Temporal range: Late Cretaceous, 80–66Ma
|Mounted cast of a Tyrannosaurus rex skeleton, Palais de la Découverte|
Tyrannosauridae (or tyrannosaurids, meaning "tyrant lizards") is a family of coelurosaurian theropod dinosaurs which comprises two subfamilies containing up to eleven genera, including the eponymous Tyrannosaurus. The exact number of genera is controversial, with some experts recognizing as few as three. All of these animals lived near the end of the Cretaceous Period and their fossils have been found only in North America and Asia.
Although descended from smaller ancestors, tyrannosaurids were almost always the largest predators in their respective ecosystems, putting them at the apex of the food chain. The largest species was Tyrannosaurus rex, one of the largest known land predators, which measured up to 12.3 metres (40 ft) in length and up to 6,500 kilograms (7.2 short tons) in weight. Tyrannosaurids were bipedal carnivores with massive skulls filled with large teeth. Despite their large size, their legs were long and proportioned for fast movement. In contrast, their arms were very small, bearing only two functional digits.
Unlike most other groups of dinosaurs, very complete remains have been discovered for most known tyrannosaurids. This has allowed a variety of research into their biology. Scientific studies have focused on their ontogeny, biomechanics and ecology, among other subjects. Soft tissue, both fossilized and intact, has been reported from one specimen of Tyrannosaurus rex.
- 1 Description
- 2 History of discovery
- 3 Distribution
- 4 Physiology
- 5 Paleoecology
- 6 Classification
- 7 Timeline of genera
- 8 References
- 9 External links
The tyrannosaurids were all large animals, with all species capable of weighing at least 1 metric ton. A single specimen of Alioramus of an individual estimated at between 5 and 6 metres (16 and 20 ft) long has been discovered, although it is considered by some experts to be a juvenile. Albertosaurus, Gorgosaurus and Daspletosaurus all measured between 8 and 10 metres (26 and 33 ft) long, while Tarbosaurus reached lengths of 12 metres (39 ft) from snout to tail. The massive Tyrannosaurus reached 12.3 metres (40 ft) in the largest specimen, FMNH PR2081.
Tyrannosaurid skull anatomy is well understood as complete skulls are known for all genera but Alioramus, which is known only from partial skull remains. Tyrannosaurus, Tarbosaurus, and Daspletosaurus had skulls which exceeded 1 metre (3 ft 3 in) in length, The largest discovered Tyrannosaurus skull measures over 1.5 metres (4 ft 11 in) long. Adult tyrannosaurids had tall, massive skulls, with many bones fused and reinforced for strength. At the same time, hollow chambers within many skull bones and large openings (fenestrae) between those bones helped to reduce skull weight. Many features of tyrannosaurid skulls were also found in their immediate ancestors, including tall premaxillae and fused nasal bones.
Tyrannosaurid skulls had many unique characteristics, including fused parietal bones with a prominent sagittal crest, which ran longitudinally along the sagittal suture and separated the two supratemporal fenestrae on the skull roof. Behind these fenestrae, tyrannosaurids had a characteristically tall nuchal crest, which also arose from the parietals but ran along a transverse plane rather than longitudinally. The nuchal crest was especially well-developed in Tyrannosaurus, Tarbosaurus and Alioramus. Albertosaurus, Daspletosaurus and Gorgosaurus had tall crests in front of the eyes on the lacrimal bones, while Tarbosaurus and Tyrannosaurus had extremely thickened postorbital bones forming crescent-shaped crests behind the eyes. Alioramus had a row of six bony crests on top of its snout, arising from the nasal bones; lower crests have been reported on some specimens of Daspletosaurus and Tarbosaurus, as well as the more basal tyrannosauroid Appalachiosaurus.
The skull was perched at the end of a thick, S-shaped neck, and a long, heavy tail acted as a counterweight to balance out the head and torso, with the center of mass over the hips. Tyrannosaurids are known for their proportionately very small two-fingered forelimbs, although remnants of a vestigial third digit are sometimes found. Tarbosaurus had the shortest forelimbs compared to its body size, while Daspletosaurus had the longest.
Tyrannosaurids walked exclusively on their hindlimbs, so their leg bones were massive. In contrast to the forelimbs, the hindlimbs were longer compared to body size than almost any other theropods. Juveniles and even some smaller adults, like more basal tyrannosauroids, had longer tibiae than femora, a characteristic of fast-running dinosaurs like ornithomimids. Larger adults had leg proportions characteristic of slower-moving animals, but not to the extent seen in other large theropods like abelisaurids or carnosaurs. The third metatarsals of tyrannosaurids were pinched between the second and fourth metatarsals, forming a structure known as the arctometatarsus.
It is unclear when the arctometatarsus first evolved; it was not present in the earliest tyrannosauroids like Dilong, but was found in the later Appalachiosaurus. This structure also characterized troodontids, ornithomimids and caenagnathids, but its absence in the earliest tyrannosauroids indicates that it was acquired by convergent evolution.
Tyrannosaurids, like their tyrannosauroid ancestors, were heterodont, with premaxillary teeth D-shaped in cross section and smaller than the rest. Unlike earlier tyrannosauroids and most other theropods, the maxillary and mandibular teeth of mature tyrannosaurids are not blade-like but extremely thickened and often circular in cross-section. Tooth counts tend to be consistent within species, and larger species tend to have lower tooth counts than smaller ones. For example, Alioramus had 76 to 78 teeth in its jaws, while Tyrannosaurus had between 54 and 60.
William Abler observed in 2001 that Albertosaurus tooth serrations resemble a crack in the tooth ending in a round void called an ampulla. Tyrannosaurid teeth were used as holdfasts for pulling meat off a body, so when a tyrannosaur would have pulled back on a piece of meat, the tension could cause a purely crack-like serration to spread through the tooth. However, the presence of the ampulla would have distributed these forces over a larger surface area, and lessened the risk of damage to the tooth under strain. The presence of incisions ending in voids has parallels in human engineering. Guitar makers use incisions ending in voids to, as Abler describes, "impart alternating regions of flexibility and rigidity" to the wood they work with. The use of a drill to create an "ampulla" of sorts and prevent the propagation of cracks through material is also used to protect airplane surfaces. Abler demonstrated that a plexiglass bar with incisions called "kerfs" and drilled holes was more than 25% stronger than one with only regularly placed incisions. Unlike tyrannosaurs, ancient predators like phytosaurs and Dimetrodon had no adaptations to prevent the crack-like serrations of their teeth from spreading when subjected to the forces of feeding.
History of discovery
The first remains of tyrannosaurids were uncovered during expeditions led by the Geological Survey of Canada, which located numerous scattered teeth. These distinctive dinosaur teeth were given the name Deinodon ("terrible tooth") by Joseph Leidy in 1856. The first good specimens of a tyrannosaurid were found in the Horseshoe Canyon Formation of Alberta, and consisted of nearly complete skulls with partial skeletons. These remains were first studied by Edward Drinker Cope in 1876, who considered them a species of the eastern tyrannosauroid Dryptosaurus. In 1905, Henry Fairfield Osborn recognized that the Alberta remains differed considerably from Dryptosaurus, and coined a new name for them: Albertosaurus sarcophagus ("flesh-eating Alberta lizard"). Cope described more tyrannosaur material in 1892, in the form of isolated vertebrae, and gave this animal the name Manospondylus gigas. This discovery was mostly overlooked for over a century, and caused controversy in the early 2000s when it was discovered that this material actually belonged to, and had name priority over, Tyrannosaurus rex.
