Information about Pelycosaur
| Pelycosaurs Fossil range: Late Carboniferous - Late Permian (non-therapsid) | ||||||||||
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Dimetrodon grandis skeleton at the National Museum of Natural History Dimetrodon grandis skeleton at the National Museum of Natural History | ||||||||||
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Caseasauria Eupelycosauria | ||||||||||
The pelycosaurs (from Greek pelyx meaning 'bowl' and sauros meaning 'lizard') were primitive Late Paleozoic synapsid amniotes. Some species were quite large and could grow up to 3 meters or more, although most species were much smaller.
Evolutionary history
The pelycosaurs appeared during the Late Carboniferous and reached their acme in the early part of the Permian Period, remaining the dominant land animals for some 40 millions of years. A few continued into the late Permian. They were succeeded by their descendants, the therapsids, which had a short but successful reign before the Permian-Triassic extinction event, giving a chance for the archosaur reptiles to take over in the Triassic.- See also: Evolution of mammals
Characteristics
At least two pelycosaur clades independently evolved a tall sail, consisting of elongated vertebral spines: the edaphosaurids and the sphenacodontids. In life, this would have been covered by skin, and possibly functioned as a thermoregulatory device or for mating display. Pelycosaur fossils have been found mainly in Europe and North America, although some small, late-surviving forms are known from Russia and South Africa.In 1940 the group was reviewed in detail and every species known at the time described (and many illustrated) in an important monograph by Alfred Sherwood Romer and Llewellyn Price.
Pelycosauria is a paraphyletic taxon because it excludes the therapsids. For that reason the term is not used in some modern books. Eupelycosauria is used to designate the clade that includes most Pelycosaurs along with the Therapsida and the Mammals. In contrast to "Pelycosaurs", this is monophyletic group. Caseasauria refers to a pelycosaur side-branch or clade that did not leave any descendants.
The pelycosaurs appear to have been a group of synapsids that had direct ancestral links with the mammalia, having differentiated teeth and a developing hard palate.
Well-known pelycosaurs include the genera Dimetrodon, Sphenacodon, Edaphosaurus, and Ophiacodon.
Systematics
In traditional classification, the order Pelycosauria is paraphyletic--that is, it is a grouping of animals that does not contain all descendants of a common ancestor, as is often required by a different system of naming organisms, phylogenetic nomenclature. In the later, Pelycosauria is treated as a clade rather than a taxon with the rank "order", and includes the clade Therapsida, which in turn contains the clade Mammalia. In traditional taxonomy, Therapsida is separated from Pelycosauria in it's own biological order, and mammals are separated from both as their own class.Taxonomy
- Order Pelycosauria*
- Suborder Caseasauria
- Family Caseidae
- Family Eothyrididae
- Suborder Eupelycosauria
- Family Edaphosauridae
- Family Haplodontidae*
- Cutleria
- Haptodus
- Palaeohatteria
- Pantelosaurus
- Family Lupeosauridae
- Lupeosaurus
- Family Ophiacodontidae
- Family Sphenacodontidae
- Family Varanopseidae
- '''Order Therapsida*
Phylogeny
In phylogenetic nomenclature, the "Pelycosauria" is not used, since it does not constitute a clade (a group of organisms descended from one common ancestor and including all the descendants of that ancestor) because the group excludes the therapsids. Instead, it represents a paraphyletic "grade" of basal synapsids leading up to the clade Therapsida. The following cladogram follows the one found on Mikko's Phylogeny Archive.| Synapsida |
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See also
References
- Reisz, R. R., 1986, Handbuch der Paläoherpetologie – Encyclopedia of Paleoherpetology, Part 17A Pelycosauria Verlag Dr. Friedrich Pfeil, ISBN 3-89937-032-5
- Romer, AS & Price L.I (1940), Review of the Pelycosauria. Geol. Soc. Amer. Spec. Papers 28: 1-538.
External links
- Introduction to the Pelycosaurs - at UCMP
- Synapsida - Pelycosauria - at Palaeos
Pennsylvanian is an epoch of the Carboniferous period lasting from roughly 325 Ma to 299 Ma (million years ago). As with most other geologic periods, the rock beds that define the period are well identified, but the exact date of the start and end are uncertain by a few million
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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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Dimetrodon
Cope, 1878
Species
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Cope, 1878
Species
- D. milleri
- D. natalis
- D. limbatus
- D. booneorum
- D. gigashomogenes
- D. grandis
- D. loomisi
- D. angelensis
- D.
