Superregnum: Eukaryota
Cladus: Unikonta
Cladus: Opisthokonta
Cladus: Holozoa
Regnum: Animalia
Subregnum: Eumetazoa
Cladus: Bilateria
Cladus: Nephrozoa
Superphylum: Deuterostomia
Phylum: Chordata
Subphylum: Vertebrata
Infraphylum: Gnathostomata
Megaclassis: Osteichthyes
Cladus: Sarcopterygii
Cladus: Rhipidistia
Cladus: Tetrapodomorpha
Cladus: Eotetrapodiformes
Cladus: Elpistostegalia
Superclassis: Tetrapoda
Cladus: Reptiliomorpha
Cladus: Amniota
Cladus: Synapsida
Cladus: Eupelycosauria
Cladus: Sphenacodontia
Cladus: Sphenacodontoidea
Cladus: Therapsida
Cladus: Theriodontia
Cladus: Cynodontia
Cladus: Eucynodontia
Cladus: Probainognathia
Cladus: Prozostrodontia
Cladus: Mammaliaformes
Classis: Mammalia
Subclassis: Trechnotheria
Infraclassis: †Allotheria
Subordines: †Cimolodonta – †Plagiaulacida
Name
Multituberculata Cope, 1884: 687
References
Primary references
Cope, E.D. 1884. The Tertiary Marsupialia. The American Naturalist 18(7): 686–697. DOI: 10.1086/273711 Open access BHL Reference page.
Additional references
McKenna, M.C. & Bell, S.K. (eds.). 1997. Classification of mammals: above the species level. Columbia University Press: New York. xii + 631 pp. ISBN 978-0-231-11012-9. Google Books Reference page.
Vernacular names
català: Multituberculats
English: Multituberculates
español: Multituberculados
français: Multituberculés
italiano: Multitubercolati
日本語: 多丘歯目
polski: Wieloguzkowce
русский: Многобугорчатые
українська: Багатогорбкозубі
Multituberculata (commonly known as multituberculates, named for the multiple tubercles of their teeth) is an extinct order of rodent-like mammals with a fossil record spanning over 130 million years.[citation needed] They first appeared in the Middle Jurassic, and reached a peak diversity during the Late Cretaceous and Paleocene. They eventually declined from the mid-Paleocene onwards, disappearing from the known fossil record in the late Eocene.[1] They are the most diverse order of Mesozoic mammals with more than 200 species known, ranging from mouse-sized to beaver-sized. These species occupied a diversity of ecological niches, ranging from burrow-dwelling to squirrel-like arborealism to jerboa-like hoppers.[2][3] Multituberculates are usually placed as crown mammals outside either of the two main groups of living mammals—Theria, including placentals and marsupials, and Monotremata[4]—but usually as closer to Theria than to monotremes.[5][6] They are considered to be closely related to Euharamiyida and Gondwanatheria as part of Allotheria.
Description
Restoration of Taeniolabis, the largest multituberculate at approximately 22 kg (49 lb).
The multituberculates had a cranial and dental anatomy superficially similar to rodents such as mice and rats, with cheek-teeth separated from the chisel-like front teeth by a wide tooth-less gap (the diasteme). Each cheek-tooth displayed several rows of small cusps (or tubercles, hence the name) that operated against similar rows in the teeth of the jaw; the exact homology of these cusps to therian ones is still a matter of debate.[citation needed] Unlike rodents, which have ever-growing teeth, multituberculates underwent dental replacement patterns typical of most mammals (though in at least some species the lower incisors continued to erupt long after the root's closure).[7] Multituberculates are notable for the presence of a massive fourth lower premolar, the plagiaulacoid; other mammals, like Plesiadapiformes and diprotodontian marsupials, also have similar premolars in both upper and lower jaws, but in multituberculates this tooth is massive and the upper premolars are not modified this way. In basal multituberculates all three lower premolars were plagiaulacoids, increasing in size posteriorly, but in Cimolodonta only the fourth lower premolar remained, with the third one remaining only as a vestigial peg-like tooth,[7] and in several taxa like taeniolabidoideans, the plagiaulacoid disappeared entirely or was reconverted into a molariform tooth.[8][9][10]
Skull of Ptilodus. Notice the massive blade-like lower premolar.
