Growth and Phosphate Transport in Barley and Tomato Plants During the Development of, and Recovery from, Phosphate-stress

Barley and tomato plants were cultured in nutrient solutionsincluding 0.15 mol m^–3 H²PO^–₄. The phosphate supplywas discontinued and the subsequent effects on growth, internalphosphorus concentrations, phosphate absorption and translocationwere measured at frequent intervals. Growth rates were at firstunchanged and the internal phosphorus concentration decreased.During this phase the rate of phosphate transport by the rootssometimes increased significantly. Growth slowed more in shootsthan in roots during a second phase of stress development andvisual symptoms of deficiency appeared in tomato but not inbarley. During this phase, enhancement of phosphate uptake capacityreached a maximum in both species. The subsequent decline inuptake capacity was associated with visible symptoms of deficiencydeveloping in barley and intensifying in tomato. When stressedplants were returned to a solution containing 0.15 mol m^–3H₂PO^–₄ rapid absorption continued for several days afterthe internal phosphorus concentration had returned to the levelof the controls. Phosphate toxicity may have been the causeof leaf lesions and necrosis during the ‘recovery’phase. Stomatal conductance in tomato was decreased at an early stageof stress development. Foliar-applied phosphate was absorbedmore rapidly by P-stressed barley leaves than by their controlsand much larger amounts were translocated from the leaves tothe roots.     

Photosynthesis and chlorophyll fluorescence in sunflower (Helianthus annuus L.) leaves as affected by phosphorus nutrition

The effects of phosphate concentration on plant growth and photosyntheticprocesses in primary leaves of young sunflower (Helianthus annuusL.) plants were examined. Plants were grown for 3 weeks on half-strengthHoagland's solution containing 0, 0.1, 0.5, 1.0, and 3.0 molm^–3 orthophosphate (Pi). It was shown that optimal photosynthesisand the highest light utilization capacity were achieved at0.5 mol m^–3 Pi in the growth medium, which was in goodagreement with the maximum content of organic phosphorus inthe leaves. Low phosphate in the medium inhibited plant growthrate. Phosphate deficiency appreciably decreased photosyntheticoxygen evolution by leaves, the efficiency of photosystem two(PSII) photochemistry and quantum efficiency of PSII electrontransport. High oxidation state of PSII primary electron acceptorQA, at 0.1 mol m^–3 Pi, however, indicates that photosyntheticelectron transport through PSII did not limit photosynthesisin Pi-deficient leaves. The results indicate that diminishedphotosynthesis under sub- and supra-optimal Pi was caused mainlyby a reduced efficiency of ribulose 1, 5-bisphosphate (RuBP)regeneration at high light intensities. These results suggestthat, under non-limiting C0₂ and irradiance, photosynthesisof the first pair of leaves could be diminished by both sub-and supra-optimal phosphorus nutrition of sunflower plants. Key words: Helianthus annuus L, phosphate nutrition, photosynthesis, photochemical efficiency     

Application of 31P NMR to Monitor Phosphorus Compounds and their Changes During Germination of Legume Seeds

Extracts of embryonic axes and cotyledons of 19 species of legumeswere analysed by ³¹P nuclear magnetic resonance; the effectof different extraction procedures on the solubilization ofthe several phosphocompounds was investigated. The contentsof phytic acid, inorganic phosphate, phosphomonoesters and phosphodiesterswere determined. The relative contents of these phosphocompoundswere very different when embryonic axes and cotyledons werecompared, and were greatly influenced by the taxonomic affiliationof the corresponding species. Phytic acid and inorganic phosphatewere by far the major phosphocompounds found in cotyledon extracts;an unusual phosphodiester component was detected only in embryonicaxes and was particularly abundant in species belonging to theLotoideae sub-family. The changes in the amount of the phosphodiestercompound were followed during germination and the results suggestthat it is not a phosphorus reserve. Furthermore, this componentwas preferentially present in the roots of the new plants. Itwas partially hydrolysed by RNAse and to a smaller extent byproteases, but not affected by DNAse. The hypothesis that thisunusual component might be a ribonucleoprotein is discussed. Key words: ³¹P NMR, legumes, seed components, phosphorus compounds, solubilization     

