378 THE PALEONTOLOGY OF MINNESOTA. 
[Clitambonites diversa. 
“Type: Pronites adscendens Pander.” (Hall, op. cit.) 
In well-preserved specimens of C. diversa the upper surface of the spondylium 
is transversely striated, these striz having three distinct curvatures in passing over 
it. Since their position and the area occupied agree with the muscular scars of this 
valve in Orthis, they are here regarded as homologous with the adductors, diductors 
and adjustors of that genus. In Lingulelasma, Lingulops and the trimerellids the mus- 
cular scars are not found in front nor underneath, but on the “platform” of those 
genera. The platform, therefore, is homologous with the spondylium of Clitambon- 
ites and Pentamerus. In Pentamerus galeatus Dalman, of the Lower Helderberg group 
of New York,* the adductors and diductors occupy nearly the entire spondylium, 
while the adjustors were probably situated on narrow flanges of the walls of the 
delthyrium. The portion of the valve immediately beneath the spondylium, and 
occasionally the sides of the septum, are strongly marked by the genital sinuses. 
Since there is no space posterior to these markings for the attachment of the 
muscles, this clearly indicates that they were situated on the upper surface of the 
spondylium. 
CLITAMBONITES DIvERSA Shaler, sp. 
PLATE XXX, FIGS. 11—17. 
1865. Orthisina diversa SHALER. Bulletin of the Museum of Comparative Zoology, no. 4, p. 67. 
1866. Orthisina verneuili BILLINGS. Catalogue of the Silurian Fossils of Anticosti, pp. 438, 74. 
1877. Hemipronites americanus WHITFIELD. Annual Report of the Geological Survey of Wisconsin, 
72 
1882. Hemipronites shee ay eaten Geology of Wisconsin, vol. iv, p. 248, pl. x, figs. 15-17. 
1889. Streptorhynchus americanus MILLER. North American Geology and Paleontology, p. 378. 
1892. Clitambonites americanus HALL. Paleontology of New York, vol. viii, p. 289, pl. xvA, figs. 1-8. 
Original description: “'Toothed [ventral] valve, usually pentagonal; socket-valve 
quadrate; hinge-line usually equal to the greatest width of the shell. Toothed valve 
very strongly projecting; depth about one-half the width; deepest point about the 
hight of hinge-line; umbo somewhat laterally compressed, usually rising high above 
the plane of the hinge-line, but very variable in this respect; umbo always laterally 
inclined indifferently towards either extremity of the hinge-line. Surface near the 
extremities of the hinge-line a little depressed and slightly recurved; area very large, 
nearly half as wide as long. Fissure from one-fourth to one third the width of the 
hinge-line; deltidium large, massive, rarely central, with distinct circular or oval 
foramen. Socket-valve with a broad and shallow mesial fold.” 
Shell of medium size; subquadrangular in outline; hinge-line straight, rarely 
shorter, and usually as long as, or slightly longer, than the greatest width of the 
shell; cardinal angles often mucronate; lateral margins straight or nearly so, sloping 
*Pal, New York, vol. iii, p. 257, pl. xLvi and xLvit, 1859. 
