Fossilization is the process by which the remains or traces of organisms from the past are preserved in the Earth’s crust. This process takes millions of years and involves several steps.
Death of Organism: When an organism dies, its remains can become buried in sediment. This is the first step in the fossilization process.
Burial and Sedimentation: The remains of the organism become buried by sediment, such as mud, silt, or sand, which protects the remains from being destroyed or decaying.
Decay and Permineralization: Over time, the organic material in the remains decays, leaving behind only the hard parts, such as bones, shells, or teeth. As the remains are buried deeper, minerals from the surrounding sediment seep into the pores of the remains, a process called permineralization. This can preserve the original structure of the remains.
Compression and Recrystallization: The weight of the sediment above the remains compresses them, causing the minerals to reorganize and recrystallize. This can help to further preserve the remains.
Discovery and Study: Once exposed, fossils can be discovered by paleontologists and studied to learn about the organisms that lived in the past and the conditions of the Earth at that time.
Study Guide for Fossilization:
Types of Fossils: Learn about the different types of fossils, such as petrified fossils, mold and cast fossils, carbon films, and preserved remains.
From Molecules to Organisms: Structures and Processes
Students who demonstrate understanding can:
Use argument based on empirical evidence and scientific reasoning to support an explanation for how characteristic animal behaviors and specialized plant structures affect the probability of successful reproduction of animals and plants respectively.