Extracellular secretion of Aspergillus phytase from Arabidopsis roots enables plants to obtain phosphorus from phytate

Phosphorus (P) deficiency in soil is a major constraint for agricultural production worldwide. Despite this, most soils contain significant amounts of total soil P that occurs in inorganic and organic fractions and accumulates with phosphorus fertilization. A major component of soil organic phosphorus occurs as phytate. We show that when grown in agar under sterile conditions, Arabidopsis thaliana plants are able to obtain phosphorus from a range of organic phosphorus substrates that would be expected to occur in soil, but have only limited ability to obtain phosphorus directly from phytate. In wild-type plants, phytase constituted less than 0.8% of the total acid phosphomonoesterase activity of root extracts and was not detectable as an extracellular enzyme. By comparison, the growth and phosphorus nutrition of Arabidopsis plants supplied with phytate was improved significantly when the phytase gene (phyA) from Aspergillus niger was introduced. The Aspergillus phytase was only effective when secreted as an extracellular enzyme by inclusion of the signal peptide sequence from the carrot extensin (ex) gene. A 20-fold increase in total root phytase activity in transgenic lines expressing ex::phyA resulted in improved phosphorus nutrition, such that the growth and phosphorus content of the plants was equivalent to control plants supplied with inorganic phosphate. These results show that extracellular phytase activity of plant roots is a significant factor in the utilization of phosphorus from phytate and indicate that opportunity exists for using gene technology to improve the ability of plants to utilize accumulated forms of soil organic phosphorus.     

The Growth and Physiology of Pinus strobus L. Seedlings as Affected by Various Nutritional Levels of Nitrogen and Phosphorus

Potted white pine (Pinus strobus L.) seedlings were grown ingravel either in outdoor cold frames or in growth chambers.They were watered every second day with a salt solution containingdifferent amounts of nitrogen and phosphorus. After 13 weeksof growth individual seedlings were illuminated separately for8 h in the presence of ¹⁴CO₂ and the rates of their apparentphotosynthesis, respiration, and translocation of recent ¹⁴C-photosynthateto their roots were observed. Roots were extracted with 80 percent ethanol and the nature of various ¹⁴C compounds in theextract was determined by paper chromatography. The best over-all growth of plants, mycorrhizal development,apparent photosynthesis, and translocation of recent photosynthateto the roots were observed in plants grown at the intermediatelevels of N and P nutrition. Sucrose was always the dominant form in which recently translocated¹⁴C occurred in the roots, although with increased nitrogensupply there was increased hydrolysis of sucrose to hexosesand appearance of ¹⁴C in the amino- and organic acids.     

The role of phosphorus on planktonic production of the Gironde plume waters in the Bay of Biscay

