Brain tumors are responsible for about 1 per cent of deaths (Ewing, 1), deaths which most often occur in early or middle adult life and are preceded by great suffering. It has been possible only within recent years to treat a few of these patients with success, a success which has been attained chiefly because of the earlier localization of the tumor. Roentgenography has contributed much to the earlier and more accurate localization of brain tumor, through the works of Schüller, Sosman, Dandy, and many others. Any further knowledge which may strengthen or clarify the diagnosis seems desirable. This paper is concerned chiefly with the occurrence and localizing value of a radiographic shadow due to calcium deposits in the choroid plexuses of the lateral cerebral ventricles. The normal gross anatomy and histology are fully described in most text-books (Fig. 1). Each of the ventricles contains a plexus — highly vascular, villous tufts, covered by epithelium (ectodermal) derived from the ependyma. They occupy a relatively small space within the ventricles, and are bathed by the ventricular fluid. They are attached to the ventricular wall by delicate laminæ which represent developmental infoldings of the pia-arachnoid (mesodermal) and which form a supporting meshwork for their many capillaries. The choroid plexuses of the lateral ventricles, with which this paper is mainly concerned, are elongated structures, diverging slightly as they pass backward from each foramen of Monro. They lie on the floor of the body of the ventricle, and terminate a little beyond the junction of the inferior and posterior horns. The posterior extremity is expanded to a diameter of about one centimeter, called the glomus. The right and left glomus lie, one on each side of the sagittal plane, separated by a distance of about five centimeters. The glomus is the only part wherein calcification occurs in sufficient amount to produce an X-ray shadow. (The suprapineal portion of the plexus of the third ventricle may be an exception.) The pineal body, which more often casts a shadow, is exactly in the sagittal plane, about two centimeters in a frontal direction, midway between the right and left glomus. The function of the choroid plexuses is to produce the cerebrospinal fluid. This they do, according to prevalent belief, not as secretory glands, but as semipermeable membranes (2). However, certain investigators believe the plexuses absorb the cerebrospinal fluid, while a minority believe they have nothing to do with the fluid (3, 4, 5). Important as their function is generally conceded to be, it is somewhat striking that no disease or symptom-complex aside from tumor has been convincingly attributed to pathologic states limited to the plexuses. Yet regressive metamorphoses are so commonly present as to be considered “physiologic.” These changes start in childhood, gradually increase with advancing years, becoming pronounced and characteristic in old age.
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