Eubrontes

{{Short description|Fossilised dinosaur footprints}}

{{Ichnobox

| image = Dinosaur State Park (Rocky Hill, CT) - close-up.JPG

| taxon = Eubrontes

| authority = Hitchcock, 1845

| type_ichnospecies = {{extinct}}Eubrontes giganteus

| type_ichnospecies_authority = (Hitchcock, 1836)

| subdivision_ranks = Ichnospecies

| subdivision =

  • {{extinct}}Eubrontes approximatus (Hitchcock, 1865)
  • {{extinct}}Eubrontes divaricatus (Hitchcock, 1865)
  • {{extinct}}Eubrontes euskelosauroides Huene, 1932
  • {{extinct}}Eubrontes giganteus (Hitchcock, 1836)
  • {{extinct}}Eubrontes nobitai Xing et al, 2020
  • {{extinct}}Eubrontes platypus Lull, 1904
  • {{extinct}}Eubrontes tatricus Michalik & Sýkora, 1976
  • {{extinct}}Eubrontes thianschanicum (Roman)
  • {{extinct}}Eubrontes tuberatus (Hitchcock, 1858)
  • {{extinct}}Eubrontes veillonensis Lapparent & Monetnat, 1967
  • {{extinct}}Eubrontes nobitai Xing et al, 2020

}}

File:Eubrontes01.JPG Moenave Formation at the St. George Dinosaur Discovery Site at Johnson Farm, southwestern Utah.]]

Eubrontes is the name of fossilised dinosaur footprints dating from the Late Triassic and Early Jurassic. They have been identified from France, Poland, Slovakia,[http://dinosaurusblog.com/2011/01/21/879373-dinosauri-ze-slovenska/ Czech article about dinosaur trace fossil finds from Slovakia] Czech Republic,[http://dinosaurusblog.com/2015/08/03/druhohorni-plazi-v-cechach-v/ Czech article about dinosaur trace fossils found in the Czech Republic] Italy, Spain, Sweden, Australia (Queensland), US,{{Cite journal | last1 = Lockley | first1 = M. | last2 = Matsukawa | first2 = M. | last3 = Jianjun | first3 = L. | title = Crouching Theropods in Taxonomic Jungles: Ichnological and Ichnotaxonomic Investigations of Footprints with Metatarsal and Ischial Impressions | doi = 10.1080/10420940390256249 | journal = Ichnos | volume = 10 | issue = 2–4 | page = 169 | year = 2003 | s2cid = 128759174 | url = http://doc.rero.ch/record/14073/files/PAL_E1227.pdf }} India,{{Cite news|last=Iqbal|first=Mohammed|date=2021-09-03|title=Rajasthan: Footprints of 3 dinosaur species found in Thar desert|language=en-IN|work=The Hindu|url=https://www.thehindu.com/sci-tech/science/rajasthan-footprints-of-3-dinosaur-species-found-in-thar-desert/article36277165.ece|access-date=2021-09-13|issn=0971-751X}} China{{cite journal |title=The new ichnotaxon Eubrontes nobitai ichnosp. nov. and other saurischian tracks from the Lower Cretaceous of Sichuan Province and a review of Chinese Eubrontes-type tracks |author=Li-Da Xing |author2=Martin G. Lockley |author3=Hendrik Klein |author4=Li-Jun Zhang |author5=Anthony Romilio |author6=W. Scott Persons IV |author7=Guang-Zhao Peng |author8=Yong Ye |author9=Miao-Yan Wang |date=5 July 2021 |journal=Journal of Palaeogeography |volume=10 |issue=1 |page=17 |doi=10.1186/s42501-021-00096-y |bibcode=2021JPalG..10...17X |s2cid=235730384 |doi-access=free }} and Brazil (South).{{Cite journal |last=Silva |first=Rafael Costa da |last2=Barboni |first2=Ronaldo |last3=Dutra |first3=Tânia |last4=Godoy |first4=Michel Marques |last5=Binotto |first5=Raquel Barros |date=2012-11-01 |title=Footprints of large theropod dinosaurs and implications on the age of Triassic biotas from Southern Brazil |url=https://www.sciencedirect.com/science/article/pii/S0895981112000831 |journal=Journal of South American Earth Sciences |series=Tectonic and climatic shaping of the northern Andes and southern Caribbean margin |volume=39 |pages=16–23 |doi=10.1016/j.jsames.2012.06.017 |issn=0895-9811}}

Eubrontes is the name of the footprints, identified by their shape, and not of the genus or genera that made them, which is as yet unknown but is presumed to be similar to Coelophysis or Dilophosaurus. They are most famous for their discovery in the Connecticut River Valley of Massachusetts in the early 19th century. They, among other footprints, were the first known non-avian dinosaur tracks to be discovered in North America, though they were initially thought to have been made by large birds.

