Early needle senescence and thinning of the crown structure of Picea abies as induced by chronic SO2 pollution. II. Field data basis, model results and tolerance limits

Field data on the sulphur and cation budget of growing Norway spruce canopies (Picea abies [L.] Karst.) are summarized. They are used to test a spruce decline model capable of quantifying effects of chronic SO₂ pollution on spruce forests. At ambient SO₂ concentrations, acute SO₂ damage is rare, but exposure to polluted air produces reversible thinning of the canopy structure with a half-time of a few years. Canopy thinning in the spruce decline model is highest (i) at elevated SO₂ pollution, (ii) in the mountains, (iii) at unfertilized sites with poor K⁺, Mg²⁺ or Zn²⁺ supply, (iv) at low spruce litter decomposition rates, and (v) acidic, shallow soils at high annual precipitation rates in the field and vice versa. Model application using field data from Würzburg (moderate SO₂ pollution, alkaline soils, no spruce decline) and from the Erzgebirge (extreme SO₂ pollution, acidic soils in the mountains, massive spruce decline) predicts canopy thinning by 2–11% in Würzburg and by 45–70% in the Erzgebirge. The model also predicts different SO₂-tolerance limits for Norway spruce depending on the site elevation and on the nutritional status of the needles. If needle loss of more than 25% (damage class 2) is taken to indicate ‘real damage’ exceeding natural variances, then for optimum soil conditions SO₂ tolerance limits range from (27.3 ± 7.4) μg m^?3 to (62.6 ± 16.5) μg m^?3. For shallow and acidic soils, SO₂ tolerance limits range from (22.0 ± 5.5) μg m^?3 to (37.4 ± 7.5) μ m^?3. These tolerance limits, which are calculated on an ecophysiological data basis for Norway spruce are close to epidemiological SO₂-toIerance limits as recommended by the IUFRO, UN-ECE and WHO. The observed statistical regression slope of the plot (damaged spruce trees vs. SO₂-pollution) in west Germany is confirmed by modelling (6% error). Model application to other forest trees allows deduction of the observed sequence of SO₂-sensitivity: Abies > Picea > Pinus > Fagus > Quercus. Thus, acute phytotoxicity of SO₂ seems not to be involved in ‘forest decline’. Chronic SO₂-pollution induces massive canopy thinning of Abies alba and Picea abies only at unfavourable sites, where natural stress factors and secondary effects of SO₂pollution act together to produce tree decline.     

Sulphate transport in the cyanobacterium Synechococcus R-2 (Anacystis nidulans, S. leopoliensis) PCC 7942

Synechococcus R-2 (PCC 1942) actively accumulates sulphate in the light and dark. Intracellular sulphate was 1.35 ± 0.23 mol m^?3 (light) and 0.894 ± 0.152 mol m^?3 (dark) under control conditions (BG-11 media: pH_o, 7.5; [SO₄^2?]_o, 0.304 mol m^?3). The sulphate transporter is different from that found in higher plants: it appears to be an ATP-driven pump transporting one SO₄^2?/ATP [ΔμSO₄^2?_i,o=+ 27.7 ± 0.24 kJ mol^?1 (light) and + 24 ± 0.34 kj mol^?1 (dark)]. The rate of metabolism of SO₄^2?at pH_o, 7.5 was 150 ± 28 pmol m^?2 s^?1 (n = 185) in the light but only 12.8 ± 3.6 pmol m^?2 s^?1 (n = 61) in the dark. Light-driven sulphate uptake is partially inhibited by DCMU and chloramphenicol. Sulphate uptake is not linked to potassium, proton, sodium or chloride transport. The alga has a constitutive over-capacity for sulphate uptake [light (n= 105): K_m= 0.3 ± 0.1 mmol m^?3, V_max, = 1.8 ± 0.6 nmol m^?2 s^?1; dark (n= 56): K_m= 1.4 ± 0.4 mmol m^?3, V_max= 41 ± 22 pmol m^?2 s^?1]. Sulphite (SO₃^2?) was a competitive inhibitor of sulphate uptake. Selenate (SeO₄^2?) was an uncompetitive inhibitor.     

