Abstract

Here we present δ 13C and δ 2H data of long-chained, even-numbered (C 27–C 31) n-alkanes from C3 (trees) and C4 (grasses) plants and from the corresponding soils from a grassland–woodland vegetation sequence in central Queensland, Australia. Our data show that δ 13C values of the C4 grassland species were heavier relative to those of C3 tree species from the woodland ( Acacia leaves) and woody grassland ( Atalaya leaves). However, n-alkanes from the C4 grasses had lighter δ 2H values relative to the Acacia leaves, but showed no significant difference in δ 2H values when compared with C3 Atalaya leaves. These results differ from those of previous studies, showing that C4 grasses had heavier δ 2H values relative to C3 grasses and trees. Those observations have been explained by C4 plants accessing the more evaporation-influenced and isotopically heavier surface water and tree roots sourcing deeper, isotopically lighter soil water (“Two-layered soil–water system”). By comparison, our data suggest that ecosystem changes (vegetation “thickening”) can significantly alter the soil hydrological characteristics. This is shown by the heavier δ 2H values in the woodland soil compared with lighter δ 2H values in the grassland soil, implying that the recent vegetation change (increased tree biomass) in the woodland had altered soil hydrological conditions. Estimated δ 2H values of the source-water for vegetation in the grassland and woodland showed that both trees and grasses in open settings accessed water with lighter δ 2H values (avg. −46‰) compared with water accessed by trees in the woodland vegetation (avg. −7‰). These data suggest that in semi-arid environments the “two-layer” soil water concept might not apply. Furthermore, our data indicate that compound-specific δ 2H and δ 13C analyses of n-alkanes from soil organic matter can be used to successfully differentiate between water sources of different vegetation types (grasses versus trees) in natural ecosystems.

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