More and more studies emphasize the status of phosphorus (P)as the principal limiting nutrient of phytoplankton growth,especially in coastal waters under the influence of freshwaterdischarges. The purpose of the present paper is to investigatethe role of P on planktonic production in the waters influencedby the Gironde discharges; the Gironde being one of the twolargest rivers on the French Atlantic coast. The survey is basedon several cruises made in 1998 and 1999. Two different patternswere observed for waters with salinity below and above 34.5.For waters with salinity < 34.5, P was found to be the firstlimiting nutrient of winter and spring phytoplankton blooms,based on undetectable phosphate (< 20 nM), high NO₃ : PO₄ratios, typically > 100 : 1, short phosphate turnover time(1 to 2 h), high alkaline phosphatase activities (mean of 176nM h^-1 in late May 1999) and ultimately great increases of chlorophylla (Chl a) and primary production in phosphate-enriched samplesrelative to controls. This limitation could be partly explainedby the Gironde nutrient supplies, which were phosphate deficientcompared with the mineral nitrogen(N_min : PO₄ was > 40 withina salinity range 16–33). In summer, corresponding to theperiod of low influence of Gironde supplies (low runoff anda spreading effect of the plume), phytoplankton growth wouldbe controlled by both P and nitrogen (N), according to low nitrateand the major effect of combined P+N (NH₄) enrichment on Chla and primary production compared with the addition of N orP singly. In early October, after the first autumn gales, themixed layer was enriched with a sufficient supply of nutrientsto support exponential phytoplankton growth for 4 days in enclosures.The pattern was different for waters at the limit of the Girondeplume and Atlantic oceanic waters (within salinity range 34.5–35.4).P would not be the single limiting nutrient of winter bloomsand spring phytoplankton growth since low phosphate, and alsolow nitrate and silicate, availability were recorded and phosphateaddition alone had no effect on phytoplankton biomass and productionin bioassays. The early P limitation of winter blooms had consequencesfor the phytoplankton community structure in the Gironde plumewaters (salinity < 34.5). Whereas major cells of these bloomswere greater than 20 µm in size, phytoplankton growthin spring and autumn was dominated by 3–20 µm (e.g.53% of Chl a in late April 1999) and < 3 µm cells (e.g.29% of Chl a). The decreasing size of phytoplankton cells isemphasized by the severe competition between bacteria and algaefor phosphate, since bacteria dominated phosphate uptake inspring (e.g. 87% in late April, 77% in late May). Bacteria tendedto have greater affinity for phosphate and seemed also to beP limited at certain times in spring, according to results fromphosphate enrichment bioassays in late May 1999. The alternativemethod for phytoplankton to obtain P would be the use of thedissolved organic phosphorus pool by alkaline phosphatase activity.According to the movement of ³³P after initial labelling ofmicrobial populations and a subsequent cold chase, the majortransfer of P occurred from the bacterial to the dissolved fraction.We hypothesize that algae obtain part of its dissolved organicphosphorus from bacteria-originated organic phosphorus compounds.     

The Growth of Etiolated Avena Seedlings in Relation to Phosphorus Nutrition

The effects of carbon dioxide, of phosphate, and of nitratenutrition on the growth of etiolated oat seedlings in relationto the amounts of reserves and of phosphorus translocated fromthe endosperm, have been studied in a 2³ factorially arrangedexperiment. For each mg of translocate 4.37 µg of phosphorus weretransferred in the untreated seedlings, and this rate was slightlyincreased by nitrates, reduced by phosphates, and hardly changedby carbon dioxide, at the concentrations used. Under treatment with phosphates a high content of phosphoruswas quickly built up in the roots, but there was an initialreduction in the quantity found in the coleoptile and leaves.Apparently, upward transport from the roots took place onlyslowly; the phosphorus in the coleoptile and leaves may thereforehave come preferentially from the endosperm. Although nitrate supply increased the flow of phosphorus fromthe endosperm, it decreased the content in the plants. Thiseffect appears to be due to a smaller uptake of phosphorus inthe presence of nitrates.     

The Influence of Carbohydrate and Mineral Nutrient Supply on the Growth of Potato Tubers

The uptake and distribution of nitrogen, phosphorus, and potassiumhas been studied throughout the life of potato plants. Thereappears to be a net loss of all three elements from the plantduring emergence growth even though uptake occurs. When daughtertubers are formed they very quickly become the dominant sinkfor mineral nutrients, the concentrations of N, P, and K remainingsteady for a long period. These concentrations are maintainedin spite of decreasing rates of uptake, indicating the transferenceof mobile ions from the haulm to the growing tubers. ¹⁴C tracer experiments have shown that after tuberization thereis a greater export of recently incorporated photosynthate fromthe leaves than takes place before tuberization. There is nogood correlation between the size of individual tubers and theamount of photosynthate transported into them. This is thoughtto be because the largest tubers are not necessarily growingfaster than the smaller tubers. The most active sinks are alsomost active in converting the mobile ¹⁴C into storage compounds.The mother tuber continues to import ¹⁴C until it is detachedfrom the plant, but over much of this period there is no changein the tuber dry-weight, indicating that there is an equivalentexport from the tuber. The similarities between these distribution patterns and thosefound in tubers showing second-growth are described and theimplications with respect to the control of tuber growth discussed.     

