TIMELINE
Palaeozaic era
Cambrian
period: (570 million years
ago) |
Ordovician period: (505 million years ago) |
Silurian period: (438 million years ago) |
Devonian period: (408 million years ago) |
Carboniforous period: (360 million years ago) |
6.
Permian period: (286 million years ago) |
Mesozaic era
Triassic period: 245 million
years ago |
Jurassic period: (208
million years ago) |
Cretaceous period: (144
million years ago) |
|
Theropods are a group of bipedal saurischian dinosaurs. Although they were primarily carnivorous, a number of theropod
groups evolved herbivory, omnivory, and insectivory. Theropods first appeared during the Carnian age of the late Triassic period about 230 million years ago and included the sole
large terrestrial carnivores from the Early Jurassic until at least the close of the
Cretaceous, about 65 Ma. Today,
they are represented by the 9,900 living species of birds, which evolved in the Jurassic from small specialized coelurosaurian dinosaurs.
Among the features linking theropods to birds are the three-toed foot, a furcula (wishbone), air-filled bones and
(in some cases) feathers and brooding of the eggs.
While historically generalized as exclusively carnivorous dinosaurs,
theropods in fact displayed a wide range of diets. All
early finds of theropod fossils showed them to be primarily carnivorous. Theropod specimens known to scientists
in the 19th and early 20th centuries all showed sharp teeth with serrated edges
for cutting flesh, and some specimens even showed direct evidence of predatory
behavior. For example, a Compsognathus fossil was found with a lizard in its stomach, and a Velociraptor specimen was
found locked in combat with a Protoceratops (a type of ornithischian dinosaur).
The first confirmed non-carnivorous theropods found were the therizinosaurs, originally
known as segnosaurs. First thought to be prosauropods, these enigmatic dinosaurs were later
proven to be highly specialized, herbivorous theropods. Therizinosaurs possessed large
abdomens for processing plant food, and small heads with beaks and leaf-shaped
teeth. Further study of maniraptoran theropods and their relationships
showed that therizinosaurs were not the only member of this group to abandon
carnivory. Several other lineages of maniraptors show adaptations for an omnivorous diet, including seed-eating
(some troodontids) and
insect-eating (many avialans and alvarezsaurs. oviraptorosaurs, ornithomimosaurs and advanced troodontids
were likely omnivorous as well, and some theropods (such as Masiakasaurus and the spinosaurids) appear to have
specialized in catching fish
Mesozoic theropods were also very diverse in terms of skin texture and
covering. Though feather-like structures are known in the related ornithischian dinosaurs, evidence
of feathers or feather-like structures has not been reported for any theropods
less advanced than the coelurosaurs. More primitive theropods show
evidence that their skin was covered in small, bumpy scales. In some species,
these were interspersed with larger scales with bony cores, or osteoderms. This
type of skin is best known in the ceratosaur Carnotaurus, which has been preserved with
extensive skin impressions.
The most primitive known protofeathered theropods are the compsognathids and early
tyrannosauroids,
both coelurosaurs. These early forms had feathers which were relatively short
and composed of simple, possibly branching filaments. Simple filaments are also seen in therizinosaurs, which also possessed large,
stiffened "quill"-like feathers.
Most feathered theropods, including modern birds, usually retain scales only
on the feet. Some forms seem to have mixed feathers elsewhere on the body as
well. Scansoriopteryx preserved scales on the
underside of the tail, and
Juravenator may have
been predominantly scaly with some simple filaments interspersed. On
the other hand, some theropods were completely covered with feathers, such as
the troodontid Anchiornis, which even had feathers on the feet
and toes
Contrary to the way theropods have often been reconstructed in art and the
popular media, the range of motion of theropod forelimbs was severely limited,
especially compared with the forelimb dexterity of humans and other primates.
