Minggu, 22 November 2009

Dryptosaurus

Dryptosaurus

Dryptosaurus
Fossil range: Late Cretaceous, 70 Ma
Scientific classification
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Superorder: Dinosauria
Order: Saurischia
Suborder: Theropoda
Superfamily: Tyrannosauroidea
Family: Dryptosauridae
Marsh, 1890
Genus: Dryptosaurus
Marsh, 1877
Species

Dryptosaurus (from Greek Drypto, "tear" and Sauros, "lizard" ) was a genus of primitive tyrannosaur that lived in Eastern North America during the Maastrichtian stage of the Late Cretaceous period. A famous painting of the genus by Charles R. Knight has made it one of the more widely-known dinosaurs, in spite of its poor fossil record. Its specific name aquilunguis is Latin for "having claws like an eagle's".

Contents


Description


An early painting of Dryptosaurus aquilunguis by Charles R. Knight.

Illustrated fossil remains of Dryptosaurus aquilunguis.

Dryptosaurus was 6.5 m (20 feet) long, 1.8 m (6 feet) high at the hips, and weighed about 1.2 tons. Like its relative Eotyrannus, it had relatively long arms with three fingers. Each of these fingers was tipped by a talon-like 8 inch claw.[1] These claws lend a meaning for the type species aquilunguis: eagle-clawed.

Discovery

In 1866, an incomplete skeleton (ANSP 9995) was found in New Jersey by workers in a quarry.[1] Paleontologist E.D. Cope described the remains, naming the creature "Laelaps" ("storm wind", after the dog in Greek mythology that never failed to catch what it was hunting). "Laelaps" became one of the first dinosaurs described from North America (following Hadrosaurus, Aublysodon and Trachodon). Subsequently, it was discovered that the name "Laelaps" had already been given to a species of mite, and Cope's lifelong rival O.C. Marsh changed the name in 1877 to Dryptosaurus.

Classification

Before the discovery of Appalachiosaurus,[2] it was classified in a number of theropod families. Originally considered a megalosaurid by Cope, it was later assigned to its own family (Dryptosauridae) by Marsh, and later found (through phylogenetic studied of the 1990s) to be a coelurosaur, though its exact placement within that group remained uncertain. The discovery of the closely related (and more complete) Appalachiosaurus made it clear that Dryptosaurus was a primitive tyrannosauroid.

The fossil material assigned to Dryptosaurus was reviewed by Ken Carpenter in 1997 in light of the many different theropods discovered since Cope's day. He felt that due to some unusual features it couldn't be placed in any existing family and warranted placement in its own family, Dryptosauridae.[3] Dryptosaurus was the only large carnivore known in eastern North America before the discovery of Appalachiosaurus.

Paleoecology

An outdated historical depiction of Dryptosaurus confronting Elasmosaurus, with two Hadrosaurus in the background. By Cope, 1869.

Although certainly a carnivore, the paucity of known Cretaceous east coast dinosaurs make ascertaining the specific diet of Dryptosaurus difficult.[1] Hadrosaurus and its relatives have been found in New Jersey as well, so they may have had a prominent part of its diet. Apart from hadrosaurids, nodosaurs were also present although less likely to be hunted due to their armor plating.

Ornithomimus

Ornithomimus

Ornithomimus
Fossil range: Late Cretaceous
Ornithomimus edmontonicus in "death pose", Royal Tyrrell Museum
Scientific classification
Kingdom: Animalia
Phylum: Chordata
Class: Sauropsida
Superorder: Dinosauria
Order: Saurischia
Suborder: Theropoda
Family: Ornithomimidae
Genus: Ornithomimus
Marsh, 1890
Species
Synonyms

Ornithomimus (pronounced /ˌɔrnɨθɵˈmaɪməs/ meaning 'bird mimic') is a genus of dinosaur from the Late Cretaceous Period of what is now North America. Ornithomimus velox was named on the basis of a foot and partial hand from the Maastrichtian Denver Formation, but better material has since been found in Canada, including the Edmontonian-age Ornithomimus edmontonicus and an excellent articulated specimen (species unknown) from Dinosaur Provincial Park. Other specimens assigned to Ornithomimus have been discovered on the Eastern Coast of the USA.

Contents


Description


Ornithomimus edmontonicus, Royal Ontario Museum.

Like other ornithomimids, Ornithomimus is characterized by a three-toed foot, long slender arms and a long neck with a birdlike skull. It differs from other ornithomimids, such as Struthiomimus, in having very slender, straight hand and foot claws and in having metacarpals and fingers of similar lengths.[1] Its hands are remarkably sloth-like in appearance, which led Henry Fairfield Osborn to suggest that they were used to hook branches during feeding.

Ornithomimus was 12 ft (3.5 meters) long, 7 feet (2.10 meters) high and weighed around 100-150 kg. It was bipedal and superficially resembled an ostrich, except for its long tail. It would have been a swift runner.

In popular culture

Ornithomimus played a prominent role in the television series Prehistoric Park, where they were featured, to a greater or lesser extent, in every episode. They were portrayed as flock animals whose chicks have fluffy feathers and imprint on the first thing they see. They were also shown to have feeding habits more like that of a duck than an ostrich, a behavior based on an hypothesis (since refuted[2]) which proposed that ornithomimids were filter feeders.[3] Ornithomimus also appeared in a variety of motion pictures, including Fantasia (1940), The Valley of Gwangi (1969), Planet of Dinosaurs (1978) and the IMAX film T-Rex: Back to the Cretaceous (1998).