Root Zone Temperature Effects on Growth and Phosphate Absorption in Rape Brassica napus cv. Emerald

Solution culture experiments with fodder rape (Brassica napuscv. Emerald) show that reduced root temperatures appear to havelittle effect on phosphate inflow over a wide range of P concentration.At a cool root temperature (10 ?C) plant growth rate was reducedbut this was compensated for by a low root: shoot ratio, sothat inflow remained relatively steady. An increased inflowper unit length of root was only achieved at an elevated roottemperature of 35 ?C. The minimum phosphate concentration towhich plants could lower the culture solution (C_mln) rangedfrom 0.15 to 2.5 mmol m^–3 according to whether roots wereat a low (5 ?C) or high (35 ?C) temperature respectively. Thetotal phosphorus concentration in tissues was affected by rootzone temperature and at low root temperatures this could bea growth limiting factor. The organic (assimilated) fractionof P in shoot tissues was smaller in low temperature plants.These showed visual symptoms of apparent P deficiency. Levelsof inorganic P in roots may also be a factor in feedback ofcontrol of inflow. Key words: Temperature, Roots, Phosphate, Rape (Brassica napus)     

Phosphate Regulation of Nitrate Assimilation in Soybean

It is known that phosphorus deficiency results in alterationsin the assimilation of nitrogen. An experiment was conductedto investigate mechanisms involved in altered ¹⁵NO^–₃ uptake,endogenous ¹⁵N translocation, and amino acid accumulation insoybean (Glycine max L. Merrill, cv. Ransom) plants deprivedof an external phosphorus supply for 20 d in solution culture.Phosphorus deprivation led to decreased rates of ¹⁵NO^–₃uptake and increased accumulation of absorbed ¹⁵N in the root.Both effects became more pronounced with time. Asparagine, theprimary transport amino acid in soybean, accumulated in largeexcess in roots and stems. In roots of phosphorus-deprived plants,concentrations of ATP and inorganic phosphate declined rapidly,but dry weight accumulation was similar to or above that ofthe control even after 20 d of treatment. Arginine accumulationin leaves was greatly enhanced, even though ¹⁵N partitioninginto the insoluble reduced-N fraction of leaves was unaffected.The results suggest that decreases in NO^–₃ uptake in lowphosphorus plants could be caused by feedback control factorsand by limited ATP availability. The decline in endogenous Ntransport from the root to the shoot may be associated withchanges in membrane properties, which also result in paralleleffects on hydraulic conductance and the upward flow of waterthrough the plant. Key words: Phosphorus stress, nitrate uptake, nitrate translocation, arginine     

Utilization of limiting concentrations of ortho-phosphate and production of extracellular organic phosphates in cultures of marine diatoms

The utilization of ortho-phosphate by two coastal marine diatomspecies, Nitzschia closterium and Cyclotella cryptica, was studiedin batch cultures. The hypothesis was tested that thresholdconcentrations in the phosphate uptake determine the lower limitof environmental phosphate, permitting the existence of species.The turn-over time of residual medium phosphate in culturesis {small tilde}10 min, indicating a rapid equilibration ofconcentration dependent on uptake with leakage of ortho-phosphate.Increasing phosphate starvation in cultures diminished the residualortho-phosphate in the range of {small tilde}60–<2nmol l^–1, as measured radiochemically after elution onSephadex® G-10 gel. These concentrations encompass the rangeof limiting phosphate concentration in continuous cultures ofthe few microalgae, for which these concentrations are actuallymeasured. The diatoms excreted {small tilde}20–100 nmolI^–1 of organic phosphate. One dominating compound, probablyan unusual nucleotide, was incompletely or not resorbed underphosphate starvation. In contrast, Nitzschia closterium excretedunder ample phosphate supply a series of three related compounds,probably phospholipids, that were resorbed under depletion.The association of the organic phosphates with macromolecularexudates is interpreted, along with the other observations,as an indication for a hardly explored periplasmatic phosphatemetabolism in these algae. ³Dedicated to Prof. Dr. H.-A. von Stosch in honour of his 75thbirthday. ⁴This study was conducted at the University of Marburg undersupport of the Humboldt Foundation Publication no. 64 of theproject "Biological Research of the Eems-Dollard Estuary".     

