Coral reef calcifiers buffer their response to ocean acidification using both bicarbonate and carbonate

Central to evaluating the effects of ocean acidification (OA) on coral reefs is understanding how calcification is affected by the dissolution of CO₂ in sea water, which causes declines in carbonate ion concentration [CO₃²⁻] and increases in bicarbonate ion concentration [HCO₃⁻]. To address this topic, we manipulated [CO₃²⁻] and [HCO₃⁻] to test the effects on calcification of the coral Porites rus and the alga Hydrolithon onkodes, measured from the start to the end of a 15-day incubation, as well as in the day and night. [CO₃²⁻] played a significant role in light and dark calcification of P. rus, whereas [HCO₃⁻] mainly affected calcification in the light. Both [CO₃²⁻] and [HCO₃⁻] had a significant effect on the calcification of H. onkodes, but the strongest relationship was found with [CO₃²⁻]. Our results show that the negative effect of declining [CO₃²⁻] on the calcification of corals and algae can be partly mitigated by the use of HCO₃⁻ for calcification and perhaps photosynthesis. These results add empirical support to two conceptual models that can form a template for further research to account for the calcification response of corals and crustose coralline algae to OA.     

Na-Stimulation of Photosynthesis in the Cyanobacterium Synechococcus UTEX 625 Grown on High Levels of Inorganic Carbon

Photosynthesis of washed cells of Synechococcus UTEX 625 grown on 5% CO₂ was markedly stimulated (647 ± 50%) at pH 8.0 by the addition of low concentrations of NaCl (concentration required for half-maximal response, K_½, = 18 micromolar). Studies with KCl and Na₂SO₄ showed that the stimulation was due to Na⁺. Photosynthesis at pH 6.1 was only slightly stimulated by Na⁺. The response of photosynthesis at pH 8.0 to [Na⁺] was strongly sigmoidal for dissolved inorganic carbon ([DIC] ≤ 500 micromolar). Cells grown with high total [DIC], but air-levels of CO₂, at pH 9.6 showed the same response to low [Na⁺]. The absence of Na⁺ could be partially, but not completely overcome, by higher [DIC]. Various methods for examining CO₂ or HCO₃⁻ use (K_½^CO₂ determination; isotopic disequilibrium; and consideration of HCO₃⁻ dehydration rate) were consistent with CO₂ use by the cells, but HCO₃⁻ use could not be ruled out. Isotopic disequilibrium studies showed that CO₂ use was stimulated by Na⁺. Cells grown on 5% CO₂ accumulated DIC against a concentration gradient by a process (or processes) dependent on Na⁺. No evidence for uptake of Na⁺ concomitant with DIC uptake could be found. The lack of O₂ evolution during the initial and most rapid period of DIC accumulation suggested that the required energy was obtained from cyclic photophosphorylation.     

Proton Pump Activity of Mitochondria-rich Cells : The Interpretation of External Proton-concentration Gradients

We have hypothesized that a major role of the apical H⁺-pump in mitochondria-rich (MR) cells of amphibian skin is to energize active uptake of Cl⁻ via an apical Cl⁻/HCO₃ ⁻-exchanger. The activity of the H⁺ pump was studied by monitoring mucosal [H⁺]-profiles with a pH-sensitive microelectrode. With gluconate as mucosal anion, pH adjacent to the cornified cell layer was 0.98 ± 0.07 (mean ± SEM) pH-units below that of the lightly buffered bulk solution (pH = 7.40). The average distance at which the pH-gradient is dissipated was 382 ± 18 μm, corresponding to an estimated “unstirred layer” thickness of 329 ± 29 μm. Mucosal acidification was dependent on serosal pCO₂, and abolished after depression of cellular energy metabolism, confirming that mucosal acidification results from active transport of H⁺. The [H⁺] was practically similar adjacent to all cells and independent of whether the microelectrode tip was positioned near an MR-cell or a principal cell. To evaluate [H⁺]-profiles created by a multitude of MR-cells, a mathematical model is proposed which assumes that the H⁺ distribution is governed by steady diffusion from a number of point sources defining a set of particular solutions to Laplace''s equation. Model calculations predicted that with a physiological density of MR cells, the [H⁺] profile would be governed by so many sources that their individual contributions could not be experimentally resolved. The flux equation was integrated to provide a general mathematical expression for an external standing [H⁺]–gradient in the unstirred layer. This case was treated as free diffusion of protons and proton-loaded buffer molecules carrying away the protons extruded by the pump into the unstirred layer; the expression derived was used for estimating stationary proton-fluxes. The external [H⁺]-gradient depended on the mucosal anion such as to indicate that base (HCO₃ ⁻) is excreted in exchange not only for Cl ⁻, but also for Br⁻ and I⁻, indicating that the active fluxes of these anions can be attributed to mitochondria-rich cells.     

