Nutrient availability affects the response of the calcifying chlorophyte Halimeda opuntia (L.) J.V. Lamouroux to low pH

Atmospheric carbon dioxide emissions cause a decrease in the pH and aragonite saturation state of surface ocean water. As a result, calcifying organisms are expected to suffer under future ocean conditions, but their physiological responses may depend on their nutrient status. Because many coral reefs experience high inorganic nutrient loads or seasonal changes in nutrient availability, reef organisms in localized areas will have to cope with elevated carbon dioxide and changes in inorganic nutrients. Halimeda opuntia is a dominant calcifying primary producer on coral reefs that contributes to coral reef accretion. Therefore, we investigated the carbon and nutrient balance of H. opuntia exposed to elevated carbon dioxide and inorganic nutrients. We measured tissue nitrogen, phosphorus and carbon content as well as the activity of enzymes involved in inorganic carbon uptake and nitrogen assimilation (external carbonic anhydrase and nitrate reductase, respectively). Inorganic carbon content was lower in algae exposed to high CO₂, but calcification rates were not significantly affected by CO₂ or inorganic nutrients. Organic carbon was positively correlated to external carbonic anhydrase activity, while inorganic carbon showed the opposite correlation. Carbon dioxide had a significant effect on tissue nitrogen and organic carbon content, while inorganic nutrients affected tissue phosphorus and N:P ratios. Nitrate reductase activity was highest in algae grown under elevated CO₂ and inorganic nutrient conditions and lowest when phosphate was limiting. In general, we found that enzymatic responses were strongly influenced by nutrient availability, indicating its important role in dictating the local responses of the calcifying primary producer H. opuntia to ocean acidification.     

Photosynthesis in Ulva fasciata: V. Evidence for an Inorganic Carbon Concentrating System, and Ribulose-1,5-Bisphosphate Carboxylase/Oxygenase CO(2) Kinetics

Evidence of an inorganic carbon concentrating system in a marine macroalga is provided here. Based on an O₂ technique, supported by determinations of inorganic carbon concentrations, of experimental media (as well as compensation points) using infrared gas analysis, it was found that Ulva fasciata maintained intracellular inorganic carbon levels of 2.3 to 6.0 millimolar at bulk medium concentrations ranging from 0.02 to 1.5 millimolar. Bicarbonate seemed to be the preferred carbon form taken up at all inorganic carbon levels. It was found that ribulose-1,5-bisphosphate carboxylase/oxygenase from Ulva had a K_m(CO₂) of 70 micromolar and saturated at about 250 micromolar CO₂. Assuming a cytoplasmic pH of 7.2 (as measured for another Ulva species, P Lundberg et al. [1988] Plant Physiol 89: 1380-1387), and given the high activity of internal carbonic anhydrase (S Beer, A Israel [1990] Plant Cell Environ [in press]) and the here measured internal inorganic carbon level, it was concluded that internal CO₂ in Ulva could, at ambient external inorganic carbon concentrations, be maintained at a high enough level to saturate ribulose-1,5-bisphosphate carboxylase/oxygenase carboxylation. It is suggested that this suppresses photorespiration and optimizes net photosynthetic production in an alga representing a large group of marine plants faced with limiting external CO₂ concentrations in nature.     

Effect of photon flux density on inorganic carbon accumulation and net CO2 exchange in a high-CO2-requiring mutant of Chlamydomonas reinhardtii

