To support the scientists' claim about major plate motions dividing two landmasses around 200 million years ago, the properties of the fossils can be categorized based on their depth and similarity across the two locations.
Here are the properties you can move:
-
Fossil snails closest to the surface:
- Similarities in the physical characteristics of surface-level fossils from both locations. (Supports the claim that they were once part of the same landmass.)
-
Fossil snails buried most deeply:
- Differences in the physical characteristics of the deeply buried fossils from both locations. (Supports the claim that after separation, the two populations evolved differently.)
So the groupings would look like this:
- Blank space 1: Similarities in the physical characteristics of surface-level fossils from both locations.
- Blank space 2: Differences in the physical characteristics of the deeply buried fossils from both locations.
This setup highlights both the shared ancestry of the fossils from when the landmasses were joined, as well as the divergence that occurred after their separation.