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Journal of Experimental Botany logoLink to Journal of Experimental Botany
. 2016 Oct 12;68(2):255–267. doi: 10.1093/jxb/erw374

Size matters for single-cell C4 photosynthesis in Bienertia

Ivan Jurić 1,2,, Vinicio González-Pérez 1, Julian M Hibberd 3, Gerald Edwards 4, Nigel J Burroughs 1,
PMCID: PMC5853773  PMID: 27733441

A spatial separation of 10 µm between primary and secondary carboxylases is sufficient for a single-cell C4 pathway, even in the absence of any intracellular diffusion barriers.

Keywords: Bienertia, C4 photosynthesis, carbon fixation, photon cost, photosynthetic efficiency, single-cell C4, spatial modelling

Abstract

Bienertia cycloptera belongs to a diverse set of plants, recently discovered to perform C4 photosynthesis within individual mesophyll cells. How these plants accomplish high photosynthetic efficiency without adopting Kranz anatomy remains unanswered. By modelling the processes of diffusion, capture, and release of carbon dioxide and oxygen inside a typical Bienertia mesophyll cell geometry, we show that a spatial separation as low as 10 μm between the primary and the secondary carboxylases, can, on its own, provide enough diffusive resistance to sustain a viable C4 pathway at 20 °C, with a CO2 leakage <35%. This critical separation corresponds to a cell diameter of 50 μm, consistent with the observed range where Bienertia’s mesophyll cells start to develop their characteristic mature anatomy. Our results are robust to significant alterations in model assumptions and environmental conditions, their applicability extending even to aquatic plants.

Introduction

An excellent example of convergent evolution is the development of the C4. photosynthetic pathway in multiple plant genera (Sage, 2004; Sage et al., 2011, 2012). The primary carbon-fixing enzyme in plants, Ribulose-1,5-biphosphate-carboxylase-oxygenase (or Rubisco, for short) can both carboxylate ribulose-1,5-biphosphate (RuBP) with CO2 and oxygenate it with O2. Carboxylation of RuBP is one of the steps in the Calvin–Benson cycle, also referred to as C3 photosynthesis. In contrast, the oxygenation reaction is detrimental, leading to a costly RuBP salvage process (termed photorespiration). Rubisco is not very discriminating with respect to the two atmospheric gases (Farquhar et al., 1980; Zhu et al., 2008), which, combined with the high levels of O2 relative to CO2 in the atmosphere, hinders the efficiency of photosynthesis. The C4 pathway circumvents Rubisco’s poor specificity by placing the enzyme in a CO2-rich environment that is actively maintained by means of a chemical CO2 pump, which we shall refer to as the C4 pump. The pump involves a number of enzymes that capture atmospheric CO2 and store it temporarily in four-carbon dicarboxylic acids (malate and aspartate) which diffuse to the compartment where Rubisco is located. Here they are decarboxylated, releasing CO2 (Jenkins et al., 1989; von Caemmerer and Furbank, 2003). This is an active process that consumes ATP. The C4 pathway, which evolved multiple times in terrestrial plants, is often associated with the development of Kranz anatomy (Sage, 2004). The fixation of atmospheric CO2 into C4 acids occurs in the mesophyll, while the bundle sheath cells, which harbour Rubisco-rich chloroplasts, are regions where CO2 is concentrated. Kranz anatomy thus separates the CO2-absorbing and releasing components of the C4 pump with multiple diffusion barriers (cell walls and plasma membranes) (von Caemmerer and Furbank, 2003). The presence of such diffusive barriers was considered crucial for an efficient C4 pathway, and Kranz anatomy was commonly viewed as a necessary and a defining property of a functional C4 plant (von Caemmerer et al., 2014).

Discovery of terrestrial C4 plants (in the Chenopodiaceae family) that lack Kranz anatomy and instead perform all the steps of the C4 pathway within the confines of an individual mesophyll cell disproved this view (Voznesenskaya et al., 2001, 2002). In the genus Bienertia (B. cycloptera, B. sinuspersici, and B. kavirense), mature chlorenchyma cells are unusually large (80–110 µm in the major dimension; Akhani et al., 2005, 2012; von Caemmerer et al., 2014) and possess a peculiar cellular architecture. The majority of the cell’s chloroplasts are located in a sphere of 20–32 µm in diameter (Akhani et al., 2005, 2012; von Caemmerer et al., 2014), which is positioned in the centre of the cell, Fig. 1a. This ‘central chloroplast compartment’ (CCC) is surrounded by a large vacuole. A portion of the cell’s chloroplasts (referred to as ‘peripheral’) are scattered along the cell’s surface, separated from the CCC by the vacuole. Narrow cytoplasmic channels cross the vacuole connecting the central compartment with the periphery (Voznesenskaya et al., 2005). The C4 pump in Bienertia functions by shuttling aspartate (a C4 acid) and alanine (a C3 acid) between the two domains (Voznesenskaya et al., 2005; Offermann et al., 2011), characteristic of NAD-malic enzyme (NAD-ME) type C4 plants. Conversion between alanine and aspartate goes through several C3 and C4 intermediaries (for full details, see, for example, von Caemmerer and Furbank, 2003). The initial carbon capture occurs in the peripheral cytoplasm where carbonic anhydrase (CA) converts CO2 to bicarbonate, which is used by phosphoenolpyruvate carboxylase (PEPC) to turn phosphoenolpyruvate (PEP, a C3 acid) into oxaloacetate (a C4 acid). Subsequent release of CO2 occurs in the mitochondria within the CCC, where malate (a C4 acid) is decarboxylated by NAD-ME. The chloroplasts in the central compartment are filled with Rubisco, which assimilates released CO2 (Voznesenskaya et al., 2005; Offermann et al., 2011). A C4 pump is thus established between the cell’s periphery and its centre.

Fig. 1.

Fig. 1.

Modelling a Bienertia mesophyll cell. (a) Micrograph of a mature Bienertia mesophyll cell, taken from Voznesenskaya et al. (2002) with permission. The arrows point to the peripheral chloroplasts. (b) Model of a Bienertia cell, showing the three compartments, and marking the location of various enzymes. The compartment’s radii, ri, rv, and re are varied in the model, so the picture should not be taken to scale. (c) Abstract schematic of reactions and flows in different spatial regions considered in the model. Yellow arrows represent the oxygen current, and light blue is the CO2 current (two-headed arrows represent diffusion). Other arrows represent the C3 and C4 acid currents (grey and dark blue), and the photorespiratory and Calvin–Benson cycle carbon currents (striped green and blue). The thin dashed line is the NADPH current originating from the Hill reaction in the core’s chloroplasts; it couples the photorespiratory and the Calvin–Benson cycle activity to the oxygen production. The boundary between the periphery and the outside is the only barrier to gas diffusion in the model.

The energy from photons absorbed by the chloroplast photosystems is used to produce the ATP and NADPH needed to support carbon assimilation. In C3 plants, this includes requirements to support the Calvin–Benson cycle, and photorespiration, while C4 plants also need to support the C4 cycle. The efficiency of the C4 pathway depends on the balance between this additional energy cost and the reduced photorespiration cost. In C3 plants, the assimilation cost rises with increasing resistance to diffusion of CO2 from the atmosphere to Rubisco (e.g. by stomatal limitation or reduced conductance of CO2 from the intercellular air space to Rubisco in photosynthetic cells), or with increasing temperature [when Rubisco’s specificity decreases (Boyd et al., 2015)]. In C4 photosynthesis the gradient of CO2 concentration is reversed, and the resistance to gas diffusion now benefits the plant. Still, a degree of CO2 leakage is inevitable, and a C4 pump must run faster than CO2 fixation by Rubisco. The fraction of pumped CO2 leaking out of the Rubisco-containing compartment ranges from 20% to 40% in plants with Kranz anatomy (Kubásek et al., 2007; von Caemmerer et al., 2014). In plants with a single-cell C4 pathway, there are few physical barriers between the locations of the initial carbon capture and CO2 release (only a couple of intracellular lipid bilayer membranes), so one would expect a significantly—even prohibitively—higher CO2 leakage (von Caemmerer, 2003). Yet studies indicate that the leakage is comparable with that of plants with Kranz anatomy (King et al., 2012; von Caemmerer et al., 2014; Stutz et al., 2014). This raises the question of how single-cell C4 plants achieve this apparently high efficacy.

