Gymnarthridae
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Gymnarthridae
Gymnarthridae is an extinct family of tuditanomorph microsaurs. Gymnarthrids are known from Europe and North America and existed from the Late Carboniferous through the Early Permian. Remains have been found from the Czech Republic, Nova Scotia, Illinois, Texas, and Oklahoma. Gymnarthrids are relatively elongate with short limbs. The skulls of gymnarthrids are also small, with a single row of large conical teeth on the margin of the jaw (a feature that distinguishes them from other microsaurs). In some genera, such as ''Bolterpeton'' and ''Cardiocephalus'', the teeth are labiolingually compressed. Gymnarthridae was first erected by E. C. Case in 1910 to include the newly described ''Gymnarthrus''. It was placed in a new suborder, Gymnarthria. Case initially considered gymnarthrids to be reptiles, but later recognized them to be amphibians, placing ''Cardiocephalus'' in the family. ''Pariotichus'' was placed within Gymnarthridae by Alfred Romer after having previously been assi ...
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Gymnarthrids
Gymnarthridae is an extinct family of tuditanomorph microsaurs. Gymnarthrids are known from Europe and North America and existed from the Late Carboniferous through the Early Permian. Remains have been found from the Czech Republic, Nova Scotia, Illinois, Texas, and Oklahoma. Gymnarthrids are relatively elongate with short limbs. The skulls of gymnarthrids are also small, with a single row of large conical teeth on the margin of the jaw (a feature that distinguishes them from other microsaurs). In some genera, such as ''Bolterpeton'' and ''Cardiocephalus'', the teeth are labiolingually compressed. Gymnarthridae was first erected by E. C. Case in 1910 to include the newly described ''Gymnarthrus''. It was placed in a new suborder, Gymnarthria. Case initially considered gymnarthrids to be reptiles, but later recognized them to be amphibians, placing ''Cardiocephalus'' in the family. ''Pariotichus'' was placed within Gymnarthridae by Alfred Romer after having previously been assi ...
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Tuditanomorpha
Tuditanomorpha is a suborder of microsaur lepospondyls. Tuditanomorphs lived from the Late Carboniferous to the Early Permian and are known from North America and Europe. Tuditanomorphs have a similar pattern of bones in the skull roof. Tuditanomorphs display considerable variability, especially in body size, proportions, dentition, and presacral vertebral count. Currently there are seven families of tuditanomorphs, with two being monotypic. Tuditanids, gymnarthrids, and pantylids first appear in the Lower Pennsylvanian. Goniorhynchidae, Hapsidopareiontidae, Ostodolepidae, and Trihecatontidae appear in the Late Pennsylvanian and Early Permian. Classification Suborder Tuditanomorpha *Family Goniorhynchidae **''Rhynchonkos'' *Family Gymnarthridae **''Cardiocephalus'' **''Elfridia'' **''Euryodus'' **''Leiocephalikon'' **''Pariotichus'' **''Sparodus'' *Family Hapsidopareiontidae **''Hapsidopareion'' **''Llistrofus'' **''Ricnodon'' **''Saxonerpeton'' *Family Ostodolepidae **' ...
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Microsaur
Microsauria ("small lizards") is an extinct, possibly polyphyletic order of tetrapods from the late Carboniferous and early Permian periods. It is the most diverse and species-rich group of lepospondyls. Recently, Microsauria has been considered paraphyletic, as several other non-microsaur lepospondyl groups such as Lysorophia seem to be nested in it. Microsauria is now commonly used as a collective term for the grade of lepospondyls that were originally classified as members of Microsauria. The microsaurs all had short tails and small legs, but were otherwise quite varied in form. The group included lizard-like animals that were relatively well-adapted to living on dry land, burrowing forms, and others that, like the modern axolotl, retained their gills into adult life, and so presumably never left the water. Distribution Microsaur remains have been found from Europe and North America in Late Carboniferous and Early Permian localities. Most North American microsaurs have bee ...
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Pariotichus
''Pariotichus'' is an extinct genus of gymnarthrid microsaurs from the early Permian of Texas. History of study ''Pariotichus'' was collected by Jacob Boll from the Wichita Group of Texas in 1878 and described by American paleontologist Edward Drinker Cope in the same year. It is one of the first 'microsaurs' to be described from North America. The type species is ''Pariotichus brachyops'', which remains the only presently recognized species of the genus. Other species of ''Pariotichus'' were described, mostly by Cope, that have subsequently been identified as captorhinomorph reptiles (including the well-known ''Captorhinus aguti'') and were reassigned by Case (1911). One other species, "''Pariotichus megalops''" is a junior synonym of the dvinosaur temnospondyl '' Isodectes obtusus.'' The osteology and relationships of ''P. brachyops'' were subsequently reviewed by Gregory et al. (1956) and Carroll & Gaskill (1978). Anatomy The holotype and only specimen of ''Pariotichus'' i ...
