Mechanism of Photosynthetic Carbon Dioxide Uptake by the Red Macroalga, Chondrus crispus

The aim of this study was to determine how Chondrus crispus, a marine red macroalga, acquires the inorganic carbon (C_i) it utilizes for photosynthetic carbon fixation. Analyses of C_i uptake were done using silicone oil centrifugation (using multicellular fragments of thallus), infrared gas analysis, and gas chromatography. Inhibitors of carbonic anhydrase (CA), the band 3 anion exchange protein and Na⁺/K⁺ exchange were used in the study. It was found that: (a) C. crispus does not accumulate C_i internally above the concentration attainable by diffusion; (b) the initial C_i fixtion rate of C. crispus fragments saturates at approximately 3 to 4 millimolar C_i; (c) CA is involved in carbon uptake; its involvement is greatest at high HCO₃⁻ and low CO₂ concentration, suggesting its participation in the dehydration of HCO₃⁻ to CO₂; (d) C. crispus has an intermediate C_i compensation point; and (e) no evidence of any active or facilitated mechanism for the transport of HCO₃⁻ was detected. These data support the view that photosynthetic C_i uptake does not involve active transport. Rather, CO₂, derived from HCO₃⁻ catalyzed by external CA, passively diffuses across the plasma membrane of C. crispus. Intracellular CA also enhances the fixation of carbon in C. crispus.     

Nature of the Inorganic Carbon Species Actively Taken Up by the Cyanobacterium Anabaena variabilis

The nature of the inorganic carbon (C_i) species actively taken up by cyanobacteria CO₂ or HCO₃⁻ has been investigated. The kinetics of CO₂ uptake, as well as that of HCO₃⁻ uptake, indicated the involvement of a saturable process. The apparent affinity of the uptake mechanism for CO₂ was higher than that for HCO₃⁻. Though the calculated V_max was the same in both cases, the maximum rate of uptake actually observed was higher when HCO₃⁻ was supplied. C_i uptake was far more sensitive to the carbonic anhydrase inhibitor ethoxyzolamide when CO₂ was the species supplied. Observations of photosynthetic rate as a function of intracellular C_i level (following supply of CO₂ or HCO₃⁻ for 5 seconds) led to the inference that HCO₃⁻ is the species which arrives at the inner membrane surface, regardless of the species supplied. When the two species were supplied simultaneously, mutual inhibition of uptake was observed.

On the basis of these and other results, a model is proposed postulating that a carboic anhydrase-like subunit of the C_i transport apparatus binds CO₂ and releases HCO₃⁻ at or near a membrane porter. The latter transports HCO₃⁻ ions to the cell interior.

     

Ethoxyzolamide Inhibition of CO(2)-Dependent Photosynthesis in the Cyanobacterium Synechococcus PCC7942

Cells of the cyanobacterium, Synechococcus PCC7942, grown under high inorganic carbon (C_i) conditions (1% CO₂; pH 8) were found to be photosynthetically dependent on exogenous CO₂. This was judged by the fact that they had a similar photosynthetic affinity for CO₂ (K_0.5[CO₂] of 3.4-5.4 micromolar) over the pH range 7 to 9 and that the low photosynthetic affinity for C_i measured in dense cell suspensions was improved by the addition of exogenous carbonic anhydrase (CA). The CA inhibitor, ethoxyzolamide (EZ), was shown to reduce photosynthetic affinity for CO₂ in high C_i cells. The addition of 200 micromolar EZ to high C_i cells increased K_0.5(CO₂) from 4.6 micromolar to more than 155 micromolar at pH 8.0, whereas low C_i cells (grown at 30 microliters CO₂ per liter of air) were less sensitive to EZ. EZ inhibition in high and low C_i cells was largely relieved by increasing exogenous C_i up to 100 millimolar. Lipid soluble CA inhibitors such as EZ and chlorazolamide were shown to be the most effective inhibitors of CO₂ usage, whereas water soluble CA inhibitors such as methazolamide and acetazolamide had little or no effect. EZ was found to cause a small drop in photosystem II activity, but this level of inhibition was not sufficient to explain the large effect that EZ had on CO₂ usage. High C_i cells of Anabaena variabilis M3 and Synechocystis PCC6803 were also found to be sensitive to 200 micromolar EZ. We discuss the possibility that the inhibitory effect of EZ on CO₂ usage in high C_i cells of Synechococcus PCC7942 may be due to inhibition of a `CA-like' function associated with the CO₂ utilizing C_i pump or due to inhibition of an internal CA activity, thus affecting CO₂ supply to ribulose bisphosphate carboxylase-oxygenase.     

