Ichnology

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Thalassinoides, burrows produced by crustaceans, from the Middle Jurassic, Makhtesh Qatan, southern Israel.

Ichnology is the branch of geology and biology that deals with traces of organismal behavior, such as burrows and footprints. It is generally considered as a branch of paleontology; however, only one division of ichnology, paleoichnology, deals with trace fossils, while neoichnology is the study of modern traces. Parallels can often be drawn between modern traces and trace fossils, helping scientists to decode the possible behavior and anatomy of the trace-making organisms even if no body fossils can be found. An ichnologist is a scientist whose area of study and research is ichnology.

Overview

Dinosaur footprints, preserved at Dinosaur Ridge.

Ichnologic studies are based on the discovery and analysis of biogenic structures: features caused by living organisms. Thus, burrows, trackways, trails and borings are all examples of biogenic structures, but not casts or molds of dead shells or other bodily remains. To keep body and trace fossils nomenclatorially separate, ichnospecies are erected for trace fossils. Ichnotaxa are classified somewhat differently in zoological nomenclature than taxa based on body fossils (see trace fossil classification for more information).

Examples include:

History

Charles Darwin's The Formation of Vegetable Mould through the Action of Worms[lower-alpha 1] is an example of a very early work on ichnology, describing bioturbation and, in particular, the burrowing of earthworms.[1]

See also

References

  1. ↑ Donovan, Stephen K., ed. (1994). The Palaeobiology of Trace Fossils. John Wiley & Sons. ISBN 0-471-94843-8.

Further reading

  1. ↑ Darwin, C. R. (1881), The formation of vegetable mould, through the action of worms, with observations on their habits, London: John Murray, retrieved 26 September 2014

External links

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