Carbon allocation to major metabolites in illuminated leaves is not just proportional to photosynthesis when gaseous conditions (CO2 and O2) vary. Issue 1 (18th January 2018)

• Record Type: Journal Article
• Authors: Abadie, Cyril; Bathellier, Camille; Tcherkez, Guillaume
• Is Part Of: New phytologist. Volume 218:Issue 1(2018)
• Page Start: 94
• Page End: 106
• Publication Date: 2018-01-18
• Subjects: carbon allocation -- labelling -- nitrogen assimilation -- nuclear magnetic resonance (NMR) -- photorespiration -- photosynthesis; Botany -- Periodicals; 580
• DOI: 10.1111/nph.14984
• Languages: English
• ISSNs: 0028-646X

Abstract

Summary: In gas‐exchange experiments, manipulating CO2 and O2 is commonly used to change the balance between carboxylation and oxygenation. Downstream metabolism (utilization of photosynthetic and photorespiratory products) may also be affected by gaseous conditions but this is not well documented. Here, we took advantage of sunflower as a model species, which accumulates chlorogenate in addition to sugars and amino acids (glutamate, alanine, glycine and serine). We performed isotopic labelling with 13 CO2 under different CO2 /O2 conditions, and determined 13 C contents to compute 13 C‐allocation patterns and build‐up rates. The 13 C content in major metabolites was not found to be a constant proportion of net fixed carbon but, rather, changed dramatically with CO2 and O2 . Alanine typically accumulated at low O2 (hypoxic response) while photorespiratory intermediates accumulated under ambient conditions and at high photorespiration, glycerate accumulation exceeding serine and glycine build‐up. Chlorogenate synthesis was relatively more important under normal conditions and at high CO2 and its synthesis was driven by phospho enol pyruvate de novo synthesis. These findings demonstrate that carbon allocation to metabolites other than photosynthetic end products is affected by gaseous conditions and therefore the photosynthetic yield of net nitrogen assimilation varies, being minimal at high CO2 and maximal at high O2 .