Wikipedia

Peytoia

Peytoia is a genus of hurdiid radiodont, an early diverging order of stem-group arthropods, that lived in the Cambrian period, containing two species, Peytoia nathorsti from the Miaolingian of Canada and Peytoia infercambriensis from Poland, dating to Cambrian Stage 3.[1] Its two frontal appendages had long bristle-like spines, it had no fan tail, and its short stalked eyes were behind its large head.

Peytoia
Temporal range: Cambrian Stage 3–Miaolingian
Fossil specimen of Peytoia nathorsti
Reconstruction of P. nathorsti
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Arthropoda
Order: †Radiodonta
Family: †Hurdiidae
Genus: †Peytoia
Walcott, 1911
Type species
†Peytoia nathorsti
Walcott, 1911
Species
Synonyms
  • Laggania
    Walcott, 1911
  • Pomerania
    Lendzion, 1975 (preoccupied)
  • Cassubia
    Lendzion, 1977

108 specimens of Peytoia are known from the Greater Phyllopod bed, where they comprise 0.21% of the community.[2]

Peytoia nathorsti and its junior synonym Laggania cambria played a major role in the discovery of the radiodont body plan. Initially interpreted as a jellyfish and a sea cucumber respectively, they were eventually shown to be the mouthparts and body of a single animal, which bore Anomalocaris-like appendages.

Peytoia infercambriensis is the geologically oldest known radiodont species.[1]

Classification

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Peytoia belongs to the clade Hurdiidae, and is closely related to the contemporary genus Hurdia.[3]

Peytoia contains two named species: Peytoia nathorsti, the type species, from the Burgess Shale of Canada and the Wheeler and Marjum Formations of the United States,[4] and Peytoia infercambriensis from the Zawiszyn Formation of Poland.[1] Another species of Peytoia may be present in the Burgess Shale, represented by a single frontal appendage from the Tulip Beds locality.[5] A specimen regarded as Peytoia cf. nathorsti is known from the Balang Formation of China.[6]

History

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Holotype oral cone of Peytoia nathorsti

The history of Peytoia is entangled with that of "Laggania" and Anomalocaris: all three were initially identified as isolated body parts and only later discovered to belong to one type of animal. This was due in part to their makeup of a mixture of mineralized and unmineralized body parts; the oral cone (mouth) and frontal appendage were considerably harder and more easily fossilized than the delicate body.[7]

The first was a detached frontal appendage of Anomalocaris, described by Joseph Frederick Whiteaves in 1892 as a phyllocarid crustacean, because it resembled the abdomen of that taxon.[7] The first fossilized oral cone was discovered by Charles Doolittle Walcott, who mistook it for a jellyfish and placed it in the genus Peytoia. In the same paper, Walcott described a poorly-preserved body specimen as Laggania; he interpreted it as a holothurian (sea cucumber). In 1978, Simon Conway Morris noted that the mouthparts of Laggania were identical to Peytoia, but interpreted this as indicating that Laggania was a composite fossil of Peytoia and the sponge Corralio undulata.[8] Later, while clearing what he thought was an unrelated specimen, Harry B. Whittington removed a layer of covering stone to discover the unequivocally connected arm thought to be a phyllocarid abdomen and the oral cone thought to be a jellyfish.[9][7] Whittington linked the two species, but it took several more years for researchers to realize that the continuously juxtaposed Peytoia, Laggania and frontal appendage represented one enormous creature.[7] Laggania and Peytoia were named in the same publication, but Conway Morris selected Peytoia as the valid name in 1978, which makes it the valid name according to International Commission on Zoological Nomenclature rules.[8][10]

 
Only specimen of Peytoia infercambriensis

The discovery that Anomalocaris, Laggania, and Peytoia represented parts of a single type of animal led to the synonymization of the three genera, with Peytoia nathorsti reclassified as Anomalocaris nathorsti.[11] Peytoia nathorsti was subsequently considered a junior synonym of Anomalocaris canadensis, while Laggania cambria became recognized as a distinct genus and species again,[12] but in 2012 it was determined that Anomalocaris canadensis had an oral cone with only three large plates, unlike that of Laggania cambria and Peytoia nathorsti with four, and Peytoia was once again recognized as valid, with Laggania its junior synonym.[10]

