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Caenagnathidae is a family of derived caenagnathoid
dinosaur Dinosaurs are a diverse group of reptiles of the clade Dinosauria. They first appeared during the Triassic Geological period, period, between 243 and 233.23 million years ago (mya), although the exact origin and timing of the #Evolutio ...
s from the
Cretaceous The Cretaceous ( ) is a geological period that lasted from about 143.1 to 66 mya (unit), million years ago (Mya). It is the third and final period of the Mesozoic Era (geology), Era, as well as the longest. At around 77.1 million years, it is the ...
of
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and
Asia Asia ( , ) is the largest continent in the world by both land area and population. It covers an area of more than 44 million square kilometres, about 30% of Earth's total land area and 8% of Earth's total surface area. The continent, which ...
. They are a member of the
Oviraptorosauria Oviraptorosaurs ("egg thief lizards") are a group of feathered maniraptoran dinosaurs from the Cretaceous Period (geology), Period of what are now Asia and North America. They are distinct for their characteristically short, beaked, parrot-like s ...
, and relatives of the Oviraptoridae. Like other oviraptorosaurs, caenagnathids had specialized beaks, long necks, and short tails, and would have been covered in feathers. The relationships of caenagnathids were long a puzzle. The family was originally named by Raymond Martin Sternberg in 1940 as a family of flightless birds. The discovery of skeletons of the related oviraptorids revealed that they were in fact non-avian theropods, and the discovery of more complete caenagnathid remains revealed that ''Chirostenotes pergracilis'', originally named on the basis of a pair of hands, and ''Citipes elegans'', originally thought to be an ornithomimid, named from a foot, were caenagnathids as well.


Discovery

The name ''Caenagnathus'' (and hence Caenagnathidae) means "recent jaws"—when first discovered, it was thought that caenagnathids were close relatives of paleognath birds (such as the
ostrich Ostriches are large flightless birds. Two living species are recognised, the common ostrich, native to large parts of sub-Saharan Africa, and the Somali ostrich, native to the Horn of Africa. They are the heaviest and largest living birds, w ...
) based on features of the lower jaw. Since it would be unusual to find a recent group of birds in the Cretaceous, the name "recent jaws" was applied. Most paleontologists, however, now think that the birdlike features of the jaw were acquired convergently with modern birds. Barsbold, R., Maryańska, T., and Osmólska, H. (1990). "Oviraptorosauria." pg. 249-258 ''in'' Weishampel, Dodson, and Osmolska (eds.) ''The Dinosauria'', University of California Press (Berkeley).


Description

Caenagnathids were some of the largest oviraptorosaurs that ever existed. The largest members are represented by the enormous '' Beibeilong'' and ''
Gigantoraptor ''Gigantoraptor'' () is a genus of large oviraptorosaur dinosaur that lived in Asia during the Late Cretaceous period. It is known from the Iren Dabasu Formation of Inner Mongolia, where the first remains were found in 2005. ''Gigantoraptor'' w ...
'', estimated around in length.Supplementary Information
Other caenagnathids were slightly smaller, such as the long ''
Hagryphus ''Hagryphus'' (meaning "Ha (mythology), Ha's griffin") is a monospecific genus of caenagnathidae, caenagnathid dinosaur from southern Utah that lived during the Late Cretaceous (upper Campanian stage, 75.95 Ma) in what is now the Kaiparowits Form ...
'', or the long '' Anzu''. Overall, the anatomy of the caenagnathids is similar to that of the closely related Oviraptoridae, but there are a number of differences. In particular, caenagnathid jaws exhibited a distinct suite of specializations not seen in other oviraptorosaurs. Compared to the oviraptorids, the jaws tended to be relatively long and shallow, suggesting that the bite was not as powerful. The inside of the lower jaws also bore a complex series of ridges and toothlike processes, as well as a pair of horizontal, shelf-like structures. Furthermore, the jaws were unusual in being hollow and air filled, apparently being connected to the air sac system. Analysis of oviraptorosaur functional morphology reveals that caenagnathids were not as well suited to herbivory as more primitive oviraptorosaurs, and their close relatives, the oviraptorids. Their mandibles have a lower mechanical advantage anteriorly but not posteriorly, similar to the dromaeosaurids, and are less robust, which makes them more suited to quicker prey capture, with their pointed beaks aiding in slashing prey. Caenagnathids also tended to be more lightly built than the oviraptorids. They had slender arms and long, gracile legs, although they lacked the extreme cursorial specializations seen in avimimids and ''Caudipteryx''.


