The growth and phosphorus utilisation of plants in sterile media when supplied with inositol hexaphosphate, glucose 1-phosphate or inorganic phosphate

Seedlings of six temperate pasture species, three grasses and three legumes, were grown for 19–24 days in sterile agar or sand-vermiculite media, in the presence of inorganic phosphate (P_i), glucose 1-phosphate (G1P) or inositol hexaphosphate (IHP). Agar (pH 5.0) had a low IHP-sorbing capacity while IHP was almost completely sorbed in sand-vermiculite. P_i and G1P were relatively available in both media. Growth of each species was measured in relation to phosphorus (P) supply and levels of P_i supply at which shoot yields reached 90% of maximum yield (P_crit) were determined. P_crit values were generally higher for the legume species than for the grasses, and were six-fold higher for Trifolium subterraneum L. seedlings when grown in sand-vermiculite relative to agar. When supplied with G1P, seedlings of the six species grew as well as plants supplied with P_i. By contrast, IHP was a poor source of P for plant growth, even when supplied in agar at levels up to 40-fold greater than P_crit. Using the growth of T. subterraneum in the presence of IHP, it was calculated that roots released approximately 0.09 nkat phytase g^-1 root dry wt per day, over 20 days of growth. By supplementing agar containing IHP with phytase from Aspergillus niger (E.C. 3.1.3.8; 0.012 nkat plant^-1, or _∼1.3 nkat g^-1 root dry wt), sufficient P became available to enable T. subterraneum seedlings to grow as well as P_i-supplied plants. These results indicate that while pasture plants can quite effectively use P from some organic P sources (e.g. G1P), the acquisition of phytate-P is limited both by availability of substrate and the capacity of plant roots to hydrolyse available IHP. This revised version was published online in June 2006 with corrections to the Cover Date.     

Effects of plant species on phosphorus availability in a range of grassland soils

Vegetative conversion from grass to forest may influence soil nutrient dynamics and availability. A short-term (40 weeks) glasshouse experiment was carried out to investigate the impacts of ryegrass (Lolium perenne) and radiata pine (Pinus radiata) on soil phosphorus (P) availability in 15 grassland soils collected across New Zealand using ³³P isotopic exchange kinetics (IEK) and chemical extraction methods. Results from this study showed that radiata pine took up more P (4.5–33.5 mg P pot^–1) than ryegrass (1.1–15.6 mg pot^–1) from the soil except in the Temuka soil in which the level of available P (e.g., E _1min P_i, bicarbonate extractable P_i) was very high. Radiata pine tended to be better able to access different forms of soil P, compared with ryegrass. There were no significant differences in the level of water soluble P (Cp, intensity factor) between soils under ryegrass and radiata pine, but the levels of Cp were generally lower compared with original soils due to plant uptake. The growth of both ryegrass and radiata pine resulted in the redistribution of soil P from the slowly exchangeable P_i pool (E _{> 10m} P_i, reduced by 31.8% on the average) to the rapidly exchangeable P_i (E _1min-1d P_i, E _1d-10m P_i) pools in most soils. The values of R/r ₁ (the capacity factor) were also generally greater in most soils under radiata pine compared with ryegrass. Specific P mineralisation rates were significantly greater for soils under radiata pine (8.4–21.9%) compared with ryegrass (0.5–10.8%), indicating that the growth of radiata pine enhanced mineralisation of soil organic P. This may partly be ascribed to greater root phosphatase activity for radiata pine than for ryegrass. Plant species × soil type interactions for most soil variables measured indicate that the impacts of plant species on soil P dynamics was strongly influenced by soil properties.     