The effect of photon flux density on inorganic carbon accumulation and photosynthetic CO₂ assimilation was determined by CO₂ exchange studies at three, limiting CO₂ concentrations with a ca-1 mutant of Chlamydomonas reinhardiii. This mutant accumulates a large internal inorganic carbon pool in the light which apparently is unavailable for photosynthetic assimilation. Although steady-state photosynthetic CO₂ assimilation did not respond to the varying photon flux densities because of CO₂ limitation, components of inorganic-carbon accumulation were not clearly light saturated even at 1100 mol photons m^-2 s^-1, indicating a substantial energy requirement for inorganic carbon transport and accumulation. Steady-state photosynthetic CO₂ assimilation responded to external CO₂ concentrations but not to changing internal inorganic carbon concentrations, confirming that diffusion of CO₂ into the cells supplies most of the CO₂ for photosynthetic assimilation and that the internal inorganic carbon pool is essentially unavailable for photosynthetic assimilation. The estimated concentration of the internal inorganic carbon pool was found to be relatively insensitive to the external CO₂ concentration over the small range tested, as would be expected if the concentration of this pool is limited by the internal to external inorganic carbon gradient. An attempt to use this CO₂ exchange method to determine whether inorganic carbon accumulation and photosynthetic CO₂ assimilation compete for energy at low photon flux densities proved inconclusive.     

Induction of HCO(3) Transporting Capability and High Photosynthetic Affinity to Inorganic Carbon by Low Concentration of CO(2) in Anabaena variabilis

The apparent affinity of photosynthesis for inorganic carbon in Anabaena variabilis strain M-3 increased during the course of adaptation from high to low CO₂ concentration (5% and 0.03% v/v CO₂ in air, respectively). This was attributed to an increased ability of the cells to accumulate inorganic carbon during the course of adaptation to low CO₂ conditions. The release of phycobiliproteins was used to evaluate the sensitivity of the cells to lysozyme treatment followed by osmotic shock. High CO₂-grown cells were more sensitive to this treatment than were low CO₂ ones. The efflux of inorganic carbon from cells preloaded with radioactive bicarbonate is faster in high than it is in low CO₂-adapted cells. It is postulated that the cell wall or membrane components undergo changes during the course of adaptation to low CO₂ conditions. This is supported by electron micrographs showing differences in the cell wall appearance between high and low CO₂-grown cells. The increasing ability to accumulate HCO₃⁻ and the lessened sensitivity to lysozyme during adaptation to low CO₂ conditions depends on protein synthesis. The increase in affinity for inorganic carbon during the adaptation to low CO₂ conditions is severely inhibited by the presence of spectinomycin. Incubation in the light significantly lessens the time required for the adaptation to low CO₂ conditions.     

Inorganic Carbon Uptake by Chlamydomonas reinhardtii

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

Functional Hybrid Rubisco Enzymes with Plant Small Subunits and Algal Large Subunits: ENGINEERED rbcS cDNA FOR EXPRESSION IN CHLAMYDOMONAS*?

There has been much interest in the chloroplast-encoded large subunit of ribulose-1,5-bisphosphate carboxylase/oxygenase (Rubisco) as a target for engineering an increase in net CO₂ fixation in photosynthesis. Improvements in the enzyme would lead to an increase in the production of food, fiber, and renewable energy. Although the large subunit contains the active site, a family of rbcS nuclear genes encodes the Rubisco small subunits, which can also influence the carboxylation catalytic efficiency and CO₂/O₂ specificity of the enzyme. To further define the role of the small subunit in Rubisco function, small subunits from spinach, Arabidopsis, and sunflower were assembled with algal large subunits by transformation of a Chlamydomonas reinhardtii mutant that lacks the rbcS gene family. Foreign rbcS cDNAs were successfully expressed in Chlamydomonas by fusing them to a Chlamydomonas rbcS transit peptide sequence engineered to contain rbcS introns. Although plant Rubisco generally has greater CO₂/O₂ specificity but a lower carboxylation V_max than Chlamydomonas Rubisco, the hybrid enzymes have 3–11% increases in CO₂/O₂ specificity and retain near normal V_max values. Thus, small subunits may make a significant contribution to the overall catalytic performance of Rubisco. Despite having normal amounts of catalytically proficient Rubisco, the hybrid mutant strains display reduced levels of photosynthetic growth and lack chloroplast pyrenoids. It appears that small subunits contain the structural elements responsible for targeting Rubisco to the algal pyrenoid, which is the site where CO₂ is concentrated for optimal photosynthesis.     