In his 1905 paper naming Albertosaurus, Osborn described two additional tyrannosaur specimens that had been collected from in Montana and Wyoming during a 1902 expedition of the American Museum of Natural History, led by Barnum Brown. Initially, Osborn considered these to be distinct species. The first, he named Dynamosaurus imperiosus ("emperor power lizard"), and the second, Tyrannosaurus rex ("king tyrant lizard"). A year later, Osborn recognized that these two specimens actually came from the same species. Despite the fact that Dynamosaurus had been found first, the name Tyrannosaurus had appeared one page earlier in his original article describing both specimens. Therefore, according to the International Code of Zoological Nomenclature (ICZN), the name Tyrannosaurus was used.
Barnum Brown went on to collect several more tyrannosaurid specimens from Alberta, including the first to preserve the shortened, two-fingered forelimbs characteristic of the group (which Lawrence Lambe named Gorgosaurus libratus, "balanced fierce lizard", in 1914). A second significant find attributed to Gorgosaurus was made in 1942, in the form of a well-preserved, though unusually small, complete skull. The specimen waited until after the end of World War II to be studied by Charles W. Gilmore, who named it Gorgosaurus lancesnis. This skull was re-studied by Robert T. Bakker, Phil Currie, and Michael Williams in 1988, and assigned to the new genus Nanotyrannus. It was also in 1946 that paleontologists from the Soviet Union began expeditions into Mongolia, and uncovered the first tyrannosaur remains from Asia. Evgeny Maleev described new Mongolian species of Tyrannosaurus and Gorgosaurus in 1955, and one new genus: Tarbosaurus ("terrifying lizard"). Subsequent studies, however, showed that all of Maleev's tyrannosaur species were actually one species of Tarbosaurus at different stages of growth. A second species of Mongolian tyrannosaurid was found later, described by Sergei Kurzanov in 1976, and given the name Alioramus remotus ("remote different branch"), though its status as a true tyrannosaurid and not a more primitive tyrannosaur is still controversial.
While earlier tyrannosauroids are found on all three northern continents, tyrannosaurid fossils are known only from North America and Asia. Sometimes fragmentary remains uncovered in the Southern Hemisphere have been reported as "Southern Hemisphere tyrannosaurids," although these seem to have been misidentified abelisaurid fossils. The exact time and place of origin of the family remain unknown due to the poor fossil record in the middle part of the Cretaceous on both continents, although the earliest confirmed tyrannosaurids lived in the early Campanian stage in western North America.
Tyrannosaurid remains have never been recovered from eastern North America, while more basal tyrannosauroids like Dryptosaurus and Appalachiosaurus persisted there until the end of the Cretaceous, indicating that tyrannosaurids must have evolved in or dispersed into western North America after the continent was divided in half by the Western Interior Seaway in the middle of the Cretaceous. Tyrannosaurid fossils have been found in Alaska, which may have provided a route for dispersal between North America and Asia. Alioramus and Tarbosaurus are found to be related in one cladistic analysis, forming a unique Asian branch of the family.
Of the two subfamilies, tyrannosaurines appear to have been more widespread. Albertosaurines are unknown in Asia, which was home to the tyrannosaurines Tarbosaurus and Alioramus. Both subfamilies were present in the Campanian and early Maastrichtian stages of North America, with tyrannosaurines like Daspletosaurus ranging throughout the Western Interior, while the albertosaurines Albertosaurus and Gorgosaurus are currently known only from the northwestern part of the continent.
By the late Maastrichtian, albertosaurines appear to have gone extinct, while the tyrannosaurine Tyrannosaurus roamed from Saskatchewan to Texas. This pattern is mirrored in other North American dinosaur taxa. During the Campanian and early Maastrichtian, lambeosaurine hadrosaurs and centrosaurine ceratopsians are common in the northwest, while hadrosaurines and chasmosaurines were more common to the south. By the end of the Cretaceous, centrosaurines are unknown and lambeosaurines are rare, while hadrosaurines and chasmosaurines were common throughout the Western Interior.
Paleontologist Gregory Erickson and colleagues have studied the growth and life history of tyrannosaurids. Analysis of bone histology can determine the age of a specimen when it died. Growth rates can be examined when the age of various individuals are plotted against their size on a graph. Erickson has shown that after a long time as juveniles, tyrannosaurs underwent tremendous growth spurts for about four years midway through their lives. After the rapid growth phase ended with sexual maturity, growth slowed down considerably in adult animals. A tyrannosaurid growth curve is S-shaped, with the maximum growth rate of individuals around 14 years of age.
The smallest known Tyrannosaurus rex individual (LACM 28471, the "Jordan theropod") is estimated to have weighed only 29.9 kilograms (66 lb) at only 2 years old, while the largest, such as FMNH PR2081 ("Sue") most likely weighed over 5,400 kg (11,900 lb), estimated to have been 28 years old, an age which may have been close to the maximum for the species. T. rex juveniles remained under 1,800 kg (4,000 lb) until approximately 14 years of age, when body size began to increase dramatically. During this rapid growth phase, a young T. rex would gain an average of 600 kg (1,300 lb) a year for the next four years. This slowed after 16 years, and at 18 years of age, the curve plateaus again, indicating that growth slowed dramatically. For example, only 600 kg (1,300 lb) separated the 28-year-old "Sue" from a 22-year-old Canadian specimen (RTMP 81.12.1). This sudden change in growth rate may indicate physical maturity, a hypothesis which is supported by the discovery of medullary tissue in the femur of an 18-year-old T. rex from Montana (MOR 1125, also known as "B-rex"). Medullary tissue is found only in female birds during ovulation, indicating that "B-rex" was of reproductive age.
Other tyrannosaurids exhibit extremely similar growth curves, although with lower growth rates corresponding to their lower adult sizes. Compared to albertosaurines, Daspletosaurus showed a faster growth rate during the rapid growth period due to its higher adult weight. The maximum growth rate in Daspletosaurus was 180 kilograms (400 lb) per year, based on a mass estimate of 1,800 kg (4,000 lb) in adults. Other authors have suggested higher adult weights for Daspletosaurus; this would change the magnitude of the growth rate but not the overall pattern. The youngest known Albertosaurus is a two-year-old discovered in the Dry Island bonebed, which would have weighed about 50 kg (110 lb) and measured slightly more than 2 metres (6 ft 7 in) in length. The 10-metre (33 ft) specimen from the same quarry is the oldest and largest known, at 28 years of age. The fastest growth rate is estimated to be around 12–16 years, reaching 122 kilograms (269 lb) per year, based on an adult 1,300 kilograms (2,900 lb) which is about five times slower than for T.-rex. For Gorgosaurus the calculated maximum growth rate is about 110 kilograms (240 lb) during the rapid growth phase, which is comparable to that of Albertosaurus.
The end of the rapid growth phase suggests the onset of sexual maturity in Albertosaurus, although growth continued at a slower rate throughout the animals' lives. Sexual maturation while still actively growing appears to be a shared trait among small and large dinosaurs as well as in large mammals such as humans and elephants. This pattern of relatively early sexual maturation differs strikingly from the pattern in birds, which delay their sexual maturity until after they have finished growing.
By tabulating the number of specimens of each age group, Erickson and his colleagues were able to draw conclusions about life history in tyranosauridae populations. Their analysis showed that while juveniles were rare in the fossil record, subadults in the rapid growth phase and adults were far more common. Over half of the known T. rex specimens appear to have died within six years of reaching sexual maturity, a pattern which is also seen in other tyrannosaurs and in some large, long-lived birds and mammals today. These species are characterized by high infant mortality rates, followed by relatively low mortality among juveniles. Mortality increases again following sexual maturity, partly due to the stresses of reproduction. While this could be due to preservation or collection biases, Erickson hypothesized that the difference was due to low mortality among juveniles over a certain size, which is also seen in some modern large mammals like elephants. This low mortality may have resulted from a lack of predation, since tyrannosaurs surpassed all contemporaneous predators in size by the age of two. Paleontologists have not found enough Daspletosaurus remains for a similar analysis, but Erickson notes that the same general trend seems to apply.
