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Peng et al.—Revision of oryctocephalid genra


937


Figure 3. Reconstructions of Arthricocephalus chauveaui (1) based on NIGP 163354, and Oryctocarella duyunensis (2) based on NWU-DYXJT 1823, both from the Balang Formation of western Hunan, China. These species show differences in glabellar outline (forwardly expanding or pestle-shaped, 1, compared to cylindrical, 2); development of the glabellar furrows (transglabellar, 1, compared to pit-like, 2); course of the axial furrow (curved, 1, compared to straight, 2); course of the facial suture (gonatoparian, 1, compared to proparian, 2); shape of the anterior cranidial border (upturned posterolaterally, 1, compared to anteriorly, 2); position of the palpebral lobe (situated at the level of the glabellar mid-point, 1, compared to located anteriorly, 2); presence,1, or absence, 2, of fulcra; thoracic segmentation (eight segments, 1, rather than 11 segments, 2); tips of pleurae (pointed, 1, rather than slightly rounded, 2); size and segmentation of pygidium (isopygous, with five pleurae, 1, compared to micropygous, with three pleurae, 2); pygidial interpleural furrows (faint, 1, rather than well defined, 2); pygidial border (upturned, 1, rather than absent, 2); development of the posterior pygidial margin (equally curved, 1, rather than with a median notch, 2); and surface prosopon (smooth to finely granulose, 1, as compared to coarsely and densely granulose, 2; surface granulation on the reconstruction of each species has been omitted).


although it has long been considered to be a meraspid of this species (e.g., Lane et al., 1988;Blaker and Peel, 1997;McNamara et al., 2003). The specimen also differs considerably from speci- mens on Bergeron’s (1899) slab reassigned to Oryctocarella duyunensis. The specimen is here reassigned to Duyunaspis


duyunensis Zhang and Qian in Zhou et al., 1977 (p. 132, pl. 41, figs. 5, 6), the type species ofDuyunaspis. The exoskeleton differs from both A. chauveaui and O. duyunensis in having a pro- portionally large glabella that is wider than the fixigena; shallow and weakly impressed glabellar furrows; a proportionally wide thoracic axis that is nearly as wide as the pleural area; and a relatively small pygidium with a broad axis. The specimen of D. duyunensis has a medial notch on the posterior margin of the pygidium, similar to O. duyunensis, but the pygidial axis in specimens of O. duyunensis is much narrower, being only about half as wide as the pleural area. The thorax of the smallest exoskeleton on Bergeron’s slab has fulcrate segments, similar to A. chauveaui, but the fulcra in the smallest specimen lie much closer to axial furrow than they do in the largest exoskeleton. We conclude that Bergeron’s (1899) original illustration


and description of A. chauveaui are based principally on the largest exoskeleton in the type series. According to Article 74.6.1 of the International Code of Zoological Nomenclature (ICZN, 1999), which states that “The inference that the speci- men is a ‘holotype’ or ‘the type’ may be by reference to an illustration or description of specimen,” the largest exoskeleton on Bergeron’s slab is inferred as ‘type’ of A. chauveaui.


In accordance with Article 74.6, “the assumption that the species-group taxon was based upon a single type specimen is deemed to have designated that specimen as the lectotype.” For these reasons, the largest exoskeleton on Bergeron’s (1899) limestone slab (E.M. 90001a) is designed the lectotype of Arthricocephalus chauveaui. Arthricocephalus is considered to be a monotypic genus. An external mold of a large pygidium (E.M. 90001g;


Figs. 1.2, 2.11) on Bergeron’s (1899) slab remains assigned to Arthricocephalus chauveaui; it is a paralectotype. Other scler- ites on the slab, which are presumed to be part of Bergeron’s suite of examined specimens and all originally referred to A. chauveaui, are also considered to be paralectotypes of A. chauveaui. All of these specimens, however, are here reas- signed as either Oryctocarella duyunensis (E.M. 90001b– 90001e, 90001h) or Duyunaspis duyunensis (E.M. 90001f).


Incorrect designation of lectotype


Circumstances surrounding the designation of a lectotype of Arthricocephalus chauveaui by Lane et al. (1988), and sub- sequent treatment of Bergeron’s (1899) suite of material, has resulted in ambiguity of the concepts of both A. chauveaui Bergeron, 1899 and Arthricocephalus Bergeron, 1899. Photographs of some Bergeron’s sclerites were first published by Lane et al. (1988). In that same article, Lane et al. (1988, p. 558) stated that they accepted the specimen upon which


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