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== History of discovery ==
== History of discovery ==
In the summer of 1947, fieldwork was done at Duchy Quarry in [[Glamorgan]] in southern Wales. Grey [[Conglomerate (geology)|conglomerate]] that formed fissure fill deposits within [[Carboniferous Limestone|Carboniferous limestone]] was extracted. In 1949, [[Walter Georg Kühne]] noted the lower cheek tooth of a primitive mammal while examing samples of the rock. He named it ''Morganucodon watsoni,'' with the species name being in honour of [[D. M. S. Watson]].<ref name=":0" /> In August 1948, an expedition to [[Lufeng, Yunnan|Lufeng]] in [[Yunnan]], China yielded a 1 in (2.5 cm) skull. It was shortly sent to Beijing (then Peking) and then eventually sent out of China, and deposited at [[University College London]] in 1960. The specimen was preliminarily described in 1963 by Harold W. Rigney, who noted the similarity to ''Morganucodon'' from Britain, and considered it cogeneric, naming the new species ''Morganucodon oehleri'' in honor of the reverend Edgar T. Oehler, who had originally collected the specimen.<ref>{{Cite journal|last=Rigney|first=Harold W.|date=1963-03|title=A Specimen of Morganucodon from Yunnan|url=http://www.nature.com/articles/1971122a0|journal=Nature|language=en|volume=197|issue=4872|pages=1122–1123|doi=10.1038/1971122a0|issn=0028-0836}}</ref>
In the summer of 1947, fieldwork was done at Duchy Quarry in [[Glamorgan]] in southern Wales. Grey [[Conglomerate (geology)|conglomerate]] that formed fissure fill deposits within [[Carboniferous Limestone|Carboniferous limestone]] was extracted. In 1949, [[Walter Georg Kühne]] noted the lower cheek tooth of a primitive mammal while examing samples of the rock. He named it ''Morganucodon watsoni,'' with the species name being in honour of [[D. M. S. Watson]].<ref name=":0" /> Additonal remains of ''M. watsoni'' were described by Kühne in 1958.<ref>{{Cite journal|last=Kühne|first=Walter Georg|date=1958-08-01|title=Rhaetische Triconodonten aus Glamorgan, ihre Stellung zwischen den Klassen Reptilia und Mammalia und ihre Bedeutung für die REICHART'sche Theorie|url=https://doi.org/10.1007/BF02989032|journal=Paläontologische Zeitschrift|language=de|volume=32|issue=3|pages=197–235|doi=10.1007/BF02989032|issn=1236-9874}}</ref> In August 1948, an expedition to [[Lufeng, Yunnan|Lufeng]] in [[Yunnan]], China yielded a 1 in (2.5 cm) skull. It was shortly sent to Beijing (then Peking) and then eventually sent out of China, and deposited at [[University College London]] in 1960. The specimen was preliminarily described in 1963 by Harold W. Rigney, who noted the similarity to ''Morganucodon'' from Britain, and considered it cogeneric, naming the new species ''Morganucodon oehleri'' in honor of the reverend Edgar T. Oehler, who had originally collected the specimen.<ref>{{Cite journal|last=Rigney|first=Harold W.|date=1963-03|title=A Specimen of Morganucodon from Yunnan|url=http://www.nature.com/articles/1971122a0|journal=Nature|language=en|volume=197|issue=4872|pages=1122–1123|doi=10.1038/1971122a0|issn=0028-0836}}</ref>


==Biology==
==Biology==

Revision as of 12:21, 24 May 2021

Morganucodon
Temporal range: Late Triassic-Middle Jurassic Rhaetian–Bathonian
Restoration of M. watsoni
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Clade: Synapsida
Clade: Therapsida
Clade: Cynodontia
Clade: Mammaliaformes
Order: †Morganucodonta
Family: †Morganucodontidae
Genus: †Morganucodon
Kühne, 1949
Type species
†Morganucodon watsoni
Kühne, 1949
Species
  • †M. watsoni Kühne, 1949
  • †M. oehleri Rigney, 1963
  • †M. heikuopengensis Young, 1980
  • †M. peyeri Clemens, 1980
  • †M. tardus Butler and Sigogneau-Russell, 2016[1]

