Skip to main page content
U.S. flag

An official website of the United States government

Dot gov

The .gov means it’s official.
Federal government websites often end in .gov or .mil. Before sharing sensitive information, make sure you’re on a federal government site.

Https

The site is secure.
The https:// ensures that you are connecting to the official website and that any information you provide is encrypted and transmitted securely.

Access keys NCBI Homepage MyNCBI Homepage Main Content Main Navigation
. 2016 Jan 25:6:19711.
doi: 10.1038/srep19711.

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

Affiliations

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

Jinzhao Liu et al. Sci Rep. .

Abstract

Leaf wax δDn-alkane values have shown to differ significantly among plant life forms (e.g., among grasses, shrubs, and trees) in higher plants. However, the underlying causes for the differences in leaf wax δDn-alkane values among different plant life forms remain poorly understood. In this study, we observed that leaf wax δDn-alkane values between major high plant lineages (eudicots versus monocots) differed significantly under the same environmental conditions. Such a difference primarily inherited from different hydrogen biosynthetic fractionations (εwax-lw). Based upon a reanalysis of the available leaf wax δDn-alkane dataset from modern plants in the Northern Hemisphere, we discovered that the apparent hydrogen fractionation factor (εwax-p) between leaf wax δDn-alkane values of major angiosperm lineages and precipitation δD values exhibited distinguishable distribution patterns at a global scale, with an average of -140‰ for monocotyledonous species, -107‰ for dicotyledonous species. Additionally, variations of leaf wax δDn-alkane values and the εwax-p values in gymnosperms are similar to those of dicotyledonous species. Therefore, the data let us believe that biological factors inherited from plant taxonomies have a significant effect on controlling leaf wax δDn-alkane values in higher plants.

PubMed Disclaimer

Figures

Figure 1
Figure 1. Whole leaf hydrogen isotope compositions from various sites in Northwestern China showing distinct difference in leaf wax δDn-alkane values between dicotyledonous species and monocotyledonous species.
Samples were from Lantian (site 1) and Xi’an (site 2) and from the Heshui County (b).
Figure 2
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 processes. The veinal structures inside the leaves (veinal water pathways, green box) control the isotopic gradients of leaf water and corresponding leaf wax (c).
Figure 3
Figure 3. Leaf wax δDn-alkane values in living angiosperms along a latitudinal gradient in the North Hemisphere.
Comparisons of leaf wax δDn-alkane values (n = 233) between herbaceous plants and woody plants, and the precipitation average δD were presented as δD = −0.037 × (latitude)2 + 1.1674 × (latitude) −35.423 from Liu and Yang (2008) (a). Comparisons between monocotyledonous and dicotyledonous species based on our expanded database (n = 503). Notice, the observed higher δDn-alkane values in Stiffkey saltmarsh (Eley et al., 2014) may be due to the fact that samples were obtained from a salt marsh (b). The parallel εwax-p values in dicotyledonous and monocotyledonous species are insensitive to variations of precipitation δD values, suggesting different biosynthetic processes between eudicots and monocots (c).
Figure 4
Figure 4. Geographic map showing sample sites in Heshui, Lantian and Xi’an and the distribution of compiled modern leaf wax δDn-alkane values of higher plants across the North hemisphere.
Black rectangles are data based upon Liu and Yang, (2008); red dots are additional data points. (Fig. 4 was created by CorelDRAW 12; My co-authors and I grant NPG to publish the image under an Open Acess license; We grant NPG to publish the image in all formats i.e. print and digital).

References

    1. Eglinton G. & Hamilton R. J. Leaf epicuticular waxes. Science 156, 1322–1335 (1967). - PubMed
    1. Bush R. T. & McInerney F. A. Leaf wax n-alkane distributions in and across modern plants: Implications for paleoecology and chemotaxonomy. Geochim. Cosmochim. Acta 117, 161–179 (2013).
    1. Yang H. & Huang Y. S. Preservation of lipid hydrogen isotope ratios in Miocene lacustrine sediments and plant fossils at Clarkia, northern Idaho, USA. Org. Geochem. 34, 413–423 (2003).
    1. Smith F. A., Wing S. L. & Freeman K. H. Magnitude of carbon isotope excursion at the Paleocene-Eocene thermal maximum: the role of plant community change. Earth Planet. Sci. Lett. 262, 50–65 (2007).
    1. Hou J. Z., William J. D. & Huang Y. S. Can sedimentary leaf waxes record D/H ratio of continental precipitation ? Field, model, and experimental assessments. Geochim. Cosmochim. Acta 72, 3503–3517 (2008).

LinkOut - more resources