Braunosteus
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Braunosteus
''Braunosteus schmidti'' is a medium-sized selenosteid arthrodire placoderm known from the Upper Frasnian Kellwasserkalk facies of Late Devonian Bad Wildungen, Germany. ''B. schmidti'' has a broad skull about 9 centimeters long, and a short, but pointed rostrum. Its appearance is very similar to that of the basal selenosteid ''Pachyosteus''. It was originally placed within a monotypic family, "Braunosteidae," by Erik Stensiö Prof Erik Helge Osvald Stensiö HFRSE (2 October 1891 – 11 January 1984) was a Sweden, Swedish paleozoology, paleozoologist. He later took his new surname from his place of origin and is occasionally referred to with both names (as Erik Ander ... in 1959. Obruchev (1964) and Miles (1969) placed it within the Trematosteidae due to the presence of a postpineal fenestra. Denison (1978) has ''B. schmidti'' placed within Selenosteidae, noting that other arthrodires in addition to trematosteids have postpineal fenestrae, as well as similar anatomy of ...
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Selenosteidae
Selenosteidae is an extinct family of small to large-sized arthrodire placoderms from the Late Devonian. With the exception of the Chinese ''Phymosteus'', selenosteids lived in shallow seas in what is now Eastern North America (the Cleveland Shale), Eastern Europe (Holy Cross Mountains, Poland, and the Kellwasserkalk fauna of Bad Wildungen), and Northeastern Africa (the Anti-Atlas Mountains, Morocco). Selenosteids have, in cross section, a rounded body, a blunt snout, and tremendous orbits. The lower jaws were slender, the inferognathals usually either being finely serrated, or adapted for crushing, though, in '' Draconichthys'', the inferognathals had long prongs for seizing prey. The rostrum is very small. Taxonomy Selenosteidae is a member of the clade Aspinothoracidi, which belongs to the clade Pachyosteomorphi, one of the two major clades within Eubrachythoraci. ''Gorgonichthys'' is closely related to the family Selenosteidae, and could possibly be included in the family. ...
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Selenosteidae
Selenosteidae is an extinct family of small to large-sized arthrodire placoderms from the Late Devonian. With the exception of the Chinese ''Phymosteus'', selenosteids lived in shallow seas in what is now Eastern North America (the Cleveland Shale), Eastern Europe (Holy Cross Mountains, Poland, and the Kellwasserkalk fauna of Bad Wildungen), and Northeastern Africa (the Anti-Atlas Mountains, Morocco). Selenosteids have, in cross section, a rounded body, a blunt snout, and tremendous orbits. The lower jaws were slender, the inferognathals usually either being finely serrated, or adapted for crushing, though, in '' Draconichthys'', the inferognathals had long prongs for seizing prey. The rostrum is very small. Taxonomy Selenosteidae is a member of the clade Aspinothoracidi, which belongs to the clade Pachyosteomorphi, one of the two major clades within Eubrachythoraci. ''Gorgonichthys'' is closely related to the family Selenosteidae, and could possibly be included in the family. ...
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Frasnian
The Frasnian is one of two faunal stages in the Late Devonian Period. It lasted from million years ago to million years ago. It was preceded by the Givetian Stage and followed by the Famennian Stage. Major reef-building was under way during the Frasnian Stage, particularly in western Canada and Australia. On land, the first forests were taking shape. In North America, the Antler orogeny peaked, which were contemporary with the Bretonic phase of the Variscan orogeny in Europe. The Frasnian coincides with the second half of the "charcoal gap" in the fossil record, a time when atmospheric oxygen levels were below 13 percent, the minimum necessary to sustain wildfires. North American subdivisions of the Frasnian include * West Falls Group * Sonyea Group * Genesee Group Name and definition The Frasnian Stage was proposed in 1879 by French geologist Jules Gosselet Jules-Auguste Gosselet (19 April 1832 – 20 March 1916) was a French geologist born in Cambrai, France.
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Enseosteus
''Enseosteus'' is an extinct genus of small selenosteid arthrodire placoderms known from the Upper Frasnian Kellwasserkalk facies of Late Devonian Germany and Morocco. ''Enseosteus'' is very similar to the other Kellwasserkalk selenosteids, though, the type species, ''E. jaekelli'', has a bulbous, knob-shaped rostrum. Denison (1978) synonymizes the genera ''Ottonosteus'' (''O. jaekeli'' = ''E. hermanni'') and ''Walterosteus ''Walterosteus'' is an extinct genus of small selenosteid arthrodire placoderms known from the Upper Frasnian Kellwasserkalk facies of Late Devonian Germany and Morocco. ''Walterosteus'' is very similar to the other Kellwasserkalk selenosteids ...'' with ''Enseosteus'', claiming that the two genera are too similar to ''Enseosteus'' to merit separate genus status. Rücklin (2011) agrees with Denison's synonymizing of ''Ottonosteus'', but rejects Denison's synonymization of ''Walterosteus'', claiming how ''Walterosteus'' has a contact between the rostra ...
