Information about Theropoda

Theropods
Fossil range: Triassic - Cretaceous
(excluding birds)

Scientific classification
Kingdom:Animalia
Phylum:Chordata
Class:Sauropsida
Superorder:Dinosauria
Order:Saurischia
Suborder:Theropoda
Marsh, 1881
Infraorders


Theropods ('beast feet') are a group of bipedal saurischian dinosaurs. Although they were primarily carnivorous, a number of theropod families evolved herbivory, during the Cretaceous Period. Theropods first appear during the Carnian age of the Late Triassic about 220 million years ago (MYA) and were the sole large terrestrial carnivores from the Early Jurassic until the close of the Cretaceous, about 65 MYA. Today, they are represented by the 9,300 living species of birds, which evolved in the Late 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.

Evolutionary history

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 from 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, though they are now thought to be basal saurischians, and may even have evolved prior to the saurischian-ornithischian split.

Enlarge picture
Theropod footprint


The earliest and most primitive unambiguous theropods (or alternatively, Eutheropoda - 'True Theropods') are the Coelophysidae. The Coelophysidae (Coelophysis, Megapnosaurus) were a group of widely distributed, lightly built and apparently gregarious animals. They included small hunters like Coelophysis and larger (6 meters) 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 (e.g. Rowe & Gauthier 1990), they may have been ancestral to all other theropods (which would make them a paraphyletic assemblage (e.g. Mortimer 2001, Carrano et al 2002).

The somewhat more advanced true Ceratosauria (including Ceratosaurus and Carnotaurus) appeared during the Early Jurassic and continued through to the Late Jurassic in Laurasia. They competed quite well alongside their more 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 Megalosauroidea (alternately Spinosauroidea or Torvosauroidea) and the Avetheropoda. They were most common during the Middle Jurassic but continued to the Middle Cretaceous. The latter clade - as their name indicates - were more closely related to birds and are again divided into the Carnosauria (including Allosaurus) and the Coelurosauria, a very large and diverse dinosaur group that was especially common during the Cretaceous.

Thus, during the late Jurassic, there were no fewer than four distinct lineages of theropods - ceratosaurs, megalosaurs, carnosaurs, and coelurosaurs - preying on the abundance of small and large herbivorous dinosaurs. All four groups survived into the Cretaceous, although only two - the abelisaurs and the coelurosaurs - seem to have made it to end of the period, where they were geographically separate, the abelisaurs in Gondwana, and the coelurosaurs in Asiamerica.

Of all the theropod groups, the coelurosaurs were by far the most diverse. Some coelurosaur clades that flourished during the Cretaceous are: tyrannosaurs, including the famous Tyrannosaurus rex, the dromaeosaurs, including Velociraptor and Deinonychus, which are remarkably similar in form to the oldest known bird, Archaeopteryx (Ostrom 1969, Paul 1988, Dingus & Rowe 1998), as well as the dromaeosaur-like Troodontidae, the omnivorous oviraptorosaurs, the omnivorous ornithomimids ("ostrich dinosaurs") and Therizinosauridae (giant-clawed herbivores) and the birds (the only dinosaur lineage to survive the end Cretaceous mass-extinction). While the roots of these various groups must have been in the Late or possibly even the Middle Jurassic, they only became abundant during the early Cretaceous. A few paleontologists, such as Gregory S. Paul, have suggested (Paul 1988, 2002) 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. While this hypothesis can explain why coelurosaurs are so rare during the Jurassic, more fossil evidence is needed before the exact relationships of advanced theropods can be accurately tested.

Systematics

Taxonomy

Phylogeny

The following cladogram is adapted from Weishampel et al., 2004.[1]

Theropoda
unnamed
Ceratosauria


Ceratosauridae


Abelisauroidea



Tetanurae

Carnosauria

Monolophosaurus


Allosauroidea


Coelurosauria




unnamed
Eumaniraptora

Deinonychosauria


Avialae












The largest theropods

Tyrannosaurus was the largest and most popular theropod known to the general public for many decades. Since its discovery, however, a number of other giant carnivorous dinosaurs have been described, including Spinosaurus, Carcharodontosaurus, Giganotosaurus, Tyrannotitan and Mapusaurus. In the film Jurassic Park 3, Spinosaurus is depicted as being larger than Tyrannosaurus and the original Spinosaurus specimens (as well as new fossils described in 2006) support this, showing that Spinosaurus was possibly 6 meters longer and at least 1 or more metric tons heavier than Tyrannosaurus (a size comparison of the largest theropods can be found in the article Dinosaur size). There is still no clear scientific explanation for exactly why these animals grew so much larger than the predators that came before and after them. Parallel to this, the smallest known theropod is the bee hummingbird.

