All of them; the movements have been ongoing so long, that every single continent has occupied effectively every latitude at some point.
This movement is called continental drift. The evidence for its occurence includes fossils found in both Brazil and South Africa, the same earthworm families found in South American and Africa, and widespread distribution of complimentory glacial sediments throughout South America, Africa and the Middle East. The continents will continue to slowly drift toward and away from each other through tectonophysics.
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