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 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     

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)     

Active Uptake of CO2 by the Diatom Navicula pelliculosa

Mass spectrometry has been used to investigate the transportof CO₂ in the freshwater diatom Navicula pelliculosa. The timecourseof CO₂ formation in the dark after addition of 100 mmol m^–3dissolved inorganic carbon (DIC) to cell suspensions showedthat no external carbonic anhydrase (CA) was present in thesecells. Upon illumination, cells pre-incubated at pH 75 with100 mmol m^–3 DIC, removed almost all free CO₂ from themedium at an initial rate of 285 µmol CO₂ mg^–1Chl h^–1. Equilibrium between HCO₃^– and CO₂ in themedium occurred rapidly upon addition of bovine CA, showingthat CO₂ depletion resulted from a selective uptake of CO₂ ratherthan an uptake of all inorganic carbon species. However, photosyntheticO₂ evolution rate remained constant after CO₂ had been depletedfrom the medium indicating that photosynthesis is sustainedprimarily by active HCO₃^– uptake. Treatment of cells with2-iodoacetamide (83 mol m^–3) completely inhibited CO₂fixation but had little effect on CO₂ transport since initialrates of CO₂ depletion were about 81% that of untreated cells.Transfer of iodoacetamide-treated cells to the dark caused arapid increase in the CO₂ concentration in the medium largelydue to the efflux of the unfixed intracellular DIC pool whichwas found to be about 194 times the concentration of that inthe external medium. These results indicate that Navicula pelliculosaactively takes up molecular CO₂ against a concentration gradientby a process distinct from HCO₃^– transport. Key words: Dissolved inorganic carbon, carbonic anhydrase, bicarbonate transport, CO₂ transport, mass spectrometry     

Transport and Fixation of Inorganic Carbon during Photosynthesis of Anabaena Grown under Ordinary Air. I. Active Species of Inorganic Carbon Utilized for Photosynthesis

Inorganic carbon transport during photosynthesis of cyanobacteriumAnabaena variabilis grown under ordinary air was investigatedby supplying ¹⁴CO₂ or H¹⁴CO₃^– solution to three differentstrains. Both CO₂ and HCO₃^– were accumulated within thealgal cells. In the cell suspension from which dissolved inorganiccarbon had been depleted by pre-illumination, CO₂ was transportedand accumulated faster than HCO₃^–. When the concentrationof HCO₃^– injected into the cell suspension of A. variabilisM3 was 25 times as high as that of CO2 (the expected ratio atequilibrium at pH 7.8), the initial rates of fixation of bothinorganic carbon species were practically the same. On the otherhand, when ¹⁴CO₂ or H¹⁴CO₃^– was added under steady statephotosynthetic conditions, both carbon species were transportedat similar rates. The ratio of fixed to transported carbon measuredafter the initial 5 s was only 23–27% regardless of thecarbon species supplied. This percentage is much lower thanthat reported for Chlorella cells. ¹ To whom reprint requests should be addressed (Received June 30, 1986; Accepted December 16, 1986)     

Nongenomic regulation by aldosterone of the epithelial NHE3 Na(+)/H(+) exchanger

The relevance of nongenomic pathways to regulation of epithelial function by aldosterone is poorly understood. Recently, we demonstrated that aldosterone inhibits transepithelial HCO₃^– absorption in the renal medullary thick ascending limb (MTAL) through a nongenomic pathway. Here, we examined the transport mechanism(s) responsible for this regulation, focusing on Na⁺/H⁺ exchangers (NHE). In the MTAL, apical NHE3 mediates H⁺ secretion necessary for HCO₃^– absorption; basolateral NHE1 influences HCO₃^– absorption by regulating apical NHE3 activity. In microperfused rat MTALs, the addition of 1 nM aldosterone rapidly decreased HCO₃^– absorption by 30%. This inhibition was unaffected by three maneuvers that inhibit basolateral Na⁺/H⁺ exchange and was preserved in MTALs from NHE1 knockout mice, ruling out the involvement of NHE1. In contrast, exposure to aldosterone for 15 min caused a 30% decrease in apical Na⁺/H⁺ exchange activity over the intracellular pH range from 6.5 to 7.7, due to a decrease in V_max. Inhibition of HCO₃^– absorption by aldosterone was not affected by 0.1 mM lumen Zn²⁺ or 1 mM lumen DIDS, arguing against the involvement of an apical H⁺ conductance or apical K⁺-HCO₃^– cotransport. These results demonstrate that aldosterone inhibits HCO₃^– absorption in the MTAL through inhibition of apical NHE3, and identify NHE3 as a target for nongenomic regulation by aldosterone. Aldosterone may influence a broad range of epithelial transport functions important for extracellular fluid volume and acid-base homeostasis through direct regulation of this exchanger. thick ascending limb; acid-base transport; epithelial Na⁺ transport; kidney     

