Information about Sauropod

Sauropods
Fossil range: Triassic - Cretaceous

Scientific classification
Kingdom:Animalia
Phylum:Chordata
Class:Sauropsida
Superorder:Dinosauria
Order:Saurischia
Suborder:Sauropodomorpha
Infraorder:Sauropoda
Marsh, 1878
Families


See text


Sauropoda, the sauropods, are a suborder or infraorder of the saurischian ("lizard-hipped") dinosaurs. They were the largest animals ever to have lived on land. Well-known genera include Apatosaurus (formerly known as Brontosaurus), Brachiosaurus and Diplodocus. 'Sauropod' is derived from 'lizard foot' in Greek. Sauropods first appeared in the late Triassic Period, where they somewhat resembled the Prosauropoda. By the Late Jurassic (150 million years ago) sauropods were widespread (especially the diplodocids and brachiosaurids). By the Late Cretaceous, only the titanosaurians survived, though with a near-global distribution. However, as with all other non-avian dinosaurs, the titanosaurians died out in the Cretaceous-Tertiary extinction event. Fossilized remains have been found on every continent except Antarctica.

Unfortunately, complete fossil sauropod finds are rare. Many species, especially the largest, are known only from isolated and disarticulated bones. Many near-complete specimens lack heads, tail tips and limbs. Some palaeontologists have postulated that these bits are those most likely to be carried off by Mesozoic scavengers after the death of the animal and before it is covered by sediment and fossilised.

Size

Enlarge picture
A statue of Diplodocus carnegiei, in Pittsburgh, Pennsylvania
Sauropods' most defining characteristic was their size. Even the dwarf sauropods (perhaps 5 to 6 metres, or 20 feet long) were counted among the largest animals in their ecosystem. Their only real competitors in terms of size are the rorqual whales, such as the Blue Whale. But unlike whales, sauropods all lived on land. Some, like the diplodocids, probably held their heads low, while others, like Camarasaurus, held them high.

Their body design did not vary as much as other dinosaurs, perhaps due to size constraints, but they still displayed ample variety. Some, like the diplodocids, were extremely long and with tremendously long tails which they may have been able to crack like a whip to make sonic booms.[1] Supersaurus, at 40 metres (130 ft), is probably the longest, but Seismosaurus and even the old record holder, Diplodocus, are still extremely long. Though a possible century-old hoax, Amphicoelias fragillimus, of which only a drawing of a single vertebra survives, at 55 to 60 metres (180 to 200 ft) would have a spine even longer than the blue whale. The longest terrestrial animal alive today, the reticulated python, only reaches lengths of 10 metres (33 ft).

Others, like the brachiosaurids, were extremely tall, with high shoulders and extremely long necks. Sauroposeidon is probably the tallest, reaching about 18 metres (60 ft) high, with the previous record for longest neck being held by Mamenchisaurus. By comparison the giraffe, the tallest of all living animals, is only 4.8 to 5.5 metres (16 to 18 ft) tall.

Some were almost incredibly massive: Argentinosaurus is probably the heaviest at 80 to 100 metric tonnes (90 to 110 tons), though Paralititan, Andesaurus, Antarctosaurus, and Argyrosaurus are of comparable sizes. There is some very poor evidence of an even more massive titanosaurian, Bruhathkayosaurus, which might have weighed between 175 to 220 tonnes (190 to 240 tons). The largest land animal alive today, the Savannah elephant, weighs no more than 10 tonnes (11 tons).

Among the smallest sauropods were the primitive Anchisaurus (2.4 m, or 7 ft long) and Ohmdenosaurus (4 m, or 13 ft long), the dwarf titanosaur Magyarosaurus (5.3 m or 17 ft long), and the dwarf brachiosaurid Europasaurus, which was 6.2 meters long as a fully-grown adult. Its small stature was probably the result of insular dwarfism of a herd of sauropods stranded on an island in what is now Germany. Also notable is the diplodocoid sauropod Brachytrachelopan, which was the shortest member of its group thanks to its unusually short neck. Unlike other sauropods, whose necks could grow to up to four times the length of their backs, the neck of Brachytrachelopan was shorter than its backbone.

Palaeobiology

They were herbivorous (plant-eating), usually long-necked quadrupeds (four-legged), with spatulate (spatula-shaped: broad at the base, narrow at the neck) teeth. They had small heads, huge bodies, and tended to have long tails. At least some of them laid eggs, like the camarasaurs and titanosaurs. According to paleontologist Robert Bakker there is a possibility they had large prehensile lips, reminiscent of moose lips.

Body armour

Some sauropods had armour. There were genera with spined backs, for instance the stegosaur-like (Agustinia) and one with a club-tail (Shunosaurus)''.

