Carbon concentration mechanisms in photosynthetic microorganisms

Unicellular green algae and cyanobacteria have mechanism to actively concentrate dissolved inorganic carbon into the cells, only if they are grown with air levels of CO2. The carbon concentration mechanisms are commonly known as "CCM" or "DIC-pumps". The DIC-pumps are environmental adaptation that function to actively transport and accumulate inorganic carbon (HCO3- and CO2; Ci) within the cell and then uses this Ci pool to actively increase the concentration of CO2 at the site of ribulose bisphosphate carboxylase-oxygenase (Rubisco), the primary CO2-fixing enzyme. The current working model for dissolved inorganic carbon concentration mechanism in unicellular green algae includes several isoforms of carbonic anhydrase (CA), and ATPase driven active transporters at the plasmalemma and at the inner chloroplast envelopes. In the past fifteen years, significant progress has been made in isolating and characterizing the various isoforms of carbonic anhydrase at the biochemical and molecular level. However, we have an inadequate understanding of active transporters that are located on the plasmalemma and at the chloroplast envelopes. In this mini-review we focus on certain aspects of the induction, function and significance of the dissolved inorganic carbon concentration mechanisms in aquatic photosynthetic microorganisms.     

Physiological and molecular aspects of the inorganic carbon-concentrating mechanism in cyanobacteria

This paper reviews progress made in elucidating the inorganic carbon concentrating mechanism in cyanobacteria at the physiological and molecular levels. Emphasis is placed on the mechanism of inorganic carbon transport, physiological and genetical analysis of high-CO₂-requiring mutants, the polypeptides induced during adaptation to low CO₂, the functional significance of carboxysomes, and the role of carbonic anhydrase. We also make occasional reference to the green algal inorganic carbon-concentrating mechanism.     

The Role of External Carbonic Anhydrase in Inorganic Carbon Acquisition by Chlamydomonas reinhardii at Alkaline pH

The role of external carbonic anhydrase in inorganic carbon acquisition and photosynthesis by Chlamydomonas reinhardii at alkaline pH (8.0) was studied. Acetazolamide (50 micromolar) completely inhibited external carbonic anhydrase (CA) activity as determined from isotopic disequilibrium experiments. Under these conditions, photosynthetic rates at low dissolved inorganic carbon (DIC) were far greater than could be maintained by CO₂ supplied from the spontaneous dehydration of HCO₃⁻ thereby showing that C. reinhardii has the ability to utilize exogenous HCO₃⁻. Acetazolamide increased the concentration of DIC required to half-saturate photosynthesis from 38 to 80 micromolar, while it did not affect the maximum photosynthetic rate. External CA activity was also removed from the cell-wall-less mutant (CW-15) by washing. This had no effect on the photosynthetic kinetics of the algae while the addition of acetazolamide to washed cells (CW-15) increased the K_½^DIC from 38 to 80 micromolar. Acetazolamide also caused a buildup of the inorganic carbon pool upon NaHCO₃ addition, indicating that this compound partially inhibited internal CA activity. The effects of acetazolamide on the photosynthetic kinetics of C. reinhardii are likely due to the inhibition of internal rather than a consequence of the inhibition of external CA. Further analysis of the isotopic disequilibrium experiments at saturating concentration of DIC provided evidence consistent with active CO₂ transport by C. reinhardii. The observation that C. reinhardii has the ability to take up both CO₂ and bicarbonate throws into question the role of external CA in the accumulation of DIC in this alga.     

