HCO3− and CO2 leakage from Synechococcus UTEX 625

The leakage of various inorganic carbon species from air-grown cells of Synechococcus UTEX 625 was investigated after a light to dark transition or during a light period using a mass spectrometer under a wide variety of experimental conditions. Total inorganic carbon efflux and CO₂ efflux during the initial period of darkness were measured with or without carbonic anhydrase in the reaction medium respectively. The HCO₃^? efflux after a light to dark transition was estimated by difference. Carbon dioxide efflux in the light was measured by inhibiting CO₂ transport with either Na₂S or COS₃ or quenching the ¹³C inorganic carbon transport by the addition of ¹²C inorganic carbon in excess. In cells in which CO₂ fixation was inhibited, when only the HCO₃^? transport system was fully operative, CO₂ effluxed continuously during the light period at a rate equal to about 25% of that in darkness. When only the CO₂ transport system was operative, HCO₃^? effluxed during the light period. The difference between the light and dark efflux rates was consistent with a 0.6 unit decrease in the intracellular pH upon darkening the cells. The permeabilities of the cell for CO₂ (2.94 ± 0.14 ± 10^?8ms^?1; mean ± SE, n=137) and HCO₃^? (1.4–1.7 ± 10^?9 ms^?1) were calculated.     

Photosynthesis and inorganic carbon acquisition in the cyanobacterium Chlorogloeopsis sp. ATCC 27193

The ability of the morphologically complex cyanobacterium Chlorogloeopsis sp. ATCC 27193 to actively transport and accumulate inorganic carbon (C₁= CO₂+ HCO₃^?+ CO₃^2?) for photosynthetic CO₂ fixation was investigated. Mass-spectrometric assays revealed that Chlorogloeopsis cells grown under C₁ limitation rapidly took up CO₂ from the medium in a light-dependent reaction which was independent of CO₂ fixation. Ethoxyzolamide, a carbonic anhydrase (CA) inhibitor, inhibited CO₂ transport. Since electrometric and mass-spectrometric assays did not detect the presence of a periplasmic CA, it is suggested that CO₂ transport was mediated by a CA-like activity which converted CO₂ to HCO₃^? during passage across the membrane. Radiochemical assays, using H¹⁴CO₃ as substrate, showed that C₃-limited cells also had a high affinity (K_0.5 HCO₃^?= 37 μM), Na⁺-independent HCO₃^? uptake mechanism. HCO₃^?uptake was light dependent and occurred against its electrochemical potential indicating a carrier-mediated, active transport process. The rate of Na⁺-independent HCO₃^? transport was sufficient to account for the steady state rate of CO₂ fixation. Although not absolutely required. Na⁺ did specifically enhance the rate of HCO₃^? transport by up to 2-fold, but had no effect on the apparent affinity of the transport system for HCO₃^? Combined CO₂ and HCO₃^? transport resulted in C₁ accumulation as high as 25 mM and in excess of 300 times the external concentration. The C₁ pool was the source of CO₂ for photo-synthetic fixation and was generated, presumably, by the dehydration of HCO₃^? catalyzed by an intracellular CA. The collective evidence indicates that Chlorogloeopsis has a physiologically functional CO₂-concentrating mechanism which is essential for photosynthesis.     

Carbonic anhydrase activity and inorganic carbon fluxes in low- and high-C1 cells of Chlamydomonas reinhardtü and Scenedesmus obliquus

Carbonic anhydrase (CA) activity associated with high- and low-dissolved inorganic carbon (C₁) grown cells was examined in whole cells by measuring ¹⁸O exchange from doubly labeled CO₂ (¹³C¹⁸O¹⁸O). Both algal species showed the presence of extracellular (periplasmic) as well as intracellular CA activity, which were both greatly increased in low-C₁ cells. The periplasmic CA activity was at least 40-fold higher in lowcompared to high-C₁ cells in both C. reinhardtii and S. obliquus. while low-C₁ cells of S. obliquus showed the highest activity of internal CA. The CA inhibitor ethoxyzolamide showed a strong inhibition of the C₁ uptake process in both C. reinhardtii and S. obliquus as in cyanobacteria. which may indicate that the nature of the primary uptake process is similar in both green algae and cyanobacteria. By using a mass spectrometnc disequilibrium technique it was possible to separate the C₁ fluxes of net HCO^?₃-uptake and net CO₂-uptake during steady-state photosynthesis in high- and Sow-C₁ grown cells of Chlamydomonas reinhardtii (WT. 2137+) and Scenedesmus obliquus (WT. D3). It was found that both high- and low-C₁ cells of the two algae can utilize both CO₂ and HCO^?₃ for photosynthesis, although low-C₁ cells have a higher affinity for the uptake of both C₁ species. Induction at low-C₁ causes an increase in the affinity of both species for HCO^?₃ and CO₂; changes in net CO₂-uptake were, however, significantly greater.     

