Information about Ornithomimosauria
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Ornithomimosaurs (meaning 'bird mimic lizards') or members of the clade Ornithomimosauria are theropod dinosaurs, like Gallimimus, which bore a superficial resemblance to modern ostriches. They were fast, fleet-footed, omnivorous or herbivorous dinosaurs from the Cretaceous Period of Laurasia (now Asia, Europe and North America). The group first appeared in the Early Cretaceous and persisted until the Late Cretaceous. They appear to be related to less-derived coelurosaurian theropods such as Compsognathus and tyrannosaurids. Primitive members of the group include Pelecanimimus, Shenzhousaurus, Harpymimus and probably the huge Deinocheirus, the arms of which reached eight feet in length. More advanced species, members of the family ornithomimidae, include Gallimimus, Archaeornithomimus, Anserimimus, Struthiomimus, and Ornithomimus. Some paleontologists, like Paul Sereno, consider the enigmatic alvarezsaurids to be close relatives of the ornithomimosaurs and place them together in the superfamily Ornithomimoidea (see classification below).
Description
The skull of ornithomimosaurs, which atop a relatively long and slender neck, was small, with large eyes. Some primitive species (such as Pelecanimimus and Harpymimus) had teeth, but most had toothless beaks.Diet
Ornithomimosaurs probably acquired most of their calories from plants. Many ornithomimosaurs, including primitive species, have been found with numerous gastroliths in their stomachs, characteristic of herbivores. Henry Fairfield Osborn suggested that the long, sloth-like 'arms' of ornithomimosaurs may have been used to pull down branches on which to feed, an idea supported by further study of their strange, hook-like hands.[1] The sheer abundance of ornithomimids — they are the most common small dinosaurs in North America — is consistent with the idea that they were plant eaters, as herbivores usually outnumber carnivores in an ecosystem.Thanks to well-preserved specimens of Ornithomimus, some of the anatomy of the inside of ornithomimid beaks has been observed. A 2001 study showed that the inside walls of the beak possessed vertical ridges, similar to those found in modern ducks. This led some paleontologists to suggest ornithomimids may have been filter feeders, which strained water through their beaks to consume small aquatic organisms.[2] However, others have argued against this interpretation, pointing out that similar structures are found in the beaks of a wide variety of non-filter feeding beaked animals, including turtles, and have no relation to filter feeding.[3]
Taxonomy
Named by Marsh in 1890, the family Ornithomimidae was originally classified as a group of "megalosaurs" (a "wastebasket taxon" containing any medium to large sized theropod dinosaurs), but as more theropod diversity was uncovered, their true relationships to other theropods started to resolve, and they were moved to the Coelurosauria. Recognizing the distinctivness of ornithomimids compared to other dinosaurs, Rinchen Barsbold placed ornithomimids within thir own infraorder, Ornithomimosauria, in 1976. The contents of Ornithomimidae and Ornithomimosauria varied from author to author as cladistic definitions began to appear for the groups in the 1990s. Paul Sereno, for example, used Ornithomimidae to include all of Ornithomimosauria in 1998, and subsequently switched to a more exlusive definition that nested Ornithomimidae (advanced ornthimomimes) within the larger stem-group Ornithomimosauria, a classification scheme that is mirrored by most other literature in the early 2000s.In the early 1990s, prominent paleontologists such as Thomas R. Holtz Jr. proposed a close relationship between theropods with an arctometatarsalian foot; that is, bipedal dinosaurs in which the upper foot bones were 'pinched' together, an adaptation for running. Holtz (1994) defined the clade Arctometatarsalia as "the first theropod to develop the arctometatarsalian pes and all of its descendants." This group included the Troodontidae, Tyrannosauroidea, and Ornithomimosauria. Holtz (1996, 2000) later refined this definition to the branch-based "Ornithomimus and all theropods sharing a more recent common ancestor with Ornithomimus than with birds." Subsequently, the idea that all arctometatarsalian dinosaurs formed a natural group was abandoned by most paleontologists, including Holtz, as studies began to demonstrate that tyrannosaurids and troodontids were more closely related to other groups of coelurosaurs than they were to ornithomimosaurs. Since the strict definition of Arctometatarsalia was based on Ornithomimus, it became redundant with the name Ornithomimosauria, and the later name remained in use, while the name Arctometatarsalia was mostly abandoned.
