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The Late Cretaceous II - North and South America

In this lecture we will look at dinosaurian faunas from a number of western hemisphere areas, These are Argentina, the Two Medicine Formation of Montana, The Judith River beds of Montana and Alberta, Canada, and the Hell Creek Formation of Wyoming and Montana.

Locations are: 1, Argentina; 2, Two Medicine Formation, Montana; 3, Judith River beds, Montana and Alberta; 4, Hell Creek Formation, Wyoming and Montana; 5, New Jersey

Argentina

Argentina has recently been producing some spectacular dinosaurian remains. Below is a classification of some of the highlights. Saurischia  Sauropodomorpha  Sauropoda  Titanosauridae  Saltosaurus   Theropoda  ?Certatosauria  Carnotaurus Saltosaurus

Saltosaurus was a small sauropod characterized by a diplodocid-type head (teeth in anterior of mouth only), but with a body covered with small bony plates imbedded in the skin. The later is the shared derived character for the group of sauropods called the Titanosauridae.


Saltosaurus


Saltosaurus skin and armor
Skin (left) and armor plate (right) of Saltosaurus, after xxxx.
When just the bony plates were found they were originally ascribed to that of ankylosaurs, which the plates resemble (e.g. plate on riight). For this course we regard the Titanosauridae as one other the three groups of sauropods in an unresolved polytomy. In fact, the Titanosauridae might br  a group within the diplodocids. While abundant in South America, members of the Titanosauridae such as Alamosaurus, spread into North America and seem to have lasted until the end of the Cretaceous.
Recently (1998) superbly preserved eggs, apparently of sauropod origin were discovered in Argentina some with preserved embryos inside.

The embryos have skin with the embedded bony plates

The overall shape of the eggs is spherical, very much like the Chinese eggs attributed to sauropods.

For more information see: http://www.canoe.com/CNEWSScienceArchive/ 981117_dinosaurs.html.


Titanosaurid eggs, based on xxxx.

Carnotaurus
 

Carnotaurus is a large theropod know from skeletal material that includes detailed impressions of skin, including the face. The skull (above) is unusually short for a theropod and its sports two horns over the eyes. (Based on Paul, 1988)

Based on xxxx.

The skull and skeleton of Carnotaurus shows similarities to Allosaurusas well as ceratosaurians. We group it with the latter here although many workers group Carnotaurus within a group called the abelisaurs that includes Majugnathus. Like certatosaurs, Carnotaurus retains a fourth digut on the very small manus.
 
 

Two Medicine - Montana

John Horner

John (Jack) Horner is presently Curator of the Museum of the Rockies and winner of the prestigious MacArthur "genius" Fellowships. His prestige and fame rests largely on his discovery and analysis of the dinosaurian fauna of the Two Medicine Formation of Montana, although he has made many additional discoveries.
 
Without benefit of a formal bachelor degree from a university, he came into paleontology as an amateur collector, after a tour of duty in the Vietnam War, Horner became a vertebrate paleontological preparator for the former Museum of Natural History at Princeton University, under the then Director and Curator, Donald Baird. There he was able to have free access to an excellent Library and during the summers spend much time collecting in his beloved Montana, especially dinosaurian remains in the Two Medicine Formation. Horner and Olsen at Wasson Bluff
He did other collecting as well, however. Above (lower center) we see Horner collecting a partial prosauropod dinosaur with Donald Baird that I had found in 1975. This skeleton, found at Wasson Bluff near Parrsboro Nova Scotia, was the first Early Jurassic dinosaur and the first prosauropod dinosaur found in Canada.
Horner (on left) always kept in touch with other amateurs, and in 1978, he was shown some small bones by owners of a rock shop in Choteau, Montana, Marion and John Brandvold. Horner recognized these to bones of a baby hadrosaur. They showed Horner where these came from and Horner began to find enormous numbers of dinosaur egg fragments, and eventually nests of eggs as well as many dinosaur bones. Many of the eggs, nests, babies, and adults turned out to be remains of a new hadrosaur, that Horner named Maiasaura peeblesorum, or "good mother lizard". Horner prepared much of the material at Princeton, where he gained fame, eventually accepting a position at the Museum of the Rockies in Montana. He became Curator of Paleontology xxxx and received an Honorary Doctorate of Science in 1986 from the University of Montana. Horner also was technical advisor for the movies Jurassic Park and The Lost World, directed by Steven Spielberg.