The Stoichiometry between CO(2) and H Fluxes Involved in the Transport of Inorganic Carbon in Cyanobacteria

The pH of the medium during CO₂ uptake into the intracellular inorganic carbon (C_i) pool of a high CO₂-requiring mutant (E₁) and wild type of Anacystis nidulans R2 was measured. Experiments were performed under conditions where photosynthetic CO₂ fixation is inhibited. There was an acidification of the medium during CO₂ uptake in the light and an alkalization during CO₂ efflux after darkening. A one to one stoichiometry existed between the amounts of H⁺ appearing in the medium and CO₂ taken up into the intracellular C_i pool, regardless of the carbon species transported. The results indicate that (a) CO₂ is taken up simultaneously with an efflux of equimolar H⁺, probably produced as a result of CO₂ hydration during transport and (b) HCO₃⁻ produced by hydration of CO₂ in the medium was transported into the cells without accompanying net flux of H⁺ or OH⁻. The influx and efflux of C_i during C_i transport produced nonequilibrium between CO₂ and HCO₃⁻ in the medium, with the concentration of HCO₃⁻ being higher than that expected under equilibrium conditions. The nonequilibrium was present even under the conditions where the influx of C_i is compensated by its efflux. The direction of this nonequilibrium suggested that efflux of HCO₃⁻ occurs during uptake of C_i.     

Inorganic carbon transport across cell compartments of the halotolerant alga Dunaliella salina

The inorganic carbon (C_i) accumulation and the intracellular location of carbonic anhydrase (CA, EC 4.2.1.1) in the halotolerant unicellular alga Dunaliella salina have been investigated. The rate of HCO₃ -dependent O₂ evolution was determined by growth conditions. Algae grown under high CO₂ conditions (5% CO₂ in air, v/v; high C_i cells) had a very low affinity for HCO₃^? at pH 7.0 and 8.2, whereas algae grown under low CO₂ conditions (0.03% CO₂ in air; low C_i cells) showed a high affinity for HCO₃^? at both pH values and were sensitive to Dextran-bound sulfonamide (DBS), an inhibitor of extracellular CA. The photosynthetic rate or HCO₄^? dependent O₂ evolution was always higher at pH 7.0 than at pH 8.2. Ethoxyzolamide (EZ), an inhibitor of total (extacellular plus intracellular) CA activity, strongly inhibited photosynthesis at both pH values. During adaptation from high to low CO₂ conditions CA activity increased in chloroplasts in a process dependent on the novo protein synthesis. Carbonic anhydrase activity was found in the supernatant and pellet fractions of chloroplast homogenates. The rate of photosynthesis of chloroplasts from low C_i cells was higher at pH 7.0 than at pH 8.2. The alkalinization of the growth medium, which took place only in the presence of C_i, was partially inhibited by DBS and completely by EZ. We suggest that in D. salina CO₂ is the general form of C_i transported across the plasma membrane and the chloroplast envelope and that bicarbonate enters the cell mainly, although not entirely, by an ‘indirect’ mechanism after dehydration to CO₂.     

