Uptake and Accumulation of Inorganic Carbon by a Freshwater Diatom

Colman, B. and Rotatore, C. 1988. Uptake and accumulation ofinorganic carbon by a freshwater diatom.—J. exp Bot 39:1025–1032. The mechanism of uptake of inorganic carbon and its accumulationhas been studied in the freshwater diatom Navicula pelliculosa.No external carbonic anhydrase could be detected, although itwas detected in cell extracts. The rate of photosynthetic O₂evolution, in media in the range pH 7.5–8.5, exceededthe calculated rate of CO₂ supply 2- to 5-fold, indicating thatHCO^–₃ was taken up by the cells. At an external pH of7.5, the internal pH, measured by ¹⁴C-dimethyloxazolidine-2,4-dione distribution between the cells and the medium, was pH7.6 in the light and pH 7.4 in the dark. Accumulation of inorganiccarbon was determined by the silicone oil centrifugation methodand inorganic carbon pools of 23.5 mol m^–3 were found,a concentration 21.6-fold that in the external medium. The resultsindicate an active accumulation of inorganic carbon againstpH and concentration gradients in this diatom, probably by activeHCO^–₃ uptake. Key words: Bicarbonate transport, carbon dioxide, carbonic anhydrase, CO₂ affinity, CO₂ concentrating mechanism, internal pH, Navicula pelliculosa     

The Location of the Transporting System for Inorganic Carbon and the Nature of the Form Translocated in Chlamydomonas reinhardtii

The permeability of the plasmalemma of Chlamydomonas reinhardtiicells was increased by treatment with poly-L-lysine or dimethylsulphoxideas indicated by 3-phosphoglyceric acid dependent O₂ evolution.These treatments decreased the ability of the cells to accumulateinorganic carbon internally and hence their photosynthetic affinityfor inorganic carbon in the medium. With saturating light andinorganic carbon, the photosynthetic rate was less affectedby the poly-L-lysine and dimethylsulphoxide treatments. Thusthe poly-L-lysine and dimethylsulphoxide did not alter the activityof the chloroplasts but rather made the intracellular inorganiccarbon pool more freely exchangeable with the medium. It isconcluded that the transporting system for inorganic carbonis located at the plasmalemma. Treatment with Diamox, an inhibitor of carbonic anhydrase, didnot affect photosynthetic rate and accumulation of inorganiccarbon when CO₂ was supplied but strongly inhibited both parameterswhen HCO^–₃ was supplied. In a mutant of Chlamydomonasreinhardtii lacking a cell wall, carbonic anhydrase leaks tothe medium and uptake of inorganic carbon is much faster whenCO₂ is supplied than when HCO^–₃ is supplied. These resultssuggest that CO₂ rather than HCO^–₃ is the inorganic carbonspecies that is actively translocated across the plasmalemma. Key words: Chlamydomonas, Inorganic carbon uptake     

Alkalization of the Medium by Unicellular Green Algae during Uptake Dissolved Inorganic Carbon

