Biogenic volatile organic compound and respiratory CO₂ emissions after ¹³C-labeling: Online tracing of C translocation dynamics in poplar plants

Background: Globally plants are the primary sink of atmospheric CO₂, but are also the major contributor of a large spectrum of atmospheric reactive hydrocarbons such as terpenes (e.g. isoprene) and other biogenic volatile organic compounds (BVOC). The prediction of plant carbon (C) uptake and atmospheric oxidation capacity are crucial to define the trajectory and consequences of global environmental changes. To achieve this, the biosynthesis of BVOC and the dynamics of C allocation and translocation in both plants and ecosystems are important. Methodology: We combined tunable diode laser absorption spectrometry (TDLAS) and proton transfer reaction mass spectrometry (PTR-MS) for studying isoprene biosynthesis and following C fluxes within grey poplar (Populus x canescens) saplings. This was achieved by feeding either ¹³CO₂ to leaves or ¹³C-glucose to shoots via xylem uptake. The translocation of ¹³CO₂ from the source to other plant parts could be traced by ¹³C-labeled isoprene and respiratory ¹³CO₂ emission. Principal Finding: In intact plants, assimilated ¹³CO₂ was rapidly translocated via the phloem to the roots within 1 hour, with an average phloem transport velocity of 20.3±2.5 cm h^-1. ¹³C label was stored in the roots and partially reallocated to the plants' apical part one day after labeling, particularly in the absence of photosynthesis. The daily C loss as BVOC ranged between 1.6% in mature leaves and 7.0% in young leaves. Non-isoprene BVOC accounted under light conditions for half of the BVOC C loss in young leaves and one-third in mature leaves. The C loss as isoprene originated mainly (76-78%) from recently fixed CO₂, to a minor extent from xylem-transported sugars (7-11%) and from photosynthetic intermediates with slower turnover rates (8-11%). Conclusion: We quantified the plants' C loss as respiratory CO₂ and BVOC emissions, allowing in tandem with metabolic analysis to deepen our understanding of ecosystem C flux.