Inorganic carbon acquisition in red tide dinoflagellates

Carbon acquisition was investigated in three marine bloom-forming dinollagellates-Prorocentrum minimum, Heterocapsa triquetra and Ceratium lineatum. In vivo activities of extracellular and intracellular carbonic anhydrase (CA), photosynthetic O2 evolution, CO2 and HCO3- uptake rates were measured by membrane inlet mass spectrometry (MIMS) in cells acclimated to low pH (8.0) and high pH (8.5 or 9.1). A second approach used short-term 14C-disequilibrium incubations to estimate the carbon source utilized by the cells. All three species showed negligible extracellular CA (eCA) activity in cells acclimated to low pH and only slightly higher activity when acclimated to high pH. Intracellular CA (iCA) activity was present in all three species, but it increased only in P. minimum with increasing pH. Half-saturation concentrations (K1/2) for photosynthetic O2 evolution were low compared to ribulose 1,5-bisphosphate carboxylase/oxygenase (Rubisco) kinetics. Moreover, apparent affinities for inorganic carbon (Ci) increased with increasing pH in the acclimation, indicating the operation of an efficient CO2 concentration mechanism (CCM) in these dinoflagellates. Rates of CO2 uptake were comparably low and could not support the observed rates of photosynthesis. Consequently, rates of HCO3- uptake were high in the investigated species, contributing more than 80% of the photosynthetic carbon fixation. The affinity for HCO3- and maximum uptake rates increased under higher pH. The strong preference for HCO3- was also confirmed by the 14C-disequilibrium technique. Modes of carbon acquisition were consistent with the 13C-fractionation pattern observed and indicated a strong species-specific difference in leakage. These results suggest that photosynthesis in marine dinoflagellates is not limited by Ci even at high pH, which may occur during red tides in coastal waters.     

The requirement for external carbonic anhydrase in diatoms is influenced by the supply and demand for dissolved inorganic carbon

Photosynthesis by marine diatoms contributes significantly to the global carbon cycle. Due to the low concentration of CO₂ in seawater, many diatoms use extracellular carbonic anhydrase (eCA) to enhance the supply of CO₂ to the cell surface. While much research has investigated how the requirement for eCA is influenced by changes in CO₂ availability, little is known about how eCA contributes to CO₂ supply following changes in the demand for carbon. We therefore examined how changes in photosynthetic rate influence the requirement for eCA in three centric diatoms. Modeling of cell surface carbonate chemistry indicated that diffusive CO₂ supply to the cell surface was greatly reduced in large diatoms at higher photosynthetic rates. Laboratory experiments demonstrated a trend of an increasing requirement for eCA with increasing photosynthetic rate that was most pronounced in the larger species, supporting the findings of the cellular modeling. Microelectrode measurements of cell surface pH and O₂ demonstrated that individual cells exhibited an increased contribution of eCA to photosynthesis at higher irradiances. Our data demonstrate that changes in carbon demand strongly influence the requirement for eCA in diatoms. Cell size and photosynthetic rate will therefore be key determinants of the mode of dissolved inorganic carbon uptake.     

Evidence for K+-dependent HCO3- utilization in the marine diatom Phaeodactylum tricornutum

