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The main coal forming element in the peat paleoswamp of the Middle Miocene ‘Chukurovo’ lignite is Taxodiaceae (paleobotanical observation). The great preponderance of diterpenoids in the resinite is a chemical confirmation for the presence of coniferous vegetation in the paleoplant taxa. Subordinate quantities of the sesquiterpenoids cuparene, valencene and cadalene types and longifolane are present...
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