Classification - Dinosaurs of the Two Medicine Formation

Ornithischia  Genasauria  Cerapoda  Ornithopoda  Hadrosauria  Maiasaura peeblesorum Saurischia  Theropoda  Tetanura  Coelurosauria  Arctometarsalia  Bullatosauria  Troodontia  Troodon formosus

Ornithischians of the Two Medicine

Maiasaura peeblesorum
Jack Horner's "good mother lizard", Maiasaura peeblesorum, is a fairly typical non-crested hadrosaur.


Modified from Carpenter in Horner and Gorman (1988)

Skull of Maiasaura peeblesorum; based on Horner, 1988. 

The skull of Maiasaura peeblesorum is also fairly typically non-crested hadrosaurian.
It has the inflated narial (nostril) area typical of most hadrosaurs as well, but one not quite as large as is typical.
But, of course its the eggs and babies that Maiasaura is really famous for.

Below left is an example of a nest of eggs and below right a cutaway view of what the fetus might look like within the egg, just before hatching.

Based on Horner, 1982. 

Based on Horner, xxxx. 

A map of the distribution of nests suggests that they were spaced about one Maiasaura apart and that they nested in large numbers.

Based on Horner (1987)

Horner has shown that there is plant matter preserved within the fossil nests and is might have been brought for protection and warmth, or it might have been food for the babies.

That the babies at least returned to the nest for quite a while is shown by the variety of sizes of juveniles that have been found within the nests. Below is a reconstruction of a hatching Maiasaura, based on xxxx.

Giant Bone Beds of the Two Medicine Formation

One of the most amazing discoveries made by Horner in the Two Medicine Formation has been the discover of giant "bone beds" of hadrosaurs (Varricchio and Horner, 1993). These include bone beds of both non-crested hadrosaurs such as Maiasaura as well as bone beds of crested forms. Generally the bone beds consist of layers one to two meters thick consisting of bones of nearly entirely one kind of dinosaur.

Horner suggests that these sorts of bone beds were created by the mass-death of huge herds of hadrosaurs, caused by volcanic ash falls.

Varricchio and Horner (1993) estimate that at least xxxxxxx individuals are in the largest of these bone beds, and that these probably came from a single vast herd. Such estimates are made by counting the number of only one kind of bone (e. g, right tibia) within a given volume and then multiplying this number times an estimate of the total volume of the bed.

Such a herd, migrating across the landscape undoubtedly had a massive effect on the plant communities.
 
 

Saurischians of the Two Medicine

Troodon formosus

Troodon is the type genus for the Troodontia. While incomplete skeletal material of adult Troodon are known (including the characteristic teeth) from the Two Medicine Formation, Horner has found nests with eggs and babies, of these dinosaurs as well.


Hell Creek Formation

The Hell Creek Formation of Wyoming and Montana contain the best documented terrestrial latest Cretaceous faunas. Indeed the Cretaceous-Tertiary boundary itself is very well exposed and dinosaurs are abundant below it.

Barnum Brown

Henry Fairfield Osborn was first hired at the American Museum of Natural History in 1891 on the suggestion of the president of Columbia University. As pointed out by Preston (1986), at that time the museum had not a single dinosaur skeleton. In 1897, Osborn hired Barnum Brown (left) who had made himself known through part time work on collecting trips. Brown eventually collected many of the most spectacular skeletons in the American Museum collection including the magnificent Apatosaurus skeleton from the Morrison and Tyrannosaurus rex skeletons from the Hell Creek.

Classification

(As in the preceding, the following classification lists only those taxa we will discuss in the sections.)

Saurischia

 Theropoda  Tetanura  Coelurosauria  Arctometarsalia  Bullatosauria  Ornithomimia  Ornithomimus Troodontia  Stenonychosaurus Tyrannosauria  Tyrannosaurus rex Maniraptora  Deinonychosauria  Dromeosaurus Ornithischia  Genasauria  Thyreophora  Ankylosauridae  Ankylosaurus Cerapoda  Ornithopoda  Hadrosauridae  Anatotitan
Edmontosaurus
Marginocephalia  Pachycephalosauria  Pachycephalosaurus Ceratopsia  Neoceratopsia  Triceratops

Tyrannosaur of the Hell Creek

Tyrannosaurus rex

Without a doubt, the most famous Hell Creek dinosaur is the other arctometatarsalian tyrannosaur, Tyrannosaurus rex.

Sue - T. rex

"Sue", a Tyrannosaurus rex. Redrawn from http://www.wyomingpaleo.com/sueintro.html.