Unlike rodents and similar therians, multituberculates had a palinal jaw stroke (front-to-back), instead of a propalinal (back-to-front) or transverse (side-to-side) one; as a consequence, their jaw musculature and cusp orientation is radically different.[4][7] Palinal jaw strokes are almost entirely absent in modern mammals (with the possible exception of the dugong[11]), but are also present in haramiyidans, argyrolagoideans and tritylodontids, the former historically united with multituberculates on that basis. Multituberculate mastication is thought to have operated in a two stroke cycle: first, food held in place by the last upper premolar was sliced by the bladelike lower pre-molars as the dentary moved orthally (upward). Then the lower jaw moved palinally, grinding the food between the molar cusp rows.[4][7]
Lower jaws and teeth of allodontid multituberculates
The structure of the pelvis in the Multituberculata suggests that they gave birth to tiny helpless, underdeveloped young, similar to modern marsupials, such as kangaroos.[2][7] However, a 2022 study reveals that they might actually have had long gestation periods like placentals.[12]However, in 2024, all Allotheria (including multituberculates) fell outside the crown group of Mammalia, implying that cimolodonts developed placental-like gestation (and viviparity in general) independently, rather than multituberculates and therians having a common viviparous ancestor.[13]
At least two lineages developed hypsodonty, in which tooth enamel extends beyond the gumline: lambdopsalid taeniolabidoideans[14] and sudamericid gondwanatheres.[15]
Studies published in 2018 demonstrated that multituberculates had relatively complex brains, some braincase regions even absent in therian mammals.[16]
Evolution
Multituberculates first appear in the fossil record during the Jurassic period, and then survived and even dominated for over one hundred million years, longer than any other order of mammaliforms, including placental mammals. The earliest known multituberculates are from the Middle Jurassic (Bathonian ~166-168 million years ago) of England and Russia, including Hahnotherium and Kermackodon from the Forest Marble Formation of England, and Tashtykia and Tagaria from the Itat Formation of Russia. These forms are only known from isolated teeth, which bear close similarity to those of euharamyidans, which they are suspected to be closely related.[17] During the Late Jurassic and Early Cretaceous, primitive multituberculates, collectively grouped into the paraphyletic "Plagiaulacida" were abundant and widespread across Laurasia (including Europe, Asia and North America). During the Aptian stage of the Early Cretaceous, the advanced subgroup Cimolodonta appeared in North America, characterised by a reduced number of lower premolars, with a blade-like lower fourth premolar. By the early Late Cretaceous (Cenomanian) Cimolodonta had replaced all other multituberculate lineages.[18]
During the Late Cretaceous, multituberculates experienced an adaptive radiation, corresponding with a shift towards herbivory.[19] Multituberculates reached their peak diversity during the early Paleocene, shortly after the Cretaceous–Paleogene extinction event, but declined from the mid Paleocene onwards, likely due to competition with placental mammals such as rodents and ungulates, the group finally became extinct in the Late Eocene.[20][21] There are some isolated records of multituberculates from the Southern Hemisphere, including the cimolodontan Corriebaatar from the Early Cretaceous of Australia,[22] and fragmentary remains from the Late Cretaceous Maevarano Formation of Madagascar.[23] The family Ferugliotheriidae from the Late Cretaceous of South America, traditionally considered gondwanatherians, may actually be cimolodontan multituberculates.[22]
