|Skeletal mount of a T. prorsus specimen at the Natural History Museum of Los Angeles|
Triceratops is an extinct genus of herbivorous chasmosaurine ceratopsid dinosaur that first appeared during the late Maastrichtian stage of the Late Cretaceous period, about 68 million years ago in what is now North America. It is one of the last-known non-avian dinosaur genera, and became extinct in the Cretaceous–Paleogene extinction event 66 million years ago. The name Triceratops, which literally means 'three-horned face', is derived from the Greek words trí- (τρί-) meaning 'three', kéras (κέρας) meaning 'horn', and ṓps (ὤψ) meaning 'face'.
Bearing a large bony frill, three horns on the skull, and a large four-legged body, exhibiting convergent evolution with rhinoceroses and bovines, Triceratops is one of the most recognizable of all dinosaurs and the most well-known ceratopsid. It was also one of the largest, up to 9 meters (30 ft) long and 12 metric tons (13 short tons) in weight. It shared the landscape with and was possibly preyed upon by Tyrannosaurus, though it is less certain that two adults did battle in the fanciful manner often depicted in museum displays and popular images. The functions of the frills and three distinctive facial horns on its head have long inspired debate. Traditionally, these have been viewed as defensive weapons against predators. More recent interpretations find it probable that these features were primarily used in species identification, courtship, and dominance display, much like the antlers and horns of modern ungulates.
Triceratops was traditionally placed within the "short-frilled" ceratopsids, but modern cladistic studies show it to be a member of the Chasmosaurinae which usually have long frills. Two species, T. horridus and T. prorsus, are considered valid today, from the seventeen species that have ever been named. Research published in 2010 concluded that the contemporaneous Torosaurus, a ceratopsid long regarded as a separate genus, represents Triceratops in its mature form. This view has been disputed; further data is needed to settle the debate.
Triceratops has been documented by numerous remains collected since the genus was first described in 1889 by American paleontologist Othniel Charles Marsh. Specimens representing life stages from hatchling to adult have been found. As the archetypal ceratopsid, Triceratops is one of the most popular dinosaurs, and has been featured in film, postal stamps, and many other types of media.
Discovery and identification
The first named fossil specimen now attributed to Triceratops is a pair of brow horns attached to a skull roof, found by George Lyman Cannon near Denver, Colorado, in the spring of 1887. This specimen was sent to Marsh, who believed that the formation from which it came dated from the Pliocene, and that the bones belonged to a particularly large and unusual bison, which he named Bison alticornis. He realized that there were horned dinosaurs by the next year, which saw his publication of the genus Ceratops from fragmentary remains, but he still believed B. alticornis to be a Pliocene mammal. It took a third and much more complete skull to change his mind.
The Triceratops holotype (YPM 1820) was collected in 1888 from the Lance Formation of Wyoming, USA, by fossil hunter John Bell Hatcher, yet Marsh initially described this specimen as another species of Ceratops. Cowboy Edmund B. Wilson had been startled by the sight of a monstrous skull poking out of the side of a ravine. He tried to recover it by throwing a lasso around one of the horns. When it broke off, the skull tumbling to the bottom of the cleft, Wilson brought the horn to his boss, the rancher and avid fossil collector Charles Arthur Guernsey, who happened to show it to Hatcher. Marsh subsequently ordered Hatcher to locate and salvage the skull. The holotype was first named Ceratops horridus. When further preparation uncovered the third nose horn, Marsh changed his mind and gave the piece the generic name Triceratops (lit. 'three horn face'), accepting his Bison alticornis as another species of Ceratops. (It would later be added to Triceratops.) The sturdy nature of the animal's skull has ensured that many examples have been preserved as fossils, allowing variations between species and individuals to be studied. Triceratops remains have subsequently been found in the American states of Montana and South Dakota (and more in Colorado and Wyoming), as well as the Canadian provinces of Saskatchewan and Alberta.
An earlier specimen, also recovered from the Lance Formation, was named Agathaumas sylvestris by Edward Drinker Cope in 1872. Originally identified as a hadrosaur, this specimen consists only of post-cranial remains and is only provisionally considered an example of Triceratops.
After Triceratops was described, between 1889 and 1891 Hatcher with great effort collected another thirty-one of its skulls. The first species had been named T. horridus by Marsh. Its specific name was derived from the Latin horridus ('rough, rugose'), perhaps referring to the type specimen's rough texture, later identified as an aged individual. The additional skulls varied to a lesser or greater degree from the original holotype. This variation is unsurprising, given that Triceratops skulls are large three-dimensional objects, coming from individuals of different ages and both sexes, and which were subjected to different amounts and directions of pressure during fossilization.
In the first attempt to understand the many species, Richard Swann Lull found two groups, although he did not say how he distinguished them: One composed of T. horridus, T. prorsus, and T. brevicornus ('the short-horned'); the other of T. elatus and T. calicornis. Two species (T. serratus and T. flabellatus) stood apart from these groups. By 1933 and his revision of the landmark 1907 Hatcher–Marsh–Lull monograph of all known ceratopsians, he retained his two groups and two unaffiliated species, with a third lineage of T. obtusus and T. hatcheri ('Hatcher's') that was characterized by a very small nasal horn. T. horridus–T. prorsus–T. brevicornus was now thought to be the most conservative lineage, with an increase in skull size and a decrease in nasal horn size, and T. elatus–T. calicornis was defined by large brow horns and small nasal horn. C. M. Sternberg made one modification, adding T. eurycephalus ('the wide-headed') and suggesting that it linked the second and third lineages closer together than they were to the T. horridus lineage.
With time, the idea that the differing skulls might be representative of individual variation within one (or two) species gained popularity. In 1986, John Ostrom and Peter Wellnhofer published a paper in which they proposed that there was only one species, Triceratops horridus. Part of their rationale was that generally there are only one or two species of any large animal in a region. To their findings, Thomas Lehman added the old Lull–Sternberg lineages combined with maturity and sexual dimorphism, suggesting that the T. horridus–T. prorsus–T. brevicornus lineage was composed of females, the T. calicornis–T. elatus lineage was made up of males, and the T. obtusus–T. hatcheri lineage was of pathologic old males.
These findings were contested a few years later by Catherine Forster, who reanalyzed Triceratops material more comprehensively and concluded that the remains fell into two species, T. horridus and T. prorsus, although the distinctive skull of T. ("Nedoceratops") hatcheri differed enough to warrant a separate genus. She found that T. horridus and several other species belonged together, and T. prorsus and T. brevicornus stood alone. Since there were many more specimens in the first group, she suggested that this meant the two groups were two species. It is still possible to interpret the differences as representing a single species with sexual dimorphism.
In 2009, John Scannella and Denver Fowler supported the separation of T. prorsus and T. horridus and noted that the two species are also separated stratigraphically within the Hell Creek Formation, indicating that they did not live together at the same time.
Synonyms and doubtful species
Some of the following species are synonyms, as indicated in parentheses ("=T. horridus" or "=T. prorsus"). All the others are each considered a nomen dubium (lit. 'dubious name') because they are based on remains too poor or incomplete to be distinguished from pre-existing Triceratops species.
