Multituberculata
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| Multituberculates Temporal range: Middle Jurassic-Late Eocene
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| Skeleton of Catopsbaatar | |
| Scientific classification | |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Mammalia |
| Subclass: | †Allotheria |
| Order: | †Multituberculata Cope, 1884 |
| Suborders | |
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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 — 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
[edit]
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]

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]

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
[edit]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 to.[17] During the Late Jurassic and Early Cretaceous, basal 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]

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
[edit]Multituberculate is generally placed within Allotheria alongside Euharamiyida, a clade of mammals known from the Middle Jurassic to Early Cretaceous of Asia and possibly Europe that possess several morphological similarities with 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]

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
[edit]Subgroups
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Based on the combined works of Mikko's Phylogeny Archive[30] and Paleofile.com.[citation needed] Suborder †Plagiaulacida Simpson 1925
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Phylogeny
[edit]After Chimento et al. 2015:[29]
| Multituberculata | |
Cladogram after Carvalho et al. 2025:[31]
Paleoecology
[edit]Behaviour
[edit]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.[32]
Extinction
[edit]The extinction of multituberculates has been a topic of controversy for several decades.[33] 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.[34]
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.[35]: 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] Adams et al. (2019) argued in favor of this hypothesis as rodents have a higher bite force than multituberculates, which would have given them access to harder, drier seeds which were becoming more abundant and had a greater range of food compared to multituberculates. The authors also argued rodents had was longer gestation periods and larger neonates which gave them a competitive advantage over multituberculates. In addition, they believed the diversity of new predators such as owls, creodonts, and carnivorans, also played a role in their extinction.[36]
However, the idea that multituberculates were competitively 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 suggests that multituberculates simply could not cope with climatic and vegetation changes, as well as the rise of new predatory eutherians, such as miacids. However, rodents probably still played a role in their decline.[34]
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.[33] A recent study seems to indeed indicate that eutherians recovered more quickly from the KT event than multituberculates.[37] Conversely, another study has shown that placental radiation did not start significantly until after the decline of multituberculates.[21]
However, competitive replacement among North American species has been called into question by Benjamin John Burger in his 2025 study. He suggests the extinction of multituberculates in North America was correlated to the decline of boreal forests that were dominated by dawn redwoods and Chinese swamp cypress. The analysis suggested that multituberculates avoided pine and spruce-dominated forests despite having similar geographic distributions to those trees. However, Burger argues competitive replacements by seed-eating passerine birds such as songbirds, and several mammalian groups such as paromomyids, may have played a role in the extinction of multituberculates, although this requires more testing.[38]
References
[edit]- ^ a b Krause, David W. (1986). "Competitive exclusion and taxonomic displacement in the fossil record". Vertebrates, Phylogeny, and Philosophy. pp. 95–117. doi:10.2113/gsrocky.24.special_paper_3.95. ISBN 978-0-941570-02-2.
- ^ a b Weil, Anne (June 1997). "Introduction to Multituberculates: The 'Lost Tribe' of Mammals". Berkeley: UCMP.
- ^ Chen, Meng; Philip Wilson, Gregory (2015). "A multivariate approach to infer locomotor modes in Mesozoic mammals". Paleobiology. 41 (2): 280–312. Bibcode:2015Pbio...41..280C. doi:10.1017/pab.2014.14. S2CID 86087687.
- ^ a b c d e Agustí-Antón 2002, pp 3-4
- ^ Benton, Michael J. Vertebrate Palaeontology (2004), p. 300
- ^ Carrano, Matthew T., and Richard W. Blob, Timothy J. Gaudin, and John R. Wible (2006). Amniote Paleobiology: Perspectives on the Evolution of Mammals, Birds, and Reptiles, p. 358.
- ^ a b c d e Kielan-Jaworowska, Zofia, Richard L. Cifelli, and Zhe-Xi Luo (2005). Mammals from the Age of Dinosaurs: Origins, Evolution, and Structure , p. 299
- ^ Gurovich 2005 p. 334[full citation needed]
- ^ Gurovich, Yamila; Beck, Robin (March 2009). "The Phylogenetic Affinities of the Enigmatic Mammalian Clade Gondwanatheria". Journal of Mammalian Evolution. 16 (1): 25–49. doi:10.1007/s10914-008-9097-3. S2CID 42799370.
