Zuul Temporal range: Campanian ~ | |
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Reconstructed skeleton | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Clade: | Dinosauria |
Clade: | † Ornithischia |
Clade: | † Thyreophora |
Suborder: | † Ankylosauria |
Family: | † Ankylosauridae |
Subfamily: | † Ankylosaurinae |
Tribe: | † Ankylosaurini |
Genus: | † Zuul Arbour & Evans, 2017 |
Species: | †Z. crurivastator |
Binomial name | |
†Zuul crurivastator Arbour & Evans, 2017 | |
Zuul is a genus of herbivorous ankylosaurine dinosaur from the Campanian Judith River Formation of Montana. The type species is Zuul crurivastator. It is known from a complete skull and tail, which represents the first ankylosaurin known from a complete skull and tail club, as well as the most complete ankylosaurid specimen thus far recovered from North America. The specimen also preserved in situ osteoderms, keratin, and skin remains.
In 2014, Theropoda Expeditions LLC was excavating a possible Gorgosaurus specimen near Havre, Montana. On 16 May, a skid-steer loader removing a 12 m (39 ft)-high overburden unexpectedly hit upon an ankylosaurian tail club. An almost complete ankylosaur skeleton proved to be present. As it had not been eroded on the surface, it was in pristine condition. It was found overturned, with the stomach facing upwards. The skeleton was largely articulated, but the skull and some neck vertebrae were separated from the main torso, while five ribs and the left ilium had shifted from their original position. The company secured the specimen in two main blocks, the largest of which weighed over 15 tonnes (17 tons). [1]
Initially identified as a new species of Euoplocephalus , the scientific importance of the specimen was immediately recognised. After preparation of the skull and tail section, Theropoda Expeditions offered it for sale. The company nicknamed the specimen "Sherman". In June 2016, it was acquired by the Canadian Royal Ontario Museum. The museum performed a laser scan of the skull, allowing its original form to be determined by the process of retro-deformation, or compensating for compression of the fossil. In 2017, before the torso had been prepared, a preliminary description was published of the skull and tail. [1]
In 2017, based on the specimen the type species Zuul crurivastator was named and described by Arbour and Evans. The generic name was adopted from the demon and demi-god Zuul, the Gatekeeper of Gozer, featured in the 1984 film Ghostbusters . This was due to Zuul's head resembling that of an ankylosaur. The specific name is derived from Latin crus, "shank", and vastator, "destroyer". The epithet, read as "Destroyer of Shins" by the naming authors, [2] refers to a presumed defensive tactic of ankylosaurids, smashing the lower legs of attacking predatory theropods with their tail clubs. [1] [3]
The specimen, which is stored as ROM 75860, was found in a sandstone layer of the Judith River Formation, part of the middle Coal Ridge Member with an age of between 76.2 and 75.2 million years. According to Theropoda Expeditions, it was 99% complete. It was described as a "dinosaur mummy", due to its preservation of soft tissues. Many osteoderms and small ossicles of the armour are present in their original position. Additionally, there are remains of keratin sheaths of the spikes and of keratin, non-bony, scales, in the form of a black film. The specimen is, as of 2017, the most complete ankylosaur find from the Judith River Formation. It was also the first North American ankylosaur specimen with well-preserved material from both the skull and tail. [1]
Zuul is estimated to have been 6 metres (20 ft) long. [4] The describing authors of Zuul, Victoria Arbour and David Evans, noted some distinguishing traits of Zuul. Some of these were autapomorphies, unique characters which set Zuul apart from all other known ankylosaurids. The caputegulae, armour tiles of the head, that lay on the nasal bones, the frontals and the parietals, are imbricated, overlapping, and pointed on top. The squamosal horns, on the rear corners of the skull roof, have conspicuous longitudinal grooves on their side surfaces. The osteoderms on the side of the tail, the knob itself excepted, have a front edge with a strongly hollow profile, while their points are off-set to the rear. The tail knob is vertically flattened with a height less than a fifth of the length. [1]