Morganucodon ("Glamorgan tooth") is an early mammaliaform genus that lived from the Late Triassic to the Middle Jurassic. It first appeared about 205 million years ago. Unlike many other early mammaliaforms, Morganucodon is well represented by abundant and well preserved (though in the vast majority of cases disarticulated) material. Most of this comes from Glamorgan in Wales (Morganucodon watsoni), but fossils have also been found in Yunnan Province in China (Morganucodon oehleri) and various parts of Europe and North America. Some closely related animals (Megazostrodon) are known from exquisite fossils from South Africa.[2]

The name comes from a Latinization of Morganuc, "South Glamorgan in the Domesday Book", the county where it was discovered by Walter Georg Kühne,[3] giving the meaning "Glamorgan tooth".

History of discovery

In the summer of 1947, fieldwork was done at Duchy Quarry in Glamorgan in southern Wales. Grey conglomerate that formed fissure fill deposits within Carboniferous limestone was extracted. In 1949, Walter Georg Kühne noted the lower cheek tooth of a primitive mammal while examing samples of the rock. He named it Morganucodon watsoni, with the species name being in honour of D. M. S. Watson.[3] Additonal remains of M. watsoni were described by Kühne in 1958.[4] In August 1948, an expedition to Lufeng in Yunnan, China yielded a 1 in (2.5 cm) skull. It was shortly sent to Beijing (then Peking) and then eventually sent out of China, and deposited at University College London in 1960. The specimen was preliminarily described in 1963 by Harold W. Rigney, who noted the similarity to Morganucodon from Britain, and considered it cogeneric, naming the new species Morganucodon oehleri in honor of the reverend Edgar T. Oehler, who had originally collected the specimen.[5]

Biology

Skull and jaws of Morganucodon oehleri
Lower jaw of M. watsoni, Natural History Museum, London

Morganucodon was a small, plantigrade animal. The tail was moderately long. According to Kemp (2005), "the skull was 2–3 cm in length and a presacral body length of about 10 cm [4 inches]. In general appearance, it would have looked like a shrew or mouse".[6] There is evidence that it had specialized glands used for grooming, which may indicate that, like present day mammals, it had fur.[7]

Like present day mammals of similar size and presumed habit, Morganucodon was likely nocturnal and spent the day in a burrow. There is no direct fossil evidence, but several lines of evidence point to a nocturnal bottleneck in the evolution of the mammal class, and almost all modern mammals of similar size to Morganucodon are still nocturnal.[8][9] Likewise, burrowing was widespread both in non-mammalian cynodonts and in primitive mammals.[10][11] The logics of phylogenetic bracketing would make Morganucodon nocturnal and burrowing too. Plant material from the conifer Hirmeriella was also found in the fissure fills, indicating Morganucudon lived in, or near, a forested area.

The diet appears to have been insects and other small animals, with a preference for hard prey such as beetles.[12] Like most modern mammal insectivores, it grew fairly quickly to adult size. [13] Its eggs were probably small and leathery, a condition still found in monotremes.[14]

The teeth grew in mammalian fashion, with deciduous teeth being replaced by permanent teeth that were retained throughout the rest of the animal's life.[15] The combination of rapid growth in juveniles and a toothless stage at infancy strongly suggests that Morganucodon raised its young by lactation; indeed, it may have been among the first animals to do so.[16] The molars in the adult had a series of raised humps and edges that fit into each other, allowing for efficient chewing. However, unlike the situation in most later mammals, the upper and lower molars did not occlude properly when they first met; as they wore against each other, however, their shapes were modified by wear to produce a precise fit.[17]

A 2020 study suggests that the metabolism of Morganucodon was significantly slower than that of comparably sized modern mammals, and that it had a life-span more similar to that of reptiles.[18] Thus it likely did not possess the fully endothermic metabolism seen in current mammals.

