Trilobites and agnostids from the Goyder Formation (Cambrian Series 3, Guzhangian; Mindyallan), Amadeus Basin, central Australia Author Smith, Patrick M. Author Paterson, John R. Author Brock, Glenn A. text Zootaxa 2018 2018-03-19 4396 1 1 67 journal article 30484 10.11646/zootaxa.4396.1.1 918f2145-a708-460e-b19b-4f67e6c99b30 1175-5326 1202723 8EEBE6DE-0ECC-4B9C-AD14-01438291782B Catillicephalidae gen. et sp. indet. Fig. 27D–F Material. A single partial cranidium figured, CPC42402. Description. Cranidium outline semicircular, incomplete specimen 3 mm long (sag.), maximum width across posterolateral projections of fixigenae, narrowest point at anterior tip of palpebral lobes (γ–γ); strongly convex (sag., tr.). Anterior strongly rounded. Posterior margin incompletely preserved, appears to have been bowed forward strongly. Anterior branches of facial suture (γ–α) converge anteriorly in a broad arc. Glabellar anterior strongly rounded, gently expanding anteriorly, obpyriform in outline; strongly convex (sag., tr.), with maximum convexity across midwidth, lateral slopes convex; width:length ratio of 75%, occupying 96% of the cranidial length; axial furrow narrow and deep. All lateral glabellar furrows except SO, effaced. Occipital ring of moderate length (sag.), becoming slightly narrower abaxially; posterior margin bowed backwards strongly; surmounted by a thin (tr.) spine near the posterior margin, spine is incompletely preserved. SO shallow, narrow (sag.), directed transversely. Anterior cranidial border lacking furrow. Preocular and preglabellar field moderately convex, downsloping toward the anterior border; short (sag.), 4% of sagittal cranidial length. Palpebral lobes small (exsag.), incompletely preserved. Eye ridge faint, extending posterolaterally from the axial furrow, just posterior of the anterior axial furrow, in a straight line towards the anterior tip of palpebral lobe. Palpebral area of fixigena slightly downsloping towards the lateral borders, maximum width (tr.) is 31% the adjacent glabellar width. Postocular field long (exsag.) and downsloping towards the posterolateral projections. Posterolateral projections of fixigena are slightly downsloping towards the lateral corners, with a steep downturn at the lateral extremities. Posterolateral corners with a small (exsag.) broad-based spine. Posterior border incompletely preserved. Prosopon over entire cranidium is smooth. Hypostome, rostral plate, thorax and pygidium unknown. Discussion. This isolated cranidium closely resembles material described as “ Catillicephalidae , gen. nov. et sp. nov.” by Öpik (1967, p. 207, pl. 9, fig. 5) from the Mindyallan Georgina Limestone , later reassigned to Catillicephalina glasgowensis (Jago & Cooper, 2005) by Bentley et al . (2009). The Goyder Formation and Georgina Limestone material both possess an effaced obpyriform glabella, faintly developed eye ridges, anteriorly situated palpebral lobes, and posterolateral projections of the fixigena that steeply downturn at the lateral extremities (cf. Öpik 1967, pl. 9, fig. 5). However, the presence of a preglabellar field and occipital spine precludes assigning the Goyder Formation specimen to C. glasgowensis . The Goyder Formation cranidium also resembles a poorly preserved specimen identified as “ Avonina sp. nov. ”, also from the Mindyallan Georgina Limestone (Öpik 1967, p. 211, pl. 9, fig. 6); however, lack of detail on the GOY cranidium prevents further comparison. Whilst the Goyder Formation cranidium possesses the typical morphology of a catillicephalid, it also closely resembles Interalia serena Öpik, 1967 from the Mungerebar Limestone of the Georgina Basin – a monotypic genus that Öpik (1967) assigned to the Lonchocephalidae Hupé, 1953 . The only obvious features that separate the Goyder Formation specimen ( Fig. 27D–F ) from I. serena (Öpik 1967, pl. 10, figs 6, 7) are the parallel-sided glabella with faint furrows in I. serena . It is possible that Interalia also belongs to the Catillicephalidae , but without an associated pygidium, this remains an open question. Given the paucity of sclerites from the Goyder Formation, this species cannot be confidently assigned to any known catillicephalid genus. Occurrence. GOY section horizon 132.7 m ( Fig. 3 ).