A Guide to Establishing Water Potential of Aqueous Two-Phase Solutions (Polyethylene Glycol plus Dextran) by Amendment with Mannitol

A practical guide to calculating the mannitol (MAN) amendment required to achieve the desired water potential (Ψ) of polyethylene glycol/dextran (PEG/DEX) aqueous two-phase systems for protoplast purification is presented. The empirically generated equation Ψ = 305[PEG′]²[MAN] + 0.74[PEG′][MAN]T − 103[PEG′][MAN] + 5.6[PEG′]²T − 623[PEG′]² − 0.25[PEG′]T + 12.7[PEG′] − 0.078[MAN]T − 22.75[MAN]accurately predicts experimental Ψ (in bars). [PEG′] indicates the presence of DEX where [DEX] = [PEG]/(0.6−0.4[PEG]). The equation is applicable for these ranges: [PEG′] from 0.047 to 0.13 gram per gram H₂O; [MAN] from 0 to 0.7 molal; T from 4.5 to 40°C. Actual Ψ should differ from derived Ψ by no more than 8% for the least negative values to 4% for the most negative values. The Ψ for solutions of MAN, of PEG, and of DEX were also determined. Equations to fit data for each were generated. Analyses indicated a significant synergistic effect on Ψ when MAN is added to PEG/DEX and, at certain concentrations, between PEG and DEX.     

Effects of High Dissolved Inorganic and Organic Carbon Availability on the Physiology of the Hard Coral Acropora millepora from the Great Barrier Reef

Coral reefs are facing major global and local threats due to climate change-induced increases in dissolved inorganic carbon (DIC) and because of land-derived increases in organic and inorganic nutrients. Recent research revealed that high availability of labile dissolved organic carbon (DOC) negatively affects scleractinian corals. Studies on the interplay of these factors, however, are lacking, but urgently needed to understand coral reef functioning under present and near future conditions. This experimental study investigated the individual and combined effects of ambient and high DIC (pCO₂ 403 μatm/ pH_Total 8.2 and 996 μatm/pH_Total 7.8) and DOC (added as Glucose 0 and 294 μmol L^-1, background DOC concentration of 83 μmol L^-1) availability on the physiology (net and gross photosynthesis, respiration, dark and light calcification, and growth) of the scleractinian coral Acropora millepora (Ehrenberg, 1834) from the Great Barrier Reef over a 16 day interval. High DIC availability did not affect photosynthesis, respiration and light calcification, but significantly reduced dark calcification and growth by 50 and 23%, respectively. High DOC availability reduced net and gross photosynthesis by 51% and 39%, respectively, but did not affect respiration. DOC addition did not influence calcification, but significantly increased growth by 42%. Combination of high DIC and high DOC availability did not affect photosynthesis, light calcification, respiration or growth, but significantly decreased dark calcification when compared to both controls and DIC treatments. On the ecosystem level, high DIC concentrations may lead to reduced accretion and growth of reefs dominated by Acropora that under elevated DOC concentrations will likely exhibit reduced primary production rates, ultimately leading to loss of hard substrate and reef erosion. It is therefore important to consider the potential impacts of elevated DOC and DIC simultaneously to assess real world scenarios, as multiple rather than single factors influence key physiological processes in coral reefs.     

