Final answer:
The presence of Mesosaurus, Cynognathus, and Lystrosaurus fossils on separate continents is evidence for continental drift since these animals, being poor swimmers, could not have crossed large oceans, indicating the continents were once connected.
Step-by-step explanation:
The shared distribution of fossils like Mesosaurus, Cynognathus, and Lystrosaurus across continents that are currently separated by vast oceans is a strong piece of evidence for continental drift. These fossils suggest that the landmasses where these creatures live must have been connected because these animals were very poor swimmers and could not have crossed such large distances. The early Mesozoic reptiles were adapted for life on land or in small bodies of water, not in the open ocean, and they reproduced by laying eggs on land, which underlines the impossibility of their distribution being due to crossing oceans.
Alfred Wegener's theory of continental drift was supported by the presence of these fossils in South America and Africa, which were part of the supercontinent Pangaea. This suggests that these continents were once joined before the drifting apart that gave us our current geographical layout. This theory helped negate the improbable hypothesis that these poorly swimming reptiles could somehow have spread across the enormous oceans.