T274 Evolution of Marine Life in the Cambrian II: Biotic, Biogeochemical, and Stratigraphic Contexts

Wednesday, 25 September 2024
1:30 PM - 5:30 PM
204C

THE EMU BAY SHALE: A UNIQUE EARLY CAMBRIAN LAGERSTÄTTE FROM A TECTONICALLY ACTIVE BASIN

Paper number: T274-4
Program: Technical Sessions
Time: 2:05 PM – 2:20 PM

Authors

Abstract

The Emu Bay Shale (EBS) of South Australia is anomalous among Cambrian Lagerstätten because it captures anatomical information that is rare in Burgess Shale-type fossils, and because of its inferred nearshore setting, the nature of which has remained controversial. Intensive study, combining outcrop and borehole data with a compilation of >25,000 fossil specimens, reveals that the EBS biota inhabited a fan delta complex within a tectonically active basin. Preservation of soft-bodied organisms in this setting is surprising and further underscores differences between the EBS and other Cambrian Lagerstätten. Environmental conditions, including oxygen fluctuations, slope instability, high suspended sediment concentrations, and episodic high-energy events, inhibited colonization of the lower prodelta by all but a few specialist species, but favored downslope transportation and preservation of other, largely endemic, shallow-water benthos. The absence of firm substrates that are characteristic of other Cambrian BST deposits appears to have presented additional challenges to sessile and facultatively mobile benthos. Conversely, a diverse and abundant nektonic community comprising taxa typical of other Cambrian Lagerstätten indicates that the upper water column was well oxygenated and largely divorced from near seafloor conditions across the fan delta complex. The EBS provides extraordinary insight into early Cambrian animal diversity from Gondwana. These results demonstrate how environmental factors determined community composition and provide a framework for understanding this unique Konservat-Lagerstätte.

Geological Society of America Abstracts with Programs. Vol. 56, No. 5

doi: 10.1130/abs/2024AM-401045

© Copyright 2024 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.