Internal Inorganic Carbon Pool of Chlamydomonas reinhardtii: EVIDENCE FOR A CARBON DIOXIDE-CONCENTRATING MECHANISM

The external inorganic carbon pool (CO₂ + HCO₃⁻) was measured in both high and low CO₂-grown cells of Chlamydomonas reinhardtii, using a silicone oil layer centrifugal filtering technique. The average internal pH values were measured for each cell type using [¹⁴C]dimethyloxazolidinedione, and the internal inorganic carbon pools were recalculated on a free CO₂ basis. These measurements indicated that low CO₂-grown cells were able to concentrate CO₂ up to 40-fold in relation to the external medium. Low and high CO₂-grown cells differed in their photosynthetic affinity for external CO₂. These differences could be most readily explained as being due to the relative CO₂-concentrating capacity of each cell type. This physiological adaptation appeared to be based on changes in the abilities of the cells actively to accumulate inorganic carbon using an energy-dependent transport system.     

Uptake of inorganic carbon by isolated chloroplasts from air-adapted dunaliella

Neither Dunaliella cells grown with 5% CO₂ nor their isolated chloroplasts had a CO₂ concentrating mechanism. These cells primarily utilized CO₂ from the medium because the K_(0.5) (HCO₃⁻) increase from 57 micromolar at pH 7.0 to 1489 micromolar at pH 8.5, where as the K_(0.5) CO₂ was about 12 micromolar over the pH range. After air adaptation for 24 hours in light, a CO₂ concentrating mechanism was present that decreased the K_0.5 (CO₂) to about 0.5 micromolar and K_0.5 (HCO₃⁻) to 11 micromolar at pH 8. These K_0.5 values suggest that air-adapted cells preferentially concentrated CO₂ but could also use HCO₃⁻ from the medium. Chloroplasts isolated from air-adapted cells had a K_(0.5) for total inorganic carbon of less than 10 micromolar compared to 130 micromolar for chloroplasts from cells grown on high CO₂. Chloroplasts from air-adapted cells, but not CO₂-grown cells, concentrate inorganic carbon internally to 1 millimolar in 60 seconds from 240 micromolar in the medium. Maximum uptake rates occurred after preillumination of 45 seconds to 3 minutes. The CO₂ concentrating mechanism by chloroplasts from air-adapted cells was light dependent and inhibited by 3-(3,4-dichlorophenyl)-1,1-dimethylurea (DCMU) or flurocarbonyl-cyamidephenylhydrazone (FCCP). Phenazine-methosulfate at 10 micromolar to provide cyclic phosphorylation partially reversed the inhibition by DCMU but not by FCCP. One to 0.1 millimolar vanadate, an inhibitor of plasma membrane ATPase, inhibited inorganic carbon accumulation by isolated chloroplasts. Vanadate had no effect on CO₂ concentration by whole cells, as it did not readily cross the cell plasmalemma. Addition of external ATP to the isolated chloroplast only slightly stimulated inorganic carbon uptake and did not reverse vanadate inhibition by more than 25%. These results are consistent with a CO₂ concentrating mechanism in Dunaliella cells which consists in part of an inorganic carbon transporter at the chloroplast envelope that is energized by ATP from photosynthetic electron transport.     

Effects of the relative extrachloroplastic concentrations of inorganic phosphate, 3-phosphoglycerate, and dihydroxyacetone phosphate on the rate of starch synthesis in isolated spinach chloroplasts

The effect of external inorganic phosphate (Pi) on starch synthesis in isolated spinach (Spinacia oleracea American Hybrid No. 424) chloroplasts in the presence of millimolar concentrations of 3-phosphoglycerate (PGA) and/or dihydroxyacetone phosphate (DAP) was examined. Whereas CO₂ fixation was relatively constant as the ratio of the external phosphate to the PGA + DAP varied from 1:3 to 3:1, starch synthesis varied from 17% to 2% of the CO₂ fixation rate. With DAP alone, maximal starch synthesis was about 10% of the CO₂ fixation rate. The data demonstrate that the Pi/(PGA + DAP) ratio in the cytoplasm of plant cells could serve to regulate the flow of newly fixed carbon into starch without alterations in the rate of CO₂ fixation.     

