Vespersaurus | |
---|---|
Holotype foot bones | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Clade: | Dinosauria |
Clade: | Saurischia |
Clade: | Theropoda |
Family: | † Noasauridae |
Subfamily: | † Noasaurinae |
Genus: | † Vespersaurus Langer et al., 2019 |
Type species | |
Vespersaurus paranaensis Langer et al., 2019 |
Vespersaurus (meaning "western lizard") is a genus of noasaurid theropod dinosaur from the Cretaceous Rio Paraná Formation in the Paraná Basin, Brazil. The type and only species is V. paranaensis, which would have lived in the giant prehistoric Botucatu Desert. [5]
The generic name is derived from the Latin "vesper," meaning "evening/west," in reference to the town Cruzeiro do Oeste ("Western Cross") near which the fossils were found, and the Greek "sauros," meaning "lizard." The specific name refers to the Paraná state. [5]
After the discovery of numerous skeletons of the pterosaurs Caiuajara and Keresdrakon at the Cemitério dos Pterossauros site near Cruzeiro do Oeste, the remains of small theropods were uncovered between 2011 and 2015. One of these was named and described in 2019 as Vespersaurus. The holotype, MPCO.V 0065d, was recovered from the Late Cretaceous period, found on dark red sandstones in the Rio Paraná Formation in the Paraná Basin, Brazil. Footprints belonging to Vespersaurus or a similar one-toed theropod were discovered near Cruzeiro do Oeste as early as the 1970s. [5]
The taxon is notable for its distinct, functionally monodactyl foot anatomy, where the singularly large third digit would have borne most of the weight while walking. Based on the proportions of its holotype remains (MPCO.V 0065d), Vespersaurus was a small theropod with an estimated body length of 1–1.5 metres (3.3–4.9 ft). This makes it comparable in size to Noasaurus and Masiakasaurus. The estimated body mass of Vespersaurus is 11.28 kilograms (24.9 lb), nearly that of the ornithischians Jeholosaurus shangyuanensis and Gasparinisaura cincosaltensis . [5]
Footprints pertaining to a functionally monodactyl dinosaur found near Cianorte were attributed to Vespersaurus or to a close relative. [5] Those footprints were found in association with the ichnospecies Brasilichnium elusivum . [6] [7] It had been suggested that Vespersaurus footprints and/or Brasilichnium elusivum could have originated myths regarding footsteps of a saint near Cianorte. [8] [9] In 2023, Leonardi et al. described these footprints as belonging to a new ichnogenus and ichnospecies, which they named Farlowichnus rapidus . [10]
In 2023, Barbosa and colleagues tested Vespersaurus' tooth and two pedal unguals using a Finite Element Analysis. They found that the teeth were not well suited to handle struggling prey items, nor well-equipped to handle hard food items, having an ideal bite angle of 45 degrees. The stresses on the unguals, in contrast, were nearly identical throughout the three different scenarios they tested, indicating that the feet were not specialised for any particular task. Based on this, the team concluded that Vespersaurus did not fill a top predator niche in the Brazilian Caiua desert where it lived, but instead filled a more generalist niche, focussing on small prey items or having an opportunistic feeding strategy. [11]
Irritator is a genus of spinosaurid dinosaur that lived in what is now Brazil during the Albian stage of the Early Cretaceous Period, about 113 to 110 million years ago. It is known from a nearly complete skull found in the Romualdo Formation of the Araripe Basin. Fossil dealers had acquired this skull and sold it to the State Museum of Natural History Stuttgart. In 1996, the specimen became the holotype of the type species Irritator challengeri. The genus name comes from the word "irritation", reflecting the feelings of paleontologists who found the skull had been heavily damaged and altered by the collectors. The species name is a homage to the fictional character Professor Challenger from Arthur Conan Doyle's novels.
Tapejara is a genus of Brazilian pterosaur from the Cretaceous Period. Tapejara crests consisted of a semicircular crest over the snout, and a bony prong which extended back behind the head. It was a small pterosaur, with a wingspan of approximately 1.23–1.3 metres (4.0–4.3 ft).
Aucasaurus is a genus of medium-sized abelisaurid theropod dinosaur from Argentina that lived during the Late Cretaceous of the Anacleto Formation. It was smaller than the related Carnotaurus, although more derived in some ways, such as its extremely reduced arms and almost total lack of fingers. The type skeleton is complete to the thirteenth caudal vertebra, and so is relatively well understood, and is the most complete abelisaurid yet described. However, the skull is damaged, causing some paleontologists to speculate that it was involved in a fight prior to death.
