Root xylem CO2 flux: an important but unaccounted-for component of root respiration

Root respiration has been considered a large component of forest soil CO2 efflux, but recent findings indicate that it may be even more important than previous measurements have shown because a substantial fraction of root-respired CO2 remains within the tree root system and moves internally with the transpiration stream. The high concentration of CO2 in roots appears to originate mainly within the root. It has been suggested that plants can take up dissolved inorganic carbon (DIC) from soil, but under most conditions uptake from soil is minimal due to the root-to-soil diffusion gradient, which suggests that most of the CO2 in root xylem is derived from root respiration. Estimates of the internal flux of CO2 through root xylem are based on combined measurements of sap flow and internal [CO2]. Results quantifying root xylem CO2 flux, obtained for a limited number of species, have raised important concerns regarding our understanding of tree respiration. Taken together, the results of these studies call into question the partitioning of ecosystem respiration into its above- and belowground components, and redefine the energetic costs of tree root metabolism and hence estimates of belowground carbon allocation. Expanding our observations of root xylem CO2 flux to more species and at longer time scales, as well as improving the techniques used to study this process, could be fruitful avenues for future research, with the potential to substantially revise our understanding of root respiration and forest carbon cycles.