Atlantica (Greek: Ατλαντικα; Atlantika) is an ancient continent that formed during the Proterozoic about 2,000 million years ago (two billion years ago, Ga) from various 2 Ga cratons located in what are now West Africa and eastern South America.[1] The name, introduced by Rogers 1996, was chosen because the parts of the ancient continent are now located on opposite sides of the South Atlantic Ocean.[2]
Formation
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]
Breakup
Atlantica separated from Nena between 1.6–1.4 Ga when Columbia — a supercontinent composed of Ur, Nena, and Atlantica — fragmented.[2] Atlantica and continents Nena and Ur and some minor plates formed the supercontinent Rodinia about 1 Ga ago. Between 1–0.5 Ga Rodinia split into three new continents: Laurasia and East and West Gondwana; Atlantica became the nucleus of West Gondwana.[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 Ocean.[4][5]
See also
Notes
- ^ a b Rogers 1996
- ^ a b Sankaran 2003, p. 1122
- ^ Yoshida, Windley & Dasgupta 2003, p. 16
- ^ Alkmim et al. 2006, Abstract
- ^ Noce et al. 2007, p. 60
References
- Alkmim, Fernando F.; Marshak, Stephen; Pedrosa-Soares, Antônio Carlos; Peres, Guilherme Gravina; Cruz, Simone Cerqueira Pereira; Whittington, Alan (September 1, 2006). "Kinematic evolution of the Araçuaí-West Congo orogen in Brazil and Africa: Nutcracker tectonics during the Neoproterozoic assembly of Gondwana". Precambrian Research. 149 (1–2): 43–64. Bibcode:2006PreR..149...43A. doi:10.1016/j.precamres.2006.06.007.
- Noce, Carlos M.; Pedrosa-Soares, Antônio Carlos; da Silva, Luiz Carlos; Armstrong, Richard; Piuzana, Danielle (2007). "Evolution of polycyclic basement complexes in the Aracuaí Orogen, based on U–Pb SHRIMP data: Implications for Brazil–Africa links in Paleoproterozoic time" (PDF). Precambrian Research. 159 (1–2): 60–78. Bibcode:2007PreR..159...60N. doi:10.1016/j.precamres.2007.06.001. hdl:1885/33132.
- Rogers, John J. W. (January 1996). "A History of Continents in the Past Three Billion Years". The Journal of Geology. 104 (1): 91–107. Bibcode:1996JG....104...91R. doi:10.1086/629803. JSTOR 30068065. S2CID 128776432.
- Sankaran, A. V. (2003). "The supercontinent medley: Recent views" (PDF). Current Science. 85 (8): 1121–1123.
- Yoshida, Masaru; Windley, Brian F.; Dasgupta, Somnath, eds. (2003). Proterozoic East Gondwana: supercontinent assembly and breakup. Vol. 206. Geological Society of London. ISBN 1-86239-125-4.
Continents of Earth | ||||||||
|---|---|---|---|---|---|---|---|---|
| ||||||||
| ||||||||
