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Chemical characterization of Lower Devonian vascular plants
Authors:Greg Ewbank  Dianne Edwards  Geoffrey D Abbott
Institution:1Fossil Fuels and Environmental Geochemistry (Postgraduate Institute): NRG, Drummond Building, University of Newcastle upon Tyne, Newcastle upon Tyne, NE1 7RU, U.K.;2Department of Geology, University of Wales, College of Cardiff, P.O. Box 914, Cardiff, CF1 3YE, U.K.
Abstract:Vegetative remains of three coalified Lower Devonian vascular plants (Zosterophyllum, Psilophyton, Renalia) were analyzed using flash pyrolysis-gas chromatography-mass spectrometry. The distributions of pyrolysis products are compared with those from younger vascular plant fossil xylem (Cordaixylon, Callixylon) and cuticle (Pachypteris). The likelihood of the chemical preservation of characteristic higher plant macromolecules (e.g., lignin and cutan) in the Lower Devonian plant fossils is considered in light of this comparison and associated thermal maturity assessments. Reflectance values from vitrinite-like macerals, which may not be vitrinite sensu stricto in the Lower Devonian host rocks for the fossils selected for this study, are shown to provide a reasonable assessment of the thermal maturity of these early vascular plant fossils. Although lignin altered through burial maturation is the most likely source of the prominent alkylphenols and aromatic hydrocarbons in the Lower Devonian tracheophyte flash pyrolysates, a contribution from thermally modified tannins cannot be ruled out. Comparison of the highly aliphatic pyrolysates from the Zosterophyllum and Psilophyton axes with that of a thermally mature fossil gymnosperm leaf revealed that cutan was an important component in the Devonian plant remains. This is the earliest chemical evidence for the presence of cutan in vascular plants.
Keywords:Lower Devonian plants  vascular plant evolution  fossil wood  fossil leaves  lignin  cutan  flash pyrolysis
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