- T. albertensis C. M. Sternberg, 1949
- T. alticornis (Marsh 1887) Hatcher, Marsh, and Lull, 1907 [originally Bison alticornis, Marsh 1887, and Ceratops alticornis, Marsh 1888]
- T. brevicornus Hatcher, 1905 (=T. prorsus)
- T. calicornis Marsh, 1898 (=T. horridus)
- T. elatus Marsh, 1891 (=T. horridus)
- T. eurycephalus Schlaikjer, 1935
- T. flabellatus Marsh, 1889 (= Sterrholophus Marsh, 1891) (=T. horridus)
- T. galeus Marsh, 1889
- T. hatcheri (Hatcher & Lull 1905) Lull, 1933 (contentious; see Nedoceratops below)
- T. ingens Marsh vide Lull, 1915
- T. maximus Brown, 1933
- T. mortuarius (Cope, 1874) Kuhn, 1936 (nomen dubium; originally Polyonax mortuarius)
- T. obtusus Marsh, 1898 (=T. horridus)
- T. serratus Marsh, 1890 (=T. horridus)
- T. sulcatus Marsh, 1890
- T. sylvestris (Cope, 1872) Olshevsky, 2000 (nomen dubium; originally Agathaumas sylvestris)
Individual Triceratops are estimated to have reached about 7.9 to 9 meters (26 to 30 ft) in length, 2.9 to 3.0 meters (9.5 to 9.8 ft) in height, and 6.1 to 12.0 metric tons (6.7 to 13.2 short tons) in weight. The most distinctive feature is their large skull, among the largest of all land animals. The largest-known skull (specimen MWC 7584, formerly BYU 12183) is estimated to have been 2.5 meters (8.2 ft) in length when complete, and could reach almost a third of the length of the entire animal. A specimen of T. horridus named Kelsey measured 7.3 meters (24 ft) long with a 2-meter (6.5 ft) skull, stood about 2.3 meters (7.5 ft) tall, and was estimated by the Black Hills institute to weight nearly 6 metric tons (6.6 short tons). A Triceratops 8 meters (26 ft) long has been estimated by Gregory S. Paul to have massed 9 metric tons (9.9 short tons).
Like all chasmosaurines, Triceratops had a large skull relative to its body size. The front of the head was equipped with a large beak in front of the teeth. The core of the top beak was formed by a special rostral bone. Behind it, the premaxillae bones were located, embayed from behind by very large circular nostrils. In chasmosaurines, the premaxillae met on their midline in a complex bone plate, the rear edge of which was reinforced by the "narial strut". From the base of this strut, a triangular process jutted out into the nostril. Triceratops differs from most relatives in that this process was hollowed out on the outer side. Behind the toothless premaxilla, the maxilla bore thirty-six to forty tooth positions, in which three to five teeth per position were vertically stacked. The teeth were closely appressed, forming a "dental battery" curving to the inside. The skull bore a single horn on the snout, above the nostrils. In Triceratops, the nose horn is sometimes recognisable as a separate ossification, the epinasal.
The skull also featured a pair of "brow" or supraorbital horns approximately 1 meter (3.3 ft) long, with one above each eye. The jugal bones pointed to below at the rear sides of the skull and were capped by separate epijugals. With Triceratops these were not particularly large and sometimes touched the quadratojugals. The bones of the skull roof were fused. By a folding of the frontal bones, a "double" skull roof was created. In Triceratops, some specimens show a fontanelle, an opening in the upper roof layer. The cavity between the layers invaded the bone cores of the brow horns.
At the rear of the skull, the outer squamosal bones and the inner parietal bones grew into a relatively short, bony frill, adorned with epoccipitals in young specimens. These were low triangular processes on the frill edge, representing separate skin ossifications or osteoderms. Typically, with Triceratops specimens there are two epoccipitals present on each parietal bone, with an additional central process on their border. Each squamosal bone had five processes. Most other ceratopsids had large parietal fenestrae, openings, in their frills, but those of Triceratops were noticeably solid, unless the genus Torosaurus represents mature Triceratops individuals. Under the frill, at the rear of the skull, a huge occipital condyle, up to 106 millimeters (4.2 in) in diameter, connected the head to the neck.
The lower jaws were elongated and met at their tips in a shared epidentary bone, the core of the toothless lower beak. In the dentary bone, the tooth battery curved to the outside to meet the battery of the upper jaw. At the rear of the lower jaw, the articular bone was exceptionally wide, matching the general width of the jaw joint. T. horridus can be distinguished from T. prorsus by having a shallower snout.
The largest Triceratops skull ever found was discovered in 1992 and excavated in 2003 in Dawson County, Montana, in the Hell Creek Formation. It is a 65-million-year-old male Triceratops skull, 9.2 feet long, 5.2 feet high and 4.6 feet wide and weighing over 600kg. It has been dubbed 'Dragon King' and is understood to be the most expensive skull to ever trade privately  
Chasmosaurines showed little variation in their postcranial skeleton. The skeleton of Triceratops is markedly robust. Both Triceratops species possessed a sturdy build, with strong limbs, short hands with three hooves each, and short feet with four hooves each. The vertebral column consisted of ten neck, twelve back, ten sacral and about forty-five tail vertebrae. The front neck vertebrae were fused into a syncervical. Traditionally, this was assumed to have incorporated the first three vertebrae which would imply that the frontmost atlas was very large and sported a neural spine. Later interpretations revived an old hypothesis by John Bell Hatcher that at the very front a vestige of the real atlas can be observed, the syncervical then consisting of four vertebrae. The vertebral count mentioned, is adjusted to this view. In Triceratops the neural spines of the neck are constant in height, instead of gradually sloping upwards. Another peculiarity is that the neck ribs only begin to lengthen with the ninth cervical vertebra.
The rather short and high vertebrae of the back were in its middle region reinforced by ossified tendons running along the tops of the neural arches. The straight sacrum was long and adult individuals show a fusion of all sacral vertebrae. In Triceratops the first four and last two sacrals had transverse processes, connecting the vertebral column to the pelvis, that were fused at their distal ends. Sacrals seven and eight had longer processes, causing the sacrum to have an oval profile in top view. On top of the sacrum a neural plate was present formed by a fusion of the neural spines of the second through fifth vertebrae. Triceratops had a large pelvis with a long ilium. The ischium was curved downwards. The foot was short with four functional toes. The phalangeal formula of the foot is 2-3-4-5-0.
Although certainly quadrupedal, the posture of horned dinosaurs has long been the subject of some debate. Originally, it was believed that the front legs of the animal had to be sprawling at a considerable angle from the thorax in order to better bear the weight of the head. This stance can be seen in paintings by Charles Knight and Rudolph Zallinger. Ichnological evidence in the form of trackways from horned dinosaurs and recent reconstructions of skeletons (both physical and digital) seem to show that Triceratops and other ceratopsids maintained an upright stance during normal locomotion, with the elbows flexed to behind and slightly bowed out, in an intermediate state between fully upright and fully sprawling, comparable to the modern rhinoceros.
The hands and forearms of Triceratops retained a fairly primitive structure compared to other quadrupedal dinosaurs such as thyreophorans and many sauropods. In those two groups, the forelimbs of quadrupedal species were usually rotated so that the hands faced forward with palms backward ("pronated") as the animals walked. Triceratops, like other ceratopsians and the related quadrupedal ornithopods, together forming the Cerapoda, walked with most of their fingers pointing out and away from the body, the original condition for dinosaurs, also retained by bipedal forms like the theropods. In Triceratops, the weight of the body was carried by only the first three fingers of the hand, while digits 4 and 5 were vestigial and lacked claws or hooves. The phalangeal formula of the hand is 2-3-4-3-1, meaning that the first or innermost finger of the forelimb has two bones, the next has three, etc.