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Cardiocephalus
''Cardiocephalus'' is an extinct genus of lepospondyl amphibian from the Permian period. It was a member of the family Gymnarthridae Gymnarthridae is an extinct family of tuditanomorph microsaurs. Gymnarthrids are known from Europe and North America and existed from the Late Carboniferous through the Early Permian. Remains have been found from the Czech Republic, Nova Scotia, .... References External links''Cardiocephalus'' fossil pictures. Gymnarthrids Cisuralian amphibians of North America Fossil taxa described in 1904 {{Lepospondyli-stub ...
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Anatomical Terms Of Location
Standard anatomical terms of location are used to unambiguously describe the anatomy of animals, including humans. The terms, typically derived from Latin or Greek roots, describe something in its standard anatomical position. This position provides a definition of what is at the front ("anterior"), behind ("posterior") and so on. As part of defining and describing terms, the body is described through the use of anatomical planes and anatomical axes. The meaning of terms that are used can change depending on whether an organism is bipedal or quadrupedal. Additionally, for some animals such as invertebrates, some terms may not have any meaning at all; for example, an animal that is radially symmetrical will have no anterior surface, but can still have a description that a part is close to the middle ("proximal") or further from the middle ("distal"). International organisations have determined vocabularies that are often used as standard vocabularies for subdisciplines of anatom ...
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Permian Amphibians
The Permian ( ) is a geologic period and stratigraphic system which spans 47 million years from the end of the Carboniferous Period million years ago (Mya), to the beginning of the Triassic Period 251.9 Mya. It is the last period of the Paleozoic Era; the following Triassic Period belongs to the Mesozoic Era. The concept of the Permian was introduced in 1841 by geologist Sir Roderick Murchison, who named it after the region of Perm in Russia. The Permian witnessed the diversification of the two groups of amniotes, the synapsids and the sauropsids (reptiles). The world at the time was dominated by the supercontinent Pangaea, which had formed due to the collision of Euramerica and Gondwana during the Carboniferous. Pangaea was surrounded by the superocean Panthalassa. The Carboniferous rainforest collapse left behind vast regions of desert within the continental interior. Amniotes, which could better cope with these drier conditions, rose to dominance in place of their amphibian ...
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Carboniferous Amphibians
The Carboniferous ( ) is a geologic period and system of the Paleozoic that spans 60 million years from the end of the Devonian Period million years ago ( Mya), to the beginning of the Permian Period, million years ago. The name ''Carboniferous'' means "coal-bearing", from the Latin '' carbō'' ("coal") and '' ferō'' ("bear, carry"), and refers to the many coal beds formed globally during that time. The first of the modern 'system' names, it was coined by geologists William Conybeare and William Phillips in 1822, based on a study of the British rock succession. The Carboniferous is often treated in North America as two geological periods, the earlier Mississippian and the later Pennsylvanian. Terrestrial animal life was well established by the Carboniferous Period. Tetrapods (four limbed vertebrates), which had originated from lobe-finned fish during the preceding Devonian, became pentadactylous in and diversified during the Carboniferous, including early amphibian line ...
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Prehistoric Amphibians Of North America
Prehistory, also known as pre-literary history, is the period of human history between the use of the first stone tools by hominins 3.3 million years ago and the beginning of recorded history with the invention of writing systems. The use of symbols, marks, and images appears very early among humans, but the earliest known writing systems appeared 5000 years ago. It took thousands of years for writing systems to be widely adopted, with writing spreading to almost all cultures by the 19th century. The end of prehistory therefore came at very different times in different places, and the term is less often used in discussing societies where prehistory ended relatively recently. In the early Bronze Age, Sumer in Mesopotamia, the Indus Valley Civilisation, and ancient Egypt were the first civilizations to develop their own scripts and to keep historical records, with their neighbors following. Most other civilizations reached the end of prehistory during the following Iron Age. T ...
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Prehistoric Amphibians Of Europe
Prehistory, also known as pre-literary history, is the period of human history between the use of the first stone tools by hominins 3.3 million years ago and the beginning of recorded history with the invention of writing systems. The use of symbols, marks, and images appears very early among humans, but the earliest known writing systems appeared 5000 years ago. It took thousands of years for writing systems to be widely adopted, with writing spreading to almost all cultures by the 19th century. The end of prehistory therefore came at very different times in different places, and the term is less often used in discussing societies where prehistory ended relatively recently. In the early Bronze Age, Sumer in Mesopotamia, the Indus Valley Civilisation, and ancient Egypt were the first civilizations to develop their own scripts and to keep historical records, with their neighbors following. Most other civilizations reached the end of prehistory during the following Iron Age. T ...
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