coprolite

A coprolite of a carnivorous dinosaur found in southwestern Saskatchewan.

A coprolite is fossilized animal dung. Coprolites are classified as trace fossils as opposed to body fossils, as they give evidence for the animal's behaviour (in this case, diet) rather than morphology. The name is derived from the Greek words κοπρος / kopros meaning 'dung' and λιθος / lithos meaning 'stone'. They were first described by William Buckland in 1829. Prior to this they were known as "fossil fir cones" and "bezoar stones." They serve a valuable purpose in paleontology because they provide direct evidence of the predation and diet of extinct organisms.^[1] Coprolites may range in size from a few millimetres to over 60 centimetres.

Coprolites, distinct from paleofaeces, are fossilized animal dung. Like other fossils, coprolites have had much of their original composition replaced by mineral deposits such as silicates and calcium carbonates. Paleofaeces, on the other hand, can be reconstituted to determine their original chemical properties.^[2]

Initial discovery

The fossil hunter Mary Anning had noticed that "bezoar stones" were often found in the abdominal region of ichthyosaur skeletons found in the Lias formation at Lyme Regis. She also noted that if such stones were broken open they often contained fossilized fish bones and scales as well as sometimes bones from smaller icthyosaurs. It was these observations by Anning that led the geologist William Buckland to propose in 1829 that the stones were fossilized feces and name them Coprolites. Buckland also suspected that the spiral markings on the fossils indicated that ichthyosaurs had spiral ridges in their intestines similar to those of modern sharks, and that some of these coprolites were black because the ichthyosaur had ingested ink from belemnites.^[3]

Research value

By examining coprolites, paleontologists are able to find information about the diet of the animal (if bones or other food remains are present), such as whether or not it was a herbivore, and the taphonomy of the coprolites, although the producer is rarely identified unambiguously, especially with more ancient examples.^[4] In one example these fossils can be analyzed for certain minerals that are known to exist in trace amounts in certain species of plant that can still be detected millions of years later.^[5] In another example, the existence of human proteins in coprolites can be used to pinpoint the existence of cannibalistic behavior in an ancient culture.^[6] Parasite remains found in human and animal coprolites have also shed new light on questions of human migratory patterns, the diseases which plagued ancient civilizations, and animal domestication practices in the past (see archaeoparasitology and paleoparasitology).

Recognizing coprolites

A Miocene pseudocoprolite from Washington state. Commonly mistaken for a coprolite because it looks so real; it is actually inorganic. Scale in mm. See Spencer (1993).

The recognition of coprolites is aided by their structural patterns, such as spiral or annular markings, by their content, such as undigested food fragments and by associated fossil remains. The smallest coprolites are often difficult to distinguish from inorganic pellets or from eggs. Most coprolites are composed chiefly of calcium phosphate, along with minor quantities of organic matter. By analyzing coprolites, it is possible to infer the diet of the animal which produced them.

Coprolites have been recorded in deposits ranging in age from the Cambrian period to recent times and are found worldwide. Some of them are useful as index fossils, such as Favreina from the Jurassic period of Haute-Savoie in France.

Some marine deposits contain a high proportion of fecal remains. However, animal excrement is easily fragmented and destroyed, so usually has little chance of becoming fossilized.

Coprolite mining

In 19th century England, coprolites were mined on an industrial scale for use as fertiliser due to their high phosphate content. The extraction occurred over the east of England, centred around Cambridgeshire and the Isle of Ely ^[7][8] with its refining being carried out in Ipswich by the Fison Company.^[8] Today, there is a Coprolite Street near Ipswich Docks where the Fisons works once stood.^[9] The industry declined in the 1880s ^[8][10] but was revived briefly during the First World War to provide phosphates for munitions.^[7]

See also

• Fossil
• Fossils and the geological timescale
• Gastrolith
• Lloyds Bank coprolite
• Regurgitalith

Look up coprolite in Wiktionary, the free dictionary.

References

• Spencer, P. K. (1993). "The "coprolites" that aren't: the straight poop on specimens from the Miocene of southwestern Washington State". Ichnos 2: 1–6. doi:10.1080/10420949309380097. 

This article incorporates text from the article "Coprolites" by Unsigned, in the Encyclopædia Britannica, Eleventh Edition, a publication now in the public domain.