Nitrogen depletion enhances endodermal suberization without restricting transporter-mediated root NO3- influx.

Roots vary their permeability to aid radial transport of solutes towards xylem vessels in response to nutritional cues. Nitrogen (N) depletion was previously shown to induce early suberization of endodermal cell walls and reduce hydraulic conductivity of barley roots suggesting reduced apoplastic transport of ions (Armand et al., 2019). Suberization may also limit transcellular ion movement by blocking access to transporters (Barberon et al., 2016). The aim of this study was to confirm that N depletion induced suberization in the roots of barley and demonstrate that this was a specific effect in response to NO3- depletion. Furthermore, in roots with early and enhanced suberization, we assessed their ability for transporter-mediated NO3- influx. N depletion induced lateral root elongation and early and enhanced endodermal suberization of the seminal root of each genotype. Both root to shoot NO3- translocation and net N uptake was half that of plants supplied with steady-state NO3-. Genes with predicted functions in suberin synthesis (HvHORST) and NO3- transport (HvNRT2.2) were induced under N-deplete conditions. N-deplete roots had a higher capacity for high-affinity NO3- influx in early suberized roots than under optimal NO3-. In conclusion, NO3- depletion induced early and enhanced suberization in the roots of barley, however, suberization did not restrict transcellular NO3- transport.

Sodium efflux in plant roots: what do we really know?

The efflux of sodium (Na(+)) ions across the plasma membrane of plant root cells into the external medium is surprisingly poorly understood. Nevertheless, Na(+) efflux is widely regarded as a major mechanism by which plants restrain the rise of Na(+) concentrations in the cytosolic compartments of root cells and, thus, achieve a degree of tolerance to saline environments. In this review, several key ideas and bodies of evidence concerning root Na(+) efflux are summarized with a critical eye. Findings from decades past are brought to bear on current thinking, and pivotal studies are discussed, both "purely physiological", and also with regard to the SOS1 protein, the only major Na(+) efflux transporter that has, to date, been genetically characterized. We find that the current model of rapid transmembrane sodium cycling (RTSC), across the plasma membrane of root cells, is not adequately supported by evidence from the majority of efflux studies. An alternative hypothesis cannot be ruled out, that most Na(+) tracer efflux from the root in the salinity range does not proceed across the plasma membrane, but through the apoplast. Support for this idea comes from studies showing that Na(+) efflux, when measured with tracers, is rarely affected by the presence of inhibitors or the ionic composition in saline rooting media. We conclude that the actual efflux of Na(+) across the plasma membrane of root cells may be much more modest than what is often reported in studies using tracers, and may predominantly occur in the root tips, where SOS1 expression has been localized.

Flux measurements of cations using radioactive tracers.

Standard procedures for the tracing of ion fluxes into roots of plants are described here, with emphasis on cations, especially potassium (K(+)). We focus in particular on the measurement of unidirectional influx by use of radiotracers and provide a brief introduction to compartmental analysis by tracer efflux (CATE).

The potential for nitrification and nitrate uptake in the rhizosphere of wetland plants: a modelling study.

BACKGROUND AND AIMS: It has recently found that lowland rice grown hydroponically is exceptionally efficient in absorbing NO3-, raising the possibility that rice and other wetland plants growing in flooded soil may absorb significant amounts of NO3- formed by nitrification of NH4+ in the rhizosphere. This is important because (a) this NO3- is otherwise lost through denitrification in the soil bulk; and (b) plant growth and yield are generally improved when plants absorb their nitrogen as a mixture of NO3- and NH4+ compared with growth on either N source on its own. A mathematical model is developed here with which to assess the extent of NO3- absorption from the rhizosphere by wetland plants growing in flooded soil, considering the important plant and soil processes operating. METHODS: The model considers rates of O2 transport away from an individual root and simultaneous O2 consumption in microbial and non-microbial processes; transport of NH4+ towards the root and its consumption in nitrification and uptake at the root surface; and transport of NO3- formed from NH4+ towards the root and its consumption in denitrification and uptake by the root. The sensitivity of the model's predictions to its input parameters is tested over the range of conditions in which wetland plants grow. KEY RESULTS: The model calculations show that substantial quantities of NO3- can be produced in the rhizosphere of wetland plants through nitrification and taken up by the roots under field conditions. The rates of NO3- uptake can be comparable with those of NH4+. The model also shows that rates of denitrification and subsequent loss of N from the soil remain small even where NO3- production and uptake are considerable. CONCLUSIONS: Nitrate uptake by wetland plants may be far more important than thought hitherto. This has implications for managing wetland soils and water, as discussed in this paper.