Photosynthetic utilization of inorganic carbon in the marine diatom Phaeodactylum tricornutum was investigated by the pH drift experiment, measurement of K(1/2) values of dissolved inorganic carbon (DIC) with pH change, and comparison of the rate of photosynthesis with the rate of the theoretical CO(2) formation from uncatalyzed HCO(3)(-) conversion in the medium. The higher pH compensation point (10.3) and insensitivity of the photosynthetic rate to acetazolamide indicate that the alga has good capacity for direct HCO(3)(-) utilization. The photosynthetic rate reached 150 times the theoretical CO(2) supply rate at 100 micromol L(-1) DIC (pH 9.0) in the presence of 10 mmol L(-1) K(+) and 46 times that in the absence of K(+), indicating that for pH 9.4-grown P. tricornutum, HCO(3)(-) in the medium is taken up through K(+)-dependent and -independent HCO(3)(-) transporters. The K(1/2) (CO(2)) values at pH 8.2 were about 4 times higher than those at pH 9.0, whereas the K(1/2) (HCO(3)(-)) values at pH 8.2 were slightly lower than those at pH 9.0 whether without or with K(+), providing further evidence for the presence of the two HCO(3)(-) transport patterns in this alga. Photosynthetic rate and affinity for HCO(3)(-) in the presence of K(+), respectively, were about 2- and 7-fold higher than those in the absence of K(+), indicating that K(+)-dependent HCO(3)(-) transport is a predominant pattern of HCO(3)(-) cellular uptake in low DIC concentration. However, as P. tricornutum was cultured at pH 7.2 or 8.0, photosynthetic affinities to HCO(3)(-) were not affected by K(+), implying that K(+)-dependent HCO(3)(-) transport is induced when P. tricornutum is cultured at high alkaline pH.     

Mechanisms contributing to intracellular pH homeostasis in an immortalised human chondrocyte cell line

The maintenance of chondrocyte pH is an important parameter controlling cartilage matrix turnover rates. Previous studies have shown that, to varying degrees, chondrocytes rely on Na(+)/H(+) exchange to regulate pH. HCO(3)(-)-dependent buffering and HCO(3)(-)-dependent acid-extrusion systems seem to play relatively minor roles. This situation may reflect minimal carbonic anhydrase activity in cartilage cells. In the present study, the pH regulation of the human chondrocyte cell line, C-20/A4 has been characterised. Intracellular pH (pH(i)) was measured using the H(+)-sensitive fluoroprobe BCECF. In solutions lacking HCO(3)(-)/CO(2), pH(i) was approximately 7.5, and the recovery from intracellular acidification was predominantly mediated by a Na(+)-dependent, amiloride- and HOE 694-sensitive process. A small additional component which was sensitive to chloro-7-nitrobenz-2-oxa-1,3-diazole, an inhibitor of the V-type H(+)-ATPase, was also apparent. In solutions containing HCO(3)(-)/CO(2), pH(i) was approximately 7.2. Comparison of buffering capacity in the two conditions showed that this variable was not significantly augmented in HCO(3)(-)/CO(2)-containing media. The recovery from intracellular acidification was more rapid in the presence of HCO(3)(-)/CO(2), although under these conditions it was again largely dependent on Na(+) ions and inhibited by amiloride and HOE 694. A small component was inhibited by SITS, although this effect did not reach the level of statistical significance. These findings indicate that HCO(3)(-)-dependent processes play only a minimal role in pH regulation in C-20/A4 chondrocytes. pH regulation instead relies heavily on the Na(+)/H(+) exchanger together with a H(+)-ATPase. The absence of extrinsic (HCO(3)(-)/CO(2)) buffering is likely to reflect the low levels of carbonic anhydrase in these cells. In addition to providing fundamental information about a widely-used cell line, these findings support the contention that the unusual nature of pH regulation in chondrocytes reflects the paucity of carbonic anhydrase activity in these cells.     

An external delta-carbonic anhydrase in a free-living marine dinoflagellate may circumvent diffusion-limited carbon acquisition

The oceans globally constitute an important sink for carbon dioxide (CO(2)) due to phytoplankton photosynthesis. However, the marine environment imposes serious restraints to carbon fixation. First, the equilibrium between CO(2) and bicarbonate (HCO(3)(-)) is pH dependent, and, in normal, slightly alkaline seawater, [CO(2)] is typically low (approximately 10 mum). Second, the rate of CO(2) diffusion in seawater is slow, so, for any cells unable to take up bicarbonate efficiently, photosynthesis could become carbon limited due to depletion of CO(2) from their immediate vicinity. This may be especially problematic for those dinoflagellates using a form II Rubisco because this form is less oxygen tolerant than the usually found form I enzyme. We have identified a carbonic anhydrase (CA) from the free-living marine dinoflagellate Lingulodinium polyedrum that appears to play a role in carbon acquisition. This CA shares 60% sequence identity with delta-class CAs, isoforms so far found only in marine algae. Immunoelectron microscopy indicates that this enzyme is associated exclusively with the plasma membrane. Furthermore, this enzyme appears to be exposed to the external medium as determined by whole-cell CA assays and vectorial labeling of cell surface proteins with (125)I. The fixation of (14)CO(2) is strongly pH dependent, suggesting preferential uptake of CO(2) rather than HCO(3)(-), and photosynthetic rates decrease in the presence of 1 mm acetazolamide, a non-membrane-permeable CA inhibitor. This constitutes the first CA identified in the dinoflagellates, and, taken together, our results suggest that this enzyme may help to increase CO(2) availability at the cell surface.     