Dromaeosaurus

Dromaeosaurus

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Dromaeosaurus
Fossil range: Late Cretaceous, 76.5–74.8 Ma
Skull cast
Scientific classification
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Superorder: Dinosauria
Order: Saurischia
Suborder: Theropoda
Family: Dromaeosauridae
Subfamily: Dromaeosaurinae
Genus: Dromaeosaurus
Matthew & Brown, 1922
Species
  • D. albertensis (type)

Dromaeosaurus (pronounced /ˌdrɒmiː.ɵˈsɔrəs/) was a genus of theropod dinosaur which lived during the Late Cretaceous period (middle late Campanian), sometime between 76.5 and 74.8 million years ago, in the western United States and Alberta, Canada. The name means 'running lizard' and is derived from the Greek dromeus (δρομευς) meaning 'runner' and sauros (σαυρος) meaning 'lizard'.

Contents


Description


Restoration

Dromaeosaurus was a small carnivore, the size of a wolf, about 2 m (6 ft) in length and 15 kg (33 lb) in weight. Its mouth was full of sharp teeth, and it had a sharp "sickle claw" on each foot.

Although only a few bones are known from the hindlimb, they indicate that Dromaeosaurus was a powerfully built animal. The presence of feathers in closely related animals makes it extremely likely that it was feathered as well.

Dromaeosaurus had remarkably large eyes and excellent vision. It also probably had a good sense of smell and hearing. Its neck was curved flexible and its jaws were solidly built. The tail was flexible at the base but sheathed in a lattice of bony rods; this allowed it to be carried in a sharply upturned position.

Discovery and later findings


Skeleton cast

Despite receiving widespread attention in popular books on dinosaurs, and the usage of a complete mounted skeleton cast in museums throughout the world, Dromaeosaurus is surprisingly poorly known from actual fossils. The preparation of the popular cast by the Tyrrell Museum was only made possible by knowledge gained from other dromaeosaurids that have been discovered more recently.

The first known Dromaeosaurus remains were discovered by paleontologist Barnum Brown during a 1914 expedition to Red Deer River on behalf of the American Museum of Natural History.[1] The area where these bones were collected is now part of Dinosaur Provincial Park in Alberta, Canada.[2] The find consisted of a partial skull 24 cm (9.4 in) in length, and some foot bones.[1][2] Several other skull fragments, and about 30 isolated teeth, are known from subsequent discoveries in Alberta and Montana.[2]

Several species of Dromaeosaurus have been described, but Dromaeosaurus albertensis is the most complete specimen.[2] Additionally, it is apparent that this genus is even rarer than other small theropods, although it was one of the first small theropods described based on reasonably good cranial material.[2]

Matthew and Brown originally placed Dromaeosaurus within "Deinodontidae" (now known as Tyrannosauridae), based on some similarities in the general proportions of the skull.[1] In 1969, John H. Ostrom recognized that Dromaeosaurus shared many features with Velociraptor and the newly-discovered Deinonychus, and assigned these forms to a new family: Dromaeosauridae.[3] Since then, many new relatives of Dromaeosaurus have been found.

Paleobiology and diet


Foot

Dromaeosaurus differs from most of its relatives in having a short, massive skull, a deep mandible, and robust teeth. The teeth tend to be more heavily worn than those of its relative Saurornitholestes, suggesting that its jaws were used for crushing and tearing rather than simply slicing through flesh. Therrien et al. (2005) estimated that Dromaeosaurus had a bite nearly three times as powerful as that of Velociraptor.[4]

It is possible that Dromaeosaurus was more of a scavenger than other small theropods, or it may be that Dromaeosaurus relied more heavily on its jaws to dispatch its prey. It was probably better suited to tackling large prey than the more lightly built Saurornitholestes.

Relationships

The relationships of Dromaeosaurus are unclear. Although its rugged build gives it a primitive appearance, it was actually a very specialized animal.[5] It is usually given its own subfamily, the Dromaeosaurinae; this group is thought to include Utahraptor, Achillobator, Adasaurus and perhaps Deinonychus.

However, the relationships of dromaeosaurs are still in a state of flux. "Dromaeosaurus Morphotype A" is the designation given to a series of unusual, ridged dromaeosaur teeth from Alberta. These teeth probably do not belong to Dromaeosaurus, although it is unclear from what animal they do come.

In popular culture

Dromaeosaurus are featured in Walking with Dinosaurs, stalking juvenile Torosaurus and attempting to steal eggs from Tyrannosaurus, despite never coexisting with the latter in real life. Dromaeosaurus makes an appearance in Jurassic Fight Club, where a pack is shown being capable of taking down Edmontosaurus in spite of the carnivores' small size, but the carcass is later taken by a Tyrannosaurus (despite the tyrannosaur not being contemporaneous with Dromaeosaurus).