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     

Utilization of inorganic carbon in the edible cyanobacterium Ge-Xian-Mi (Nostoc) and its role in alleviating photo-inhibition

The present work investigated the inorganic carbon (C_i) uptake, fluorescence quenching and photo‐inhibition of the edible cyanobacterium Ge‐Xian‐Mi (Nostoc) to obtain an insight into the role of CO₂ concentrating mechanism (CCM) operation in alleviating photo‐inhibition. Ge‐Xian‐Mi used HCO₃^– in addition to CO₂ for its photosynthesis and oxygen evolution was greater than the theoretical rates of CO₂ production derived from uncatalysed dehydration of HCO₃^–. Multiple transporters for CO₂ and HCO₃^– operated in air‐grown Ge‐Xian‐Mi. Na⁺‐dependent HCO₃^– transport was the primary mode of active C_i uptake and contributed 53–62% of net photosynthetic activity at 250 µmol L^?1 KHCO₃ and pH 8.0. However, the CO₂‐uptake systems and Na⁺‐independent HCO₃^– transport played minor roles in Ge‐Xian‐Mi and supported, respectively, 39 and 8% of net photosynthetic activity. The steady‐state fluorescence decreased and the photochemical quenching increased in response to the transport‐mediated accumulation of intracellular C_i. Inorganic carbon transport was a major factor in facilitating quenching during the initial stage and the initial rate of fluorescence quenching in the presence of iodoacetamide, an inhibitor of CO₂ fixation, was 88% of control. Both the initial rate and extent of fluorescence quenching increased with increasing external dissolved inorganic carbon (DIC) and saturated at higher than 200 µmol L^?1 HCO₃^–. The operation of the CCM in Ge‐Xian‐Mi served as a means of diminishing photodynamic damage by dissipating excess light energy and higher external DIC in the range of 100–10000 µmol L^?1 KHCO₃ was associated with more severe photo‐inhibition under strong irradiance.     

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.     

Massive light-dependent cycling of inorganic carbon between oxygenic photosynthetic microorganisms and their surroundings

Membrane inlet mass spectrometry indicated massive light-dependent cycling of inorganic carbon between the medium and the cells of various phytoplankton species representing the main groups of aquatic primary producers. These included diatoms, symbiotic and free living dinoflagellates, a coccolithophorid, a green alga and filamentous and single cell cyanobacteria. These organisms could maintain an ambient CO₂ concentration substantially above or below that expected at chemical equilibrium with HCO₃ ⁻. The coccolithophorid Emiliania huxleyishifted from net CO₂ uptake to net CO₂ efflux with rising light intensity. Differing responses of CO₂ uptake and CO₂ fixation to changing light intensity supported the notion that these two processes are not compulsorily linked. Simultaneous measurements of CO₂ and O₂ exchange and of the fluorescence parameters in Synechococcus sp. strain PCC 7942, showed that CO₂ uptake can serve as a sensitive probe of the energy status of the photosynthetic reaction centers. However, during transitions in light intensity, changes in CO₂ uptake did not accord with those expected from fluorescence change. Quantification of the net fluxes of CO₂, HCO₃ ⁻ and of photosynthesis at steady-state revealed that substantial HCO₃ ⁻ efflux accompanied CO₂ uptake and fixation in the case of `CO<sub>2</sub> users'. On the other hand, `HCO₃ ⁻ users' were characterized by a rate of net CO₂ uptake below that of CO₂ fixation. The results support the notion that entities associated with the CCM function not only in raising the CO₂ concentration at the site of Rubisco; they may also serve as a means of diminishing photodynamic damage by dissipating excess light energy. This revised version was published online in August 2006 with corrections to the Cover Date.     

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.     

