Chlamydoselachus Bracheri
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Chlamydoselachus Bracheri
''Rolfodon bracheri'' is an extinct species from the family Chlamydoselachidae. It lived during the Miocene. ''R. bracheri'' was named by Pfeil in 1983. Originally it was described as a species belonging to the genus ''Chlamydoselachus ''Chlamydoselachus'' is a genus of sharks and the sole extant member of the family (biology), family Chlamydoselachidae, in the order (biology), order Hexanchiformes. It contains two extant and several extinct species. The most widely known speci ...''; Cappetta, Morrison & Adnet (2019) transferred it to the chlamydoselachid genus ''Rolfodon''. References Chlamydoselachidae Miocene fish Fish described in 1983 {{paleo-shark-stub ...
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Miocene
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the ...
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Chlamydoselachus
''Chlamydoselachus'' is a genus of sharks and the sole extant member of the family (biology), family Chlamydoselachidae, in the order (biology), order Hexanchiformes. It contains two extant and several extinct species. The most widely known species still surviving is the frilled shark (''Chlamydoselachus anguineus''). It is known as a living fossil, along with ''Chlamydoselachus africana'', also known as the southern African frilled shark, which is only found along coastal areas of South Africa. The only two extant species of this genus are deep-sea creatures which are typically weakened in areas closer to the surface. Species * ''Southern African frilled shark, Chlamydoselachus africana'' David A. Ebert, Ebert & Leonard Compagno, Compagno, 2009 (southern African frilled shark) * ''Frilled shark, Chlamydoselachus anguineus'' Samuel Garman, Garman, 1884 (frilled shark) * †''Chlamydoselachus bracheri'' Pfeil, 1983 * †''Chlamydoselachus fiedleri'' Pfeil, 1983 * †''Chlamydosela ...
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Chlamydoselachidae
''Chlamydoselachus'' is a genus of sharks and the sole extant member of the family Chlamydoselachidae, in the order Hexanchiformes. It contains two extant and several extinct species. The most widely known species still surviving is the frilled shark (''Chlamydoselachus anguineus''). It is known as a living fossil, along with ''Chlamydoselachus africana'', also known as the southern African frilled shark, which is only found along coastal areas of South Africa. The only two extant species of this genus are deep-sea creatures which are typically weakened in areas closer to the surface. Species * '' Chlamydoselachus africana'' Ebert & Compagno, 2009 (southern African frilled shark) * '' Chlamydoselachus anguineus'' Garman, 1884 (frilled shark) * †'' Chlamydoselachus bracheri'' Pfeil, 1983 * †'' Chlamydoselachus fiedleri'' Pfeil, 1983 * †'' Chlamydoselachus garmani'' Welton, 1983 * †''Chlamydoselachus goliath ''Rolfodon goliath'' is an extinct species of large frilled ...
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Miocene Fish
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the late ...
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