Paronychodon

Paronychodon

Paronychodon
Fossil range: Late Cretaceous
Scientific classification
Kingdom: Animalia
Phylum: Chordata
Class: Sauropsida
Superorder: Dinosauria
Suborder: Theropoda
Infraorder: Coelurosauria
Genus: Paronychodon
Species: P. lacustris
Binomial name
Paronychodon lacustris
Cope, 1876
Synonyms
?Zapsalis abradens
Cope, 1876

Paronychodon (meaning "beside claw tooth") was a theropod dinosaur genus. It lived during the Late Cretaceous in what is now Montana. This genus is a tooth taxon.

The type species, discovered by Edward Drinker Cope in 1876, is Paronychodon lacustris. It is considered dubious because of the fragmentary nature of the fossils.

References




Troodon

Troodon

Troodon
Fossil range: Late Cretaceous, 75–65 Ma
Restoration of Troodon preying on an insect
Scientific classification
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Superorder: Dinosauria
Order: Saurischia
Suborder: Theropoda
Family: Troodontidae
Genus: Troodon
Leidy, 1856
Species
Synonyms

Troodon (or Troödon in older sources) is a genus of relatively small, bird-like dinosaur from the Late Cretaceous period (75-65 mya). Discovered in 1855, it was among the first dinosaurs found in North America.

Its name (pronounced /ˈtroʊ.ɵdɒn/ TROE-o-don) is Greek for "wounding tooth", referring to the dinosaur's teeth, which are different from those of most other theropods. The teeth bear prominent, apically oriented serrations. These "wounding" serrations, however, are morphometrically more similar to those of herbivorous reptiles, and suggest a possibly omnivorous diet.[1]

Contents


Characteristics

Troodon was a small dinosaur, around 2 metres (6.6 ft) in length, 1 metre (3.3 ft) tall, and weighed about 27 to 45 kilograms (60 to 99 lb).[2] It had very long, slender limbs, suggesting that the animal was able to move quickly. It had long 'arms' that folded against the wall of the thorax like a bird's. It had large, retractable sickle-shaped claws on its second toes, which were raised off the ground when running.

Because of these features scientists regard Troodon as a member of the Maniraptora. Its eyes were large (perhaps suggesting nocturnal activity) and slightly forward facing, giving Troodon some depth perception. In fact most reconstructions give Troodon eyes which point in a more forwards direction than almost any other dinosaur, which implies that it had better binocular vision than most dinosaurs. Their light skulls contained a capsule similar to those found in ostrich dinosaurs.

Troodon had one of the largest known brains of any dinosaur, relative to its body mass[2] (comparable to modern birds). Hence it is believed to have been one of the most intelligent dinosaurs, even more intelligent than mammals of that era.[citation needed]

Distribution

Troodon is known from the Judith River Formation and the upper Two Medicine Formation of Montana, the Judith River Group of Alberta, the Horseshoe Canyon Formation of Alberta, the North Slope of Alaska, and in the famous Lance and Hell Creek Formations of the USA. There is some evidence that Troodon favored cooler climates, as it seems to have been particularly abundant in northern areas and during cooler intervals, such as the Early Maastrichtian.

It seems unlikely that all of these fossils, which come from localities hundreds or thousands of miles apart, separated by millions of years of time, represent a single species of Troodon. However, further study and more fossils are needed to determine how many species of Troodon existed.

Paleobiology

Troodon is thought to have been a predator like other theropods. This view is supported by its Maniraptoran features (sickle claw on foot) and apparently good binocular vision.

Troodon teeth, however, are different from most other theropods. One comparative study of the feeding apparatus suggests that Troodon could have been an omnivore.[1] The jaws met in a broad, U-shaped symphysis similar to that of an iguana, a lizard species adapted to a plant-eating lifestyle. Additionally, the teeth of Troodon bore large serrations each of which is called a denticle. There are pits at the intersections of the denticles, and the points of the denticles point towards the tip, or apex, of each tooth. The teeth show wear facets on their sides. Holtz (1998) also noted that characteristics used to support a predatory habit for Troodon - the grasping hands, large brain and stereoscopic vision, are all characteristics shared with the herbivorous/omnivorous primates and omnivorous Procyon (raccoon).

One study was based on the many Troodon teeth that have been collected from Late Cretaceous deposits from northern Alaska. These teeth are much larger than those collected from more southern sites, providing evidence that northern Alaskan populations of Troodon grew to larger average body size. The study suggests that the Alaskan Troodons may have had access to large animals as prey because there were no tyrannosaurids in their habitat to provide competition for those resources. This study also provides an analysis of the proportions and wear patterns of a large sample of Troodon teeth. It proposes that the wear patterns of all Troodon teeth suggest a diet of soft foods - inconsistent with bone chewing, invertebrate exoskeletons, or tough plant items. This study hypothesizes a diet primarily consisting of meat[3]

Age determination studies performed on the fossilized remains of Troodon using growth ring counts suggest that the longevity of this dinosaur was around 3–5 years.[4]

Reproduction


A clutch of Troodon formosus eggs partly encased in matrix. Museum of the Rockies specimen on loan to the Burke Museum. Photographed at Dinoday 2009.