When Chlorella vulgaris 11h, Chlorella vulgaris C-l, Chlamydomonasreinhardtii, Chlamydomonas moewusii, Scenedesmus obliquus, orDunaliella tertiolecta were illuminated in with 0.5 mM NaHCO₃,the pH of the medium increased in a few minutes from 6 to about9 or 10. The alkalization, which was accompanied by O₂ evolution,was dependent on light, external dissolved inorganic carbon(DIC) as HCO^-₃, and algae grown or adapted to a low, air-levelCO₂ in order to develop a DIC concentrating mechanism. Therewas little pH increase by algae without a DIC concentratingprocess from growth on 3% CO₂ in air. Photosynthetic O₂ evolutionwithout alkalization occurred using either internal DIC or externalCO₂ at acidic pH. The PH increase stopped between pH 9 to 10,but the alkalization would restart upon re-acidification betweenpH 6 and 8. Alkalization was suppressed by the carbonic anhydraseinhibitors, acetazolamide, ethoxyzolamide or carbon oxysulfide.The pH increase appeared to be the consequence of the externalconversion of HCO^–₃ into CO₂ plus OH^– during photosynthesisby cells with a high affinity for CO₂ uptake. Cells grown onhigh CO₂ to suppress the DIC pump, when given low levels ofHCO^–₃ in the light, acidified the medium from pH 10 to7. Air adapted Scenedesmus cells with a HCO^–₃ pump, aswell as a CO₂ pump, alkalized the medium very rapidly in thelight to a pH of over 10, as well as slower in the dark or inthe light with DCMU or without external DIC and O₂ evolution.Alkalization of the medium during photosynthetic DIC uptakeby algae has been considered to be part of the global carboncycle for converting H₂CO₃ to HCO^–₃ and for the formationof carbonate salts by calcareous algae from the alkaline conversionof bicarbonate to carbonate. These processes seem to be a consequenceof the algal CO₂ concentrating process. ¹Present address: Department of Biology, Faculty of Science,Niigata University, Niigata, 950-21 Japan.     

Transport and Fixation of Inorganic Carbon during Photosynthesis in Cells of Anabaena Grown under Ordinary Air: III. Some Characteristics of the HCO3--Transport System in Cells Grown under Ordinary Air

In cells of cyanobacterium Anabaena variabilis grown under ordinaryair (low-CO₂ cells), the transport of both CO₂ and HCO₃^–was significantly enhanced by Na⁺. This effect was pronouncedas the external pH increased. When low-CO₂ cells were treatedwith an inhibitor of carbonic anhydrase (CA), only CO₂ transportbut not HCO₃^– transport, was inhibited. The initial rateof photosynthetic carbon fixation as a function of the concentrationof internal inorganic carbon (IC) was practically the same irrespectiveof whether CO₂ or HCO₃^– was externally supplied. Theseresults suggest that IC is actively transported through theplasma membrane in a form of HCO₃^– probably by some transporterand that the transmembrane Na⁺ gradient is involved in thisIC transport system. Free CO₂ may be hydrated by CA to HCO₃^–and then transported to the cells by this transporter. On the other hand, CO₂ is actively taken up by cells grown withair containing 5% CO₂ (high-CO₂ cells) though the enhancingeffect of Na⁺ was much smaller in high- CO₂ cells than in low-CO₂cells. The initial rate of fixation as a function of internal IC concentrationindicated that the rate of the carboxylation reaction of accumulatedIC is higher in I0W-CO₂ cells than in high-CO₂ cells. The studieswith ethoxyzolamide indicated that even in low-CO₂ cells, CAdoes not function inside Anabaena cells. These results suggestthat inside the low-CO₂ cells of Anabaena, some mediator(s)facilitates the transport of IC to RuBPCase. (Received January 23, 1987; Accepted April 24, 1987)     

Transport and Fixation of Inorganic Carbon in the Cells of Chlorella vulgaris 11h Grown under Ordinary Air

Intracellular accumulation of inorganic carbon (C_i) and itsfixation in photosynthesis were investigated using siliconeoil layer filtering centrifugation technique with the cellsof Chlorella vulgaris 11h grown under ordinary air. Both CO₂and HCO₃^– were transported into the cells from the reactionmedium and accumulated in the cells, but the rate of transportwas much faster for the former than the latter. ¹⁴C-fixationfrom the total transported C_i was much more efficient when CO₂was added in the external medium than when HCO₃^– was added.This indicates that CO₂ and HCO₃^– were not converted tothe common compound in the cells during the initial period ofphotosynthesis. Accumulation of Cⁱ into the cells was much lesssusceptible to low temperature than its fixation. Accumulationof Cⁱ was also observed in the dark. Ethoxyzolamide, an inhibitorof carbonic anhydrase (CA), inhibited the fixation of accumulatedCO₂ in the cells, suggesting that CA enhanced the supply ofCO₂ to the reaction site of ribulose bisphosphate carboxylasein the stroma. Mechanism for transport and fixation of Cⁱ duringphotosynthesis in low-CO₂ cells of C. vulgaris 1lh was proposedfrom these results. (Received March 19, 1986; Accepted June 26, 1986)     

