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Pan-African Ocean
Hypothesized paleo-ocean whose closure created the supercontinent of Pannotia From Wikipedia, the free encyclopedia
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The Pan-African Ocean is a hypothesized paleo-ocean whose closure created the supercontinent of Pannotia.[1] The ocean may have existed before the break-up of the supercontinent of Rodinia. The ocean closed before the beginning of the Phanerozoic Eon, when the Panthalassa ocean expanded, and was eventually replaced by it.
This article needs additional citations for verification. (January 2009) |
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See also
- Mirovia – Hypothesized superocean surrounding the supercontinent Rodinia in the Neoproterozoic Era
- Pan-African orogeny – Series of major mountain-forming events in the Neoproterozoic
References
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