Varriccho et al. (2002) have described eight Troodon nests. All of these nests are from the Two Medicine Formation of Montana. These are all in the collection of the Museum of the Rockies and their accession numbers are MOR 246, 299, 393, 675, 676, 750, 963, 1139. The first of these were discovered by John Horner in 1983. Horner (1984) found isolated bones and partial skeletons of the hypsilophodont Orodromeus very near the nests in the same horizon and described the eggs as those of Orodromeus.[5] Horner and Weishampel (1996) reexamined the embryos preserved in the eggs and determined that they were those of Troodon, not Orodromeus.[6]

Varricchio et al. (1997) made this determination with even more certainty when they described a partial skeleton of an adult Troodon (MOR 748) in contact with a clutch of at least five eggs (MOR 750), probably in a brooding position.[7]

Varricchio et al. (1997) described the exact structure of Troodon nests. They were built from sediments, they were dish shaped, about 100 cm in internal diameter, and with a pronounced raised rim encircling the eggs. The more complete nests had between 16 (minimum number in MOR 246) and 24 (MOR 963) eggs. The eggs are shaped like elongated teardrops, with the more tapered ends pointed downwards and imbedded about halfway in the sediment. The eggs are pitched at an angle so that, on average, the upper half is closer to the center of the nest. There is no evidence that plant matter was present in the nest.

Varricchio et al.(1997) were able to extract enough evidence from the nests to infer several characteristics of Troodon reproductive biology. The results are that Troodon appears to have a type of reproduction that is intermediate between crocodiles and birds, as phylogeny would predict. The eggs are statistically grouped in pairs, which suggests that the animal had two functional oviducts, like crocodiles, rather than one, as in birds. Crocodiles lay many eggs that are small proportional to adult body size. Birds lay fewer, larger, eggs. Troodon was intermediate, laying an egg of about 0.5 kg for a 50 kg adult. This is 10 times larger than reptiles of the same mass, but two Troodon eggs are roughly equivalent to the 1.1 kg egg predicted for a 50 kg bird.

Varricchio et al. also found evidence for iterative laying, where the adult might lay a pair of eggs every one or two days, and then ensured simultaneous hatching by delaying brooding until all eggs were laid. MOR 363 was found with 22 empty (hatched) eggs, and the embryos found in the eggs of MOR 246 were in very similar states of development, implying that all of the young hatched simultaneously. The embryos had an advanced degree of skeletal development, implying that they were precocial or even superprecocial. The authors estimated 45 to 65 total days of adult nest attendance for laying, brooding, and hatching. The authors found no evidence that the young remained in the nest after hatching and suggested that, instead, they dispersed like hatchling crocodiles or megapode birds.[8]

Varricchio et al. (2008) examined the bone histology of Troodon specimen MOR 748 and found that it lacked the bone resorption patterns that would indicate it was an egg-laying female. They also measured the ratio of the total volume of eggs in Troodon clutches to the body mass of the adult. They graphed correlations between this ratio and the type of parenting strategies used by extant birds and crocodiles and found that the ratio in Troodon was consistent with that in birds where only the adult male broods the eggs. From this they concluded that Troodon females likely did not brood eggs, that the males did, and this may be a character shared between maniraptoran dinosaurs and basal birds.[9]

History

Troodon was originally spelled Troödon (with a diaeresis) by Joseph Leidy in 1856, which was officially amended to its current status by Sauvage in 1876.


The original tooth

The Troodon tooth was originally classified as a "lacertian" (lizard) by Leidy, but re-assigned as a megalosaurid dinosaur by Nopsca in 1901 (Megalosauridae having historically been a wastebin taxon for most carnivorous dinosaurs). In 1924, Gilmore suggested that the tooth belonged to the herbivorous pachycephalosaur Stegoceras, and that Stegoceras was in fact a junior synonym of Troodon (the similarity of troodontid teeth to those of herbivorous dinosaurs continues to lead many paleontologists to believe that these animals were omnivores). In 1945, Charles Mortram Sternberg rejected the possibility that Troodon was a pachycephalosaur due to its stronger similarity to the teeth of other carnivorous dinosaurs.

The first specimen of Troodon that was not a tooth, then referred to its own genus (Stenonychosaurus), was named by Sternberg in 1932, based on a foot, fragments of a hand, and some caudal vertebrae from Alberta. A remarkable feature of these remains was the enlarged claw on the second toe, which is now recognized as characteristic of Deinonychosauria. Sternberg initially classified Stenonychosaurus as a member of the family Coeluridae. Later, Sternberg (1951) speculated that since Stenonychosaurus had a "very peculiar pes" and Troodon "equally unusual teeth", they may be closely related. Unfortunately, no comparable specimens were available at that time to test the idea.


Head and neck of Dale Russell's Troodon sculpture, from the Natural History Museum, London.

A more complete skeleton of Stenonychosaurus was described by Dale Russell in 1969, which eventually formed the scientific foundation for a famous life-sized sculpture of Stenonychosaurus accompanied by its fictional, human-like descendant, the "dinosauroid". Stenonychosaurus became a well-known theropod in the 1980s, when the feet and braincase were described in more detail. Phil Currie, reviewing the known Troodontidae in 1987, reclassified Stenonychosaurus inequalis as a junior synonym of Troodon formosus. This synonymy has been widely adopted by other paleontologists, and therefore all of the specimens once called Stenonychosaurus are now referred to as Troodon in the recent scientific literature.