Herein we investigate the efficacy of the C4 pathway in Bienertia through construction of a spatial mathematical model of a Bienertia mesophyll cell. We concentrate on the role of its specific cellular architecture, and, in particular, on the effect that the spatial separation between the periphery and the central compartment has on the efficiency of the C4 pathway. Our model goes beyond the previous compartmental models of carbon fixation in plants that tend to oversimplify the spatial aspects of photosynthetic processes (von Caemmerer, 2003, 2013; von Caemmerer et al., 2014). We show that spatial separation alone can act as an effective diffusion barrier provided the cell is larger than a certain critical size.

Model description

Full details of the model, including more detailed justifications of the underlying assumptions can be found in the Supplementary Model at JXB online. In the following, we provide a brief decription of its main features. Our model focuses exclusively on cell processes that involve CO2 and O2, namely their absorption, production, and diffusion. We look at a single spherical Bienertia mesophyll cell, formed of three concentric compartments (Fig. 1b): ‘the core’, ‘the vacuole’, and ‘the periphery’. Their sizes are defined by their radii, ri, rv, and re, respectively. We model these regions as follows:

  • (i) The core region (i.e. the CCC) is composed of mitochondria and Rubisco-rich chloroplasts. CO2 is produced in the mitochondria through decarboxylation of malate by NAD-ME and as a photorespiratory by-product. We assume little or no CA in the core cytoplasm (Offermann et al., 2015), so CO2–bicarbonate conversion can be neglected. CO2 can diffuse out of the core region, or react with Rubisco (active site concentration cR), which we assume is always primed with RuBP and activated. O2 is also produced in the core by PSII in the core chloroplasts, and can react with Rubisco, triggering the photorespiratory cycle reactions.

  • (ii) The vacuole combines both the tonoplast interior and the cytoplasmic channels. CO2 and O2 diffuse freely here, and no reactions take place.

  • (iii) The periphery cytoplasm is rich in CA and PEPC (active site concentration cP) (Voznesenskaya et al., 2002; Offermann et al., 2015). Inorganic carbon will predominantly be in bicarbonate form, which is used by PEPC to carboxylate PEP. Diffusion of CO2 and O2 between the surrounding airspace and the cell periphery is hampered by the cell wall and membrane (permeability σB), which form the only diffusion barrier in the model.

Although the cell is conceptually divided into three distinct spatial compartments, no intracellular diffusion barriers are placed between these regions. This is a deliberate choice to test the viability of the C4 pump when there is nothing but a spatial separation to provide diffusive resistance to gases in the liquid phase. We note that Bienertia mesophyll cells are not actually spherical. However, since we are interested in the general effects of size on the efficiency of a C4 pathway, a simpler model (which is also more amenable to numerical investigation) will suffice.

The enzymatic reactions follow Michaelis–Menten kinetics. Since detailed kinetic data for Bienertia’s Rubisco are not presently available, we use kinetic parameters for maize (Zea mays) (Cousins et al., 2010), a well-studied C4 plant. When assessing temperature dependence, we also use the data for another C4 plant, Setaria viridis (Boyd et al., 2015), to infer Rubisco’s temperature response. PEPC and NAD-ME kinetic parameters are taken from Z. mays and Arabidopsis thaliana, respectively (Kai et al., 1999; Tronconi et al., 2008). Values of all the parameters are listed in Table 1 and their temperature dependence in Supplementary Table S1.

Table 1.

Parameter values used for modelling C4 photosynthesis at 20 °C

Description Symbol Units Value
Rubisco active sites concentration in the core c R mM Variable
Rubisco carboxylation catalysis rate (Cousins et al., 2010) k catC s–1 4.7
Rubisco oxygenation catalysis rate (Cousins et al., 2010) k catO s–1 0.49
Rubisco Michaelis concentration for CO2 (Cousins et al., 2010) K C µM 16.2
Rubisco Michaelis concentration for O2 (Cousins et al., 2010) K O µM 183
PEPC concentration in the periphery c P mM Variable
PEPC carboxylation catalysis rate (Kai et al., 1999) k catP s–1 150
PEPC Michaelis constant for HCO3 (Kai et al., 1999) K P µM 100
NAD-ME decarboxylation catalysis rate (Tronconi et al., 2008) k catN s–1 37.6
NAD-ME Michaelis constant for malate (Tronconi et al., 2008) K M µM 300
Diffusion constant for carbon dioxide (Mazarei and Sandall, 1980) D C µm2 s–1 1800
Diffusion constant for oxygen (Mazarei and Sandall, 1980) D O µm2 s–1 1800
Combined permeability of the cell wall and plasma membrane σB µm s–1 Variable
Concentration of dissolved CO2 in equilibrium with air at 20 °C c Ceq µM 15.4
and standard atmospheric pressure (with 400 ppm of CO2) (Carroll et al., 1991)
Concentration of dissolved O2 in equilibrium with air c Oeq µM 284
at 20 °C and standard atmospheric pressure (Murray and Riley, 1969)
Radius of the core r i µm Variable
Radius of the vacuole r v µm Variable
Radius of the cell r e µm Variable
Base photon cost of RuBP regeneration (Zhu et al., 2010) φC 1 8
Base photorespiration photon cost (Zhu et al., 2010) φO 1 9
Base cost of pyruvate-to-PEP conversion (Zhu et al., 2010) φC4 1 4

The model implicitly assumes that other reactions of the C4 cycle, and those involving Rubisco (activation and RuBP binding), as well as the light intake by PSI and PSII, are not rate limiting. This also implies that the base C3 substrate (alanine), as well as the C4 product (aspartate), are abundant within the cell—a necessary condition for optimal functioning of the C4 pathway in any case. We do not model bicarbonate kinetics explicitly, only modelling dissolved CO2. This is justified, because HCO3 can only equilibrate with CO2 in the periphery, where CA is present, and their interconversion elsewhere will be negligible (Heinhorst et al., 2006; Johnson, 1982; see Supplementary Model for details).

We solve a set of partial differential equations for the radial concentrations of CO2 and O2, cC(r) and cO(r), respectively, under steady-state conditions. The C3/C4 acid currents and the O2 production are determined by flux balance conditions. Namely, the CO2 production in the core must match the photorespiratory activity and the rate of the PEPC carboxylation in the periphery, while the O2 production has to match NADPH requirements of the Calvin–Benson cycle and photorespiration.

The efficiency of carbon fixation is expressed in terms of the photon cost (the inverse of the quantum yield) associated with assimilation. This is the minimal number of photons (measured per carbon atom assimilated) that need to be collected by PSI and PSII to cover the ATP and NADPH requirements of the Calvin–Benson cycle, the photorespiration, and the C4 pump operation (Farquhar et al., 1980; Zhu et al., 2010; Kramer and Evans, 2011). To analyse the effects of cell geometry on the photosynthetic efficacy, we always optimize the C4 pump reaction kinetics; that is, for given compartment radii, we find the concentration of PEPC in the periphery for which the photon cost is minimized. If the optimal cost is achieved at a non-vanishing PEPC concentration, we can say that the C4 photosynthetic pathway is a viable and preferable alternative to C3-only photosynthesis for the selected cell geometry.

