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The supercontinent cycle: A retrospective essay
Institution:1. Department of Geological Sciences, 316 Clippinger Laboratories, Ohio University, Athens, OH 45701, USA;2. Department of Earth Sciences, St. Francis Xavier University, Antigonish, Nova Scotia, Canada B2G 2W5;3. China University of Geosciences Beijing, 29 Xueyuan Road, Haidian District, 100083 Beijing, China;4. Faculty of Science, Kochi University, Kochi 780-8520, Japan;1. Geodynamics Team, Geological Survey of Norway, Leiv Eirikssons vei 39, 7040 Trondheim, Norway;2. The Centre for Earth Evolution and Dynamics, University of Oslo, Sem Selands vei 24, 0316 Oslo, Norway;3. School of Geosciences, University of the Witwatersrand, Johannesburg, South Africa
Abstract:The recognition that Earth history has been punctuated by supercontinents, the assembly and breakup of which have profoundly influenced the evolution of the geosphere, hydrosphere, atmosphere and biosphere, is arguably the most important development in Earth Science since the advent of plate tectonics. But whereas the widespread recognition of the importance of supercontinents is quite recent, the concept of a supercontinent cycle is not new and advocacy of episodicity in tectonic processes predates plate tectonics. In order to give current deliberations on the supercontinent cycle some historical perspective, we trace the development of ideas concerning long-term episodicity in tectonic processes from early views on episodic orogeny and continental crust formation, such as those embodied in the chelogenic cycle, through the first realization that such episodicity was the manifestation of the cyclic assembly and breakup of supercontinents, to the surge in interest in supercontinent reconstructions. We then chronicle some of the key contributions that led to the cycle's widespread recognition and the rapidly expanding developments of the past ten years.
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