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Pan-African Ocean

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This is the current revision of this page, as edited by Qwerfjkl (talk | contribs) at 19:35, 11 July 2021 (Removed 'a(n)' from the beginning of the short description per WP:SDFORMAT, from a request at Wikipedia:Reward board#Remove "A" as the first word from short descriptions. (via WP:JWB)). The present address (URL) is a permanent link to this version.

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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.

See also

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  • 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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  1. ^ Linnemann, Ulf; R. Damian Nance; Petr Kraft; Gernold Zulauf (2007). The Evolution of the Rheic Ocean: From Avalonian-Cadomian Active Margin to Alleghenian-Variscan Collision. Geological Society of America. p. 28. ISBN 978-0-8137-2423-2.