We emphasize that the comparison of the C3 and C4 pathway efficiencies is always made for the Bienertia-like cell geometry. The architecture of mesophyll cells in C3 plants is different (Tholen and Zhu, 2011), and such mesophyll cells would probably outperform Bienertia-like C3 cells of equal size. Our aim is instead to find the minimal mesophyll cell size above which a plant using a single-cell C4 pump (in Bienertia-like cell geometry) is certain to benefit from its use.

Results

The model has several parameters that can affect the photosynthetic efficiency: the radii of the three compartments, ri, rv, and re, the PEPC concentration in the periphery, cP, the concentration of Rubisco active sites in the core, cR, and the cell barrier (wall and membrane) permeability, σB. To study the model in depth, we initially examine the system’s behaviour at a particular Rubisco concentration and cell barrier permeability. The value of cR=2 mM is in line with general estimates of the Rubisco active site concentration within chloroplast stroma (2–5 mM) (von Caemmerer, 2000), allowing for the fact that the core also contains mitochondria. Estimates of the permeability of the cell wall and cell membrane vary over two orders of magnitude (Terashima et al., 2006; Evans et al., 2009). We set σB=100 µm s–1, but also investigate the effects of varying σB (and cR) in a later section. With the PEPC concentration optimized for minimal photon cost, only the geometrical parameters remain. We fix the thickness of the peripheral layer, rerv to 5 µm (it should not be much wider than the width of a peripheral chloroplast). Reasonable variation in the peripheral thickness will not affect the results as variation in the PEPC concentration will compensate. Two parameters remain: the core radius, ri, and the periphery to core distance (i.e. the depth of the surrounding vacuole), rvri. We investigate Beinertia’s assimilation efficiency in a geometry space defined by these two parameters.

Optimal PEPC concentration and photon cost

Figure 2a shows the optimal PEPC concentration, cPopt (the concentration at which the photon cost is minimized), as a function of ri and rvri. For corresponding NAD-ME concentrations, see Supplementary Fig. S1. Three distinct regions are visible. Cells with small cores, ri ~6 µm, fall in a ‘C3 region’, where cPopt=0, so the system prefers to deactivate the C4 pump and function as a C3 plant. At the other extreme is the region where the optimal PEPC concentration is unbounded (i.e. the C4 cycle works best when PEPC is present in abundance). [Our numerical method can produce a finite PEPC solution for cP up to ~2 mM. Where no photon cost minimum is found in this range, we use the abundant-cP solution (see Supplementary Model) to evaluate the minimal photon cost.] The photon cost in this case essentially levels off for cP >1 mM, so above this value the actual concentration of PEPC will be constrained by other factors. In this ‘abundant-PEPC regime’, the concentration of dissolved inorganic carbon in the periphery will be negligible, as the periphery effectively absorbs all CO2 diffusing into it from the cell exterior and the vacuole. Between these two regions is an intermediate regime where the minimal photon cost is found at finite PEPC concentration, cPopt. Figure 2b shows how the photon cost changes with PEPC concentration in these three regions, with the photon cost minimum at zero, finite, and infinite PEPC concentration, respectively.

Fig. 2.

Fig. 2.

C4-optimized PEPC levels. (a) Optimal PEPC concentration as a function of the core radius, ri, and the periphery to core distance, rvri, for a cell at 20 °C with Rubisco concentration of cR=2 mM and cellular barrier permeability of σB=100 μm. Other parameters are as in Table 1. Level lines are in white. The abundant PEPC region, which appears white, has PEPC concentration >1 mM; the black region on the left is the C3 region, with zero PEPC concentration. (b) Dependence of the photon cost on PEPC concentration, cP, at three exemplary points in different regions of (a), with co-ordinates ri=5.5 μm, 10.5 μm, and 12.6 μm, and rvri=26 μm. Arrows mark the positions of the photon cost minima (i.e. the optimal PEPC concentrations) in the three cases (discussed in the text).

Figure 3 shows how the C4-optimized photon cost (i.e. the minimal cost obtained under optimal C4 pump operational conditions) depends on the core radius, ri, and the periphery to core distance, rvri. This photon cost ‘landscape’ showcases the main results of this study. In the C3 region, the optimal photon cost rises as ri increases, due to the increasing ratio of oxygenation to carboxylation as Rubisco becomes starved of CO2 in the enlarging core. Around ri ~6 μm (the exact point depending on the periphery to core distance), we cross into the C4 region and the photon cost starts to decrease as the C4 pump becomes operational and its activity (i.e. the PEPC concentration cPopt) rises. Here we are entering a ‘valley’ in the photon cost landscape—as once we cross into the abundant PEPC region, the photon cost again starts to increase with ri due to rising photorespiration (see later). The bottom of this elongated valley (marked by a red line in Fig. 3) roughly coincides with the border between the regions of finite and abundant cPopt. We shall refer to this valley bottom as the ‘optimal-geometry line’ as it determines the minimal photon cost (and the corresponding optimal core radius) achievable at a particular periphery to core distance (or cell size). The depth and shape of the photon cost valley can be more clearly seen in the constant rvri cross-section profiles of the photon cost landscape in Fig. 4. The valley is fairly shallow, but the difference between the C3 pathway and the C4 pathway costs at the same cell geometry [i.e. at a given point (ri, rvri) within the valley] is large. The C4-optimized photon cost within the valley is ~3–4 photons per CO2 higher when compared with the cost for very small ri in the C3 region (however, there is a limit to how small a CCC can become, and values of ri < 3 μm are not realistic). The valley is not present at small cell sizes (i.e. for small rvri), but only forms at cell radii re above ~25 μm. We can compare the position of the valley on Fig. 3 with the dimensions of mature Bienertia cells and their central compartments. Measured CCC radii range from 10 µm (B. kavirense) (Akhani et al., 2012) to 16 µm (B. sinuspersici) (Akhani et al., 2005). Bienertia cells are only approximately spherical, and their major and minor dimensions can differ substantially. As a representative measure, we take half the largest reported width (26 µm, in B. cycloptera; Akhani, et al., 2005) and half the shortest length (41 µm, in B. kavirense; Akhani et al., 2012) as our reference cell radii re range. These ranges (light blue parallelogram in Fig. 3) nicely encompass the early part of the optimal-geometry line.

Fig. 3.

Fig. 3.

C4-optimized photon cost as a function of the core radius, ri, and the periphery to core distance, rvri. The lines of constant photon cost are in white. The red line traces the local minima (in ri) of the C4-optimized photon cost. Dashed black lines mark boundaries between regions where the optimum cost is found at zero, finite, and abundant PEPC concentration (compare Fig. 2a, also see the main text). The light-blue parallelogram shows the measured range of a mature Bienertia cell and CCC sizes (from Akhani et al., 2005, 2012). Parameters are as in Fig. 2.

Fig. 4.

Fig. 4.

Photon cost variation with core radius. (a) C4-optimized photon cost as a function of the core radius, ri, for a choice of fixed periphery to core distances, rvri. The dashed black line shows the C3-only pathway cost at a medium rvri of 18 μm; it has negligible dependence on the periphery to core distance. (b) Breakdown of the C4-optimized photon cost into the costs connected with the operation of the Calvin–Benson, the photorespiratory, and the C4 cycle (green, orange, and blue), for the line in (a) with rvri=26 μm. The red line shows the C3 pathway photon cost at the same cell geometry. The dotted blue line shows the photon cost when the C4 pump runs with PEPC in abundance (in the finite-PEPC region this cost is not optimal). The vertical dotted line marks the position of the optimal-geometry line (the red line in Fig. 3). Parameters are as in Fig. 2.

