Erlikosaurus

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Erlikosaurus
Temporal range: Late Cretaceous,
~96–89  Ma
Erlikosaurus Skeleton Reconstruction.jpg
Skeletal diagram of the holotype
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Dinosauria
Clade: Saurischia
Clade: Theropoda
Superfamily:† Therizinosauroidea
Family:† Therizinosauridae
Genus:† Erlikosaurus
Barsbold & Perle, 1980
Type species
†Erlikosaurus andrewsi
Barsbold & Perle, 1980
Synonyms

Erlikosaurus (meaning "Erlik's lizard") is a genus of therizinosaurid that lived in Asia during the Late Cretaceous period. The fossils, a skull and some post-cranial fragments, were found in the Bayan Shireh Formation of Mongolia in 1972, dating to around 96 million and 89 million years ago. These remains were later described by Altangerel Perle and Rinchen Barsbold in 1980, naming the new genus and species Erlikosaurus andrewsi. It represents the second therizinosaur taxon from this formation (alongside Enigmosaurus and Segnosaurus ) with the most complete skull among members of this peculiar family of dinosaurs.

Contents

In contrast to most therizinosaurids, Erlikosaurus was a small member reaching nearly 3.4 m (11 ft) in length and 150 to 250 kg (330 to 550 lb) in mass. It had a well-developed beak at the snout tip and toothed jaws that were used for its herbivorous diet. The feet ended in four toes with the first one articulated to the ankle—in contrast to the vestigial first toe of most theropods. Like other therizinosaurids, Erlikosaurus had a large gut for food processing, strong arms ending in elongated claws, and a backwards directed pelvis.

Erlikosaurus is classified as a therizinosaur within the Therizinosauridae. Therizinosaurs were long-enigmatic dinosaurs with unclear relationships during the early years of research. Subsequent studies proved their true nature as theropodan dinosaurs and systematic position among maniraptorans. The beak and jaws of Erlikosaurus indicate a leaf-stripping feeding method characterized by the active use of the beak aided by the neck. Several differences with the sympatric Segnosaurus shows that these related genera were niche partitioned.

Discovery and naming

Fossil localities in Mongolia. Locality of Erlikosaurus in Bayshin Tsav, at Area C Cretaceous-aged dinosaur fossil localities of Mongolia.PNG
Fossil localities in Mongolia. Locality of Erlikosaurus in Bayshin Tsav, at Area C

The holotype specimen, MPC-D 100/111, was found in layers from the Bayshin Tsav locality on the Bayan Shireh Formation, consisting of an exceptionally well preserved skull, a virtually complete right pes only lacking the proximal end of metatarsals II, III and IV, and an almost complete left humerus. Other remains include some fragmentary cervical vertebrae, however, the count is not specified and they were not illustrated. These findings were made during a Soviet-Mongolian expedition in the Ömnögovi Province in 1972. [1] [2] Eight years later, the genus and type species, Erlikosaurus andrewsi, was named and described (although very briefly) by paleontologists Rinchen Barsbold and Altangerel Perle in 1980, however, Barsbold was not indicated as the name-giver of this particular species. The generic name, Erlikosaurus, was taken from that of the demon king Erlik, from Turko-Mongolian mythology and the Greek σαῦρος (sauros, meaning lizard). The specific name, andrewsi, is in honour to the American paleontologist Roy Chapman Andrews, who was the leader of the American Asiatic Expeditions from 1922 to 1930. [1] Apparently, in the original description a left pes was claimed to be part of the holotype, [1] however, this statement has not been mentioned again. [2] [3] [4] [5]

Skull and right pes of the holotype Erlikosaurus skull and foot.jpg
Skull and right pes of the holotype

Confusingly, in 1981 Perle again named and described the species as if it were new, but this time in more detail and spelling the generic name as a Latinised "Erlicosaurus". [2] It is today widely accepted by most authors that the original name, Erlikosaurus, is valid. At the time of its discovery it was the only known therizinosaur (then called segnosaurs [6] ) for which a complete skull had been discovered, this helped shed light on a puzzling and poorly known group of dinosaurs. It still represents the most completely known therizinosaurian skull. [4] [5]

