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Corrugatagnostus convergens
Taxonomy
Corrugatagnostus convergens was named by Weir (1959) [= 1862 Olenus? Baily, p. 10 ffig. la.
= 1939 Agnostus cf. perrugatus Harper (in Smyth and others), p. 303.
= 1942 Agnostus cf. perrugatus Harper, p. 216.]. Its type specimen is B.M. In. 53361, a cephalon/head, and it is a 3D body fossil. Its type locality is Stream on south-eastern boundary of Ballyvorgal South, Slieve Bemagh Mountains, which is in a Katian marine mudstone in Ireland.
Synonymy list
| Year | Name and author |
|---|---|
| 1959 | Corrugatagnostus convergens Weir pp. 370 - 371 figs. Plate 62, fig. 17- [9 |
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If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.
†Corrugatagnostus convergens Weir 1959
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Diagnosis
| Reference | Diagnosis | |
|---|---|---|
| J. A. Weir 1959 | Corrugatagnostus with median furrow on preglabellar field reaching anterior border, flanked by two converging furrows not reaching border. Antcrior and middle glabellar lobes bearing elongate median ridges. |