Anion-Sensitive, H-Pumping ATPase of Oat Roots : Direct Effects of Cl, NO(3), and a Disulfonic Stilbene

To understand the mechanism and molecular properties of the tonoplast-type H⁺-translocating ATPase, we have studied the effect of Cl⁻, NO₃⁻, and 4,4′-diisothiocyano-2,2′-stilbene disulfonic acid (DIDS) on the activity of the electrogenic H⁺-ATPase associated with low-density microsomal vesicles from oat roots (Avena sativa cv Lang). The H⁺-pumping ATPase generates a membrane potential (Δψ) and a pH gradient (ΔpH) that make up two interconvertible components of the proton electrochemical gradient (μh⁺). A permeant anion (e.g. Cl⁻), unlike an impermeant anion (e.g. iminodiacetate), dissipated the membrane potential ([¹⁴C]thiocyanate distribution) and stimulated formation of a pH gradient ([¹⁴C]methylamine distribution). However, Cl⁻-stimulated ATPase activity was about 75% caused by a direct stimulation of the ATPase by Cl⁻ independent of the proton electrochemical gradient. Unlike the plasma membrane H⁺-ATPase, the Cl⁻-stimulated ATPase was inhibited by NO₃⁻ (a permeant anion) and by DIDS. In the absence of Cl⁻, NO₃⁻ decreased membrane potential formation and did not stimulate pH gradient formation. The inhibition by NO₃⁻ of Cl⁻-stimulated pH gradient formation and Cl⁻-stimulated ATPase activity was noncompetitive. In the absence of Cl⁻, DIDS inhibited the basal Mg,ATPase activity and membrane potential formation. DIDS also inhibited the Cl⁻-stimulated ATPase activity and pH gradient formation. Direct inhibition of the electrogenic H⁺-ATPase by NO₃⁻ or DIDS suggest that the vanadate-insensitive H⁺-pumping ATPase has anion-sensitive site(s) that regulate the catalytic and vectorial activity. Whether the anion-sensitive H⁺-ATPase has channels that conduct anions is yet to be established.     

Characterization of the na-requirement in cyanobacterial photosynthesis

The Na⁺ requirement for photosynthesis and its relationship to dissolved inorganic carbon (DIC) concentration and Li⁺ concentration was examined in air-grown cells of the cyanobacterium Synechococcus leopoliensis UTEX 625 at pH 8. Analysis of the rate of photosynthesis (O₂ evolution) as a function of Na⁺ concentration, at fixed DIC concentration, revealed two distinct regions to the response curve, for which half-saturation values for Na⁺ (K_½[Na⁺]) were calculated. The value of both the low and the high K_½(Na⁺) was dependent upon extracellular DIC concentration. The low K_½(Na⁺) decreased from 1000 micromolar at 5 micromolar DIC to 200 micromolar at 140 micromolar DIC whereas over the same DIC concentration range the high K_½(Na⁺) decreased from 10 millimolar to 1 millimolar. The most significant increases in photosynthesis occurred in the 1 to 20 millimolar range. A fraction of total photosynthesis, however, was independent of added Na⁺ and this fraction increased with increased DIC concentration. A number of factors were identified as contributing to the complexity of interaction between Na⁺ and DIC concentration in the photosynthesis of Synechococcus. First, as revealed by transport studies and mass spectrometry, both CO₂ and HCO₃⁻ transport contributed to the intracellular supply of DIC and hence to photosynthesis. Second, both the CO₂ and HCO₃⁻ transport systems required Na⁺, directly or indirectly, for full activity. However, micromolar levels of Na⁺ were required for CO₂ transport while millimolar levels were required for HCO₃⁻ transport. These levels corresponded to those found for the low and high K_½(Na⁺) for photosynthesis. Third, the contribution of each transport system to intracellular DIC was dependent on extracellular DIC concentration, where the contribution from CO₂ transport increased with increased DIC concentration relative to HCO₃⁻ transport. This change was reflected in a decrease in the Na⁺ concentration required for maximum photosynthesis, in accord with the lower Na⁺-requirement for CO₂ transport. Lithium competitively inhibited Na⁺-stimulated photosynthesis by blocking the cells' ability to form an intracellular DIC pool through Na⁺-dependent HCO₃⁻ transport. Lithium had little effect on CO₂ transport and only a small effect on the size of the pool it generated. Thus, CO₂ transport did not require a functional HCO₃⁻ transport system for full activity. Based on these observations and the differential requirement for Na⁺ in the CO₂ and HCO₃⁻ transport system, it was proposed that CO₂ and HCO₃⁻ were transported across the membrane by different transport systems.     