Influence of dietary calcium and phosphorus supply on epithelial phosphate transport in preruminant goats

P homeostasis affected by high or low Ca and/or P supply in preruminant goats was characterized by balance studies in vivo. The main excretion pathway was the renal P_i excretion whose extent was modulated by variations in dietary P and/or Ca supply. Faecal P excretion remained low irrespective of dietary regimen. The balance data were combined with respective in vitro data on P_i transport properties and their adaptation in response to changes in dietary Ca and/or P intake. Therefore, P_i transport capacities were determined by P_i uptake into brush border membrane vesicles of jejunum and kidney. Epithelial P_i transporters were determined semiquantitatively by northern and western blot analyses in jejunum, kidney and salivary gland. Renal P_i transport was downregulated by doubling dietary P supply while doubling both, Ca and P as well as restrictive Ca at unchanged P led to slight, but not significant reductions in renal P_i transport. Jejunal P_i transport was reduced by P excess (doubling P and doubling both, Ca and P), but only NaPi IIb protein expression was significantly diminished. In conclusion, the significance of epithelial adaptation to dietary Ca and P supply for P homeostasis is discussed in preruminant goats.     

Rapid whole-plant bioassay for phosphorus phytoavailability in soils

Chemical P extraction from soils is an indirect and frequently questionable index for P availability. To monitor the dynamics of P availability in soils more directly following the application of P fertilizer, manure or sludge, a rapid, whole-plant bioassay was developed using tomato (Lycopersicon esculentum Mill.), Chinese cabbage (Brassica rapa L. var.pekinensis) and wheat (Triticum aestivum L.). Plant P extracted in 0.1 M H₂SO₄ (P_i) and total P (P_t) concentration or content in stem, leaves or whole shoots were highly correlated (P < 0.01) with P fertilizer rates or water-soluble (WSP) or Olsen P in various soils, over wide ranges of soil P status. The whole-plant P_i content was found to be as informative as the more complicated indices of P_t or P_iconcentration. The assay was used to compare availability of fertilizer-P and sewage-sludge-P after incorporation into alluvial soil during 1–100 days of incubation. While both soil and plant indices had shown that fertilizer-P was more highly available than sewage-sludge-P in each period, the bioassay was much more sensitive than the Olsen-P or WSP soil indices in showing P fixation and decrease of availability during incubation time. The bioassay is sufficiently rapid (5–12 days) to allow a study of short-term changes in soil-P availability following incorporation of various P additives, and it is applicable to a very wide range of P availability values (6–535 mg Olsen-P kg^–1), extending from lower than desired for crop production to higher than permitted from an environmental standpoint.     

Assay of nitrogen supplying capacity of tropical rice soils

Summary The nitrogen supplying capacity of 39 wetland rice soils evaluated by two anaerobic incubation methods and six chemical methods was compared with N uptake of IR 26 rice grown on these soils under flooded conditions in a greenhouse pot study. The uptake of N by rice correlated highly with the N supplying capacity determined by anaerobic incubation methods involving incubation of soils at 30°C for 2 weeks (r=0.84^**) or at 40°C for 1 week (r=0.82^**) as well as with the organic carbon (r=0.82^**) and total N (r=0.84^**) contents of soils. Among the chemical indexes, available N determined by the oxidative release of soil N by alkaline permanganate, acid permanganate, acid dichromate and hydrogen peroxide also provided good index of soil N availability to rice. According to these results soil organic carbon and total N contents seem to be good indexes of available nitrogen in tropical wetland rice soils.     

Gas Exchange Responses to CO2 Concentration Instantaneously Elevated in Flag Leaves of Winter Wheat Cultivars Released in Different Years

Three winter wheat (Triticum aestivum L.) cultivars, representatives of those widely cultivated in Beijing over the past six decades, were grown in the same environmental conditions. Net photosynthetic rate (P _N) per unit leaf area and instantaneous water use efficiency (WUE) of flag leaves increased with elevated CO₂ concentration. With an increase in CO₂ concentration from 360 to 720 µmol mol^–1, P _N and WUE of Jingdong 8 (released in 1990s and having the highest yield) increased by 173 and 81 %, while those of Nongda 139 (released in 1970s) increased by 88 and 66 %, and Yanda 1817 (released in 1945, with lowest yield) by 76 and 65 %. Jingdong 8 had the highest P _N and WUE values under high CO₂ concentration, but Yanda 1817 showed the lowest P _N. Stomatal conductance (g _s) of Nongda 139 and Yanda 1817 declined with increasing CO₂ concentration, but g _s of Jingdong 8 firstly went down and then up as the CO₂ concentration further increased. Intercellular CO₂ concentration (C _i) of Jingdong 8 and Nongda 139 increased when CO₂ concentration elevated, while that of Yanda 139 increased at the first stage and then declined. Jingdong 8 had the lowest C _i of the three wheat cultivars, and Yanda 1817 had the highest C _i value under lower CO₂ concentrations. However, Jingdong 8 had the highest P _N and lowest C _i at the highest CO₂ concentration which indicates that its photosynthetic potential may be high.     

