Oligokyphus

Oligokyphus
Temporal range: Late Triassic–Early Jurassic
life restoration of Oligokyphus
Scientific classification
Kingdom: Animalia
Phylum: Chordata
Clade: Synapsida
Order: Therapsida
Suborder: Cynodontia
Family: †Tritylodontidae
Genus: †Oligokyphus
Type species
Oligokyphus triserialis
Hennig E, 1922
Species
  • †O. triserialis Hennig E, 1922
  • †O. major Kühne WG, 1956
  • †O. lufengensis Luo Z & Sun A, 1993
  • †O. sp. Sues H-D, 1985
Synonyms
  • Chalepotherium plieningeri
  • Mucrotherium
  • Uniserium

Oligokyphus was an advanced herbivorous cynodont of the late Triassic to early Jurassic periods. Originally considered to be an early mammal, it is now classified as a Mammaliamorph (nearly a mammal) because Oligokyphus does not have the mammalian jaw attachments and it retains a vestigial joint between the quadrate bone and the squamosal bone in the skull.

Description

Oligokyphus (meaning "small curved animal"), was a small animal, around 50 centimetres (20 in) in length, belonging to the herbivorous Tritylodontidae family. It resembled a weasel in appearance, with a long and slim body. Oligokyphus was found widely across North America, Europe and China.

Skull and jaw

The teeth of the upper and lower jaw contain bump rows that fit together perfectly in order to maintain an accurate bite. Oligokyphus had a face similar to that of modern mammals, although there were differences in the cheekbones and eye sockets. It had a bony secondary palate and double-rooted cheek teeth. Unlike mammals, the teeth of Oligokyphus did not occlude. The jaw was double jointed, and the neck was flexible, with an atlas and axis and a double occipital condyle.

The teeth were different from those of related cynodonts; there were no canine teeth, and unusually large, rodent-like incisors. There is a large gap, or diastema, separating the cheek teeth from the incisors. The lower jaw of these animals moved back and forth when the mouth was shut so that the food could be chopped up. Oligokyphus had no premaxilla, but did have a lateral extension of the maxilla.

While the postcanines in non-mammalians, such as Oligokyphus, are difficult to differentiate from canines, the lower postcanines of Oligokyphus (also considered to be pre-molars) are defining from other Tritylodonts. On lower postcanine teeth of Trityldonts, two cusps can be found per row; however, Oligokyphus have two rows with three cusps in each row.[1] These cusps, specific to Oligokyhpus Tritylodonts, allowed for a well-fitting bite that was particularly good at shredding plant material dense in fiber. The foremost incisors are similar to those of today's rodents, extremely intensified and enlarged. The typical location of canine teeth is left empty with Oligokyphus. Instead, a gap is inserted in this area of the jaw as Oligokyphus lack the teeth commonly known as canines.[2]

Cladistics

Oligokyphus is in the family Trityledontidae. The family is named after the shape of their teeth. Trityledontidae means "three knob teeth". The members of this family were all small to medium-sized advanced synapsids with combined specialized structures for herbivorous eating. They were the last members of the non-mammalian synapsids. The first Trityledont was found in South Africa in upper Jurassic rocks. It was first thought to be one of the earliest mammals. This classification has since been adjusted. These non-mammals became progressively more mammal-like. They are now classified as the closest relatives to the mammals and this is supported by their high, flat, crested jaw, large zygomatic arches, well developed secondary palate, and specialized dentition.

There have also been comparisons between the cranial nerves of Trityledonts and mammals. The shoulder girdle and forelimb structures were suggestive of digging animals. These animals were extremely active and burrowed in leaf litter and dirt, which suggests characteristics of rodents and rabbits. They naturally had a metabolism that was partially or completely endothermic. They were thought to be driven out by relatives such as mammals competing for the same ecological niches. Another reason that this animal could have gone extinct was due to new plant development. Some flowering plants, or angiosperms, could have been detrimental to these animals since they may not have been used to eating new plants.

Oligokyphus is placed into the subgroup Probainognathia. This forms a monophyletic group with the tritheledontid Pachygenelus.

