The interrelationship between HCO 3 − , NO 3 − , and Cl− as effective anions in the photosynthetic electron transport

Thylakoids were isolated from the leaves of three different plants (Pisum sativium L., Lactuca sativa L., and Raphanus sativus L.). The addition of HCO ₃ ^? to a suspension of salt-and HCO ₃ ^? -epleted thylakoids (suspended in salt-free medium) raised the rate of O₂ evolution up to fourfold. This stimulation could be partially replaced by the addition of chloride or nitrate ions. However, the addition of HCO ₃ ^? in the presence of Cl^? or NO ₃ ^? resulted in a higher stimulation of O₂ evolution (sixfold in the presence of nitrate and sevenfold in the presence of chloride). On the other hand, the addition of HCO ₃ ^? to the thylakoids depleted from salt only raised the rate of O₂ evolution by 10–15%, whereas 40–70% was obtained by the addition of nitrate or chloride ions. The fluorescence induction studies indicated a significant decrease in the yield of the variable fluorescence of the salt- and HCO ₃ ^? -depleted thylakoids. A partial increase in the fluorescence yield was obtained by the addition of HCO ₃ ^? alone. A typical fluorescence induction curves were obtained by the addition of HCO ₃ ^? in the presence of Cl^? or NO ₃ ^? ions. The data obtained suggest a similar role for chloride and nitrate ions in O₂ evolution in the Hill-reaction, which is restricted at the donor side of photosystem II, whereas bicarbonate plays its role at both sides (acceptor and donor sides). The presented data are those obtained for the thylakoids of P. sativium, which were more or less similar to those obtained for L. sativa and R. sativus.     

Alteration in enrichment of NO 3 − and reduced-N in xylem exudate during and after extended plant exposure to15NO 3 −

Summary Distinctly different patterns of¹⁵N enrichment were observed in the nitrate and reduced-N fractions of xylem exudate from soybean plants during and after 5 to 6 days of exposure to¹⁵NO ₃ ^– . Within 1 d after changes in solution NO ₃ ^– label, more than 90% of the exudate NO ₃ ^– originated from the exogenous supply. Alterations in the enrichment of exudate reduced-N were much slower, however, and the enrichment reached only 40% even after 5 d of continuous exposure to¹⁵NO ₃ ^– . Taking into account possible reduction of endogenous NO ₃ ^– and delayed translocation of NO ₃ ^– reduction products, it was concluded that root reduction could have contributed only 30 to 42% of the reduced-N found in the exudate.     

Short-term studies of NO 3 − uptake in Pisum using 13NO 3 −

Influx, efflux and net uptake of NO ₃ ^– was studied in Pisum sativum L. cv. Marma in short-term experiments where ¹³NO ₃ ^– was used to trace influx. The influx rate in N-limited plants was similar both during net uptake at external concentrations of around 50 M, and at low external NO ₃ ^– concentrations (4–6 M) when net uptake was practically zero. Efflux could be inferred from discrepancies between influx and net uptake but was never very high in the N-limited plants during net uptake. Close to the threshold concentration for not NO ₃ ^– uptake, efflux was high and equalled influx. Thus, the threshold concentration can be regarded as a NO ₃ ^– compensation point. The inclusion of NH ₄ ⁺ in the outer medium decreased influx by about 40% but did not significantly affect efflux. The roles of NO ₃ ^– fluxes and nitrate-reductase activity in regulating/limiting NO ₃ ^– utilization are discussed.Abbreviations DW dry weight - FW fresh weight - R_N relative nitrogen addition rate     

Root apoplastic transport and water relations cannot account for differences in Cl− transport and Cl−/NO3 − interactions of two grapevine rootstocks differing in salt tolerance

