The effects of wildfire on the water chemistry of dilute,acidic lakes in southern Norway

Changes in lake water chemistry were studied for >4 years following a large wildfire in a boreal forest area in Mykland, southern Norway, an area characterized by thin and patchy, base-poor and slow-weathering soils and bedrock. Accordingly, the lakes have low acid neutralizing capacity (ANC), calculated as the difference between the total concentration of base cations ([ΣBC]) and strong acid anions ([SAA]). During the initial post-fire period, and peaking about two months after the fire, the mobilization of SAA from terrestrial to aquatic systems caused a dramatic drop in ANC. In one of the lakes, ANC dropped from about 20 to ?80 μeq L^?1, while [H⁺] and inorganic aluminum ([Al_i]) increased to 38 μeq L^?1 (pH 4.42) and 326 μg Al L^?1 (36.2 μeq L^?1 as Al³⁺), respectively. Sulfate and chloride were the predominant anions responsible for this decline in ANC, as the nitrate increase was small. After the severe chemical episode, [SAA] in the lakes declined faster than [ΣBC], and within about one year after the wildfire, ANC was back to almost pre-fire values. However, despite the fact that [SAA] also continued to decline faster than [ΣBC] the following years, no further increase in ANC was documented. The strong ionic strength decline and the increase in TOC during the same period have likely counteracted for the potential ANC increase. There were large lake-to-lake variations in water chemistry of the wildfire affected lakes. Hydrology, geology, lake residence time and the catchment area to lake area ratio are important explanatory factors.     

An approach at estimating present day base cation weathering rates: a case study for the Hermine watershed,Canada

A new methodological approach is described for estimating Ca, Mg and K fluxes from soil mineral weathering. This method combines Na flux in surface waters in the Hermine watershed with base cation (BC) concentrations to Na molar ratios from the soil weatherable pool obtained using sequential extraction method. Comparison of BC:Na molar ratios of the weatherable pool with those from other compartments of the watershed suggests possible accumulation of base cations in some areas of the watershed, while losses or minimal changes are observed in others. On average, present day Na weathering rates estimated using the watershed input–output budget method was 0.26 (range 0.16–0.36) kmol_c ha^?1 yearr^?1, over the period of 1995–2006. For Ca, Mg and K, present day weathering rates estimated with the new methodological approach averaged 0.44 (range 0.27–0.60), 0.11 (range 0.07–0.15) and 0.02 (range 0.01–0.02) kmol_c ha^?1 year^?1, respectively. These values are within the range of present day rates previously calculated for the same site and for forested soils from similar granitic environments using other methods. Candidate models for predicting BC weathering rates on individual annual observations were developed using Akaike’s information criterion. The best model includes the number of frost days (inverse relationship) and explained 51% of the variation in total BC weathering rates. The newly developed method may be applicable to other watersheds, providing yearly estimates of nutrient BC at the watershed scale.     

Rationale of selection for specific nutritional characters in crop improvement withPhaseolus vulgaris L. as a case study

Genetic effects are obtainable for any aspect of transport, accumulation, and efficiency of nutrient use by plants, and for virtually any element. Some of the important characters are: tolerance to acid soils (18% of soils or 2.4 billion ha), tolerance to high pH induced Fe-chlorosis, and tolerance to salinity (about 1,000 m ha). Genotypes which made better use of N and P would be the means of saving fertilizers, especially important to developing countries. A 10% economy of fertilizer use represents a minimum world saving of US$6 billion annually. Phaseolus vulgaris is taken as a model to show that although we know quite a lot about the extent of its nutritional variation, e.g. adaptability to acid soils, and the crop's utilization of N and P, we are handicapped in exploiting this because of lack of genetic information. This in turn depends on knowledge of specific mechanisms, and investigating these must be a priority.IAEA Project BRA/5/009     

Hydration-State Change of Horse Heart Cytochrome c Corresponding to Trifluoroacetic-Acid-Induced Unfolding