Typical radial profiles of the CO2 and O2 concentration in the cell are shown in Fig. 5. A substantial spatial variation in the CO2 concentration is visible. In the C3 region of the parameter space, CO2 is partially depleted in the core. Turning on the C4 pump leads to an increase in the core CO2 concentration, which can surpass the external dissolved CO2 concentration (i.e. the concentration of dissolved CO2 at equilibrium with the partial CO2 pressure in the surrounding air) by several-fold. On the other hand, the concentration of CO2 in the periphery decreases, and the periphery becomes depleted of inorganic carbon when we enter the abundant PEPC regime. The O2 concentration also varies spatially, but to a lesser extent. It is highest in the core, where it is produced by the Hill reaction.

Fig. 5.

Fig. 5.

CO2 and O2 concentration profiles. Radial profiles of carbon dioxide (a) and oxygen (b) concentration for a fixed periphery to core distance, rvri=26 μm, and varying core radii, ri. Selected radii correspond to the C3 region (ri=4.5 μm, blue), finite PEPC region (ri=8.5 μm, green), and abundant PEPC (ri=12.5 μm, 16.5 μm, red and light-blue respectively). Distances are scaled by the cell radius, re. The dashed, dotted, and full vertical lines mark the ri, rv, and re radii. Parameters are as Fig. 2.

CO2 concentration and leakage

Figure 6a shows the C4-optimized CO2 concentration at the cell centre, relative to the external dissolved concentration [cC (r=0)/cCeq]), as a function of core radius, ri, and the periphery to core distance, rvri. The central CO2 concentration is maximal (from 2- to 7-fold higher than the external dissolved CO2 concentration) along the finite–abundant PEPC boundary, close to the optimal-geometry line. This is expected, since a high concentration of CO2 around Rubisco reduces the photorespiratory losses as O2 is outcompeted. However, the high CO2 concentration in the centre will also result in increased CO2 leakage from the core region, and correspondingly in an increase in the fraction of wasted C4 pump cycles (i.e. the futile cycles). The CO2 leakage, shown in Fig. 6b, is thus also maximal along the finite–abundant PEPC border, and is highest at small core radii and periphery to core separations.

Fig. 6.

Fig. 6.

CO2 concentration and leakage. (a) Concentration of CO2 in the cell centre relative to the external dissolved concentration (i.e. the concentration of dissolved CO2 in equilibrium with air at standard atmospheric pressure and 20 °C, cC (r=0)/cCeq, as a function of ri and rvri. (b) CO2 leakage from the cell core as a proportion of the C4 pump current. The optimal-geometry line is marked light-blue. Other lines are as in Fig. 3. Parameters are as in Fig. 2.

What determines the finite–abundant PEPC border? Or, why is the C4 pump operation ‘scaled back’ in the finite PEPC region? If we decrease the core radius while within the abundant PEPC region, the central CO2 concentration will rise, as the release of the carbon collected at the periphery is concentrated in a smaller volume. This quenches photorespiration but incurs increasingly high pump running costs as CO2 leakage from the core intensifies. At some critical ri—which defines the finite–abundant PEPC border—the cost of shuttling back leaked carbon cannot be compensated by further reduction in photorespiration, and the C4-optimized cost (at smaller ri) is achieved by throttling down the C4 pump (i.e. by lowering the PEPC concentration)—leading to a decrease in the central CO2 concentration and reduced leakage. As the activity of the Hill process is dictated by requirements for reducing power, the O2 concentration in the centre displays a similar, though less pronounced trend (Supplementary Fig. S2).

The trade-off between lower photorespiration and increased CO2 leakage can be best seen in Fig. 4b, which shows the breakdown of the total photon cost into its Calvin–Benson cycle (RuBP regeneration), photorespiration, and C4 pump components, along a fixed periphery to core distance (see also Supplementary Fig. S3). Optimization of the photon cost is accomplished by reducing photorespiration—minimized at the finite–abundant PEPC region border—even if it means using up to 40% of the collected photons to run the C4 pump. The CO2 leakage along the optimal-geometry line does not exceed 36% (Fig. 6b), in accordance with experimental observations (von Caemmerer et al., 2014). Hence, we may conclude that even a modest spatial separation (≥10 µm) between the locations of carboxylation and decarboxylation in an optimized C4 pathway suffices to constrain the leakage to acceptable levels (i.e. physical diffusion barriers are not necessary).

Variations of the model

The findings presented in previous sections are surprisingly robust to changes in the model parameters, and qualitative features generally remain fully preserved. Changing the position of mitochondria within the central compartment (Supplementary Fig. S10), changing the type or concentration of Rubisco in the core region (Supplementary Figs S11, S12), changing the CO2 concentration in the surrounding airspace (Supplementary Fig. S13), and even changing the surrounding environment from air to water (Supplementary Fig. S14) merely result in some, mostly minor, changes to the photon cost. These variations are addressed in the Discussion. In the following, we examine the influence of the two parameters that show the most pronounced impact on the photosynthetic efficiency. These are the ambient temperature and the permeability of the cell’s boundary.

Varying the ambient temperature

Temperature dependence is relevant because C4 photosynthesis is generally—and for Bienertia in particular—an adaptation to arid and hot climates. An increase in temperature causes a rise in Rubisco activity, but reduces its carboxylation to oxygenation specificity, making carbon-concentrating mechanisms all the more beneficial (Boyd et al., 2015). Many parameters used in the model will change with temperature. Unfortunately, in many cases, the temperature dependence is unknown. We use reasonable (but tentative) conjectured temperature dependencies. These are provided, together with their justification, in Supplementary Table S1.

Figure 7ac shows how the photon cost landscape changes with temperature. The cost rises with temperature, and the photon cost valley shifts to smaller core radii; this can be explained by the combination of a lower Rubisco specificity and a higher ratio of dissolved O2 to CO2 at a higher temperature, which makes it necessary to concentrate the CO2 intake from the cell surface into a smaller core volume. The photon cost also rises with temperature in the C3 region of the landscape, becoming equal to or larger than its value in the C4 valley region. C4 photosynthesis thus becomes a winning strategy across the landscape at higher temperatures.

Fig. 7.

Fig. 7.

Temperature dependence of C4 photosynthesis. (a–c) C4-optimized photon cost landscapes at ambient temperatures of 10, 30, and 40 °C, plotted as Fig. 3 (20 °C). (d) and (e) Comparisons of the CO2 leakage, photon cost, and assimilation rates at two fixed cell geometries at various temperatures. The three compartment radii in (d) and (e) are marked on the left-most tricolour meters, and can be read on the left y-axis. The values of other quantities are to be read on the right y-axis. The comparison in (d) is taken at a point in the photon cost landscape that lies on the optimal-geometry line at 20 °C, with a photon cost (at 20 °C) of 15 photons per CO2. The comparison in (e) is taken at a point that lies on the optimal-geometry line at 30 °C, with a photon cost (at 30 °C) of 15.5 photons per CO2. The first point lies within the observed range of Bienertia cell dimensions; the second is positioned slightly outside this range. The CO2 leakage is zero at 10°C because both points lie within the C3 region of the photon cost landscape at that temperature. Parameters are as in Supplementary Table S1.

