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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 is a fossil?

Image of a Ovis catclawensis on exhibition in a museum.

© Oklahoma University

Fossil of Ovis catclawensis, which belongs to the family of bighorn sheep, but much larger than the modern bighorn sheep. It lived in the Pleistocene epoch.

A fossil is any evidence of past life. Fossils formed from animal bodies or their imprints are called body fossils. When people think about fossils, they usually think about body fossils. Trace fossils are another kind of fossil. A trace fossil is any evidence of the life activity of an animal that lived in the past. Burrows, tracks, trails, feeding marks, and resting marks are all examples of trace fossils. It is usually hard to figure out exactly which kind of animal made a particular trace fossil. Trace fossils are useful to paleontologists (scientists who study past geologic time based on fossils), however, because they tell something about the environment where the animal lived and the animal's behavior.

 

Earth Science Images

Animations

News

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: May 13, 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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