Preserved skin of Triceratops is known from a specimen found in Wyoming, though it has not been formally published in the scientific literature. These consist of large ~50–60 millimetres (2.0–2.4 in) across hexagonal tubercles, along with larger ~ 100 millimetres (3.9 in) across tubercles with conical projections.
Triceratops is the best-known genus of the Ceratopsidae, a family of large, mostly North American horned dinosaurs. The exact relationship of Triceratops among the ceratopsids has been debated over the years. Confusion stemmed mainly from the combination of a short, solid frill (similar to that of Centrosaurinae), with long brow horns (more akin to Chasmosaurinae). In the first overview of horned dinosaurs, R. S. Lull hypothesized the existence of two lineages, one of Monoclonius and Centrosaurus leading to Triceratops, the other with Ceratops and Torosaurus, making Triceratops a centrosaurine as the group is understood today. Later revisions supported this view, Lawrence Lambe in 1915 formally describing the first, short-frilled group as the Centrosaurinae (including Triceratops), and the second, long-frilled group as the Chasmosaurinae.
In 1949, Charles M. Sternberg was the first to question this position, proposing instead that Triceratops was more closely related to Arrhinoceratops and Chasmosaurus based on skull and horn features, making Triceratops a chasmosaurine ("ceratopsine" in his usage) genus. He was largely ignored, with John Ostrom and later David Norman placing Triceratops within the Centrosaurinae.
Subsequent discoveries and analyses, however, proved the correctness of Sternberg's view on the position of Triceratops, with Thomas Lehman defining both subfamilies in 1990 and diagnosing Triceratops as "ceratopsine" on the basis of several morphological features. Apart from the one feature of a shortened frill, Triceratops shares no derived traits with centrosaurines. Further research by Peter Dodson, including a 1990 cladistic analysis and a 1993 study using RFTRA (resistant-fit theta-rho analysis), a morphometric technique which systematically measures similarities in skull shape, reinforces Triceratops' placement in the chasmosaurines.
For many years after its discovery, the deeper evolutionary origins of Triceratops and its close relatives remained largely obscure. In 1922, the newly discovered Protoceratops was seen as its ancestor by Henry Fairfield Osborn, but many decades passed before additional findings came to light. Recent years have been fruitful for the discovery of several antecedents of Triceratops. Zuniceratops, the earliest-known ceratopsian with brow horns, was described in the late 1990s, and Yinlong, the first known Jurassic ceratopsian, in 2005.
These new finds have been vital in illustrating the origins of horned dinosaurs in general, suggesting an Asian origin in the Jurassic, and the appearance of truly horned ceratopsians by the beginning of the Late Cretaceous in North America.
In phylogenetic taxonomy, the genus Triceratops has been used as a reference point in the definition of Dinosauria; dinosaurs have been designated as all descendants of the most recent common ancestor of Triceratops and modern bird. Furthermore, the bird-hipped dinosaurs have been defined as those dinosaurs more closely related to Triceratops than to modern birds.
Although Triceratops are commonly portrayed as herding animals, there is currently little evidence that they lived in herds. While several other genera of horned dinosaurs are known from bone beds preserving bones from two to hundreds or thousands of individuals, to date there is only one documented bonebed dominated by Triceratops bones: a site in southeastern Montana with the remains of three juveniles. It may be significant that only juveniles were present. In 2012, a group of three Triceratops in relatively complete condition, each of varying sizes from a full-grown adult to a small juvenile, were found near Newcastle, Wyoming. The remains are currently under excavation by paleontologist Peter Larson and a team from the Black Hills Institute. It is believed that the animals were traveling as a family unit, but it remains unknown if the group consists of a mated pair and their offspring, or two females and a juvenile they were caring for. The remains also show signs of predation or scavenging from Tyrannosaurus, particularly on the largest specimen, with the bones of the front limbs showing breakage and puncture wounds from Tyrannosaurus teeth. New evidence presented in 2020 by Illies and Fowler et al. suggests that Triceratops lived in small groups of perhaps between five and ten individuals based on fossils collected in the previous decade.
For many years, Triceratops finds were known only from solitary individuals. These remains are very common; for example, Bruce Erickson, a paleontologist of the Science Museum of Minnesota, has reported having seen 200 specimens of T. prorsus in the Hell Creek Formation of Montana. Similarly, Barnum Brown claimed to have seen over 500 skulls in the field.: 79 Because Triceratops teeth, horn fragments, frill fragments, and other skull fragments are such abundant fossils in the Lancian faunal stage of the late Maastrichtian (Late Cretaceous, 66 mya) Period of western North America, it is regarded as among the dominant herbivores of the time, if not the most dominant herbivore. In 1986, Robert Bakker estimated it as making up five sixths of the large dinosaur fauna at the end of the Cretaceous. Unlike most animals, skull fossils are far more common than postcranial bones for Triceratops, suggesting that the skull had an unusually high preservation potential.
Analysis of the endocranial anatomy of Triceratops suggest its sense of smell was poor compared to that of other dinosaurs. Its ears were attuned to low frequency sounds given the short cochlear lengths recorded in an analysis by Sakagami et al,. This same study also suggests that Triceratops held its head about 45 degrees to the ground; an angle which would showcase the horns and frill most effectively while simultaneously allowing the animal to take advantage of food through grazing.
Dentition and diet
Triceratops were herbivorous, and because of their low slung head, their primary food was probably low growing vegetation, although they may have been able to knock down taller plants with their horns, beak, and bulk. The jaws were tipped with a deep, narrow beak, believed to have been better at grasping and plucking than biting.
Triceratops teeth were arranged in groups called batteries, of 36 to 40 tooth columns in each side of each jaw, with 3 to 5 stacked teeth per column, depending on the size of the animal. This gives a range of 432 to 800 teeth, of which only a fraction were in use at any given time (Tooth replacement was continuous throughout the life of the animal). They functioned by shearing in a vertical to near-vertical orientation. The great size and numerous teeth of Triceratops suggests that they ate large volumes of fibrous plant material, with some researchers suggesting palms and cycads, and others suggesting ferns, which then grew in prairies.
Functions of the horns and frill
There has been much speculation over the functions of Triceratops' head adornments. The two main theories have revolved around use in combat and in courtship display, with the latter now thought to be the most likely primary function.
Early on, Lull postulated that the frills may have served as anchor points for the jaw muscles to aid chewing by allowing increased size and thus power for the muscles. This has been put forward by other authors over the years, but later studies do not find evidence of large muscle attachments on the frill bones.
Triceratops were long thought to have used their horns and frills in combat with predators such as Tyrannosaurus, the idea being discussed first by Charles H. Sternberg in 1917 and 70 years later by Robert Bakker. There is evidence that Tyrannosaurus did have aggressive head-on encounters with Triceratops, based on partially healed tyrannosaur tooth marks on a Triceratops brow horn and squamosal; the bitten horn is also broken, with new bone growth after the break. Which animal was the aggressor is not known. Since the Triceratops wounds healed, it is most likely that the Triceratops survived the encounter. Tyrannosaurus is also known to have fed on Triceratops, as shown by a heavily tooth-scored Triceratops ilium and sacrum.