In 2010, Gregory S. Paul challenged the validity of this taxon, arguing that Erlikosaurus may be synonymous with Enigmosaurus (named in 1983 [7] ), since the remains of the latter were found in the same geologic formation, and only known from pelvic remains, whereas the pelvis in Erlikosaurus is unknown; this would make Enigmosaurus a junior synonym of Erlikosaurus. [8] However, since the holotype hip of Enigmosaurus did not closely resemble that of the specimen in Segnosaurus as would be expected for the Segnosaurus-like remains of Erlikosaurus, and there is a considerable size difference, paleontologist Rinchen Barsbold disputed the alleged synonymy. [9] Additional to this, the remains of Erlikosaurus and Enigmosaurus are known from upper and lower boundary, respectively. [3] [7] [10] Consequently, Enigmosaurus and Erlikosaurus are generally considered separated genera. [11]

Description

Life restoration Erlikosaurus Restoration.png
Life restoration

As the genus is only known from very fragmentary material, it has been problematic to determine the size of Erlikosaurus, especially as most of the vertebral column of the holotype is missing. The skull of the holotype specimen length is approximately 25 cm (250 mm) long, indicating a very small individual. Overall, Erlikosaurus was a small-sized therizinosaurid, estimated to have reach about 3.4 m (11 ft) with a more lightly built than the ponderous Segnosaurus . [12] In 2012 Stephan Lautenschlager and colleagues used theropod-specific equations to estimate the body mass of Erlikosaurus and other therizinosaurs. However, since the femur is unknown, they used bivariate regression analyses on log-transformed data for Erlikosaurus. The results ended up on a femoral length of 44.33 cm (443.3 mm) and a weight of 173.7 kg (383 lb). Given the uncertainties of these estimates, they established an overall mass range between 150 and 250 kg (330 and 550 lb). [5] Alternative estimations have suggested a maximum length of 6 m (20 ft) long, [9] and a more conservative length of 4.5 metres and a weight of 500 kg (1,100 lb). [13] Though Erlikosaurus largely lacks body remains, as a therizinosaurid it would have had a strong arm build with large claws, a broad and bulky torso, and an opisthopubic (directed backwards) pelvis. [14] It is known that therizinosaurs were feathered animals based on the preserved feather impressions in specimens of Beipiaosaurus and Jianchangosaurus , so it is likely that Erlikosaurus was feathered as well. [15] [16]

Skull

Erlikosaurus and Halszkaraptor skull (cropped).png
Reconstructed skull of the holotype in lateral (A) and dorsal (C) views
Erlikosaurus right and left hemimandibles.png
Holotype right (A) and left (B-C) hemimandibles

The snout is moderately elongated, with a premaxilla featuring elongated nasal processes. A fine, vertical lamina of bone is connected rostrally to the medial margin of the premaxilla, indicating that when the animal was alive, a cartilaginous internasal septum was present. Additional to this, the premaxilla features lateral and medial foramina that are connected by a complex system of vascular canals, which pervades the structure of the premaxilla and is probably associated with the sensory branches of the neurovasculature and ophthalmic nerve supporting the rhamphotheca (beak). The maxilla is triangular in shape and preserves 24 alveoli, the teeth are homodont with coarse serrations. The dentary is wedge-shaped elongated and preserves 31 alveoli. In a dorsal view, it is U-shaped and flattened at the back with an expansion lying across. The lateral and ventral surfaces in the symphyseal region bears a series of foramina that measure 2 to 5 mm (0.20 to 0.50 cm) in diameter. Isolated foramina are connected internally by a complex neurovascular canal. When restored, the skull measures 26 cm (260 mm) long and the mandible is about 24 cm (240 mm). [17]

The well preserved braincase is very much complete, only missing the sphenethmoid-mesethmoid complex, whereas the laterosphenoids and orbitosphenoids are incompletely preserved in medial view. The bones around the braincase are strongly coossified, but the sutures between individual elements are not visible superficially, except for a few areas. [3] However, these internal sutures can be traced in CT scans and therefore, braincase elements could be differentiated one from other. [17] The restored brain of the specimen is somewhat elongated. The olfactory apparatus and the cerebral hemispheres are very notorious, with the olfactory tract being far larger than the actual brain. The cerebral hemispheres are large and broad. On the cerebral surface complex vascular grooves can be found, which are typically found in birds and mammals, as well as other dinosaurs. Lastly, the cerebellum is not very notorious as previous elements, it is elongated and stocky. [5]

