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Odaraia alata

An arthropod that looks like a submarine

3D animation of Odaraia alata.

ANIMATION BY PHLESCH BUBBLE © ROYAL ONTARIO MUSEUM

Taxonomy:

Kingdom: Animalia
Phylum: Arthropoda
Higher Taxonomic assignment: Hymenocarines, Family Odaraiidae
Species name: Odaraia alata
Remarks:

Odaraia was originally considered a crustacean (Walcott 1912; Briggs 1981; Briggs and Fortey 1989; Hou and Bergstrom 1997; Wills et al. 1998), following previous interpretations on the affinities of other bivalved arthropods (hymenocarines), like Branchiocaris (Briggs 1976) or Canadaspis (Briggs 1978). In the early 2000s, the affinities of Odaraia were re-evaluated and placed in the stem lineage of arthropods (Budd 2002, 2008). Following the discovery of mandibles in several hymenocarines and the re-interpretation of this group as early mandibulate arthropods (which include myriapods, crustaceans and insects), Odaraia was moved to the stem of mandibulates (Aria and Caron 2017; Vannier et al. 2018), and was perhaps even more closely related to myriapods (Aria et al. 2021). Odaraia gives its name to the family Odaraiidae, a group of hymenocarines with highly multisegmented bodies, reduced or absent antennulae and highly multisegmented legs, which includes other Burgess Shale taxa such as Nereocaris or Fibulacaris.

Described by: Walcott
Description date: 1912
Etymology:

Odaraia – from Odaray Mountain (3,159 m) in Yoho Park, which was named by J. J. McArthur in 1887 from the Stoney First Nation Nakoda expression for “many waterfalls.”

alata – from the Latin ala, “wing,” referring to the wing-like fins of the tail.

Type Specimens: Lectotype –USNM57722 (O. alata) in the National Museum of Natural History, Smithsonian Institution, Washington, DC, USA.
Other species:

Burgess Shale and vicinity: none.

Other deposits: none.

Age & Localities:

Age:
Cambrien moyen, étage Wuliuen, formation des schistes de Burgess (environ 505 millions d’années).
Principal localities:

The Walcott and Raymond Quarries on Fossil Ridge.

History of Research:

Brief history of research:

Odaraia was first described by Walcott (1912), and was re-examined briefly by Simonetta and Delle Cave (1975) A major restudy of Odaraia was published by Briggs (1981). New morphological features of the head were later incorporated, including a sclerite (Budd 2008) and nervous tissue (Ortega-Hernández 2015). A triad of organs or simple eyes at the front of the head have been associated with a sclerite known in other early arthropods (Ortega-Hernández 2015). The legs of Odaraia have been redescribed, highlighting a potential differentiation between the proximal and distal part (Aria and Caron 2017), a study which also illustrated the sternites (ventral segments) of the animal. Several closely related species to Odaraia, Jugatacaris agilis and different species of Pectocaris (Hou et al. 2004; Jin et al. 2021) have been discovered from the Lower Cambrian Chengjiang in China (Fu and Zhang 2011). The family Odaraidae was originally defined by Simonetta and Delle Cave, 1975. Since then, it has not been formally re-defined, but many other hymenocarines probably belong to this group.

Description:

Morphology:

Much of the body of Odaraia is contained within a prominent bivalved carapace in which the valves extend and meet on the ventral surface, similar to Nereocaris briggsi. The carapace forms a tube open at the front and back. The anteriormost, visible part of the head, protruding from the front of the carapace, consists of a rounded projection housing three organs or small eyes arranged triangularly, covered by a possible sclerite, and to which is attached pair of large, spherical eyes. Behind the head, the body consisted of approximately 47 narrow segments, each bearing a pair of appendages. Each limb is biramous, and has a segmented inner branch (endopod) and a paddle-like outer branch (exopod). The tail or telson has three blades or flukes, two of which extend laterally and the third of which extends vertically into a fin-like structure. The gut is typically straight with phosphatized paired midgut glands.

Abundance:

Odaraia typically makes up less than 0.5% of the community in Walcott Quarry, from which over 200 specimens have been collected (Caron and Jackson, 2008). About a dozen specimens are known from Raymond Quarry.

