Information about Hadrosaurid

Hadrosaurids
Fossil range: Late Cretaceous
Enlarge picture
Corythosaurus and trackway

Corythosaurus and trackway
Scientific classification
Kingdom:Animalia
Phylum:Chordata
Class:Sauropsida
Superorder:Dinosauria
Order:Ornithischia
Suborder:Cerapoda
Infraorder:Ornithopoda
Superfamily:Hadrosauroidea
Family:Hadrosauridae
Cope, 1869
Subfamilies
Synonyms
  • Trachodontidae Lydekker, 1888
  • Saurolophidae Brown, 1914
  • Lambeosauridae Parks, 1923 vide Horner, 1990
Hadrosaurids or duck-billed dinosaurs are members of the family Hadrosauridae, and include ornithopods such as Edmontosaurus and Parasaurolophus. They were common herbivores in the Upper Cretaceous Period of what are now Asia, Europe and North America. They are descendants of the Upper Jurassic/Lower Cretaceous iguanodontian dinosaurs and had similar body layout. They were ornithischians.

Hadrosaurids are divided into two subfamilies. The lambeosaurines (Lambeosaurinae) have large cranial crests or tubes, and are less bulky. The hadrosaurines (Hadrosaurinae) lack the cranial crests or tubes and are larger.

Characteristics

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Skull of Edmontosaurus, showing duck-bill and dentition Oxford University Museum of Natural History.
The hadrosaurs are known as the duck-billed dinosaurs due to the similarity of their head to that of modern ducks. In some species, most notably Anatotitan, the whole front of the skull was flat and broadened out to form a beak, ideal for clipping leaves and twigs from the forests of Asia, Europe and North America. However, the back of the mouth contained literally thousands of teeth suitable for grinding food before it was swallowed. Hadrosaurs, like their iguanodontian cousins, had a rudimentary dental specialisation analogous to incisors and molars. This has been hypothesized to have been a crucial factor in the success of this group in the Cretaceous, compared to the sauropods which were still largely dependent on gastroliths for grinding their food.
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Fossilized skeletion (partial) of a young hadrosaur excavated and displayed at the Escalante-Grand Staircase National Mounument in Southern Utah. Click image for display placard text.

Discoveries

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An old drawing of the defunct hadrosaur genus "Trachodon"
Hadrosaurids were the first dinosaur family to be identified in North America, the first traces being found in 1855-1856 with the discovery of fossil teeth. Joseph Leidy examined the teeth, and erected the genera Trachodon and Thespesius (others included Troodon, Deinodon and Palaeoscincus). One species was named Trachodon mirabilis. Now it seems that the teeth genus Trachodon is a mixture of all sorts of cerapod dinosaurs, including ceratopsids. In 1858 the teeth were associated with Leidy's eponymous Hadrosaurus foulkii, named after the fossil hobbyist William Parker Foulke. More and more teeth were found, resulting in even more (now obsolete) genera.

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Skin impressions of Edmontosaurus.
A second duck-bill skeleton was unearthed, and was named Diclonius mirabilis in 1883 by Edward Drinker Cope, which he incorrectly used in favor of Trachodon mirabilis. But Trachodon, together with other poorly typed genera, was used more widely and, when Cope's famous "Diclonius mirabilis" skeleton was mounted at the American Museum of Natural History, it was labeled as "Trachodont dinosaur". The duck-billed dinosaur family was then named Trachodontidae.

A very well-preserved complete hadrosaurid specimen (Edmontosaurus annectens) was recovered in 1908 by the fossil collector Charles Hazelius Sternberg and his three sons, in Converse County, Wyoming. It was known as the "Trachodon mummy". This specimen's skin was almost completely preserved, together with some muscles and was analysed by Henry Osborn in 1912. Sternberg was in Cope's camp during his famous competition to name new species with Othniel Charles Marsh. This discovery was a victory for Cope in the Bone Wars.

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A well preserved specimen of Edmontosaurus.
Lawrence Lambe erected the genus Edmontosaurus ("lizard from Edmonton") in 1917 from a find in the lower Edmonton Formation (now Horseshoe Canyon Formation), Alberta. Hadrosaurid systematics were a mess until 1942, when Richard Swann Lull and Nelda Wright proposed the genus Anatosaurus. Cope's famous mount at the AMNH became Anatosaurus copei. In 1975, Anatosaurus was moved to Edmontosaurus, because the species were just too similar to the Edmontosaurus type species, E. regalis and because Edmontosaurus was older, it had precedence. The original sample was probably a young Edmontosaurus. One former Anatosaurus species was distinct enough from Edmontosaurus to be placed in a separate genus, named Anatotitan, so in 1990 the AMNH mount was re-labelled Anatotitan copei.