During the Late Cretaceous and Paleocene the multituberculates radiated into a wide variety of morphotypes, including the squirrel-like arboreal ptilodonts. The peculiar shape of their last lower premolar is their most outstanding feature. These teeth were larger and more elongated than the other cheek-teeth and had an occlusive surface forming a serrated slicing blade. Though it can be assumed that this was used for crushing seeds and nuts, it is believed that most small multituberculates also supplemented their diet with insects, worms, and fruits.[4] Tooth marks attributed to multituberculates are known on Champsosaurus fossils, indicating that at least some of these mammals were scavengers.[24] A ptilodont that thrived in North America was Ptilodus. Thanks to the well-preserved Ptilodus specimens found in the Bighorn Basin, Wyoming, we know that these multituberculates were able to abduct and adduct their big toes, and thus that their foot mobility was similar to that of modern squirrels, which descend trees head first.[4]
Restoration of Catopsbaatar
Another group of multituberculates, the taeniolabids, were heavier and more massively built, indicating that they lived a fully terrestrial life. The largest specimens weighed probably as much as 22 kg (49 lb), making them comparable in size to large rodents like the modern beaver.[25][26]
Classification
Multituberculate is generally placed in the Allotheria alongside Euharamiyida, a clade of mammals known from the Middle Jurassic to Early Cretaceous of the Asia and possibly Europe that several morphological similarities to multituberculates.[17][27]
Gondwanatheria is a monophyletic group of allotherians that was diverse in the Late Cretaceous of South America, India, Madagascar and possibly Africa and occurs onwards into the Paleogene of South America and Antarctica. Their placement within Allotheria is highly controversial, with some phylogenies recovering the group as deeply nested within multituberculates, while others recover them as a distinct branch of allotherians separate from multituberculates.[27]
Restoration of Taeniolabis taoensis
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, representing the more primitive evolutionary grade. Its members are the more basal Multituberculata. Chronologically, they ranged from perhaps the Middle Jurassic until the mid-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. The superfamilies Djadochtatherioidea, Taeniolabidoidea, Ptilodontoidea are recognized, as is 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.[28][better source needed]
Taxonomy
Subgroups
Based on the combined works of Mikko's Phylogeny Archive[30] and Paleofile.com.
Suborder †Plagiaulacida Simpson 1925
- Genus ?†Argillomys Cifelli, Gordon & Lipka 2013
- Species †Argillomys marylandensis Cifelli, Gordon & Lipka 2013
- Genus ?†Janumys Eaton & Cifelli 2001
- Species †Janumys erebos Eaton & Cifelli 2001
- Super family †Allodontoidea Marsh 1889
- Genus †?Glirodon Engelmann & Callison, 2001
- Species †G. grandis Engelmann & Callison, 2001
- Family †Arginbaataridae Hahn & Hahn, 1983
- Genus †Arginbaatar Trofimov, 1980
- Species †A. dmitrievae Trofimov, 1980
- Genus †Arginbaatar Trofimov, 1980
- Family †Zofiabaataridae Bakker, 1992
- Genus †Zofiabaatar Bakker & Carpenter, 1990
- Species †Z. pulcher Bakker & Carpenter, 1990
- Genus †Zofiabaatar Bakker & Carpenter, 1990
- Family †Allodontidae Marsh, 1889
- Genus †Passumys Cifelli, Davis & Sames 2014
