Corythosaurus

''Corythosaurus'' (; ) is a genus of hadrosaurid "duck-billed" dinosaur from the Late Cretaceous period, about 77–75.7 million years ago, in what is now western North America. Its name is derived from the Greek word κόρυς, meaning "helmet", named and described in 1914 by Barnum Brown. ''Corythosaurus'' is now thought to be a lambeosaurine, thus related to ''Lambeosaurus'', '' Nipponosaurus'', '' Velafrons'', ''Hypacrosaurus'', and '' Olorotitan''. ''Corythosaurus'' has an estimated length of and has a skull, including the crest, that is tall.

''Corythosaurus'' is known from many complete specimens, including the nearly complete holotype found by Brown in 1911. The holotype skeleton is only missing the last section of the tail and part of the front legs, but was preserved with impressions of polygonal scales. ''Corythosaurus'' is known from many skulls with tall crests that resemble those of the cassowary and a Corinthian helmet. The most likely function of the crest is thought to be vocalization. As in a trombone, sound waves would travel through many chambers in the crest and then get amplified when ''Corythosaurus'' exhaled. One ''Corythosaurus'' specimen has even been preserved with its last meal in its chest cavity. Inside the cavity were remains of conifer needles, seeds, twigs, and fruits, suggesting that ''Corythosaurus'' probably fed on all of these.

The two species of ''Corythosaurus'' are both present in slightly different levels of the Dinosaur Park Formation. Both still co-existed with theropods and other ornithischians, like '' Daspletosaurus'', '' Brachylophosaurus'', '' Parasaurolophus'', '' Scolosaurus'', and ''Chasmosaurus''.

Discovery and species

The first specimen, AMNH 5240, was discovered in 1911 by Barnum Brown in Red Deer River of Alberta and secured by him in the Fall of 1912. As well as an almost complete skeleton, the find was notable because impressions of much of the creature's skin had also survived. The specimen came from the Belly River Group of the province. The left or underside of the skeleton was preserved in carbonaceous clay, making it difficult to expose the skin to the elements. The skeleton was articulated and only missing about the last of the tail and front legs. Both scapulae and coracoids are preserved in position, but the rest of the front legs are gone (except for phalanges and pieces of the humeri, ulnae, and radii). Apparently, the remaining front legs were weathered or eroded away. Impressions of the integument were preserved covering over a large part of the skeleton’s outlining and shows the form of the body. Another specimen, AMNH 5338, was found in 1914 by Brown and Peter Kaisen. Both specimens are now housed in the American Museum of Natural History in their original death poses.

The type species, ''Corythosaurus casuarius'', was named by Barnum Brown in 1914, based on the first specimen collected by him in 1912. AMNH 5240 is thus the holotype. In 1916, the original author, Brown, published a more detailed description that was also based on AMNH 5338, which is therefore the plesiotype. ''Corythosaurus'' is among many lambeosaurines that possess crests and it was the crest that lends ''Corythosaurus'' its name. The generic name ''Corythosaurus'' is derived from the Greek κόρυθος,(''korythos''), "Corinthian helmet", and means "helmeted lizard". The specific name, ''casuarius'', refers to the cassowary, a bird with a similar skull crest. The full binomial of ''Corythosaurus casuarius'' thus means "Cassowary-like reptile, with a Corinthian helmet crest".

The two best preserved specimens of ''Corythosaurus'', found by Charles H. Sternberg in 1912, were lost on December 6, 1916, while being carried by the '' SS Mount Temple'' to the United Kingdom during World War I. They were being sent to Arthur Smith Woodward, a paleontologist of the British Museum of Natural History in England, when the ship transporting them was sunk by the German merchant raider in the middle of the ocean.p. 495 in Tanke, D.H. & Carpenter, K. (2001).

