Rhynchosauroides is an ichnogenus, a form taxon based on footprints. The organism producing the footprints was likely a lepidosaur[1] and may have been a sphenodont, an ancestor of the modern tuatara. The footprint consists of five digits, of which the fifth is shortened and the first highly shortened.[2]

Rhynchosauroides
Temporal range: Triassic-Cretaceous
~252–89 Ma
Trace fossil classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Ichnofamily: Rhynchosauroidae
Ichnogenus: Rhynchosauroides
Maidwell 1911
Ichnospecies

See text

Species edit

  • R. beasleyi Nopsca, 1923[3]
  • R. bornemanni Haubold, 1966[3]
  • R. brunswickii Ryan and Willard, 1947[4]
  • R. gangresci da Silva et al., 2012[5]
  • R. hyperbates Baird, 1957[6]
  • R. kuletae Baird, 1957[7]
  • R. majus Demathieu, 1967[8]
  • R. maximus Gand, 1974[9]
  • R. minutipes Maidwell, 1914[3]
  • R. pallinii Conti et al.', 1977[7]
  • R. palmatus Lull, 1942[10]
  • R. petri Demathieu, 1966[11]
  • R. pusillus Haubold, 1966[3]
  • R. rdzaneki Ptaszynski, 2000[12]
  • R. rectipes Beasley, 1911[13]
  • R. retroversipes da Silva et al., 2008[5]
  • R. santanderensis Demathieu and Saiz de Omeñaca, 1977[5]
  • R. schochardti von Lilienstern, 1939[14]
  • R. sphaerodactylus Demathieu, 1971[15]
  • R. tirolicus Abel, 1926[12]
  • R. triangulus Gand, 1977[16]
  • R. virgiliae Demathieu et al., 1978[5]

See also edit

References edit

  1. ^ Gand, G.; Demathieu, G. (2005). "Les pistes dinosauroïds du Trias moyen français: interprétation et réévaluation de la nomenclature [The French Middle Triassic dinosauroid trackways: interpretation and nomenclatural reevaluation]". Geobios. 38: 725–749. doi:10.1016/j.geobios.2005.04.001.
  2. ^ Hunt, Adrian P.; Lucas, Spencer G. (2007). "Late Triassic tetrapod tracks of western North America". New Mexico Museum of Natural History & Science Bulletin. 40: 215–230.
  3. ^ a b c d Demathieu, G.R.; Haubold, H. (1972). "Stratigraphische Aussagen der Tetrapodenfährten aus der terrestrischen Trias Europas [Stratigraphic statements about the tetrapod tracks from the European terrestrial Triassic]". Geologie. 21: 802–836.
  4. ^ Olsen, P.E.; Baird, D. (1986). "Milford revisited: with notes on a new ichnofaunule from the Norian of New Jersey". First International Symposium on Dinosaur Tracks and Traces, Abstracts with Program: 21–22.
  5. ^ a b c d Silva, Rafael Costa da; Sedor, Fernando Antonio; Fernandes, Antonio Carlos Sequeira (1 October 2012). "Fossil footprints from the Late Permian of Brazil: An example of hidden biodiversity". Journal of South American Earth Sciences. 38: 31–43. Bibcode:2012JSAES..38...31D. doi:10.1016/j.jsames.2012.05.001.
  6. ^ Baird, D. (1957). "Triassic reptile footprint faunules from Milford, New Jersey". Bulletin of the Museum of Comparative Zoology. 117 (5): 449–520.
  7. ^ a b Ptaszyński, T.; Niedźwiedzki, G. (2004). "Late Permian vertebrate tracks from the Tumlin Sandstone, Holy Cross Mountains, Poland". Acta Palaeontologica Polonica. 49 (2): 289–320. Retrieved 30 November 2021.
  8. ^ Demathieu, G.R. (1970). "Empreintes de Pas de Vertébrés du Trias de la Bordure Nord-Est du Massif Central (Vertebrate Footprints from the Triassic of the Northeast Border of the Massif Central]". Cahiers de Paléontologie: 1–211.
  9. ^ Gand, G. (1974). "Une nouvelle espèce ichnologique des Grès à Empreintes du Trias Moyen [A new ichnological species from the Middle Triassic Grès à Empreintes]". Bulletin Trimestriel de la Société d'Histoire Naturelle et des Amis du Muséum d'Autun. 70: 10–16.
  10. ^ Lull, R.S. (1942). "Chugwater footprints from Wyoming". American Journal of Science. 240 (7): 500–504. Bibcode:1942AmJS..240..500L. doi:10.2475/ajs.240.7.500.
  11. ^ Demathieu, G. (1966). "Rhynchosauroides petri et Spingopus ferox, nouvelles empreintes de Reptiles de grès triasiques de la bordure Nord-Est du Massif Central [Rhynchosauroides petri and Spingopus ferox, new reptile footprints from the Triassic sandstones of the northeast border of the Massif Central]". Comptes Rendus de l'Académie des Sciences, Série D. 263: 482–486.
  12. ^ a b Klein, Hendrik; Voigt, Sebastian; Saber, Hafid; Schneider, Jörg W.; Hminna, Abdelkbir; Fischer, Jan; Lagnaoui, Abdelouahed; Brosig, Andreas (July 2011). "First occurrence of a Middle Triassic tetrapod ichnofauna from the Argana Basin (Western High Atlas, Morocco)". Palaeogeography, Palaeoclimatology, Palaeoecology. 307 (1–4): 218–231. Bibcode:2011PPP...307..218K. doi:10.1016/j.palaeo.2011.05.021. S2CID 128396482.
  13. ^ Klein, Hendrik; Voigt, Sebastian; Hminna, Abdelkbir; Saber, Hafid; Schneider, Jörg; Hmich, Driss (31 August 2010). "Early Triassic Archosaur-Dominated Footprint Assemblage from the Argana Basin (Western High Atlas, Morocco)". Ichnos. 17 (3): 215–227. Bibcode:2010Ichno..17..215K. doi:10.1080/10420940.2010.510030. S2CID 140685089.
  14. ^ Klein, H.; Lucas, S.G. (2010). "Review of the tetrapod ichnofauna of the Moenkopi Formation/Group (Early-Middle Triassic) of the American Southwest". New Mexico Museum of Natural History and Science Bulletin. 50: 1–67.
  15. ^ Demathieu, G. (1971). "Cinq nouvelles espèces d'empreintes de Reptiles du Trias de la bordure nord-edt du Massif Central" [Five new species of reptile footprints from the Triassic of the northeastern border of the Massif Central]. Comptes Rendus de l'Académie des Sciences, Série D. 272: 812–814.
  16. ^ Gand, G. (1977). "Note sure un nouvel assemblage à traces de Vertébrés de l'Autunois. Son interprétation géologique [Note on a new assemblage with vertebrate traces from the Autunois. Its geological interpretation]". Bulletin trimestriel de la Société d'Histoire Naturelle et des Amis du Muséum d'Autun. 82: 9–16.