Machairagnostus, Harrington & Leanza, 1957

Taylor, John F., Loch, James D. & Repetski, John E., 2024, Taxonomy and stratigraphic distribution of Lotagnostus (Agnostida: Agnostidae) and associated trilobites and conodonts in the Upper Cambrian (Furongian) of Laurentia, Zootaxa 5422 (1), pp. 1-66 : 58

publication ID

https://doi.org/ 10.11646/zootaxa.5422.1.1

publication LSID

lsid:zoobank.org:pub:AE955C5E-803E-44CB-A3B2-9C2616D9F185

persistent identifier

https://treatment.plazi.org/id/926387DB-FF8E-CA13-FF38-85DEFAD91380

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Plazi

scientific name

Machairagnostus
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Machairagnostus View in CoL cf. M. corrugatus ( Suárez-Soruco, 1975)

( Plate 7.20 View PLATE 7 )

Discussion. A single exfoliated pygidium from collection 5/22/08B conforms to the diagnosis of Naimark (2016) for Machairagnostus by exhibiting a clearly defined intranotular axis (=lanceolate field) bounded by well-impressed notular furrows, and a terminal node just inside the border furrow.Although a few exfoliated pygidia of Neoagnostus parki from the same collection display very faint notular furrows (e.g. Pl. 15 View PLATE 15 , fig. 10), none compare in depth of incision or are associated with scrobiculae on the pleural fields like those on the specimen here assigned to Machairagnostus . Moreover, this specimen is proportionally narrower (tr.) than N. parki pygidia of similar size. Given these differences, we consider it unlikely that this unique pygidium is a variant of N. parki .

The Windfall specimen differs from all pygidia illustrated for the seven species of Machairagnostus listed by Naimark (2016) in displaying a broader, flat border and much longer marginal spines that diverge posteriorly, rather than being subparallel. The pygidia of the type species, M. tmetus ( Harrington & Leanza, 1957) , and the species identified as M. sp. by Lazarenko et al. (2008, pl. 20, fig. 14, pl. 21, fig. 12) also differ in lacking scrobiculae on the pleural fields and having the sides of the posteroaxis more clearly defined by faintly impressed axial furrows. The pygidium of M. ornatus ( Lisogor, 1977, pl. 31, fig. 1) is less quadrate, more coarsely scobiculate, and lacks clear definition of the intranotular axis. The poor preservation of the illustrated pygidia of M. kentauensis ( Ergaliev, 1983, p. 43–44, pl. 3, figs 3–4) makes comparisons difficult. However, the Khazakhstanian specimens clearly display a much broader border furrow and narrower border of less variable width than the Windfall pygidium. Machairagnostus houchengensis ( Zhang, 1981, pl. 55, fig. 12) has a poorly defined intranotular axis, more strongly constricted acrolobe, and much smaller and more anteriorly positioned posterolateral spines than the Nevada pygidium. The axial features of the Windfall pygidium most closely resemble those displayed by the three pygidia of M. corrugatus ( Suárez-Soruco, 1975) illustrated by Tortello & Esteban (2003, figs 4.CC–EE). Indeed, the similarity is so strong that the Windfall pygidium might represent that species, with the wider border and longer, more posteriorly positioned spines attributable to intraspecific (ontogenetic) variation. Whether the Windfall pygidium is an ontogenetic variant of M. corrugatus or a new, closely related species cannot be determined at present owing to the poor preservation of the border and marginal spines in the smallest pygidium illustrated by Tortello & Esteban (2003, fig. 4.DD), which is similar in size to the Windfall specimen, and the lack of an associated cephalon in the Nevada collection.

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