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Insights into preservation of fossil plant cuticles using thermally assisted hydrolysis methylation
Authors:Anne-Marie Aucour  Pierre Faure  Bernard Gomez  Yann Hautevelle  Raymond Michels  Frédéric Thévenard
Affiliation:1. Laboratoire des Sciences de la Terre, CNRS-UMR 5570, Ecole Normale Supérieure de Lyon, Université Lyon 1, 2 rue Dubois, 69622 Villeurbanne Cedex, France;2. Géologie et Gestion des Ressources Minérales et Energétiques (G2R), UMR 7566, Nancy Université, CNRS BP 239, 54506 Vandoeuvre-les-Nancy Cedex, France;3. Paléoenvironnements Paléobiosphère (PEPS), CNRS-UMR 5125, Université Lyon 1, 7 rue Dubois, 69622 Villeurbanne Cedex, France;4. Géologie et Gestion des Ressources Minérales et Energétiques (G2R), UMR 7566, Nancy Université, CNRS BP 40, 54506 Vandoeuvre-les-Nancy Cedex, France
Abstract:The chemical composition of Cretaceous leaf remains showing exceptionally well preserved cuticles was investigated using pyrolysis gas chromatography–mass spectrometry (Py-GC–MS) and thermally assisted hydrolysis methylation (THM)-GC–MS. Samples of Coniferales (Frenelopsis) and Ginkgoales (Nehvizdya penalveri) leaf remains were collected from freshwater and coastal marine depositional environments. Material for pyrolysis included (i) untreated leaves and cuticles obtained after extraction from mineral rock matrix and bleaching, (ii) kerogen fraction from both materials, (iii) non-hydrolysable fraction from kerogen. The THM-GC–MS data from untreated leaves and bleached cuticles show that the fossil cuticle geopolymer essentially released aliphatic components upon thermal treatment, with a dominance of fatty acids (FAs) and n-alkanes/n-alkenes. The FAs are essentially resistant to bleaching and remain after solvent extraction. They occur mainly as short chain compounds ranging from C6 to C16 and with maximum abundance at C8–C9. The n-alkanes/n-alkenes from kerogen and the non-hydrolysable residue occur mainly as short chain compounds in the range C10–C16, with the highest abundance at C9–C12. The THM-GC–MS pyrograms of the fossil cuticles differ from those of cutan from fresh living plants. They support the preservation model via polymerization of monomers derived from cutin or from unsaturated cell FAs.
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