References

1. ^ Weishampel, David B.; Dodson, Peter; Osmólska, Halszka (eds.) (2004). The Dinosauria, Second Edition. University of California Press., 861 pp.
  • Carrano, M. T., Sampson, S. D. & Forster, C. A., (2002), The osteology of Masiakasaurus knopfleri, a small abelisauroid (Dinosauria: Theropoda) from the Late Cretaceous of Madagascar. Journal of Vertebrate Paleontology Vol. 22, #3, pp. 510-534
  • Dingus, L. & Rowe, T. (1998), The Mistaken Extinction: Dinosaur Evolution and the Origin of Birds, Freeman
  • Kirkland, J. I., Zanno, L. E., Sampson, S. D., Clark, J. M. & DeBlieux, D. D., (2005) A primitive therizinosauroid dinosaurs from the Early Cretaceous of Utah, Nature: Vol. 435, pp. 84-87
  • Mortimer, M., (2001) "Rauhut's Thesis", Dinosaur Mailing List Archives, 4 Jul 2001
  • Ostrom, J.H. (1969). Osteology of Deinonychus antirrhopus, an unusual theropod from the Lower Cretaceous of Montana, Peabody Museum Nat. History Bull., 30, 1-165
  • Paul, G.S., (1988) Predatory Dinosaurs of the World Simon and Schuster Co., New York (ISBN 0-671-61946-2)

  • (2002) Dinosaurs of the Air (ISBN 0-8018-6763-0):
  • Rowe, T., & Gauthier, J., (1990) Ceratosauria. 151-168 in Weishampel, D. B., Dodson, P., & Osmólska, H. (eds.), The Dinosauria, University of California Press, Berkley, Los Angeles, Oxford.
The Triassic is a geologic period that extends from about 251 to 199 Ma (million years ago). As the first period of the Mesozoic Era, the Triassic follows the Permian and is followed by the Jurassic. Both the start and end of the Triassic are marked by major extinction events.
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The Cretaceous Period is one of the major divisions of the geologic timescale, reaching from the end of the Jurassic Period (i.e. from 145.5 ± 4.0 million years ago (Ma)) to the beginning of the Paleocene epoch of the Tertiary Period (about 65.5 ± 0.3 Ma).
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Tyrannosaurus
Osborn, 1905

Species
  • T. rex (type)
    Osborn, 1905
Synonyms
  • Manospondylus
    Cope, 1892
  • Dynamosaurus
    Osborn, 1905
  • ?Nanotyrannus

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Scientific classification or biological classification is a method by which biologists group and categorize species of organisms. Scientific classification also can be called scientific taxonomy, but should be distinguished from folk taxonomy, which lacks scientific basis.
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Chordata
Bateson, 1885

Typical Classes

See below

Chordates (phylum Chordata) are a group of animals that includes the vertebrates, together with several closely related invertebrates.
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Sauropsida*
Goodrich, 1916

Subclasses
  • Anapsida
  • Diapsida
Synonyms
  • Reptilia Laurenti, 1768
Reptiles are tetrapods and amniotes, animals whose embryos are surrounded by an amniotic membrane, and members of the class
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Dinosauria *
Owen, 1842

Orders & Suborders
  • Ornithischia
  • Cerapoda
  • Thyreophora
  • Saurischia

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Saurischia
Seeley, 1887

Suborders
  • Theropoda
  • Sauropodomorpha


Saurischia (from the Greek sauros (σαυρος) meaning 'lizard' and ischion (
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Othniel Charles Marsh (October 29, 1831 - March 18, 1899) was one of the pre-eminent paleontologists of the 19th century, who discovered and named many fossils found in the American West.