Grapevine is moderately sensitive to salinity and accumulation of toxic levels of Cl^? in leaves is the major reason for salt-induced symptoms. In this study, apoplastic Cl^? uptake and transport mechanism(s) were investigated in two grapevine (Vitis sp.) rootstock hybrids differing in salt tolerance; 1103 Paulsen (salt tolerant) and K 51–40 (salt sensitive). Increased external salinity caused high Cl^? accumulation in shoots of the salt sensitive K 51–40 in comparison to Paulsen. Measurement of ¹⁵NO₃ ^? net fluxes under high salinity showed that by increasing external Cl^? concentrations K 51–40 roots showed reduced NO₃ ^? accumulation. This was associated with increased accumulation of Cl^?. In comparison to Paulsen, K 51–40 showed reduced NO₃ ^?/Cl^? root selectivity with increased salinity, but Paulsen had lower selectivity over the whole salinity range (0–45 mM). To examine if root hydraulic and permeability characterisations accounted for differences between varieties, the root pressure probe was used on excised roots. This showed that the osmotic Lp_r was significantly smaller than hydrostatic Lp_r, but no obvious difference was observed between the rootstocks. The reflection coefficient (σ) values (0.48–0.59) were the same for both rootstocks, and root anatomical studies showed no obvious difference in apoplastic barriers of the main and lateral roots. Comparing the uptake of Cl^? with an apoplastic tracer, PTS (3-hydroxy-5,8,10-pyrentrisulphonic acid), showed that there was no correlation between Cl^? and PTS transport. These results indicated that bypass flow of salts to the xylem is the same for both rootstocks (0.77 ± 0.2 and 1.05 ± 0.12 %) and hence pointed to differences in membrane transport to explain difference in Cl^? transport to the shoot.     

Antarctic archaea–virus interactions: metaproteome-led analysis of invasion,evasion and adaptation

Despite knowledge that viruses are abundant in natural ecosystems, there is limited understanding of which viruses infect which hosts, and how both hosts and viruses respond to those interactions—interactions that ultimately shape community structure and dynamics. In Deep Lake, Antarctica, intergenera gene exchange occurs rampantly within the low complexity, haloarchaea-dominated community, strongly balanced by distinctions in niche adaptation which maintain sympatric speciation. By performing metaproteomics for the first time on haloarchaea, genomic variation of S-layer, archaella and other cell surface proteins was linked to mechanisms of infection evasion. CRISPR defense systems were found to be active, with haloarchaea responding to at least eight distinct types of viruses, including those infecting between genera. The role of BREX systems in defending against viruses was also examined. Although evasion and defense were evident, both hosts and viruses also may benefit from viruses carrying and expressing host genes, thereby potentially enhancing genetic variation and phenotypic differences within populations. The data point to a complex inter-play leading to a dynamic optimization of host–virus interactions. This comprehensive overview was achieved only through the integration of results from metaproteomics, genomics and metagenomics.     

NO 2 − Efflux and its regulation in cyanobacterium Nostoc MAC

NO ₂ ^– efflux and its regulation have been studied in the cyanobacterium Nostoc MAC. 3-(3,4-Dichlorophenyl)-1,1-dimethylurea (DCMU), carbonyl cyanide-m-chlorophenyl hydrazone (CCCP), sodium azide, p-chloromercuribenzoate (PCMB), and dicyclohexylcarbodiimide (DCCD), a specific inhibitor of bacterial ATPase, inhibited the NO ₂ ^– efflux activity singificantly. No NO ₂ ^– efflux activity was observed under dark-aerobic as well as under dark-anaerobic conditions; however, the addition of ATP resulted in NO ₂ ^– efflux even under dark-aerobic condition. Maximum NO ₂ ^– efflux activity was observed when NO ₃ ^– served as the sole nitrogen source. However, NH ₄ ⁺ ions inhibited the NO ₂ ^– efflux activity when both NO ₃ ^– and NH ₄ ⁺ wer simulatneously available to the cells. The NO ₂ ^– efflux was freed from NH ₄ ⁺ repression by l-methionine-dl-sulfoximine (MSX), an irreversible inhibitor of glutamine synthetase (GS). Chloramphenicol, a protein synthesis inhibitor, inhibited the derepression of NO ₂ ^– efflux system when NH ₄ ⁺ -incubated cells were transferred to NO ₃ ^– medium. Tungstate-treated cells lacking functional NO ₃ ^– reductase but having NO ₃ ^– uptake activity also lacked NO ₂ ^– efflux activity. These results suggest that (i) NO ₂ ^– efflux in Nostoc MAC is NO ₃ ^– dependent and an energy-dependent process that can be regulated at the levels of NO ₃ ^– uptake and NO ₃ ^– reductase; (ii) NO ₂ ^– efflux system is NH ₄ ⁺ repressible; however, the product of NH ₄ ⁺ assimilation via GS is being required for repression to occur; (iii) de novo protein synthesis is required for derepression of the NO ₂ ^– efflux system; and (iv) the catalytic activity of NO ₂ ^– reductase also seems to play an important role in the regulation of NO ₂ ^– efflux system.     