Teeth from the dentary bone Dentary teeth of Erlikosaurus.png
Teeth from the dentary bone

Keratinous beaks, or rhamphothecae, are well documented among diverse groups within the Dinosauria. [17] Ornithomimosaurs have solid evidence for it. [18] [19] However, this is not an indicative to suggest the lack of this anatomical feature in other groups. Several characteristics are indicative of a rhamphothecae, such as an edentulous premaxilla with a thin, tapering lower edge, the successive loss of maxillary and dentary teeth, a mandibular concavity in the lower side, the displacement of the lower surface in the dentary, and a rostral projection of the mandibular symphysis. [17]

In Erlikosaurus, the presence of a keratinous beak on the maxilla and premaxilla can be inferred by the presence of numerous neurovascular foramina on the rostral and lateral surfaces in the skull, furthermore, it bears all the mentioned features above, however, it is unclear the extension of the beak. [17] The preserved rhamphotheca in specimens of Gallimimus and Ornithomimus evidences that the keratin sheath covered the premaxilla and overlapped it on the lower side by a few millimeters. [18] In some extant birds, the rhamphotheca is typically restricted to the premaxilla and maxilla, although in some cases it partially covers the nasal process in some birds. [20] Apparently, in Erlikosaurus the rhamphotheca covered the nasal process of the premaxilla. [17]

Postcranial skeleton

Holotype right foot of Erlikosaurus with unguals removed Erlikosaurus foot (cropped).png
Holotype right foot of Erlikosaurus with unguals removed

Body remains of Erlikosaurus are very sparse compared to the cranial elements, consisting of a humerus, a right foot and some cervical vertebrae. The particular cervicals were not figured and counted but briefly described. The cervicals are platycoelus (slightly concave at both ends) with low neural arches. [1] Being relatively robust, they have thick prezygapophyses and large parapophyses. Additional, the cervicals show some resemblance to those of Segnosaurus, however, being much smaller. [2]

The preserved right pes is virtually complete, only missing the proximal end of the metatarsals II, III and IV. It is shortened in length, with robust metatarsals that bear widened articular extremities, and form a non-compact metatarsus. The metatarsal I is the shortest in comparison, it measures 7 cm (70 mm) long and expands the laterally extended proximal articular surface of the metatarsus. All of the remaining metatarsals, are somewhat equal in size, metatarsal II covers 11 cm (110 mm) in length. The pedal digits are very peculiar in structure; the first digit is reduced in length, with all the remaining digits being nearly equal in length, however the fourth digit is very thin compared to the others. The phalanges of the three first digits are shortened, robust with comparable structure. The second and third phalanx of fourth digit are discoidal and stocky. Lastly, the unguals are recurved, exceptionally large, and strongly flattened laterally. [1] [2] Gregory S. Paul surmised that the long, slender claws of the feet were used for self-defence mechanism. [13]

The left humerus is the only preserved remain from the pectoral region. The humerus shows an elongated epiphyses and a relatively large deltoideal process. [1] It is robust with an estimated length of 30 cm (300 mm). It has a reduced shaft. The proximal end of the humeurs is greatly broad. The humeral head features an articular surface that is convex and broad, in the middle it is reduced toward the margins. A prominent deltopectoral crest is present with the top located 1/3 at the length of the humerus from the proximal end. The articulation condyles for the radius and ulna are differentiated and divided by a shortened, furrow-like fossa and overall, they are very reduced in size. The fossa for the ulnar process is moderately deep and wide. The internal roughness of the head is prominent, [2] as in the unrelated Dromaeosauridae. [21]

Classification

Outdated quadrupedal, prosauropod-like restoration of Erlikosaurus Erlikosaurus.jpg
Outdated quadrupedal, prosauropod-like restoration of Erlikosaurus

Erlikosaurus was by Perle assigned to the Segnosauridae, [1] a group today known as the Therizinosauridae, confirmed by later cladistic analyses. [4] Therizinosaurs were a strange group of theropods that ate plants instead of meat, and had a backward-facing pubis, like ornithischians. Also like ornithischians, their jaws were tipped by a broad rounded bony beak useful for cropping off plants. [9] [4]

