Canadaspis

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Canadaspis
Temporal range: Cambrian Stage 3–Wuliuan
Canadaspis perfecta USNM 57703.jpg
Specimen of Canadaspis perfecta from the Burgess Shale
Canadaspis laevigata.png
Life restoration of Canadaspis laevigata
Scientific classification e
Kingdom: Animalia
Phylum: Arthropoda
Order: †Hymenocarina
Family: †Canadaspididae
Genus: †Canadaspis
Briggs, 1978
Species
  • C. perfecta Briggs, 1978 (type)
  • Hou and Bergström, 1991 C. laevigata

Canadaspis ("Shield of Canada") is an extinct genus of bivalved Cambrian arthropod, known from North America and China. They are thought to have been benthic feeders that moved mainly by walking and possibly used its biramous appendages to stir mud in search of food. They have been placed within the Hymenocarina, which includes other bivalved Cambrian arthropods.

Description

Diagrammatic reconstruction of C. perfecta

The bivalved carpaces of Canadaspis perfecta are typically 8–52 millimetres (0.31–2.05 in) in length, which taper towards the front end. There are a small pair of eyes borne on short stalks. The body has 8 abdominal and 7 thorax segments, which terminate with a spined telson. The abdominal segments have 10 associated pairs of segmented biramous limbs.[1]

Canadaspis had claws on the end of its frontal appendages which may have been used to stir up sediment, or to scrape off the top layer,[2] which may have been a nutritious layer of microbes. Large particles it stirred up would have been captured by spines on the inside of its legs; these spines would have directed the food particles to the organism's mouth, where it used its mandibles to grind larger particles.[2]

Its antennae served a sensory function.[2] Spines on its head probably served to protect its vulnerable eyes from predators.[2] Its limbs probably moved in sequence to produce a rippling motion. Although Canadaspis probably did not swim, this could have helped propel the organism from under soft sediments. The appendages also produced currents which would have helped with feeding and respiration.[2]

Members of the species Canadaspis perfecta appear to have engaged in synchronised group moulting.[3]

Classification

Three alternatives exist for Canadaspis's classification. They concern its relationship to the crustacea; it was originally thought that it falls within that clade, but this no longer appears to be the case.[4] The alternatives are that it is a stem group crustacean, but others believe it is more basal still, falling in the base of the Euarthropoda.[5] It is currently thought to be a member of the group Hymenocarina, which are interpreted as mandibulate stem-crustaceans.[6]

Fossil occurrences

4525 specimens of Canadaspis are known from the Greater Phyllopod bed, where they comprise 8.6% of the community.[7] Canadapsis perfecta, the type species, comes from the Cambrian-age Burgess Shale in British Columbia, Canada. Canadaspis are also found in different formations of the House Range of western Utah[8] as well as the Pioche Shale of Nevada.[5] Canadaspis laevigata, coming from the Chengjiang biota and thus some 10 million years older than Canadapsis perfecta,[9] is an equivocal member of the genus. Some scientists believe Canadaspis laevigata to be a more primitive Crustaceomorpha antecedent of Canadaspis, and others consider it a bi-valved arthropod of uncertain affinity.

References

  1. ^ "Canadaspis perfecta". The Burgess Shale. Royal Ontario Museum. Retrieved 2022-10-28.
  2. ^ a b c d e Briggs, D. (1978). "The morphology, mode of life, and affinities of Canadaspis perfecta (Crustacea: Phyllocarida), Middle Cambrian, Burgess Shale, British Columbia". Phil. Trans. R. Soc. Lond. B. 281 (984): 439–487. doi:10.1098/rstb.1978.0005.
  3. ^ Haug, Joachim T; Caron, Jean-Bernard; Haug, Carolin (December 2013). "Demecology in the Cambrian: synchronized molting in arthropods from the Burgess Shale". BMC Biology. 11 (1): 64. doi:10.1186/1741-7007-11-64. ISSN 1741-7007. PMC 3685569. PMID 23721223.
  4. ^ Butterfield, N.J. (2002). "Leanchoilia guts and the interpretation of three-dimensional structures in Burgess Shale-type fossils". Paleobiology. 28 (1): 155–171. doi:10.1666/0094-8373(2002)028<0155:LGATIO>2.0.CO;2.
  5. ^ a b Lieberman, B.S. (2003). "A new soft-bodied fauna: the Pioche Formation of Nevada". Journal of Paleontology. 77 (4): 674–690. doi:10.1666/0022-3360(2003)077<0674:ANSFTP>2.0.CO;2.
  6. ^ Vannier, Jean; Aria, Cédric; Taylor, Rod S.; Caron, Jean-Bernard (2018). "Waptia fieldensis Walcott, a mandibulate arthropod from the middle Cambrian Burgess Shale". Royal Society Open Science. 5 (6): 172206. Bibcode:2018RSOS....572206V. doi:10.1098/rsos.172206. PMC 6030330. PMID 30110460.
  7. ^ Caron, Jean-Bernard; Jackson, Donald A. (October 2006). "Taphonomy of the Greater Phyllopod Bed community, Burgess Shale". PALAIOS. 21 (5): 451–65. doi:10.2110/palo.2003.P05-070R. JSTOR 20173022.
  8. ^ Briggs, D.E.G.; Lieberman, B.S.; Hendricks, J.R.; Halgedahl, S.L.; Jarrard, R.D. (2008). "Middle Cambrian arthropods from Utah". Journal of Paleontology. 82 (2): 238–254. doi:10.1666/06-086.1.
  9. ^ HOU, X; J. BERGSTRÖM (1991). "The arthropods of the Lower Cambrian Chengjiang fauna, with relationships and evolutionary significance". In A. M. Simonetta; S. Conway Morris (eds.). The Early Evolution of Metazoa and the Significance of Problematic Taxa. Cambridge: Cambridge University Press. pp. 179–187. ISBN 0-521-40242-5.

External links

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