Pan-African Ocean

E226604

The Pan-African Ocean was a vast ancient ocean that surrounded the supercontinent Pannotia during the late Precambrian era.

All labels observed (1)

Label Occurrences
Pan-African Ocean canonical 1

How this entity was disambiguated

Statements (32)

Predicate Object
instanceOf ancient ocean
paleo-ocean
associatedWith Pan-African orogeny
closedBy continental collisions during Pan-African orogeny
closedDuring assembly of Gondwana
contained mid-ocean ridges
subduction zones
disappearedBy early Paleozoic
existedDuring Neoproterozoic Era
surface form: Neoproterozoic Eon

late Precambrian
followedBy Iapetus Ocean
Paleo-Tethys Ocean
geologicalAgeMa about 650–540 million years ago
geologicalContext Neoproterozoic supercontinent assembly and breakup
knownFrom geochronological data of Neoproterozoic rocks
paleogeographic reconstructions
structural geology of Pan-African belts
linkedTo formation of Neoproterozoic accretionary belts
growth of Gondwanan continental crust
location global, between fragments of Rodinia and later Pannotia margins
namedAfter Pan-African orogeny
openedAfter fragmentation of Rodinia
partOf Neoproterozoic plate-tectonic system
Precambrian supercontinent cycle
precededBy Mirovia Ocean
relatedConcept Gondwana
Pannotia
supercontinent Rodinia
surface form: Rodinia
relatedTo breakup of Rodinia
surrounded Pannotia
supercontinent Pannotia
tectonicSetting global ocean around Pannotia

How these facts were elicited

Referenced by (1)

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

supercontinent Pannotia oceanSurrounding Pan-African Ocean
subject surface form: Pannotia