Kinetic Studies on the Active Species of Inorganic Carbon Absorbed by the Cells of Dunaliella tertiolecta

Cells of Dunaliella tertiolecta which had been grown in ordinaryair (low-CO₂ cells) had high carbonic anhydrase (CA) activityon the cell surface and mainly utilized HCO₃^– for photosynthesis.When CA activity on the cell surface was inhibited by Diamoxor subtilisin, the cells utilized CO₂. When bovine CA was added,the subtilisin-treated low-CO₂ cells utilized mainly HCO₃^–.When grown in air containing 2% CO₂, the cells had low CA activityon the cell surface, and preferred CO₂ to HCO₃^–. Kineticanalysis of these results indicated that low-CO₂ cells of D.tertiolecta absorb CO₂ which was converted from HCO₃^–via the CA located on the cell surface. (Received June 29, 1985; Accepted October 9, 1985)     

Utilization Modes of Inorganic Carbon for Photosynthesis in Various Species of Chlorella

Rates of CO₂ and HCC₃^– fixation in cells of various Chlorellaspecies in suspension were compared from the amounts of ¹⁴Cfixed during the 5 s after the injection of a solution containingonly ¹⁴CO₂ or H¹⁴CO₃^–. Results indicated that irrespectiveof the CO₂ concentration during growth, Chlorella vulgaris 11h and C. miniata mainly utilized CO₂, whereas C. vulgaris C-3,C. sp. K. and C. ellipsoidea took up HCO₃^– in additionto CO₂. Cells of C. pyrenoidosa that had been grown with 1.5%CO₂ (high-CO₂ cells) mainly utilized CO₂, whereas those grownwith air (low-CO₂ cells) utilized HCO₃^– in addition toCO₂. Cells that utilized HCO₃^– had carbonic anhydrase(CA) on their surfaces. The effects of Diamox and CA on the rates of CO₂ and HCO₃^–fixation are in accord with the inference that HCO₃^– wasutilized after conversion to CO₂ via the CA located on the cellsurface. CA was found in both the soluble and insoluble fractions;the CA on the cell surface was insoluble. Independent of the modes of utilization, the apparent K_m (NaHCO₃)for photosynthesis was much lower in low-CO₂ cells than in high-CO₂ones. The fact that the CA in the soluble fraction in C. vulgarisC-3 was closely correlated with the K_m(NaHCO₃) indicates thatsoluble CA lowers the K_m. ¹ Dedicated to the late Professor Joji Ashida, one of the foundersand first president of the Japanese Society of Plant Physiologists. ⁴ On leave from Research and Production Laboratory of Algology,Bulgarian Academy of Sciences, Sofia. (Received September 14, 1982; Accepted March 1, 1983)     

Form of Inorganic Carbon Utilized for Photosynthesis in Chlamydomonas reinhardtii1

The effect of carbonic anhydrase (CA) on time courses of photosynthetic¹⁴C incorporation in the presence of ¹⁴CO₂ or NaH¹⁴CO₃ was studiedwith cells of Chlamydomonas reinhardtii which had been grownunder ordinary air (low-CO₂ cells) or air enriched with 4% CO₂(high-CO₂ cells). Experimental data obtained at 20°C andpH 8.0 suggested that the major form of inorganic carbon utilizedby high-CO₂ cells was CO₂, while that utilized by low-CO₂ cellswas HCO₃^–. The cell suspension showed CA activity which was comparableto that observed in the sonicate of cells. Both activities werehigher in low-CO₂ cells than in high-CO₂ cells. The mechanism by which HCO₃^– is utilized by low-CO₂ cellsof C. reinhardtii is discussed. ³Present address: Department of Biology, Faculty of Science,University of Niigata, Niigata 950-21, Japan. (Received August 4, 1982; Accepted January 19, 1983)     