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National Museum of Natural History is a museum administered by the Smithsonian Institution, located on the National Mall in Washington, D.C.
The museum's collections total over 125 million specimens of plants, animals, fossils, minerals, rocks, meteorites, and human cultural
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The museum's collections total over 125 million specimens of plants, animals, fossils, minerals, rocks, meteorites, and human cultural
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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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Tetrapoda
Broili, 1913
Classes
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Broili, 1913
Classes
- Amphibia
- Aves
- Mammalia
- Sauropsida (Reptilia)
- Synapsida
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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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In phylogenetics, a group of organisms is said to be paraphyletic (Greek para = near and phyle = race) if the group contains its most recent common ancestor, but does not contain all the descendants of that ancestor.
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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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Cope was born in Philadelphia to Quaker parents.
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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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Caseasauria
Williston, 1912
Genera and Families
Caseidae
Eothyrididae
?Phreatophasma
The Caseasauria are one of the two main clades of early synapsids, the other being the Eupelycosauria.
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Williston, 1912
Genera and Families
Caseidae
Eothyrididae
?Phreatophasma
The Caseasauria are one of the two main clades of early synapsids, the other being the Eupelycosauria.
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Eupelycosauria
Kemp, 1982
Families and Clades
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Kemp, 1982
Families and Clades
- Varanopseidae
- Ophiacodontidae
- Edaphosauridae
- Sphenacodontia *
- Sphenacodontidae
- Therapsida *
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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 Paleozoic Era (from the Greek palaio, "old" and zoion, "animals", meaning "ancient life") is the earliest of three geologic eras of the Phanerozoic eon.
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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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Amniota
Haeckel, 1866
Living subgroups
See text
The amniotes are a group of tetrapod vertebrates that include the Synapsida (mammals and mammal-like reptiles) and Sauropsida (reptiles and dinosaurs, including birds).
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Haeckel, 1866
Living subgroups
See text
The amniotes are a group of tetrapod vertebrates that include the Synapsida (mammals and mammal-like reptiles) and Sauropsida (reptiles and dinosaurs, including birds).
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Pennsylvanian is an epoch of the Carboniferous period lasting from roughly 325 Ma to 299 Ma (million years ago). As with most other geologic periods, the rock beds that define the period are well identified, but the exact date of the start and end are uncertain by a few million
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The Carboniferous is a major division of the geologic timescale that extends from the end of the Devonian period, about 359.2 ± 2.5 Ma (million years ago), to the beginning of the Permian period, about 299.0 ± 0.8 Ma (ICS 2004).
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Cisuralian is the first of the three epochs of the Permian.
Permian period
Cisuralian Guadalupian Lopingian
Asselian | Sakmarian
Artinskian | Kungurian Roadian | Wordian
Capitanian Wuchiapingian
Changhsingian
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Permian period
Cisuralian Guadalupian Lopingian
Asselian | Sakmarian
Artinskian | Kungurian Roadian | Wordian
Capitanian Wuchiapingian
Changhsingian
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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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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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Lopingian is the third of the three epoches of the Permian. The world was hot and arid. The epoch saw one the largest deserts of all time, in the middle of Pangea. Monsoons probably prevailed in the coasts or a little further inland.
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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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Archosauria
Cope, 1869
Clades
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Cope, 1869
Clades
- Crurotarsi
- Aetosauria
- Crocodilia (crocodiles)
- Phytosauria
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Sauropsida*
Goodrich, 1916
Subclasses
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Goodrich, 1916
Subclasses
- Anapsida
- Diapsida
- Reptilia Laurenti, 1768
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Mammalia
Linnaeus, 1758
Subclasses
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Linnaeus, 1758
Subclasses
- Allotheria*
- Order Multituberculata (extinct)
- Order Volaticotheria (extinct)
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Cladistics is a philosophy of classification that arranges organisms only by their order of branching in an evolutionary tree and not by their morphological similarity, in the words of Luria et al. (1981).
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Edaphosauridae
Cope, 1882
Genera
The Edaphosauridae
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Cope, 1882
Genera
- Edaphosaurus
- Ianthasaurus
- Glaucosaurus
The Edaphosauridae
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