Effects of natural and artificially induced reduction on soil solution phosphorus in rice soils

The effect of natural and artificial reduction on P extractability from soils used for rice production and the relation of these values to response to fertilizer P were investigated. Soil solution P increased from a mean of 3.8 mg P·kg^?1 soil for naturally oxidized slurries of 28 soils to 19.8mg P·kg^?1 when the soils were naturally reduced. The mean values were further increased to 40.8 and 45.3 mg·kg^?1 when the soils were reduced with 0.1M Na₂S₂O₄ and 0.2M Na₂S₂O₄, respectively. These P-values compare with 18.2 mg kg^?1 when the dry soils were extracted with Bray No. 1 extractant. When the yields of rice were correlated with solution and extracted P, the R²'s for the quadratic relationships were 0.40^**, 0.31^*, 0.34^**, 0.30^*, and 0.55^** for the naturally oxidized, the naturally reduced, 0.1M Na₂S₂O₄, 0.2M Na₂S₂O₄ and Bray No. 1, respectively. The Cate-Nelson calculation confirmed the superiority of the weak acid Bray extractant and the critical value of 8.6 mg P·kg^?1 soil needed for satisfactory yields of rice. There was little response of rice to added fertilizer P on soils with solution P-values greater than 0.09 mg P·l^?1 in oxygenated soil slurries. Some soils with solution P of this order and high amounts of Bray No. 1 extractable P still gave modest responses to fertilizer P. Although natural or chemically induced reduction increased soil solution P, it did not improve prediction of yield response of rice to added fertilizer P.     

Functional expression of rat renal Na/Pi-cotransport (NaPi-2) in Sf9 cells by the baculovirus system

The recently cloned Na/P _i -cotransport system NaPi-2 is an apical membrane protein of rat proximal tubular cells and is involved in proximal phosphate reabsorption. To make the protein available for further functional/structural studies, this transport system has been expressed in Sf9 insect cells using a recombinant baculovirus. Sf9 cells infected with NaPi-2 (or 6His tagged NaPi-2) expressed functional Na/P _i -cotransport up to 20- to 50-fold over noninfected Sf9 cells. Transport of phosphate in infected cells was highly dependent on sodium, exhibited a K _m for P _i of 0.114 mm and an apparent K _m for Na of 63 mm (Hill coefficient of approximately 3) and was stimulated by high external pH. Infected cells expressed a polypeptide of 65 kDa representing a nonglycosylated form of the 85 kDa mature NaPi-2 transporter as present in proximal tubular brush-border membranes. By confocal microscopy expression of NaPi-2 protein was observed in the plasma membrane, yet submembranous accumulation of NaPi-2 protein could not be excluded. This demonstrates that the rat proximal tubular Na/P _i -cotransport system NaPi-2 can be successfully expressed in Sf9 cells with characteristics similar to that in isolated brush-border membranes. The 6His tagging will permit isolation of the NaPi-2 cotransporter in amounts sufficient for structural/functional studies.We would like to thank W. Scherle and M. Lötscher (Institute of Anatomy) for their generous help using the confocal microscope and Ch. Gasser for the art work. Financial support by the Swiss National Fonds [Grant No. 32-30785.91 (to H.M.) and 32-28664.90 (to J.B.)] and by Stiftung für wissenschaftliche Forschung an der Universitát Zürich is greatly acknowledged.     

