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Atlantica (Greek: Ατλαντικα; Atlantika) is 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. [1] The name, introduced by Rogers 1996, was chosen because the continent opened up to form the South Atlantic Ocean. [2]
Atlantica formed simultaneously with Nena at about 1.9 Ga from Archaean cratons, including Amazonia in present-day South America, and the Congo, West Africa and North Africa Cratons in Africa.[3]
Atlantica separated from Nena between 1.6–1.4 Ga when Columbia — a supercontinent composed of Ur, Nena, and Atlantica — fragmented. [2] 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. [1] 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. [4][5]
Africa
Antarctica
Asia
Australia
Europe
North America
South America
Afro-Eurasia
Americas
Eurasia
Oceania
Argentina, Colombia, Bolivia, Brazil, Peru
Sudan, Egypt, South Africa, Algeria, Morocco
India, Bangladesh, Singapore, Saudi Arabia, China
Azerbaijan, United Kingdom, Spain, Turkey, France
Antarctica, Africa, Asia, Precambrian, Europe
Earth, Iceland, Nitrogen, Geology, Ice age
Antarctica, South America, Africa, Asia, Europe
Period (geology), Paleogene, Neogene, Precambrian, Paleoproterozoic
Atlantica, Zealandia (continent), Amazonian Shield, Appalachia (Mesozoic), Arctica