Detoxification of SO2 in conifers differing in SO2-tolerance

Contents of organic sulfur, sulfate and the inorganic cations K⁺, Ca²⁺, Mg²⁺, Mn²⁺ and Na⁺ were compared in needles of three conifer species differing in tolerance to chronic SO₂ immissions. Sulfate and organic sulfur compounds were also measured in bark and wood. Field material was collected from Norway Spruce (Picea abies (L.) Karst.), Colorado Spruce (Picea pungens Engelm.) and Scots Pine (Pinus sylvestris L.) at sites where the SO₂ concentration in air was high, and at another site where it was low. In general, sulfate contents were higher but cation contents lower at the sites where SO₂ concentrations were high than where they were low. Up to 114mmol · (kg DW)^–1 sulfate was measured in fouryear-old needles of Norway Spruce from the Erzgebirge (annual mean of SO₂ in air 32 nl · 1^–1). Sulfate accumulation in this SO₂-sensitive conifer increased with SO₂ concentration in ambient air and with needle age, indicating that the main part of the sulfate resulted from the oxidative detoxification of SO₂. Loss of inorganic cations from ageing needles was reduced, or cation levels even increased, with increasing needle age, while sulfate accumulated. Apparently, cations served as counter-ions for sulfate, which is sequestered in the vacuoles. Individual trees differed in regard to the nature of cations which accumulated with sulfate. Calcium, potassium and magnesium were the dominating cations. Sodium levels were very low. Needles of the SO₂-tolerant conifers Colorado Spruce and Scots Pine growing next to Norway Spruce in the Erzgebirge did not accumulate, or accumulated less, sulfate with increasing needle age as compared to needles of Norway Spruce. However, somewhat more sulfate was found in the bark of the SO₂-tolerant species than in the bark of Norway Spruce. Scots Pine contained distinctly more sulfate in the wood than the other conifers. Since accumulation of organic sulfur compounds could not be observed with increasing needle age, or in bark and wood, reduction does not appear to play a major role in the detoxification of SO₂ by the investigated species. Physiological mechanisms permitting Colorado Spruce and Scots Pine to avoid the sulfate accumulation in the needles and the accompanying sequestration of cations that are observed in neighbouring Norway Spruce are discussed on the basis of the obtained data.Abbreviations S_org organic sulfur compounds Died June 10, 1991, aged 29, in a traffic accident. He initiated this work.This work was supported by the Sonderforschungsbereich 251 of the University of Würzburg and by the Projektgruppe Bayern zur Erforschung der Wirkung von Umweltschadstoffen (PBWU). The authors with to thank Prof. Dr. W Kaiser and Prof. Dr. W. Urbach (both Julius-von-Sachs-Institut, University of Würzburg, Germany) for HPLC-analysis and ICP-analysis.     

Stomatal SO2 uptake and sulfate accumulation in needles of Norway spruce stands (Picea abies) in Central Europe

Monthly uptake rates and the annual deposition of gaseous SO₂ via the stomata of six Norway spruce canopies (Picea abies (L.) Karst.) in Germany (Königstein im Taunus, Witzenhausen, Grebenau, Frankenberg, Spessart, Fürth im Odenwald) were calculated (i) from statistical response functions of stomatal aperture depending on meteorological data, and (ii) from the synchronously measured SO₂ immission at these stands. The stomatal response functions had been derived on the basis of thorough stomatal water conductance measurements in the field. Calculations of the SO₂ conductance of spruce twigs and SO₂ uptake rates via stomata need continuously measured complete data sets of the (i) light intensity, (ii) air temperature, (iii) air humidity and (iv) SO₂ concentration in spruce forests from all the year. These data were recorded half hourly in different German spruce forests. The apparent needle water vapour pressure difference and transpiration rates were calculated from meteorological data. Additional use of canopy through flow data in dry years allowed the estimation of the mean stomatal conductance for H₂O and SO₂ of whole spruce canopies. The annual SO₂ uptake of a mean unit needle surface in spruce forests was 32% of the SO₂ uptake rate of exposed needles at the top of spruce crowns. There is significant SO₂ uptake all the year. The mean SO₂ dose at all sites and years received through the stomata was (0.25±0.07) mol SO₂ m^-2 (total needle surface) (nPa Pa^-1)^-1 (annual mean of SO₂ immission; 1 nPa (SO₂) Pa^-1 (air) = 1 ppb) day^-1 (vegetation period per year). Comparison of calculated SO₂ uptake rates into needles with measured SO₄ ^2- accumulation rates in needles from the mentioned sites and additionally from Würzburg, Schneeberg (Fichtelgebirge) and from three sites in the eastern Erzgebirge (Höckendorf, Kahleberg, Oberbärenburg) revealed that oxidative SO₂ detoxification (SO₄ ^2- formation) dominates only at sites with high SO₂ immission and short vegetation periods. Under these conditions 70 to 90% of the annual stomatal SO₂ uptake is detoxified via SO₄ ^2- accumulation in needles. Cations are needed for neutralization of accumulating SO₄ ^2- which are inavailable to support growth. Thus, SO₂ induces a dominant and competitive additional nutrient cation demand, cation deficiency symptoms and enhanced needle loss (spruce decline symptoms) mainly at sites, where the ratio R=(SO₂ immission): (length of the vegetation period) is higher than R=0.07 nPa Pa^-1 day^-1. Correlation analysis of the relative needle loss versus the SO₂-dependent SO₄ ^2- formation rate revealed a significant increase of needle loss at the 98% level (Student). At sites with small SO₂ immission and long vegetation periods (R<0.07 nPa Pa^-1 day^-1) reductive SO₂ detoxification via growth (and/or phloem export of SO₄ ^2-) is not kinetically overburdened. Under these conditions only 30% of the annual SO₂ uptake is detoxified via SO₄ ^2- formation and spruce decline is small or absent. On the basis of the critical value R0.07 nPa Pa^-1 day^-1 recommended SO₂ immission limits can be deduced on a mere ecophysiological basis. These deduced values are close to the proposed SO₂ immission limits of the IUFRO, WHO and the UNECE.     

