Metabolic origin of the δ13C of respired CO2 in roots of Phaseolus vulgaris

Abstract

• Root respiration is a major contributor to soil CO2 efflux, and thus an important component of ecosystem respiration. But its metabolic origin, in relation to the carbon isotope composition (δ13C), remains poorly understood. • Here, 13C analysis was conducted on CO2 and metabolites under typical conditions or under continuous darkness in French bean (Phaseolus vulgaris) roots. 13C contents were measured either under natural abundance or following pulse-chase labeling with 13C-enriched glucose or pyruvate, using isotope ratio mass spectrometer (IRMS) and nuclear magnetic resonance (NMR) techniques. • In contrast to leaves, no relationship was found between the respiratory quotient and the δ13C of respired CO2, which stayed constant at a low value (c. -27.5‰) under continuous darkness. With labeling experiments, it is shown that such a pattern is explained by the 13C-depleting effect of the pentose phosphate pathway; and the involvement of the Krebs cycle fueled by either the glycolytic input or the lipid/protein recycling. The anaplerotic phosphoenolpyruvate carboxylase (PEPc) activity sustained glutamic acid (Glu) synthesis, with no net effect on respired CO2. • These results indicate that the root δ13C signal does not depend on the availability of root respiratory substrates and it is thus plausible that, unless the 13C photosynthetic fractionation varies at the leaf level, the root δ13C signal hardly changes under a range of natural environmental conditions. © The Authors (2008).