A second species, Peytoia infercambriensis, was named in 1975 as Pomerania infercambriensis. Its discoverer, Kazimiera Lendzion, interpreted it as a member of Leanchoiliidae,[13] a family which now known as part of the unrelated megacheirans (great appendage arthropods). It was subsequently renamed Cassubia infercambriensis because the name Pomerania had already been used for an ammonoid.[14] C. infercambriensis was later recognized as a radiodont.[15] It was later determined that the specimen was a composite of a radiodont frontal appendage and the body of an unknown arthropod.[1] Due to the close similarity of the appendage to Peytoia nathorsti, C. infercambriensis was reassigned to Peytoia.[1]

Description

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  •  
    Comparison of the frontal appendages of Peytoia with other members of Hurdiidae
  •  
    Morphology and movement range of the frontal appendage of Peytoia nathorsti
  •  
    Oral cone of Peytoia nathorsti in comparison to Anomalocaris and Hurdia
  •  
    Size diagram

P. nathorsti had body length about 28.7–30.3 cm (11.3–11.9 in).[16] The oral cone of Peytoia nathorsti has four large plates, similar to Hurdia, as compared to three in Anomalocaris. However, unlike Hurdia, the oral cone of Peytoia lacks inner rows of spines.[17] The frontal appendages have 13 podomeres in their distal part, as is typical and likely ancestral for radiodonts. Like other hurdiid radiodonts, the frontal appendages have five blade-like endites, which have short auxiliary spines. An intercalary podomere is present, separating the proximal and distal ends of the appendage. The appendages also have large medial spines, sometimes referred to as "gnathites", which face towards the opposite appendage.[18] The trunk consists of 13 segments, which are associated with wide swimming flaps. Compared to Hurdia, Peytoia has less prominent setal blades.[19]

Phylogeny

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Phylogenetic position of Peytoia within Panarthropoda, according to Pates et al. (2022).[20]

Ecology

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It has been proposed that the frontal appendages of Peytoia were used to sift sediment for prey, however, some authors have considered this unlikely due to the small size and irregular spacing of the auxiliary spines. It has been alternatively proposed that Peytoia was a predator, using its appendages to capture slow-moving, relatively large benthic prey.[21]