- ^ Rougier et al. 2009 p.233[full citation needed]
- ^ Lanyon, J. M.; Sanson, G. D. (February 2006). "Degenerate dentition of the dugong (Dugong dugon), or why a grazer does not need teeth: morphology, occlusion and wear of mouthparts". Journal of Zoology. 268 (2): 133–152. doi:10.1111/j.1469-7998.2005.00004.x.
- ^ "New study challenges old views on what's 'primitive' in mammalian reproduction". 25 July 2022.
- ^ Mao, Fangyuan; Li, Zhiyu; Wang, Zhili; Zhang, Chi; Rich, Thomas; Vickers-Rich, Patricia; Meng, Jin (2024-04-03). "Jurassic shuotheriids show earliest dental diversification of mammaliaforms". Nature. doi:10.1038/s41586-024-07258-7. ISSN 0028-0836.
- ^ Williamson, Thomas E.; Brusatte, Stephen L.; Secord, Ross; Shelley, Sarah (2015). "A new taeniolabidoid multituberculate (Mammalia) from the middle Puercan of the Nacimiento Formation, New Mexico, and a revision of taeniolabidoid systematics and phylogeny". Zoological Journal of the Linnean Society. 177: 183–208. doi:10.1111/zoj.12336.
- ^ "Gondwanatheria".[dead link]
- ^ Crompton, A. W.; Musinsky, C.; Rougier, G. W.; Bhullar, B.-A. S.; Miyamae, J. A. (September 2018). "Origin of the Lateral Wall of the Mammalian Skull: Fossils, Monotremes and Therians Revisited". Journal of Mammalian Evolution. 25 (3): 301–313. doi:10.1007/s10914-017-9388-7. S2CID 16072755.
- ^ a b Averianov, Alexander O.; Martin, Thomas; Lopatin, Alexey V.; Schultz, Julia A.; Schellhorn, Rico; Krasnolutskii, Sergei; Skutschas, Pavel; Ivantsov, Stepan (May 2021). "Multituberculate mammals from the Middle Jurassic of Western Siberia, Russia, and the origin of Multituberculata". Papers in Palaeontology. 7 (2): 769–787. doi:10.1002/spp2.1317. ISSN 2056-2799. S2CID 219067218.
- ^ Weaver, Lucas N.; Wilson, Gregory P.; Krumenacker, L. J.; Mclaughlin, Kayla; Moore, Jason R.; Varricchio, David J. (2019-03-04). "New multituberculate mammals from the mid-Cretaceous (lower Cenomanian) Wayan Formation of southeastern Idaho and implications for the early evolution of Cimolodonta". Journal of Vertebrate Paleontology. 39 (2) e1604532. Bibcode:2019JVPal..39E4532W. doi:10.1080/02724634.2019.1604532. ISSN 0272-4634. S2CID 196655261.
- ^ Wilson, Gregory P.; Evans, Alistair R.; Corfe, Ian J.; Smits, Peter D.; Fortelius, Mikael; Jernvall, Jukka (March 2012). "Adaptive radiation of multituberculate mammals before the extinction of dinosaurs". Nature. 483 (7390): 457–460. Bibcode:2012Natur.483..457W. doi:10.1038/nature10880. ISSN 1476-4687. PMID 22419156. S2CID 4419772.
- ^ Adams, Neil F.; Rayfield, Emily J.; Cox, Philip G.; Cobb, Samuel N.; Corfe, Ian J. (March 2019). "Functional tests of the competitive exclusion hypothesis for multituberculate extinction". Royal Society Open Science. 6 (3) 181536. Bibcode:2019RSOS....681536A. doi:10.1098/rsos.181536. ISSN 2054-5703. PMC 6458384. PMID 31032010.
- ^ a b Brocklehurst, Neil; Panciroli, Elsa; Benevento, Gemma Louise; Benson, Roger B. J. (July 2021). "Mammaliaform extinctions as a driver of the morphological radiation of Cenozoic mammals". Current Biology. 31 (13): 2955–2963.e4. doi:10.1016/j.cub.2021.04.044. PMID 34004143. S2CID 234782605.
