Aysheaiidae
| Aysheaiidae Temporal range:
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|---|---|
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| Fossil of Aysheaia | |
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| Fossil of Palaeocampa | |
Scientific classification 
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| Kingdom: | Animalia |
| Clade: | Panarthropoda |
| Phylum: | †Lobopodia |
| Class: | †Xenusia |
| Order: | †Protonychophora |
| Family: | †Aysheaiidae Walcott, 1911 |
| Type species | |
| Aysheaia pedunculata Walcott, 1911
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| Genera | |
Aysheaiidae is a family of lobopodians known from the Cambrian, Ordovician, Carboniferous and possibly Ediacaran.[1] This family contains at most four genera, the type genus Aysheaia, the fragmentary Hadranax (although this may not be a member of the family), the aberrant Palaeocampa, and an undescribed Ordovician fossil from the Soom Shale.
Description
[edit]-
Reconstruction of Aysheaia -
Reconstruction of Palaeocampa -
Diagrammatic reconstruction of Hadranax
This family is characterised by bearing eleven annulated limb pairs (ten pairs of walking limbs and one pair of frontal appendages), often with a large number of claws (Aysheaia has around seven) at their tips. Members of this family lack eyes or hardened appendages, bearing a simple circular mouth surrounded by papillae. The posterior portion of the body "blends into" the last leg pair, with the anus situated between the legs.[2]
Aysheaia is the most typical member of the family, exhibiting all its defining traits. The body is relatively rough, with annulations (regular "wrinkling") and small spines protruding from it, alongside a few larger spines on its limbs. Its frontal appendages somewhat resemble those of siberiids, both being annulated and triangular in shape with a few large spines on their inward-facing side. Aside from this, it is relatively "generic", as it does not have any particularly unusual traits.[3]
Palaeocampa is a very divergent form, as while still retaining ten walking limb pairs and a frontal appendage pair, it has a second set of much smaller frontal appendages alongside a rounded sclerite on its head, alongside its limbs being clawless. By far its most unusual trait is that it bears hundreds of spines in two sets of bundles; shorter spines on its sides and longer ones sticking upwards at a 45-degree angle. These spines bear an intricate microstructure, with septa (constrictions), longitudinal ridges, shingle-like spines along the ridges and a rook-like tip consisting of a ring of multiple spines around a spongy area. These spines are also associated with slight discolouration, which upon spectrometry analysis was found to be remnants of an aldehyde likely used as toxin, thus making this the earliest known definitively toxic animal. These spines are also firmly attached into their bundles, making them most like the spines of polychaetes (such as the fireworms it was mistaken for). It also appears to have been freshwater, as it is found in the Montceau-les-Mines lagerstätte, a montane basin at least 300 km away from the nearest ocean at the time.[4]
It is unclear whether Hadranax belongs to Aysheaiidae, as while it has been recovered as such in various studies,[4] it is only known from sections of the body and frontal appendages, meaning many of its characteristics are unknown. Like Palaeocampa it lacks claws on its appendages, and bears unusual clustered structures on its back (although in Hadranax these are nodes instead of spine bundles. However, its frontal appendages are likely much longer than Palaeocampa's, alongside bearing at least one endite along their length. Unusually, the grouped nodes along its back are actually similar to those of Kerygmachela, possibly suggesting a shared ancestry.[5]
Another potential aysheaiid is known from the Soom Shale, however it remains unnamed. This lobopodian unusually shows branching limbs, with one broader and one shorter branch on the anteriormost few limbs. The head remains unpreserved, although its specialised frontal appendages are at least partially known with their thinner branch splitting into multiple tips.[6] This lobopodian was found to be close to Palaeocampa and Hadranax in the latter's 2025 redescription on account of a possible second frontal appendage pair.[4]
Palaeobiology
[edit]Aysheaia is known from the Burgess Shale, a diverse deep-water escarpment biota with many different genera of most phyla from the time. It is often found associated with sponges, which may suggest it fed on them, however this is unclear.[7] Hadranax is from the less diverse Sirius Passet, a deepwater habitat located near an oxygen minimum zone.[8] It likely was a benthic predator using its long appendages to feel for and capture prey, which may have consisted of small arthropods.[5] Palaeocampa, in contrast to other aysheaiids, lived in brackish to freshwater environments in Mazon Creek and Montceau-les-Mines, alongside amphibians, fish and a wide range of invertebrates including onychophorans. Its toxic, ridged spines likely deterred predators, but as no mouth is preserved the rest of its ecology is uncertain.[4] The Soom Shale aysheaiid also is of unclear ecology, but it was likely benthic as shown by the morphology. It dwelled in a cold southern ocean basin with periods of anoxic water, alongside a low-diversity community mostly consisting of arthropods and chordates.[6]
References
[edit]- ^ Chen, Zhe; Chen, Xiang; Zhou, Chuanming; Yuan, Xunlai; Xiao, Shuhai (June 2018). "Late Ediacaran trackways produced by bilaterian animals with paired appendages". Science Advances. 4 (6). doi:10.1126/sciadv.aao6691.
- ^ Robison, R. A. (1985). "Affinities of Aysheaia (Onychophora), with Description of a New Cambrian Species". Journal of Paleontology. 59 (1): 226–235. ISSN 0022-3360.
- ^ Whittington, H. B. (16 November 1978). "The Lobopod Animal Aysheaia Pedunculata Walcott, Middle Cambrian, Burgess Shale, British Columbia". Philosophical Transactions of the Royal Society of London. B, Biological Sciences. 284 (1000): 165–197. doi:10.1098/rstb.1978.0061.
- ^ a b c d Knecht, Richard J.; McCall, Christian R. A.; Tsai, Cheng-Chia; Rabideau Childers, Richard A.; Yu, Nanfang (23 July 2025). "Palaeocampa anthrax, an armored freshwater lobopodian with chemical defenses from the Carboniferous". Communications Biology. 8 (1). doi:10.1038/s42003-025-08483-0.
- ^ a b Budd, Graham E.; Peel, John S. (1998), "A new xenusiid lobopod from the early Cambrian Sirius Passet fauna of north Greenland" (PDF), Palaeontology, 41: 1201–1213
- ^ a b Whittle, Rowan J.; Gabbott, Sarah E.; Aldridge, Richard J.; Theron, Johannes (May 2009). "AN ORDOVICIAN LOBOPODIAN FROM THE SOOM SHALE LAGERSTÄTTE, SOUTH AFRICA". Palaeontology. 52 (3): 561–567. doi:10.1111/j.1475-4983.2009.00860.x.
- ^ Frood, Arran (June 2008). "Palaeobiology: The Cambrian smorgasbord". Nature. 453 (7196): 717–718. doi:10.1038/453717a.
- ^ Harper, David A. T.; Hammarlund, Emma U.; Topper, Timothy P.; Nielsen, Arne T.; Rasmussen, Jan A.; Park, Tae-Yoon S.; Smith, M. Paul (November 2019). "The Sirius Passet Lagerstätte of North Greenland: a remote window on the Cambrian Explosion". Journal of the Geological Society. 176 (6): 1023–1037. doi:10.1144/jgs2019-043.