(paleontology) The single order of the nominally mammalian suborder Allotheria; multituberculates had enlarged incisors, the coracoid bones were fused to the scapula, and the lower jaw consisted of the dentary bone alone.
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(paleontology) The single order of the nominally mammalian suborder Allotheria; multituberculates had enlarged incisors, the coracoid bones were fused to the scapula, and the lower jaw consisted of the dentary bone alone.
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An order in the class Mammalia, subclass Allotheria, comprising a major group of early mammals, ranging from Late Jurassic to Late Eocene (about 155 to 35 million years ago). The group is best known from North America, Mongolia, and Europe. Most multituberculates were mouselike in size, although the North American Paleocene Taeniolabis was larger, probably closer to the woodchuck (Marmota monax) in its proportions. Multituberculates appear primarily to have been terrestrial creatures, but some were probably arboreal and others fossorial. The Eocene decline and extinction of multituberculates may reflect competition from small placental mammals, especially primates and rodents. See also Archaic ungulate; Rodentia.
The most primitive multituberculates are traditionally classified in the suborder Plagiaulacoidea (Late Jurassic to Early Cretaceous), and the advanced multituberculates are traditionally classified in the suborders Ptilodontoidea and Taeniolabidoidea (both Late Cretaceous to Eocene).
Although clearly mammalian and often characterized as rodentlike, multituberculates are unlike rodents or other living mammals in several important features. The dentition is distinctive and, with associated jaw fragments, it is all that is known for most species. Microscopic wear patterns on multituberculate tooth enamel show that jaw motion differed radically from that in other mammals: during chewing, the mandible moved only in the vertical plane, not transversely, and was strongly retracted during the power stroke. These studies also imply that most multituberculates were probably omnivores, although species having gnawing incisors were likely specialized herbivores feeding on tough plant tissues. See also
Attempts to determine multituberculate relationships to other mammals have long been inconclusive. See also Allotheria; Mammalia.
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| Multituberculates Fossil range: Middle Jurassic-Oligocene, 160–35 Ma |
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| Skull of Ptilodus | |
| Scientific classification | |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Mammalia |
| Subclass: | Allotheria |
| Order: | †Multituberculata Cope, 1884 |
| Suborders | |
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The Multituberculata (multituberculates) are a major branch of mammals that survived for a long period of time but eventually became completely extinct at the end of the Paleogene period.
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They lived for over 100 million years, and are often considered the most successful mammals in natural history[citation needed]. Rodent-like, they first appeared in the middle Jurassic 160 million years ago, survived the mass extinction in the Cretaceous, and became extinct in the early Oligocene epoch, 35 million years ago.
With the possible exception of some poorly preserved South American material, multituberculates are only known from the northern hemisphere. A southern grouping, Gondwanatheria, has in the past been referred to the order, though this placement currently has little support.
In the late Cretaceous multituberculates were widespread and diverse in the northern hemisphere, making up more than half of the mammal species of typical faunas. Although some lineages became extinct during the faunal turnover at the end of the Cretaceous, multituberculates managed very successfully to cross the K/T boundary and reached their peak of diversity during the Paleocene. They were an important component of nearly all Paleocene faunas of Europe and North America, and of some late Paleocene faunas of Asia. Multituberculates also were most diverse in size during the Paleocene, ranging from the size of a very small mouse to that of a beaver.
The structure of the pelvis in the Multituberculata suggests that they gave birth to tiny helpless young, similar to modern marsupials. They are named for their molar teeth, which had many cusps (tubercles) arranged in rows, hence "multituberculates". They also had a single pair of lower incisors and no canines, reminiscent of modern rodents. The multituberculates were also the first mammals to live in trees like the modern squirrel[citation needed]. In the northern hemisphere during the late Cretaceous, more than half of typical land mammalian species were multituberculates.
About 80 genera of Multituberculata are known, including Lambdopsalis, Ptilodus and Meniscoessus.
In their 2001 study, Kielan-Jaworowska and Hurum found that most multituberculates could be referred to two suborders: Plagiaulacida and Cimolodonta. The exception is the genus Arginbaatar, which shares characteristics with both groups.
"Plagiaulacida" is paraphyletic; it is an informal suborder which does not satisfy the cladistic criterion of consisting of an ancestor and all of its descendants. Its members are the more basal Multituberculata. Chronologically, they ranged from perhaps the middle Jurassic (unnamed material), until the lower Cretaceous. This group is further subdivided into three informal groupings: the Allodontid line, the Paulchoffatiid line, and the Plagiaulacid line.
Cimolodonta is apparently a natural (monophyletic) suborder. This includes the more derived Multituberculata, which have been identified from the lower Cretaceous to the Eocene. Recognized are the superfamilies Djadochtatherioidea, Taeniolabidoidea, Ptilodontoidea and the Paracimexomys group.
Additionally, there are the families Cimolomyidae, Boffiidae, Eucosmodontidae, Kogaionidae, Microcosmodontidae and the two genera Uzbekbaatar and Viridomys. More precise placement of these types awaits further discoveries and analysis.
This entry is from Wikipedia, the leading user-contributed encyclopedia. It may not have been reviewed by professional editors (see full disclaimer)
| Ptilodontoidea (paleontology) | |
| Taeniolabidoidea (paleontology) | |
| Allotheria (mammalia) |
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