Gobipteryx Temporal range: Late Cretaceous, | |
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Eggs of Gobipteryx minuta | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Clade: | Dinosauria |
Clade: | Saurischia |
Clade: | Theropoda |
Clade: | Avialae |
Clade: | † Enantiornithes |
Family: | † Gobipterygidae |
Genus: | † Gobipteryx Elżanowski, 1974 |
Species: | †G. minuta |
Binomial name | |
†Gobipteryx minuta Elżanowski, 1974 | |
Synonyms | |
Gobipteryx (from Gobi [referring to the Gobi Desert where it was first discovered], and Greek pteryx "wing") is a genus of prehistoric bird from the Campanian Age of the Late Cretaceous Period. [1] It is not known to have any direct descendants. [1] Like the rest of the enantiornithes clade, Gobipteryx is thought to have gone extinct near the end of the Cretaceous. [2]
Based on a skull length of 45 millimeters, Gobipteryx has been estimated to be approximately the size of a partridge. [3] Its bones are fibrolamellar. [4]
The skull's general shape is gradually tapering toward the front. [1] Gobipteryx has a toothless beak [1] formed from the fusion of the premaxillae bones. [5] The skull is characterized as being rhynchokinetic [1] with the pterygoid bones articulating with both the vomers [3] [6] and the palatine. [1] [3] The nares are tear shaped and the choana is located below them, more rosteral than in most modern birds. [7] The nares are smaller than the antorbital fenestrae, a basal feature for ornithurae birds. [7] In addition, Gobipteryx's skull has an articulated rostrum. [7] The jaw hinge is associated with the articulation of the quadrate with the pterygoid processes. [1] The articular region of the mandible contains internal and retroarticular processes and has uniform symphysis. [1] This animal has a large, uniform, and sutureless braincase. [1]
The vertebral column consists of at least 19 presacral vertebrae, the last six of these being dorsals. [8] The neural spines of the twelfth and thirteenth vertebrae form the nuchal blade, which represents the point of greatest elevation in the vertebral column. [8]
The scapula contains a prominent glenoid labrum and tapers backward, ending as thin rods. [8] The coracoids are slightly concave anteriorly and are separate from the scapulae dorsally. They also stick out from the neck on either side. [8] Gobipteryx's clavicles curve in a way that is consistent with that of other birds. [8]
The humerus is posteriorly convex (a normal trait for birds) and the head is comma-shaped. [8] Gobipteryx's ulna is about twice as thick as the radius. [8] Metacarpals II and III have been found in embryonic fossils and are observed to be about equal size and are in close contact with each other. [8]
Gobipteryx is believed to have been capable of flight. [4] [8] The scapula is long, and therefore, well suited for flight by having more area for muscle attachment. [8] In addition, the forelimb of Gobipteryx is more than twice the length of the thorax, falling within the acceptable range observed in flying birds. [8]
Gobipteryx, along with other enantiornithes, is thought to have superprecocial development, in which it was capable of flying upon hatching. [4] [8] Evidence for this comes from the fact that the forelimbs and shoulders of advanced embryos are almost completely ossified. [8] In addition, the growth of G. minuta has been shown to slow down immediately following hatching. [4] This suggests that it was highly mobile in its life, since locomotion has been shown to slow the growth of young birds by focusing energy and resources elsewhere. [4] This onset of flight so early in life is not seen in most modern birds, which begin flying when they have reached or are close to full size. [4]
The first specimens were two damaged skulls discovered as part of the 1971 Polish-Mongolian Paleontological Expedition to the Gobi Desert by Dr. Teresa Maryańska, [1] however, at the time, it was not immediately recognized that both of these skulls belonged to Gobipteryx. [3] [6] It was first found in the sandstones of the Lower Nemegt Beds of the Barun Goyot Formation of the Nemegt Basin. [1] The holotype specimen is housed at the Institute of Paleobiology of the Polish Academy of Sciences [8] in Warsaw, Poland and was first described by Dr. Andrzej Elżanowski using a single damaged skull. [1] Initially, Gobipteryx was classified as a member of the clade Palaeognathae on the basis of its jaw and palate. [1] However, in 1981, Dr. Cyril Walker defined the clade enantiornithes [9] and Gobipteryx was reclassified as an enantiornithes bird.
