Effect of bicarbonate on the water-oxidizing complex of photosystem II in the super-reduced S-states

It is shown that the hydrazine-induced transition of the water-oxidizing complex (WOC) to super-reduced S-states depends on the presence of bicarbonate in the medium so that after a 20 min treatment of isolated spinach thylakoids with 3 mM NH(2)NH(2) at 20 degrees C in the CO(2)/HCO(3)(-)-depleted buffer the S-state populations are: 42% of S(-3), 42% of S(-2), 16% of S(-1) and even formal S(-4) state is reached, while in the presence of 2 mM NaHCO(3), the same treatment produces 30% of S(-3), 38% of S(-2), and 32% of S(-1) and there is no indication of the S(-4) state. Bicarbonate requirement for the oxygen-evolving activity, very low in untreated thylakoids, considerably increases upon the transition of the WOC to the super-reduced S-states, and the requirement becomes low again when the WOC returns back to the normal S-states using pre-illumination. The results are discussed as a possible indication of ligation of bicarbonate to manganese ions within the WOC.     

Interactions of photosystem II with bicarbonate, formate and acetate

In this study, we probe the effects of bicarbonate (hydrogencarbonate), BC, removal from photosystem II in spinach thylakoids by measuring flash-induced oxygen evolution patterns (FIOPs) with a Joliot-type electrode. For this we compared three commonly employed methods: (1) washing in BC-free medium, (2) formate addition, and (3) acetate addition. Washing of the samples with buffers depleted of BC and CO₂ by bubbling with argon (Method 1) under our conditions leads to an increase in the double hit parameter of the first flash (β₁), while the miss parameter and the overall activity remain unchanged. In contrast, addition of 40–50 mM formate or acetate results in a significant increase in the miss parameter and to an ∼50% (formate) and ∼10% (acetate) inhibition of the overall oxygen evolution activity, but not to an increased β₁ parameter. All described effects could be reversed by washing with formate/acetate free buffer and/or addition of 2–10 mM bicarbonate. The redox potential of the water-oxidizing complex (WOC) in samples treated by Method 1 is compared to samples containing 2 mM bicarbonate in two ways: (1) The lifetimes of the S₀, S₂, and S₃ states were measured, and no differences were found between the two sample types. (2) The S₁, S₀, S₋₁, and S₋₂ states were probed by incubation with small concentrations of NH₂OH. These experiments displayed a subtle, yet highly reproducible difference in the apparent S_i/S_−i state distribution which is shown to arise from the interaction of BC with PSII in the already reduced states of the WOC. These data are discussed in detail by also taking into account the CO₂ concentrations present in the buffers after argon bubbling and during the measurements. These values were measured by membrane-inlet mass spectrometry (MIMS).     

The sensitivity of Photosystem II to damage by UV-B radiation depends on the oxidation state of the water-splitting complex

The water-oxidizing complex of Photosystem II is an important target of ultraviolet-B (280-320 nm) radiation, but the mechanistic background of the UV-B induced damage is not well understood. Here we studied the UV-B sensitivity of Photosystem II in different oxidation states, called S-states of the water-oxidizing complex. Photosystem II centers of isolated spinach thylakoids were synchronized to different distributions of the S₀, S₁, S₂ and S₃ states by using packages of visible light flashes and were exposed to UV-B flashes from an excimer laser (λ = 308 nm). The loss of oxygen evolving activity showed that the extent of UV-B damage is S-state-dependent. Analysis of the data obtained from different synchronizing flash protocols indicated that the UV-sensitivity of Photosystem II is significantly higher in the S₃ and S₂ states than in the S₁ and S₀ states. The data are discussed in terms of a model where UV-B-induced inhibition of water oxidation is caused either by direct absorption within the catalytic manganese cluster or by damaging intermediates of the water oxidation process.     

