Protichnites

''Protichnites'' is an ichnogenus of trace fossil consisting of the imprints made by the walking activity of certain arthropods. It consists of two rows of tracks and a medial furrow between the two rows. This furrow, which may be broken, set at an angle, and of varying width and depth, is thought to be the result of the tail region contacting the substrate.

The first footprints on land

Sir Richard Owen, the noted British paleontologist and anatomist who coined the term “ Dinosauria”, based ''Protichnites'' on trackways that were shipped to him from the Cambrian Potsdam Sandstone of Quebec.Owen, 1851 He was correct in recognizing that these were the oldest known footprints on land, having been produced in intertidal and supratidal environments during what would now be called Cambrian times.Collette and Hagadorn, 2010

The ''Protichnites'' makers

Owen first thought that these trackways were made by tortoises, but new material convinced him that “articulates” (a group that included the arthropods) were responsible.Owen, 1852 He further suggested a kinship with ''Limulus'', the modern horseshoe crab. Additional material was collected in Quebec, Ontario, New York, Wisconsin, and Missouri for the next 150 years without a single fossil of the maker of these traces. Finally, body fossils of potential makers were found in two of the same quarries that preserved ''Protichnites'' from the Elk Mound Group of Blackberry Hill, Wisconsin, and the Potsdam Group of Melocheville, Quebec. The animals, ''Mosineia macnaughtoni'' and ''Mictomerus melochevillensis'', were euthycarcinoids, extinct arthropods that may have given rise to the mandibulates. Fossils that clearly tie euthycarcinoids to ''Protichnites'' were then found at Blackberry Hill.Collette et al., 2012

It is possible that other extinct arthropods, such as members of the Aglaspidida, may also have produced some of these trackways. Trilobites have been suggested as well; however, no trilobites have been found thus far in the strata that contain this ichnogenus. Similar trackways are present in post-Cambrian strata; however, those are seldom referred to as ''Protichnites''.

Possible mating behavior

It has been suggested that one form of ''Protichnites'', ''P. eremita'' Form 1, may have been produced by an ambulating pair of individuals, as in amplexus. In this form, the medial furrow is discontinuous and each section is set at an angle, such that the series of medial imprints have a shingled appearance, as might result if the female were displacing her tail to minimize its interference with external fertilization. A second set of medial imprints observed in Form 1 is postulated to have been produced by the tail region of the male of the pair. ''Protichnites eremita'' was originally interpreted as early evidence of hermit crab-like behavior.

Relationship with ''Diplichnites''

Differing only in the presence or absence of a medial furrow, ''Protichnites'' and ''Diplichnites'' trackways could both be produced by the same individual animal. In cases where the feet penetrate the sediment more deeply than does the tail, ''Diplichnites'' could be created on the underlying layer while ''Protichnites'' is being produced on the surface.Hoxie, 2005

References

Further reading

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External links

Discusses a major source of ''Protichnites'' trackways.

{{Taxonbar, from=Q7251819

Cambrian arthropods
Arthropod trace fossils
Paleozoic life of Ontario