Barnum Brown collected several excellent specimens of Tyrannosaurus rex for the American Museum of Natural History. Including the spectacular skeleton on exhibit as well as the huge skull. The name means "king of the tyrant lizards" and apart possibly from Giganotosaurus, Tyrannosaurus rex is the largest known carnivore to have lived. Another skeleton of T. rex collected by Brown was given to the Carnegie Museum of Pittsburgh PA, when it was thought New York might be bombed during WW II (Preston, 1986). More recently a virtually complete skeleton was uncovered by the Black Hills Paleontological Institute, consvicated by the FBI because of an oownership dispute and eventually found its way to the Field Museum in Chicago, where it is on display now. This specimen (above) was dubbed "Sue" after its discoverer.
 

T. rex manus

The foot of Tyrannosaurus rex (right) has the characteristic arctometatarsalian proximally pinched metatarsal III. This is a left pes. Note the extremely short radius (r), ulna (u), and humerus (h), relative to the phalanges.

The forelimbsof Tyrannosaurus rex (on left) is proportionally very small, even for a tyrannosaur (left). However, as pointed out by Bakker (1986) they were absolutely quite large and powerful. As previously discussed, the reduction of the size of the forelimbs and the reduction of the manus to two digits is the shared derived character for the Tyrannosauria. This is a left manus.
T. rex pes

Exactly what the function of the relatively minute hands of T. rex was, remains controversial. They are too short to reach the head. One idea is that the arms were used to prevent the dinosaur from slipping forward when in trying to get up off the ground. Another, is that they acted as braces against prey, while ripping out large chunks of flesh..

T. rex rising from a nap. Redrawn from Norman (198x).

No one argues that T. rex was not a meat eater. However, Horner (xxxx) has hypothesized that it was a scavenger, eating dead carcasses, and that it was too slow to capture its own prey. Farlow et al. (1995) have even gone so far as to argue that T. rex was so massive that if it ran and tripped it would be fatally injured by the fall! Personally, I find these arguments unconvincing, although it must be stressed that it is very hard to make behavior arguments for extinct forms when there is not even a remote living analog.
 
 
T. rex skull There is no doubt, however, that the skull of T. rex was a massive meat-eating machine (left). The over all structure of the skull, like that of other theropods, was strong in tension (while pulling). Indeed, there parts of the skull was unusually flexible - an area lower jaws, allowing the jaw to flex while ingesting particularly bulky prey or bits of prey. (Drawing based on Paul, 1988)

 
 
 


Cast of AMNH 5027, collected by Barnum Brown in 1908, on display at the the North Carolina Museum of Natural History.

The teeth of Tyrannosaurus rex average about xx cm and have a design particularly well suited to ripping out massive chunks of flesh. As described by Paul (1988) each premaxillary tooth is somewhat "D"-shaped in cross-section (left). As a bite proceeded the blunt side of the tooth would be relatively ineffective at cutting, but would tend to push the tooth posteriorly as the tooth was pushed into the flesh. The rear cutting edge would thus be forced backward and inward at the same time. This action would have automatically sliced out flesh in the bite stroke.

 

Ornithischia of the Hell Creek

Ankylosaurus

Brown collected a large number of ornithischians from the Hell Creek beds, mostly Triceratops. However other dinosaurs included hadrosaurs and ankylosaurs. The remains of Ankylosaurus comprise the most common ankylosaur in the Hell Creek Formation. Obviously it is a member of the Ankylosauridae and displays the characteristic shared derived characters of the group.
 
 
Reconstruction of Ankylosaurus

 

Reconstruction of skeleton (without armor) of Ankylosaurus


 

The skull of Ankylosaurus is expanded transversely (left), unlike that of nodosaurids. Missing is the central forehead plate of nodosaurids as well (retention of a primitive character). Again, the polygonal plates visible on the skull roof are osteoderms, not the bones of the skull itself (which are under the osteoderms).

The tail has the main shared derived character of the Ankylosauridae, a massive club at the end of a stiffened tail (right). Note that the distal tail vertebrae have interlocking processes that stiffened the tail to support swings of the massive club.

Ankylosaurus is not as well known as its relative Euoplocephalus, and therefore additional comments on the Ankylosauridae will be dealt with under the latter genus, below, when we consider the Judith River beds.
 
 

Anatotitan

Anatotitan, or as it is perhaps better known by is younger synonym Anatosaurus, is the quintessential "duck billed dinosaur". Its name means "titan duck" and images of its skeletons and reconstructions have appeared in popular books since Brown's beautiful set of skeletons was mounted.