The tyrannosaurids spent as much as half its life in the juvenile phase before ballooning up to near-maximum size in only a few years. This, along with the complete lack of predators intermediate in size between huge adult tyrannosaurids and other small theropods, suggests these niches may have been filled by juvenile tyrannosaurids. This is seen in modern Komodo dragons, where hatchlings start off as tree-dwelling insectivores and slowly mature into massive apex predators capable of taking down large vertebrates. For example, Albertosaurus have been found in aggregations that some have suggested to represent mixed-age packs.
Locomotion abilities are best studied for Tyrannosaurus and there are two main issues concerning this: how well it could turn; and what its maximum straight-line speed was likely to have been.Tyrannosaurus may have been slow to turn, possibly taking one to two seconds to turn only 45° – an amount that humans, being vertically oriented and tail-less, can spin in a fraction of a second. The cause of the difficulty is rotational inertia, since much of Tyrannosaurus’ mass was some distance from its center of gravity, like a human carrying a heavy timber.
Scientists have produced a wide range of maximum speed estimates, mostly around 11 metres per second (25 mph), but a few as low as 5–11 metres per second (11–25 mph), and a few as high as 20 metres per second (45 mph). Researchers have to rely on various estimating techniques because, while there are many tracks of very large theropods walking, so far none have been found of very large theropods running — and this absence may indicate that they did not run.
Jack Horner and Don Lessem argued in 1993 that Tyrannosaurus was slow and probably could not run (no airborne phase in mid-stride). However, Holtz (1998) concluded that tyrannosaurids and their close relatives were the fastest large theropods. Christiansen (1998) estimated that the leg bones of Tyrannosaurus were not significantly stronger than those of elephants, which are relatively limited in their top speed and never actually run (there is no airborne phase), and hence proposed that the dinosaur's maximum speed would have been about 11 metres per second (25 mph), which is about the speed of a human sprinter. Farlow and colleagues (1995) have argued that a 6-8 ton Tyrannosaurus would have been critically or even fatally injured if it had fallen while moving quickly, since its torso would have slammed into the ground at a deceleration of 6 g (six times the acceleration due to gravity, or about 60 meters/s²) and its tiny arms could not have reduced the impact. However, giraffes have been known to gallop at 50 km/h (31 mph), despite the risk that they might break a leg or worse, which can be fatal even in a "safe" environment such as a zoo. Thus it is quite possible that Tyrannosaurus also moved fast when necessary and had to accept such risks; this scenario has been studied for Allosaurus too. Most recent research on Tyrannosaurus locomotion does not narrow down speeds further than a range from 17 to 40 kilometres per hour (11 to 25 mph), i.e. from walking or slow running to moderate-speed running. A computer model study in 2007 estimated running speeds, based on data taken directly from fossils, and claimed that T. rex had a top running speed of 8 metres per second (18 mph). (probably a juvenile individual).
Long filamentous structures have been preserved along with skeletal remains of numerous coelurosaurs from the Early Cretaceous Yixian Formation and other nearby geological formations from Liaoning, China. These filaments have usually been interpreted as "protofeathers," homologous with the branched feathers found in birds and some non-avian theropods, although other hypotheses have been proposed. A skeleton of Dilong was described in 2004 that included the first example of "protofeathers" in a tyrannosauroid. Similarly to down feathers of modern birds, the "protofeathers" found in Dilong were branched but not pennaceous, and may have been used for insulation.
It has also been theoretized that tyrannosaurids had such protofeathers. However, rare skin impressions from adult tyrannosaurids in Canada and Mongolia show pebbly scales typical of other dinosaurs. While it is possible that protofeathers existed on parts of the body which have not been preserved, a lack of insulatory body covering is consistent with modern multi-ton mammals such as elephants, hippopotamus, and most species of rhinoceros. As an object increases in size, its ability to retain heat increases due to its decreasing surface area-to-volume ratio. Therefore, as large animals evolve in or disperse into warm climates, a coat of fur or feathers loses its selective advantage for thermal insulation and can instead become a disadvantage, as the insulation traps excess heat inside the body, possibly overheating the animal. Protofeathers may also have been secondarily lost during the evolution of large tyrannosaurids, especially in warm Cretaceous climates.
The eye-sockets of Tyrannosaurus are positioned so that the eyes would point forward, giving them binocular vision slightly better than that of modern hawks. Jack Horner also pointed out that the tyrannosaur lineage had a history of steadily improving binocular vision. It is hard to see how natural selection would have favored this long-term trend if tyrannosaurs had been pure scavengers, which would not have needed the advanced depth perception that stereoscopic vision provides. In modern animals, binocular vision is found mainly in predators (the principal exceptions are primates, which need it for leaping from branch to branch). Unlike Tyrannosaurus, Tarbosaurus had a narrower skull more typical of other tyrannosaurids in which the eyes faced primarily sideways. All of this suggests that Tarbosaurus relied more on its senses of smell and hearing than on its eyesight. In Gorgosaurus specimens, the eye socket was circular rather than oval or keyhole-shaped as in other tyrannosaurid genera. In Daspletosaurus this was a tall oval, somewhere in between the circular shape seen in Gorgosaurus and the 'keyhole' shape of Tyrannosaurus.
Bony crests are found on the skulls of many theropods, including many of tyrannosaurids. Alioramus, a possible tyrannosaurid from Mongolia, bears a single row of five prominent bony bumps on the nasal bones; a similar row of much lower bumps is present on the skull of Appalachiosaurus, as well as some specimens of Daspletosaurus, Albertosaurus, and Tarbosaurus. In Albertosaurus, Gorgosaurus and Daspletosaurus, there is a prominent horn in front of each eye on the lacrimal bone. The lacrimal horn is absent in Tarbosaurus and Tyrannosaurus, which instead have a crescent-shaped crest behind each eye on the postorbital bone. These head crests may have been used for display, perhaps for species recognition or courtship behavior.
Tyrannosaurus, like most dinosaurs, was long thought to have an ectothermic ("cold-blooded") reptilian metabolism but was challenged by scientists like Robert T. Bakker and John Ostrom in the early years of the "Dinosaur Renaissance", beginning in the late 1960s. Tyrannosaurus rex itself was claimed to have been endothermic ("warm-blooded"), implying a very active lifestyle. Since then, several paleontologists have sought to determine the ability of Tyrannosaurus to regulate its body temperature. Histological evidence of high growth rates in young T. rex, comparable to those of mammals and birds, may support the hypothesis of a high metabolism. Growth curves indicate that, as in mammals and birds, T. rex growth was limited mostly to immature animals, rather than the indeterminate growth seen in most other vertebrates. It has been indicated that the temperature difference may have been no more than 4 to 5 °C (7 to 9 °F) between the vertebrae of the torso and the tibia of the lower leg. This small temperature range between the body core and the extremities was claimed by paleontologist Reese Barrick and geochemist William Showers to indicate that T. rex maintained a constant internal body temperature (homeothermy) and that it enjoyed a metabolism somewhere between ectothermic reptiles and endothermic mammals. Later they found similar results in Giganotosaurus specimens, who lived on a different continent and tens of millions of years earlier in time. Even if Tyrannosaurus rex does exhibit evidence of homeothermy, it does not necessarily mean that it was endothermic. Such thermoregulation may also be explained by gigantothermy, as in some living sea turtles.