- ^ a b Rich, Thomas; Trusler, Peter; Kool, Lesley; White, Matt A.; Bevitt, Joseph; Morton, Steven; Vickers−Rich, Patricia (2022). "Second specimen of Corriebaatar marywaltersae from the Lower Cretaceous of Australia confirms its multituberculate affinities". Acta Palaeontologica Polonica. 67. doi:10.4202/app.00924.2021. ISSN 0567-7920. S2CID 247905998.
- ^ Krause, David W.; Hoffmann, Simone; Werning, Sarah (December 2017). "First postcranial remains of Multituberculata (Allotheria, Mammalia) from Gondwana". Cretaceous Research. 80: 91–100. Bibcode:2017CrRes..80...91K. doi:10.1016/j.cretres.2017.08.009.
- ^ Longrich, Nicholas R.; Ryan, Michael J. (2010). "Mammalian tooth marks on the bones of dinosaurs and other Late Cretaceous vertebrates". Palaeontology. 53 (4): 703–709. Bibcode:2010Palgy..53..703L. doi:10.1111/j.1475-4983.2010.00957.x.
- ^ Krause et al 2021
- ^ Wilson et al 2012
- ^ a b Hoffmann, Simone; Beck, Robin M. D.; Wible, John R.; Rougier, Guillermo W.; Krause, David W. (2020-12-14). "Phylogenetic placement of Adalatherium hui (Mammalia, Gondwanatheria) from the Late Cretaceous of Madagascar: implications for allotherian relationships". Journal of Vertebrate Paleontology. 40 (sup1): 213–234. Bibcode:2020JVPal..40S.213H. doi:10.1080/02724634.2020.1801706. ISSN 0272-4634. S2CID 230968231.
- ^ Dykes Multituberculata (Cope 1884)
- ^ a b Nicolás R. Chimento; Federico L. Agnolin; Fernando E. Novas (2015). "The bizarre 'metatherians' Groeberia and Patagonia, late surviving members of gondwanatherian mammals". Historical Biology: An International Journal of Paleobiology. 27 (5): 603–623. doi:10.1080/08912963.2014.903945. hdl:11336/85076. S2CID 216591096.
- ^ Mikko's Phylogeny Archive Haaramo, Mikko (2007). "Mammaliaformes – mammals and near-mammals". Retrieved 30 December 2015.
- ^ Carvalho, Victor F.; Camilo, Bruno; Araújo, Ricardo; Castro, Lígia; Kullberg, José C.; Desmet, Hilde G. B.; Nerinckx, Ignace; Leite, Marco; Reis, Diego (March 2025). "Cambelodon torreensis , a new pinheirodontid multituberculate from the Upper Jurassic of western Portugal". Papers in Palaeontology. 11 (2). doi:10.1002/spp2.70012. ISSN 2056-2799.
- ^ Weaver, Lucas N.; Varricchio, David J.; Sargis, Eric J.; Chen, Meng; Freimuth, William J.; Wilson Mantilla, Gregory P. (2 November 2020). "Early mammalian social behaviour revealed by multituberculates from a dinosaur nesting site". Nature Ecology & Evolution. 5 (1): 32–37. doi:10.1038/s41559-020-01325-8. PMID 33139921. S2CID 226241443.
- ^ a b Wood, D. Joseph (2010). The Extinction of the Multituberculates Outside North America: a Global Approach to Testing the Competition Model (M.S.). The Ohio State University. Archived from the original on 2015-04-08. Retrieved 2015-04-03.
- ^ a b Ostrander, Gregg (1 January 1984). "The Early Oligocene (Chadronian) Raben Ranch Local Fauna, Northwest Nebraska: Multituberculata; with Comments on the Extinction of the Allotheria". Transactions of the Nebraska Academy of Sciences and Affiliated Societies.
- ^ Wood, D. Joseph (2010). The Extinction of the Multituberculates Outside North America: a Global Approach to Testing the Competition Model (Thesis). The Ohio State University. Archived from the original on 2023-05-19. Retrieved 2023-05-19.
- ^ Adams, Neil F.; Rayfield, Emily J.; Cox, Philip G.; Cobb, Samuel N.; Corfe, Ian J. (2019). "Functional tests of the competitive exclusion hypothesis for multituberculate extinction". Royal Society Open Science. 6 (3). doi:10.1098/rsos.181536. PMC 6458384.
