Everything about Coprolites totally explained
A
Coprolite is the fossil that results when human or animal dung is
fossilized. They 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. They serve a valuable purpose in
paleontology because they provide direct evidence of the predation and diet of extinct organisms. Coprolites may range in size from a few millimetres to over 60 centimetres.
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 indentified unambiguously, especially with more ancient examples. 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. In another example, the existence of human proteins in coprolites can be used to pinpoint the existence of cannibalistic behavior in an ancient culture.
Recognizing coprolites
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 can, in some cases, be possible to determine 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, centered around
Cambridgeshire and the
Isle of Ely with its refining being carried out in
Ipswich by the Fison Company. Today, there's a Coprolite Street near Ipswich Docks where the Fisons works once stood. The industry declined in the 1880s but was revived briefly during the
First World War to provide phosphates for munitions.
Further Information
Get more info on 'Coprolites'.
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