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Ordovician conodont biostratigraphy of the Willara Formation in the Canning Basin, Western Australia

Yong Yi Zhen*, Robert S. Nicoll, Leon S. Normore, Ian G. Percival, John R. Laurie, Louisa M. Dent

*Corresponding author for this work

    Research output: Contribution to journalArticlepeer-review

    Abstract

    The conodont fauna from the Willara Formation, a carbonate-dominated stratigraphic unit widely distributed in the subsurface Canning Basin of Western Australia, is represented by 41 species, including a new species, Erraticodon neopatu Zhen n. sp. The Jumudontus gananda and Histiodella altifrons biozones are recognized in the lower and upper parts, respectively, of the Willara Formation. Deposited primarily in shallow nearshore settings, the Willara Formation is characterized by the occurrence of predominantly long-range coniform species of Triangulodus, Scalpellodus, Drepanoistodus, Drepanodus, and Kirkupodus. Several widely distributed age-diagnostic species, including Histiodella altifrons, Histiodella holodentata, Histiodella serrata, and Jumudontus gananda, serve as keys for biostratigraphic analysis and correlation. Our study also shows that the basal and top boundaries of the Willara Formation are diachronous across the basin, extending from the middle Floian (Oepikodus communis Biozone) to middle Darriwilian (Histiodella holodentata-Eoplacognathus pseudoplanus Biozone). This contribution provides crucial new biostratigraphic data for precise correlation of the Willara Formation with its time equivalents regionally and internationally.

    Original languageEnglish
    Pages (from-to)249-277
    Number of pages29
    JournalPalaeoworld
    Volume30
    Issue number2
    DOIs
    Publication statusPublished - Jun 2021

    Keywords

    • biostratigraphy
    • Canning Basin
    • Conodonts
    • Dapingian
    • Ordovician
    • Willara Formation

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