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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?

How do paleontologists identify fossils?

A palentologist excavating fossils using tools.

© Michael Collier

This paleontologist is excavating fossils in Colorado's Dry Mesa Quarry. It is part of the Morrison Formation and has a great diversity of animals from the Jurassic Period. It is considered to be the best quarry in the world for the Jurassic. Located near Delta, Colorado excavation at the Dry Mesa Quarry began in 1972.

A paleontologist collects as many fossils as possible from a rock or sediment. Once the fossils are prepared by scraping and cleaning, they are sorted by geometry. Fossils with very similar geometry are assumed to belong to a single species. Fossils with somewhat different geometry are assumed to belong to a different species. Usually the fossil species has already been studied and named. Sometimes, however, the species is a new one. Then the paleontologist writes a detailed description of the new species, gives the new species a name, and publishes the description for others to read and use in their own work. Not much excites a paleontologist more than discovering a new species!

Sorting fossils is tricky business, for several reasons. Some organisms died when they were young and still developing, and some died when they were old. Some were male and some were female. Also, most species show a lot of natural variability. You know that from looking at other members of your own species! It's often impossible for paleontologists to decide whether they are looking at a single species with a lot of variability, or two similar species.

Fossilized algae.

© Marli Miller, University of Oregon

Precambrian stromatolites. This sample is Conophyton - a species of conical shaped stromatolites. Stromatolites, algae and cyanobacteria were the earliest life forms to populate the oceans of Earth.

The oldest fossils are more than three and a half billion years old. They are simple unicellular (single-celled) algae, very similar to algae that still exist today. Evolution was very slow until about seven hundred million years ago, when unicellular organisms with larger and more complex cells evolved. Not long after that, a little more than half a billion years ago, multicellular (many-celled) organisms appeared. Instead of consisting of just a single cell, multicellular organisms have an enormous number of cells, grouped according to their function. Several kinds of multicellular organisms evolved in a very short time, geologically. Paleontologists still do not understand very well how this happened. Many of these early kinds of multicellular organisms, like clams, snails, and corals, are still abundant today. More complex kind of animals, like reptiles, birds, and mammals, evolved even more recently in geologic time.

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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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