“…Early diagenesis of terrestrial organic matter from higher plants, in modern sediments, peat, lignite, etc., is one of focuses in geological research (Cranwell, 1985;Del Rio et al, 1992;Dehmer, 1995;Pancost et al, 2002;Hajje and Jaffe, 2006), in which some important discoveries about aliphatic hydrocarbons from higher plants have been reported: n-alkanes mainly originate from cuticle waxes and alcohols in higher plants and the dominance of long chain n-alkanes with odd carbon number predominance can indicate higher plant origin (Dehmer, 1995). Terpenoids are common constituents of the resins of higher plants, and they are important biomarkers for higher plants, especially for conifers.…”