The relationships of therizinosaurs were quite complicated when the first members were discovered. As an example, the first known therizinosaur taxon, Therizinosaurus , was interpreted to represent turtle-like animals that used the elongated claws to feed on seaweed. [22] However, in 1970, Rozhdestvensky proposed the idea that therizinosaurs (then known as segnosaurs) instead of being non-dinosaur creatures, they were in fact, theropods. [23] Later, in 1980, segnosaurs were thought to be slow, semiaquatic animals, with this, Gregory S. Paul claimed that these controversial animals had no theropod characteristics and they were prosauropods with ornithischian adaptations, also, they shared evolutionary relationships. [24] However, with the description of more genera such as Alxasaurus , [25] Nanshiungosaurus , [26] and the redescription of the skull of Erlikosaurus, more theropod evidence began to be supported. [3] With the discovery and description of the feathered Beipiaosaurus , therizinosaurs were utterly recognized as theropods, and started to be reconstructed in an accurate, bipedal posture. [15]

Consequently, therizinosaurs are now classified as theropods, within the Coelurosauria. Lindsay Zanno was one of the first authors to examine in detail the relationships and affinites of therizinosaurs. Her work has been useful in many phylogenetic analyses. [4] The cladogram below is the result of the phylogenetic analysis performed by Hartman et al. 2019 using the data provided by Zanno in 2010. Erlikosaurus occupied a very derived position in a clade with the two Nothronychus species: [11]

Holotype skull of Erlikosaurus (below) and endocranial elements of other therizinosaurs Therizinosaur endocranial elements.png
Holotype skull of Erlikosaurus (below) and endocranial elements of other therizinosaurs
Therizinosauridae
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Suzhousaurus Suzhousaurus.JPG

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Neimongosaurus Neimongosaurus.jpg

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Therizinosaurus Therizinosaurus Restoration.png

Erliansaurus Erliansaurus bellamanus.jpg

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Nanchao embryos THERIZINOSAURUS.jpg

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Nanshiungosaurus Nanshiungosaurus Restoration.png

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Segnosaurus Segnosaurus Restoration.jpg

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Erlikosaurus Erlikosaurus Restoration.png

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Nothronychus graffami Nothronychus graffami Restoration.png

Nothronychus mckinleyi Nothronychus mckinleyi Restoration.png

Paleobiology

Senses

Reconstructed brain of Erlikosaurus Erlikosaurus cranial endocast.png
Reconstructed brain of Erlikosaurus

Erlikosaurus is poorly known from postcranial material, but the holotype skull became the focus of study in Computed Tomography (CT) scans that were published back in 2012 by the paleontologist Stephan Lautenschlager and Dr Emily Rayfield of Bristol University School of Earth Sciences, Professor Lindsay Zanno of the North Carolina Museum of Natural History and North Carolina State University, and Lawrence Witmer, Chang Professor of Paleontology at the Ohio University Heritage College of Osteopathic Medicine. Analysis of the brain cavity revealed that Erlikosaurus, and quite likely most other therizinosaurids, had well developed senses of smell, hearing, and balance, traits better associated with carnivorous theropods. The enlarged forebrain of Erlikosaurus may also have been useful in complex social behavior and predator evasion. These senses were also well-developed in earlier coelurosaurs and other theropods, indicating that therizinosaurs may have inherited many of these traits from their carnivorous ancestors and used them for their different and specialized dietary purposes. [5]

In 2019, Graham M. Hughes and John A. Finarelli analyzed the olfactory bulb ratio in modern birds and preserved skulls of several extinct dinosaur species to predict how many genes would have been involved in the olfactory strength of these extinct species. Their analysis found that Erlikosaurus had about 477 genes encoding its olfactory receptors and an olfactory bulb ratio of 40, indicating moderate senses of smell. The scores of Erlikosaurus were higher than most dromaeosaurids despite the herbivorous life-style in this taxon, and may reflect a transition to complex sociality and/or reduced visual capacities. Hughes and Finarelli pointed out that as dinosaurian lineages became larger, the size of the olfactory bulb increased, which may suggest olfaction as the main sensory modality in large-bodied non-avian dinosaurs. [27]

Feeding and bite force

Proposed feeding method by Lautenschlager: Erlikosaurus reaches vegetation (A) and then rips it off with its beak (B) Erlikosaurus feeding.png
Proposed feeding method by Lautenschlager: Erlikosaurus reaches vegetation (A) and then rips it off with its beak (B)