Energy Sources for HCO3? and CO2 Transport in Air-Grown Cells of Synechococcus UTEX 625

Light-dependent inorganic C (C_i) transport and accumulation in air-grown cells of Synechococcus UTEX 625 were examined with a mass spectrometer in the presence of inhibitors or artificial electron acceptors of photosynthesis in an attempt to drive CO₂ or HCO₃⁻ uptake separately by the cyclic or linear electron transport chains. In the presence of 3-(3,4-dichlorophenyl)-1,1-dimethylurea, the cells were able to accumulate an intracellular C_i pool of 20 mm, even though CO₂ fixation was completely inhibited, indicating that cyclic electron flow was involved in the C_i-concentrating mechanism. When 200 μm N,N-dimethyl-p-nitrosoaniline was used to drain electrons from ferredoxin, a similar C_i accumulation was observed, suggesting that linear electron flow could support the transport of C_i. When carbonic anhydrase was not present, initial CO₂ uptake was greatly reduced and the extracellular [CO₂] eventually increased to a level higher than equilibrium, strongly suggesting that CO₂ transport was inhibited and that C_i accumulation was the result of active HCO₃⁻ transport. With 3-(3,4-dichlorophenyl)-1,1-dimethylurea-treated cells, C_i transport and accumulation were inhibited by inhibitors of CO₂ transport, such as COS and Na₂S, whereas Li⁺, an HCO₃⁻-transport inhibitor, had little effect. In the presence of N,N-dimethyl-p-nitrosoaniline, C_i transport and accumulation were not inhibited by COS and Na₂S but were inhibited by Li⁺. These results suggest that CO₂ transport is supported by cyclic electron transport and that HCO₃⁻ transport is supported by linear electron transport.     

Regulation of the mechanism for HCO 3 − use by the inorganic carbon level in Porphyra leucosticta Thur. in Le Jolis (Rhodophyta)

The capacity for HCO₃ ⁻ use by Porphyra leucosticta Thur. in Le Jolis grown at different concentrations of inorganic carbon (C_i) was investigated. The use of HCO₃ ⁻ at alkaline pH by P. leucosticta was␣demonstrated by comparing the O₂ evolution rates measured with the O₂ evolution rates theoretically supported by the CO₂ spontaneously formed from HCO₃ ⁻ . Both external and internal carbonic anhydrase (CA; EC 4.2.1.1) were implied in HCO₃ ⁻ use during photosynthesis because O₂ evolution rates and the increasing pH during photosynthesis were inhibited in the presence of azetazolamide and ethoxyzolamide (inhibitors for external and total CA respectively). Both external and internal CA were regulated by the C_i level at which the algae were grown. A high C_i level produced a reduction in total CA activity and a low C_i level produced an increase in total CA activity. In contrast, external CA was increased at low C_i although it was not affected at high C_i . Parallel to the reduction in total CA activity at high C_i is a reduction in the affinity for C_i, as estimated from photosynthesis versus C_i curves, was found. However, there was no evident relationship between external CA activity and the capacity for HCO₃ ⁻ use because the presence of external CA became redundant when P. leucosticta was cultivated at high C_i. Our results suggest that the system for HCO₃ ⁻ use in P. leucosticta is composed of different elements that can be activated or inactivated separately. Two complementary hypotheses are postulated: (i) internal CA is an absolute requirement for a functioning C_i-accumulation mechanism; (ii) there is a CO₂ transporter that works in association with external CA. Received: 20 April 1996 / Accepted: 5 August 1996     

Isolation and Characterization of High CO(2)-Requiring-Mutants of the Cyanobacterium Synechococcus PCC7942 : Two Phenotypes that Accumulate Inorganic Carbon but Are Apparently Unable to Generate CO(2) within the Carboxysome