Changes in soil phosphorus fractions following positive and negative phosphorus balances for long periods

The effect of phosphorus (P) balance (addition, in both fertilizers and farmyard manure (FYM), minus removal in crops) on eight soil P fractions determined by sequential extraction, was measured on archived soils from various long-term experiments run by Rothamsted Experimental Station in the United Kingdom. It has been established unequivocally that, for all the soils investigated, no one of the eight P fractions was increased or decreased during long periods of P addition or depletion, respectively. However, changes were mainly in the resin (24–30%) and the inorganic (P_i) component of the four fractions extracted sequentially by 0.5 M NaHCO₃, 0.1 M NaOH, 1.0 M NaOH, 0.5 M H₂SO₄ (41–60%). For the sandy loam there were also consistent changes in the organic (P_o) fraction (25%), especially that extracted by bicarbonate, presumably because the soil contained only a little clay and presumably had low sorption capacity. When the soils were cropped without P addition the largest proportional change was in the P extracted by resin, 0.5 M NaHCO₃ and 0.1 M NaOH, suggesting that the P in these fractions is readily available, or has the potential to become available, for crop growth. This was supported by changes in the overall P balance. On the heavier textured soils, 50–80% of the change in total soil P (P_T) was in these fractions; on the sandy soil this increased to more than 90%. The change in the sum of the first five fractions accounted, on average, for 90% of the P balance. However these changes in the P in the plough layer frequently left large amounts of P unaccounted for in some of the excessively P enriched soils. The amount of P_i extracted by resin and bicarbonate (P_i(r+b)) ranged between 14 and 50% of the sum of the P_i fractions. Soils with the lower percentages were those known to be most responsive to P fertilizers. P_i(r+b) accounted for an average of 70% of the P balance (negative) in P depleting soils where crop offtake was not offset or exceeded by annual P additions (positive balance). The ratio between P_i(r+b) and P_i(sum) could be a guide in defining soils deficient in P and those which are excessively enriched.     

Effect of soil moisture and phosphate level on root hair growth of corn roots

Summary Root hairs have been shown to enhance P uptake by plants growing in low P soil. Little is known of the factors controlling root hair growth. The objective of this study was to investigate the influence of soil moisture and P level on root hair growth of corn (Zea mays L.). The effect of volumetric soil moistures of 22% (M₀), 27% (M₁), and 32% (M₂) and soil (Raub silt loam, Aquic Argiudoll) P levels of, 0.81 (P₀), 12.1 (P₁), 21.6 (P₂), 48.7 (P₃), and 203.3 (P₄) mol P L^–1 initially in the soil solution, on shoot and root growth, P uptake, and root hair growth of corn was studied in a series of pot experiments in a controlled climate chamber. Root hair growth was affected more by soil moisture than soil P. The percentage of total root length with root hairs and the density and length of root hairs on the root sections having root hairs all increased as soil moisture was reduced from M₂ to M₀. No relationship was found between root hair length and soil P. Density of root hairs, however, was found to decrease with an increase in soil P. No correlation was found between root hair growth parameters and plant P content, further suggesting P plays a secondary role to moisture in regulating root hair growth in soils. The increase in root hair growth appears to be a response by the plant to stress as yield and P uptake by corn grown at M₀ were only 0.47 to 0.82, and 0.34 to 0.74, respectively, of that measured at M₁ across the five soil P levels. The increase in root hair growth at M₀, which represents an increase of 2.76 to 4.03 in root surface area, could offset, in part, the reduced rate of root growth, which was the primary reason for reduced P uptake under limited soil moisture conditions.Journal Paper No. 10,066 Purdue Univ. Agric. Exp. Stn., W. Lafayette, IN 47907. Contribution from the Dep. of Agron. This paper was supported in part by a grant from the Tennessee Valley Authority.     

