Agorophius
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Agorophius
''Agorophius'' is an extinct genus of toothed whale that lived during the Oligocene period, approximately , in the waters off what is now South Carolina. Taxonomy The holotype of ''Agorophius pygmaeus'', MCZ 8761, was first mentioned in an 1848 report on the geology of South Carolina by Michael Tuomey. It was eventually described as ''Zeuglodon pygmaeus'' by Johannes Peter Müller in 1849. Louis Agassiz coined the name ''Phocodon holmesii'' for the same specimen, classifying it as an odontocete. Later authors considered ''Zeuglodon pygmaeus'' a species of either ''Dorudon'' or ''Squalodon'', and in 1895 Edward Drinker Cope eventually recognized it as being a distinct genus, which he named ''Agorophius''. Although the skull is lost and the tooth is the only extant part of MCZ 8761, Fordyce (1981) was able to diagnose ''Agorophius'' based on existing descriptions of the skull by Muller, Cope, and Agassiz.R. E. Fordyce. 1981. Systematics of the odontocete whale Agorophius pygmaeus a ...
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Xenorophus
''Xenorophus'' is a genus of primitive odontocete from late Oligocene ( Chattian) marine deposits in South Carolina belonging to Xenorophidae. Classification ''Xenorophus'' was originally described on the basis of a skull from the Chandler Bridge Formation of South Carolina in the collections of the USNM. Later authors, but also Remington Kellogg who described the genus, classified it in the family Agorophiidae ''Agorophius'' is an extinct genus of toothed whale that lived during the Oligocene period, approximately , in the waters off what is now South Carolina. Taxonomy The holotype of ''Agorophius pygmaeus'', MCZ 8761, was first mentioned in an 1848 ..., which eventually became a repository for primitive odontocetes. Whitmore and Sanders (1977) and Fordyce (1981), however, preferred to treat ''Xenorophus'' as Odontoceti ''incertae sedis''. A cladistic analysis by Mark Uhen published in 2008 recognized ''Xenorophus'' as belonging with '' Archaeodelphis'' and '' Albertodelp ...
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Ashley Formation
The Ashley Formation is a geologic formation in South Carolina. It preserves fossils dating back to the Paleogene period Period may refer to: Common uses * Era, a length or span of time * Full stop (or period), a punctuation mark Arts, entertainment, and media * Period (music), a concept in musical composition * Periodic sentence (or rhetorical period), a concept .... Vertebrate fauna Mammals Reptiles Fish Cartilaginous fish Bony fish See also * List of fossiliferous stratigraphic units in South Carolina * Paleontology in South Carolina References * Paleogene geology of South Carolina {{SouthCarolina-geologic-formation-stub ...
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Chandler Bridge Formation
The Chandler Bridge Formation is a geologic formation in South Carolina. It preserves fossils dating back to the Chattian (Late Oligocene) of the Paleogene period, corresponding to the Arikareean in the NALMA classification.Chandler Bridge Formation
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The formation overlies the and is overlain by the Edisto Formation.
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Oligocene
The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified but the exact dates of the start and end of the epoch are slightly uncertain. The name Oligocene was coined in 1854 by the German paleontologist Heinrich Ernst Beyrich from his studies of marine beds in Belgium and Germany. The name comes from the Ancient Greek (''olígos'', "few") and (''kainós'', "new"), and refers to the sparsity of extant forms of molluscs. The Oligocene is preceded by the Eocene Epoch and is followed by the Miocene Epoch. The Oligocene is the third and final epoch of the Paleogene Period. The Oligocene is often considered an important time of transition, a link between the archaic world of the tropical Eocene and the more modern ecosystems of the Miocene. Major changes during the Oligocene included a global expansion o ...
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Prehistoric Cetacean 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. T ...
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Prehistoric Mammals Of North America
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. T ...
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Oligocene Cetaceans
The Oligocene ( ) is a geologic epoch of the Paleogene Period and extends from about 33.9 million to 23 million years before the present ( to ). As with other older geologic periods, the rock beds that define the epoch are well identified but the exact dates of the start and end of the epoch are slightly uncertain. The name Oligocene was coined in 1854 by the German paleontologist Heinrich Ernst Beyrich from his studies of marine beds in Belgium and Germany. The name comes from the Ancient Greek (''olígos'', "few") and (''kainós'', "new"), and refers to the sparsity of extant forms of molluscs. The Oligocene is preceded by the Eocene Epoch and is followed by the Miocene Epoch. The Oligocene is the third and final epoch of the Paleogene Period. The Oligocene is often considered an important time of transition, a link between the archaic world of the tropical Eocene and the more modern ecosystems of the Miocene. Major changes during the Oligocene included a global expansion ...
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Prehistoric Toothed Whales
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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Xenorophidae
Xenorophidae is an extinct family of odontocetes currently known from the Oligocene of the southeastern US. Known genera of xenorophids include '' Albertocetus'', '' Archaeodelphis'', ''Xenorophus ''Xenorophus'' is a genus of primitive odontocete from late Oligocene ( Chattian) marine deposits in South Carolina belonging to Xenorophidae. Classification ''Xenorophus'' was originally described on the basis of a skull from the Chandler Bri ...'', '' Cotylocara'', '' Echovenator'', and '' Inermorostrum''.. References Prehistoric toothed whales Prehistoric mammal families Oligocene cetaceans {{paleo-whale-stub ...
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Archaeodelphis
''Archaeodelphis'' is an extinct genus of primitive odontocete cetacean from late Oligocene ( Chattian) marine deposits in South Carolina, and belonging to the family Xenorophidae Xenorophidae is an extinct family of odontocetes currently known from the Oligocene of the southeastern US. Known genera of xenorophids include '' Albertocetus'', '' Archaeodelphis'', ''Xenorophus ''Xenorophus'' is a genus of primitive odonto .... Description ''Archaeodelphis'' has polydont teeth, like other xenorophids.G. M. Allen. 1921. A new fossil cetacean. Bulletin of the Museum of Comparative Zoology 65(1):1-14. References Oligocene cetaceans Fossil taxa described in 1921 {{paleo-whale-stub ...
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Edward Drinker Cope
Edward Drinker Cope (July 28, 1840 – April 12, 1897) was an American zoologist, paleontologist, comparative anatomist, herpetologist, and ichthyologist. Born to a wealthy Quaker family, Cope distinguished himself as a child prodigy interested in science; he published his first scientific paper at the age of 19. Though his father tried to raise Cope as a gentleman farmer, he eventually acquiesced to his son's scientific aspirations. Cope married his cousin and had one child; the family moved from Philadelphia to Haddonfield, New Jersey, although Cope would maintain a residence and museum in Philadelphia in his later years. Cope had little formal scientific training, and he eschewed a teaching position for field work. He made regular trips to the American West, prospecting in the 1870s and 1880s, often as a member of United States Geological Survey teams. A personal feud between Cope and paleontologist Othniel Charles Marsh led to a period of intense fossil-finding competition ...
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