In 2013, Lautenschlager performed digital reconstructions for the cranial musculature in Erlikosaurus and found a relatively weak bite force compared to other theropods. As a whole, the adductor musculature of the jaws—which primarily function to close the jaws—generates a total force of 374 and 570 N but only a small portion is actually used when biting because the bite force starts to decline as the more the distance of the bite point is to the jaw joint. Lautenschlager found the lowest force at the snout tip with 43–65 N, and the highest at the last maxillar tooth region, with 90–134 N. Factors like the presence of a large gut to process vegetation and the lack of damage patterns on the teeth suggest that Erlikosaurus used only the tip of the snout and the premaxillary region to reach for soft foliage or fruits, and the lesser bite force for Erlikosaurus better served in leaf-stripping and plant-cropping feeding mechanism, rather than active mastication. In this study, Lautenschlager also suggested that Erlikosaurus may have been able to process mainly thin branches and plant matter based on Stegosaurus . Moreover, the comparably narrow width of the snout could indicate selective feeding in this therizinosaurid. Lastly, the branch‐stripping behaviour of Erlikosaurus may have been compensated by the postcranial musculature. [28] During the same year, Lautenschlager and team made digital models of the skull of Erlikosaurus to test the function the rhamphotheca (keratinous beak), finding that this structure in the jaws acted as a stress-mitigating structure. They concluded that keratinous beaks are beneficial to enhance the stability of the skull making it less susceptible to bending and/or deformation during feeding. [29]

Optimal and maximum jaw gapes of Allosaurus (A), Tyrannosaurus (B) and Erlikosaurus (C) Theropod jaw gape.jpg
Optimal and maximum jaw gapes of Allosaurus (A), Tyrannosaurus (B) and Erlikosaurus (C)

The well preserved jaws also allowed a study by the University of Bristol to determine how its feeding style and dietary preferences were linked to how wide they could open the mouth. In the study, performed by Lautenshlager and colleagues in 2015, it was revealed that Erlikosaurus could open its mouth to a 43 degree angle at maximum. Also included in the study for comparison were the carnivorous theropods Allosaurus and Tyrannosaurus . From the comparisons, it was indicated that carnivorous dinosaurs had wider jaw gapes than herbivores, much as modern carnivorous animals do today. [30]

In 2016, using Finite Element Analysis (FEA) and a Multibody Dynamics Analysis (MDA), the bite forces of Erlikosaurus, Plateosaurus and Stegosaurus were tested in order to estimate dietary habits. The resulting bite force for Erlikosaurus was between 50 and 121 N, with a skull characterised by high susceptibility to stress and deformation that indicates a feeding behaviour specialized in the active use of the beak. The results further support that Erlikosaurus relied on postcranial musculature to compensate the low bite force and to relieve stresses on cranial structure. [31]

Paleoenvironment

Erlikosaurus compared to the known Dinosauria of the Bayan Shireh Formation (Erlikosaurus in red, fourth from right) Bayan Shireh Formation Fauna.png
Erlikosaurus compared to the known Dinosauria of the Bayan Shireh Formation (Erlikosaurus in red, fourth from right)

The holotype of Erlikosaurus was unearthed from the Bayshin Tsav locality at the upper boundary of the Bayan Shireh Formation, in a quarry composed of gray sands with conglomerates, gravels, and gray claystones. Bayshi Tsav is thought to have been deposited by meandering rivers. [32] [3] [33] The examination of the magnetostratigraphy of the formation seems to confirm that the entire Bayan Shireh lies within the Cretaceous Long Normal, which lasted only until the end of the Santonian stage. Moreover, calcite U–Pb measurements estimate the age of the Bayan Shireh Formation from 95.9 ± 6.0 million to 89.6 ± 4.0 million years ago, Cenomanian through Santonian ages. [33] [34]

