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

    Access Status
    Open access via publisher
    Authors
    Grotheer, H.
    Le Métayer, P.
    Piggott, M.
    Lindeboom, E.
    Holman, A.
    Twitchett, R.
    Grice, Kliti
    Date
    2017
    Type
    Journal Article
    
    Metadata
    Show full item record
    Citation
    Grotheer, H. and Le Métayer, P. and Piggott, M. and Lindeboom, E. and Holman, A. and Twitchett, R. and Grice, K. 2017. Occurrence and significance of phytanyl arenes across the Permian-Triassic boundary interval. Organic Geochemistry. 104: pp. 42-52.
    Source Title
    Organic Geochemistry
    DOI
    10.1016/j.orggeochem.2016.12.002
    Additional URLs
    https://epic.awi.de/id/eprint/45676/
    ISSN
    0146-6380
    School
    Department of Chemistry
    Funding and Sponsorship
    http://purl.org/au-research/grants/arc/DP130100577
    URI
    http://hdl.handle.net/20.500.11937/51064
    Collection
    • Curtin Research Publications
    Abstract

    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.

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