Phosphorus Nutrition and the Intracellular Distribution of Inorganic Phosphate in Pea Root Tips: A Quantitative Study using31P-NMR

Pea plants (Pisum sativum L.) were supplied with external phosphatefor differing periods of time, so that their phosphorus statusvaried, and the intracellular distribution of inorganic phosphate(P₁) in the roots was examined by ³¹P nuclear magnetic resonance.Over the range of phosphorus nutrition investigated, the quantityof vacuolar P₁ per unit fresh weight of root tip changed considerably,whereas the quantity of cytoplasmic P₁ per unit fresh weightof root tip did not alter. The relative volumes of the cytoplasmand the vacuole in pea root tips seemed to be little affectedby differences in phosphorus nutrition, and this implied thatthe concentration of P₁ in the cytoplasm was kept almost constant,at a level estimated to be 18 mM. The rate of absorption of ³²P-labelled phosphate was negativelycorrelated with the vacuolar P₁ concentration, but there wasno clear correlation with the concentration of P₁ in the cytoplasm. Key words: Compartmentation, Cytoplasm, Vacuole, Concentration, Absorption     

Fate of ($ ) S-methyl-L-cysteine sulfoxide in Chinese cabbage, Brassica pekinensis RUPR.

($) S-methyl-L-cysteine sulfoxide (MCS) was scarcely found inseeds of Chinese cabbage, but was present in relatively largeamounts in all plant parts after germination. Changes in MCScontent paralleled those for soluble sulfur content of tissue. When Na₂³⁵SO₄ was fed to plants, the ³⁵S was predominantly incorporatedinto MCS in the free amino acid fraction in both sulfur-sufficientand deficient plants, but it was incorporated to a greater extentin the former. ³⁵S-MCS was metabolized more readily in deficientthan in sufficient plants, and its sulfur was found not onlyin various soluble compounds but in the insoluble fractionsfrom plants as well. These results indicate that MCS is a conspicuousconstituent in the free amino acid pool of Chinese cabbage andmay play an important role in sulfur metabolism by acting asa soluble pool for organic sulfur. (Received June 22, 1970; )     

The Influence of Nitrate and Ammonium Nutrition on the Growth of Wheat (Triticum aestivum) and Maize (Zea mays) Plants

The effects of NO^-₃ and NH⁺₄ nutrition on hydroponically grownwheat (Triticum aestivum L.) and maize (Zea mays L.) were assessedfrom measurements of growth, gas exchange and xylem sap nitrogencontents. Biomass accumulation and shoot moisture contents ofwheat and maize were lower with NH⁺₄ than with NO^-₃ nutrition.The shoot:root ratios of wheat plants were increased with NH⁺₄compared to NO^-₃ nutrition, while those of maize were unaffectedby the nitrogen source. Differences between NO^-₃ and NH⁺₄-fedplant biomasses were apparent soon after introduction of thenitrogen into the root medium of both wheat and maize, and thesedifferences were compounded during growth. Photosynthetic rates of 4 mM N-fed wheat were unaffected bythe form of nitrogen supplied whereas those of 12 mM NH⁺₄-fedwheat plants were reduced to 85% of those 12 mM NO^-₃-fed wheatplants. In maize supplied with 4 and 12 mM NH⁺₄ the photosyntheticrates were 87 and 82% respectively of those of NO^-₃-fed plants.Reduced photosynthetic rates of NH⁺₄ compared to NO^-₃-fed wheatand maize plants may thus partially explain reduced biomassaccumulation in plants supplied with NH⁺₄ compared to NO^-₃ nutrition.Differences in the partitioning of biomass between the shootsand roots of NO^-₃-and NH⁺₄-fed plants may also, however, arisefrom xylem translocation of carbon from the root to the shootin the form of amino compounds. The organic nitrogen contentof xylem sap was found to be considerably higher in NH⁺₄- thanin NO^-₃-fed plants. This may result in depletion of root carbohydrateresources through translocation of amino compounds to the shootin NH⁺₄-fed wheat plants. The concentration of carbon associatedwith organic nitrogen in the xylem sap of maize was considerablyhigher than that in wheat. This may indicate that the shootand root components of maize share a common carbon pool andthus differences induced by different forms of inorganic nitrogenare manifested as altered overall growth rather than changesin the shoot:root ratios.Copyright 1993, 1999 Academic Press Triticum aestivum, wheat, Zea mays, maize, nitrogen, growth, photosynthesis, amino acids, xylem     

