Bicarbonate uptake via an anion exchange protein is the main mechanism of inorganic carbon acquisition by the giant kelp Macrocystis pyrifera (Laminariales,Phaeophyceae) under variable pH

Macrocystis pyrifera is a widely distributed, highly productive, seaweed. It is known to use bicarbonate (HCO₃^?) from seawater in photosynthesis and the main mechanism of utilization is attributed to the external catalyzed dehydration of HCO₃^? by the surface‐bound enzyme carbonic anhydrase (CA_ext). Here, we examined other putative HCO₃^? uptake mechanisms in M. pyrifera under pH_T 9.00 (HCO₃^?: CO₂ = 940:1) and pH_T 7.65 (HCO₃^?: CO₂ = 51:1). Rates of photosynthesis, and internal CA (CA_int) and CA_ext activity were measured following the application of AZ which inhibits CA_ext, and DIDS which inhibits a different HCO₃^? uptake system, via an anion exchange (AE) protein. We found that the main mechanism of HCO₃^? uptake by M. pyrifera is via an AE protein, regardless of the HCO₃^?: CO₂ ratio, with CA_ext making little contribution. Inhibiting the AE protein led to a 55%–65% decrease in photosynthetic rates. Inhibiting both the AE protein and CA_ext at pH_T 9.00 led to 80%–100% inhibition of photosynthesis, whereas at pH_T 7.65, passive CO₂ diffusion supported 33% of photosynthesis. CA_int was active at pH_T 7.65 and 9.00, and activity was always higher than CA_ext, because of its role in dehydrating HCO₃^? to supply CO₂ to RuBisCO. Interestingly, the main mechanism of HCO₃^? uptake in M. pyrifera was different than that in other Laminariales studied (CA_ext‐catalyzed reaction) and we suggest that species‐specific knowledge of carbon uptake mechanisms is required in order to elucidate how seaweeds might respond to future changes in HCO₃^?:CO₂ due to ocean acidification.     

The role of extracellular carbonic anhydrase for accumulation of inorganic carbon in the green alga Chlamydomonas reinhardtii. A comparison between wild-type and cell-wall-less mutant cells

The role of extracellular carbonic anhydrase (CA_ex) for dissolved inorganic carbon (DIC) accumulation in the green alga Chlamydomonas reinhardtii was investigated. It was found that when algal cells were bubbled with ambient air, cell-wall-less mutant cells exhibited the same high photosynthetic affinity for CO₂ as wild-type cells despite a 10 times lower activity of CA^ex. It was also found that the affinity for CO₂ was further increased when the total DIC concentration of the algal medium was reduced from that in equilibrium with ambient air to even lower levels. This increased affinity was not correlated with any further increase in the CA_ex activity. Dextran-bound sulfonamide (DBS. 100 μM bound ligand) completely inhibited the activity of CA_ex in intact, low-DIC grown, wild-type cells, while photosynthesis at <2 μM CO₂(aq) proceeded at a far greater rate than could be maintained by CO₂ supplied from the spontaneous dehydration of HCO^?₃. DBS-inhibition of CA_ex, during the induction of the DIC-accumulating mechanism in previously high-DIC grown cells, only caused a 50% inhibition of photosynthesis at 10 μM CO₂(aq) after 1 h of low-DIC acclimation. It was also shown that 50 μM acetazolamide (AZ) inhibited photosynthesis at low DIC concentrations to a relatively higher degree than DBS, suggesting that AZ inhibited intracellular CA as well. Taken together, these results suggest that low-DIC grown cells of C. reinhardtii have the ability to transport HCO^?₃ across the plasma membrane in addition to the CA_ex-mediated, facilitated diffusion and/or transport of CO₂. It is also suggested that the relative importance of these two fluxes (CO₂ or HCO^?₃) is dependent on the growth and experimental conditions. Facilitated CO₂ uptake seems to be most prevalent, supported by HCO^?₃-transport under more or less extreme situations, such as a reduction of CO₂ to extremely low concentrations, leakage of CA_ex to the medium as in cultures of cell-wall-less mutant cells or when the activity of CA_ex has been artificially inhibited.     

