Isopodichnus
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.[2]
- Isopodichnus trace fossil from the upper carboniferous - (Scotland, St Monans, Fife) (two penny piece for scale)
- Close up
- Cruziana trace, possibly formed by a Trilobite.
Isopodichnus | |
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Trace fossil classification | |
Kingdom: | Animalia |
Phylum: | Arthropoda |
Subphylum: | Crustacea |
Class: | Malacostraca |
Superorder: | Peracarida |
Order: | Isopoda (?) |
Ichnogenus: | †Isopodichnus Bornemann 1889 |
Ichnospecies[1] | |
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See also
References
- IRMNG (2019). Isopodichnus Bornemann, 1889 †. Accessed at: http://www.irmng.org/aphia.php?p=taxdetails&id=1012179 on 2020-02-24
- Richard G. Bromley (1996): Trace Fossils: Biology, Taphonomy and Applications. Second Edition, Chapman & Hall, p. 187 (GoogleBooks).
External links
Further reading
- Mikuláš R. (1992): Trace fossils from the Kosov Formation of the Bohemian Upper Ordovician, Sbor. geol. Věd, Paleont., 32, 9-54
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