Another clade, Ornithomimiformes, was defined by Sereno (2005) as (Ornithomimus velox > Passer domesticus) and is useful in phylogenetic taxonomy only if alvarezsaurids or some other group are actually closer relatives of ornithomimosaurs than maniraptorans. The Ornithomimosauria is an inclusive clade that contains primitive ornithomimosaurs and ornithomimids proper.
Classification
- Infraorder ORNITHOMIMOSAURIA
- Pelecanimimus (central Spain)
- Shenzhousaurus (Liaoning, Northeastern China)
- Family Deinocheiridae
- Deinocheirus (Mongolia)
- Family Garudimiminae
- Garudimimus (Mongolia)
- Family Harpymimidae
- Harpymimus (Mongolia)
- Family Ornithomimidae
- Anserimimus (Mongolia)
- Archaeornithomimus (China)
- Dromiceiomimus (Alberta, Canada)
- Gallimimus (Mongolia)
- Ornithomimus (Colorado and Alberta in North America)
- Sinornithomimus (Inner Mongolia, China)
- Struthiomimus (Montana and Alberta in North America)
Phylogeny
Cladogram after Barsbold & Osmólska (1990), Kobayashi & Lü (2003), and Ji et al. (2003).[1]Ornithomimiformes (=Arctometatarsalia)?Alvarezsauridae `--Ornithomimosauria?TimimusPelecanimimus `--+--Shenzhousaurus `--+--Harpymimus `--Ornithomimoidea?DeinocheirusGarudimimus `--OrnithomimidaeArchaeornithomimus `--+--Sinornithomimus `--Ornithomiminae+--Gallimimus | `--Anserimimus `--OrnithomiminiStruthiomimus `--+--Dromiceiomimus `--Ornithomimus
Other evidence
Note that, Timimus, early Cretaceous fossil remains (a femur) from Dinosaur Cove in Victoria in southeastern Australia are possibly ornithomimosaurian.References
1. ^ Nicholls, E. L., and Russell, A. P. (1985). "Structure and function of the pectoral girdle and forelimb of Struthiomimus altus (Theropoda: Ornithomimidae)." Palaeontology, 28: 643-677.
2. ^ Norell, M. A., Makovicky, P., and Currie, P. J. (2001). "The beaks of ostrich dinosaurs." Nature, 412: 873-874.
3. ^ Barrett, P. M. (2005). "The diet of ostrich dinosaurs (Theropoda: Ornithomimosauria)." Palaeontology, 48: 347-358.
2. ^ Norell, M. A., Makovicky, P., and Currie, P. J. (2001). "The beaks of ostrich dinosaurs." Nature, 412: 873-874.
3. ^ Barrett, P. M. (2005). "The diet of ostrich dinosaurs (Theropoda: Ornithomimosauria)." Palaeontology, 48: 347-358.
External links
- A Guide to Ornithomimosauria with pictures
- Khalaf-von Jaffa, Norman Ali Bassam Ali Taher (2006). Ornithomimid Dinosaur Tracks from Beit Zeit, West of Jerusalem, Palestine.Gazelle: The Palestinian Biological Bulletin. Number 56, August 2006. pp. 1-7.
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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Gallimimus
Species: G. bullatus
Binomial name
Gallimimus bullatus
Osmólska, Roniewics & Barsbold, 1972
Gallimimus
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Species: G. bullatus
Binomial name
Gallimimus bullatus
Osmólska, Roniewics & Barsbold, 1972
Gallimimus
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Natural History Museum is one of three large museums on Exhibition Road, South Kensington, London (the others are the Science Museum, and the Victoria and Albert Museum). Its main frontage is on Cromwell Road.
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London
Canary Wharf is the centre of London's modern office towers
London shown within England
Coordinates:
Sovereign state United Kingdom
Constituent country England
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Canary Wharf is the centre of London's modern office towers
London shown within England
Coordinates:
Sovereign state United Kingdom
Constituent country England
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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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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
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Goodrich, 1916
Subclasses
- Anapsida
- Diapsida
- Reptilia Laurenti, 1768
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Dinosauria *
Owen, 1842
Orders & Suborders
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Owen, 1842
Orders & Suborders
- Ornithischia
- Cerapoda
- Thyreophora
- Saurischia
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Saurischia
Seeley, 1887
Suborders
Saurischia (from the Greek sauros (σαυρος) meaning 'lizard' and ischion (
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Seeley, 1887
Suborders
- Theropoda
- Sauropodomorpha
Saurischia (from the Greek sauros (σαυρος) meaning 'lizard' and ischion (
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Theropoda
Marsh, 1881
Infraorders
Theropods ('beast feet') are a group of bipedal saurischian dinosaurs.
