Drivers of intra-seasonal δ 13 C signal in tree-rings of Pinus sylvestris as indicated by compound-specific and laser ablation isotope analysis.

Carbon isotope composition of tree-ring (δ 13 C Ring ) is a commonly used proxy for environmental change and ecophysiology. δ 13 C Ring reconstructions are based on a solid knowledge of isotope fractionations during formation of primary photosynthates (δ 13 C P ), such as sucrose. However, δ 13 C Ring is not merely a record of δ 13 C P . Isotope fractionation processes, which are not yet fully understood, modify δ 13 C P during sucrose transport. We traced, how the environmental intra-seasonal δ 13 C P signal changes from leaves to phloem, tree-ring and roots, for 7 year old Pinus sylvestris, using δ 13 C analysis of individual carbohydrates, δ 13 C Ring laser ablation, leaf gas exchange and enzyme activity measurements. The intra-seasonal δ 13 C P dynamics was clearly reflected by δ 13 C Ring , suggesting negligible impact of reserve use on δ 13 C Ring . However, δ 13 C P became increasingly 13 C-enriched during down-stem transport, probably due to post-photosynthetic fractionations such as sink organ catabolism. In contrast, δ 13 C of water-soluble carbohydrates, analysed for the same extracts, did not reflect the same isotope dynamics and fractionations as δ 13 C P , but recorded intra-seasonal δ 13 C P variability. The impact of environmental signals on δ 13 C Ring , and the 0.5 and 1.7‰ depletion in photosynthates compared ring organic matter and tree-ring cellulose, respectively, are useful pieces of information for studies exploiting δ 13 C Ring .