Fossil finds

Though Oligokyphus is very widespread, it was not until 1953 that representatives of this group were found. Information was first collected from the Kayenta Formation on Comb Ridge in northeastern Arizona. Numerous specimens of Oligokyphus were obtained by Harvard University and the Museum of Northern Arizona in the "Silty Facies". Many fossils have also been found throughout the UK, Germany and China. Some very small fragment remains have also been found in Antarctica. By these fossil records, one can see that Oligokyphus have a vertical humerus and a minor trochanter. This broad distribution indicates that there were no barriers to separate this terrestrial vertebrate.

Paleoecology

Habitat

Oligokyphus were small tetrapod, terrestrial animals. They have long been considered as mammaliomorphs, a link between reptiles and mammals. It is believed these animals were primarily land dwelling, living amongst small shrubs or bushes. It is also thought that Oligokyphus fed on seeds or nuts, as their teeth resemble those of modern animals that also feed on seeds and nuts.[2] It is rather difficult to estimate the social behaviors of Oligokyphus as most of it does not preserve in the fossil record. However, considering the conditions on the planet during the times that Oligokyphus was alive and thriving (late Triassic and early Jurassic) and also the locations of which fossils of these animals were found, some educated predictions can be made about their metabolism and feeding habits. Oligokyphus, with its conveniently placed leg and hip structures, likely was quick-moving and fed off of low-lying plant life. With its long weasel-like body, it may have even been possible for Oligokyphus to reach higher vegetation simply by standing on its hind legs. It probably had good use of its hands to manipulate seeds and other digestively pleasing foods. There has not been any support showing Oligokyphus had the ability to climb vertically, as some rodents are capable of doing today.

A definitive radiometric dating of the area preserved in the formation where Oligokyphus lived has not yet been made, and the available stratigraphic correlation has been based on a combination of radiometric dates from vertebrate fossils, magnetostratigraphy and pollen evidence.[3] It has been surmised that the Kayenta Formation was deposited during the Sinemurian and Pliensbachian stages of the Early Jurassic Period or approximately 199 to 182 million years ago.[4] This formation is part of the Glen Canyon Group that includes formations not only in northern Arizona but also parts of southeastern Utah, western Colorado, and northwestern New Mexico. The formation was primarily deposited by rivers. During the Early Jurassic period, the land that is now the Kayenta Formation experienced rainy summers and dry winters. By the Middle Jurassic period it was being encroached upon from the north by a sandy dune field that would become the Navajo Sandstone.[5] The animals here were adapted to a seasonal climate and abundant water could be found in streams, ponds and lakes.

Paleofauna

Oligokyphus lived beneath the feet of dinosaurs, such as the theropods Dilophosaurus, Kayentavenator[6] Megapnosaurus kayentakatae, the "Shake N Bake" theropod, the basal sauropodomorph Sarahsaurus,[7]heterodontosaurids, and the armored dinosaurs Scelidosaurus and Scutellosaurus. The Kayenta Formation has produced that remains of three coelophysoid taxa of different body size, which represents the most diverse ceratosaur fauna yet known.[8] The Kayenta Formation has yielded a small but growing assemblage of organisms. Vertebrates present here at the time of Oligokyphus included hybodont sharks, bony fish known as osteichthyes, lungfish, salamanders, the frog Prosalirus, the caecilian Eocaecilia, the turtle Kayentachelys, a sphenodontian reptile, various lizards. Also present were the synapsids Dinnebiton and Kayentatherium,[9] several early crocodylomorphs including Calsoyasuchus, Eopneumatosuchus, Kayentasuchus, and Protosuchus), and the pterosaur Rhamphinion.[9][10][11][12] The possible presence of the early true mammal Dinnetherium, and a haramyid mammal has also been proposed, based on fossil finds.[10] Vertebrate trace fossils from this area included coprolites[13] and the tracks of therapsids, lizard-like animals, and dinosaurs, which provided evidence that these animals were also present.[14] Non-vertebrates in this ecosystem included microbial or "algal" limestone,[13] freshwater bivalves, freshwater mussels and snails,[5] and ostracods.[15] The plant life known from this area included trees that became preserved as petrified wood.[11]

Parental care

There is a good possibility that Oligokyphus had parental care. This is assumed to be true because of the transitional state Oligokyphus was in from reptiles to mammalian. Today most mammals and some reptiles show parental care to their young. This makes a good argument to the possibility of parental care with Oligokyphus, but with all prehistoric creatures, behavioral studies always have a great deal of uncertainty.

