Removed Servers List

Removed servers/continents are places where you could join the game but now are underwater, joined other servers to make superservers or just broke apart to smaller pieces like during Great Rainforest Collapse.

## List

● **Vaalbara-** proposed first testing server for terrestrial life. added propably from the start of Paleoarchean (3.6) to 2.7 Gya.

● **Ur-** Another proposed testing server added during Paleoarchean 3.1 Gya.

● **Kenorland-** Superserver added during Neoarchean around 2.7 Gya.

● **Arctica-** Server added during Neoarchean around 2.565 Gya.

● **Columbia-** Superserver added around 2.1-1.5 Gya at Paleoproterozoic.

● **Atlantica-** Continent added around 2.0 Gya during Paleoproterozoic.

● **Nena-** Superserver introduced at Paleoproterozoic around 1.9 Gya.

● **Baltica-** Server from Mesoproterozoic ~1.0 Gya. later it joined the Supercontinent Rodinia.

● **Rodinia-** Superserver added between 1.1 and 0.633 Gya.

● **Avalonia-** Neoproterozoic Server From 750 Mya.

● **Pannotia-** Short living Superserver from Neoproterozoic during 650- 500 Mya.

● **Pampia-** Microserver added during around start of Cambrian Expansion.

● **Gondwana-** Very famous Server from 550 Mya the end of Neoproterozoic and start of Beta 1.1.1.

● **Cimmeria-** Another Server added during **Ediacaran** at 550 Mya.

● **Laurasia-**Other famous server from 550 Mya. introduced in the north of Gondwana.

● **Cuyania-** Microserver from ~490-390 Mya.

● **Chilenia-** another microserver from ~490-390 Mya. it affected many rocks in South america server.

● **Pangaea-** Superserver added around 335 Mya. Famous because of introduction of Dinosaurs and Great Dying Event. it started to broke around 200 Mya.

● **Mauritia-** Microserver added during Precambrian but deleted around 70-60 Mya.

## References

1. ↑ http://www.geo.uu.nl/Research/Paleomagnetism/publications/Zegers98b.pdf
2. ↑ https://www.researchgate.net/publication/222049723
3. ↑ Pesonen, L. J.; Elming, S.-Å.; Mertanen, S.; Pisarevsky, S.; D’Agrella-Filho, M. S.; Meert, J. G.; Schmidt, P. W.; Abrahamsen, N.; Bylund, G. (2003). "Palaeomagnetic configuration of continents during the Proterozoic". *Tectonophysics*. **375** (1–4): 289–324
4. ↑ Vernikovsky, V. A.; Dobretsov, N. L. (2015). "Geodynamic evolution of the Arctic Ocean and modern problems in geological studies of the Arctic region". *Herald of the Russian Academy of Sciences*. **85** (3): 206–212.
5. ↑ Zhao, G.; Cawood, P. A.; Wilde, S. A.; Sun, M. (2002). "Review of global 2.1–1.8 Ga orogens: implications for a pre-Rodinia supercontinent". *Earth-Science Reviews*. **59** (1): 125–162.
6. ↑ https://dx.doi.org/10.1086/629803
7. ↑ Cocks, L. R. M.; Torsvik, T. H. (2005). "Baltica from the late Precambrian to mid-Palaeozoic times: the gain and loss of a terrane's identity" (PDF). *Earth-Science Reviews*. **72** (1–2): 39–66
8. ↑ Gaucher, Claudio; Bossi, Jorge; Blanco, Gonzalo (2009). "Palaeogeography". *Neoproterozoic-Cambrian Tectonics, Global Change and Evolution: A Focus on South Western Gondwana*. Developments in Precambrian Geology. **16**. pp. 131–41.
9. ↑ Murphy, J. B.; Pisarevsky, S. A.; Nance, R. D.; Keppie, J. D. (2001). Jessell, M. J. (ed.). "Animated history of Avalonia in Neoproterozoic - Early Proterozoic". General Contributions. *Journal of the Virtual Explorer*. **3**: 45–58.
10. ↑ Scotese 2009, Reconstruction of Rodinia and Pannotia, p. 68
11. ↑ Gaucher, Claudio; Bossi, Jorge; Blanco, Gonzalo (2009). "Palaeogeography". *Neoproterozoic-Cambrian Tectonics, Global Change and Evolution: A Focus on South Western Gondwana*. Developments in Precambrian Geology. **16**. pp. 131–41
12. ↑ Bradley, D.C. (2011). "Secular Trends in the Geologic Record and the Supercontinent Cycle". *Earth-Science Reviews*. **108** (1–2): 16–33.
13. ↑ Buchs, D. M.; Bagheri, S.; Martin, L.; Hermann, J.; Arculus, R. (2013). "Paleozoic to Triassic ocean opening and closure preserved in Central Iran: Constraints from the geochemistry of meta-igneous rocks of the Anarak area". *Lithos*. **172**: 267–287.
14. ↑ Blakey 2003, Assembly of Western Pangaea: Carboniferous–Permian, pp. 453–454; Assembly of Eastern Pangaea: Late Permian–Jurassic, p. 454; Fig. 10, p. 454
15. ↑ http://sp.lyellcollection.org/cgi/content/abstract/246/1/305
16. ↑ Rapalini, A.E. 2005. The accretionary history of southern South America from the latest Proterozoic to the Late Palaeozoic: some palaeomagnetic constraints. From: Vaughan, A. R M., Leat, P. T. & Pankhurst, R. J, (eds). Terrane Processes at the Margins of Gondwana. Geological Society, London, Special Publications, 246, 305-328
17. ↑ Blakey 2003, Assembly of Western Pangaea: Carboniferous–Permian, pp. 453–454; Assembly of Eastern Pangaea: Late Permian–Jurassic, p. 454; Fig. 10, p. 454
18. ↑ Torsvik, Trond H.; Amundsen, Hans; Hartz, Ebbe H.; Corfu, Fernando; Kusznir, Nick; Gaina, Carmen; Doubrovine, Pavel V.; Steinberger, Bernhard; Ashwal, Lewis D.; Jamtveit, Bjørn (24 February 2013). "A Precambrian microcontinent in the Indian Ocean" (PDF). *Nature Geoscience*. **6** (3): 223–227