Summary of East Gondwanan Conodont Data through the Ireviken Event at Boree Creek

Andrew Simpson; David Mathieson; Jiri Fryda; Barbora Frydová

doi:10.1007/s12583-021-1310-9

Volume 32 Issue 3

Jun 2021

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Journal of Earth Science > 2021 > 32(3): 512-523.

Andrew Simpson, David Mathieson, Jiri Fryda, Barbora Frydová. Summary of East Gondwanan Conodont Data through the Ireviken Event at Boree Creek. Journal of Earth Science, 2021, 32(3): 512-523. doi: 10.1007/s12583-021-1310-9

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Andrew Simpson, David Mathieson, Jiri Fryda, Barbora Frydová. Summary of East Gondwanan Conodont Data through the Ireviken Event at Boree Creek. Journal of Earth Science, 2021, 32(3): 512-523. doi: 10.1007/s12583-021-1310-9

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Summary of East Gondwanan Conodont Data through the Ireviken Event at Boree Creek

doi: 10.1007/s12583-021-1310-9

1.
Archives and Collections, University Library, Macquarie University, Sydney NSW 2109, Australia
2.
Department of Biological Sciences, Macquarie University, Sydney NSW 2109, Australia
3.
Department of Environmental Geosciences, Czech University of Life Sciences Prague, 16500 Prague, Czech Republic

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Corresponding author: Andrew Simpson, andrew.simpson@mq.edu.au
Received Date: 10 Oct 2020
Accepted Date: 13 May 2021
Publish Date: 01 Jun 2021

Abstract

Abstract

The Ireviken Event was the first Middle Paleozoic event consisting of synchronised faunal, isotopic and facies change to be recognised. An analysis of the conodont faunas throughout the Boree Creek/Borenore Limestone succession in the central western region of the Tasman fold belt of New South Wales (Australia) revealing all five conodont zones that comprise the event is presented. While some zonal boundaries are precise, allowing direct comparison of stratigraphic intervals on other paleo-continents, some can only be approximated. Conodont data from pre-Ireviken Event strata, in contrast, only permit the identification of a broad Telychian chronology. The identification of Wenlock post-Ireviken Event conodont zones is incomplete due to lithological variability, namely the presence of tuffaceous beds near the top of the formation and an unconformity between the Boree Creek and overlying Borenore Limestone. The Boree Creek Formation contains the only example of the Ireviken Event discovered to date from the Tasman fold belt of eastern Gondwanaland.
- conodonts,
- extinction,
- Ireviken Event,
- Silurian,
- Boree Creek,
- eastern Gondwanaland

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References(65)

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Summary of East Gondwanan Conodont Data through the Ireviken Event at Boree Creek

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