Definition
The Huronian glaciation is the oldest series of protracted climatic refrigeration events that extensively affected Earth. It occurred between 2.45 and 2.22 Ga in association with the rise of atmospheric oxygen. Three glaciations of that series, the classical Huronian ice ages, are bracketed in time between ~2.45 and 2.32 Ga; the fourth event, recognized so far only in South Africa, is ~2.22 Ga in age. During these events, glaciers covered continents, extended to low latitudes, and reached to 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 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 northeastern part of the Huronian Basin in Ontario, Canada; just a...
References and Further Reading
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Bekker, A. (2014). Huronian Glaciation. In: Amils, R., et al. Encyclopedia of Astrobiology. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-27833-4_742-4
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DOI: https://doi.org/10.1007/978-3-642-27833-4_742-4
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Huronian Glaciation- Published:
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DOI: https://doi.org/10.1007/978-3-642-27833-4_742-5
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DOI: https://doi.org/10.1007/978-3-642-27833-4_742-4