Aytonerpeton

http://dbpedia.org/resource/Aytonerpeton

Aytonerpeton is an extinct genus of stem-tetrapod from the Ballagan Formation of Scotland. It was one of five new genera of early limbed vertebrates from the Ballagan Formation described by Clack et al. in 2016. These vertebrates were among the only known in the world from a period of time known as Romer's gap. Romer's gap, which spans most of the Mississippian age of the Carboniferous, is characterized by a comparative rarity of tetrapod and stem-tetrapod fossils compared to the periods of time directly older and younger than it. However, Aytonerpeton and other Ballagan stem-tetrapods help to close in this gap in the vertebrate fossil record. rdf:langString
Aytonerpeton microps è un tetrapode estinto, i cui resti fossili sono stati ritrovati in terreni risalenti al Carbonifero inferiore (Tournaisiano, circa 355 - 350 milioni di anni fa) in Scozia. rdf:langString
rdf:langString Aytonerpeton
rdf:langString Aytonerpeton microps
rdf:langString Aytonerpeton
xsd:integer 58243909
xsd:integer 1043225979
rdf:langString Clack et al., 2016
rdf:langString Early Carboniferous,
rdf:langString Fossil material of Aytonerpeton microps
rdf:langString Aytonerpeton
rdf:langString †Aytonerpeton microps
rdf:langString Clack et al., 2016
rdf:langString Aytonerpeton is an extinct genus of stem-tetrapod from the Ballagan Formation of Scotland. It was one of five new genera of early limbed vertebrates from the Ballagan Formation described by Clack et al. in 2016. These vertebrates were among the only known in the world from a period of time known as Romer's gap. Romer's gap, which spans most of the Mississippian age of the Carboniferous, is characterized by a comparative rarity of tetrapod and stem-tetrapod fossils compared to the periods of time directly older and younger than it. However, Aytonerpeton and other Ballagan stem-tetrapods help to close in this gap in the vertebrate fossil record.
rdf:langString Aytonerpeton microps è un tetrapode estinto, i cui resti fossili sono stati ritrovati in terreni risalenti al Carbonifero inferiore (Tournaisiano, circa 355 - 350 milioni di anni fa) in Scozia.
xsd:nonNegativeInteger 1939

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