Evaluation of chemical methods for estimating available zinc and response of green gram (Phaseolus aureus roxb) to applied zinc in non-calcareous soils

Summary Studies were conducted in 22 non-calcareous soils (India) to evaluate various extractants,viz. (6N HCl, 0.1N HCl, EDTA (NH₄)₂CO₃, EDTA NH₄OAc, DTPA+CaCl₂ and 1M MgCl₂) to find critical levels of soil and plant Zn for green gram (Phaseolus aureus Roxb.). The order of extractability by the different extractants was 6N HCl>0.1N HCl>EDTA (NH₄)₂CO₃<EDTA NH₄OAc DTPA+CaCl₂>1M MgCl₂. Critical levels of 0.48 ppm DTPA × CaCl₂ extractable Zn, 0.80 ppm EDTA NH₄OAc extractable Zn, 0.70 ppm EDTA (NH₄)₂CO₃ extractable Zn, and 2.2 ppm 0.1N HCl extractable Zn were estimated for the soils tested. The critical Zn concentration in 6 weeks old plants was found to be 19 ppm. The 0.1N HCl method gave the best correlation (r=0.588^**) between extractable Zn and Bray's per cent yield, while with DTPA+CaCl₂, it was slightly low (r=0.542^**). The DTPA + CaCl₂ method gave significant (r=0.73^**) correlation with plant Zn concentration. The 0.1N HCl gave the higher correlation with Zn uptake (r=0.661^**) than DTPA (r=0.634^**) 6N HCl and 1M MgCl₂ method gave nonsignificant positive relationship with Bray's per cent yield. For noncalcareous soils apart from the common use of DTPA+CaCl₂, 0.1N HCl can also be used for predicting soil available Zn. The use of 0.1N HCl would be much cheaper than DTPA and other extractants used in the study.     

Seasonal variation in organic and inorganic phosphorus fractions of temperate-climate sandy soils

Soils from an arable plot, a grassland plot and pasture plot were sampled over an 18-month period. Inorganic (P_i) and organic (P_o) soil phosphorus fractions were extracted sequentially with resin, NaHCO₃, and NaOH. Soil solution was sampled on the arable plot and pasture plot during 12 months with teflon suction cups, and the contents of P_i and P_o were determined.The patterns of the variation for all soil fractions were similar for the three plots. All soil P_i fractions were at minimum in the cool moist winter period. The soil P_o fractions varied less systematically than P_i fractions. The sum of P_o fractions had a winter maximum and a spring minimum. For all soil P fractions temporal variation was highly significant (p<0.0001). The magnitude of change in P_i and P_o soil fractions was 4–40 times greater than what would be expected from the magnitude of new N mineralization.The content of P in the inorganic soil P fractions was negatively correlated with soil moisture. The variation in organic soil P could not be explained by any single factor, but it is suggested that the variation is caused by changes in solubility rather than by biological transformations. Thus, physicochemical processes masked the impact of biological transformations on the temporal variation of soil phosphorus fractions.Both soil solution P_i and P_o varied significantly with time on field scale. In contrast to soil P_i fractions, solution P_i was initially low in the early autumn, increased by a factor 4 during the following 6 weeks, and thereafter decreased to a low level by the end of the sampling period. Soil solution P_o had several fluctuations during the sampling period.     

On the assessment of root and soil respiration for soils of different textures: interactions with soil moisture contents and soil CO2 concentrations

Estimates of root and soil respiration are becoming increasingly important in agricultural and ecological research, but there is little understanding how soil texture and water content may affect these estimates. We examined the effects of soil texture on (i) estimated rates of root and soil respiration and (ii) soil CO₂ concentrations, during cycles of soil wetting and drying in the citrus rootstock, Volkamer lemon (Citrus volkameriana Tan. and Pasq.). Plants were grown in soil columns filled with three different soil mixtures varying in their sand, silt and clay content. Root and soil respiration rates, soil water content, plant water uptake and soil CO₂ concentrations were measured and dynamic relationships among these variables were developed for each soil texture treatment. We found that although the different soil textures differed in their plant-soil water relations characteristics, plant growth was only slightly affected. Root and soil respiration rates were similar under most soil moisture conditions for soils varying widely in percentages of sand, silt and clay. Only following irrigation did CO₂ efflux from the soil surface vary among soils. That is, efflux of CO₂ from the soil surface was much more restricted after watering (therefore rendering any respiration measurements inaccurate) in finer textured soils than in sandy soils because of reduced porosity in the finer textured soils. Accordingly, CO₂ reached and maintained the highest concentrations in finer textured soils (> 40 mmol CO₂ mol⁻¹). This study revealed that changes in soil moisture can affect interpretations of root and soil measurements based on CO₂ efflux, particularly in fine textured soils. The implications of the present findings for field soil CO₂ flux measurements are discussed. This revised version was published online in June 2006 with corrections to the Cover Date.     

