Myllokunmingia
| Myllokunmingia Temporal range: Atdabanian[1]
| |
|---|---|
| Holotype fossil | |
| Restoration | |
| Scientific classification | |
| Kingdom: | Animalia |
| Phylum: | Chordata |
| Infraphylum: | Agnatha |
| Order: | †Myllokunmingiida |
| Family: | †Myllokunmingiidae |
| Genus: | †Myllokunmingia Shu, Zhang & Han, 1999 |
| Species: | †M. fengjiaoa
|
| Binomial name | |
| †Myllokunmingia fengjiaoa Shu, Zhang & Han, 1999
| |
Myllokunmingia is an extinct genus of primitive jawless fish that lived in during the Cambrian period, approximately 518 million years ago, in what is now the Yunnan Province of China. It was discovered alongside Haikouichthys, another genus of primitive jawless fish, in 1999 and is considered to be among the earliest known vertebrate animals in the fossil record. The holotype of the type species, Myllokunmingia fengjiaoa — and the only uncontroversial specimen thereof — was found in the Yuanshan member of the Qiongzhusi Formation in the Eoredlichia Zone near Haikou at Ercaicun, Kunming City, Yunnan, China.[2]
Description
The holotype is 28 mm long and 6 mm high. The animal has a distinct head and body with a forward, sail-like (1.5 mm) dorsal fin and a ventral fin fold further back (probably paired). The head has five or six gill pouches with hemibranchs. In the body, there are 25 muscle segments (myomeres) with rearward-facing, double-V-shaped chevrons. There is a notochord, a pharynx and a digestive tract that may run all the way to the rear tip of the animal. A mouth cannot be clearly identified. There may be a pericardial cavity. There are no fin radials. The tip of the tail in the holotype is buried in sediment.[2]
Taxonomy
Although typically treated as a distinct taxon, there has been considerable uncertainty on the assignment of this name with respect to other myllokunmingiid specimens.
Hou and colleagues in 2002 argued that Haikouichthys is a subjective junior synonym of this taxon (using the principle of the first reviser due to the two taxa being described on the same date) on the basis of the apparent presence of fin rays in Haikouichthys specimens being lithological artifacts, the gill structures missing from specimens referred to both genera being present in the specimen they studied, and the argued triviality of the difference in shapes between them.[3] However, subsequent studies led by the British paleontologist Simon Conway Morris identified both genera to be distinct on the basis of different gill arrangement,[4] the absence of branchial rays in Myllokunmingia and the myomeres having a more acute shape in Haikouichthys.[5]
Nevertheless, Hou et al. in 2017 in their book, The Cambrian Fossils of Chengjiang, China, suggested that specimens referred to Myllokunmingia, Haikouichthys and Zhongjianichthys may be taphonomic variants (i.e., of the same animal but in different states of decay) and due to what they argue to be the lack of certainty in the reliability of the distinguishing characters between the three taxa, they follow the opinion of Hou et al., 2002, and use Myllokunmingia for all of them.[6]
See also
References
- ^ Yang, C.; Li, X.-H.; Zhu, M.; Condon, D. J.; Chen, J. (2018). "Geochronological constraint on the Cambrian Chengjiang biota, South China" (PDF). Journal of the Geological Society. 175 (4): 659–666. Bibcode:2018JGSoc.175..659Y. doi:10.1144/jgs2017-103. ISSN 0016-7649. S2CID 135091168.
- ^ a b Shu, D-G.; Luo, H-L.; Conway Morris, S.; Zhang, X-L.; Hu, S-X.; Chen, L.; Han, J.; Zhu, M.; Li, Y.; Chen, L-Z. (1999). "Lower Cambrian vertebrates from south China". Nature. 402 (6757): 42. Bibcode:1999Natur.402...42S. doi:10.1038/46965. S2CID 4402854.
- ^ Hou, X.-G.; Aldridge, R. J.; Siveter, D. J.; Feng, X.-H. (2002). "New evidence on the anatomy and phylogeny of the earliest vertebrates". Proc Biol Sci. 269 (1503): 1865–1869. doi:10.1098/rspb.2002.2104. PMC 1691108. PMID 12350247.
- ^ Conway Morris, S. (29 June 2006). "Darwin's dilemma: the realities of the Cambrian 'explosion'". Philosophical Transactions of the Royal Society B: Biological Sciences. 361 (1470): 1069–1083. doi:10.1098/rstb.2006.1846. PMC 1578734. PMID 16754615.
- ^ Conway Morris, Simon; Caron, Jean-Bernard (2012). "Pikaia gracilens Walcott, a stem-group chordate from the Middle Cambrian of British Columbia". Biological Reviews. 87 (2): 480–512. doi:10.1111/j.1469-185X.2012.00220.x. PMID 22385518. S2CID 27671780.
- ^ Hou, Xian-guang; Siveter, David J.; Siveter, Derek J.; Aldridge, Richard J.; Cong, Pei-yun; Gabbott, Sarah E.; Ma, Xiao-ya; Purnell, Mark A.; Williams, Mark (2017-04-12). The Cambrian Fossils of Chengjiang, China: The Flowering of Early Animal Life (1 ed.). Wiley. doi:10.1002/9781118896372.ch24. ISBN 978-1-118-89638-9.
External links
- http://www.sciencenews.org/sn_arc99/11_6_99/fob1.htm Archived 2013-05-24 at the Wayback Machine
- https://web.archive.org/web/20030511135309/http://www.gs-rc.org/repo/repoe.htm
- Lower Cambrian vertebrates from south China
- Oldest fossil fish caught