How chloride functions to enable proton conduction in photosynthetic water oxidation: Time-resolved kinetics of intermediates (S-states) in vivo and bromide substitution

Chloride (Cl⁻) is essential for O₂ evolution during photosynthetic water oxidation. Two chlorides near the water-oxidizing complex (WOC) in Photosystem II (PSII) structures from Thermosynechococcus elongatus (and T. vulcanus) have been postulated to transfer protons generated from water oxidation. We monitored four criteria: primary charge separation flash yield (P* → P⁺Q_A⁻), rates of water oxidation steps (S-states), rate of proton evolution, and flash O₂ yield oscillations by measuring chlorophyll variable fluorescence (P* quenching), pH-sensitive dye changes, and oximetry. Br-substitution slows and destabilizes cellular growth, resulting from lower light-saturated O₂ evolution rate (−20 %) and proton release (−36 % ΔpH gradient). The latter implies less ATP production. In Br- cultures, protonogenic S-state transitions (S₂ → S₃ → S₀’) slow with increasing light intensity and during O₂/water exchange (S₀’ → S₀ → S₁), while the non-protonogenic S₁ → S₂ transition is kinetically unaffected. As flash rate increases in Cl⁻ cultures, both rate and extent of acidification of the lumen increase, while charge recombination is suppressed relative to Br⁻. The Cl⁻ advantage in rapid proton escape from the WOC to lumen is attributed to correlated ion-pair movement of H₃O⁺Cl⁻ in dry water channels vs. separated Br⁻ and H⁺ ion movement through different regions (>200-fold difference in Bronsted acidities). By contrast, at low flash rates a previously unreported reversal occurs that favors Br⁻ cultures for both proton evolution and less PSII charge recombination. In Br⁻ cultures, slower proton transfer rate is attributed to stronger ion-pairing of Br⁻ with AA residues lining the water channels. Both anions charge-neutralize protons and shepherd them to the lumen using dry aqueous channels.     

Function of plastoquinone in heat stress reactions of plants

The effect of high temperature treatment (40 °C, 3 h, illumination at 100 μmol m^− 2 s^− 1) on the photosynthetic electron flow in barley seedlings of different age was investigated. Thermoinduced inhibition of the liner electron flow due to partial impairment of the water oxidizing complex (WOC) and the increase in the extent of Q_A⁻ reoxidation by Tyr_z^ox in thylakoids isolated from 4-day-old leaves was shown by measurements of oxygen evolution using benzoquinone or potassium ferricyanide as electron acceptors, as well as by following Q_A⁻ reoxidation kinetics in the absence and presence of exogenous electron acceptors, DCBQ and DMBQ. Using HPLC analysis, an increase in the oxidation of the photoactive plastoquinone pool in young leaves under heating was shown. In older, 11-day-old leaves, heat treatment limited both photosynthetic electron flow and oxygen evolution. The same effects of heat shock on oxygen evolution caused an inhibition of electron flow on the donor side of PSII only. However, a rise in the proportion of PSII with Q_A⁻ reoxidized through recombination with the S₂/S₃ state of the WOC was observed. The addition of exogenous electron acceptors (DCBQ and DMBQ) and a donor (DPC) showed that the thermoinduced decrease in the electron transport rate was caused by an impediment of electron flow from Q_A⁻ to acceptor pool. The decrease in size of the photoactive PQ-pool and a change in the proportions of oxidized and reduced PQ in older leaves under heat treatment were shown. It was suggested that a thermoinduced change of the redox state of the PQ-pool and a redistribution of plastoquinone molecules between photoactive and non-photoactive pools are the mechanisms which reflect and regulate the response of the photosynthetic apparatus under heat stress conditions.     