A total of 24 high CO₂-requiring-mutants of the cyanobacterium Synechococcus PCC7942 have been isolated and partially characterized. These chemically induced mutants are able to grow at 1% CO₂, on agar media, but are incapable of growth at air levels of CO₂. All the mutants were able to accumulate inorganic carbon (C_i) to levels similar to or higher than wild type cells, but were apparently unable to generate intracellular CO₂. On the basis of the rate of C_i release following a light (5 minutes) → dark transition two extreme phenotypes (fast and slow release mutants) and a number of `intermediate' mutants (normal release) were identified. Compared to wild-type cells, Type I mutants had the following characteristics: fast C_i release, normal internal C_i pool, normal carbonic anhydrase (CA) activity in crude extracts, reduced internal exchange of ¹⁸O from ¹⁸O-labeled CO₂, 1% CO₂ requirement for growth in liquid media, normal affinity of carboxylase for CO₂, and long, rod-like carboxysomes. Type II mutants had the following characteristics: slow C_i release, increased internal C_i pool, normal CA activity in crude extracts, normal internal ¹⁸O exchange, a 3% CO₂ requirement for growth in liquid media, high carboxylase activity, normal affinity of carboxylase for CO₂, and normal carboxysome structure but increased in numbers per cell. Both mutant phenotypes appear to have genetic lesions that result in an inability to convert intracellular HCO₃⁻ to CO₂ inside the carboxysome. The features of the type I mutants are consistent with a scenario where carboxysomal CA has been mistargeted to the cytosol. The characteristics of the type II phenotype appear to be most consistent with a scenario where CA activity is totally missing from the cell except for the fact that cell extracts have normal CA activity. Alternatively the type II mutants may have a lesion in their capacity for H⁺ import during photosynthesis.     

Uptake of HCO3? and CO2 in Cells and Chloroplasts from the Microalgae Chlamydomonas reinhardtii and Dunaliella tertiolecta

Mass-spectrometric disequilibrium analysis was applied to investigate CO₂ uptake and HCO₃⁻ transport in cells and chloroplasts of the microalgae Dunaliella tertiolecta and Chlamydomonas reinhardtii, which were grown in air enriched with 5% (v/v) CO₂ (high-Ci cells) or in ambient air (low-Ci cells). High- and low-Ci cells of both species had the capacity to transport CO₂ and HCO₃⁻, with maximum rates being largely unaffected by the growth conditions. In high- and low-Ci cells of D. tertiolecta, HCO₃⁻ was the dominant inorganic C species taken up, whereas HCO₃⁻ and CO₂ were used at similar rates by C. reinhardtii. The apparent affinities of HCO₃⁻ transport and CO₂ uptake increased 3- to 9-fold in both species upon acclimation to air. Photosynthetically active chloroplasts isolated from both species were able to transport CO₂ and HCO₃⁻. For chloroplasts from C. reinhardtii, the concentrations of HCO₃⁻ and CO₂ required for half-maximal activity declined from 446 to 33 μm and 6.8 to 0.6 μm, respectively, after acclimation of the parent cells to air; the corresponding values for chloroplasts from D. tertiolecta decreased from 203 to 58 μm and 5.8 to 0.5 μm, respectively. These results indicate the presence of inducible high-affinity HCO₃⁻ and CO₂ transporters at the chloroplast envelope membrane.     

Two Systems for Concentrating CO(2) and Bicarbonate during Photosynthesis by Scenedesmus

