The magnitude of diurnal variation in carbon isotopic composition of leaf dark respired CO2 correlates with the difference between δ13C of leaf and root material
Spatial and temporal variations in δ13C of dark respired CO2 (δ13Cres) and total and water-soluble organic matter (WSOM) were analysed in four plant species. There was an increase in δ13Cres over the light period (measured 5 min after darkening) in leaves, whereas no distinct diurnal pattern was detected in roots. Furthermore, large differences in δ13Cres were found along the plant axis during day time. The amount of daily δ13Cres enrichment in leaves relative to the putative substrate (WSOM) varied largely between species (3.2–15.9‰), probably due to different carbon allocation strategies. Positional pyruvate labelling was used to detect whether variations in δ13Cres were related to changes in the relative activity of pyruvate dehydrogenase (PDH) and Krebs cycle (KC). The results indicate that one reason for the increase in δ13Cres in leaves during daylight is an increasing carbon flux through the PDH relative to the KC. Labelling experiments revealed no clear diurnal variations in PDH and KC activity in roots. Further, we found new evidence that the fractionation process that leads to the diurnal δ13C increase in leaf dark respiration is related to the well known 13C depletion of leaf material compared with heterotrophic tissues.