Meniscoessus

Last updated

Meniscoessus
Temporal range: Late Cretaceous
Meniscoessus skull.jpg
Meniscoessus skull in the Rocky Mountain Dinosaur Resource Center, Woodland Park, Colorado
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Mammalia
Order: Multituberculata
Family: Cimolomyidae
Genus: Meniscoessus
Cope, 1882
Species
  • M. collomensis
  • M. conquistus
  • M. ferox
  • M. intermedius
  • M. major
  • M. robustus
  • M. seminoensis

Meniscoessus is a genus of extinct multituberculates from the Upper Cretaceous Period that lived in North America.

Contents

It is a member of the order Multituberculata, belonging to the suborder Cimolodonta and family Cimolomyidae. The multituberculates were primitive, rodent-like mammals occupying the modern rodent ecological niche. They were significant for having diverged early in mammalian evolution, co-existing with dinosaurs for ~100 million years, surviving through the Cretaceous–Paleogene extinction event and lasting until the end of the Paleogene, likely having been replaced by true rodents. [1] [2] [3] [4]

Meniscoessus lived during the Santonian, Campanian and Maastrichtian ages of the Upper Cretaceous. This was a period of significant diversification of multiturbiculates, and evidence that contradicts the popular misconception that mammals were unable to thrive due to being outcompeted by the dinosaurs. [5] [6] [7] They are useful as index fossils for the Judithian, Edmontonian, and Lancian faunal stages. [8] Like most early mammals, Meniscoessus fossils mainly consist of teeth. Zofia Kielan-Jaworowska and Jørn Hurum considered them to be the "best known" members of the Cimolomyidae. [9]

Taxonomy

History

The genus Meniscoessus was named by Edward Drinker Cope in 1882. [10] Members of this genus have been previously classified under the following genus names: Cimolomys (partly); Dipriodon ; Halodon; Oracodon; Moeniscoessus; Selenacodon (partly); and Tripriodon. As Osborn pointed out in 1891, a number of erroneous discoveries had been made as a result of analyzing different teeth of the same animal, different individuals of the same species, and violating the principle of priority due to workers ignoring previously published discoveries. [11]

There may have been confusion with some teeth described as belonging to small carnivorous dinosaurs. [ citation needed ] These were further christened Dipriodon, Tripriodon, and others, including Triprotodon.[ citation needed ] Close similarities were then noticed with an already established dinosaur genus, Paronychodon (Cope 1876), also based on teeth from the Laramie Formation. [ citation needed ] Over time, an impressive school of names was synonymized under P. However, this is now considered a nomen dubium .

M. robustus tooth Meniscoessus robustus.jpg
M. robustus tooth

Species

M. robustus skull Multituberculate skull.jpg
M. robustus skull

Several other names have been in circulation, such as Meniscoessus bustus, and Meniscoessus coelatus. The first is probably a variant of M. robustus, while the latter seems to have been connected with dinosaur teeth. [ citation needed ]

Notes

  1. Weil
  2. Prothero, 2006, pp 55-61, 157
  3. Benton 2015, pp 330,337-338
  4. Wilson et al, 2012
  5. Benton, 2015, pg 338
  6. Carroll, 1988, pg 419
  7. Wilson et al, 2012, pg 459
  8. Cifelli et al, 2004
  9. Kielan-Jaworowska and Hurum, 2001, pg 408
  10. Cope, 1882, pg 830
  11. Osborn, 1891, pg 597-598
  12. Lillegraven, 1987
  13. Wilson et al, 2010, pg 499
  14. Cifelli et al, 2004, pg 28 and Table 2.2
  15. Wilson et al, 2012, Supplemental Table 5
  16. Cope, 1882, pg 831
  17. Paleobiology Database, Meniscoessus
  18. Fox, 1971
  19. Fox, 1976
  20. Wilson et al, 2012, Supplemental Table 5
  21. Wilson et al, 2012, Supplemental Table 5
  22. Cifelli et al 2004, pp 35-36: discussion of dispute
  23. Marsh 1889, pp 85-89
  24. Wilson et al, 2012, Supplemental Table 5
  25. Osborn, 1891, pg 607
  26. Eberle and Lillegraven, 1998, pp. 33-35
  27. Carroll, 1988, 417-418: Carroll notes that the premolars and specialized dentition in multituberculates are particularly significant
  28. Wilson et al, 2012, Supplemental Table 5

Related Research Articles

Zofiabaatar is a genus of extinct mammal from the Upper Jurassic period. It was a relatively early member of the extinct order Multituberculata within the suborder "Plagiaulacida". It lived in North America along with dinosaurs such as Diplodocus and Allosaurus.