We investigate the hydration state of horse-heart cytochrome c (hh cyt c) in the unfolding process induced by trifluoroacetic acid (TFA). The conformation of hh cyt c changes from the native (N) state (2.9 < pH < 6.0) to the acid-unfolded (U_A) state (1.7 < pH < 2.0) to the acid-induced molten globule (A) state (pH ∼1.2). Hydration properties of hh cyt c during this process are measured at 20°C by high-resolution dielectric relaxation (DR) spectroscopy, UV-vis absorbance, and circular dichroism spectroscopy. Constrained water of hh cyt c is observed at every pH as an ∼5-GHz Debye component (DC) (DR time, τ_D ∼30 ps) and its DR amplitude (DRA) is increased by 77% upon N-to-U_A transition, when pH changes from 6.0 to 2.0. Even in the N state, the DRA of the constrained-water component is found to be increased by 22% with decreasing pH from 6.0 to 2.9, suggesting an increase in the accessible surface area of native hh cyt c. Moreover, hypermobile water around native hh cyt c is detected at pH 6.0 as a 19-GHz DC (τ_D ∼ 8.4 ps < τ_DW = 9.4 ps), but is not found at other pH values. The DRA signal of constrained water is found to return to the pH 2.9 (N-state) level upon U_A-to-A transition. Fast-response water (slightly slower than bulk) around A-state hh cyt c is detected at pH 1.2, and this suggests some accumulation of TFA⁻ ions around the peptide chain. Thus, this high-resolution DR spectroscopy study reveals that hh cyt c exhibits significant hydration-state change in the TFA-unfolding process.     

Transport of auxin (indoleacetic acid) through lipid bilayer membranes

Summary Diffusion of auxin (indole-3-acetic acid) through planar lipid bilayer membranes was studied as a function of pH and auxin concentration. Membranes were made of egg or soybean lecithin or phosphatidyl serine inn-decane (25–35 mg/ml). Tracer and electrical techniques were used to estimate the permeabilities to nonionized (HA) and ionized (A^–) auxin. The auxin tracer flux is unstirred layer limited at low pH and membrane limited at high pH, i.e., when [A^–][HA]. The tracer flux is not affected by the transmembrane voltage and is much higher than the flux predicted from the membrane conductance. Thus, only nonionized auxin crosses the membrane at a significant rate. Auxin transport shows saturation kinetics, but this is due entirely to unstirred layer effects rather than to the existence of an auxin carrier in the membrane. A rapid interconversion of A^– and HA at the membrane surface allows A^– to facilitate the auxin flux through the unstirred layer. Thus, the total flux is higher than that expected for the simple diffusion of HA alone. The relation between flux (J _A), concentrations and permeabilities is: 1/J _A=1/P ^UL([A^–]+[HA])+1/P _HA ^M [HA]. By fitting this equation to our data we find thatP ^UL=6.9×10^–4 cm/sec andP _HA ^M =3.3×10^–3 cm/sec for egg lecithin-decane bilayers. Similar membrane permeabilities were observed with phosphatidyl serine or soybean lipids. Thus, auxin permeability is not affected by a net surface charge on the membrane. Our model describing diffusion and reaction in the unstirred layers can explain the anomolous relationship between pH and weak acid (or weak base) uptake observed in many plant cells.     

Effects of external pH,fusicoccin and butyrate on the cytoplasmic pH in barley root tips measured by 31P-nuclear magnetic resonance spectroscopy

³¹P-Nuclear magnetic resonance spectroscopy was used to measure the cytoplasmic pH (pH_c) in barley (Hordeum vulgare L.) root tips. As the external pH was raised from 4–10, pH_c was found to increase from 7.44 to 7.75. The sensitivity of pH_c to changes in external pH decreased with increasing external pH. Metabolic inhibition by sodium azide caused pH_c to fall by 0.3 units. Addition of 10 mM butyrate resulted in a gradual decline in pH_c, by approx. 0.3 units over 90 min. At a concentration of 1 mM, butyrate had no effect on pH_c even after 2 h. Fusicoccin caused pH_c to rise by 0.1–0.2 units. In maize (Zea mays L.) root tips, pH_c was shown to have a similar sensitivity to fusicoccin. The results are discussed in relation to the regulation of pH_c and the possible role of pH_c in determining transmembrane electrical potential differences.Abbreviations and symbols FC Fusicoccin - NMR nuclear magnetic resonance - p.d. membrane electrical potential difference - pH_c cytoplasmic pH - P1 inorganic phosphate - chemical shift     