See also

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References

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  1. ^ a b c d e Daley, A. C.; Legg, D. A. (2015). "A morphological and taxonomic appraisal of the oldest anomalocaridid from the Lower Cambrian of Poland". Geological Magazine. 152 (5): 949–955. Bibcode:2015GeoM..152..949D. doi:10.1017/S0016756815000412. S2CID 130745134.
  2. ^ Caron, Jean-Bernard; Jackson, Donald A. (October 2006). "Taphonomy of the Greater Phyllopod Bed community, Burgess Shale". PALAIOS. 21 (5): 451–65. Bibcode:2006Palai..21..451C. doi:10.2110/palo.2003.P05-070R. JSTOR 20173022. S2CID 53646959.
  3. ^ Vinther, J.; Stein, M.; Longrich, N. R.; Harper, D. A. T. (2014). "A suspension-feeding anomalocarid from the Early Cambrian" (PDF). Nature. 507 (7493): 497–499. Bibcode:2014Natur.507..496V. doi:10.1038/nature13010. PMID 24670770. S2CID 205237459.
  4. ^ Pates, Stephen; Lerosey-Aubril, Rudy; Daley, Allison C.; Kier, Carlo; Bonino, Enrico; Ortega-Hernández, Javier (2021-01-19). "The diverse radiodont fauna from the Marjum Formation of Utah, USA (Cambrian: Drumian)". PeerJ. 9: e10509. doi:10.7717/peerj.10509. ISSN 2167-8359. PMC 7821760. PMID 33552709.
  5. ^ Daley, Allison C.; Budd, Graham E.; Caron, Jean-Bernard (2013-03-22). "Morphology and systematics of the anomalocaridid arthropod Hurdia from the Middle Cambrian of British Columbia and Utah". Journal of Systematic Palaeontology. 11 (7): 743–787. doi:10.1080/14772019.2012.732723. eISSN 1478-0941. ISSN 1477-2019. S2CID 86465719.
  6. ^ Liu, Qing (2013-05-02). "The first discovery of anomalocaridid appendages from the Balang Formation (Cambrian Series 2) in Hunan, China". Alcheringa: An Australasian Journal of Palaeontology. 37 (3): 338–343. doi:10.1080/03115518.2013.753767. eISSN 1752-0754. ISSN 0311-5518. S2CID 129212098.
  7. ^ a b c d Gould, Stephen Jay (1989). Wonderful life: the Burgess Shale and the nature of history. New York: W.W. Norton. pp. 194–206. ISBN 0-393-02705-8.
  8. ^ a b Conway Morris, S. (1978). "Laggania cambria Walcott: A composite fossil". Journal of Paleontology. 52 (1): 126–131.
  9. ^ Conway Morris, S. (1998). The crucible of creation: the Burgess Shale and the rise of animals. Oxford [Oxfordshire]: Oxford University Press. pp. 56–9. ISBN 0-19-850256-7.
  10. ^ a b Daley, A. and Bergström, J. (2012). "The oral cone of Anomalocaris is not a classic 'peytoia'." Naturwissenschaften, doi:10.1007/s00114-012-0910-8
  11. ^ Whittington, H. B.; Briggs, D. E. G. (1985-05-14). "The largest Cambrian animal, Anomalocaris, Burgess Shale, British Columbia". Philosophical Transactions of the Royal Society of London. Series B, Biological Sciences. 309 (1141): 569–609. Bibcode:1985RSPTB.309..569W. doi:10.1098/rstb.1985.0096. JSTOR 2396268.
  12. ^ Collins, Desmond (1996). "The "Evolution" of Anomalocaris and Its Classification in the Arthropod Class Dinocarida (nov.) and Order Radiodonta (nov.)". Journal of Paleontology. 70 (2): 280–293. Bibcode:1996JPal...70..280C. doi:10.1017/S0022336000023362. JSTOR 1306391. S2CID 131622496.
  13. ^ Lendzion, Kazimiera (1975). "Fauna of the Mobergella zone in the Polish Lower Cambrian". Geological Quarterly. 19 (2): 237–242.
  14. ^ Lendzion, Kazimiera (1977). "Cassubia - a new generic name for Pomerania Lendzion, 1975". Geological Quarterly. 21 (1).
  15. ^ Dzik, J.; Lendzion, K. (1988). "The Oldest Arthropods of the East European Platform". Lethaia. 21: 29–38. doi:10.1111/j.1502-3931.1988.tb01749.x.
  16. ^ Lerosey-Aubril, Rudy; Pates, Stephen (2018-09-14). "New suspension-feeding radiodont suggests evolution of microplanktivory in Cambrian macronekton". Nature Communications. 9 (1): 3774. Bibcode:2018NatCo...9.3774L. doi:10.1038/s41467-018-06229-7. ISSN 2041-1723. PMC 6138677. PMID 30218075. Dryad Data
  17. ^ Daley, Allison C.; Bergström, Jan (June 2012). "The oral cone of Anomalocaris is not a classic peytoia". Naturwissenschaften. 99 (6): 501–504. Bibcode:2012NW.....99..501D. doi:10.1007/s00114-012-0910-8. ISSN 0028-1042. PMID 22476406. S2CID 253633303.
  18. ^ Moysiuk, Joseph; Caron, Jean-Bernard (November 2021). "Exceptional multifunctionality in the feeding apparatus of a mid-Cambrian radiodont". Paleobiology. 47 (4): 704–724. Bibcode:2021Pbio...47..704M. doi:10.1017/pab.2021.19. ISSN 0094-8373. S2CID 236552819.
  19. ^ Pates, Stephen; Daley, Allison C.; Lieberman, Bruce S. (January 2018). "Hurdiid radiodontans from the middle Cambrian (Series 3) of Utah". Journal of Paleontology. 92 (1): 99–113. Bibcode:2018JPal...92...99P. doi:10.1017/jpa.2017.11. ISSN 0022-3360. S2CID 135388079.
  20. ^ Pates, Stephen; Wolfe, Joanna M.; Lerosey-Aubril, Rudy; Daley, Allison C.; Ortega-Hernández, Javier (2022-02-09). "New opabiniid diversifies the weirdest wonders of the euarthropod stem group". Proceedings of the Royal Society B: Biological Sciences. 289 (1968). doi:10.1098/rspb.2021.2093. PMC 8826304. PMID 35135344.
  21. ^ De Vivo, Giacinto; Lautenschlager, Stephan; Vinther, Jakob (2021-07-28). "Three-dimensional modelling, disparity and ecology of the first Cambrian apex predators". Proceedings of the Royal Society B: Biological Sciences. 288 (1955): 20211176. doi:10.1098/rspb.2021.1176. ISSN 0962-8452. PMC 8292756. PMID 34284622.
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