To ascertain the temperature response of an individual plant, in Fig. 7d, e we make a comparison of photosynthetic efficacy measures at a fixed cell geometry (assuming that a cell can ‘throttle’ its C4 pump, by adjusting its PEPC and NAD-ME levels, in response to a temperature change, so as to optimize its photosynthetic efficiency at that temperature). The comparison is made at two points in the photon cost landscape, each lying on an optimal-geometry line at a particular temperature (20 °C in Fig. 7d and 30 °C in Fig. 7e). The photon cost at a fixed cell geometry grows steadily with temperature, but the CO2 leakage, as well as the carbon assimilation rate (see Discussion), is maximal at the temperature at which the particular cell geometry lies on the optimal-geometry line. An increase in temperature, beyond the value at which a plant’s cell geometry is optimal, results in increased Rubisco activity leading to more RuBP carboxylation (and thus to lower CO2 leakage), but also to more RuBP oxygenation (and thus more photorespiration), which lowers the net carbon assimilation rate and increases the photon cost. The CO2 leakage, which is often used as a proxy for estimating the efficacy of C4 photosynthesis (lower leakage translating to better performance), is thus in fact maximized under optimal photosynthesis conditions. A reduction in CO2 leakage with an increase in temperature has been reported in multiple experiments (Kubien et al., 2003; Stutz et al., 2014; von Caemmerer et al., 2014). Our model suggests that this reduction may be a consequence of an adaptive re-optimization of C4 biochemistry in plants that optimally photosynthesize at a lower temperature.

Varying the permeability of the cell boundary

The optimal-geometry line and the photon cost valley in Fig. 7 move entirely out of the observed range of central compartment and cell sizes at temperatures beyond 30 °C, seemingly bringing into question the model’s accuracy or the assumption that the photon cost is the major selective pressure. However, the photon cost can also vary significantly with the permeability of the cell boundary. In Fig. 8 the combined cell wall and membrane permeability, σB, is varied across two orders of magnitude, covering the range of estimates in the literature (Terashima et al., 2006; Evans et al., 2009). (Note also that the occlusion of internal airspace by other mesophyll cells translates to a lower effective permeability of the cell barrier.) Lowering σB to 10 µm s–1 leads to a large shift of the C4 region in the photon cost landscape towards larger periphery to core distances (i.e. thicker vacuoles), placing the predicted size of a C4 pathway-utilizing organism completely outside the observed range (Fig. 8a). The reason for this shift is that the CO2 concentration in the centre (Supplementary Fig. S4) is significantly reduced due to the lower CO2 intake at the cell surface, which is limited by σB. Achieving the necessary level of CO2 concentration to quench photorespiration properly—and so make the C4 pump profitable—now requires a larger surface area, hence a larger cell. Increasing the permeability to 1000 µm s–1, on the other hand, leads to a shift of the abundant-PEPC region toward larger core radii (Fig. 8c). This shift is due to the higher maximal CO2 intake at the cell’s surface, which allows for efficient photorespiration quenching even when the C4 pump is not running at full capacity, expanding the region of the finite-PEPC regime.

Fig. 8.

Fig. 8.

C4-optimized photon cost landscapes for three values of the cell boundary permeability. (a) σB=10 μm s–1; (b) σB=102 μm s–1 (as Fig. 3); (c) σB=103 μm s–1. Lines are as in Fig. 3. Other parameters are as in Fig. 2.

The position of the photon cost valley and the optimal-geometry line in these two extreme cases is far from the observed range of the central compartment and cell sizes for Bienertia. The effective permeability of the cell boundary (taking the occlusion by other mesophyll cells into account) can thus be no lower than ~102 µm s–1, as that would lead to an exorbitantly high photon cost. Increasing the permeability substantially beyond 102 µm s–1 also takes the optimal-geometry line outside the observed size range (Fig. 8c), but we cannot conclusively reject a high (103 µm s–1) permeability value, since the effect mingles with the effects of temperature variation: at 40 °C the high-end permeability estimate places the optimal-geometry line back into the observed sizes range (Supplementary Fig. S5). Because of the conjectural nature of our temperature dependency forecasts, this cannot serve as a definite indicator of the actual value of the cell boundary permeability, but it is clear from Fig. 8 and Supplementary Fig. S5 that increasing σB results in an efficiency boost in the case of single-cell C4 photosynthesis.

Discussion

We have developed a spatial model of single-cell C4 photosynthesis in a cellular geometry typical of Bienertia mesophyll cells. It includes the key enzymes of the C4 pathway (the primary carboxylase PEPC, and the final decarboxylase NAD-ME), Rubisco carboxylation and oxygenation kinetics, a streamlined photorespiratory cycle, and O2 production via the Hill process. The model allowed us to quantify the efficacy of C4 photosynthesis and to examine the influence of various factors on the efficiency of the C4 pump. We demonstrated that the Bienertia mesophyll cell geometry allows for a functional and frugal C4 photosynthetic pathway provided the cell is sufficiently large. It can then accommodate a sizeable core compartment with sufficient separation from the peripheral cytoplasm. There is an optimal core size for a given cell size, that minimizes the carbon fixation cost. A C4 pump in cells with a thus optimized geometry is an evolutionarily stable advantage against small perturbations in cell dimensions since the photon cost landscape has a valley. The pathway’s efficiency, expressed in terms of the photon cost of carbon fixation, rises with a further increase in cell size, although for cells larger than ~50 µm in radius further gains appear to be marginal.

A photon cost of ~14–16 photons per CO2 is achievable for this C4 system (Fig. 3), with the CO2 leakage ranging between 20% and 35% (Fig. 6b). This can be achieved for reasonably sized cells—the photon cost drops to 15 photons per CO2 for cells that are 38 µm in radius, with a 12 µm radius core (Fig. 3). These costs are similar to the lowest costs measured in a number of C4 species, where photon costs under limiting light were estimated to be 13–17 photons absorbed per assimilated CO2 or evolved O2 (Ehleringer and Björkman, 1977; Furbank et al., 1990; Lal and Edwards, 1995). Our model can thus explain how Bienertia’s C4 system achieves an efficacy comparable with that of other C4 plants.

We have shown that the diffusive resistance due to spatial separation can, alone, reproduce the observed levels of CO2 leakage from the core compartment in Bienertia (von Caemmerer et al., 2014). The leakage in the model does not exceed 36%, a value comparable with those measured in Kranz-type C4 plants (Kubásek et al., 2007). Our examination of temperature dependence suggests that, assuming a plant can adjust the levels of the C4 cycle enzymes, CO2 leakage will be maximal at the temperature at which its cellular/leaf anatomy is best adapted for photosynthesis. At higher temperatures, the leakage decreases—a tendency observed in experiments on C4 plants (Kubien et al., 2003; Stutz et al., 2014; von Caemmerer et al., 2014). The increase in carbon assimilation rate, combined with the effective quenching of Rubisco oxygenation activity via carbon-concentrating mechanisms, would provide a vast advantage to C4 pump-utilizing plants at high temperatures. In contrast, at low temperatures a plant would benefit from throttling down the C4 pump or shutting it down completely. In this regard, we note that while the carbon isotope composition analysis of leaf biomass in Bienertia that grew in natural habitats in Central Asia (under high light and warm climate conditions) consistently indicate a C4-type carbon isotope composition (Akhani et al., 2005), the experiments with chamber-grown Bienertia plants suggest that environmental conditions can influence the expression of the C4 pump, the carbon isotope composition ranging from C4 to C3–C4 intermediate values (Stutz et al., 2014).

Based on the energy cost of carbon fixation, the local selection pressure within the photon cost valley would keep the C4 pump operational and select for increasing the size of the cell and of the core region so as to reach and then slide along the optimal-geometry line. On shorter time scales, optimization pressures could also guide a maturing Bienertia mesophyll cell to follow the same path. The valley in the photon cost landscape only appears at cell radii larger than ~25 µm, so a smaller cell would prefer to keep its plastids undifferentiated, utilizing the C3 photosynthetic pathway. Photon cost optimization thus explains why activation of the C4 pump in Bienertia cells occurs only once they reach a certain size [as witnessed in specialization of plastid biochemistry (Voznesenskaya et al., 2005; Park et al., 2009)], but it cannot explain how this cellular architecture evolved in the first place, as there is no continuous evolutionary path of decreasing cost from the C3 to the C4 region in the photon cost landscape. A path of low resistance goes over a ‘hill’ in the landscape at ri ~6 µm. The climb is not steep—the photon cost rises from 12 at ri ~3 µm to <15 at the summit—but this ‘crossing’ is possible only at a large enough rvri, in other words when a cell is already large. Hence, other factors had to contribute to the initial increase in cell size before the improvement of photosynthetic efficacy led to the development of a C4 pathway. It has been suggested that the evolution of the C4 mechanism occurred via intermediates, where the first step in increasing photosynthesis under limiting CO2 was to develop two domains, with photorespired CO2 refixed in the internal domain (‘C2 photosynthesis’) (Sage et al., 2012).