TRANSPORT OF INORGANIC CARBON AND THE ‘CO2 CONCENTRATING MECHANISM’ IN CHLORELLA EMERSONII (CHLOROPHYCEAE)1

Chlorella emersonii Shihira et Krauss var. emersonii exhibits ‘C₄-like’ gas exchange characteristics when grown at air levels of CO₂, but is ‘C₃-like’ when grown with extra CO₂. The total inorganic carbon concentration, and the free CO₂ concentration, averaged over the cell interior are higher in air-adapted cells than can be accounted for by passive CO₂ equilibration from the medium and the mean intracellular pH value. The ‘extra’ inorganic C in the air-grown cells probably cannot all be accounted for in terms of binding to proteins and requires an active transport process to account for it. The electrical potential of the cell interior becomes more negative when the ‘CO₂ concentrating mechanism’ is operative; this is most readily explained if the active step in inorganic C accumulation is primary active uniport of HCO₃^?. Since the ‘CO₂ concentrating mechanism’ can operate when CO₂ is the species crossing the outer permeation barrier, it is suggested that the site of active HCO₃^? transport in Chlorella (and other eukaryotes) is the chloroplast envelope, and the plasmalemma in cyanobacteria. This scheme explains the obligatory role of the de-repressed carbonic anhydrase in C₄-like photosynthesis in algae, but some other data support an explanation of C₄-like photosynthesis in terms of special properties of carbonic anhydrase as a carbon donor to RuBP carboxylase-oxygenase.     

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.     

The case for chloroplast thylakoid carbonic anhydrase

Washed thylakoid membranes and photosystem II-enriched membrane fragments from cyanobacteria, green algae, and chloroplasts from both C₃ and C₄ plants possess the ability to reversibly hydrate CO₂. That is, the membranes have an intrinsic carbonic anhydrase activity. The present review outlines the discovery of thylakoid carbonic anhydrase and presents the evidence that it is a unique isozyme, distinct from other cellular carbonic anhydrases. It appears that at least some thylakoid carbonic anhydrase is closely associated with photosystem II and may be required for electron transport. This would explain why all inhibitors of carbonic anhydrase also inhibit photosystem II. Several speculative functions of thylakoid carbonic anhydrase are discussed. These include a possible role in carbon metabolism, in the protonation of plastoquinone, and/or in oxygen evolution.     

Oxygen inhibition of dissolved inorganic carbon uptake in unicellular green algae

Unicellular green algae have a dissolved inorganic carbon (DIC) concentrating mechanism, commonly known as the DIC pump, to concentrate inorganic carbon into cells and chloroplasts. The DIC pump activity is normally measured as the K_0.5(DIC) that equals the CO₂ plus HCO₃‐ concentration at a cited pH at which the rate of DIC‐dependent photosynthetic O₂ evolution is half‐maximal, or by the amount of intra‐cellular DIC accumulation in 15–60 s, using a limited amount of NaH¹⁴CO₃, measured by the silicone oil cen‐trifugation technique. The dissolved oxygen in the assay inhibits or reduces the DIC uptake by the cells of unicellular green algae Chlamydomonas reinhardtii Dangeard, strain 137 and in a cell wall‐less marine algae Dunaliella tertiolecta Butcher. The algal cells concentrated the highest amount of DIC when little or no oxygen was present in the assay medium. The results suggest that the amount of O₂ and DIC must be carefully monitored before DIC‐pump assay.     

Historical perspective on microalgal and cyanobacterial acclimation to low- and extremely high-CO2 conditions

Reports in the 1970s from several laboratories revealed that the affinity of photosynthetic machinery for dissolved inorganic carbon (DIC) was greatly increased when unicellular green microalgae were transferred from high to low-CO₂ conditions. This increase was due to the induction of carbonic anhydrase (CA) and the active transport of CO₂ and/or HCO₃ ⁻ which increased the internal DIC concentration. The feature is referred to as the `CO₂-concentrating mechanism (CCM)'. It was revealed that CA facilitates the supply of DIC from outside to inside the algal cells. It was also found that the active species of DIC absorbed by the algal cells and chloroplasts were CO₂ and/or HCO₃ ⁻, depending on the species. In the 1990s, gene technology started to throw light on the molecular aspects of CCM and identified the genes involved. The identification of the active HCO₃ ⁻ transporter, of the molecules functioning for the energization of cyanobacteria and of CAs with different cellular localizations in eukaryotes are examples of such successes. The first X-ray structural analysis of CA in a photosynthetic organism was carried out with a red alga. The results showed that the red alga possessed a homodimeric β-type of CA composed of two internally repeating structures. An increase in the CO₂ concentration to several percent results in the loss of CCM and any further increase is often disadvantageous to cellular growth. It has recently been found that some microalgae and cyanobacteria can grow rapidly even under CO₂ concentrations higher than 40%. Studies on the mechanism underlying the resistance to extremely high CO₂ concentrations have indicated that only algae that can adopt the state transition in favor of PS I could adapt to and survive under such conditions. It was concluded that extra ATP produced by enhanced PS I cyclic electron flow is used as an energy source of H⁺-transport in extremely high-CO₂ conditions. This same state transition has also been observed when high-CO₂ cells were transferred to low CO₂ conditions, indicating that ATP produced by cyclic electron transfer was necessary to accumulate DIC in low-CO₂ conditions. This revised version was published online in August 2006 with corrections to the Cover Date.     