Maximum Size:
150 mm

Ecology:

Life habits: Mobile, Nektobenthic
Feeding strategies: Predator, Suspension feeder
Ecological Interpretations:

The tubular carapace of Odaraia would have enclosed the ventral appendages, making it difficult for the animal to use its appendages for walking on the sea floor. It therefore seems to have swum through the water column by waving the outer branches of its biramous appendages, although this does not rule out interactions with other organisms on the sea floor. The large eyes and phosphatized gut glands (Butterfield 2002) suggest that Odaraia was a predator, seeking out floating or swimming organisms and sieving them out the water as the current passed through the tubular carapace. However, the lack of prehensile or sensory appendages also suggest Odaraia might have been a suspension feeder. To minimize the drag created by its dorsal hinge, it was proposed that Odaraia swam on its back, similar to horseshoe crabs, and the related hymenocarine Fibulacaris. The large telson would have been used to stabilize the animal while swimming to prevent it from rolling, and to help with steering and braking.

References:

  • ARIA, C. and CARON, J. B. 2017. Burgess Shale fossils illustrate the origin of the mandibulate body plan. Nature, 545: 89–92.
  • BRIGGS, D. E. G. 1976. The arthropod Branchiocaris n. gen., middle Cambrian, Burgess Shale, British Columbia. Geological Survey of Canada, Energy, Mines and Resources Canada, 264: 1–29.
  • BRIGGS, D. E. G. 1978. The morphology, mode of life, and affinities of Canadaspis perfecta (Crustacea: Phyllocarida), middle Cambrian, Burgess Shale, British Columbia. Phylosophical Transactions of The Royal Society of London, 281: 439–487.
  • BRIGGS, D. E. G. 1981. The arthropod Odaraia alata Walcott, middle Cambrian, Burgess Shale, British Columbia. Philosophical Transactions of the Royal Society of London. B, Biological Sciences, 291: 541–582.
  • BRIGGS, D. E. G. and FORTEY, R. A. 1989. The early radiation and relationships of the major arthropod groups. Science, 246: 241–243.
  • BUDD, G. E. 2002. A palaeontological solution to the arthropod head problem. Nature, 417: 271–275.
  • BUDD, G. E. 2008. Head structure in upper stem-group euarthropods. Palaeontology, 51: 561–573.
  • BUTTERFIELD, N. J. 2002. Leanchoilia guts and the interpretation of three-dimensional structures in Burgess Shale-type fossils. Paleobiology, 28: 155–171.
  • FU, D. and ZHANG, X. 2011. A new arthropod Jugatacaris agilis n. gen. n. sp. from the early Cambrian Chengjiang Biota, South China. Journal of Paleontology, 85: 567–586.
  • HOU, X.-G. and BERGSTROM, J. 1997. Arthropods of the Lower Cambrian Chengjiang fauna, southwest China. Fossils and Strata No, 45: 1–116.
  • HOU, X.-G., BERGSTRÖM, J. and XU, G.-H. 2004. The Lower Cambrian Crustacean Pectocaris from the Chengjiang Biota , Yunnan , China. Journal of Paleontology, 78: 700–708.
  • JIN, C., MAI, H., CHEN, H., LIU, Y. U., HOU, X.-G., WEN, R. and ZHAI, D. 2021. A new species of the Cambrian bivalved euarthropod Pectocaris with axially differentiated enditic armatures. Papers in Palaeontology, 7: 1781–1792.
  • ORTEGA-HERNÁNDEZ, J. 2015. Homology of head sclerites in Burgess Shale euarthropods. Current Biology, 25: 1625–1631.
  • SIMONETTA, A. M. and DELLE CAVE, L. 1975. The Cambrian non trilobite arthropods from the Burgess Shale of British Columbia. A study of their comparative morphology, taxonomy and evolutionary significance. Palaeontographia italica, 69 (n.s. 3: 1–37.
  • VANNIER, J., ARIA, C., TAYLOR, R. S. and CARON, J. B. 2018. Waptia fieldensis Walcott, a mandibulate arthropod from the middle Cambrian Burgess Shale. Royal Society Open Science, 5:172206:
  • WALCOTT, C. D. 1912. Cambrian geology and paleontology II: Middle Cambrian Branchiopoda, Malacostraca, Trilobita and Merostomata. Smithsonian Miscellaneous Collections, 57: 145–228.
  • WILLS, M. A., BRIGGS, D. E. G., FORTEY, R. A., WILKINSON, M. and SNEATH, P. H. A. 1998. An arthropod phylogeny based on fossil and recent taxa. In EDGECOMBE, G. D. (ed.) Arthropod Fossils and Phylogeny, Columbia University Press, New York, 33.105 pp.
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