Reedocalymene unicornis ( Reed, 1917 )

Fortey, Richard A., Wernette, Shelly J. & Hughes, Nigel C., 2022, Revision of F. R. C. Reed’s Ordovician trilobite types from Myanmar (Burma) and western Yunnan Province, China, Zootaxa 5162 (4), pp. 301-356 : 337

publication ID

https://doi.org/ 10.11646/zootaxa.5162.4.1

publication LSID

lsid:zoobank.org:pub:DD2279FA-E8F1-4951-A5CA-91082E875580

DOI

https://doi.org/10.5281/zenodo.6810354

persistent identifier

https://treatment.plazi.org/id/03CB8784-6E71-1D2D-FF3A-C1184E73F4E1

treatment provided by

Plazi

scientific name

Reedocalymene unicornis ( Reed, 1917 )
status

 

Reedocalymene unicornis ( Reed, 1917) View in CoL

Figs 12.1–6 View FIGURE 12 , 8 View FIGURE 8 , 10 View FIGURE 10

1917 Calymene unicornis sp. nov.; Reed p. 52–54, pl. 8, figs 10–13.

1951 Reedocalymene unicornis ( Reed, 1917) View in CoL ; Kobayashi, p. 45, pl. 4, figs 12–14.

1975 Reedocalymene unicornis ( Reed, 1917) View in CoL ; Lu, p. 447.

2002 Reedocalymene unicornis ( Reed, 1917) View in CoL ; Turvey, p. 55.

2005 Reedocalymene unicornis ( Reed, 1917) Turvey View in CoL , p. 550.

Material. Lectotype (selected by Turvey, 2005): damaged cephalon, Figs 12.1-3 View FIGURE 12 ( Reed, 1917, pl. 8, fig. 10), GSI 11913. Additional type material: cephalic fragments, Figs 12.5 View FIGURE 12 /8 and 12.10/6 ( Reed, 1917, pl. 8, figs 12,11 respectively), GSI 11912; pygidium, Fig. 12.4 View FIGURE 12 ( Reed, 1917, pl. 8, fig. 13), GSI 11911? All material from the Shihtien Formation (Darriwilian) at Pupiao, western Yunnan.

Discussion. Reed (1917) described the limited material of this species in some detail, and new cast material does not greatly enhance our knowledge. The lectotype is more distorted than Brock’s original drawing suggests, and the upward curvature of the anterior pro/jection shown by Reed (1917, pl. 8, fig. 10a, GSI 11913) may have been exaggerated by this. However, the comparatively laterally expanded L1 on the glabella is probably a real feature, which is not so clear on the original drawing. This differs from other species assigned to the genus by Lu (1975) that have a uniformly deeply parabolic glabellar outline. In this respect R. unicornis more closely resembles species that have been assigned to Calymenesun and Vietnamia (see Turvey, 2002). However, it is possible that deformation may have contributed to this distinction. A very incomplete cranidium shows the outline of the posterior fixed cheek. A backwardly displaced free cheek with a narrow border is best displayed on Reed’s pl. 8, fig. 11; we have not been able to cast this specimen, nor the only example of a pygidium ( Reed, 1917, pl. 8, fig. 13) reproduced here. The imperfect thorax and pygidium from Pupiao figured by Reed (1917, pl. 8, fig. 14) is refigured here ( Fig. 12.7 View FIGURE 12 ). It is likely to belong to a reedocalymenine, and possibly to Reedocalymene rather than Neseuretinus . However, the pygidial pleural ribs appear to be more pronounced than is the case with the pygidium assigned with more certainty to R. unicornis by Reed (1917, pl. 8, fig.13), and its assignment must remain uncertain.

GSI

Geological Survey of India

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