Diversity of inorganic carbon acquisition mechanisms by intact microbial mats of Microcoleus chthonoplastes (Cyanobacteriae, Oscillatoriaceae)

The dissolved inorganic carbon (DIC) acquisition mechanisms were researched in intact microbial mats dominated by the cyanobacteria Microcoleus chthonoplastes Thuret, by determining the effect on photosynthesis of different inhibitors. The microbial mats exhibited high affinity for DIC at alkaline pH, with K(m(DIC)) values similar to the ones described for pure cultures of cyanobacteria and algae in which carbon concentrating mechanisms have been researched. Besides, the photosynthesis was non-sensitive to pH changes within the range of 5.6-9.6, indicating that HCO(3)(-) was the main DIC source used for photosynthesis. The M. chthonoplastes mats featured external and internal carbonic anhydrase (CA) activity as measured in intact cells and cell extracts, respectively. Acetazolamide (AZ, which slowly enters the cell and then inhibits mainly the external CA) and ethoxyzolamide (EZ, which inhibits both external and internal CA) reduced significantly the oxygen evolution rates, demonstrating that the CA was implied in the DIC acquisition. Vanadate inhibited photosynthesis by 60% although its application, when CA being inhibited (i.e. after applying AZ + EZ), did not produce any additional effect. It could indicate that ATPase-dependent HCO(3)(-) use occurred and also that this putative mechanism was coupled with CA-like activity at the plasma membrane. The involvement of Na(+)-dependent HCO(3)(-) transporters in DIC acquisition was also inferred as monensin and 4-4'-diisothiocyanatostibilene-2,2'-disulfonate (DIDS) reduced photosynthesis by 70%. DIDS produced a strong inhibitory effect even after application of AZ + EZ + vanadate, indicating that this mechanism was not related to CA activity. The microbial mats become subject to very unfavourable conditions for Rubisco carboxylation at their natural habitats (e.g. external pH of 10.5 and O(2) concentration doubled with respect to saturation concentration); therefore, this putative diversity of DIC acquisition mechanisms could ensure their growth under these extreme conditions.     

EFFECT OF CARBONIC ANHYDRASE INHIBITORS ON THE INORGANIC CARBON UPTAKE BY PHYTOPLANKTON NATURAL ASSEMBLAGES1

The role of carbonic anhydrase (CA) in inorganic carbon acquisition (dissolved inorganic carbon, DIC) was examined in Alboran Sea phytoplankton assemblages. The study area was characterized by a relatively high variability in nutrient concentration and in abundance and taxonomic composition of phytoplankton. Therefore, the relationship between environmental variability and capacity for using HCO₃^? via external CA (eCA) was examined. Acetazolamide (AZ, an inhibitor of eCA) inhibited the primary productivity (PP) in 50% of the samples, with inhibition percentages ranging from 13% to 60%. The AZ effect was more prominent in the samples that exhibited PP >1 mg C · m^?3 · h^?1, indicating that the contribution of eCA to the DIC photosynthetic flux was irrelevant at low PP. The inhibition of primary productivity by AZ was significantly correlated to the abundance of diatoms. However, there was no a relationship between AZ effect and CO₂ partial pressure (pCO₂) or nutrient concentration, indicating that the variability in the PP percentage supported by eCA was mainly due to differences in taxonomic composition of the phytoplankton assemblages. Ethoxyzolamide (EZ, an inhibitor of both external and internal CA) affected 13 of 14 analyzed samples, with PP inhibition percentages varying from 50% to 95%. The effects of AZ and EZ were partially reversed by doubling DIC concentration. These results imply that CA activity (external and/or internal) was involved in inorganic carbon acquisition in most the samples. However, EZ effect was not correlated with pCO₂ or taxonomic composition of the phytoplankton.     