Classification

The type specimen of Troodon has caused problems with classification, as the entire genus is based only on a single tooth from the Judith River Formation. Since the discovery of the original tooth, postcranial material from a related animal were given the name Stenonychosaurus. More complete remains of Stenonychosaurus convinced most paleontologists that it in fact was the same animal as the original tooth, so the name Stenonychosaurus was replaced with its senior synonym, Troodon. Other genera, including Polyodontosaurus and Pectinodon, have also been assigned to Troodon based on the assumption that this particular tooth type is limited to only a single type of dinosaur. For this reason, the future of the name Troodon itself is dubious—in similar situations, genera based on teeth have been abandoned in favor of names based on better remains. Familiar names like Deinodon and Trachodon have been abandoned in this way, and further research may require Troodon be replaced with Stenonychosaurus. In a chapter of the 2005 book Dinosaur Provincial Park, Phil Currie (one of the leading experts on North American troodontids) resurrects the type species of Stenonychosaurus (S. inequalis) within the genus Troodon as Troodon inequalis (Currie, 2005).

The "Dinosauroid"


A model of the hypothetical Dinosauroid, Dinosaur Museum, Dorchester

In 1982 paleontologist Dale Russell, curator of vertebrate fossils at the National Museum of Canada in Ottawa, conjectured a possible evolutionary path that might have been taken by Troodon had it not perished in the K/T extinction event 65 million years ago,[10] suggesting that it could have evolved into intelligent beings similar in body plan to humans. Over geologic time, Russell noted that there had been a steady increase in the encephalization quotient or EQ (the relative brain weight when compared to other species with the same body weight) among the dinosaurs.[10] Russell had discovered the first Troodontid skull, and noted that, while its EQ was low compared to humans, it was six times higher than that of other dinosaurs. If the trend in Troodon evolution had continued to the present, its brain case could by now measure 1,100 cm3; comparable to that of a human.[10] Troodontids had semi-manipulative fingers, able to grasp and hold objects to a certain degree, and binocular vision.[10]

Russell proposed that this Dinosauroid, like most dinosaurs of the troodontid family, would have had large eyes and three fingers on each hand, one of which would have been partially opposed. As with most modern reptiles (and birds), he conceived of its genitalia as internal. Russell speculated that it would have required a navel, as a placenta aids the development of a large brain case. However, it would not have possessed mammary glands, and would have fed its young, as birds do, on regurgitated food. He speculated that its language would have sounded somewhat like bird song.[11]

Russell's thought experiment has been met with criticism from other paleontologists since the 1980s, many of whom point out that Russell's Dinosauroid is overly anthropomorphic. Gregory S. Paul (1988) and Thomas R. Holtz Jr., consider it "suspiciously human" (Paul, 1988) and argue that a large-brained, highly intelligent troodontid would retain a more standard theropod body plan, with a horizontal posture and long tail, and would probably manipulate objects with the snout and feet in the manner of a bird, rather than with human-like "hands".[11]

In popular culture

Troodon is featured in ITV's Prehistoric Park in 2006, where it was portrayed as a highly intelligent scavenger. It was also shown in two episodes of Dinosaur Planet. In one, a pack of dwarf Troodon make "friends" with a Pyroraptor; in another, a pack of Troodon attack a flock of Orodromeus. Troodon was also featured in an episode of Animal Armageddon and was the focus of an episode of Paleoworld, called "Troodon: Dinosaur Genius". This episode also featured the Dinosauroid.

In fiction, Troodon feature prominently in the 1994 science-fiction novel End of an Era by Robert J. Sawyer, in which they are the preferred host vehicle for intelligent Martian viral invaders. Also, an intelligent saurian species very like the Troodon, called the saurs, appears in Ken MacLeod's "Engines of Light" series of books.

In the Star Trek novel First Frontier by Diane Carey and James Kirkland, several members of the Enterprise crew travel back in time and find that Troodon has rudimentary language and were well coordinated hunters. They also encounter evolved Troodons, called Clan Ru, from the future that were transplanted before the extinction by the Preservers and were sentient beings capable of warp travel.

In the children’s television show Dinosaur Train, the eponymous train is run by a Troodon.

In the Land Before Time series, two wise and philosophical Troodon make an appearance as mysterious, possibly space-faring dinosaurs called Rainbow-Faces.

Albertosaurus

Albertosaurus

Albertosaurus
Fossil range: 75–67.5 Ma
Late Cretaceous
Albertosaurus skeleton at the Royal Tyrrell Museum in Alberta
Scientific classification
Kingdom: Animalia
Phylum: Chordata
Class: Reptilia
Superorder: Dinosauria
Order: Saurischia
Suborder: Theropoda
Family: Tyrannosauridae
Genus: Albertosaurus
Osborn, 1905
Species
  • A. sarcophagus (type)
    Osborn, 1905
Synonyms

Albertosaurus (pronounced /ælˌbɜrtɵˈsɔrəs/; meaning "Alberta lizard") is a genus of tyrannosaurid theropod dinosaur that lived in western North America during the Late Cretaceous Period, more than 70 million years ago. The type species, A. sarcophagus, was restricted in range to the modern-day Canadian province of Alberta, after which the genus is named. Scientists disagree on the content of the genus, with some recognizing Gorgosaurus libratus as a second species.

As a tyrannosaurid, Albertosaurus was a bipedal predator with tiny, two-fingered hands and a massive head with dozens of large, sharp teeth. It may have been at the top of the food chain in its local ecosystem. Although relatively large for a theropod, Albertosaurus was much smaller than its more famous relative Tyrannosaurus, probably weighing less than 2 metric tons.