Scenedesmus cells grown on high CO₂, when adapted to air levels of CO₂ for 4 to 6 hours in the light, formed two concentrating processes for dissolved inorganic carbon: one for utilizing CO₂ from medium of pH 5 to 8 and one for bicarbonate accumulation from medium of pH 7 to 11. Similar results were obtained with assays by photosynthetic O₂ evolution or by accumulation of dissolved inorganic carbon inside the cells. The CO₂ pump with K_0.5 for O₂ evolution of less than 5 micromolar CO₂ was similar to that previously studied with other green algae such as Chlamydomonas and was accompanied by plasmalemma carbonic anhydrase formation. The HCO₃⁻ concentrating process between pH 8 to 10 lowered the K_0.5 (DIC) from 7300 micromolar HCO₃⁻ in high CO₂ grown Scenedesmus to 10 micromolar in air-adapted cells. The HCO₃⁻ pump was inhibited by vanadate (K_i of 150 micromolar), as if it involved an ATPase linked HCO₃⁻ transporter. The CO₂ pump was formed on low CO₂ by high-CO₂ grown cells in growth medium within 4 to 6 hours in the light. The alkaline HCO₃⁻ pump was partially activated on low CO₂ within 2 hours in the light or after 8 hours in the dark. Full activation of the HCO₃⁻ pump at pH 9 had requirements similar to the activation of the CO₂ pump. Air-grown or air-adapted cells at pH 7.2 or 9 accumulated in one minute 1 to 2 millimolar inorganic carbon in the light or 0.44 millimolar in the dark from 150 micromolar in the media, whereas CO₂-grown cells did not accumulate inorganic carbon. A general scheme for concentrating dissolved inorganic carbon by unicellular green algae utilizes a vanadate-sensitive transporter at the chloroplast envelope for the CO₂ pump and in some algae an additional vanadate-sensitive plasmalemma HCO₃⁻ transporter for a HCO₃⁻ pump.     

Is There a Role for the 42 Kilodalton Polypeptide in Inorganic Carbon Uptake by Cyanobacteria?

Cyanobacterial cells accumulate substantial amounts of a membrane-associated 42 kilodalton polypeptide during adaptation to low CO₂ conditions. The role of this polypeptide in the process of adaptation and in particular in the large increase in the ability to accumulate inorganic carbon (C_i), which accompanies this process, is not yet understood. We have isolated a mutant Synechococcus PCC7942 that does not accumulate the 42 kilodalton polypeptide. The mutant requires a high-CO₂ concentration for growth and exhibits a very low apparent photosynthetic affinity for extracellular C_i. The latter might be attributable to the observed defective ability of the mutant to utilize the intracellular C_i pool for photosynthesis. The 42 kilodalton polypeptide does not appear to participate directly in the active transport of C_i, since the difference between the observed capabilities for CO₂ and HCO₃⁻ uptake of the mutant and the wild type is not sufficient to account for their different growth and photosynthetic performance. Furthermore, high CO₂-grown wild-type cells, where we could not detect the 42 kilodalton polypeptide, transported CO₂ faster than the mutant. An analysis of the curves relating the rate of accumulation of C_i to the concentration of CO₂ or HCO₃⁻ supplied, in the presence or absence of carbonic anhydrase, indicated that under the experimental conditions used here, CO₂ was the preferred C_i species taken up by Synechococcus.     

Inorganic Carbon Uptake by Chlamydomonas reinhardtii

The rates of CO₂-dependent O₂ evolution by Chlamydomonas reinhardtii, grown with either air levels of CO₂ or air with 5% CO₂, were measured at varying external pH. Over a pH range of 4.5 to 8.5, the external concentration of CO₂ required for half-maximal rates of photosynthesis was constant, averaging 25 micromolar for cells grown with 5% CO₂. This is consistent with the hypothesis that these cells take up CO₂ but not HCO₃⁻ from the medium and that their CO₂ requirement for photosynthesis reflects the K_m(CO₂) of ribulose bisphosphate carboxylase. Over a pH range of 4.5 to 9.5, cells grown with air required an external CO₂ concentration of only 0.4 to 3 micromolar for half-maximal rates of photosynthesis, consistent with a mechanism to accumulate external inorganic carbon in these cells. Air-grown cells can utilize external inorganic carbon efficiently even at pH 4.5 where the HCO₃⁻ concentration is very low (40 nanomolar). However, at high external pH, where HCO₃⁻ predominates, these cells cannot accumulate inorganic carbon as efficiently and require higher concentrations of NaHCO₃ to maintain their photosynthetic activity. These results imply that, at the plasma membrane, CO₂ is the permeant inorganic carbon species in air-grown cells as well as in cells grown on 5% CO₂. If active HCO₃⁻ accumulation is a step in CO₂ concentration by air-grown Chlamydomonas, it probably takes place in internal compartments of the cell and not at the plasmalemma.     

