Alfred Wegener proposed the theory of continental drift in 1912, which stated that around 250 million years ago, all the continents were joined together in a supercontinent called Pangaea, and have been gradually drifting apart to their current positions. As evidence, the continents appear to fit together like puzzle pieces, the same plant and animal fossils are found on different continents' coastlines, identical rock formations and sequences are found across separated continents, and tropical plant remains have been discovered in Antarctica along with evidence of simultaneous glaciation in other modern landmasses. However, the theory lacked a proposed mechanism for continental movement and was not widely accepted by the scientific community at the time.