There were formerly up to seven species described, including ''C. casuarius'', ''C. bicristatus'' (Parks 1935), ''C. brevicristatus'' (Parks 1935), ''C. excavatus'' (Gilmore 1923), ''C. frontalis'' (Parks 1935), and ''C. intermedius'' (Parks 1923). In 1975, Peter Dodson studied the differences between the skulls and crests of different species of lambeosaurine dinosaurs. He found that the differences in size and shape may have actually been related to the sex and age of the animal. Only one species is currently recognized for certain, ''C. casuarius'', although ''C. intermedius'' has been recognized as valid in some studies. It is based on specimen ROM 776, a skull found by Levi Sternberg in 1920, was named by William Parks in 1923. Originally, he named it '' Stephanosaurus intermedius'' earlier that year. The specific name of ''C. intermedius'' is derived from its apparent intermediate position according to Parks. ''C. intermedius'' lived at a slightly later time in the Campanian than ''C. casuarius'' and the two species are not identical, which supported the separation of them in a 2009 study. The invalid species, ''C. excavatus'' (specimen UALVP 13), was based on only a skull found in 1920 and wouldn't be reunited with the rest of its remains until 2012.

Description

Size

Benson ''et al.'' (2012) estimated that ''Corythosaurus'' has an average length of . In 1962, Edwin H. Colbert used models of specific dinosaurs, including ''Corythosaurus'', to estimate their weight. The ''Corythosaurus'' model used was modelled by Vincent Fusco, after a mounted skeleton, and supervised by Barnum Brown. After testing, it was concluded that the average weight of ''Corythosaurus'' was . The total length of ''Corythosaurus'' specimen AMNH 5240 was found to be long, with a weight close to . In 2016, Gregory S. Paul estimated that ''C. casuarius'' reached long and in weight and that ''C. intermedius'' reached in length and in weight. A "morphologically adult-sized specimen" of ''C. casuarius'' measured approximately long.

Proportionally, the skull is much shorter and smaller than that of ''Edmontosaurus'' (formerly '' Trachodon''), '' Kritosaurus'', or '' Saurolophus''. But, when including its crest, its superficial area is almost as large.

Skull

Over twenty skulls have been found from this dinosaur. As with other lambeosaurines, the animal bore a tall, elaborate, bony crest atop its skull that contained the elongate narial passages. The narial passages extended into the crest, first into separate pockets in the sides, then into a single central chamber, and onward into the respiratory system. The skull of the type specimen has no dermal impressions on it. During preservation, it was compressed laterally and the width is now about two-thirds of what it would have been in real life. According to Brown, the compression also caused the nasals to shift where they pressed down on the premaxillaries. Because they were pressed on the premaxillaries, the nasals would have closed the nares. Apart from the compression, the skull appears to be normal. Contrary to what Brown assumed, the areas concerned were fully part of the praemaxillae.

As aforementioned, the crests of ''Corythosaurus'' resemble that of a cassowary or a Corinthian helmet. They are formed by a combination of the praemaxillae, nasals, prefrontals, and frontals, as in ''Saurolophus'', but instead of projecting backwards as a spine, they rise up to make the highest point above the orbit. The two halves of the crest are separated by a median suture. In front of the orbit, the crest is made of thick bone.

The nasals make up most of the crest. Brown assumed that they extended from the beaks' tip to the highest spot along the crest and that, unlike those in other genera, the nasals meet in the center and are not separated in front by an ascending premaxillary process. However, Brown mistook the praemaxillae for the nasals. The snout is actually largely formed by them and they do separate the nasals. Brown also thought that, on the top and back of the crest, the whole external face is covered by the frontals. Again he made a mistake, as what he assumed to be the frontals are in fact the nasals. The nasals end at the back of the squamosals in a hooked, short process. The prefrontals also make up part of the crest. However, Brown mistook the lower upper branch of the praemaxilla for the prefrontal. The actual prefrontal, which is triangular in shape, is located at the side of the crest base. It was seen by Brown as a part of the frontal. The real frontals, which are largely internal to the crest base structure, are not visible from the side.