Emission of hydrogen sulfide by twigs of coniferes — acomparison of Norway spruce (Picea abies (L.) Karst.), Scotch pine (Pinus sylvestris L.) and Blue spruce (Picea pungens Engelm.)

The emission of reduced volatile sulfur compounds from twigs of Norway spruce (Picea abies (L.) Karst.) was measured in the field by cryosampling and gaschromatographic analysis. Trees were growing in the Erzgebirge (E-Germany) at Oberbärenburg and at the Kahleberg and at a third stand in NW-Bavaria (S-Germany). Emission rates were also measured for Scotch pine (Pinus sylvestris L.) and Blue spruce (Picea pungens Engelm.) at the Kahleberg. Twigs still attached to the trees were enclosed in a flow-through gas exchange cuvette. H₂S was detected as the predominant reduced sulfur compound emitted from the twigs. The mean H₂S emission rate from twigs of Norway spruce varied between 0.04 pmol kg^-1 dw s^-1 at Würzburg and 6.21 pmol kg^-1 dw s^-1 at the Kahleberg. Comparing different species at the Kahleberg, the mean H₂S emission rate was almost the same from twigs of Norway spruce (6.2 pmol kg^-1 dw s^-1) and Blue Spruce trees (5.9 pmol kg^-1 dw s^-1) but it was approximately 18 times higher for Scotch pine (110 pmol kg^-1 dw s^-1). The percentage of SO₂-exclusion via H₂S-emission of the tree species investigated at the Kahleberg is calculated on the basis of data on SO₂ fluxes. It is very small for Norway spruce and Blue spruce. However, for Scotch pine, H₂S emission contributes about 10% to the detoxification of SO₂.     

Leaching of solutes by the action of acidic rain: a comparison of efflux from twigs and single needles of Picea abies (L. Karst.)

Abstract. Leaching of inorganic cations (K⁺, Mg²⁺) and in some cases of inorganic anions and sugars from detached twigs and single needles of spruce Picea abies L. Karst.) in the presence of acid rain (H₂SO₄, 1 mol m^?3) or salt solutions (Na₂ SO₄, 1 mol m^?3) was examined under laboratory conditions. Cation leaching (as percentage of the total water soluble ion content of the tissue per hour) was: K⁺: 0.01-0.02%; Mg²⁺: 0.005-0.01%; Ca²⁺: 0.1-0.2%. Leaching rates of anions were even lower than that and concentrations in the leachate were often below the detection limit of anion chromatography. Spraying with H₂SO₄ (pH 2.95, 1 mol m^?3) increased leaching only transiently. Similar effects were found when Na₂SO₄ was used instead of H₂SO₄. The transiently enhanced leaching was apparently due to H⁺/cation or cation/cation exchange at the twig or leaf surfaces. Feeding of K⁺ or Al³⁺ through the stems increased leaching of all cations within a few hours, again demonstrating rapid ion exchange in the apoplast. Leaching of potassium and magnesium from single needles occurred at similar relative rates as from twigs. Loss of Ca²⁺ ions, however, was even smaller from needles than from twigs. Apparently, a large part of the Ca²⁺ lost from twigs originated from the bark and not from the needles. Efflux of ions from longitudinal needle sections was about 1000 times taster than the rates obtained with intact needles, indicating that the cuticle was the main barrier Preventing solute loss. In relation to the total amount of mineral nutrients in trees, leaching is considered to be too small to be the primary cause of damage to trees stressed by acid rain, as has been suggested in the literature.     

Calcium regulation in the freshwater-adapted mummichog

In light of recent findings of an unusual pattern of ionoregulation (high Na⁺ uptake and negligible Cl^- uptake) in the freshwater-adapted mummichog Fundulus heteroclitus, the pattern of Ca²⁺ regulation was examined. Under control conditions (water Ca²⁺= 200μEq l^-1), unidirectional Ca²⁺ influx was 11 ± 4 nEq g^-1 h^-1. Acute variation of external Ca²⁺ levels revealed a saturable Ca²⁺ uptake system with a relatively high affinity (K_m= 125 ± 36 μEq 1^-1) and a transport capacity (J_max= 31 ± 4 nEq g^-1 h^-1) comparable to those of other teleosts. Lanthanum (equimolar to [Ca²⁺]) significantly blocked Ca²⁺ uptake by 67% whereas magnesium had no effect. Chronic low Ca²⁺ exposure (50 μEq 1^-1) stimulated Ca²⁺ uptake almost three-fold above control values, whereas chronic high Ca²⁺ exposure (20000 μEq 1^-1) had no effect. Lanthanum and chronic low Ca²⁺ treatments disturbed the normally positive Ca²⁺ and Na⁺ balances of the animals whereas acid-base balance and ammonia excretion were undisturbed. The results indicate that Ca²⁺ regulation by the mummichog conforms to the model for freshwater Ca²⁺ transport whereby chloride cells on the gills take up Ca²⁺ actively from the water. However, the absence of extra-intestinal Cl^- uptake and the recent demonstration of significant Ca²⁺ uptake by opercular epithelia raise questions about the relative roles of branchial and opercular epithelial chloride cells in freshwater F. heteroclitus.     