Posture

From early on there has been speculation by Osborn and others[2] that sauropods could reach up on hind legs, using their tail as the third 'leg' of a tripod (somewhat like kangaroos), and a famous restoration of a Barosaurus rearing up on hind legs in the American Museum of Natural History illustrates this hypothesis well. One interesting study[3]has postulated that if sauropods had adopted a bipedal posture at times there would be evidence of stress fractures in the forelimb 'hands'. However, none were found after examining a large number of sauropod skeletons.

If a sauropod stood in the tripod posture, there would be a heavy weight load on the haemal spines on part of the tail. As the sauropod got heavier as it grew, when it reared, these haemal spines would have to carry more and more load, until some of them would break due to stress fracture, and that would make rearing painful and the sauropod would have to stay on four feet after that. That may have evolved as a safety measure to prevent rearing when it got too heavy for rearing to be safe. There are reports of such haemal spine fractures being found in sauropod tail vertebrae.

Taxonomy

Classification of the sauropods has largely stabilised in recent years, though there are still some uncertainties, such as the position of Euhelopus, Haplocanthosaurus, Jobaria and Nemegtosauridae. The following are two alternative recent classifications (showing supra-generic clades only in the second example). These are by no means an exhaustive list of recent sauropod classification schemes. In some cases, families like Vulcanodontidae, Cetiosauridae and Omeisauridae are not included because they are considered paraphyletic, or even (in the case of Camarasauridae) polyphyletic.

Classification

This taxonomy follows Wilson & Sereno 1998, Yates 2003, Galton 2001,[1] and Wilson 2002,[3] with ranks after Benton, 2004.[4]

Phylogeny

Cladogram simplified after Wilson, 2002.[3]

Sauropoda





Omeisaurus


Mamenchisaurus

label3=unnamed




Haplocanthosaurus





Euhelopus


Titanosauria










References

1. ^ Peterson, Ivars (March 2000). Whips and Dinosaur Tails. Science News. Retrieved on 2007-07-07.
2. ^ Osborn HF."A skeleton of Diplodocus, recently mounted in the American Museum,". Science, new series, vol. 10 (1899), pp. 870-874
3. ^ Rothschild BM, Molnar RE (2005). "Sauropod Stress Fractures as Clues to Activity", in Carpenter, Kenneth and Tidswell, Virginia (ed.): Thunder Lizards: The Sauropodomorph Dinosaurs. Indiana University Press, 381–391. ISBN 0-253-34542-1. 
4. ^ Benton, M.J. (2004). Vertebrate Palaeontology, Third Edition. Blackwell Publishing, 472 pp.
5. ^ Wilson, J. A. (2002). "Sauropod dinosaur phylogeny: critique and cladistic analysis." Zoological Journal of the Linnean Society, 136: 217-276.

Further reading

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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Apatosaurus
Marsh, 1877

Species
  • A. ajax (type)
  • A. excelsus (Marsh, 1879c) Riggs, 1903
  • A. louisae Holland, 1915
  • A.

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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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Sauropodomorpha
von Huene, 1932

Infraorders

Prosauropoda
Sauropoda

The Sauropodomorpha were a group of long-necked, herbivorous dinosaurs that eventually dropped down on all fours and became the largest animals that ever walked the earth.
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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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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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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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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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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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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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Apatosaurus
Marsh, 1877

Species
  • A. ajax (type)
  • A. excelsus (Marsh, 1879c) Riggs, 1903
  • A. louisae Holland, 1915
  • A.

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Brontosaurus (pronounced /ˈbɹɒn.təˌsɔː.ɹəs/), meaning "thunder lizard" (from the Greek brontē/βροντη meaning 'thunder' and
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Brachiosaurus
Riggs, 1903

Species

B. altithorax Riggs, 1903 (type)
B. brancai Janensch, 1914
?B. nougaredi de Lapparent, 1960

Synonyms

Giraffatitan Paul, 1988
Abdallahsaurus
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Diplodocus
Marsh, 1878

Species

D. carnegiei Hatcher, 1901
D. hallorum (Gillette, 1991) Lucas et al., 2004
D. hayi Holland, 1924
D.
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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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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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Prosauropoda
von Huene, 1920

Families

See text
Prosauropoda or prosauropods were a group of early herbivorous dinosaurs that lived during the Triassic and early Jurassic periods.
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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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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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Titanosauria
Bonaparte & Coria, 1993
Superfamily: Titanosauroidea
Lydekker, 1895

Families
  • Andesauridae
  • Antarctosauridae
  • Euhelopodidae
  • Nemegtosauridae
  • Saltasauridae
Titanosaurs
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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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1 metre =
SI units
1000 mm 0 cm
US customary / Imperial units
0 ft 0 in
The metre or meter[1](symbol: m) is the fundamental unit of length in the International System of Units (SI).
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