The mouth of the holotype of ''Corythosaurus'' is narrow. The praemaxillae each form two long folds that enclose air passages extending the narial passages to the front of the snout. There, they end in narrow openings, sometimes called "pseudonares", which are false bony nostrils. These were mistaken by Brown for the real nares or nostrils. These are actually situated inside the crest, above the eye sockets. As in ''Saurolophus'', the expanded portion of the premaxillary in front of the pseudonaris' opening is elongate. By comparison, the bill of ''Kritosaurus'' is short and the pseudonares extend far forward. At the end of the ''Corythosaurus'' bill, the two pseudonares unite into one. Because of his incorrect identification, Brown assumed that the holotype's inferior process of the premaxillary was shorter than in ''Kritosaurus'' and ''Saurolophus'' and that the process does not unite with the lacrimal, which is another difference from those genera. The praemaxilla actually does touch the lacrimal and extends to the rear until well behind the eye socket.

The lower jaw of the holotype is long and deep. The total length of the crest from the beak to the uppermost tip of the type specimen is , its total length is , and its height is .

Soft tissue

In the holotype of ''C. casuarius'', the sides and tail are covered in scales of several types. Polygonal tuberculate scales, covered in small bumps, vary in size across the body. Conical limpet-like scales are only preserved on a fold of skin preserved on the back of the tibia, but this was probably from the bottom of the belly instead of the leg. Separating the polygonal scales of ''C. casuarius'' are shieldlike scales, arranged close together in rows. Ossified tendons are present on all the vertebrae, except for those in the cervical region. On no vertebrae do the tendons extend below the transverse processes. Each tendon is flattened at its origin, transversely ovoid in the central rod, and ends at a rounded point.

Aside from those found on ''Corythosaurus casuarius'', extensive skin impressions have been found on ''Edmontosaurus annectens'' and notable integument has also been found on '' Brachylophosaurus canadensis'', '' Gryposaurus notabilis'', '' Parasaurolophus walkeri'', '' Lambeosaurus magnicristatus'', ''L. lambei'', ''Saurolophus angustirsotris'', and on unidentified ornithopods. Of these, ''L. lambei'', ''C. casuarius'', ''G. notabilis'', ''P. walkeri'', and ''S. angustirsotris'' have preserved polygonal scales. The scales on ''L. lambei'', ''S. angustirostris'', and ''C. casuarius'' are all similar. ''Corythosaurus'' is one of very few hadrosaurids which have preserved skin impressions on the hind limbs and feet. A study in 2013 showed that, amongst hadrosaurids, '' Saurolophus angustirostris'' preserved the best and most complete foot and limb integument, although other species like '' S. osborni'', '' Edmontosaurus annectens'', and ''Lambeosaurus lambei'' (= ''L. clavinitialis'') share a fair amount of preserved tissue on those regions.

It was once thought that this dinosaur lived mostly in the water, due to the appearance of webbed hands and feet. However, it was later discovered that the so-called "webs" were in fact deflated padding, much like that found on many modern mammals.

Distinguishing characteristics

A set of characters were indicated by Barnum Brown in 1914 to distinguish ''Corythosaurus'' from all other hadrosaurids from Alberta. These include a comparatively short skull with a high helmet-like crest formed by the nasals, prefrontals, and frontals; the nasals not being separated in front by the premaxillaries; a narrow beak with an expansion in front of an elongated naris; and a small narial opening.

In 1916, Brown expanded the character set to include even more features. In the revised version, these extra features include a comparatively short skull with a high helmet-like crest formed by nasals, prefrontals, and frontals; the nasals not being separated in front by premaxillaries; a narrow beak; expanded section in front of the elongated nares; a small narial opening; a vertebral formula of 15 cervicals, 19 dorsals, 8 sacrals, and 61+ caudals; possession of dorsal spines of a medium height; high anterior caudal spines; long chevrons; long scapulae that possess a blade of medium width; a radius considerably longer than the humerus; comparatively short metacarpals, an anteriorly decurved ilium; a long ischium with a foot-like terminal expansion; a pubis with an anterior blade that is short and broadly expanded at the end; a femur that is longer than the tibia; the phalanges of pes are short; that the integument over the sides and tail composed of polygonal tuberculate scales without pattern, but graded in size in different parts of the body; and a belly with longitudinal rows of large conical limpet-like scales separated by uniformly large polygonal tubercles. Again, the presumed traits of the snout are incorrect because Brown confused the praemaxillae with the nasal bones and the nasal bones with the frontals. Most of the postcranial traits are today known to be shared with various other lambeosaurines.

