatParasponia parviflora possesses N₂-fixing capacity and can be distinguished in this respect from the non-nitrogen-fixingTrema cannabina tested by the same method. Therefore, δ¹⁵N can be used to monitor N₂ fixation in natural ecosystems. Hydrogen evolution and the relative efficiency of N₂ fixation in this relation have been determined. DetachedParasponia parviflora root nodules grown in soil and tested in an argon/oxygen atmosphere produced appr. 4 μmol H₂.h⁻¹.g⁻¹ fresh weight root nodules. The relative efficiency of hydrogen utilization as measured in argon, air, and in the presence of C₂H₂ 10% (v/v) was for both equations used for to express this efficiency 0.96 and 0.97, respectively. This indicates that Parasponia like the root nodules of some actinorhizal symbioses (Alnus, Myrica, Elaeagnus) and some tropical legumes (Vigna sinensis) has evolved mechanisms of minimizing net hydrogen production in air, thus increasing the efficiency of electron transfer to nitrogen. The oxygen relation of nitrogen fixation (C₂H₂) inParasponia parviflora root nodules was determined. The nitrogenase activity of Parasponia root nodules increased at increasing oxygen concentrations up till c. 40% O₂. At oxygen levels above 40% O₂, the nitrogenase activity of the root nodules was nil or very erratic suggesting that at these oxygen levels the nitrogenase is not longer protected against the harmful effect of oxygen. In this respect Parasponia root nodules differ from actinorhizal root nodules in other nonlegumes, where optimal nitrogenase activity was observed in the range of 12–25% oxygen. Respiration experiments with Parasponia root nodules showed that in the range 10, 20, and 40% oxygen, the respiration rate (CO₂ evolution) increased concomitantly with an increase of the acetylene reduction rate. The CO₂/C₂H₄ values obtained varied between 8.1 and 19.2, being therefore 2–3 times higher than similar estimations in some actinorhizal and legume root nodules. The respiratory quotient (RQ) of detachedParasponia parviflora root nodules was in air initially approximately 2.0, but this value dropped to about 1.0 in a 3-hours period.     

Symbiotic effectiveness of Hup+ Rhizobium,VAM fungi and phosphorus levels in relation to nitrogen fixation and plant growth ofCajanus cajan

Effect of hydrogen uptake positive (Hup⁺) strain ofRhizobium sp. (pigeon pea) and VAM fungus (Glomus fasciculatum) was studied on the symbiotic parameters of pigeon pea (Cajanus cajan) cv. AL-15 at various levels of phosphorus. The Hup⁺ Rhizobium strain showed more nodulation, plant biomass and plant nitrogen content than its Hup⁻ counterpart. VAM infection in pigeon pea roots helped in translocating phosphorus from the soil and improved nitrogen fixation. Similarly, addition of phosphorus was found to play a positive role in enhancing all these parameters. Dual inoculation of Hup⁺ Rhizobium strain and VAM significantly increased nodulation, nitrogenase activity, plant nitrogen and phosphorus content and plant biomass compared to single inoculation of either organism and dual inoculation with Hup⁻ and VAM fungus.     

Comparison of Nitrogen Fixation for North- and South-facing <Emphasis Type="Italic">Robinia pseudoacacia</Emphasis> Stands in Central Korea

The nitrogenase activity, root nodule biomass, and rates of nitrogen (N) fixation were measured in 25-year-old pure north- and south-facing Robinia pseudoacacia stands in an urban forest of Seoul (Kkachisan Mountain) in central Korea. The nitrogenase activity was estimated using an acetylene reduction (AR) assay, which showed an increasing trend during the early growing season, with sustained high rates from June through to September with a decrease thereafter. July had the highest nitrogenase activity rate (micromoles C₂H₄ per gram dry nodule per hour), averaging 95.8 and 115.1 for the north- and south-facing stands, respectively. The maximum root nodule biomass (kilograms per hectare) was 45.7 and 9.1 for the north- and south-facing stands in July, respectively. The AR rate appeared to be strongly correlated to the soil temperature (r ² = 0.68, P < 0.001) and soil pH (r ² = 0.59, P < 0.001) while root nodule biomass was correlated to the soil temperature (r ² = 0.36, P < 0.01) and water content (r ² = 0.35, P < 0.05). The soil temperature showed clear differences between seasons, while there was a significant difference in soil pH, organic matter, total N concentrations, and available phosphorus between the north- and south-facing stands. The N₂ fixation rates during the growing season varied from 0.1 to 37.5 kg N ha⁻¹ month⁻¹ depending on the sampling location and time. The annual N₂ fixation rate (kg N per hectare per year) was 112.3 and 23.2 for the north- and south-facing stands, respectively. The differences in N₂ fixation rate between the two stands were due mainly to the differences in total nodule biomass.     