Fluvial, lacustrine and caliche-based sedimentation indicates a lesser semi-arid climate, with the presence of wet environments composed of large meanders and lakes. Largescale cross-stratification in many of the sandstone layers at the Bayn Shireh and Burkhant localities seems to indicate large meandering rivers, and these large water bodies may have drained the eastern part of the Gobi Desert. [35] [33] Numerous fossilized fruits have been recovered from the Bor Guvé and Khara Khutul localities. [36] A vast diversity of fauna is known in the formation, compromising dinosaur and non-dinosaur genera. Fellow theropods include the large Achillobator , [37] and the deinocheirid Garudimimus . [38] Other herbivorous dinosaurs are represented by the ankylosaurs Talarurus and Tsagantegia , [39] small marginocephalians Amtocephale and Graciliceratops , [40] [41] the hadrosauroid Gobihadros , [10] and the sauropod Erketu . [36] Other fauna include semiaquatic reptiles like crocodylomorphs and nanhsiungchelyid turtles. [42] [43]

Coexistence with Segnosaurus

Lower jaw of Erlikosaurus (bottom) and Segnosaurus (top) Erlikosaurus and Segnosaurus lower jaw.png
Lower jaw of Erlikosaurus (bottom) and Segnosaurus (top)

Erlikosaurus lived alongside a larger species of therizinosaurid in the Bayan Shireh Formation, Segnosaurus . In 2016, Zanno and colleagues re-examined the lower jaws and dentition of Segnosaurus making direct comparisons with those of Erlikosaurus in the process. They identified rather complex features in the dentary teeth of Segnosaurus, which are represented by the presence of numerous carinae (cutting edges) and folded carinae with denticulated front edges, and the enlargement of denticles (serrations). These traits together create a roughened, shredding surface near the base of the tooth crowns that was unique to Segnosaurus and suggest it consumed unique food resources or used highly specialized feeding strategies, with the addition of a higher degree of oral food processing than the sympatric—related species that lived in the same area at the same time—Erlikosaurus. On the contrary, the latter has very symmetrical teeth with moderate denticles. The respective indistinct and specialized dentition of Erlikosaurus and Segnosaurus indicates that these two therizinosaurids were separated by niche differentiation in food acquisition, processing, or resources. This conclusion is strengthened by the large difference in estimated body masses, which is up to 500%. [44]

Life restoration of the larger and sympatric Segnosaurus Segnosaurus Restoration.jpg
Life restoration of the larger and sympatric Segnosaurus

In a 2017 study of niche partitioning in therizinosaurs through digital simulations, Lautenschlager found the straighter and more elongated dentaries of primitive therizinosaurs had the highest magnitudes of stress and strain during extrinsic feeding scenarios. In contrast, Erlikosaurus and Segnosaurus were aided by the down-turned tip of the lower jaws and symphyseal (bone union) regions, and probably also by stress and strain-mitigating beaks. The results also showed a difference in bite forces between Segnosaurus and Erlikosaurus, indicating the former would have been able to feed on tougher vegetation, while the overall robustness of the latter suggests greater flexibility in its manner of feeding. Lautenschlager pointed out the two taxa were adapted to different modes food acquisition, and that the difference in size and heights between the two therizinosaurids further separated their niches. While Segnosaurus was adapted to use its specialized dentition to procure or process food, Erlikosaurus mostly relied on its beak and neck musculature for cropping while foraging. [45]

In addition to these cranial differences, in 2019 Button and Zanno note that herbivorous dinosaurs followed two main distinct modes of feeding. One of these was processing food in the gut which is characterized by gracile skulls and relatively low bite forces, and the second was oral food processing, characterized by features associated with extensive processing such as the lower jaws or dentition. Segnosaurus was found to be in the former mode, whereas Erlikosaurus was more likely to fall in the second group, further supporting that these two therizinosaurids were separated by a well-defined niche differentiation. [46]

See also

Related Research Articles

<i>Segnosaurus</i> Extinct genus of therizinosaurid dinosaur from late Cretaceous

Segnosaurus is a genus of therizinosaurid dinosaur that lived in what is now southeastern Mongolia during the Late Cretaceous, about 102–86 million years ago. Multiple incomplete but well-preserved specimens were discovered in the Gobi Desert in the 1970s, and in 1979 the genus and species Segnosaurus galbinensis were named. The generic name Segnosaurus means "slow lizard" and the specific name galbinensis refers to the Galbin region. The known material of this dinosaur includes the lower jaw, neck and tail vertebrae, the pelvis, shoulder girdle, and limb bones. Parts of the specimens have gone missing or become damaged since they were collected.

