Information about Anapsid
| Anapsids Fossil range: Permian - Recent | ||||||||||||
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Anapsid skull | ||||||||||||
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Testudines (Turtles, tortoises & terrapins) Mesosauria - extinct Millerettidae - extinct Nyctiphruretidae - extinct Pareiasauridae - extinct Procolophonidae - extinct Captorhinida - extinct | ||||||||||||
An anapsid is an amniote whose skull does not have openings near the temples.[1]
While "anapsid reptiles" or "anapsida" are traditionally spoken of as if they were a coherent group, it has been suggested that several groups of reptiles that had anapsid skulls may be only distantly related: scientists still debate the exact relationship between the basal (original) reptiles which first appeared in the late Carboniferous, the various Permian reptiles which had anapsid skulls, and the Testudines (turtles, tortoises, and terrapins). Many modern paleontologists believe the Testudines are descended from diapsid reptiles which lost their temporal fenestrae, although that view is not generally accepted yet (see Parareptilia for details and references).
The only living reptiles with anapsid skulls are the Testudines. The earliest fossil testudines are from the Triassic, but they were already too like modern turtles to be near the start of their lineage - in particular they already had limb joints within the rib cage. The main article about Testudines covers the debate about their ancestry.
Most of the other reptiles with anapsid skulls, including the millerettids, nyctiphrurets, and pareiasaurs, became extinct in the late Permian period by the Permian-Triassic extinction event. But the procolophonids managed to survive into the Triassic.
References
1. ^ Pough, F. H. et al. (2002) Vertebrate Life, 6th Ed. Prentice Hall Inc., Upper Saddle River, NJ. ISBN 0130412481
See also
External links
- Introduction to Anapsida from UCMP
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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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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Vertebrata
Cuvier, 1812
Classes and Clades
See below
Vertebrates are members of the subphylum Vertebrata (within the phylum Chordata), specifically, those chordates with backbones or spinal columns.
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Cuvier, 1812
Classes and Clades
See below
Vertebrates are members of the subphylum Vertebrata (within the phylum Chordata), specifically, those chordates with backbones or spinal columns.
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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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Sauropsida*
Goodrich, 1916
Subclasses
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Goodrich, 1916
Subclasses
- Anapsida
- Diapsida
- Reptilia Laurenti, 1768
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Henry Fairfield Osborn (August 8, 1857–November 6, 1935) was an American geologist, paleontologist, and eugenicist.
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Biography
Osborn was born in Fairfield, Connecticut, and studied at Princeton University...... Read more.
Testudines
Linnaeus, 1758
Diversity
ca. 300 species in 14 extant families.
Suborders
Cryptodira
Pleurodira
See text for families.
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Linnaeus, 1758
Diversity
ca. 300 species in 14 extant families.
blue: sea turtles, black: land turtles
Suborders
Cryptodira
Pleurodira
See text for families.
..... Read more.
Testudinidae
Genera
Chersina
Cylindraspis (extinct)
Dipsochelys
Geochelone
Gopherus
Homopus
Indotestudo
Kinixys
Malacochersus
Manouria
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Genera
Chersina
Cylindraspis (extinct)
Dipsochelys
Geochelone
Gopherus
Homopus
Indotestudo
Kinixys
Malacochersus
Manouria
..... Read more.
Mesosauria
Family: Mesosauridae
Baur, 1889
Genera
Brasileosaurus
Stereosternum
Mesosaurus
Mesosaur
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Family: Mesosauridae
Baur, 1889
Genera
Brasileosaurus
Stereosternum
Mesosaurus
Mesosaur
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Millerettidae
Genera
..... Read more.
Genera
- Broomia
- Heleophilus
- Milleretoides
- Milleretta
- Millerettops
- Milleropsis
- Millerosaurus
- Nanomilleretta
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Pareiasauridae
Lydekker, 1889
Genera
Bradysaurus
Nochelesaurus
Embrithosaurus
Deltavjatia
Velosauria
Shihtienfenia
Pareiasuchus
Pareiasaurus
Scutosaurus
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Lydekker, 1889
Genera
Bradysaurus
Nochelesaurus
Embrithosaurus
Deltavjatia
Velosauria
Shihtienfenia
Pareiasuchus
Pareiasaurus
Scutosaurus
..... Read more.
