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Neopteroplax
''Neopteroplax'' is an extinct genus of eogyrinid embolomere closely related to European genera such as ''Eogyrinus'' and '' Pteroplax''. Members of this genus were among the largest embolomeres (and Carboniferous tetrapods in general) in North America. ''Neopteroplax'' is primarily known from a large (~40 cm) skull found in Ohio, although fragmentary embolomere fossils from Texas and New Mexico have also been tentatively referred to the genus. Despite its similarities to specific European embolomeres, it can be distinguished from them due to a small number of skull and jaw features, most notably a lower surangular at the upper rear portion of the lower jaw. Discovery The type species, ''Neopteroplax conemaughensis'', is known from a large skull found in Late Carboniferous shale during railroad renovations in Bloomingdale, Ohio. Although damaged by excavators, most of the left side of the skull can be reconstructed based on surviving fragments. The only other ''Neopteroplax' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eogyrinidae
Eogyrinidae is an extinct family of large, long-bodied tetrapods that lived in the rivers of the Late Carboniferous period. Gallery image:Eogyrinus BW.jpg, '' Eogyrinus''. image:Pteroplax DB.jpg, '' Pteroplax''. image:Diplovertebron BW.jpg, ''Diplovertebron ''Diplovertebron'' (from el, διπλοῦς , 'double' and la, vertebron, 'vertebra') is an extinct genus of embolomere that lived in the Late Carboniferous period (Moscovian), about 310 million years ago. ''Diplovertebron'' was a medium-siz ...'' Embolomeres Carboniferous vertebrates Pennsylvanian first appearances Pennsylvanian extinctions Prehistoric tetrapod families {{paleo-amphibian-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Embolomeri
Embolomeri is an order of tetrapods or stem-tetrapods, possibly members of Reptiliomorpha. Embolomeres first evolved in the Early Carboniferous (Mississippian) Period and were the largest and most successful predatory tetrapods of the Late Carboniferous (Pennsylvanian) Period. They were specialized semiaquatic predators with long bodies for eel-like undulatory swimming. Embolomeres are characterized by their vertebral centra, which are formed by two cylindrical segments, the pleurocentrum at the rear and intercentrum at the front. These segments are equal in size. Most other tetrapods have pleurocentra and intercentra which are drastically different in size and shape. Embolomeres were among the earliest large carnivorous tetrapods, with members such as the crocodilian-like '' Proterogyrinus'' appearing in the Visean stage of the Carboniferous. They declined in diversity during the Permian period, though at least one representative ('' Archeria)'' was common in the Early Permia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alfred Romer
Alfred Sherwood Romer (December 28, 1894 – November 5, 1973) was an American paleontologist and biologist and a specialist in vertebrate evolution. Biography Alfred Romer was born in White Plains, New York, the son of Harry Houston Romer and his wife, Evalyn Sherwood. He was educated at White Plains High School. He studied at Amherst College for his Bachelor of Science Honours degree in biology, then at Columbia University for an M.Sc in Biology and a doctorate in zoology in 1921. Romer joined the department of geology and paleontology at the University of Chicago as an associate professor in 1923. He was an active researcher and teacher. His collecting program added important Paleozoic specimens to Chicago's Walker Museum of Paleontology. In 1934 he was appointed professor of biology at Harvard University. In 1946, he became director of the Harvard Museum of Comparative Zoology (MCZ). In 1954 Romer was awarded the Mary Clark Thompson Medal from the National Academy of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Thrifty Formation
The Thrifty Formation is a geologic formation in Texas. It preserves fossils 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, shells, exoskeletons, stone imprints of animals or microbes, objects preserved in .... See also * List of fossiliferous stratigraphic units in Texas * Paleontology in Texas References * Geologic formations of Texas {{Texas-geologic-formation-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cladodus