Inhibition studies of soybean (Glycine max) urease with heavy metals,sodium salts of mineral acids,boric acid,and boronic acids

Various inhibitors were tested for their inhibitory effects on soybean urease. The K_i values for boric acid, 4-bromophenylboronic acid, butylboronic acid, and phenylboronic acid were 0.20?±?0.05?mM, 0.22?±?0.04?mM, 1.50?±?0.10?mM, and 2.00?±?0.11?mM, respectively. The inhibition was competitive type with boric acid and boronic acids. Heavy metal ions including Ag⁺, Hg²⁺, and Cu²⁺ showed strong inhibition on soybean urease, with the silver ion being a potent inhibitor (IC₅₀ = 2.3?×?10^?8 mM). Time-dependent inhibition studies exhibited biphasic kinetics with all heavy metal ions. Furthermore, inhibition studies with sodium salts of mineral acids (NaF, NaCl, NaNO₃, and Na₂SO₄) showed that only F^? inhibited soybean urease significantly (IC₅₀ = 2.9?mM). Competitive type of inhibition was observed for this anion with a K_i value of 1.30?mM.     

Ca2+ - and Nitric Oxide-Dependent Stimulation of Cyclic GMP Synthesis in Neuronal Cell Line Induced by P2-Purinergic/Pyrimidinergic Receptor

Abstract: The mechanism by which cyclic GMP synthesis is activated through a nucleotide receptor was studied in mouse neuroblastoma × rat glioma hybrid cells [108CC15 (NG 108-15)]. The transient increase in cyclic GMP level induced by ATP reached its maximum at 20 s and lasted for ～1 min. The maximal rise in cyclic GMP level achieved was highest for ATP and decreased in the following order: ATP = adenosine 5′-(γ-thio)triphosphate > UTP = 2-methylthio-ATP > ADP ? CTP, AMP, α,β-methylene-ATP, 2′- and 3′-O-(4-benzoylbenzoyl)ATP. The EC₅₀ of 1 ± 0.2 µM for UTP was significantly lower than that for ATP (14 ± 8 µM) and for all the other nucleotides tested. The rank order of potency is consistent with the pharmacology of a P_2u receptor. At submaximal concentrations of the nucleotides ATP and UTP, the rise in cyclic GMP level was inhibited by suramin (IC₅₀ = 40–60 µM) or the pyridoxal phosphate analogue pyridoxal phosphate-6-azophenyl-2′,4′-disulfonic acid (IC₅₀ = 20–30 µM). Pretreatment of cells with the Ca²⁺ ionophore ionomycin or with 2,5-di(tert-butyl)-1,4-benzohydroquinone, an inhibitor of Ca²⁺-ATPase in the endoplasmic reticulum, a maneuver to deplete internal Ca²⁺ stores, suppressed the ATP- or UTP-induced stimulation of cyclic GMP synthesis. Similarly, loading of the cells with the Ca²⁺ chelator 1,2-bis(2-aminophenoxy)ethane-N,N,N′,N′-tetraacetic acid inhibited cyclic GMP formation by ATP. Preincubation with forskolin to raise the cyclic AMP level potentiated the ATP-induced rise in cyclic GMP level by 60%. The cyclic GMP response caused by ATP was suppressed either by arginine analogues (IC₅₀ for nitroarginine = 1 µM) or by hemoglobin (IC₅₀ = 2 µM). This indicates that ATP/UTP via a P₂-receptor causes formation of nitric oxide, which activates guanylate cyclase. The synthesis of nitric oxide depends on a preceding rise in cytosolic Ca²⁺ level, mostly due to release of Ca²⁺ from internal stores. Bradykinin induces a rise in cyclic GMP level with an amplitude and time course comparable to that caused by ATP. Therefore, we studied cross-desensitization between ATP and bradykinin receptors. Pretreatment with bradykinin completely suppressed a subsequent response to ATP. However, stimulation with ATP reduced a following response to bradykinin by ～40% only. This indicates a heterologous cross-desensitization predominantly in one direction (bradykinin ? ATP).     