Concentration-Dependent Effects on Intracellular and Surface pH of Exposing <Emphasis Type="Italic">Xenopus</Emphasis> oocytes to Solutions Containing NH<Subscript>3</Subscript>/NH<Subscript>4</Subscript><Superscript>+</Superscript>

Others have shown that exposing oocytes to high levels of (10–20 mM) causes a paradoxical fall in intracellular pH (pH_i), whereas low levels (e.g., 0.5 mM) cause little pH_i change. Here we monitored pH_i and extracellular surface pH (pH_S) while exposing oocytes to 5 or 0.5 mM NH₃/NH₄ ⁺. We confirm that 5 mM causes a paradoxical pH_i fall (−ΔpH_i ≅ 0.2), but also observe an abrupt pH_S fall (−ΔpH_S ≅ 0.2)—indicative of NH₃ influx—followed by a slow decay. Reducing [NH₃/NH₄ ⁺] to 0.5 mM minimizes pH_i changes but maintains pH_S changes at a reduced magnitude. Expressing AmtB (bacterial Rh homologue) exaggerates −ΔpH_S at both levels. During removal of 0.5 or 5 mM NH₃/NH₄ ⁺, failure of pH_S to markedly overshoot bulk extracellular pH implies little NH₃ efflux and, thus, little free cytosolic NH₃/NH₄ ⁺. A new analysis of the effects of NH₃ vs. NH₄ ⁺ fluxes on pH_S and pH_i indicates that (a) NH₃ rather than NH₄ ⁺ fluxes dominate pH_i and pH_S changes and (b) oocytes dispose of most incoming NH₃. NMR studies of oocytes exposed to ¹⁵N-labeled show no significant formation of glutamine but substantial accumulation in what is likely an acid intracellular compartment. In conclusion, parallel measurements of pH_i and pH_S demonstrate that NH₃ flows across the plasma membrane and provide new insights into how a protein molecule in the plasma membrane—AmtB—enhances the flux of a gas across a biological membrane.

Application of the Marcus theory for analysis of the temperature dependence of the reactions leading to photosynthetic water oxidation: results and implications

The temperature dependence of donor side reactions was analysed within the framework of the Marcus theory of nonadiabatic electron transfer. The following results were obtained for PS II membrane fragments from spinach: (1) the reorganisation energy of P680^+? reduction by Y_Z is of the order of 0.5?eV in samples with a functionally fully competent water oxidising complex (WOC); (2) destruction of the WOC by Tris-washing gives rise to a drastic increase of λ to values of the order of 1.6?eV; (3) the reorganisation energies of the oxidation steps in the WOC are dependent, on the redox states S _i with values of about 0.6?eV for the reactions Y_Z ^OX S ₀→Y_Z S ₁ and Y_Z ^OX S ₁→Y_Z S ₂, 1.6?eV for the reaction Y_Z ^OX S ₂→Y_Z S ₃ and 1.1?eV (above a characteristic temperature u_c of about 6??°C) for the reaction Y_Z ^OX S ₃→→Y_Z S ₀+O₂. Using an empirical rate constant-distance relationship, the van der Waals distance between Y_Z and P680 was found to be about 10?Å, independent of the presence or absence of the WOC, whereas the distance between Y_Z and the manganese cluster in the WOC was ≥15?Å. Based on the calculated activation energies the environment of Y_Z is inferred to be almost "dry" and hydrophobic when the WOC is intact but becomes enriched with water molecules after WOC destruction. Furthermore, it is concluded that the transition S ₂→S ₃ is an electron transfer reaction gated by a conformational change, i.e. it comprises significant structural changes of functional relevance. Measurements of kinetic H/D isotope exchange effects support the idea that none of these reactions is gated by the break of a covalent O-H bond. The implications of these findings for the mechanism of water oxidation are discussed.     

