Ischyrocyon
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Ischyrocyon
''Ischyrocyon'' is an extinct genus of bear dogs, of the subfamily Amphicyoninae, which inhabited North America during the Late Miocene. It lived ~13.6—10.3 Ma ago, existing for approximately . Behavior In a study published in 2020, examination of the relative grinding area of the molars of ''Ischyrocyon'' indicated that it was purely carnivorous, and not omnivorous as previously assumed. Both ''Ischyrocyon'' and its relative, ''Amphicyon'' possessed skeletal features that are characteristic of both ambush and pursuit living predators. As such, it is believed via this evidence that ''Ischyrocyon'' probably pursued prey for longer distances but at slower speeds than living ambush predators do. Upon catching up to its prey, ''Ischyrocyon'' probably grabbed its victims using its powerfully muscled forelimbs before killing them by tearing into the prey's ribcage or neck using its large, strong canines set in its narrow snout. Fossil distribution * Blair Junction, Esmeralda Coun ...
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Amphicyon
''Amphicyon'' ("ambiguous dog") is an extinct genus of large carnivorous bone-crushing mammals, popularly known as bear dogs, of the family Amphicyonidae, subfamily Amphicyoninae, from the Burdigalian Epoch until the late Pliocene, with the creature having bear-like and dog-like features. They ranged over North America, Europe, Asia, and Africa from 16.9 to 2.6 Ma ago, existing for approximately . Morphology ''Amphicyon'' was the typical bear-dog amphicyonid with morphology similar to both bears and dogs. With its robust build and maximum length of 2.5 m (8 ft), the largest species looked more like a bear than a dog. It had a large heavy tail, thick neck, robust limbs and teeth like a wolf. It was probably an omnivore with a lifestyle comparable to that of the brown bear. The ''Amphicyon'' was very large for predators of its time but this advantage eventually became a disadvantage because its large body mass was too large to take faster prey. ''A. major'' has been est ...
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Bear Dog
Amphicyonidae is an extinct family of terrestrial carnivorans belonging to the suborder Caniformia. They first appeared in North America in the middle Eocene (around 45 mya), spread to Europe by the late Eocene (35 mya), and appear in Asia, and Africa by the early Miocene (23 mya). They had largely disappeared worldwide by the late Miocene (8 mya), with the latest recorded species at the end of the Miocene in Pakistan. They were among the first carnivorans to evolve large body size. Later in their history, they came into competition with hesperocyonine and borophagine canids. As dogs evolved similar body sizes and cranial and dental adaptations, the rise of these groups may have led to their extinction. Amphicyonids are often colloquially referred to as "bear-dogs". Taxonomy The family was erected by Haeckel (1886) lso attributed to Trouessart (1885) Their exact position has long been disputed. Some early paleontologists defined them as members of the family Canidae, but ...
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Amphicyoninae
Amphicyoninae is a subfamily of extinct bear-dogs, large terrestrial carnivores belonging to the suborder Caniformia and which inhabited North America, Eurasia, and Africa from ~37.2—2.6  Ma. Amphicyoninae existed for approximately ~. Amphicyoninae was named by Trouessart (1885). It was assigned to Canidae by Matthew (1902); to Ursidae by Ginsburg (1977); and to Amphicyonidae by Hunt (1998). Genera include: *''Agnotherium'', found in both Europe and N. Africa *''Amphicyon'', found in both Europe and N. America *''Cynelos'', synonyms include ''Absonodaphoenus'' (from Florida) and ''Hecubides'' (from Africa), endemic to N. America *'' Cynodictis'' *''Ischyrocyon'', ''Hadrocyon'' is a synonym, endemic to N. America *''Goupilictis'' *''Magericyon'' *''Pliocyon'', endemic to N. America *''Pseudocyon'', ''Amphicyonopsis'' is a synonym, endemic to Europe and N. America *''Ysengrinia'', found in both Europe and N. America Fossil distribution Specimens have been recovered from: ...
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Bear Dogs
Amphicyonidae is an extinct Family (biology), family of Terrestrial animal, terrestrial carnivorans belonging to the suborder Caniformia. They first appeared in North America in the middle Eocene (around 45 mya), spread to Europe by the late Eocene (35 mya), and appear in Asia, and Africa by the early Miocene (23 mya). They had largely disappeared worldwide by the late Miocene (8 mya), with the latest recorded species at the end of the Miocene in Pakistan. They were among the first carnivorans to evolve large body size. Later in their history, they came into competition with Hesperocyoninae, hesperocyonine and Borophaginae, borophagine Canidae, canids. As dogs evolved similar body sizes and cranial and dental adaptations, the rise of these groups may have led to their extinction. Amphicyonids are often colloquially referred to as "bear-dogs". Taxonomy The family was erected by Haeckel (1886) [also attributed to Trouessart (1885)]. Their exact position has long been disputed. So ...
