Seazzadactylus

Last updated

Seazzadactylus
Temporal range: Late Triassic, Norian
Seazzadactylus.png
Holotype specimen
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Pterosauromorpha
Order: Pterosauria
Clade: Caviramidae
Family: Austriadraconidae
Genus: Seazzadactylus
Dalla Vecchia, 2019
Type species
Seazzadactylus venieri
Dalla Vecchia, 2019

Seazzadactylus is a basal pterosaur genus that lived during the late Triassic (Norian stage, about 219-214 million years ago) [1] in the area of present Italy.

Contents

Discovery and naming

In 1997, amateur paleontologist Umberto Venier discovered the skeleton of a pterosaur in a boulder laying in the bed of the Seazza brook, just before it joins the Tagliamento river, near Preone in the Dolomites. Venier brought the find to the Museo Friulano di Storia Naturale at Udine. After partial preparation paleontologist Fabio Marco Dalla Vecchia announced the discovery in the scientific literature in 2000. [2] In 2003, Dalla Vecchia referred the specimen to Eudimorphodon . [3] In 2009 however, further preparation made him conclude that it was a species new to science, not identical to either Eudimorphodon or Carniadactylus . [4]

In 2019, Dalla Vecchia named and described the type species Seazzadactylus venieri. The generic name combines that of the Seazza with the Greek daktylos, 'finger'. The specific name honours Venier as discoverer.

The holotype, MFSN 21545, was found in a layer of the Dolomia di Forni Formation dating from the middle to upper Norian. It consists of a partial skeleton with skull and lower jaws. The skeleton is not articulated but the bones are in close association. It lacks the tail and most feet bones. It represents a subadult individual, not fully grown. [5]

Description

Reconstructed skull Seazzadactylus skull.png
Reconstructed skull

Dalla Vecchia established a number of apomorphic traits. In the praemaxilla the teeth are limited to the front half of the body. The jugal bone has a high front branch, tapering to the front and below into a sharp needle-like point. The main body of the jugal bone is pierced in the middle by a large foramen. The front branch of the pterygoid bone makes a right angle to the outer side. The ectopterygoid bone is positioned behind the pterygoid and has a recurved outer side branch in the direction of the jugal as well as a rear branch. Teeth in the maxilla and the dentary bone possess multiple cusps, sometimes as high as six or seven, while erupted teeth with three cusps are absent. The first, second and third maxillary teeth are recurved, with the curvature gradually diminishing along the series. The shoulder blade is fan-like expanded to the rear. The pteroid bone is small and slender, formed like an exclamation mark. [5]

Phylogeny

Seazzadactylus was placed in the Pterosauria in 2019, in a basal position outside of the Monofenestrata. A cladistic analysis showed it was part of a yet-unnamed clade also containing Arcticodactylus , Austriadraco , Carniadactylus, Raeticodactylus and Caviramus . [5] This unnamed clade was eventually named as Caviramidae in a 2020 study by Matthew G. Baron. [6] In the evolutionary tree Seazzadactylus would be positioned directly above Austriadraco and below Carniadactylus. Eudimorphodon was not recovered as a close relative but in a more derived position instead, under Campylognathoides . [5]

See also

Notes

  1. Müller R.T., Ezcurra M.D., Garcia M.S., Agnolín F.L., Stocker M.R., Novas F.E., Soares M.B., Kellner A.W.A. & Nesbitt S.J. (2023). ”New reptile shows dinosaurs and pterosaurs evolved among diverse precursors”. Nature 620(7974): p. 589–594. doi:10.1038/s41586-023-06359-z
  2. Dalla Vecchia F.M. 2000. "A wing phalanx of a large basal pterosaur (Diapsida, Pterosauria) from the Norian (Late Triassic) of NE Italy". Bollettino della Società Paleontologica Italiana39(2): 229–234
  3. Dalla Vecchia F.M. 2003. "New morphological observations on Triassic pterosaurs". In: Buffetaut E, Mazin J-M, eds. Evolution and Palaeobiology of Pterosaurs. Vol. 217. London: Geological Society London, Special Publication, p 23–44
  4. Dalla Vecchia F.M. 2009. "Anatomy and systematics of the pterosaur Carniadactylus gen. n. rosenfeldi (Dalla Vecchia, 1995)". Rivista Italiana di Paleontologia e Stratigrafia115(2): 159–186
  5. 1 2 3 4 Dalla Vecchia, Fabio Marco (25 July 2019). "Seazzadactylus venieri gen. et sp. nov., a new pterosaur (Diapsida: Pterosauria) from the Upper Triassic (Norian) of northeastern Italy". PeerJ. 7: e7363. doi: 10.7717/peerj.7363 . PMC   6661147 . PMID   31380153.
  6. Matthew G. Baron (2020). "Testing pterosaur ingroup relationships through broader sampling of avemetatarsalian taxa and characters and a range of phylogenetic analysis techniques". PeerJ. 8: e9604. doi:10.7717/peerj.9604. PMC 7512134. PMID   33005485.