Intracellular Cl? Dependence of Na-H Exchange in Barnacle Muscle Fibers under Normotonic and Hypertonic Conditions

We previously showed that shrinking a barnacle muscle fiber (BMF) in a hypertonic solution (1,600 mosM/kg) stimulates an amiloride-sensitive Na-H exchanger. This activation is mediated by a G protein and requires intracellular Cl⁻. The purpose of the present study was to determine (a) whether Cl⁻ plays a role in the activation of Na-H exchange under normotonic conditions (975 mosM/kg), (b) the dose dependence of [Cl⁻]_i for activation of the exchanger under both normo- and hypertonic conditions, and (c) the relative order of the Cl⁻- and G-protein-dependent steps. We acid loaded BMFs by internally dialyzing them with a pH-6.5 dialysis fluid containing no Na⁺ and 0–194 mM Cl⁻. The artificial seawater bathing the BMF initially contained no Na⁺. After dialysis was halted, adding 50 mM Na⁺ to the artificial seawater caused an amiloride-sensitive pH_i increase under both normo- and hypertonic conditions. The computed Na-H exchange flux (J _Na-H) increased with increasing [Cl⁻]_i under both normo- and hypertonic conditions, with similar apparent K _m values (∼120 mM). However, the maximal J _Na-H increased by nearly 90% under hypertonic conditions. Thus, activation of Na-H exchange at low pH_i requires Cl⁻ under both normo- and hypertonic conditions, but at any given [Cl⁻]_i, J _Na-H is greater under hyper- than normotonic conditions. We conclude that an increase in [Cl⁻]_i is not the primary shrinkage signal, but may act as an auxiliary shrinkage signal. To determine whether the Cl⁻-dependent step is after the G-protein-dependent step, we predialyzed BMFs to a Cl⁻-free state, and then attempted to stimulate Na-H exchange by activating a G protein. We found that, even in the absence of Cl⁻, dialyzing with GTPγS or AlF₃, or injecting cholera toxin, stimulates Na-H exchange. Because Na-H exchange activity was absent in control Cl⁻-depleted fibers, the Cl⁻-dependent step is at or before the G protein in the shrinkage signal-transduction pathway. The stimulation by AlF₃ indicates that the G protein is a heterotrimeric G protein.     

H-ATPase Activity from Storage Tissue of Beta vulgaris: II. H/ATP Stoichiometry of an Anion-Sensitive H-ATPase

The H⁺/ATP stoichiometry was determined for an anion-sensitive H⁺-ATPase in membrane vesicles believed to be derived from tonoplast. Initial rates of proton influx were measured by monitoring the alkalinization of a weakly buffered medium (pH 6.13) following the addition of ATP to a suspension of membrane vesicles of Beta vulgaris L. Initial rates of ATP hydrolysis were measured in an assay where ATP hydrolysis is coupled to NADH oxidation and monitored spectrophotometrically (A₃₄₀) or by monitoring the release of ³²P from [γ-³²P]ATP. Inasmuch as this anion-sensitive H⁺-ATPase is strongly inhibited by NO₃⁻, initial rates of H⁺ influx and ATP hydrolysis were measured in the absence and presence of NO₃⁻ to account for ATPase activity not involved in H⁺ transport. The NO₃⁻-sensitive activities were calculated and used to estimate the ratio of H⁺ transported to ATP hydrolyzed. These measurements resulted in an estimate of the H⁺/ATP stoichiometry of 1.96 ± 0.14 suggesting that the actual stoichiometry is 2 H⁺ transported per ATP hydrolyzed. When compared with the reported values of the electrochemical potential gradient for H⁺ across the tonoplast measured in vivo, our result suggests that the H⁺-ATPase does not operate near equilibrium but is regulated by cellular factors other than energy supply.     

