Carbon-dioxide exchange in lichens: determination of transport and carboxylation characteristics

Measurements were made of net rates of CO₂ assimilation in lichens at various ambient concentrations of CO₂ in air and in helox (79% He, 21% O₂). Because of the faster rate of CO₂ diffusion in the pores of lichen thalli when filled with helox than when filled with air, a given net rate of assimilation was achieved at a lower ambient concentration of CO₂ in helox. The differences were used to estimate resistances to diffusion through the gas-filled pore systems in lichens. The technique was first tested with five lichen species, and then applied in a detailed study with Ramalina maciformis, in which gas-phase resistances were determined in samples at four different states of hydration and with two irradiances. By assuming, on the basis of previous evidence, that the phycobiont in R. maciformis is fully turgid and photosynthetically competent at the smallest hydration imposed (equilibration with vapour at 97% relative humidity), and that, with this state of hydration, diffusion of CO₂ to the phycobiont takes place through continuously gas-filled pores, it was possible also to determine both the dependence of net rate of assimilation in the phycobiont on local concentration of CO₂ in the algal layer, and, with the wetter samples, the extents to which diffusion of CO₂ to the phycobiont was impeded by water films. In equilibrium with air of 97% relative humidity, the thallus water content being 0.5 g per g dry weight, the resistance to CO₂ diffusion through the thallus was about twice as large as the resistance to CO₂ uptake within the phycobiont. Total resistance to diffusion increased rapidly with increase in hydration. At a water content of 2 g per g it was about 50 times as great as the resistance to uptake within the phycobiont and more than two-thirds of it was attributable to impedance of transfer by water. The influences of water content on rate of assimilation at various irradiances are discussed. The analysis shows that the local CO₂ compensation concentration of the phycobiont in R. maciformis is close to zero, indicating that photorespiratory release of CO₂ does not take place in the alga, Trebouxia sp., under the conditions of these experiments.Symbols and Units rate of CO₂ diffusion in air relative to that in carrier gas (unity if the carrier gas is air and 0.43 if is helox) - A₁ net rate of CO₂ uptake by the lichen - A_p gross rate of carboxylation minus photorespiratory decarboxylation in the phycobiont, i.e. net rate of light-activated CO₂ exchange - A_* maximum, CO₂-saturated magnitude of A_p - c concentration of CO₂ - c_a ambient concentration of CO₂ - c_i c_a minus difference in CO₂ concentration across air-filled pore space in the thallus - c₈ CO₂ concentration equivalent to partial pressure of CO₂ at the surface of the phycobiont - ₁ magnitude of c_a at which A₁ = 0 - _* magnitude of c_* at which A_p = 0 - R rate of dark respiration in the lichen (mycobiont and phycobiont) - R rate of dark respiration in region between the surface of the lichen and an arbitrary distance from the surface within the thallus - r resistance to CO₂ transfer from lichen surface to the surface of the phycobiont - r resistance to CO₂ transfer between effective source of dark respiration in the lichen and the surface of the phycobiont - r_g, r_g components of r and r, respectively, attributable to transfer in air-phase - r_w, r_w components of r and r, respectively, attributable to transfer in water-phase - r component of r between surface of lichen and an arbitrary distance from the surface within the thallus - r_* resistance to CO₂ transfer and carboxylation in the phycobiont - RH relative humidity