Fossils of more than thirty individuals have been recovered, providing scientists with a more detailed knowledge of Albertosaurus anatomy than is available for most other tyrannosaurids. The discovery of 22 individuals at one site provides evidence of pack behavior and allows studies of ontogeny and population biology which are impossible with lesser-known dinosaurs.

Contents


Description


Albertosaurus sarcophagus with a human for scale

Albertosaurus was smaller than the truly gigantic tyrannosaurids like Tarbosaurus and Tyrannosaurus. Typical adults measured up to 9 meters (30 ft) long,[1][2] while rare individuals of great age could grow to over 10 meters (33 ft) in length.[3] Several independent mass estimates, obtained by different methods, suggest that an adult Albertosaurus weighed between 1.3 tonnes (1.4 short tons)[4] and 1.7 tonnes (1.9 tons).[5]

The massive skull of Albertosaurus, perched on a short, S-shaped neck, was approximately 1 meter (3.3 ft) long in the largest adults.[6] Wide openings in the skull (fenestrae) reduced the weight of the head while also providing space for muscle attachment and sensory organs. Its long jaws contained more than 60 banana-shaped teeth; larger tyrannosaurids possessed fewer teeth. Unlike most theropods, Albertosaurus and other tyrannosaurids were heterodont, with teeth of different forms depending on their position in the mouth. The premaxillary teeth at the tip of the upper jaw were much smaller than the rest, more closely packed, and D-shaped in cross section.[2] Above the eyes were short bony crests that may have been brightly colored in life and used in courtship to attract a mate.[7]


Skeleton at Maryland Science Center

All tyrannosaurids, including Albertosaurus, shared a similar body appearance. Typically for a theropod, Albertosaurus was bipedal and balanced the heavy head and torso with a long tail. However, tyrannosaurid forelimbs were extremely small for their body size and retained only two digits. The hind limbs were long and ended in a four-toed foot. The first digit, called the hallux, was short and only the other three contacted the ground, with the third (middle) digit longer than the rest.[2] Albertosaurus may have been able to reach speeds of 25–30 miles per hour.[7]

Classification and systematics

Cladogram of Tyrannosauridae highlighting the position of Albertosaurus
Tyrannosauridae

Tyrannosaurinae


Albertosaurinae

Albertosaurus



Gorgosaurus




Albertosaurus is a member of the theropod family Tyrannosauridae, in the subfamily Albertosaurinae. Its closest relative is the slightly older Gorgosaurus libratus (sometimes called Albertosaurus libratus; see below).[8] These two species are the only described albertosaurines, although other undescribed species may exist.[9] Thomas Holtz found Appalachiosaurus to be an albertosaurine in 2004,[2] but his more recent unpublished work locates it just outside Tyrannosauridae,[10] in agreement with other authors.[11]

The other major subfamily of tyrannosaurids is the Tyrannosaurinae, including Daspletosaurus, Tarbosaurus and Tyrannosaurus. Compared with these robust tyrannosaurines, albertosaurines had slender builds, with proportionately smaller skulls and longer bones of the lower leg (tibia) and feet (metatarsals and phalanges).[6][8]

Discovery and naming

Albertosaurus was named by Henry Fairfield Osborn in a very brief note at the end of his 1905 description of Tyrannosaurus rex. The name honors Alberta, the Canadian province in which the first remains were found. The generic name also incorporates the Greek term σαυρος/sauros ("lizard"), the most common suffix in dinosaur names. The type species is A. sarcophagus, which means "flesh-eater" and has the same etymology as the funeral container with which it shares its name: a combination of the Ancient Greek words σαρξ/sarx ("flesh") and Φαγειν/phagein ("to eat").[12] More than thirty specimens of all ages are known to science.[3][9]

Early discoveries


The Red Deer River near Drumheller, Alberta. Almost three-quarters of all Albertosaurus remains have been discovered alongside the river, in outcrops like the ones on either side of this picture.

The type specimen is a partial skull, collected in 1884 from an outcrop of the Horseshoe Canyon Formation alongside the Red Deer River in Alberta. This specimen and a smaller skull associated with some skeletal material were recovered by expeditions of the Geological Survey of Canada, led by the famous geologist Joseph B. Tyrrell. The two skulls were assigned to the preexisting species "Laelaps incrassatus" by Edward Drinker Cope in 1892,[13] despite the fact that the name Laelaps was preoccupied by a genus of mite and had been changed to Dryptosaurus in 1877 by Othniel Charles Marsh. Cope refused to recognize the new name created by his archrival Marsh, so it fell to Lawrence Lambe to change "Laelaps incrassatus" to Dryptosaurus incrassatus when he described the remains in detail in 1904.[14] Shortly later, Osborn pointed out that D. incrassatus was based on generic tyrannosaurid teeth, so the two Alberta skulls could not be confidently referred to that species. The Alberta skulls also differed markedly from the remains of D. aquilunguis, type species of Dryptosaurus, so Osborn created the new name Albertosaurus sarcophagus for them in 1905. He did not describe the remains in any great detail, citing Lambe's complete description the year before.[12] Both specimens (CMN 5600 and 5601) are stored in the Canadian Museum of Nature in Ottawa.

