Figure 2 | Scientific Reports

Figure 2

From: Different hydrogen isotope fractionations during lipid formation in higher plants: Implications for paleohydrology reconstruction at a global scale

Figure 2

Variations in leaf water and corresponding leaf wax δDn-alkane values.

Variations of leaf water and corresponding leaf wax δDn-alkane values on whole leaves from Xi’an, Lantian and Binxian (a). Treatment on segmented leaf sections conducted from base to tip in monocotyledonous leaves and in base-to-tip and center-to-margin directions in dicotyledonous leaves, resulting difference in εwax-lw between dicotyledonous and monocotyledonous species. The difference in εwax-lw values derived from the quality-weighted mean εwax-lw values from segmented leaves was responsible for the difference in leaf wax δDn-alkane values of whole leaf (b). Conceptual diagram illustrating a model of hydrogen isotope transformation in terrestrial plants. The transformation comprises two processes: D-enrichment by evapotranspiration and D-depletion by biosynthetic processes10. The veinal structures inside the leaves (veinal water pathways, green box) control the isotopic gradients of leaf water and corresponding leaf wax (c).

Back to article page