Editing Rodinia (section)

===Breakup===
In 2009 UNESCO's [[International Geoscience Programme]] project 440, named "Rodinia Assembly and Breakup," concluded that Rodinia broke up in four stages between 825 and 550 Ma:<ref>{{Harvnb|Bogdanova|Pisarevsky|Li|2009|loc=Breakup of Rodinia (825–700 Ma), pp. 266–267}}</ref>
* The breakup was initiated by a [[superplume]] around 825–800 Ma whose influence—such as crustal arching, intense bimodal magmatism, and accumulation of thick rift-type sedimentary successions—has been recorded in South Australia, South China, Tarim, Kalahari, India, and the Arabian-Nubian Craton.
* Rifting progressed in the same cratons 800–750 Ma and spread into Laurentia and perhaps Siberia. India (including Madagascar) and the Congo–São Francisco Craton were either detached from Rodinia during this period or simply never were part of the supercontinent.
* As the central part of Rodinia reached the Equator around 750–700 Ma, a new pulse of magmatism and rifting continued the disassembly in western Kalahari, West Australia, South China, Tarim, and most margins of Laurentia.
* 650–550 Ma several events coincided: the opening of the [[Iapetus Ocean]]; the closure of the Braziliano, [[Adamastor Ocean|Adamastor]], and Mozambique oceans; and the [[Pan-African orogeny]]. The result was the formation of [[Gondwana]].

The Rodinia hypothesis assumes that [[rift]]ing did not start everywhere simultaneously. Extensive lava flows and volcanic eruptions of Neoproterozoic age are found on most continents, evidence for large scale rifting about 750 Ma.<ref name="mcmenamin" /> As early as 850 to 800 Ma,<ref name="Torsvik2003" /> a rift developed between the continental masses of present-day Australia, East Antarctica, India and the Congo and Kalahari cratons on one side and later Laurentia, Baltica, Amazonia and the West African and Rio de la Plata cratons on the other.<ref>{{Harvnb|Torsvik|2003|loc=Fig. 'Rodinia old and new', p. 1380}}</ref> This rift developed into the Adamastor Ocean during the [[Ediacaran]].

Around 550 Ma, near the boundary between the Ediacaran and Cambrian, the first group of cratons fused again with Amazonia, West Africa and the Rio de la Plata cratons<ref>See for example reconstructions in {{Harvnb|Pisarevsky|Murphy|Cawood|Collins|2008|loc=Fig. 4, p. 19}}</ref> during the Pan-African orogeny, which caused the development of Gondwana.

In a separate rifting event about 610 Ma, the Iapetus Ocean formed. The eastern part of this ocean formed between Baltica and Laurentia, the western part between Amazonia and Laurentia. Because the timeframe of this separation and the partially contemporaneous Pan-African orogeny are difficult to correlate, it might be that all continental mass was again joined in one supercontinent between roughly 600 and 550 Ma. This hypothetical supercontinent is called [[Pannotia]].