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Preserved lignin structures in early eocene Surat lignites,Cambay Basin,Western India
Authors:Suryendu Dutta  Sanket Bhattacharya  Monalisa Mallick  Ashish Chandra Shukla  Ulrich Mann
Affiliation:(1) Department of Palaeontology, Royal Belgian Institute of Natural Sciences, rue Vautier 29, 1000 Brussels, Belgium;(2) Department of Geology, H.N.B. Garhwal University, Srinagar, 246175, Uttaranchal, India;(3) Aspirant FWO Vlaanderen, Research Unit of Palaeontology, University of Ghent, Krijgslaan 281-S8, 9000 Ghent, Belgium;(4) Center for Functional Anatomy and Evolution, Johns Hopkins University School of Medicine, Baltimore, MD 21205, USA;(5) Centre of Advanced Study in Geology, Panjab University, Chandigarh, 160014, India;(6) Birbal Sahni Institute of Palaeobotany, 53 University Road, Lucknow, 226007, India
Abstract:Lignite samples from Vastan and Tadkeshwar lignite mines, Cambay Basin have been analysed to elucidate lignin precursor using thermochemolysis-gas chromatography-mass spectrometry. The thermochemolysis products of lignites are characterized by monomethoxy-, dimethoxy-, and trimethoxybenzene derivatives originated from p-hydroxyphenyl, guaiacyl, and syringyl units of lignin polymer, respectively. The other compounds obtained in thermochemolysates of studied lignites are some resin derived C15 sesquiterpenoids, with a series of fatty acid methyl esters and n-alkanes/alkenes. The methylated guaiacyl and syringyl derivatives originate from the cleavage of β-O-4 linkages and subsequent methylation of acidic hydroxyl groups of preserved lignin. Gymnosperm lignin is characterized mainly by guaiacyl derivatives whereas angiosperm lignin yields some syringyl-type compounds in addition to guaiacyl-type compounds. By analogy with the lignin structure of modern trees, the abundant occurrences of syringyl derivatives in the thermochemolysis products of Surat lignites clearly demonstrate that the palaeofloral community was dominated by angiosperms during the deposition of these lignites.
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