Species

Species Author Year Status Temporal range Location Formations Notes & description
Morganucodon watsoni Kuehne 1949 Early Jurassic (Hettangian-Sinemurian) England, Wales Various fissure fill deposits
Morganucodon heikuopengensis Young 1978 Early Jurassic (Sinemurian) Yunnan, China Lufeng
Morganucodon oehleri Rigney 1963 Early Jurassic (Hettangian)
Morganucodon peyeri Clemens 1980 Late Triassic (Rhaetian) Switzerland, France Klettgau, grès infraliasiques (Saint-Nicolas-de-Port)
Morganucodon tardus Butler and Sigogneau-Russel 2016 Middle Jurassic (Bathonian) England Forest Marble

Classification

Life restoration of Morganucodon watsoni

Morganucodon is the type genus for the order Morganucodonta, a group of generally similar mammaliaforms known from the Late Triassic to Late Jurassic epochs,[19][20] with one possible member (Purbeckodon) dating to the Early Cretaceous.[21] All were small and likely insectivorous. Morganucodon is the best preserved and best understood member of Morganucodonta.

There is currently controversy about whether or not to classify Morganucodon as a mammal or as a non-mammalian mammaliaform. Some researchers limit the term "mammal" to the crown group mammals, which would not include Morganucodon and its relatives. Others, however, define "mammals", as a group, by the possession of a special, secondarily evolved jaw joint between the dentary and the squamosal bones, which has replaced the primitive one between the articular and quadrate bones in all modern mammalian groups. Under this definition, Morganucodon would be a mammal. Nevertheless, its lower jaw retains some of the bones found in its non-mammalian ancestors in a very reduced form rather than being composed solely of the dentary. Furthermore, the primitive reptile-like jaw joint between the articular and quadrate bones, which in modern mammals has moved into the middle ear and become part of the ear ossicles as malleus and incus, is still to be found in Morganucodon.[22] Morganucodon also suckled (it may have been the earliest animal to do so), had only two sets of teeth and grew rapidly to adult size and stopped growing thereafter, all typical mammalian traits.[23]

