Impact of growth and uptake patterns of arbuscular mycorrhizal fungi on plant phosphorus uptake—a modelling study

In this paper we present a mathematical model for estimating external mycelium growth of arbuscular mycorrhizal fungi and its effect on root uptake of phosphate (P). The model describes P transport in soil and P uptake by both root and fungi on the single root scale. We investigate differences in soil P depletion and overall P influx into a mycorrhizal root by assuming that different spatial regions of mycelia are active in P uptake. When all external hyphae contribute to P uptake, overall uptake is dominated by the fungus and the most effective growth pattern appears to be the one using a high level of anastomosis. The same is true when only the proportion of external hyphae assumed to be active contributes to uptake. When uptake is restricted to the tips, hyphal contribution to overall P uptake is less dominant; the most effective growth pattern appears to be the one characterised by nonlinear branching where branching stops at a given maximal hyphal tip density. Comparison to measured P depletion in the literature suggests that the scenario where active hyphae are contributing to P uptake is likely to fit the data best. These quantitative predictions promote our understanding of the mycorrhizal symbiosis and its role in plant P nutrition.     

Phosphorus uptake by root systems: mathematical modelling in ecosys

The uptake of P by plant root systems is believed to be controlled by the concentration of soluble orthophosphate at the root surface. If a P transformation model in which this concentration is calculated were coupled to a root and mycorrhizal growth model in which this concentration is used to calculate P uptake, then it should be possible to simulate P uptake under different soil and climate conditions if soil properties relevant to the control of P concentration are known. To test this idea, models for the transformation and transport of inorganic and organic P were coupled to ones for root growth and nutrient uptake as part of the ecosys modelling program. Seasonal estimates of soluble P concentration, root growth and P uptake from the combined models were tested with data measured from barley under fertilized and unfertilized treatments in a long term P fertilizer experiment conducted on two different soils. In both soils the fertilizer treatment increased simulated and measured soluble P concentrations from 0.1-0.2 to 0.2-0.4 g m^-3, annual P uptake from 0.6-0.7 to 1.2-1.4 g m^-2, and annual DM accumulation from 400-500 to 700-800 g m^-2. Increases in soluble P concentrations caused by fertilizer P were reproduced in the model from changes in the balance between the desorption and dissolution of solid P on one hand, and the uptake of P by root and mycorrhizal systems on the other. Increases in P uptake caused by fertilizer P were reproduced in the model from higher solution P concentrations, root uptake kinetics, and from functional equilibria for C and P exchange simulated among mycorrhizal, root and shoot components of the plant. There was a tendency in the model to overestimate P uptake later in the growing season in the unfertilized treatment which could be corrected if parameters for root uptake kinetics were reduced after anthesis. Because the model is constructed independently of data for P uptake, and avoids the use of site-specific parameters, it may provide a means of estimating uptake under different managements and climates from soils of known properties.     

Native soil and fresh fertilizer phosphorus uptake as affected by rate of application and P fertilizers

³²P labelled fertilizers were used to measure native soil and fresh fertilizer phosphorus uptake byLolium perenne L. in greenhouse experiments. The P source evaluation was carried out for multiple rates of application for a standard P fertilizer (DAP) on low and medium soil P levels and for North Carolina rock phosphate (RP) at the medium soil P level only. At the low soil P level, the native P uptake increase was independent of P-DAP applied, and represented 19% of the nil P uptake. At the medium soil P level, the variability of the native soil as a nutrient P source depended on the phosphate fertilizer applied, and the rate of application. Consequently the amount of total P uptake could conceal differences in P fertilizer evaluations as the nutrient P source. Fresh P uptake increased linearly with the rates of P applied as standard or tested P fertilizer. The comparison of various P sources by means of fresh P uptake ratio (i.e. fresh P uptake from tested phosphate divided by fresh P uptake from standard phosphate) was independent of the rate of application. It was therefore suggested that various phosphorus sources be evaluated by measuring the fresh P uptake for a single rate of application.     