- ^ Pires, Mathias M.; Rankin, Brian D.; Silvestro, Daniele; Quental, Tiago B. (2018). "Diversification dynamics of mammalian clades during the K–Pg mass extinction". Biology Letters. 14 (9): 2058. doi:10.1098/rsbl.2018.0458. PMC 6170748. PMID 30258031.
- ^ Burger, Benjamin John (2025). "Comparative spatial paleoecology: assessing niche competition between Eocene North American multituberculates and rodents regarding forest resources to elucidate the cause of multituberculate extinction". Paleobiology: 1–16. doi:10.1017/pab.2025.10048.
Sources
[edit]- 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.
Multituberculata
View on GrokipediaAnatomy and Morphology
Dentition and Skull
Multituberculates possessed a highly specialized dentition characterized by enlarged, ever-growing incisors, a prominent diastema separating the incisors from the cheek teeth, and distinctive molars and premolars adapted for both shearing and grinding. The cheek teeth featured multiple longitudinal rows of cusps, typically two or three, arranged on the occlusal surfaces of the upper and lower molars and premolars, enabling efficient pulverization of food through precise cusp-to-cusp occlusion. A defining feature was the enlarged fourth lower premolar, known as the plagiaulacoid, which formed a blade-like structure with serrated edges and multiple cusps, functioning primarily for shearing tough plant material or possibly small invertebrates. This dentition supported a palinal (posteriorly directed) jaw stroke during mastication, where the lower teeth moved backward relative to the uppers, contrasting with the propalinal motion seen in rodents.[4][2] The skull of multituberculates exhibited an elongated, rodent-like rostrum that housed the procumbent incisors and contributed to the mechanical efficiency of feeding. A substantial diastema between the incisors and the first premolar allowed space for jaw movement without interference, while the zygomatic arches were robust to accommodate powerful masseter muscles. The palate often lacked vacuities in more primitive forms but showed variations, and the braincase was relatively narrow with a prominent petrosal bone forming much of the lateral wall. Recent high-resolution CT scans of specimens, such as the kogaionid Litovoi tholocephalos, reveal an endocast with intermediate complexity: a narrow overall shape reminiscent of early mammals, yet incorporating therian-like features such as expanded paraflocculi and a relatively large cochlea, bridging primitive and derived mammalian neuroanatomy.[5][6] Dentition varied significantly across multituberculate groups, reflecting evolutionary progression from primitive to advanced forms. In the basal Plagiaulacida, the plagiaulacoid premolar was fully developed and blade-like, with premolars and molars bearing simpler, more triangular cusps suited to an omnivorous or insectivorous diet, and low-crowned (brachyodont) teeth overall. In contrast, the more derived Cimolodonta, dominant from the Late Cretaceous onward, showed reduction or modification of the plagiaulacoid, with molars evolving toward hypsodonty—taller crowns with increased occlusal wear surfaces—in later Paleogene taxa, enhancing adaptation to abrasive herbaceous diets. These shifts paralleled broader cranial refinements, such as a more robust rostrum and enhanced jaw musculature in cimolodontans.[7]Postcranial Features
Multituberculates displayed considerable variation in body size, ranging from diminutive, shrew-like forms to large, beaver-sized individuals, reflecting their adaptation to diverse ecological niches across the Mesozoic and Cenozoic eras. The earliest known multituberculate, Rugosodon eurasiaticus from the Middle Jurassic of China, represents one of the smallest, with a total body length of approximately 20 cm and an estimated mass under 100 g, comparable to modern shrews.[8] In contrast, the Paleocene taeniolabidoid Taeniolabis taoensis from North America achieved the largest size among all multituberculates, with estimated body masses of up to approximately 40 kg based on cranial measurements, akin to a large beaver, and postcranial elements indicating a robust build consistent with this size.[9][10] This size disparity, spanning over three orders of magnitude, underscores the group's evolutionary flexibility in response to environmental changes.