In addition to combat with predators using horns, Triceratops are popularly shown engaging each other in combat with horns locked. While studies show that such activity would be feasible, if unlike that of present-day horned animals, there is disagreement about whether they did so. Although pitting, holes, lesions, and other damage on Triceratops skulls (and the skulls of other ceratopsids) are often attributed to horn damage in combat, a 2006 study finds no evidence for horn thrust injuries causing these forms of damage (for example, there is no evidence of infection or healing). Instead, non-pathological bone resorption, or unknown bone diseases, are suggested as causes. A newer study compared incidence rates of skull lesions and periosteal reaction in Triceratops and Centrosaurus and showed that these were consistent with Triceratops using its horns in combat and the frill being adapted as a protective structure, while lower pathology rates in Centrosaurus may indicate visual rather than physical use of cranial ornamentation, or a form of combat focused on the body rather than the head. The frequency of injury was found to be 14% in Triceratops. The researchers also concluded that the damage found on the specimens in the study was often too localized to be caused by bone disease. Histological examination reveals that the frill of Triceratops is composed of fibrolamellar bone which contains fibroblasts that play a critical role in wound healing, and are capable of rapidly depositing bone during remodeling.
One skull was found with a hole in the jugal bone, apparently a puncture wound sustained while the animal was alive, as indicated by signs of healing. The hole has a diameter close to that of the distal end of a Triceratops horn. This, and other apparent healed wounds in the skulls of ceratopsians, has been cited as evidence of non-fatal intraspecific competition in these dinosaurs.
The large frill also may have helped to increase body area to regulate body temperature. A similar theory has been proposed regarding the plates of Stegosaurus, although this use alone would not account for the bizarre and extravagant variation seen in different members of the Ceratopsidae, which would rather support the sexual display theory.
The theory that frills functioned as a sexual display was first proposed by Davitashvili in 1961 and has gained increasing acceptance since. Evidence that visual display was important, either in courtship or other social behavior, can be seen in the horned dinosaurs differing markedly in their adornments, making each species highly distinctive. Also, modern living creatures with such displays of horns and adornments use them similarly. A 2006 study of the smallest Triceratops skull, ascertained to be a juvenile, shows the frill and horns developed at a very early age, predating sexual development and thus probably important for visual communication and species recognition in general. The use of the exaggerated structures to enable dinosaurs to recognize their own species has been questioned, as no such function exists for such structures in modern species.
Growth and ontogeny
In 2006, the first extensive ontogenetic study of Triceratops was published in the journal Proceedings of the Royal Society. The study, by John R. Horner and Mark Goodwin, found that individuals of Triceratops could be divided into four general ontogenetic groups: babies, juveniles, subadults, and adults. With a total number of 28 skulls studied, the youngest was only 38 centimeters (15 in) long. Ten of the 28 skulls could be placed in order in a growth series with one representing each age. Each of the four growth stages were found to have identifying features. Multiple ontogenetic trends were discovered, including the size reduction of the epoccipitals, development and reorientation of postorbital horns, and hollowing out of the horns.
Torosaurus as growth stage of Triceratops
Torosaurus is a ceratopsid genus first identified from a pair of skulls in 1891, two years after the identification of Triceratops by Charles Marsh. The genus Torosaurus resembles Triceratops in geological age, distribution, anatomy and size and it has been recognised as a close relative. Its distinguishing features are an elongated skull and the presence of two fenestrae, or holes, in the frill. Paleontologists investigating dinosaur ontogeny (growth and development of individuals over the life span) in Montana's Hell Creek Formation have recently presented evidence that the two represent a single genus.
John Scannella, in a paper presented in Bristol at the conference of the Society of Vertebrate Paleontology (September 25, 2009), reclassified Torosaurus as especially mature Triceratops individuals, perhaps representing a single sex. Horner, Scannella's mentor at Bozeman Campus, Montana State University, noted that ceratopsian skulls consist of metaplastic bone. A characteristic of metaplastic bone is that it lengthens and shortens over time, extending and resorbing to form new shapes. Significant variety is seen even in those skulls already identified as Triceratops, Horner said, "where the horn orientation is backwards in juveniles and forward in adults". Approximately 50% of all subadult Triceratops skulls have two thin areas in the frill that correspond with the placement of "holes" in Torosaurus skulls, suggesting that holes developed to offset the weight that would otherwise have been added as maturing Triceratops individuals grew longer frills. A paper describing these findings in detail was published in July 2010 by Scannella and Horner. It formally argues that Torosaurus and the similar contemporary Nedoceratops are synonymous with Triceratops.
The assertion ignited debate. Andrew Farke had in 2006 stressed that, apart from the frill, no systematic differences could be found between Torosaurus and Triceratops. He nevertheless disputed Scannella's conclusion by arguing in 2011 that the proposed morphological changes required to "age" a Triceratops into a Torosaurus would be without precedent among ceratopsids. Such changes would include the growth of additional epoccipitals, reversion of bone texture from an adult to immature type and back to adult again, and growth of frill holes at a later stage than usual. A study by Nicholas Longrich and Daniel Field analyzed 35 specimens of both Triceratops and Torosaurus. The authors concluded that Triceratops individuals too old to be considered immature forms are represented in the fossil record, as are Torosaurus individuals too young to be considered fully mature adults. The synonymy of Triceratops and Torosaurus cannot be supported, they said, without more convincing intermediate forms than Scannella and Horner initially produced. Scannella's Triceratops specimen with a hole on its frill, they argued, could represent a diseased or malformed individual rather than a transitional stage between an immature Triceratops and mature Torosaurus form.
Other genera as growth stages of Triceratops
Opinion has varied on the validity of a separate genus for Nedoceratops. Scannella and Horner regarded it as an intermediate growth stage between Triceratops and Torosaurus. Farke, in his 2011 redescription of the only known skull, concluded that it was an aged individual of its own valid taxon, Nedoceratops hatcheri. Longrich and Fields also did not consider it a transition between Torosaurus and Triceratops, suggesting that the frill holes were pathological.
As described above, Scannella had argued in 2010 that Nedoceratops should be considered a synonym of Triceratops. Farke (2011) maintained that it represents a valid distinct genus. Longrich agreed with Scannella about Nedoceratops and made a further suggestion: that the recently described Ojoceratops was likewise a synonym. The fossils, he argued, are indistinguishable from the Triceratops horridus specimens that were previously attributed to the defunct species Triceratops serratus.
Longrich observed that another newly described genus, Tatankaceratops, displayed a strange mix of characteristics already found in adult and juvenile Triceratops. Rather than representing a distinct genus, Tatankaceratops could as easily represent a dwarf Triceratops or a Triceratops individual with a developmental disorder that caused it to stop growing prematurely.
Triceratops lived during the Late Cretaceous of North America, its fossils coming from the Evanston Formation, Scollard Formation, Laramie Formation, Lance Formation, Denver Formation, and Hell Creek Formation. These fossil formations date back to the time of the Cretaceous–Paleogene extinction event, which has been dated to 66 ± 0.07 million years ago. Many animals and plants have been found in these formations, but mostly from the Lance Formation and Hell Creek Formation. Triceratops was one of the last ceratopsian genera to appear before the end of the Mesozoic. The related Torosaurus, and the more distantly related diminutive Leptoceratops, were also present, though their remains have been rarely encountered.
Theropods from these formations include genera of dromaeosaurids, tyrannosaurids, ornithomimids, troodontids, avialans, and caenagnathids, Dromaeosaurids from the Hell Creek Formation are Acheroraptor and Dakotaraptor. Indeterminate dromaeosaurs are known from other fossil formations. Common teeth previously referred to Dromaeosaurus and Saurornitholestes later were considered to be Acheroraptor. The tyrannosaurids from the formation are Nanotyrannus and Tyrannosaurus, although the former might be a junior synonym of the latter. Among ornithomimids are the genera Struthiomimus as well as Ornithomimus; an undescribed animal named "Orcomimus" could be from the formation. Troodontids are only represented by Pectinodon and Paronychodon in the Hell Creek Formation; with a possible species of Troodon from the Lance Formation. One species of coelurosaur is known from Hell Creek and similar formations by a single species, Richardoestesia. Only three oviraptorosaurs are from the Hell Creek Formation: Anzu, Leptorhynchos and a giant species of caenagnathid, very similar to Gigantoraptor, from South Dakota. However, only fossilized foot prints were discovered. The avialans known from the formation are Avisaurus, multiple species of Brodavis, and several other species of hesperornithoforms, as well as several species of true birds including Cimolopteryx.