Enzymatic Inactivation of Extracellular Carbonic Anhydrase and its Effect on K1/2 (CO2) for Photosynthesis in Chlorella ellipsoidea C-27

The ratio of the extracellular to the intracellular activityof carbonic anhydrase (CA) in cells of Chlorella ellipsoideaC-27, adapted to low levels of CO₂ for 24 h (low-CO₂ cells),was about one to one. Treatment of intact cells with PronaseP inactivated about one-half of the extracellular CA activitywithout affecting photosynthetic activity. The CA activity incell homogenates and in cell-wall ghosts liberated during celldivision was completely inactivated by the same treatment. Pretreatmentwith Glycosidase mix, Chitosanase and Macerozyme enhanced theinactivation of the CA activity in intact cells. These resultssuggest that extracellular CA is evenly distributed throughoutthe whole cell-wall region. The apparent K_1/2 for dissolved inorganic carbon (DIC) in low-CO₂cells doubled when extracellular CA was inactivated by treatmentwith Pronase P, but the K_1/2 obtained was still one-half ofthat in high-CO₂ cells. Photosynthetic ¹⁴CO₂-fixation in low-CO₂cells was enhanced by acetazolamide, whereas H¹⁴CO₃^–-fixationwas suppressed. The results suggest that CO₂ is a dominant substrateutilized by cells and that HCO₃^– is utilized after conversionto CO₂. The present results show that both intracellular andextracellular CA contribute to the increase in affinity forDIC during photosynthesis in low-CO₂ cells of Chlorella ellipsoideaC-27. (Received May 7, 1990; Accepted July 18, 1990)     

Utilization of Sediment CO2 by Selected North American Isoetids

The photosynthetic uptake of root-zone CO₂ was determined forEriocaulon septangulare, Gratiola aurea, Isoetes macrospora,Littorella uniflora var. americana and Lobelia dortmanna aspart of a study of the photosynthetic carbon economy of submergedaquatic isoetids. The pH and dissolved inorganic carbon (DIC)of the sediment interstitial water in four Wisconsin lakes reflectedthe water column character, where the DIC increased with depthin the sediment to concentrations five to ten times those ofthe water column. Sediment free CO₂ concentrations were 5–50times those in the water column and were similar at all sites(about 05–1.0mM CO₂ in the root-zone). In ‘pH-drift’studies these plants were unable to take up HCO₂^–. Laboratory determinations of the carbon uptake from the rootand shoot-zones were made for all five species. These experimentsshowed that CO₂ in the root-zone accounted for 65–95 percent of external carbon uptake for the five species. For G.aurea and E. septangulare, root-zone CO₂ was > 85 per centof carbon uptake. Carbon, CO₂, photosynthesis, sediment, isoetid, Eriocaulon septangulare, Gratiola aurea, Isoetes macrospora, Littorella uniflora, Lobelia dortmanna     

Analogue Inhibition of the Active HCO-3 Transport Site in the Characean Plasma Membrane

Competitive inhibition of the HCO^–₃ transport site, atthe plasmalemma of Chara coraUina, by the CO^2–₃ ion isdemonstrated. This CO^2–₃ inhibition was used to demonstratethat HCO^–₃ ions enter the cell by facilitated ‘diffusion’when the HCO^–₃ transport system has been inactivated bytreatment with 10 mM K⁺. Use of CO^2–₃ as a HCO^–₃analogue is limited, however, because of the necessity to employsolutions of high pH. Inhibition was not observed in the presenceof a range of organic and inorganic acid anions. These resultsdemonstrate the stereo-specific nature of the HCO^–₃ bindingsite. A variety of amino compounds were found to inhibit H¹⁴CO^–₃influx. Inhibition appeared to be competitive, being completelyrelieved at higher substrate (HCO^–₃) concentrations. Asimple correlation was not found between the degree of inhibitionand the concentration of neutral base. A combination of thepresence of neutral base and experimental pH values of at least8·0 was required to produce the reactive species thatinhibited HCO^–₃ transport. This species is consideredto be the amino carbamate. These results are discussed withrespect to further HCO^–₃ analogue experiments.     

