To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

Brachychirotherium

From Wikipedia, the free encyclopedia

Brachychirotherium
Temporal range: Middle Triassic-Early Jurassic
~247–190 Ma
Brachychirotherium sp. from the Redonda Formation of New Mexico (New Mexico Museum of Natural History and Science)
Trace fossil classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Clade: Archosauria
Clade: Pseudosuchia
Ichnofamily: Chirotheriidae
Ichnogenus: Brachychirotherium
Beurlen, 1950
Ichnospecies

See text

Brachychirotherium is an ichnogenus, a form taxon based on footprints. It is a type of chirothere ('hand beast'), a term referring to the footprints of five-toed Triassic reptiles with a short fifth digit, leaving an appearance similar to a reverse human hand print. Brachychirotherium was first characterized from fossils found in Triassic beds in Germany,[1] but has since been found in France,[2] South Africa,[3] Argentina, Peru,[4] Bolivia,[5][6] and North America.[7]

Description

Front (manus) and rear (pes) footprints are distinguishable, though manus prints are not always preserved. The pes prints show five toes, which are proportionally shorter and stubbier than those of other chirotheres. Digit III is the longest, followed by digits II and IV, though they are all of a similar length. Digit I is notably shorter, and the impression of digit V is reduced to an oval pad at the sole. The manus prints likewise show up to five short digits, with the pad of digit V separate from the rest. The surfaces of the sole and palm are broad, and creases are indistinct. The prints were likely produced by some form of large pseudosuchian (reptiles related to crocodilians), such as aetosaurs or quadrupedal rauisuchids.[8]

Species

[incomplete list]

  • B. circaparvum Willruth, 1971
  • B. eyermani Baird, 1957
  • B. gallicum (Willruth, 1917)
  • B. hassfurtenese Beurlen, 1950 (type species)
  • B. lorteci Willruth, 1971
  • B. thuringiacum (Ruhle von Lilienstern, 1938)
  • B. tintati Willruth, 1971

See also

References

  1. ^ Beurlen, K. (1950). "Neue Fährtenfunde aus der Fränkischen Trias [New track discoveries in the Franconian Triassic]". Neues Jahrbuch für Geologie und Paläontologie - Monatshefte. 1950: 308–320.
  2. ^ Gand, G.; Demathieu, G.; Montenat, C. (2007). "Les traces de pas d'amphibiens, de dinosaures et autres reptiles du Mesozoïque français: Inventaire et interpretations [Footprints of amphibians, dinosaurs, and other reptiles from the French Mesozoic: inventory and interpretations]" (PDF). Palaeovertebrata. 2007 (1–4): 1–149. Retrieved 24 November 2021.
  3. ^ Olsen, P.E.; Galton, P.M. (1984). "A review of the reptile and amphibian assemblages from the Stormberg of southern Africa, with special emphasis on the footprints and the age of the Stormberg". Palaeontologia Africana. 25: 87–110. Retrieved 24 November 2021.
  4. ^ Salas Gismondi, Rodolfo; Chacaltana Budiel, César Augusto (2010). "Huellas de un arcosaurio triásico en la Formación Sarayaquillo (Cuenca Ene, Perú) y el icnoregistro de vertebrados en el mesozoico del Perú". Repositorio Institucional INGEMMET.
  5. ^ Apesteguía, Sebastián; Riguetti, Facundo; Citton, Paolo; Veiga, Gonzalo D.; Poiré, Daniel G.; de Valais, Silvina; Gabriel Zacarías, Gerardo (2021-11-02). "The Ruditayoj-Tunasniyoj fossil area (Chuquisaca, Bolivia): a Triassic chirotheriid megatracksite and reinterpretation of purported thyreophoran tracks". Historical Biology. 33 (11): 2883–2896. Bibcode:2021HBio...33.2883A. doi:10.1080/08912963.2020.1833328. ISSN 0891-2963. S2CID 226324294.
  6. ^ Leonardi, G. (1994). Annotated Atlas of South America in Argentina, Peru and Bolivia. Tetrapod Footprints (Devonian to Holocene) with an Appendix on Mexico and Central America. Brasília: República Federativa do Brasil, Ministério de Minas e Energia, Secretaria de Minas e Metalurgia, Companhia de Pesquisa de Recursos Minerais. pp. 1–248.
  7. ^ Conrad, Kelly; Lockley, Martin G.; Prince, Nancy K. (1987). "Triassic and Jurassic vertebrate-dominated trace fossil assemblages of the Cimarron Valley region--Implications for paleoecology and biostratigraphy" (PDF). New Mexico Geological Society Field Conference Series. 38: 127–138. Retrieved 1 September 2020.
  8. ^ Hunt, Adrian P.; Lucas, Spencer G.; Klein, Hendrik (2018), Tanner, Lawrence H. (ed.), "Late Triassic Nonmarine Vertebrate and Invertebrate Trace Fossils and the Pattern of the Phanerozoic Record of Vertebrate Trace Fossils", The Late Triassic World: Earth in a Time of Transition, Topics in Geobiology, Cham: Springer International Publishing, pp. 447–544, doi:10.1007/978-3-319-68009-5_12, ISBN 978-3-319-68009-5, retrieved 2023-07-19


This page was last edited on 11 February 2024, at 09:31
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.