Ornithischians are abundant in the Scollard, Laramie, Lance, Denver, and Hell Creek Formation. The main groups of ornithischians are ankylosaurians, ornithopods, ceratopsians, and pachycephalosaurians. Three ankylosaurians are known: Ankylosaurus, Denversaurus, and possibly a species of Edmontonia or an undescribed genus. Multiple genera of ceratopsians are known from the formation other than Triceratops, the leptoceratopsid Leptoceratops, and the chasmosaurine ceratopsids Torosaurus, Nedoceratops and Tatankaceratops. Ornithopods are common in the Hell Creek Formation, and are known from several species of the ornithopod Thescelosaurus and the hadrosaurid Edmontosaurus. Several pachycephalosaurians have been found in the Hell Creek Formation and in similar formations. Among them are the derived pachycephalosaurids Stygimoloch, Dracorex, Pachycephalosaurus, Sphaerotholus, and an undescribed specimen from North Dakota. The first two might be junior synonyms of Pachycephalosaurus.
Mammals are plentiful in the Hell Creek Formation. Groups represented include multituberculates, metatherians, and eutherians: The multituberculates represented include Paracimexomys; the cimolomyids Paressonodon, Meniscoessus, Essonodon, Cimolomys, Cimolodon, and Cimexomys; and the neoplagiaulacids Mesodma, and Neoplagiaulax. The metatherians are represented by the alphadontids Alphadon, Protalphodon, and Turgidodon; the pediomyids Pediomys, Protolambda, and Leptalestes; the stagodontid Didelphodon; the deltatheridiid Nanocuris; the herpetotheriid Nortedelphys; and the glasbiid Glasbius. A few eutherians are known, being represented by Alostera; Protungulatum; the cimolestids Cimolestes and Batodon; the gypsonictopsid Gypsonictops; and the possible nyctitheriid Paranyctoides.
Depiction in popular media
Triceratops is the official state fossil of South Dakota, and the official state dinosaur of Wyoming. In 1942, Charles R. Knight painted a mural incorporating a confrontation between a Tyrannosaurus and a Triceratops in the Field Museum of Natural History for the National Geographic Society, establishing them as enemies in the popular imagination. Paleontologist Bob Bakker said of the imagined rivalry between Tyrannosaurus and Triceratops, "No matchup between predator and prey has ever been more dramatic. It's somehow fitting that those two massive antagonists lived out their co-evolutionary belligerence through the last days of the last epoch of the Age of Dinosaurs."
- "Melbourne Museum acquires world's most complete triceratops skeleton in 'immense' dinosaur deal". the Guardian. December 2, 2020. Retrieved February 10, 2021.
- Carpenter, K. (2006). "Bison" alticornis and O.C. Marsh's early views on ceratopsians". In Carpenter, K. (ed.). Horns and Beaks: Ceratopsian and Ornithopod Dinosaurs. Bloomington and Indianapolis: Indiana University Press. pp. 349–364. ISBN 978-0-253-34817-3.
- Marsh, O.C. (1887). "Notice of new fossil mammals". American Journal of Science. 34 (202): 323–331. Bibcode:1887AmJS...34..323M. doi:10.2475/ajs.s3-34.202.323. S2CID 129984410.
- Marsh, O.C. (1888). "A new family of horned Dinosauria, from the Cretaceous". American Journal of Science. 36 (216): 477–478. Bibcode:1888AmJS...36..477M. doi:10.2475/ajs.s3-36.216.477. S2CID 130243398.
- Marsh, O.C. (1889a). "Notice of new American Dinosauria". American Journal of Science. 37 (220): 331–336. Bibcode:1889AmJS...37..331M. doi:10.2475/ajs.s3-37.220.331. S2CID 131729220.
- Dodson, P. (1996). The Horned Dinosaurs. Princeton, New Jersey: Princeton University Press. ISBN 978-0-691-02882-8.
- Marsh, O.C. (1889b). "Notice of gigantic horned Dinosauria from the Cretaceous". American Journal of Science. 38 (224): 173–175. Bibcode:1889AmJS...38..173M. doi:10.2475/ajs.s3-38.224.173. S2CID 131187857.
- Hatcher, J. B.; Marsh, O. C.; Lull, R. S. (1907). The Ceratopsia. Washington, D.C.: Government Printing Office. ISBN 978-0-405-12713-7.
- Breithaupt, B. H. (1999). "First Discovery of Dinosaurs in the American West". In Gillette, D. D. (ed.). Vertebrate Paleontology In Utah. Utah Geological Survey. pp. 59–65. ISBN 978-1-55791-634-1.
- Lull, R. S. (1933). "A revision of the Ceratopsia or horned dinosaurs". Memoirs of the Peabody Museum of Natural History. 3 (3): 1–175. doi:10.5962/bhl.title.5716. Retrieved November 20, 2010.
- Goussard, Florent (2006). "The skull of Triceratops in the palaeontology gallery, Muséum national d'Histoire naturelle, Paris". Geodiversitas. 28 (3): 467–476 – via ResearchGate.
- Sternberg, C. M. (1949). "The Edmonton fauna and description of a new Triceratops from the Upper Edmonton member; phylogeny of the Ceratopsidae". National Museum of Canada Bulletin. 113: 33–46.
- Ostrom, J. H.; Wellnhofer, P. (1986). "The Munich specimen of Triceratops with a revision of the genus". Zitteliana. 14: 111–158.
- Lehman, T. M. (1990). "The ceratopsian subfamily Chasmosaurinae: sexual dimorphism and systematics". In Carpenter, K.; Currie, P. J. (eds.). Dinosaur Systematics: Perspectives and Approaches. Cambridge: Cambridge University Press. pp. 211–229. ISBN 978-0-521-36672-4.
- Forster, C.A. (1996). "Species resolution in Triceratops: cladistic and morphometric approaches". Journal of Vertebrate Paleontology. 16 (2): 259–270. doi:10.1080/02724634.1996.10011313.
- Lehman, T. M. (1998). "A gigantic skull and skeleton of the horned dinosaur Pentaceratops sternbergi from New Mexico". Journal of Paleontology. 72 (5): 894–906. doi:10.1017/S0022336000027220. JSTOR 1306666.
- Scannella, J. B.; Fowler, D. W. (2009). "Anagenesis in Triceratops: evidence from a newly resolved stratigraphic framework for the Hell Creek Formation". 9th North American Paleontological Convention Abstracts. Cincinnati Museum Center Scientific Contributions 3. pp. 148–149.
- "T Dinosaurs Page 2". DinoDictionary.com. Retrieved August 3, 2010.
- "Triceratops in The Natural History Museum's Dino Directory". Internt.nhm.ac.uk. Archived from the original on February 17, 2009. Retrieved August 3, 2010.
- Alexander, R.M. (1985). "Mechanics of posture and gait of some large dinosaurs". Zoological Journal of the Linnean Society. 83: 1–25. doi:10.1111/j.1096-3642.1985.tb00871.x.
