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Learning about Fossils

  1. What is a fossil?
  2. How do fossils form?
  3. What effect does sediment size have on fossils?
  4. In what types of rocks do fossils form?
  5. What kinds of fossils are there?
  6. Under what conditions do fossils form?
  7. How do species change over geologic time?
  8. What can we tell from the fossil record?
  9. How can we tell how old rocks are?
  10. How do paleontologists identify fossils?
  11. How are living things adapted to their environments?

What kinds of fossils are there?

Picture of a fossilized fish.

© Michael Collier

This is a fossil of a fish that is common in the sedimentary rocks that were deposited in Cenozoic lakes in Utah.

Sediments are home for many kinds of marine animals. Some animals live on the surface of the sediment, and some burrow into it. Some fossil shells are found mixed with the mud they lived in. Other fossil shells were moved by strong currents and deposited along with sand or even gravel. If the shells are buried by more sediment before they are worn away or dissolved, they become fossilized.


Picture of a fossilized clam next to a hammer.

© Michael Collier

This fossil clam was found in the Green River Formation near Utah's Roan Cliffs.

Sometimes a fossil consists of original shell material. This is common in very young sediments that have not yet been turned into rock. Older sediments usually have been buried deeply by later sediments and turned into rock. Then it is more likely that the original shell has been dissolved away by water seeping through the pore spaces in the sediment. The fossil is left as an imprint of the original shell. An imprint like that is called a mold. Sometimes the space that was occupied by the shell is now empty. In other cases that space has been filled with later minerals that were precipitated by the flowing pore water. That material, which has the shape of the original shell, is called a cast.

Picture of a fossilized clam.

© Oklahoma University

Clams valves are hinged along one edge.

Clams have shells that are in two parts, called valves. The valves are hinged along one edge. They are left and right, like your hands when you put them together along your little fingers. The clam can open its shell to feed and close its shell for protection. Think about what you might see when the clam shell is fossilized. Each valve has an outer surface and an inner surface. Depending on which valve you are seeing, and whether you are seeing the inside or the outside of it, and whether you are seeing its cast or its mold, eight different views are possible! Paleontologists have to be very careful to match up the fossils they see. Otherwise, they might think they are seeing fossils of several different kinds of animal rather than just one.

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Fossil of the skull of a saber-toothed cat, an extinct mammal that lived in the Pleistocene epoch. Albert Copley © Oklahoma University; Image Courtesy of the Earth Science World Image Bank.  Photo ID: hn81e5

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Last updated:July 23, 2008


This project is supported by the AGI Foundation. Opinions expressed are those of the authors and not necessarily those of the Foundation.

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