High misses after odd flashes in oxygen evolution in thoroughly dark-adapted thylakoids from pea and Chenopodium album

In Photosystem II (PS II), water is oxidized to molecular oxygen and plastoquinone is reduced to plastoquinol. The oxidation of water requires the accumulation of four oxidizing equivalents, through the so-called S-states of the oxygen evolving complex; the production of plastoquinol requires the accumulation of two reducing equivalents on a bound plastoquinone, Q_B. It has been generally believed that during the flash-induced transition of each of the S-states (S_n S_n+1, where n=0, 1, 2 and 3), a certain small but equal fraction of the PS II reaction centers are unable to function and, thus, miss being turned over. We used thoroughly dark-adapted thylakoids from peas (Pisum sativum) and Chenopodium album (susceptible and resistant to atrazine) starting with 100% of the oxygen evolving complex in the S₁ state. Thylakoids were illuminated with saturating flashes, providing a double hit parameter of about 0.07. Our experimental data on flashnumber dependent oscillations in the amount of oxygen per flash fit very well with a binary pattern of misses: 0, 0.2, 0, 0.4 during S₀ S₁, S₁ S₂, S₂ S₃ and S₃ S₀ transitions. Addition of 2 mM ferricyanide appears to shift this pattern by one flash. These results are consistent with the bicycle model recently proposed by V. P. Shinkarev and C. A. Wraight (Oxygen evolution in photosynthesis: From unicycle to bicycle, 1993, Proc Natl Acad Sci USA 90: 1834–1838), where misses are due to the presence of P⁺ or Q_A ^- among the various equilibrium states of PS II centers.Abbreviations miss parameter - double hit parameter - PS II Photosystem II - Q_A primary one-electron acceptor of PS II, a plastoquinone molecule - Q_B secondary plastoquinone two-electron acceptor of PS II - S-states (S_n, where n=0, 1, 2, 3 or 4) redox states of the oxygen evolving complex     

Optical characterization of intermediates in the water-splitting enzyme system of photosynthesis — possible states and configurations of manganese and water

Absorption changes coupled with the individual transitions S₀–S₃ and redox reactions in the water-splitting enzyme system S of photosynthesis have been measured. The principal difficulties of measuring the very small absorption changes in the ultraviolet coupled with those reactions have been reduced drastically through the use of a highly purified Photosystem II complex isolated from the Cyanobacterium synechococcus. The general problem caused by the mixing of the S states during a train of flashes and the falsification through the overlap with absorption changes of Q_B (binary oscillations) have been treated as follows. (1) The binary oscillations were bypassed through the use of silicomolybdate and high concentrations of DCBQ, respectively, as external electron acceptor. (2) Stable absorption changes of the mixed S-state transitions have been deconvoluted through fitting procedures to get the changes of the individual transitions of S₁ → S₂ → S₃ → S₀ → S₁. (3) Kinetically resolved absorption changes of the S-states in the 100-μs range gave independent information on the individual transitions. (4) Stable absorption changes of the S₀ → S₁ transitions in the forefront were induced after shifting the S states through low concentrations of NH₂OH two units backwards. Analysis of the resulting sequence S_x → S₀ → S₁ → S₂ → S₃ → S₀, beginning with an NH₂OH depending pre-state, S_x, and followed by an S₀ → S₁ transition not mixed with the opposite S₃ → S₀ transition, increased the conclusiveness considerably. It results that the ultraviolet spectrum of the S₀ → S₁ transition is different from the spectra of the S₁ → S₂ and S₂ → S₃ transition. Possible states of manganese, water and surplus charges responsible for these spectra are presented.     