Adaptation of Chlamydomonas reinhardtii High-CO(2)-Requiring Mutants to Limiting CO(2)

Photosynthetic characteristics of four high-CO₂-requiring mutants of Chlamydomonas reinhardtii were compared to those of wild type before and after a 24-hour exposure to limiting CO₂ concentrations. The four mutants represent two loci involved in the CO₂-concentrating system of this unicellular alga. All mutants had a lower photosynthetic affinity for inorganic carbon than did the wild type when grown at an elevated CO₂ concentration, indicating that the genetic lesion in each is expressed even at elevated CO₂ concentrations. Wild type and all four mutants exhibited adaptive responses to limiting CO₂ characteristic of the induction of the CO₂-concentrating system, resulting in an increased affinity for inorganic carbon only in wild type. Although other components of the CO₂-concentrating system were induced in these mutants, the defective component in each was sufficient to prevent any increase in the affinity for inorganic carbon. It was concluded that the genes corresponding to the ca-1 and pmp-1 loci exhibit at least partially constitutive expression and that all components of the CO₂-concentrating system may be required to significantly affect the photosynthetic affinity for inorganic carbon.     

A 36 Kilodalton Limiting-CO(2) Induced Polypeptide of Chlamydomonas Is Distinct from the 37 Kilodalton Periplasmic Carbonic Anhydrase

Chlamydomonas reinhardtii possesses a CO₂-concentrating mechanism, induced by limiting CO₂, which involves active transport and accumulation of inorganic carbon within the cell. Synthesis of several proteins is induced by limiting CO₂, but, of those, only periplasmic carbonic anhydrase has an identified function in the system. No proteins involved in active transport have yet been identified, but induced, membrane-associated polypeptides, such as the 36 kilodalton polypeptide focused on in this paper, would seem to be candidates for such involvement. The 36 kilodalton polypeptide was shown to be synthesized de novo upon transfer of cells to limiting CO₂. It was purified using SDS-PAGE and used to produce polyclonal antibodies. Antibodies were used to confirm the air-specific nature of the polypeptide, its strict association with membrane fractions, and the time course of its induction. Using the antibodies, a single, 36 kilodalton polypeptide was found to be specifically immunoprecipitated from in vitro translation products of poly(A⁺) RNA from cells only after exposure to limiting CO₂. The absence of translatable mRNA for this polypeptide in CO₂-enriched cells indicated that regulation occurs at the level of message abundance. The antibodies were also used to demonstrate the distinction between the limiting-CO₂ induced 36 kilodalton polypeptide and the similarly sized, limiting-CO₂ induced periplasmic carbonic anhydrase.     

Relationship between the Kinetic Properties and the Small Subunit Composition of Nicotiana Ribulose-1, 5-bisphosphate Carboxylase

Genetic variability in the large and small subunits of ribulose-1,5-bisphosphate carboxylase/oxygenase (RuBPCase) in several Nicotiana species has been characterized by isoelectric focusing patterns. This heritable variation provides an opportunity to examine the functional role of each of these subunits. In this study, specifically designed RuBPCase enzymes composed of identical large subunits but different small subunits were constructed in vivo by interspecific hybridization between the species N. sylvestris, N. tabacum, N. glauca, N. glutinosa, N. plumbaginifolia, and N. tomentosiformis. Small subunit polypeptides were combined to form a sequence of one, two, three, and four polypeptides with the large subunit of N. sylvestris. Kinetic properties of these hybrid enzymes were compared. No differences in the specific activity of either carboxylation or oxygenation nor in K_m values for ribulose 1,5-bisphosphate, CO₂, or O₂ were detected among the RuBPCase enzymes from the various interspecific hybrids. Likewise, the ratio of carboxylation to oxygenation was constant.     