Nitrogen fertilization raises CO2 efflux from inorganic carbon: A global assessment

Nitrogen (N) fertilization is an indispensable agricultural practice worldwide, serving the survival of half of the global population. Nitrogen transformation (e.g., nitrification) in soil as well as plant N uptake releases protons and increases soil acidification. Neutralizing this acidity in carbonate‐containing soils (7.49 × 10⁹ ha; ca. 54% of the global land surface area) leads to a CO₂ release corresponding to 0.21 kg C per kg of applied N. We here for the first time raise this problem of acidification of carbonate‐containing soils and assess the global CO₂ release from pedogenic and geogenic carbonates in the upper 1 m soil depth. Based on a global N‐fertilization map and the distribution of soils containing CaCO₃, we calculated the CO₂ amount released annually from the acidification of such soils to be 7.48 × 10¹² g C/year. This level of continuous CO₂ release will remain constant at least until soils are fertilized by N. Moreover, we estimated that about 273 × 10¹² g CO₂‐C are released annually in the same process of CaCO₃ neutralization but involving liming of acid soils. These two CO₂ sources correspond to 3% of global CO₂ emissions by fossil fuel combustion or 30% of CO₂ by land‐use changes. Importantly, the duration of CO₂ release after land‐use changes usually lasts only 1–3 decades before a new C equilibrium is reached in soil. In contrast, the CO₂ released by CaCO₃ acidification cannot reach equilibrium, as long as N fertilizer is applied until it becomes completely neutralized. As the CaCO₃ amounts in soils, if present, are nearly unlimited, their complete dissolution and CO₂ release will take centuries or even millennia. This emphasizes the necessity of preventing soil acidification in N‐fertilized soils as an effective strategy to inhibit millennia of CO₂ efflux to the atmosphere. Hence, N fertilization should be strictly calculated based on plant‐demand, and overfertilization should be avoided not only because N is a source of local and regional eutrophication, but also because of the continuous CO₂ release by global acidification.     

Further identification of the nature and linkage of the carbohydrate in hemoglobin A1c.

We have found that Hb A_1c contains neutral sugars which are only partially hydrolyzed from the N-termini of β chains. In both normal and diabetic Hb A_1c, 0.2–0.3 equivalents of hexose were released, composed primarily of glucose and mannose in a 3:1 ratio. When Hb A_1c was reduced with ³HNa BH₄ and then treated with periodic acid, most of the radioactivity was recovered as ³H-formic acid with much lesser amounts of ³H-formaldehyde. From these results, we propose that in the red cell, glucose binds to the α-amino position of hemoglobin β-chains (valine) in an aldimine (Schiff base) linkage. This aldimine can then partially rearrange in a reversible manner to form a ketoamine linkage which is stable to acid hydrolysis. This Amadori-type rearrangement accounts for the formation of mannose, the C-2 epimer of glucose, as well as the inability to demonstrate ³HNa BH₄ reduction at the C-1 position.     

