Information about Kentrosaurus

Kentrosaurus
Fossil range: Late Jurassic
Enlarge picture
Kentrosaurus skeleton,
Museum für Naturkunde,
der Humboldt Universitat zu Berlin

Kentrosaurus skeleton,
Museum für Naturkunde,
der Humboldt Universitat zu Berlin
Conservation status
Extinct (fossil)
Scientific classification
Kingdom:Animalia
Phylum:Chordata
Class:Sauropsida
Superorder:Dinosauria
Order:Ornithischia
Suborder:Thyreophora
Infraorder:Stegosauria
Family:Stegosauridae
Genus:Kentrosaurus
Species


K. aethiopicus (type)
?K. longispinus


Kentrosaurus meaning 'pointed lizard' (pronounced: KEN-troh-Saw-rus)(from the Greek kentron/κεντρον meaning 'point' or 'prickle' and sauros/σαυρος meaning 'lizard') was a Jurassic genus of dinosaur closely related to the better-known Stegosaurus. Kentrosaurs were African cousins of the North American Stegosaurus. They differed in size, in the shape of their armour plating and in their bodily flexibility, however.

The ceratopsid dinosaur Centrosaurus from the late Cretaceous period derives its name from the same Ancient Greek words, but the initial letter has changed to a 'C' and is pronounced as a soft C to avoid confusion.

Discovery and species

Enlarge picture
life restoration of Kentrosaurus
The 19091912 German expedition to East Africa resulted in the discovery of several new dinosaur species, of which Kentrosaurus was one of the most important, for the reason outlined above — it implied a former proximity of Tanzania to the Morrison Formation, in the eastern part of the Rocky Mountains. Of the three paleontologists on this expedition, it was Edwin Hennig who first described Kentrosaurus, in 1915. An almost-complete skeleton was at one time recovered and mounted in the Humboldt Museum, of the University of Berlin but the museum was bombed during World War II and most of the bones were lost.

Paleobiology

Kentrosaurus was smaller than Stegosaurus. Kentrosaurus was just 16 feet (4.9 metres) long and had a much lower weight (although no accurate estimates can yet be made) It was certainly small for a stegosaur.

Armour

Kentrosaurus armour is also rather different from that of Stegosaurus. Kentrosaurus had small dorsal plates along its neck and shoulders. Along the rest of the back and down the tail were several — typically six — spectacular pairs of imposing caudal spikes, each up to a foot in length (see also: Thagomizer). Like other stegosaurs, such as the European Lexovisaurus, it had another pair of spikes jutting backwards from the hips (or possibly the shoulders). Unlike Stegosaurus, which may have used its plates for thermoregulation, the spines of Kentrosaurus could only have served one purpose: armour for self-defence.

Kentrosaurus would have been preyed upon by theropods similar to Allosaurus. It could have used its tail to ward off attacks by lashing the tail from side to side. Too, the spines along Kentrosaurus' flanks would have helped protect the animal from attacks.

Posture

Kentrosaurus also differed from Stegosaurus in one other key feature — it lacked the pronounced spines on the backbone, near the hip and tail region, that characterise the vertebrae of a Stegosaurus. The length of the thigh bone compared with the rest of the leg indicates that Kentrosaurus was a slow and inactive dinosaur. It may have reared up on its hind legs to reach twigs and leaves, but would normally have been fully quadrupedal.

Environment

The similarities and differences between kentrosaurs and stegosaurs illustrate well the geological principle of continental drift. The similarity between the kentrosaur fossils found in Tendaguru, Tanzania and the stegosaur fossils found in North America are evidence that these two points of the globe, now widely separated, were once very close together and indeed part of a supercontinent, known by geologists as Pangaea and, later, the northern half, known as Laurasia. These two points must also have had very similar climatic conditions, in order to have produced such similar specimens. Meanwhile, the differences between the animals illustrate the changes that their different ancestors underwent divergent evolution as the two groups of animals parted company, because of the subsequent separation of the tectonic plates.

References

  • Liddell & Scott (1980). Greek-English Lexicon, Abridged Edition. Oxford University Press, Oxford, UK. ISBN 0-19-910207-4. 