- Scannella, J.; Horner, J.R. (2010). "Torosaurus Marsh, 1891, is Triceratops Marsh, 1889 (Ceratopsidae: Chasmosaurinae): synonymy through ontogeny". Journal of Vertebrate Paleontology. 30 (4): 1157–1168. doi:10.1080/02724634.2010.483632. S2CID 86767957.
- Lambert, D. (1993). The Ultimate Dinosaur Book. Dorling Kindersley, New York. pp. 152–167. ISBN 978-1-56458-304-8.
- "A Triceratops Named 'Kelsey'". www.bhigr.com. Retrieved December 22, 2017.
- Paul, G. S. (2010). The Princeton Field Guide to Dinosaurs. Princeton University Press. pp. 265–267. ISBN 978-0-691-13720-9.
- Dodson, P.; Forster, C. A.; Sampson, S. D. (2004). "Ceratopsidae". In Weishampel, D. B.; Dodson, P.; Osmólska, H. (eds.). The Dinosauria (second ed.). Berkeley: University of California Press. pp. 494–513. ISBN 978-0-520-24209-8.
- "Denver museum unveils 7-foot-long, 1,000-pound Triceratops skull". The Daily Courier. November 18, 2003. Retrieved December 26, 2013.
- Scannella, John B.; Fowler, Denver W.; Goodwin, Mark B.; Horner, John R. (July 15, 2014). "Evolutionary trends in Triceratops from the Hell Creek Formation, Montana". Proceedings of the National Academy of Sciences. 111 (28): 10245–10250. Bibcode:2014PNAS..11110245S. doi:10.1073/pnas.1313334111. ISSN 0027-8424. PMC 4104892. PMID 24982159.
- "Making A Triceratops. Science Supplies Missing Part! Of Skeleton". Boston Evening Transcript. October 24, 1901. Retrieved December 26, 2013.
- Fujiwara, Shin-Ichi (December 12, 2009). "A reevaluation of the manus structure in Triceratops (Ceratopsia: Ceratopsidae)". Journal of Vertebrate Paleontology. 29 (4): 1136–1147. doi:10.1671/039.029.0406. ISSN 0272-4634. S2CID 86519018.
- Christiansen, P.; Paul, G.S. (2001). "Limb bone scaling, limb proportions, and bone strength in neoceratopsian dinosaurs" (PDF). Gaia. 16: 13–29.
- Thompson, S.; Holmes, R. (2007). "Forelimb stance and step cycle in Chasmosaurus irvinensis (Dinosauria: Neoceratopsia)". Palaeontologia Electronica. 10 (1): 17 p.
- Rega, E.; Holmes, R.; Tirabasso, A. (2010). "Habitual locomotor behavior inferred from manual pathology in two Late Cretaceous chasmosaurine ceratopsid dinosaurs, Chasmosaurus irvinensis (CMN 41357) and Chasmosaurus belli (ROM 843)". In Ryan, Michael J.; Chinnery-Allgeier, Brenda J.; Eberth, David A. (eds.). New Perspectives on Horned Dinosaurs: The Royal Tyrrell Museum Ceratopsian Symposium. Bloomington and Indianapolis: Indiana University Press. pp. 340–354. ISBN 978-0-253-35358-0.
- Martin, Anthony J. (2006). Introduction to the study of dinosaurs (2nd ed.). Malden, MA: Blackwell Pub. ISBN 978-1405134132. OCLC 61130756.
- Witton, Mark (December 24, 2015). "Mark Witton.com Blog: Dinosaur scales: some thoughts for artists". Mark Witton.com Blog. Retrieved June 25, 2021.
- "What is special about the Triceratops?". Dinosaurios.org. July 24, 2013. Retrieved December 26, 2013.
- Lambe, L.M. (1915). "On Eoceratops canadensis, gen. nov., with remarks on other genera of Cretaceous horned dinosaurs". Canada Department of Mines Geological Survey Museum Bulletin. 12: 1–49. ISBN 978-0-665-82611-5. Archived from the original on June 29, 2011.
- Ostrom, J. H. (1966). "Functional morphology and evolution of the ceratopsian dinosaurs". Evolution. 20 (3): 290–308. doi:10.2307/2406631. JSTOR 2406631. PMID 28562975.
- Norman, David (1985). The Illustrated Encyclopaedia of Dinosaurs. London: Salamander Books. ISBN 978-0-517-46890-6.
- Dodson, P.; Currie, P. J. (1990). "Neoceratopsia". In Weishampel, D. B.; Dodson, P.; Osmólska, H. (eds.). The Dinosauria. Berkeley: University of California Press. pp. 593–618. ISBN 978-0-520-06727-1.
- Dodson, P. (1993). "Comparative craniology of the Ceratopsia" (PDF). American Journal of Science. 293: 200–234. Bibcode:1993AmJS..293..200D. doi:10.2475/ajs.293.A.200.
- Longrich, N. R. (2014). "The horned dinosaurs Pentaceratops and Kosmoceratops from the upper Campanian of Alberta and implications for dinosaur biogeography". Cretaceous Research. 51: 292–308. doi:10.1016/j.cretres.2014.06.011.
- Gauthier, J. A. (1986). "Saurischian monophyly and the origin of birds. The Origin of Birds and the Evolution of Flight, K. Padian (ed.)". Memoirs of the California Academy of Sciences. 8: 1–55.
- Sereno, P. C. (1998). "A rationale for phylogenetic definitions, with application to the higher-level taxonomy of Dinosauria". Neues Jahrbuch für Geologie und Paläontologie, Abhandlungen. 210 (1): 41–83. doi:10.1127/njgpa/210/1998/41.
- Mathews, Joshua C.; Brusatte, Stephen L.; Williams, Scott A.; Henderson, Michael D. (2009). "The first Triceratops bonebed and its implications for gregarious behavior". Journal of Vertebrate Paleontology. 29 (1): 286–290. doi:10.1080/02724634.2009.10010382. S2CID 196608646.
- Smith, Matt (June 4, 2013). "Triceratops trio unearthed in Wyoming - CNN". CNN. Retrieved December 22, 2017.
- Barrera, Nathanial A. (January 9, 2020). "More than old bones: New study sheds light on Triceratops behavior and living habits". The Dickinson Press. Retrieved March 31, 2020.
- Erickson, B. R. (1966). "Mounted skeleton of Triceratops prorsus in the Science Museum". Scientific Publications of the Science Museum. 1: 1–16.
- Bakker, R. T. (1986). The Dinosaur Heresies: New Theories Unlocking The Mystery of the Dinosaurs and Their Extinction. New York: William Morrow. p. 438. ISBN 978-0-14-010055-6.
- Derstler, K. (1994). "Dinosaurs of the Lance Formation in eastern Wyoming". In Nelson, G. E. (ed.). The Dinosaurs of Wyoming. Wyoming Geological Association Guidebook, 44th Annual Field Conference. Wyoming Geological Association. pp. 127–146.
- Sakagami, Rina; Kawabe, Soichiro (2020). "Endocranial anatomy of the ceratopsid dinosaur Triceratops and interpretations of sensory and motor function". PeerJ. 8: e9888. doi:10.7717/peerj.9888. PMC 7505063. PMID 32999761.
- Tait, J.; Brown, B. (1928). "How the Ceratopsia carried and used their head". Transactions of the Royal Society of Canada. 22: 13–23.
- Ostrom, J. H. (1964). "A functional analysis of jaw mechanics in the dinosaur Triceratops" (PDF). Postilla. 88: 1–35. Retrieved November 20, 2010.