Most
notably, theropods and other bipedal saurischian dinosaurs (including the
bipedal prosauropods) could not pronate their hands—that is, they could not rotate
the forearm so that the palms faced the ground or backwards towards the legs. In
humans, pronation is achieved by motion of the radius relative to the ulna (the two bones of the forearm). In saurischian
dinosaurs, however, the end of the radius near the elbow was actually locked
into a groove of the ulna, preventing any movement. Movement at the wrist was
also limited in many species, forcing the entire forearm and hand to move as a
single unit with little flexibility. In
theropods and prosauropods, the only way for the palm to face the ground would
have been by lateral splaying of the entire forelimb, as in a bird raising its
wing.
In carnosaurs
like Acrocanthosaurus, the hand itself retained
a relatively high degree of flexibility, with mobile fingers. This was also true
of more basal theropods such as herrerasaurs and dilophosaurs. Coelurosaurs showed a shift in the use of the
forearm, with greater flexibility at the shoulder allowing the arm to be raised
towards the horizontal plane, and to even greater degrees in flying birds. However, in coelurosaurs such as ornithomimosaurs and
especially dromaeosaurs, the hand itself had lost most
flexibility, with highly inflexible fingers. Dromaeosaurs and other maniraptorans also showed
increased mobility at the wrist not seen in other theropods, thanks to the
presence of a specialized half-moon shaped wrist bone (the semi-lunate carpal)
that allowed the whole hand to fold backward towards the forearm in the manner
of modern birds
During the late Triassic, a
number of primitive proto-theropod and theropod dinosaurs existed and evolved
alongside each other.
The earliest and most primitive of the carnivorous dinosaurs were Eoraptor of Argentina and the herrerasaurs. The
herrerasaurs existed during the early late Triassic (Late Carnian to Early Norian). They were found in North America and South America and possibly also India and Southern Africa. The herrerasaurs were characterised by a mosaic of primitive
and advanced features. Some paleontologists have in the past considered the
herrerasaurians to be members of Theropoda, while other theorized the group to
be basal
saurischians, and may even have evolved prior to the saurischian-ornithischian
split. Cladistic analysis following the discovery
of Tawa,
another Triassic dinosaur, suggests the herrerasaurs likely were early
theropods.
The earliest and most primitive unambiguous theropods (or alternatively,
"Eutheropoda" - 'True Theropods') are the Coelophysoidea. The Coelophysoidea were a group
of widely distributed, lightly built and potentially gregarious animals. They
included small hunters like Coelophysis and (possibly) larger predators
like Dilophosaurus.
These successful animals continued from the Late Carnian (early Late Triassic)
through to the Toarcian (late Early Jurassic). Although
in the early cladistic classifications they were included under the
Ceratosauria and considered
a side-branch of more advanced theropods, they may have been ancestral to all other theropods (which would make them a paraphyletic
group).
The somewhat more advanced ceratosaurs (including Ceratosaurus and Carnotaurus) appeared during the Early Jurassic
and continued through to the Late Jurassic in Laurasia. They competed alongside their more
anatomically advanced tetanuran relatives and—in the form of the abelisaur lineage—lasted to the end
of the Cretaceous in Gondwana.
The Tetanurae are more
specialised again than the ceratosaurs. They are subdivided into the basal Spinosauroidea (alternately
Megalosauroidea or Torvosauroidea) and the
more derived Avetheropoda. Megalosauridae were primarily Middle Jurassic to
Early Cretaceous predators, and their spinosaurid relatives' remains are mostly from
Early and Middle Cretaceous rocks. Avetheropoda, as their name indicates, were
more closely related to birds and are again divided into the Allosauroidea (the diverse carcharodontosaurs) and the Coelurosauria (a very large
and diverse dinosaur group including the birds).
Thus, during the late Jurassic, there were no fewer than four distinct
lineages of theropods—ceratosaurs, megalosaurs, allosaurs, and
coelurosaurs—preying on the abundance of small and large herbivorous dinosaurs.
All four groups survived into the Cretaceous, and three of those—the
ceratosaurs, coelurosaurs, and allosaurs—survived to end of the period, where
they were geographically separate, the ceratosaurs and allosaurs in Gondwana,
and the coelurosaurs in Laurasia.
Of all the theropod groups, the coelurosaurs were by far the most diverse.