Discovery and identity

The footprints were first described by Edward Hitchcock, a professor of Amherst College, who thought they were made by a large bird. He originally assigned them to ichnotaxon Ornithichnites in 1836, then Ornithoidichnites in 1841, before coining Eubrontes in 1845. The name means "true thunder," probably referring to the supposed weight of the animal impacting on the ground.

in 1858 Hitchcock still described the tracks as those of "a thick-toed bird," since there was no evidence of tail drag marks. But by the time that Richard Swann Lull began working on the tracks in 1904, they were thought to belong to a dinosaur. Lull originally thought they were from a herbivore, but by 1953 he concluded they were from a carnivorous theropod. Many later authors have agreed with this interpretation, but some have suggested that they are from a prosauropod. Regardless, they are almost certainly saurischian.Robert E. Weems. 2003. "Plateosaurus foot structure suggests a single trackmaker for Eubrontes and Gigandipus footprints." In P. M. LeTourneau & P. E. Olsen (eds.). The Great Rift Valleys of Pangea in Eastern North America, Volume 2: Sedimentology, Stratigraphy, and Paleontology. New York: Columbia University Press, pp. 294–295.

A typical Eubrontes print is from 25–50 cm long, with three toes that terminate in sharp claws. It belongs to a biped that must have been over one metre high at the hip and from 5–6 metres long. In the 1960s Edwin Colbert and others supposed that a large heavy carnivore like Teratosaurus (then considered to be a dinosaur) made the track, but a possible candidate is Dilophosaurus, a large theropod related to Coelophysis, or a close relative such as Podokesaurus. However no Dilophosaurus fossil material is associated with Eubrontes tracks. The tracks may also be from a plateosaurid. In 2016 Molina-Perez and Larramendi based on the 45 cm (1.48 ft) long footprint estimated the size of the animal at 8.4 meters (27.5 ft) and 600 kg (1.323 lbs).{{Cite book|last=Molina-Perez & Larramendi|title=Récords y curiosidades de los dinosaurios Terópodos y otros dinosauromorfos|publisher=Larousse|year=2016|location=Spain|pages=95 & 120}} Another 60.5 cm (1.98 ft) long footprint belongs to an 8.1 meter (26.6 ft), 1.1 tonne (2.425 lbs) individual, that was very similar to Sinosaurus triassicus.

File:Dinosaur State Park (Rocky Hill, CT) - prints.JPG]]

Another major find occurred at Rocky Hill, Connecticut in 1966. Nearly 600 prints are preserved there in an area now designated Dinosaur State Park.

Paleopathology

A trackway attributed to the ichnogenus Eubrontes had a missing second digit on the right foot. The animal could have either lost the toe due to injury or it was malformed.Molnar, R. E., 2001, Theropod paleopathology: a literature survey: In: Mesozoic Vertebrate Life, edited by Tanke, D. H., and Carpenter, K., Indiana University Press, p. 337-363.

See also

Notes

{{Reflist}}

References

  • Colbert, E., Dinosaurs, Hutchinson & Co, 1962
  • {{cite web |archive-url=https://web.archive.org/web/20091027064247/http://www.geocities.com/stegob/eubrontesconnecticut.html |title=Dino Land State Fossils: Eubrontes of Connecticut |url=http://www.geocities.com/stegob/eubrontesconnecticut.html?200611 |archive-date=2009-10-27 }}
  • Queensland Dinosaur Trackways home.alphalink.com.au/dannj/larkqury.htm

{{Taxonbar|from=Q5405450}}

Category:Theropod trace fossils

Category:Fossil trackways

Category:Symbols of Connecticut

Category:Symbols of Massachusetts