Dry Island bonebed

In 1910, American paleontologist Barnum Brown uncovered the remains of a large group of Albertosaurus at another quarry alongside the Red Deer River. Because of the large number of bones and the limited time available, Brown's party did not collect every specimen, but made sure to collect remains from all of the individuals they could identify in the bonebed. Among the bones deposited in the American Museum of Natural History collections in New York City are seven sets of right metatarsals, along with two isolated toe bones that did not match any of the metatarsals in size. This indicated the presence of at least nine individuals in the quarry. The Royal Tyrrell Museum of Palaeontology rediscovered the bonebed in 1997 and resumed fieldwork at the site, which is now located inside Dry Island Buffalo Jump Provincial Park.[15] Further excavation from 1997 to 2005 turned up the remains of 13 more individuals of various ages, including a diminutive two-year-old and a very old individual estimated at over 10 meters (33 ft) in length. None of these individuals are known from complete skeletons, and most are represented by remains in both museums.[3][4]

Gorgosaurus libratus


Sub-adult Gorgosaurus specimen in "death pose", Royal Tyrrell Museum of Palaeontology

In 1913, paleontologist Charles H. Sternberg recovered another tyrannosaurid skeleton from the slightly older Dinosaur Park Formation in Alberta. Lawrence Lambe named this dinosaur Gorgosaurus libratus in 1914.[16] Other specimens were later found in Alberta and Montana. Finding few differences to separate the two genera, Dale Russell declared the name Gorgosaurus a junior synonym of Albertosaurus, which had been named first, and G. libratus was renamed Albertosaurus libratus in 1970. This addition extended the temporal range of the genus Albertosaurus backwards by several million years and its geographic range southwards by hundreds of kilometers.[1]

In 2003, Phil Currie compared several tyrannosaurid skulls and came to the conclusion that the two species are more distinct than previously thought. The decision to use one or two genera is rather arbitrary, as the two species are sister taxa, more closely related to each other than to any other species. Recognizing this, Currie nevertheless recommended that Albertosaurus and Gorgosaurus be retained as separate genera, as they are no more similar than Daspletosaurus and Tyrannosaurus, which are almost always separated. In addition, several albertosaurine specimens have been recovered from Alaska and New Mexico, and Currie suggested that the Albertosaurus-Gorgosaurus situation may be clarified once these are described fully.[9] Most authors have followed Currie's recommendation,[2][4][17] but some have not.[11]

Other discoveries

William Parks described a new species, Albertosaurus arctunguis, based on a partial skeleton excavated near the Red Deer River in 1928,[18] but this species has been considered identical to A. sarcophagus since 1970.[1] Parks' specimen (ROM 807) is housed in the Royal Ontario Museum in Toronto. Six more skulls and skeletons have since been discovered in Alberta and are housed in various Canadian museums. Fossils have also been reported from the American states of Montana, New Mexico, and Wyoming, but these probably do not represent A. sarcophagus and may not even belong to the genus Albertosaurus.[2][9]

Albertosaurus megagracilis was based on a small tyrannosaurid skeleton from the Hell Creek Formation of Montana.[19] It was renamed Dinotyrannus in 1995,[20] but is now thought to represent a juvenile Tyrannosaurus rex.[6]

Paleobiology

Growth pattern


A graph showing the hypothesized growth curves (body mass versus age) of four tyrannosaurids, with Albertosaurus drawn in red[4]

Most age categories of Albertosaurus are represented in the fossil record. Using bone histology, the age of an individual animal at the time of death can often be determined, allowing growth rates to be estimated and compared with other species. The youngest known Albertosaurus is a two-year-old discovered in the Dry Island bonebed, which would have weighed about 50 kilograms (110 lb) and measured slightly more than 2 meters (7 ft) in length. The 10 meter (33 ft) specimen from the same quarry is the oldest and largest known, at 28 years of age. When specimens of intermediate age and size are plotted on a graph, an S-shaped growth curve results, with the most rapid growth occurring in a four-year period ending around the sixteenth year of life, a pattern also seen in other tyrannosaurids. The growth rate during this phase was 122 kilograms (268 lb) per year, based on an adult 1.3 tonnes (1.4 short tons). Other studies have suggested higher adult weights; this would affect the magnitude of the growth rate but not the overall pattern. Tyrannosaurids similar in size to Albertosaurus had similar growth rates, although the much larger Tyrannosaurus rex grew almost five times faster (601 kilograms 1325 lb per year) at its peak.[3] 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.[3][4] Sexual maturation while still actively growing appears to be a shared trait among small[21] and large[22] dinosaurs as well as in large mammals such as humans and elephants.[22] 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.[17][22]

Life history


Albertosaurus skeleton at the Redpath Museum, Montreal

Most known Albertosaurus individuals were aged 14 years or more at the time of death. Juvenile animals are rarely found as fossils for several reasons, mainly preservation bias, where the smaller bones of younger animals were less likely to preserved by fossilization than the larger bones of adults, and collection bias, where smaller fossils are less likely to be noticed by collectors in the field.[23] Young Albertosaurus are relatively large for juvenile animals, but their remains are still rare in the fossil record compared with adults. It has been suggested that this phenomenon is a consequence of life history, rather than bias, and that fossils of juvenile Albertosaurus are rare because they simply did not die as often as adults did.[3]

