Stephen D. Tyerman

Wheat grain yield on saline soils is improved by an ancestral Na+ transporter gene

The ability of wheat to maintain a low sodium concentration ([Na+]) in leaves correlates with improved growth under saline conditions. This trait, termed Na+ exclusion, contributes to the greater salt tolerance of bread wheat relative to durum wheat. To improve the salt tolerance of durum wheat, we explored natural diversity in shoot Na+ exclusion within ancestral wheat germplasm. Previously, we showed that crossing of Nax2, a gene locus in the wheat relative Triticum monococcum into a commercial durum wheat (Triticum turgidum ssp. durum var. Tamaroi) reduced its leaf [Na+] (ref. 5). Here we show that a gene in the Nax2 locus, TmHKT1;5-A, encodes a Na+-selective transporter located on the plasma membrane of root cells surrounding xylem vessels, which is therefore ideally localized to withdraw Na+ from the xylem and reduce transport of Na+ to leaves. Field trials on saline soils demonstrate that the presence of TmHKT1;5-A significantly reduces leaf [Na+] and increases durum wheat grain yield by 25% compared to near-isogenic lines without the Nax2 locus.

The Role of Plasma Membrane Intrinsic Protein Aquaporins in Water Transport through Roots: Diurnal and Drought Stress Responses Reveal Different Strategies between Isohydric and Anisohydric Cultivars of Grapevine

We report physiological and anatomical characteristics of water transport across roots grown in soil of two cultivars of grapevine (Vitis vinifera) differing in response to water stress (Grenache, isohydric; Chardonnay, anisohydric). Both cultivars have similar root hydraulic conductances (Lo; normalized to root dry weight) that change diurnally. There is a positive correlation between Lo and transpiration. Under water stress, both cultivars have reduced minimum daily Lo (predawn) attributed to the development of apoplastic barriers. Water-stressed and well-watered Chardonnay had the same diurnal change in amplitude of Lo, while water-stressed Grenache showed a reduction in daily amplitude compared with well-watered plants. Hydraulic conductivity of root cortex cells (Lpcell) doubles in Chardonnay but remains unchanged in Grenache. Of the two most highly expressed plasma membrane intrinsic protein (PIP) aquaporins in roots (VvPIP1;1 and VvPIP2;2), only VvPIP2;2 functions as a water channel in Xenopus laevis oocytes. VvPIP1;1 interacts with VvPIP2;2 to induce 3-fold higher water permeability. These two aquaporins are colocated in the root from in situ hybridization and immunolocalization of VvPIP1 and VvPIP2 subfamily members. They occur in root tip, exodermis, root cortex (detected up to 30 mm), and stele. VvPIP2;2 mRNA does not change diurnally or with water stress, in contrast to VvPIP1;1, in which expression reflects the differences in Lo and Lpcell between cultivars in their responses to water stress and rewatering. VvPIP1;1 may regulate water transport across roots such that transpirational demand is matched by root water transport capacity. This occurs on a diurnal basis and in response to water stress that corresponds to the difference in drought tolerance between the cultivars.

Aquaporins: Highly Regulated Channels Controlling Plant Water Relations

Aquaporins are highly regulated water channels that contribute to the control of water movement at the cell, tissue, and organ levels and, hence, to the overall plant water relations in varying environmental conditions. Plant growth and development are dependent on tight regulation of water movement. Water diffusion across cell membranes is facilitated by aquaporins that provide plants with the means to rapidly and reversibly modify water permeability. This is done by changing aquaporin density and activity in the membrane, including posttranslational modifications and protein interaction that act on their trafficking and gating. At the whole organ level aquaporins modify water conductance and gradients at key “gatekeeper” cell layers that impact on whole plant water flow and plant water potential. In this way they may act in concert with stomatal regulation to determine the degree of isohydry/anisohydry. Molecular, physiological, and biophysical approaches have demonstrated that variations in root and leaf hydraulic conductivity can be accounted for by aquaporins but this must be integrated with anatomical considerations. This Update integrates these data and emphasizes the central role played by aquaporins in regulating plant water relations.

New potent inhibitors of aquaporins: silver and gold compounds inhibit aquaporins of plant and human origin

Silver and gold compounds were tested as potential inhibitors of aquaporins of plant‐ and human origin. Silver as AgNO3 or silver sulfadiazine inhibited with high potency (EC50 1–10 μM) the water permeability of the peribacteroid membrane from soybean (containing Nodulin 26), the water permeability of plasma membrane from roots (containing plasma membrane integral proteins), and the water permeability of human red cells (containing aquaporin 1). Gold as HAuCl4 was less effective but still inhibited peribacteroid membrane water permeability (EC50=10 μM). Silver and gold are more potent inhibitors of aquaporins than the presently widely used mercury containing compounds.

