Glossopteris flora was the first fossil to be linked to the theory of continental drift.
In the Permian and Triassic eras, Glossopteris was a common seed fern that thrived. Glossopteris fossils have been discovered in rocks that also include the plant's fossilised remains and imprints.
Geologist Eduard Suess unearthed fossilised remains of the extinct seed fern Glossopteris on three distinct continents during the first half of the 20th century. This made him think that the continents had once been part of a single, enormous supercontinent that had later drifted apart.
<h3>What is Continental drift ?</h3>
In the early 20th century, scientists began to gather data that suggested the continents could move about on the surface of the Earth. Evidence for continental drift has been based on the fit of the continents, the distribution of prehistoric fossils, rocks, and mountain ranges, as well as the locations of prehistoric climatic zones.
- The discovery of the fossilised remains of the freshwater reptile Mesosaurus in South Africa and Brazil serves as one example. The discovery of Lystrosaurus fossils in strata from the same age in regions of Africa, India, and Antarctica is another example.
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