Answer:
Step-by-step explanation:
The Glossopteridales fossil occurs on most landmasses. This suggests that the continents were once merged into supercontinents. The Glossopteridales were a group of plants that lived during the Permian period and were found on every continent that existed at the time. The fact that these fossils are found on multiple continents suggests that the continents were once connected as part of a supercontinent, which eventually broke apart and drifted to their current locations. This supports the theory of plate tectonics, which suggests that the Earth's crust is made up of several plates that move and shift over time.