Wegener used several lines of fossil evidence to support his theories of continental drift and plate tectonics. One piece of evidence was the discovery of identical fossil plants and animals on continents that are now separated by vast oceans, such as the same fossil ferns found in South America, Africa, India, and Australia. Another piece of evidence was the existence of ancient marine fossils found at high elevations and in inland areas, suggesting that these areas were once submerged under a large body of water. Wegener also pointed to the discovery of fossils of similar land animals on different continents, implying that these continents were once connected and shared a common environment.
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Wegener used fossil evidence to support his theories of continental drift and plate tectonics. He found identical plant and animal fossils on continents now separated by oceans. He also discovered ancient marine fossils at high elevations and inland areas. Wegener's findings also included similar land animal fossils on different continents, suggesting they were once connected.
To support his theories of continental drift and plate tectonics, Wegener used several lines of fossil evidence. First, he noted that identical fern fossils were found in South America and Africa, suggesting that these continents were once connected. Second, he observed that the fossils of certain land-dwelling reptiles, such as the Mesosaurus, were found in both South America and Africa. This indicated that these continents were once joined, as these reptiles would not have been able to swim long distances across oceans. Lastly, he found similar fossil assemblages of plants and animals in locations that are now separated by vast bodies of water, supporting the idea that these landmasses were once connected.
