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  • Glossopteris: The Fossil Evidence for Continental Drift
    The fossil fern that supported the hypothesis of continental drift is Glossopteris.

    Here's why:

    * Wide Distribution: Glossopteris fossils were found on widely separated landmasses, including South America, Africa, India, Australia, and Antarctica. This distribution was difficult to explain if the continents were always in their current positions.

    * Unique Features: Glossopteris had distinctive features, such as tongue-shaped leaves and a unique vein pattern, that made it easy to identify and distinguish from other ferns.

    * Climate and Environment: Glossopteris was a type of fern adapted to a temperate climate. The fact that it was found on continents with vastly different climates today (like tropical India and frigid Antarctica) indicated that these landmasses must have been closer together in the past.

    Alfred Wegener, a key proponent of continental drift, used the widespread distribution of Glossopteris as evidence to support his theory. The discovery of Glossopteris, along with other fossil evidence and geological observations, helped to build the case for the movement of continents over millions of years.

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