The impact of seawater saturation state and bicarbonate ion concentration on calcification by new recruits of two Atlantic corals

Rising concentrations of atmospheric CO₂ are changing the carbonate chemistry of the oceans, a process known as ocean acidification (OA). Absorption of this CO₂ by the surface oceans is increasing the amount of total dissolved inorganic carbon (DIC) and bicarbonate ion (HCO₃ ⁻) available for marine calcification yet is simultaneously lowering the seawater pH and carbonate ion concentration ([CO₃ ²⁻]), and thus the saturation state of seawater with respect to aragonite (Ω_ar). We investigated the relative importance of [HCO₃ ⁻] versus [CO₃ ²⁻] for early calcification by new recruits (primary polyps settled from zooxanthellate larvae) of two tropical coral species, Favia fragum and Porites astreoides. The polyps were reared over a range of Ω_ar values, which were manipulated by both acid-addition at constant pCO₂ (decreased total [HCO₃ ⁻] and [CO₃ ²⁻]) and by pCO₂ elevation at constant alkalinity (increased [HCO₃ ⁻], decreased [CO₃ ²⁻]). Calcification after 2 weeks was quantified by weighing the complete skeleton (corallite) accreted by each polyp over the course of the experiment. Both species exhibited the same negative response to decreasing [CO₃ ²⁻] whether Ω_ar was lowered by acid-addition or by pCO₂ elevation—calcification did not follow total DIC or [HCO₃ ⁻]. Nevertheless, the calcification response to decreasing [CO₃ ²⁻] was nonlinear. A statistically significant decrease in calcification was only detected between Ω_ar = <2.5 and Ω_ar = 1.1–1.5, where calcification of new recruits was reduced by 22–37% per 1.0 decrease in Ω_ar. Our results differ from many previous studies that report a linear coral calcification response to OA, and from those showing that calcification increases with increasing [HCO₃ ⁻]. Clearly, the coral calcification response to OA is variable and complex. A deeper understanding of the biomineralization mechanisms and environmental conditions underlying these variable responses is needed to support informed predictions about future OA impacts on corals and coral reefs.     

Human SLC4A11 Is a Novel NH3/H+ Co-transporter

SLC4A11 has been proposed to be an electrogenic membrane transporter, permeable to Na⁺, H⁺ (OH⁻), bicarbonate, borate, and NH₄⁺. Recent studies indicate, however, that neither bicarbonate or borate is a substrate. Here, we examined potential NH₄⁺, Na⁺, and H⁺ contributions to electrogenic ion transport through SLC4A11 stably expressed in Na⁺/H⁺ exchanger-deficient PS120 fibroblasts. Inward currents observed during exposure to NH₄Cl were determined by the [NH₃]_o, not [NH₄⁺]_o, and current amplitudes varied with the [H⁺] gradient. These currents were relatively unaffected by removal of Na⁺, K⁺, or Cl⁻ from the bath but could be reduced by inclusion of NH₄Cl in the pipette solution. Bath pH changes alone did not generate significant currents through SLC4A11, except immediately following exposure to NH₄Cl. Reversal potential shifts in response to changing [NH₃]_o and pH_o suggested an NH₃/H⁺-coupled transport mode for SLC4A11. Proton flux through SLC4A11 in the absence of ammonia was relatively small, suggesting that ammonia transport is of more physiological relevance. Methylammonia produced currents similar to NH₃ but with reduced amplitude. Estimated stoichiometry of SLC4A11 transport was 1:2 (NH₃/H⁺). NH₃-dependent currents were insensitive to 10 μm ethyl-isopropyl amiloride or 100 μm 4,4′- diisothiocyanatostilbene-2,2′-disulfonic acid. We propose that SLC4A11 is an NH₃/2H⁺ co-transporter exhibiting unique characteristics.     

The Physiological Response of Two Green Calcifying Algae from the Great Barrier Reef towards High Dissolved Inorganic and Organic Carbon (DIC and DOC) Availability