Inhibition of the catalase reaction of Photosystem II by anions

A new binding site for anions which inhibit the water oxidizing complex (WOC) of Photosystem II in spinach has been identified. Anions which bind to this site inhibit the flash-induced S₂/S₀ catalase reaction (2H₂O₂2H₂O+O₂) of the WOC by displacing hydrogen peroxide. Using a mass spectrometer and gas permeable membrane to detect the ³²O₂ product, the yield and lifetime of the active state of the flash-induced catalase (to be referred to simply as flash-catalase) reaction were measured after forming the S₂ or S₀-states by a short flash. The increase in flash-catalase activity with H₂O₂ concentration exhibits a K_m=10–20 mM, and originates from an increase in the lifetime by 20-fold of the active state. The increased lifetime in the presence of peroxide is ascribed to formation of the long-lived S₀-state at the expense of the unstable S₂-state. The anion inhibition site differs from the chloride site involved in stimulating the photolytic water oxidation reaction (2H₂OO₂+4e^-+4H⁺). Whereas water oxidation requires Cl^- and is inhibited with increasing effectiveness by F^-CN^-N₃ ^-, the flash-catalase reaction is weakly inhibited by Cl^-, and with increasing effectiveness by F^-CN^-, N₃ ^-. Unlike water oxidation, chloride is unable to suppress or reverse inhibition of the flash-catalase reaction caused by these anions. The inhibitor effectiveness correlates with the pK_a of the conjugate acid, suggesting that the protonated species may be the active inhibitor. The reduced activity arises from a shortening of the lifetime of the flash-induced catalase active state by 3–10 fold owing to stronger anion binding in the flash-induced states, S₂ and S₀, than in the dark S-states, S₁ and S_-1. To account for the paradoxical result that higher anion concentrations are required to inhibit at lower H₂O₂ concentrations, where S₂ forms initially after the flash, than at higher H₂O₂ concentrations, where S₀ forms initially after the flash, stronger anion binding to the S₀-state than to the S₂-state is proposed. A kinetic model is given which accounts for these equilibria with anions and H₂O₂. The rate constant for the formation/release of O₂ by reduction of S₂ in the WOC is <0.4 s^-1.Abbreviations ADRY acceleration of the deactivation reactions of the water splitting enzyme system Y - BTP bis [tris(hydroxymethyl)methylamino]-propane - CCCP carbonylcyanide m-chlorophenylhyrazone - DCBQ 2,5-dichlorobenzoquinone - DMBQ 2,3-dimethylbenzoquinone - WOC water oxidizing complex     

Evidence for intermediate S-states as initial phase in the process of oxygen-evolving complex oxidation

We have analyzed flash-induced period-four damped oscillation of oxygen evolution and chlorophyll fluorescence with the aid of a kinetic model of photosystem II. We have shown that, for simulation of the period-four oscillatory behavior of oxygen evolution, it is essential to consider the so-called intermediate S-state as an initial phase of each of the S_n-S_n+1, (n = 0, 1, 2, 3) transitions. The intermediate S-states are defined as []-states (n = 0, 1, 2, 3) and are formed with rate constant k_iSn ∼1.5 × 10⁶ s⁻¹, which was determined from comparison of theoretical predictions with experimental data. The assumed intermediate S-states shift the equilibrium in reaction more to the right and we suggest that kinetics of the intermediate S-states reflects a relaxation process associated with changes of the redox equilibrium in the above reaction. The oxygen oscillation is simulated without the miss and double-hit parameters, if the intermediate S-states, which are not the source of the misses or the double-hits, are included in the simulation. Furthermore, we have shown that the intermediate S-states, together with charge recombination, are prerequisites for the simulation of the period-four oscillatory behavior of the chlorophyll fluorescence.     

Mechanistic and structural aspects of photosynthetic water oxidation

Conclusions on the functional and structural organisation of photosynthetic water oxidation are gathered from a critical survey of the wealth of data reported in the literature and author's own experimental research: (1) the water oxidising complex (WOC) contains a tetranuclear manganese cluster of dimer of dimers' structure and functional heterogeneity of the metal centers, (2) the four step univalent oxidative pathway leading to water oxidation into molecular oxygen and four protons comprises only manganese, tyrosine Y_Z of polypeptide Dl and the substrate as redox active species, (3) the redox transitions S₀→ S₁ and S₁→ S₂ are manganese centered whereas S₂→ S₃ is most likely a ligand-centered reaction, (4) there exist several lines of evidence for a marked structural change that accompanies the redox transition S₂→ S₃, (5) one Ca²⁺ is an indispensible constituent of a functionally competent WOC while the role of Cl is much less clear and a direct participation disputable, (6) substrate water is most likely bound in all redox states S₀,…,S₃ and exchangeable with the bulk phase. The protonation state is determined by the redox state S₁ and the protein microenvironment. A mechanism is proposed for water oxidation in the WOC that is based on three key postulates: (1) water oxidation takes place in the first coordination sphere of one manganese dimer [Mn_aMn_b]; (2) the essential O-O bond is preformed in S₃ as part of a rapid redox isomerism S₃(I)→S₃(II) where in S₃(II) a nuclear geometry and electronic configuration is attained that corresponds to a peroxidic-type species; and (3) S₃(II) is an ‘entatic state’ for the formation of complexed dioxygen triggered by Y_Z^OX induced electron abstraction from the WOC and electronic redistribution to S₀(O₂).     