Evaluation of sulphur cycling in managed forest stands by means of stable S-isotope analysis

Sulphur cycling was evaluated in a 20 to 60 year old Norway spruce (Picea abies L. Karst) ecosystem in the Black Forest near Schluchsee, SW Germany, by means of stable sulphur isotope analysis.Soil and plant material were analysed for S-content and S-isotopic composition to gather information on the S-distribution in the ecosystem. Two out of three adjacent watershed areas, highly comparable to each other were fertilized with MgSO₄ and (NH₄)₂SO₄ respectively, where sulphate was enriched in the ³⁴S-isotope compared to the sulphur present in the ecosystem. As the fertilizer S served as a tracer, comparison of the S-isotopic composition of total and inorganic S in the soil and S in spruce needles from both the treated and the control sites led to new information of S-turnover processes.The S-isotopic composition of spruce needles changed markedly after the fertilizer application. Within half a year a shift towards the S-isotopic composition of the fertilizers sulphate indicated uptake of the sulphate by the trees, although this uptake did not become visible with the S content of the needles.Regarding the soil, a shift in the S-isotopic composition of the total sulphur was not that striking as with the needles, although the phosphate extractable sulphate showed a clear shift towards the S-isotopic composition of the fertilizer sulphate.     

Growth of coniferous trees exposed to SO2 and O3 using an open-air fumigation system

Scots pine (Pinus sylvestris L.), Norway spruce (Picea abies (L.) Karst.) and Sitka spruce (Picea sitchensis Bong. Carr.) were planted as 2-year-old seedlings in an open-air fumigation facility at Liphook in southern England in March 1985. The soil was a humoferric podzol of pH 4. SO₂ fumigation began in May 1987 and continued until December 1990. Long-term mean SO₂ concentrations were 4,13 and 22 nmol mo^?1. Three plots, one at each SO₂ level, were also exposed to O₃ at an average of 1–3.times the ambient level. O₃ fumigation ran from March to December 1988, May to December 1989 and February to December 1990. Each species reacted differently to treatment. Scots pine showed no growth response to either pollutant, although other work on the site demonstrated a number of deleterious effects of SO₂ on this species, including increased leaf loss and foliar injury. Stem basal diameter growth of Norway spruce was depressed in SO₂-treated plots. In contrast, extension growth of shoots of Sitka spruce increased in SO₂-treated plots, in apparent response to codeposition of NH₃-N. However, diameter growth of Sitka spruce main stems did not increase. No effects of O₃ on growth were recorded for any species.     

Effect of P2Y Agonists on Adenosine Transport in Cultured Chromaffin Cells

Abstract: Adenosine transport in cultured chromaffin cells was inhibited by purinergic P_2y-receptor agonists without significant changes in the affinity constant, the values being between 1 ± 0.4 and 1.6 ± 0.6 μM. The V_max parameter was modified significantly, being 40 ± 1.0, 26 ± 5.0, 32 ± 3.0, and 22 ± 4.7 pmol/10⁶ cells/min for control, adenosine-5′-O-(2-thiodiphosphate), 5′-adenylylimidodiphosphate, and P¹,P⁴-di(adenosine-5′-) tetraphosphate (Ap₄A) (100 μM for every effector), respectively. Ap₄A, a physiological ligand for P_2y receptors in chromaffin cells, showed the highest inhibitory effect (45%). This transport inhibition is explained by an increase in the cytosolic Ca²⁺ concentration ([Ca²⁺]_i) and the activation of protein kinase C (PKC). Experiments of [Ca²⁺]_i measurement with the fura-2 technique showed that P_2y agonists, as well as bradykinin, were able to increase [Ca²⁺]_i, this effect being independent of the presence of extracellular Ca²⁺. The peptide bradykinin, determined to be coupled to phosphatidylinositol hydrolysis and internal Ca²⁺ mobilization in chromaffin cells, exhibited a behavior similar to that of P_2y agonists in adenosine transport inhibition (39%). P_2y agonists and bradykinin increased PKC activity associated with the membrane fraction (about 50% increase in particulate PKC activity with respect to controls). The present studies suggest that adenosine transport is regulated by P_2y-purinergic receptors mediated via Ca²⁺ mobilization and PKC activation.     

Effect of open-air fumigation with sulphur dioxide and ozone on phyllosphere and endophytic fungi of conifer needles

