Kuru kulla

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Kuru
Temporal range: Late Cretaceous (Maastrichtian), [1] 72–71  Ma
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Kuru kulla skull diagram.png
Diagram of known skull material from the holotype (unknown material in dark grey)
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Dinosauria
Clade: Saurischia
Clade: Theropoda
Clade: Paraves
Family:† Dromaeosauridae
Clade:† Eudromaeosauria
Subfamily:† Velociraptorinae
Genus:† Kuru
Napoli et al., 2021
Type species
†Kuru kulla
Napoli et al., 2021
Synonyms

Kuru ( /ˈkuruˈkʊlə/ , after Kurukullā, a Tibetan Buddhist deity) 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. [2]

Contents

Discovery and naming

A map of the Khulsan locality with a photo of some paleontologists at the site Shri ZPAL MgD-I 97 map locality.png
A map of the Khulsan locality with a photo of some paleontologists at the site

The holotype of Kuru kulla was discovered by an American-Mongolian expedition at Khulsan in the Gobi Desert, Mongolia, on 5 July 1991 a few hours before the discovery of the related taxon Shri and was reposited at the Institute of Geology at the Mongolian Academy of Sciences in Ulaanbaatar. The specimen was given the designation IGM 100/981 and consists of a fragmentary skeleton including a right premaxillary bone, the right lacrimal bone, a partial right dentary, the right surangular bone, 14 presacral vertebrae, three caudal vertebrae, fragments of both upper limb bones, a fragmentary ilium, distal ends of both pubes, both femora, a right tibia, and fragments of the right and left feet. The quality of the preservation was inconsistent when the specimen was fossilized, and it is generally poorly-preserved when compared to the remains of the contemporaneous Shri. [2]

In 1992, the holotype was reported as a distinct dromaeosaurid taxon at a Society of Vertebrate Paleontology conference in Toronto, Canada. In their paper describing the large dromaeosaurid Achillobator , Perle and colleagues listed a bibliographic entry titled "Morphology of a Dromaeosaurian dinosaur - Airakoraptor from the Upper Cretaceous of Mongolia". [3] [4]

However, this bibliographic entry is believed to be an error as no such paper is known to exist and it is probably a reference to an unpublished work or an abstract from a conference. This would mean the name "Airakoraptor" is a nomen nudum and is therefore invalid. Napoli and colleagues, in their formal description of Kuru, presume that the name "Airakoraptor" means "Kumis thief", after kumis, also known as "airag" or "airak", a donkey-milk product made in Central Asia. In their description, Napoli and colleagues also explicitly state that the naming of Kuru is not a reference to the disease of the same name. [5]

In 2006, its surangular bone was described in the paper which named the dromaeosaurid Tsaagan . [6] However, later that year, this specimen was confused with the so-called "Zos Wash specimen" found in 1998, which was catalogued under the number IGM 100/3503 and referred to the genus Velociraptor . [2] [7] The holotype was formally described and named in 2021 by James G. Napoli, Alexander Altieri Ruebenstahl, Bhart-Anjan Singh Bhullar, Alan Hamilton Turner, and Mark Allen Norell. [2]

Description

Life restoration of Kuru based on related taxa Kuru UDL.png
Life restoration of Kuru based on related taxa

Kuru is a small-bodied eudromaeosaur, similar in size to Velociraptor . The holotype specimen is known from an incomplete skeleton that is overall similar to other known eudromaeosaurs, indicating that in life it would have resembled its better-understood relatives like Velociraptor and Tsaagan . Napoli and colleagues distinguished Kuru from all other eudromaeosaurs by identifying several autapomorphies including: a deep groove in front of the anterior margin of the external naris, a small horn-like projection on the lacrimal bone, two foramina on the rear of the surangular bone, and pleurocoels on the dorsal vertebrae which are shifted forward compared to related taxa. [2]

Napoli and colleagues in their description of the holotype note that the body proportions indicate that Kuru had a more robust skull than related eudromaeosaurs, but also had proportionally longer limbs and a reduced "killing claw" in its second toe. No study of its functional anatomy has been completed, but the authors hypothesize that these traits suggest slight ecological differences between Kuru and its closest relatives. [2]