External links

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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conservation status of a species is an indicator of the likelihood of that species continuing to survive either in the present day or the future. Many factors are taken into account when assessing the conservation status of a species: not simply the number remaining, but the
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For other uses of the term, see Fossil (disambiguation)


FOSSIL is a standard for allowing serial communication for telecommunications programs under the DOS operating system.
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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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Ornithischia
Seeley, 1888

Suborders
  • Cerapoda
  • Thyreophora


Ornithischia or Predentata is an order of beaked, herbivorous dinosaurs.
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Thyreophora
Nopcsa, 1915

Infraorders
  • Ankylosauria
  • Stegosauria


The Thyreophora ("shield bearers", often known simply as "armored dinosaurs" - Greek: θυρεος
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Stegosauria
Marsh, 1877

Families

Huayangosauridae
Stegosauridae

Known colloquially as stegosaurs, the Stegosauria are a group of herbivorous dinosaurs of the Jurassic and Early Cretaceous Periods, being found mostly in the Northern
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Stegosauria
Marsh, 1877

Families

Huayangosauridae
Stegosauridae

Known colloquially as stegosaurs, the Stegosauria are a group of herbivorous dinosaurs of the Jurassic and Early Cretaceous Periods, being found mostly in the Northern
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species is one of the basic units of biological classification. A species is often defined as a group of organisms capable of interbreeding and producing fertile offspring.
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A type species fixes the name of a genus (or of a taxon in a rank lower than genus).

Strictly speaking, a type species exists only in zoological nomenclature. As set in article 42.
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Ancient Greek refers to the second stage in the history of the Greek language[1] as it existed during the Archaic (9th–6th centuries BC) and Classical (5th–4th centuries BC) periods in Greece.
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The Jurassic Period is a major unit of the geologic timescale that extends from about 199.6 ± 0.6 Ma (million years ago) to 145.4 ± 4.0 Ma, the end of the Triassic to the beginning of the Cretaceous.
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genus (plural: genera) is part of the Latinized name for an organism. It is a name which reflects the classification of the organism by grouping it with other closely similar organisms.
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Dinosauria *
Owen, 1842

Orders & Suborders
  • Ornithischia
  • Cerapoda
  • Thyreophora
  • Saurischia

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Stegosaurus
Marsh, 1877

Species
  • S. armatus Marsh, 1877 (type)
  • S. stenops Marsh, 1887
  • S. longispinus Gilmore, 1914


Stegosaurus (IPA:
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Africa is the world's second-largest and second most-populous continent, after Asia. At about 30,221,532 km² (11,668,545 sq mi) including adjacent islands, it covers 6% of the Earth's total surface area, and 20.4% of the total land area.
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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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Armour (or armor) in animals is external or superficial protection against attack by predators, formed as part of the body (rather than the behavioural use of protective external objects), usually through the hardening of body tissues, outgrowths or secretions.
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Ceratopsidae
Marsh, 1890

Genera

See text.

Ceratopsids, or members of the Ceratopsidae (or Ceratopidae), are a diverse group of marginocephalian dinosaurs like Triceratops and Styracosaurus.
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Centrosaurus
Lambe, 1904

Species

C. apertus Lambe, 1904
C. brinkmani Ryan & Russell, 2005

The name Centrosaurus (SEN-tro-sawr-us) means "pointed lizard" (from Greek
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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 hard c vs. a soft c is a feature that occurs in many languages, including English, in which there are two sounds represented by the letter "c".
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19th century - 20th century - 21st century
1870s  1880s  1890s  - 1900s -  1910s  1920s  1930s
1906 1907 1908 - 1909 - 1910 1911 1912

Year 1909 (MCMIX
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19th century - 20th century - 21st century
1880s  1890s  1900s  - 1910s -  1920s  1930s  1940s
1909 1910 1911 - 1912 - 1913 1914 1915

Year 1912 (MCMXII
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East Africa or Eastern Africa is the easternmost region of the African continent, variably defined by geography or geopolitics. In the UN scheme of geographic regions, 19 territories constitute Eastern Africa:

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Morrison Formation is a distinctive sequence of Late Jurassic sedimentary rock that is found in the western United States and Canada, which has been the most fertile source of dinosaur fossils in North America.
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