The phyllosphere microbial populations inhabiting the needles of three conifer species, Scots pine (Pinus sylvestris L.), Sitka spruce (Picea sitchensis L.) and Norway spruce (Picea abies (L.) Karst.), exposed to SO₂ and O₃, in an open-air fumigation experiment were analysed over a 3 year period using serial dilution after washing, direct plating and a fluorescein diacetate (FDA) enzyme assay. Total fungal populations ranged from 10² to 10⁵ colonyforming units (CPU) g^?1 fresh weight of needles. The dominant fungi isolated from needles varied with tree species and isolation technique; Aureobasidium pullulans (de Bary) Arnaud was most common on Scots pine and Norway spruce and white yeasts on Sitka spruce using the dilution plating method. However, direct plating of needle segments onto culture media indicated that Sclerophoma pythiophila (Corda) Hohnel was dominant on Scots pine and A. pullulans on Sitka and Norway spruce. Green needles of Sitka spruce were found to be endophytically colonized by Rhizosphaera kalkhoffii Bubak, but seldom by Lophodermium piceae (Fuckel) Hohn during extensive sampling in 1990. Statistical analyses revealed significant differences (P<0.05) between plots in the 3 year mean of the total fungal populations or the fungal biomass (FDA assay) on all three tree species. Differences between plots were also observed for a number of dominant component species. Data were also analysed for treatment effects. A significant effect of SO₂ treatment was observed on the total fungal populations on Sitka spruce (P<0.05) which were reduced markedly by the low-SO₂ treatment, while the O₃ treatment caused a significant increase in total fungal numbers on Scots pine (P<0.05). The FDA activity on needles of both Scots pine and Sitka spruce was noticeably higher in the 0₃-only treatment plot, but the overall O₃ effect was not significant. Treatment effects were also detected on the occurrence of component species. The serial dilution method revealed an SO₂ effect (P<0.05) of a reduction in the occurrence of pink yeasts on Sitka spruce and an O₃ effect (P<0.05) of an increase in the occurrence of S. pythiophila on Sitka spruce (P<0.01) but a decrease of Epicoccum nigrum Link and Cladosporium spp. on Scots pine. The direct-plating method revealed an SO₂ effect of an increase in S. pythiophila on Norway spruce (P<0.05). Ozone treatment caused a significant increase in the isolation of a black strain of A. pullulans on Norway spruce (P<0.05). Endophytic colonization of Sitka spruce needles by R. kalkhoffii was found to be increased on two occasions by O₃ exposure.     

Characterization of Exchange Inhibitory Peptide Effects on Na+/Ca2+ Exchange in Rat and Human Brain Plasma Membrane Vesicles

Abstract: The inhibitory effects of Na⁺/Ca²⁺ exchange inhibitory peptide (XIP), which corresponds to residues 219–238 of the Na⁺/Ca²⁺ exchange protein from canine heart, were studied in both rat and human brain plasma membrane vesicles. XIP had very high potency with respect to the inhibition of the initial velocity of intravesicular Na⁺-dependent Ca²⁺ uptake in both rat brain [IC₅₀ = 3.05 ± 0.69 µM (mean ± SE)] and human brain (IC₅₀ = 3.58 ± 0.58 µM). The maximal inhibition seen in rat brain vesicles was ～80%, whereas human brain vesicles were inhibited 100%. XIP also inhibited extravesicular Na⁺-dependent Ca²⁺ release, and the inhibitory effect was enhanced by increasing the extravesicular Na⁺ concentration. In contrast, the inhibitory effect of bepridil was competitive with respect to extravesicular Na⁺. When XIP was added at steady state (5 min after the initiation of intravesicular Na⁺-dependent Ca²⁺ uptake), it was found that the intravesicular Ca²⁺ content declined with time. Analysis of unidirectional fluxes for Ca²⁺ at steady state showed that 50 µM XIP inhibited Ca²⁺ influx and efflux ～85 and 70%, respectively. This result suggested that XIP inhibited both Na⁺/Ca²⁺ exchange and Ca²⁺/Ca²⁺ exchange but had no effect on the passive release pathway for Ca²⁺. The results suggest structural homology among cardiac, rat, and human brain exchangers in the XIP binding domain and that the binding of Na⁺ or other monovalent cations, e.g., K⁺, is required for XIP to have its inhibitory effect on Ca²⁺ transport.     

Differential expression and signaling of the human histamine H3 receptor isoforms of 445 and 365 amino acids expressed in human neuroblastoma SH-SY5Y cells