Further Characteristics of Salt-Dependent Bicarbonate Use by the Seagrass Zostera muelleri

Millhouse, J. and Strother, S. 1987. Further characteristicsof salt-dependent bicarbonate use by the seagrass Zostera muelleri.—J.exp. Bot. 38: 1055–1068. The contribution of HCO^–₃to photosynthetic O₂ evolutionin the seagrass Zostera muelleri Irmisch ex Aschers. increasedwith increasing salinity of the bathing seawater when the inorganiccarbon concentration was kept constant. K_1/2 (seawater salts)for HCO^–₃ -dependent photosynthesis was 66% of seawatersalinity. Both short- and long-term pretreatment at low salinitiesstimulated photosynthesis in full strength seawater. Twentyfour hours pre-incubation of seagrass plants in 3·0 molm^–3 NaHCO₃ resulted in increased photosynthesis at allsalinities, apparently due to stimulation of HCO^–₃ use(K_1/2 (seawater salts) = 26%). V_max (HCO^–₃) was not affectedby low salinity pretreatment. The kinetics of HCO^–₃ stimulationby the major seawater cations was investigated. Ca²⁺ was themost effective cation with the highest V_max (HCO^–₃) andwith K_1/2(Ca²⁺) = 14 mol m^–3. Mg²⁺ was also very effectiveat less than 50 mol m^–3 but higher concentrations wereinhibitory. This inhibition cannot be accounted for solely byprecipitation of MgCO₃. Na⁺ and K⁺ were both capable of stimulatingHCO^–₃ use. Stimulation was in two distinct parts. Up to500 mol m^–3, both citrate and chloride salts gave similarresults (K_1/2(Na⁺) 81 mol m^–3, V_max(HCO^–₃) 0·26µmol O₂ mg^–1 chl min^–1), but use of citratesalts above 500 mol m^–2 caused a second stimulation ofHCO^–₃ use (K_1/2(Na⁺) 830 mol m^–3, V_max(HCO^–₃)0·68 µmol O₂ mg^–1 chl min^–1). V_max(HCO^–₃)for the second-phase Na⁺ or K⁺ stimulation was of the same orderas for Ca²⁺-stimulated HCO^–₃ use. To further characterizesalt-dependent HCO^–₃ use, the sensitivity of photosynthesisto Tris and TES buffers was investigated. The effects of Trisappear to be due to the action of Tris⁺ causing stimulationof HCO^–₃ -dependent photosynthesis in the absence of salt,but inhibition of HCO^–₃ use in saline media. TES has noeffect on photosynthesis. External carbonic anhydrase, althoughimplicated in salt-dependent HCO^–₃ use in Z. muelleri,could not be detected in whole leaves. Key words: Zostera muelleri, HCO^–₃ use, salinity     

Na+-dependent HCO3- uptake into the rat choroid plexus epithelium is partially DIDS sensitive

Several studies suggest the involvement of Na⁺ and HCO₃^– transport in the formation of cerebrospinal fluid. Two Na⁺-dependent HCO₃^– transporters were recently localized to the epithelial cells of the rat choroid plexus (NBCn1 and NCBE), and the mRNA for a third protein was also detected (NBCe2) (Praetorius J, Nejsum LN, and Nielsen S. Am J Physiol Cell Physiol 286: C601–C610, 2004). Our goal was to immunolocalize the NBCe2 to the choroid plexus by immunohistochemistry and immunogold electronmicroscopy and to functionally characterize the bicarbonate transport in the isolated rat choroid plexus by measurements of intracellular pH (pH_i) using a dual-excitation wavelength pH-sensitive dye (BCECF). Both antisera derived from COOH-terminal and NH₂-terminal NBCe2 peptides localized NBCe2 to the brush-border membrane domain of choroid plexus epithelial cells. Steady-state pH_i in choroidal cells increased from 7.03 ± 0.02 to 7.38 ± 0.02 (n = 41) after addition of CO₂/HCO₃^– into the bath solution. This increase was Na⁺ dependent and inhibited by the Cl^– and HCO₃^– transport inhibitor DIDS (200 µM). This suggests the presence of Na⁺-dependent, partially DIDS-sensitive HCO₃^– uptake. The pH_i recovery after acid loading revealed an initial Na⁺ and HCO₃^–-dependent net base flux of 0.828 ± 0.116 mM/s (n = 8). The initial flux in the presence of CO₂/HCO₃^– was unaffected by DIDS. Our data support the existence of both DIDS-sensitive and -insensitive Na⁺- and HCO₃^–-dependent base loader uptake into the rat choroid plexus epithelial cells. This is consistent with the localization of the three base transporters NBCn1, Na⁺-driven Cl^– bicarbonate exchanger, and NBCe2 in this tissue. bicarbonate metabolism; BCECF; cerebrospinal fluid; acid/base transport; ammonium prepulse     

