Coloradesmus manitou Shear & Steinmann, 2019
publication ID |
https://dx.doi.org/10.3897/subtbiol.32.38161 |
publication LSID |
lsid:zoobank.org:pub:731EF530-E43D-4FB8-AAA3-9B4A0AD1AE09 |
persistent identifier |
https://treatment.plazi.org/id/0AF33302-F58F-4A31-ACAF-99DA75F6B27B |
taxon LSID |
lsid:zoobank.org:act:0AF33302-F58F-4A31-ACAF-99DA75F6B27B |
treatment provided by |
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scientific name |
Coloradesmus manitou Shear & Steinmann |
status |
sp. nov. |
Coloradesmus manitou Shear & Steinmann sp. nov. Figs 16-20 View Figures 15–20 , 21 View Figures 21–25
Types.
Male holotype and many male and female paratypes from Manitou Cave, El Paso Co.: Colorado, 7000' asl, collected 3 August 1996, by D. Hubbard.
Diagnosis.
A larger species, like C. aquiliensis and C. hopkinsae , but differing in that the metazonital setal tubercles are very low and often scattered across the metazonite, not in rows. The gonopod endomerite is stouter than in C. aquiliensis and emerges from the acropodite at almost a right angle, then turning distad; the distal zone is shorter and often curved. Unlike C. hopkinae , the gonopod pore is compact with few cuticular projections.
Etymology.
The species epithet is a noun in apposition, after the type locality.
Description.
Male paratype. Length 8.0-10.5 mm, depending on degree of extension, greatest width 0.9 mm. With the characters of the genus. Head densely setose, basal joint of mandibles slightly exceeding width of collum ( Fig. 16 View Figures 15–20 ). Collum with three rows of long, acute setae ( Fig. 16 View Figures 15–20 ). Midbody metazonites nearly smooth, setal tubercles low to absent; setae becoming shorter posteriorly ( Fig. 17 View Figures 15–20 ), rows disrupted so that setae may appear scattered. Telson with 12-15 long, acute, scattered setae, rounded, epiproct hardly distinct. Gonopod socket occupying entire width of prozonite, nearly circular with strong projecting anterior margin, not indenting sternite nine ( Fig. 19 View Figures 15–20 ). Gonopods with subhemispherical coxae (cx, Fig. 19 View Figures 15–20 ) immovable, completely filling socket; acropodite arises on distinct stem (s, Fig. 19 View Figures 15–20 ); prefemoral process relatively narrow, margins even, not scoop-like (pfp, Figs 20 View Figures 15–20 , 21 View Figures 21–25 ); acropodite (a, Figs 20 View Figures 15–20 , 21 View Figures 21–25 ) robust, distal zone (dz, Fig. 21 View Figures 21–25 ) short, strongly curved; endomerite (e, Figs 20 View Figures 15–20 , 21 View Figures 21–25 ) nearly as large, robust as acropodite, at wide angle to acropodite.
Female paratype. Closely similar to male in all nonsexual characters.
Distribution.
COLORADO: Fremont Co.: Fly Cave, 7 August 1996, D. Hubbard, 2 males; Marble Cave, 7 August 1996, D. Hubbard, 7 males and 8 females (these two caves are nearly adjacent at 38°36'N, 105°13'6.500"W (1982 m) asl; El Paso Co.: Cave of the Winds, 7000' (2134 m) asl, 38°55'N, 104°55'W, 2 August 1996, D. Hubbard, 10 males, 6 females and 20 February 2007, David Steinmann, 6 males, 6 females; Dilation Cave, 7400' (2256 m) asl, 38°48'N, 104°52'W, 19 June 2009, D. Steinmann, male; Pedro’s Cave, 6800' (2073 m) asl, 38°55'N, 104°55'W, 5 January 2008, D. Steinmann, male, females, juveniles.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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