Gastonia Temporal range: Early Cretaceous, | |
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Reconstructed skeleton of G. burgei, BYU Museum of Paleontology | |
Scientific classification | |
Domain: | Eukaryota |
Kingdom: | Animalia |
Phylum: | Chordata |
Clade: | Dinosauria |
Clade: | † Ornithischia |
Clade: | † Thyreophora |
Clade: | † Ankylosauria |
Family: | † Nodosauridae |
Subfamily: | † Polacanthinae |
Genus: | † Gastonia Kirkland, 1998 |
Type species | |
†Gastonia burgei Kirkland, 1998 | |
Species | |
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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.
The type specimen of Gastonia burgei (CEUM 1307) was discovered in a bonebed from the limestone strata of the lower Cedar Mountain Formation in Yellow Cat Quarry, Grand County, eastern Utah, the type specimen consisting of a single skull. [1] [2] The type specimen was found alongside 4 partial skeletons of Gastonia that were placed as paratypes, along with the type specimen of Utahraptor and an iguanodontid. [1] [2] Gastonia is among the most common dinosaur fossils in the Cedar Mountain Formation, with many individuals being found across several quarries in the southwest. [1] [2] In 2004, the number of skulls was reported as four, [3] in 2014 this had risen to ten. [4] Gastonia was formally named and described by James Kirkland in 1998, from the holotype specimen and other fossil material recovered beginning in 1989. [2] The name Gastonia honors US palaeontologist and CEO of Gaston Design Inc. Robert Gaston. The species G. burgei was named for the director of the College of Eastern Utah Prehistoric Museum, Donald L. Burge. [2]
Gastonia burgei, was found in rocks of the Cedar Mountain Formation's Yellow Cat Member, which has been dated to the Valanginian, 139 to 134.6 million years ago. [5]
A second species, G. lorriemcwhinneyae, was described from the Ruby Ranch Member in 2016 based on a large bonebed that had been found by Lorrie McWhinney in 1999, probably formed when a group died of drought or drowning. [1] The type specimen and its paratypes were collected by the Denver Museum of Nature and Science from Lorrie's Site in Grand County, Utah and belonged to the Ruby Ranch Member of the Cedar Mountain Formation. [1] The type specimen is incomplete, consisting only of a skull roof, though many additional elements are paratypes from many portions of the skeleton. [1]
All together, more complete material exists for Gastonia than for any other basal ankylosaur. [6] A wealth of disarticulated material from a bonebed presents problems as it can be hard to tell how many spikes a particular Gastonia actually had. [6]
In the late twentieth century a skeleton was mounted made of polyurethane casts of skeletal elements of various individuals. Distortions in the fossils were corrected and missing elements completed. This made Gastonia the first basal ankylosaurian dinosaur to have been mounted for display at the Denver Museum of Nature and Science, together with the related Gargoyleosaurus . [7]
Gastonia was a medium-sized ankylosaur. In 1998, Kirkland estimated its length at 6 metres. [2] In 2010, Gregory S. Paul indicated a body length of 5 metres and a weight of 1.9 tonnes. [8] The skeleton mount is 459 centimetres long with a hip height of 112 centimetres. [7]
It is difficult to determine distinguishing traits of Gastonia because its affinities are uncertain. However, in 1998 Kirkland established three characters which were unique for the Ankylosauria as a whole and thus likely autapomorphies, unique derived traits. On the midline of the front snout, the bony core of the upper horny beak, a broad, gradually curved, notch is present between the snout bones, the praemaxillae. The bony nostrils are placed far to the rear. At the underside of the braincase, the basisphenoid, the basipterygoid processes are longitudinally stretched. [2]
Gastonia had a flat and, even for an ankylosaurian, very broad rump, the belly strongly protruding between the short powerful limbs. The tail was moderately long and lacked a tail club. The neck was relatively long and the skull probably rather small.