Evidence for critical-period programming of intestinal transport function: variations in the dietary ratio of polyunsaturated to saturated fatty acids alters ontogeny of the rat intestine

2-week isocaloric modifications in the dietary ratio of polyunsaturated/saturated fatty acids (P/S) alters intestinal transport in rats. This study was undertaken to test the hypotheses that (1) the fatty acid composition of a nutritionally adequate diet in early life has lasting consequences for active and passive intestinal transport processes; and (2) early life feeding experiences with diets of varying fatty acid composition influence the intestines' ability to adaptively up- or down-regulate intestinal transport in later life. Female Sprague-Dawley rats were weaned onto S or P and were maintained on these diets for 2, 10 or 12 weeks. An in vitro uptake technique was used in which the bulk phase was vigorously stirred to reduce the effective resistance of the intestinal unstirred water layer. P decreased and S increased the uptake of glucose, and this effect was progressive from 2 to 12 weeks. Switching from a P to an S diet decreased jejunal but increased ileal uptake of glucose, whereas switching from an S to a P diet was associated with a decline in both the jejunal and the ileal uptake of glucose. The ileal uptake of galactose increased as the animals grew on either P or S. Switching from P to S resulted in a decline in ileal uptake of galactose, whereas the opposite effect was observed when switching from S to P. The effect of feeding P or S on hexose uptake was influenced by the animals' dietary history: ileal glucose and galactose uptake was lower in animals fed P at an early age (PSP) than in animals fed P for the first time in later life (SSP). Jejunal glucose and galactose uptake was also lower in animals fed S at an early age (SPS) than in those fed S for the first time in later life (PPS). The alterations in the uptake of long-chain saturated and unsaturated fatty acids and cholesterol did not progress with longer periods of feeding, and in the jejunum, lipid uptake did not change when switching from P to S or S to P. Early feeding with P (PSP vs. SSP) was associated with lower jejunal uptake of 18:3 and lower ileal uptake of 12:0, whereas previous feeding with S (SPS vs. PPS) was associated with lower ileal uptake of cholesterol. The changes in uptake of hexoses and lipids was not explained by differences in the animals' food consumption, body or intestinal weight or mucosal surface area.(ABSTRACT TRUNCATED AT 400 WORDS)     

Phosphate uptake in rat skeletal muscle is reduced during isometric contractions.

During contractions, there is a net efflux of phosphate from skeletal muscle, likely because of an elevated intracellular inorganic phosphate (P(i)) concentration. Over time, contracting muscle could incur a substantial phosphate deficit unless P(i) uptake rates were increased during contractions. We used the perfused rat hindquarter preparation to assess [(32)P]P(i) uptake rates in muscles at rest or over a range of energy expenditures during contractions at 0.5, 3, or 5 Hz for 30 min. P(i) uptake rates were reduced during contractions in a pattern that was dependent on contraction frequency and fiber type. In soleus and red gastrocnemius, [(32)P]P(i) uptake rates declined by approximately 25% at 0.5 Hz and 50-60% at 3 and 5 Hz. Uptake rates in white gastrocnemius decreased by 65-75% at all three stimulation frequencies. These reductions in P(i) uptake are not likely confounded by changes in precursor [(32)P]P(i) specific activity in the interstitium. In soleus and red gastrocnemius, declines in P(i) uptake rates were related to energy expenditure over the contraction duration. These data imply that P(i) uptake in skeletal muscle is acutely modulated during contractions and that decreases in P(i) uptake rates, in combination with expected increases in P(i) efflux, exacerbate the net loss of phosphate from the cell. Enhanced uptake of P(i) must subsequently occur because skeletal muscle typically maintains a relatively constant total phosphate pool.     