Skull

Reconstructed skull of the closely-related Adasaurus Adasaurus Skull.png
Reconstructed skull of the closely-related Adasaurus

The cranium is represented by the anterior part of the right premaxilla (in front of the nostril) and the posterior half of the right lacrimal bone. The premaxilla has only two dental alveoli preserved, but Napoli and colleagues stated that it likely had four premaxillary teeth, which is the condition seen in all toothed theropods. Several features on the surface of the bone are also preserved. The most prominent of these is a c-shaped groove which is anterior to the naris. A similar structure is present in the premaxillae of the related taxa Tsaagan and Linheraptor , but it is much less pronounced in these genera. [2]

The lacrimal is only partially preserved, but based on the parts which are preserved it is inferred to have been t-shaped, like those of other dromaeosaurs. At the anterior end, the lacrimal's articular surface with the nasal bone is preserved and it forms a shelf-like protrusion which would have connected to the ventral side of the nasal in life. On its dorsal posterior side, there is a horn-like protrusion which borders the orbit. The dorsal side of this "hornlet" possessed a rugose surface, similar to those seen in other dromaeosaurs, although they are much more pronounced in Kuru. The lacrimal also preserved a deep excavation on its ventral side, which was interpreted by Napoli and colleagues to be the canal through which the nasolacrimal duct passed. [2]

The mandible is represented by a nearly complete left dentary and surangular bone, but these bones were not preserved continuously and consist of several discrete pieces. There are also nine preserved dentary teeth and three isolated teeth that are either from the dentary or the maxilla. The dentary is straight along its length, unlike most other velociraptorines, and similar to Dromaeosaurus and Deinonychus . It preserved 14 (or possibly 15) tooth positions, which is much higher than the 11-12 typical of other dromaeosaurs, although it is similar to Saurornitholestes , which has a comparable number of dentary teeth. The teeth are ziphodont in shape (narrower along the mediolateral axis than the anteroposterior axis) and possess deep roots and serrations on the front and back edges, at least in the case of the teeth that are well-preserved enough to contain such details. However, they do not possess the enamel ridges on the sides of the teeth which are seen in some other dromaeosaurs. Notably, the third dentary tooth is highly elongated, forming a characteristic "fang" in the lower jaw which is much greater in length than the second or fourth dentary teeth. However, the fourth dentary alveolus is as large at the third, so Napoli and colleagues suggest that the fourth tooth of the type specimen was not fully erupted and may have been of a similar size as the third tooth when finished erupting. [2]

The surangular is mostly complete and contains several diagnostic traits of the Kuru genus. Most notable among these are two foramina, rather than a single one. The prevalence of this trait in velociraptorines is ambiguous due to incompleteness and poor preservation in this area of the skull in Tsaagan and Linheraptor. Napoli and colleagues also comment that the putative tyrannosauroid Bagaraatan has two surangular foramina, but remark that the specimen may be a chimera and thus may offer limited comparative value. The surangular also exhibits a shelf that is inclined dorsally. This is the condition seen in Deinonychus, but differs from that of all other dromaeosaurs in which the same structure is inclined laterally. [2]

Post-cranial skeleton

Numerous vertebrae are preserved with the holotype. Most of them are not continuous or articulated, and several of them only preserve the vertebral centra. Four cervical vertebrae, ten dorsal vertebrae, and three caudal vertebrae in total are preserved. The exact positions of the vertebrae in the spinal column is not known, but comparisons with the related taxa Tsaagan and Shri enabled Napoli and colleagues to give them tentative assignments. Some of the dorsal vertebrae were also incompletely prepared, and could only be observed and analyzed by the use of computer tomography. Although they are partial and fragmentary, the dorsal centra appear to decrease in length from the anterior to the posterior of the spine. [2]

The forelimb of Kuru includes the distal ends of both humeri, a proximal fragment of the right humerus, the proximal end of the right ulna, the proximal and distal ends of the right radius, three left metacarpals articulated with the left semilunate carpal, several isolated phalanges, and two manual claws. The humerus preserves rugose elements along its length, which Napoli and colleagues interpret as muscle attachment sites. They also note that the ulna does not appear to preserve any quill knobs (as have been found in Velociraptor ), although this is possibly a result of poor preservation. There is a ridge which extends distally from the coronoid process of the ulna, which is seen in the controversial genus Balaur . Kuru is also emblematic of pennaraptorans in that it exhibits a flattened expansion at the distal end of the radius. The bones of the hand do not appear to preserve any unique features that distinguish Kuru from any other dromaeosaurids. [2]