Secreted acid phosphatase is expressed in cluster roots of lupin in response to phosphorus deficiency

The roots of white lupin (Lupinus albus L. cv. Kievskij mutant) secrete acid phosphatase, S-APase, when they grow under conditions of low available phosphorus (P). S-APases hydrolyze organic phosphate compounds in the rhizosphere and supply inorganic phosphate to the plants. Low phosphorus availability also induces vigorous growth of cluster roots. In this study, the function of cluster roots was investigated with reference to S-APase secretion. White lupins were grown in hydroponic culture in a greenhouse under P-deficient and P-sufficient conditions. S-APase in the excised roots after treatment was detected by staining with 4-methylumbelliferone phosphate (MUP). Gene expression of S-APase in cluster and normal roots was also investigated. Activity was greatest in the roots of plants grown under conditions of P -deficiency, particularly in cluster roots. S-APase gene expression was induced by a decrease in internal P concentrations, and was especially high in cluster roots formed under conditions of P -deficiency. It was suggested that decrease of internal P concentration stimulated both of the S-APase expression and cluster root formation.     

Nitrogen and Phosphorus in a Stretch of the Guadalupe River,Texas, with Five Main-Stream Impoundments by

Nitrogen and phosphorus were studied in a 168-km stretch of the Guadalupe River that had five main-stream impoundments. Flow through the study area was controlled by releases from these five reservoirs and from Canyon Reservoir, a deep-storage reservoir, located 30 km upstream. Parameters measured monthly on a diel basis at 16 stations were nitrate nitrogen, nitrite nitrogen, ammonia nitrogen, Kjeldahl nitrogen, inorganic phosphate phosphorus, organic phosphate phosphorus, and total phosphate phosphorus.Inorganic nitrogen concentrations observed in this study were as high or higher than that previously reported for other bodies of water. Nitrate nitrogen entered the study area in relatively high concentrations from Comal Springs which was a major source of water for the Guadalupe River. Water from Canyon Reservoir, the other major source of water, was relatively low in nitrate nitrogen. The concentration of nitrate nitrogen was, therefore, dependent in part upon the portion of the total river flow originating from the two sources. Increased discharge from Canyon Reservoir and utilization by plants in areas of high chlorophyll a resulted in low nitrate-nitrogen levels. Retention of water in reservoirs reduced the concentration of nitrate nitrogen due to increased utilization by plants in areas of low flow. Nitrate nitrogen, in general, reached seasonal minima in summer and maxima in winter. Nitrite nitrogen showed considerable variation with no meaningful pattern except that higher concentrations occurred in association with high chlorophyll a and high Kjeldahl nitrogen, regions and periods of low river flow, and large phytoplankton populations. There was no increase in concentration of any form of nitrogen in the vicinity of sewage outfalls and no downstream accrual.Phosphorus levels in the study area were as high or higher than those reported in studies of other bodies of water. Sewage treatment plants at New Braunfels and Seguin, Texas, were major sources of phosphorus to the Guadelupe River. Total phosphate phosphorus was determined to be the most critical phosphate parameter in assessing eutrophication. Seasonally, it ranged from a winter high to a summer low. Concentrations were highest immediately below sewage outfalls and decreased as water progressed downstream. Inorganic-phosphate-phosphorus concentrations showed no clear seasonal trend but were clearly associated with sewage outfalls. Since large standing crops of phytoplankton were observed in areas of low inorganic phosphate phosphorus, it was not considered to limit photosynthesis. Total organic phosphate phosphorus varied seasonally, with high concentrations occurring during the spring and low concentrations in the fall. Total organic phosphate phosphorus showed no correlation with sewage outfalls, but was correlated to a degree with total Kjeldahl nitrogen and chlorophyll a. No consistent pattern of diel fluctuations was evident for any phosphorus or nitrogen compounds analyzed.     