- Species †Passumys angelli Cifelli, Davis & Sames 2014
- Genus †Ctenacodon Marsh, 1879
- Species †C. serratus Marsh, 1879
- Species †C. nanus Marsh, 1881
- Species †C. laticeps (Marsh, 1881) [Allodon laticeps Marsh 1881]
- Species †C. scindens Simpson, 1928
- Genus †Psalodon Simpson, 1926
- Species †P. potens (Marsh, 1887) [Ctenacodon potens Marsh 1887]
- Species †P. fortis (Marsh, 1887) Simpson 1929 [Allodon fortis Marsh 1887]
- Species †P. marshi Simpson, 1929
- Genus †Passumys Cifelli, Davis & Sames 2014
- Genus †?Glirodon Engelmann & Callison, 2001
- Super family †Paulchoffatioidea Hahn 1969 sensu Hahn & Hahn 2003
- Genus ?†Mojo Hahn, LePage & Wouters 1987
- Species †Mojo usuratus Hahn, LePage & Wouters 1987
- Genus ?†Rugosodon Yuan et al., 2013
- Species †Rugosodon eurasiaticus Yuan et al., 2013
- Family †Pinheirodontidae Hahn & Hahn, 1999
- Genus †Bernardodon Hahn & Hahn, 1999
- Species †B. atlanticus Hahn & Hahn, 1999
- Species †B. sp. Hahn & Hahn, 1999
- Genus †Cantalera Badiola, Canudo & Cuenca-Bescos, 2008
- Species †Cantalera abadi Badiola, Canudo & Cuenca-Bescos, 2008
- Genus †Ecprepaulax Hahn & Hahn, 1999
- Species †E. anomala Hahn & Hahn, 1999
- Genus †Gerhardodon Kielan-Jaworowska & Ensom, 1992
- Species †G. purbeckensis Kielan-Jaworowska & Ensom, 1992
- Genus †Iberodon Hahn & Hahn, 1999
- Species †I. quadrituberculatus Hahn & Hahn, 1999
- Genus †Lavocatia Canudo & Cuenca-Bescós, 1996
- Species †L. alfambrensis Canudo & Cuenca-Bescós, 1996
- Genus †Pinheirodon Hahn & Hahn, 1999
- Species †P. pygmaeus Hahn & Hahn, 1999
- Species †P. vastus Hahn & Hahn, 1999
- Genus †Bernardodon Hahn & Hahn, 1999
- Family †Paulchoffatiidae Hahn, 1969
- Genus ?†Galveodon Hahn & Hahn, 1992
- Species †G. nannothus Hahn & Hahn, 1992
- Genus ?†Sunnyodon Kielan-Jaworowska & Ensom, 1992
- Species †S. notleyi Kielan-Jaworowska & Ensom, 1992
- subfamily †Paulchoffatiinae Hahn, 1971
- Genus †Paulchoffatia Kühne, 1961
- Species †P. delgador Kühne, 1961
- Genus †Pseudobolodon Hahn, 1977
- Species †P. oreas Hahn, 1977
- Species †P. krebsi Hahn & Hahn, 1994
- Genus †Henkelodon Hahn, 1987
- Species †H. naias Hahn, 1987
- Genus †Guimarotodon Hahn, 1969
- Species †G. leiriensis Hahn, 1969
- Genus †Meketibolodon (Hahn, 1978) Hahn, 1993
- Species †M. robustus (Hahn, 1978) Hahn, 1993 [Pseudobolodon robusutus Hahn 1978]
- Genus †Plesiochoffatia Hahn & Hahn, 1999 [Parachoffatia Hahn & Hahn 1998 non Mangold 1970]
- Species †P. thoas (Hahn & Hahn, 1998) Hahn & Hahn 1999 [Parachoffatia thoa Hahn & Hahn 1998]
- Species †P. peparethos (Hahn & Hahn, 1998) Hahn & Hahn 1999 [Parachoffatia peparethos Hahn & Hahn 1998]
- Species †P. staphylos (Hahn & Hahn, 1998) Hahn & Hahn 1999 [Parachoffatia staphylos Hahn & Hahn 1998]
- Genus †Xenachoffatia Hahn & Hahn, 1998
- Species †X. oinopion Hahn & Hahn, 1998
- Genus †Bathmochoffatia Hahn & Hahn, 1998
- Species †B. hapax Hahn & Hahn, 1998
- Genus †Kielanodon Hahn, 1987
- Species †K. hopsoni Hahn, 1987
- Genus †Meketichoffatia Hahn, 1993
- Species †M. krausei Hahn, 1993
- Genus †Renatodon Hahn, 2001
- Species †Renatodon amalthea Hahn, 2001
- Genus †Paulchoffatia Kühne, 1961
- Subfamily †Kuehneodontinae Hahn, 1971
- Genus †Kuehneodon Hahn, 1969
- Species †K. dietrichi Hahn, 1969
- Species †K. barcasensis Hahn & Hahn, 2001
- Species †K. dryas Hahn, 1977
- Species †K. guimarotensis Hahn, 1969
- Species †K. hahni Antunes, 1988
- Species †K. simpsoni Hahn, 1969
- Species †K. uniradiculatus Hahn, 1978
- Genus †Kuehneodon Hahn, 1969
- Genus ?†Galveodon Hahn & Hahn, 1992
- Genus ?†Mojo Hahn, LePage & Wouters 1987
Plagiaulacoidea
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Phylogeny[29]
