Eddy covariance captures four‐phase crassulacean acid metabolism (CAM) gas exchange signature in Agave

Mass and energy fluxes were measured over a field of Agave tequilana in Mexico using eddy covariance (EC) methodology. Data were gathered over 252 d, including the transition from wet to dry periods. Net ecosystem exchanges (F_N,EC) displayed a crassulacean acid metabolism (CAM) rhythm that alternated from CO₂ sink at night to CO₂ source during the day, and partitioned canopy fluxes (F_A,EC) showed a characteristic four‐phase CO₂ exchange pattern. Results were cross‐validated against diel changes in titratable acidity, leaf‐unfurling rates, energy exchange fluxes and reported biomass yields. Projected carbon balance (g C m^?2 year^?1, mean ± 95% confidence interval) indicated the site was a net sink of ?333 ± 24, of which contributions from soil respiration were +692 ± 7, and F_A,EC was ?1025 ± 25. EC estimated biomass yield was 20.1 Mg (dry) ha^?1 year^?1. Average integrated daily F_A,EC was ?234 ± 5 mmol CO₂ m^?2 d^?1 and persisted almost unchanged after 70 d of drought conditions. Regression analyses were performed on the EC data to identify the best environmental predictors of F_A. Results suggest that the carbon acquisition strategy of Agave offers productivity and drought resilience advantages over conventional semi‐arid C3 and C4 bioenergy candidates.