The skull is somewhat elongated and pointy, measuring 295 by 283 millimetres in the holotype. The top profile of the skull is convex, the rear skull roof curving below the level of the upper rim of the eye sockets. The quadrate is very strongly inclined to the rear. The occipital condyle, the contact with the neck, is obliquely pointing to below, an ankylosaurid trait causing the head to be pointing downwards. The beak is toothless. The tooth rows of the maxillae are rather straight and each consist of fifteen to sixteen small teeth, lacking a true cingulum, swollen basis. There is no armour on the snout. More to behind, the bony tiles of the skull roof, the caputegulae, are rather indistinctively patterned though a small central plate on the parietal bones is visible. The squamosal horns, at the rear skull corners, and jugal horns, at the cheeks, are small. [2]
The sacrum consists of three sacral vertebrae, with a caudo-sacral vertebra behind them. Stiffened rear tail vertebrae or a tail club are absent. The shoulder blade resembles that of nodosaurids in possessing an acromion that is blade-like, but differs in the acromion originating from the front edge, not the outer side of the scapula, not being wrapped to behind and not ending in a knob. It is thus not a typical nodosaurid "pseudoacromion". The coracoid is square in form, a typical ankylosaurid trait. The humerus has a large deltopectoral crest extending downwards to the middle of the shaft, a derived trait. The ulna is very robust with an enormous olecranon. The shinbone is very expanded at both the upper and lower end. [2]
Gastonia was protected by osteoderms, skin ossifications. The neck was covered by at least two bone rings. Usually in ankylosaurs these have the form of "halfrings" leaving the underside unprotected, but with Gastonia only two segments seem present, one at each side of the midline, causing Kirkland to refer to them as "quarter rings". Each segment had a pointed keel and a hollow underside. Kirkland stressed that the rump armour was hard to reconstruct because it had not been found in articulation. The sides of the thorax seem to have been covered by about five pairs of large flat triangular spikes. They are recurved and have a deep groove in the rear side. They gradually decline in length to behind, the groove becoming relatively shorter and the base length increasing. According to Kirkland the function of the groove was to receive the front edge of the next spike. Other large flat spikes found, lacked the groove. They were often very curved, the point at a right angle with the base. Kirkland assumed these formed two vertical rows, one at each side of the rump midline. Lower triangular spikes he placed at the sides of the tail, again gradually decreasing to the rear. In between the horizontal and vertical spikes of the rump probably rows of osteoderms were present having the profile of a droplet, with a vertical point at the broader end. The top of the tail had oval plates. The hip region was covered by a large pelvic shield consisting of fused osteoderms. These were patterned as rosettes with a larger plate in the middle, surrounded by at least two rings of smaller plates. Kirkland assumed that four pairs of triangular spikes covered the sides of the pelvic shield also, [2] but this was denied by Paul. [8] The area between all these larger elements was covered by small ossicles, round bony scutes with a diameter of up to two centimetres, hundreds of which have been discovered. [2]
G. lorriemcwhinneyae differs from G. burgei in having a flat skull roof, shorter and narrower paroccipital processes, a postacetabular process that is only 36% the length of the preacetabular process, and an ischium that has an unkinked, smooth bottom edge. [1]
Kirkland in 1998 placed Gastonia in the Ankylosauridae, more precisely the Polacanthinae. Later, polacanthines were often seen as Nodosauridae. However, in 2014 an analysis by Victoria Arbour recovered Gastonia as a non-polacanthine basal member of the Ankylosauridae. [9]
A phylogenetic analysis conducted by Rivera-Sylva et al. (2018) and modified by Madzia et al. (2021) is reproduced below. [10] [11]
Nodosauridae |
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Gastonia lived in a partly wooded habitat, with riverine forests being separated by open areas. The climate was rather dry with a short wet season. [8] Other dinosaurs of the Yellow Cat include the ornithopods Hippodraco and Cedrorestes , the sauropods Cedarosaurus and Moabosaurus , and the theropods Martharaptor , Nedcolbertia , and Utahraptor . Gastonia was the only ankylosaurian present and one of the most common species of its fauna. [2]
Kirkland suggested that Gastonia could have been so abundant because its armour effectively protected it against the apex predator of its habitat, the giant dromaeosaurid Utahraptor, remains of which have been found in the original Gastonia quarry. Gastonia would have shown a typical polacanthine defence, which Kirkland understood to have consisted of a combination of passive protection offered by the vertical spikes and active protection by hitting a predator with the horizontal spikes of the flexible tail. The armour would also have served intraspecific antagonistic behaviour, i.e. fighting between males. The vertical spikes could have intimidated rivals and animals could have determined who was the strongest by ramming their heads together. Kirkland proposed that the typical ankylosaurid down-turned head, made possible by a more ventrally directed occipital condyle compared to nodosaurids, and an increased loosening of the rear skull elements to absorb shocks, were adaptations to this kind of behaviour. [2]
Ankylosaurs are often assumed to have been solitary living animals because their short legs seem poorly adapted to the trekking behaviour of herds, but the concentration of Gastonia fossils seems to contradict this. [3]
Ankylosauria is a group of herbivorous dinosaurs of the clade Ornithischia. It includes the great majority of dinosaurs with armor in the form of bony osteoderms, similar to turtles. Ankylosaurs were bulky quadrupeds, with short, powerful limbs. They are known to have first appeared in North Africa during the Middle Jurassic, and persisted until the end of the Late Cretaceous. The two main families of ankylosaurians, Nodosauridae and Ankylosauridae are primarily known from the Northern Hemisphere, but the more basal Parankylosauria are known from southern Gondwana during the Cretaceous.
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 large herbivorous ankylosaurid dinosaurs, living during the Late Cretaceous of Canada. It has only one named species, Euoplocephalus tutus.
Hylaeosaurus is a herbivorous ankylosaurian dinosaur that lived about 136 million years ago, in the late Valanginian stage of the early Cretaceous period of England. It was found in the Grinstead Clay Formation.
Animantarx is a genus of nodosaurid ankylosaurian dinosaur from the Early and Late Cretaceous of western North America. Like other nodosaurs, it would have been a slow-moving quadrupedal herbivore covered in heavy armor scutes, but without a tail club. The skull measures approximately 25 cm in length, suggesting the animal as a whole was no more than 3 meters long.
