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Aysheaia pedunculata

A worm-like precursor of arthropods

Reconstruction of Aysheaia pedunculata.

© Marianne Collins

Taxonomy:

Kingdom: Animalia
Phylum: Lobopodia
Higher Taxonomic assignment: None
Species name: Aysheaia pedunculata
Remarks:

Aysheaia is one of a variety of lobopodian taxa from the Cambrian, which are early members of the lineage that gave rise to arthropods, and whose only modern survivors are onychophorans (velvet worms) and tardigrades (water bears). Lobopodians characteristically have annulated, unjointed bodies and bear soft limbs after which they are called: the lobopods. Although the finding is not consensual, the type of claws and orientation of rear limbs suggest that Aysheaia could be the earliest member of the water bear lineage.

Described by: Walcott
Description date: 1911
Etymology:

Genus – after the nearby Aysha peak (since renamed Ayesha peak) in the Wapta icefield (3,065 m); original meaning unknown.

species – from the Latin pedunculus, “foot.”

Type Specimens: Holotype –USNM57655 in the National Museum of Natural History, Smithsonian Institution, Washington, DC, USA.
Other species:

Burgess Shale and vicinity: none

Other deposits: A.? prolata from the Middle Cambrian of Utah (Robison, 1985).

Age & Localities:

Age:
Middle Cambrian, Wuliuan stage, Burgess Shale Formation (approximately 505 million years ago).
Principal localities:

The Walcott Quarry on Fossil Ridge.

History of Research:

Brief history of research:

Walcott originally described Aysheaia as an annelid worm (Walcott 1911). It was later re-described as a velvet worm (or a close relative) (Brues 1923; Walton 1927; Hutchinson 1930; Walcott 1931), although it lacked features such as jaws and slime glands. Certain authors advocated a position in its own phylum (Tiegs & Manton 1958). A morphological reinterpretation based on photographs (Delle Cave & Simonetta 1975) prompted a detailed re-study of the fossil specimens (Whittington 1978), and relationships were suggested with the water bears (tardigrades) (Bergström 1978). Although some more recent phylogenetic approaches resolve Aysheaia as a basal lobopodian (Smith & Ortega-Hernandez 2014; Yang et al. 2015), other find support for a more derived affinity and a close relationship with tardigrades (Caron & Aria 2017, 2020).

Description:

Morphology:

Aysheaia is a worm-like animal, 1 to 6 cm in length and about 5 mm broad, bearing ten pairs of clawed, spiny limbs on the lower part of its body. It did not have a separate head, but a mouth occupied the very front of the body, accompanied by a pair of appendages and a circlet of bumps (papillae). The animal had a soft, flexible, non-mineralized cuticle, which had a corrugated, accordion-like form. Each stubby limb had ten corrugations, some of which bore a spiny projection. The terminal pair of limbs was oriented towards the front of the animal. A suite of claws also adorned the end of each stub-foot. A faint line running down the axis of the organism is interpreted as its gut.

Abundance:

Aysheaia is rare in the Walcott Quarry representing less than 0.04% of the specimens counted in the community (Caron and Jackson, 2008).

Maximum Size:
60 mm

Ecology:

Life habits: Epibenthic, Mobile
Feeding strategies: Carnivorous, Grazer
Ecological Interpretations:

Aysheaia is frequently associated with the remains of sponges, and an ecological association has been posited. Considering recent evidence that other lobopodians lived anchored to a substrate for suspension-feeding (Caron & Aria 2017), it is possible that Aysheaia also used sponges as substrate for its lifestyle, although the animal lacked the morphological specializations of a suspension feeder, and more likely grazed or predated walking on their surface.

References:

  • BERGSTRÖM, J. 1978. Morphology of fossil arthropods as a guide to phylogenetic relationships. In Arthropod Phylogeny, Van Nostrand Reinhold Co., New York, 1–56 pp.
  • BRUES, C. 1923. The geographical distribution of the Onychophora. American Naturalist, 57, 210–217.
  • CARON, J. and ARIA, C. 2020. The Collins’ monster, a spinous suspension‐feeding lobopodian from the Cambrian Burgess Shale of British Columbia. Palaeontology, 63, 979–994.
  • CARON, J.-B. and ARIA, C. 2017. Cambrian suspension-feeding lobopodians and the early radiation of panarthropods. BMC Evolutionary Biology, 17, 29.
  • DELLE CAVE, L. and SIMONETTA, A. M. 1975. Notes on the morphology and taxonomic position of Aysheaia (Onycophora?) and of Skania (undetermined phylum). Monitore Zoologico Italiano, (N.S.), 67–81.
  • HUTCHINSON, G. E. 1930. Restudy of some Burgess Shale fossils. Proceedings of the United States National Museum, 78, 59.
  • SMITH, M. R. and ORTEGA-HERNANDEZ, J. 2014. Hallucigenia’s onychophoran-like claws and the case for Tactopoda. Nature, 514, 363–366.
  • TIEGS, O. W. and MANTON, S. M. 1958. The evolution of the Arthropoda. Biological Reviews, 33, 255–333.
  • WALCOTT, C. 1911. Cambrian Geology and Paleontology II. Middle Cambrian annelids. Smithsonian Miscellaneous Collections, 57(5), 109–145.
  • WALCOTT, C. 1931. Addenda to descriptions of Burgess Shale fossils. Smithsonian Miscellaneous Collections, 85(3), 1–46.
  • WALTON, L. B. 1927. The polychaete ancestry of the insects. American Naturalist, 61, 226–250.
  • WHITTINGTON, H. B. 1978. The lobopod animal Aysheaia pedunculata Walcott, Middle Cambrian, Burgess Shale, British Columbia. Philosophical Transactions of the Royal Society of London B, 284, 165–197.
  • YANG, J., ORTEGA-HERNANDEZ, J., GERBER, S., BUTTERFIELD, N. J., HOU, J., LAN, T. and ZHANG, X. 2015. A superarmored lobopodian from the Cambrian of China and early disparity in the evolution of Onychophora. Proceedings of the National Academy of Sciences of the United States of America, 112, 8678–8683.
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