Electron transfer from Cyt b 559 and tyrosine-D to the S2 and S3 states of the water oxidizing complex in photosystem II at cryogenic temperatures

The Mn₄CaO₅ cluster of photosystem II (PSII) catalyzes the oxidation of water to molecular oxygen through the light-driven redox S-cycle. The water oxidizing complex (WOC) forms a triad with Tyrosine_Z and P₆₈₀, which mediates electrons from water towards the acceptor side of PSII. Under certain conditions two other redox-active components, Tyrosine_D (Y_D) and Cytochrome b ₅₅₉ (Cyt b ₅₅₉) can also interact with the S-states. In the present work we investigate the electron transfer from Cyt b ₅₅₉ and Y_D to the S₂ and S₃ states at 195 K. First, Y_D ^? and Cyt b ₅₅₉ were chemically reduced. The S₂ and S₃ states were then achieved by application of one or two laser flashes, respectively, on samples stabilized in the S₁ state. EPR signals of the WOC (the S₂-state multiline signal, ML-S₂), Y_D ^? and oxidized Cyt b ₅₅₉ were simultaneously detected during a prolonged dark incubation at 195 K. During 163 days of incubation a large fraction of the S₂ population decayed to S₁ in the S₂ samples by following a single exponential decay. Differently, S₃ samples showed an initial increase in the ML-S₂ intensity (due to S₃ to S₂ conversion) and a subsequent slow decay due to S₂ to S₁ conversion. In both cases, only a minor oxidation of Y_D was observed. In contrast, the signal intensity of the oxidized Cyt b ₅₅₉ showed a two-fold increase in both the S₂ and S₃ samples. The electron donation from Cyt b ₅₅₉ was much more efficient to the S₂ state than to the S₃ state.     

Insights into the function of PsbR protein in Arabidopsis thaliana

The functional state of the Photosystem (PS) II complex in Arabidopsis psbR T-DNA insertion mutant was studied. The ΔPsbR thylakoids showed about 34% less oxygen evolution than WT, which correlates with the amounts of PSII estimated from Y_D^ox radical EPR signal. The increased time constant of the slow phase of flash fluorescence (FF)-relaxation and upshift in the peak position of the main TL-bands, both in the presence and in the absence of DCMU, confirmed that the S₂Q_A⁻ and S₂Q_B⁻ charge recombinations were stabilized in ΔPsbR thylakoids. Furthermore, the higher amount of dark oxidized Cyt-b559 and the increased proportion of fluorescence, which did not decay during the 100s time span of the measurement thus indicating higher amount of Y_D⁺Q_A⁻ recombination, pointed to the donor side modifications in ΔPsbR. EPR measurements revealed that S₁-to-S₂-transition and S₂-state multiline signal were not affected by mutation. The fast phase of the FF-relaxation in the absence of DCMU was significantly slowed down with concomitant decrease in the relative amplitude of this phase, indicating a modification in Q_A to Q_B electron transfer in ΔPsbR thylakoids. It is concluded that the lack of the PsbR protein modifies both the donor and the acceptor side of the PSII complex.     