Classification

Originally, Brown referred to ''Corythosaurus'' as a member of the family Trachodontidae (now Hadrosauridae). Inside Trachodontidae were the subfamilies Trachodontinae and Saurolophinae. Brown classified '' Hadrosaurus'', ''Trachodon'', '' Claosaurus'', and ''Kritosaurus'' in Trachodontinae, whereas he classified ''Corythosaurus'', ''Stephanosaurus'', and ''Saurolophus'' in Saurolophinae.

Later, Brown revised the phylogeny of ''Corythosaurus'', finding that it was closely related and possibly ancestral to ''Hypacrosaurus''. The only differences he found between them were the development of the vertebrae and the proportions of the legs. During a study of dinosaurian ilia in the 1920s, Alfred Sherwood Romer proposed that the two orders of dinosaurs might have evolved separately and that birds, based on the shape and proportions of their ilia, might truly be specialized ornithischians. He used both ''Tyrannosaurus'' and ''Corythosaurus'' as a base model to analyze which theory is more likely true. He found that, even though birds are thought of as saurischians, it is very plausible for them to have evolved their specific pelvic musculature and anatomy if they evolved from ornithschians like ''Corythosaurus''. However, even though the pelvic structure of ''Corythosaurus'' and other ornithischians does bear a greater superficial resemblance to birds than the saurischian pelvis does, birds are now known to be highly derived maniraptoran theropods.

''Corythosaurus'' is currently classified as a hadrosaurid in the subfamily Lambeosaurinae. It is related to other hadrosaurs such as ''Hypacrosaurus'', ''Lambeosaurus'', and '' Olorotitan''. With the exception of '' Olorotitan'', they all share similar looking skulls and crests. However, research published in 2003 has suggested that even though it possesses a unique crest, '' Olorotitan'' is ''Corythosaurus'''s closest known relative. Benson ''et al.'' (2012) found that ''Corythosaurus'' was closely related to '' Velafrons'', '' Nipponosaurus'', and ''Hypacrosaurus'', with them forming a group of fan-crested lambeosaurines.

In 2014, a study including the description of '' Zhanghenglong'' was published in the journal '' PLOS ONE''. The study included an almost complete cladogram of hadrosauroid relationships, including ''Corythosaurus'' as the most derived lambeosaurine and being the sister taxon to ''Hypacrosaurus''. The below cladogram is a simplified version including only Lambeosaurini.

Paleobiology

Comparisons between the scleral rings of ''Corythosaurus'' and modern reptiles suggest that it may have been cathemeral, meaning it was most active throughout the day at short intervals. The sense of hearing in hadrosaurids, specifically such as '' Lophorhothon'', also seems to have been greatly developed because of an elongated lagena. The presence of a thin stapes (an ear bone that is rod-like in reptiles), combined with a large eardrum, implies the existence of a sensitive middle ear. It is possible that hadrosaurid ears are sensitive enough to detect as much sound as a modern crocodilian.

Crest function

The internal structures of the crest of ''Corythosaurus'' are quite complex, making possible a call that could be used as a warning or for attracting a mate. Nasal passageways of ''Corythosaurus'', as well as ''Hypacrosaurus'' and ''Lambeosaurus'', are S-shaped, with ''Parasaurolophus'' only possessing U-shaped tubes. Any vocalization would travel through these elaborate chambers and probably get amplified. Scientists speculate that ''Corythosaurus'' could make loud, low pitched cries "like a wind or brass instrument", such as a trombone. The sounds could serve to alert other ''Corythosaurus'' to the presence of food or a potential threat from a predator. The nasal passages emit low-frequency sounds when ''Corythosaurus'' exhaled. The individual crests would produce different sounds, so it is likely that each species of lambeosaurine would have had a unique sound. However, even though the range for different lambeosaurine nasal passages vary greatly, they all probably made low-pitched sounds. This might be because low sounds (below 400 Hz) travel a set distance in any environment, while higher sounds (above 400 Hz) have a larger spread in the distance travelled.