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Paleoecology
Behaviour
Multituberculates are some of the earliest mammals to display complex social behaviours. One species, Filikomys, from the Late Cretaceous of North America, engaged in multi-generational group nesting and burrowing.[31]
Extinction
The extinction of multituberculates has been a topic of controversy for several decades.[32] After at least 88 million years of dominance over most mammalian assemblies, multituberculates reached the peak of their diversity in the early Palaeocene, before gradually declining across the final stages of the epoch and the Eocene, finally disappearing in the early Oligocene.[33]
The last multituberculate species, Ectypodus childei, went extinct near the end of the Eocene in North America. It is unclear why this particular species persisted for so long when all of its counterparts succumbed to replacement by rodents.[34]: 43
Traditionally, the extinction of multituberculates has been linked to the rise of rodents (and, to a lesser degree, earlier placental competitors like hyopsodonts and Plesiadapiformes), which supposedly competitively excluded multituberculates from most mammalian faunas.[1]
However, the idea that multituberculates were replaced by rodents and other placentals has been criticised by several authors. For one thing, it relies on the assumption that these mammals are "inferior" to more derived placentals, and ignores the fact that rodents and multituberculates had co-existed for at least 15 million years. According to some researchers, multituberculate "decline" is shaped by sharp extinction events, most notably after the Tiffanian, where a sudden drop in diversity occurs. Finally, the youngest known multituberculates do not exemplify patterns of competitive exclusion; the Oligocene Ectypodus is a rather generalistic species, rather than a specialist. This combination of factors suggests that, rather than gradually declining due to pressure from rodents and similar placentals, multituberculates simply could not cope with climatic and vegetation changes, as well as the rise of new predatory eutherians, such as miacids.[33]
More recent studies show a mixed effect. Multituberculate faunas in North America and Europe do indeed decline in correlation to the introduction of rodents in these areas. However, Asian multituberculate faunas co-existed with rodents with minimal extinction events, implying that competition was not the main cause for the extinction of Asiatic multituberculates. As a whole, it seems that Asian multituberculates, unlike North American and European species, never recovered from the KT event, which allowed the evolution and propagation of rodents in the first place.[32] A recent study seems to indeed indicate that eutherians recovered more quickly from the KT event than multituberculates.[35] Conversely, another study has shown that placental radiation did not start significantly until after the decline of multituberculates.[21]
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Sources
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Agustí, Jordi; Antón, Mauricio (2002). Mammoths, Sabertooths, and Hominids: 65 Millions Years of Mammalian Evolution in Europe. New York: Columbia University Press. ISBN 978-0-231-11640-4.
Dykes, Trevor. "Multituberculata (Cope 1884)". Archived from the original on December 28, 2009.
Kielan-Jaworowska, Zofia; Hurum, Jørn H. (2001). "Phylogeny and Systematics of multituberculate mammals" (PDF). Palaeontology. 44 (3): 389–429. Bibcode:2001Palgy..44..389K. doi:10.1111/1475-4983.00185. S2CID 83592270.
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