Characterisation of carbon dioxide and bicarbonate transport during steady-state photosynthesis in the marine cyanobacterium Synechococcus strain PCC7002

Net O₂ evolution, gross CO₂ uptake and net HCO _inf3 ^su– uptake during steady-state photosynthesis were investigated by a recently developed mass-spectrometric technique for disequilibrium flux analysis with cells of the marine cyanobacterium Synechococcus PCC7002 grown at different CO₂ concentrations. Regardless of the CO₂ concentration during growth, all cells had the capacity to transport both CO₂ and HCO _inf3 ^su– ; however, the activity of HCO _inf3 ^su– transport was more than twofold higher than CO₂ transport even in cyanobacteria grown at high concentration of inorganic carbon (C_i = CO₂ + HCO _inf3 ^su– ). In low-C_i cells, the affinities of CO₂ and HCO _inf3 ^su– transport for their substrates were about 5 (CO₂ uptake) and 10 (HCO _inf3 ^su– uptake) times higher than in high-C_i cells, while air-grown cells formed an intermediate state. For the same cells, the intracellular accumulated C_i pool reached 18, 32 and 55 mM in high-C_i, air-grown and low-C_i cells, respectively, when measured at 1 mM external C_i. Photosynthetic O₂ evolution, maximal CO₂ and HCO _inf3 ^su– transport activities, and consequently their relative contribution to photosynthesis, were largely unaffected by the CO₂ provided during growth. When the cells were adapted to freshwater medium, results similar to those for artificial seawater were obtained for all CO₂ concentrations. Transport studies with high-C_i cells revealed that CO₂ and HCO _inf3 ^su– uptake were equally inhibited when CO₂ fixation was reduced by the addition of glycolaldehyde. In contrast, in low-C_i cells steady-state CO₂ transport was preferably reduced by the same inhibitor. The inhibitor of carbonic anhydrase ethoxyzolamide inhibited both CO₂ and HCO _inf3 ^su– uptake as well as O₂ evolution in both cell types. In high-C_i cells, the degree of inhibition was similar for HCO _inf3 ^su– transport and O₂ evolution with 50% inhibition occurring at around 1 mM ethoxyzolamide. However, the uptake of CO₂ was much more sensitive to the inhibitor than HCO _inf3 ^su– transport, with an apparent I₅₀ value of around 250 M ethoxyzolamide for CO₂ uptake. The implications of our results are discussed with respect to C_i utilisation in the marine Synechococcus strain.Abbreviations Chl chlorophyll - C_i inorganic carbon (CO₂ + HCO _inf3 ^su– ) - CA carbonic anhydrase - CCM CO₂-concentrating mechanism - EZA ethoxyzolamide - GA glycolaldehyde - K_1/2 concentration required for half-maximal response - Rubisco ribulose-1,5,-bisphosphate carboxylase-oxygenase D.S. is a recipient of a research fellowship from the Deutsche Forschungsgemeinschaft (D.F.G.). In addition, we are grateful to Donald A. Bryant, Department of Molecular and Cell Biology and Center of Biomolecular Structure Function, Pennsylvania State University, USA, for sending us the wild-type strain of Synechococcus PCC7002.     

Effects of inorganic carbon accumulation on photosynthetic oxygen reduction and cyclic electron flow in the cyanobacterium Synechococcus PCC7942

