Occurrence and significance of phytanyl arenes across the Permian-Triassic boundary interval

• Published in: Organic Geochemistry
• Main Authors: Grotheer, H., Le Métayer, P., Piggott, M., Lindeboom, E., Holman, A., Twitchett, R., Grice, Kliti
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Pergamon 2017
• Subjects: Greenland; Spitsbergen
• Online Access: https://hdl.handle.net/20.500.11937/51064; https://doi.org/10.1016/j.orggeochem.2016.12.002

Phytanyl benzene and phytanyl toluene occur in mudstones from several key Permian-Triassic Boundary (PTB) sections from mid-northern palaeolatitudes (Spitsbergen and Eastern Greenland), as well as mid-southern palaeolatitudes (Western Australia). The occurrence of these compounds through the different PTB sections is related to the occurrence of the previously identified C33 n-alkyl cyclohexane, suggesting their parent organism shared a similar unique ecological niche and was associated with the extinction horizon. Further, the lack of these compounds in the carbonate-dominated palaeoequatorial, Global Stratotype Section and Point (GSSP), Meishan-1 (South China) section possibly points to their source being temperature and climate controlled.