Some coelurosaur groups that flourished during the Cretaceous were the tyrannosaurids (including
Tyrannosaurus) the
dromaeosaurids
(including Velociraptor and Deinonychus, which are remarkably similar in
form to the oldest known bird, Archaeopteryx[19][20]), the
bird-like troodontids and oviraptorosaurs, the ornithomimosaurs (or
"ostrich dinosaurs"), the strange giant-clawed herbivorous therizinosaurs, and the avialans, which include modern birds and is the only dinosaur lineage to
survive the Cretaceous-Paleogene
extinction event.
While the roots of these various groups are found in the Middle Jurassic, they
only became abundant during the Early Cretaceous. A few paleontologists, such as
Gregory S. Paul, have suggested that some or
all of these advanced theropods were actually descended from flying dinosaurs or
proto-birds like Archaeopteryx that lost the ability to fly and returned
to a terrestrial habitat.
The name Theropoda (meaning "beast feet") was first coined by O.C. Marsh
in 1881. Marsh
initially named Theropoda as a suborder to include the family Allosauridae, but later
expanded its scope, re-ranking it as an order to include a wide array of "carnivorous"
dinosaur families, including Megalosauridae, Compsognathidae, Ornithomimidae, Plateosauridae and Anchisauridae (now known to
be herbivorous prosauropods)
and Hallopodidae (now known to be relatives of
crocodilians). Due to the scope of Marsh's Order Theropoda, it came to replace a
previous taxonomic group that Marsh's rival E.D. Cope had created in 1866 for the
carnivorous dinosaurs, Goniopoda ("angled feet").
By the early 20th century, some paleontologists, such as Friedrich von
Huene, no longer considered carnivorous dinosaurs to have formed a natural
group. Huene abandoned the name Theropoda, instead using Harry Seeley's Order Saurischia, which Huene divided into the suborders
Coelurosauria and Pachypodosauria.
Huene placed most of the small theropod groups into Coelurosauria, and the large
theropods and prosauropods into Pachypodosauria, which he considered ancestral
to the Sauropoda (prosauropods
were still thought of as carnivorous at this time, owing to the incorrect
association of rauisuchian
skulls and teeth with prosauropod bodies, in animals such as Teratosaurus).[24] In W.D.
Matthew and Barnum Brown's
1922 description of the first known dromaeosaurid (Dromaeosaurus albertensis),
they became the first paleontologists to exclude prosauropods from the
carnivorous dinosaurs, and attempted to revive the name Goniopoda for that
group, though neither of these suggestions were accepted by other
scientists.
It was not until 1956 that Theropoda came back into use as a taxon containing the carnivorous dinosaurs and their
descendants, when Alfred
Romer re-classified the Order Saurischia into two suborders, Theropoda and
Sauropoda. This basic division has
survived into modern paleontology, with the exception of, again, the
Prosauropoda, which Romer included as an infraorder of theropods. Romer also maintained
a division between Coelurosauria and Carnosauria (which he also ranked as infraorders).
This dichotomy was upset by the discovery of Deinonychus and Deinocheirus in 1969, neither of which could
be classified easily as "carnosaurs" or "coelurosaurs." In light of these and
other discoveries, by the late 1970s Rinchen Barsbold created a new series of
theropod infraorders: Coelurosauria, Deinonychosauria, Oviraptorosauria, Carnosauria, Ornithomimosauria,
and Deinocheirosauria.
With the advent of cladistics
and phylogenetic nomenclature in the
1980s, and their development in the 1990s and 2000s, a clearer picture of
theropod relationships began to emerge. Several major theropod groups were named
by Jacques
Gauthier in 1986, including the clade
Tetanurae for one branch of a
basic theropod split with another group, the Ceratosauria. As more information about the link
between dinosaurs and birds came to light,
the more bird-like theropods were grouped in the clade Maniraptora (also named by Gauthier in 1986). These
new developments also came with a recognition among most scientists that birds
arose directly from maniraptoran theropods and, with the abandonment of ranks in
cladistic classification, the re-evaluation of birds as a subset of theropod
dinosaurs that happened to have survived the Mesozoic extinctions into the
present.
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