Acraman-Bunyeroo impact event (Ediacaran), South Australia, and environmental consequences: twenty-five years on
Date
2005
Authors
Williams, G.
Gostin, V.
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Advisors
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Volume Title
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Journal article
Citation
Australian Journal of Earth Sciences, 2005; 52(4-5):607-620
Statement of Responsibility
G. E. Williams & V. A. Gostin
Conference Name
Abstract
Multidisciplinary research during the past 25 years has established that the Acraman impact structure in the 1.59 Ga Gawler Range Volcanics on the Gawler Craton, and an ejecta horizon found 240-540 km from Acraman in the ≤ 580 Ma Bunyeroo Formation in the Adelaide Fold Belt and Dey Dey Mudstone in the Officer Basin, record a Late Neoproterozoic (Ediacaran) event of major environmental importance. Research since 1995 has verified Acraman as a complex impact structure that has undergone as much as 3-5 km of denudation and which originally had a transient cavity up to 40 km in diameter and a final structural rim possibly 85-90 km in diameter. The estimated impact energy of 5.2 × 10<sup>6</sup> Mt (TNT) for Acraman exceeds the threshold of 10<sup>6</sup> Mt nominally set for global catastrophe, and the impact probably caused a severe perturbation of the Ediacaran environment. The occurrence of the impact at a low palaeolatitude (12.5 + 7.1/- 6.1°) may have magnified the environmental effects by perturbing the atmosphere in both hemispheres. These findings are consistent with independent data from the Ediacaran palynology of Australia and from isotope and biomarker chemostratigraphy that the Acraman impact induced major biotic change. Future research should seek geological, isotopic and biological imprints of the Acraman-Bunyeroo impact event across Australia and on other continents. © Geological Society of Australia.