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Ash Hollow Formation
The Ash Hollow Formation of the Ogallala Group is a geological formation found in Nebraska and South Dakota. It preserves fossils dating back to the Neogene period. It was named after Ash Hollow, Nebraska and can be seen in Ash Hollow State Historical Park. Ashfall Fossil Beds State Historical Park is within this formation. Fossil content Mammals Bats Carnivorans Eulipotyphlans Lagomorphs Rodents Ungulates Proboscideans Reptiles Birds Crocodilians Squamates Testudines Amphibians Plants See also * List of fossiliferous stratigraphic units in South Dakota * Paleontology in South Dakota * List of fossiliferous stratigraphic units in Nebraska * Paleontology in Nebraska The location of the state of Nebraska Paleontology in Nebraska refers to paleontological research occurring within or conducted by people from the U.S. state of Nebraska. Nebraska is world-famous as a source of fossils. During the early Paleozoic ... References * Neogene Unite ...
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Dove Spring Formation
The Dove Spring Formation (formerly the Ricardo Formation) is a geologic formation in the western Mojave Desert of California. It preserves fossils dating back to the Miocene epoch of the Neogene period. Fossil content Mammals Bats Carnivorans Eulipotyphlans Lagomorphs Proboscideans Rodents Ungulates Reptiles Birds Squamates Testudines Amphibians Fish Plants See also * List of fossiliferous stratigraphic units in California * Paleontology in California Paleontology in California refers to paleontologist research occurring within or conducted by people from the U.S. state of California. California contains rocks of almost every age from the Precambrian to the Recent. Precambrian fossils are pres ... References * Neogene California {{Neogene-stub ...
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Goliad Formation
The Goliad Formation (Tg)Page et al., 2005, p.5 is a geologic formation in Texas. It preserves fossils dating back to the Serravallian to earliest Pliocene stages (Clarendonian, Hemphillian and earliest Blancan in the NALMA classification) of the Neogene period,Goliad Formation
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including the '''' among many other fossil mammals, reptiles, birds and ...
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Iron Canyon Site
The Iron Canyon Site is a Miocene assemblage of vertebrate fossils located in Kern County, California within the Dove Spring Formation The Dove Spring Formation (formerly the Ricardo Formation) is a Formation (geology), geologic formation in the western Mojave Desert of California. It preserves fossils dating back to the Miocene epoch of the Neogene Period (geology), period. Fos ... dating from ~23.03—5.33 Ma. Specimens located Proboscidea (Gomphotheriidae) *Gomphotherium Rhinocerotidae *Peraceras *Serbelodon ''S. burnhami'' Equidae *Dinohippus *Pliohippus ''P. tantalus'' *Megahippus ''M. matthewi'' Amphicyonidae *Ischyrocyon ''I. mohavensis'' Canidae *Epicyon E. saevus Artiodactyla *Alluvisorex ''A. chasseae'' *Paracosoryx ''P. furlongi'' *Merychyus Lipotyphla *Limnoecus *Erinaceidae Lagomorpha *Hesperolagomys Rodentia *Thomomys *Cupidinimus ''C. avawatzensis, C. tertius'' *Perognathus P. minutus *Geomyidae *Eucastor *Copemys ''C. dentalis, C. longidens, C. russelli'' Re ...
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Barstovian
The Barstovian North American Stage on the geologic timescale is the North American faunal stage according to the North American Land Mammal Ages chronology (NALMA), typically set from 16,300,000 to 13,600,000 years BP, a period of . It is usually considered to overlap the Langhian and Serravallian stages of the Middle Miocene. The Barstovian is preceded by the Hemingfordian and followed by the Clarendonian NALMA stages. The Barstovian can be further divided into the substages of: * late Late Barstovian: Lower boundary source of the base of the Langhian (approximate) * early Late Barstovian: Base of the Langhian (approximate) * early/lower Barstovian: Upper boundary source: base of Clarendonian (approximate) Correlations The Barstovian (15.97 to 13.6 Ma) correlates with: * SALMA ** Colloncuran (15.5-13.8 Ma)
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Snake Creek Formation
The Snake Creek Formation is a geologic formation in Nebraska. It preserves fossils dating back to the Neogene period. See also * List of fossiliferous stratigraphic units in Nebraska * Paleontology in Nebraska The location of the state of Nebraska Paleontology in Nebraska refers to paleontological research occurring within or conducted by people from the U.S. state of Nebraska. Nebraska is world-famous as a source of fossils. During the early Paleozoic ... References * Neogene geology of Nebraska {{Neogene-stub ...
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Miocene Mammals Of North America
The Miocene ( ) is the first geological epoch of the Neogene The Neogene ( ), informally Upper Tertiary or Late Tertiary, is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period million years ago ( Mya) to the beginning of the present Quaternary Period Mya. ... 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, t ...
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Miocene Bear Dogs
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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