A coprolite is fossilized feces, classed as a trace fossil because it records what an animal ate rather than what it looked like. Much of the original material has been replaced by minerals such as silicates and calcium carbonates. William Buckland named them in 1829, after Mary Anning noticed that "bezoar stones" in ichthyosaur skeletons at Lyme Regis held fish bones and scales. Coprolites range from a few millimetres to over 60 centimetres and are known from rocks of Cambrian age to recent times worldwide.

Is this coprolite?

2-step field check

Run through these checks against the specimen in your hand. The more boxes tick, the more confident the ID.

  • 1
    Name the organism
    Decide what left the fossil before worrying about the rock. Organism: Trace fossil (fossilized feces); producer varies. Age: Cambrian to recent.
  • 2
    Check the preservation
    Preservation: Original material largely replaced by minerals such as silicates and calcium carbonates. That controls the weight, the hardness and how the piece takes a polish.

All properties

Uses
Scientific research
Organism
Trace fossil (fossilized feces); producer varies
Age
Cambrian to recent
Preservation
Original material largely replaced by minerals such as silicates and calcium carbonates

Where rockhounds find coprolite

Classic worldwide localities

  • Lias formation, Lyme Regis, England

More coprolite photos

  • Shark coprolite from the Cooper River, South Carolina
  • Brown coprolite with a deeply cracked surface

Common questions

Where is coprolite found?+
Notable localities include Lias formation, Lyme Regis, England.
What is coprolite used for?+
Coprolite is used in scientific research.

Find coprolite on the map

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