supercontinent Rodinia

E43459

Rodinia was an ancient supercontinent that assembled during the Proterozoic Eon and existed before the later supercontinent Pangaea, profoundly influencing Earth’s early tectonic and climatic evolution.

Aliases (1)

Statements (49)
Predicate Object
instanceOf ancient landmass
supercontinent
affected atmospheric composition
global ocean circulation
nutrient delivery to oceans
assembledDuring Proterozoic Eon
assemblyLinkedTo Grenville orogenic belt
assemblyTimeInterval 1.3–0.9 billion years ago
associatedWith Grenville orogeny
breakupLinkedTo Neoproterozoic glaciations
Neoproterozoic rifting
Snowball Earth events
breakupTimeInterval 900–700 million years ago
brokeUpApproximately 750 million years ago
900 million years ago
contains Amazonia craton (in many models)
Antarctica craton (in many models)
Australia craton (in many models)
Baltica craton (in many models)
Kalahari craton (in many models)
Laurentia craton
Siberia craton (in some models)
South China craton (in some models)
cratonic blocks
continentType supercontinent
durationEstimate several hundred million years
followedBy Gondwana supercontinent
Pangaea supercontinent
Pannotia supercontinent
formedApproximately 1.1 billion years ago
1.3 billion years ago
geologicalEon Proterozoic Eon
hasUncertainConfiguration true
influenced Earth climatic evolution
Earth tectonic evolution
locatedIn Southern Hemisphere (reconstructed position)
nameMeaning “to give birth” in Russian (rodina)
nameProposedBy Mark W. McMenamin
partOf Earth supercontinent cycle
Neoproterozoic supercontinent cycle
precededBy Columbia supercontinent
precedes Gondwana
Pangaea
Pannotia
recognizedIn plate tectonic reconstructions of the Proterozoic
reconstructedUsing geological correlations
orogenic belts
paleomagnetic data
relatedTo evolution of early eukaryotes (indirectly)

Referenced by (4)
Subject (surface form when different) Predicate
Columbia ("Rodinia")
Nuna ("Rodinia")
predates
Proterozoic Eon
includes
Columbia ("Rodinia")
precedesInSequence

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