Increasing dissolved inorganic carbon (DIC) concentrations associated with ocean acidification can affect marine calcifiers, but local factors, such as high dissolved organic carbon (DOC) concentrations through sewage and algal blooms, may interact with this global factor. For calcifying green algae of the genus Halimeda, a key tropical carbonate producer that often occurs in coral reefs, no studies on these interactions have been reported. These data are however urgently needed to understand future carbonate production. Thus, we investigated the independent and combined effects of DIC (pCO₂ 402 μatm/ pH_tot 8.0 and 996 μatm/ pH_tot 7.7) and DOC (added as glucose in 0 and 294 μmol L^-1) on growth, calcification and photosynthesis of H. macroloba and H. opuntia from the Great Barrier Reef in an incubation experiment over 16 days. High DIC concentrations significantly reduced dark calcification of H. opuntia by 130 % and led to net dissolution, but did not affect H. macroloba. High DOC concentrations significantly reduced daily oxygen production of H. opuntia and H. macroloba by 78 % and 43 %, respectively, and significantly reduced dark calcification of H. opuntia by 70%. Combined high DIC and DOC did not show any interactive effects for both algae, but revealed additive effects for H. opuntia where the combination of both factors reduced dark calcification by 162 % compared to controls. Such species-specific differences in treatment responses indicate H. opuntia is more susceptible to a combination of high DIC and DOC than H. macroloba. From an ecological perspective, results further suggest a reduction of primary production for Halimeda-dominated benthic reef communities under high DOC concentrations and additional decreases of carbonate accretion under elevated DIC concentrations, where H. opuntia dominates the benthic community. This may reduce biogenic carbonate sedimentation rates and hence the buffering capacity against further ocean acidification.     

Electrodiffusion,Barrier, and Gating Analysis of DIDS-insensitive Chloride Conductance in Human Red Blood Cells Treated with Valinomycin or Gramicidin

Current-voltage curves for DIDS-insensitive Cl⁻ conductance have been determined in human red blood cells from five donors. Currents were estimated from the rate of cell shrinkage using flow cytometry and differential laser light scattering. Membrane potentials were estimated from the extracellular pH of unbuffered suspensions using the proton ionophore FCCP. The width of the Gaussian distribution of cell volumes remained invariant during cell shrinkage, indicating a homogeneous Cl⁻ conductance among the cells. After pretreatment for 30 min with DIDS, net effluxes of K⁺ and Cl⁻ were induced by valinomycin and were measured in the continued presence of DIDS; inhibition was maximal at ∼65% above 1 μM DIDS at both 25°C and 37°C. The nonlinear current-voltage curves for DIDS-insensitive net Cl⁻ effluxes, induced by valinomycin or gramicidin at varied [K⁺]_o, were compared with predictions based on (1) the theory of electrodiffusion, (2) a single barrier model, (3) single occupancy, multiple barrier models, and (4) a voltage-gated mechanism. Electrodiffusion precisely describes the relationship between the measured transmembrane voltage and [K⁺]_o. Under our experimental conditions (pH 7.5, 23°C, 1–3 μM valinomycin or 60 ng/ml gramicidin, 1.2% hematocrit), the constant field permeability ratio P_K/P_Cl is 74 ± 9 with 10 μM DIDS, corresponding to 73% inhibition of P_Cl. Fitting the constant field current-voltage equation to the measured Cl⁻ currents yields P _Cl = 0.13 h⁻¹ with DIDS, compared to 0.49 h⁻¹ without DIDS, in good agreement with most previous studies. The inward rectifying DIDS-insensitive Cl⁻ current, however, is inconsistent with electrodiffusion and with certain single-occupancy multiple barrier models. The data are well described either by a single barrier located near the center of the transmembrane electric field, or, alternatively, by a voltage-gated channel mechanism according to which the maximal conductance is 0.055 ± 0.005 S/g Hb, half the channels are open at −27 ± 2 mV, and the equivalent gating charge is −1.2 ± 0.3.     

Evidence for Na-Independent HCO(3) Uptake by the Cyanobacterium Synechococcus leopoliensis

