Bulletin of the Geological Society of Greece Vol. 36, 2004 MOLECULAR INDICATORS FOR TAXODIUM DUBIUM AS COAL PROGENITOR OF "CHUKUROVO" LIGNITE, BULGARIA Stefanova M. Institute of Organic Chemistry, Bulgarian Academy of Science https://doi.org/10.12681/bgsg.16682 Copyright © 2018 M. Stefanova To cite this article: Stefanova, M. (2004). MOLECULAR INDICATORS FOR TAXODIUM DUBIUM AS COAL PROGENITOR OF "CHUKUROVO" LIGNITE, BULGARIA. Bulletin of the Geological Society of Greece, 36(1), 342-347. doi:https://doi.org/10.12681/bgsg.16682 http://epublishing.ekt.gr | e-Publisher: EKT | Downloaded at 20/02/2020 22:18:16 | Δελτίο της Ελληνικής Γεωλογικής Εταιρίας τομ. XXXVI, 2004 Bulletin of the Geological Society of Greece vol. XXXVI, 2004 Πρακτικά 10°u Διεθνούς Συνεδρίου. Θεσ/νίκη Απρίλιος 2004 Proceedings of the 10,h International Congress, Thessaloniki, April 2004 MOLECULAR INDICATORS FOR TAXODIUM DUBIUM AS COAL PROGENITOR OF "CHUKUROVO" LIGNITE, BULGARIA Stefanova M. Institute of Organic Chemistry, Bulgarian Academy of Science, Sofia 1113, BULGARIA
[email protected] ABSTRACT The coal sediment under study was of Miocene/Pliocene geological age. The petrological data pointed to Tortonian/Sarmatian age, while the paleobotanical ones - to Middle Miocene. It was documented that "Chukurovo" basin was determined by coal fades indices as limnic ombrotrophic forester swamp. Fossilized trees predominated in "Chukurovo" lignites. Well preserved wood tissue of stems and twigs impregnated by clays and enriched in organic matter were macroscopically ob served. Four types of phytocenosis - aquatic, swamp, flood plain, forests, i.e. mesophilous and mesohygrophilous were proposed. The composition of the last one confirmed the predominance of evergreen laurel and laurel-oaks communities during the Miocene.