Related Research Articles

<i>Tanystropheus</i> Extinct genus of reptiles

Tanystropheus is an extinct genus of archosauromorph reptile which lived during the Triassic Period in Europe, Asia, and North America. It is recognisable by its extremely elongated neck, longer than the torso and tail combined. The neck was composed of 13 vertebrae strengthened by extensive cervical ribs. Tanystropheus is one of the most well-described non-archosauriform archosauromorphs, known from numerous fossils, including nearly complete skeletons. Some species within the genus may have reached a total length of 6 meters (20 ft), making Tanystropheus the longest non-archosauriform archosauromorph as well. Tanystropheus is the namesake of the family Tanystropheidae, a clade collecting many long-necked Triassic archosauromorphs previously described as "protorosaurs" or "prolacertiforms".

<i>Eudimorphodon</i> Genus of eudimorphodontid pterosaur from the Late Triassic

Eudimorphodon was a pterosaur that was discovered in 1973 by Mario Pandolfi in the town of Cene, Italy and described the same year by Rocco Zambelli. The nearly complete skeleton was retrieved from shale deposited during the Late Triassic, making Eudimorphodon one of the oldest pterosaurs known. It had a wingspan of about 100 centimeters (3.3 ft) and at the end of its long bony tail may have been a diamond-shaped flap like in the later Rhamphorhynchus. If so, the flap may have helped it steer while maneuvering in the air. Eudimorphodon is known from several skeletons, including juvenile specimens.

<i>Preondactylus</i> Genus of preondactylian pterosaur from the Late Triassic

Preondactylus is a genus of long-tailed pterosaurs from the Late Triassic that inhabited what is now Italy. It contains a single known species, Preondactylus buffarinii, which was discovered by Nando Buffarini in 1982 at the Forni Dolostone near Udine in the Preone valley of the Italian Alps.

<span class="mw-page-title-main">Anurognathidae</span> Family of pterosaurs from the Jurassic and Cretaceous periods

Anurognathidae is a family of small, short-tailed pterosaurs that lived in Europe, Asia, and possibly North America during the Jurassic and Cretaceous periods. Five genera are known: Anurognathus, from the Late Jurassic of Germany; Jeholopterus, from the Middle to Late Jurassic of China; Dendrorhynchoides, from the Middle Jurassic of China; Batrachognathus, from the Late Jurassic of Kazakhstan; and Vesperopterylus, from the Early Cretaceous of China. Bennett (2007) suggested that the holotype of Mesadactylus, BYU 2024, a synsacrum, belonged to an anurognathid, though this affinity has been questioned by other authors. Mesadactylus is from the Late Jurassic Morrison Formation of the United States. Indeterminate anurognathid remains have also been reported from the Middle Jurassic Bakhar Svita of Mongolia and the Early Cretaceous of North Korea.

<i>Peteinosaurus</i> Genus of pterosaur from the Late Triassic

Peteinosaurus was a prehistoric genus of pterosaur. It lived in the late Triassic period in the late Norian age, and at a wingspan of around 60 cm (24 in), was one of the smallest and earliest pterosaurs, although other estimates suggest a wingspan of up to 1 m (3.3 ft).

<i>Austriadactylus</i> Genus of preondactylian pterosaur from the Late Triassic

Austriadactylus is a genus of "rhamphorhynchoid" pterosaur. The fossil remains were unearthed in Late Triassic rocks of Austria.

Caviramus is a genus of caviramid pterosaur from the Late Triassic lower Kössen Formation of the Northern Calcareous Alps of Switzerland.

<i>Raeticodactylus</i> Genus of raeticodactylid pterosaur from the Late Triassic

Raeticodactylus is a genus of non-pterodactyloid pterosaur from the late Norian-early Rhaetian-age Upper Triassic lower Kössen Formation of the central Austroalpine of Grisons, Switzerland. It is known from holotype BNM 14524, a single disarticulated partial skeleton including an almost complete skull, found in August 2005. This genus was named and described in 2008 by its discoverer Rico Stecher; the type species is Raeticodactylus filisurensis. The specific name refers to Filisur.

<i>Turfanosuchus</i> Extinct genus of reptiles

Turfanosuchus is a genus of archosauriform reptile, likely a gracilisuchid archosaur, which lived during the Middle Triassic (Anisian) of northwestern China. The type species, T. dabanensis, was described by C.C. Young in 1973, based on a partially complete but disarticulated fossil skeleton found in the Kelamayi Formation of the Turfan Basin.