CO2 uptake and transport in leaf mesophyll cells

Abstract The acquisition of inorganic carbon for photosynthetic assimilation by leaf mesophyll cells and chloroplasts is discussed with particular reference to membrane permeation of CO₂ and HCO^?₃. Experimental evidence indicates that at the apoplast pH normally experienced by leaf mesophyll cells (pH 6–7) CO₂ is the principal species of inorganic carbon taken up. Uptake of HCO^?₃ may also occur under certain circumstances (i.e. pH 8.5), but its contribution to the net flux of inorganic carbon is small and HCO^?₃ uptake does not function as a CO₂-concentrating mechanism. Similarly, CO₂ rather than HCO^?₃ appears to be the species of inorganic carbon which permeates the chloroplast envelope. In contrast to many C₃ aquatic plants and C₄ plants, C₃ terrestrial plants lack specialized mechanisms for the acquisition and transport of inorganic carbon from the intercellular environment to the site of photosynthetic carboxylation, but rely upon the diffusive uptake of CO₂.     

HCO-3对植物生长发育及代谢的促进作用

重碳酸盐(bicarbonate, HCO^-₃)是碳酸盐岩经岩溶作用风化的产物,它深刻地影响着植物的生长发育和岩溶地区的生态环境。以往研究大都关注HCO^-₃对植物生长代谢的负面影响,如抑制植物的光合作用、降低碳氮代谢关键酶活性、破坏离子平衡等,少有人关注其对植物生长代谢的积极作用。该文依据前人的研究结果,综述了HCO^-₃对植物生长代谢的促进作用。已有的研究工作显示,HCO^-₃不仅在干旱等逆境胁迫下为植物提供短期的碳源和水源,促进气孔打开,恢复光合作用,而且通过调节碳氮代谢关键酶活性促进植物的碳氮代谢,参与调控植物的碳同化和氮还原等复杂的生理过程; 此外,HCO^-₃还通过影响葡萄糖代谢歧化,改变植物糖酵解途径和磷酸戊糖途径的分配,以增强植物的抗逆能力,从而获取生存机会。HCO^-₃的这些积极作用不仅使之成为促进植物生理代谢的关键因子,而且成为连接光合作用和岩溶作用的纽带。阐明HCO^-₃对植物生长发育的积极作用,可为维护喀斯特生态系统的生物多样性和稳定性、优化喀斯特生态系统功能提供理论依据。     

Bicarbonate-stimulated ATPase in the renal proximal tubule luminal (brush border) memebrane.

Brush border membranes of the rabbit renal tubule have an ATPase which was stimulated 60% by 50 mm HCO₃^?. The K_a for HCO₃^? was 36 mm. Kinetic studies of the “HCO₃^?-ATPase” indicate that HCO₃^? had no effect on the K_m for ATP and ATP did not alter the K_a for HCO₃^?. Several anions, notably SO₃^2?, also accelerated the rate of dephosphorylation of ATP. The V for “SO₃^2?-ATPase” was fivefold greater than that for “HCO₃^?-ATPase.” The K_a for SO₃^2? was 0.78 mm. Other anions including Cl^? and phosphates, did not enhance ATPase activity. Thus, of the anions present in the glomerular filtrate in appreciable concentrations only HCO₃^? stimulated the luminal membrane enzyme. The anion-stimulated ATPase activity increased sharply from pH 6.1 to 7.1 and moderately with higher pH. The renal ATPase was not inhibited by SCN^? nor methyl sulfonyl chloride and was relatively insensitive to oligomycin and quercetin. Carbonyl cyanide p-trifluoromethoxy phenylhydrazone increased the basal rate of the membranal ATPase, suggesting that the ATPase activity is limited by transmembrane H⁺ flux. Carbonic anhydrase significantly increased the HCO₃^?-stimulated ATPase activity. This increment was blocked by Diamox. These findings provide evidence consistent with the hypothesis that the brush border membrane ATPase is involved in the extrusion of H⁺ from tubular cell to lumen and support suggested interrelationships between HCO₃^?-stimulated ATPase, H⁺ secretion, and bicarbonate transport in the kidney.     