The CO2concentrating mechanism in cyanobactiria and microalgae

Over the past 10 years it has become clear that cyanobacteria and microalgae possess mechanisms for actively acquiring inorganic carbon from the external medium and are able to use this to elevate the CO₂ concentration around the active site of the primary photosynthetic carboxylating enzyme, ribulose bisphosphate carboxylase-oxygenase (Rubisco). This results in a vastly enhanced photosynthetic affinity for inorganic carbon (C_i) and improved photosynthetic efficiency. The CO₂ concentrating mechanism is dependent on the existence of membrane bound C_i transport systems, and a microenvironment within the cell where the accumulated C_i can be used to elevate CO₂ at the site of Rubisco. Evidence presented in this review suggests that in cyanobacteria this is achieved by the packaging of Rubisco and carbonic anhydrase (CA) into discrete structures, which are termed carboxysomes. Analogous structures in microalgae, termed pyrenoids, may perform a similar function. The recovery and analysis of high-CO₂-requiring mutants has greatly advanced our understanding of the mechanisms and genes underlying these systems, especially in cyanobacteria, and this review places particular emphasis on the contribution made by molecular genetic approaches.     

Active uptake of inorganic carbon by Chlorella saccharophila is not repressed by growth in high CO2

Regulation of transport of dissolved inorganic carbon (DIC)in response to CO₂ concentration in the external medium hasbeen compared in two closely-related green algae, Chlorellaellipsoidea and Chlorella saccharophila. C. ellipsoidea, whengrown in high CO₂, had reduced activities of both CO₂ and transport and DIC transport activitieswere increased after the cells had acclimated to air. However,high CO₂-grown C. saccharophila had a comparable level of photosyntheticaffinity for DIC to that of air-grown C. ellipsoidea and thiswas accompanied by a capacity to accumulate high internal concentrationsof DIC. The high photosynthetic affinity and the high intracellularDIC accumulation did not change in cells grown in air exceptthat the occurrence of external carbonic anhydrase (CA) in air-grownC. saccharophila stimulated the intracellular DIC accumulationin the absence of added CA. These data indicate that activeDIC transport is constitutively expressed in C. saccharophila,presumably because this alga is insensitive to the repressiveeffect of high CO₂ on DIC transport. This strongly supportsthe existence of a direct sensing mechanism for external CO₂in Chlorella species, but also indicates that external CA isregulated independently of DIC transport in Chlorella species. Key words: Carbonic anhydrase, Chlorella, CO₂-insensitive, DIC transport, wild type     

Carbonic anhydrases in plants and algae

Carbonic anhydrases catalyse the reversible hydration of CO₂, increasing the interconversion between CO₂ and HCO₃⁻ + H⁺ in living organisms. The three evolutionarily unrelated families of carbonic anhydrases are designated α-, β-and γ-CA. Animals have only the α-carbonic anhydrase type of carbonic anhydrase, but they contain multiple isoforms of this carbonic anhydrase. In contrast, higher plants, algae and cyanobacteria may contain members of all three CA families. Analysis of the Arabidopsis database reveals at least 14 genes potentially encoding carbonic anhydrases. The database also contains expressed sequence tags (ESTs) with homology to most of these genes. Clearly the number of carbonic anhydrases in plants is much greater than previously thought. Chlamydomonas, a unicellular green alga, is not far behind with five carbonic anhydrases already identified and another in the EST database. In algae, carbonic anhydrases have been found in the mitochondria, the chloroplast thylakoid, the cytoplasm and the periplasmic space. In C₃ dicots, only two carbonic anhydrases have been localized, one to the chloroplast stroma and one to the cytoplasm. A challenge for plant scientists is to identify the number, location and physiological roles of the carbonic anhydrases.     

