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Breakup of Rodinia

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Encyclopedia of Geobiology

Part of the book series: Encyclopedia of Earth Sciences Series ((EESS))

Synonyms

Break-up of the supercontinent Rodinia

Definition

Supercontinent Rodinia . The earth’s geodynamic system periodically pushes almost all continents together to form a single landmass – a supercontinent. The best known supercontinent is Pangaea (or Pangea) that existed between 320 and 170 Ma. A less known supercontinent Rodinia is believed to have existed between 900 Ma (some believe 1,000 Ma) and 750 Ma. The name “Rodinia” was coined by McMenamin and McMenamin (1990) from the Russian word “rodit” meaning “to beget” or “to give birth.” McMenamin and McMenamin (1990, p. 95) considered Rodinia to have been the supercontinent that spawned all subsequent continents, while “the edges (continental shelves ) of Rodinia were the cradle of the earliest animals.” Three landmark paper in 1991 (Moores, 1991; Dalziel, 1991; Hoffman, 1991) triggered a global debate on this supercontinent hypothesis. The configuration of Rodinia is still controversial today, with some alternative...

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Bibliography

  • Anderson, D. L., 1994. Superplume or supercontinents? Geology, 22, 39–42.

    Article  Google Scholar 

  • Bond, G. C., Nickeson, P. A., and Kominz, M. A., 1984. Breakup of a supercontinent between 625 Ma and 555 Ma: new evidence and implications for continental histories. Earth and Planetary Science Letters, 70, 325–345.

    Article  Google Scholar 

  • Cawood, P. A., and Pisarevsky, S. A., 2006. Was Baltica right-way-up or upside-down in the Neoproterozoic? Journal of the Geological Society, 163, 753–759.

    Article  Google Scholar 

  • Dalziel, I. W. D., 1991. Pacific margins of Laurentia and East Antarctica - Australia as a conjugate rift pair: evidence and implications for an Eocambrian supercontinent. Geology, 19, 598–601.

    Article  Google Scholar 

  • Hoffman, P. F., 1991. Did the breakout of Laurentia turn Gondwanaland inside-out? Science, 252, 1409–1412.

    Article  Google Scholar 

  • Kendall, B., Creaser, R. A., and Selby, D., 2006. Re-Os geochronology of postglacial black shales in Australia: constraints on the timing of “Sturtian” glaciation. Geology, 34, 729–732.

    Article  Google Scholar 

  • Li, Z. X., Li, X. H., Kinny, P. D., and Wang, J., 1999. The breakup of Rodinia: did it start with a mantle plume beneath South China? Earth and Planetary Science Letters, 173(3), 171–181.

    Article  Google Scholar 

  • Li, Z. X., Li, X. H., Kinny, P. D., Wang, J., Zhang, S., and Zhou, H., 2003. Geochronology of Neoproterozoic syn-rift magmatism in the Yangtze Craton, South China and correlations with other continents: evidence for a mantle superplume that broke up Rodinia. Precambrian Research, 122(1–4), 85–109.

    Article  Google Scholar 

  • Li, Z. X., Evans, D. A. D., and Zhang, S., 2004. A 90° Spin on Rodinia: possible causal links between the Neoproterozoic supercontinent, superplume, true polar wander and low-latitude glaciation. Earth and Planetary Science Letters, 220, 409–421.

    Article  Google Scholar 

  • Li, Z. X., Bogdanova, S. V., Collins, A. S., Davidson, A., De Waele, B., Ernst, R. E., Fitzsimons, I. C. W., Fuck, R. A., Gladkochub, D. P., Jacobs, J., Karlstrom, K. E., Lu, S., Natapov, L. M., Pease, V., Pisarevsky, S. A., Thrane, K., and Vernikovsky, V., 2008. Assembly, configuration, and break-up history of Rodinia: a synthesis. Precambrian Research, 160(1–2), 179–210.

    Article  Google Scholar 

  • Maruyama, S., Santosh, M., and Zhao, D., 2007. Superplume, supercontinent, and post-perovskite: Mantle dynamics and anti-plate tectonics on the Core-Mantle Boundary. Gondwana Research, 11(1–2), 7–37.

    Article  Google Scholar 

  • McMenamin, M. A. S., and McMenamin, D. L. S., 1990. The Emergence of Animals: The Cambrian Breakthrough. New York: Colombia University Press, 217 pp.

    Google Scholar 

  • Moores, E. M., 1991. Southwest U.S.-East Antarctic (SWEAT) connection: a hypothesis. Geology, 19, 425–428.

    Article  Google Scholar 

  • Pisarevsky, S. A., Wingate, M. T. D., Powell, C. M., Johnson, S., and Evans, D. A. D., 2003. Models of Rodinia assembly and fragmentation. In Yoshida, M., Windley, B. F., and Dasgupta, S. (eds.), Proterozoic East Gondwana: Supercontinent Assembly and Breakup. Geological Society of London Special Publications 206, pp. 35–55.

    Google Scholar 

  • Powell, C. M., Preiss, W. V., Gatehouse, C. G., Krapez, B., and Li, Z. X., 1994. South Australian record of a Rodinian epicontinental basin and its mid-Neoproterozoic breakup (∼ 700 Ma) to form the palaeo-Pacific Ocean. Tectonophysics, 237(3–4), 113–140.

    Article  Google Scholar 

  • Preiss, W. V., 2000. The Adelaide Geosyncline of South Australia and its significance in Neoproterozoic continental reconstruction. Precambrian Research, 100, 21–63.

    Article  Google Scholar 

  • Torsvik, T. H. et al., 2001. Rodinia refined or obscured: palaeomagnetism of the Malani Igneous Suite (NW India). Precambrian Research, 108(3–4), 319–333.

    Article  Google Scholar 

  • Wang, X. C., Li, X. H., Li, W. X., and Li, Z. X., 2007. Ca. 825 Ma komatiitic basalts in South China: First evidence for >1500 °C mantle melts by a Rodinian mantle plume. Geology, 35(12), 1103–1106.

    Article  Google Scholar 

  • Wingate, M. T. D., and Giddings, J. W., 2000. Age and palaeomagnetism of the Mundine Well dyke swarm, Western Australia: implications for an Australia-Laurentia connection at 755 Ma. Precambrian Research, 100, 335–357.

    Article  Google Scholar 

  • Zhong, S., Zhang, N., Li, Z. X., and Roberts, J. H., 2007. Supercontinent cycles, true polar wander, and very long-wavelength mantle convection. Earth and Planetary Science Letters, 261, 551–564.

    Article  Google Scholar 

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Li, ZX. (2011). Breakup of Rodinia. In: Reitner, J., Thiel, V. (eds) Encyclopedia of Geobiology. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-9212-1_38

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