What is Pannotia?
Q: What is Pannotia?
A: Pannotia is a Neoproterozoic supercontinent.
Q: When did Pannotia exist?
A: Pannotia may have existed during the Ediacaran period (~600 mya), to the end of the Precambrian (about 541 mya).
Q: What happened to Pannotia after it existed?
A: After it existed, Pannotia split into smaller continents.
Q: What were the smaller continents that Pannotia split into?
A: The smaller continents that Pannotia split into were Laurentia, Siberia and Baltica.
Q: What was the main landmass south of the smaller continents?
A: The main landmass south of the smaller continents was Gondwana.
Q: In what era did Pannotia come to exist?
A: Pannotia came to exist in the Neoproterozoic era.
Q: When did the Precambrian era end?
A: The Precambrian era ended about 541 million years ago.
