Jump to content
 







Main menu
   


Navigation  



Main page
Contents
Current events
Random article
About Wikipedia
Contact us
Donate
 




Contribute  



Help
Learn to edit
Community portal
Recent changes
Upload file
 








Search  

































Create account

Log in
 









Create account
 Log in
 




Pages for logged out editors learn more  



Contributions
Talk
 



















Contents

   



(Top)
 


1 Description  





2 References  





3 External links  














Psephoderma






العربية
Deutsch
Español
Français
Galego

Italiano
עברית
Nederlands

Polski

 

Edit links
 









Article
Talk
 

















Read
Edit
View history
 








Tools
   


Actions  



Read
Edit
View history
 




General  



What links here
Related changes
Upload file
Special pages
Permanent link
Page information
Cite this page
Get shortened URL
Download QR code
Wikidata item
 




Print/export  



Download as PDF
Printable version
 




In other projects  



Wikimedia Commons
 
















Appearance
   

 






From Wikipedia, the free encyclopedia
 


Psephoderma

Temporal range: Late Triassic

P. alpinum fossil
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Superorder: Sauropterygia
Order: Placodontia
Family: Placochelyidae
Genus: Psephoderma
Meyer, 1858
Species
  • P. alpinum Meyer, 1858 (type)
  • P. anglicum Meyer, 1867

Psephoderma (meaning "pebbly skin", from the Ancient Greek psepho (ψῆφος), "pebbly", and derma (δέρμα), "skin") is a genus of placodonts very similar to the related genera Placochelys and Cyamodus. Psephoderma had a flattened skull and a narrow, straight rostrum, much narrower than that of its relatives. Inside this skull, embedded in the jaws, were rounded teeth specialized for crushing the shellfish it ate. Unlike henodontid placodonts, Psephoderma's carapace was divided into two pieces, one on the shoulders and back, and another on the ventral end. Psephoderma grew to 180 centimetres (5.9 ft) long, larger than many of its relatives,[1] and lived in the Late Triassic (Norian - Rhaetian), about 210 million years ago. It was one of the last placodonts to live.[citation needed] Fossils of Psephoderma have been found in the Rhaetian deposits in the Alps and in England, hence the specific names.[2]

Description

[edit]
Life restoration of Psephoderma alpinum

Psephoderma had a long, narrow rostrum, which was the main difference between its skull and those of its relatives. This rostrum bore paired grooves on the inside of the mouth, which led to the internal nares and are a diagnostic feature for the genus. The anterior processes of the maxillae stretched forwards a long way along the rostrum, while the posterior processes of the premaxillae stretched a long way back up the rostrum and came between the external nares and between the nasal bones. The nasal bones were very small, mere splinters of bone. The orbits were large and somewhat irregularly shaped, and indicate that the eyes were on top of the head looking upwards. Its pineal foramen was large, and anteriorly placed, with its anterior edge bordered by the frontal bones. Unlike most of its relatives, its ectopterygoid is not known and may not be present, as in Protenodontosaurus. The P. alpinum species had decidedly elongated, posterior, tooth-bearing plates for crushing the shellfish that formed its diet. No teeth were present along the premaxillae or the rostral area of the maxillae, but four crushing teeth were in each side of the palate, the first three in a triangle of small, rounded teeth and the fourth a short distance behind them. The fourth tooth was huge, far larger than the first three. The lack of teeth near the front of the mouth and rostrum indicate that the elongated rostrum was mainly used for rooting out or digging up shellfish, which would then be taken into the back of the mouth and crushed by the large teeth. Psephoderma'stemporal fossae were narrow, but highly elongated. The posterior process of the postorbital bones reached far back into the temporal arches, underneath the temporal fossae. The whole skull was highly ventrodorsally compressed. It had temporal tubercles, but they were small, and restricted solely to the posterior ends of the squamosal bones. Its occiput was deeply excavated and its entire braincase very small. However, the braincase walls were quite thick and well armoured.[2]

The carapace of Psephoderma was made up of two parts, one of which covered the rib cage and thorax and the other of which covered the pelvis. Both parts of the carapace were made of partially fused scutes, roughly hexagonal or circular in shape. Its tail was quite long, up to about 80 cm, and had scutes all the way down it. The limbs were relatively small and would have been used as paddles, but had individual toes rather than a flipper.[citation needed]

P. alpinum shell

References

[edit]
  1. ^ Lawrence H. Tanner (2018). The Late Triassic World: Earth in a Time of Transition. Springer Nature. p. 281. ISBN 978-3-319-68008-8. Retrieved 12 September 2022.
  • ^ a b Rieppel, Olivier (2001). The cranial anatomy of Placochelys placodonta Jaekel, 1902, and a review of the Cyamodontoidea (Reptilia, Placodonta). Field Museum of Natural History.
  • [edit]


  • t
  • e

  • Retrieved from "https://en.wikipedia.org/w/index.php?title=Psephoderma&oldid=1188021434"

    Categories: 
    Placodonts
    Late Triassic reptiles of Europe
    Fossil taxa described in 1858
    Fossils of Italy
    Fossils of Israel
    Sauropterygian genera
    Triassic reptile stubs
    Hidden categories: 
    Articles with short description
    Short description is different from Wikidata
    Articles needing additional references from February 2021
    All articles needing additional references
    Articles with 'species' microformats
    All articles with unsourced statements
    Articles with unsourced statements from July 2019
    All stub articles
     



    This page was last edited on 2 December 2023, at 22:12 (UTC).

    Text is available under the Creative Commons Attribution-ShareAlike License 4.0; additional terms may apply. By using this site, you agree to the Terms of Use and Privacy Policy. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc., a non-profit organization.



    Privacy policy

    About Wikipedia

    Disclaimers

    Contact Wikipedia

    Code of Conduct

    Developers

    Statistics

    Cookie statement

    Mobile view



    Wikimedia Foundation
    Powered by MediaWiki