Mechanisms of Cl- transport contributing to salt tolerance

Mechanisms of Cl(-) transport in plants are poorly understood, despite the importance of minimizing Cl(-) toxicity for salt tolerance. This review summarizes Cl(-) transport processes in plants that contribute to genotypic differences in salt tolerance, identifying key traits from the cellular to whole-plant level. Key aspects of Cl(-) transport that contribute to salt tolerance in some species include reduced net xylem loading, intracellular compartmentation and greater efflux of Cl(-) from roots. We also provide an update on the biophysics of anion transport in plant cells and address issues of charge balance, selectivity and energy expenditure relevant to Cl(-) transport mechanisms. Examples are given of anion transport systems where electrophysiology has revealed possible interactions with salinity. Finally, candidate genes for anion transporters are identified that may be contributing to Cl(-) movement within plants during salinity. This review integrates current knowledge of Cl(-) transport mechanisms to identify future pathways for improving salt tolerance.

Root ion channels and salinity

Abstract A variety of ion channels has now been identified in plant cell membranes that is likely to have key roles in both toxicity to high salt (NaCl) and tolerance mechanisms. In this review we examine the function of cation and anion channels under saline conditions and mainly for root cells. This is done in context with other active and passive transport processes, and taking into account the voltage sensitivity of the channels and the likely passive gradients for Na+ and Cl−. For the plasma membrane channels there are secondary effects of high external salt and low external Ca2+ activity that additionally influence both the types of channels that are involved and the way that the channels interact via membrane voltage. Recent work on cereal roots indicates that there are voltage-independent non-selective cation channels in the plasma membrane that may be primarily responsible for Na+ influx. At least one of these types of channels is sensitive to external calcium. For wheat and maize there is a good correlation between the Ca2+ sensitivity of Na+ influx into roots and the Ca2+-sensitivity of the Na+ currents through the non-selective cation channel. Anion channels in the plasma membrane may allow transient passive influx of Cl− under some circumstances but more information is required on the Cl− gradient across the plasma membrane which may change rapidly after an increase in external salinity. Anion efflux channels could be involved in the regulation of Cl− concentration in the cytoplasm. There is now sufficient background information to identify targets for study on horticultural plants. It is very likely that non-selective cation channels that are sensitive to external Ca2+ will be present in root membranes of horticultural plants. With the methods available to select specific cell-types it should be possible to test this quickly on the cells that are important for root selectivity; for example, passage cells in the hypodermis of citrus.

The identification of aluminium-resistance genes provides opportunities for enhancing crop production on acid soils

Acid soils restrict plant production around the world. One of the major limitations to plant growth on acid soils is the prevalence of soluble aluminium (Al(3+)) ions which can inhibit root growth at micromolar concentrations. Species that show a natural resistance to Al(3+) toxicity perform better on acid soils. Our understanding of the physiology of Al(3+) resistance in important crop plants has increased greatly over the past 20 years, largely due to the application of genetics and molecular biology. Fourteen genes from seven different species are known to contribute to Al(3+) tolerance and resistance and several additional candidates have been identified. Some of these genes account for genotypic variation within species and others do not. One mechanism of resistance which has now been identified in a range of species relies on the efflux of organic anions such as malate and citrate from roots. The genes controlling this trait are members of the ALMT and MATE families which encode membrane proteins that facilitate organic anion efflux across the plasma membrane. Identification of these and other resistance genes provides opportunities for enhancing the Al(3+) resistance of plants by marker-assisted breeding and through biotechnology. Most attempts to enhance Al(3+) resistance in plants with genetic engineering have targeted genes that are induced by Al(3+) stress or that are likely to increase organic anion efflux. In the latter case, studies have either enhanced organic anion synthesis or increased organic anion transport across the plasma membrane. Recent developments in this area are summarized and the structure-function of the TaALMT1 protein from wheat is discussed.

