Palaeos Earth: Paleogeography: Pannotia
Palaeos: Palaeos Paleogeography
PALEOGEOGRAPHY Pannotia

 

Pannotia

Named Pannotia by Dalziel, 1997, and sometimes loosely referred to as the "Vendian supercontinent", this was a late Neoproterozoic Supercontinent that evolved from Rodinia (Dalziel, 1991). According to Dalziel, Pannotia resided in the Southern Hemisphere. Pannotia underwent rifting into smaller components during latest Neoproterozoic time, one of the largest being Gondwana. Parts of it continued to assemble during the Cambrian, while breaking apart in others regions. The three main daughter continents were Gondwana, Laurentia, and Baltica (at the time mostly submerged by shallow sea).



images not loading? | error messages? | broken links? | suggestions? | criticism?

contact us
page uploaded 2 June 2002 MAK, edited RFVS111108
checked ATW080121
unless otherwise specified, text © M. Alan Kazlev 2002
this material may be freely used for non-commercial purposes