The hind limb elements consist of the left postacetabular process and ischiadic peduncle of the ilium, the distal ends of both pubes, both femora, the proximal end of the left tibia, the three left metatarsals and two of the right metatarsals, the left astragalus, sixteen pedal phalanges including some from both feet, and two toe claws. The hind limbs are most similar to Velociraptor and Shri. All three taxa have an enlarged ridge on the lateral surface of the femur. The fourth trochanter is apparently absent in Kuru, but there is a ridge on the femur that is seemingly homologous with it. [2]

Classification

In their description of Kuru, Napoli and colleagues conducted a phylogenetic analysis using a wide variety of paravian taxa. The data set that they use is primarily drawn from the matrix used in the phylogenetic analysis conducted by Steve Brusatte and colleagues in 2014 [8] with the addition of several taxa scored by Pei and colleagues in 2020. [9] Napoli and colleagues adjusted some of the scores from these matrices for the taxa Adasaurus , Tsaagan , and Velociraptor based on independent observation. [2]

In their analysis, they recovered Kuru as the sister taxon to Adasaurus, which is from the slightly younger Nemegt Formation. The uniting synapomorphies for these two taxa include a posterior surangular foramen that excavates 30% of the depth of the bone, an absence of the fourth trochanter, and thoracic centra that are longer than they are wide. Kuru also appears to have had a reduced "killing claw", similar to Adasaurus. This was based on the size of the surface of the pedal phalanges, since the killing claw is not preserved in the holotype of Kuru. [2]

Their analysis recovered the controversial taxon Balaur from Romania as a velociraptorine, [2] which mirrored the analysis of Brusatte and colleagues in 2014. [8] Other analyses have suggested that it may be a true avialan. [10] More conventional results of their analysis include the recovery of Rahonavis as an unenlagiine and of anchiornithids as stem-avialans [2] instead of troodontids. [8] However, the authors also note that the support values for their analysis are relatively low and that further sampling of existing and new taxa would be needed to resolve a more well-supported phylogeny. Additionally, several taxa had to be omitted from their analysis in order to resolve a more defined tree. An abbreviated version of their results, compiled from 100,000 of the most parsimonious trees, can be seen below. [2]

Paraves

In the years since its initial description, dromaeosaurs have been the subject of several phylogenetic analyses. The first of these was published in February of 2022 by Mark J. Powers, Matteo Fabbri, Michael R. Doschak, Bhart-Anjan Bhullar, Davis Evans, Mark A. Norell, and Philip J. Currie. Powers and colleagues conducted a broad phylogenetic analysis using a data set accrued by the use of CT scanning applied to the maxillae of several eudromaeosaurs. They used this new data to attempt to resolve the specific relationships of eudromaeosaurs due to inconsistent results in prior analyses. This analysis did not itself include Kuru, but it did contain the data set used in future analyses. [11]

The first major analysis to include Kuru by name was the publication which described the new genus Daurlong from the Longjiang Formation of northeastern China. This analysis, published by Xuri Wang, Andrea Cau, and colleagues in November of 2022 included a wide variety of maniraptoran taxa, including Kuru and several dromaeosaurs. Their results corroborated the findings of Napoli and colleagues by finding a close relationship between Kuru and Adasaurus . [2] [12] However, they found both taxa as being more closely related to Saurornitholestes than to Tsaagan or Velociraptor . Their analysis also recovers Rahonavis and anchiornithids as true avialans. [12]

The most recent phylogeny to include Kuru was published by Łukasz Czepiński and accompanied his description of a skull assigned to the genus Shri . In his publication, Czepiński replicated the analyses of Napoli and colleagues [2] as well as of Powers and colleagues [11] using the data sets they provided. [13] This data, combined with their own data, which included several measurements of the skull, provided few discrepancies with the prior analyses. Czepiński's primary concern was with the genus Shri and its relationship to Velociraptor, and both analyses resulted in substantially similar placements on the tree for these genera. This focus also meant that Czepiński did not hypothesize in regard to the implications their analysis had on the wider phylogeny. Notable among his results was the recovery of Adasaurus as being outside the dromaeosaurine-velociraptorine-saurornitholestine split. The tree produced using the modified data set of Powers and colleagues is shown below. [13]

