fossiilittomiin
Fossilization is the process by which remains, impressions, or traces of animals, plants, and other organisms are preserved in the Earth's crust. This process occurs over millions of years and involves the replacement of organic material with minerals, the preservation of imprints, or the entrapment of organisms in amber. Fossilization is a critical aspect of paleontology, the study of prehistoric life, as it provides evidence of past life forms and their environments.
The process of fossilization begins when an organism dies and is buried in sediment, such as sand,
1. Body fossils: These are the most common type of fossils and include the preserved remains of
2. Trace fossils: These are evidence of an organism's activity, such as footprints, burrows, or coprolites (fossilized
3. Impression fossils: These occur when an organism is buried in sediment, and the surrounding material hardens,
4. Amber fossils: These are organisms preserved in tree resin, which hardens over time. Amber fossils provide
Fossilization is influenced by various factors, including the type of organism, the environment in which it