Ground wētā in vines of the Awatere Valley,Marlborough: biology,density and distribution

The endemic New Zealand ground wētā (Hemiandrus sp. ‘promontorius’) has a Naturally Uncommon conservation status. This is because of the paucity of information on its density and distribution. Here, the biology, density and distribution of a population of this wētā found in and around vineyards in the Awatere Valley, Marlborough was studied. Wētā density was assessed in vineyards, paddocks and shrublands in this valley. Soil moisture, penetration resistance, pH and organic matter were recorded at locations with and without wētā. Wētā density in vineyards was significantly higher than in either paddocks or shrub habitats. In vineyards, the density of this insect was significantly higher under-vines than in the inter-rows. Higher numbers of this wētā were found in moist soils that required lower force to burrow. Females laid an average of 55 eggs between March and April, which hatched in September. These findings highlight the intersection between agriculture and conservation.     

Aquaporins and unloading of phloem-imported water in coats of developing bean seeds

Nutrients are imported into developing legume seeds by mass flow through the phloem, and reach developing embryos following secretion from their symplasmically isolated coats. To sustain homeostasis of seed coat water relations, phloem-delivered nutrients and water must exit seed coats at rates commensurate with those of import through the phloem. In this context, coats of developing French bean seeds were screened for expression of aquaporin genes resulting in cloning PvPIP1;1, PvPIP2;2 and PvPIP2;3. These genes were differentially expressed in all vegetative organs, but exhibited their strongest expression in seed coats. In seed coats, expression was localized to cells of the nutrient-unloading pathway. Transport properties of the PvPIPs were characterized by expression in Xenopus oocytes. Only PvPIP2;3 showed significant water channel activity (Pos = 150-200 microm s(-1)) even when the plasma membrane intrinsic proteins (PIPs) were co-expressed in various combinations. Permeability increases to glycerol, methylamine and urea were not detected in oocytes expressing PvPIPs. Transport active aquaporins in native plasma membranes of seed coats were demonstrated by measuring rates of osmotic shrinkage of membrane vesicles in the presence and absence of mercuric chloride and silver nitrate. The functional significance of aquaporins in nutrient and water transport in developing seeds is discussed.     

Nonselective currents and channels in plasma membranes of protoplasts from coats of developing seeds of bean

In developing bean (Phaseolus vulgaris) seeds, phloem-imported nutrients move in the symplast from sieve elements to the ground parenchyma cells where they are transported across the plasma membrane into the seed apoplast. To study the mechanisms underlying this transport, channel currents in ground parenchyma protoplasts were characterized using patch clamp. A fast-activating outward current was found in all protoplasts, whereas a slowly activating outward current was observed in approximately 25% of protoplasts. The two currents had low selectivity for univalent cations, but the slow current was more selective for K(+) over Cl(-) (P(K):P(Cl) = 3.6-4.2) than the fast current (P(K):P(Cl) = 1.8-2.5) and also displayed Ca(2+) selectivity. The slow current was blocked by Ba(2+), whereas both currents were blocked by Gd(3+) and La(3+). Efflux of K(+) from seed coat halves was inhibited 25% by Gd(3+) and La(3+) but was stimulated by Ba(2+) and Cs(+), suggesting that only the fast current may be a component in the pathway for K(+) release. An "instantaneous" inward current observed in all protoplasts exhibited similar pharmacology and permeability for univalent cations to the fast outward current. In outside-out patches, two classes of depolarization-activated cation-selective channels were observed: one slowly activating of low conductance (determined from nonstationary noise to be 2.4 pS) and another with conductances 10-fold higher. Both channels occurred at high density. The higher conductance channel in 10 mM KCl had P(K):P(Cl) = 2.8. Such nonselective channels in the seed coat ground parenchyma cell could function to allow some of the efflux of phloem-imported univalent ions into the seed apoplast.     