Extracellular Carbonic Anhydrase Facilitates Carbon Dioxide Availability for Photosynthesis in the Marine Dinoflagellate Prorocentrum micans

This study investigated inorganic carbon accumulation in relation to photosynthesis in the marine dinoflagellate Prorocentrum micans. Measurement of the internal inorganic carbon pool showed a 10-fold accumulation in relation to external dissolved inorganic carbon (DIC). Dextran-bound sulfonamide (DBS), which inhibited extracellular carbonic anhydrase, caused more than 95% inhibition of DIC accumulation and photosynthesis. We used real-time imaging of living cells with confocal laser scanning microscopy and a fluorescent pH indicator dye to measure transient pH changes in relation to inorganic carbon availability. When steady-state photosynthesizing cells were DIC limited, the chloroplast pH decreased from 8.3 to 6.9 and cytosolic pH decreased from 7.7 to 7.1. Re-addition of HCO₃⁻ led to a rapid re-establishment of the steady-state pH values abolished by DBS. The addition of DBS to photosynthesizing cells under steady-state conditions resulted in a transient increase in intracellular pH, with photosynthesis maintained for 6 s, the amount of time needed for depletion of the intracellular inorganic carbon pool. These results demonstrate the key role of extracellular carbonic anhydrase in facilitating the availability of CO₂ at the exofacial surface of the plasma membrane necessary to maintain the photosynthetic rate. The need for a CO₂-concentrating mechanism at ambient CO₂ concentrations may reflect the difference in the specificity factor of ribulose-1,5 bisphosphate carboxylase/oxygenase in dinoflagellates compared with other algal phyla.     

Different mechanisms of inorganic carbon acquisition in red macroalgae (Rhodophyta) revealed by the use of TRIS buffer

The effects on photosynthesis of acetazolamide (AZ, an inhibitor of the external carbonic anhydrase) and TRIS buffer at pH 8.7 were assessed in 24 species of red macroalgae. Only Palmaria palmata was unaffected by both substances. The rest of species were classified into three groups according to their sensitivity to TRIS and AZ. Photosynthesis of fourteen species was significantly inhibited by both TRIS and AZ. Inhibition by TRIS varied from almost 100% to 25% while AZ produced similar effects. Inhibition by TRIS was completely reverted by increasing the dissolved inorganic carbon concentration (DIC). This species group had half-saturation constants for photosynthesis (K_m(DIC)) ranging from 0.5 to 1.1 mM of DIC. TRIS produced a significant increase of K_m(DIC). Altogether, these results indicate that the algae sensitive to TRIS are capable of using HCO₃⁻ efficiently at pH 8.7. Furthermore, the buffering capacity of TRIS was responsible for its inhibitory effect on photosynthesis suggesting that HCO₃⁻ use was facilitated by excretion of protons outside the plasma membrane, which creates regions of low pH resulting in a higher-than-ambient CO₂ concentration. In contrast, photosynthesis by two Porphyra species analysed was slightly stimulated by TRIS and completely inhibited by AZ, suggesting that the mechanism was different. In a third group of seaweeds, photosynthesis was insensitive to TRIS but it was significantly inhibited by AZ. These species had relatively high values of K_m(DIC) indicating that they relied on purely diffusive entry of CO₂ generated by external carbonic anhydrase activity. Consequently, the results demonstrate that external carbonic anhydrase is widespread among red macroalgae since only P. palmata was insensitive to AZ. The functional significance of this enzyme was quite variable among the tested species.     