Coexistence of Daspletosaurus and Gorgosaurus
In the Dinosaur Park Formation, Gorgosaurus lived alongside a rarer species of the tyrannosaurine Daspletosaurus. This is one of the few examples of two tyrannosaur genera coexisting. Similarly-sized predators in modern predator guilds are separated into different ecological niches by anatomical, behavioral or geographical differences that limit competition. Niche differentiation between the Dinosaur Park tyrannosaurids is not well-understood. In 1970, Dale Russell hypothesized the more common Gorgosaurus actively hunted fleet-footed hadrosaurs, while the rarer and more troublesome ceratopsians and ankylosaurians (horned and heavily armoured dinosaurs) were left to the more heavily built Daspletosaurus. However, a specimen of Daspletosaurus (OTM 200) from the contemporaneous Two Medicine Formation of Montana preserves the digested remains of a juvenile hadrosaur in its gut region. Unlike some other groups of dinosaurs, neither genus was more common at higher or lower elevations than the other. However, Gorgosaurus appears more common in northern formations like the Dinosaur Park, with species of Daspletosaurus more abundant to the south. The same pattern is seen in other groups of dinosaurs. Chasmosaurine ceratopsians and hadrosaurine hadrosaurs are also more common in the Two Medicine Formation of Montana and in southwestern North America during the Campanian, while centrosaurine and lambeosaurines dominate in northern latitudes. Holtz has suggested this pattern indicates shared ecological preferences between tyrannosaurines, chasmosaurines and hadrosaurines. At the end of the later Maastrichtian stage, tyrannosaurines like Tyrannosaurus rex, hadrosaurines like Edmontosaurus and chasmosaurines like Triceratops were widespread throughout western North America, while albertosaurines and centrosaurines went extinct, and lambeosaurines were rare.
There is limited evidence of social behavior among the tyrannosaurids. For example, the "Sue" T.-rex specimen apparently died from a massive bite to the head, which could only have been inflicted by another tyrannosaur. Researchers reported that a subadult and a juvenile skeleton were found in the same quarry as the "Sue" specimen, which has been used to support the hypothesis that tyrannosaurs may have lived in social groups of some kind. While there is no evidence of gregarious behavior in Gorgosaurus, there is evidence of some pack behavior for Albertosaurus and Daspletosaurus.
A young specimen of the Dinosaur Park Daspletosaurus species (TMP 94.143.1) shows bite marks on the face that were inflicted by another tyrannosaur. The bite marks are healed over, indicating that the animal survived the bite. A full-grown Dinosaur Park Daspletosaurus (TMP 85.62.1) also exhibits tyrannosaur bite marks, showing that attacks to the face were not limited to younger animals. While it is possible that the bites were attributable to other species, intraspecific aggression, including facial biting, is very common among predators. Facial bites are seen in other tyrannosaurs like Gorgosaurus and Tyrannosaurus, as well as in other theropod genera like Sinraptor and Saurornitholestes. Darren Tanke and Phil Currie hypothesize that the bites are due to intraspecific competition for territory or resources, or for dominance within a social group.
Evidence that Daspletosaurus lived in social groups comes from a bonebed found in the Two Medicine Formation of Montana. The bonebed includes the remains of three Daspletosaurus, including a large adult, a small juvenile, and another individual of intermediate size. At least five hadrosaurs are preserved at the same location. Geologic evidence indicates that the remains were not brought together by river currents but that all of the animals were buried simultaneously at the same location. The hadrosaur remains are scattered and bear many marks from tyrannosaur teeth, indicating that the Daspletosaurus were feeding on the hadrosaurs at the time of death. The cause of death is unknown. Currie speculates that the daspletosaurs formed a pack, although this cannot be stated with certainty. Other scientists are skeptical of the evidence for social groups in Daspletosaurus and other large theropods; Brian Roach and Daniel Brinkman have suggested that Daspletosaurus social interaction would have more closely resembled the modern Komodo dragon, where non-cooperative individuals mob carcasses, frequently attacking and even cannibalizing each other in the process.
The Dry Island bonebed discovered by Barnum Brown and his crew contains the remains of 22 Albertosaurus, the most individuals found in one locality of any Cretaceous theropod, and the second-most of any large theropod dinosaur behind the Allosaurus assemblage at the Cleveland Lloyd Dinosaur Quarry in Utah. The group seems to be composed of one very old adult; eight adults between 17 and 23 years old; seven sub-adults undergoing their rapid growth phases at between 12 and 16 years old; and six juveniles between the ages of 2 and 11 years, who had not yet reached the growth phase. The near-absence of herbivore remains and the similar state of preservation between the many individuals at the Albertosaurus bonebed quarry led Phil Currie to conclude that the locality was not a predator trap like the La Brea Tar Pits in California, and that all of the preserved animals died at the same time. Currie claims this as evidence of pack behavior. Other scientists are skeptical, observing that the animals may have been driven together by drought, flood or for other reasons.
Tyrannosaur tooth marks are the most commonly preserved feeding traces of carnivorous dinosaurs. They have been reported from ceratopsians, hadrosaurs and other tyrannosaurs. Tyrannosaurid bones with tooth marks represent about 2% of known fossils with preserved tooth marks. Tyrannosaurid teeth were used as holdfasts for pulling meat off a body, rather than knife-like cutting functions. Tooth wear patterns hint that complex head shaking behaviors may have been involved in tyrannosaur feeding.
Speculation on the pack-hunting habits of Albertosaurus were made by a few researchers who suggest that the younger members of the pack may have been responsible for driving their prey towards the adults, who were larger and more powerful, but also slower. Juveniles may also have had different lifestyles than adults, filling predator niches between those of the enormous adults and the smaller contemporaneous theropods, the largest of which were two orders of magnitude smaller than an adult Albertosaurus in mass. However, as the preservation of behavior in the fossil record is exceedingly rare, these ideas cannot readily be tested. Phil Currie speculates that the Daspletosaurus formed packs to hunt, although this cannot be stated with certainty. There is no evidence of such gregarious behavior in Gorgosaurus.
The debate about whether Tyrannosaurus was a predator or a pure scavenger is as old as the debate about its locomotion. Lambe (1917) described a good skeleton of Tyrannosaurus’ close relative Gorgosaurus and concluded that it and therefore also Tyrannosaurus was a pure scavenger, because the Gorgosaurus’ teeth showed hardly any wear. This argument is no longer taken seriously, because theropods replaced their teeth quite rapidly. Ever since the first discovery of Tyrannosaurus most scientists have agreed that it was a predator, although like modern large predators it would have been happy to scavenge or steal another predator's kill if it had the opportunity.
Noted hadrosaur expert Jack Horner is currently the major advocate of the idea that Tyrannosaurus was exclusively a scavenger and did not engage in active hunting at all. Horner has presented several arguments to support the pure scavenger hypothesis. The presence of large olfactory bulbs and olfactory nerves suggests a highly developed sense of smell for sniffing out carcasses over great distances. The teeth could crush bone, and therefore could extract as much food (bone marrow) as possible from carcass remnants, usually the least nutritious parts. At least some of its potential prey could move quickly, while evidence suggests that it walked instead of ran.
Other evidence suggests hunting behavior in Tyrannosaurus. The eye-sockets of tyrannosaurs are positioned so that the eyes would point forward, giving them binocular vision slightly better than that of modern hawks. Tyrannosaur-inflicted damage has been found on skeletons of hadrosaurs and Triceratops that seemed to have survived initial attacks. Some researchers argue that if Tyrannosaurus were a scavenger, another dinosaur had to be the top predator in the Amerasian Upper Cretaceous. The top prey were the larger marginocephalians and ornithopods. The other tyrannosaurids share so many characteristics with Tyrannosaurus that only small dromaeosaurs remain as feasible top predators. In this light, scavenger hypothesis adherents have suggested that the size and power of tyrannosaurs allowed them to steal kills from smaller predators. Most paleontologists accept that Tyrannosaurus was both an active predator and a scavenger.