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

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

Seasonal variations of pH, pCO2, pO2, HCO3- and Ca2+ in the haemolymph: implications on the calcification physiology in Anodonta cygnea

A study about the relationship between the physical–chemical parameters and the calcium carbonate balance between the haemolymph fluid and mantle calcareous structures was carried out in Anodonta cygnea. An intense peak of HCO₃ ⁻ and a highest pH in December–January months may be understood as a preparation period for creating alkaline conditions. An intense pH decrease from January to February in parallel with the HCO₃ ⁻ reduction seems to indicate the beginning process of carbonate precipitation. On the other hand, the following calcium and HCO₃ ⁻ increases in February–May associated with a continuous and gradual pH fall profile may infer two combined aspects: calcium and HCO₃ ⁻ absorption from external environment and a simultaneous intense calcium carbonate deposition in the haemolymph. So, the pCO₂ peak in this period reflects a subsequent result on equilibrium balance between HCO₃ ⁻ absorption and deposition. The only significant pO₂ increase in the next period, from February to June, is related with an energetic increase to support the metabolic activity favouring the posterior intense pCO₂ peaks. The extended time of CO₂ production in the haemolymph from May to November should induce an increased metabolic acidosis with subsequent intense formation of both HCO₃ ⁻ and Ca²⁺ ions in the same period. This seems to result from CaCO₃ deposits dissolution in the haemolymph, the most direct calcareous source. Additionally, the later increase of metabolic succinic acid during autumn may greatly potentiate this acidosis increasing the dissolution process. Consequently, the pH profile present two simultaneous alkaline peaks in July and October, probably due to a strong HCO₃ ⁻ release from the CaCO₃ dissolution. So, the present seasonal results indicate that in the freshwater bivalve A. cygnea, the low metabolism with higher pH from the early winter is the main cause which may favour a calcareous precipitation, while the high metabolism with lower pH from the early summer may function as an inductor of calcareous dissolution in the haemolymph.     

Intracellular Carbonic Anhydrase Activity Sensitizes Cancer Cell pH Signaling to Dynamic Changes in CO2 Partial Pressure

Carbonic anhydrase (CA) enzymes catalyze the chemical equilibration among CO₂, HCO₃⁻ and H⁺. Intracellular CA (CA_i) isoforms are present in certain types of cancer, and growing evidence suggests that low levels correlate with disease severity. However, their physiological role remains unclear. Cancer cell CA_i activity, measured as cytoplasmic CO₂ hydration rate (k_f), ranged from high in colorectal HCT116 (∼2 s⁻¹), bladder RT112 and colorectal HT29, moderate in fibrosarcoma HT1080 to negligible (i.e. spontaneous k_f = 0.18 s⁻¹) in cervical HeLa and breast MDA-MB-468 cells. CA_i activity in cells correlated with CAII immunoreactivity and enzymatic activity in membrane-free lysates, suggesting that soluble CAII is an important intracellular isoform. CA_i catalysis was not obligatory for supporting acid extrusion by H⁺ efflux or HCO₃⁻ influx, nor for maintaining intracellular pH (pH_i) uniformity. However, in the absence of CA_i activity, acid loading from a highly alkaline pH_i was rate-limited by HCO₃⁻ supply from spontaneous CO₂ hydration. In solid tumors, time-dependence of blood flow can result in fluctuations of CO₂ partial pressure (pCO₂) that disturb cytoplasmic CO₂-HCO₃⁻-H⁺ equilibrium. In cancer cells with high CA_i activity, extracellular pCO₂ fluctuations evoked faster and larger pH_i oscillations. Functionally, these resulted in larger pH-dependent intracellular [Ca²⁺] oscillations and stronger inhibition of the mTORC1 pathway reported by S6 kinase phosphorylation. In contrast, the pH_i of cells with low CA_i activity was less responsive to pCO₂ fluctuations. Such low pass filtering would “buffer” cancer cell pH_i from non-steady-state extracellular pCO₂. Thus, CA_i activity determines the coupling between pCO₂ (a function of tumor perfusion) and pH_i (a potent modulator of cancer cell physiology).     

The induction of inorganic carbon transport and external carbonic anhydrase in Chlamydomonas reinhardtii is regulated by external CO2 concentration

Induction of the carbon concentrating mechanism (CCM) has been investigated during the acclimation of 5% CO₂‐grown Chlamydomonas reinhardtii 2137 mt + cells to well‐defined dissolved inorganic carbon (C_i) limited conditions. The CCM components investigated were active HCO₃^? transport, active CO₂ transport and extracellular carbonic anhydrase (CA_ext) activity. The CA_ext activity increased 10‐fold within 6 h of acclimation to 0·035% CO₂ and there was a further slight increase over the next 18 h. The CA_ext activity also increased substantially after an 8 h lag period during acclimation to air in darkness. Active CO₂ and HCO₃^? uptake by C. reinhardtii cells were induced within 2 h of acclimation to air, but active CO₂ transport was induced prior to active HCO₃^? transport. Similar results were obtained during acclimation to air in darkness. The critical C_i concentrations effecting the induction of active C_i transport and CA_ext activity were determined by allowing cells to acclimate to various inflow CO₂ concentrations in the range 0·035–0·84% at constant pH. The total C_i concentration eliciting the induction and repression of active C_i transport was higher during acclimation at pH 7·5 than at pH 5·5, but the external CO₂ concentration was the same at both pHs of acclimation. The concentration of external CO₂ required for the full induction and repression of C_i transport and CA_ext activity were 10 and 100 μM , respectively. The induction of CA_ext and active C_i transport are not correlated temporally, but are regulated by the same critical CO₂ concentration in the medium.     