Other traits were not unique but distinguished Zuul from various relatives in the Ankylosaurinae. The caputegulae on the prefrontals, the frontoparietals and the middle supraorbitals are pyramid-shaped, in contrast to the conical caputegulae with Nodocephalosaurus and Talarurus . The squamosal horn protrudes to behind the rear edge of the skull roof, just as with Scolosaurus but different from Anodontosaurus , Euoplocephalus or Ziapelta . The caputegulae behind the eye socket are small and sparsely distributed, again like Scolosaurus but differing from Anodontosaurus, Euoplocephalus or Ziapelta. The osteoderms on the handle of the tail club are relatively larger and more pointed than those of Asian ankylosaurines of the Nemegt Formation of Mongolia. [1]
With a length of about 50 centimetres (20 in), the skull of Zuul is of considerable size, being only surpassed among the ankylosaurs of Laramidia (western North America) by the three known skulls of Ankylosaurus , specimens AMNH 5214, AMNH 5895 and CMN 8880. The skull is also rather flat but this is partly caused by compression. The snout is wide and truncated at the front. The bony nostrils are pointing to the front. In each nostril only a single nasal opening is visible, perhaps homologous to "Aperture A" in related species. [1]
Behind a narrow pair of nasal armour plates, rows of caputegulae stretch to the rear. The two front rows consists of pairs of rectangular plates. Part of the third row is a small central hexagonal caputegula. More to the back, the osteoderms all become square or hexagonal in profile and more strongly imbricating. Above the eye socket the front and rear supraorbitals form a sharp edge, protruding sideways. Deep in each eye socket, a bony plate is present. Similar plates in specimens of Euoplocephalus and Dyoplosaurus were reported by Walter Preston Coombs as bony eyelids. The squamosal horns on the rear corners of the skull roof are robust and pyramidal in shape. They have a sharp keel on top and deep grooves running towards the tip. The quadratojugal horns on the lower cheeks are also robust, with a convex front edge and a straight rear edge. They were seen as being mainly outgrowths of the quadratojugal bones themselves. [1]
The lower jaw is long and low. At its rear side, a large armour plate is present. According to Arbour and Evans, this is not a fused osteoderm, but instead an outgrowth of the jaw bones themselves. The adductor fossa, the opening through which the muscles closing the jaw entered its hollow inside, is relatively small and shallow. The dentary, the bone bearing the teeth, at the front curves sharply to the inside. This way both dentaries together had a profile fitting in the broad snout. The tooth row has a length of about 16 centimetres (6.3 in). [1]
At the rear underside of the right lower jaw numerous ossicles, small bony scales, are visible. The largest of these are rectangular and up to 14 mm (0.55 in) high. They lie directly below the large armour plate. Even lower, rows of smaller hexagonal or diamond-shaped ossicles are positioned, of about 6 mm (0.24 in) in diameter, grouped in rosettes. [1]
The teeth are placed in tooth rows which together have a fluted profile. The tooth rows of the upper jaws bear about eighteen to twenty teeth. Those of the lower jaws bear twenty-eight teeth. The teeth are small, leaf-shaped and transversely flattened. The front teeth of the dentary have a base width, measured from the front to the rear, of about 6 mm (0.24 in). Their crown height is about 7 mm (0.28 in). The teeth have in total twelve to fourteen cusps on their edges. The cusp forming the tip of the tooth is off-set to behind. Around the neck of the crown, a thickened cingulum, or shelf, is present. [1]
Of the remainder of the skeleton only the tail had been prepared in 2017. The tail has a total length of 278 centimetres (109 in). The tail is divided into "free" front caudal vertebrae of the base and a "tail club" at the rear. In the latter organ Coombs distinguished again a "handle" and a "knob". The tail club, including the handle, has a length of 210 centimetres (83 in), a record among North American ankylosaurids. [1]
In the handle, thirteen vertebrae are present. Probably another three are covered by the knob. To increase the chance of a damaging plastic deformation on impact of the knob, the handle is a stiff structure, the lack of flexibility caused by special connections between the vertebrae. The paired front joint processes, the prezygapophyses, are strongly elongated and overlap half of the preceding vertebra. They form a V-like structure, the branches angled at about 20°. Their joint facets are rotated to above and embrace the neural spine of the preceding vertebra. This spine is wedge-shaped and bent to behind with a flat top surface to fit into the V. This way a series of interlocking connections is formed, covering the entire top surface of the handle. The handle is further stiffened by bundles of ossified tendons, closely appressed to the vertebral sides. The tendons are over 50 centimetres (20 in) long and 5–8 mm (0.20–0.31 in) in diameter, with tapering ends. [1]