Eudromaeosauria

Paleoecology

Diet

The diet and ecology of Kuru has not been thoroughly studied. However, multiple publications note the apparent occurrence of at least three distinct dromaeosaurs in the Barun Goyot Formation. These include Kuru, Shri , and an undescribed specimen which has been referred to Velociraptor , but may represent a new taxon. [2] [14]

It has been speculated that these animals may have had similar prey preferences, [2] but it is also possible that they each filled a unique ecological niche due to the presumed difference in the skull length of Shri and Kuru. [13] However, multiple researchers have noted that the skulls are too incompletely known to make any concrete hypotheses on the matter. [14]

Paleoenvironment

A map of the world in the Campanian, with the Barun Goyot Formation labeled "6-8" Late Cretaceous metatherian locales - ZooKeys 465.jpg
A map of the world in the Campanian, with the Barun Goyot Formation labeled "6-8"

The type and only specimen of Kuru was found at a locality called Khulsan of the Barun Goyot Formation, which is near the Mongolian city of Gurvan Tes in the Ömnögovi Province. [2] This locality is very close to an outcropping of the Nemegt Formation, which is believed to be younger than the Barun Goyot Formation. [15] [16]

The sediments of the formation were deposited in various conditions, with the lower part consisting of alternating dune deposits and lakes that existed in interdune areas, while the upper part consisted of sediments that were deposited over an area similar to takyrs that was flooded at irregular intervals. [17] This formation is mostly characterized by series of red beds, mostly light-coloured sands (yellowish, grey-brown, and rarely reddish) that are locally cemented. Sandy claystones, siltstones, conglomerates, and large-scale trough cross-stratification in sands are also common across the unit. In addition, structureless, medium-grained, fine-grained and very fine-grained sandstones predominate in sediments of the formation. [15] [16]

The overall geology of the formation indicates that sediments were deposited under relatively arid to semiarid climates in alluvial plain, lacustrine, and aeolian paleoenvironments, with addition of other short-lived water bodies. [1] [18]

Contemporary fauna

An artistic rendition of the contemporary Natovenator in its environment Natovenator hunting fish.png
An artistic rendition of the contemporary Natovenator in its environment

The Barun Goyot Formation is similar to the underlying Djadochta Formation in being composed of aeolian dune deposits which primarily preserve small and mid-sized animals. Several named lizard genera are known including Gobiderma and Estesia . Mammals were also abundant in the region during the Cretaceous. They are represented by multituberculates such as Catopsbaatar and Nemegtbaatar , metatherians like Deltatheridium , and eutherians like Asioryctes and Barunlestes . [18] [19]

Dinosaurs are the most well-represented vertebrates from Barun Goyot. There are several ankylosaur fossils including Saichania , Tarchia , Zaraapelta , and an undecribed taxon from the Hermiin Tsav locality. [20] A single sauropod skull is also known from Barun Goyot, and was given the name Quaesitosaurus . [21] Marginocephalians are also present and are represented by the pachycephalosaur Tylocephale and the ceratopsian Bagaceratops , which is the most common animal found in the formation. [22]

The most species-rich dinosaur group represented at Barun Goyot are the maniraptorans. They include at least four alvarezsaurs ( Ceratonykus , Khulsanurus , Ondogurvel , and Parvicursor ) [23] and several oviraptorosaurs, such as Nemegtomaia , which are also found in the Nemegt Formation. [24] Dromaeosaurs were also common and included Shri , the possibly semiaquatic Natovenator , and an unnamed taxon. [2] [25] The smallest maniraptorans present were the birds. These included the enigmatic Hollanda , the more well-understood Gobipteryx , and numerous fossilized eggs which preserve bird embryos. [26] [27]

See also

Related Research Articles

<i>Velociraptor</i> Dromaeosaurid dinosaur genus from the Late Cretaceous

Velociraptor is a genus of small dromaeosaurid dinosaurs that lived in Asia during the Late Cretaceous epoch, about 75 million to 71 million years ago. Two species are currently recognized, although others have been assigned in the past. The type species is V. mongoliensis, named and described in 1924. Fossils of this species have been discovered in the Djadochta Formation, Mongolia. A second species, V. osmolskae, was named in 2008 for skull material from the Bayan Mandahu Formation, China.