Procolophonidae
Seeley, 1888
Genera
Owenetta
Procolophon
Hypsognathus
The Procolophonids - family Procolophonidae (Superfamily Procolophonoidea)- are a group of small reptiles.
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Seeley, 1888
Genera
Owenetta
Procolophon
Hypsognathus
The Procolophonids - family Procolophonidae (Superfamily Procolophonoidea)- are a group of small reptiles.
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Captorhinida *
Families
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Families
- Bolosauridae
- Captorhinidae
- Millerettidae
- Protorothyrididae
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Anaspida ("Without Shields") are stem gnathostomes, and are classically regarded as the ancestors of lampreys. Anaspids were small marine agnathans that lacked scales and paired fins.
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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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Temple indicates the side of the head behind the eyes. The bone beneath is the temporal bone.
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Anatomy
Cladists classify land vertebrates based on the presence of an upper hole, a lower hole, both, or neither in the cover of dermal bone which formerly covered the..... Read more.
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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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.
..... Read more.
..... Read more.
Testudines
Linnaeus, 1758
Diversity
ca. 300 species in 14 extant families.
Suborders
Cryptodira
Pleurodira
See text for families.
..... Read more.
Linnaeus, 1758
Diversity
ca. 300 species in 14 extant families.
blue: sea turtles, black: land turtles
Suborders
Cryptodira
Pleurodira
See text for families.
..... Read more.
Testudines
Linnaeus, 1758
Diversity
ca. 300 species in 14 extant families.
Suborders
Cryptodira
Pleurodira
See text for families.
..... Read more.
Linnaeus, 1758
Diversity
ca. 300 species in 14 extant families.
blue: sea turtles, black: land turtles
Suborders
Cryptodira
Pleurodira
See text for families.
..... Read more.
Testudinidae
Genera
Chersina
Cylindraspis (extinct)
Dipsochelys
Geochelone
Gopherus
Homopus
Indotestudo
Kinixys
Malacochersus
Manouria
..... Read more.
Genera
Chersina
Cylindraspis (extinct)
Dipsochelys
Geochelone
Gopherus
Homopus
Indotestudo
Kinixys
Malacochersus
Manouria
..... Read more.
A terrapin is a turtle that lives in fresh or brackish water.[1]
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Etymology
The word is derived from an Algonquian for the brackish water species diamondback terrapin, Malaclemys terrapin...... Read more.
Diapsida
Osborn, 1903
Groups
See text
Diapsids ("two arches") are a group of tetrapod animals that developed two holes (temporal fenestra) in each side of their skulls, about 300 million years ago during the late Carboniferous period.
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Osborn, 1903
Groups
See text
Diapsids ("two arches") are a group of tetrapod animals that developed two holes (temporal fenestra) in each side of their skulls, about 300 million years ago during the late Carboniferous period.
..... Read more.
Parareptilia
Olson, 1947
Groups
See cladograms below
Parareptilia ("at the side of reptiles") is a subclass or clade of Reptiles which are variously defined as an extinct group of primitive anapsids, or a more cladistically correct alternative to
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Olson, 1947
Groups
See cladograms below
Parareptilia ("at the side of reptiles") is a subclass or clade of Reptiles which are variously defined as an extinct group of primitive anapsids, or a more cladistically correct alternative to
..... Read more.
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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Testudines
Linnaeus, 1758
Diversity
ca. 300 species in 14 extant families.
Suborders
Cryptodira
Pleurodira
See text for families.
..... Read more.
Linnaeus, 1758
Diversity
ca. 300 species in 14 extant families.
blue: sea turtles, black: land turtles
Suborders
Cryptodira
Pleurodira
See text for families.
..... Read more.
Millerettidae
Genera
..... Read more.
Genera
- Broomia
- Heleophilus
- Milleretoides
- Milleretta
- Millerettops
- Milleropsis
- Millerosaurus
- Nanomilleretta
..... Read more.
Pareiasauridae
Lydekker, 1889
Genera
Bradysaurus
Nochelesaurus
Embrithosaurus
Deltavjatia
Velosauria
Shihtienfenia
Pareiasuchus
Pareiasaurus
Scutosaurus
..... Read more.
Lydekker, 1889
Genera
Bradysaurus
Nochelesaurus
Embrithosaurus
Deltavjatia
Velosauria
Shihtienfenia
Pareiasuchus
Pareiasaurus
Scutosaurus
..... Read more.