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Cheliderpeton Latirostre
''Glanochthon'' is an extinct genus of temnospondyl amphibian from the Early Permian of Germany. Fossils have been found from the Meisenheim Formation in the Saar–Nahe Basin. References

Cisuralian temnospondyls of Europe Fossils of Germany Stereospondylomorpha Prehistoric amphibian genera Fossil taxa described in 2009 {{temnospondyli-stub ...
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Early Permian
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2009 In Paleontology
Arthropods Cephalopods Three new species of extinct Octopoda discovered in 2009. The species – '' Keuppia hyperbolaris'', '' Keuppia levante'', and '' Styletoctopus annae'' – lived about 95 million years ago, and bear a strong resemblance to modern octopuses, suggesting that the Octopoda order has remained relatively unchanged for tens of millions of years. The fossils included evidence of arms, muscles, rows of suckers, ink, and internal gills. The discovery was made by a team led by Dirk Fuchs of the Freie University, which is located at Berlin, Germany.Rare fossil octopuses found
NBC News, March 18, 2009
The fossils were found at Hakel and Hadjoula, .
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Genus
Genus (; : genera ) is a taxonomic rank above species and below family (taxonomy), family as used in the biological classification of extant taxon, living and fossil organisms as well as Virus classification#ICTV classification, viruses. In binomial nomenclature, the genus name forms the first part of the binomial species name for each species within the genus. :E.g. ''Panthera leo'' (lion) and ''Panthera onca'' (jaguar) are two species within the genus ''Panthera''. ''Panthera'' is a genus within the family Felidae. The composition of a genus is determined by taxonomy (biology), taxonomists. The standards for genus classification are not strictly codified, so different authorities often produce different classifications for genera. There are some general practices used, however, including the idea that a newly defined genus should fulfill these three criteria to be descriptively useful: # monophyly – all descendants of an ancestral taxon are grouped together (i.e. Phylogeneti ...
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Temnospondyl
Temnospondyli (from Greek language, Greek τέμνειν, ''temnein'' 'to cut' and σπόνδυλος, ''spondylos'' 'vertebra') or temnospondyls is a diverse ancient order (biology), order of small to giant tetrapods—often considered Labyrinthodontia, primitive amphibians—that flourished worldwide during the Carboniferous, Permian and Triassic periods, with fossils being found on every continent. A few species continued into the Jurassic and Early Cretaceous periods, but all had gone extinct by the Late Cretaceous. During about 210 million years of evolutionary history, they adapted to a wide range of habitats, including freshwater, terrestrial, and even coastal marine environments. Their life history is well understood, with fossils known from the larval stage, metamorphosis and maturity. Most temnospondyls were semiaquatic, although some were almost fully terrestrial, returning to the water only to breed. These temnospondyls were some of the first vertebrates fully adapted t ...
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Meisenheim Formation
Meisenheim () is a town in the Bad Kreuznach district in Rhineland-Palatinate, Germany. It belongs to the like-named ''Verbandsgemeinde'', and is also its seat. Meisenheim is a state-recognized recreational resort (''Erholungsort'') and it is set out as a middle centre in state planning. Geography Location Meisenheim lies in the valley of the River Glan at the northern edge of the North Palatine Uplands. The municipal area measures 1 324 ha. Neighbouring municipalities Clockwise from the north, Meisenheim's neighbours are Raumbach, Rehborn, Callbach, Reiffelbach, Odenbach, Breitenheim and Desloch, all of which likewise lie within the Bad Kreuznach district, except for Odenbach, which lies in the neighbouring Kusel district. Constituent communities Also belonging to Meisenheim are the outlying homesteads of Hof Wieseck, Keddarterhof and Röther Hof. History Meisenheim is believed to have arisen in the 7th century AD, and its name is often derived from the to ...
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Saar–Nahe Basin
Saar–Nahe Basin is a molasse basin in southwest Germany. The basin is located south of the Hunsrück mountains between the rivers Nahe and the Saar. The aggregation of sediments in the basin started in the late Carboniferous and Early Permian as part of the Variscan orogeny The Variscan orogeny, or Hercynian orogeny, was a geologic mountain-building event caused by Late Paleozoic continental collision between Euramerica (Laurussia) and Gondwana to form the supercontinent of Pangaea. Nomenclature The name ''Varis .... See also * Saar-Nahe Hills Further reading * * * * * * * * * * * * * * * {{DEFAULTSORT:Saar-Nahe Basin Structural geology Sedimentology Geology of Germany Basins of Europe ...
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Cisuralian Temnospondyls Of Europe
The Cisuralian, also known as the Early Permian, is the first series/epoch of the Permian. The Cisuralian was preceded by the Pennsylvanian and followed by the Guadalupian. The Cisuralian Epoch is named after the western slopes of the Ural Mountains in Russia and Kazakhstan and dates between 298.9 ± 0.15 – 272.3 ± 0.5 Ma. In the regional stratigraphy of southwestern North America, the Cisuralian encompasses two series: the Wolfcampian (Asselian to mid-Artinskian) and Leonardian (mid-Artinskian to Kungurian). The series saw the appearance of beetles and flies and was a relatively stable warming period of about 21 million years. Name and background The Cisuralian is the first series or epoch of the Permian. The Cisuralian was preceded by the last Pennsylvanian epoch (Gzhelian) and is followed by the Permian Guadalupian Epoch. The name "Cisuralian" was proposed in 1982, and approved by the International Subcommission on Permian Stratigraphy in 1996. The Cisuralian Epoch is n ...
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Fossils Of Germany
A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, seashell, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in #Resin, amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Though the fossil record is incomplete, numerous studies have demonstrated that there is enough information available to give a good understanding of the pattern of diversification of life on Earth. In addition, the record can predict and fill gaps such as the discovery of ''Tiktaalik'' in the arctic of Canada. Paleontology includes the study of fossils: their age, method of formation, and evolutionary significance. Specimens are sometimes considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years to 4.1 billion years old. Early edition, published online bef ...
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Stereospondylomorpha
Stereospondylomorpha is a clade of temnospondyls. It includes the superfamily Archegosauroidea and the more diverse group Stereospondyli. Stereospondylomorpha was first proposed by Yates and Warren (2000), who found Archegosauroidea and Stereospondyli to be sister taxa in their phylogenetic analysis. A similar clade is Archegosauriformes, named by Schoch and Milner (2000), which includes Stereospondyli and some Permian temnospondyls that are similar in appearance to stereospondyls, including the archegosauroids. However, according to Schoch and Milner's phylogeny, Archegosauroidea is a paraphyletic group of taxa that are successively basal (phylogenetics), basal to Stereospondyli, rather than a monophyletic sister taxon. ''Chinlestegophis'', a putative Triassic stereospondyl considered to be related to Metoposauroidea, metoposauroids such as ''Rileymillerus'', has been noted to share many features with caecilians, a living group of legless burrowing amphibians. If ''Chinlestegoph ...
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Prehistoric Amphibian Genera
Prehistory, also called pre-literary history, is the period of human history between the first known use of stone tools by hominins  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 years ago. It took thousands of years for writing systems to be widely adopted, with writing having spread to almost all cultures by the 19th century. The end of prehistory therefore came at different times in different places, and the term is less often used in discussing societies where prehistory ended relatively recently. It is based on an old conception of history that without written records there could be no history. The most common conception today is that history is based on evidence, however the concept of prehistory hasn't been completely discarded. In the early Bronze Age, Sumer in Mesopotamia, the Indus Valley Civilis ...
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