Constancy of nitrogen turnover kinetics in the plant cell: insights into the integration of subcellular N fluxes.

Compartmental analysis with 13N was used to determine cytosolic nitrate (NO3-) pools, and their turnover rates, in roots of intact barley (Hordeum vulgare L. cv Klondike) seedlings. Influx, efflux, flux to the vacuole and assimilation, and flux to the xylem, varied as much as 300-fold over a wide range of external NO3- conditions. By contrast, the kinetic constant kc describing cytosolic NO3- turnover varied by less than 4% from a mean value of 0.0407 min(-1). Accordingly, cytosolic NO3- pools varied linearly with influx. A literature survey showed that kc constancy is observed with both NO3- and ammonium (NH4+) fluxes in many plant species, including H. vulgare, Arabidopsis thaliana, Picea glauca, and Oryza sativa. The regulatory system implied by this phenomenon is fundamentally different from that of potassium (K+) fluxes, in which cytosolic pool size is held constant while kc varies with external K+ concentrations. We further present data showing that barley plants, grown on one steady-state concentration of NH4+, restore kc within minutes of exposure to new, non-steady-state, NH4+ concentrations. We propose the existence of a high-fidelity mechanism governing the timing of cytosolic N turnover, and discuss its implications for attempts to improve plants biotechnologically.

Futile transmembrane NH4(+) cycling: a cellular hypothesis to explain ammonium toxicity in plants.

Most higher plants develop severe toxicity symptoms when grown on ammonium (NH(4)(+)) as the sole nitrogen source. Recently, NH(4)(+) toxicity has been implicated as a cause of forest decline and even species extinction. Although mechanisms underlying NH(4)(+) toxicity have been extensively sought, the primary events conferring it at the cellular level are not understood. Using a high-precision positron tracing technique, we here present a cell-physiological characterization of NH(4)(+) acquisition in two major cereals, barley (Hordeum vulgare), known to be susceptible to toxicity, and rice (Oryza sativa), known for its exceptional tolerance to even high levels of NH(4)(+). We show that, at high external NH(4)(+) concentration ([NH(4)(+)](o)), barley root cells experience a breakdown in the regulation of NH(4)(+) influx, leading to the accumulation of excessive amounts of NH(4)(+) in the cytosol. Measurements of NH(4)(+) efflux, combined with a thermodynamic analysis of the transmembrane electrochemical potential for NH(4)(+), reveal that, at elevated [NH(4)(+)](o), barley cells engage a high-capacity NH(4)(+)-efflux system that supports outward NH(4)(+) fluxes against a sizable gradient. Ammonium efflux is shown to constitute as much as 80% of primary influx, resulting in a never-before-documented futile cycling of nitrogen across the plasma membrane of root cells. This futile cycling carries a high energetic cost (we record a 40% increase in root respiration) that is independent of N metabolism and is accompanied by a decline in growth. In rice, by contrast, a cellular defense strategy has evolved that is characterized by an energetically neutral, near-Nernstian, equilibration of NH(4)(+) at high [NH(4)(+)](o). Thus our study has characterized the primary events in NH(4)(+) nutrition at the cellular level that may constitute the fundamental cause of NH(4)(+) toxicity in plants.

Comparative kinetic analysis of ammonium and nitrate acquisition by tropical lowland rice: implications for rice cultivation and yield potential.

Nitrogen limitation compromises the realization of yield potential in cereals more than any other single factor. In rice, the world's most important crop species, the assumption has long been that only ammonium-N is efficiently utilized. Consequently, nitrate utilization has been largely ignored, although fragmentary data have suggested that growth could be substantial on nitrate. Using the short-lived radiotracer 13 N, we here provide direct comparisons of root transmembrane fluxes and cytoplasmic pool sizes for nitrate- and ammonium-N in a major variety of Indica rice (Oryza sativa), and show that nitrate acquisition is not only of high capacity and efficiency but is superior to that of ammonium. We believe our results have implications for rice breeding and molecular genetics as well as the design of water-management and fertilization regimes. Potential strategies to harness this hitherto unexplored N-utilization potential are proposed.

AtAMT1 gene expression and NH4+ uptake in roots of Arabidopsis thaliana: evidence for regulation by root glutamine levels.

