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 History  



1.1  Forgery  







2 References  














Tridentinosaurus







 

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
 
















Appearance
   

 






From Wikipedia, the free encyclopedia
 


Tridentinosaurus
Temporal range: Early Permian (Cisuralian), Kungurian

O

S

D

C

P

T

J

K

Pg

N

Holotype specimen, with forged body outline
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Amniota
Clade: Sauropsida
Class: Reptilia
Genus: Tridentinosaurus
Species:
T. antiquus
Binomial name
Tridentinosaurus antiquus

Leonardi, 1959

Tridentinosaurus (meaning "Trentino lizard") is a dubious genus of extinct fossil reptile from the early Permian Regnana Formation of the Italian Alps. The genus contains a single species, T. antiquus. Tridentinosaurus represents one of the oldest known vertebrate fossils found in Italy. The only parts of the skeleton that are preserved are the long bones of the hind limbs, and the supposed soft tissue body outline is a forgery done with paint, though some genuine scales may also be preserved. Due to the poor preservation of the limb bones, the validity of the taxon is questionable.

History

[edit]

The Tridentinosaurus holotype specimen, MGP-PD 26567, was discovered in 1931 in tuffaceous sandstone layers of the Regnana Formation ('Stramaiolo' (Redebus) locality) in Trentino-Alto Adige, Italy. The specimen appears to consist of a carbonized outline—missing the tip of the tail and most of the skull—of a lizard-like animal surrounding a fragmentary skeleton. Reports of the full body outline as preserved range from 23.5–26.5 centimetres (9.3–10.4 in). The specimen appears to demonstrate an elongated, slender neck and torso. The outline shows that the first through fourth toes get progressively longer, with the fifth toe being notably smaller.[1][2]

Shortly after its discovery, Giambattista Dal Piaz reported on this specimen, informally giving it the name "Tridentinosaurus antiquus".[3] In 1959, Piero Leonardi described Tridentinosaurus antiquus as a new genus and species of araeoscelidan reptile based on these remains. The generic name, "'Tridentinosaurus", combines a modified form of the Italian province "Trentino"—a reference to the location of the discovery—with the Greek『σαῦρος』("sauros"), meaning "reptile". The specific name, "antiquus", means "ancient" in Latin.[4][2]

Leonardi's taxonomic assignment of Tridentinosaurus to the Araeoscelida was later called into question, with a 1997 review of Paleozoic vertebrate fossils from the Alps considering this classification doubtful.[5] Some later reviews instead considered it more appropriate to assign Tridentinosaurus to the Protorosauria,[6][2] or, more broadly, the Diapsida.[7]

The specimen was briefly mentioned several times in the following years, with some publications drawing comparisons between the inferred body shape of Tridentinosaurus and other new fossils.[8][9][10] In their 2019 description of the mesenosaurine varanopid Cabarzia, Spindler, Werneburg & Schneider noted similarities between the proportions of the apparent Tridentinosaurus body shape and other taxa. For example, the slender neck is similar to the varanopid Mesenosaurus, and the limb proportions—especially the large manus—are similar to the araeoscelidan Petrolacosaurus.[11][12]

Forgery

[edit]

In 2024, Rossi and colleagues published the results of several detailed analyses of the holotype specimen of Tridentinosaurus. They found that the purported carbonized soft tissues seen on the specimen were forged, instead being the result of a manufactured pigment like black paint. Using ultraviolet light, 3D surface modeling, scanning electron microscopy with energy dispersive spectroscopy, micro x-ray diffraction, Raman and attenuated total reflectance Fourier transformed infrared spectroscopy, they determined that the body shape had been carved by hand, possibly in an effort to reveal additional skeletal material, and that the coloration was added later. For example, UV light revealed that the body outline fluoresced, something that fossilized organic materials do not typically do, but coatings like glues, varnishes, and some pigments do. It is unknown when the forgery was made or who was involved, but the discovery of carbonized plant fossils with a similar dark outline in a similar locality played a significant role in misleading paleontologists. Thus, previous inferences derived from observations of the body outline are unreliable, and the validity of Tridentinosaurus is questionable.[1]

The only visible bones belong to the hindlimbs, consisting of poorly preserved femora, tibiae, and fibulae. While the body outline is not real, the researchers did observe skin impressions near the shoulder and pelvic girdles, consisting of small rhomboidal scales that may represent osteoderms. It is possible that future analyses, such as using CT scan technology, may reveal more bones.[1][13]