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Pachyosteus
''Pachyosteus'' is an extinct monospecific genus of medium-sized selenosteid arthrodire placoderm known from the Upper Frasnian Kellwasserkalk facies of Late Devonian Bad Wildungen, Germany and from the Famennian portions of the Holy Cross Mountains of Poland. The type species ''Pachyosteus bulla'' has a broad skull about long, a comparatively long median dorsal plate, and a short rostral plate that meets the pineal plate. Phylogeny ''Pachyosteus'' is a member of the family Selenosteidae of the clade Aspinothoracidi, which belongs to the clade Pachyosteomorphi, one of the two major clades within Eubrachythoraci. The cladogram below shows the phylogeny of ''Pachyosteus'': In his cladogram, Rücklin (2011) regards ''Pachyosteus bulla'' as a basal selenosteid, being the sister taxon of the American genera, and the Kellwasserkalk genera of Germany and Morocco Morocco (),, ) officially the Kingdom of Morocco, is the westernmost country in the Maghreb region of North ...
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Germany
Germany,, officially the Federal Republic of Germany, is a country in Central Europe. It is the second most populous country in Europe after Russia, and the most populous member state of the European Union. Germany is situated between the Baltic and North seas to the north, and the Alps to the south; it covers an area of , with a population of almost 84 million within its 16 constituent states. Germany borders Denmark to the north, Poland and the Czech Republic to the east, Austria and Switzerland to the south, and France, Luxembourg, Belgium, and the Netherlands to the west. The nation's capital and most populous city is Berlin and its financial centre is Frankfurt; the largest urban area is the Ruhr. Various Germanic tribes have inhabited the northern parts of modern Germany since classical antiquity. A region named Germania was documented before AD 100. In 962, the Kingdom of Germany formed the bulk of the Holy Roman Empire. During the 16th ce ...
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Bad Wildungen
Bad Wildungen is a state-run spa and a small town in Waldeck-Frankenberg district in Hesse, Germany. It is located on the German Timber-Frame Road. Geography Location Bad Wildungen lies in the eastern foothills of the Kellerwald range in the so-called ''Waldeck'' holiday region, 11 km west of Fritzlar, and 35 km southwest of Kassel. The town, which spreads out east of the Homberg, is crossed by the river Wilde, which empties into the Eder at the constituent community of Wega. The constituent communities of Wega and Mandern lie on the Eder, on which also lies the Edersee, a reservoir lying only about 10 km northwest (in a straight line) of the main town of Bad Wildungen. The river Urff flows through the southwest constituent communities of Hundsdorf, Armsfeld and Bergfreiheit. The nearest large towns are Kassel (about 35 km; northeast), Marburg (about 60 km; southwest) and Korbach (about 28 km; northwest). Neighbouring communities Bad Wildungen ...
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Devonian
The Devonian ( ) is a geologic period and system of the Paleozoic era, spanning 60.3 million years from the end of the Silurian, million years ago (Mya), to the beginning of the Carboniferous, Mya. It is named after Devon, England, where rocks from this period were first studied. The first significant adaptive radiation of life on dry land occurred during the Devonian. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. The arthropod groups of myriapods, arachnids and hexapods also became well-established early in this period, after starting their expansion to land at least from the Ordovician period. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the Age of Fishes. The placoderms began dominating ...
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Arthrodire
Arthrodira (Greek for "jointed neck") is an Order (biology), order of extinct armored, jawed fishes of the class Placodermi that flourished in the Devonian period before their sudden extinction, surviving for about 50 million years and penetrating most marine ecological niches. Arthrodires were the largest and most diverse of all groups of Placoderms. Description Arthrodire placoderms are notable for the movable joint between armor surrounding their heads and bodies. Like all placoderms, they lacked distinct teeth; instead, they used the sharpened edges of a bony plate on their jawbone as a biting surface. The eye sockets are protected by a bony ring, a feature shared by birds and some ichthyosaurs. Early arthrodires, such as the genus ''Arctolepis'', were well-armoured fishes with flattened bodies. The largest member of this group, ''Dunkleosteus'', was a true superpredator of the latest Devonian period, reaching as much as 6 m in length. In contrast, the long-nosed ''Rolfosteus ...
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Erik Stensiö
Prof Erik Helge Osvald Stensiö HFRSE (2 October 1891 – 11 January 1984) was a Sweden, Swedish paleozoology, paleozoologist. He later took his new surname from his place of origin and is occasionally referred to with both names (as Erik Andersson Stensiö, Erik A. Stensiö or Erik A:son Stensiö) Life Erik Helge Oswald Andersson, as his original name was, was born in the village of Stensjö by in Döderhult parish in Kalmar County, the son of Johan Fredrik Andersson (d.1907), a farmer, and his wife, Otilia Maria Erlandson (d.1940). He was educated at Linköping Gymnasium. He then studied science at the University of Uppsala, graduating BSc in 1912. He received his Ph.D. and a docentship in paleontology from Uppsala University in 1921 and became professor and keeper at the Zoopaleontological (later called the Paleozoological) department of the Swedish Museum of Natural History in Stockholm in 1923, a position he held until his retirement in 1959. Stensiö specialized in the ...
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