Characterization of Photosynthetic 14Carbon Assimilation by Potamogeton lucens L.

Photosynthetic assimilation of exogenous ¹⁴CO₂ and H¹⁴CO₃^–by the aquatic angiosperm Potamogeton lucens L. is reported.Equivalent maximum rates of assimilation (1.5 µmol s^–1m^–2) were obtained in the presence of saturating levelsof ¹⁴CO₂ (1.0 mol m^–3, pH 5.3) or H¹⁴CO₃^– (1.5 molm^–3, pH, 9.2). Under subsaturating ¹⁴CO₂ levels, bothgaseous diffusion and H¹⁴CO₃^– transport were shown tooperate simultaneously, such that maximal photosynthetic rateswere established. An induction lag of approximately 3 min was observed when exogenous¹⁴CO₂ was assimilated. A longer lag of approximately 12 minwas required, however, before linear assimilation rates wereestablished when H¹⁴CO₃ acted as the carbon source. The light-activatedH¹⁴CO₃^– transport system was found to be quite labile.A brief (5 min) dark treatment returned the system to the inactivestate. Bicarbonate transport was shown to be competitively inhibitedby CO₃^2–ions. The possibility is discussed that this formof inhibition may be common to many HCO₃^– assimilators. Preliminary polar cation transport studies (from lower to upperleaf surface) indicated an almost exact one to one relationshipbetween the rates of Na⁺ influx and efflux and H¹⁴CO₃^–assimilation. The possible relationship(s) between these transportprocesses and the requirement for electrical neutrality is brieflydiscussed.     

The Mechanism of Photosynthetic Use of Bicarbonate by Hydrodictyon africanum

Hydrodictyon africanum can photosynthesize at high pH underconditions in which HCO₃^– rather than CO₂ is the carbonspecies entering the cell. A passive entry of HCO₃^– seemsunlikely; a metabolic HCO₃^– pump is proposed. It is possiblethat such a pump is related to a light-dependent reaction specificto the use of HCO₃^–. This reaction is dependent on photosystem2, but appears to be independent of ATP. These characteristicsare similar to those of active lightdependent Cl influx in H.africanum, and suggest a similar energy source for the two pumps.The HCO₃^– pump may be electrogenic.     

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.     

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     

Photosynthetic Fixation of 14Carbon by Internodal Cells of Chara corallina

Maximum fixation rates of 120 and 60 pmol cm^–2 s ^–1wereobtained when exogenous carbon was supplied as ¹CO₂ and H¹⁴CO₃^–respectively. These values are considerably higher than thosepreviously reported for this species. A kinetic analysis wasperformed on this data. Substrate saturation in the concentrationrange 1.0–1.5 mM was observed for both CO₂ and HCO₃^– In the presence of exogenous CO², a linear relationship wasobserved between light intensity and fixation while the HCO₃^–relationship was slightly sigmoidal. Fixation saturated at intensitiesof 15–20 W m^–2 and 13–15 W m^–2 for exogenous¹⁴CO² and H¹⁴CO₃^–respectively. The presence, in this species, of an extremely active HCO₃^–transport system, situated in the plasmalemma, demonstratesthat when alkaline solutions are employed the involvement ofthis ion cannot be ignored during electrical studies on thismembrane. The maximum H¹⁴CO₃^– influxes obtained duringthis study are the largest ionic fluxes measured for any Characeanspecies. It was demonstrated that CO² for fixation can be supplied simultaneouslyby gaseous diffusion and HCO₃^– transport (cf. Raven, 1968).Inhibition of H¹⁴CO₃^– influx was observed in the presenceof Tris, Tricine, and borate buffers, and CO₃^{2 –} alsoappeared to act as a strong inhibitor. The possible mechanism(s)by which this inhibition occurs is discussed.     