Inorganic and organic P in soil solutions from three upland soils

Soil solutions from three P-deficient Cambisols were analyzed for inorganic orthophosphate (P_i), organically combined phosphorus (P_o), total phosphorus (P_t) and residual phosphorus (P_r=P_t–(P_o+P_i)). The solutions were obtained by centrifugation of soil samples wetted-up to 90% field capacity. Increasing the centrifugal force from 750 to 1400×g (for 60 minutes) increased the volume of soil solution obtained by 17–35%. Increasing the centrifugation period from 30 to 90 minutes (at 1000×g) increased the volume by 2–12%. The effect of the different centrifugation conditions on the P composition of soil solutions were not critical and had little effect on either P_t concentration or on the distribution of P between P_i, P_o and P_r fractions. Soil solutions were also obtained on a seasonal basis over a 2-year period. The soils, fresh from the field, were wetted-up to 90% field capacity and centrifuged at 1000×g for 60 minutes to isolate the soil solution. Although the soils were derived from contrasting parent rock, and had different Fe and Al sesquioxide contents, the P_t concentrations of the soil solutions and the distribution between the fractions were similar. Annual average P_t concentrations for the 3 soils ranged from 93 to 114 and 63 to 89 g dm^-3 during the first and second year, respectively. Seasonal changes were of a similar order as those resulting from differences in soil type. During May, June, August and October soil solutions had average P_t concentrations ranging from 82 to 111 and 51 to 119 g P dm^-3 in 1989 and 1990, respectively. P_o was a major P component in soil solution and exceeded the amount of P_i by about 5–20 times.     

Observation of Two Inorganic Phosphate NMR Resonances in the Perfused Hypothermic Rat Heart

The effect of hypothermia on isolated perfused rat hearts was studied with³¹P NMR. Hearts were continuously perfused with phosphate-free Krebs–Henseleit buffer while the perfusate temperature was adjusted. Perfusate pH was kept at 7.40 ± 0.02 throughout the experiments. Using the chemical shift difference between PCr and P_ithe intracellular pH was estimated. At 36, 20, and 10°C a cytosolic alkalinization at a pH of 7.05 ± 0.04, 7.21 ± 0.05, and 7.40 ± 0.03 was observed, respectively. At 10°C two P_iresonances were observed with a separation of 0.25 ppm. This resonance corresponded to a P_iresonance of a cellular compartment with a local pH of 7.78 ± 0.06, likely mitochondrial. This additional resonance disappeared upon warming of the hearts back to 36°C.     

Uptake kinetics and assimilation of phosphorus byCatenella nipaeandUlva lactucacan be used to indicate ambient phosphate availability

Uptake, assimilation and compartmentation of phosphate were studied in the opportunist green macroalgaUlva lactucaand the estuarine red algal epiphyteCatenella nipae. The Michaelis–Menten model was used to describe uptake rates of inorganic phosphate (P_i) at different concentrations. Maximum uptake rates (V _max) of P-starved material exceededV _maxof P-enriched material; this difference was greater forC. nipae. Uptake and allocation of phosphorus (P) to internal pools was measured using trichloroacetic acid (TCA) extracts and³²P. Both species demonstrated similar assimilation paths: when P-enriched, most³²P accumulated as free phosphate. When unenriched,³²P was rapidly assimilated into the TCA-insoluble pool.C. nipaeconsistently assimilated more³²P into this pool thanU. lactuca, indicatingC. nipaehas a greater P-storage capacity. In both species,³²P release data showed two internal compartments with very different biological half-lives. The rapidly exchanging compartment had a short half-life of 2 to 12 min, while the slowly exchanging compartment had a much longer half-life of 12 days in P-starvedC. nipaeor 4 days in P-starvedU. lactuca. In both species, the slowly exchanging compartment accounted for more than 90% of total tissue.U. lactucaandC. nipaeresponded differently to high external P_i.U. lactucarapidly took up P_i, transferring this P_iinto tissue phosphate and TCA-soluble P in a few hours (90% of total P).C. nipaetook up P_iat lower rates and stored much of this P in less mobile TCA-insoluble forms. Long-term storage of refractory forms of P makesC. nipaea useful bioindicator of the prevailing conditions of P_iavailability over at least the previous 7 days, whereas the P-status ofU.lactucamay reflect conditions over no more than the previous few hours or days.C. nipaeis a more useful bioindicator for P status of estuarine and marine waters thanU. lactuca.     