First observation of diffusion-limited plant root phosphorus uptake from nutrient solution

Diffusion towards the root surface has recently been shown to control the uptake of metal ions from solutions. The uptake flux of phosphorus (P) from solutions often approaches the maximal diffusion flux at low external concentrations, suggesting diffusion-controlled uptake also for P. Potential diffusion limitation in P uptake from nutrient solutions was investigated by measuring P uptake of Brassica napus from solutions using P-loaded Al(2) O(3) nanoparticles as mobile P buffer. At constant, low free phosphate concentration, plant P uptake increased up to eightfold and that of passive, diffusion-based samplers up to 40-fold. This study represents the first experimental evidence of diffusion-limited P uptake by plant roots from nutrient solution. The Michaelis constant of the free phosphate ion obtained in unbuffered solutions (K(m) = 10.4 μmol L(-1) ) was 20-fold larger than in the buffered system (K(m) ～0.5 μmol L(-1) ), indicating that K(m) s determined in unbuffered solutions do not represent the transporter affinity. Increases in the P uptake efficiency of plants by increasing the carrier affinity are therefore unlikely, while increased root surface area or exudation of P-solubilizing compounds are more likely to enhance P uptake. Furthermore, our results highlight the important role natural nanoparticles may have in plant P nutrition.     

Soil solution phosphate,root uptake kinetics and nutrient acquisition: implications for a patchy soil environment

Summary The importance of increased root phosphate (P) uptake kinetics, root proliferation and local increases of soil solution P (P₁) for P acquisition from fertile soil microsites was explored with a simulation model and calculated uptake was compared with experimental data. Based on the partitioning of added P in microsites to P₁ and P adsorbed on soil particles and the results of a dual-isotope-labeling experiment (Caldwell et al. 1991a), acquisition of P from the fertile microsites was some 20 X that of uptake from an equal volume of soil which received only water. Simulations were in general agreement and also showed that elevation of root P uptake kinetics could contribute more to the increased acquisition than did root proliferation under these circumstances. Although increased physiological uptake capacity for P has generally been considered to be of little benefit because of diffusion limitation, in patchy soil environments selective elevation of P uptake kinetics in fertile microsites may be of considerable benefit. These tests were conducted in calcareous soil which releases much less P into the soil solution than do many other soils. In many noncalcareous soils the benefits of selective elevation of root uptake kinetics would likely be greater.     

Age-related changes in calcium and phosphorus uptake by rat small intestine

The purpose of these experiments was to determine whether there are changes in intestinal Ca and P uptake with age and whether the regulation of Ca and P uptake changes with age. Experiments were performed in male Fischer 344 rats aged 2-3 months (young), 12-14 months (adult) and 22-24 months (old). Ca and P uptake were measured simultaneously by incubating everted intestinal sacs in a buffered salt solution containing radiolabeled 0.25 mM Ca and 1.0 mM P for 15 min. Ca uptake declined by over 50% with age in the duodenum, and P uptake showed a similar decline in both the duodenum and jejunum. The biggest decrease was seen between the young and adult age groups. These decreases in uptake were paralleled by decreases in serum 1,25-dihydroxyvitamin D with age. Administration of 1,25-dihydroxyvitamin D-3 increased Ca uptake by 50-65% in the duodenum and increased P uptake by 85-120% in the duodenum and jejunum of both young and adult rats. Although 1,25-dihydroxyvitamin D-3 increased uptake by about the same percentage in each age group, the maximal uptake was much greater in the young than in the adult. Feeding a low-Ca diet increased duodenal Ca uptake by 68% and increased serum 1,25-dihydroxyvitamin D over 2-fold in young rats. There was no significant increase in either parameter in adult rats fed a low-Ca diet. However, duodenal P uptake was stimulated by a low-Ca diet by 87% in young rats and by 51% in adult rats. These results demonstrate that there is an age-related decline in Ca and P uptake by the intestinal mucosa. In addition, there is decreased capacity of 1,25-dihydroxyvitamin D-3 and a low-Ca diet to stimulate intestinal uptake in the adult.     