In 1996, Evgeny Kurochkin described a new bird known as Nanantius valifanovi also from the Barun Goyot Formation. [10] However, it was later discovered that N. valifanoi was actually a new misidentified specimen of Gobipteryx minuta. [7] The mistake was, at least in part, due to a misidentification of the maxilla and dentary bones of the skull. [7]
In 1994, an expedition to the Gobi Desert was conducted by the American Museum of Natural History and the Mongolian Academy of Sciences, where a well preserved Gobiptetyx minuta skull was found in the Nemegt Basin. [7] This new specimen provided further evidence for the placement of Gobipteryx into enantiornithes. [7] In addition, it allowed for the reconstruction of the palate, which was poorly understood in Mesozoic birds. [7]
Also during the 1971 Polish-Mongolian Paleontological Expedition to the Gobi Desert, in which the first specimens were found, advanced embryos of Gobipteryx minuta were found. [8] Seven specimens in total were found, including two skeletons in the redbeds of Khermeen Tsav in Mongolia's Gobi Desert. [8] These embryos made up the second confirmed embryonic fossils from before the Quaternary Period as well as the first confirmed postcranial fossils of G. minuta found. [8]
Catopsbaatar is a genus of multituberculate, an extinct order of rodent-like mammals. It lived in what is now Mongolia during the late Campanian age of the Late Cretaceous epoch, about 72 million years ago. The first fossils were collected in the early 1970s, and the animal was named as a new species of the genus Djadochtatherium in 1974, D. catopsaloides. The specific name refers to the animal's similarity to the genus Catopsalis. The species was moved to the genus Catopsalis in 1979, and received its own genus in 1994. Five skulls, one molar, and one skeleton with a skull are known; the last is the genus' most complete specimen. Catopsbaatar was a member of the family Djadochtatheriidae.
The Enantiornithes, also known as enantiornithines or enantiornitheans in literature, are a group of extinct avialans, the most abundant and diverse group known from the Mesozoic era. Almost all retained teeth and clawed fingers on each wing, but otherwise looked much like modern birds externally. Over eighty species of Enantiornithes have been named, but some names represent only single bones, so it is likely that not all are valid. The Enantiornithes became extinct at the Cretaceous–Paleogene boundary, along with Hesperornithes and all other non-avian dinosaurs.
Avimimus, meaning "bird mimic", is a genus of oviraptorosaurian theropod dinosaur, named for its bird-like characteristics, that lived in the late Cretaceous in what is now Mongolia, around 85 to 70 million years ago.
Opisthocoelicaudia is a genus of sauropod dinosaur of the Late Cretaceous Period discovered in the Gobi Desert of Mongolia. The type species is Opisthocoelicaudia skarzynskii. A well-preserved skeleton lacking only the head and neck was unearthed in 1965 by Polish and Mongolian scientists, making Opisthocoelicaudia one of the best known sauropods from the Late Cretaceous. Tooth marks on this skeleton indicate that large carnivorous dinosaurs had fed on the carcass and possibly had carried away the now-missing parts. To date, only two additional, much less complete specimens are known, including part of a shoulder and a fragmentary tail. A relatively small sauropod, Opisthocoelicaudia measured about 11.4–13 m (37–43 ft) in length. Like other sauropods, it would have been characterised by a small head sitting on a very long neck and a barrel shaped trunk carried by four column-like legs. The name Opisthocoelicaudia means "posterior cavity tail", alluding to the unusual, opisthocoel condition of the anterior tail vertebrae that were concave on their posterior sides. This and other skeletal features lead researchers to propose that Opisthocoelicaudia was able to rear on its hindlegs.
Bagaceratops is a genus of small protoceratopsid dinosaurs that lived in Asia during the Late Cretaceous, around 72 to 71 million years ago. Bagaceratops remains have been reported from the Barun Goyot Formation and Bayan Mandahu Formation. One specimen may argue the possible presence of Bagaceratops in the Djadochta Formation.
Breviceratops is a genus of protoceratopsid dinosaur that lived during the Late Cretaceous in what is now the Barun Goyot Formation, Mongolia.
Tylocephale is a genus of pachycephalosaurid dinosaur, a group of dome-headed, herbivorous ornithischians, that lived during the Late Campanian stage of the Late Cretaceous in what is now Mongolia. It is known from a partial skull and associated mandible that were unearthed in 1971 by a Polish-Mongolian Expedition to the Barun Goyot Formation of the Gobi Desert. The specimen was described in 1974 by Polish paleontologists Teresa Maryańska and Halszka Osmólska as a new genus and species.
