Laggania

''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. Its two frontal appendages had long bristle-like spines, it had no fan tail, and its short stalked eyes were behind its large head.

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

''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.

Classification

''Peytoia'' belongs to the clade Hurdiidae, and is closely related to the contemporary genus ''Hurdia''.

''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, and ''Peytoia infercambriensis'' from the Zawiszyn Formation of Poland. Another species of ''Peytoia'' may be present in the Burgess Shale, represented by a single frontal appendage from the Tulip Beds locality. A specimen regarded as ''Peytoia'' cf. ''nathorsti'' is known from the Balang Formation of China.

History

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.

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. 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''. 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. 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. ''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.

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''. ''Peytoia nathorsti'' was subsequently considered a junior synonym of ''Anomalocaris canadensis'', while ''Laggania cambria'' became recognized as a distinct genus and species again, 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.

A second species, ''Peytoia infercambriensis'', was named in 1975 as ''Pomerania infercambriensis''. Its discoverer, Kazimiera Lendzion, interpreted it as a member of Leanchoiliidae, 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. ''C. infercambriensis'' was later recognized as a radiodont. It was later determined that the specimen was a composite of a radiodont frontal appendage and the body of an unknown arthropod. Due to the close similarity of the appendage to ''Peytoia nathorsti'', ''C. infercambriensis'' was reassigned to ''Peytoia''.

Description

''P. nathorsti'' had body length about . 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. 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. The trunk consists of 13 segments, which are associated with wide swimming flaps. Compared to ''Hurdia'', ''Peytoia'' has less prominent setal blades.

Phylogeny

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

Ecology

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.

See also

* Paleobiota of the Burgess Shale

References

External links

*

{{Taxonbar, from=Q20672130

Burgess Shale fossils
Cambrian arthropods
Radiodonta
Fossil taxa described in 1911