Pannotia
id:
pannotia-251-49015
title:
Pannotia
text:
Pannotia, also known as the Vendian supercontinent, Greater Gondwana, and the Pan-African supercontinent, was a relatively short-lived Neoproterozoic supercontinent that formed at the end of the Precambrian during the Pan-African orogeny, during the Cryogenian period and broke apart 560 Ma with the opening of the Iapetus Ocean, in the late Ediacaran and early Cambrian.
Pannotia formed when Laurentia was located adjacent to the two major South American cratons, Amazonia and Río de la Plata. The o
brand slug:
wiki
category slug:
encyclopedia
description:
Hypothesized Neoproterozoic supercontinent
original url:
https://en.wikipedia.org/wiki/Pannotia
date created:
date modified:
2024-03-24T20:30:28Z
main entity:
{"identifier":"Q208078","url":"https://www.wikidata.org/entity/Q208078"}
image:
{"content_url":"https://upload.wikimedia.org/wikipedia/commons/3/33/Panotiaggg.jpg","width":411,"height":208}
fields total:
13
integrity:
15