Diplichnites

Diplichnites
Temporal range:
Oblique bedding plane view of large Diplichnites from the Joggins Formation (Pennsylvanian), Cumberland Basin, Nova Scotia. This trackway was made by the myriapod Arthropleura.
Trace fossil classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Arthropoda
Ichnogenus: Diplichnites
d'Orbigny, 1842

Diplichnites are arthropod trackways with two parallel rows of blunt to elongate, closely spaced tracks oriented approximately perpendicularly to the mid-line of the trackway. The term is more often used for the ichnofossils of this description; however, similar trackways from recent arthropods are sometimes given this name as well.