When they were first described, crested hadrosaurs were thought to be aquatic, an assessment based incorrectly on webbing that is now known to be padding. The theory was that the animals could swim deep in the water and use the crest to store air to breathe. However, it has now been proven that the crest did not have any holes in the end and the water pressure at even would be too great for the lungs to be able to inflate.p. 35 in Norrell, M. ''et al.'' (2000).

Growth

''Corythosaurus casuarius'' is one of a few lambeosaurines, along with ''Lambeosaurus lambei'', ''Hypacrosaurus stebingeri'', and ''H. altispinus'', to have had surviving fossilized juveniles assigned to it. Juveniles are harder to assign to species because, at a young age, they lack the distinctive larger crests of adults. As they age, lambeosaurine crests tend to grow and become more prominent come maturity. In the Dinosaur Park Formation, over fifty articulated specimens have been found that come from many different genera. Among them, juveniles are hard to identify at the species level. Earlier, four genera and thirteen species were recognized from the formation's area when paleontologists used differences in size and crest shape to differentiate taxa. The smallest specimens were identified as ''Tetragonosaurus'', now seen as a synonym of ''Procheneosaurus'', and the largest skeletons were called either ''Corythosaurus'' or ''Lambeosaurus''. An adult was even identified as '' Parasaurolophus''. Small lambeosaurines from the Horseshoe Canyon Formation were referred to '' Cheneosaurus''.

''Corythosaurus'' started developing its crest when they were half the size of adults, but ''Parasaurolophus'' juveniles grew crests when they were only 25% as long as adults. Juvenile ''Corythosaurus'', along with adults, had a premaxilla-nasal fontanelle. Young and adult ''Corythosaurus'' are similar to ''Lambeosaurus'' and ''Hypacrosaurus'', but dissimilar to ''Parasaurolophus'' in that the sutures of the skull are sinuous, not smooth and straight. This feature helps to differentiate Parasaurolophini from Lambeosaurini. Generally, the crests of juveniles of lambeosaurines like ''Corythosaurus'', ''Lambeosaurus'', ''Hypacrosaurus stebingeri'', parasaurolophines like ''Parasaurolophus'', and primitive lambeosaurines like ''Kazaklambia'' are quite alike, although other features can be used to distinguish them.

Work by Dodson (1975) recognized that there were many less taxa present in Alberta. ''Tetragonosaurus'' was found to be juveniles of ''Corythosaurus'' or ''Lambeosaurus''. ''T. erectofrons'' was assigned to ''Corythosaurus'' based largely on biometric information. The only non-typic specimen of ''Tetragonosaurus'', assigned to ''T. erectofrons'', was later found to be referable to ''Hypacrosaurus'', although the holotype of the species was still found to be assignable to ''Corythosaurus''.

Diet

''Corythosaurus'' was an ornithopod, therefore being a herbivore. Benson ''et al.'' (2012) realized that the beak of ''Corythosaurus'' was shallow and delicate, concluding that it must have been used to feed upon soft vegetation. Based on the climate of the Late Cretaceous, they guessed that ''Corythosaurus'' would have been a selective feeder, eating only the juiciest fruits and youngest leaves. A ''Corythosaurus'' specimen has been preserved with its last meal in its chest cavity. Inside the cavity were remains of conifer needles, seeds, twigs, and fruits, meaning that ''Corythosaurus'' probably fed on all of these, implying that it was a browser.

Paleoecology

Fossils have been found in the upper Oldman Formation and lower Dinosaur Park Formation of Canada. The Oldman Formation dates to the Campanian, about 77.5 to 76.5 million years ago, and the Dinosaur Park Formation dates from 76.6 to 74.8 million years ago. ''Corythosaurus'' lived from ~77–75.7 million years ago. In the Dinosaur Park Formation, ''C. casuarius'' lived from 76.6 to 75.9 mya, with ''C. intermedius'' living from 75.8 to 75.7 mya. In the Oldman Formation, ''C. casuarius'', the only species of ''Corythosaurus'' from the deposits, lived about 77 to 76.5 mya. The holotype specimen was clearly a carcass that had floated up on a beach, as '' Unio'' shells, water-worn bones, and a baenid turtle were preserved all around it. ''Corythosaurus'' probably lived in a woodland forest and might have occasionally wandered into swampy areas.