<i>Protoceratops</i> Genus of reptiles (fossil)

Protoceratops is a genus of small protoceratopsid dinosaurs that lived in Asia during the Late Cretaceous, around 75 to 71 million years ago. The genus Protoceratops includes two species: P. andrewsi and the larger P. hellenikorhinus. The former was described in 1923 with fossils from the Mongolian Djadokhta Formation, and the latter in 2001 with fossils from the Chinese Bayan Mandahu Formation. Protoceratops was initially believed to be an ancestor of ankylosaurians and larger ceratopsians, such as Triceratops and relatives, until the discoveries of other protoceratopsids. Populations of P. andrewsi may have evolved into Bagaceratops through anagenesis.

<i>Atrociraptor</i> Extinct genus of dinosaurs

Atrociraptor is a genus of dromaeosaurid dinosaur that lived during the Late Cretaceous in what is now Alberta, Canada. The first specimen, a partial skull, was discovered in 1995 by the fossil collector Wayne Marshall in the Horseshoe Canyon Formation, about 5 km (3 mi) from the Royal Tyrrell Museum of Palaeontology where it was brought for preparation. In 2004, the specimen became the holotype of the new genus and species Atrociraptor marshalli; the generic name is Latin for "savage robber", and the specific name refers to Marshall. The holotype consists of the premaxillae, a maxilla, the dentaries, associated teeth, and other skull fragments. Isolated teeth from the same formation have since been assigned to Atrociraptor.

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

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.

<i>Adasaurus</i> Extinct genus of dinosaurs

Adasaurus is a genus of dromaeosaurid dinosaur that lived in Asia during the Late Cretaceous period about 70 million years ago. The genus is known from two partial specimens found in the Nemegt Formation of Mongolia that were partially described in 1983 by the paleontologist Rinchen Barsbold.

<i>Achillobator</i> Extinct dromaeosaurid genus from the Late Cretaceous

Achillobator is a genus of large dromaeosaurid theropod dinosaur that lived during the Late Cretaceous period about 96 million to 89 million years ago in what is now the Bayan Shireh Formation of Mongolia. The genus is currently monotypic, only including the type species A. giganticus. The first remains were found in 1989 during a Mongolian-Russian field expedition and later described in 1999. Remains at the type locality of Achillobator may represent additional specimens. It represents the first and largest dromaeosaurid known from the Bayan Shireh Formation.

<i>Bagaceratops</i> Protoceratopsid dinosaur genus from the Late Cretaceous

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.

<i>Tylocephale</i> Extinct genus of dinosaurs

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.

<i>Hulsanpes</i> Extinct genus of dinosaurs

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.

<span class="mw-page-title-main">Barun Goyot Formation</span> Geological formation in Mongolia

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.

<i>Tsaagan</i> Extinct genus of dinosaurs

Tsaagan is a genus of dromaeosaurid dinosaur from the Djadokhta Formation of the Late Cretaceous of Mongolia.

<i>Ceratonykus</i> Extinct genus of dinosaurs

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.

<i>Linheraptor</i> Extinct genus of dinosaurs

Linheraptor is a genus of dromaeosaurid dinosaur which lived in what is now China in the Late Cretaceous. It was named by Xu Xing and colleagues in 2010, and contains the species Linheraptor exquisitus. This bird-like dinosaur was less than 2 m (6.5 ft) long and was found in Inner Mongolia. It is known from a single, nearly complete skeleton.

<span class="mw-page-title-main">Eudromaeosauria</span> Extinct clade of dinosaurs

Eudromaeosauria is a subgroup of terrestrial dromaeosaurid theropod dinosaurs. They were small to large-sized predators that flourished during the Cretaceous Period. Eudromaeosaur fossils are known almost exclusively from the northern hemisphere.