Photosynthetic Nitrogen Metabolism in High and Low CO2-adapted Scenedesmus: I. INORGANIC CARBON-DEPENDENT O2 EVOLUTION, NITRATE UTILIZATION AND NITROGEN RECYCLING

Larsson, M., Larsson, C.-M. and Guerrero, M. G. 1985. Photosyntheticnitrogen metabolism in high and low CO₂-adapted Scenedesmus.I. Inorganic carbon-dependent O2 evolution, nitrate utilizationand nitrogen recycling.—J. exp Bot. 36: 1373–1386 Scenedesmus obtusiusculus Chod. was grown on an inorganic mediumflushed with either air or air supplemented with 3% CO₂. Inair-grown cells, O₂ evolution dependent on low, but not high,HCO^–₃ concentrations was strongly inhibited by the carbonicanhydrase inhibitor acetazolamide. Cells grown with 3% CO² exhibitedlow rates of O2 evolution at low external inorganic C; however,after 30 min in air O2 evolution rates at low inorganic C approachedthose of air-grown cells. These results are compatible withthe view that Scenedesmus develops a ‘CO² concentratingmechanism’ in air, with carbonic anhydrase as an importantconstituent When 3% CO²-grown cells were subjected to air-level of CO²,just a transient decline in NO^–₃ utilization was observed,but in the presence of acetazolamide the rate of the processdecreased drastically in response to the decrease in the CO²level. In CO²-free air NO₃^– was taken up at high ratesbut in a deregulated manner, leading to release of NH₄⁺. A portionof the NO₃^– taken up in the absence of CO² was apparentlyassimilated Cellular nitrate reductase (NR) activity initially decreasedbut subsequently recovered after a transition from 3% CO² toair. In the presence of acetazolamide, a persistent decreasein NR activity was observed. Cellular glutamine synthetase (GS)activity increased after transition from 3% CO² to air, theactivity increase being unaffected by acetazolamide. NH₄⁺ releaseto the medium in the presence of L-methionine-D, L-sulphoximine(MSO) transiently increased in 3% CO²-grown cells in responseto a transfer to air. MSO-induced NH₄⁺ release was in fact higherin air-grown cells than in 3% CO²-grown cells. Glycollate wasinitially released after transition from 3% CO² to air, butthere was no difference in glycollate release between MSO-treatedand untreated cells. In air-adapted Scenedesmus, N recyclingseems to be of minor importance in comparison to primary N assimilation Key words: CO²-fixation, N recycling, nitrate uptake, Scenedesmus     