The effect of pH on the inorganic carbon source for photosynthesis in the seagrass Zostera muelleri irmisch ex aschers

The ability of the seagrass Zostera muelleri Irmisch ex Aschers. to use HCO₃⁻ as well as CO₂ for photosynthesis was investigated by measuring photosynthetic O₂ evolution over a range of pH values. It was found that the apparent K_m CO₂ fell from 0.128 mM at pH 7.9 to 0.016 mM at pH 9.1 indicating that HCO₃⁻ as well as CO₂ may act as a substrate for photosynthesis.The true K_m CO₂ could not be determined due to inhibition of photosynthesis at pHs less than 7.8 K_m CO₂ must be at least 0.128 mM, the apparent K_m at pH 7.9, and is probably of the order of 0.200 mM CO₂, the same as that reported for other marine plants. K_m HCO₃⁻¹ is about 20 mM when CO₂-dependent photosynthesis is minimal. Such a high K_m HCO₃⁻ resembles values reported for freshwater, rather than marine plants.Photosynthetic O₂ evolution is not saturated with respect to total inorganic carbon in natural seawater (pH 8.2). It is suggested that the distinctive shoulder from pH 8.1 to 8.5 in the pH profile of photosynthetic O₂ evolution at a constant concentration of inorganic carbon is caused by an effect of pH on HCO₃⁻ uptake. The effect of pH on HCO₃⁻ uptake was determined by constructing a pH profile of photosynthesis at constant HCO₃⁻ concentration, and subtracting the estimated contribution of CO₂ to photosynthesis from this rate. The resultant curve has a maximum at pH 8.4 and declines sharply at pHs less than 8.     

CARBON‐USE STRATEGIES IN MACROALGAE: DIFFERENTIAL RESPONSES TO LOWERED PH AND IMPLICATIONS FOR OCEAN ACIDIFICATION1

Ocean acidification (OA) is a reduction in oceanic pH due to increased absorption of anthropogenically produced CO₂. This change alters the seawater concentrations of inorganic carbon species that are utilized by macroalgae for photosynthesis and calcification: CO₂ and HCO₃^? increase; CO₃^2? decreases. Two common methods of experimentally reducing seawater pH differentially alter other aspects of carbonate chemistry: the addition of CO₂ gas mimics changes predicted due to OA, while the addition of HCl results in a comparatively lower [HCO₃^?]. We measured the short‐term photosynthetic responses of five macroalgal species with various carbon‐use strategies in one of three seawater pH treatments: pH 7.5 lowered by bubbling CO₂ gas, pH 7.5 lowered by HCl, and ambient pH 7.9. There was no difference in photosynthetic rates between the CO₂, HCl, or pH 7.9 treatments for any of the species examined. However, the ability of macroalgae to raise the pH of the surrounding seawater through carbon uptake was greatest in the pH 7.5 treatments. Modeling of pH change due to carbon assimilation indicated that macroalgal species that could utilize HCO₃^? increased their use of CO₂ in the pH 7.5 treatments compared to pH 7.9 treatments. Species only capable of using CO₂ did so exclusively in all treatments. Although CO₂ is not likely to be limiting for photosynthesis for the macroalgal species examined, the diffusive uptake of CO₂ is less energetically expensive than active HCO₃^? uptake, and so HCO₃^?‐using macroalgae may benefit in future seawater with elevated CO₂.     

