Island benthic assemblages: with examples from the late Ordovician of Eastern Australia

Ian G. Percival*, Barry D. Webby

*Corresponding author for this work

    Research output: Contribution to journalArticlepeer-review

    21 Citations (Scopus)

    Abstract

    The Benthic Assemblage (B.A.) concept, developed by A.J. Boucot two decades ago principally for continental marine margins, is extended to offshore island settings. Characteristics of modem island biotas, including ecological displacement, and the effects of r and K selection, can be identified in Late Ordovician volcanic islands of central New South Wales. Two variants of B.A.1 are represented, a quiet-water lingulide biofacies, and a rough-water rhynchonellide biofacies. The quiet-water Eodinobolus biofacies occupied a B.A.1-2 position, onshore of and sheltered by a Tetradium wave-baffle (B.A.2). The offshore shelfal high diversity strophomenide biofacies is equivalent to B.A.3. Remnants of periplatformal B.A.4-5 communities are recognised in allochthonous limestone breccias which were displaced downslope into graptolitic B.A.6 sediments. Steeper offshore gradients, typical of islands, laterally compress the B.A. profiles, and also contribute to downslope slumping. Ecological displacement in island environments results in extension of the habitat range of species into adjacent B.A.s. Reefs complicate the usual B.A. profile by introducing distinct sheltered and turbulent water environments. These characteristics may have applicability in interpretation of islands throughout the Palaeozoic record.

    Original languageEnglish
    Pages (from-to)171-185
    Number of pages15
    JournalHistorical Biology
    Volume11
    Issue number1-4
    Publication statusPublished - 1996

    Keywords

    • Benthic assemblages
    • Biofacies
    • Island palaeoecology
    • Ordovician

    Fingerprint

    Dive into the research topics of 'Island benthic assemblages: with examples from the late Ordovician of Eastern Australia'. Together they form a unique fingerprint.

    Cite this