A model of photosynthetic CO2 assimilation and carbon-isotope discrimination in leaves of certain C3−C4 intermediates

A model of leaf, photosynthesis has been developed for C₃–C₄ intermediate species found in the generaPanicum, Moricandia, Parthenium andMollugo where no functional C₄ pathway has been identified. Model assumptions are a functional C₃ cycle in both mesophyll and bundle-sheath cells and that glycine formed in the mesophyll, as a consequence of the oxygenase activity of ribulose-1,5-bisphosphate carboxylase-oxygenase (Rubisco, EC 4.1.1.39), diffuses to the bundle sheath, where most of the photorespiratory CO₂ is released. The model describes the observed gas-exchange characteristics of these C₃–C₄ intermediates, such as low CO₂-compensation points () at an O₂ pressure of 200 mbar, a curvilinear response of to changing O₂ pressures, and typical responses of CO₂-assimilation rate to intercellular CO₂ pressure. The model predicts that bundle-sheath CO₂ concentration is highest at low mesophyll CO₂ pressures and decreases as mesophyll CO₂ pressure increases. A partitioning of 5–15% of the total leaf Rubisco into the bundle-sheath cells and a bundlesheath conductance similar to that proposed for C₄ species best mimics the gas-exchange results. The model predicts C₃-like carbon-isotope discrimination for photosynthesis at atmospheric levels of CO₂, but at low CO₂ pressures it predicts a higher discrimination than is typically found during C₃ photosynthesis at lower CO₂ pressures.Abbreviations and symbols PEP phosphoenolpyruvate - Rubisco ribulose-1,5-bisphosphate carboxylase-oxygenase (EC 4.1.1.39) - RuBP ribulose-1,5-bisphosphate - p(CO₂) partial pressure of CO₂ - p(O₂) partial pressure of O₂. See also p. 471     

Endothelial NO and O2− production rates differentially regulate oxidative,nitroxidative, and nitrosative stress in the microcirculation

Endothelial dysfunction causes an imbalance in endothelial NO and O₂⁻ production rates and increased peroxynitrite formation. Peroxynitrite and its decomposition products cause multiple deleterious effects including tyrosine nitration of proteins, superoxide dismutase (SOD) inactivation, and tissue damage. Studies have shown that peroxynitrite formation during endothelial dysfunction is strongly dependent on the NO and O₂⁻ production rates. Previous experimental and modeling studies examining the role of NO and O₂⁻ production imbalance on peroxynitrite formation showed different results in biological and synthetic systems. However, there is a lack of quantitative information about the formation and biological relevance of peroxynitrite under oxidative, nitroxidative, and nitrosative stress conditions in the microcirculation. We developed a computational biotransport model to examine the role of endothelial NO and O₂⁻ production on the complex biochemical NO and O₂⁻ interactions in the microcirculation. We also modeled the effect of variability in SOD expression and activity during oxidative stress. The results showed that peroxynitrite concentration increased with increase in either O₂⁻ to NO or NO to O₂⁻ production rate ratio (Q_O2⁻/Q_NO or Q_NO/Q_O2⁻, respectively). The peroxynitrite concentrations were similar for both production rate ratios, indicating that peroxynitrite-related nitroxidative and nitrosative stresses may be similar in endothelial dysfunction or inducible NO synthase (iNOS)-induced NO production. The endothelial peroxynitrite concentration increased with increase in both Q_O2⁻/Q_NO and Q_NO/Q_O2⁻ ratios at SOD concentrations of 0.1–100 μM. The absence of SOD may not mitigate the extent of peroxynitrite-mediated toxicity, as we predicted an insignificant increase in peroxynitrite levels beyond Q_O2⁻/Q_NO and Q_NO/Q_O2⁻ ratios of 1. The results support the experimental observations of biological systems and show that peroxynitrite formation increases with increase in either NO or O₂⁻ production, and excess NO production from iNOS or from NO donors during oxidative stress conditions does not reduce the extent of peroxynitrite mediated toxicity.     