Some paleontologists found a hadrosaurid leg bone in Paleocene rocks, but it was probably reworked from a Cretaceous source.[1]

Systematics

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Family tree of the Hadrosauroidea. Representative genera of each tribe are shown to scale.

Taxonomy

The family Hadrosauridae was first used by Edward Drinker Cope in 1869. Since its creation, a major division has been recognized in the group, between the (generally crested) subfamily Lambeosaurinae and (generally crestless) subfamily Hadrosaurinae. Phylogenetic analysis has increased the resolution of hadrosaurid relationships considerably (see Phylogeny below), leading to the widespread usage of tribes (a taxonomic unit below subfamily) to describe the finer relationships within each group of hadrosaurids. However, hadrosaurid tribes commonly recognized in online sources have not yet been formally defined or seen wide use in the literature. Several were briefly mentioned but not named as such in the first edition of The Dinosauria, under informal names. In this 1990 reference, "gryposaurs" included Aralosaurus, Gryposaurus, Hadrosaurus, and Kritosaurus; "brachylophosaurs" included Brachylophosaurus and Maiasaura; "saurolophs" included Lophorhothon, Prosaurolophus, and Saurolophus; and "edmontosaurs" included Anatotitan, Edmontosaurus, and Shantungosaurus.[2]

Lambeosaurines have also been split into Parasaurolophini (Parasaurolophus) and Corythosaurini (Corythosaurus, Hypacrosaurus, and Lambeosaurus).[3] Corythosaurini and Parasaurolophini as terms entered the formal literature in Evans and Reisz's 2007 redescription of Lambeosaurus magnicristatus. Corythosaurini is defined as all taxa more closely related Corythosaurus casuarius than to Parasaurolophus walkeri, and Parasaurolophini as all those taxa closer to P. walkeri than to C. casuarius. In this study, Charonosaurus and Parasaurolophus are parasaurolophins, and Corythosaurus, Hypacrosaurus, Lambeosaurus, Nipponosaurus, and Olorotitan are corythosaurins.[4]

The following taxonomy includes dinosaurs currently referred to the Hadrosauridae and its subfamilies. Hadrosaurids that were accepted as valid but were not placed in a cladogram at the time of the 2004 review in The Dinosauria,[5] or, in the case of lambeosaurines, the 2007 redescription of Lambeosaurus magnicristatus,[4] are included at the highest level to which they were placed (either then, or in their description if they postdate the papers used here).

Phylogeny

Hadrosauridae was first defined as a clade, by Forster in a 1997 abstract, as simply "Labeosaurinae plus Hadrosaurinae and their most recent common ancestor." In 1998, Paul Sereno defined the clade Hadrosauridae as the most inclusive possible group containing Saurolophus (a well-known hadrosaurine) and Parasaurolophus (a well-known lambeosaurine), later emending the definition to include Hadrosaurus, the type genus of the family, which ICZN rules state must be included, despite its status as a nomen dubium. According to some studies, Sereno's definition would place a few other well-known hadrosaurs (such as Telmatosaurus and Bactrosaurus) outside the family, which led Horner et al. (2004) to define the family to include Telmatosaurus by default.

The following cladogram is after the 2004 review by Jack Horner, David B. Weishampel, and Catherine Forster, in the second edition of The Dinosauria.[5]

 Hadrosauridae 

 Hadrosaurinae 

unnamed




Brachylophosaurus


Maiasaura





unnamed

"Kritosaurus" australis


Naashoibitosaurus


Saurolophus




 Lambeosaurinae 



Lambeosaurus


Corythosaurus


Hypacrosaurus






Lambeosaurinae cladogram

The following cladogram is after the 2007 redescription of Lambeosaurus magnicristatus (Evans and Reisz, 2007):[4]

