Scientists use evidence of past environments preserved in rock in the following two ways:
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To confirm whether an organism could have lived where its fossils are found: By analyzing the characteristics of the rock and its fossil content, scientists can infer the environmental conditions that existed when the organisms were alive. This helps determine if the specific organism could have thrived in that environment.
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To confirm that conditions in different places have changed: Studying the layers of rock and the fossils within them can reveal how environments have shifted over time across different regions. This allows scientists to understand geological and climatic changes and how they may have influenced the evolution of life on Earth.
These applications help reconstruct past ecosystems and inform our understanding of biological and environmental changes throughout Earth's history.