Peltura sp. B

Ahlberg, Per, Szaniawski, Hubert, Clarkson, Euan N. K. & Bengtson, Stefan, 2005, Phosphatised olenid trilobites and associated fauna from the Upper Cambrian of Västergötland, Sweden, Acta Palaeontologica Polonica 50 (3), pp. 429-440 : 434-437

publication ID

https://doi.org/ 10.5281/zenodo.13620385

persistent identifier

https://treatment.plazi.org/id/315A9976-FFA3-FFE2-FCD6-5895FE01FC16

treatment provided by

Felipe

scientific name

Peltura sp. B
status

 

Peltura sp. B

Fig. 3J View Fig .

Material.—One transitory pygidium with a length of about 0.5 mm and an estimated width of 1.0 mm.

Remarks.—The pygidium is subtriangular in outline with three axial rings and a terminal piece. There are four pairs of stout marginal spines, the outermost directed backwards and the innermost directed backwards and slightly inwards. While this pygidium is noted here as a separate species, it may merely represent a different growth stage of Peltura sp. A .

Indeterminate olenid fragments

Figs. 3K–P View Fig , 4A–H View Fig .

Material.—Three broken occipital rings, two thoracic “axial rings”, one broken thoracic tergite, four thoracic pleurae, one hypostome, one partial librigena with the eye, and two detached visual surfaces.

Remarks.—None of these fragments can be referred with certainty to any genus. The occipital rings ( Fig. 3K–M View Fig ), of width 0.6, 0.9, and 1.0 mm respectively, all of which have an occipital spine, appear to belong to three different species. They differ in their surface sculpture. The occipital ring shown in Fig. 3L View Fig has broadly spaced nodules along the posterior margin, the one shown in Fig. 3M View Fig is granulose, whereas the occipital ring shown in Fig. 3K View Fig has dense, closely packed and prominent granules.

The axial rings ( Fig. 3N, O View Fig ) again appear to belong to two different species. The axial ring shown in Fig. 3O View Fig has a smooth, lensoidal articulating half−ring (0.7 mm wide), approximately the same length (sag.) as the main part of the axial ring, which has a straight posterior margin, a distinct medial node, and a granular sculpture. The axial ring in Fig. 3N View Fig is seen edge on and is strongly arched with a broad−based and stout axial spine.

The incomplete thoracic tergite ( Fig. 3P View Fig ; estimated width 1.3 mm) has a smooth external surface. The axial ring proper is slightly wider than the pleura and about the same length (sag.) as the articulating half−ring. It has a conspicuous medial node. The pleurae lack a distinct pleural furrow and the lateral margins are somewhat rounded anteriorly, posteriorly making an angle of about 80 ° with the posterior margin.

Three pleurae (1.2, 1.3, and 1.6 mm wide; Fig. 4A–C View Fig ) are all broken off at the axial furrow, but can be referred to the same species. They are 0.4 times as long (exsag.) as they are wide with nearly straight and transversely parallel margins. The curving antero−lateral margin terminates in a broad−based spine, directed posteriorly and slightly laterally. Articulating facets are absent. An oblique pleural furrow traverses the pleura almost as far as the base of the spine. The external surface is granulose, except antero−laterally. Three to five larger nodes, irregularly spaced, are present along a transverse line in front of the posterior margin. A thin ridge, subparallel with the pleural furrow, extends from the anterior margin about a third of the way from the axial furrow to the middle part of the antero−lateral margin. Terrace lines run along the outer edge of the pleura, particularly on the spine.

The fourth pleura ( Fig. 4D View Fig ; 0.6 mm long exsag.) consists of the lateral part only and is seen in ventral view. It appears to have been very long (exsag.) and extends laterally into a sharp, postero−laterally directed spine. The doublure is clearly visible as a subtriangular area joining with the spine. It has an almost straight inner edge in the exsagittal plane, sharply curved posteriorly into a narrow shelf along the posterior margin of the pleura. Anteriorly the inner edge of the doublure curves slightly inwards to meet the anterior margin of the pleura. Seven terrace lines are arranged subparallel with the inner edge of the doublure. The inner surface of the pleura is smooth. There seems to be a hollow space between the doublure and the dorsal exoskeleton.

The two detached visual surfaces ( Fig. 4E, F View Fig ) and the librigena with an intact eye ( Fig. 4G View Fig ) probably belong to the same species, maybe a species of Ctenopyge . These detached eyes (0.55 and 0.60 mm long) are nearly spherical with between a hundred and two hundred lenses. In one specimen there is clear lens packing discontinuity (running from northeast to southwest in Fig. 4E View Fig ). The librigena has a regularly curved outer margin with a raised lateral border, about the same width as the narrowest distance from the border furrow to the base of the eye. The posterior branch of the facial suture is short, strongly convex forwards, and cuts the lateral border at a sharp angle. That part of the anterior branch of the facial suture still preserved curves slightly forwards from the top of the eye. The palpebral suture is straight adaxially. The external surface is smooth.

A poorly preserved hypostome ( Fig. 4H View Fig ), 0.5 mm long, is frayed laterally and its original external contour cannot be distinguished. The anterior margin is slightly convex forwards. Only part of the posterior border is preserved, but it is evidently longer (sag.) than the anterior border. The ovoid and convex middle body is distinct.

Kingdom

Animalia

Phylum

Arthropoda

Class

Trilobita

Order

Lichida

Family

Lichidae

Genus

Peltura

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