[11] Limb morphology in multituberculates was diverse, supporting a range of locomotor strategies from terrestrial cursoriality to potential scansorial or saltatorial behaviors. In taxa like the Cretaceous Kryptobaatar dashzevegi from Mongolia, the forelimbs were robust with abducted humeri and strong muscular attachments, suggesting adaptations for digging or burrowing activities, as evidenced by the twisted humeral shaft and large deltopectoral crest for powerful forelimb retraction. Hindlimbs in many forms, such as the Paleocene Ptilodus gracilis, featured relatively elongated femora and tibiae with a large greater trochanter and pronounced peroneal process on the calcaneus, indicating saltatorial capabilities for leaping or possibly arboreal climbing, though phalangeal robusticity points more toward generalized terrestrial locomotion than specialized arborealism.[12] Overall, limb proportions reflect a predominantly sprawling posture with abducted limbs, but with parasagittal elements in the hindlimb for efficient forward propulsion during asymmetrical gaits.[13] Vertebral and pelvic structures provided support for dynamic movement and reproductive strategies. The vertebral column in Asian multituberculates like Kryptobaatar included long, craniodorsally sloping lumbar spinous processes, facilitating an asymmetrical gait with short jumps and enhanced spinal flexibility for maneuvering. Pelvic adaptations, such as a deep acetabulum with a large iliosacral angle of 35–37° and dorsoventral contact between ilium and sacrum, suggest stability for weight-bearing during locomotion and potential for live birth, as the broad pelvic canal accommodated passage of young without the narrow constraints seen in monotremes. Recent bone histology analyses further support a placental-like reproductive strategy with extended gestation, implying live birth to relatively developed offspring rather than marsupial-style pouch rearing. In Taeniolabis, the robust pelvis and short caudal vertebrae indicate a stable base for its large body mass, with fossorial elements in the calcaneus hinting at digging behaviors.[10] Fossil evidence for soft tissues includes tail and fur impressions, offering insights into sensory and thermoregulatory functions. Caudal vertebrae in forms like Catopsbaatar catopsaloides were numerous and elongated, suggesting a long, flexible tail possibly used for balance during jumping or as a sensory organ, similar to modern rodents.[14] Fur impressions preserved in coprolites of the Eocene Lambdopsalis bulla reveal a dense pelage with guard hairs and underfur, indicating homeothermy and protection against environmental stresses, with no evidence for prehensile capabilities but potential for insulation in varied habitats. These features align with the group's inferred warm-blooded physiology and active lifestyles.Taxonomy and Phylogeny
Historical Classification
The first recognized multituberculate fossils were teeth from the Early Cretaceous Purbeck Group of England, described as the genus Plagiaulax by Hugh Falconer in 1857.[15] Falconer interpreted these specimens as belonging to an extinct herbivorous marsupial rodent, based on their multicusped premolars and overall dental morphology. This initial classification reflected the limited understanding of Mesozoic mammals at the time, with the unusual tuberculate teeth leading to comparisons with both reptilian and marsupial forms rather than recognizing their distinct mammalian affinities. Subsequent work by Richard Owen in 1871 expanded on these discoveries through a monograph detailing Mesozoic mammals from the British Museum collections, including additional Plagiaulax material and new genera like Bolodon. Owen confirmed their mammalian nature but emphasized their aberrant dentition, placing them in a provisional group separate from typical therian mammals and suggesting possible links to monotremes due to shared primitive features. In the late 19th century, Edward Drinker Cope advanced the taxonomy by naming numerous North American Paleogene species, such as Taeniolabis in 1882, and formally establishing the order Multituberculata in 1884 as a suborder within Marsupialia, highlighting similarities in their specialized cheek teeth to those of rodents. Cope's framework sparked ongoing debates about multituberculate affinities, with some researchers, including Henry Fairfield Osborn in his studies of early 20th-century Paleocene faunas, proposing closer ties to rodents based on ecological and dental parallels. George Gaylord Simpson's 1928 catalogue of Mesozoic mammals synthesized these early findings and provided the first comprehensive classification, dividing Multituberculata into three suborders: the primitive Plagiaulacida (encompassing Jurassic and Early Cretaceous forms like Plagiaulax), and the more derived Ptilodontoidea and Taeniolabidoidea (dominating Late Cretaceous and Paleogene