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.     

A 31P NMR study of the internal pH of yeast peroxisomes

The internal pH of peroxisomes in the yeasts Hansenula polymorpha, Candida utilis and Trichosporon cutaneum X4 was estimated by ³¹P nuclear magnetic resonance (NMR) spectroscopy. ³¹P NMR spectra of suspensions of intact cells of these yeasts, grown under conditions of extensive peroxisomal proliferation, displayed two prominent P_i-peaks at different chemical shift positions. In control cells grown on glucose, which contain very few peroxisomes, only a single peak was observed. This latter peak, which was detected under all growth conditions, was assigned to cytosolic P_i at pH 7.1. The additional peak present in spectra of peroxisome-containing cells, reflected P_i at a considerably lower pH of approximately 5.8–6.0. Experiments with the protonophore carbonyl cyanide m-chlorophenylhydrazon (CCCP) and the ionophores valinomycin and nigericin revealed that separation of the two P_i-peaks was caused by a pH-gradient across a membrane separating the two pools. Experiments with chloroquine confirmed the acidic nature of one of these pools. In a number of transfer experiments with the yeast H. polymorpha it was shown that the relative intensity of the P_i-signal at the low pH-position was correlated to the peroxisomal volume fraction. These results strongly suggest that this peak has to be assigned to P_i in peroxisomes, which therefore are acidic in nature. The presence of peroxisome-associated P_i was confirmed cytochemically.Abbreviations CCCP Carbonyl cyanide m-chlorophenylhydrazon - DCCD N,N-dicyclohexylcarbodiimide     

Expression of the mosquitocidal cryIVB gene under the control of different promoters in Bacillus sphaericus 2362 and acrystalliferous Bacillus thuringiensis subsp. israelensis c4Q2-72

The 3.7 kb XbaI fragment harbouring the cryIVB gene which encoded a 130 kDa mosquitocidal toxin protein from Bacillus thuringiensis subsp. israelensis (B.t.i.) was placed downstream to the cat-86 gene promoter (P _cat-86, spore stage specific expression) or bgaB gene promoter (P _bgaB , vegetative stage specific expression). The constructs were subcloned into pBC16 to obtain pBTC3 and pBTC6, respectively. Both plasmids and the other construct, pBTC1 were successfully transferred into B. thuringiensis subsp. israelensis c4Q2-72 and B. sphaericus 2362. Western blot analysis showed that P _bgaB in front of P _cryIVB could enable cells to produce a 130 kDa protein from the vegetative stage (4 h) whereas those with P _cat-86 could not. The positive detection of 130 kDa crystal protein during the vegetative stage (4 h) by Western blot analysis indicated the vegetative-stage-specific expression of P _bgaB , while the 130 kDa crystal protein produced from cryIVB gene under control of P _cat-86 was detected only at 48 h. The strong activity of P _bgaB , together with P _cryIVB within pBTC6 in both bacterial hosts was also shown by the toxicity assay against Aedes aegypti larvae (B.t.i. c4Q2-72, 5.6 ± 3.6 × 10² c.f.u./ml; B. sphaericus 2362, 5.4 ± 2.5 × 10² c.f.u./ml) which were 100-fold and 10-fold more toxic to such larvae when compared with pBTC3 (P _cat-86 together with P _cryIVB ) and pBTC1 (contained only its self promoter) in the same bacterial host strains, respectively. The plasmid pBTC6 is not stable in either Bacillus host.