''Cladodus'' is an extinct genus of cartilaginous fishes in the family Cladoselachidae. As the name implies, they are a type of cladodont, primitive sharks with teeth designed to snag fish and swallow them whole, instead of sawing off chunks to swallow. Fossils of ''Cladodus'' have been found in Barkip, Scotland and in the Pitkin Formation (Carboniferous period) in Arkansas, United States. In addition, fossils attributable to ''Cladodus'' are known from the Manning Canyon Shale of Carboniferous age in the state of Utah. Species *†''Cladodus alternatus'' St. John & Worthen, 1875 *†''Cladodus angulatus'' Newberry & Worthen, 1866 *†''Cladodus bellifer'' St. John & Worthen, 1875 *†''Cladodus divaricatus'' Trautschold, 1874 *†''Cladodus elegans'' Newberry & Worthen, 1870 Remains (braincase and a tooth) have been found in Scotland (Clackmannan Group). *†''Cladodus eriensis'' Bryant, 1935 *†''Cladodus formosus'' Hay, 1902 *†''Cladodus gailensis'' Feichtin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Petalodontiformes
Petalodontiformes ("thin-plate teeth") is an extinct order of marine cartilaginous fish related to modern day chimaera found in what is now the United States of America and Europe.Lund, Richard, E. D. Grogan, and M. Fath. "On the relationships of the Petalodontiformes (Chondrichthyes)." Paleontological Journal 48.9 (2014): 1015-1029. Most species are known only from isolated teeth.Dalla Vecchia, Fabio Marco, and Museo Paleontologico Cittadino. "A new petalodont tooth (Chondrichthyes, Petalodontiformes) from the Lower Permian of the Carnic Alps (Friuli, NE Italy)." Bollettino della Società Paleontologica Italiana 39 (2000): 225-228. All fossils range from the Carboniferous to the Permian, where they are presumed to have died out during the Permian/Triassic extinction event. The two best known species are '' Belantsea montana'', from the Carboniferous Bear Gulch, Montana, and '' Janassa bituminosa'', from the upper Permian The Permian ( ) is a geologic period and stratig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conemaugh Series
Conemaugh may refer to the following locations in Pennsylvania: * Conemaugh Township, Cambria County, Pennsylvania **East Conemaugh, Pennsylvania, a borough within the township *Conemaugh Township, Indiana County, Pennsylvania *Conemaugh Township, Somerset County, Pennsylvania *Conemaugh River, a tributary of the Kiskiminetas River **Little Conemaugh River The Little Conemaugh River is a tributary of the Conemaugh River, approximately 30 mi (48 km) long, in western Pennsylvania in the United States. The main branch rises in eastern Cambria County, along the western slope of the Appalachi ..., a tributary of the Conemaugh River * Lake Conemaugh See also * * {{disambiguation, geo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Permian
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 th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Texas
Texas (, ; Spanish language, Spanish: ''Texas'', ''Tejas'') is a state in the South Central United States, South Central region of the United States. At 268,596 square miles (695,662 km2), and with more than 29.1 million residents in 2020, it is the second-largest U.S. state by both List of U.S. states and territories by area, area (after Alaska) and List of U.S. states and territories by population, population (after California). Texas shares borders with the states of Louisiana to the east, Arkansas to the northeast, Oklahoma to the north, New Mexico to the west, and the Mexico, Mexican States of Mexico, states of Chihuahua (state), Chihuahua, Coahuila, Nuevo León, and Tamaulipas to the south and southwest; and has a coastline with the Gulf of Mexico to the southeast. Houston is the List of cities in Texas by population, most populous city in Texas and the List of United States cities by population, fourth-largest in the U.S., while San Antonio is the second most pop ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Platyhystrix
''Platyhystrix'' (from el, πλατύς , 'flat' and el, ῠ̔́στρῐξ , 'porcupine') was a temnospondyl amphibian with a distinctive sail along its back, similar to the unrelated synapsids, ''Dimetrodon'' and ''Edaphosaurus''. It lived during the boundary between the latest Carboniferous and earliest Permian periods in Texas, about 300 million years ago. Palaeobiology ''Platyhystrix'' may have been preyed upon by larger temnospondyls such as '' Eryops'', or by larger carnivorous reptiles, which were becoming more common and diverse in the drier climate of the Permian. The skull was large and strongly built, with a frog-like face. ''Platyhystrix'' had a compact body, reaching long including the tail, and its short, sturdy legs indicate a mainly terrestrial life. ''Platyhystrix'' appeared rather unusual: the dorsal vertebrae were extraordinarily lengthened, and in life they probably formed a skin-covered sail. This structure was possibly for thermal regulation, as in oth ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
