Wintonopus Explained

Wintonopus is an ichnogenus of dinosaur footprint. Its footprints have been found at Lark Quarry in Queensland Australia. The genus is named after the Winton Formation in which the tracks were found.^[1] Other tracks were found in the Broome Sandstone of Dampier Peninsula, Western Australia.

See also

• List of dinosaur ichnogenera

Further reading

• Book: Glut, Donald F. . Dinosaurs: The Encyclopedia. 3rd Supplement . 2003 . McFarland & Company, Inc. . Jefferson, North Carolina . 0-7864-1166-X . Appendix: Dinosaur Tracks and Eggs . 613–652 . registration . https://archive.org/details/dinosaursencyclo00glut_2/page/613 .
• S. W. Salisbury, A. Romilio, M. C. Herne, R. T. Tucker, and J. P. Nair. 2016. The Dinosaurian Ichnofauna of the Lower Cretaceous (Valanginian–Barremian) Broome Sandstone of the Walmadany Area (James Price Point), Dampier Peninsula, Western Australia. Society of Vertebrate Paleontology Memoir 16. Journal of Vertebrate Paleontology 36(6, suppl.):1-152
• R. A. Thulborn and M. Wade. 1984. Dinosaur trackways in the Winton Formation (mid-Cretaceous) of Queensland. Memoirs of the Queensland Museum 21(2):413-517

Notes and References

1. http://www.fossilworks.org/cgi-bin/bridge.pl?a=taxonInfo&taxon_no=81250 Wintonopus