Cl- uptake mechanism in freshwater-adapted tilapia (Oreochromis mossambicus)

In this study, the correlation between Cl(-) influx in freshwater tilapia and various transporters or enzymes, the Cl(-)/HCO(3)(-) exchanger, Na(+),K(+)-ATPase, V-type H(+)-ATPase, and carbonic anhydrase were examined. The inhibitors 2x10(-4) M ouabain (a Na(+),K(+)-ATPase inhibitor), 10(-5) M NEM (a V-type H(+)-ATPase inhibitor), 10(-2) M ACTZ (acetazolamide, a carbonic anhydrase inhibitor), and 6x10(-4) M DIDS (a Cl(-)/HCO(3)(-) exchanger inhibitor) caused 40%, 60%-80%, 40%-60%, and 40%-60% reduction in Cl(-) influx of freshwater tilapia, respectively. The inhibitor 2x10(-4) M ouabain also caused 50%-65% inhibition in gill Na(+),K(+)-ATPase activity. Western blot results showed that protein levels of gill Na(+),K(+)-ATPase, V-type H(+)-ATPase, and carbonic anhydrase in tilapia acclimated in low-Cl(-) freshwater were significantly higher than those acclimated to high-Cl(-) freshwater. Based on these data, we conclude that Na(+),K(+)-ATPase, V-H(+)-ATPase, the Cl(-)/HCO(3)(-) exchanger, and carbonic anhydrase may be involved in the active Cl(-) uptake mechanism in gills of freshwater-adapted tilapia.     

Inorganic-carbon transport in some marine eukaryotic microalgae

Inorganic-carbon transport was investigated in the eukaryotic marine microalgaeStichococcus minor, Nannochloropsis oculata and aMonallantus sp. Photosynthetic O₂ evolution at constant inorganic-carbon concentration but varying pH showed thatS. minor had a greater capacity for CO₂ rather than HCO ₃ ^– utilization but forN. oculata andMonallantus HCO ₃ ^– was the preferred source of inorganic carbon. All three microalgae had a low affinity for CO₂ as shown by the measurement of inorganic-carbon-dependent photosynthetic O₂ evolution at pH 5.0. At pH 8.3, where HCO ₃ ^– is the predominant form of inorganic carbon, the concentration of inorganic carbon required for half-maximal rate of photosynthetic O₂ evolution [K _0.5 (CO₂)] was 53 M forMonallantus sp. and 125 M forN. oculata, values compatible with HCO ₃ ^– transport. Neither extra- nor intracellular carbonic anhydrase was detected in these three microalgal species. It is concluded that these microalgae lack a specific transport system for CO₂ but that HCO ₃ ^– transport occurs inN. oculata andMonallantus, and in the absence of intracellular carbonic anhydrase the conversion of HCO ₃ ^– to CO₂ may be facilitated by the internal pH of the cell.     

不同理化因子对雨生红球藻CG-11碳酸酐酶活性的影响

以雨生红球藻CG-11为实验藻株,探讨在不同CO2、HCO3-、Zn2＋浓度以及pH和氮磷比例条件下,藻细胞的碳酸酐酶活性对这些理化因子的响应。结果表明,通入空气实验组的碳酸酐酶活性最高,为（75.20±1.53）U·mg-1（Chla）,通入5%CO2条件下的碳酸酐酶活性为（9.96±1.43）U·mg-1（Chla）;高浓度HCO3-对碳酸酐酶活性亦具有明显抑制作用,培养液中可溶性无机碳的浓度与碳酸酐酶活性呈负相关;在实验设置的pH范围内,pH9.0时碳酸酐酶活性最高,为（62.32±3.25）U·mg-1（Chla）;适当的氮磷比与Zn2＋浓度显著提高了雨生红球藻CG-11的生长速率,碳酸酐酶的活性亦有明显提高。     