Photosynthetic Carbon Sources of Stream Macrophytes

Rates of photosynthesis of four submerged stream macrophyteswere examined under varying pH and composition of inorganiccarbon species. Callitriche stagnatis and Sparganium simplexused only CO₂ for photosynthesis. Potamogeton crispus and P.pectinatus used HCO₃ in addition to CO₂, but with much lowerefficiency. The photosynthetic rates at air equilibrium anda total inorganic carbon concentration of 5.0 mM were 2–3times lower than maximum rates at CO2 saturation for the HCO₃users and 10–14 times lower for the CO₂ users. The CO₂compensation point of entire plants of Callitriche (2.5 µM)and Sparganium (6.0µM) was well below the equilibriumconcentration (15 µM). and the low saturation points (250–500µM) also pointed to efficient use of CO2. Callitricheand Sparganium compete successfully with HCO₃^– users inhardwater streams, which have a higher exchange and generationcapacity of CO2 than stagnant and more soft waters. Rates ofphotosynthesis of Potamogeton crispus and P. pectinatus decreasedat high pH. Depending on the two alternative hypotheses forHCO₃use, this decline can be explained by CO₃^––inhibition of HCO₃^– uptake or by increasing capacity tobuffer H+efflux from the plant. Habitats subject to high pH,e. g. small ponds with dense vegetation, may have a strong selectionfor efficient mechanisms of HCO₃ use. Key words: Photosynthesis, Macrophytes, Carbon-source     

Effect of Carbonic Anhydrase on the Activity of Ribulose Bisphosphate Carboxylase

At concentrations of CO₂ less than saturating, carbonic anhydrase(EC 4.2.1.1 [EC] ) stimulates the carboxylation of ribulose bisphosphatecatalysed by ribulose bisphosphale carboxylase (EC 4.1.1.3 [EC] .9)in vitro. This is not through any beneficial association ofthe two enzymes but is a consequence of the increased rate ofconversion of HCO₃^– ion to CO₂, the substrate for thecarboxylation. Carbonic anhydrase should always be includedin reaction mixtures used to determine the Michaelis constantof ribulose bisphosphate carboxylase for CO₂ where fixationof radioactive CO₂ into phosphoglycerate is the basis of rateestimation. The effect is to decrease the value obtained forthe Michaelis constant.     

Accumulation and Utilization of Dissolved Inorganic Carbon by a Marine Unicellular Coccolithophorid, Emiliania huxleyi

The mechanism for utilization of dissolved inorganic carbon(DIC) was investigated in the marine unicellular calcareousalga Emiliania huxleyi, grown with constant aeration. The apparentK_0.5 (DIC), the concentration of DIC which attains one-halfof the maximum velocity of apparent photosynthesis, for photosyntheticevolution of O₂, measured under saturating light, was 5.5 mM(55 µM for CO₂) at pH 8.0 and 25°C. The value of K_0.5was not affected by inhibitors of carbonic anhydrase (CA), andan electrometric assay of CA showed that the enzyme was notinvolved in photosynthesis in this alga. The rate of photosyntheticfixation of ¹⁴C-DIC into acid-stable products was about 20 timeshigher than that into CaCO₃, irrespective of the external concentrationof DIC. In short-term experiments, ¹⁴C-DIC was usually incorporatedinto the internal pool of DIC (IIC) to concentrations up to13 to 16 times higher than that of the external DIC. CO₂ addedexternally was utilized mainly for fixation of CO₂ and accumulationof IIC. By contrast, HCO^-₃ was utilized mainly for productionof CaCO₃ and accumulation of IIC. Incorporation of ¹⁴C intoIIC was partially suppressed by DCMU or in darkness but itstransfer to CaCO₃ was unaffected. These results suggest thataccumulation of IIC in this alga, even under ordinary circumstances,is only partially responsible for increasing the efficiencyof utilization of DIC by photosynthetic fixation but may bemost useful for the production of CaCO₃. (Hydroxyethylidene) bisphosphonic acid, an inhibitor of thegrowth of CaCO₃ crystals, completely suppressed production ofCaCO₃. The accumulation of IIC was also partially suppressed,but photosynthetic fixation of CO₂ was enhanced. In a pulse-chaseexperiment with ¹⁴CDIC, ¹⁴C incorporated into IIC and CaCO₃in darkness was transferred to acid-stable products of photosynthesisin the light. These results suggest that ¹⁴C-DIC in IIC andpre-formed CaCO₃ may be useful sources of carbon for fixationof CO₂. (Received July 2, 1993; Accepted January 10, 1994)     

