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Interaction of Nitrate Assimilation and Photorespiration at Elevated CO2

Konrad Krämer, Judith Brock, Arnd G. Heyer

2022Frontiers in Plant Science21 citationsDOIOpen Access PDF

Abstract

It has been shown repeatedly that exposure to elevated atmospheric CO 2 causes an increased C/N ratio of plant biomass that could result from either increased carbon or – in relation to C acquisition - reduced nitrogen assimilation. Possible reasons for diminished nitrogen assimilation are controversial, but an impact of reduced photorespiration at elevated CO 2 has frequently been implied. Using a mutant defective in peroxisomal hydroxy-pyruvate reductase ( hpr1-1 ) that is hampered in photorespiratory turnover, we show that indeed, photorespiration stimulates the glutamine-synthetase 2 (GS) / glutamine-oxoglutarate-aminotransferase (GOGAT) cycle, which channels ammonia into amino acid synthesis. However, mathematical flux simulations demonstrated that nitrate assimilation was not reduced at elevated CO 2 , pointing to a dilution of nitrogen containing compounds by assimilated carbon at elevated CO 2 . The massive growth reduction in the hpr1-1 mutant does not appear to result from nitrogen starvation. Model simulations yield evidence for a loss of cellular energy that is consumed in supporting high flux through the GS/GOGAT cycle that results from inefficient removal of photorespiratory intermediates. This causes a futile cycling of glycolate and hydroxy-pyruvate. In addition to that, accumulation of serine and glycine as well as carboxylates in the mutant creates a metabolic imbalance that could contribute to growth reduction.

Topics & Concepts

PhotorespirationNitrogen assimilationGlutamine synthetaseNitrogen cycleNitrate reductaseAssimilation (phonology)BiochemistryNitrateRuBisCOAmmoniaChemistrySerineMetabolismGlycineGlutamineAlaninePhotosynthesisNitrogenBiologyAmino acidEnzymeEcologyPhilosophyOrganic chemistryLinguisticsPhotosynthetic Processes and MechanismsPlant nutrient uptake and metabolismPlant responses to elevated CO2
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