- Weishampel, D. B. (1984). Evolution of jaw mechanisms in ornithopod dinosaurs. Advances in Anatomy Embryology and Cell Biology. 87. pp. 1–110. doi:10.1007/978-3-642-69533-9. ISBN 978-3-540-13114-4. PMID 6464809. S2CID 12547312.
- Coe, M. J.; Dilcher, D. L.; Farlow, J. O.; Jarzen, D. M.; Russell, D. A. (1987). "Dinosaurs and land plants". In Friis, E. M.; Chaloner, W. G.; Crane, P. R. (eds.). The Origins of Angiosperms and their Biological Consequences. Cambridge University Press. pp. 225–258. ISBN 978-0-521-32357-4.
- Lull, R. S. (1908). "The cranial musculature and the origin of the frill in the ceratopsian dinosaurs". American Journal of Science. 4 (25): 387–399. Bibcode:1908AmJS...25..387L. doi:10.2475/ajs.s4-25.149.387.
- Forster, C. A. (1990). The cranial morphology and systematics of Triceratops, with a preliminary analysis of ceratopsian phylogeny (Ph.D. Dissertation thesis). Philadelphia: University of Pennsylvania. p. 227.
- Sternberg, C. H. (1917). Hunting Dinosaurs in the Badlands of the Red Deer River, Alberta, Canada. San Diego, California. p. 261.
- Happ, J. (2008). "An analysis of predator-prey behavior in a head-to-head encounter between Tyrannosaurus rex and Triceratops". In Larson, P.; Carpenter, K. (eds.). Tyrannosaurus rex, the Tyrant King (Life of the Past). Bloomington: Indiana University Press. pp. 355–368. ISBN 978-0-253-35087-9.
- Erickson, Gregory M.; Olson, Kenneth H. (March 19, 1996). "Bite marks attributable to Tyrannosaurus rex: Preliminary description and implications". Journal of Vertebrate Paleontology. 16 (1): 175–178. doi:10.1080/02724634.1996.10011297. ISSN 0272-4634.
- Farke, A. A. (2004). "Horn Use in Triceratops (Dinosauria: Ceratopsidae): Testing Behavioral Hypotheses Using Scale Models" (PDF). Palaeo-electronica. 7 (1): 1–10. Retrieved November 20, 2010.
- Tanke, D. H.; Farke, A. A. (2006). "Bone resorption, bone lesions, and extracranial fenestrae in ceratopsid dinosaurs: a preliminary assessment". In Carpenter, K. (ed.). Horns and Beaks: Ceratopsian and Ornithopod Dinosaurs. Bloomington: Indiana University Press. pp. 319–347. ISBN 978-0-253-34817-3.
- Farke, A.A.; Wolff, E.D.S.; Tanke, D.H.; Sereno, Paul (2009). Sereno, Paul (ed.). "Evidence of Combat in Triceratops". PLOS ONE. 4 (1): e4252. Bibcode:2009PLoSO...4.4252F. doi:10.1371/journal.pone.0004252. PMC 2617760. PMID 19172995.
- Peterson, JE; Dischler, C; Longrich, NR (2013). "Distributions of Cranial Pathologies Provide Evidence for Head-Butting in Dome-Headed Dinosaurs (Pachycephalosauridae)". PLOS ONE. 8 (7): e68620. Bibcode:2013PLoSO...868620P. doi:10.1371/journal.pone.0068620. PMC 3712952. PMID 23874691.
- Wall, Michael (January 27, 2009). "Scars Reveal How Triceratops Fought –". Wired. Retrieved August 3, 2010.
- Reid, R.E.H. (1997). "Histology of bones and teeth". In Currie, P. J.; Padian, K. (eds.). Encyclopedia of Dinosaurs. San Diego, CA.: Academic Press. pp. 329–339.
- Horner, JR; Goodwin, MB (2009). "Extreme Cranial Ontogeny in the Upper Cretaceous Dinosaur Pachycephalosaurus". PLOS ONE. 4 (10): e7626. Bibcode:2009PLoSO...4.7626H. doi:10.1371/journal.pone.0007626. PMC 2762616. PMID 19859556.
- Horner, JR; Lamm, E (2011). "Ontogeny of the parietal frill of Triceratops: a preliminary histological analysis". Comptes Rendus Palevol. 10 (5–6): 439–452. doi:10.1016/j.crpv.2011.04.006.
- Farlow, J. O.; Dodson, P. (1975). "The behavioral significance of frill and horn morphology in ceratopsian dinosaurs". Evolution. 29 (2): 353–361. doi:10.2307/2407222. JSTOR 2407222. PMID 28555861.
- Martin, A. J. (2006). Introduction to the Study of Dinosaurs (Second ed.). Oxford: Blackwell Publishing. pp. 299–300. ISBN 978-1-4051-3413-2.
- Wheeler, P.E. (1978). "Elaborate CNS cooling structures in large dinosaurs". Nature. 275 (5679): 441–443. Bibcode:1978Natur.275..441W. doi:10.1038/275441a0. PMID 692723. S2CID 4160470.
- Farlow, J. O.; Thompson, C. V.; Rosner, D. E. (1976). "Plates of the dinosaur Stegosaurus: Forced convection heat loss fins?". Science. 192 (4244): 1123–5. Bibcode:1976Sci...192.1123F. doi:10.1126/science.192.4244.1123. PMID 17748675. S2CID 44506996.
- Davitashvili, L. Sh. (1961). Teoriya Polovogo Otbora (Theory of Sexual Selection). Izdatel'stvo Akademii nauk SSSR. p. 538.
- Farlow, J.O. & Dodson, P. (1975). "The behavioral significance of frill and horn morphology in ceratopsian dinosaurs". Evolution. 29 (2): 353–361. doi:10.2307/2407222. JSTOR 2407222. PMID 28555861.
- Goodwin, M.B.; Clemens, W.A.; Horner, J.R. & Padian, K. (2006). "The smallest known Triceratops skull: new observations on ceratopsid cranial anatomy and ontogeny" (PDF). Journal of Vertebrate Paleontology. 26 (1): 103–112. doi:10.1671/0272-4634(2006)26[103:TSKTSN]2.0.CO;2. ISSN 0272-4634. Archived from the original (PDF) on November 5, 2015. Retrieved January 21, 2007.
- Hone, D. W. E.; Naish, D. (2013). "The 'species recognition hypothesis' does not explain the presence and evolution of exaggerated structures in non-avialan dinosaurs". Journal of Zoology. 290 (3): 172–180. doi:10.1111/jzo.12035.
- Horner, J.R.; Goodwin, M.B. (2006). "Major cranial changes during Triceratops ontogeny". Proceedings of the Royal Society B: Biological Sciences. 273 (1602): 2757–2761. doi:10.1098/rspb.2006.3643. PMC 1635501. PMID 17015322.
- Farke, A. A. (2006). "Cranial osteology and phylogenetic relationships of the chasmosaurine ceratopsid Torosaurus latus". In Carpenter, K. (ed.). Horns and Beaks: Ceratopsian and Ornithopod Dinosaurs. Bloomington: Indiana University Press. pp. 235–257. ISBN 978-0-253-34817-3.
- "New Analyses Of Dinosaur Growth May Wipe Out One-third Of Species". Science News. ScienceDaily.com. October 31, 2009. Retrieved November 3, 2009.
