Otozoum

Otozoum ("giant animal") is an extinct ichnospecies of fossilized sauropodomorph dinosaur footprints and other markings in sandstones. They were made by heavy, bipedal animals (probably dinosaurs) with a short stride that walked on four toes directed forward.

Otozoum Temporal range: Late Triassic - Middle Jurassic, 221–175 Ma PreꞒ Ꞓ O S D C P T J K Pg N
Otozoum moodyi footprint
Trace fossil classification
Kingdom:	Animalia
Phylum:	Chordata
Clade:	Dinosauria
Clade:	Saurischia
Suborder:	†Sauropodomorpha
Ichnofamily:	†Otozoidae
Ichnogenus:	†Otozoum Hitchcock, 1847
Ichnospecies
†Otozoum caudatum Hitchcock, 1871 †Otozoum minus Lull, 1915 †Otozoum moodii Hitchcock, 1847 (type ichnospecies) †Otozoum moodyi Hitchcock, 1847

Otozoum tracks were discovered by American paleontologist Edward Hitchcock, who described Otozoum as the "most extraordinary track yet brought to light in this valley [the Connecticut River] representing a bipedal animal... distinguished from all others... in the sandstone of New England". The ichnogenus was named by him in 1847, after the giant Otus.[1]

In 1953, Yale University paleontologist Richard Swann Lull revised Hitchcock's work, suggesting that the track maker might have been a prosauropod. Other sources have been proposed, including a crocodile-like animal (e.g. the phytosaur Rutiodon), or an ornithopod dinosaur, although recent osteological comparisons (e.g., Rainforth, 2003) support Lull's hypothesis that the track maker was indeed a prosauropod.[2]

Hitchcock noted the excellent preservation of some tracks, preserving details of the skin, pads, and even impressions of Jurassic raindrops. Excellent Otozoum specimens from the Portland Quarry may be seen in the Dinosaur State Park and Arboretum in Rocky Hill, Connecticut.