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Another important piece of evidence in the Continental Drift theory is the fossil relevance. There are various examples of fossils found on separate continents and in no other regions. This indicates that these continents had to be once joined together because the extensive oceans between these land masses act as a type of barrier for fossil transfer.
Alfred Wegener and the Theory of Continental Drifting. The theory of continental drifting was first introduced by a German meteorologist and geophysicist named Alfred Wegener in 1915, when he published his book, The Origin of Continents and Oceans.lfred Wegener and the Theory of Continental Drifting. The theory of continental drifting was first introduced by a German meteorologist and geophysicist named Alfred Wegener in 1915, when he published his book, The Origin of Continents and Oceans.