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Marsh, 1881
Infraorders
- Carnosauria
- Ceratosauria
- Deinonychosauria
- Ornithomimosauria
- Oviraptorosauria
Theropods ('beast feet') are a group of bipedal saurischian dinosaurs.
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Dr. Rinchen Barsbold (Mongolian: Ринченгийн Барсбол?, Rinchyengiin Barsbold) is a Mongolian paleontologist and geologist.
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family (Latin: familia, plural familiae) is a rank, or a taxon in that rank. Exact details of formal nomenclature depend on the Nomenclature Code which applies.
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Garudimimidae
Barsbold, 1981
Genus: Garudimimus
Binomial name
Garudimimus brevipes
Barsbold, 1981
Garudimimus
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Barsbold, 1981
Genus: Garudimimus
Binomial name
Garudimimus brevipes
Barsbold, 1981
Garudimimus
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Harpymimidae
Barsbold & Perle, 1984
Genus: Harpymimus
Binomial name
Harpymimus oklandnikovi
Barsbold & Perle, 1984
Harpymimus
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Barsbold & Perle, 1984
Genus: Harpymimus
Binomial name
Harpymimus oklandnikovi
Barsbold & Perle, 1984
Harpymimus
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Deinocheiridae
Osmólska & Roniewics, 1970
Genus: Deinocheirus
Binomial name
Deinocheirus mirificus
Osmólska & Roniewics, 1970
Deinocheirus
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Osmólska & Roniewics, 1970
Genus: Deinocheirus
Binomial name
Deinocheirus mirificus
Osmólska & Roniewics, 1970
Deinocheirus
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Ornithomimosauria
Barsbold, 1976
Families
Ornithomimosaurs (meaning 'bird mimic lizards') or members of the clade Ornithomimosauria
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Barsbold, 1976
Families
- Garudimimidae
- Harpymimidae
- Deinocheiridae
- Ornithomimidae
Ornithomimosaurs (meaning 'bird mimic lizards') or members of the clade Ornithomimosauria
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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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Linnaeus, 1758
Orders
About two dozen - see section below
Birds (class Aves) are bipedal, warm-blooded, egg-laying vertebrate animals.
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This article has been tagged since July 2007.
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Theropoda
Marsh, 1881
Infraorders
Theropods ('beast feet') are a group of bipedal saurischian dinosaurs.
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Marsh, 1881
Infraorders
- Carnosauria
- Ceratosauria
- Deinonychosauria
- Ornithomimosauria
- Oviraptorosauria
Theropods ('beast feet') are a group of bipedal saurischian dinosaurs.
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Dinosauria *
Owen, 1842
Orders & Suborders
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Owen, 1842
Orders & Suborders
- Ornithischia
- Cerapoda
- Thyreophora
- Saurischia
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Gallimimus
Species: G. bullatus
Binomial name
Gallimimus bullatus
Osmólska, Roniewics & Barsbold, 1972
Gallimimus
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Species: G. bullatus
Binomial name
Gallimimus bullatus
Osmólska, Roniewics & Barsbold, 1972
Gallimimus
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Struthionidae
Vigors, 1825
Genus: Struthio
Linnaeus, 1758
Species: S.
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Vigors, 1825
Genus: Struthio
Linnaeus, 1758
Species: S.
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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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Laurasia (IPA: /lɔˈreɪʃiə, lɔˈreɪʃiʒə/[1]) was a supercontinent that most recently existed as a part of the split of the Pangaean supercontinent in the late
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Asia is the world's largest and most populous continent. It covers 8.6% of the Earth's total surface area (or 29.4% of its land area) and, with almost 4 billion people, it contains more than 60% of the world's current human population.
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Europe is one of the seven traditional continents of the Earth. Physically and geologically, Europe is the westernmost peninsula of Eurasia, west of Asia. Europe is bounded to the north by the Arctic Ocean, to the west by the Atlantic Ocean, to the south by the Mediterranean Sea,
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North America is a continent [1] in the Earth's northern hemisphere and (chiefly) western hemisphere. It is bordered on the north by the Arctic Ocean, on the east by the North Atlantic Ocean, on the southeast by the Caribbean Sea, and on the south and west
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The Early Cretaceous (timestratigraphic name) or the Lower Cretaceous (logstratigraphic name), is the earlier of the two major divisions of the Cretaceous Period. It began about 146 million years ago.
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