A Model for HCO(3) Accumulation and Photosynthesis in the Cyanobacterium Synechococcus sp: Theoretical Predictions and Experimental Observations

A simple model based on HCO₃⁻ transport has been developed to relate photosynthesis and inorganic carbon fluxes for the marine cyanobacterium, Synechococcus sp. Nägeli (strain RRIMP N1). Predicted relationships between inorganic carbon transport, CO₂ fixation, internal carbonic anhydrase activity, and leakage of CO₂ out of the cell, allow comparisons to be made with experimentally obtained data. Measurements of inorganic carbon fluxes and internal inorganic carbon pool sizes in these cells were made by monitoring time-courses of CO₂ changes (using a mass spectrometer) during light/dark transients. At just saturating CO₂ conditions, total inorganic carbon transport did not exceed net CO₂ fixation by more than 30%. This indicates CO₂ leakage similar to that estimated for C₄ plants.

For this leakage rate, the model predicts the cell would need a conductance to CO₂ of around 10⁻⁵ centimeters per second. This is similar to estimates made for the same cells using inorganic carbon pool sizes and CO₂ efflux measurements. The model predicts that carbonic anhydrase is necessary internally to allow a sufficiently fast rate of CO₂ production to prevent a large accumulation of HCO₃⁻. Intact cells show light stimulated carbonic anhydrase activity when assayed using ¹⁸O-labeled CO₂ techniques. This is also supported by low but detectable levels of carbonic anhydrase activity in cell extracts, sufficient to meet the requirements of the model.

     

Effect of dissolved inorganic carbon on the expression of carboxysomes,localization of Rubisco and the mode of inorganic carbon transport in cells of the cyanobacterium Synechococcus UTEX 625

In the cyanobacterium Synechococcus UTEX 625, the extent of expression of carboxysomes appeared dependent on the level of inorganic carbon (CO₂+HCO _inf3 ^sup- ) in the growth medium. In cells grown under 5% CO₂ and in those bubbled with air, carboxysomes were present in low numbers (<2 · longitudinal section^-1) and were distributed in an apparently random manner throughout the centroplasm. In contrast, cells grown in standing culture and those bubbled with 30 l CO₂ · 1^-1 possessed many carboxysomes (>8 · longitudinal section^-1). Moreover, carboxysomes in these cells were usually positioned near the cell periphery, aligned along the interface between the centroplasm and the photosynthetic thylakoids. This arrangement of carboxysomes coincided with the full induction of the HCO _inf3 ^sup- transport system that is involved in concentrating inorganic carbon within the cells for subsequent use in photosynthesis. Immunolocalization studies indicate that the Calvin cycle enzyme ribulose bisphosphate carboxylase was predominantly carboxysome-localized, regardless of the inorganic carbon concentration of the growth medium, while phosphoribulokinase was confined to the thylakoid region. It is postulated that the peripheral arrangement of carboxysomes may provide for more efficient photosynthetic utilization of the internal inorganic carbon pool in cells from cultures where carbon resources are limiting.Abbreviations Chl chlorophyll - DIC dissolved inorganic carbon (CO₂+HCO _inf3 ^sup- +CO _inf3 ^sup2- ) - PRK phosphoribulokinase - RuBP ribulose 1,5-bisphosphate - Rubisco LS large subunit of ribulose 1,5-bisphosphate carboxylase/oxygenase     

Effect of Varying CO(2) Partial Pressure on Photosynthesis and on Carbon Isotope Composition of Carbon-4 of Malate from the Crassulacean Acid Metabolism Plant Kalanchoë daigremontiana Hamet et Perr