Photosynthetic Response to Alkaline pH in Anabaena variabilis

The rate of O₂ evolution and alkalization of the medium in low CO_2⁻ grown Anabaena variabilis was observed as affected by the pH in the medium. Both rates are severely inhibited by pH values higher than 9.5, but the latter is more sensitive to this treatment. This finding, as well as the lag observed in alkalization of the medium, but not in O₂ evolution, following the addition of HCO₃⁻ indicates that the transport of HCO₃ and OH⁻ (or H⁺) are not compulsorily coupled. The inhibition of photosynthesis by strongly alkaline pH is attributed to an alteration of the internal pH and, hence, the rate of carboxylation. This conclusion is supported by data showing that the rate of O₂ evolution is affected by pH more strongly at saturating [HCO₃⁻] than at limiting [HCO₃⁻]. Also, the rate of O₂ evolution at saturating light intensity is affected by pH more strongly than is the initial slope of the curve against light intensity or the rate of dark respiration.     

Bicarbonate effects on chlorophyll a fluorescence transients in the presence and the absence of diuron

We investigated the effect of HCO^?₃ addition to CO₂-depleted thylakoids by means of fluorescence techniques. (1) In the presence of diuron (3-(3,4-dichlorophenyl)-1,1-dimethylurea), the net reduction of the primary quinone-type electron acceptor (Q) of Photosystem (PS) II is about 2-times faster in the absence of HCO^?₃ than in its presence, whether normal, heat-treated or NH₂OH-treated samples are used. This effect of HCO^?₃ is, therefore, not on the O₂-evolving apparatus. It is, however, interpreted to be due to an influence of HCO^?₃ on the kinetics of the reduction of Q, perhaps combined with an effect on the back reaction of Q^? with P-680⁺, the oxidized form of the PS II reaction center chlorophyll a. (2) Fluorescence experiments in the absence of diuron indicate that the absence of HCO^?₃ results in a complete block at the quinone level; the area over the fluorescence induction curve in the absence of HCO^?₃ was found to be 2.2-times higher in the absence than in the presence of diuron, pointing to a complete block of BH₂ oxidation in the absence of HCO^?₃. (3) No change in the midpoint potential of Q is observed when HCO^?₃ is added to CO₂-depleted membranes. HCO^?₃ not only has a large (on/off) effect on the reoxidation of BH₂, but also a smaller effect between P-680 and Q. We propose that HCO^?₃ binding to its specific site in the thylakoid membrane results in a conformational change, allowing normal electron transport between the two photosystems.     

Two modes of bicarbonate utilization in the marine green macroalga Ulva lactuca

The green marine macroalga Ulva lactuca L. was found to be able to utilize HCO₃^? from sea water in two ways. When grown in flowing natural sea water at 16°C under constant dim irradiance, photosynthesis at pH8.4 was suppressed by acetazolamide but unaffected by 4,4′-diisothiocyanostilbene-2,2′-disulphonate. These responses indicate that photosynthetic HCO₃^? utilization was via extracellular carbonic anhydrase (CA) -mediated dehydration followed by CO₂ uptake. The algae were therefore described as being in a ‘CA state’. If treated for more than 10 h in a sea water flow-through system at pH9.8, these thalli became insensitive to acetazolamide but sensitive to 4,4′-diisothiocyanostilbene-2,2′-disulphonate. This suggests the involvement of an anion exchanger (AE) in the direct uptake of HCO₃^?, and these plants were accordingly described as being in an ‘AE state’. Such thalli showed an approximately 10-fold higher apparent affinity for HCO₃^? (at pH9.4) than those in the ‘CA state’, while thalli of both states showed a very high apparent affinity for CO₂. These results suggest that the two modes of HCO₃^? utilization constitute two ways in which inorganic carbon may enter the Ulva lactuca cells, with the direct entry of HCO₃^?, characterizing the ‘AE state’, being inducible and possibly functioning as a complementary uptake system at high external pH values (e.g. under conditions conducive to high photosynthetic rates). Both mechanisms of entry appear to be connected to concentrating CO₂ inside the cell, probably via a separate mechanism operating intracellularly.     