Photolysis of the ion pair [Pt(NH3)5Cl]S2O8: reduction of platinum(IV) induced by outer-sphere charge transfer excitation

The ion pair [Pt^IV(NH₃)₅Cl]³⁺S₂O₈²⁻ shows a S₂O₈²⁻ → [Pt(NH₃)₅Cl]³⁺ outer-sphere charge transfer (OSCT) absorption at λ_max=267 nm. OSCT excitation leads to the reduction of Pt(IV) by S₂O₈²⁻ to Pt(II) with φ=3×10⁻³ at λ_irr=280 nm.     

Oxidation state changes of the Mn<Subscript>4</Subscript>Ca cluster in Photosystem II

A detailed electronic structure of the Mn₄Ca cluster is required before two key questions for understanding the mechanism of photosynthetic water oxidation can be addressed. They are whether all four oxidizing equivalents necessary to oxidize water to O₂ accumulate on the four Mn ions of the oxygen-evolving complex, or do some ligand-centered oxidations take place before the formation and release of O₂ during the S₃ → [S₄] → S₀ transition, and what are the oxidation state assignments for the Mn during S-state advancement. X-ray absorption and emission spectroscopy of Mn, including the newly introduced resonant inelastic X-ray scattering spectroscopy have been used to address these questions. The present state of understanding of the electronic structure and oxidation state changes of the Mn₄Ca cluster in all the S-states, particularly in the S₂ to S₃ transition, derived from these techniques is described in this review.     

Effect of calcium ions and anaerobic microbial activity on sedimentation of oil sands tailings

Oil sands tailings ponds contain large volumes (∼10⁸ m³) of fine tailings, originating from bitumen production by surface mining. These sediment rapidly in dilute suspension but then form a network, which consolidates much more slowly. The overall process increases solid content to up to 85% (w/w) and is referred to as tailings densification. Addition of gypsum (CaSO₄·2H₂O) to a mixture of sand and fines gives a non-segregating, consolidated tailings slurry in which calcium ions serve as a cross-linking agent. Tailings ponds also harbor active anaerobic microbial consortia, which are thought to contribute to densification through microbial activity, including gas production, creating dewatering channels. To determine the roles of calcium ions and anaerobic microbial activity in tailings sedimentation, we placed 70% (v/v) tailings, containing 77% (w/w) solids, and 30% (v/v) defined medium with various amendments in anaerobic test tubes with an N₂–CO₂ headspace. Following mixing the initial sedimentation rate R of the water-tailings boundary and the final percentage (v/v) of sedimentation S_F were measured. Amendment with 0–20 mM CaCl₂ increased R from 0.006 to up to 0.012 day⁻¹, but decreased S_F from 14–15% to 8–10% (v/v), whereas subsequent amendment with lactate increased both R and S_F. To determine the effect of the type of anaerobic microbial activity, tubes were amended with (i) 20 mM NaCl or 10 mM CaCl₂, (ii) 10 mM Na₂SO₄ or 10 mM CaSO₄, (iii) 20 mM NaNO₃ or 10 mM Ca(NO₃)₂, or (iv) no additions. Following mixing, duplicate tubes were monitored continuously to determine S_F, whereas another set of duplicate tubes was re-mixed once per week to determine R, as well as headspace methane, and the concentrations of sulfate, sulfide, nitrate and nitrite in the supernatant fluid. Microbial activity was boosted after 63 days by adding 20 mM lactate to all tubes. The data for this experiment also indicated that R increased, whereas S_F decreased by addition of calcium ions. Lactate significantly boosted microbial activity with increased methanogenesis, sulfate reduction or nitrate reduction being observed in tubes amended with no electron acceptor, sulfate or nitrate, respectively. Addition of lactate increased S_F by 2–4% (v/v) in most tubes, except in tubes with Ca(NO₃)₂ in which S_F increased by 15% (v/v). The solids content increased from 69 to 78% under these conditions, representing a significant progression to the maximum values observed in tailings ponds over a short period of time.     