Determination of Solute Permeability in Chara Internodes by a Turgor Minimum Method : Effects of External pH

The analysis of Sha'afi et al. (Sha'afi, Rich, Mickulecky, Solomon 1970 J Gen Physiol 55: 427-450) for determining solute permeability in red blood cells has been modified and applied to turgid plant cells. Following the addition of permeating solute to the external medium, a biphasic response of cell turgor can be measured with the pressure probe in isolated internodes of Chara corallina. After an initial decrease in turgor due to water flow (water phase), turgor increases due to the uptake of the solute (solute phase) until the original turgor is reattained. From the pressure/time course in the neighborhood of the minimum turgor, the permeability of the osmotic solute can be determined. The data obtained by the minimum method for rapidly permeating (ethanol, methanol) and slowly permeating (formamide, dimethylformamide) solutes are similar to those calculated from the half-time of pressure changes during the solute phase and to data obtained by other workers using radioactive tracers. The methods employing the pressure probe were applied to examine the effect of high pH (up to pH 11) on the membrane permeability. There appeared to be no effect of high pH on the permeability coefficients, reflection coefficients, and hydraulic conductivity.     

Plasma membrane of Beta vulgaris storage root shows high water channel activity regulated by cytoplasmic pH and a dual range of calcium concentrations

Plasma membrane vesicles isolated by two-phase partitioning from the storage root of Beta vulgaris show atypically high water permeability that is equivalent only to those reported for active aquaporins in tonoplast or animal red cells (Pf=542 microm s(-1)). The values were determined from the shrinking kinetics measured by stopped-flow light scattering. This high Pf was only partially inhibited by mercury (HgCl2) but showed low activation energy (Ea) consistent with water permeation through water channels. To study short-term regulation of water transport that could be the result of channel gating, the effects of pH, divalent cations, and protection against dephosphorylation were tested. The high Pf observed at pH 8.3 was dramatically reduced by medium acidification. Moreover, intra-vesicular acidification (corresponding to the cytoplasmic face of the membrane) shut down the aquaporins. De-phosphorylation was discounted as a regulatory mechanism in this preparation. On the other hand, among divalent cations, only calcium showed a clear effect on aquaporin activity, with two distinct ranges of sensitivity to free Ca2+ concentration (pCa 8 and pCa 4). Since the normal cytoplasmic free Ca2+ sits between these ranges it allows for the possibility of changes in Ca2+ to finely up- or down-regulate water channel activity. The calcium effect is predominantly on the cytoplasmic face, and inhibition corresponds to an increase in the activation energy for water transport. In conclusion, these findings establish both cytoplasmic pH and Ca2+ as important regulatory factors involved in aquaporin gating.     

Pulsing Cl- channels in coat cells of developing bean seeds linked to hypo-osmotic turgor regulation

Seed coat cells in the developing seeds of grain legumes release nutrients to the developing embryo. This occurs into an apoplastic space that separates the maternal (seed coat) and filial (embryo) generations. Protoplasts of seed coat cells from coats of Phaseolus vulgaris L. seeds were isolated and whole-cell current across their plasma membranes was characterized using the patch-clamp technique. A pulsing inward current that displayed a spontaneous activation and voltage-dependent inactivation was observed. The frequency and magnitude of the current pulses were positively dependent on cytoplasmic Cl(-) concentrations and independent of external cations. The pulse current was inhibited by DIDS and La(3+), but not by Gd(3+). Single channel events (conductance=18 pS) could be identified with the inactivating phase of the pulses. Together, these findings are consistent with the current being carried by a burst of Cl(-) efflux through Cl(-)-permeable channels that activate almost simultaneously. Neomycin caused a reversible inhibition of the pulsed current, suggesting that its activation is likely to be modulated by an IP(3)-dependent intracellular Ca(2+) release. The pharmacological profiles of Cl(-) efflux from excised seed coats were comparable with those of the Cl(-) channels in the whole cell configuration, suggesting that the Cl(-) channels may underpin Cl(-) efflux from the seed coats. Efflux of Cl(-) from the seed coats was also stimulated by hypo-osmotic treatment as was the frequency and magnitude of Cl(-) channel in whole-cell patch clamp experiments. This implies that the Cl(-) channels responsible for the pulsed Cl(-) currents are likely to be a component of the turgor-regulatory mechanism in developing bean seeds.     

