Simulation of C1 fluxes in cyanobacteria: comparison between the carboxysome hypothesis and the equilibrium proposal
Inorganic carbon fluxes were simulated by a mathematical model using an equilibrium hypothesis for a wide range of conditions in a closed system composed of air-grown cells of Synechococcus UTEX 625 in a reaction vessel connected to a mass spectrometer. The metabolic scheme took into account the input fluxes of CO2 and HCO3− transport into the cells, the output fluxes of CO2 and HCO3− efflux, the diversion of Q toward the formation of the internal C2 pool, and photosynthetic CO2 fixation. The equations expressed the variation in concentration of each inorganic species outside and inside the cell as a function of time. The input fluxes were previously characterized by their kinetic constants (K1/2 and Vm) both during initial uptake occurring upon illumination of the cells and under steady-state photosynthesis conditions. The efflux rates of the various Ci species from the cells were investigated under a wide variety of experimental conditions. Using these efflux rates, the permeability coefficients of the cell for CO2 and HCO3− were calculated previously. Using the kinetic constants for CO2 and HCO3− transport, the permeability coefficients of the cell for CO2 and HCO3− and the geometrical characteristics of the cells, the model simulated precisely the [HCO3−]/[CO2] ratio and the [CO2] and [O2] changes in the extracellular medium as well as the rate of filling of the internal Ci pool under various conditions. Accurate fitting of experimental data with calculated values were possible only when the intracellular Ci species were assumed to be in equilibrium throughout the entire cell volume. Results are discussed and compared with those given by previous hypotheses. Key words: Synechococcus UTEX 625, blue green algae, cyanobacteria, mathematical model, active CO2 transport, active HCO3− transport, steady state, photosynthesis, Ci concentrating mechanism.