But in the extinct mammal-like reptiles of the Permian and Triassic of South Africa and Russia the skeleton of the pectoral and pelvic girdles and limbs progressively approaches the mam malian type. Their limbs were adapted for running rather than crawling; the body was lifted well above the ground and the trackway became narrower so that the feet gave a more direct support to the weight. In the later mammal-like reptiles the feet were small and short, and from the reduction in the number of phalanges or toe-joints, to the mammalian number (three in each toe, except the first, which has two) we may infer that the fore feet were at least partly "digitigrade," i.e., raised off the ground at the wrist. So too the humerus of the cynodonts, or higher mammal-like reptiles, approached the lower mammalian types, and from the form and position of its joint surfaces we may infer that the angle at the elbow was opening out toward the mam malian condition.
The remaining elements of the primitive mammalian fore-limb, the humerus, radius and ulna, carpus, metacarpus and digits, were derived with only minor changes from those of the cynodonts.
Meanwhile the femur has undergone corresponding changes in the passage from crawling to running habits. In the primitive crawling types the short stout femur projected widely from the body, its head, or surface for articulation with the pelvis, was a broad oval set directly on top of the shaft ; there was a large deep pit for the insertion of the obturator muscles on the under-side of the femur below the head, and a high ridge for the adductor muscles, also on the under-side of the shaft. In primitive mam mals, the femur is long, slender, with a cylindrical shaft, the head is globular, set off at a sharp angle and separated from the shaft by a well-defined neck; there is a large flange (greater trochanter) on the outer upper part of the shaft, the proximal pit (or digital fossa) is small, the primary adductor ridge is lost and there is a process, the lesser trochanter, not found in reptiles.
In primitive reptiles the bend between the lower end of the shank and the foot was not sharp ; the two main bones of the tarsus, the astragalus and calcaneum, were flat, more or less circu lar elements located in the same general plane ; the calcaneum did not project backward to form a heel-bone. In the running foot of the typical mammal, on the other hand, there is a sharp bend between the shin-bone and the instep, the astragalus and calca neum are highly differentiated, the former resting upon the latter, the one forming a pulley for the tibia, the other a heel or lever for the powerful muscles of the shank.