This paper examines the effect of inorganic carbon transport and accumulation in Synechococcus PCC7942 on fluorescence quenching, photosynthetic oxygen reduction and both linear and cyclic electron flow. The data presented support the previous findings of Miller et al. (1991) that the accumulation of Ci by the CO₂ concentrating mechanism is able to stimulate oxygen photoreduction, particularly so when CO₂ fixation is inhibited by PCR cycle inhibitors such as glycolaldehyde. This effect is found with both high and low-Ci grown cells, but the potential for oxygen photoreduction is about two-fold higher in low-Ci grown cells. This greater potential for O₂ photoreduction is also correlated with a higher ability of low-Ci cells to photoreduce H₂O₂. Experiments with a mutant which transports Ci but does not accumulate it internally, indicates that the stimulation of O₂ photoreduction appears to be a direct effect of the internal accumulation of Ci rather than from its participation in the transport process. In the absence of Ci, no specific partial reactions of photosynthetic electron transport appear to be inhibited, and the PS 1 acceptors PNDA and MV as well as the PS 2 acceptor DMQ can all run electron transport at levels approaching those during active CO₂ fixation. Measurements of P700⁺ show that when the cells are depleted of Ci during photosynthesis, P700 becomes more oxidised. This indicates that the resupply of electrons from the intersystem chain is relatively more restricted under conditions of Ci limitation than is the availability of PS 1 electron acceptors. It is proposed that the accumulated Ci pool can directly stimulate the ability of O₂ to act as a PS 1 acceptor and that the ability of PS 1 acceptors, such as O₂, to relieve restrictions on intersystem electron transfer is perhaps a result of a reduction in cyclic electron flow and a subsequent increase in the oxidation state of the plastoquinone pool.Abbreviations BTP 1,3-bis[tris(hydroxymethyl)-methylaminopropane] - CA carbonic anhydrase' - Ci inorganic carbon (CO₂+HCO₃ ^–+CO₃ ^2–) - DCMU 3-(3,4-dichlorophenyl)-1,1-dimethylurea - DMQ 2,6-dimethylbenzoquinone - EZ ethoxyzolamide or 6-ethoxy-2-benzothiazole-sulfonamide - FCCP carbonyl cyanide p-trifluoro methoxyphenyl-hydrazone - F steady-state chlorophyll fluorescence - F_m chlorophyll fluorescence during a saturating light pulse - F_o chlorophyll fluorescence in the dark, prior to illumination by actinic light - MV methyl viologen or 1,1-dimethyl-4,4-bipyridinium dichloride - PCR cycle photosynthetic carbon reduction cycle - PNDA N,N-dimethyl-p-nitrosoaniline - _{PS 1} the quantum yield of Photosystem 1 - _{PS 2} the quantum yield of Photosystem 2     

The CO2‐concentrating mechanism in the bloom‐forming cyanobacterium Microcystis aeruginosa (Cyanophyceae) and effects of UVB radiation on its operation1

The bloom‐forming cyanobacterium Microcystis aeruginosa (Kütz.) Kütz. 854 was cultured with 1.05 W · m^?2 ultraviolet‐B radiation (UVBR) for 3 h every day, and the CO₂‐concentrating mechanism (CCM) within this species as well as effects of UVBR on its operation were investigated. Microcystis aeruginosa 854 possessed at least three inorganic carbon transport systems and could utilize external HCO₃^? and CO₂ for its photosynthesis. The maximum photosynthetic rate was approximately the same, but the apparent affinity for dissolved inorganic carbon was significantly decreased from 74.7 μmol · L^?1 in the control to 34.7 μmol · L^?1 in UVBR‐treated cells. At 150 μmol · L^?1 KHCO₃ and pH 8.0, Na⁺‐dependent HCO₃^? transport contributed 43.4%–40.2% to the photosynthesis in the control and 34.5%–31.9% in UVBR‐treated cells. However, the contribution of Na⁺‐independent HCO₃^? transport increased from 8.7% in the control to 18.3% in UVBR‐treated cells. The contribution of CO₂‐uptake systems showed little difference: 47.9%–51.0% in the control and 49.8%–47.2% in UVBR‐treated cells. Thus, the rate of total inorganic carbon uptake was only marginally affected, although UVBR had a differential effect on various inorganic carbon transporters. However, the number of carboxysomes in UVBR‐treated cells was significantly decreased compared to that in the control.     

The role of extracellular carbonic anhydrase for accumulation of inorganic carbon in the green alga Chlamydomonas reinhardtii. A comparison between wild-type and cell-wall-less mutant cells

The role of extracellular carbonic anhydrase (CA_ex) for dissolved inorganic carbon (DIC) accumulation in the green alga Chlamydomonas reinhardtii was investigated. It was found that when algal cells were bubbled with ambient air, cell-wall-less mutant cells exhibited the same high photosynthetic affinity for CO₂ as wild-type cells despite a 10 times lower activity of CA^ex. It was also found that the affinity for CO₂ was further increased when the total DIC concentration of the algal medium was reduced from that in equilibrium with ambient air to even lower levels. This increased affinity was not correlated with any further increase in the CA_ex activity. Dextran-bound sulfonamide (DBS. 100 μM bound ligand) completely inhibited the activity of CA_ex in intact, low-DIC grown, wild-type cells, while photosynthesis at <2 μM CO₂(aq) proceeded at a far greater rate than could be maintained by CO₂ supplied from the spontaneous dehydration of HCO^?₃. DBS-inhibition of CA_ex, during the induction of the DIC-accumulating mechanism in previously high-DIC grown cells, only caused a 50% inhibition of photosynthesis at 10 μM CO₂(aq) after 1 h of low-DIC acclimation. It was also shown that 50 μM acetazolamide (AZ) inhibited photosynthesis at low DIC concentrations to a relatively higher degree than DBS, suggesting that AZ inhibited intracellular CA as well. Taken together, these results suggest that low-DIC grown cells of C. reinhardtii have the ability to transport HCO^?₃ across the plasma membrane in addition to the CA_ex-mediated, facilitated diffusion and/or transport of CO₂. It is also suggested that the relative importance of these two fluxes (CO₂ or HCO^?₃) is dependent on the growth and experimental conditions. Facilitated CO₂ uptake seems to be most prevalent, supported by HCO^?₃-transport under more or less extreme situations, such as a reduction of CO₂ to extremely low concentrations, leakage of CA_ex to the medium as in cultures of cell-wall-less mutant cells or when the activity of CA_ex has been artificially inhibited.     

