Identify how fossil evidence supports plate tectonics and continental drift?

Fossil evidence supports plate tectonics and continental drift by showing that identical species of plants and animals, such as the Mesosaurus and Glossopteris, are found on continents that are now widely separated, like South America and Africa. This distribution suggests these continents were once connected, allowing species to inhabit a continuous landmass. Additionally, the presence of similar fossils across different continents indicates that they were once part of a single supercontinent, lending credence to the theory of continental drift. Overall, fossil evidence provides a historical record of how landmasses have shifted over geological time.