In the 1600s, the first accurate world maps became available. People noticed that the continents apparently fit together like jigsaw-puzzle pieces. This was the first evidence of continental drift. It was hundreds of years later that Wegener began to see further evidence from other sources.
In 1855, the German scientist Edward Suess found fossils of the extinct Glossopteris fern tree in South America, Africa, Australia, India, and Antarctica (see dark green). Typically, seeds can be spread by wind, water or being eaten animals and as the animals travel, they deposited the seeds in their feces/waste in new locations. Glossopteris seeds were too heavy to travel by wind and too fragile to survive the trip across the salty oceans so they must have been spread by traveling animals. To Wegener and other early believers of continental drift, this suggested that these landmasses must have once been much closer together for the fern to have spread so widely.