4.7 Article

The Ediacara Member, South Australia: Lithofacies and palaeoenvironments of the Ediacara biota

期刊

GONDWANA RESEARCH
卷 80, 期 -, 页码 321-334

出版社

ELSEVIER
DOI: 10.1016/j.gr.2019.09.017

关键词

Ediacara biota; Ediacara Member; Lithofacies; Flinders Ranges; Stratigraphy

资金

  1. Australian Government Research Training Program Scholarship
  2. South Australian Museum Early Career Researcher Postgraduate Scholarship

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The Ediacara Member of the Rawnsley Quartzite in the Flinders Ranges (South Australia) has undergone considerable investigation due to its placement within the package of terminal Ediacaran sediments in the region and as the host sediments of the Ediacara biota fossils. A focus on palaeoenvironment reconstruction and taphonomy has seen a succession of lithofacies models presented. These have evolved with the expansion of recognised Ediacara biota localities and prevailing palaeontological methodologies. Much of the recent descriptive lithofacies work has focused on the Nilpena fossil site in the west of the Flinders Ranges. This location is particularly fossil-rich but does not represent a typical section through the Ediacara Member. The Ediacara Member elsewhere in the region contains up to six para-sequences with total thicknesses varying from ten to 260 m. With the exclusion of the Ikara-Chace Range region, the majority of studied locations external to Nilpena do not show clear evidence for significant (canyon-scale), intra-member erosional features. In this study we review existing facies models for the Ediacara Member and compile a best-fit revised facies model by incorporating the modern facies interpretations (largely based at Nilpena) and previous basin-wide observations, models and stratigraphic sections. The revised model is assessed against a series of newly measured stratigraphic sections from across the basin. We propose the division of the wave-base facies into two facies, representative of the upper and lower storm wave-base environments respectively and the re-inclusion of a facies representative of a shoreface palaeoenvironment. Additional characters and identifiers for the facies have been incorporated to aid field identification, as the ability to identify facies of fossil-bearing isolated hand-specimens can allow fossils found on scree slopes to be traced back to source beds. Likewise, palaeoenvironmental interpretations are critical to the reconstruction of Ediacara biota habitat and preservational environments. (c) 2019 International Association for Gondwana Research. Published by Elsevier B.V. All rights reserved.

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