- Farke, Andrew A. (2011). Claessens, Leon (ed.). "Anatomy and taxonomic status of the chasmosaurine ceratopsid Nedoceratops hatcheri from the Upper Cretaceous Lance Formation of Wyoming, U.S.A". PLOS ONE. 6 (1): e16196. Bibcode:2011PLoSO...616196F. doi:10.1371/journal.pone.0016196. PMC 3024410. PMID 21283763.
- Longrich, Nicholas R.; Field, Daniel J. (February 29, 2012). "Torosaurus Is Not Triceratops: Ontogeny in Chasmosaurine Ceratopsids as a Case Study in Dinosaur Taxonomy". PLOS ONE. 7 (2): e32623. Bibcode:2012PLoSO...732623L. doi:10.1371/journal.pone.0032623. ISSN 1932-6203. PMC 3290593. PMID 22393425.
- Bowdler, Neil (March 1, 2012). "Triceratops and Torosaurus dinosaurs 'two species, not one'". BBC News. Retrieved July 29, 2013.
- Scannella, J. B.; Horner, J. R. (2011). Claessens, Leon (ed.). "'Nedoceratops': An Example of a Transitional Morphology". PLOS ONE. 6 (12): e28705. Bibcode:2011PLoSO...628705S. doi:10.1371/journal.pone.0028705. PMC 3241274. PMID 22194891.
- Longrich, Nicholas R. (2011). "Titanoceratops ouranous, a giant horned dinosaur from the Late Campanian of New Mexico". Cretaceous Research. 32 (3): 264–276. doi:10.1016/j.cretres.2010.12.007.
- Weishampel, D.B.; Dodson, Peter; Osmólska, H. (2004). The Dinosauria (Second ed.). Berkeley: University of California Press. p. 861. ISBN 978-0-520-24209-8.
- Husson, D. E.; Galbrun, B.; Laskar, J.; Hinnov, L. A.; Thibault, N.; Gardin, S.; Locklair, R. E. (2011). "Astronomical calibration of the Maastrichtian (Late Cretaceous)". Earth and Planetary Science Letters. 305 (3–4): 328–340. Bibcode:2011E&PSL.305..328H. doi:10.1016/j.epsl.2011.03.008.
- Longrich, N. R.; Tokaryk, T.; Field, D. J. (2011). "Mass extinction of birds at the Cretaceous-Paleogene (K-Pg) boundary". Proceedings of the National Academy of Sciences. 108 (37): 15253–15257. Bibcode:2011PNAS..10815253L. doi:10.1073/pnas.1110395108. PMC 3174646. PMID 21914849.
- Lamanna, M. C.; Sues, H. D.; Schachner, E. R.; Lyson, T. R. (2014). "A New Large-Bodied Oviraptorosaurian Theropod Dinosaur from the Latest Cretaceous of Western North America". PLOS ONE. 9 (3): e92022. Bibcode:2014PLoSO...992022L. doi:10.1371/journal.pone.0092022. PMC 3960162. PMID 24647078.
- Evans, D. C.; Larson, D. W.; Currie, P. J. (2013). "A new dromaeosaurid (Dinosauria: Theropoda) with Asian affinities from the latest Cretaceous of North America". Naturwissenschaften. 100 (11): 1041–1049. Bibcode:2013NW....100.1041E. doi:10.1007/s00114-013-1107-5. PMID 24248432. S2CID 14978813.
- Triebold, M. (1997). Wolberg, D.; Stump, E.; Rosenberg, G. (eds.). "The Sandy site: Small dinosaurs from the Hell Creek Formation of South Dakota". Dinofest International: Proceedings of a Symposium: 245–248.
- Maltese, Anthony (December 17, 2013). "Giant Oviraptor Tracks from the Hell Creek". RMDRC paleo lab. Retrieved December 17, 2013.
- Martin, L. D.; Kurochkin, E. N.; Tokaryk, T. T. (2012). "A new evolutionary lineage of diving birds from the Late Cretaceous of North America and Asia". Palaeoworld. 21: 59–63. doi:10.1016/j.palwor.2012.02.005.
- Ott, C.J.; Larson, P.L. (2010). "A New, Small Ceratopsian Dinosaur from the Latest Cretaceous Hell Creek Formation, Northwest South Dakota, United States: A Preliminary Description". In Ryan, M.J.; Chinnery-Allgeier, B.J.; Eberth, D.A. (eds.). New Perspectives on Horned Dinosaurs: The Royal Tyrrell Museum Ceratopsian Symposium. Bloomington: Indiana University Press. p. 656.
- Campione, N. S. E.; Evans, D. C. (2011). "Cranial Growth and Variation in Edmontosaurs (Dinosauria: Hadrosauridae): Implications for Latest Cretaceous Megaherbivore Diversity in North America". PLOS ONE. 6 (9): e25186. Bibcode:2011PLoSO...625186C. doi:10.1371/journal.pone.0025186. PMC 3182183. PMID 21969872.
- Bakker, R.T.; Sullivan, R.M.; Porter, V.; Larson, P.; Saulsbury, S.J. (2006). Lucas, S.G.; Sullivan, R.M. (eds.). "Dracorex hogwartsia, n. gen., n. sp., a spiked, flat-headed pachycephalosaurid dinosaur from the Upper Cretaceous Hell Creek Formation of South Dakota". Late Cretaceous Vertebrates from the Western Interior. New Mexico Museum of Natural History and Science Bulletin. 35: 331–345.
- Kielan-Jaworowska, Zofia; Cifelli, Richard L.; Luo, Zhe-Xi (2004). Mammals from the Age of Dinosaurs: Origins, Evolution, and Structure. New York: Columbia University Press. pp. 98–99. ISBN 978-0-231-11918-4.
- Wilson, G. P. (2013). "Mammals across the K/Pg boundary in northeastern Montana, U.S.A.: Dental morphology and body-size patterns reveal extinction selectivity and immigrant-fueled ecospace filling". Paleobiology. 39 (3): 429–469. doi:10.1666/12041. S2CID 36025237.
- Archibald, J. D.; Zhang, Y.; Harper, T.; Cifelli, R. L. (2011). "Protungulatum, Confirmed Cretaceous Occurrence of an Otherwise Paleocene Eutherian (Placental?) Mammal". Journal of Mammalian Evolution. 18 (3): 153–161. doi:10.1007/s10914-011-9162-1. S2CID 16724836.
- State of South Dakota. "Signs and Symbols of South Dakota..." Archived from the original on February 20, 2008. Retrieved January 20, 2007.
- State of Wyoming. "State of Wyoming – General Information". Archived from the original on February 10, 2007. Retrieved January 20, 2007.
- Bakker, R. T. (1986). The Dinosaur Heresies. New York: Kensington Publishing. p. 240. On that page, Bakker has his own T. rex/Triceratops fight.
- Media related to Triceratops at Wikimedia Commons
- Wikijunior Dinosaurs/Triceratops at Wikibooks
- Works related to Notice of Gigantic Horned Dinosauria from the Cretaceous at Wikisource
- Data related to Triceratops at Wikispecies
- Triceratops at The Dinosaur Picture Database
- LiveScience: Facts about Triceratops at LiveScience.com
- on YouTube
- Dinosaur Mailing List post on Triceratops stance
- Smithsonian Exhibit
- Triceratops at the Internet Archive
- Triceratops in the Dino Directory
- Triceratops (short summary and good color illustration)
- Triceratops For Kids (a fact sheet about the Triceratops with activities for kids)
- Triceratops, BBC Dinosaurs
- (in French) Triceratops - Liste de Dinosauria et Extinction