In stably-transfected human neuroblastoma SH-SY5Y cells, we have compared the effect of activating two isoforms of 445 and 365 amino acids of the human histamine H₃ receptor (hH₃R₄₄₅ and hH₃R₃₆₅) on [³⁵S]-GTPγS binding, forskolin-induced cAMP formation, depolarization-induced increase in the intracellular concentration of Ca²⁺ ions ([Ca²⁺]i) and depolarization-evoked [^3?H]-dopamine release. Maximal specific binding (B_max) of [^3?H]-N-methyl-histamine to cell membranes was 953?±?204 and 555?±?140?fmol/mg protein for SH-SY5Y-hH₃R₄₄₅ and SH-SY5Y-hH₃R₃₆₅ cells, respectively, with similar dissociation constants (K_d, 0.86?nM and 0.81?nM). The mRNA of the hH₃R₃₆₅ isoform was 40.9?±?7.9% of the hH₃R₄₄₅ isoform. No differences in receptor affinity were found for the H₃R ligands histamine, immepip, (R)(-)-α-methylhistamine (RAMH), A-331440, clobenpropit and ciproxifan. Both the stimulation of [³⁵S]-GTPγS binding and the inhibition of forskolin-stimulated cAMP accumulation by the agonist RAMH were significantly larger in SH-SY5Y-hH₃R₄₄₅ cells ([³⁵S]-GTPγS binding, 158.1?±?7.5% versus 136.5?±?3.6% for SH-SY5Y-hH₃R₃₆₅ cells; cAMP accumulation, ?74.0?±?4.9% versus ?43.5?±?5.3%), with no significant effect on agonist potency. In contrast, there were no differences in the efficacy and potency of RAMH to inhibit [^3?H]-dopamine release evoked by 100?mM K⁺ (?18.9?±?3.0% and ?20.5?±?3.3%, for SH-SY5Y-hH₃R₄₄₅ and SH-SY5Y-hH₃R₃₆₅ cells), or the inhibition of depolarization-induced increase in [Ca²⁺]i (S2/S1 ratios: parental cells 0.967?±?0.069, SH-SY5Y-hH₃R₄₄₅ cells 0.639?±?0.049, SH-SY5Y-hH₃R₃₆₅ cells 0.737?±?0.045). These results indicate that in SH-SY5Y cells, hH₃R₄₄₅ and hH₃R₃₆₅ isoforms regulate in a differential manner the signaling pathways triggered by receptor activation.     

Adenosine A1 Agonists and the Ca2+ Channel Agonist Bay K 8644 Produce a Synergistic Stimulation of the GTPase Activity of Go in Rat Frontal Cortical Membranes

Abstract: The identity and role of G proteins in coupling adenosine receptors to effectors have been studied to a limited degree. We have identified the G proteins whose GTPase activity is stimulated by adenosine receptor agonists in neuronal membranes. (R)-Phenylisopropyladenosine, 2-chloroadenosine, and N-ethylcarboxamideadenosine produced a concentration-dependent stimulation of GTPase. At 10^?5M, the increase above basal GTPase in frontal cortex was 25 ± 4, 20 ± 3, and 8 ± 1%, respectively, and in the cerebellum 55 ± 2, 41 ± 4, and 22 ± 2%, respectively. The effects of (R)-phenylisopropyladenosine and 2-chloroadenosine were inhibited by (1) A₁ antagonists (76–96% reduction), (2) pretreatment with pertussis toxin (90–100% reduction), and (3) antibodies raised against the α-subunit of G_i and G_o (55–57% reduction by each), suggesting that A₁ receptors interact equally with G_i and G_o. (R)-Phenylisopropyladenosine increased the binding of a nonhydrolyzable analogue of GTP to membranes in a pertussis toxin-sensitive manner, indicative of activation of G_i or G_o. Previously, (±)-Bay K 8644 enhanced GTP hydrolysis by G_o but not G_i. Now we report a profound synergistic stimulation of GTPase in the presence of (R)-phenylisopropyladenosine and (±)-Bay K 8644 (10^?7 to 10^?5M). (±)-Bay K 8644 had no effect on nucleotide exchange and, thus, cannot activate G_o. It appears that a positive cooperative stimulation of G_o occurs when it is first activated by A₁ receptors and subsequently interacts with the L-type Ca²⁺ channel.     

The effects of SO2 and O3 on the foliar nutrition of Scots pine, Norway spruce and Sitka spruce in the Liphook open-air fumigation experiment

Foliar elements were analysed in Scots pine, Sitka spruce and Norway spruce over a 6 year period before and during continuous exposure to SO₂ and O₃ in an open-air fumigation experiment. Sulphur dioxide treatment elevated foliar sulphur concentration in all species, and there were increases in foliar nitrogen in the two spruce species but not in pine. The concentrations of cations were frequently increased by SO₂ treatment, but there was no correlation between the sulphur concentration of needles and their total cation charge. SO₂-related elevations of foliar magnesium were correlated with the concentration of this element in soil solution, but the mechanism by which other cations were enhanced remains unclear. The only consistent effects on nutrient ratios were for SO₂ treatments to increase sulphur/cation ratios.     

Leaf surface properties of Norway spruce needles exposed to sulphur dioxide and ozone in an open-air fumigation system at Liphook

Samples of current-year and 1-year-old foliage were taken from Norway spruce (Picea abies (L.) Karst.) trees in April 1991, 4 months after a 3–4 year controlled fumigation with O₃ and SO₂ in the open at Liphook, south-east England. Trees were grown in seven plots, and treated in a factorial design with three levels of SO₂ and two levels of O₃ (ambient and c. 1.3 × ambient), with an extra ambient air plot. All statistical analyses were made on plot means. Leaf wettability, as measured by the contact angle of water droplets, was significantly affected by needle age and by SO₂ treatment (P≤0–05. in older needles, decreasing with increasing SO₂ concentration. There was no effect of O₃ on wettability, and no effect of any treatment on amounts of surface wax extracted by immersion of needles in chloroform. Electrolyte leakage rates from detached current-year needles were not affected by prior exposure to O₃, but decreased significantly (P= 0.034) with increasing exposure to SO₂. There was no detectable effect of fumigation on the rate of water loss from detached needles. Similarly, there was no effect of fumigation on the dry weight/fresh weight ratio of needles. The total sulphur content of needles increased significantly (P≤0.0001) with exposure to SO₂ and with needle age. Amounts of water-extractable sulphate, however, varied greatly among plots, but with no pattern with respect to fumigation treatment. It is concluded that leaf wettability and electrolyte leakage rates may be good indicators of the persistent effects of SO₂ on Norway spruce growing in the open air, and that the observed changes in leaf surface properties in response to SO₂ fumigation have implications for the processes, both biotic and abiotic, that occur on leaf surfaces.     

