Seasonal contribution of C3 and C4 species to ecosystem respiration and photosynthesis estimated from isotopic measurements of atmospheric CO2 at a grassland in Japan

Measurements of δ¹³C in atmospheric CO₂ and plant samples were made in 2003, along with CO₂ flux measurements, at a grassland site in Tsukuba in central Japan. The objective of the study was to obtain estimates of relative seasonal contributions of C₃ and C₄ plants to the net CO₂ flux over a C₃/C₄ grassland area influenced by the Asian monsoon. C₄ contribution to the ecosystem respiration (f_4R) increased from June to September, and then became constant at 63–67% through October and November. The seasonal variation in f_4R reflected the biomass composition of C₃ and C₄ plants at the measurement site. The seasonal C₄ contribution to photosynthesis (f_4P) was significantly different from its contribution to f_4R in May (8%) while it showed similar values to f_4R after June. The seasonal variations in f_4R and f_4P reflect the biomass composition ratio. Such seasonal transition from C₃ to C₄ of relative contribution to the carbon flux is similar to that observed in humid prairie ecosystems, while it is different from that in dry prairie ecosystems where the contribution of C₃ plants is lower and the seasonal maximum of the C₄-plant contribution occurs earlier compared to the humid prairie ecosystems.