Classification

The family Caenagnathidae, together with its sister group the Oviraptoridae, comprises the superfamily Caenagnathoidea. In phylogenetic taxonomy, the
clade In biology, a clade (), also known as a Monophyly, monophyletic group or natural group, is a group of organisms that is composed of a common ancestor and all of its descendants. Clades are the fundamental unit of cladistics, a modern approach t ...
Caenagnathidae is defined as the most inclusive group containing '' Caenagnathus collinsi'' but not '' Oviraptor philoceratops''. While before 2010s only about two to six species were commonly recognized as belonging to the Caenagnathidae, currently that number may be much greater, with new discoveries and theories about older species that may inflate this number to up to ten. Much of this historical difference centers on the first caenagnathid to be described, ''Chirostenotes pergracilis''. Due to the poor preservation of most caenagnathid remains and resulting misidentifications, different bones and different specimens of ''Chirostenotes'' have historically been assigned to a number of different species. For example, the feet of one species, named ''Macrophalangia canadensis'', were known from the same region from which ''Chirostenotes pergracilis'' was recovered, but the discovery of a new specimen with both hands and feet preserved provided the support to combine them, while the later discovery of a partial skull with hands and feet suggested that ''Chirostenotes'' and ''Caenagnathus'' were the same animal, and current studies of caenagnathid relationships continue to find them as closely related genera. Hendrickx and colleagues (2015) defined a subgroup of Caenagnathidae, the Caenagnathinae, as all caenagnathids more closely related to ''Caenagnathus collinsi'' than to ''Elmisaurus rarus''. The group Elmisaurinae is defined as including all species more closely related to ''Elmisaurus rarus'' than to ''Caenagnathus collinsi''. The
cladogram A cladogram (from Greek language, Greek ''clados'' "branch" and ''gramma'' "character") is a diagram used in cladistics to show relations among organisms. A cladogram is not, however, an Phylogenetic tree, evolutionary tree because it does not s ...
below follows an analysis by Gregory Funston in 2020.


Evolution

The earliest known caenagnathid is ''Microvenator celer'', from the Early Cretaceous Cloverly Formation. Caenagnathids likely dispersed to Asia from North America with some caenagnathids later reappearing in western North America, during the Campanian. Caenagnathids showed considerable variation in form. The tiny jaws of ''Caenagnathasia'' suggest a small animal, perhaps the size of a turkey. '' Anzu wyliei'', from the Hell Creek Formation is a much larger animal, considerably larger than a human. If ''Gigantoraptor erlianensis'' is a caenagnathid, then it would represent far and away the largest member of the group, measuring up to in length and weighing up to . Their beaks also show considerable variation; that of ''Caenagnathasia'' is relatively short and deep, while that of ''Caenagnathus'' is long and shovel-shaped. This variation in size and beak shape suggests that caenagnathids evolved to exploit a range of ecological niches. Caenagnathids persisted up until the end of the Cretaceous period, as shown by the presence of ''Anzu'' and another, unnamed species of elmisaurine (all caenagnathids closer to ''Elmisaurus'' than to ''Caenagnathus)'' in the late Maastrichtian Hell Creek Formation, before vanishing at the end of the Cretaceous along with all other non-avian dinosaurs.


