Milliped Taxonomy and Distribution 141 
mi. N of Clinton, Anderson Co., Tennessee; J. A. Payne leg. 18 July 
1965. 
Lateral projections of syntelopodite process nearly straight, only a 
little longer than the median (Fig. 2); all three extend cephalad between 
median branches of colpocoxites, latter similar to those of fracta but the 
outer branch distinctly more slender distally and drawn out into a long 
narrow blade. (Fig. 6). 
Body size slightly less than in fracta and ingens, length of adult males 
about 25 mm. Dorsal surface of metaterga nearly smooth, dorsolateral 
knobs of segments 3-5 not tilted upward. Ocelli of holotype 19 in four 
rows. Coloration grayish-purple, with lighter areolation as in the other 
subspecies. 
As shown by open circles on the map (Fig. 9), this milliped appears to 
be confined to caves and epigean sites along the Clinch River, west and 
northwest of Knoxville. Material has been examined from the following 
localities (all collections from Anderson County by Jerry A. Payne, for 
whom the subspecies is named; all material at present in my personal 
collection): 
TENNESSEE: Anderson County. — Moore’s Bridge Cave, 2 mi. N 
of Clinton, 22 July 1965; Melton Hill Cave No. 1, 5 mi. S of Oak Ridge, 
19 May 1965; Bee Hole Cave, 4 mi. N of Clinton, 30 May 1965; Marie’s 
Cave, 1 mi. N of Andersonville, 29 May 1965; Wright’s Cave, ca. 2 mi. N 
of Clinton, 31 May 1965 and 2 August 1965; Wallace’s Cave, ca. 5 mi. N 
of Clinton, 4 April 1965; Markli’s Cave, 4 mi. S of Clinton, 31 May 1965. 
Knox County. — Rock Hill Cave, 2 mi. S of Heiskell, 12 June 1965, E. 
F. Menhinick. Roane County. — Eblen’s Cave near Kingston, 1 August 
1955, S. I. Auerbach; Obed River bluff opposite Harriman, 21 May 1961, 
Leslie Hubricht; wooded hillside 1.3 mi. S of Pine Grove, 30 May 1963, 
Hubricht. 
Pseudotremia fracta ingens, new subspecies 
Figs. 3, 7 
Holotype $ and paratype $ (RLH) from New Mammoth Cave, ca. 1 1 
mi. NW of LaFolette, Campbell County, Tennessee; T. C. Barr leg. 16 
September 1979. 2$ and 1$ paratypes (NCSM A3646) from same local- 
ity, T. C. Barr and J. R. Holsinger leg. 21 November 1979. 
Lateral arms of syntelopodite process long and apically divergent, 
median projection rudimentary (Fig. 7); outer branch (solenomerite) of 
colpocoxite more slender than in fracta and paynei, its outer subterminal 
process (x) much smaller than inner (y); undivided basal region of coxa 
smaller than in the other three races owing to a deeper diastemma 