Bicarbonate effect on electron flow in a cyanobacteriumSynechocystis PCC 6803

In this communication, evidence is presented from the kinetics of Q_A ^? decay (where Q_A is the first plastoquinone electron acceptor of photosystem II) and oxygen evolution for the requirement of bicarbonate in the electron transport in a cyanobacteriumSynechocystis (Pasteur Culture Collection 6803). A large slowing down of Q_A ^? oxidation, measured from the variable chlorophylla fluorescence after saturating actinic flashes, was observed in the thylakoids ofSynechocystis 6803 depleted of bicarbonate in the presence of 25 mM formate. Qualitatively similar results were obtained with DCMU-treated thylakoids. This shows that bicarbonate depletion inhibits electron transport on the acceptor side of photosystem II between Q_A and the plastoquinone (PQ) pool in cyanobacteria. Addition of 2.5 mM HCO₃ ^? fully reversed the inhibition of electron flow caused by bicarbonate depletion. Two exponential phases of Q_A ^? decay, a fast one and a slow one, were observed with halftimes of approx. 400 μs (fast) and 26 ms (slow) at pH 6.5. At pH 7.5, these phases were approx. 330 μs (fast) and 21 ms (slow), respectively. The amplitude, but not the halftime, of the fast component decreased by about 70% (pH 6.5) or 50% (pH 7.5); this was accompanied by a concomittant increase in the slow phase. Twenty mM bicarbonate stimulated, by a factor of 4, the Hill reaction in bicarbonate-depletedSynechocystis cells. This effect is independent of CO₂ fixation as it was observed even in the presence of an inhibitor DBMIB.     

Evaluation of the potential role of the macroalga Laminaria japonica for alleviating coastal eutrophication

The rapid development of human activities has caused serious eutrophication of coastal waters in China in the recent decades. The study of the biofiltration capacity of Laminaria japonica under laboratory conditions showed a significant nutrient uptake. After 36 h of incubation, around 42%, 46%, 44% of N and 45%, 42%, 35% of P were removed from three gradients of medium concentrations, respectively. In the conditions of different ratios of N/P and NO₃–N/NH₄–N, the optimum N/P ratio for nutrient uptake was 7.4 and L. japonica prefered NO₃–N rather than NH₄–N as nitrogen source. Temperature and irradiance affected uptake rates significantly. The maximal N uptake rate appeared at 10 °C and 18 μmol photons m⁻² s⁻¹ and the maximal P uptake rate was found at 15 °C and 144 μmol photons m⁻² s⁻¹. Moreover, further studies were needed to investigate the bioremediation potential of L. japonica in the open sea.     

Factors influencing hydroxylamine inactivation of photosynthetic water oxidation

The kinetics of Mn release during NH₂OH inactivation of the water oxidizing reaction is largely insensitive to the S-state present during addition of NH₂OH. This appears to reflect reduction by NH₂OH of higher S-states to a common more reduced state (S₀ or S_?1) which alone is susceptible to NH₂OH inactivation. Sequences of saturating flashes with dark intervals in the range 0.2–5 s^?1 effectively prevent NH₂OH inactivation and the associated liberation of manganese. This light-induced protection disappears rapidly when the dark interval is longer than about 5 s. Under continuous illumination, protection against NH₂OH inactivation is maximally effective at intensities in the range 10³–10⁴ erg · cm^?2 · s^?1. This behavior differs from that of NH₂OH-induced Mn release, which is strongly inhibited at all intensities greater than 10³ erg · cm^?2 · s^?1. This indicates that two distinct processes are responsible for inactivation of water oxidation at high and low intensities. Higher S-states appear to be immune to the reaction by which NH₂OH liberates manganese, although the overall process of water oxidation is inactivated by NH₂OH in the presence of intense light. The light-induced protection phenomenon is abolished by 50 μM DCMU, but not by high concentrations of carbonyl cyanide m-chlorophenylhydrazone, which accelerates inactivation reactions of the water-splitting enzyme, Y (an ADRY reagent). The latter compound accelerates both inactivation of water oxidation and manganese extraction in the dark.