Effects of Ammonia and Methylamine on Cl- Transport and on the pH Changes and Circulating Electric Currents Associated with HCO3- Assimilation in Chara corallina

Low concentrations of ammonia and methylamine greatly increaseCl^– influx into Chara corallina. Both amines have theirmaximum effect at pH 6.5–7.5. The amine stimulation ofCl^– influx is small below about pH 5.5. Above pH 8.5 theremay be inhibition of influx by amines. Concentrations of 10–25µM ammonia are sufficient to cause the maximum stimulationof Cl^– influx; the corresponding methylamine concentrationsare 0.1–0.2 mM. It is concluded that entry of amine cations(NH₄^$ and CH₃NH₃^$), rather than unionized bases (NH₃ and CH₃NH₂),causes Cl^– transport to be increased. Increases in rates of Cl^– transport are not necessarilyaccompanied by effects on HCO₃^$ assimilation and OH^– efflux.Measurements of localized pH differences at the cell surfaceand of circulating electric currents in the bathing solutionshow that these phenomena are only significantly affected byammonia at or above 50 µM and by methylamine at or above1.0 mM. The significance of the effects of amines is assessedin relation to current ideas about transport of Cl^–, HCO₃^–,and OH^–.     

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)     

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     

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)     

The Effect of External pH on the Apparent CO2 Affinity of Chlorella saccharophila

The carbon dioxide compensation point of the unicellular greenalga, Chloretla saccharophila, was determined in aqueous mediumby a gas chromatographic method. Compensation points decreasedmarkedly from 63 cm³ m^–3 at an external pH of 4.0 to 3.2cm³ m^–3 at pH 8.0 and were not affected by the O₂ concentrationof the medium. The calculated CO² concentration required tosupport the half-maximum photosynthetic rate of the algal cellsranged from 6.0 mmol m_–3 at an external pH of 60 to 1.5mmol m^–3 at pH 8.0 and these values were not affectedby O₂ concentration. The K_m(CO₂) of nbulose-l,5-bisphosphatecarboxylase isolated from cells grown either at pH 4.0 or pH8.0 was determined to be 64 mmol m^–3. These results indicatethat loss of CO₂ by photorespiration does not occur in C. saccharophilacells at acid pH and the disparity between the apparent affinityfor CO₂ of the intact cells and that of the carboxylase indicatesthe operation of a ‘CO₂ concentrating mechanism’in this alga at acid pH. Key words: Acidophilic alga, bicarbonate transport, Chlorella saccharophila, compensation point, CO₂ affinity, PH, RuBP carboxylase     

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)     

Interaction of Respiration, Ion Regulation, and Acid-Base Balance in the Everyday Life of Aquatic Crustaceans

Extracellular and intracellular acid-base balance is necessaryfor the maintenance of normal metabolic processes. The primarysource of acid is metabolically produced CO₂, and the CO₂/HCO₃^–system is the most significant buffer. The regulation of acid-basebalance is complex, involving the interaction between respiratorygas exchange and ion transport. In aquatic crustaceans respirationis governed by the need to extract oxygen from water, an O₂-poormedium; thus, acid-base balance is maintained primarily throughion transport mechanisms. These mechanisms include Na⁺/H⁺ andCl^–/HCO₃^– exchange processes that are sensitiveto the extracellular acid-base status of the animal. In marinecrabs, ion regulation and acid-base balance are accomplishedby the posterior gills, while in freshwater species all gillsand the antennal gland perform these functions. Intracellularacid-base balance appears to be maintained primarily by iontransport across the cell membrane. Hemolymph pH varies inverselywith acclimation temperature and salinity. In both cases Pco₂remains nearly constant, and the pH change is a result of changesin hemolymph HCO₃^– concentrations brought about by ionexchange mechanisms. Environmental hypercapnia or hyperoxiainduces a repiratory acidosis characterized by increased Pco₂,low pH, and elevated HCO₃^–; this is partially compensatedfor by ion exchange processes that bring about a further increasein hemolymph HCO₃^–. Exercise causes a mixed respiratoryand metabolic acidosis with compensation via H⁺ ion excretionand hyperventilation.     