Model of the carbon concentrating mechanism in chloroplasts of eukaryotic algae

A generic chloroplast-based model for the carbon concentrating mechanism (CCM) in eukaryotic algae is presented. The fine structure of chloroplasts is represented by separate compartments: marginal and bulk stroma, pyrenoid, girdle lamella, bulk thylakoids, and central lamella traversing the pyrenoid. The roles of the individual structural elements of the chloroplast with respect to the CCM and the effect of carbonic anhydrase activity in various compartments are analysed. Hypothetical HCO(-)(3)transport into the acidic thylakoid lumen is adjusted by imposing an optimization principle: a given [CO(2)] at the site of RuBisCO is achieved with minimum energy costs for the CCM. Our model is highly efficient in terms of saturation of RuBisCO carboxylase activity and the affinity of the chloroplast for CO(2), if either a girdle lamella or a pyrenoid is present. The highest efficiency is achieved with a pyrenoid. A eukaryotic CCM is not necessarily associated with accumulation of dissolved inorganic carbon (DIC) as in cyanobacteria. Chloroplasts are categorized into four types corresponding to morphological characteristics of all major algal classes with regard to the presence of pyrenoids, girdle lamellae, and the distribution of CA activity.     

Dissolved inorganic carbon concentration mechanism in Chlamydomonas moewusii

The dissolved inorganic carbon concentrating mechanism(s) of Chlamydomonas moewusii CC 55 was compared with C. reinhardtii strain 137. C. moewusii is similar to C. reinhardtii with respect to maximal rates of photosynthetic oxygen evolution, CO₂ fixation, respiration, and the ability to efficiently concentrate inorganic carbon. C. moewusii has a low, but measurable amount of external carbonic anhydrase (CA) that was not inhibited by acetazolamide (AZ), an inhibitor of periplasmic carbonic anhydrase (pCA) in C. reinhardtii. The K_0.5(CO₂) for air-grown C. moewusii is about 1 μM and the algal cells accumulated dissolved inorganic carbon (DIC) to a level of about 1 mM in 60 s. AZ did not inhibit CO₂ fixation and the DIC accumulation by air-grown cells of C. moewusii. The K_0.5(CO₂) for both species remains constant from pH 6.5 to 9.5 while K_0.5(HCO₃^-) increased logarithmically, which indicates that CO₂ is the apparent inorganic carbon species that enters the cells in both algae. Antiserum prepared against the 37 kDa peptide of pCA from C. reinhardtii was immunoreactive with polypeptides of 26, 28, and 32 kDa in C. moewusii. The periplasmic carbonic anhydrase (pCA) activity is a part of the dissolved inorganic carbon concentrating mechanism in C. reinhardtii, but C  moewusii accomplished inorganic carbon accumulation without an AZ-sensitive pCA.     

Effect of Carbonic Anhydrase Inhibitors on Inorganic Carbon Accumulation by Chlamydomonas reinhardtii

Membrane-permeable and impermeable inhibitors of carbonic anhydrase have been used to assess the roles of extracellular and intracellular carbonic anhydrase on the inorganic carbon concentrating system in Chlamydomonas reinhardtii. Acetazolamide, ethoxzolamide, and a membrane-impermeable, dextran-bound sulfonamide were potent inhibitors of extracellular carbonic anhydrase measured with intact cells. At pH 5.1, where CO₂ is the predominant species of inorganic carbon, both acetazolamide and the dextran-bound sulfonamide had no effect on the concentration of CO₂ required for the half-maximal rate of photosynthetic O₂ evolution (K_0.5[CO₂]) or inorganic carbon accumulation. However, a more permeable inhibitor, ethoxzolamide, inhibited CO₂ fixation but increased the accumulation of inorganic carbon as compared with untreated cells. At pH 8, the K_0.5(CO₂) was increased from 0.6 micromolar to about 2 to 3 micromolar with both acetazolamide and the dextran-bound sulfonamide, but to a higher value of 60 micromolar with ethoxzolamide. These results are consistent with the hypothesis that CO₂ is the species of inorganic carbon which crosses the plasmalemma and that extracellular carbonic anhydrase is required to replenish CO₂ from HCO₃⁻ at high pH. These data also implicate a role for intracellular carbonic anhydrase in the inorganic carbon accumulating system, and indicate that both acetazolamide and the dextran-bound sulfonamide inhibit only the extracellular enzyme. It is suggested that HCO₃⁻ transport for internal accumulation might occur at the level of the chloroplast envelope.     

