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fossils
the preserved remains or traces of ancient organisms, often found in sedimentary rocks, providing insights into past life and environments.
Requirements of fossilization
Must be Dead (there are NO living fossils!)
Must have hard parts: bones, teeth, shells, etc.
Rapid burial: to prevent being eaten by scavengers or others.
Remain undisturbed: not be exposed or dug up by erosion processes or avengers.
Methods of fossilization
Various processes, including permineralization, cast and mold formation, and amber preservation, that lead to the preservation of organic remains.
Types of fossils
Preserved remains
Trace fossil
Mold fossil
Cast fossil
Petrified fossil
Carbon film
Original remains
Fossils that include the actual tissue of the organism, preserved in its original form, such as insects in amber or frozen mammoths.
Replacement
A form of fossilization where the original organic material is replaced with minerals, preserving the structure of the organism.
Carbonization
only a thin organic film remains of organism, usually preserved in shale; remainder of flesh & bone has decayed away.
Permineralization
A process of fossilization where minerals fill the spaces within the organic tissues, preserving the internal structure of the organism.
Recrystallization
A fossilization process in which original minerals of a shell or skeletal structure dissolve and re-form into new crystals, often making them more stable.
Trace fossils
Fossilized evidence of an organism's activity, such as footprints, burrows, or feces, rather than the organism itself.
Casts & Molds
external and internal impressions of the organism; most common type of fossil
Coprolites (dung)
fossilized feces that provide insight into an animal's diet and behavior.