Secondary factors that can be important determinants of a plant’s fitness are the specific carbon assimilation rates, notably the net per-Rubisco assimilation rate and the net assimilation rate per cell volume. The importance of the per-Rubisco assimilation rate stems from the high cost of Rubisco production, which tends to consume a major share of the cell’s resources (it is the most abundant protein in the cell). The per-volume assimilation rate is also important since general cellular maintenance costs grow with cell volume. The two assimilation rates are shown along the optimal-geometry line in Fig. 9. The region of high per-Rubisco assimilation rate matches the location of the photon cost valley (Supplementary Fig. S6a), and the assimilation rate rises along the optimal-geometry line by 40% as the cell’s radius increases from 30 µm to 70 µm. In contrast, the per-volume assimilation rate drops sharply with cell size (Supplementary Fig. S6b). This places an upper limit on the cell size, as the net carbon assimilation rate would have to cover the daily respiratory losses as well as growth demands, which increase with cell size.

Fig. 9.

Fig. 9.

Net carbon assimilation rates per cell volume and per Rubisco enzyme. The assimilation rates are compared along the optimal-geometry line (the red line in Fig. 3). Parameters are as in Fig. 2.

The per-volume assimilation rate is not the only factor that will constrain the maximal cell size. The PEPC requirements in larger cells are another, as the model generally predicts a high PEPC concentration in the C4 valley region. This is consistent with the measured ratio of total PEPC and Rubisco carboxylation capacities in Bienertia mesophyll cells, which is ~5 (von Caemmerer et al., 2014), corresponding to the abundant-PEPC regime in our model. The third limiting factor, which is implicit in the model, is the diffusive transport of C3 and C4 acids between the core and the periphery. This transport has to support the carboxylation current, but is likely to be constrained to narrow cytoplasmic strands penetrating the vacuole (Voznesenskaya et al., 2005), so it may be rate limiting. The fraction of vacuole area covered by the strands is unknown. If a conservative estimate of 1% is assumed, the concentration of C3 acids in the core and C4 acids in the periphery would have to be >100 mM to sustain the predicted carboxylation flux in very large cells (re >70 µm) (Supplementary Fig. S7). Within the region of observed Bienertia cell sizes, however, the required difference in C3 and C4 acid concentrations between the core and the periphery regions would be ≤50 mM, which is comparable with concentration differences found in Kranz anatomy C4 species (Hatch and Osmond, 1976). Photosynthesis may also be constrained by light levels and cyclic versus linear flow balance (Björkman and Demmig-Adams, 1995; Zhu et al., 2008). In particular, the peripheral chloroplasts appear to be PSII deficient (Voznesenskaya et al., 2002), although they seem to retain some capacity for linear electron flow (Offermann et al., 2011). Examination of these concerns (Supplementary Figs S8, S9) shows that, without NADPH production in the periphery, Bienertia mesophyll cells would require very high insolation to achieve the optimal assimilation rate. A co-ordinated energy production between the peripheral and core chloroplasts may be necessary to support C4 photosynthesis, while light availability could be a limiting factor to carbon assimilation rate and to mesophyll cell size in Bienertia.

The main model results are robust to model assumptions and to poorly known parameters. Plasma membrane and cell wall permeability is a key factor in limiting transport of CO2, but is difficult to measure. Our model shows that Bienertia is not viable with permeabilities near the lower end of their estimated range (10 µm s–1), while permeabilities in the mid range of 100 µm s–1 give realistic photon costs at 20 °C, with an optimal geometry close to that observed (Fig. 8). At a higher temperature (~40 °C) those conditions are again satisfied, if a permeability close to the higher end of the estimated range (103 µm s–1) is assumed. The pronounced sensitivity of the photon cost to some of the parameters, notably the cell boundary permeability and the temperature dependence of Rubisco kinetics, shows that more reliable measurements are needed in order to model photosynthesis accurately.

The model assumes a uniform mixture of chloroplasts and mitochondria in the central compartment. The micrographs of Bienertia cells, however, suggest that mitochondria in the CCC are positioned closer to its centre, surrounded by chloroplasts (Voznesenskaya et al., 2002; Park et al., 2009; Lung et al., 2011). To see the impact of mitochondrial positioning, we explored what happens when the mitochondrial release of CO2 is limited to the inner part of the core. Supplementary Fig. S10 shows that the impact is marginal—resulting in approximately half a photon decrease in photon cost—even in an extreme case when the mitochondrial release is constrained to the central 11% of the core region volume. There is little change to the assimilation rate, even though the central CO2 concentration increases by an order of magnitude (Supplementary Fig. S10c). The CO2 leakage is, however, substantially reduced, dropping from 36% to 28% at the start of the optimal-geometry line (Supplementary Fig. S10d). The large drop in CO2 leakage results only in miniscule gains in the photon cost along the optimal-geometry line because photorespiration is already fully suppressed.

Changing the type of Rubisco expressed in the core, from a C4 variety (maize; Cousins et al., 2010) to C3 varieties [such as from spinach (Zhu et al., 1998) or wheat (Cousins et al., 2010)], leads to a minor increase in photon cost of up to 1 photon per CO2, but does not noticeably change the position or the depth of the C4 valley (Supplementary Fig. S11). Changing the concentration of Rubisco in the core moves the position of the optimal-geometry line but does not alter the photon cost at its starting point (Supplementary Fig. S12). The per-volume assimilation rate increases with Rubisco concentration (Supplementary Fig. S12d). The chloroplasts, however, tend to be already fully packed with Rubisco, and mixing them with mitochondria in the core can only lower the effective Rubisco concentration. The cell probably has to establish a fine balance between filling the core with chloroplasts and providing sufficient mitochondria to decarboxylate the incoming malate. Gathering the mitochondria in the inner part of the core, which had little direct impact on photosynthetic efficiency or assimilation rates, may be advantageous in this regard. Another scenario where it might prove beneficial is when, for whatever reason, the C4 pump runs suboptimally and photorespiration is high. The reduced CO2 leakage due to mitochondrial central localization would then translate into more tangible improvements in the photon cost.

Reducing the CO2 concentration in the surrounding airspace (Supplementary Fig. S13) increases the cost of carbon fixation, but also makes the C4 valley deeper, showing that the C4 pump provides a greater advantage under conditions of CO2 deprivation (such as when stomata are closed). Even changing the external environment from air to water, with the corresponding 10 000-fold decrease in the diffusion rate outside the cell (Lugg, 1968; Mazarei and Sandall, 1980), results in little qualitative change in the photon cost landscape (Supplementary Fig. S14). This suggests that a Bienertia-like cell architecture could also provide an evolutionary advantage to aquatic plants. The cells would need to be somewhat larger—the photon cost valley starts at a periphery to core separation of 23 µm. This value is comparable with the general size ranges of single-cell C4 aquatic plants Hydrilla verticillata and Orcuttia viscida (Keeley, 1998; Bowes et al., 2002; von Caemmerer et al., 2014) (though they have a different cell geometry). The same criterion would, however, disqualify the allegedly C4-photosynthesizing diatom Thalassiosira weissflogii (Reinfelder et al., 2000, 2004).

