The Paleogene vegetation and petroleum system in the tropics: A biomarker approach

• Published in: Marine and Petroleum Geology
• Main Authors: RUDRA, A, DUTTA, S, RAJU, SV
• Format: Article in Journal/Newspaper
• Language: English
• Published: ELSEVIER SCI LTD 2017
• Subjects: Beaufort-Mackenzie Basin; Equatorial Rain-Forest; Upper Assam Basin; Early Eocene; Late Paleocene; Crude Oils; Structural Identification; Diterpenoid Hydrocarbons; Depositional Environment; Terpenoid Composition; Assam Basin; Cenozoic; Hydrocarbons; Molecular Fossils; Rainforest Elements; Mackenzie Basin
• Online Access: https://doi.org/10.1016/j.marpetgeo.2017.05.008

The present study investigates the biomarker signatures of sediments and crude oils to infer the pale vegetation from the two petroleum systems of Assam Basin, eastern India. They are classified as the Paleocene-middle Eocene and the middle Eocene-Oligocene petroleum systems. The sediments are oil and gas prone with an early catagenetic stage of thermal evolution. Here we report tricyclic diterpanes such as rimuane, pimarane, rosane and isopimarane along with tetracyclic diterpanes: ent-beyerane, phyllocladane, kaurane from Paleocene-Eocene coal-bearing sediments and crude oils. These diterpane biomarkers attest dominant contribution from conifers, possibly from Podocarpaceae and Araucariaceae. However, diterpanes are not detected in Oligocene sediments and oils. Crude oils from both Paleocene Eocene and Oligocene reservoirs and organic rich sediments contain angiosperm biomarkers such oleanane and related triterpanes along with bicadinane, a biomarker specific for the Dipterocarpaceae family of angiosperms. The equatorial position of India during early Paleogene along with the presence of angiosperm signatures including Dipterocarpaceae and gymnosperms reflect the emergence of tropical rainforest elements in eastern India. Absence of diterpenoids in Oligocene samples and difference in angiosperm parameters from Paleocene-Eocene samples suggests a change in source vegetation and organofacies. (C) 2017 Elsevier Ltd. All rights reserved.