Water channels in Chara corallina

Water relations parameters ofChara corallina inter-nodes weremeasured using the single cell pressure probe. The effect ofmercurials, which are recognized as non-specific water channelinhibitors, was examined. HgCl₂ concentrations greater than5 mmol m^–3 were found to inhibit hydraulic conductivity{Lp) close to 90%, whereas pCMPS was found to have no effecton Lp. The activation energy of water flow was increased significantlyfrom 21.0 kJ mol^–1 to 45.6 kJ mol^–1, following theapplication of HgCl₂. These results are in accordance with evidencefor Hg²⁺sensitive water channels in the plasma membrane of charophytes(Henzler and Steudle, 1995; Tazawa et al., 1996). The metaboliceffects must, however, be considered in view of the rapid inhibitionof respiration and the depolarization of the membrane potentialwith HgCl₂ concentrations lower than those found to affect Lp.It was possible to measure simultaneously water relations andmembrane PD, in order to examine the contribution of potassiumchannels to Lp. Cells were induced into a K⁺ permeable state.The K⁺ channels, assumed to be open, were subsequently blockedby various blockers. No significant difference in Lp was foundfor any of these treatments. Finally, the permeability of C.corallina membranes to ethanol was examined. HgCl₂ was foundto cause a decrease in reflection coefficient, coinciding witha decrease in Lp, but there was no change in the ethanol permeabilitycoefficient. This has been interpreted in terms of both thefrictional model and composite model of non-electrolyte membranetransport. Key words: Water channels, Chara, hydraulic, conductivity, membrane transport models, reflection coefficient     

A channel that allows inwardly directed fluxes of anions in protoplasts derived from wheat roots

An anion channel that only allows outward current flow (anion influx) has been identified in protoplasts derived from wheat (Triticum aestivum L., Triticum turgidum L.) roots. The anion outward rectifier (anion OR) measured by patch-clamp of whole cells activated very quickly, usually reaching a steady-state level in less than 100 ms and was easily distinguished from the cation outward rectifier (cation OR) which activated more slowly during membrane depolarisation. The anion OR is permeable to NO ₃ ^– and Cl^–, moderately permeable to I^–, and relatively impermeable to H₂PO₄/^– and ClO₄/^–. An anomalous mole-fraction effect between ClO_4/ ^– and Cl^– was observed on the outward current, indicating that the channel is a multi-ion pore. The anion OR is gated by both voltage and external anion concentration such that it activates near to the equilibrium potential for the permeant anion. It activated at more negative membrane potentials when NO ₃ ^– was substituted for Cl^– in the external medium, indicating that the channel may function to allow NO ₃ ^– influx under luxuriant external NO ₃ ^– concentrations. For most experiments, K⁺ and Cl^– were the main cation and anion in solution, and under these conditions it appeared likely that the anion OR functioned in membrane-potential regulation by facilitating a Cl^– influx at membrane potentials more positive than the chloride reversal potential (E_Cl). If E_Cl was more negative than the K⁺ reversal potential (E_K) then the anion OR dominated but both the anion and cation ORs occurred together when the membrane potential difference (V_m) was positive of both E_Cl and E_K. The cation OR was inhibited by increasing external Cl^– concentrations, but the anion OR was not affected by external K⁺ or Na⁺ concentration. The anion-transport inhibitors, zinc and phenylglyoxal were ineffective in blocking the anion OR. 4,4-Di-isothiocyanostilbene-2, 2-disulfonic acid (DIDS) irreversibly blocked about 34% of the current when applied extracellularly at a concentration of 25 M, and about 69% at a concentration of 200 M. However, DIDS (200 M) also occasionally acted as an irreversible blocker of the cation OR. Perchlorate blocked irreversibly 75% of the current at an external concentration of 10 mM and did not block the cation OR. Whole-cell currents also indicated that the anion OR was insensitive to external pH (pH=5–7) and calcium concentration ([Ca²⁺]=0.1–10 mM). Increasing intracellular calcium concentration significantly increased the occurrence of the fast outward current in whole cells (P < 0.005, X² test). With approximately 10 nM calcium inside the cell the anion outward current was observed in 64% (n = 45) of cells and with 50 nM calcium inside the cell the anion current was observed in 88% (n = 69) of cells. Single-anion OR channels observed in outside-out patches had a conductance in 300 mM KCl (external) of about 4 pS. When voltage pulses were applied to outside-out patches the average currents were similar to those observed in whole cells. The significance of the anion OR as a likely route for Cl uptake in high salinities is discussed.Abbreviations Bath solution bathing the extracellular face of the membrane - DIDS (4,4-diisothiocyanostilbene-2,2-disulfonic acid) - E_x reversal potential for ion x - OR outward rectifier - Pip solution inside the pipette - TEACl (tetraethyl-ammonium chloride) - V_m membrane potential difference We thank the Australian Research Council for financial support, G.P. Findlay and A. Garrill for helpful discussions, and K. Morris and D. Mackenzie for expert technical assistance. M.S. was supported by an Australian Postgraduate Research Award.