1. Wider Geographic Distribution:
* Fossils: Many fossil species lived across vast geographic areas, including different continents. This makes them excellent indicators of time periods, even if the rock types themselves differ.
* Rock Types: Rock types often form in specific environments and can be limited in their geographic distribution. A sandstone layer in one continent might not necessarily be the same age as a sandstone layer on another continent.
2. Greater Specificity in Time:
* Fossils: Certain fossils, known as index fossils, represent specific time periods. They evolve and become extinct rapidly, making them highly effective for dating rock layers.
* Rock Types: Rock types can form over long periods, making it difficult to pinpoint an exact time period for a layer.
3. Unique Evolutionary History:
* Fossils: Each fossil species represents a unique point in evolutionary history. This helps to establish the relative ages of rock layers, even if the rock types themselves are similar.
* Rock Types: While rock types can provide clues about the environment of formation, they don't necessarily indicate the time period as directly as fossils.
4. Less Susceptible to Local Variation:
* Fossils: Fossils often represent organisms that lived over wide geographic areas, making them less influenced by local environmental factors that can alter rock types.
* Rock Types: Rock types can be significantly influenced by local conditions, making it difficult to correlate layers across continents based on lithology (rock type) alone.
Example:
Imagine two continents, separated by a vast ocean, with rock layers containing fossils of the same dinosaur species. Even though the rock types might differ due to different geological processes, the presence of the same dinosaur fossil strongly suggests that the layers are roughly the same age.
Conclusion:
While rock types can provide some information about the age and environment of formation, fossils offer a more reliable and specific way to correlate rock layers across continents. Their unique evolutionary history, wide geographic distribution, and distinct time signatures make them invaluable tools for understanding Earth's history.