Based on xxxxxxxxx



Anatotitan at the Tyrell Museum
The skull of Anatotitan is unusual because in lateral view (left) it is low and, sleek. A dorsal view (right), however, shows the broad expansion as the anterior of the skull that supported the duck-like bill. 
Of course, unlike birds, Anatotitan has a typically hadrosaurine dental battery. This dental battery consists of teeth set in a regular alternating pattern making a dense stack in the jaw. Growing teeth at the base of the dental battery displace the entire apparatus through the jaw. Wear on vegetable matter and the opposing teeth wear the entire batter down and n the process create a broad rasp-like surface comprised of obliquely work teeth, The surface is kept ever fresh by growth from the base of the battery and the wear. Weishample (1984) has shown that the lower jaws moved against the upper jaws in a circular motion, with the two lower jaws moving in mirror image motions against the upper jaws.

 

Edmontosaurus

Edmontosaurus, based on xxxxx.


Edmontosaurus is a very well known non-crested hadrosaur. It was originally described from the Judith River beds, in Alberta - Edmonton being the province's capital. Nonetheless, perhaps the most famous specimen comes from the Hell Creek Formation of Wyoming. It was collected by the famous team of professional collectors the Sternbergs.
Skull of Edmontosaurus from the Judith River beds (below) on display at the North Carolina Museum of Natural History.

The Sternberg team consisted of Charles Sternberg and his three sons/ As described by Preston (1986), the Sternbergs were on a collecting trip in Hell Creek beds for a Triceratops skull for the British Museum of Natural History in London. Triceratops is the most common dinosaur in the Hell Creek. One of Charles Sternberg sons, George found a hadrosaur skeleton, and in the process of excavation the elder Sternberg notice that much of the skeleton was covered in skin impressions preserved in the sandstone encasing the Edmontosaurus. This specimen was purchased by the American Museum of Natural History where it gained great fame as "the dinosaur mummy". It is one of the most remarkable specimens on display at the museum.

.

Until recently it was quite common for hadrosaurs to be thought of a semiaquatic. Some evidence for this was supposed to be webbing visible on the Edmontosaurus mummy's hands (left). Bakker (xxxx), however, has pointed out that the supposed webbing is more like loose skin left by decay of thick pads. Bakker also points out that the front feet are minute compared of the hind feet and would have provided minimum propulsive force in swimming. Bakker also argues that although hadrosaur tails were dorsoventrally deep the transverse spines on the anterior caudal vertebrae were very short compared to an animal that uses its tail to swim, like a crocodile. These transverse processes support that muscles that move the tail from side to side.
Footprints described by Lockley and Hunt (1995) show that hadrosaurs, such as Edmontosaurus clearly walked both bipedally and quadrupedally, and on land.

 

Triceratops
When the first horn cores of Triceratops were discovered in xxxx and brought to O. C. March, they were proclaimed an extinct bison. But when additional skulls were uncovered they proved to be of an extraordinary three horned dinosaur, Marsh named Triceratops. Barnum Brown later collected many specimens for the American Museum, a wonderful example of which is presently on display.

Triceratops, based on Dodson (1996).


Unlike most other neoceratopsians, the frill on the skull of Triceratops is solid, lacking the large fenestrae usually present. There are nubbins of bone around the frill that must have given it a serrated appearance. there is a short, upward pointing horn on the nose and much longer forward pointing horns over the eyes. (Drawing based on Hatcher et al., 1907.) Skull of Triceratops
There is considerable debate on whether how neoceratopsians ran. Bakker (xxxx; xxxx) has argued that they could gallop, like a rhinoceros. Recall that a gallop is a kind of run in which all four feet are off the ground in part of the step cycle. When this was first proposed it was considered a radical idea. However, subsequently, Webb et al. (1982) has shown that some crocodiles can gallop, so it seems perhaps less surprising. However, Dodson (1996) claims that the front legs were held in a somewhat sprawling position, which would make galloping very difficult.
Lockley and Hunt (1995) describe putative neoceratopsian tracks and suggest that their forelimbs were not held in a sprawling position, but Dodson (1996) looking at the same kind of data suggest otherwise. To me, such speculation is premature, because criteria for recognizing neoceratopsian tracks have not been established in the first place.

There are other kinds of neoceratopsians, with varied horns and frills, found with Triceratops, but these will be discussed below.

