Pannotia

E229288

Pannotia was a short-lived Neoproterozoic supercontinent that formed after the breakup of Rodinia and existed roughly 650–540 million years ago.

All labels observed (1)

Label Occurrences
Pannotia canonical 8

How this entity was disambiguated

Statements (47)

Predicate Object
instanceOf Neoproterozoic supercontinent ⓘ
supercontinent ⓘ
alsoKnownAs Greater Gondwana ⓘ
linked to: Gondwana

Vendian supercontinent ⓘ
approximatePaleolatitude high southern latitudes ⓘ
assemblyProcess collision and amalgamation of Neoproterozoic cratons ⓘ
associatedOrogeny Brasiliano orogeny ⓘ
Cadomian orogeny ⓘ
Kuunga orogeny ⓘ
Pan-African orogeny ⓘ
associatedWith Ediacaran Period ⓘ
late Neoproterozoic glaciations ⓘ
breakupContributedTo opening of the Iapetus Ocean ⓘ
opening of the early Paleozoic ocean basins ⓘ
breakupLedTo formation of separate continents including Laurentia, Baltica, and Gondwana ⓘ
breakupProcess rifting and continental fragmentation ⓘ
characteristic short-lived compared to other supercontinents ⓘ
chronologicalPosition immediately precedes the Cambrian explosion in time ⓘ
pre-Cambrian supercontinent ⓘ
continentAssembly aggregation of Gondwana-related cratons with Laurentia, Baltica, and Siberia ⓘ
duration approximately 110 million years ⓘ
endExistence approximately 540 million years ago ⓘ
evidenceType geochronology ⓘ
orogenic belts correlation ⓘ
paleomagnetic data ⓘ
structural geology ⓘ
followedBy Gondwana ⓘ
formedAfter Rodinia ⓘ
geologicalEon Neoproterozoic Eon ⓘ
linked to: Neoproterozoic Era
includedContinent Baltica ⓘ
Gondwana core ⓘ
linked to: Gondwana

Laurentia ⓘ
Siberia ⓘ
namedBy geologists studying Neoproterozoic supercontinents ⓘ
oceanicCounterpart Pan-African oceans (broad sense) ⓘ
paleogeographicModel continents arranged in a mostly equatorial to high-latitude ring around a large ocean ⓘ
precededBy Rodinia ⓘ
relatedConcept supercontinent cycle ⓘ
significance reorganization of global plate tectonics before the Cambrian ⓘ
represents a stage between Rodinia and Gondwana in the supercontinent cycle ⓘ
startExistence approximately 650 million years ago ⓘ
status hypothesized and reconstructed from geological evidence ⓘ
tectonicSetting assembly of continental blocks around the South Pole ⓘ
timeSpanOverlaps Cryogenian Period ⓘ
Ediacaran Period ⓘ
late Neoproterozoic Era ⓘ
uncertainty configuration and extent are debated among geologists ⓘ

How these facts were elicited

Referenced by (8)

Full triples — surface form annotated when it differs from this entity's canonical label.

Rodinia → precedes → Pannotia ⓘ
subject linked to: supercontinent Rodinia
Laurentia → wasPartOf → Pannotia ⓘ
Pan-African Ocean → surrounded → Pannotia ⓘ
Proto-Africa → partOf → Pannotia ⓘ
subject linked to: proto-Africa
Proto-Africa → formedMajorPartOf → Pannotia ⓘ
subject linked to: proto-Africa
Proto-Africa → relatedConcept → Pannotia ⓘ
subject linked to: proto-Africa