Kuru is a genus of dromaeosaurid theropod from the Late Cretaceous Barun Goyot Formation of Mongolia. The genus contains only a single species, the type species Kuru kulla, which is known from a fragmentary skeleton including a partial skull.
Hulsanpes is a genus of halszkaraptorine theropod dinosaurs that lived during the Late Cretaceous in what is now the Barun Goyot Formation of Mongolia, about 75-72 million years ago. The remains were found in 1970 and formally described in 1982 by Halszka Osmólska, who noted that the genus is represented by an immature individual. Hulsanpes represents the first record of the basal dromaeosaurid subfamily Halszkaraptorinae.
The Barun Goyot Formation is a geological formation dating to the Late Cretaceous Period. It is located within and is widely represented in the Gobi Desert Basin, in the Ömnögovi Province of Mongolia.
The Nemegt Formation is a geological formation in the Gobi Desert of Mongolia, dating to the Late Cretaceous. The formation consists of river channel sediments and contains fossils of fish, turtles, crocodilians, and a diverse fauna of dinosaurs, including birds.
The Djadochta Formation is a highly fossiliferous geological formation situated in Central Asia, Gobi Desert, dating from the Late Cretaceous period, about 75 million to 71 million years ago. The type locality is the Bayn Dzak locality, famously known as the Flaming Cliffs. Reptile and mammal remains are among the fossils recovered from the formation.
Nanantius is a genus of extinct enantiornithean avialan known from the Early Cretaceous of Australia.
Ceratonykus is a monospecific genus of alvarezsaurid dinosaur from Mongolia that lived during the Late Cretaceous in what is now the Barun Goyot Formation. The type and only species, Ceratonykus oculatus, is known from a fragmentary skeleton, including an incomplete skull, of an adult individual. It was named and described in 2009 by Vladimir Alifanov and Rinchen Barsbold. Its describers questioned the traditional placement of alvarezsaurs in Theropoda, instead suggesting they were ornithischians, but this has not been accepted since. Ceratonykus has an estimated length of 75 centimetres and weight of 760 grams. It has been considered as a possible junior synonym of Parvicursor.
Styloolithus is an oogenus of highly distinctive fossil egg from the Upper Cretaceous Djadokhta Formation and the Barun Goyot Formation in Mongolia.
Gobioolithus is an oogenus of fossil bird egg native to Mongolia. They are small, smooth-shelled, and elongated eggs that were first discovered in the 1960s and early 70s during a series of fossil-hunting expeditions in the Gobi desert. Two oospecies have been described: Gobioolithus minor and G. major. The eggs were probably laid in colonial nesting sites on the banks of rivers and lakes.
Khulsanurus is an extinct genus of alvarezsaurid theropod dinosaur from the Late Cretaceous Barungoyot Formation of the Khulsan Locality in the Gobi Desert region of Mongolia. The type and only species is Khulsanurus magnificus.
Ondogurvel is a genus of alvarezsaurid dinosaur from the Late Cretaceous (Campanian) Barun Goyot Formation in southern Mongolia. The type and only species is O. alifanovi, known from a partial skeleton consisting of fragments of two last dorsal vertebrae, three anterior sacral vertebrae, right ilium, left and right pubis and ischium, articulated right tibia, fibula, metatarsals II and IV, and phalanges IV-1 and IV-2, right carpometacarpus, left and right manual phalanx II-1, right femur, left pedal phalanx II-1, and fragments of unidentified phalanges.
Natovenator is a genus of halszkaraptorine dromaeosaurid dinosaur from the Late Cretaceous Barun Goyot Formation of Mongolia. The genus is known from a single species, N. polydontus. Natovenator is crucial to the understanding of halszkaraptorines due to it providing more support for the semi-aquatic lifestyle that has been proposed for this clade. This discovery is important as the semi-aquatic lifestyles of halszkaraptorines was contested in early 2022.
Jaculinykus is an extinct genus of alvarezsaurid theropod dinosaur from the Late Cretaceous Baruungoyot Formation of Mongolia. The genus contains a single species, J. yaruui, known from a nearly complete articulated skeleton including bones of the skull. Jaculinykus is notable for its unique hand, which has a hypertrophied first digit and greatly reduced second digit, which is intermediate between the tridactyl hand of Shuvuuia and monodactyl hand of Linhenykus.