Mechanism of augmented duodenal HCO(3)(-) secretion after elevation of luminal CO(2)

The proximal duodenum is exposed to extreme elevations of P(CO(2)) because of the continuous mixture of secreted HCO(3)(-) with gastric acid. These elevations (up to 80 kPa) are likely to place the mucosal cells under severe acid stress. Furthermore, we hypothesized that, unlike most other cells, the principal source of CO(2) for duodenal epithelial cells is from the lumen. We hence examined the effect of elevated luminal P(CO(2)) on duodenal HCO(3)(-) secretion (DBS) in the rat. DBS was measured by the pH-stat method. For CO(2) challenge, the duodenum was superfused with a high Pco(2) solution. Intracellular pH (pH(i)) of duodenal epithelial cells was measured by ratio microfluorometry. CO(2) challenge, but not isohydric solutions, strongly increased DBS to approximately two times basal for up to 1 h. Preperfusion of the membrane-permeant carbonic anhydrase inhibitor methazolamide, or continuous exposure with indomethacin, fully inhibited CO(2)-augmented DBS. Dimethyl amiloride (0.1 mM), an inhibitor of the basolateral sodium-hydrogen exchanger 1, also inhibited CO(2)-augumented DBS, although S-3226, a specific inhibitor of apical sodium-hydrogen exchanger 3, did not. DIDS, an inhibitor of basolateral sodium-HCO(3)(-) cotransporter, also inhibited CO(2)-augemented DBS, as did the anion channel inhibitor 5-nitro-2-(3-phenylpropylamino) benzoic acid. CO(2) decreased epithelial cell pH(i), followed by an overshoot after removal of the CO(2) solution. We conclude that luminal CO(2) diffused in the duodenal epithelial cells and was converted to H(+) and HCO(3)(-) by carbonic anhydrase. H(+) initially exited the cell, followed by secretion of HCO(3)(-). Secretion was dependent on a functioning basolateral sodium/proton exchanger, a functioning basolateral HCO(3)(-) uptake mechanism, and submucosal prostaglandin generation and facilitated hydration of CO(2) into HCO(3)(-) and H(+).     

Carbonic acid production and the role of carbonic anhydrase in decarboxylation in brain

Sudden oxygenation of a thin film of rat brain homogenate, suspended between the surface of a glass pH-sensitive electrode and a gas-permeable membrane, is accompanied by a fall in pH, which is greater when carbonic anhydrase is inhibited. The result suggests that oxidative decarboxylation yields carbonic acid (HCO(3)- and H(+)), which dissociates to form molecular carbon dioxide. Brain carbonic anhydrase facilitates the formation of carbon dioxide from the decarboxylation products.     

The energy source for CO<Subscript>2</Subscript> transport in the marine microalga <Emphasis Type="Italic">Nannochloris atomus</Emphasis>

CO2 fluxes in the marine microalga Nannochloris atomus were studied by mass spectrometry using inhibitors and artificial acceptors of photosynthetic electron transport to investigate the energy source for CO2 uptake. This algal species is capable of taking up CO2 from the external medium by active transport but lacks active HCO(3)(-) transport and extracellular carbonic anhydrase. The capacity of cells to take up CO2 was a function of photosynthetic photon flux density. Dark respiration rates were also dependent upon the light intensity during the preceding illumination period, indicating the presence of light-enhanced dark respiration. Addition of 3-(3',4'-dichlorophenyl)-1,1-dimethylurea to illuminated cell suspensions that had been allowed to concentrate inorganic carbon internally during photosynthesis caused a rapid burst of CO2, demonstrating that active CO2 transport had been abolished. A similar response was obtained when cell suspensions were treated with 2,5-dibromo-6-isopropyl-3methyl-1,4-benzoqinone or hydroxylamine. When methyl viologen was used to drain electrons from ferredoxin, cells were still able to take up CO2 from the external medium, although C-fixation decreased with time. These results demonstrate that active CO2 transport in N. atomus is supported by photosynthetic linear electron transport.     