<i>Therizinosaurus</i> Therizinosaurid genus from the Late Cretaceous period

Therizinosaurus is a genus of very large therizinosaurid that lived in Asia during the Late Cretaceous period in what is now the Nemegt Formation around 70 million years ago. It contains a single species, Therizinosaurus cheloniformis. The first remains of Therizinosaurus were found in 1948 by a Mongolian field expedition at the Gobi Desert and later described by Evgeny Maleev in 1954. The genus is only known from a few bones, including gigantic manual unguals, from which it gets its name, and additional findings comprising fore and hindlimb elements that were discovered from the 1960s through the 1980s.

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

Beipiaosaurus is a genus of therizinosauroid theropod dinosaurs that lived in Asia during the Early Cretaceous in the Yixian Formation. The first remains were found in 1996 and formally described in 1999. Before the discovery of Yutyrannus, Beipiaosaurus were among the heaviest dinosaurs known from direct evidence to be feathered. Beipiaosaurus is known from three reported specimens. Numerous impressions of feather structures were preserved that allowed researchers to determine the feathering color which turned out to be brownish.

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

Therizinosaurs were large herbivorous theropod dinosaurs whose fossils have been found across the Middle Jurassic to Late Cretaceous deposits in Europe, Asia and North America. Various features of the forelimbs, skull and pelvis unite these finds as both theropods and maniraptorans, making them relatives of birds. The name of the representative genus, Therizinosaurus, is derived from the Greek θερίζω and σαῦρος. The older representative, Segnosaurus, is derived from the Latin sēgnis ('slow') and the Greek σαῦρος.

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

Nothronychus is a genus of therizinosaurid theropod dinosaurs that lived in North America during the Late Cretaceous period. The type species, Nothronychus mckinleyi, was described by James Kirkland and Douglas G. Wolfe in 2001. It was recovered near New Mexico's border with Arizona, in an area known as the Zuni Basin, from rocks assigned to the Moreno Hill Formation, dating to the late Cretaceous period, around 92 million years ago. A second specimen, described in 2009 as a second species, Nothronychus graffami, was found in the Tropic Shale of Utah, dating to the early Turonian, between one million and a half million years older than N. mckinleyi.

<i>Deinocheirus</i> Genus of theropod dinosaurs

Deinocheirus is a genus of large ornithomimosaur that lived during the Late Cretaceous around 70 million years ago. In 1965, a pair of large arms, shoulder girdles, and a few other bones of a new dinosaur were first discovered in the Nemegt Formation of Mongolia. In 1970, this specimen became the holotype of the only species within the genus, Deinocheirus mirificus; the genus name is Greek for "horrible hand". No further remains were discovered for almost fifty years, and its nature remained a mystery. Two more complete specimens were described in 2014, which shed light on many aspects of the animal. Parts of these new specimens had been looted from Mongolia some years before, but were repatriated in 2014.

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

Enigmosaurus is a genus of therizinosauroid that lived in Asia during the Late Cretaceous period. It was a medium-sized, ground-dwelling, bipedal herbivore that represents the third therizinosaur taxon from the Bayan Shireh Formation, although it is known from the lower part. The genus is monotypic, including only the type species E. mongoliensis, known from a well preserved pelvis and other tentative body remains.

<i>Garudimimus</i> Ornithomimosaur genus from the Late Cretaceous

Garudimimus is a genus of ornithomimosaur that lived in Asia during the Late Cretaceous. The genus is known from a single specimen found in 1981 by a Soviet-Mongolian paleontological expedition in the Bayan Shireh Formation and formally described in the same year by Rinchen Barsbold; the only species is Garudimimus brevipes. Several interpretations about the anatomical traits of Garudimimus were made in posterior examinations of the specimen, but most of them were criticized during its comprehensive redescription in 2005. Extensive undescribed ornithomimosaur remains at the type locality of Garudimimus may represent additional specimens of the genus.

<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>Alxasaurus</i> Therizinosauroid dinosaur genus from the Early Cretaceous

Alxasaurus is a genus of therizinosauroid theropod dinosaurs from the Early Cretaceous Bayin-Gobi Formation of Inner Mongolia.

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

Harpymimus is a basal ornithomimosaurian theropod dinosaur from the Early Cretaceous Period of what is now Mongolia. Unlike later, more derived ornithomimosaurs, Harpymimus still possessed teeth, although they appear to have been restricted to the dentary of the lower jaw.

