Information about Creodonta
| Creodonta Fossil range: Paleocene - Pliocene | ||||||||||||
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Hyaenodontidae Oxyaenidae | ||||||||||||
Creodonts were an important group of carnivorous mammals from 55 to 35 million years ago in the ecosystems of Africa, Eurasia and North America. In Oligocene Africa, they were the dominant predatory group. They competed with the Mesonychids, and the Entelodonts and ultimately outlasted them by the start of the Oligocene and by the middle of the Miocene, respectively, but the Creodonts lost ground to the Carnivorans. The last genus went extinct 8 MYA, and carnivorans now occupy their ecological niches.
Evolution and Taxonomy
Creodonts were previously considered ancestral to the carnivores, Carnivora, but are now considered to have shared a common ancestor further back. They share with the Carnivora the carnassial shear, scissor teeth that evolved to slice meat and gave both orders the tools to dominate the niche. Some researchers argue that the creodonts represent a group of mammals of diverse biological ancestry that resemble one another via convergent evolution, rather than being the descendants of a single common ancestor. Their origins lie at least as far back as the late Cretaceous, though they did not radiate much until the Cenozoic.[1] Creodonts were the dominant carnivorous mammals from 55 to 35 MYA, peaking in diversity and prevalence during the Eocene.[2] By the mid Oligocene, the Creodonts supplanted both the Mesonychids, and giant flightless predatory birds entirely in North America, Eurasia and Africa, and in turn, competed with their relatives, the true carnivores until the last creodont genus, Dissopsalis, went extinct about 8 million years ago.Habitat
The creodonts ranged across North America, Eurasia and Africa, in forms that resemble those of modern carnivores. Amongst their number was Megistotherium, which some argue was the largest mammalian land predator of all time, the size of a bison and with a skull twice as big as a tiger's. Megistotherium may have rivaled Andrewsarchus mongoliensis in size. Their dominance over the early Carnivora, known as miacids, began to wane after 35 MYA. The creodonts survived until 8 million years ago; the last form, Dissopsalis, died out in Pakistan. Bears, cats, mustelids, hyenas, canids such as wolves and other Carnivora now occupy the former creodont niches.Why did creodonts become extinct?
It is not known exactly why the Creodonts were replaced by Carnivora. The Creodonts' smaller brains and somewhat less energy-efficient (especially while running) mostly plantigrade locomotion may have given the Carnivora a subtle advantage that over millions of years allowed them to take over. The Creodont lumbosacral spine was not arranged as efficiently for running as in Carnivora. In addition, the arrangement of the teeth was somewhat different. In the miacids (and thus in the modern Carnivora), the last upper premolar and the first lower molar are the carnassials, allowing grinding teeth to be retained behind for feeding on non-meat foods (the Canidae are the closest modern analog to miacid dentition). In creodonts, the carnassials were further back - either first upper and second lower molars, or second upper and third lower molars. This committed them to eating meat almost exclusively.Note that in the Felidae, the most strictly carnivorous of modern Carnivora, the second and third molars have disappeared completely, and the first upper molars behind the carnassials have become vestigial. Modern cats thus eat plant food only incidentally.
References
- The Velvet Claw: A Natural History of the Carnivores, David Macdonald, BBC Books, ISBN 0-563-20844-9
- David Lambert and the Diagram Group. The Field Guide to Prehistoric Life. New York: Facts on File Publications, 1985. ISBN 0-8160-1125-7
Footnotes
The Paleocene, "early dawn of the recent", is a geologic epoch that lasted from 65.5 ± 0.3 Ma to 55.8 ± 0.2 Ma (million years ago). It is the first epoch of the Palaeogene Period in the modern Cenozoic era.
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The Pliocene epoch (spelled Pleiocene in some older texts) is the period in the geologic timescale that extends from 5.332 million to 1.806 million years before present.
The Pliocene is the second epoch of the Neogene period in the Cenozoic era.
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The Pliocene is the second epoch of the Neogene period in the Cenozoic era.
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Hyaenodon
Leidy, 1869
Species [1]
H. bavaricus
H. brevirostris
H. chunkhtensis
H. crucians
H. eminus
H. exicuus
H. gigas
H. horridus
H.
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Leidy, 1869
Species [1]
H. bavaricus
H. brevirostris
H. chunkhtensis
H. crucians
H. eminus
H. exicuus
H. gigas
H. horridus
H.
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Scientific classification or biological classification is a method by which biologists group and categorize species of organisms. Scientific classification also can be called scientific taxonomy, but should be distinguished from folk taxonomy, which lacks scientific basis.
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Chordata
Bateson, 1885
Typical Classes
See below
Chordates (phylum Chordata) are a group of animals that includes the vertebrates, together with several closely related invertebrates.
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Bateson, 1885
Typical Classes
See below
Chordates (phylum Chordata) are a group of animals that includes the vertebrates, together with several closely related invertebrates.
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Mammalia
Linnaeus, 1758
Subclasses & Infraclasses
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Linnaeus, 1758
Subclasses & Infraclasses
- Subclass †Allotheria*
- Subclass Prototheria
- Subclass Theria
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Eutheria
Orders[1]
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Orders[1]
- Bobolestes
- Eomaia
- Maelestes
- Montanalestes
- Murtoilestes
- Prokennalestes
- Placentalia
- Superorder
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Laurasiatheria
Orders
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Orders
- Erinaceomorpha
- Soricomorpha
- Chiroptera
- Cetartiodactyla
- Cetacea
- Artiodactyla
- Perissodactyla
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Edward Drinker Cope (July 28, 1840–April 12, 1897) was an American paleontologist and comparative anatomist, as well as a noted herpetologist and ichthyologist.