Inorganic carbon uptake by an Antarctic sea-ice diatom,Nitzschia frigida

There have been no studies to date on the mechanisms of inorganic carbon acquisition by Antarctic microalgae. Consequently, we have examined inorganic carbon (DIC) use inNitzschia frigida, a diatom typical of the Antarctic bottom-ice community. The K_0.5(CO₂) of photosynthesis in this organism was estimated to be 1.09 μM at pH 7.5. The internal concentration of DIC was approximately 4050 μM at an external [DIC] of 45 μM. At air-equilibration levels of inorganic carbon this would be sufficient for a ten-fold accumulation ratio of CO₂. Cells ofN. frigida are capable of carbon-dependent photosynthesis at rates that exceed that expected from uncatalysed CO₂ supply to the cell. About 25% of the total carbonic anhydrase activity appears to be associated with the cell surface inN. frigida. These results support the hypothesis thatN. frigida, like many microalgae from temperate waters, has an active carbon-concentrating mechanism, associated with the ability to utilize external HCO ₃ ⁻ for photosynthesis.     

CO2 concentrating mechanisms in cyanobacteria: molecular components,their diversity and evolution

Cyanobacteria have evolved an extremely effective single-cell CO(2) concentrating mechanism (CCM). Recent molecular, biochemical and physiological studies have significantly extended current knowledge about the genes and protein components of this system and how they operate to elevate CO(2) around Rubisco during photosynthesis. The CCM components include at least four modes of active inorganic carbon uptake, including two bicarbonate transporters and two CO(2) uptake systems associated with the operation of specialized NDH-1 complexes. All these uptake systems serve to accumulate HCO(3)(-) in the cytosol of the cell, which is subsequently used by the Rubisco-containing carboxysome protein micro-compartment within the cell to elevate CO(2) around Rubisco. A specialized carbonic anhydrase is also generally present in this compartment. The recent availability of at least nine cyanobacterial genomes has made it possible to begin to undertake comparative genomics of the CCM in cyanobacteria. Analyses have revealed a number of surprising findings. Firstly, cyanobacteria have evolved two types of carboxysomes, correlated with the form of Rubisco present (Form 1A and 1B). Secondly, the two HCO(3)(-) and CO(2) transport systems are distributed variably, with some cyanobacteria (Prochlorococcus marinus species) appearing to lack CO(2) uptake systems entirely. Finally, there are multiple carbonic anhydrases in many cyanobacteria, but, surprisingly, several cyanobacterial genomes appear to lack any identifiable CA genes. A pathway for the evolution of CCM components is suggested.     

羧酶体结构及其CO_2浓缩机制研究进展

羧酶体(Carboxysome)是高效的固碳微体,在CO2浓缩机制(CO2-concentrating mechanism,CCM)中发挥重要作用。在蓝藻及某些化能自养菌中,羧酶体作为类细胞器包裹1,5-二磷酸核酮糖羧化酶/加氧酶(RubisCO)和碳酸酐酶(Carbonic anhydrase,CA),它与无机碳转运蛋白共同在胞质中积累HCO3–,通过增加RubisCO周围的CO2浓度来提高固碳效率。随着羧酶体结构和功能的阐明,异源表达羧酶体已成功实现,并且已鉴定出编码羧酶体壳蛋白及内部组分的基因。首先简要介绍羧酶体的发现和种类,然后系统分析其结构及在CCM机制中的作用,并对其在代谢工程上的广阔应用前景进行了展望。     

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