Along the sides of the handle runs a series of five pairs of osteoderms. Zuul is the first American ankylosaurid in which such handle osteoderms have actually been discovered; they had only been assumed for other species. On the free vertebrae of the tail base another three pairs are present. Between the large osteoderms smaller ossicles are positioned. The side tail osteoderms are flattened and have a triangular profile in top view, with a sharp point. Those more at the front have a sharper point, being longer than wide. They are almost shaped as an equilateral triangle with straight front and rear edges. More to behind the triangles are lower and wider. From the fifth pair onwards the front edges become longer and strongly concave, off-setting the point to the rear. The last pair, immediately before the knob, is strongly rounded. [1]
The front three side osteoderm pairs are covered by a black film that could be the remnant of their original keratin sheaths. If so, these added 1–2 centimetres (0.39–0.79 in) to their length. The sheaths show clear grooves and ridges directed towards the point. At the left osteoderm of the third pair, a layered structure is visible at its base, resembling the construction of horn bases in bovids. At the rear osteoderms, the film covering is incomplete, showing that the underlying bone structure does not conform to the sheath riles as it is much smoother. [1]
The knob is relatively large with a length of 52.5 centimetres (20.7 in), a width of 36.8 centimetres (14.5 in), and a vertical height of 8 centimetres (3.1 in). The bulk of the knob is formed by a pair of large osteoderms, each positioned at the side. In the holotype individual, the left side osteoderm is distinctively longer than the right one, giving the knob as whole a rather asymmetrical profile. This osteoderm also overlaps the last left triangular spike. The general profile of the knob is oval as spikes or keels are lacking. The side osteoderms almost touch each other at the top surface; at the underside a midline hiatus is present. At the rear of the knob, a cluster of small osteoderms is positioned. The outer corners of this cluster are formed by two trapezium-shaped elements. The very rear is formed by a covering triangular midline osteoderm. As a whole, the rear cluster has a straight posterior edge in top view. The bone tissue of the knob has a sponge-like texture with many pits. [1]
Apart from these bony structures, the tail also preserves non-bony scales. These are not skin impressions but remains of the keratin skin tissue itself. Such fossil scale remains are exceedingly rare. In between the third pair of tail osteoderms a transverse row of five large scales is present. Behind it a further row is visible, running more to below, and containing two scales. The scales are relatively large with a diameter of between 5–6.5 centimetres (2.0–2.6 in). In cross-section, they have the form of a truncated cone with a rounded top pointing somewhat to behind. More dispersed scales are visible at the base of the fourth osteoderm pair and the front base of the fifth pair. [1]
In 2017, Arbour and Evans placed Zuul within the Ankylosauridae, based on a phylogenetic analysis. More specifically, they identified it as an ankylosaurin ankylosaurine ankylosaurid, forming a clade with Ankylosaurus , Anodontosaurus, Dyoplosaurus and Scolosaurus. Although the consensus of the phylogenetic trees recovered by the analysis was inconclusive regarding the interrelationships of ankylosaurins, this was influenced mainly by the relative placements of Anodontosaurus and Ziapelta within the tree. Out of the ten most parsimonious trees they recovered, nine of them have Zuul as the sister group of Dyoplosaurus, while in the remaining tree Zuul is closer to Anodontosaurus. The consensus of 50% of the trees is reproduced below for ankylosaurin interrelationships; the remainder follows the full consensus of all of the trees. [1]
Ankylosaurinae |
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Ankylosaurus is a genus of armored dinosaur. Its fossils have been found in geological formations dating to the very end of the Cretaceous Period, about 68–66 million years ago, in western North America, making it among the last of the non-avian dinosaurs. It was named by Barnum Brown in 1908; it is monotypic, containing only A. magniventris. The generic name means "fused" or "bent lizard", and the specific name means "great belly". A handful of specimens have been excavated to date, but a complete skeleton has not been discovered. Though other members of Ankylosauria are represented by more extensive fossil material, Ankylosaurus is often considered the archetypal member of its group, despite having some unusual features.