Role of hemoglobin in proton transfer to the active site of carbonic anhydrase.

The binding of bovine oxyhemoglobin to bovine carbonic anhydrase with a dissociation constant between 10(-5) and 10(-7) M has been determined by countercurrent distribution using aqueous, biphasic polymer systems. This result provides an explanation for the very efficient proton transfer between hemoglobin and carbonic anhydrase, a transfer which enhances the catalytic activity of carbonic anhydrase as measured by 18O exchange between bicarbonate and water at chemical equilibrium (Silverman, D. N., Tu, C. K., and Wynns, G. C. (1978) J. Biol. Chem, 253, 2563-2567). Two rate constants describing 18O exchange activity of carbonic anhydrase at pH 7.5 show saturation behavior when plotted against hemoglobin concentration consistent with a dissociation constant of 2.5 X 10(-6) M between bovine hemoglobin and carbonic anhydrase. Interpretation of these rate constants in terms of a two-step model for 18O exchange indicates that hemoglobin enhances the rate of exchange from carbonic anhydrase of water containing the oxygen abstracted from bicarbonate, but does not affect the catalytic interconversion of CO2 and HCO3- at chemical equilibrium.     

氮磷营养限制影响三角褐指藻光合无机碳利用和碳酸酐酶活性

以海洋硅藻三角褐指藻为实验材料, 研究了不同氮磷比培养对其光合无机碳利用和碳酸酐酶活性的影响, 结果显示三角褐指藻生长速率在N:P=16:1时最大, 高于或低于16:1时明显下降, 表明其最适生长受到氮磷的限制。氮限制(N:P=4:1或1:1)导致叶绿素a含量分别下降30.1% 和47.6%, 磷限制(N:P=64:1或256:1)下降39.1%和52.4%, 但氮或磷限制对叶绿素c含量并没有明显影响。不同营养水平培养对光饱和光合速率具有明显的影响, 与营养充足培养相比, 在严重氮磷限制(N:P=1:1或256:1)培养下光饱和光合速率分别下降39.7%和48.0%, 光合效率与暗呼吸速率也明显下降。在氮磷限制培养下藻细胞pH补偿点明显下降; K0.5CO2值在磷限制下降低30%, 表明磷限制有助于提高细胞对CO2的亲和力, 但氮限制并没有明显影响。在氮磷限制培养的细胞反应液中Fe (CN)63-浓度下降速率较慢, 表明在氮磷限制环境中生长的细胞质膜氧化还原能力明显低于营养充足条件下生长的细胞。氮磷限制也导致胞内、外碳酸酐酶活性明显下降, 其中在氮限制下胞外碳酸酐酶活性分别下降50%和37.5%, 在磷限制下下降22.3%和42.1%。严重的氮(N:P=1:1)或磷(N:P=256:1)限制导致胞内碳酸酐酶活性下降36.5%和42.9%。研究结果表明, 三角褐指藻细胞在氮磷营养限制的环境中, 可以通过调节叶绿素含量、无机碳的利用方式和碳酸酐酶的活性以维持适度的生长。       

Acid-base effects on electrolyte transport in CA II-deficient mouse colon

To determine the role of carbonic anhydrase (CA) in colonic electrolyte transport, we studied Car-2(0) mice, mutants deficient in cytosolic CA II. Ion fluxes were measured under short-circuit conditions in an Ussing chamber. CA was analyzed by assay and Western blots. In Car-2(0) mouse colonic mucosa, total CA activity was reduced 80% and cytosolic CA I and membrane-bound CA IV activities were not increased. Western blots confirmed the absence of CA II in Car-2(0) mice. Normal mouse distal colon exhibited net Na(+) and Cl(-) absorption, a serosa-positive PD, and was specifically sensitive to pH. Decrease in pH stimulated active Na(+) and Cl(-) absorption whether it was caused by increasing solution PCO(2), reducing HCO(-)(3) concentration, or reducing pH in CO(2)/HCO(-)(3)-free HEPES-Ringer solution. Membrane-permeant methazolamide, but not impermeant benzolamide, at 0.1 mM prevented the effects of pH. Car-2(0) mice exhibited similar basal transport rates and responses to pH and CA inhibitors. We conclude that basal and pH-stimulated colonic electrolyte absorption in mice requires CA I. CA II and IV may have accessory roles.     