assemblages). Simpson's scheme underscored their evolutionary distinctiveness while maintaining debates on rodent-like adaptations, such as grinding dentition suited to herbivory. By the mid-20th century, Zofia Kielan-Jaworowska's expeditions to the Gobi Desert in the 1960s and 1970s uncovered exceptionally preserved Late Cretaceous specimens, including skulls and postcrania, which demonstrated unique anatomical features like inflected angular processes and specialized jaw mechanics, solidifying Multituberculata's status as a separate mammalian order rather than a marsupial or rodent offshoot. These contributions culminated in the 1970s with the broader recognition of Multituberculata within the subclass Allotheria, a grouping initially proposed by Cope but refined to encompass their basal position relative to other mammals, based on shared dental and cranial traits with extinct Jurassic haramiyidans. This historical progression from misclassification as marsupials or reptiles to an independent clade laid the groundwork for understanding their long evolutionary history.Modern Suborders and Families
The modern taxonomic framework for Multituberculata recognizes two primary suborders based on dental morphology, postcranial features, and stratigraphic distribution, as outlined in the comprehensive revision by Kielan-Jaworowska, Cifelli, and Luo (2001).[16] The suborder Plagiaulacida is considered paraphyletic, representing a grade of early, primitive forms that bridge the basal multituberculates to more derived lineages, while Cimolodonta forms a monophyletic clade defined by shared apomorphies such as advanced occlusal patterns in the lower premolars.[16] This classification has remained influential, though recent phylogenetic studies using tip-dating methods have refined relationships among early allotherians, rejecting a strict monophyly of Allotheria and suggesting some haramiyidan-like forms may nest within multituberculate diversity, with Gondwanatheria positioned outside the group.[17] Plagiaulacida spans the Middle Jurassic to Early Cretaceous and is characterized by simpler tuberculate dentition suited to insectivory or omnivory, with fossils primarily from Laurasian continents. Key families include Plagiaulacidae (e.g., Plagiaulax from the Early Cretaceous of Europe), Albionbaataridae (e.g., Albionbaatar from the Early Cretaceous of England), and Paulchoffatiidae (e.g., Paulchoffatia from the Late Jurassic of Portugal). The earliest definitive multituberculates date to the Middle Jurassic Bathonian stage, such as Hahnotherium from England. An important early multituberculate, Rugosodon eurasiaticus, from the Late Jurassic Tiaojishan Formation of China, exemplifies early dental specializations like multiple premolars. These taxa exhibit low diversity, with fewer than 50 described species, reflecting their role as stem-group forms before the cimolodontan radiation. Cimolodonta, the dominant suborder, ranges from the Early Cretaceous to the late Eocene and achieved peak diversity in the Late Cretaceous and Paleogene of North America and Asia, with over 150 species described. This suborder is divided into several superfamilies, including Ptilodontoidea (e.g., families Ptilodontidae with Ptilodus from the Paleocene of North America, known for its rodent-like grinding dentition) and Taeniolabidoidea (e.g., Taeniolabididae with Taeniolabis, the largest known multituberculate at up to 50 kg body mass from the Paleocene of North America). Other notable families include Djadochtatheriidae (e.g., Kryptobaatar from the Late Cretaceous of Mongolia, renowned for well-preserved skeletons showing cursorial adaptations) and Eucosmodontidae (e.g., Eucosmodon from the Late Cretaceous of North America). Cimolodontans occupied diverse niches, from arboreal to terrestrial, across Laurasia, with isolated records in Europe and Asia. The following table summarizes major families within each suborder, highlighting temporal and geographic distributions:| Suborder | Family | Temporal Range | Geographic Range | Key Genera Examples |
|---|---|---|---|---|
| Plagiaulacida | Plagiaulacidae | Late Jurassic–Early Cretaceous | Europe | Plagiaulax, Bolodon |
| Plagiaulacida | Albionbaataridae | Early Cretaceous | Europe | Albionbaatar |
| Plagiaulacida | Paulchoffatiidae | Late Jurassic | Europe | Paulchoffatia |
| Cimolodonta | Ptilodontidae | Late Cretaceous–Eocene | North America | Ptilodus, Baiotomeus |
| Cimolodonta | Taeniolabididae | Paleocene–Eocene | North America | Taeniolabis, Catopsalis |
| Cimolodonta | Djadochtatheriidae | Late Cretaceous | Asia | Kryptobaatar, Nemegtbaatar |