The name Deinodontidae was coined by Edward Drinker Cope in 1866 for this family, and continued to be used in place of the newer name Tyrannosauridae through the 1960s. The type genus of the Deinodontidae is Deinodon, which was named after isolated teeth from Montana. However, in a 1970 review of North American tyrannosaurs, Dale Russell concluded that Deinodon was not a valid taxon, and used the name Tyrannosauridae in place of Deinodontidae, stating that this was in accordance with ICZN rules. Therefore, Tyrannosauridae is preferred by modern experts.
Tyrannosaurus was named by Henry Fairfield Osborn in 1905, along with the family Tyrannosauridae. The name is derived from the Ancient Greek words τυραννος/tyrannos ('tyrant') and σαυρος/sauros ('lizard'). The very common suffix -idae is normally appended to zoological family names and is derived from the Greek suffix -ιδαι/-idai, which indicates a plural noun.
Tyrannosauridae is uncontroversially divided into two subfamilies. Albertosaurinae comprises the North American genera Albertosaurus and Gorgosaurus, while Tyrannosaurinae includes Daspletosaurus, Teratophoneus, Alioramus, Tarbosaurus, Nanotyrannus, Zhuchengtyrannus, and Tyrannosaurus itself. Some authors include the species Gorgosaurus libratus in the genus Albertosaurus and Tarbosaurus bataar in the genus Tyrannosaurus, while others prefer to retain Gorgosaurus and Tarbosaurus as separate genera. Albertosaurines are characterized by more slender builds, lower skulls, and proportionately longer tibiae than tyrannosaurines. In tyrannosaurines, the sagittal crest on the parietals continues forward onto the frontals. Some authors, such as George Olshevsky and Tracy Ford, have created finer subdivisions or tribes for various combinations of tyrannosaurs within the subfamilies. However, these have not been phylogenetically defined, and usually consisted of genera which are now considered synonymous with other genera or species.
Additional subfamilies have been named for more fragmentary genera, including Aublysodontinae and Deinodontinae. However, the genera Aublysodon and Deinodon are usually considered nomina dubia, so they and their eponymous subfamilies are usually excluded from taxonomies of tyrannosaurids. An additional tyrannosaurid, Raptorex, was initially described as a more primitive tyrannosauroid, but likely represents a juvenile tyrannosaurine similar to Tarbosaurus. However, as it is known only from a juvenile specimen, it is also currently considered a nomen dubium.
With the advent of phylogenetic taxonomy in vertebrate paleontology, Tyrannosauridae has been given several explicit definitions. The original was produced by Paul Sereno in 1998, and included all tyrannosauroids closer to Tyrannosaurus than to either Alectrosaurus, Aublysodon or Nanotyrannus. However, Nanotyrannus is often considered to be a juvenile Tyrannosaurus rex, while Aublysodon is usually regarded as a nomen dubium unsuitable for use in the definition of a clade. Definitions since then have been based on more well-established genera.
In 2001 Thomas R. Holtz, Jr. published a cladistic analysis of the tyrannosauridae. He concluded that there were two subfamilies, a more primitive Aublysodontinae "characterized by unserrated premaxillary teeth," and the tyrannosaurinae. The Aublysodontinae included Aublysodon, the "Kirtland Aublysodon", and Alectrosaurus. Holtz also found that Siamotyrannus exhibited some of the synapomorphies of the tyrannosauridae, but lay "outside the [family] proper."
Later in the same paper he proposed that Tyrannosauridae be defined as "all descendants of the most recent common ancestor of Tyrannosaurus and Aublysodon." He also criticized definitions previously proposed by other workers, like one proposed by Paul Sereno, that the Tyrannosauridae was "all taxa closer to "Tyrannosaurus" than to Alectrosaurus, Aublysodon, and Nanotyrannus." Holtz observed that since Nanotyrannus was probably a misidentified T. rex juvenile, Sereno's proposed definition would have the family Tyrannosauridae as a subtaxon of the genus Tyrannosaurus! Further, his proposed definition of the subfamily Tyrannosaurinae would also be limited to Tyrannosaurus.
A 2003 attempt by Christopher Brochu included Albertosaurus, Alectrosaurus, Alioramus, Daspletosaurus, Gorgosaurus, Tarbosaurus and Tyrannosaurus in the definition. Holtz redefined the clade in 2004 to use all of the above as specifiers except for Alioramus and Alectrosaurus, which his analysis could not place with certainty. However, in the same paper, Holtz also provided a completely different definition, including all theropods more closely related to Tyrannosaurus than to Eotyrannus. The most recent definition is that of Sereno in 2005, which defined Tyrannosauridae as the least inclusive clade containing Albertosaurus, Gorgosaurus and Tyrannosaurus.
Cladistic analyses of tyrannosaurid phylogeny often find Tarbosaurus and Tyrannosaurus to be sister taxa, with Daspletosaurus more basal than either. A close relationship between Tarbosaurus and Tyrannosaurus is supported by numerous skull features, including the pattern of sutures between certain bones, the presence of a crescent-shaped crest on the postorbital bone behind each eye, and a very deep maxilla with a noticeable downward curve on the lower edge, among others. An alternative hypothesis was presented in a 2003 study by Phil Currie and colleagues, which found weak support for Daspletosaurus as a basal member of a clade also including Tarbosaurus and Alioramus, both from Asia, based on the absence of a bony prong connecting the nasal and lacrimal bones. Alioramus was found to be the closest relative of Tarbosaurus in this study, based on a similar pattern of stress distribution in the skull.
A related study also noted a locking mechanism in the lower jaw shared between the two genera. In a separate paper, Currie noted the possibility that Alioramus might represent a juvenile Tarbosaurus, but stated that the much higher tooth count and more prominent nasal crests in Alioramus suggest it is a distinct genus. Similarly, Currie uses the high tooth count of Nanotyrannus to suggest that it may be a distinct genus, rather than a juvenile Tyrannosaurus as most other experts believe. The discovery and description of Qianzhousaurus however, reveals that Alioramus is not a close relation to Tarbosaurus, instead belonging to a newly described family of tyrannosaurids; the Alioramini. Qianzhousaurus further reveals that similar long-snouted tyrannosaurids were widely distributed throughout Asia and would have shared the same environment while avoiding competition with larger and more robust tyrannosaurines by hunting different prey.
Timeline of genera
||This article uses bare URLs for citations, which may be threatened by link rot. (May 2014)|
- Holtz, Thomas R. Jr. (2012) Dinosaurs: The Most Complete, Up-to-Date Encyclopedia for Dinosaur Lovers of All Ages, Winter 2011 Appendix.
- Hutchinson, John R.; Bates, Karl T.; Molnar, Julia; Allen, Vivian; Makovicky, Peter J.; Claessens, Leon (2011). "A Computational Analysis of Limb and Body Dimensions in Tyrannosaurus rex with Implications for Locomotion, Ontogeny, and Growth". PLoS ONE 6 (10): e26037. doi:10.1371/journal.pone.0026037.
- Erickson, Gregory M., GM; Makovicky, Peter J.; Currie, Philip J.; Norell, Mark A.; Yerby, Scott A.; & Brochu, Christopher A. (2004). "Gigantism and comparative life-history parameters of tyrannosaurid dinosaurs". Nature 430 (7001): 772–775. doi:10.1038/nature02699. PMID 15306807. "Sampled longevities for T. rex ranged from 2 to 28 years" and corresponding body mass estimates ranged from 29.9 to 5654 kg
- Holtz, Thomas R. (2004). "Tyrannosauroidea". In Weishampel, David B.; Dodson, Peter; & Osmólska, Halszka (eds.). The Dinosauria (Second ed.). Berkeley: University of California Press. pp. 111–136. ISBN 0-520-24209-2.