Interactions of transmembrane carbonic anhydrase, CAIX, with bicarbonate transporters

Association of some plasma membrane bicarbonate transporters with carbonic anhydrase enzymes forms a bicarbonate transport metabolon to facilitate metabolic CO₂-HCO₃^– conversions and coupled HCO₃^– transport. The transmembrane carbonic anhydrase, CAIX, with its extracellular catalytic site, is highly expressed in parietal and other cells of gastric mucosa, suggesting a role in acid secretion. We examined in transfected HEK293 cells the functional and physical interactions between CAIX and the parietal cell Cl^–/HCO₃^– exchanger AE2 or the putative Cl^–/HCO₃^– exchanger SLC26A7. Coexpression of CAIX increased AE2 transport activity by 28 ± 7% and also activated transport mediated by AE1 and AE3 (32 ± 10 and 37 ± 9%, respectively). In contrast, despite a transport rate comparable to that of AE3, coexpressed CAIX did not alter transport associated with SLC26A7. The CAIX-associated increase of AE2 activity did not result from altered AE2 expression or cell surface processing. CAIX was coimmunoprecipitated with the coexpressed SLC4 polypeptides AE1, AE2, and AE3, but not with SLC26A7. GST pull-down assays with a series of domain-deleted forms of CAIX revealed that the catalytic domain of CAIX mediated interaction with AE2. AE2 and CAIX colocalized in human gastric mucosa, as indicated by coimmunofluorescence. This is the first example of a functional and physical interaction between a bicarbonate transporter and a transmembrane carbonic anhydrase. We conclude that CAIX can bind to some Cl^–/HCO₃^– exchangers to form a bicarbonate transport metabolon. SLC4; SLC26; bicarbonate transport metabolon     

Inorganic Carbon Transport and Fixation in Cells of Anabaena variabilis Adapted to Mixotrophic Conditions

The Cyanobacterium Anabaena variabilis ATCC 29413 grown at lowCO₂ concentration under mixotrophic conditions with fructoseshowed a repression in the ability to fix inoganic carbon. Thisrepression was not due to a diminution in the ability to transportexternal inorganic carbon but could be explained by a decreaseof two enzymatic activities involved in the assimilation ofinorganic carbon: carbonic anhydrase and Rubisco. Carbonic anhydraseactivity was close to 50% lower in mixotrophic than in autotrophiccells. Moreover growth under mixotrophic conditions reducedRubisco activity at all dissolved inorganic carbon concentrationsassayed (5–60 mM). Maximum Rubisco activity (V_max decreasedfrom µmol CO₂ mg protein^-1h^-1 in autotrophic cells to2.3 µmol CO₂ mg protein^-1h^-1 in mixotrophic cells. Nosignificant differences in K_m(C₁) between autotrophic and mixotrophiccells were however observed. The possible mechanisms involvedin the inhibition of Rubisco are discussed. (Received November 8, 1994; Accepted October 12, 1995)     

HCO-3 as an Exogenous Carbon Source for Aquatic Bryophytes Fontinalis antipyretica and Fissidens grandifrons

The aquatic bryophytes Fontinalis antipyretica Hedw. and Fissidensgrandifrons Brid. were investigated for their ability to utilizeHCO^–₃ and CO₂ as exogenous carbon sources for photosynthesis.In NaHCO₃ solutions Fontinalis increased the pH to a maximumof 9.6 corresponding to a CO₂ compensation point of 1.1 mmolm^–3 CO₂. Measured photosynthetic rates cannot be explainedonly by uptake of CO₂. Net photosynthesis decreased at highpH but did not decline to zero until pH 10.10 in Fissidens andpH 11.8–12.0 in Fontinalis. Furthermore, photosynthesiswas increased by higher HCO_–3 concentrations at constantCO₂ concentration. It is concluded that Fontinalis antipyreticahas the capability to utilize HCO₃. Key words: Carbon source, Photosynthesis, Aquatic bryophytes