Variation in phosphorus uptake efficiency by genotypes of cowpea (Vigna unguiculata) due to differences in root and root hair length and induced rhizosphere processes

The lengths of roots and root hairs and the extent of root-induced processes affect phosphorus (P) uptake efficiency by plants. To assess the influence of variation in the lengths of roots and root hairs and rhizosphere processes on the efficiency of soil phosphorus (P) uptake, a pot experiment with a low-P soil and eight selected genotypes of cowpea (Vigna unguiculata (L) WALP) was conducted. Root length, root diameter and root hair length were measured to estimate the soil volume exploited by roots and root hairs. The total soil P was considered as a pool of Olsen-P, extractable with 0.5 M NaHCO₃ at pH 8.5, and a pool of non-Olsen-P. Model calculations were made to estimate P uptake originated from Olsen-P in the root hair zone and the Olsen-P moving by diffusion into the root hair cylinder and non-Olsen-P uptake. The mean uptake rate of P and the mean rate of non-Olsen-P depletion were also estimated. The genotypes differed significantly in lengths of roots and root hairs, and in P uptake, P uptake rates and growth. From 6 to 85% of total P uptake in the soil volume exploited by roots and root hairs was absorbed from the pool of non-Olsen-P. This indicates a considerable activity of root-induced rhizosphere processes. Hence the large differences show that traits for more P uptake-efficient plants exist in the tested cowpea genotypes. This opens the possibility to breed for more P uptake-efficient varieties as a way to bring more sparingly soluble soil P into cycling in crop production and obtain capitalisation of soil P reserves.     

Characterization of Xylose Uptake in the Yeasts Pichia heedii and Pichia stipitis

The kinetics of xylose uptake were investigated in the efficient xylose fermenter Pichia stipitis and in the more readily genetically manipulated, strictly respiratory yeast Pichia heedii. Both yeasts demonstrated more than one xylose uptake system, differing in substrate affinity. The K_m of high-affinity xylose uptake in both organisms was similar to that of the efficient high-affinity glucose uptake system of Saccharomyces cerevisiae. In P. heedii, low-affinity xylose uptake was enhanced with growth on 2% but not 0.05% xylose and high-affinity uptake was reduced. In contrast to glucose uptake, xylose uptake in P. heedii was inhibited by dinitrophenol. Dinitrophenol inhibited both glucose and xylose uptake by P. stipitis. Glucose uptake was not inhibited by a 100-fold molar excess of xylose in P. heedii. It is suggested that xylose uptake in P. heedii is via a carrier system(s) distinct from those for glucose uptake.     

Effects of Substance P on Carbachol-Stimulated 45Ca2+ Uptake into Cultured Adrenal Chromaffin Cells

Substance P is known to modulate acetylcholine-induced catecholamine release from adrenal chromaffin cells. To investigate the mechanisms involved in this modulation, the present study examined the effects of substance P on net 45Ca2+ fluxes in cultures of bovine adrenal chromaffin cells. Two effects of substance P were observed: (1) Substance P inhibited carbachol-induced 45Ca2+ uptake and 45Ca2+ efflux and (2) substance P protected against desensitization of carbachol-induced 45Ca2+ uptake and 45Ca2+ efflux. Thus substance P modulates two other cholinergic responses, 45Ca2+ uptake and 45Ca2+ efflux, in a manner similar to its modulation of catecholamine release. The results also indicate that substance P's inhibition of net carbachol-induced 45Ca2+ uptake is due to inhibition of 45Ca2+ uptake rather than enhancement of 45Ca2+ efflux. Substance P almost completely inhibited carbachol-induced 45Ca2+ uptake in both Na+-containing and Na+-free media, suggesting that substance P can inhibit the uptake of 45Ca2+ induced by carbachol regardless of whether 45Ca2+ is taken up through voltage-sensitive or acetylcholine receptor-linked channels. However, substance P produced only a small inhibition of K+-induced 45Ca2+ uptake, indicating that substance P does not interact directly with voltage-sensitive Ca2+ channels. In addition, substance P's inhibition of carbachol-induced 45Ca2+ uptake was noncompetitive with respect to Ca2+, were unable to overcome substance P's inhibition of [3H]-norepinephrine ( [3H]NE) release. It is concluded that substance P does not interact directly with Ca2+ channels in bovine adrenal chromaffin cells.     

