Carbon Acquisition Mechanisms of Algae: Carbon Dioxide Diffusion and Carbon Dioxide Concentrating Mechanisms
Carbon Acquisition Mechanisms of Algae: Carbon Dioxide Diffusion and Carbon Dioxide Concentrating Mechanisms
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DOI:
10.1007/978-94-007-1038-2_11
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发表时间:
2003
期刊:
影响因子:
--
通讯作者:
J. Raven;J. Beardall
中科院分区:
文献类型:
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作者:
J. Raven;J. Beardall
At least 95% ofthe organic carbon in cyanobacteria and algae has been fixed as CO2by Rubisco. The kinetic properties of Rubisco are such that even the genetic variants with the highest CO2: 02selectivity would show limited CO2fixation and significant oxygenase activity if CO2and 02 fluxes into cells are driven solely by diffusion. This is especiallythe case for submerged algae with lowgas diffusion coefficients relative to diffusion boundary layer thicknesses. There is evidence from gas exchange properties and intracellular inorganic concentration that inorganic carbon concentrating mechanisms (CCMs) function in all cyanobacteria and many algae. CCMs can, in theory, operate through three categories of mechanism: the first mechanism is active transport of HCOj and/or CO2across membranes, the second is CO2pumping by a biochemical mechanism analogous to C4 and CAM (Crassulacean Acid Metabolism) pathways in higher land plants, and the third mechanism involves active transport of H+ producing an acid compartment supplied with HCOj, which generates a high (equilibrium) CO2concentration that supplies CO2to Rubisco in a nearby more alkaline compartment. Most evidence favors the first mechanism as being responsible for CCM activity in algae. The CO2 (and HCOj) permeability of membranes is crucial in defining the extent of inorganic C leakage from CCMs, and the functioning ofdiffusive CO2supply to Rubisco from the medium. Like carbonic anhydrases, CCMs, are probably polyphyletic.