Triceratops and Tyrannosaurus rex were certainly among the last of the dinosaurs. Their remains are found within a few meters of the Cretaceous-Tertiary boundary and there is little reason to believe they did not make it right to the end.
 
 

Judith River Beds- Alberta, Montana

The Late Cretaceous Judith River beds may be the best studied assemblage of dinosaurs in the world. The strata outcrop along the Judith, Red Deer, and Belly rivers in Alberta and Montana. The fame of the dinosaurian assemblage rests largely with largely Barnum Brown and then a series of collection efforts later in the 1900s from The Royal Ontario Museum in Toronto. Many Museums have spectacular skeletons from these beds.

Tyrrell Museum

Classification

(As in the preceding, the following classification lists only those taxa we will discuss in the sections.) Ornithischia  Genasauria  Thyreophora  Ankylosauria  Nodosauridae  Edmontonia Ankylosauridae  Euoplocephalus Cerapoda  Ornithopoda  Hypsilophodontia  Thescelosaurus Hadrosauridae  Parasaurolophus
Lambeosaurus
Corythrosaurus
Marginocephalia  Pachycephalosauria  Stegoceras
Pachycephalosaurus
Ceratopsia  Neoceratopsia  Chasmosaurus
Monoclonius
Centrosaurus
Styracosaurus
Saurischia  Theropoda  Tetanura  Coelurosauria  Arctometatarsalia  Bullatosauria  Ornithomimosauria  Struthiomimus altus
Ornithomimus
Troodontia  Troodon formosus
Sauroidithoides
Tyrannosauria  Albertosaurus
Daspletosaurus
Oviraptoria  Caenagnathus Maniraptora  Deinonychosauria  Dromeosaurus Segnosauria  ?Erlikosaurus

Ornithischians of the Judith River beds

Edmontonia and Euoplocephalus

Two very well preserved members of the Ankylosauria (within the Tyreophora) are known from the Judith River fauna. These are the nodosaurid Edmontonia and the ankylosaurid Euoplocephalus.

Edmontonia, based on xxxx (xxxx).

Edmontonia is a typical nodosaurian with a plate in the middle of the forehead and a slender tapering tail, lacking club. It has, however, prominent shoulder spikes.

Euoplocephalus (below) is a typical ankylosaurid, and the best known genus in the family. Like Ankylosaurus, it has a massive club at the end of a stiffened tail.

Euoplocephalus, based on xxxx (xxxx).


Nodosaurids and ankylosaurids developed elaborate nasal systems, showing some parallels to mammals, but do it is somewhat different ways. On the left are cross-sections through the skulls of Edmontonia and Euoplocephalus. The nodosaurid Edmontonia has a very complex nasal passage with a fully developed hard palate. Euoplocephalus, the ankylosaurid, as a less complex system with more anterior internal nostrils (choanae). Presumably these features developed to allow more vigorous simultaneous chewing and breathing, as in mammals.

 

Thescelosaurus

While the ornithopod Hypsilophodon has traditionally been the most famous hypsilophodontid, Thescelosaurus from the Judith River beds is known from much better and more abundant material, including one specimen that may preserve a heart.

Thescelosaurus

Thescelosaurus, based on xxxx (xxxx).

Thescelosaurus resembles Hypsilophodon in most respects, however, it is larger and seems to have a proportionally smaller skull. Based on recent analysis, it may be more primitive than Hypsilophodon, despite its younger age.

In Spring 2000 an article on the front page of the New York Times announced the discovery and analysis of a heart preserved in the thorax of a Thescelosaurus skeleton nicknamed "Willow" in the collections of the North Carolina Museum of Natural History.
 

heart of Willow The putative heart (left) is preserved as a concretion within the chest cavity, which shows upon CAT-scanning, what appears to be a four chambered heart, according to Fisher et al. (2000). According to the latter, the fossilized heart is four chambered, with fully separated ventricles. If correctly interpreted, this would mean that ornithischians had a bird- (or mammal-) like heart with complete separation of the blood pumped through the body (deoxygenated) and blood pumped thorough the lungs (oxygenated) as seen on right.

Abbreviations are: c, right coracoid; h, heart; hu, humerus; r, rib; s, scapula.

Such a separation is only partial in crocodilians, the living sister group of dinosaurs and birds, and there is only a three chambered heart in living non-archosaurian sauropsids. The three chambered heart mixes oxygenated blood and oxygen depleted blood which makes sustained activity difficult. Because a four chambered heart is present in the avian theropods, if one was present in Thescelosaurus, the most parsimonious hypothesis is that it was primitive for dinosaurs in general, adding more evidence to the argument that dinosaurs had high activity levels and were metabolically similar to birds and mammals.