Impact of commonly used agrochemicals on bacterial diversity in cultivated soils

The effects of three selected agrochemicals on bacterial diversity in cultivated soil have been studied. The selected agrochemicals are Cerox (an insecticide), Ceresate and Paraquat (both herbicides). The effect on bacterial population was studied by looking at the total heterotrophic bacteria presence and the effect of the agrochemicals on some selected soil microbes. The soil type used was loamy with pH of 6.0–7.0. The soil was placed in opaque pots and bambara bean (Vigna subterranean) seeds cultivated in them. The agrochemicals were applied two weeks after germination of seeds at concentrations based on manufacturer’s recommendation. Plant growth was assessed by weekly measurement of plant height, foliage appearance and number of nodules formed after one month. The results indicated that the diversity index (Di) among the bacteria populations in untreated soil and that of Cerox-treated soils were high with mean diversity index above 0.95. Mean Di for Ceresate-treated soil was 0.88, and that for Paraquattreated soil was 0.85 indicating low bacterial populations in these treatment-type soils. The study also showed that application of the agrochemicals caused reduction in the number of total heterotrophic bacteria population sizes in the soil. Ceresate caused 82.50% reduction in bacteria number from a mean of 40 × 10⁵ cfu g⁻¹ of soil sample to 70 × 10⁴ cfu g⁻¹. Paraquat-treated soil showed 92.86% reduction, from a mean of 56 × 10⁵ cfu g⁻¹ to 40 × 10⁴ cfu g⁻¹. Application of Cerox to the soil did not have any remarkable reduction in bacterial population number. Total viable cell count studies using Congo red yeast-extract mannitol agar indicated reduction in the number of Rhizobium spp. after application of the agrochemicals. Mean number of Rhizobium population numbers per gram of soil was 180 × 10⁴ for the untreated soil. Cerox-treated soil recorded mean number of 138 × 10⁴ rhizobial cfu g⁻¹ of soil, a 23.33% reduction. Ceresate- and Paraquat-treated soils recorded 20 × 10⁴ and 12 × 10⁴ cfu g⁻¹ of soil, respectively, representing 88.89% and 93.33% reduction in Rhizobium population numbers. Correspondingly, the mean number of nodules per plant was 44 for the growth in untreated soil, 30 for the plant in the Cerox-treated soil, 8 for the plant in Paraquat-treated soil and 3 for the plant in Ceresate-treated soil. The study has confirmed detrimental effect of insecticide on bacterial populations in the soil. Total heterotrophic counts, rhizobial counts as well as the number of nodules of all samples taken from the chemically treated soils were all low as compared to values obtained for the untreated soil. However, the effect of the insecticide was minimal in all cases as compared to the effects of the herbicides on the soil fauna. Indiscriminate use of agrochemicals on farms can therefore affect soil flora and subsequently food production.     

Effects of H2O2 on the growth, secretion, and metabolism of hybridoma cells in culture

Summary The effect of low concentrations of hydrogen peroxide (H₂O₂) (5 × 10⁻⁷−9.5 × 10⁻⁷ M) on cell growth and antibody production was investigated with murine hybridoma cells (Mark 3 and anti-hPL) in culture. Cell growth, measured by flow cytometry with morphological parameters, was significantly stimulated by H₂O₂ (8 × 10⁻⁷ M) but H₂O₂ concentration of 7 × 10⁻⁶ M and above increased cell death. H₂O₂ stimulation of antibody production was nonsignificant. The metabolism of cells treated with 8 × 10⁻⁷ or 1 × 10⁻⁵ M H₂O₂ was similar to that of the control in terms of glucose and glutamine consumption, lactate and ammonia production, and amino acid concentrations in the medium. The concentrations of lactate dehydrogenase, a marker of cell death, in test and control cells were similar. However, concentrations of intracellular free radicals measured by flow cytometry with dihydrorhodamine 123 (DHR 123) and dichlorofluorescein diacetate (DCFH-DA) as fluorochromes were different. The reactive oxygen species content of cells in 8 × 10⁻⁷ M H₂O₂ was similar to that of the controls, but there was a sudden, marked production of superoxide anions (detected with DHR 123) and H₂O₂ or peroxides (detected with DCFH-DA) by cells incubated with 1 × 10⁻⁵ M H₂O₂ which increased with increasing H₂O₂ until cell death.     