干出和沉水不同条件下羊栖菜光合作用碳源获得机制比较(英文)

经济海洋褐藻羊栖菜(Hizikia fusiforme(Harv.)Okamura)低潮时常常周期性地暴露于空气中。为了认识这种海藻在潮汐循环背景下的光合特征,对其在高潮沉水和低潮干出不同条件下的光合作用碳素获得机制进行了比较。沉水时,羊栖菜主要利用海水中HCO_3~-作为外源无机碳源驱动光合作用;而在干出条件下,其光合作用的主要碳源为空气中的CO_2。在这两种不同环境条件下,光合作用与pH值的关系不同:沉水状态时,羊栖菜在高pH值(10.0)下光合活性很弱;而在干出条件下,羊栖菜在高pH值时仍有较高的光合活性。然而,光合作用无论是在沉水还是在干出条件下,对外源碳源的获得都表现出对胞外碳酸酐酶(CA)强烈的依赖性,并且其光合速率都受周围环境中无机碳源水平的限制。此外,在沉水和干出两种环境条件下,羊栖菜光合作用都表现出对氧气的敏感性。这表明,在羊栖菜中,依赖胞外CA的碳源获得机制不能使细胞内CO_2浓度提高到阻碍其光呼吸的程度。增加空气中或海水中无机碳的浓度,能促进羊栖菜的光合作用,进而增加这种海藻的水产养殖产量。     

The effects of exogenous extracellular carbonic anhydrase on CO2 excretion in rainbow trout (Oncorhynchus mykiss): role of plasma buffering capacity

The buffering capacity (beta) of rainbow trout (Oncorhynchus mykiss) plasma was manipulated prior to intravascular injection of bovine carbonic anhydrase to test the idea that proton (H+) availability limits the catalysed dehydration of HCO3- within the extracellular compartment. An extracorporeal blood shunt was employed to continuously monitor blood gases in vivo in fish exhibiting normal plasma beta (-3.9+/-0.3 mmol 1(-1) pH unit(-1)), and in fish with experimentally (using N-[2-hydroxyethyl]piperazine-N'-[2-ethanesulfonic acid]) elevated plasma beta (-12.1+/-1.1 mmol 1(-1) pH unit(-1)). An injection of 5 mg kg(-1) carbonic anhydrase equally reduced (after 90 min) the arterial partial pressure of CO2 in trout with regular (-0.23+/-0.05 Torr) or high (-0.20+/-0.05 Torr) plasma beta; saline injection was without effect. Because ventilation and venous blood gases were unaffected by carbonic anhydrase, the effect of extracellular carbonic anhydrase in lowering arterial partial pressure of CO2 was likely caused solely by a specific enhancement of CO2 excretion owing to acceleration of HCO3- dehydration within the plasma. The lowering of arterial partial pressure of CO2 in trout after injection of exogenous carbonic anhydrase provides the first in vivo evidence that the accessibility of plasma HCO3- to red blood cell carbonic anhydrase constrains CO2 excretion under resting conditions. Because the velocity of red blood cell Cl-/HCO3- exchange governs HCO3- accessibility to red blood cell carbonic anhydrase, the present study also provides evidence that CO2 excretion at rest is limited by the relatively slow rate of Cl-/HCO3- exchange. The effect of carbonic anhydrase in lowering arterial partial pressure of CO2 was unrelated to plasma buffering capacity. While these data could suggest that H+ availability does not limit extracellular HCO3- dehydration in vivo at resting rates of CO2 excretion, it is more likely that the degree to which plasma beta was elevated in the present study was insufficient to drive a substantially increased component of HCO3- dehydration through the plasma.     