- Kurzanov, Sergei M.. "A new carnosaur from the Late Cretaceous of Nogon-Tsav, Mongolia". The Joint Soviet-Mongolian Paleontological Expedition Transactions (in Russian) 3: 93–104.
- Currie, Philip J. (2003). "Cranial anatomy of tyrannosaurids from the Late Cretaceous of Alberta". Acta Palaeontologica Polonica 48 (2): 191–226.
- Russell, Dale A. (1970). "Tyrannosaurs from the Late Cretaceous of western Canada". National Museum of Natural Sciences Publications in Paleontology 1: 1–34.
- Maleev, Evgeny A. (1955). "New carnivorous dinosaurs from the Upper Cretaceous of Mongolia". Doklady Akademii Nauk SSSR (in Russian) 104 (5): 779–783.
- Currie, Philip J. (2000). "Theropods from the Cretaceous of Mongolia". The Age of Dinosaurs in Russia and Mongolia. Cambridge: Cambridge University Press. pp. 434–455. ISBN 978-0-521-54582-2.
- "Museum unveils world's largest T-rex skull". Montana State University. 7 April 2006. Retrieved 13 September 2008.
- Carr, Thomas D.; Williamson, Thomas E.; Schwimmer, David R. (2005). "A new genus and species of tyrannosauroid from the Late Cretaceous (middle Campanian) Demopolis Formation of Alabama". Journal of Vertebrate Paleontology 25 (1): 119–143. doi:10.1671/0272-4634(2005)025[0119:ANGASO]2.0.CO;2. ISSN 0272-4634.
- Quinlan, Elizabeth D.; Derstler, Kraig; Miller, Mercedes M. (2007). "Anatomy and function of digit III of the Tyrannosaurus rex manus". Geological Society of America Annual Meeting — Abstracts with Programs: 77. [abstract only]
- Xu Xing, X; Norell, Mark A.; Kuang Xuewen; Wang Xiaolin; Zhao Qi; Jia Chengkai. (2004). "Basal tyrannosauroids from China and evidence for protofeathers in tyrannosauroids". Nature 431 (7009): 680–684. doi:10.1038/nature02855. PMID 15470426.
- Holtz, Thomas R. (1994). "The phylogenetic position of the Tyrannosauridae: implications for theropod systematics". Journal of Palaeontology 68 (5): 1100–1117. JSTOR 1306180.
- Currie, Philip J.; Hurum, Jørn H; Sabath, Karol. (2003). "Skull structure and evolution in tyrannosaurid phylogeny". Acta Palaeontologica Polonica 48 (2): 227–234.
- Abler, W.L. 2001. A kerf-and-drill model of tyrannosaur tooth serrations. p. 84–89. In: Mesozioc Vertebrate Life. Ed.s Tanke, D. H., Carpenter, K., Skrepnick, M. W. Indiana University Press.
- Carpenter, K. (1992). "Tyrannosaurs (Dinosauria) of Asia and North America." Pp. 250–268 in Mateer, N. and Chen, P.−J. (eds.), Aspects of Nonmarine Cretaceous Geology. Beijing: China Ocean Press.
- Breithaup, BH; Southwell EH; Matthews NA (2006). "Dynamosaurus imperiosus and the earliest discoveries of Tyrannosaurus rex in Wyoming and the West". New Mexico Museum of Natural History and Science Bulletin 35: 257–258.
- Bakker R.T, Williams M., Currie P. (1988). "Nanotyrannus, a new genus of pygmy tyrannosaur, from the latest Cretaceous of Montana". Hunteria 1: 1–30.
- Dodson, Peter & Britt, Brooks & Carpenter, Kenneth & Forster, Catherine A. & Gillette, David D. & Norell, Mark A. & Olshevsky, George & Parrish, J. Michael & Weishampel, David B. (1993). "Abelisaurus". Age of Dinosaurs. Publications International, LTD. p. 105. ISBN 0-7853-0443-6.
- Fiorillo, Anthony R.; Gangloff, Roland A. (2000). "Theropod teeth from the Prince Creek Formation (Cretaceous) of northern Alaska, with speculations on arctic dinosaur paleoecology". Journal of Vertebrate Paleontology 20 (4): 675–682. doi:10.1671/0272-4634(2000)020[0675:TTFTPC]2.0.CO;2. ISSN 0272-4634.
- Thomas R. Holtz, Jr. (1994). "The Phylogenetic Position of the Tyrannosauridae: Implications for Theropod Systematics". Journal of Paleontology 68 (5): 1100–1117. JSTOR 1306180.
- Horner, J.R. & Padian, K. (2004). "Age and growth dynamics of Tyrannosaurus rex". Proceedings of the Royal Society of London B 271 (1551): 1875–1880. doi:10.1098/rspb.2004.2829. PMC 1691809. PMID 15347508.
- Lee, Andrew H.; Werning, Sarah (2008). "Sexual maturity in growing dinosaurs does not fit reptilian growth models". Proceedings of the National Academy of Sciences 105 (2): 582–587. doi:10.1073/pnas.0708903105. PMC 2206579. PMID 18195356.
- Schweitzer, M.H., Wittmeyer, J.L., & Horner, J.R. (2005). "Gender-specific reproductive tissue in ratites and Tyrannosaurus rex". Science 308 (5727): 1456–1460. doi:10.1126/science.1112158. PMID 15933198.
- Erickson, G.M., Currie, P.J., Inouye, B.D., & Winn, A.A. (2006). "Tyrannosaur life tables: an example of nonavian dinosaur population biology". Science 313 (5784): 213–217. doi:10.1126/science.1125721. PMID 16840697.
- Erickson, Gregory M.; Curry Rogers, Kristi; Varricchio, David J.; Norell, Mark.; & Xu, Xing (2007). "Growth patterns in brooding dinosaurs reveals the timing of sexual maturity in non-avian dinosaurs and genesis of the avian condition". Biology Letters 3 (5): 558–561. doi:10.1098/rsbl.2007.0254. PMC 2396186. PMID 17638674.
- Lee, Andrew H.; Werning, Sarah (2008). "Sexual maturity in growing dinosaurs does not fit reptilian growth models". PNAS 105 (2): 582–587. doi:10.1073/pnas.0708903105. PMC 2206579. PMID 18195356.
- Ricklefs, Robert E. (2007). "Tyrannosaur ageing". Biology Letters 3 (2): 214–217. doi:10.1098/rsbl.2006.0597. PMC 2375931. PMID 17284406.
- Tanke, Darren H.; Currie, Philip J. (1998). "Head-biting behavior in theropod dinosaurs: paleopathological evidence" (PDF). Gaia 15: 167–184. [not printed until 2000]
- Currie, Philip J.; Trexler, David; Koppelhus, Eva B.; Wicks, Kelly; & Murphy, Nate. (2005). "An unusual multi-individual tyrannosaurid bonebed in the Two Medicine Formation (Late Cretaceous, Campanian) of Montana (USA)". In Carpenter, Kenneth (ed.). The Carnivorous Dinosaurs. Bloomington: Indiana University Press. pp. 313–324. ISBN 978-0-253-34539-4.
- "Tyrannosaurus had poor turning circle"
- Carrier, D.R., Walter, R.M., and Lee, D.V. (15 November 2001). "Influence of rotational inertia on turning performance of theropod dinosaurs: clues from humans with increased rotational inertia". Journal of Experimental Biology (The Company of Biologists Limited) 204 (Pt 22): 3917–3926. PMID 11807109.
- Hutchinson, J.R. (2004). "Biomechanical Modeling and Sensitivity Analysis of Bipedal Running Ability. II. Extinct Taxa" (PDF). Journal of Morphology 262 (1): 441–461. doi:10.1002/jmor.10240. PMID 15352202.
