Quantifying isotope parameters associated with carbonyl‐water oxygen exchange during sucrose translocation in tree phloem

Summary Stable oxygen isotope ratio of tree‐ring α‐cellulose (δ 18 O cel) yields valuable information on many aspects of tree–climate interactions. However, our current understanding of the mechanistic controls on δ 18 O cel is incomplete, with a knowledge gap existent regarding the fractionation effect characterizing carbonyl‐water oxygen exchange during sucrose translocation from leaf to phloem. To address this insufficiency, we set up an experimental system integrating a vapor 18 O‐labeling feature to manipulate leaf‐level isotopic signatures in tree saplings enclosed within whole‐canopy gas‐exchange cuvettes. We applied this experimental system to three different tree species to determine their respective relationships between 18 O enrichment of sucrose in leaf lamina (Δ 18 O lₛuc) and petiole phloem (Δ 18 O phlₛuc) under environmentally/physiologically stable conditions. Based on the determined Δ 18 O phlₛuc ‐Δ 18 O lₛuc relationships, we estimated that on average, at least 25% of the oxygen atoms in sucrose undergo isotopic exchange with water along the leaf‐to‐phloem translocation path and that the biochemical fractionation factor accounting for such exchange is c. 34‰, markedly higher than the conventionally assumed value of 27‰. Our study represents a significant step toward quantitative elucidation of the oxygen isotope dynamics during sucrose translocation in trees. This has important implications with respect to improving the δ 18 O cel model and its related applications in paleoclimatic and ecophysiological contexts.