The fate and path of assimilation products in the stem of 8-year-old Scots pine (Pinus sylvestris L.) trees

Summary

¹⁴CO₂ at ambient concentration was administered to a section of an upper branch of 8-year-old Scots pines and the import of radiocarbon into the stem and roots was determined after various chase periods. ¹⁴CO₂ fixation was performed in October when export of carbon into the stems and roots was maximal. In the short-term experiments the trees were harvested 1 h, 2 days and 5 days after a 3-h ¹⁴C pulse, while chase periods of 5 or 8 months were used in the long-term experiments. Loss of ¹⁴C was initially substantial, and even after a 5-day chase had not come down to a rate which indicated decrease only by respiration. After 5 days, more than 10% of the recovered radiocarbon (53% of the ¹⁴C translocated into the stem) had entered the roots and approximately the same amount was found in the stem. Extension of the chase period beyond 5 months did not result in a further significant loss of ¹⁴C by respiration, and the bulk of the label could be localized in the cell-wall fraction. No substantial redistribution of radiocarbon prior and subsequent to the formation of the new shoots could be observed, thus indicating that the stored material was utilized for thickening the stem and roots. Radioautography of stem cross-sections revealed a narrow helical strip of ¹⁴C from the feeding branch to the root in the phloem region. In the tree harvested after bud break the utilization of the ¹⁴C-labelled material stored in the stem for the production of the first layers of earlywood and the corresponding phloem was apparent.