Langobardisaurus is an extinct genus of tanystropheid archosauromorph reptile, with one valid species, L. pandolfii. Its fossils have been found in Italy and Austria, and it lived during the Late Triassic period, roughly 228 to 201 million years ago. Langobardisaurus was initially described in 1994, based on fossils from the Calcare di Zorzino Formation in Northern Italy. Fossils of the genus are also known from the Forni Dolostone of Northern Italy and the Seefeld Formation of Austria.

The Forni Dolostone, also known as the Dolomia di Forni, is a Late Triassic dolomite geological formation in northeastern Italy. The formation was deposited in a lagoonal to shallow marine environment.

<i>Carniadactylus</i> Genus of pterosaur from the Late Triassic

Carniadactylus is a genus of pterosaur which existed in Europe during the Late Triassic period. The genus contains a single species, Carniadactylus rosenfeldi.

Faxinalipterus is a genus of ornithodiran archosaur, originally described as a pterosaur, from the Late Triassic Caturrita Formation of southern Brazil. A study from 2022 reinterpreted the fossil remains and instead suggests them to belong to a member of the Lagerpetidae, another clade of pterosauromorphs.

<span class="mw-page-title-main">Eopterosauria</span> Clade of basal pterosaurs

Eopterosauria is a group of basal pterosaurs from the Triassic, which form their own clade. The term was first used in Andres et al. (2014) to include Preondactylus, Austriadactylus, Peteinosaurus and Eudimorphodontidae. Inside the group were two other new clades, Preondactylia, which included Preondactylus and Austriadactylus, and Eudimorphodontoidea, to include Eudimorphodontidae and Raeticodactylidae. Eopterosauria was defined as "the least inclusive clade containing Preondactylus buffarinii and Eudimorphodon ranzii". The specimen BSP 1994, previously assigned to Eudimorphodon, was named the separate taxon Austriadraco in 2015, and assigned to the new family Austriadraconidae, but further classification was not described. The following phylogenetic analysis follows the topology of Andres et al. (2014).

<span class="mw-page-title-main">Eudimorphodontidae</span> Family of eopterosaurs from the Late Triassic

Eudimorphodontidae is an extinct family of early pterosaurs from the Late Triassic of Europe. It was named by Peter Wellnhofer in 1978 to include Eudimorphodon ranzii. Some phylogenetic analyses suggested that Eudimorphodontidae is a junior synonym of Campylognathoididae, however more comprehensive analyses found Eudimorphodontidae to be basal to Macronychoptera that includes Campylognathoididae and more derived pterosaurs (Breviquartossa). Wang et al. (2009) found Eudimorphodontidae to include six species, but they didn't defined the clade. Brian Andres define Eudimorphodontidae and found Peteinosaurus to be most closely related to it. Furthermore, he found monophyletic Eudimorphodon clade, and defined two subfamilies within Eudimorphodontidae. The Eudimorphodontinae includes all taxa more closely related to Eudimorphodon ranzii than to Raeticodactylus filisurensis while the Raeticodactylinae includes all taxa more closely related to Raeticodactylus filisurensis than to Eudimorphodon ranzii. More recently, Raeticodactylus and Caviramus were moved into their own family, Raeticodactylidae. The below cladogram follows that analysis.

Arcticodactylus is a genus of basal pterosaur living during the Late Triassic in the area of present Greenland. Its only species was previously attributed to Eudimorphodon, and its closest relatives may have been Eudimorphodon or Austriadraco.

Austriadraco is a genus of pterosaur living during the Late Triassic in the area of present Austria. Its only species—Austriadraco dallavecchiai—was previously attributed to Eudimorphodon, and its closest relatives may have been Eudimorphodon or Arcticodactylus.

<i>Bergamodactylus</i> Genus of campylognathoidid pterosaur from the Late Triassic

Bergamodactylus is a putative genus of basal pterosaur which lived during the Late Triassic in the area of present-day Bergamo province in Italy. Its only species is Bergamodactylus wildi. It was named in 2015 based on a pterosaur specimen which had previously been regarded as a juvenile Eudimorphodon or as identical to Carniadactylus. Some Triassic pterosaur specialists consider the distinguishing features of Bergamodactylus to be invalid or insufficient to distinguish it from Carniadactylus, and thus retain the specimen in that genus.

<i>Caelestiventus</i> Genus of pterosaur from the Late Triassic

Caelestiventus is a pterosaur genus from the Late Triassic found in western North America. The type species, Caelestiventus hanseni, honors Robin Hansen, the Bureau of Land Management geologist (BLM), who facilitated access to the excavation site.

<span class="mw-page-title-main">Caviramidae</span> Family of basal pterosaurs from the Late Triassic

Caviramidae is a group of basal pterosaurs. It was erected by paleontologist Matthew G. Baron in 2020. It was defined as the least inclusive clade that includes Arcticodactylus cromptonellus and Caviramus schesaplanensis.