Biology:Hylonomus
| Hylonomus | |
|---|---|
| |
| Model | |
Scientific classification 
| |
| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Class: | Reptilia |
| Clade: | Eureptilia |
| Genus: | †Hylonomus Dawson, 1860 |
| Type species | |
| †Hylonomus lyelli Dawson, 1860
| |
Hylonomus (/haɪˈlɒnəməs/; hylo- "forest" + nomos "dweller")[1] is an extinct genus of reptile that lived 312 million years ago during the Late Carboniferous period.[2] It is the earliest unquestionable reptile (Westlothiana is older, but in fact it may have been an amphibian, and Casineria is rather fragmentary). The only species is the type species Hylonomus lyelli. Despite being amongst the oldest known reptiles, it is not the most primitive member of group, being a eureptile more derived than either parareptiles or captorhinids.
Description
Hylonomus was 20–25 centimetres (8–10 in) long (including the tail). Most of them are 20 cm long and probably would have looked rather similar to modern lizards. It had small sharp teeth and it likely ate small invertebrates such as millipedes or early insects.[3] They are also described to have slender and lightweight leg and arm bones, as well as long and slim hands and feet. A narrow and tongue-shaped part in the roof of the mouth, a deep groove on a certain bone in the skull, a bumpy structure on the back bones, changes in the height of certain back bone parts, having a hole in a specific place on the skull, having arm and leg bones that are the same length, having a short fourth toe bone compared to the shin bone, having a short fifth toe bone compared to the fourth toe bone, having long neck bones, and having a well-developed opening below the eye. [4]
Fossils of Hylonomus have been found in the remains of fossilized club moss stumps in the Joggins Formation, Joggins, Nova Scotia, Canada. It is supposed that, after harsh weather, the club mosses would crash down, with the stumps eventually rotting and hollowing out. Small animals such as Hylonomus, seeking shelter, would enter and become trapped, starving to death. An alternative hypothesis is that the animals made their nests in the hollow tree stumps.[5]
Fossils of the basal pelycosaur Archaeothyris and the basal diapsid Petrolacosaurus are also found in the same region of Nova Scotia, although from a higher stratum, dated approximately 6 million years later.[2]
Fossilized footprints found in New Brunswick have been attributed to Hylonomus, at an estimated age of 315 million years.[6]
This animal was discovered by John William Dawson in the mid-19th century.[7] The species' name was given it by Dawson's teacher, the geologist Sir Charles Lyell. While it has traditionally been included in the group Protorothyrididae, it has since been recovered outside this group.[8][9]
Hylonomus lyelli was named the Provincial Fossil of Nova Scotia in 2002.[10]
References
- ↑ Genus Hylonomus Etymology
- ↑ 2.0 2.1 van Tuinen, Marcel; Elizabeth A. Hadly (2004). "Error in Estimation of Rate and Time Inferred from the Early Amniote Fossil Record and Avian Molecular Clocks". Journal of Molecular Evolution 59 (2): 267–276. doi:10.1007/s00239-004-2624-9. PMID 15486700. Bibcode: 2004JMolE..59..267V. http://www.stanford.edu/group/hadlylab/pdfs/vantuinenhadlyJME04.pdf. Retrieved 2009-09-02.
- ↑ Palmer, D., ed (1999). The Marshall Illustrated Encyclopedia of Dinosaurs and Prehistoric Animals. London: Marshall Editions. p. 62. ISBN 978-1-84028-152-1.
- ↑ Muller, J.; Reisz, R.R. (2006). "The phylogeny of early eureptiles: Comparing parsimony and Bayesian approaches in the investigation of a basal fossil clade". Systematic Biology. 55 (3): 503–511. doi:10.1080/10635150600755396. PMID 16861212.
- ↑ McGhee, George R. Jr. (12 November 2013). When the Invasion of Land Failed: The Legacy of the Devonian Extinctions. Columbia University Press. pp. 254–5. ISBN 978-0-231-16057-5. https://books.google.com/books?id=wFqrAgAAQBAJ&pg=PA254. Retrieved 10 June 2015.
- ↑ Falcon-Lang, H.J., Benton, M.J. & Stimson, M. (2007): Ecology of early reptiles inferred from Lower Pennsylvanian trackways. Journal of the Geological Society, London, 164; no. 6; pp 1113-1118. article
- ↑ J. W. Dawson. 1860. On a Terrestrial Mollusk, a Chilognathous Myriapod, and some New Species of Reptiles, from the Coal-Formation of Nova Scotia. Quarterly Journal of the Geological Society of London 16:268-277
- ↑ Muller, J.; Reisz, R.R. (2006). "The phylogeny of early eureptiles: Comparing parsimony and Bayesian approaches in the investigation of a basal fossil clade". Systematic Biology 55 (3): 503–511. doi:10.1080/10635150600755396. PMID 16861212.
- ↑ Ford, David P.; Benson, Roger B. J. (January 2020). "The phylogeny of early amniotes and the affinities of Parareptilia and Varanopidae" (in en). Nature Ecology & Evolution 4 (1): 57–65. doi:10.1038/s41559-019-1047-3. ISSN 2397-334X. PMID 31900445. https://www.nature.com/articles/s41559-019-1047-3.
- ↑ "Provincial Fossil Act". https://nslegislature.ca/sites/default/files/legc/statutes/provfoss.htm.
External links
- Fossils of Nova Scotia - The Tree Stump Animals
- Transitional Vertebrate Fossils FAQ Part 1B
- Early Researchers & Finds of the Joggins Fossil Cliffs
- The Science of the Joggins Fossil Cliffs
- Hylonomus: Provincial Fossil of Nova Scotia
- A photograph of the disarticulated skeleton, credited to J. Calder
- Another photo of the specimen, from Dr. Melissa Grey's twitter account
Wikidata ☰ Q132458 entry
 |  |
