Definition
The Mount McRae Shale is a 2.5-Ga-old unit of mudstone, siltstone, chert, iron formation, and dolomite in the Hamersley basin of the Pilbara craton, Western Australia. It is characterized by a high concentration of organic carbon (∼2–8 wt%), abundant disseminated pyrite (∼1 to ∼10 wt% S in the bulk rocks), and pyrite nodules (∼1–10 cm radius). Analysis of S and Fe isotopic compositions of carbonaceous pyritic shale recovered in the NASA-sponsored Astrobiology Drilling Program revealed variations in isotopic compositions that have been linked to changes in the composition of the ocean and the atmosphere and to fluctuations and a temporary rises of atmospheric oxygen that preceded the Great Oxygenation Event (GOE) at 2.32 Ga.
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© 2014 Springer-Verlag Berlin Heidelberg
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Arndt, N. (2014). Mount McRae Shale. In: Amils, R., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_1029-3
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DOI: https://doi.org/10.1007/978-3-642-27833-4_1029-3
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Publisher Name: Springer, Berlin, Heidelberg
Online ISBN: 978-3-642-27833-4
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Mount McRae Shale- Published:
- 11 March 2021
DOI: https://doi.org/10.1007/978-3-642-27833-4_1029-4
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Mount McRae Shale- Published:
- 29 April 2015
DOI: https://doi.org/10.1007/978-3-642-27833-4_1029-3