Processes regulating temporal and longitudinal variations in the chemistry of a low-order woodland stream in the Adirondack region of New York

Watershed processes influence the acid neutralizing capacity of surface waters by mediating changes in concentration of ionic solutes. Acidification of surface waters by atmospheric deposition of mineral acids and the extent to which ecosystem transformations neutralize this acidity are of particular concern. Seasonal variations in flow paths of water through soil and biological processes result in short-term changes in chemistry that may be critical to surface water ecology. In this study, we assessed longitudinal and temporal variations in the chemistry of a low-order stream, Pancake-Hall Creek, located in the west-central Adirondack region of New York. By quantifying changes in ionic solute concentration (e.g. Ca²⁺, Al^a+, SO ₄ ^2– , NO ₃ ^– ) we were able to evaluate processes responsible for short-term fluctuations in acid/base chemistry.In the headwater sites, stream water was acidic; changes in pH, acid neutralizing capacity (ANC) and Al were primarily due to seasonal variations in basic cation and NO ₃ ^– concentrations. At the downstream sites, water migrated through a large beaver impoundment and thick till resulting in higher pH, acid neutralizing capacity and basic cation concentrations, and lower concentrations of Al. Neutralization of acidity was particularly evident during the low flow summer period and coincided with retention of SO ₄ ^2– in the beaver impoundment. During the high flow non-summer (October to June) period, depressed pH and ANC, and elevated Al concentrations were observed in the downstream sites. Acidic conditions during the non-summer period were not due to the oxidation of reduced sulfur deposits (e.g. SO ₄ ^2– events) but rather the resumption of conservative SO ₄ ^2– transport through the beaver impoundment (e.g. minimal SO ₄ ^2– retention) coupled with increases in NO ₃ ^– .     

Ageing of added copper in bentonite without and with humic acid

Abstract

The ageing of metals in soils plays an important role in assessing ecological risk and soil quality criteria, it therefore is necessary to understand the ageing processes. Using a sequential extraction procedure and a parabolic diffusion equation, the ageing of added copper(Cu) in bentonite without and with humic acid (HA) was investigated as a function of incubation time over one year. At the same time, the effect of pH on Cu ageing in bentonite with HA was also studied. The most labile Cu fractions (water-soluble Cu, Cu extracted by NH₄NO₃ and EDTA) gradually transformed into less extractable forms. The modelled diffusion equation suggested that the ageing processes were controlled by surface nucleation/precipitation and diffusion. In the presence of HA, the contribution from surface nuclea-tion/precipitation increased significantly, whereas that from diffusion decreased, this indicated the addition of HA significantly enhanced the short-term ageing by complexation with Cu ions, but strongly inhibited the further diffusion of Cu ions into interlayer of bentonite during long-term ageing owing to the more stable complexes formed on solid surface. With increasing pH in bentonite with HA, the apparent diffusion rate coefficient (D/r²) increased greatly, which showed that during long-term ageing pH played an important role in reducing the extractability as a result of the significant increase in residual Cu (RES-Cu), the most inert fraction, due to micropore diffusion.     

Enzymatic synthesis of β-lactam antibiotics: A thermodynamic background

The equilibrium constants and the respective standard Gibbs energy changes for hydrolysis of some β-lactam antibiotics have been determined. Native and immobilized penicillin amidase (EC 3.5.1.11) from Escherichia coli has been used as a catalyst. The values of standard Gibbs energy changes corresponding to the pH-independent product of equilibrium concentrations (ΔG⁰_c = ? RT ln K_c) have been calculated. The differences in the structure of the antibiotics nucleus hardly ever affect the value of the pH-independent component of the standard Gibbs energy change (ΔG⁰_c) and value of apparent standard Gibbs energy change at a fixed pH (ΔG^0′_c). At the same time, the value of ΔG⁰_c is more sensitive to the structure of the acyl moiety of the antibiotic; when ampicillin is used instead of benzylpenicillin, ΔG⁰_c increases by ～6.3 kJ mol^?1 (1.5 kcal mol^?1). pH-dependences of the apparent standard Gibbs energy changes for hydrolysis of β-lactam antibiotics have been calculated. The pH-dependences of ΔG^0′_c for hydrolysis of all β-lactam antibiotics have a similar pattern. The thermodynamic pH optimum of the synthesis of these compounds is in the acid pH range (pH < 5.0). The breakage of the β-lactam ring leads to a sharp decrease in the ΔG^0′_c value and a change in the pattern of the pH-dependence. For example, at pH 5.0 ΔG^0′_c decreases from 14.4 kJ mol^?1 for benzylpenicillin to ?1.45 kJ mol^?1 for benzylpenicilloic acid. The reason for these changes is mainly a considerable increase in the pK of the amino group of the nucleus of the antibiotic and, as a consequence, a decrease in the component of standard Gibbs energy change, corresponding to the ionization of the system. The thermodynamic potentials of the enzymatic synthesis of semisynthetic penicillins and cephalosporins on the basis of both free acids and their derivatives (N-acylated amino acids, esters) are discussed. It is shown that with esters of the acids, a high yield of the antibiotic can, in principle, be achieved at higher pH values.     

