Chomatodus Gracillimus
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Chomatodus Gracillimus
''Chomatodus'' (from el, χωμα , 'mound' and el, ὀδούς 'tooth') is a prehistoric cartilaginous fish genus. Species *†''Chomatodus affinis'' Newberry & Worthen, 1866 *†''Chomatodus angulatus'' Newberry & Worthen, 1866 *†''Chomatodus angustus'' Newberry, 1879 *†''Chomatodus arcuatus'' St. John, 1870 *†''Chomatodus chesterensis'' St. John & Worthen, 1875 *†''Chomatodus comptus'' St. John & Worthen, 1875 *†''Chomatodus costatus'' Newberry & Worthen, 1866 *†''Chomatodus cultellus'' Anonymous author(s) *†''Chomatodus davisi'' Woodward, 1889 *†''Chomatodus dentatus'' Anonymous author(s) *†''Chomatodus elegans'' Newberry & Worthen, 1866 Remains have been found in Keokuk Limestone, Keokuk, Iowa, United States. *†''Chomatodus gracillimus'' Newberry & Worthen, 1866 *†''Chomatodus inconstans'' St. John & Worthen, 1875 *†''Chomatodus incrassatus'' Anonymous author(s) *†''Chomatodus insignis'' Leidy, 1857 *†''Chomatodus lamelliformis'' Dav ...
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Louis Agassiz
Jean Louis Rodolphe Agassiz ( ; ) FRS (For) FRSE (May 28, 1807 – December 14, 1873) was a Swiss-born American biologist and geologist who is recognized as a scholar of Earth's natural history. Spending his early life in Switzerland, he received a PhD at Erlangen and a medical degree in Munich. After studying with Georges Cuvier and Alexander von Humboldt in Paris, Agassiz was appointed professor of natural history at the University of Neuchâtel. He emigrated to the United States in 1847 after visiting Harvard University. He went on to become professor of zoology and geology at Harvard, to head its Lawrence Scientific School, and to found its Museum of Comparative Zoology. Agassiz is known for observational data gathering and analysis. He made institutional and scientific contributions to zoology, geology, and related areas, including multivolume research books running to thousands of pages. He is particularly known for his contributions to ichthyological classification, ...
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Keokuk Limestone
The Keokuk Limestone is a geologic formation in Illinois, Iowa and Missouri Missouri is a state in the Midwestern region of the United States. Ranking 21st in land area, it is bordered by eight states (tied for the most with Tennessee): Iowa to the north, Illinois, Kentucky and Tennessee to the east, Arkansas t .... It preserves fossils dating back to the Mississippian sub-period. See also * List of fossiliferous stratigraphic units in Illinois * List of fossiliferous stratigraphic units in Iowa * List of fossiliferous stratigraphic units in Missouri References * Carboniferous Illinois Carboniferous Iowa Carboniferous Missouri Carboniferous southern paleotropical deposits {{US-geologic-formation-stub ...
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List Of Prehistoric Cartilaginous Fish Genera
This list of prehistoric cartilaginous fish genera is an attempt to create a comprehensive listing of all genera that have ever been included in the class chondrichthyes ''and'' are known from the fossil record. This list excludes purely vernacular terms, genera that are now considered invalid, doubtful (nomina dubia), or were not formally published (nomina nuda), as well as junior synonyms of more established names, and genera that are no longer considered to be cartilaginous fish. It includes all commonly accepted genera. This list currently contains 804 generic names. * Extinct genera are marked by a dagger ( †). * Extant taxon genera are bolded. Naming conventions and terminology Naming conventions and terminology follow the International Code of Zoological Nomenclature. Technical terms used include: * Junior synonym: A name which describes the same taxon as a previously published name. If two or more genera are formally designated and the type specimens are later ass ...
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Prehistoric Cartilaginous Fish Genera
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. ...
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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 Montana () is a state in the Mountain West division of the Western United States. It is bor ...
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Fossil Taxa Described In 1838
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 amber, hair, petrified wood and DNA remnants. The totality of fossils is known as the ''fossil record''. Paleontology is the study of fossils: their age, method of formation, and evolutionary significance. Specimens are usually considered to be fossils if they are over 10,000 years old. The oldest fossils are around 3.48 billion years old to 4.1 billion years old. Early edition, published online before print. The observation in the 19th century that certain fossils were associated with certain rock strata led to the recognition of a geological timescale and the relative ages of different fossils. The development of radiometric dating techniques in the early 20th century allowed scientists to quantitatively measure the absol ...
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