Phosphorus uptake from different sources of phosphatic fertilizers by maize and wheat at two stages of growth

The results of pot experiments on wheat and maize with³²P labelled phosphatic fertilizers showed that P uptake after one month of sowing and at ear emergence in case of wheat has significant positive correlations with dry matter yield where as P uptake after one month of sowing has only significant positive correlation with dry matter yield and P uptake at tasseling has no correlation with dry matter yield in case of maize. P uptake and P concentration have significant correlation at both the stages of growth in case of wheat but P uptake from fertilizer and its respective concentration has only significant correlation at both the stages in case of maize.     

The stoichiometry of nitrogen and phosphorus spiralling in heterotrophic and autotrophic streams

1. Nutrient spiralling provides a conceptual framework and a whole‐system approach to investigate ecosystem responses to environmental changes. We use spiralling metrics to examine how the coupling of nitrogen and phosphorus uptake varies between streams dominated by either heterotrophic (i.e. bacteria‐dominated) or autotrophic (algal‐dominated) microbial communities. 2. Algae generally exhibit greater capacity to store nutrients than bacteria because of differences in cellular structures. These differences led us to hypothesise that the uptake of N and P in heterotrophic ecosystems should have reduced stoichiometric variation in response to changes in supply N : P compared to autotrophic ecosystems when assimilation dominates nutrient uptake. 3. To test this hypothesis, we used an array of serial nutrient additions in several streams in the South Fork Eel River watershed in Northern California. In one set of experiments, N and P were added alone and simultaneously in separate experiments to two small, heterotrophic streams to assess uptake rates and interactions between nutrient cycles. In a second set of experiments, N and P were added simultaneously at a range of N : P in one heterotrophic and one autotrophic stream to assess differences in uptake responses to changes in supply N : P. 4. Results of these experiments suggest two important conclusions. First, increased N supply significantly shortened P uptake lengths, while P addition had little impact on N uptake in both streams, indicating that uptake of non‐limiting nutrients is tightly coupled to the availability of the limiting element. Second, changes in P uptake and uptake ratios (U_N : U_P) with increased supply N : P supported our hypothesis that heterotrophic streams are more homeostatic in their responses to changes in nutrient supply than autotrophic streams, suggesting that physiological controls on nutrient use scale up to influence ecosystem‐scale patterns in nutrient cycling.     

Genotypic differences in the presence of hairs on roots and gynophores of peanuts (Arachis hypogaea L.) and their significance for phosphorus uptake

Root hairs substantially increase the surface area of plant roots with positive effects for phosphorus (P) uptake, but the ability of peanuts to form root hairs has been questioned. The aim was to examine hair development on roots and gynophores of a variety of peanut genotypes and to relate genotypic differences in hair formation to differences in P uptake. Five out of eighteen genotypes completely lacked hairs on both organs whereas others consistently developed hairs on roots and gynophores, although with considerable variation in hair density. The ability to form root hairs as well as root hair density concurred with the presence and density of hairs on gynophores, suggesting a possible connection between both developmental processes. The contribution of root hairs to P uptake was studied in three genotypes differing in hair density. The final amount of P taken up by roots did not differ between genotypes but two distinct P uptake strategies could be identified. The genotype lacking root hairs maintained P uptake due to the development of a large root system whereas densely covered roots of genotype 'Wasedairyu' were three times as efficient in extracting P from a P-deficient soil. Furthermore P uptake through gynophores contributed about 20% to the total P uptake of Wasedairyu but only insignificant amounts to other genotypes. The ability to form hairs on roots and gynophores can therefore be seen as an adaptation to low P availability and if combined with a large root system, could substantially increase the tolerance of peanuts to P deficiency.     