 

Parasaurolophus

The Hadrosauridae are very well represented in the Judith River deposits. In addition to non-crested forms, such as Edmontosaurus, already considered, are the crested forms represented by three genera, Parasaurolophus, Lambeosaurus and Corythrosaurus. Parasaurolophus was probably the most spectacular of these forms.

Parsaurolophus

Parasaurolophus, based on xxxx (xxxx).

Parasaurolophus skulls Parasaurolophus has a skull with a truly remarkable nasal crest. As in Saurolophus the nasal passage passes through this crest. In other respects the skeleton is quite similar to Saurolophus but the genus is probably more closely related to Lambeosaurus and Corythosaurus. There appear to be two morphs of Parasaurolophus that probably represent male and female. Left skull based on ROM 764 and 768, right on Norman (1988).

 

Lambeosaurus and Corythosaurus

Lambeosaurus and Corythrosaurus both and have body morphology very similar to Parasaurolophus. The crests, however are remarkably different.

The Lambeosaurus skull has a complicated curved nasal crest with a differently shaped nasal passage inside. The genus is named after Charles Lambe. Morphs identified as probable females to smaller crests. Based on Norman (1988).

Corythosaurus, has a crest resembling a corinthian helemt, hence the genus name. In juveniles the crest is small in size and apparently as individuals grew the crest grew disproportionally larger. Based on Norman (1988).


Lambeosaurus and Corythrosaurus

Vocalization in Hadrosaurs

Analysis of the skulls of the crested hadrosaurs by Dodson (1975) and Weishample (1981) reveals that within each basic crest style there tends to be marked variation attributable to growth and sexual dimorphism. Two slightly different crest types seem to present within each type. Dodson argued that these are different sexes. But what function could the crests serve?

t has been suggested that the crests were weapons, but they are made of paper-thin bone. It was also suggested that the crests might serve as some kind of snorkel. There is no opening at the end, however. Finally, the crests have been interpreted as some kind of extra air supply, which seems very unlikely, because of its minute volume 

In contrast with these seeming quite silly speculations, Weishample (1991) has argued that both the growth pattern and the sexual dimorphism implies a role in species identification and sexual selection. Weishample (1991) hypothesized that the crests, which always carried the nasal passage, were resonating organs that in some way enhanced vocalizations and served in mate recognition and interspecific display.


 

To test his hypothesis, Weishample constructed models of the crests and produced noises with them that were indeed enhanced in different ways depending on their shape. Thus, the hypothesis was corroborated, and its serves as the best explanation of the crest variation to date.

More recently Diegert and Williamson (see http://www.sandia.gov/media/dinosaur.htm) have developed a computer model of the sounds that might have been made by Parasaurolophus.


Stegoceras and Pachycephalosaurus

Marginocephalians are extraordinarily well represented in the Judith River beds. Two genera of pachycephalosaurs are present. Stegoceras is a small form similar to Prenocephale from Mongolia, while Pachycephalosaurus is considerably larger and has a very spiky cranium.

Stegoceras skeleton mounted in the Academy of Natural Sciences of Philadelphia.

In contrast to Stegoceras, the much larger Pachycephalosaurus, has a skull (see right) that has a series of well developed spikes around the margin. The skull of Pachycephalosaurus shown on the right is on display at the North Carolina Museum of Natural Science NC Pachycephalosaurus
brain cavity in Pachycephalosaurus Despite the apparently cerebral appearence of Pachycephalosaurus, the size of the brain was relatively quite small in pachycephalosaurs. Image on left based on deisplay at the American Museum of Natural History. Abbreviations are: br, endocranial cavity (cavity for brain); fm, foramen magnum, through which the spinal cord passes; oc, occipital condyle, on which the skull rests on the vertebral column.
 
The Neoceratopsians Chasmosaurus, Centrosaurus,Monoclonius, and Styracosaurus
 

Ceratopsians, specifically neoceratopsian are extraordinarily diverse in the Judith River assemblages. Here we will look at just a few that differe primarily in the form of their crests and horns, but otherwse have post-cranial skeltons similar to Triceratops


Cranium of Chasmosaurus at the Tyrell Museum.

 
 
Chasmosaurus, Centrosaurus, Monoclonius, and Styracosaurus have very different styles of horns and frills. This seemingly bizarre assemblage of skull types actually recalls the array of horn styles seen in antelopes living in East Africa. Again mate selection and dominance displays and combat probably played a critical role.