Expression of Human Carbonic Anhydrase in the Cyanobacterium Synechococcus PCC7942 Creates a High CO(2)-Requiring Phenotype : Evidence for a Central Role for Carboxysomes in the CO(2) Concentrating Mechanism

Active human carbonic anhydrase II (HCAII) protein was expressed in the cyanobacterium Synechococcus PCC7942 by means of transformation with the bidirectional expression vector, pCA. This expression was driven by the bacterial Tac promoter and was regulated by the IacIQ repressor protein, which was expressed from the same plasmid. Expression levels reached values of around 0.3% of total cell protein and this protein appeared to be entirely soluble in nature and located within the cytosol of the cell. The expression of this protein has dramatic effects on the photosynthetic physiology of the cell. Induction of expression of carbonic anhydrase (CA) activity in both high dissolved inorganic carbon (C_i) and low C_i grown cells leads the creation of a high C_i requiring phenotype causing: (a) a dramatic increase in the K_0.5 (C_i) for photosynthesis, (b) a loss of the ability to accumulate internal C_i, and (c) a decrease in the lag between the initial C_i accumulation following illumination and the efflux of CO₂ from the cells. In addition, the effects of the expressed CA can largely be reversed by the carbonic anhydrase inhibitor ethoxyzolamide. As a result of the above findings, it is concluded that the CO₂ concentrating mechanism in Synechococcus PCC7942 is largely dependent on (a) the absence of CA activity from the cytosol, and (b) the specific localization of CA activity in the carboxysome. A theoretical model of photosynthesis and C_i accumulation is developed in which the carboxysome plays a central role as both the site of CO₂ generation from HCO_3⁻ and a resistance barrier to CO₂ efflux from the cell. There is good qualitative agreement between this model and the measured physiological effects of expressed cytosolic CA in Synechococcus cells.     

UPTAKE,EFFLUX, AND PHOTOSYNTHETIC UTILIZATION OF INORGANIC CARBON BY THE MARINE EUSTIGMATOPHYTE NANNOCHLOROPSIS SP.1

Uptake, efflux and utilization of inorganic carbon were investigated in the marine eustigmatophyte Nannochloropsis sp. grown under an air level of CO₂. Maximal photosynthetic rate was hardly affected by raising the pH porn 5.0 to 9.0. The apparent photosynthetic affinity for dissolved inorganic carbon (DIC) was 35 μM DIC between pH 6.5 to 9.0, but increased approximately threefold at pH 5.0 suggesting that HCO₃- was the main DIC species used from the medium. No external carbonic anhydrase (CA) activity could be detected by the pH drift method. However, application of ethoxyzolamide (an inhibitor of CA) resulted an a significant inhibition of photosynthetic O₂ evolution and carbon utilization, suggesting involvement of internal CA or CA-like activity in DIC utilization. Under high light conditions, the rate of HCO₃^? uptake and its internal conversion to CO₂ apparently exceeded the rate of carbon fixation, resulting in a large leak of CO₂ from the cells to the external medium. When the cells were exposed to low DIC concentrations, the ratio of internal to external DIC concentration was about eight. On the other hand, in the presence of 2 mM DIC, conditions prevailing in the marine environment, the internal concentration of DIC was only 50% higher than the external one.     

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.     

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).     