At low levels of dissolved inorganic carbon (DIC) and alkaline pH the rate of photosynthesis by air-grown cells of Synechococcus leopoliensis (UTEX 625) was enhanced 7- to 10-fold by 20 millimolar Na⁺. The rate of photosynthesis greatly exceeded the CO₂ supply rate and indicated that HCO₃⁻ was taken up by a Na⁺-dependent mechanism. In contrast, photosynthesis by Synechococcus grown in standing culture proceeded rapidly in the absence of Na⁺ and exceeded the CO₂ supply rate by 8 to 45 times. The apparent photosynthetic affinity (K_½) for DIC was high (6-40 micromolar) and was not markedly affected by Na⁺ concentration, whereas with air-grown cells K_½ (DIC) decreased by more than an order of magnitude in the presence of Na⁺. Lithium, which inhibited Na⁺-dependent HCO₃⁻ uptake in air-grown cells, had little effect on Na⁺-independent HCO₃⁻ uptake by standing culture cells. A component of total HCO₃⁻ uptake in standing culture cells was also Na⁺-dependent with a K_½ (Na⁺) of 4.8 millimolar and was inhibited by lithium. Analysis of ¹⁴C-fixation during isotopic disequilibrium indicated that standing culture cells also possessed a Na⁺-independent CO₂ transport system. The conversion from Na⁺-independent to Na⁺-dependent HCO₃⁻ uptake was readily accomplished by transferring cells grown in standing to growth in cultures bubbled with air. These results demonstrated that the conditions experienced during growth influenced the mode by which Ssynechococcus acquired HCO₃⁻ for subsequent photosynthetic fixation.     

Stoichiometry of proton translocation coupled to substrate oxidation in plant mitochondria

The proton translocation coupled to the electron flux from succinate, exogenous NADH, and NAD⁺-linked substrates (malate and isocitrate) to cytochrome c and to oxygen was studied in purified potato (Solanum tuberosum) mitochondria using oxygen and ferricyanide pulse techniques. In the presence of valinomycin plus K⁺ (used as a charge compensating cation), optimum values of H⁺/2 e⁻ were obtained when low amounts of electron acceptors (oxygen or ferricyanide) were added to the mitochondria (1-2 nanogram [2 e⁻] equivalents per milligram protein). The stoichiometry of proton translocation to electron flux was unaffected in the presence of N-ethylmaleimide, an inhibitor of the Pi/H⁺ symport. With succinate as substrate, H⁺/2 e⁻ ratios were 4.0 ± 0.2 and 3.7 ± 0.3 with oxygen and ferricyanide as electron acceptors, respectively. With exogenous NADH, H⁺/2e⁻ ratios were 4.1 ± 0.9 and 3.4 ± 0.2, respectively. The proton translocation coupled to the oxidation of NAD⁺-linked substrates (malate, isocitrate) was dependent upon the presence of adenylates (ADP, AMP, or ATP). For malate (+ glutamate) oxidation the observed H⁺/2 e⁻ ratios were increased from 3.6 ± 2.2 to 6.5 ± 0.5 in the presence of 20 micromolar ADP.     

The Membrane Subunit NuoL(ND5) Is Involved in the Indirect Proton Pumping Mechanism of Escherichia coli Complex I

Complex I pumps protons across the membrane by using downhill redox energy. Here, to investigate the proton pumping mechanism by complex I, we focused on the largest transmembrane subunit NuoL (Escherichia coli ND5 homolog). NuoL/ND5 is believed to have H⁺ translocation site(s), because of a high sequence similarity to multi-subunit Na⁺/H⁺ antiporters. We mutated thirteen highly conserved residues between NuoL/ND5 and MrpA of Na⁺/H⁺ antiporters in the chromosomal nuoL gene. The dNADH oxidase activities in mutant membranes were mostly at the control level or modestly reduced, except mutants of Glu-144, Lys-229, and Lys-399. In contrast, the peripheral dNADH-K₃Fe(CN)₆ reductase activities basically remained unchanged in all the NuoL mutants, suggesting that the peripheral arm of complex I was not affected by point mutations in NuoL. The proton pumping efficiency (the ratio of H⁺/e⁻), however, was decreased in most NuoL mutants by 30–50%, while the IC₅₀ values for asimicin (a potent complex I inhibitor) remained unchanged. This suggests that the H⁺/e⁻ stoichiometry has changed from 4H⁺/2e⁻ to 3H⁺ or 2H⁺/2e⁻ without affecting the direct coupling site. Furthermore, 50 μm of 5-(N-ethyl-N-isopropyl)-amiloride (EIPA), a specific inhibitor for Na⁺/H⁺ antiporters, caused a 38 ± 5% decrease in the initial H⁺ pump activity in the wild type, while no change was observed in D178N, D303A, and D400A mutants where the H⁺ pumping efficiency had already been significantly decreased. The electron transfer activities were basically unaffected by EIPA in both control and mutants. Taken together, our data strongly indicate that the NuoL subunit is involved in the indirect coupling mechanism.     