Acquisition of Ca2+ and HCO3 −/CO3 2− for shell formation in embryos of the common pond snail Lymnaea stagnalis

Embryos of the freshwater common pond snail Lymnaea stagnalis develop to hatch within 10 days under control conditions (22°C, Miami-Dade tap water) and this development is impaired by removal of ambient calcium. In contrast, embryos did not exhibit dependence upon an ambient HCO₃ ⁻/CO₃ ²⁻ source, developing and hatching in HCO₃ ⁻/CO₃ ²⁻-free water at rates comparable to controls. Post-metamorphic, shell-laying embryos exhibited a significant saturation-type calcium uptake as a function of increasing ambient calcium concentration. However, changes in ambient bicarbonate concentration did not influence calcium or apparent titratable alkalinity uptake. There was a distinct shift from no significant flux in pre-metamorphic embryos to net uptake of calcium in post-metamorphic stages as indicated by an increased uptake from the micro-environment surrounding the egg mass and increased net uptake in 24-h, whole egg mass flux measurements. Furthermore, HCO₃ ⁻/CO₃ ²⁻ acquisition as measured by titratable alkalinity flux is at least partially attributable to an endogenous carbonate source that is associated with acid extrusion. Thus, calcium requirements for embryonic shell formation are met via uptake but HCO₃ ⁻/CO₃ ²⁻, which is also necessary for shell formation is acquired in part from endogenous sources with no detectable correlation to ambient HCO₃ ⁻/CO₃ ²⁻ availability.     

Biosynthesis of indole-3-acetic acid in tomato shoots: Measurement,mass-spectral identification and incorporation of −2H from −2H2O into indole-3-acetic acid,d- and l-tryptophan,indole-3-pyruvate and tryptamine

Indole-3-acetic acid (IAA) and its putative precursors, l- and d-tryptophan, indole-3-pyruvate, and tryptamine were isolated from tomato (Lycopersicon esculentum (L.) Mill.) shoots, identified by mass spectrometry, and measured using capillary gas chromatography with an electron capture detector and radioactive internal standards. Average amounts present were 7.9ng · (g FW)^–-1 IAA, 5.7ng · (g FW)^–-1 indole-3-pyruvate, 132 ng · (g FW)^–-1 tryptamine, 103 ng · (g FW)^–-1 d-tryptophan, and 2250 ng · (g FW)^–-1 l-tryptophan. Indole-3-acetaldoxime was not found; detection limits were less than 1ng · (g FW)^–-1. When tomato shoots were incubated for 6, 10 and 21 h in 30% ^–2H₂O, up to four positions in IAA, l- and d-tryptophan, tryptamine and indole-3-pyruvate became labelled with ^–2H. Compounds became labelled rapidly with 10% of IAA molecules containing ^–2H after 6 h. The percentage of labelled molecules of IAA and l-tryptophan increased up to 10 h but then decreased again, correlating with an increase in the total shoot tryptophan and presumably a result of protein hydrolysis in the excised, slowly senescing tissue. The amount of ^–2H in d-tryptophan also showed an increase followed by a decrease, but the proportion of labelled molecules was much less than in l-tryptophan and IAA. Tryptamine became labelled initially at a similar rate to IAA but continued to accumulate ^–2H up to 21 h. We conclude that tryptamine is synthesized from a different pool of tryptophan from that used in IAA synthesis, and is not a major endogenous precursor of IAA in tomato shoots. Indole-3-pyruvate was the most heavily labelled compound after 6 and 10 h incubation (21-h data not available). Furthermore, the proportion of ^–2H-labelled indole-3-pyruvate molecules was quantitatively consistent with the amount of label in IAA. On the other hand, a quantitative comparison of the IAA turnover rate and the rate of ^–2H incorporation into both l- and d-tryptophan indicates that IAA is not made from the total shoot pool of either l- or d-tryptophan. Instead IAA appears to be synthesized from a restricted pool which is turning over rapidly and which has access to both newly synthesized tryptophan and that from protein hydrolysis.Abbreviations GC-ecd gas chromatography with electroncapture detector - GC-MS combined gas chromatography-mass spectrometry - HPLC high-performance liquid chromatography - IAA indole-3-acetic acid - IAOX indole-3-acetaldoxime - IPyA indole-3-pyruvate - PFB pentafluorobenzyl - R_T retention time - TNH₂ tryptamine - Trp tryptophan - SIM selected ion monitoring We wish to thank Ms. Sue Alford for running the mass spectra and Dr Harry Young for advice with the mass spectrometry. The work was supported by grants from the University of Auckland Research Committee and the C. Alma Baker Trust fund. The mass spectrometer was supported jointly by the University Grants Commitee (NZ) and the DSIR Division of Horticulture and Processing.     

