Biology:Haikouella

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Short description: Extinct genus of Cambrian organisms


Haikouella
Temporal range: Cambrian Stage 3, 518 Ma[1]
Haikouella NT.jpg
Artist's restoration of Haikouella lanceolata.
Scientific classification e
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Infraphylum: Agnatha
Family: Haikouellidae
Genus: Haikouella
Type species
Haikouella lanceolata
Chen, Huang & Li, 1999[2]
Other species
  • H. jianshanensis

Haikouella is an agnathan chordate from the Lower Cambrian Maotianshan Shales of Chengjiang County in Yunnan Province, China . An analysis in 2015 placed Haikouella as a junior synonym of Yunnanozoon, another Maotianshan shale Cambrian chordate.[3][4]

It is similar to the form Yunnanozoon,[5] which is possibly a hemichordate.[6] Still, there are anatomical differences from Yunnanozoon, including a larger stomach and smaller (0.1 mm) pharyngeal teeth. Haikouella does not have bones or a movable jaw, but it otherwise resembles vertebrates. Haikouichthys and Myllokunmingia, which seem to share significant fish-like characters, have been found in the same beds. Suspected hemichordates are also known from these deposits as well as from the Middle Cambrian Burgess Shale of British Columbia. Other than possible fish scales/plates from the Upper Cambrian of Wyoming and conodonts, teeth plates of extinct Agnatha, these Chinese fish-like chordates are one of the only known pre-Ordovician craniates.

Haikouella lanceolata fossil from Chengjiang, China.
Haikouella lanceolata fossil from the Chlupáč Museum, Prague.

Haikouella is known from 305 specimens mostly from a single bed in the Maotianshan Shales. The animal is 20 to 30 mm (40 mm max) in length and has a head, gills, brain, notochord, well developed musculature, heart and circulatory system. It has a bent caudal projection of the notochord that might be a primitive tail fin. It might have a pair of lateral eyes. Very small (0.1 mm) structures that are probably pharyngeal teeth are present in the body cavity. A few specimens display dorsal and ventral fins.

There are two known species, the type species, H. lanceolata, and H. jianshanensis.[7]

References

  1. Yang, C.; Li, X.-H.; Zhu, M.; Condon, D. J.; Chen, J. (2018). "Geochronological constraint on the Cambrian Chengjiang biota, South China" (in en). Journal of the Geological Society 175 (4): 659–666. doi:10.1144/jgs2017-103. ISSN 0016-7649. Bibcode2018JGSoc.175..659Y. http://nora.nerc.ac.uk/id/eprint/521412/1/2018-JGS-Chuan%20Yang%20et%20al.pdf. 
  2. Chen, J.-Y.; Huang, D.-Y.; Li, C.-W. (1999). "An early Cambrian craniate-like chordate". Nature 402 (6761): 518–522. doi:10.1038/990080. Bibcode1999Natur.402..518C. 
  3. Cong, Pei-Yun; Hou, Xian-Guang; Aldridge, Richard J.; Purnell, Mark A.; Li, Yi-Zhen (2015). Smith, Andrew. ed. "New data on the palaeobiology of the enigmatic yunnanozoans from the Chengjiang Biota, Lower Cambrian, China" (in en). Palaeontology 58 (1): 45–70. doi:10.1111/pala.12117. https://onlinelibrary.wiley.com/doi/10.1111/pala.12117. 
  4. Tian, Qingyi; Zhao, Fangchen; Zeng, Han; Zhu, Maoyan; Jiang, Baoyu (2022-07-08). "Ultrastructure reveals ancestral vertebrate pharyngeal skeleton in yunnanozoans" (in en). Science 377 (6602): 218–222. doi:10.1126/science.abm2708. ISSN 0036-8075. PMID 35857544. Bibcode2022Sci...377..218T. https://www.science.org/doi/10.1126/science.abm2708. 
  5. Chen, J.-Y. (2009). "The sudden appearance of diverse animal body plansduring the Cambrian explosion". The International Journal of Developmental Biology 53 (5–6): 733–751. doi:10.1387/ijdb.072513cj. PMID 19557680. 
  6. Shu, D.; X. Zhang; L. Chin (4 April 1996). "Reinterpretation of Yunnanozoon as the earliest known hemichordate". Nature 380 (6573): 428–430. doi:10.1038/380428a0. Bibcode1996Natur.380..428S. 
  7. Shu, D. et al. (2003). "A new species of Yunnanozoan with implications for deuterostome evolution". Science 299 (5611): 1380–1384. doi:10.1126/science.1079846. PMID 12610301. 

External links

Wikidata ☰ Q2532425 entry