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.     

Photosynthetic capacity in relation to nitrogen content and its partitioning in lichens with different photobionts

We tested the hypothesis that lichen species with a photosynthetic CO₂-concentrating mechanism (CCM) use nitrogen more efficiently in photosynthesis than species without this mechanism. Total ribulose bisphosphate carboxylase-oxygenase (Rubisco; EC 4.1.1.39) and chitin (the nitrogenous component of fungal cell walls), were quantified and related to photosynthetic capacity in eight lichens. The species represented three modes of CO₂ acquisition and two modes of nitrogen acquisition, and included one cyanobacterial ( Nostoc ) lichen with a CCM and N₂ fixation, four green algal ( Trebouxia ) lichens with a CCM but without N₂ fixation and three lichens with green algal primary photobionts ( Coccomyxa or Dictyochloropsis ) lacking a CCM. The latter have N₂-fixing Nostoc in cephalodia. When related to thallus dry weight, total thallus nitrogen varied 20-fold, chitin 40-fold, Chl a 5-fold and Rubisco 4-fold among the species. Total nitrogen was lowest in three of the four Trebouxia lichens and highest in the bipartite cyanobacterial lichen. Lichens with the lowest nitrogen invested a larger proportion of this into photosynthetic components, while the species with high nitrogen made relatively more chitin. As a result, the potential photosynthetic nitrogen use efficiency was negatively correlated to total thallus nitrogen for this range of species. The cyanobacterial lichen had a higher photosynthetic capacity in relation to both Chl a and Rubisco compared with the green algal lichens. For the range of green algal lichens both Chl a and Rubisco contents were linearly related to photosynthetic capacity, so the data did not support the hypothesis of an enhanced photosynthetic nitrogen use efficiency in green-algal lichens with a CCM.     

Soil CO2 efflux in contrasting boreal deciduous and coniferous stands and its contribution to the ecosystem carbon balance

Similar nonsteady‐state automated chamber systems were used to measure and partition soil CO₂ efflux in contrasting deciduous (trembling aspen) and coniferous (black spruce and jack pine) stands located within 100 km of each other near the southern edge of the Boreal forest in Canada. The stands were exposed to similar climate forcing in 2003, including marked seasonal variations in soil water availability, which provided a unique opportunity to investigate the influence of climate and stand characteristics on soil CO₂ efflux and to quantify its contribution to the net ecosystem CO₂ exchange (NEE) as measured with the eddy‐covariance technique. Partitioning of soil CO₂ efflux between soil respiration (including forest‐floor vegetation) and forest‐floor photosynthesis showed that short‐ and long‐term temporal variations of soil CO₂ efflux were related to the influence of (1) soil temperature and water content on soil respiration and (2) below‐canopy light availability, plant water status and forest‐floor plant species composition on forest‐floor photosynthesis. Overall, the three stands were weak to moderate sinks for CO₂ in 2003 (NEE of ?103, ?80 and ?28 g C m^?2 yr^?1 for aspen, black spruce and jack pine, respectively). Forest‐floor respiration accounted for 86%, 73% and 75% of annual ecosystem respiration, in the three respective stands, while forest‐floor photosynthesis contributed to 11% and 14% of annual gross ecosystem photosynthesis in the black spruce and jack pine stands, respectively. The results emphasize the need to perform concomitant measurements of NEE and soil CO₂ efflux at longer time scales in different ecosystems in order to better understand the impacts of future interannual climate variability and vegetation dynamics associated with climate change on each component of the carbon balance.     