Synthesis and characterization of [Pt(COD)Cl(NO3)] and [Pt(COD)(NO3)2] and the use of [Pt(COD)Clx(NO3)2−x] in the preparation of cis[Pt(PPh3)2Clx(NO3)2−x] (x=0, 1, 2) and [Pt(PPh3)3L](NO3) (L=Cl,NO3)

[Pt(COD)Cl₂] (COD=1,5-cyclooctadiene) is a versatile starting material for the synthesis of Pt(II) compounds. The preparations of the new compounds [Pt(COD)Cl(NO₃)], [Pt(COD)(NO₃)₂] and [Pt(PPh₃)₃(NO₃)](NO₃) and also of the known compounds cis[Pt(PPh₃)₂Cl₂], cis [Pt(PPh₃)₂Cl(NO₃)], cis[Pt(PPh₃)₂(NO₃)₂] and [Pt(PPh₃)₃Cl](NO₃)are reported. The compounds are characterized by elemental analysis, ³¹P{¹H} NMR spectroscopy and IR spectroscopy.     

High-Affinity NO− 3-H+ Cotransport in the Fungus Neurospora: Induction and Control by pH and Membrane Voltage

High-affinity nitrate transport was examined in intact hyphae of Neurospora crassa using electrophysiological recordings to characterize the response of the plasma membrane to NO⁻ ₃ challenge and to quantify transport activity. The NO⁻ ₃-associated membrane current was determined using a three electrode voltage clamp to bring membrane voltage under experimental control and to compensate for current dissipation along the longitudinal cell axis. Nitrate transport was evident in hyphae transferred to NO⁻ ₃-free, N-limited medium for 15 hr, and in hyphae grown in the absence of a nitrogen source after a single 2-min exposure to 100 μm NO⁻ ₃. In the latter, induction showed a latency of 40–80 min and rose in scalar fashion with full transport activity measurable approx. 100 min after first exposure to NO⁻ ₃; it was marked by the appearance of a pronounced sensitivity of membrane voltage to extracellular NO⁻ ₃ additions which, after induction, resulted in reversible membrane depolarizations of (+)54–85 mV in the presence of 50 μm NO⁻ ₃; and it was suppressed when NH₄ ⁺ was present during the first, inductive exposure to NO⁻ ₃. Voltage clamp measurements carried out immediately before and following NO⁻ ₃ additions showed that the NO⁻ ₃-evoked depolarizations were the consequence of an inward-directed current that appeared in parallel with the depolarizations across the entire range of accessible voltages (−400 to +100 mV). Measurements of NO⁻ ₃ uptake using NO⁻ ₃-selective macroelectrodes indicated a charge stoichiometry for NO⁻ ₃ transport of 1(+):1(NO⁻ ₃) with common K _m and J _max values around 25 μm and 75 pmol NO⁻ ₃ cm⁻²sec⁻¹, respectively, and combined measurements of pH _o and [NO⁻ ₃] _o showed a net uptake of approx. 1 H⁺ with each NO⁻ ₃ anion. Analysis of the NO⁻ ₃ current demonstrated a pronounced voltage sensitivity within the normal physiological range between −300 and −100 mV as well as interactions between the kinetic parameters of membrane voltage, pH _o and [NO⁻ ₃] _o . Increasing the bathing pH from 5.5 to 8.0 reduced the current and the associated membrane depolarizations 2- to 4-fold. At a constant pH _o of 6.1, driving the membrane voltage from −350 to −150 mV resulted in an approx. 3-fold reduction in the maximum current and a 5-fold rise in the apparent affinity for NO⁻ ₃. By contrast, the same depolarization effected an approx. 20% fall in the K _m for transport as a function in [H⁺] _o . These, and additional results are consistent with a charge-coupling stoichiometry of 2(H⁺) per NO⁻ ₃ anion transported across the membrane, and implicate a carrier cycle in which NO⁻ ₃ binding is kinetically adjacent to the rate-limiting step of membrane charge transit. The data concur with previous studies demonstrating a pronounced voltage-dependence to high-affinity NO⁻ ₃ transport system in Arabidopsis, and underline the importance of voltage as a kinetic factor controlling NO⁻ ₃ transport; finally, they distinguish metabolite repression of NO⁻ ₃ transport induction from its sensitivity to metabolic blockade and competition with the uptake of other substrates that draw on membrane voltage as a kinetic substrate. Received: 17 March 1997/Revised: 20 June 1997     