Hydrogen production and uptake by pea nodules as affected by strains of Rhizobium leguminosarum

Hydrogen evolution from root nodules has been reported to make N₂ fixation by some legume-Rhizobium symbiotic systems inefficient. We have surveyed the extent of H₂ evolution and estimated relative efficiencies of nodules of Austrian winter peas formed by 15 strains of R. leguminosarum. Their rates of H₂ evolution in air were about 30% of the rates of H₂ evolution under an atmosphere in which N₂ was replaced by Ar. Relative efficiency values based on C₂H₂ reduction rates ranged from 0.55 to 0.80. With some of the strains, hydrogenase activities were demonstrated in intact nodules and in bacteroids, but the levels of activity were insufficient to recycle all the H₂ evolved by the nitrogenase system. In both intact nodules and bacteroids the hydrogenase is less sensitive to O₂ damage than the nitrogenase system, so H₂ uptake capacity was observed in intact nodules by suppressing the nitrogenase-dependent H₂ evolution with an atmosphere containing a high O₂ concentration, and in bacteroids by using aerobically prepared bacteroid suspensions. The hydrogenase activity of both was dependent on O₂ consumption. A K _mfor H₂ of near 4 M was determined in suspension of bacteroids from nodules formed by strains 128C53 and 128C56.     

A transmissible plant shoot factor promotes uptake hydrogenase activity in Rhizobium symbionts

Shoot/root grafting studies showed organ and host cultivar effects on net H₂ evolution from Pisum sativum L. root nodules. Net H₂ evolution from those nodules represents the sum of H₂ formed by Rhizobium nitrogenase and H₂ oxidized by any uptake hydrogenase present in the bacteria. Grafts between pea cultivars `JI1205' or `Alaska' and `Feltham First' in symbioses with R. leguminosarum 128C53 showed that shoots of both JI1205 and Alaska increased H₂ uptake significantly (P ≤ 0.05) in Feltham First root nodules. The same plants also had less net H₂ evolution at similar rates of C₂H₂ reduction than plants formed by grafting Feltham First shoots on Feltham First roots. Although JI1205 and Alaska shoots increased H₂-uptake activity of Feltham First root nodules 28 days after the graft was made, intermediate to high levels of H₂ uptake activity were still present in nodules on roots of both JI1205 and Alaska grafted to Feltham First shoots. These results indicate the presence of a transmissible shoot factor(s) which can increase uptake hydrogenase activity in a Rhizobium symbiont and show that root genotype also can influence that parameter.

Parallel grafting experiments using the same pea cultivars in symbioses with R. leguminosarum strain 300, which lacks uptake hydrogenase activity, suggested that a transmissible shoot factor(s) altered H₂ formation from nitrogenase by changing the electron allocation coefficient of that enzyme complex.

The root and shoot factor(s) detected in this study had no permanent effect on strain 128C53. Bacterial cells isolated from Feltham First nodules with low H₂ uptake activity formed root nodules on JI1205 and Alaska with high H₂ uptake activity. Bacteroids isolated from nodules on intact JI1205, Alaska, or Feltham First plants with high, medium, or low H₂ uptake activity, respectively, maintained those phenotypes during in vitro assays.

     

Acetylene reduction,H2 evolution and 15N2 fixation in the Alnus incana-Frankia symbiosis

Acetylene reduction, ¹⁵N₂ reduction and H₂ evolution were measured in root systems of intact plants of grey alder (Alnus incana (L.) Moench) in symbiosis with Frankia. The ratios of C₂H₂: ¹⁵N₂ were compared with C₂H₂:N₂ ratios calculated from C₂H₂ reduction and H₂ evolution, and with C₂H₂:N₂ ratios calculated from accumulated C₂H₄ production and nitrogen content. It was possible to calculate C₂H₂:N₂ ratios from C₂H₂ reduction and H₂ evolution because this source of Frankia did not show any hydrogenase activity. The ratios obtained using the different methods ranged from 2.72 to 4.42, but these values were not significantly different. It was also shown that enriched ¹⁵N could be detected in the shoot after a 1-h incubation of the root-system. It is concluded that the measurement of H₂ evolution in combination with C₂H₂ reduction represents a nondestructive assay for nitrogen fixation in a Frankia symbiosis which shows no detectable hydrogenase activity.     

Acetylene reduction and indoleacetic acid production by Azospirillum isolates from Cactaceous plants

Azospirillum isolates were obtained from rhizosphere soil and roots of three cactaceae species growing under arid conditions. All Azospirillum isolates from rhizosphere and roots ofStenocereus pruinosus andStenocereus stellatus were identified asA. brasilense; isolates of surface-sterilized roots fromOpuntia ficus-indica were bothA. brasilense andA. lipoferum. Azospirilla per g of fresh root in the three species ranged from 70×10³ to 11×10³. The most active strains in terms of C₂H₂ reduction (25–49.6 nmol/h·ml) and indoleacetic acid (IAA) production (36.5–77 μg/ml) were those identified asA. brasilense and isolated from Stenocereus roots.A. lipoferum isolated from Opuntia roots produced low amounts of IAA (6.5–17.5 μg/ml) and low C₂H₂-reduction activity (17.8–21.2 nmol/h·ml).