Here's why:
* Plate tectonics: The Earth's continents are situated on large tectonic plates that move and interact with each other over geological time.
* Pangea: During the late Paleozoic, all the continents were joined together in a supercontinent called Pangea. This single landmass existed in a different position than any of the modern continents.
* Continental drift: After Pangea broke apart, the continents continued to drift and shift, ultimately forming the continents we see today.
Therefore, no single continent can be said to occupy the exact same position as it did in the late Paleozoic.
However, we can say that parts of multiple modern continents were part of Pangea and therefore occupied similar geographic positions.