<i>Bolodon</i> Extinct genus of mammals

Bolodon is a genus of extinct mammal from the Lower Cretaceous of Europe and North America. It was a member of the extinct order of Multituberculata and belongs to the suborder Plagiaulacida and family Plagiaulacidae.

Albionbaatar is an extinct mammal from the Lower Cretaceous Lulworth Formation of England. It was a member of the also extinct order Multituberculata and shared the world with the much larger dinosaurs. It is in the suborder "Plagiaulacida", family Albionbaataridae. The genus Albionbaatar was named by Kielan-Jaworowska Z. and Ensom P.C. in 1994 based on a single species.

Iberodon is a small, extinct mammal of the Lower Cretaceous from Portugal. It was a member of the also extinct order Multituberculata, and led its obscure and plant-eating existence in the company of dinosaurs. It lies within the suborder "Plagiaulacida" and family Pinheirodontidae.

Paracimexomys is a genus of extinct mammals in the extinct Multituberculata order. Paracimexomys lived during the Cretaceous period. The few fossils remains come from North America. Some Romanian fossils were also tentatively assigned to this genus, though that classification now seems doubtful.

<i>Cimexomys</i> Extinct genus of North American mammal

Cimexomys is an extinct North American mammal that lived from the Upper Cretaceous to the Paleocene. For a while, it shared the world with dinosaurs, but outlived them. It was a member of the extinct order Multituberculata and lies within the suborder Cimolodonta. It is perhaps a member of the Paracimexomys group, though it is not certain.

Bulganbaatar is a Central Asian mammal genus from the Upper Cretaceous. It existed in the company of dinosaurs. This animal was a member of the extinct order Multituberculata. It's within the suborder Cimolodonta and is a member of the superfamily Djadochtatherioidea. The genus Bulganbaatar was named by Kielan-Jaworowska Z. in 1974.

<i>Nemegtbaatar</i> Extinct genus of multituberculates

Nemegtbaatar is a genus of mammal from the Upper Cretaceous Period of what is now Mongolia. It existed in the company of much larger dinosaurs, found together in the Nemegt Basin. This creature was a member of the extinct order Multituberculata. It is within the suborder Cimolodonta and is a member of the superfamily Djadochtatherioidea. It was a hopping, gerboa-like species.

<i>Catopsalis</i> Extinct genus of mammals

Catopsalis is a genus of extinct mammal from the Paleocene of North America. This animal was a relatively large member of the extinct order of Multituberculata. Most Multituberculates were much smaller.

Neoplagiaulax is a mammal genus from the Paleocene of Europe and North America. In the case of the latter continent, there may possibly be some slightly earlier, Upper Cretaceous material too. It existed in the age immediately following the extinction of the last dinosaurs. This animal was a member of the extinct order Multituberculata, lying within the suborder Cimolodonta and family Neoplagiaulacidae.

Mesodma is an extinct genus of mammal, a member of the extinct order Multituberculata within the suborder Cimolodonta, family Neoplagiaulacidae. It lived during the upper Cretaceous and Paleocene Periods of what is now North America. The earliest definitive record is from the late Santonian stage strata of the Straight Cliffs Formation. A single premolar tooth from the lower Cenomanian stage strata of the Cedar Mountain Formation has been tentatively assigned to this genus based on its similarity, but its describers noted that it is unlikely that Mesodma lived during that time.

<i>Kogaionon ungureanui</i> Genus of mammals

Kogaionon is a mammal genus from the Upper Cretaceous of Romania. It lived in Transylvania the same time as some of the last non-avian dinosaurs and was a member of the extinct order of Multituberculata. It was named after Kogaionon, the holy mountain of the ancient Dacians. It lies within the suborder Cimolodonta and the family Kogaionidae. The genus Kogaionon was named by Rădulescu R. and Samson P. in 1996.