 Hadrosauridae 





unnamed



P. tubicen


P. walkeri




unnamed

unnamed

Lambeosaurus lambei


L. magnicristatus


unnamed

Corythosaurus



Hypacrosaurus altispinus


H. stebingeri











References

1. ^ Fassett, J, Zielinski, R.A., and Budahn, J.R. (2002). Dinosaurs that did not die; evidence for Paleocene dinosaurs in the Ojo Alamo Sandstone, San Juan Basin, New Mexico. In: Koeberl, C., and MacLeod, K. (eds.). Catastrophic events and mass extinctions: impacts and beyond. Special Paper - Geological Society of America 356:307-336.
2. ^ Weishampel, David B.; and Horner, Jack R. (1990). "Hadrosauridae", in Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 1st, Berkeley: University of California Press, 534-561. ISBN 0-520-06727-4. 
3. ^ Glut, Donald F. (1997). Dinosaurs: The Encyclopedia. Jefferson, North Carolina: McFarland & Co, 69. ISBN 0-89950-917-7. 
4. ^ Evans, David C.; and Reisz, Robert R. (2007). "Anatomy and relationships of Lambeosaurus magnicristatus, a crested hadrosaurid dinosaur (Ornithischia) from the Dinosaur Park Formation, Alberta". Journal of Vertebrate Paleontology 27 (2): 373-393. 
5. ^ Horner, John R.; Weishampel, David B.; and Forster, Catherine A (2004). "Hadrosauridae", in Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press, 438-463. ISBN 0-520-24209-2. 
6. ^ Evans, David C.; and Reisz, Robert R. (2007). "Anatomy and relationships of Lambeosaurus magnicristatus, a crested hadrosaurid dinosaur (Ornithischia) from the Dinosaur Park Formation, Alberta". Journal of Vertebrate Paleontology 27 (2): 373-393. 

External links

Late Cretaceous (100mya - 65mya) refers to the second half of the Cretaceous Period, named after the famous white chalk cliffs of southern England, which date from this time. Rocks deposited during the Late Cretaceous Period are referred to as the Upper Cretaceous Series.
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Corythosaurus
Brown, 1914

Species: C. casuarius

Binomial name
Corythosaurus casuarius
Brown, 1914

Corythosaurus
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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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Cerapoda
Sereno, 1986

Infraorders
  • Ceratopsia
  • Ornithopoda
  • Pachycephalosauria


Cerapoda is a clade or suborder of the order Ornithischia. They are the sister group of the Thyreophora within the clade Genasauria.
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Ornithopoda
Marsh, 1881

Families
  • Hypsilophodontidae*
  • Rhabdodontidae
  • Dryosauridae
  • Camptosauridae
  • Iguanodontidae
  • Hadrosauridae


Ornithopods
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Hadrosauroidea
Cope, 1869

Families
  • Hadrosauridae
Hadrosauroidea is a clade or superfamily of ornithischian dinosaurs that includes the "duck-billed" dinosaurs, or hadrosaurids, and their close relatives.
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Edward Drinker Cope (July 28, 1840–April 12, 1897) was an American paleontologist and comparative anatomist, as well as a noted herpetologist and ichthyologist.

Cope was born in Philadelphia to Quaker parents.
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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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Hadrosauridae
Cope, 1869

Subfamilies
  • Hadrosaurinae Cope, 1869
  • Lambeosaurinae Parks, 1923
Synonyms
  • Trachodontidae Lydekker, 1888
  • Saurolophidae Brown, 1914
  • Lambeosauridae Parks, 1923 vide Horner, 1990

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Hadrosauridae
Cope, 1869

Subfamilies
  • Hadrosaurinae Cope, 1869
  • Lambeosaurinae Parks, 1923
Synonyms
  • Trachodontidae Lydekker, 1888
  • Saurolophidae Brown, 1914
  • Lambeosauridae Parks, 1923 vide Horner, 1990

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William Arthur Parks (11 December 1868 – 3 October 1939) was a Canadian geologist and paleontologist, following in the tradition of Lawrence Lambe.

Born in Hamilton, Ontario, he described Arrhinoceratops (1925), Dyoplosaurus (1924), Lambeosaurus (1923), and
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In scientific nomenclature, synonyms are different scientific names used for a single taxon. Usage and terminology are different for zoology and botany.

Zoology

In zoological nomenclature, synonyms are different scientific names that pertain to the same taxon, for example
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Richard Lydekker (July 25, 1849 - April 16, 1915) was an English naturalist, geologist and writer of numerous books on natural history.

Lydekker was born in London. In 1874 he joined the Geological Survey of India and made studies of the vertebrate paleontology of northern
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Barnum Brown (1873-1963), born February 12, 1873 in Carbondale, Kansas. He was named after the circus showman P.T. Barnum, and was perhaps the most famous fossil hunter of the early Twentieth Century.
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John "Jack" R. Horner (born June 15, 1946) is an American paleontologist who discovered and named the Maiasaura, providing the first clear evidence that some dinosaurs cared for their young. He is one of the most well known paleontologists in the United States.
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Dinosauria *
Owen, 1842

Orders & Suborders
  • Ornithischia
  • Cerapoda
  • Thyreophora
  • Saurischia

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Ornithopoda
Marsh, 1881

Families
  • Hypsilophodontidae*
  • Rhabdodontidae
  • Dryosauridae
  • Camptosauridae
  • Iguanodontidae
  • Hadrosauridae


Ornithopods
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Parasaurolophus
Parks, 1922

Species
  • P. walkeri (type)
  • P. tubicen Wiman, 1931
  • P. cyrtocristatus Ostrom, 1961


Parasaurolophus (meaning "near crested lizard" in reference to
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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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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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