Photosynthesis and inorganic carbon acquisition in the cyanobacterium Chlorogloeopsis sp. ATCC 27193

The ability of the morphologically complex cyanobacterium Chlorogloeopsis sp. ATCC 27193 to actively transport and accumulate inorganic carbon (C₁= CO₂+ HCO₃^?+ CO₃^2?) for photosynthetic CO₂ fixation was investigated. Mass-spectrometric assays revealed that Chlorogloeopsis cells grown under C₁ limitation rapidly took up CO₂ from the medium in a light-dependent reaction which was independent of CO₂ fixation. Ethoxyzolamide, a carbonic anhydrase (CA) inhibitor, inhibited CO₂ transport. Since electrometric and mass-spectrometric assays did not detect the presence of a periplasmic CA, it is suggested that CO₂ transport was mediated by a CA-like activity which converted CO₂ to HCO₃^? during passage across the membrane. Radiochemical assays, using H¹⁴CO₃ as substrate, showed that C₃-limited cells also had a high affinity (K_0.5 HCO₃^?= 37 μM), Na⁺-independent HCO₃^? uptake mechanism. HCO₃^?uptake was light dependent and occurred against its electrochemical potential indicating a carrier-mediated, active transport process. The rate of Na⁺-independent HCO₃^? transport was sufficient to account for the steady state rate of CO₂ fixation. Although not absolutely required. Na⁺ did specifically enhance the rate of HCO₃^? transport by up to 2-fold, but had no effect on the apparent affinity of the transport system for HCO₃^? Combined CO₂ and HCO₃^? transport resulted in C₁ accumulation as high as 25 mM and in excess of 300 times the external concentration. The C₁ pool was the source of CO₂ for photo-synthetic fixation and was generated, presumably, by the dehydration of HCO₃^? catalyzed by an intracellular CA. The collective evidence indicates that Chlorogloeopsis has a physiologically functional CO₂-concentrating mechanism which is essential for photosynthesis.     

Mutants of Synechocystis PCC6803 Defective in Inorganic Carbon Transport

Eighty mutants of Synechocystis PCC6803 that require high CO₂ for growth were examined with a mass spectrometer for their ability to take up CO₂ in the light. Two of these mutants (type A) did not show any CO₂ uptake while the rest of the mutants (type B) took up CO₂ actively. Type A mutants (RKa and RKb) and one type B mutant (RK11) were partially characterized. At 3% CO₂, growth rates of the mutants and the wild type (WT) were similar. Under air levels of CO₂, growth of RKa and RKb was very slow, and RK11 did not grow at all. The photosynthetic affinities for inorganic carbon (C_i) in these three mutants were about 100 times lower than the affinity in WT. The following characteristics of type A mutants indicated that the mutants have a defect in their CO₂-transport system: (a) the activity of ¹³C¹⁸O₂ uptake in RKa and RKb in the light was less than 5% the activity in WT, and (b) each mutant had only a low level of activity of ¹⁴CO₂ uptake as measured by the method of silicone oil-filtering centrifugation. The HCO₃⁻-transport system was also impaired in these mutants. The activity of H¹⁴CO₃⁻ uptake was negligibly low in RKb and was one-third the activity of WT in RKa. On the other hand, the type B mutant, RK11, transported CO₂ and HCO₃⁻ into the intracellular C_i pool as actively as WT but was unable to utilize it for photosynthesis. Complementation analysis of type A mutants indicated that RKa and RKb have mutations in different regions of the genome. These results suggested that at least two kinds of proteins are involved in the C_i-transport system.     

