Isopodichnus

{{Short description|Trace fossil}}

{{Ichnobox

| fossil_range = {{fossil range|221.5-205.6}}

| image =

| image_alt =

| image_caption =

| parent_authority =

| taxon = Isopodichnus

| authority = Bornemann 1889

| type_ichnospecies =

| type_ichnospecies_authority =

| subdivision_ranks = Ichnospecies

| subdivision_ref = IRMNG (2019). Isopodichnus Bornemann, 1889 †. Accessed at: http://www.irmng.org/aphia.php?p=taxdetails&id=1012179 on 2020-02-24

| subdivision = *{{extinct}}Isopodichnus queenslandensis Cook & Bann, 2000

| synonyms =

| synonyms_ref =

}}

Isopodichnus is an ichnogenus of trace fossil. Ribbon-like in form, Isopodichnus traces were likely formed by the activity of an isopod crustacean foraging within the preserved sediment. Parallel to the bedding plane, a central furrow is flanked by two hypichnial ridges. Trails may also exhibit scratch marks and be associated with Rusophycus-like resting traces. Isopodichnus are very similar in form to Cruziana traces, making delineation of the two forms difficult, and controversial.Richard G. Bromley (1996): Trace Fossils: Biology, Taphonomy and Applications. Second Edition, Chapman & Hall, p. 187 ([https://books.google.com/books?id=ngZI35A1os0C&pg=PA184 GoogleBooks)].

Image:trace2.jpg|Isopodichnus trace fossil from the upper carboniferous - (Scotland, St Monans, Fife) (two penny piece for scale)

Image:trace3.jpg|Close up

Image:Cruziana2.jpg| Cruziana trace, possibly formed by a Trilobite.

See also

References

{{Reflist}}

Further reading

  • Mikuláš R. (1992): Trace fossils from the Kosov Formation of the Bohemian Upper Ordovician, Sbor. geol. Věd, Paleont., 32, 9-54

{{Taxonbar|from=Q6086224}}

Category:Arthropod trace fossils

{{trace-fossil-stub}}