Species

Roughly a dozen caenagnathid species have been named, but it remains unclear how many are valid. Many species are known from fragmentary remains, such as jaws, hands, or feet, making comparisons between them difficult. ''Caenagnathus sternbergi'', for example, was described on the basis of a jaw bone. It has been interpreted as either the jaws of ''Chirostenotes pergracilis'' (described on the basis of a pair of hands) or ''Chirostenotes elegans'' (described on the basis of a foot), but because no complete skeleton is known, it is difficult to be certain which animal it belongs to. The relationships of other species remain in doubt. ''Gigantoraptor'' was originally interpreted as an oviraptorid, but may in fact represent a primitive caenagnathid. * '' Anzu wyliei'' - (
Hell Creek Formation The Hell Creek Formation is an intensively studied division of mostly Upper Cretaceous and some lower Paleocene rocks in North America, named for exposures studied along Hell Creek, near Jordan, Montana. The Formation (stratigraphy), formation s ...
, North Dakota and South Dakota, United States) * ''Apatoraptor pennatus'' - ( Horseshoe Canyon Formation, Alberta) * '' Beibeilong sinensis'' - ( Gaogou Formation, China) * '' Caenagnathasia martinsoni'' - (
Bissekty Formation The Bissekty Formation (sometimes referred to as Bissekt) is a formation (geology), geologic formation and Lagerstätte which outcrop, crops out in the Kyzyl Kum desert of Uzbekistan, and dates to the Late Cretaceous Period (geology), Period. Laid ...
, Uzbekistan) * '' Citipes elegans'' - (
Dinosaur Park Formation The Dinosaur Park Formation is the uppermost member of the Belly River Group (also known as the Judith River Group), a major geologic unit in southern Alberta. It was deposited during the Campanian stage of the Late Cretaceous, between about 7 ...
, Alberta, Canada) * '' Chirostenotes pergracilis'' - (
Dinosaur Park Formation The Dinosaur Park Formation is the uppermost member of the Belly River Group (also known as the Judith River Group), a major geologic unit in southern Alberta. It was deposited during the Campanian stage of the Late Cretaceous, between about 7 ...
, Alberta, Canada) * '' Caenagnathus collinsi'' - (
Dinosaur Park Formation The Dinosaur Park Formation is the uppermost member of the Belly River Group (also known as the Judith River Group), a major geologic unit in southern Alberta. It was deposited during the Campanian stage of the Late Cretaceous, between about 7 ...
, Alberta, Canada) * '' Elmisaurus rarus'' - ( Nemegt Formation, Mongolia) * '' Eoneophron infernalis'' - (
Hell Creek Formation The Hell Creek Formation is an intensively studied division of mostly Upper Cretaceous and some lower Paleocene rocks in North America, named for exposures studied along Hell Creek, near Jordan, Montana. The Formation (stratigraphy), formation s ...
,
South Dakota South Dakota (; Sioux language, Sioux: , ) is a U.S. state, state in the West North Central states, North Central region of the United States. It is also part of the Great Plains. South Dakota is named after the Dakota people, Dakota Sioux ...
) * '' Epichirostenotes curriei'' - ( Horseshoe Canyon Formation, Alberta, Canada) * '' Gigantoraptor erlianensis'' - ( Iren Dabasu Formation, Inner Mongolia, China) * '' Hagryphus giganteus'' - (
Kaiparowits Formation The Kaiparowits Formation is a sedimentary geological formation, rock formation found in the Kaiparowits Plateau in Grand Staircase–Escalante National Monument, in the southern part of Utah in the western United States. It is over 2800 feet (8 ...
, Utah, United States) * '' Leptorhynchos gaddisi'' - ( Aguja Formation, Texas, United States) *'' Nomingia gobiensis -'' ( Nemegt Formation, Mongolia) * '' Ojoraptorsaurus boerei'' - (
Ojo Alamo Formation The Ojo Alamo Formation is a geologic Formation (geology), formation in New Mexico spanning the Mesozoic/Cenozoic boundary. Non-avian dinosaur fossils have controversially been identified in beds of this formation dating from after the Cretaceous ...
, New Mexico, United States) Caenagnathids are only known from the Late Cretaceous of North America and Asia. The earliest and most primitive known caenagnathid is '' Caenagnathasia martinsoni'', from the Bissekty Formation of Uzbekistan.


See also

* Timeline of oviraptorosaur research


References


External links


Overview of Caenagnathidae by Jaime Headden.
{{Taxonbar, from=Q133539 Dinosaur families Cretaceous dinosaurs