On the other hand, it seems almost certain that the horns were also used for defense against predators such as tyrannosaurs. In fact, various neoceratopsian skeletal elements have been found with tooth marks that match those of tyrannosaurs, so they did have something to defend against.


 

Saurischians of the Judith River beds

Struthiomimus and Dromiceomimus

A diverse assemblage of Coelurosauria are present in the Judith River including ornithomimids, troodontids, tyrannosaurs, and oviraptorids. First we will consider the Arctometatarsalia, specifically the Ornithomimosauria, of the Bullatosauria.

Two ornithomimids are Struthiomimus altus and Dromiceomimus

Struthiomimus skeleton

Skeleton of Struthiomimus altus as displayed in the old hall of Cretaceous Dinosaurs in the American Museum of Natural History/


Dromiceomimus skull

Dromiceomimus skull as it was displayed at the American Museum of Natural History.

Dromiceomimus is rather similar to Struthiomimus. Its skull (left) is shows the typical ornithomimid condition of being edentulous and having very large eye sockets with a large brain case (bullatosaurian features).

Troodontids, namely Troodon formosus and Sauroidithoidesare also present.
 
 

Albertosaurus and Daspletosaurus

The Tyrannosauria are abundant in the Judith River beds. Albertosaurus is the best known form and is represented by excellent skeletons. In most ways it is very similar to Tyrannosaurus, but is smaller and more delicate - if you can say that of a tyrannosaur.

Albertosaurus skeleton

Skeleton of Albertosaurus mounted in the Tyrrell Museum, Alberta.


A particularly realistic reconstruction of Albertosaurus is on display at the Tyrrell museum. It probably had a least a few feathers here or there in addition to the scales shown here.
Another tyrannosaurid is Daspletosaurus with a distinctively different looking skull (right).

An oviraptorid Caenagnathusis presnt, with a skull not quite as bizzar as Oviraptor itself.
 
 

Dromeosaurus

The deinonychosaurian maniraptoran Dromeosaurus is present as good skeletons.

Dromeosaurus skeleton

Skeleton of Dromeosaurus mounted at the Tyrell Museum.

Dromeosaurus is similar to both Velociraptor and Deinonychus, but has a stouter, more boxy head.
 
 

Eastern US - New Jersey

New Jersey was home to the first dinosaur complete enough to mount and show that it was bipedal. Unfortunately the New Jersey Cretaceous is mostly marine, and so dinosaur finds are very rare. There are continental sequences, but these have abundant lignites (wood accumulations that are halfway between peat and coal) indicating a =n acid environment that may have dissolved bones.

While most of the dinosaur material from the marine beds consist of scraps, there is a surprising diversity of forms. In addition, an excellent Cretaceous-Tertiary boundary section is presently exposed.

Classification

Ornithischia  Genasauria  Cerapoda  Ornithopoda  Hadrosauria  Hadrosaurus foulki
Gyposaurus (Hadrosaurus) minor
Saurischia  Theropoda  Tetanura  Coelurosauria  Arctometatarsalia  Bullatosauria  Ornithomimia  Coelosaurus antiquus Tyrannosauria  Albertosaurus
?Dryptosaurus aqilunguis
Gyposaurus (Hadrosaurus) minor

Reconstructtion of Gyposaurus.


Hadrosaurus foulkihas already been described, but at least one other hadrosaur is present. Originally described as Hadrosaurus minor by Colbert (1948) this form actually seems to be a member of the genus Gyposaurus. It was found in beds immediately below the Cretaceous-Tertiary boundary in the last remaining active marl pit in Eastern North America.

Another ornithischian is represented by a scrap of ankylosaur armor.

Fragmentary remains of ornithomimids (Coelosaurus antiquus of Cope) and perhaps tyrannosaurs (Dryptosaurus aqilunguis of Cope and Albertosaurus) are present (see reconstruction above).
 
 

Master Cladograms

We have now looked at all the dinosaurs we will examine in this course. The relationships, ages, and locationms of allof these dinosaurs and the groups to which they belong are given in the "master cladograms" at:http://www.ldeo.columbia.edu/edu/dees/courses/v1001/masterclads.html.

Trends through latest Cretaceous

The most dramatic tend noticeable in faunas through the Cretaceous is the tendency for the small dinosaur niche to be filled by birds, meaning there were no non-avian dinosaurs of adult size smaller than Velociraptor present. This may have been critical in the non-avian dinosaurs' extinction.

