Aysheaia
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''Aysheaia'' is an extinct genus of soft-bodied lobopod, known from the middle Cambrian of North America, with an average body length of 1–6 cm.


Anatomy

''Aysheaia'' has ten body segments, each of which has a pair of spiked, annulate legs. The animal is segmented, and looks somewhat like a bloated caterpillar with a few spines added on — including six finger-like projections around the mouth and two grasping legs on the "head". Each leg has a subterminal row of about six curved claws. No jaw apparatus is evident. A pair of legs marks the posterior end of the body, unlike in onychophorans where the anus projects posteriad; this may be an adaptation to the terrestrial habit.


Ecology

Based on its association with
sponge Sponges, the members of the phylum Porifera (; meaning 'pore bearer'), are a basal animal clade as a sister of the diploblasts. They are multicellular organisms that have bodies full of pores and channels allowing water to circulate throug ...
remains, it is believed that ''Aysheaia'' was a
sponge Sponges, the members of the phylum Porifera (; meaning 'pore bearer'), are a basal animal clade as a sister of the diploblasts. They are multicellular organisms that have bodies full of pores and channels allowing water to circulate throug ...
grazer and may have protected itself from
predator Predation is a biological interaction where one organism, the predator, kills and eats another organism, its prey. It is one of a family of common feeding behaviours that includes parasitism and micropredation (which usually do not kill th ...
s by seeking refuge within sponge colonies. ''Aysheaia'' probably used its claws to cling to sponges. A terminal mouth is also seen in tardigrades that are omnivores or predators (but not detritovores or algivores) — this may provide an ecological signal.


Affinity

Unlike many early Cambrian forms whose relationships are obscure and puzzling, ''Aysheaia'' is remarkably similar to a modern phylum, the
Onychophora Onychophora (from grc, ονυχής, , "claws"; and , , "to carry"), commonly known as velvet worms (due to their velvety texture and somewhat wormlike appearance) or more ambiguously as peripatus (after the first described genus, '' Peripatus ...
(velvet worms). Notable differences are the lack of jaws and antennae, possible lack of visual organs, and the terminal mouth.


Distribution

Species of ''Aysheaia'' are known from
fossil A fossil (from Classical Latin , ) is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, objects preserved ...
s found in the middle Cambrian
Burgess shale The Burgess Shale is a fossil-bearing deposit exposed in the Canadian Rockies of British Columbia, Canada. It is famous for the exceptional preservation of the soft parts of its fossils. At old (middle Cambrian), it is one of the earliest fo ...
of
British Columbia British Columbia (commonly abbreviated as BC) is the westernmost province of Canada, situated between the Pacific Ocean and the Rocky Mountains. It has a diverse geography, with rugged landscapes that include rocky coastlines, sandy beaches, ...
, and from the Wheeler Formation in
Utah Utah ( , ) is a state in the Mountain West subregion of the Western United States. Utah is a landlocked U.S. state bordered to its east by Colorado, to its northeast by Wyoming, to its north by Idaho, to its south by Arizona, and to it ...
. Similar taxa are known from the lower Cambrian
Maotianshan shale The Maotianshan Shales are a series of Early Cambrian deposits in the Chiungchussu Formation, famous for their '' Konservat Lagerstätten'', deposits known for the exceptional preservation of fossilized organisms or traces. The Maotianshan Shales ...
s of China. Other than the 20 specimens from the Greater
Phyllopod bed The Phyllopod bed, designated by USNM locality number 35k, is the most famous fossil-bearing member of the Burgess Shale fossil ''Lagerstätte''. It was quarried by Charles Walcott from 1911–1917 (and later named Walcott Quarry), and was t ...
, where they comprise 2% of the community, only 19 specimens of ''A. pedunculata'' are known. ''A. prolata'' was described as a separate species from the similarly-aged
Wheeler Shale The Wheeler Shale (named by Charles Walcott) is a Cambrian ( 507  Ma) fossil locality world-famous for prolific agnostid and '' Elrathia kingii'' trilobite remains (even though many areas are barren of fossils) and represents a Konzen ...
Formation of
Utah Utah ( , ) is a state in the Mountain West subregion of the Western United States. Utah is a landlocked U.S. state bordered to its east by Colorado, to its northeast by Wyoming, to its north by Idaho, to its south by Arizona, and to it ...
but in fact represents the frontal appendage of a '' Stanleycaris''-like
radiodont Radiodonta is an extinct order of stem-group arthropods that was successful worldwide during the Cambrian period. They may be referred to as radiodonts, radiodontans, radiodontids, anomalocarids, or anomalocaridids, although the last two original ...
.


