A dynamic hydro-mechanical and biochemical model of stomatal conductance for C4 photosynthesis

C 4 plants are major grain (maize [ Zea mays ] and sorghum [ Sorghum bicolor ]), sugar (sugarcane [ Saccharum officinarum ]), and biofuel ( Miscanthus spp.) producers and contribute ∼20% to global productivity. Plants lose water through stomatal pores in order to acquire CO 2 (assimilation [ A ]) and control their carbon-for-water balance by regulating stomatal conductance ( g S ). The ability to mechanistically predict g S and A in response to atmospheric CO 2 , water availability, and time is critical for simulating stomatal control of plant-atmospheric carbon and water exchange under current, past, or future environmental conditions. Yet, dynamic mechanistic models for g S are lacking, especially for C 4 photosynthesis. We developed and coupled a hydromechanical model of stomatal behavior with a biochemical model of C 4 photosynthesis, calibrated using gas-exchange measurements in maize, and extended the coupled model with time-explicit functions to predict dynamic responses. We demonstrated the wider applicability of the model with three additional C 4 grass species in which interspecific differences in stomatal behavior could be accounted for by fitting a single parameter. The model accurately predicted steady-state responses of g S to light, atmospheric CO 2 and oxygen, soil drying, and evaporative demand as well as dynamic responses to light intensity. Further analyses suggest that the effect of variable leaf hydraulic conductance is negligible. Based on the model, we derived a set of equations suitable for incorporation in land surface models. Our model illuminates the processes underpinning stomatal control in C 4 plants and suggests that the hydraulic benefits associated with fast stomatal responses of C 4 grasses may have supported the evolution of C 4 photosynthesis.