Phylogeny [24]
Mammaliaformes 

See also

References

  1. ^ Butler, P.M. and Sigogneau-Russell, D. 2016. Diversity of triconodonts in the Middle Jurassic of Great Britain. Palaeontologia Polonica 67, 35–65. LSID urn:lsid:zoobank.org: pub: C4D90BB6-A001-4DDB-890E-2061B4793992
  2. ^ Pages 21–33, 174 in Zofia Kielan-Jaworowska, Richard L. Cifelli, and Zhe-Xi Luo, Mammals from the Age of Dinosaurs: Origins, Evolution, and Structure, Columbia University Press, New York, 2004 ISBN 0-231-11918-6
  3. ^ a b Walter G. Kühne, "On a Triconodont tooth of a new pattern from a Fissure-filling in South Glamorgan", Proceedings of the Zoological Society of London, volume 119 (1949–1950) pages 345–350
  4. ^ Kühne, Walter Georg (1958-08-01). "Rhaetische Triconodonten aus Glamorgan, ihre Stellung zwischen den Klassen Reptilia und Mammalia und ihre Bedeutung für die REICHART'sche Theorie". Paläontologische Zeitschrift (in German). 32 (3): 197–235. doi:10.1007/BF02989032. ISSN 1236-9874. {{cite journal}}: Check |issn= value (help)
  5. ^ Rigney, Harold W. (1963-03). "A Specimen of Morganucodon from Yunnan". Nature. 197 (4872): 1122–1123. doi:10.1038/1971122a0. ISSN 0028-0836. {{cite journal}}: Check date values in: |date= (help)
  6. ^ Kemp T.S. 2005. The origin and evolution of mammals, Oxford University Press, page 143. ISBN 0-19-850760-7.
  7. ^ Ruben, J.A.; Jones, T.D. (2000). "Selective Factors Associated with the Origin of Fur and Feathers". American Zoologist. 40 (4): 585–596. doi:10.1093/icb/40.4.585.
  8. ^ Hall, M. I.; Kamilar, J. M.; Kirk, E. C. (24 October 2012). "Eye shape and the nocturnal bottleneck of mammals". Proceedings of the Royal Society B: Biological Sciences. 279 (1749): 4962–4968. doi:10.1098/rspb.2012.2258. PMC 3497252. PMID 23097513.
  9. ^ Muchlinski, Magdalena N. (June 2010). "A comparative analysis of vibrissa count and infraorbital foramen area in primates and other mammals". Journal of Human Evolution. 58 (6): 447–473. doi:10.1016/j.jhevol.2010.01.012. PMID 20434193.
  10. ^ Damiani, R.; Modesto, S.; Yates, A.; Neveling, J. (22 August 2003). "Earliest evidence of cynodont burrowing". Proceedings of the Royal Society B: Biological Sciences. 270 (1525): 1747–1751. doi:10.1098/rspb.2003.2427. PMC 1691433. PMID 12965004.
  11. ^ KIELAN, ZOFIA; GAMBARYAN, PETR P. (December 1994). "Postcranial anatomy and habits of Asian multituberculate mammals". Lethaia. 27 (4): 300. doi:10.1111/j.1502-3931.1994.tb01578.x.
  12. ^ Gill, Pamela G.; Purnell, Mark A.; Crumpton, Nick; Robson-Brown, Kate; Gostling, Neil J.; Stampanoni, M.; Rayfield, Emily J. (21 August 2014). "Dietary specializations and diversity in feeding ecology of the earliest stem mammals". Nature. 512 (7514): 303–305. doi:10.1038/nature13622. hdl:2381/29192. PMID 25143112. S2CID 4469841.
  13. ^ Chinsamy, A.; Hurum, J.H. (2006). "Bone microstructure and growth patterns of early mammals" (PDF). Acta Palaeontologica Polonica. 51 (2): 325–338. Retrieved 30 August 2013.
  14. ^ Parente, Raphael Câmara Medeiros; Bergqvist, Lílian Paglarelli; Soares, Marina Bento; Filho, Olimpio Barbosa Moraes (2011). "The history of vaginal birth". Archives of Gynecology and Obstetrics. 284 (1): 1–11. doi:10.1007/s00404-011-1918-6. PMID 21547459. S2CID 22997887.
  15. ^ Alexander F. H. van Nievelt and Kathleen K. Smith, "To replace or not to replace: the significance of reduced functional tooth replacement in marsupial and placental mammals", Paleobiology, Volume 31, Issue 2 (June 2005) pages 324–346
  16. ^ Kielan-Jaworowska, Zofia; Cifelli, Richard L.; Luo, Zhe-Xi (2004). Mammals from the age of dinosaurs : origins, evolution, and structure. New York: Columbia University Press. pp. 148–153. ISBN 978-0231119184.
  17. ^ Crompton, A. W.; Jenkins, F. Jr. (1968). "Molar occlusion in late Triassic mammals". Biological Reviews. 43 (4): 427–458. doi:10.1111/j.1469-185x.1968.tb00966.x. PMID 4886687. S2CID 1044399.
  18. ^ Newham, Elis; et al. (2020). "Reptile-like physiology in Early Jurassic stem-mammals". Nature Communications. 11 (1): 5121. doi:10.1038/s41467-020-18898-4.
  19. ^ Martin, T.; Averianov, A. O.; Jäger, K. R. K.; Schwermann, A. H.; Wings, O. (2019). "A large morganucodontan mammaliaform from the Late Jurassic of Germany" (PDF). Fossil Imprint. 75 (3–4): 504–509. doi:10.2478/if-2019-0030.
  20. ^ pages 511–512, Malcolm C. McKenna and Susan K. Bell, Classification of Mammals Above the Species Level, Columbia University Press, 1997. ISBN 0-231-11012-X
  21. ^ P. M. Butler, D. Sigogneau-Russell and P. C. Ensom (2011). "Possible persistence of the morganucodontans in the Lower Cretaceous Purbeck Limestone Group (Dorset, England)". Cretaceous Research. 33: 135–145. doi:10.1016/j.cretres.2011.09.007.
  22. ^ Kermack, K. A.; Mussett, Frances; Rigney, H. W. (1981). "The skull of Morganucodon". Zoological Journal of the Linnean Society. 71: 1–158. doi:10.1111/j.1096-3642.1981.tb01127.x.
  23. ^ Mammals of the Mesozoic: The least mammal-like mammals
  24. ^ Close, Roger A.; Friedman, Matt; Lloyd, Graeme T.; Benson, Roger BJ (2015). "Evidence for a mid-Jurassic adaptive radiation in mammals". Current Biology. 25 (16): 2137–2142. doi:10.1016/j.cub.2015.06.047. PMID 26190074.
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