References

[edit]
  1. ^ a b c Rossi, Valentina; Bernardi, Massimo; Fornasiero, Mariagabriella; Nestola, Fabrizio; Unitt, Richard; Castelli, Stefano; Kustatscher, Evelyn (2024-02-15). "Forged soft tissues revealed in the oldest fossil reptile from the early Permian of the Alps". Palaeontology. 67 (1). e12690. doi:10.1111/pala.12690. hdl:11577/3513043. ISSN 0031-0239.
  • ^ a b c Altichieri, Luca (1980). "Il Tridentinosauro". I vertebrati fossili italiani (PDF) (in Italian). Verona: Catalogo della Mostra. pp. 49–50.
  • ^ Dal Piaz Gb. 1932 (1931). Scoperta degli avanzi di un rettile (lacertide) nei tufi compresi entro i porfidi quarziferi permiani del Trentino. Atti Soc. Ital. Progr. Scienze, XX Riunione, v. 2, pp. 280-281. [The discovery of the remains of a reptile (lacertide) in tuffs including within the Permian quartz porphyry of Trentino.]
  • ^ Leonardi, Piero (1959). "Tridentinosaurus antiquus Gb. Dal Piaz rettile protorosauro permiano del trentino orientale". Memorie degli Istituti di Geologia e Mineralogia degll'Università di Padova (in Italian). 21: 1–17.
  • ^ Blieck, Alain R. M.; Conti, Maria A.; Vecchia, Fabio M. D.; Flügel, Helmut W.; Gand, Georges; Hubmann, Bernhard; Lelièvre, Hervé; Mariotti, Nino; Nicosia, Umberto; Poplin, Cécile; Schneider, Jörg W.; Werneburg, Ralf (1997). "Paleozoic vertebrates of the Alps: a review". Bulletin de la Société Géologique de France. 168 (3): 343–350.
  • ^ Dalla Vecchia, Fabio M. (1997). "Mesozoic Amphibia and Reptilia stored at the Museum of Paleontology of the University of Padua". Natura Nascosta. 15: 34–43 – via Academia.edu.
  • ^ Sennikov, A. G. (1997). "An enigmatic reptile from the Upper Permian of the Volga River Basin". Paleontological Journal. 31 (1): 94–101.
  • ^ Ronchi, Ausonio; Sacchi, Eva; Romano, Marco; Nicosia, Umberto (2011-12-01). "A Huge Caseid Pelycosaur from North-Western Sardinia and Its Bearing on European Permian Stratigraphy and Palaeobiogeography". Acta Palaeontologica Polonica. 56 (4): 723–738. doi:10.4202/app.2010.0087. ISSN 0567-7920.
  • ^ Spindler, Frederik; Werneburg, Ralf; Schneider, Joerg W.; Luthardt, Ludwig; Annacker, Volker; Rößler, Ronny (2018-06-01). "First arboreal 'pelycosaurs' (Synapsida: Varanopidae) from the early Permian Chemnitz Fossil Lagerstätte, SE Germany, with a review of varanopid phylogeny". PalZ. 92 (2): 315–364. Bibcode:2018PalZ...92..315S. doi:10.1007/s12542-018-0405-9. ISSN 1867-6812. S2CID 133846070.
  • ^ Citton, Paolo; Ronchi, Ausonio; Maganuco, Simone; Caratelli, Martina; Nicosia, Umberto; Sacchi, Eva; Romano, Marco (2018-07-24). Somerville, I. D. (ed.). "First tetrapod footprints from the Permian of Sardinia and their palaeontological and stratigraphical significance". Geological Journal. 54 (4): 2084–2098. doi:10.1002/gj.3285. ISSN 0072-1050. S2CID 135216684.
  • ^ Spindler, Frederik; Werneburg, Ralf; Schneider, Jörg W. (2019-06-01). "A new mesenosaurine from the lower Permian of Germany and the postcrania of Mesenosaurus: implications for early amniote comparative osteology". PalZ. 93 (2): 303–344. Bibcode:2019PalZ...93..303S. doi:10.1007/s12542-018-0439-z. ISSN 1867-6812. S2CID 91871872.
  • ^ Marchetti, Lorenzo; Forte, Giuseppa; Kustatscher, Evelyn; DiMichele, William A.; Lucas, Spencer G.; Roghi, Guido; Juncal, Manuel A.; Hartkopf-Fröder, Christoph; Krainer, Karl; Morelli, Corrado; Ronchi, Ausonio (2022-03-01). "The Artinskian Warming Event: an Euramerican change in climate and the terrestrial biota during the early Permian". Earth-Science Reviews. 226: 103922. Bibcode:2022ESRv..22603922M. doi:10.1016/j.earscirev.2022.103922. ISSN 0012-8252. S2CID 245892961.
  • ^ Ashworth, James. "'Skin' of ancient reptile was painted on, new research claims". Natural History Museum. Retrieved 2024-02-19.

  • Retrieved from "https://en.wikipedia.org/w/index.php?title=Tridentinosaurus&oldid=1234595577"

    Categories: 
    Permian Italy
    Fossils of Italy
    Kungurian life
    Prehistoric reptile genera
    Fossil taxa described in 1959
    Fossil forgeries
    Hidden categories: 
    CS1 Italian-language sources (it)
    Articles with short description
    Short description is different from Wikidata
    Articles with 'species' microformats
    Taxonbars without primary Wikidata taxon IDs
     



    This page was last edited on 15 July 2024, at 05:05 (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