Assembly and Breakup of Rodinia (Some results of IGCP project 440)

  • S. V. Bogdanova
  • S. A. Pisarevsky
  • Z. X. Li

DOI: 10.1134/S0869593809030022

Cite this article as:
Bogdanova, S.V., Pisarevsky, S.A. & Li, Z.X. Stratigr. Geol. Correl. (2009) 17: 259. doi:10.1134/S0869593809030022


The principal results of project 440 “Assembly and Breakup of Rodinia” of the International Geological Correlation Programme (IGCP) are reviewed in this work. A map of that supercontinent compiled using geological and paleomagnetic data describes global paleogeography 900 Ma ago. The assembly of Rodinia, which comprised most of Precambrian continental blocks, lasted ca. 400 m.y. (from 1300 to 900 Ma). Its breakup presumably triggered by mantle superplume took place between 830 and 650 Ma. The correlation between tectonic events in different continental blocks is considered. Some problems concerning the Rodinia reconstruction and history, e.g., the slow growth of juvenile crust and effects of mantle-plume events during the amalgamation period and of glaciations at the breakup time, are discussed. The latter caused changes in the biosphere and climate, whereas postglacial periods stimulated progress in biota evolution.

Key words

Mesoproterozoic Neoproterozoic Rodinia paleogeographic reconstruction supercontinent mantle plume glaciation 

Copyright information

© Pleiades Publishing, Ltd. 2009

Authors and Affiliations

  • S. V. Bogdanova
    • 1
  • S. A. Pisarevsky
    • 2
  • Z. X. Li
    • 3
  1. 1.Department of GeologyLund UniversityLundSweden
  2. 2.School of GeoSciencesUniversity of EdinburghEdinburghGreat Britain
  3. 3.Department of Applied GeologyCurtin University of TechnologySydney, West AustraliaAustralia

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