The mechanisms involved in regulating high-affinity ammonium (NH4+) uptake and the expression of the AtAMT1 gene encoding a putative high-affinity NH4+ transporter were investigated in the roots of Arabidopsis thaliana. Under conditions of steady-state nitrogen (N) supply, transcript levels of the AtAMT1 gene and Vmax values for high-affinity 13NH4+ influx were inversely correlated with levels of N provision. Following re-supply of NH4NO3 to N-starved plants, AtAMT1 mRNA levels and 13NH4+ influx declined rapidly but remained high when the conversion of NH4+ to glutamine (Gln) was blocked with methionine sulfoximine (MSX). This result demonstrates that end products of NH4+ assimilation, rather than NH4+ itself, are responsible for regulating AtAMT1 gene expression. Consistent with this hypothesis, AtAMT1 gene expression and NH4+ influx were suppressed by provision of Gln alone, or together with NH4NO3 plus MSX. Furthermore, AtAMT1 transcript levels and 13NH4+ influx were negatively correlated with root Gln concentrations, following re-supply of N to N-starved plants. In addition to this level of control, the data suggest that high cytoplasmic [NH4+] may inhibit NH4+ influx.

Kinetics of NH4+ Influx in Spruce.

Influxes of 13NH4+ across the root plasmalemma were measured in intact seedlings of Picea glauca (Moench) Voss. Two kinetically distinct uptake systems for NH4+ were identified. In N-deprived plants, a Michaelis-Menten-type high-affinity transport system (HATS) operated in a 2.5 to 350 [mu]M range of external NH4+ concentration ([NH4 +]o). The Vmax of this HATS was 1.9 to 2.4 [mu]mol g-1 h-1, and the Km was 20 to40 [mu]M. At [NH4+]o from 500 [mu]M to 50 mM, a linear low-affinity system (LATS) was apparent. Both HATS and LATS were constitutive. A time-dependence study of NH4+ influx in previously N-deprived seedlings revealed a small transient increase of NH4+ influx after 24 h of exposure to 100 [mu]M [NH4+]o. This was followed by a decline of influx to a steady-state value after 4 d. In seedlings exposed to 100 [mu]M external NO3- concentration for 3 d, the Vmax for NH4+ uptake by HATS was increased approximately 30% compared to that found in N-deprived seedlings, whereas LATS was down-regulated. The present study defines the much higher uptake capacity for NH4+ than for N03- in seedlings of this species.

Analysis of 13NH4+ Efflux in Spruce Roots (A Test Case for Phase Identification in Compartmental Analysis).

13NH4+-efflux analyses were conducted with roots of intact Picea glauca (Moench) Voss. seedlings at external NH4+ concentrations of 100 [mu]M and 1.5 mM. Three kinetically distinct phases were identified with half-lives of exchange of approximately 2 s, 30 s, and 14 min. The presumed identities of the subcellular compartments corresponding to these phases were confirmed by several techniques, including pretreatment of roots (a) at 75[deg]C or with SDS, (b) with [alpha]-keto-glutarate or L-methionine-DL-sulfoximine, (c) at elevated levels of Ca2+, and (d) at low pH or with Al3+ at low pH. Treatments a and b selectively influenced phase III without affecting phases I and II. Similarly, treatment c selectively perturbed phase II, and treatment d affected phases II and III. Based on these findings and the assumption of an in-series arrangement of root cell compartments, it was concluded that phase III corresponded to the cytoplasm, phase II corresponded to the Donnan free space, and phase I corresponded to a film of solution adhering to the root surface.

Kinetics of NO3- Influx in Spruce.

Influxes of 13NO3- across the root plasmalemma were measured in intact seedlings of Picea glauca (Moench) Voss. Three kinetically distinct uptake systems for NO3- were identified. In seedlings not previously exposed to external NO3-, a single Michaelis-Menten-type constitutive high-affinity transport system (CHATS) operated in a 2.5 to 500 [mu]M range of external NO3- [NO3-]o. The Vmax of this system was 0.1 [mu]mol g-1 h-1, and the Km was approximately 15 [mu]M. Following exposure to NO3- for 3 d, this CHATS activity was increased approximately 3-fold, with no change of Km. In addition, a NO3--inducible high-affinity system became apparent with a Km of approximately 100[mu]M. The combined Vmax for these discrete saturable components was 0.7 [mu]mol g-1 h-1. In both uninduced and induced plants a linear low-affinity system, additive to CHATS and an NO3--inducible high-affinity system, operated at [NO3-]o [greater than or equal to] 1 mM. The time taken to achieve maximal rates of uptake (full induction) was 2 d from 1.5 mM [NO3-]o and 3 d from 200 [mu]M [NO3-]o.