A limited fauna is known from the upper section of the Oldman Formation and ''Corythosaurus casuarius'', as well as ''C. intermedius'', are among the taxa. Also from the section of the formation are the theropods '' Daspletosaurus'' and '' Saurornitholestes'', the hadrosaurids '' Brachylophosaurus'', '' Gryposaurus'', and '' Parasaurolophus'', the ankylosaurid '' Scolosaurus'', and the ceratopsians '' Coronosaurus'' and ''Chasmosaurus''. Other genera are known, but do not persist from the upper section of the formation, therefore not being contemporaries of ''Corythosaurus''.

''Corythosaurus casuarius'' is widespread throughout the lower unit of the Dinosaur Park Formation. In it, ''Corythosaurus'' was found to be closely associated with the ceratopsid '' Centrosaurus apertus''. Their associating was found in the Dinosaur Park, Judith River, and Mesaverde formations, as well as the Wind River Basin and the Wheatland County area. ''Corythosaurus'' lived alongside numerous other giant herbivores, such as the hadrosaurids ''Gryposaurus'' and ''Parasaurolophus'', the ceratopsids ''Centrosaurus'' and ''Chasmosaurus'', and the ankylosaurids ''Scolosaurus'', '' Edmontonia'', and '' Dyoplosaurus'' in the earliest stages of the formation, '' Dyoplosaurus'', '' Panoplosaurus'', and '' Euoplocephalus'' in the middle age, and ''Euoplocephalus'' alone in later stages of the formation. Studies of the jaw anatomy and mechanics of these dinosaurs suggests they probably all occupied slightly different ecological niches in order to avoid direct competition for food in such a crowded eco-space. The only large predators known from the same levels of the formation as ''Corythosaurus'' are the tyrannosaurids '' Gorgosaurus libratus'' and an unnamed species of '' Daspletosaurus''.

Thomas M. Lehman has observed that ''Corythosaurus'' hasn't been discovered outside of southern Alberta, even though it is one of the most abundant Judithian dinosaurs in the region. Large herbivores like the hadrosaurs living in North America during the Late Cretaceous had "remarkably small geographic ranges" despite their large body size and high mobility. This restricted distribution strongly contrasts with modern mammalian faunas whose large herbivores' ranges "typical y... span much of a continent."

See also

* Timeline of hadrosaur research

Footnotes

p. 158 in Norrell, M. ''et al.'' (2000).
p. 559 in Brown, B. (1914).
p. 560 in Brown, B. (1914).
p. 159 in Norrell, M. ''et al.'' (2000).


p. 561 in Brown, B. (1914).
p. 710 in Brown, B. (1916).
p. 711 in Brown, B. (1916).
p. 345 in Benson ''et al.'' (2012).
p. 563 in Brown, B. (1914).
p. 709 in Brown, B. (1916).
p. 41 in Norrell, M. ''et al''. (2000).
pp. 712–715 in Brown, B. (1916).

p. 564 in Brown, B. (1914).
p. 565 in Brown, B. (1914).
Dodson, Peter & Britt, Brooks & Carpenter, Kenneth & Forster, Catherine A. & Gillette, David D. & Norell, Mark A. & Olshevsky, George & Parrish, J. Michael & Weishampel, David B. (1994). ''The Age of Dinosaurs''. Publications International, LTD. p. 137. .


pp. 54–82 in Currie, P.J. & Koppelhus, E.B. (2005).
pp. 1117–1135 in Arbour, V.M. ''et al.'' (2009).
pp. 310–328 in Tanke, D.H. & Carpenter, K. (2001).

References

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External links

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{{Taxonbar, from=Q131078

Lambeosaurinae
Dinosaur genera
Campanian dinosaurs
Oldman Formation
Dinosaur Park Formation
Taxa named by Barnum Brown
Fossil taxa described in 1914
Dinosaurs of Canada