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Glossopteris, a seed fern found in fossil records across several continents, played a crucial role in Alfred Wegener's hypothesis of continental drift. Its widespread distribution in now-separated landmasses, such as South America, Africa, Antarctica, and Australia, provided evidence that these continents were once joined. The presence of Glossopteris in these diverse locations suggested that they must have been connected in a single landmass, which Wegener named Gondwana. This fossil evidence supported his argument for the movement of continents over geological time.
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