The discussion centers on the methods of dating fossils and rock layers as described in "Concepts in Modern Biology." It highlights that both fossils and rock layers can help determine each other's ages, provided there is a solid understanding of the geological sequence. Fossils known to exist only in specific geological periods, such as mid-Jurassic, can indicate the age of the rocks they are found in. Indicator fossils, which evolved rapidly and had short lifespans, can narrow down rock ages to within a few million years. While relative dating methods, such as stratigraphy, can establish the sequence of ages (e.g., one fossil being younger than another), absolute dating through radioactive methods is necessary for precise age determination. The discussion emphasizes that much of the sedimentary rock in the UK was assigned relative ages before the advent of radioactive dating, demonstrating the effectiveness of stratigraphy and fossil evidence in dating geological formations.