Effects of phosphate and pH stress on the growth and function of apple roots

Summary Effects of phosphate and pH stress on the growth and uptake functions of apple roots were studied over a period of fourteen days using split-root (2-way) seedlings in solution culture. The level of P fed to either or both halves of the root system was varied and a demineralized water control was also included. pH treatments consisted of using acidic nutrient solutions (pH 3 to 4) or nutrient solutions adjusted to pH 5.0 before use.Solution pH proved of paramount importance for the expression of P deficiency effects on root growth and water uptake. Where initial solution pH was favourable for root growth (pH 5), P deficiency stimulated root growth and water uptake per seedling even if the stress was localized. On the other hand, acidic solutions and the water control inhibited root growth and water uptake compared with +P controls. Where solution pH was favourable, P stress also led to an increase in the mean length per root versus the +P control suggesting that the plant adapted to stress by developing an exploratory type of root.Water use per seedling was predominantly a function of root size rather than leaf area since the treatments influenced root size to a much greater extent than leaf area. Uptake was positively related to root size in that adjusted solutions gave a higher water use than nonadjusted solutions. However, efficiency of water use per unit weight of root was consistently higher in the nonadjusted solutions and this appeared to be due to the presence of a larger number of root tips per unit weight of root in such solutions compared with root systems in pH adjusted solutions.Uptake of P per half root was higher from pH adjusted than from nonadjusted solutions and was also increased by increasing the P concentration. Further, for any one treatment P uptake per half root increased throughout the experiment indicating that uptake was influenced by root growth. However, in contrast to water uptake, uptake of P per unit weight or per unit surface area of root was not changed by pH adjustment nor was this parameter of uptake concentration dependent. That is, the above-mentioned pH and concentration effects on P uptake were mediated through effects on root growth.Comparing localized versus uniform placement of P, uptake of P was significantly higher from the uniform application. However, uptake from localized placement at pH 5 was markedly higher than uptake under pH stress and therefore if the pH of the medium remains favourable for root growth then the lower value for localized placement could probably be compensated for by further increasing the concentration of P applied.     

How do plants achieve tolerance to phosphorus deficiency? Small causes with big effects

Genotypic differences in phosphorus (P) uptake from P-deficient soils may be due to higher root growth or higher external root efficiency (micrograms of P taken up per square centimeter of root surface area). Both factors are highly interrelated because any additional P provided by externally efficient roots will also stimulate root growth. It will be necessary to separate both factors to identify a primary mechanism to formulate hypotheses on pathways and genes causing genotypic differences in P uptake. For this purpose, a plant growth model was developed for rice (Oryza sativa) grown under highly P-deficient conditions. Model simulations showed that small changes in root growth-related parameters had big effects on P uptake. Increasing root fineness or the internal efficiency for root dry matter production (dry matter accumulated per unit P distributed to roots) by 22% was sufficient to increase P uptake by a factor of three. That same effect could be achieved by a 33% increase in external root efficiency. However, the direct effect of increasing external root efficiency accounted for little over 10% of the 3-fold increase in P uptake. The remaining 90% was due to enhanced root growth as a result of higher P uptake per unit root size. These results demonstrate that large genotypic differences in P uptake from a P-deficient soil can be caused by rather small changes in tolerance mechanisms. Such changes will be particularly difficult to detect for external efficiency because they are likely overshadowed by secondary root growth effects.     

Combining a modelling with a genetic approach in establishing associations between genetic and physiological effects in relation to phosphorus uptake

The Pup1 locus confers tolerance to phosphorus (P) deficiency in rice (Oryza sativa L.). Transferring the Pup1 locus to an intolerant genotype increased P uptake by a factor 3 to 4. Lines with the Pup1 locus maintained higher root growth rates under P deficiency, but only as they started to diverge from intolerant lines in P uptake. It was thus not possible to determine if differences in root growth preceded and caused differences in P uptake or whether high root growth was the result of higher external P uptake efficiency (P influx per root size). The purpose of this paper is to review experimental evidence on the effect of Pup1 in light of recent results in modelling cause-and-effect relations between root growth, external efficiency and P uptake. Model simulations suggested that only very small changes in factors enhancing root growth were needed to explain the effect of Pup1 on P uptake. A 22% increase in root fineness or in internal P utilization efficiency (root dry matter per root P) was sufficient to triple P uptake . External root efficiency had to increase by 33 to account for the effect of Pup1. However, the most noticeable effect of increases in external efficiency was a subsequent stimulation of root growth that contributed eight times more to final P uptake compared to the change in external efficiency. Comparisons of model simulations with empirical data suggested that measured differences in external efficiency between Nipponbare and NIL-Pup1 were sufficiently large to account for the increase in P uptake. A segregation analysis using several pairs of contrasting NILs (at the Pup1 locus) further confirmed this as Pup1 co-segregated with external efficiency but not with seedling root growth or internal efficiency.     