History of research


Description by Walcott (1911)

Aysheaia was described by Walcott in his 1911 work on annelid worms; Walcott imagined that a head (not observed) was present to support a polychaete affinity. His attention was soon drawn to the organism's resemblance to velvet worms, which was supported by other early researchers (1920s-30s) who also recognized a similarity with the
onychophora Onychophora (from grc, ονυχής, , "claws"; and , , "to carry"), commonly known as velvet worms (due to their velvety texture and somewhat wormlike appearance) or more ambiguously as peripatus (after the first described genus, '' Peripatus ...
, although because Aysheaia does not fall within the range of living onychophora, it has also been allocated to a phylum of its own. Nevertheless, an Onychophoran affinity represented the common opinion until the fossil was redescribed in the late 1970s.


Major redescription by Whittington, 1978

In the 1970s, Whittington undertook a thorough redescription, and associated Aysheaia with the tardigrade lineage concept promoted a couple of years earlier by Delle Cave and Simonetta, and first proposed in 1958. Thus, his interpretation places Aysheaia in the stem group to Tardigrada + Onychophora, although the view at the time was that these two modern phyla represented a group within a polyphyletic Arthropoda. A possible link to '' Xenusion'' was also brought up, although at this time the affinities of this group were unclear, and a link to the rangeomorphs had been proposed.


Response to Whittington (1980s)

The response to Whittington's redescription can be loosely classed into three camps: one school, predominantly Bergström, downplayed the similarities to the Onychophora and focussed on the Tardigrade interpretation; whereas others (after Simonetta and Delle Cave) recognized a group of lobopods containing Onychophora, Tardigrada, and ''Aysheaia'' (with features of both). Robison preferred to interpret Onychophora as the sister group to Arthropoda, and placed ''Aysheaia'' in the Onychophoran stem group in a taxon called Protonychophora (solely containing ''Aysheaia''). These were differentiated from Euonychophora (the crown group) by the number of lobopod legs and claws, the unusual head appendages, the absence of eyes, jaws, antennae and slime glands, the morphology of the rear of the body, and the terminal mouth.


Modern era

Later work uncovered further material of ''Xenusion'' and relatives, particularly from the Chinese fossil deposits. In light of the cladistic revolution of the 1990s, ''Aysheaia'' and its relatives were recognized as early offshoots of the lineage leading to arthropods and onychophorans. Looking from the opposite direction, Budd points out that there are no characters that exclude ''Aysheaia'' from the Arthropoda. It may be premature to assign ''Aysheaia'' to the onychophora over Arthropoda, as it lacks any distinctive features of the onychophoran crown group; rather, both Onychophora and Arthropoda may have arisen from animals resembling ''Aysheaia'' and its kin. Budd sees ''Aysheaia''-like organisms as representing a paraphyletic grade from which both modern onychophoran and arthropods evolved.


Etymology

The genus name commemorates a mountain peak named "Ayesha" due north of the Wapta Glacier. This peak was originally named Aysha in the 1904 maps of the region, and was renamed Ayesha after the heroine of Rider Haggard's 1887 novel '' She''.


References


External links


Further reading

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External links


Smithsonian Institution image
{{Taxonbar, from=Q139787 Cambrian invertebrates Burgess Shale fossils Xenusia Cambrian genus extinctions Wheeler Shale