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Huronian Glaciation

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Encyclopedia of Astrobiology

Synonyms

Paleoproterozoic ice ages; Paleoproterozoic Snowball Earth

Keywords

Paleoproterozoic, ice ages, snowball earth, rise of atmospheric oxygen

Definition

The Huronian glaciation is the oldest series of protracted climatic refrigeration events that extensively affected Earth between 2.45 and 2.22 Ga in association with the rise of the atmospheric oxygen. During these events, glaciers covered continents, extended to low latitudes, and reached there sea level. The ice ages were followed by a protracted time interval with greenhouse (warm and humid) conditions. The name is derived from the Huronian Supergroup, a glacio-marine to fluvio-deltaic sedimentary sequence of dolostone, siltstone, argillites, diamictites, and sandstones exposed on the north shore of Lake Huron in Ontario, Canada between Sault Ste. Marie, Sudbury, and Cobalt.

History

The Huronian glacial deposits were first recognized by Coleman (1907) in the north-eastern part of the Huronian Basin in Ontario, Canada; just a...

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References and Further Reading

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  • Evans DA, Beukes NJ, Kirschvink JL (1997) Low-latitude glaciation in the Paleoproterozoic era. Nature 386:262–266

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Correspondence to Andrey Bekker .

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© 2011 Springer-Verlag Berlin Heidelberg

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Bekker, A. (2011). Huronian Glaciation. In: Gargaud, M., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-11274-4_742

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