A Prototypic Intracellular Calcium Antagonist, TMB-8, Protects Cultured Cerebellar Granule Cells Against the Delayed, Calcium-Dependent Component of Glutamate Neurotoxicity

Abstract: The effect(s) of a prototypic intracellular Ca²⁺ antagonist, 8-(N,N-diethylamino)octyl-3,4,5-trimethoxybenzoate (TMB-8), on glutamate-induced neurotoxicity was investigated in primary cultures of mouse cerebellar granule cells. Glutamate evoked an increase in cytosolic free-Ca²⁺ levels ([Ca²⁺]_i) that was dependent on the extracellular concentration of Ca²⁺ ([Ca²⁺]_o). In addition, this increase in [Ca²⁺]_i correlated with a decrease in cell viability that was also dependent on [Ca²⁺]_o. Glutamate-induced toxicity, quantified by 3-(4,5-dimethylthiazol-2-yl)-2,5-diphenyltetrazolium bromide (MTT) staining, was shown to comprise two distinct components, an “early” Na⁺/Cl^?-dependent component observed within minutes of glutamate exposure, and a “delayed” Ca²⁺-dependent component (ED₅₀～50 µM) that coincided with progressive degeneration of granule cells 4–24 h after a brief (5–15 min) exposure to 100 µM glutamate. Quantitative analysis of cell viability and morphological observations identify a “window” in which TMB-8 (at >100 µM) protects granule cells from the Ca²⁺-dependent, but not the Na⁺/Cl^?-dependent, component of glutamate-induced neurotoxic damage, and furthermore, where TMB-8 inhibits glutamate-evoked increases in [Ca²⁺]_i. These findings suggest that Ca²⁺ release from a TMB-8-sensitive intracellular store may be a necessary step in the onset of glutamate-induced excitotoxicity in granule cells. However, these conclusions are compromised by additional observations that show that TMB-8 (1) exhibits intrinsic toxicity and (2) is able to reverse its initial inhibitory action on glutamate-evoked increases in [Ca²⁺]_i and subsequently effect a pronounced time-dependent potentiation of glutamate responses. Dantrolene, another putative intracellular Ca²⁺ antagonist, was completely without effect in this system with regard to both glutamate-evoked increases in [Ca²⁺]_i and glutamate-induced neurotoxicity.     

Seasonal and spatial patterns of S,Ca, and N dynamics of a Northern Hardwood forest ecosystem

Seasonal dynamics of S, Ca and N were examined at the Huntington Forest, a northern hardwood ecosystem in the central Adirondacks of New York for a period of 34 months (1985–1988). Solute concentrations and fluxes in bulk precipitation, throughfall (TF) and leachates from the forest floor, E horizon and B horizon were quantified. Both above and below-ground elemental fluxes mediated by vegetation (e.g. uptake, litter inputs, and fine roots production) were also determined. The roles of abiotic and biotic processes were ascertained based on both changes in solute concentrations through the strata of the ecosystem as well as differences between dormant and growing seasons. Concentrations of SO₄ ²⁻, NO₃ ⁻, NH₄ ⁺ and Ca²⁺ were greater in TF than precipitation. Forest floor leachates had greater concentrations of SO₄ ²⁻, NO₃ ⁻ + NH₄ ⁺ and Ca²⁺ (9, 6 and 77 μeq L⁻¹, respectively) than TF. There were differences in concentrations of ions in leachates from the forest floor between the dormant and growing seasons presumably due to vegetation uptake and microbial immobilization. Concentrations and fluxes of NO₃ ⁻ and NH; were greatest in early spring followed by a rapid decline which coincided with a demand for N by vegetation in late spring. Vegetation uptake (44.7 kg N ha⁻¹ yr⁻¹ ) could account for the low leaching rates of N0₃ ⁻. Within the mineral soil, changes with soil depth and the absence of seasonal patterns suggest that cation exchange (Ca⁺) or anion sorption (SO₄ ²⁻) are primarily responsible for regulating solute concentrations. The increase in SO₄ ²⁻ concentration after leachates passed through the mineral soil may be attributed to desorption of sulfate that was adsorbed during an earlier period when SO₄ ²⁻ concentrations would have been greater due to elevated S inputs.