Atlantica (Greek: Ατλαντικα; Atlantika) is the name given to an ancient continent that formed during the Proterozoic about (two billion years ago, Ga) from various 2 Ga cratons located in what is now West Africa and eastern South America.  The name, introduced by Rogers 1996, was chosen because the continent opened up to form the South Atlantic Ocean. 
Atlantica separated from Nena between 1.6–1.4 Ga when Columbia — a supercontinent composed of Ur, Nena, and Atlantica — fragmented.  Together with continents Nena and Ur and some minor plates, Atlantica formed the supercontinent Rodinia about 1 Ga ago. The rifting of Rodinia between 1–0.5 Ga resulted in the formation of three new continents: Laurasia and East and West Gondwana, of which Atlantica became the nucleus of the latter.  During this later stage, the Neoproterozoic era, a Brasiliano-Pan African orogenic system developed. The central part of this system, the Araçuaí-West Congo orogen, has left a distinct pattern of deformations, still present on both sides of the Atlantic. 
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