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... little is known about the geodynamic state of Rodinia.
The latitude of individual plates at the time of Rodinia can be known from clues provided by paleomagnetism, but the longitude of where it was at that time must be inferred from similar geological features that are now scattered around the world.
About 700 million years ago, during the Ice Age, the Earth entered a snowball Earth state, and the global temperature dropped rapidly.
The rapid evolution of organisms in the Ed ...
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