CFTR-mediated anion secretion in parathyroid hormone-treated Caco-2 cells is associated with PKA and PI3K phosphorylation but not intracellular pH changes or Na+/K+-ATPase abundance

Parathyroid hormone (PTH) has previously been shown to enhance the transepithelial secretion of Cl^? and HCO₃^? across the intestinal epithelia including Caco-2 monolayer, but the underlying cellular mechanisms are not completely understood. Herein, we identified the major signaling pathways that possibly mediated the PTH action to its known target anion channel, i.e., cystic fibrosis transmembrane conductance regulator anion channel (CFTR). Specifically, PTH was able to induce phosphorylation of protein kinase A and phosphoinositide 3-kinase. Since the apical HCO₃^? efflux through CFTR often required the intracellular H⁺/HCO₃^? production and/or the Na⁺-dependent basolateral HCO₃^? uptake, the intracellular pH (pH_i) balance might be disturbed, especially as a consequence of increased endogenous H⁺ and HCO₃^? production. However, measurement of pH_i by a pH-sensitive dye suggested that the PTH-exposed Caco-2 cells were able to maintain normal pH despite robust HCO₃^? transport. In addition, although the plasma membrane Na⁺/K⁺-ATPase (NKA) is normally essential for basolateral HCO₃^? uptake and other transporters (e.g., NHE1), PTH did not induce insertion of new NKA molecules into the basolateral membrane as determined by membrane protein biotinylation technique. Thus, together with our previous data, we concluded that the PTH action on Caco-2 cells is dependent on PKA and PI3K with no detectable change in pH_i or NKA abundance on cell membrane.     

Vanadyl(IV) conalbumin. II. Mixed metal and anion binding studies

Electron paramagnetic resonance (epr) studies demonstrate that at low levels of conalbumin (CA) saturation with Fe³⁺ or VO²⁺, a ph-dependent preference of the metal exists for different protein binding-site configurations,A, B, and C. The vanadyl ion epr spectra of mixed VO²⁺, Fe³⁺-conalbumin in which Fe³⁺ is preferentially bound to the N- or C-terminal binding site are consistent with all three configurations being formed at both metal sites. At high pH the spectra suggest interaction between binding sites. In the absence of HCO₃^?, VO²⁺ is bound almost exclusively in B configuration; a full binding capacity of 2 VO²⁺ per CA is retained. Stoichiometric amounts of HCO₃^? convert the epr spectrum from B to an A, B, C type. Addition of oxalate to bicarbonate-free preparations converts the B spectrum to an A′, B, C′ type where the B resonances have lost intensity to the A′ and C′ resonances but have not changed position. The data suggest that configuration B is anion independent and that only one equivalent of binding sites at pH 9 responds to the presence of HCO₃^1? or oxalate by changing configuration but not metal binding capability. The form of the bound anion may be HCO₃^? rather than CO₃^2?. The formation rate of the colored ferric conalbumin complex by oxidizing Fe²⁺ to Fe³⁺ in limited HCO₃^? at pH 9 is also consistent with one equivalent of sites having different anion requirements than the remaining sites. Increased NaCl or NaClO₄ concentration or substitution of D₂O for water as solvent affect the environment of bound VO²⁺, but the mechanisms of action are unknown.     

Evidence for HCO(3) Transport by the Blue-Green Alga (Cyanobacterium) Coccochloris peniocystis

The possibility of HCO₃⁻ transport in the blue-green alga (cyanobacterium) Coccochloris peniocystis has been investigated. Coccochloris photosynthesized most rapidly in the pH range 8 to 10, where most of the inorganic C exists as HCO₃⁻. If photosynthesis used only CO₂ from the external solution the rate of photosynthesis would be limited by the rate of HCO₃⁻ dehydration to CO₂. Observed rates of photosynthesis at alkaline pH were as much as 48-fold higher than could be supported by spontaneous dehydration of HCO₃⁻ in the external solution. Assays for extracellular carbonic anhydrase were negative. The evidence strongly suggests that HCO₃⁻ was a direct C source for photosynthesis.     

The enhancing effects of anion channel blockers on sperm activation by bicarbonate

We found that anion channel blockers such as phosphotungstate and 4,4′-diisothiocyanatostilbene-2-2′-disulfonate (DIDS)_enhanced HCO₃^?-induced activation on porcine epididymal sperm. In the presence of these compounds, HCO₃^? increased the motility, respiration rate and especially the cAMP content of the sperm to a greater extent than did HCO₃^? alone. The enhancing effects were not observed in the absence of HCO₃^?, but were evident when the concentration of HCO₃^? was low. These compounds did not significantly alter the intracellular pH and did inhibit the adenylate cyclase activity of the sperm plasma membrane. When these compounds were added to sperm homogenate with ATP, the cAMP formed was reduced compared to the control. In addition, these compounds inhibited both the SO₄^2? influx and efflux of the sperm. From these results, we conclude that the anion channel blockers tested principally inhibit the efflux of endogenous HCO₃^? derived from metabolic CO₂, so that HCO₃^? accumulates intracellularly and stimulates the adenylate cyclase of the sperm.     

