Modeling acclimation of leaf photosynthesis to atmospheric CO2 enrichment

Publication Type

Journal contribution (peer reviewed)

Authors

Biernath, C.J., Bittner, S., Klein, C., Gayler, S., Hentschel, R., Hoffmann, P., Högy, P., Fangmeier, A., Priesack, E.

Year of publication

2013

Published in

European Journal of Agronomy

Band/Volume

48/

DOI

10.1016/j.eja.2013.02.008

Page (from - to)

74-87

In this study, we developed and analyzed a new model for the simulation of  photosynthetic active nitrogen (NP ) turnover dynamics in crops and assessed  its impact on the acclimation of canopy photosynthesis to atmospheric CO2 enrichment. Typical canopy models assume a vertical exponential decline of  light interception following the Beer-Lambert law and vertical distributions of  leaf NP contents directly proportional to the light distribution. This assumption  is often inconsistent with experimental observations. We therefore modified and extended the photosynthesis model of the GECROS crop model to consider the trade-off that occurs between the use of degraded NP for plant growth and the synthesis of new NP. This model extension thus enabled the examination of the CO2-induced down-regulation of photosynthesis hypothesis using a crop model. The simulation results of the original and modified GECROS model were compared and evaluated based upon measurements of field-grown spring wheat. The modified GECROS model better simulated the dynamics of crop growth under varying atmospheric CO2 concentrations. Furthermore, the application of different temperature functions to NP degradation strongly influenced the simulation results, revealing the necessity for improving the understanding of the temperature dependence of NP turnover for different crop species and varieties. In conclusion, the redistribution of nitrogen within the plant and its alternative use either for growth or the optimization of the photosynthetic apparatus is an important mechanism for crop growth acclimation to regionally changing climatic conditions and in particular, atmospheric CO2 enrichment.