Studies by Russell (1984) and Sheehan and Fastovsky (1992) detect no statistically significant reduction in total dinosaurian diversity through the late Cretaceous. The matter is still highly controversial, however.
 
 

REFERENCES

Farlow, J. O., Smith, M. B. & Robinson, J. M., 1995, Body mass, bone "stregth indicator" and cursorial potential of Tyrannosaurus rex. Journal of Vertebrate Paleontology v. 15, p. 713-725.

Bakker, R. T., 1986, The Dinosaur Heresies. Kensington Publishing, New York, 481 p.

Colbert, E. H. 1948 A hadrosaurian dinosaur from New Jersey. Proceeding of the Aademy of Natural Sciences of Philadephia v. 100, p. 23-37.

Dodson, P., 1975, Taxonomic implications of relative growth in lambeosaurine hadrosaurs. Systematic Zoology v. 24, p. 37-54.

Dodson, P., 1996, The Horned Dinosaurs. Princeton University Press, Princeton, 346 p.

Fisher, P. E., Russell, D. A., Stoskopf,M. K., Barrick, R. E., Hammer, M., and Kuzmitz, A. A., 2000, Cardiovascular evidence for an intermediate or higher metabolic rate in and ornithiscian dinosaur. Science 288, p. 503-505.

Hatcher, J. B., Marsh, O. C.; Lull, R. S., 1907, The Ceratopsia. Washington: Government Printing Office, 1907. Series: United States Geological Survey. Monograph 49.

Horner, J. R. and Makela, R. 1979. Nest of juveniles provides evidence of family structure among dinosaurs. Nature 282: 296-298

Horner, J. R. 1982. Evidence of colonial nesting and 'site fidelity' among ornithischian dinosaurs. Nature 297: 675-676.

Horner, J. R. 1983. Cranial osteology and morphology of the type specimen of Maiasaura peeblesorum (Ornithischia: Hadrosauridae), with discussion of its phylogenetic position. Journal Vertebrate Paleontology 3(1): 29-38.

Horner, J. R. 1987. Ecologic and behavioral implications derived from a dinosaur nesting site. In Dinosaurs Past and Present, Vol. II, S. J. Czerkas and E. C. Olson (Eds.), Univ. Washington Press (Seattle). 51-63.

Horner, J. R. and Lessam, D., 1993, The Complete T. rex. Simon & Schuster, New York, 239 p.

Lockley, M. and Hunt, A. P., 1995, Dinosaur Tracks and Other Fossil Footprints of the Western United States. Columbia University Press, 338 p.

Paul, G. S., 1988, Predatory Dinosaur of ther World. New York Academy of Sciences, New York, 464 p.

Preston, D. J., 1986, Dinosaurs in the Attic. Ballantine Books, New York, 308 p.

Russell, D. A., 1984, The gradual decline of the dinosaurs; fact or fallacy?. Nature v. 307, p. 360-361.

Sheehan, P. M. and Fastovsky, D. E., 1992, Major extinctions of land-dwelling vertebrates at the Cretaceous-Tertiary boundary, eastern Montana. Geology v. 20, p. 556-560.

Varricchio, D. J. and Horner, J. R. 1993. Hadrosaurid and Lambeosaurid bone beds from the Upper Cretaceous Two Medicine Formation of Montana: taphonomic and biologic implications. Canadian Journal of Earth Sciences, 30: 997-1006.

Varricchio, D. J., F. Jackson, J. Borlowski, and J. R. Horner. 1997. Nest and egg clutches of the dinosaur Troodon formosus and the evolution of avian reproductive traits. Nature 385:247-249.

Webb, Grahame J.W. and Carl Gans. 1982. Galloping in Crocodylus johnstoni - A reflection of terrestrial activity?. Records of the Australian Museum v. 34, p. 607-618.

Weishample, D. B., 1981, Acoustic analysis of potential vocalization in lameosaurine dinosaurs (Reptilia: Ornithischia). Paleobiology, v. 7, p. 252-261.

Weishample, D. B., 1984, Evolution of jaw mechanics in ornithopod dinosaurs. Advances in Anatomy, Cell Biology, and Cell Biology v. 87, p. 1-110.

Weishampel, D. B. and Horner, J. R. 1990. Hadrosauridae. Chap. 26 in The Dinosauria, D. B. Weishampel, P. Dodson and H. Osmolska (Eds.), University of California Press (Berkeley). 534-561.


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