Kinetic characteristics of bicarbonate-chloride exchange across the neonatal human red cell membrane

The kinetics of HCO₃^?/Cl^? exchange across red cell membrane of newborn infants was studied using a stopped-flow rapid reaction apparatus with a glass pH electrode attached. The measured apparent permeability P is (1.35±0.08 (S.E.)) · 10^?4 cm/s (n=30) for newborns, compared with (3.1 ± 0.4) · 10^?4 cm/s (n=15) for adults. These correspond to half-times of 0.2 s for newborns and 0.1 s for adults indicating that neonatal red cells exchange Cl^? for HCO₃^? only half as fast as do adult cells. The temperature dependence of the exchange rate was studied from 2 to 42°C. From the Arrhenius plot the activation energy of the exchange process in neonatal red cells changes from 22.9 kcal/mol (low temperature) to 4.8 kcal/mol (physiological temperature) at a transition temperature of 17°C. These values are lower than the corresponding values for adult red cells, 34.7 and 10.2 kcal/mol. HCO₃^?/Cl^? exchanges in both adult and neonatal red cells are inhibited by phlorizin. Inhibition constants K_i are 0.8 mM and 2.5 mM for adults and newborns, respectively. The differences in the values of the HCO₃^?/Cl^? exchange rate constant and the activation energy of the exchange process between neonatal and adult red cells indicate that there is a modification of HCO₃^?/Cl^? transport system in the neonatal red cell membranes.     

Regulation of Intracellular pH in Guinea Pig Cerebral Cortex Ex Vivo Studied by 31P and 1H Nuclear Magnetic Resonance Spectroscopy: Role of Extracellular Bicarbonate and Chloride

Abstract: The role of transmembrane processes that are dependent on external anions in the regulation of cerebral intracellular pH (pH_i), high-energy metabolites, and lactate was investigated using ³¹P and ¹H NMR spectroscopy in an ex vivo brain slice preparation. During oxygenated superfusion, removal of external HCO₃^?/CO₂ in the presence of Na⁺ led to a sustained split of the inorganic phosphate (P_i) peak so that the pH_i indicated by one part of the peak was 0.38 pH units more alkaline and by the other part 0.10 pH units more acidic at 5 min than in the presence of HCO₃^?. The pH in the compartment with a higher pH_i value returned to 7.29 ± 0.04 by 10.5 min of superfusion in a HCO₃^?-free medium, whereas the pH_i in an acidic compartment was reduced to 7.02. In the presence of 4,4′-diisothiocyanatostilbene-2,2′-disulfonic acid or the absence of external Cl^?, removal of HCO₃^? caused alkalinization without split of the P_i peak. Both treatments reduced the rate of pH_i normalization following alkalinization. Simultaneous omission of external HCO₃^? and Na⁺ did not inhibit alkalinization of the pH_i following CO₂ exit. All these data show that the acid loading mechanism at neutral pH_i is mediated by an Na⁺-independent anion transport. During severe hypoxia, pH_i dropped from 7.29 ± 0.05 to 6.13 ± 0.16 and from 7.33 ± 0.03 to 6.67 ± 0.05 in the absence and presence of HCO₃^?, respectively, in Na⁺-containing medium. Lactate accumulated to 18.7 ± 2.8 and 19.6 ± 1.5 mmol/kg under the respective conditions. In the HCO₃^?-free medium supplemented with 1 mM amiloride, the pH_i fell only to 6.94 ± 0.08 despite the lactate concentration of 18.9 ± 2.4 mmol/kg. Acidification caused by hypoxia was also small in the slice preparations superfused in the absence of both HCO₃^? and Cl^?, as the pH_i was 7.01 ± 0.12 at a lactate concentration of 24.5 ± 2.4 mmol/kg. These data indicate that apart from anaerobic glucose metabolism, separate acidifying mechanisms are functioning during hypoxia under these conditions. Recovery of phosphocreatine levels following reoxygenation was >75% relative to the prehypoxic level in the slice preparations superfused in the absence of HCO₃^? but <47% in those preparations superfused without HCO₃^? and Cl^?. This indicates that either neutral pH_i or absence of Cl^? during hypoxia was deleterious to the energy metabolism. The present data indicate that Cl^?/HCO₃^? exchange mechanisms have distinct roles in cerebral H⁺ homeostasis depending on the level of pH_i and energy state.