Cearadactylus is a genus of large anhanguerid pterodactyloid pterosaur from the Romualdo Formation of Brazil, South America. Fossil remains of Cearadactylus dated back to the Albian stage of the Early Cretaceous period, about 112 million years ago. The only known species is C. atrox, described and named in 1985 by Giuseppe Leonardi and Guido Borgomanero. The name refers to the Brazilian state Ceará, and combines this with Greek daktylos, "finger", a reference to the wing finger of pterosaurs. The Latin atrox means "frightful", a reference to the fearsome dentition of the species.
The Candeleros Formation is a geologic formation that crops out in the Río Negro, Neuquén, and Mendoza provinces of northern Patagonia, Argentina. It is the oldest formation in the Neuquén Group and belongs to the Rio Limay Subgroup. Formerly that subgroup was treated as a formation, and the Candeleros Formation was known as the Candeleros Member.
The Huincul Formation is a geologic formation of Late Cretaceous age of the Neuquén Basin that outcrops in the Mendoza, Río Negro and Neuquén Provinces of northern Patagonia, Argentina. It is the second formation in the Río Limay Subgroup, the oldest subgroup within the Neuquén Group. Formerly that subgroup was treated as a formation, and the Huincul Formation was known as the Huincul Member.
The Snow Hill Island Formation is an Early Maastrichtian geologic formation found on James Ross Island, James Ross Island group, Antarctica. Remains of a paravian theropod Imperobator antarcticus have been recovered from it, as well as the elasmarian ornithopods Trinisaura santamartaensis, Biscoveosaurus and Morrosaurus antarcticus, the ankylosaurian Antarctopelta oliveroi, and the shark Notidanodon sp. Alongside these described genera are also the remains of indeterminate elasmosaurids, lithostrotian titanosaurs and an indeterminate pterosaur.
The Alcântara Formation is a geological formation in northeastern Brazil whose strata date back to the Cenomanian of the Late Cretaceous.
The Botucatu Formation is an Aptian geologic formation of the Paraná and Pelotas Basins in southern Brazil and northern Uruguay. The formation is composed of quartzitic sandstones, deposited in an eolian environment. Fossil theropod tracks have been reported from the formation.
Caiuajara is an extinct genus of tapejarid pterosaur from the Early Cretaceous period of Brazil. It is known from a single type species, Caiuajara dobruskii.
The year 2011 in Archosaur paleontology was eventful. Archosaurs include the only living dinosaur group — birds — and the reptile crocodilians, plus all extinct dinosaurs, extinct crocodilian relatives, and pterosaurs. Archosaur palaeontology is the scientific study of those animals, especially as they existed before the Holocene Epoch began about 11,700 years ago. The year 2011 in paleontology included various significant developments regarding archosaurs.
This timeline of ceratosaur research is a chronological listing of events in the history of paleontology focused on the ceratosaurs, a group of relatively primitive, often horned, predatory theropod dinosaurs that became the apex predators of the southern hemisphere during the Late Cretaceous. The nature and taxonomic composition of the Ceratosauria has been controversial since the group was first distinguished in the late 19th century. In 1884 Othniel Charles Marsh described the new genus and species Ceratosaurus nasicornis from the Late Jurassic Morrison Formation of the western United States. He felt that it belonged in a new family that he called the Ceratosauridae. He created the new taxon Ceratosauria to include both the Ceratosauridae and the ostrich-like ornithomimids. The idea of the Ceratosauria was soon contested, however. Later that same decade both Lydekker and Marsh's hated rival Edward Drinker Cope argued that the taxon was invalid.
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The Goio-Erê Formation is a geological formation in Brazil. It is sometimes thought to be deposited between the Turonian and Campanian stages of the Late Cretaceous, but an Aptian-Albian date has also been proposed. It primarily consists of sandstone and was deposited in a desert environment. It is known for its exceptional 3-D preservation of fossils, which include those of the pterosaurs Keresdrakon and Caiuajara, the dinosaur Berthasaura as well as the iguanian lizard Gueragama. It is laterally equivalent to the Rio Paraná Formation.
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This article records new taxa of every kind of fossil archosaur that were scheduled to be described during 2023, as well as other significant discoveries and events related to the paleontology of archosaurs that were published in 2023.
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