<i>Shri devi</i> Extinct species of dromaeosaurid dinosaurs

Shri is a genus of small dromaeosaurid dinosaur that lived in Asia during the Late Cretaceous epoch, with fossils reported from Barun Goyot Formation in Khulsan, Mongolia. The type and only species, Shri devi, was described in 2021 by paleontologist Alan H. Turner and colleagues.

<i>Kansaignathus</i> Extinct genus of dinosaurs

Kansaignathus is an extinct genus of dromaeosaurid theropod from the Late Cretaceous Yalovach Formation of Tajikistan. The genus contains only one species, the type species, K. sogdianus. The generic name of Kansaignathus comes from near the town of Konsoy where it was discovered and the Greek word "gnathos" meaning "jaw". The specific epithet "sogdianus" is derived from the historical region of Sogdiana, which was an ancient name for the Fergana Valley region where the fossil was discovered. Kansaignathus is known from a single right dentary bone and a few post-cranial bone fragments. It was the first, and so far the only, dinosaur from Tajikistan to be described and named.

<i>Ondogurvel</i> Genus of alvarezsaurid dinosaur

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.

<i>Natovenator</i> Genus of dromaeosaurid dinosaurs from the Late Cretaceous

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.

<i>Jaculinykus</i> Genus of alvarezsaurid dinosaurs

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.

<i>Harenadraco</i> Genus of troodontid dinosaurs

Harenadraco is an extinct genus of troodontid theropod dinosaurs from the Late Cretaceous Baruungoyot Formation of Mongolia. The genus contains a single species, H. prima, known from a fragmentary skeleton. Harenadraco represents the first troodontid known from the Baruungoyot Formation. Since members of this family are also known from the Nemegt and Djadochta Formations, the discovery of Harendraco indicates that troodontids were important faunal components of every formation within the Nemegt Basin.