The prospect of introducing a C4 pathway into C3 crop plants has been investigated in recent years, with the aim of enhancing photosynthesis and productivity (von Caemmerer, 2003; Zhu et al., 2010). An approach based on a single-cell C4 cycle is appealing as it circumvents the need to engineer Kranz anatomy into the plant. Our results show that such approaches hold promise, provided that the mesophyll cells are sufficiently large, or can be engineered to be sufficiently large. Targeting PEP carboxylation and malate decarboxylation to specific locations within the cell could then create the required spatial separation. Surprisingly, this separation need not be very large: in our model, the photon cost drops below 15 at periphery to core separations of just over 21 µm—even without imposing any diffusion barriers between the carboxylation and decarboxylation regions. On the other hand, where an adequate spatial separation is not feasible, such as on the level of individual chloroplasts, engineering a C4 pump would not provide any gains.

Supplementary data

Supplementary data are available at JXB online

Supplementary model description

Table S1. Parameter values for modelling C4 photosynthesis at different temperatures.

Figure S1. Optimal PEPC and NAD-ME concentrations.

Figure S2. Oxygen concentration in the cell centre.

Figure S3. Optimized photon cost along the optimal-geometry line.

Figure S4. CO2 concentration in the cell centre at different cell boundary permeabilities.

Figure S5. Photon cost landscape at 40 °C with the cell boundary permeability of 103 µm s–1.

Figure S6. Net carbon assimilation rates.

Figure S7. C4 acid concentration levels needed to drive the C4 pump.

Figure S8. Fraction of the electron current due to cyclic electron flow.

Figure S9. Photosynthetically active photon flux needed to sustain photosynthesis.

Figure S10. Repositioning mitochondria at the centre of the core region.

Figure S11. Comparison of C4 pump efficiency for differing Rubisco enzyme characteristics.

Figure S12. Varying the Rubisco concentration in the core.

Figure S13. Varying the ambient CO2 concentration.

Figure S14. Comparison of water and air environments.

Supplementary Material

Supplementary_Model_S1
Supplementary_Table_S1_Figures_S1_S14

Acknowledgements

This research was supported by the BBSRC project grant BB/M011291/1 and the NSF grants MCB-1359634 and MCB-1146928. We would like to thank Mike Blatt from the University of Glasgow, UK, and others in the 'MAGIC' consortium (http://magic.psrg.org.uk/) for valuable comments.

