Abstract

Stomata regulate leaf CO2 assimilation (A) and water loss. The Ball–Berry and Medlyn models predict stomatal conductance (g s) with a slope parameter (m or g 1) that reflects the sensitivity of g s to A, atmospheric CO2 and humidity, and is inversely related to water use efficiency (WUE). This study addressed knowledge gaps about what the values of m and g 1 are in C4 crops under field conditions, as well as how they vary among genotypes and with drought stress. Four inbred maize genotypes were unexpectedly consistent in how m and g 1 decreased as water supply decreased. This was despite genotypic variation in stomatal patterning, A and g s. m and g 1 were strongly correlated with soil water content, moderately correlated with predawn leaf water potential (Ψpd), but not correlated with midday leaf water potential (Ψmd). This implied that m and g 1 respond to long‐term water supply more than short‐term drought stress. The conserved nature of m and g 1 across anatomically diverse genotypes and water supplies suggests there is flexibility in structure‐function relationships underpinning WUE. This evidence can guide the simulation of maize g s across a range of water supply in the primary maize growing region and inform efforts to improve WUE.

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