- Horner, John R.; Don Lessem (1993). The complete T. rex. New York City: Simon & Schuster. ISBN 0-671-74185-3.[page needed]
- Holtz, Thomas R. (1 May 1996). "Phylogenetic taxonomy of the Coelurosauria (Dinosauria; Theropoda)". Journal of Paleontology 70 (3): 536–538. Retrieved 3 October 2008.
- Christiansen, P. (1998). "Strength indicator values of theropod long bones, with comments on limb proportions and cursorial potential" (PDF). Gaia 15: 241–255. ISSN 0871-5424.
- Farlow, James O.; Smith, Matthew B.; Robinson, John M. (1995). "Body mass, bone "strength indicator", and cursorial potential of Tyrannosaurus rex". Journal of Vertebrate Paleontology 15 (4): 713–725. doi:10.1080/02724634.1995.10011257.
- "The bigger they come, the harder they fall" New Scientist, 7 October 1995, p. 18.
- "Giraffe". WildlifeSafari.info. Retrieved 29 April 2006.
- "The History of Woodland Park Zoo — Chapter 4". Retrieved 29 April 2006.[dead link]
- Alexander, R.M. (August 7, 2006). "Dinosaur biomechanics". Proc Biol Sci. (The Royal Society) 273 (1596): 1849–1855. doi:10.1098/rspb.2006.3532. PMC 1634776. PMID 16822743.
- Hanna, Rebecca R. (2002). "Multiple injury and infection in a sub-adult theropod dinosaur (Allosaurus fragilis) with comparisons to allosaur pathology in the Cleveland-Lloyd dinosaur quarry collection". Journal of Vertebrate Paleontology 22 (1): 76–90. doi:10.1671/0272-4634(2002)022[0076:MIAIIA]2.0.CO;2. ISSN 0272-4634. catalogs the injuries of the Allosaurus known as "Big Al" - at least one was attributed to a fall.
- Hutchinson, John R.; Garcia, M (28 February 2002). "Tyrannosaurus was not a fast runner". Nature 415 (6875): 1018–1021. doi:10.1038/4151018a. PMID 11875567.
- Hajdul, R. (1997). Tendons. Dinosaur Cards. Orbis Publishing Ltd. D36044311.
- Sellers, W.I., and Manning, P.L. (July 2007). "Estimating dinosaur maximum running speeds using evolutionary robotics". Proc. R. Soc. B (The Royal Society) 274 (1626): 2711–6. doi:10.1098/rspb.2007.0846. PMC 2279215. PMID 17711833. This may be a preliminary version of Sellers, W. I., Manning, P.L., Crompton, R.H. and Codd, J.R., . (2007), "Exploring elastic energy storage effects in bipedal locomotion using evolutionary robotics", Journal of Biomechanics, in-review
- Liz Seward: "T. rex 'would outrun footballer'". BBC News website, Tuesday, 21 August 2007. The article quotes Dr Bill Sellers, University of Manchester, co-author of a paper published in Proceedings of the Royal Society B. Retrieved 22 August 2007.
- Callison, G.; H. M. Quimby (1984). "Tiny dinosaurs: Are they fully grown?". Journal of Vertebrate Paleontology 3 (4): 200–209. doi:10.1080/02724634.1984.10011975.
- Zhou Zhonghe, Z; Barrett, Paul M.; Hilton, Jason. (2003). "An exceptionally preserved Lower Cretaceous ecosystem". Nature 421 (6925): 807–814. doi:10.1038/nature01420. PMID 12594504.
- Chen Peiji, Pei-ji; Dong Zhiming; Zhen Shuonan. (1998). "An exceptionally well-preserved theropod dinosaur from the Yixian Formation of China". Nature 391 (6663): 147–152. Bibcode:1998Natur.391..147C. doi:10.1038/34356.
- Xu Xing, X; Zhou Zhonghe & Prum, Richard A. (2003). "Branched integumental structures in Sinornithosaurus and the origin of feathers". Nature 410 (6825): 200–204. doi:10.1038/35065589. PMID 11242078.
- Lingham-Soliar, Theagarten; Feduccia, Alan & Wang, Xiaolin. (2007). "A new Chinese specimen indicates that 'protofeathers' in the Early Cretaceous theropod dinosaur Sinosauropteryx are degraded collagen fibres". Proceedings of the Royal Society of London. Series B, Biological Sciences 274 (1620): 1823–1829. doi:10.1098/rspb.2007.0352. PMC 2270928. PMID 17521978.
- D. Tanke (25 March 1996). "Tyrannosaur Skin Impression Found In Alberta". Dinosauria.com. Archived from the original on 7 September 2008. Retrieved 9 September 2008.
- Stevens, Kent A. (June 2006). "Binocular vision in theropod dinosaurs". Journal of Vertebrate Paleontology 26 (2): 321–330. doi:10.1671/0272-4634(2006)26[321:BVITD]2.0.CO;2. ISSN 0272-4634.
- Jaffe, Eric (1 July 2006). "Sight for 'Saur Eyes: T. rex vision was among nature's best". Science News 170 (1): 3–4. doi:10.2307/4017288. JSTOR 4017288. Retrieved 6 October 2008.
- Saveliev, Sergei V.; Alifanov, Vladimir R. (2005). "A new study of the brain of the predatory dinosaur Tarbosaurus bataar (Theropoda, Tyrannosauridae)". Paleontological Journal 41 (3): 281–289. doi:10.1134/S0031030107030070.
- Carr, Thomas D. (1999). "Craniofacial ontogeny in Tyrannosauridae (Dinosauria, Coelurosauria)". Journal of Vertebrate Paleontology 19 (3): 497–520. doi:10.1080/02724634.1999.10011161.
- Bakker, Robert T. (1968). "The superiority of dinosaurs". Discovery 3 (2): 11–12.
- Bakker, Robert T. (1972). "Anatomical and ecological evidence of endothermy in dinosaurs". Nature 238 (5359): 81–85. Bibcode:1972Natur.238...81B. doi:10.1038/238081a0.
- Bakker, Robert T. (1986). The Dinosaur Heresies. New York: Kensington Publishing. ISBN 0-688-04287-2. OCLC 13699558.[page needed]
- Barrick, Reese E.; William J. Showers (July 1994). "Thermophysiology of Tyrannosaurus rex: Evidence from Oxygen Isotopes". Science (New York City) 265 (5169): 222–224. doi:10.1126/science.265.5169.222. PMID 17750663. Retrieved 7 October 2008.
- Barrick, Reese E.; William J. Showers (October 1999). "Thermophysiology and biology of Giganotosaurus: comparison with Tyrannosaurus". Palaeontologia Electronica 2 (2).
- Paladino, Frank V.; James R. Spotila and Peter Dodson (1999). "A blueprint for giants: modeling the physiology of large dinosaurs". In James O. Farlow and M. K. Brett-Surman. The Complete Dinosaur. Bloomington: Indiana University Press. pp. 491–504. ISBN 0-253-21313-4.
- Chinsamy, Anusuya; Willem J. Hillenius (2004). "Physiology of nonavian dinosaurs". In David B. Weishampel, Peter Dodson and Halszka Osmólska. The dinosauria. Berkeley: University of California Press. pp. 643–659. ISBN 0-520-24209-2.
- Farlow, James O.; Pianka, Eric R. (2002). "Body size overlap, habitat partitioning and living space requirements of terrestrial vertebrate predators: implications for the paleoecology of large theropod dinosaurs". Historical Biology 16 (1): 21–40. doi:10.1080/0891296031000154687.