Dual role of CO2/HCO3(-) buffer in the regulation of intracellular pH of three-dimensional tumor growths

Intracellular pH (pH(i)), a major modulator of cell function, is regulated by acid/base transport across membranes. Excess intracellular H(+) ions (e.g. produced by respiration) are extruded by transporters such as Na(+)/H(+) exchange, or neutralized by HCO(3)(-) taken up by carriers such as Na(+)-HCO(3)(-) cotransport. Using fluorescence pH(i) imaging, we show that cancer-derived cell lines (colorectal HCT116 and HT29, breast MDA-MB-468, pancreatic MiaPaca2, and cervical HeLa) extrude acid by H(+) efflux and HCO(3)(-) influx, largely sensitive to dimethylamiloride and 4,4'-diisothiocyanatostilbene-2,2'-disulfonate (DIDS), respectively. The magnitude of HCO(3)(-) influx was comparable among the cell lines and may represent a constitutive element of tumor pH(i) regulation. In contrast, H(+) efflux varied considerably (MDA-MB-468 > HCT116 > HT29 > MiaPaca2 > HeLa). When HCO(3)(-) flux was pharmacologically inhibited, acid extrusion in multicellular HT29 and HCT116 spheroids (～10,000 cells) was highly non-uniform and produced low pH(i) at the core. With depth, acid extrusion became relatively more DIDS-sensitive because the low extracellular pH at the spheroid core inhibits H(+) flux more than HCO(3)(-) flux. HCO(3)(-) flux inhibition also decelerated HCT116 spheroid growth. In the absence of CO(2)/HCO(3)(-), acid extrusion by H(+) flux in HCT116 and MDA-MB-468 spheroids became highly non-uniform and inadequate at the core. This is because H(+) transporters require extracellular mobile pH buffers, such as CO(2)/HCO(3)(-), to overcome low H(+) ion mobility and chaperone H(+) ions away from cells. CO(2)/HCO(3)(-) exerts a dual effect: as substrate for membrane-bound HCO(3)(-) transporters and as a mobile buffer for facilitating extracellular diffusion of H(+) ions extruded from cells. These processes can be augmented by carbonic anhydrase activity. We conclude that CO(2)/HCO(3)(-) is important for maintaining uniformly alkaline pH(i) in small, non-vascularized tumor growths and may be important for cancer disease progression.     

Mitochondrial-driven bicarbonate transport supports photosynthesis in a marine microalga

The CO(2)-concentrating mechanism (CCM) of the marine eustigmatophycean microalga Nannochloropsis gaditana consists of an active HCO(3)(-) transport system and an internal carbonic anhydrase to facilitate accumulation and conversion of HCO(3)(-) to CO(2) for photosynthetic fixation. Aqueous inlet mass spectrometry revealed that a portion of the CO(2) generated within the cells leaked to the medium, resulting in a significant rise in the extracellular CO(2) concentration to a level above its chemical equilibrium that was diagnostic for active HCO(3)(-) transport. The transient rise in extracellular CO(2) occurred in the light and the dark and was resolved from concurrent respiratory CO(2) efflux using H(13)CO(3)(-) stable isotope techniques. H(13)CO(3)(-) pump-(13)CO(2) leak activity of the CCM was unaffected by 10 microM 3(3,4-dichlorophenyl)-1,1-dimethylurea, an inhibitor of chloroplast linear electron transport, although photosynthetic O(2) evolution was reduced by 90%. However, low concentrations of cyanide, azide, and rotenone along with anoxia significantly reduced or abolished (13)CO(2) efflux in the dark and light. These results indicate that H(13)CO(3)(-) transport was supported by mitochondrial energy production in contrast to other algae and cyanobacteria in which it is supported by photosynthetic electron transport. This is the first report of a direct role for mitochondria in the energization and functioning of the CCM in a photosynthetic organism.