SCN− and HSCN transport through lipid bilayer membranes: A model for SCN− inhibition of gastric acid secretion

Diffusion of thiocyanate (SCN?) and thiocyanic acid (HSCN) (pK=?1.8) through lipid bilayer membranes was studied as a function of pH. Membranes were made of egg phosphatidylcholine or phosphatidylcholine plus cholesterol (1:1 mol ratio) dissolved in decane or tetradecane. Tracer fluxes and electrical conductances were used to estimate the permeabilities to HSCN and SCN?. Over the pH range 1.0 to 3.3 only HSCN crosses the membrane at a significant rate. The relation between the total SCN flux (JA), concentrations and permeabilities is: 1/JA=1/Pul([A?]+[HA])+1/PHAm[HA], where [A?] and [HA] are the concentrations of SCN? and HSCN, Pul is permeability coefficient of the unstirred layer, and PHAm is the membrane permeability to HSCN. By fitting this equation to the data we find that PHAm = 2.6 cm · s?1 and Pul = 9.0 · 10?4 cm · s?1. Conductance measurements indicate that PA?m is 5 · 10?9 cm · s?1. Addition of cholesterol to phosphatidylcholine (1:1 mol ratio) reduces PHAm by a factor of 0.4 but has no effect on PA?m. SCN? is potent inhibitor of acid secretion in gastric mucosa, but the mechanism of SCN? action is unknown. Our results suggest that SCN? acts by combining with H+ in the mucosal unstirred layer (secretory pits) and diffusing back into the cells as HSCN, thus dissipating the proton gradient across the secretory membrane. A similar mechanism of action is proposed for some other inhibitors of gastric acid secretion, e.g. nitrite (NO2?), cyanate (CNO?) and NH4+.     

A saturable site responsible for polar transport of indole-3-acetic acid in sections of maize coleoptiles

The velocity of transport and shape of a pulse of radioactive indole-3-acetic acid (IAA) applied to a section of maize (Zea mays L.) coleoptile depends strongly on the concentration of nonradioactive auxin in which the section has been incubated before, during, and after the radioactive pulse. A pulse of [³H]IAA disperses slowly in sections incubated in buffer (pH 6) alone; but when 0.5–5 M IAA is included, the pulse achieves its maximum velocity of about 2 cm h^-1. At still higher IAA concentrations in the medium, a transition occurs from a discrete, downwardly migrating pulse to a slowly advancing profile. Specificity of IAA in the latter effect is indicated by the observation that benzoic acid, which is taken up to an even greater extent than IAA, does not inhibit movement of [³H]IAA. These results fully substantiate the hypothesis that auxin transport consists of a saturable flux of auxin anions (A^-) in parallel with a nonsaturable flux of undissociated IAA (HA), with both fluxes operating down their respective concentration gradients. When the anion site saturates, the movement of [³H]IAA is nonpolar and dominated by the diffusion of HA. Saturating polar transport also results in greater cellular accumulation of auxin, indicating that the same site mediates the cellular efflux of A^-. The transport inhibitors napthylphthalamic acid and 2,3,5-triiodobenzoic acid specifically block the polar A^- component of auxin transport without affecting the nonsaturable component. The transport can be saturated at any point during its passage through the section, indicating that the carriers are distributed throughout the tissue, most likely in the plasmalemma of each cell.Abbreviations A^- auxin anion - HA undissociated auxin - IAA indole-3-acetic acid - NPA N-1-napthylphthalamic acid - TIBA 2,3,5-triiodobenzoic acid     