Intracellular pH Regulation in Cultured Astrocytes from Rat Hippocampus : II. Electrogenic Na/HCO3 Cotransport

In the preceding paper (Bevensee, M.O., R.A. Weed, and W.F. Boron. 1997. J. Gen. Physiol. 110: 453–465.), we showed that a Na⁺-driven influx of HCO₃ ⁻ causes the increase in intracellular pH (pH_i) observed when astrocytes cultured from rat hippocampus are exposed to 5% CO₂/17 mM HCO₃ ⁻. In the present study, we used the pH-sensitive fluorescent indicator 2′,7′-biscarboxyethyl-5,6-carboxyfluorescein (BCECF) and the perforated patch-clamp technique to determine whether this transporter is a Na⁺-driven Cl-HCO₃ exchanger, an electrogenic Na/HCO₃ cotransporter, or an electroneutral Na/HCO₃ cotransporter. To determine if the transporter is a Na⁺-driven Cl-HCO₃ exchanger, we depleted the cells of intracellular Cl⁻ by incubating them in a Cl⁻-free solution for an average of ∼11 min. We verified the depletion with the Cl⁻-sensitive dye N-(6-methoxyquinolyl)acetoethyl ester (MQAE). In Cl⁻-depleted cells, the pH_i still increases after one or more exposures to CO₂/HCO₃ ⁻. Furthermore, the pH_i decrease elicited by external Na⁺ removal does not require external Cl⁻. Therefore, the transporter cannot be a Na⁺-driven Cl-HCO₃ exchanger. To determine if the transporter is an electrogenic Na/ HCO₃ cotransporter, we measured pH_i and plasma membrane voltage (V_m) while removing external Na⁺, in the presence/absence of CO₂/HCO₃ ⁻ and in the presence/absence of 400 μM 4,4′-diisothiocyanatostilbene-2,2′-disulphonic acid (DIDS). The CO₂/HCO₃ ⁻ solutions contained 20% CO₂ and 68 mM HCO₃ ⁻, pH 7.3, to maximize the HCO₃ ⁻ flux. In pH_i experiments, removing external Na⁺ in the presence of CO₂/HCO₃ ⁻ elicited an equivalent HCO₃ ⁻ efflux of 281 μM s⁻¹. The HCO₃ ⁻ influx elicited by returning external Na⁺ was inhibited 63% by DIDS, so that the predicted DIDS-sensitive V_m change was 3.3 mV. Indeed, we found that removing external Na⁺ elicited a DIDS-sensitive depolarization that was 2.6 mV larger in the presence than in the absence of CO₂/ HCO₃ ⁻. Thus, the Na/HCO₃ cotransporter is electrogenic. Because a cotransporter with a Na⁺:HCO₃ ⁻ stoichiometry of 1:3 or higher would predict a net HCO₃ ⁻ efflux, rather than the required influx, we conclude that rat hippocampal astrocytes have an electrogenic Na/HCO₃ cotransporter with a stoichiometry of 1:2.     

Negative Impact on Growth and Photosynthesis in the Green Alga Chlamydomonas reinhardtii in the Presence of the Estrogen 17α-Ethynylestradiol

It is well known that estrogenic compounds affect development of fertilized eggs of many species of birds, fish and amphibians through disrupted activity of carbonic anhydrase (CA). The most potent activity comes from the most commonly occurring synthetic sterol, 17α-Ethynylestradiol (EE2). Less is known about the responses of aquatic phytoplankton to these compounds. Here we show for the first time that, in comparision to the control, the addition of 7 µM EE2 reduced the growth rate of the green alga Chlamydomonas reinhardtii by 68% for cells grown at high CO₂. When cells were grown in ambient air (low C_i) with a fully activated carbon concentrating mechanism through the induction of CA activity, the growth rates were reduced by as much as 119%. A reduced growth rate could be observed at EE2 concentrations as low as 10 pM. This was accompanied by a reduced maximum capacity for electron transport in photosystem II as determined by a lower F_V/F_M for low C_i-grown cells, which indicates the involvement of CAH3, a CA specifically located in the thylakoid lumen involved in proton pumping across the thylakoid membranes. These results were in agreement with an observed reduction in the chloroplastic affinity for C_i as shown by a strong increase in the Michaelis-Menten K_0.5 for HCO₃ ⁻. In itself, a lowering of the growth rate of a green alga by addition of the sterol EE2 warrants further investigation into the potential environmental impact by the release of treated waste water.