Intact leaves of Kalanchoë daigremontiana were exposed to CO₂ partial pressures of 100, 300, and 1000 microbars. Malic acid was extracted, purified, and degraded in order to obtain isotopic composition of carbon-1 and carbon-4. From these data, it is possible to calculate the carbon isotope composition of newly fixed carbon in malate. In all three treatments, the isotopic composition of newly introduced carbon is the same as that of the CO₂ source and is independent of CO₂ partial pressures over the range tested. Comparison with numerical models described previously (O'Leary 1981 Phytochemistry 20: 553-567) indicates that we would expect carbon 4 of malate to be 4‰ more negative than source CO₂ if diffusion is totally limiting or 7‰ more positive than source CO₂ if carboxylation is totally limiting. Our results demonstrate that stomatal aperture adjusts to changing CO₂ partial pressures and maintains the ratio of diffusion resistance to carboxylation resistance approximately constant. In this study, carboxylation and diffusion resistances balance so that essentially no fractionation occurs during malate synthesis. Gas exchange studies of the same leaves from which malate was extracted show that the extent of malate synthesis over the whole night is nearly independent of CO₂ partial pressure, although there are small variations in CO₂ uptake rate. Both the gas exchange and the isotope studies indicate that the ratio of external to internal CO₂ partial pressure is the same in all three treatments. Inasmuch as a constant ratio will result in constant isotope fractionation, this observation may explain why plants in general have fairly invariable ¹³C contents, despite growing under a variety of environmental conditions.     

Uptake and utilization of inorganic carbon by cyanobacteria

In the cyanobacteria, mechanisms exist that allow photosynthetic CO₂ reduction to proceed efficiently even at very low levels of inorganic carbon. These inducible, active transport mechanisms enable the cyanobacteria to accumulate large internal concentrations of inorganic carbon that may be up to 1000-fold higher than the external concentration. As a result, the external concentration of inorganic carbon required to saturate cyanobacterial photosynthesis in vivo is orders of magnitude lower than that required to saturate the principal enzyme (ribulose bisphosphate carboxylase) involved in the fixation reactions. Since CO₂ is the substrate for carbon fixation, the cyanobacteria somehow perform the neat trick of concentrating this small, membrane permeable molecule at the site of CO₂ fixation. In this review, we will describe the biochemical and physiological experiments that have outlined the phenomenon of inorganic carbon accumulation, relate more recent genetic and molecular biological observations that attempt to define the constituents involved in this process, and discuss a speculative theory that suggests a unified view of inorganic carbon utilization by the cyanobacteria.Abbreviations C_i Inorganic carbon - H-cells Cells grown under high CO₂ - L-cells Cells grown under low CO₂ - RuBP Ribulose-1,5-bisphosphate - WT Wild type     

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.     

Membrane-Associated Polypeptides Induced in Chlamydomonas by Limiting CO(2) Concentrations

Chlamydomonas reinhardtii and other unicellular green algae have a high apparent affinity for CO₂, little O₂ inhibition of photosynthesis, and reduced photorespiration. These characteristics result from operation of a CO₂-concentrating system. The CO₂-concentrating system involves active inorganic carbon transport and is under environmental control. Cells grown at limiting CO₂ concentrations have inorganic carbon transport activity, but cells grown at 5% CO₂ do not. Four membrane-associated polypeptides (M_r 19, 21, 35, and 36 kilodaltons) have been identified which either appear or increase in abundance during adaptation to limiting CO₂ concentrations. The appearance of two of the polypeptides occurs over roughly the same time course as the appearance of the CO₂-concentrating system activity in response to CO₂ limitation.     

Evidence for Inorganic Carbon Transport by Intact Chloroplasts of Chlamydomonas reinhardtii

Isolated intact chloroplasts from wall-less mutants of Chlamydomonas reinhardtii accumulate inorganic carbon (C_i) from the medium provided the cells had been adapted to low CO₂ photoautotrophic growth conditions. Chloroplasts from cultures grown on high (5%) CO₂ or photoheterotrophically with acetate did not accumulate inorganic carbon. Chloroplast C_i accumulation from low CO₂ grown cells was light dependent and was inhibited by uncouplers and inhibitors of electron transport. In a model for C_i accumulation by Chlamydomonas, it is proposed that CO₂ diffuses into the cell and C_i accumulation occurs in the chloroplast.