Evidence for Cotransport of Nitrate and Protons in Maize Roots : II. Measurement of NO(3) and H Fluxes with Ion-Selective Microelectrodes

We report here on an investigation of net nitrate and proton fluxes in root cells of maize (Zea mays L.) seedlings grown without (noninduced) and with (induced) 0.1 millimolar nitrate. A microelectrode system described previously (IA Newman, LV Kochian, MA Grusak, WJ Lucas [1987] Plant Physiol 84: 1177-1184) was utilized to quantify net ionic fluxes from the measurement of electrochemical potential gradients for NO₃⁻ and H⁺ within the unstirred layer at the root surface. The nitrate-inducibility, pH dependence, and concentration dependence of net NO₃⁻ uptake correlated quite closely with the electrical response of maize roots to nitrate under the same experimental conditions (as described in PR McClure, LV Kochian, RM Spanswick, JE Shaff [1990] Plant Physiol 93: 281-289). Additionally, it was found that potential inhibitors of the plasmalemma H⁺-ATPase (vandate, diethylstilbestrol), which were shown to abolish the electrical response to NO₃⁻ (in PR McClure, LV Kochian, RM Spanswick, JE Shaff [1990] Plant Physiol 93: 281-289), dramatically inhibited NO₃⁻ absorption. These results strongly indicate that the NO₃⁻ electrical response is due to the operation of a NO₃⁻ transport system in the plasmalemma of maize root cells. Furthermore, the results from the H⁺-ATPase inhibitor studies indicate that the NO₃⁻ transport system is linked to the H⁺-ATPase, presumably as a NO₃⁻/H⁺ symport. This is further supported by the pH response of the NO₃⁻ transport system (inhibition at alkaline pH values) and the change in net H⁺ flux from a moderate efflux in the absence of NO₃⁻, to zero net H⁺ flux after exposing the maize root to exogenous nitrate. Although these results can be explained by other interpretations, the simplest model that fits both the electrical responses and the NO₃⁻/H⁺ flux data is a NO₃⁻/H⁺ symport with a NO₃⁻:H⁺ flux stoichiometry >1, whose operation results in the stimulation of the H⁺-ATPase due to the influx of protons through the cotransport system.     

Climate change and ocean acidification effects on seagrasses and marine macroalgae

Although seagrasses and marine macroalgae (macro‐autotrophs) play critical ecological roles in reef, lagoon, coastal and open‐water ecosystems, their response to ocean acidification (OA) and climate change is not well understood. In this review, we examine marine macro‐autotroph biochemistry and physiology relevant to their response to elevated dissolved inorganic carbon [DIC], carbon dioxide [CO₂], and lower carbonate [CO₃^2?] and pH. We also explore the effects of increasing temperature under climate change and the interactions of elevated temperature and [CO₂]. Finally, recommendations are made for future research based on this synthesis. A literature review of >100 species revealed that marine macro‐autotroph photosynthesis is overwhelmingly C₃ (≥ 85%) with most species capable of utilizing HCO₃^?; however, most are not saturated at current ocean [DIC]. These results, and the presence of CO₂‐only users, lead us to conclude that photosynthetic and growth rates of marine macro‐autotrophs are likely to increase under elevated [CO₂] similar to terrestrial C₃ species. In the tropics, many species live close to their thermal limits and will have to up‐regulate stress‐response systems to tolerate sublethal temperature exposures with climate change, whereas elevated [CO₂] effects on thermal acclimation are unknown. Fundamental linkages between elevated [CO₂] and temperature on photorespiration, enzyme systems, carbohydrate production, and calcification dictate the need to consider these two parameters simultaneously. Relevant to calcifiers, elevated [CO₂] lowers net calcification and this effect is amplified by high temperature. Although the mechanisms are not clear, OA likely disrupts diffusion and transport systems of H⁺ and DIC. These fluxes control micro‐environments that promote calcification over dissolution and may be more important than CaCO₃ mineralogy in predicting macroalgal responses to OA. Calcareous macroalgae are highly vulnerable to OA, and it is likely that fleshy macroalgae will dominate in a higher CO₂ ocean; therefore, it is critical to elucidate the research gaps identified in this review.