Euoplocephalus is a genus of very large, herbivorous ankylosaurid dinosaurs, living during the Late Cretaceous of Canada. It has only one named species, Euoplocephalus tutus.
Pinacosaurus is a genus of ankylosaurid thyreophoran dinosaur that lived in Asia during the Late Cretaceous, mainly in Mongolia and China.
Saichania is a genus of herbivorous ankylosaurid dinosaur from the Late Cretaceous period of Mongolia and China.
Gastonia is a genus of herbivorous ankylosaurian dinosaur from the Early Cretaceous of North America, around 139 to 134.6 million years ago. It is often considered a nodosaurid closely related to Polacanthus. Gastonia has a sacral shield and large shoulder spikes.
Ankylosauridae is a family of armored dinosaurs within Ankylosauria, and is the sister group to Nodosauridae. The oldest known Ankylosaurids date to around 122 million years ago and went extinct 66 million years ago during the Cretaceous–Paleogene extinction event. These animals were mainly herbivorous and were obligate quadrupeds, with leaf-shaped teeth and robust, scute-covered bodies. Ankylosaurids possess a distinctly domed and short snout, wedge-shaped osteoderms on their skull, scutes along their torso, and a tail club.
Anodontosaurus is an extinct genus of ankylosaurid dinosaurs within the subfamily Ankylosaurinae. It is known from the entire span of the Late Cretaceous Horseshoe Canyon Formation of southern Alberta, Canada. It contains two species, A. lambei and A. inceptus.
Dyoplosaurus is a monospecific genus of ankylosaurid dinosaur from Alberta that lived during the Late Cretaceous in what is now the Dinosaur Park Formation. Dyoplosaurus represents a close relative of Scolosaurus and Anodontosaurus, two ankylosaurids known from the Horseshoe Canyon and Dinosaur Park Formation.
Mymoorapelta is a nodosaurid ankylosaur from the Late Jurassic Morrison Formation of western Colorado and central Utah, USA. The animal is known from a single species, Mymoorapelta maysi, and few specimens are known. The most complete specimen is the holotype individual from the Mygatt-Moore Quarry, which includes osteoderms, a partial skull, vertebrae, and other bones. It was initially described by James Kirkland and Kenneth Carpenter in 1994. Along with Gargoyleosaurus, it is one of the earliest known nodosaurids.
Tianzhenosaurus is a monospecific genus of ankylosaurid dinosaur from the Shanxi Province that lived during the Late Cretaceous in what is now the Huiquanpu Formation. Tianzhenosaurus may represent a junior synonym of Saichania, an ankylosaurine known from the Barun Goyot and Nemegt Formation.
Tarchia is a genus of herbivorous ankylosaurid dinosaur from the late Cretaceous of Mongolia.
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.
