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  • Continental Drift: How Fossil Evidence Supports Plate Tectonics
    The fact that similar fossils are found on both sides of the ocean is evidence for continental drift.

    Here's why:

    * Fossil Distribution: The presence of identical or very similar fossils on continents now separated by vast oceans suggests that these landmasses were once connected.

    * Pangea: The theory of continental drift proposes that all the continents were once joined together in a supercontinent called Pangea.

    * Evidence for Drift: Fossils of land animals, freshwater plants, and other organisms that could not have crossed vast oceans provide strong evidence that these continents were once contiguous.

    For example: Fossils of the ancient reptile Mesosaurus have been found in both South America and Africa. Mesosaurus was a freshwater reptile that could not have swum across the Atlantic Ocean. This suggests that South America and Africa were once joined together.

    Other evidence for continental drift:

    * Matching geological formations: Rock formations and mountain ranges on different continents align perfectly when the continents are reconstructed into Pangea.

    * Paleoclimatic data: Glacial deposits and ancient climates in different regions point to a connected landmass.

    Overall, the distribution of similar fossils across continents is a key piece of evidence supporting the theory of continental drift and the existence of Pangea.

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