A hypothesis of Albertosaurus life history postulates that hatchlings died in large numbers, but have not been preserved in the fossil record due to their small size and fragile construction. After just two years, juveniles were larger than any other predator in the region aside from adult Albertosaurus, and more fleet of foot than most of their prey animals. This resulted in a dramatic decrease in their mortality rate and a corresponding rarity of fossil remains. Mortality rates doubled at age twelve, perhaps the result of the physiological demands of the rapid growth phase, and then doubled again with the onset of sexual maturity between the ages of fourteen and sixteen. This elevated mortality rate continued throughout adulthood, perhaps due to high physiological demands, stress and injuries received during intraspecific competition for mates and resources, and eventually, the ever-increasing effects of senescence. The higher mortality rate in adults may explain their more common preservation. Very large animals were rare because few individuals survived long enough to attain such sizes. High infant mortality rates, followed by reduced mortality among juveniles and a sudden increase in mortality after sexual maturity, with very few animals reaching maximum size, is a pattern observed in many modern large mammals, including elephants, African buffalo, and rhinoceros. The same pattern is also seen in other tyrannosaurids. The comparison with modern animals and other tyrannosaurids lends support to this life history hypothesis, but bias in the fossil record may still play a large role, especially since more than two-thirds of all Albertosaurus specimens are known from one locality.[3][17]

Pack behavior


Albertosaurus models, Royal Tyrell Museum.

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.[3]

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.[15] Other scientists are skeptical, observing that the animals may have been driven together by drought, flood or for other reasons.[3][23][24]

There is abundant evidence for gregarious behavior among herbivorous dinosaurs, including ceratopsians and hadrosaurs.[25] However, only rarely are so many dinosaurian predators found at the same site. Small theropods like Deinonychus,[26] Coelophysis and Megapnosaurus (Syntarsus) rhodesiensis[27] have been found in aggregations, as have larger predators like Allosaurus and Mapusaurus.[28] There is some evidence of gregarious behavior in other tyrannosaurids as well. Fragmentary remains of smaller individuals were found alongside "Sue," the Tyrannosaurus mounted in the Field Museum of Natural History in Chicago, and a bonebed in the Two Medicine Formation of Montana contains at least three specimens of Daspletosaurus, preserved alongside several hadrosaurs.[29] These findings may corroborate the evidence for social behavior in Albertosaurus, although some or all of the above localities may represent temporary or unnatural aggregations.[15] Others have speculated that instead of social groups, at least some of these finds represent Komodo dragon-like mobbing of carcasses, where aggressive competition leads to some of the predators being killed and cannibalized.[23]

Currie also offers speculation on the pack-hunting habits of Albertosaurus. The leg proportions of the smaller individuals were comparable to those of Ornithomimids, which were probably among the fastest dinosaurs. Younger Albertosaurus were probably equally fleet-footed, or at least faster than their prey. Currie hypothesized 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.[15] Juveniles may also have had different lifestyles than adults, filling predator niches between the enormous adults and the smaller contemporaneous theropods, the largest of which were two orders of magnitude smaller than adult Albertosaurus in mass.[2] A similar situation is observed in modern Komodo dragons, with hatchlings beginning life as small insectivores before growing to become the dominant predators on their islands.[30] However, as the preservation of behavior in the fossil record is exceedingly rare, these ideas cannot readily be tested.

Paleoecology

All identifiable fossils of Albertosaurus sarcophagus are known from the Horseshoe Canyon Formation in Alberta. This geologic formation dates to the early Maastrichtian stage of the Late Cretaceous Period, 73 to 70 Ma (million years ago). Immediately below this formation is the Bearpaw Shale, a marine formation representing a section of the Western Interior Seaway. The seaway was receding as the climate cooled and sea levels subsided towards the end of the Cretaceous, exposing land that had previously been underwater. It was not a smooth process, however, and the seaway would periodically rise to cover parts of the region throughout Horseshoe Canyon times before finally receding altogether in the years after. Due to the changing sea levels, many different environments are represented in the Horseshoe Canyon Formation, including offshore and near-shore marine habitats and coastal habitats like lagoons, estuaries and tidal flats. Numerous coal seams represent ancient peat swamps. Like most of the other vertebrate fossils from the formation, Albertosaurus remains are found in deposits laid down in the deltas and floodplains of large rivers during the later half of Horseshoe Canyon times.[31]

The fauna of the Horseshoe Canyon Formation is well-known, as vertebrate fossils, including those of dinosaurs, are quite common. Sharks, rays, sturgeons, bowfins, gars and the gar-like Aspidorhynchus made up the fish fauna. Mammals included multituberculates and the marsupial Didelphodon. The saltwater plesiosaur Leurospondylus has been found in marine sediments in the Horseshoe Canyon, while freshwater environments were populated by turtles, Champsosaurus, and crocodilians like Leidyosuchus and Stangerochampsa. Dinosaurs dominate the fauna, especially hadrosaurs, which make up half of all dinosaurs known, including the genera Edmontosaurus, Saurolophus and Hypacrosaurus. Ceratopsians and ornithomimids were also very common, together making up another third of the known fauna. Along with much rarer Ankylosaurians and pachycephalosaurs, all of these animals would have been prey for a diverse array of carnivorous theropods, including troodontids, dromaeosaurids, and caenagnathids. Adult Albertosaurus were the apex predators in this environment, with intermediate niches possibly filled by juvenile albertosaurs.