Influence of pH,exchangeable aluminium and 0.02M CaCl2-extractable aluminium on the growth and nitrogen-fixing activity of white clover (Trifolium repens) in some New Zealand soils

The effects of soil acidity on the growth and N₂-fixing activity of white clover in seven acid topsoils and subsoils of New Zealand were investigated using a glasshouse experiment.The application of phosphate (Ca(H₂PO₄)₂) to the soils resulted in very large increases in white clover growth on all soils. The application of phosphate, as well as increasing P supply, also decreased 0.02M CaCl₂-extractable Al levels, but had little effect on exchangeable Al levels.Where adequate phosphate was applied, increasing rates of lime (CaCO₃) resulted in increased plant growth on most soils. N₂[C₂H₂]-fixing activity was increased by the first level of lime for one soil, but generally remained approximately constant or declined slightly at higher rates of lime. Up to the point of maximum yield, white clover top weight was more highly correlated with 0.02M CaCl₂-extractable soil Al than with exchangeable Al or pH. At pH values greater than 5.5, plant yield declined on some soils, apparently because of Zn deficiency. The data suggest that white clover is unlikely to be affected by Al toxicity at 0.02M CaCl₂-extractable Al levels of less than about 3.3 g g^–1. However, there were differences between soils in apparent plant tolerance to 0.02M CaCl₂-extractable Al, which appeared to be caused by differing C levels in the 0.02M CaCl₂ extracts.     

One-electron reactions in biochemical systems as studied by pulse radiolysis. VI. Stages in the reduction of ferricytochrome c

When ferricytochrome c at pH about 9 is reduced by hydrated electrons and/or CO₂^?, it gives rise to an unstable form of ferrocytochrome c whose absorption spectrum, particularly in the Soret region, differs from that of normal ferrocytochrome c. This form changes intramolecularly (life-time about 0.1 s at ambient temperature) to yield normal ferrocytochrome c, and by 0.5 s the change in absorption spectrum in the range 225–600 nm produced by e^?_aq and/or CO₂^? is identical to the final change produced by reduction with an equivalent amount of sodium dithionite. This shows that both e^?_aq and CO^?₂ reduce cytochrome c with practically 100% efficiency. In the range 600–800 nm the spectrum of the unstable form is the same as that of normal ferrocytochrome c, both having small absorptions at 695 nm as compared with ferricytochrome c. As the unstable form disappears however a further loss of absorption at 695 nm occurs. This is taken to imply that the unstable form decays to a second unstable form which then rapidly donates an electron to the unchanged neutral form of ferricytochrome c, so reducing absorption in the 695 nm band. Subsequent to this process the absorption in the 695 nm band increases over a period of minutes owing to re-equilibration between the neutral and alkaline formes of ferricytochrome c. Between pH 7 and 10 the effect of pH on the absorption changes is consistent with the hypothesis of a second unstable form of ferrocytochrome c. Additional phenomena arise in more alkaline solutions. The rates of the various unimolecular processes are thought to be determined by the rates of change of conformation of the protein parts of the molecule following the change in oxidation state.     

Photosynthetic and Stomatal Responses of Two Mangrove Species, Aegiceras corniculatum and Avicennia marina, to Long Term Salinity and Humidity Conditions