- Varricchio, David J. (2001). "Gut contents from a Cretaceous tyrannosaurid: implications for theropod dinosaur digestive tracts". Journal of Paleontology 75 (2): 401–406. doi:10.1666/0022-3360(2001)075<0401:GCFACT>2.0.CO;2. ISSN 0022-3360.
- Brochu, C.A. (December 2003). "Lessons From A Tyrannosaur: The Ambassadorial Role Of Paleontology". PALAIOS 18 (6): 475. doi:10.1669/0883-1351(2003)018<0475:LFATTA>2.0.CO;2. ISSN 0883-1351.
- Guinness World Records Ltd. (2003). 2003 Guinness World Records. pg 90.
- Eberth, David A.; McCrea, Richard T. (2001). "Were large theropods gregarious?". Journal of Vertebrate Paleontology 21 ((Supplement to 3 – Abstracts of Papers, 61st Annual Meeting of the Society of Vertebrate Paleontology)): 46A.[published abstract only]
- Roach, Brian T.; Brinkman, Daniel L. (2007). "A reevaluation of cooperative pack hunting and gregariousness in Deinonychus antirrhopus and other nonavian theropod dinosaurs". Bulletin of the Peabody Museum of Natural History 48 (1): 103–138. doi:10.3374/0079-032X(2007)48[103:AROCPH]2.0.CO;2.
- Currie, Philip J. (1998). "Possible evidence of gregarious behavior in tyrannosaurids". Gaia 15: 271–277.(not printed until 2000)
- Roach, Brian T.; Brinkman, Daniel T. (2007). "A reevaluation of cooperative pack hunting and gregariousness in Deinonychus antirrhopus and other nonavian theropod dinosaurs". Bulletin of the Peabody Museum of Natural History 48 (1): 103–138. doi:10.3374/0079-032X(2007)48[103:AROCPH]2.0.CO;2.
- Jacobsen, A.R. 2001. Tooth-marked small theropod bone: An extremely rare trace. p. 58-63. In: Mesozioc Vertebrate Life. Ed.s Tanke, D. H., Carpenter, K., Skrepnick, M. W. Indiana University Press.
- Abler, W.L. 2001. A kerf-and-drill model of tyrannosaur tooth serrations. p. 84-89. In: Mesozioc Vertebrate Life. Ed.s Tanke, D. H., Carpenter, K., Skrepnick, M. W. Indiana University Press.
- Lambe, L. B. (1917). "The Cretaceous theropodous dinosaur Gorgosaurus". Memoirs of the Geological Survey of Canada 100: 1–84. doi:10.4095/101672.
- Farlow, J. O. and Holtz, T. R. (2002). "The fossil record of predation in dinosaurs" (PDF). In Kowalewski, M. and Kelley, P.H. The Fossil Record of Predation. The Paleontological Society Papers 8. pp. 251–266.
- Dorey, M. (1997). Tyrannosaurus. Dinosaur Cards. Orbis Publishing Ltd. D36045907.
- Horner, J.R. (1994). "Steak knives, beady eyes, and tiny little arms (a portrait of Tyrannosaurus as a scavenger)". The Paleontological Society Special Publication 7: 157–164.
- Amos, J. (31 July 2003). "T. rex goes on trial". BBC.
- Walters, M., Paker, J. (1995). Dictionary of Prehistoric Life. Claremont Books. ISBN 1-85471-648-4.
- Erickson G. M., Olson K. H. (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.
- Carpenter, K. (1998). "Evidence of predatory behavior by theropod dinosaurs". Gaia 15: 135–144. Archived from the original on 17 November 2007. Retrieved 5 December 2007.
- Fowler, Denver W.; Robert M. Sullivan (2006). "A ceratopsid pelvis with toothmarks from the Upper Cretaceous Kirtland Formation, New Mexico: evidence of late Campanian tyrannosaurid feeding behavior". New Mexico Museum of Natural History and Science Bulletin 35: 127–130.
- Cope E.D. (1866). "Discovery of a gigantic dinosaur in the Cretaceous of New Jersey". Proceedings of the Academy of Natural Sciences of Philadelphia 18: 275–279.
- Maleev E.A. (1955). "New carnivorous dinosaurs from the Upper Cretaceous Mongolia". Doklady Akademii Nauk SSSR 104 (5): 779–783.
- Leidy, Joseph (1856). "Notice of remains of extinct reptiles and fishes, discovered by Dr. F.V. Hayden in the badlands of the Judith River, Nebraska Territory". Proceedings of the Academy of Natural Sciences of Philadelphia 8: 72–73.
- Osborn, Henry F. (1905). "Tyrannosaurus and other Cretaceous carnivorous dinosaurs". Bulletin of the American Museum of Natural History 21 (3): 259–265. doi:10.1111/j.1468-5965.2007.00735_17.x.
- Liddell, Henry G.; Scott, Robert (1980). Greek-English Lexicon (Abridged ed.). Oxford: Oxford University Press,. ISBN 0-19-910207-4.
- Paul, Gregory S. (1988). Predatory Dinosaurs of the World. New York: Simon & Schuster. pp. 464pp. ISBN 0-671-61946-2.
- Olshevsky, George (1995). "The origin and evolution of the tyrannosaurids". Kyoryugaku Saizensen [Dino Frontline] 9–10: 92–119.
- Olshevsky G., Ford T.L. (1995). "The origin and evolution of the Tyrannosauridae, part 2 [in Japanese]". Dino Frontline 6: 75–99.
- Fowler DW, Woodward HN, Freedman EA, Larson PL, Horner JR (2011) Reanalysis of “Raptorex kriegsteini”: A Juvenile Tyrannosaurid Dinosaur from Mongolia. PLoS ONE 6(6): e21376. doi:10.1371/journal.pone.0021376
- Loewen, M.A.; Irmis, R.B.; Sertich, J.J.W.; Currie, P. J.; Sampson, S. D. (2013). "Tyrant Dinosaur Evolution Tracks the Rise and Fall of Late Cretaceous Oceans". In Evans, David C. PLoS ONE 8 (11): e79420. doi:10.1371/journal.pone.0079420.
- Brusatte, S.L.; Norell, M.A.; Carr, T.D.; Erickson, G.M.; Hutchinson, J.R.; Balanoff, A.M.; Bever, G.S.; Choiniere, J.N.; Makovicky, P.J.; and Xu, X. (2010). "Tyrannosaur paleobiology: new research on ancient exemplar organisms". Science 329 (5998): 1481−1485. Bibcode:2010Sci...329.1481B. doi:10.1126/science.1193304. PMID 20847260.
- Sereno, Paul C. (1998). "A rationale for phylogenetic definitions, with application to the higher-level taxonomy of Dinosauria". Neues Jahrbuch für Geologie und Paläontologie Abhandlungen (in German) 210: 41–83.
- Holtz, TR, Jr. (2001), The phylogeny and taxonomy of the Tyrannosauridae in K Carpenter & D Tanke [eds.], Mesozoic Vertebrate Life. Indiana Univ. Press, pp. 64-83.
- Brochu, Christopher R. (2003). "Osteology of Tyrannosaurus rex: insights from a nearly complete skeleton and high-resolution computed tomographic analysis of the skull". Society of Vertebrate Paleontology Memoirs 7: 1–138. doi:10.2307/3889334. JSTOR 3889334.
- Sereno, Paul C. (7 November 2005). "Stem Archosauria—TaxonSearch". Retrieved 14 January 2008.
- Hurum, Jørn H.; Sabath, Karol. (2003). "Giant theropod dinosaurs from Asia and North America: Skulls of Tarbosaurus bataar and Tyrannosaurus rex compared" (abstract). Acta Palaeontologica Polonica 48 (2): 161–190.
- Tyrannosauridae specimen list and discussion at The Theropod Database