“…The distributions of the aromatic compounds in metamorphic samples show a similar pattern characterized by the predominance of bibenzyl (I), 1-methyl-2-[(3-methylphenyl)methyl]benzene (IV), 1-methyl-3-[(4-methylphenyl)methyl]benzene (V), cadalene (VI) and 2,3-dihydro-1,1,3-trimethyl-3-phenyl 1H-indene (VII). Bibenzyl (I), derivate products of indene, ethylene naphthalene and hydrogenated aromatic hydrocarbons are observed in hydrous pyrolysis products from coal and oil (e.g., Spiteller and Jovanović, 1999;Jovanović et al, 2002;Nuzzi and Marcandalli, 2003). The cadalene-type sesquiterpenoids (compounds III and VI) are associated with a terrestrial plant origin (Albaiges et al, 1984) and are thought to be formed by reductive processes, probably by decarboxylation of the resin fatty acid precursors linked to the kerogen (Otto and Simoneit, 2002) with concurrent hydrogenation and oxidation leading to the aromatic counterparts (cadalene; VI).…”