Fossil Formation and Dating: Petrification, Types, and Processes

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Last updated 3:22 AM on 1/27/26
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19 Terms

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Petrification / permineralization

Sequence of events that turn the remains of organisms into a cast made of stone.

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Step 1 of Petrification

Animals or plants die and get covered with sediment.

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Step 2 of Petrification

The soft parts are decomposed by bacteria, but hard parts remain.

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Step 3 of Petrification

Sediment covering becomes compacted into rock, and water drains down through sediments bringing dissolved minerals.

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Step 4 of Petrification

Dissolved minerals replace other materials in bones and hard parts but maintain the shape of the material.

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Where to find fossils?

Sedimentary rock layers such as limestone, shale, and sandstone, often exposed by erosion.

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How are fossils created?

Dead organisms are rapidly buried by sediment to prevent decomposition.

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Ideal place for fossil formation

Bottom of a quiet area of a lake, safe from damage.

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Relative dating

Determines chronological order of fossils as older or younger based on position in rock layers without a specific age.

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Absolute dating

Calculates actual age in years using methods such as radiometric dating.

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Crinoids

Marine invertebrates, such as starfish, sea urchins, and scallops, are characterized by circular, stacked disc-shaped columnals.

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Trilobites

Extinct marine arthropods with three-lobed bodies were abundant during the Cambrian period.

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Coprolites

Fossilized poop that provides evidence of prehistoric animal diets and behaviors, classified as trace fossils.

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Amber

Fossilized tree sap containing preserved insects or plant matter.

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Brachiopods

Preserved shells of marine invertebrates that look like clams.

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Fossilized teeth

Mineralized remains of teeth from sharks, dinosaurs, or other vertebrates.

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Petrified wood

Wood that has turned into stone through the process of permineralization, where minerals replace the structure.

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Mold

Imprint in wet mud or sand that hardens. (into stone)

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Cast

Models formed from sediment or minerals filling a mold or decomposing organism replaced by minerals. (turned into stone)

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