Marsh was born in Lockport, New York.
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order (Latin: ordo, plural ordines) is a rank between class and family (termed a taxon at that rank). The superorder is a rank between class and order. Exact details of formal nomenclature depend on the Nomenclature Code which applies.
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Carnosauria
von Huene, 1920

Families

Allosauridae
Carcharodontosauridae
Sinraptoridae

Carnosauria is a group of large predatory dinosaurs that lived during the Jurassic and Cretaceous periods.
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Ceratosauria
Marsh, 1884

Families

Abelisauridae
Ceratosauridae
Noasauridae

Ceratosaurs are a group of theropod dinosaurs defined as all theropods sharing a more recent common ancestry with Ceratosaurus than with birds.
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Deinonychosauria
Colbert & Russell, 1969

Families
  • Dromaeosauridae
  • Troodontidae
The Deinonychosauria ("fearsome claw lizards") were a successful clade of theropods in the Late Jurassic and Cretaceous Periods.
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Ornithomimosauria
Barsbold, 1976

Families
  • Garudimimidae
  • Harpymimidae
  • Deinocheiridae
  • Ornithomimidae


Ornithomimosaurs (meaning 'bird mimic lizards') or members of the clade Ornithomimosauria
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Oviraptorosauria
Barsbold, 1976

Families
  • Avimimidae
  • Caudipteridae
  • Caenagnathidae
  • Oviraptoridae


Oviraptorosaurs
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Bipedalism is standing, or moving for example by walking, running, or hopping, on two appendages (typically legs). An animal or machine that usually moves in a bipedal manner is known as a biped (/'baɪ.
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Saurischia
Seeley, 1887

Suborders
  • Theropoda
  • Sauropodomorpha


Saurischia (from the Greek sauros (σαυρος) meaning 'lizard' and ischion (
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Dinosauria *
Owen, 1842

Orders & Suborders
  • Ornithischia
  • Cerapoda
  • Thyreophora
  • Saurischia

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Herbivory is a form of predation in which an organism known as an herbivore, consumes principally autotrophs[1] such as plants, algae and photosynthesizing bacteria.
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The Cretaceous Period is one of the major divisions of the geologic timescale, reaching from the end of the Jurassic Period (i.e. from 145.5 ± 4.0 million years ago (Ma)) to the beginning of the Paleocene epoch of the Tertiary Period (about 65.5 ± 0.3 Ma).
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A geologic period is a subdivision of geologic time that divides an era into smaller timeframes. The equivalent term used to demarcate rock layers and the fossil record is the system; thus the rocks of the Devonian System were laid down during the Devonian Period.
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For the Carnian Alps, see Carnic Alps.


The Carnian (less commonly, Karnian) is the first stage of the Upper Triassic, Mesozoic. Its boundaries are not characterized by major extinctions or biotic turnovers, but a climatic event (known as the
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The Triassic is a geologic period that extends from about 251 to 199 Ma (million years ago). As the first period of the Mesozoic Era, the Triassic follows the Permian and is followed by the Jurassic. Both the start and end of the Triassic are marked by major extinction events.
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mya or "m.y.a." is an abbreviation for million years ago. This abbreviation is commonly used as a unit of time to denote length of time before the present or "B.P." (before AD 1950). Specifically, one mya is equal to 106 years ago.
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Early Jurassic (in geology referred to as the Lower Jurassic, originally (and still in Europe) the "Lias") is the earliest of three epochs of the Jurassic period.
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The Cretaceous Period is one of the major divisions of the geologic timescale, reaching from the end of the Jurassic Period (i.e. from 145.5 ± 4.0 million years ago (Ma)) to the beginning of the Paleocene epoch of the Tertiary Period (about 65.5 ± 0.3 Ma).
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Aves
Linnaeus, 1758

Orders

About two dozen - see section below

Birds (class Aves) are bipedal, warm-blooded, egg-laying vertebrate animals.
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Late Jurassic (or Malm) Epoch of the Jurassic Period is the unit of geologic time from 161.2 ± 4.0 to 145.5 ± 4.0 million years ago, which is preserved in Upper Jurassic strata.
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Coelurosauria
von Huene, 1914

Sub-groups
  • Compsognathidae
  • Maniraptora
  • Ornithomimosauria
  • Tyrannosauroidea
Coelurosauria is a diverse group of theropod dinosaurs that includes a number of subgroups, such as Tyrannosauroidea,
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