Gas exchange characteristics were studied in two mangrove species, Aegiceras corniculatum (L.) Blanco and Avicennia marina (Forstk.) Vierh. var australasica (Walp.) Moldenke, grown under a variety of salinity and humidity conditions. The assimilation rate was measured as a function of the intercellular CO₂ concentration [A(c_i) curve]. The photosynthetic capacity decreased with increase in salinity from 50 to 500 millimolar NaCl, as shown by decline in both the initial linear slope and the upper plateau of the A(c_i) curve, with A. corniculatum being the more sensitive species. The decline in photosynthetic capacity was enhanced by increase in the leaf to air vapor pressure difference from 6 to 24 millibars, but this treatment caused a decrease in only the upper plateau of the A(c_i) curve. Stomatal conductance was such that the intercellular CO₂ concentration obtaining under normal atmospheric conditions occurred near the transition between the lower linear and upper plateau portions of the A(c_i) curves. Thus, stomatal conductance and photosynthetic capacity together co-limited the assimilation rate, which declined with increasing salinity and decreasing humidity. The marginal water cost of carbon assimilation was similar in most treatments, despite variation in the water loss/carbon gain ratio.     

Study on ATP concentration changes in cytosol of individual cultured neurons during glutamate-induced deregulation of calcium homeostasis

For the first time, simultaneous monitoring of changes in the concentration of cytosolic ATP ([ATP]_c), pH (pH_c), and intracellular free Ca²⁺ concentration ([Ca²⁺]_i) of the individual neurons challenged with toxic glutamate (Glu) concentrations was performed. To this end, the ATP-sensor AT1.03, which binds to ATP and therefore enhances the efficiency of resonance energy transfer between blue fluorescent protein (energy donor) and yellow-green fluorescent protein (energy acceptor), was expressed in cultured hippocampal neurons isolated from 1–2-day-old rat pups. Excitation of fluorescence in the acceptor protein allowed monitoring changes in pH_c. Cells were loaded with fluorescent low-affinity Ca²⁺ indicators Fura-FF or X-rhod-FF to register [Ca²⁺]_i. It was shown that Glu (20 μM, glycine 10 μM, Mg²⁺-free) produced a rapid acidification of the cytosol and decrease in [ATP]_c. An approximately linear relationship (r ² = 0.56) between the rate of [ATP]_c decline and latency of glutamate-induced delayed calcium deregulation (DCD) was observed: higher rate of [ATP]_c decrease corresponded to shorter DCD latency period. DCD began with a decrease in [ATP]_c of as much as 15.9%. In the phase of high [Ca²⁺]_i, the plateau of [ATP]_c dropped to 10.4% compared to [ATP]_c in resting neurons (100%). In the presence of the Na⁺/K⁺-ATPase inhibitor ouabain (0.5 mM), glutamate-induced reduction in [ATP]_c in the phase of the high [Ca²⁺]_i plateau was only 36.6%. Changes in [ATP]_c, [Ca²⁺]_i, mitochondrial potential, and pH_c in calcium-free or sodium-free buffers, as well as in the presence of the inhibitor of Na⁺/K⁺-ATPase ouabain, led us to suggest that in addition to increase in proton conductivity and decline in [ATP]_c, one of the triggering factors of DCD might be a reversion of the neuronal plasma membrane Na⁺/Ca²⁺ exchange.     

Photoinhibition of Photosystem I electron transfer activity in isolated Photosystem I preparations with different chlorophyll contents