<i>Barbatodon</i> Extinct family of mammals

Barbatodon is a mammal genus from the Upper Cretaceous period. It lived in Transylvania at the same time as some of the last dinosaurs and was a member of the extinct order of Multituberculata. It is within the suborder of Cimolodonta, and the family Kogaionidae. The genus Barbatodon was named by Constantin Rădulescu and Petre Mihai Samson in 1986.

<i>Cimolomys</i> Extinct family of mammals

Cimolomys is a mammal genus from the Upper Cretaceous of North America. It was a member of the extinct order Multituberculata within the suborder Cimolodonta and family Cimolomyidae.

Viridomys is a genus of extinct mammal from the Upper Cretaceous of North America. It was a member of the extinct order of Multituberculata, and lived during the Mesozoic, also known as the "age of the dinosaurs." It's within the suborder of Cimolodonta, though its further affinities are unclear.

Ferugliotheriidae is one of three known families in the order Gondwanatheria, an enigmatic group of extinct mammals. Gondwanatheres have been classified as a group of uncertain affinities or as members of Multituberculata, a major extinct mammalian order. The best-known representative of Ferugliotheriidae is the genus Ferugliotherium from the Late Cretaceous epoch in Argentina. A second genus, Trapalcotherium, is known from a single tooth, a first lower molariform, from a different Late Cretaceous Argentinean locality. Another genus known from a single tooth, Argentodites, was first described as an unrelated multituberculate, but later identified as possibly related to Ferugliotherium. Finally, a single tooth from the Paleogene of Peru, LACM 149371, perhaps a last upper molariform, and a recent specimen from Mexico, may represent related animals.

<i>Repenomamus</i> Extinct genus of mammals

Repenomamus is a genus of opossum- to badger-sized gobiconodontid mammal containing two species, Repenomamus robustus and Repenomamus giganticus. Both species are known from fossils found in China that date to the early Cretaceous period, about 125-123.2 million years ago. R. robustus is one of several Mesozoic mammals for which there is good evidence that it fed on vertebrates, including dinosaurs. Though it is not entirely clear whether or not these animals primarily hunted live dinosaurs or scavenged dead ones, evidence for the former is present in fossilized remains showcasing the results of what was most likely a predation attempt by R. robustus directed at a specimen of the dinosaur Psittacosaurus lujiatunensis. R. giganticus is among the largest mammals known from the Mesozoic era.

<i>Protungulatum</i> Extinct genus of mammals

Protungulatum is an extinct genus of eutherian mammals within extinct family Protungulatidae, and is possibly one of the earliest known placental mammals in the fossil record, that lived in North America from the Late Cretaceous to early Paleocene.

<span class="mw-page-title-main">Zofia Kielan-Jaworowska</span> Polish paleobiologist (1925–2015)

Zofia Kielan-Jaworowska was a Polish paleobiologist. In the mid-1960s, she led a series of Polish-Mongolian paleontological expeditions to the Gobi Desert. She was the first woman to serve on the executive committee of the International Union of Geological Sciences. The most notable dinosaur species she discovered include: Deinocheirus and Gallimimus while Kielanodon and Zofiabaatar were named in her honour.

Argentodites is a possible multituberculate mammal from the Cretaceous of Argentina. The single species, Argentodites coloniensis, is known from a single blade-like fourth lower premolar (p4) from the La Colonia Formation, which is mostly or entirely Maastrichtian in age. The p4 is 4.15 mm long and bears eight cusps on its upper margin and long associated ridges on both sides. The enamel consists of prisms that are completely or partly surrounded by a sheath and that are on average 6.57 μm apart. Zofia Kielan-Jaworowska, who described and named the fossil in 2007, regarded it as a multituberculate, perhaps a cimolodontan—and thus, a member of a mostly Laurasian (northern) group and an immigrant to Argentina from North America—on the basis of the shape of the tooth and features of its enamel. In 2009, however, two teams argued that Argentodites may in fact be close to or identical with Ferugliotherium, a member of the small Gondwanan (southern) group Gondwanatheria; although their relationships are disputed, gondwanatheres may themselves be multituberculates.

References