Leaf-wax n-alkanes record the plant-water environment at leaf flush

Leaf-wax n-alkanes H-2/H-1 ratios are widely used as a proxy in climate reconstruction. Although the broad nature of the relationship between n-alkanes delta H-2 values and climate is appreciated, the quantitative details of the proxy remain elusive. To examine these details under natural environmental conditions, we studied a riparian broadleaf angiosperm species, Populus angustifolia, growing on water with a constant delta H-2 value and monitored the delta H-2 values of leaf-wax n-alkanes and of stem, leaf, stream, and atmospheric waters throughout the entire growing season. Here we found the delta H-2 values of leaf-wax n-alkanes recorded only a 2-wk period during leaf flush and did not vary for the 19 weeks thereafter when leaves remained active. We found delta H-2 values of leaf-wax n-alkanes of P. angustifolia record conditions earlier in the season rather than fully integrating the entire growing season. Using these data, we modeled precipitation delta H-2 values during the time of wax synthesis. We observed that the isotope ratios of this precipitation generally were H-2-enriched compared with mean annual precipitation. This model provides a mechanistic basis of the often-observed H-2-enrichment from the expected fractionation values in studies of broadleaf angiosperm leaf-wax delta H-2. In addition, these findings may have implications for the spatial and temporal uses of n-alkane delta H-2 values in paleoapplications; when both plant community and growth form are known, this study allows the isolation of the precipitation dynamics of individual periods of the growing season.