How changing root system architecture can help tackle a reduction in soil phosphate (P) levels for better plant P acquisition

The readily available global rock phosphate (P) reserves may run out within the next 50–130 years, causing soils to have a reduced P concentration which will affect plant P uptake. Using a combination of mathematical modelling and experimental data, we investigated potential plant‐based options for optimizing crop P uptake in reduced soil P environments. By varying the P concentration within a well‐mixed agricultural soil, for high and low P (35.5–12.5 mg L^?1 respectively using Olsen's P index), we investigated branching distributions within a wheat root system that maximize P uptake. Changing the root branching distribution from linear (evenly spaced branches) to strongly exponential (a greater number of branches at the top of the soil) improves P uptake by 142% for low‐P soils when root mass is kept constant between simulations. This causes the roots to emerge earlier and mimics topsoil foraging. Manipulating root branching patterns, to maximize P uptake, is not enough on its own to overcome the drop in soil P from high to low P. Further mechanisms have to be considered to fully understand the impact of P reduction on plant development.     

Comparison of acid and alkaline soil and liquid culture growth systems for studies of shoot and root characteristics of white lupin (Lupinus albus L.) genotypes

Four quantitative trait loci (QTLs) for P uptake were previously identified in a rice population that had been developed from a cross between the indica landrace Kasalath (high P uptake) with the japonica cultivar Nipponbare (low P uptake). For further studies, near isogenic lines (NILs) were developed for a major QTL linked to marker C443 on chromosome 12 and for a minor QTL linked to C498 on chromosome 6. On a highly P-deficient upland soil (aerobic conditions), NIL-C443 had three to four times the P uptake of Nipponbare, whereas the advantage of NIL-C498 was in the range of 60–90%. The superiority of NILs over Nipponbare vanished when grown in the same soil under anaerobic paddy conditions. All genotypes had high P uptake when P was supplied at a rate of 60 kg P ha^–1, regardless of soil conditions. These results confirmed the presence of both QTLs and furthermore implied that QTLs affected absorption mechanisms that specifically increased P uptake in a P deficient upland soil.Additional experiments were conducted to investigate if the effect of QTLs is linked to an increase in root growth or due to more efficient P uptake per unit root size (higher root efficiency). Root size did not differ significantly between genotypes in the plus-P treatment. P deficiency, however, reduced the root surface area of Nipponbare by more than 80% whereas NIL-C443 maintained almost half of its non-stress root surface area. The low root growth of Nipponbare observed under P deficiency was probably the result of insufficient P uptake to sustain plant growth, including root growth. Genotypic differences in the ability to maintain root growth, therefore are likely caused by some mechanism that increases the efficiency of roots to access P forms not readily available. This however, only had an effect in aerobic soil. Potential mechanisms leading to higher P uptake of NILs are discussed.     

Plant factors influencing phosphorus uptake by white clover from solution culture

Summary The phosphorus (P) uptake rate of several white clover populations was determined in two solution culture experiments. Populations and cultivars differed in P uptake per plant and per unit root length in both experiments. Correlation and multiple regression analysis showed that differences between populations for P uptake per plant were largely related (r²>80%) to differences in leaf area and absolute growth rate, when plants had been grown at high-P levels, and by differences in root size and absolute growth rate when plants had been grown at low-P levels. Differences between populations for P uptake per unit root length were related (r²≈50%) to leaf area and relative growth rate in experiment 1 and to transpiration rate and water influx in experiment 2, when plants were pretreated at high-P levels. Differences between populations for P uptake per unit root length were negatively related to root size when plants had been grown at low-P levels. On the basis of these and other results it is suggested that P uptake per plant is determined largely by shoot factors. However, P uptake per unit root length is negatively related to root size, because demand for P is largely determined by shoot factors, and so differences in root size lead to an apparent difference in uptake per unit of root size.