The phosphate uptake mechanism

The slow rate of diffusion of phosphate in soil results in a zone of depletion of phosphate ions in solution around the roots of plants in low phosphate soils. Transfer of phosphate to the site of uptake into the root symplasm limits phosphate uptake in such soils. This transfer involves movement across the depletion zone and through the root apoplasm. The apoplasm is made up of the cell walls of epidermal and cortical cells, together with the associated intercellular spaces. Although the pores in the open latticework of these cell walls permit movement of nutrients around cells, they increase the path length across which phosphate ions have to diffuse. The structural components and net negative charges of the cell walls also influence the effective concentrations of phosphate in the apoplasm. This concentration may be further modified by excreted organic compounds around cell walls and the presence of micro-organisms that use such compounds as carbon sources. A membrane on the inner surface of the cell wall, the plasmalemma, separates the apoplasm from the symplasm. Uptake of nutrients into the root symplasm occurs through transporter proteins embedded in this membrane. Understanding of the mechanisms by which phosphate is transported across the plasmalemma into the plant symplasm has advanced considerably over the past 4 years due to the application of molecular techniques. Genes encoding the transporters involved in this process have been isolated from a number of plant species. These transporters belong to a family of membrane proteins characterized by having 12 membrane-spanning domains arranged in a '6+6' configuration. H₂PO₄ ^– ions, together with protons, are transported through this protein. This transport process is driven by the potential across the membrane maintained by the action of a H⁺-ATPase, the `proton pump', that extrudes protons to the outer surface of the membrane. The expression of genes encoding high-affinity root phosphate transporters is regulated by the phosphorus (P) status of the plant. The transduction pathway involved in this regulation is not known at present. It is a systemic response rather than a localized response, however, the overall phosphate status of the plant being the controlling factor. Under phosphate stress, the expression of genes encoding these phosphate transporters is up-regulated. This results in a greater number of transporter proteins in the plasmalemma and enhanced phosphate uptake rates, if phosphate is available at the membrane surface. Uptake occurs around the root tip, into epidermal cells with their associated root hairs and into cells in the outer layers of the root cortex. Further back along the root axis, phosphate can also be taken up by transfer from mycorrhizal fungi to root cortical cells.Strategies for increasing nutrient uptake by overexpressing genes encoding high-affinity phosphate transporters are likely to be mainly applicable to situations where a reasonable phosphate concentration can be maintained at the outer surface of the plasmalemma. Maintaining such a concentration is a major problem in the phosphate deficient soils of the semi-arid tropics (SAT), so emphasis in these soils is on strategies to improve the movement of phosphate to the surface of the plasmalemma. There may be scope, however, for manipulating the expression of genes involved in the internal mobilisation of phosphate within the plant, thereby improving phosphate utilisation.     

Differential uptake of orthophosphate and organic phosphorus substrates by bacteria and algae in Lake Kinneret

The availability of six organic phosphorus substrates (OPS)to serve as sources of this nutrient for natural populationsof phytoplanktonic algae and bacteria was tested by measuringthe degree to which the organic substrates decreased uptakeof [³²P]orthophosphate (³²Pⁱ). When added to samples of LakeKinneret water, six organo-phosphorus compounds usually loweredthe amount of ³²P_i] taken up by microplankton retained on 0.2-µfilters.In contrast, OPS addition generally stimulated ³²P_i uptake intothe mainly algal fraction (>3 µm), indicating thatthe bacteria were mostly responsible for utilising OPS. Thesparing effect of OPS addition on ³²P₁ uptake was very fast,suggestingthat the micro-organisms possessed constitutive or rapidly inducedenzyme systems to exploit the OPS.The results of this studyindicate that a significant flux of phosphorus may pass viaDOP into microbiota, especially bacteria, in some aquatic systems.     

Solubility of phosphorus added to four Manitoba soils with different calcium and magnesium contents

Summary The solubility of phosphorus was found to approximate that of dicalcium phosphate dihydrate and/or dimagnesium phosphate trihydrate when KH₂-PO₄, H₃PO₄ and K₂HPO₄ were added to four Manitoba soils. Eighty to one hundred, seventy to ninety and sixty to eighty per cent of the phosphorus added remained in solution when H₃PO₄, KH₂PO₄ and K₂HPO₄ were added, respectively. The solubility of the added phosphorus was high in all samples and relatively soluble compounds, dicalcium phosphate dihydrate and dimagnesium phosphate trihydrate, were most likely formed in the samples indicating that phosphorus added to these soils would be readily available to plants. Associate Professor and Professor respectively.