To accurately infer information about the rock sample based on relative dating methods, principles of stratigraphy, and index fossils, one would typically analyze the characteristics of the layers (strata) and the fossils present within them. The presence of specific index fossils and the order of the strata can help determine the relative ages of the rock layers and suggest how the environment may have changed over time.
Given the options provided, the most reasonable inference might be:
"In the past, the environment was aquatic but over time the environment changed to a terrain that required climbing."
This choice indicates a change in the environmental conditions, which is often supported by the presence of different types of fossils and sedimentary structures in various strata. For instance, if lower layers contain aquatic fossils and higher layers show evidence of terrestrial organisms or structures, it would suggest a transition from an aquatic to a terrestrial environment.
However, without specific details about the rock layers and the fossils present, it's challenging to draw definitive conclusions. The other options would need to be evaluated based on the actual evidence in the rock samples.