Photoinhibition of the light-induced Photosystem I (PS I) electron transfer activity from the reduced dichlorophenol indophenol to methyl viologen was studied. PS I preparations with Chl/P700 ratios of about 180 (PS I-180), 100 (PS I-100) and 40 (PS I(HA)-40) were isolated from spinach thylakoid membranes by the treatments with Triton X-100, followed by sucrose density gradient centrifugation and hydroxylapatite column chromatography. White light irradiation (1.1 × 10⁴E m^–2 s^–1) of PS I-180 for 2 hours bleached 50% of the chlorophyll and caused a 58% decrease in the electron transfer activity with virtually no loss of the primary donor, P700. The flash-induced absorbance change showed the decay phase with a half time of about 10 s that was attributed to the P700 triplet, suggesting that the photoinhibitory light treatment caused the destruction of the PS I acceptor(s), F_x and possibly A₁. PS I-100 was similarly photobleached by the irradiation and the electron transfer activity decreased. There was, however, no apparent photoinhibition of the electron transport activity in PS I(HA)-40. Photoinhibition similar to that seen in PS I-180 also occurred in membrane fragments that were isolated without any detergent from a PS II-deficient mutant strain of the cyanobacterium Synechocystis sp. PCC 6803. PS I-180 was not photoinhibited under anaerobic conditions. The production of superoxide and fatty acid hydroperoxide during white light irradiation was significantly greater in PS I-180 than in PS I(HA)-40. The mechanism of photoinhibition in PS I preparations is discussed in relation to the formation of toxic oxygen molecules.Abbreviations A₀,A₁ primary and secondary electron acceptors of PS I - CD circular dichroism - DCPIP 2,6-dichlorophenol indophenol - F_A, F_B, F_X iron-sulfur centers A, B, X - HA hydroxylapatite - LHCI lightharvesting complex of PS I - MDA malondialdehyde - MV methyl viologen - Na-Asc sodium L-ascorbate - P700 primary electron donor of PS I - PFD photon flux density - PS I-A and PS I-B psaA and psaB gene products - TBA thiobarbituric acid     

Monitoring submersed vegetation in a mesotrophic lake: correlation of two spatio-temporal scales of change

The submersed vegetation of mesotrophic, alkaline Chenango Lake in New York, USA, was monitored at two spatio-temporal scales: a 200 m² grid censused annually from 1978 to 1993 and again in 2001 (12,800 quadrats), and a 1.8 ha littoral zone sampled every 6–10 years (1978, 1984, 1991, and 2001; 3600 quadrats). The grid vegetation fluctuated rather erratically for the first 11 years with each of the dominant species showing a different pattern of change. Frequency values for Chara vulgaris were the most dynamic, while those for Vallisneria americana were the most stable. After 1989, grid vegetation declined, so that by 2001, only four of the original 11 species were present (including the original dominants), and the total number of observations declined to <10% of the maximum recorded. This decline is attributed to vigorous benthic feeding by carp (Cyprinus carpio), not noted in 1978 but relatively abundant by 2001. Frequency changes of species in the 200 m² grid were positively correlated with corresponding frequency changes in the 1.8 ha littoral zone, indicating that a small, carefully chosen area may reflect vegetation at a larger scale. This was particularly true when vegetation change was appreciable.     

Assessment of annual carbon exchange in a water-stressed Pinus radiata plantation: an analysis based on eddy covariance measurements and an integrated biophysical model

We used a combination of eddy flux, chamber and environmental measurements with an integrated suite of models to analyse the seasonality of net ecosystem carbon uptake (F_CO2) in an 8-year-old, closed canopy Pinus radiata D.Don plantation in New Zealand (42°52′ S, 172°45′ E). The analyses utilized a biochemically based, big-leaf model of tree canopy photosynthesis (A_c), coupled to multiplicative environmental-constraint functions of canopy stomatal conductance (G_c) via environmental measurements, a temperature-dependent model of ecosystem respiration (R_eco), and a soil water balance model. Available root zone water storage capacity at the measurement site is limited to about 50 mm for the very stony soil, and annual precipitation is only 660 mm, distributed evenly throughout the year. Accordingly the site is prone to soil moisture deficit throughout the summer. G _c and A_c obtained maximum rates early in the growing season when plentiful soil water supply was associated with sufficient quantum irradiance (Q_abs), and moderate air saturation deficit (D) and temperature (T). From late spring onwards, soil water deficit and D confined G_c and A_c congruously, which together with the solely temperature dependency of R_eco resulted in the pronounced seasonality in F_CO2. Reflecting a light-limitation of A_c in the closed canopy, modelled annual carbon (C) uptake was most sensitive to changes in Q_abs. However, Q_abs did not vary significantly between years, and changes in annual F_CO2 were mostly due to variability in summer rainfall and D. Annual C-uptake of the forest was 717 g C m^–2 in a near-average rainfall year, exceeding by one third the net uptake in a year with 20% less than average rainfall (515 g C m^–2).