Characterization of the non-photochemical quenching of chlorophyll fluorescence that occurs during the active accumulation of inorganic carbon in the cyanobacterium Synechococcus PCC 7942

Previous work has shown that the maximum fluorescence yield from PS 2 of Synechococcus PCC 7942 occurs when the cells are at the CO₂ compensation point. The addition of inorganic carbon (C_i), as CO₂ or HCO₃ ^–, causes a lowering of the fluorescence yield due to both photochemical (q_p) and non-photochemical (q_N) quenching. In this paper, we characterize the q_N that is induced by C_i addition to cells grown at high light intensities (500 mol photons m^–2 s^–1). The C_i-induced q_N was considerably greater in these cells than in cells grown at low light intensities (50 mol photons m^–2 s^–1), when assayed at a white light (WL) intensity of 250 mol photons m^–2 s^–1. In high-light grown cells we measured q_N values as high as 70%, while in low-light grown cells the q_N was about 16%. The q_N was relieved when cells regained the CO₂ compensation point, when cells were illuminated by supplemental far-red light (FRL) absorbed mainly by PS 1, or when cells were illuminated with increased WL intensities. These characteristics indicate that the q_N was not a form of energy quenching (q_E). Supplemental FRL illumination caused significant enhancement of photosynthetic O₂ evolution that could be correlated with the changes in q_p and q_N. The increases in q_p induced by C_i addition represent increases in the effective quantum yield of PS 2 due to increased levels of oxidized Q_A. The increase in q_N induced by C_i represents a decrease in PS 2 activity related to decreases in the potential quantum yield. The lack of diagnostic changes in the 77 K fluorescence emission spectrum argue against q_N being related to classical state transitions, in which the decrease in potential quantum yield of PS 2 is due either to a decrease in absorption cross-section or by increased spill-over of excitation energy to PS 1. Both the C_i-induced q_p (t _0.5<0.5 s) and q_N (t _0.51.6 s) were rapidly relieved by the addition of DCMU. The two time constants give further support for two separate quenching mechanisms. We have thus characterized a novel form of q_N in cyanobacteria, not related to state transitions or energy quenching, which is induced by the addition of C_i to cells at the CO₂-compensation point.Abbreviations BTP- 1,3-bis[tris(hydroxymethyl)-methylaminopropane] - Chl- chlorophyll - C_i- inorganic carbon (CO₂+HCO₃ ^–+CO₃ ^2–) - DCMU- 3-(3,4-dichlorophenyl)-, 1-dimethylurea) - F- chlorophyll fluorescence measured at any time in the absence of a saturating flash - F_o- chlorophyll fluorescence with only the weak modulated measuring beam on - F_M'- chlorophyll fluorescence during a saturating flash - F_M- maximum chlorophyll fluorescence, measured in the presence of WL and FRL at the CO₂-compensation point or in the presence of DCMU - F_V- variable fluorescence (= F_M'–F₀) - FRL- supplemental illumination with far red light - MB- modulated measuring beam of the PAM fluorometer - MV- methyl viologen - PAM- pulse amplitude modulation - PFD- incident photon flux density - PS 1, 2- Photosystems 1 and 2 - Q_A- primary electron-accepting plastoquinione of PS 2 - q_N- non-photochemical quenching of chlorophyll fluorescence - q_p- photochemical quenching of chlorophyll fluorescence; rubisco-ribulose bisphosphate carboxylase/oxygenase - SF- saturating flash (600 ms duration) - WL- white light illumination     

Sap flow rates and sapwood density are critical factors in within- and between-tree variation in CO2 efflux from stems of mature Dacrydium cupressinum trees

Measurements of CO2 efflux from stems and branches, sap velocity, and respiratory activity of excised wood cores were conducted in Dacrydium cupressinum trees that differed in diameter, age, and canopy emergence. The objective of this study was to determine if consistent linkages exist among respiratory production of CO2 within stems, xylem transport of CO2, and the rate of CO2 diffusing from stem surfaces. Stem CO2 efflux was depressed during periods of sap flow compared with the efflux rate expected for a given stem temperature and was positively correlated with sapwood density. By contrast, no significant relationships were observed between CO2 efflux and the respiratory activity of wood tissues. Between 86 and 91% of woody tissue respiration diffused to the atmosphere over a 24-h period. However, at certain times of the day, xylem transport and internal storage of CO2 may account for up to 13-38% and 12-18%, respectively, of woody tissue respiration. These results demonstrate that differences in sap flow rates and xylem anatomy are critically important for explaining within- and between-tree variation in CO2 efflux from stems.     

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.