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ovement of a skeletal member. Both direct anatomical evidence and inferred functional relations were used to satisfy the purposes of the study here reported on. The following account reports the results of my efforts to: 1, reconstruct the adductor muscles of the mandible in _Captorhinus_ and _Dimetrodon_; 2, reconstruct the external adductors of the mandible in the cynodont _Thrinaxodon_; and 3, learn the causes of the appearance and continued expansion of the temporal fenestrae among the reptilian ancestors of mammals. The osteology of these three genera is comparatively well-known. Although each of the genera is somewhat specialized, none seems to have departed radically from its relatives that comprised the line leading to mammals. I thank Prof. Theodore H. Eaton, Jr., for suggesting the study here reported on, for his perceptive criticisms regarding it, and for his continued patience throughout my investigation. Financial assistance was furnished by his National Science Foundation Grant (NSF-G8624) for which I am also appreciative. I thank Dr. Rainer Zangerl, Chief Curator of Geology, Chicago Museum of Natural History, for permission to examine the specimens of _Captorhinus_ and _Dimetrodon_ in that institution. I am grateful to Mr. Robert F. Clarke, Assistant Professor of Biology, The Kansas State Teachers College, Emporia, Kansas, for the opportunity to study his specimens of _Captorhinus_ from Richard's Spur, Oklahoma. Special acknowledgment is due Mr. Merton C. Bowman for his able preparation of the illustrations. Captorhinus The outlines of the skulls of _Captorhinus_ differ considerably from those of the skulls of the primitive captorhinomorph _Protorothyris_. Watson (1954:335, Fig. 9) has shown that in the morphological sequence, _Protorothyris--Romeria--Captorhinus_, there has been flattening and rounding of the skull-roof and loss of the primitive "square-cut" appearance in transverse section. The quadrates in _Captorhinus_ are farther from the midline than in _Protorothyris_, and the adductor chambers in _Captorhinus_ are considerably wider than they were primitively. Additionally, the postorbital region of _Captorhinus_ is relatively longer than that of _Protorothyris_, a specialization that has increased the length of the chambers within. In contrast with these dimensional changes there has been little shift in the pattern of the dermal bones that roof the adductor chambers. The most con
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