References

  1. 1 2 Gradziński, R.; Jerzykiewicz, T. (1974). "Sedimentation of the Barun Goyot Formation" (PDF). Palaeontologia Polonica. 30: 111−146.
  2. 1 2 3 4 5 6 7 8 9 10 11 12 13 14 15 16 17 18 19 20 21 22 23 24 Napoli, J. G.; Ruebenstahl, A. A.; Bhullar, B.-A. S.; Turner, A. H.; Norell, M. A. (2021). "A New Dromaeosaurid (Dinosauria: Coelurosauria) from Khulsan, Central Mongolia" (PDF). American Museum Novitates (3982): 1–47. doi:10.1206/3982.1. hdl:2246/7286. ISSN   0003-0082. S2CID   243849373.
  3. ↑ Norell, M. A.; Clark, J. M.; Perle, A. (1992). "New dromaeosaur material from the Late Cretaceous of Mongolia". Journal of Vertebrate Paleontology. 12 (3): 45A.
  4. ↑ Perle, A.; Norell, M. A.; Clark, J. M. (1999). "A new maniraptoran Theropod – Achillobator giganticus (Dromaeosauridae) – from the Upper Cretaceous of Burkhant, Mongolia". Contribution No. 101 of the Mongolian-American Paleontological Project: 1–105.
  5. ↑ Norell, M.A.; P.J. Makovicky (1997). "Important features of the dromaeosaur skeleton: information from a new specimen". American Museum Novitates (3215): 1–45.
  6. ↑ Norell, M.A.; Clark, James Matthew; Turner, Alan Hamilton; Makovicky, Peter J.; Barsbold, Rinchin; Rowe, Timothy (2006). "A new dromaeosaurid theropod from Ukhaa Tolgod (Ömnögov, Mongolia)". American Museum Novitates (3545): 1–51. doi:10.1206/0003-0082(2006)3545[1:ANDTFU]2.0.CO;2.
  7. ↑ Turner, A.H.; P.J. Makovicky; M.A. Norell (2007). "Feather quill knobs in the dinosaur Velociraptor" (PDF). Science. 317 (5845): 1721. Bibcode:2007Sci...317.1721T. doi:10.1126/science.1145076. PMID   17885130. S2CID   11610649.
  8. 1 2 3 Brusatte, Stephen L.; Lloyd, Graeme T.; Wang, Steve C.; Norell, Mark A. (2014). "Gradual Assembly of Avian Body Plan Culminated in Rapid Rates of Evolution across the Dinosaur-Bird Transition" (PDF). Current Biology. 24 (20): 2386–2392. Bibcode:2014CBio...24.2386B. doi:10.1016/j.cub.2014.08.034. PMID   25264248. S2CID   8879023.
  9. ↑ Pei, Rui; Pittman, Michael; Goloboff, Pablo A.; Dececchi, T. Alexander; Habib, Michael B.; Kaye, Thomas G.; Larsson, Hans C.E.; Norell, Mark A.; Brusatte, Stephen L.; Xu, Xing (2020). "Potential for Powered Flight Neared by Most Close Avialan Relatives, but Few Crossed Its Thresholds" (PDF). Current Biology. 30 (20): 4033–4046.e8. Bibcode:2020CBio...30E4033P. doi:10.1016/j.cub.2020.06.105. PMID   32763170. S2CID   221015472.
  10. ↑ Cau, Andrea; Brougham, Tom; Naish, Darren (2015). "The phylogenetic affinities of the bizarre Late Cretaceous Romanian theropod Balaur bondoc(Dinosauria, Maniraptora): Dromaeosaurid or flightless bird?". PeerJ. 3: e1032. doi: 10.7717/peerj.1032 . PMC   4476167 . PMID   26157616.
  11. 1 2 Powers, Mark J.; Fabbri, Matteo; Doschak, Michael R.; Bhullar, Bhart-Anjan S.; Evans, David C.; Norell, Mark A.; Currie, Philip J. (2021). "A new hypothesis of eudromaeosaurian evolution: CT scans assist in testing and constructing morphological characters". Journal of Vertebrate Paleontology. 41 (5). Bibcode:2021JVPal..41E0087P. doi:10.1080/02724634.2021.2010087. S2CID   247039404.
  12. 1 2 Wang, Xuri; Cau, Andrea; Guo, Bin; Ma, Feimin; Qing, Gele; Liu, Yichuan (2022). "Intestinal preservation in a birdlike dinosaur supports conservatism in digestive canal evolution among theropods". Scientific Reports. 12 (1): 19965. Bibcode:2022NatSR..1219965W. doi:10.1038/s41598-022-24602-x. PMC   9675785 . PMID   36402874.
  13. 1 2 3 Czepiński, Łukasz (2023). "Skull of a dromaeosaurid Shri devi from the Upper Cretaceous of the Gobi Desert suggests convergence to the North American forms". Acta Palaeontologica Polonica. 68. doi: 10.4202/app.01065.2023 . S2CID   259441055.
  14. 1 2 Ruebenstahl, Alexander; Napoli, James; Turner, Alan; Bhullar, Bhart-Anjan; Norell, Mark A. (2021). "Two New Eudromaeosaurs from Khulsan (Central Mongolia) Reveal Modern-Like Faunal Predatory Structure Amoung [sic] Non-Avian Dinosaurs". Geological Society of America. Geological Society of America Abstracts with Programs. doi:10.1130/abs/2021AM-368751. S2CID   240115476.