References

  1. Akhani H, Barroca J, Koteeva N, Voznesenskaya E, Franceschi V, Edwards G, Ghaffari SM, Ziegler H. 2005. Bienertia sinuspersici (Chenopodiaceae): a new species from Southwest Asia and discovery of a third terrestrial C4 plant without Kranz anatomy. Systematic Botany 30, 290–301. [Google Scholar]
  2. Akhani H, Chatrenoor T, Dehghani M, Khoshravesh R, Mahdavi P, Matinzadeh Z. 2012. A new species of Bienertia (Chenopodiaceae) from Iranian salt deserts: a third species of the genus and discovery of a fourth terrestrial C4 plant without Kranz anatomy. Plant Biosystems 146, 550–559. [Google Scholar]
  3. Björkman O, Demmig-Adams B. 1995. Regulation of photosynthetic light energy capture, conversion, and dissipation in leaves of higher plants. In PDE-D Schulze, PDMM Caldwell, eds, Ecophysiology of Photosynthesis, Springer, Berlin Heidelberg. [Google Scholar]
  4. Bowes G, Rao SK, Estavillo GM, Reiskind JB. 2002. C4 mechanisms in aquatic angiosperms: comparisons with terrestrial C4 systems. Functional Plant Biology 29, 379–392. [DOI] [PubMed] [Google Scholar]
  5. Boyd RA, Gandin A, Cousins AB. 2015. Temperature responses of C4 photosynthesis: biochemical analysis of Rubisco, phosphoenolpyruvate carboxylase, and carbonic anhydrase in Setaria viridis. Plant Physiology 169, 1850–1861. [DOI] [PMC free article] [PubMed] [Google Scholar]
  6. Carroll JJ, Slupsky JD, Mather AE. 1991. The solubility of carbon dioxide in water at low pressure. Journal of Physical and Chemical Reference Data 20, 1201. [Google Scholar]
  7. Cousins AB, Ghannoum O, Caemmerer SV, Badger MR. 2010. Simultaneous determination of Rubisco carboxylase and oxygenase kinetic parameters in Triticum aestivum and Zea mays using membrane inlet mass spectrometry. Plant, Cell and Environment 33, 444–452. [DOI] [PubMed] [Google Scholar]
  8. Ehleringer J, Björkman O. 1977. Quantum yields for CO2 uptake in C3 and C4 plants dependence on temperature, CO2, and O2 concentration. Plant Physiology 59, 86–90. [DOI] [PMC free article] [PubMed] [Google Scholar]
  9. Evans JR, Kaldenhoff R, Genty B, Terashima I. 2009. Resistances along the CO2 diffusion pathway inside leaves. Journal of Experimental Botany 60, 2235–2248. [DOI] [PubMed] [Google Scholar]
  10. Farquhar GD, von Caemmerer S, Berry JA. 1980. A biochemical model of photosynthetic CO2 assimilation in leaves of C3 species. Planta 149, 78–90. [DOI] [PubMed] [Google Scholar]
  11. Furbank RT, Jenkins CLD, Hatch MD. 1990. C4 photosynthesis: quantum requirement, C4 and overcycling and Q-cycle involvement. Functional Plant Biology 17, 1–7. [Google Scholar]
  12. Hatch MD, Osmond CB. 1976. Compartmentation and transport in C4 photosynthesis. In: Stocking CR, Heber U, eds. Transport in plants III.Berlin: Springer, 144–184. [Google Scholar]
  13. Heinhorst S, Williams EB, Cai F, Murin CD, Shively JM, Cannon GC. 2006. Characterization of the carboxysomal carbonic anhydrase CsoSCA from Halothiobacillus neapolitanus. Journal of Bacteriology 188, 8087–8094. [DOI] [PMC free article] [PubMed] [Google Scholar]
  14. Jenkins CLD, Furbank RT, Hatch MD. 1989. Mechanism of C4 photosynthesis a model describing the inorganic carbon pool in bundle sheath cells. Plant Physiology 91, 1372–1381. [DOI] [PMC free article] [PubMed] [Google Scholar]
  15. Johnson KS. 1982. Carbon dioxide hydration and dehydration kinetics in seawater. Limnology and Oceanography 27, 849–855. [Google Scholar]
  16. Kai Y, Matsumura H, Inoue T, Terada K, Nagara Y, Yoshinaga T, Kihara A, Tsumura K, Izui K. 1999. Three-dimensional structure of phosphoenolpyruvate carboxylase: a proposed mechanism for allosteric inhibition. Proceedings of the National Academy of Sciences, USA 96, 823–828. [DOI] [PMC free article] [PubMed] [Google Scholar]
  17. Keeley JE. 1998. C4 photosynthetic modifications in the evolutionary transition from land to water in aquatic grasses. Oecologia 116, 85–97. [DOI] [PubMed] [Google Scholar]
  18. King JL, Edwards GE, Cousins AB. 2012. The efficiency of the CO2-concentrating mechanism during single-cell C4 photosynthesis: single-cell C4 photosynthetic efficiency. Plant, Cell and Environment 35, 513–523. [DOI] [PubMed] [Google Scholar]
  19. Kramer DM, Evans JR. 2011. The importance of energy balance in improving photosynthetic productivity. Plant Physiology 155, 70–78. [DOI] [PMC free article] [PubMed] [Google Scholar]
  20. Kubásek J, Šetlík J, Dwyer S, Šantrůček J. 2007. Light and growth temperature alter carbon isotope discrimination and estimated bundle sheath leakiness in C4 grasses and dicots. Photosynthesis Research 91, 47–58. [DOI] [PubMed] [Google Scholar]
  21. Kubien DS, von Caemmerer S, Furbank RT, Sage RF. 2003. C4 photosynthesis at low temperature. a study using transgenic plants with reduced amounts of Rubisco. Plant Physiology 132, 1577–1585. [DOI] [PMC free article] [PubMed] [Google Scholar]
  22. Lal A, Edwards GE. 1995. Maximum quantum yields of O2 evolution in C4 plants under high CO2. Plant and Cell Physiology 36, 1311–1317. [Google Scholar]
  23. Lugg GA. 1968. Diffusion coefficients of some organic and other vapors in air. Analytical Chemistry 40, 1072–1077. [Google Scholar]
  24. Lung S-C, Yanagisawa M, Chuong SDX. 2011. Protoplast isolation and transient gene expression in the single-cell C4 species, Bienertia sinuspersici. Plant Cell Reports 30, 473–484. [DOI] [PubMed] [Google Scholar]
  25. Mazarei AF, Sandall OC. 1980. Diffusion coefficients for helium, hydrogen, and carbon dioxide in water at 25°C. AIChE Journal 26, 154–157. [Google Scholar]
  26. Murray CN, Riley JP. 1969. The solubility of gases in distilled water and sea water—II. Oxygen. Deep Sea Research and Oceanographic Abstracts 16, 311–320. [Google Scholar]
  27. Offermann S, Friso G, Doroshenk KA, Sun Q, Sharpe RM, Okita TW, Wimmer D, Edwards GE, van Wijk KJ. 2015. Developmental and subcellular organization of single-cell C4 photosynthesis in Bienertia sinuspersici determined by large-scale proteomics and cDNA assembly from 454 DNA sequencing. Journal of Proteome Research 14, 2090–2108. [DOI] [PubMed] [Google Scholar]
  28. Offermann S, Okita TW, Edwards GE. 2011. Resolving the compartmentation and function of C4 photosynthesis in the single-cell C4 species Bienertia sinuspersici. Plant Physiology 155, 1612–1628. [DOI] [PMC free article] [PubMed] [Google Scholar]
  29. Park J, Knoblauch M, Okita TW, Edwards GE. 2009. Structural changes in the vacuole and cytoskeleton are key to development of the two cytoplasmic domains supporting single-cell C4 photosynthesis in Bienertia sinuspersici. Planta 229, 369–382. [DOI] [PubMed] [Google Scholar]
  30. Reinfelder JR, Kraepiel AML, Morel FMM. 2000. Unicellular C4 photosynthesis in a marine diatom. Nature 407, 996–999. [DOI] [PubMed] [Google Scholar]
  31. Reinfelder JR, Milligan AJ, Morel FMM. 2004. The role of the C4 pathway in carbon accumulation and fixation in a marine diatom. Plant Physiology 135, 2106–2111. [DOI] [PMC free article] [PubMed] [Google Scholar]
  32. Sage RF. 2004. The evolution of C4 photosynthesis. New Phytologist 161, 341–370. [DOI] [PubMed] [Google Scholar]
  33. Sage RF, Christin P-A, Edwards EJ. 2011. The C4 plant lineages of planet Earth. Journal of Experimental Botany 62, 3155–3169. [DOI] [PubMed] [Google Scholar]
  34. Sage RF, Sage TL, Kocacinar F. 2012. Photorespiration and the evolution of C4 photosynthesis. Annual Review of Plant Biology 63, 19–47. [DOI] [PubMed] [Google Scholar]
  35. Stutz SS, Edwards GE, Cousins AB. 2014. Single-cell C4 photosynthesis: efficiency and acclimation of Bienertia sinuspersici to growth under low light. New Phytologist 202, 220–232. [DOI] [PubMed] [Google Scholar]
  36. Terashima I, Hanba YT, Tazoe Y, Vyas P, Yano S. 2006. Irradiance and phenotype: comparative eco-development of sun and shade leaves in relation to photosynthetic CO2 diffusion. Journal of Experimental Botany 57, 343–354. [DOI] [PubMed] [Google Scholar]
  37. Tholen D, Zhu X-G. 2011. The mechanistic basis of internal conductance: a theoretical analysis of mesophyll cell photosynthesis and CO2 diffusion. Plant Physiology 156, 90–105. [DOI] [PMC free article] [PubMed] [Google Scholar]
  38. Tronconi MA, Fahnenstich H, Weehler MCG, Andreo CS, Flügge U-I, Drincovich MF, Maurino VG. 2008. Arabidopsis NAD-malic enzyme functions as a homodimer and heterodimer and has a major impact on nocturnal metabolism. Plant Physiology 146, 1540–1552. [DOI] [PMC free article] [PubMed] [Google Scholar]
  39. von Caemmerer S. 2000. Biochemical models of leaf photosynthesis. In Techniques in Plant Science, CSIRO, Collingwood. [Google Scholar]
  40. von Caemmerer S. 2003. C4 photosynthesis in a single C3 cell is theoretically inefficient but may ameliorate internal CO2 diffusion limitations of C3 leaves. Plant, Cell and Environment 26, 1191–1197. [Google Scholar]
  41. von Caemmerer S. 2013. Steady-state models of photosynthesis. Plant, Cell and Environment 36, 1617–1630. [DOI] [PubMed] [Google Scholar]
  42. von Caemmerer S, Edwards GE, Koteyeva N, Cousins AB. 2014. Single cell C4 photosynthesis in aquatic and terrestrial plants: a gas exchange perspective. Aquatic Botany 118, 71–80. [Google Scholar]
  43. von Caemmerer S, Furbank RT. 2003. The C4 pathway: an efficient CO2 pump. Photosynthesis Research 77, 191–207. [DOI] [PubMed] [Google Scholar]
  44. von Caemmerer S, Ghannoum O, Pengelly JJL, Cousins AB. 2014. Carbon isotope discrimination as a tool to explore C4 photosynthesis. Journal of Experimental Botany 65, 3459–3470. [DOI] [PubMed] [Google Scholar]
  45. Voznesenskaya EV, Franceschi VR, Kiirats O, Artyusheva EG, Freitag H, Edwards GE. 2002. Proof of C4 photosynthesis without Kranz anatomy in Bienertia cycloptera (Chenopodiaceae). The Plant Journal 31, 649–662. [DOI] [PubMed] [Google Scholar]
  46. Voznesenskaya EV, Franceschi VR, Kiirats O, Freitag H, Edwards GE. 2001. Kranz anatomy is not essential for terrestrial C4 plant photosynthesis. Nature 414, 543–546. [DOI] [PubMed] [Google Scholar]
  47. Voznesenskaya EV, Koteyeva NK, Chuong SDX, Akhani H, Edwards GE, Franceschi VR. 2005. Differentiation of cellular and biochemical features of the single-cell C4 syndrome during leaf development in Bienertia cycloptera (Chenopodiaceae). American Journal of Botany 92, 1784–1795. [DOI] [PubMed] [Google Scholar]
  48. Zhu G, Jensen RG, Bohnert HJ, Wildner GF, Schlitter J. 1998. Dependence of catalysis and CO2/O2 specificity of Rubisco on the carboxy-terminus of the large subunit at different temperatures’. Photosynthesis Research 57, 71–79. [Google Scholar]
  49. Zhu X-G, Long SP, Ort DR. 2008. What is the maximum efficiency with which photosynthesis can convert solar energy into biomass?Current Opinion in Biotechnology 19, 153–159. [DOI] [PubMed] [Google Scholar]
  50. Zhu X-G, Long SP, Ort DR. 2010. Improving photosynthetic efficiency for greater yield. Annual Review of Plant Biology 61, 235–261. [DOI] [PubMed] [Google Scholar]

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