Three distinct mechanisms of HCO3- secretion in rat distal colon

HCO₃^– secretion has long been recognized in the mammalian colon, but it has not been well characterized. Although most studies of colonic HCO₃^– secretion have revealed evidence of lumen Cl^– dependence, suggesting a role for apical membrane Cl^–/HCO₃^– exchange, direct examination of HCO₃^– secretion in isolated crypt from rat distal colon did not identify Cl^–-dependent HCO₃^– secretion but did reveal cAMP-induced, Cl^–-independent HCO₃^– secretion. Studies were therefore initiated to determine the characteristics of HCO₃^– secretion in isolated colonic mucosa to identify HCO₃^– secretion in both surface and crypt cells. HCO₃^– secretion was measured in rat distal colonic mucosa stripped of muscular and serosal layers by using a pH stat technique. Basal HCO₃^– secretion (5.6 ± 0.03 µeq·h^–1·cm^–2) was abolished by removal of either lumen Cl^– or bath HCO₃^–; this Cl^–-dependent HCO₃^– secretion was also inhibited by 100 µM DIDS (0.5 ± 0.03 µeq·h^–1·cm^–2) but not by 5-nitro-3-(3-phenylpropyl-amino)benzoic acid (NPPB), a Cl^– channel blocker. 8-Bromo-cAMP induced Cl^–-independent HCO₃^– secretion (and also inhibited Cl^–-dependent HCO₃^– secretion), which was inhibited by NPPB and by glibenclamide, a CFTR blocker, but not by DIDS. Isobutyrate, a poorly metabolized short-chain fatty acid (SCFA), also induced a Cl^–-independent, DIDS-insensitive, saturable HCO₃^– secretion that was not inhibited by NPPB. Three distinct HCO₃^– secretory mechanisms were identified: 1) Cl^–-dependent secretion associated with apical membrane Cl^–/HCO₃^– exchange, 2) cAMP-induced secretion that was a result of an apical membrane anion channel, and 3) SCFA-dependent secretion associated with an apical membrane SCFA/HCO₃^– exchange. chloride/bicarbonate exchange; short-chain fatty acid/bicarbonate exchange; anion channel; pH stat     

Regulation of the human NBC3 Na+/HCO3- cotransporter by carbonic anhydrase II and PKA

Human NBC3 is an electroneutral Na⁺/HCO₃^– cotransporter expressed in heart, skeletal muscle, and kidney in which it plays an important role in HCO₃^– metabolism. Cytosolic enzyme carbonic anhydrase II (CAII) catalyzes the reaction CO₂ + H₂O HCO₃^– + H⁺ in many tissues. We investigated whether NBC3, like some Cl^–/HCO₃^– exchange proteins, could bind CAII and whether PKA could regulate NBC3 activity through modulation of CAII binding. CAII bound the COOH-terminal domain of NBC3 (NBC3Ct) with K_d = 101 nM; the interaction was stronger at acid pH. Cotransfection of HEK-293 cells with NBC3 and CAII recruited CAII to the plasma membrane. Mutagenesis of consensus CAII binding sites revealed that the D1135-D1136 region of NBC3 is essential for CAII/NBC3 interaction and for optimal function, because the NBC3 D1135N/D1136N retained only 29 ± 22% of wild-type activity. Coexpression of the functionally dominant-negative CAII mutant V143Y with NBC3 or addition of 100 µM 8-bromoadenosine to NBC3 transfected cells reduced intracellular pH (pH_i) recovery rate by 31 ± 3, or 38 ± 7%, respectively, relative to untreated NBC3 transfected cells. The effects were additive, together decreasing the pH_i recovery rate by 69 ± 12%, suggesting that PKA reduces transport activity by a mechanism independently of CAII. Measurements of PKA-dependent phosphorylation by mass spectroscopy and labeling with [-³²P]ATP showed that NBC3Ct was not a PKA substrate. These results demonstrate that NBC3 and CAII interact to maximize the HCO₃^– transport rate. Although PKA decreased NBC3 transport activity, it did so independently of the NBC3/CAII interaction and did not involve phosphorylation of NBC3Ct. pH regulation; bicarbonate transport; metabolon