Cope was born in Philadelphia to Quaker parents.
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Cope was born in Philadelphia to Quaker parents.
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family (Latin: familia, plural familiae) is a rank, or a taxon in that rank. Exact details of formal nomenclature depend on the Nomenclature Code which applies.
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Hyaenodontidae
Genera
See text
Hyaenodontidae ("Hyena teeth") is a family of the extinct order Creodonta, which contains several dozen genera.
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Genera
See text
Hyaenodontidae ("Hyena teeth") is a family of the extinct order Creodonta, which contains several dozen genera.
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Oxyaenidae
Subfamilies
Ambloctoninae
Oxyaeninae
Tytthaeninae
?Machaeroidinae
Oxyaenidae is a family of the extinct order Creodonta; it contains three subfamilies comprising ten genera.
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Subfamilies
Ambloctoninae
Oxyaeninae
Tytthaeninae
?Machaeroidinae
Oxyaenidae is a family of the extinct order Creodonta; it contains three subfamilies comprising ten genera.
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extinction is the cessation of existence of a species or group of taxa, reducing biodiversity. The moment of extinction is generally considered to be the death of the last individual of that species (although the capacity to breed and recover may have been lost before this point).
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order (Latin: ordo, plural ordines) is a rank between class and family (termed a taxon at that rank). The superorder is a rank between class and order. Exact details of formal nomenclature depend on the Nomenclature Code which applies.
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Mammalia
Linnaeus, 1758
Subclasses & Infraclasses
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Linnaeus, 1758
Subclasses & Infraclasses
- Subclass †Allotheria*
- Subclass Prototheria
- Subclass Theria
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The Paleocene, "early dawn of the recent", is a geologic epoch that lasted from 65.5 ± 0.3 Ma to 55.8 ± 0.2 Ma (million years ago). It is the first epoch of the Palaeogene Period in the modern Cenozoic era.
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The Pliocene epoch (spelled Pleiocene in some older texts) is the period in the geologic timescale that extends from 5.332 million to 1.806 million years before present.
The Pliocene is the second epoch of the Neogene period in the Cenozoic era.
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The Pliocene is the second epoch of the Neogene period in the Cenozoic era.
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Carnivora
Bowdich, 1821
Families
The diverse order Carnivora (IPA: /kɑrˈnɪvərə/
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Bowdich, 1821
Families
- 17, See classification
The diverse order Carnivora (IPA: /kɑrˈnɪvərə/
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Africa is the world's second-largest and second most-populous continent, after Asia. At about 30,221,532 km² (11,668,545 sq mi) including adjacent islands, it covers 6% of the Earth's total surface area, and 20.4% of the total land area.
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Eurasia is an immense landmass covering about 53,990,000 km² (or about 10.6%) of the Earth's surface. Often reckoned as a single continent, Eurasia comprises the traditional continents of Europe and Asia, concepts which date back to classical antiquity and the borders for which are
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North America is a continent [1] in the Earth's northern hemisphere and (chiefly) western hemisphere. It is bordered on the north by the Arctic Ocean, on the east by the North Atlantic Ocean, on the southeast by the Caribbean Sea, and on the south and west
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The Oligocene epoch is a geologic period that extends from about 33.9 million to 23 million years before the present. As with other older geologic periods, the rock beds that define the period are well identified but the exact dates of the start and end of the period are slightly
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Mesonychia
Families
Hapalodectidae
Mesonychidae
Triisodontidae
Mesonychia ("Middle Claws") are an extinct order of medium to large-sized carnivorous mammals that were closely related to artiodactyls (even-toed ungulates), and to cetaceans
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Families
Hapalodectidae
Mesonychidae
Triisodontidae
Mesonychia ("Middle Claws") are an extinct order of medium to large-sized carnivorous mammals that were closely related to artiodactyls (even-toed ungulates), and to cetaceans
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Entelodontidae
Lydekker, 1883
Genera
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Lydekker, 1883
Genera
- Archaeotherium
- Brachyhyops
- Cypretherium
- Daeodon
- Entelodon
- Eoentelodon
- Paraentelodon
- Elotheridae
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The Miocene Epoch is a period of time that extends from about 23.03 to 5.332 million years before the present. As with other older geologic periods, the rock beds that define the start and end are well identified but the exact dates of the start and end of the period are uncertain.
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Carnivora
Bowdich, 1821
Families
The diverse order Carnivora (IPA: /kɑrˈnɪvərə/
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Bowdich, 1821
Families
- 17, See classification
The diverse order Carnivora (IPA: /kɑrˈnɪvərə/
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Carnivora
Bowdich, 1821
Families
The diverse order Carnivora (IPA: /kɑrˈnɪvərə/
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Bowdich, 1821
Families
- 17, See classification
The diverse order Carnivora (IPA: /kɑrˈnɪvərə/
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Carnassials are large teeth found in many carnivorous mammals, used for shearing flesh and bone in a scissor-like way. In the Carnivora, the carnassials are the modified last upper premolar and the first lower molar, but in the prehistoric creodonts, the carnassials were further
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niche (pronounced nich, neesh or nish)[] is a term describing the relational position of a species or population in its ecosystem[1]. The ecological niche describes how an organism or population responds to the distribution of resources and competitors (e. g.
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