Nodocephalosaurus is a monospecific genus of ankylosaurid dinosaur from New Mexico that lived during the Late Cretaceous in what is now the De-na-zin member of the Kirtland Formation. The type and only species, Nodocephalosaurus kirtlandensis, is known only from a partial skull. It was named in 1999 by Robert M. Sullivan. Nodocephalosaurus has an estimated length of 4.5 metres and weight of 1.5 tonnes. It is closely related and shares similar cranial anatomy to Akainacephalus.
Zhongyuansaurus is a monospecific genus of ankylosaurid dinosaur from Henan that lived during the Early Cretaceous in what is now the Haoling Formation. Zhongyuansaurus is possibly a junior synonym of Gobisaurus, a basal ankylosaurid from the Ulansuhai Formation of Inner Mongolia.
Ahshislepelta is a monospecific genus of ankylosaur dinosaur from New Mexico that lived during the Late Cretaceous in what is now the Hunter Wash Member of the Kirtland Formation. The type and only species, Ahshislepelta minor, is known only from an incomplete postcranial skeleton of a small subadult or adult individual. It was named in 2011 by Michael Burns and Robert M. Sullivan. Based on the size of the humerus, Ahshislepelta is larger than Pinacosaurus mephistocephalus but smaller than Talarurus and Pinacosaurus grangeri.
Oohkotokia is a genus of ankylosaurid dinosaur within the subfamily Ankylosaurinae. It is known from the upper levels of the Two Medicine Formation of Montana, United States. The discovery of Oohkotokia supports that Ankylosaurine dinosaurs existed and flourished continuously in Montana and/or Alberta throughout the late Campanian and early Maastrichtian stages in the Late Cretaceous period. It was a large, heavily built, quadrupedal, herbivore, that could grow up to 5 metres (16 ft) long and weigh up to 2 metric tons.
Europelta is a monospecific genus of nodosaurid dinosaur from Spain that lived during the Early Cretaceous in what is now the lower Escucha Formation of the Teruel Province. The type and only species, Europelta carbonensis, is known from two associated partial skeletons, and represents the most complete ankylosaur known from Europe. Europelta was named in 2013 by James I. Kirkland and colleagues. Europelta has an estimated length of 5 metres and weight of 1.3 tonnes, making it the largest member of the clade Struthiosaurini.
Ziapelta is an extinct genus of ankylosaurid. Its fossils have been found in the Hunter Wash and De-na-zin members of the Kirtland Formation of Upper Cretaceous (Campanian) New Mexico. It was named in 2014, in a research paper led by ankylosaur researcher Victoria Arbour. There is a single species in the genus, Ziapelta sanjuanensis. The genus is named after the Zia sun symbol, a stylized sun with four groups of rays, having religious significance to the Zia people of New Mexico, and the iconic symbol on the state flag of New Mexico, and pelta (Latin), a small shield, in reference to the osteoderms found on all ankylosaurids. The specific name is in reference to San Juan County and the San Juan basin, where the fossils were found. Multiple specimens have been described to date, though the fossils are mostly from the front part of the animal. Its closest relative appears to be either Scolosaurus or Nodocephalosaurus, depending on what cladistic model is used.
Platypelta is an extinct genus of herbivorous ankylosaurid dinosaurs within the subfamily Ankylosaurinae. It is known from the Late Cretaceous Dinosaur Park Formation of southern Alberta, Canada. The type species is Platypelta coombsi.
Akainacephalus is a monospecific genus of ankylosaurid dinosaur from southern Utah that lived during the Late Cretaceous in what is now the Horse Mountain Gryposaur Quarry of the Kaiparowits Formation. The type and only species, Akainacephalus johnsoni, is known from the most complete ankylosaur specimen ever discovered from southern Laramidia, including a complete skull, tail club, a number of osteoderms, limb elements and part of its pelvis, among other remains. It was described in 2018 by Jelle P. Wiersma and Randall B. Irmis. It is closely related and shares similar cranial anatomy to Nodocephalosaurus.