Cormodesmus hirrutellus Chamberlin 1923

Cormodesmus hirrutellus Chamberlin, 1923 Figs 6, 7 Cormodesmus hirrutellus Chamberlin, 1923: 57, plate 21: figs 145–148, plate 22: fig. 149, (male holotype from Colombia: San Lorenzo, 4500 ft., deposited in MCZ [MCZ:IZ:DIPL-5147]); Jeekel 1971: 255. Cormodesmus hirsutellus [sic!]: Attems, 1938: 69, figs 80–81; Hoffman 1969: 280. Diagnosis. As for the genus. Material examined. COLOMBIA ● 1 ♂; Magdalena, Santa Marta, Cuchilla de San Lorenzo, Vía Minca—La Tagua. (11°05'04.40" N, 74°02'47.29" W), 7 December 2023, L. Reyes & S. Alvear leg., (MHNUC-MD-0302). Remarks: C. hirrutellus is easily recognizable by its strongly modified tergites and paranota (Fig. 6A, C, E), as well as its highly setose and granulate sternites (Fig. 6B, D, F). Ca originates from the posterior rim of the Cx and connects with the telopodite above a basal extension of the Pfe (Fig. 7A, B). The PfP is large and rounded, and shields the S and t (Fig. 7C, D). The telopodite bears two macrosetae facing ventrad, that are diagnostic for the tribe (Fig. 7). These morphological features strongly support the tribal position of C. hirrutellus within Batodesmini.