Pathways for the permeation of Na+ and Cl− into protoplasts derived from the cortex of wheat roots

Sodium permeation into cortex cells of wheat roots was examined under conditions of high external NaCI and low Ca(2+). Two types of K(+) inward rectifier were observed in some cells. The time-dependent K(+) inward rectifier was Ca(2+)-sensitive, increasing in magnitude as external Ca(2+) was decreased from 10 mM to 0.1 mM, but did not show significant permeability to Na(+). However, the spiky inward rectifier showed significant Na+ permeation at Ca(2+) concentrations of 1 and 10 mM. In cells that initially did not show K(+) inward rectifier channels, fast and sometimes slowly activating whole-cell inward currents were induced at membrane potentials negative of zero with high external Na(+) and low Ca(2+) concentrations. With 1 mM Ca(2+) in the external solution, large inward currents were carried by Rb(+), Cs(+), K(+), Li(+), and Na(+). The permeability sequence shows that K(+), Rb(+) and Cs(+) are all more permeant than Na(+), which is about equally as permeant as Li(+). When some K(+) was present with high concentrations of Na(+) the inward currents were larger than with K(+) or Na(+) alone. About 60% of the inward current was reversibly blocked when the external Ca(2+) activity was increased from 0.03 mM to 2.7 mM (half inhibition at 0.31 mM Ca(2+) activity). Changes in the characteristics of the current noise indicated that increased Ca(2+) reduced the apparent single channel amplitude. In outside-out patches inward currents were observed at membrane potentials more positive than the equilibrium potentials for K(+) and Cl(-) when the external Na(+) concentration was high. These channels were difficult to analyse but three analysis methods yielded similar conductances of about 30 pS.

Review: Nutrient loading of developing seeds

Interest in nutrient loading of seeds is fuelled by its central importance to plant reproductive success and human nutrition. Rates of nutrient loading, imported through the phloem, are regulated by transport and transfer processes located in sources (leaves, stems, reproductive structures), phloem pathway and seed sinks. During the early phases of seed development, most control is likely to be imposed by a low conductive pathway of differentiating phloem cells serving developing seeds. Following the onset of storage product accumulation by seeds, and, depending on nutrient species, dominance of path control gives way to regulation by processes located in sources (nitrogen, sulfur, minor minerals), phloem path (transition elements) or seed sinks (sugars and major mineral elements, such as potassium). Nutrients and accompanying water are imported into maternal seed tissues and unloaded from the conducting sieve elements into an extensive post-phloem symplasmic domain. Nutrients are released from this symplasmic domain into the seed apoplasm by poorly understood membrane transport mechanisms. As seed development progresses, increasing volumes of imported phloem water are recycled back to the parent plant by process(es) yet to be discovered. However, aquaporins concentrated in vascular and surrounding parenchyma cells of legume seed coats could provide a gated pathway of water movement in these tissues. Filial cells, abutting the maternal tissues, take up nutrients from the seed apoplasm by membrane proteins that include sucrose and amino acid/H+ symporters functioning in parallel with non-selective cation channels. Filial demand for nutrients, that comprise the major osmotic species, is integrated with their release and phloem import by a turgor-homeostat mechanism located in maternal seed tissues. It is speculated that turgors of maternal unloading cells are sensed by the cytoskeleton and transduced by calcium signalling cascades.

Cell-Specific Vacuolar Calcium Storage Mediated by CAX1 Regulates Apoplastic Calcium Concentration, Gas Exchange, and Plant Productivity in Arabidopsis

Mineral elements are often preferentially stored in vacuoles of specific leaf cell types, but the mechanism and physiological role for this phenomenon is poorly understood. We use single-cell analysis to reveal the genetic basis underpinning mesophyll-specific calcium storage in Arabidopsis leaves and a variety of physiological assays to uncover its fundamental importance to plant productivity. The physiological role and mechanism of nutrient storage within vacuoles of specific cell types is poorly understood. Transcript profiles from Arabidopsis thaliana leaf cells differing in calcium concentration ([Ca], epidermis <10 mM versus mesophyll >60 mM) were compared using a microarray screen and single-cell quantitative PCR. Three tonoplast-localized Ca2+ transporters, CAX1 (Ca2+/H+-antiporter), ACA4, and ACA11 (Ca2+-ATPases), were identified as preferentially expressed in Ca-rich mesophyll. Analysis of respective loss-of-function mutants demonstrated that only a mutant that lacked expression of both CAX1 and CAX3, a gene ectopically expressed in leaves upon knockout of CAX1, had reduced mesophyll [Ca]. Reduced capacity for mesophyll Ca accumulation resulted in reduced cell wall extensibility, stomatal aperture, transpiration, CO2 assimilation, and leaf growth rate; increased transcript abundance of other Ca2+ transporter genes; altered expression of cell wall–modifying proteins, including members of the pectinmethylesterase, expansin, cellulose synthase, and polygalacturonase families; and higher pectin concentrations and thicker cell walls. We demonstrate that these phenotypes result from altered apoplastic free [Ca2+], which is threefold greater in cax1/cax3 than in wild-type plants. We establish CAX1 as a key regulator of apoplastic [Ca2+] through compartmentation into mesophyll vacuoles, a mechanism essential for optimal plant function and productivity.