  15. 1 2 Jerzykiewicz, Tomasz; Currie, Philip J.; Fanti, Federico; Lefeld, Jerzy (2021). "Lithobiotopes of the Nemegt Gobi Basin1". Canadian Journal of Earth Sciences. 58 (9): 829–851. doi:10.1139/cjes-2020-0148. S2CID   233882352.
  16. 1 2 Eberth, D. A. (2018). "Stratigraphy and paleoenvironmental evolution of the dinosaur-rich Baruungoyot-Nemegt succession (Upper Cretaceous), Nemegt Basin, southern Mongolia". Palaeogeography, Palaeoclimatology, Palaeoecology. 494: 29–50. Bibcode:2018PPP...494...29E. doi:10.1016/j.palaeo.2017.11.018.
  17. ↑ Saneyoshi, Mototaka; Watabe, Mahito; Suzuki, Shigeru; Tsogtbaatar, Khishigjav (2011). "Trace fossils on dinosaur bones from Upper Cretaceous eolian deposits in Mongolia: Taphonomic interpretation of paleoecosystems in ancient desert environments". Palaeogeography, Palaeoclimatology, Palaeoecology. 311 (1–2): 38–47. Bibcode:2011PPP...311...38S. doi:10.1016/j.palaeo.2011.07.024.
  18. 1 2 Gradziński, R.; Jaworowska, Z. K.; Maryańska, T. (1977). "Upper Cretaceous Djadokhta, Barun Goyot and Nemegt formations of Mongolia, including remarks on previous subdivisions". Acta Geologica Polonica. 27 (3): 281–326.
  19. ↑ Novacek, Michael J.; Hoffman, Eva A.; o'Leary, Maureen A. (2022). "First occurrence of the eutherian mammal Asioryctes nemegtensis from the Upper Cretaceous Djadokhta Formation, Gobi Desert, Mongolia, and a revised alpha taxonomy based on the skull and dentition". Journal of Vertebrate Paleontology. 42 (4). Bibcode:2022JVPal..42E6320N. doi: 10.1080/02724634.2023.2196320 . S2CID   258470274.
  20. ↑ Arbour, V. M.; Currie, P. J.; Badamgarav, D. (2014). "The ankylosaurid dinosaurs of the Upper Cretaceous Baruungoyot and Nemegt formations of Mongolia". Zoological Journal of the Linnean Society. 172 (3): 631−652. doi:10.1111/zoj.12185.
  21. ↑ Wilson, J. A. (2005). "Redescription of the Mongolian Sauropod Nemegtosaurus mongoliensis Nowinski (Dinosauria: Saurischia) and Comments on Late Cretaceous Sauropod Diversity". Journal of Systematic Palaeontology. 3 (3): 283−318. Bibcode:2005JSPal...3..283W. doi:10.1017/S1477201905001628. S2CID   54070651.
  22. ↑ Czepiński, Ł. (2019). "Ontogeny and variation of a protoceratopsid dinosaur Bagaceratops rozhdestvenskyi from the Late Cretaceous of the Gobi Desert". Historical Biology. 32 (10): 1394–1421. doi:10.1080/08912963.2019.1593404. S2CID   132780322.
  23. ↑ Alexander O. Averianov; Alexey V. Lopatin (2022-02-19). "A new alvarezsaurid theropod dinosaur from the Upper Cretaceous of Gobi Desert, Mongolia". Cretaceous Research. 135: 105168. Bibcode:2022CrRes.13505168A. doi:10.1016/j.cretres.2022.105168. S2CID   247000540.
  24. ↑ Funston, G. F.; Mendonca, S. E.; Currie, P. J.; Barsbold, R. (2018-04-01). "Oviraptorosaur anatomy, diversity and ecology in the Nemegt Basin". Palaeogeography, Palaeoclimatology, Palaeoecology. THE LATE CRETACEOUS NEMEGT ECOSYSTEM: DIVERSITY, ECOLOGY, AND GEOLOGICAL SIGNATURE. 494: 101–120. Bibcode:2018PPP...494..101F. doi:10.1016/j.palaeo.2017.10.023. ISSN   0031-0182.
  25. ↑ Lee, S.; Lee, Y.-N.; Currie, P. J.; Sissons, R.; Park, J.-Y.; Kim, S.-H.; Barsbold, R.; Tsogtbaatar, K. (2022). "A non-avian dinosaur with a streamlined body exhibits potential adaptations for swimming". Communications Biology. 5 (1185): 1185. doi: 10.1038/s42003-022-04119-9 . ISSN   2399-3642. PMC   9715538 . PMID   36456823.
  26. ↑ Bell, Alyssa K.; Chiappe, Luis M.; Erickson, Gregory M.; Suzuki, Shigeru; Watabe, Mahito; Barsbold, Rinchen; Tsogtbaatar, K. (2010). "Description and ecologic analysis of Hollanda luceria, a Late Cretaceous bird from the Gobi Desert (Mongolia)". Cretaceous Research. 31 (1): 16–26. Bibcode:2010CrRes..31...16B. doi:10.1016/j.cretres.2009.09.001.
  27. ↑ Varricchio, David J.; Balanoff, Amy M.; Norell, Mark A. (2015). "Reidentification of Avian Embryonic Remains from the Cretaceous of Mongolia". PLOS ONE. 10 (6): e0128458. Bibcode:2015PLoSO..1028458V. doi: 10.1371/journal.pone.0128458 . PMC   4452496 . PMID   26030147.
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