Edmontonia is a genus of panoplosaurin nodosaurid dinosaur from the Late Cretaceous Period. It is part of the Nodosauridae, a family within Ankylosauria. It is named after the Edmonton Formation, the unit of rock where it was found.
Pinacosaurus is a genus of ankylosaurid thyreophoran dinosaur that lived in Asia during the Late Cretaceous, mainly in Mongolia and China.
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.
Aletopelta is a monospecific genus of basal ankylosaurid dinosaur from Southern California that lived during the Late Cretaceous in what is now the Point Loma Formation. The type and only species, Aletopelta coombsi, is known from a partial skeleton preserving osteoderms. It was originally described in 1996 by W. P. Coombs, Jr. and T.A. Deméré before being named in 2001 by Tracy Ford and James Kirkland. Aletopelta has an estimated size of 5 metres and weight of 2 tonnes. The holotype formed a miniature reef and was scavenged upon by invertebrates and sharks.
Sauropelta is a genus of nodosaurid dinosaur that existed in the Early Cretaceous Period of North America. One species has been named although others may have existed. Anatomically, Sauropelta is one of the most well-understood nodosaurids, with fossilized remains recovered in the U.S. states of Wyoming, Montana, and possibly Utah. It is also the earliest known genus of nodosaurinae; most of its remains are found in a section of the Cloverly Formation dated to 108.5 million years ago.
Texasetes is a genus of ankylosaurian dinosaurs from the late Lower Cretaceous of North America. This poorly known genus has been recovered from the Paw Paw Formation near Haslet, Tarrant County, Texas, which has also produced the nodosaurid ankylosaur Pawpawsaurus.
Cedarpelta is an extinct genus of basal ankylosaurid dinosaur from Utah that lived during the Late Cretaceous period in what is now the Mussentuchit Member of the Cedar Mountain Formation. The type and only species, Cedarpelta bilbeyhallorum, is known from multiple specimens including partial skulls and postcranial material. It was named in 2001 by Kenneth Carpenter, James Kirkland, Don Burge, and John Bird. Cedarpelta has an estimated length of 7 metres and weight of 5 tonnes (11,023 lbs). The skull of Cedarpelta lacks extensive cranial ornamentation and is one of the only known ankylosaurs with individual skull bones that are not completely fused together.
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.
Tarchia is a genus of herbivorous ankylosaurid dinosaur from the late Cretaceous of Mongolia.
Antarctopelta is a genus of ankylosaurian dinosaur, a group of large, quadrupedal herbivores, that lived during the Maastrichtian stage of the Late Cretaceous period on what is now James Ross Island, Antarctica. Antarctopelta is the only known ankylosaur from Antarctica and a member of Parankylosauria. The only described specimen was found in 1986, the first dinosaur to be found on the continent, by Argentine geologists Eduardo Olivero and Robert Scasso. The fossils were later described in 2006 by paleontologists Leonardo Salgado and Zulma Gasparini, who named the type species A. oliveroi after Olivero.
Polacanthinae is a subfamily of ankylosaurs, most often nodosaurids, from the Late Jurassic through Early Cretaceous of Europe and potentially North America and Asia. The group is defined as the largest clade closer to Polacanthus foxii than Nodosaurus textilis or Ankylosaurus magniventris, as long as that group nests within either Nodosauridae or Ankylosauridae. If Polacanthus, and by extent Polacanthinae, falls outside either family-level clade, then the -inae suffix would be inappropriate, and the proper name for the group would be the informally defined Polacanthidae.
Peloroplites is a monospecific genus of nodosaurid dinosaur from Utah that lived during the Late Cretaceous in what is now the Mussentuchit Member of the Cedar Mountain Formation. The type and only species, Peloroplites cedrimontanus, is known from a partial skull and postcranial skeleton. It was named in 2008 by Kenneth Carpenter and colleagues. Peloroplites was 6 metres long and weighed 2 tonnes, making it one of the largest known nodosaurids, and came from a time when ankylosaurids and nodosaurids were attaining large sizes.
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.
This timeline of ankylosaur research is a chronological listing of events in the history of paleontology focused on the ankylosaurs, quadrupedal herbivorous dinosaurs who were protected by a covering bony plates and spikes and sometimes by a clubbed tail. Although formally trained scientists did not begin documenting ankylosaur fossils until the early 19th century, Native Americans had a long history of contact with these remains, which were generally interpreted through a mythological lens. The Delaware people have stories about smoking the bones of ancient monsters in a magic ritual to have wishes granted and ankylosaur fossils are among the local fossils that may have been used like this. The Native Americans of the modern southwestern United States tell stories about an armored monster named Yeitso that may have been influenced by local ankylosaur fossils. Likewise, ankylosaur remains are among the dinosaur bones found along the Red Deer River of Alberta, Canada where the Piegan people believe that the Grandfather of the Buffalo once lived.
Parankylosauria is a group of basal ankylosaurian dinosaurs known from the Cretaceous of South America, Antarctica, and Australia. It is thought the group split from other ankylosaurs during the mid-Jurassic period, despite this being unpreserved in the fossil record.
Media related to Gastonia (dinosaur) at Wikimedia Commons