Effects of NO2 − or NO3 − supply on polyamine accumulation and ethylene production of wheat roots at acidic and neutral pH: implications for root growth

Exposure of plant tissues to nitrite ion or nitrite-derived NO at acidic pH results in the degradation of important macromolecules and may lead to the formation of reactive molecular species. Polyamines as free radical scavengers protect plant tissues against membrane and DNA damage during stress and may contribute to the acclimation processes caused by nitrite as an abiotic stressor at acidic pH. The putrescine content of wheat roots grown under low salt conditions increased only transiently at pH 7.0 when the nutrient solution was replaced by 1mM KNO₂, KNO₃, NaNO₂ or NaNO₃, but the concentration of this diamine remained high after a 24-hour incubation at pH 4.0. The acid stress-induced putrescine accumulation was further enhanced by an external N source, especially by nitrite. The contents of spermine and spermidine in the 24-hour samples were also higher in N-supplied roots at acidic pH. Polyamine contents were not closely correlated with the ethylene production by the intact roots. Nitrite treatment, however, significantly decreased the ethylene release from the root apex, but not from the basal parts at pH 4.0. The peroxidative capacities of the tissues in the soluble fractions were also inhibited by nitrite in the apical zones, which might modify the H₂O₂-coupled oxidative processes. Nitrite ion at acidic pH may react directly with guaiacol-like phenolic compounds and in this way interfere with the lignification process. The low ethylene release by the apical zones in acidic environment may be a symptom of the nitrite-induced inhibition of root extension.     

Immunohistochemical expressions of mGluR5, P2Y2 receptor,PLC-β1, and IP3R-I and -II in Merkel cells in rat sinus hair follicles

We previously found that Merkel cells (MCs) of the rat and monkey show a strong immunoreaction of the -subunit of Gq protein. The Gq-subunit isoform activates isozymes of phospholipase C- (PLC-), which produces inositol-(1,4,5)-triphosphate (IP3) which mobilizes intracellular Ca⁺⁺ from calcium stores via IP3 receptors. Glutamate and adenosine triphosphate (ATP), which are candidates for neurotransmitters in Merkel endings, are known to couple to Gq. Although MCs showed positive immunoreactions of metabotropic glutamate receptor 5 (mGluR5) in our preliminary study, these cells were not reactive to all antibodies to PLC- isozymes. We, therefore, reinvestigated immunohistochemical affinities to MCs of antibodies to PLC- isozymes and mGluRs using frozen sections of rat sinus hair follicles that were briefly postfixed in formaldehyde. We also studied the immunohistochemical expressions of P2Y receptors for ATP and IP3 receptor subtypes using similar sections. Merkel cells showed positive immunoreactions of PLC-1 and mGluR5. It was also found that MCs show positive immunoreactions of P2Y2, IP3R-I, and IP3R-II receptors. These results suggest that the Gq isoform in MCs couples to both the P2Y2 receptor and mGluR5 and regulates the intracellular Ca⁺⁺ concentration via the PLC-–IP3 cascade.