References

  1. ↑ Trevor Dykes. "JURASSIC CYNODONTS; Tritylodontidae, an internet directory". Retrieved June 2012.
  2. 1 2 Sovak, J. 1999. Before the Dinosaurs (Coloring Book). Dover Publications. p.43 ISBN 0-486-40568-0
  3. ↑ J. M. Clark and D. E. Fastovsky. 1986. Vertebrate biostratigraphy of the Glen Canyon Group in northern Arizona. The Beginning of the Age of the Dinosaurs: Faunal change across the Triassic-Jurassic boundary, N. C. Fraser and H.-D. Sues (eds.), Cambridge University Press 285–301
  4. ↑ Padian, K (1997) Glen Canyon Group In: Encyclopedia of Dinosaurs, edited by Currie, P. J., and Padian, K., Academic Press.
  5. 1 2 Harshbarger, J. W.; Repenning, C. A.; Irwin, J. H. (1957). Stratigraphy of the uppermost Triassic and the Jurassic rocks of the Navajo country. Professional Paper 291. Washington, D.C.: U.S. Geological Survey.
  6. ↑ Gay, R. 2010. Kayentavenator elysiae, a new tetanuran from the early Jurassic of Arizona. Pages 27–43 in Gay, R. Notes on early Mesozoic theropods. Lulu Press (on-demand online press).
  7. ↑ Rowe, T. B., Sues, H.-D., and Reisz, R. R. 2011. Dispersal and diversity in the earliest North American sauropodomorph dinosaurs, with a description of a new taxon. Proceedings of the Royal Society B: Biological Sciences 278(1708):1044–1053.
  8. ↑ Tykoski, R. S., 1998, The Osteology of Syntarsus kayentakatae and its Implications for Ceratosaurid Phylogeny: Theses, The University of Texas, December 1998.
  9. 1 2 Jenkins, F. A., Jr., Crompton, A. W., and Downs, W. R. 1983. Mesozoic mammals from Arizona: new evidence in mammalian evolution. Science 222(4629):1233–1235.
  10. 1 2 Lucas, S. G.; Heckert, A. B.; Tanner, L. H. (2005). "Arizona's Jurassic fossil vertebrates and the age of the Glen Canyon Group". In Heckert, A. B.; and Lucas, S. G. editors. Vertebrate paleontology in Arizona. Bulletin 29. Albuquerque, NM: New Mexico Museum of Natural History and Science. pp. 95–104.
  11. 1 2 Jenkins, F. A., Jr. and Shubin, N. H. 1998. Prosalirus bitis and the anuran caudopelvic mechanism. Journal of Vertebrate Paleontology 18(3):495–510.
  12. ↑ Curtis, K., and Padian, K. 1999. An Early Jurassic microvertebrate fauna from the Kayenta Formation of northeastern Arizona: microfaunal change across the Triassic-Jurassic boundary. PaleoBios 19(2):19–37.
  13. 1 2 Luttrell, P. R., and Morales, M. 1993. Bridging the gap across Moenkopi Wash: a lithostratigraphic correlation. Aspects of Mesozoic geology and paleontology of the Colorado Plateau. Pages 111–127 in Morales, M., editor. Museum of Northern Arizona, Flagstaff, AZ. Bulletin 59.
  14. ↑ Hamblin, A. H., and Foster, J. R. 2000. Ancient animal footprints and traces in the Grand Staircase-Escalante National Monument, south-central Utah. Pages 557–568 in Sprinkel, D. A., Chidsey, T. C., Jr., and Anderson, P. B. editors. Geology of Utah's parks and monuments. Utah Geological Association, Salt Lake City, UT. Publication 28.
  15. ↑ Lucas, S. G., and Tanner L. H. 2007. Tetrapod biostratigraphy and biochronology of the Triassic-Jurassic transition on the southern Colorado Plateau, USA. Palaeogeography, Palaeoclimatology, Palaeoecology 244(1–4):242–256.

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