<span class="mw-page-title-main">Therizinosauridae</span> Extinct family of dinosaurs

Therizinosauridae is a family of derived (advanced) therizinosauroid dinosaurs whose fossil remains have been found in mostly Late Cretaceous boundary. Even though representative fossils have only been found throughout Asia and North America, the range of Therizinosauridae is believed to have spanned much of the supercontinent of Laurasia based on several footprints and isolated remains in Europe and Africa. Currently, Therizinosauridae comprises eight described and named taxa.

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

The Bayan Shireh Formation is a geological formation in Mongolia, that dates to the Cretaceous period. It was first described and established by Vasiliev et al. 1959.

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

Tsagantegia is a genus of medium-sized ankylosaurid thyreophoran dinosaur that lived in Asia during the Late Cretaceous period. The genus is monotypic, including only the type species, T. longicranialis. The specimen consists of a very partial individual, comprising the skull and lacking postcranial remains. Since it only preserves the skull, Tsagantegia is mainly characterized by its elongated snout and the flattened facial osteoderms, greatly differing from other ankylosaurs.

<i>Talarurus</i> Ankylosaurid dinosaur genus from the Late Cretaceous

Talarurus is a genus of ankylosaurid dinosaur that lived in Asia during the Late Cretaceous period, about 96 million to 89 million years ago. The first remains of Talarurus were discovered in 1948 and later described by the Russian paleontologist Evgeny Maleev with the type species T. plicatospineus. It is known from multiple yet sparse specimens, making it one of the most well known ankylosaurines, along with Pinacosaurus. Elements from the specimens consists of various bones from the body; five skulls have been discovered and assigned to the genus, although the first two were very fragmented.

<i>Erketu</i> Sauropod genus from the Late Cretaceous

Erketu is a genus of somphospondylan sauropod dinosaur that lived in Asia during the Late Cretaceous roughly between 96 million and 89 million years ago. Its fossils were found in Mongolia between 2002 and 2003 during a field expedition and first described in 2006; later on in 2010 due to some cervicals that were left behind in the expedition. Erketu represents one of the first sauropods described from the Bayan Shireh Formation. The elongated cervical vertebrae of Erketu indicates that it was the sauropod with the longest neck relative to its body size.

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

Neimongosaurus is a genus of herbivorous therizinosaur theropod dinosaur that lived in Asia during the Cenomanian stage of the Late Cretaceous period in what is now the Iren Dabasu Formation.

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

Nanshiungosaurus is a genus of therizinosaurid that lived in what is now Asia during the Late Cretaceous of South China. The type species, Nanshiungosaurus brevispinus, was first discovered in 1974 and described in 1979 by Dong Zhiming. It is represented by a single specimen preserving most of the cervical and dorsal vertebrae with the pelvis. A supposed and unlikely second species, "Nanshiungosaurus" bohlini, was found in 1992 and described in 1997. It is also represented by vertebrae but this species however, differs in geological age and lacks authentic characteristics compared to the type, making its affinity to the genus unsupported.

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

Suzhousaurus is a genus of large therizinosauroid dinosaur from the Early Cretaceous of China. The genus is known from two specimens discovered on the Xiagou Formation and Zhonggou Formation—which are situated in the Xinminbao Group. These findings were made during field-works in 1999 and 2004. Though Suzhousaurus is known from these two specimens, an earlier named and described therizinosauroid from the adjacent basin, "Nanshiungosaurus" bohlini, may be synonymous with the former. However, Suzhousaurus can not be compared to this species due to non-overlapping material and the loss of the same. Moreover, this synonymy will result in Suzhousaurus bohlini with "N". bohlini having priority.

<span class="mw-page-title-main">Timeline of therizinosaur research</span>

The timeline of therizinosaur research is a chronological listing of events in the history of paleontology focused on therizinosaurs. They were unusually long-necked, pot-bellied, and large-clawed herbivorous theropods most closely related to birds. The early history of therizinosaur research occurred in three phases. The first phase was the discovery of scanty and puzzling fossils in Asia by the Central Asiatic Expeditions of the 1920s and Soviet-backed research in the 1950s. This phase resulted in the discovery of the Therizinosaurus cheloniformis type specimen. Soviet paleontologist Evgeny Maleev interpreted these unusual remains as belonging to some kind of gigantic turtle.

References

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