Information about Lystrosaurus
| Lystrosaurus Fossil range: Early Triassic | ||||||||||||||||
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Lystrosaurus murrayi | ||||||||||||||||
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Distribution of Lystrosaurus (brown) in the Gondwana supercontinent.
Lystrosaurus is notable for dominating land during the Early Triassic, being found on every continent, for millions of years. This genus survived the end-Permian mass extinction and went on to thrive, becoming the most common group of terrestrial vertebrates during the Early Triassic. It is the only time a single species of animal dominated the Earth to such a degree. Lystrosaurus's survival of the Permian-Triassic extinction event may be due to chance alone. Alternatively, adaptations for subsisting on more resilient plant material may have contributed.
Its discovery at Coalsack Bluff in the Transantarctic Mountains by Edwin H. Colbert and his team in 1969-70 helped confirm the theory of plate tectonics and convince the last of the doubters, for Lystrosaurus had already been found in the lower Triassic of southern Africa as well as in India and China.[1]
Lystrosaurus in popular culture
Lystrosaurus played a role in the BBC television series Walking with Monsters: Life Before Dinosaurs. One episode followed the journey of a group across a ravine and through a river full of the ancient crocodile relative Proterosuchus.Notes
External links
- Palaeos.com: Dicynodontia
- Hugh Rance, The Present is the Key to the Past: "Mammal-like reptiles of Pangea"
- Lystrosaurus, Gondwana Studios
The Early Triassic (also known as Lower Triassic, Buntsandstein, or Scythian) is the first of three epochs of the Triassic period. It spans the time between 251 ± 0.4 Ma and 245 ± 1.5 Ma (million years ago).
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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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Synapsida *
Osborn, 1903
Orders & Suborders
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Osborn, 1903
Orders & Suborders
- '''Order Pelycosauria *
- Suborder Caseasauria
- Suborder Eupelycosauria *
- Order Therapsida
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Therapsida *
Broom, 1905
Clades
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Broom, 1905
Clades
- Suborder Biarmosuchia *
- Suborder Dinocephalia
- Suborder Anomodontia *
- Infraorder Dicynodontia
- (unranked) Theriodontia *
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Anomodontia
Owen, 1859
Groups
Anomocephalus
Patranomodon
Venyukoviidae
Dromasauria
Dicynodontia
The Anomodontia are one of the three major groups of therapsids. They were mostly toothless herbivores.
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Owen, 1859
Groups
Anomocephalus
Patranomodon
Venyukoviidae
Dromasauria
Dicynodontia
The Anomodontia are one of the three major groups of therapsids. They were mostly toothless herbivores.
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Dicynodontia
Owen, 1859
Clades & Genera
see "Taxonomy"
The Dicynodontia are a taxon of Therapsids or mammal-like reptiles. Dicynodonts were small to large herbivorous animals with two tusks, hence their name, which means 'two dog tooth'.
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Owen, 1859
Clades & Genera
see "Taxonomy"
The Dicynodontia are a taxon of Therapsids or mammal-like reptiles. Dicynodonts were small to large herbivorous animals with two tusks, hence their name, which means 'two dog tooth'.
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This chart shows concisely the most common way in which the International Phonetic Alphabet (IPA) is applied to represent the English language.
See International Phonetic Alphabet for English for a more complete version and Pronunciation respelling for English for phonetic
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See International Phonetic Alphabet for English for a more complete version and Pronunciation respelling for English for phonetic
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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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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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Therapsida *
Broom, 1905
Clades
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Broom, 1905
Clades
- Suborder Biarmosuchia *
- Suborder Dinocephalia
- Suborder Anomodontia *
- Infraorder Dicynodontia
- (unranked) Theriodontia *
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Synapsida *
Osborn, 1903
Orders & Suborders
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Osborn, 1903
Orders & Suborders
- '''Order Pelycosauria *
- Suborder Caseasauria
- Suborder Eupelycosauria *
- Order Therapsida
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Mammalia
Linnaeus, 1758
Subclasses & Infraclasses
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Linnaeus, 1758
Subclasses & Infraclasses
- Subclass †Allotheria*
- Subclass Prototheria
- Subclass Theria
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Mammal-like reptiles is a term used to describe the prehistoric animals that appear to be the reptilian ancestors of mammals. The term "mammal-like reptiles" is most commonly used to describe the group Therapsida, although it can be also used more broadly to describe non-mammalian
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Dicynodontia
Owen, 1859
Clades & Genera
see "Taxonomy"
The Dicynodontia are a taxon of Therapsids or mammal-like reptiles. Dicynodonts were small to large herbivorous animals with two tusks, hence their name, which means 'two dog tooth'.
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Owen, 1859
Clades & Genera
see "Taxonomy"
The Dicynodontia are a taxon of Therapsids or mammal-like reptiles. Dicynodonts were small to large herbivorous animals with two tusks, hence their name, which means 'two dog tooth'.
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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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Sus
Linnaeus, 1758
Species
Sus barbatus
Sus bucculentus†
Sus cebifrons
Sus celebensis
Sus domestica
Sus falconeri†
Sus heureni
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Linnaeus, 1758
Species
Sus barbatus
Sus bucculentus†
Sus cebifrons
Sus celebensis
Sus domestica
Sus falconeri†
Sus heureni
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Hippopotamus
Species: H. amphibius
Binomial name
Hippopotamus amphibius
Linnaeus, 1758[1]
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Species: H. amphibius
Binomial name
Hippopotamus amphibius
Linnaeus, 1758[1]
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Permian is a geologic period that extends from about 299.0 ± 0.8 Ma to 251.0 ± 0.4 Ma (million years before the present; ICS 2004). It is the last period of the Paleozoic Era.
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Transantarctic Mountains (abbreviated TAM) compose a mountain range in Antarctica which extend, with some interruptions, across the continent from Cape Adare in northern Victoria Land to Coats Land.
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Plate tectonics (from Greek τέκτων, tektōn "builder" or "mason") is a theory of geology that has been developed to explain the observed evidence for large scale motions of the Earth's lithosphere.
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The British Broadcasting Corporation (BBC)
Type Broadcast radio and television
Country United Kingdom
Availability National
International
Founder John Reith
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Type Broadcast radio and television
Country United Kingdom
Availability National
International
Founder John Reith
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Walking with Monsters (also distributed as Before the Dinosaurs: Walking With Monsters) is a three-part British documentary film series about life in the Paleozoic, bringing to life extinct arthropods, fish, amphibians, synapsids, and reptiles.
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Proterosuchus
Broom, 1903
Proterosuchus was a large Triassic reptile equivalent in size to today's Komodo Dragons. It looked somewhat similar to a primitive crocodile, and shared many of their modern features while retaining several of its own
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Broom, 1903
Proterosuchus was a large Triassic reptile equivalent in size to today's Komodo Dragons. It looked somewhat similar to a primitive crocodile, and shared many of their modern features while retaining several of its own
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Herod_Archelaus