The Zonal Origins of the Mineralocorticoid Hormones in the 21-Hydroxylation Deficiency of Congenital Adrenal Hyperplasia*

The 0800 h plasma concentrations of the mineralocorticoid hormones, 18-hydroxydeoxycorticosterone (18-OHDOC), deoxycorticosterone (DOC), corticosterone, 18-hydroxycorticosterone (18-OHB), and aldosterone, in six patients with nonsalt-losing congenital adrenal hyperplasia revealed two groupings of these steroids: in one group, DOC, 18-OHB, and aldosterone were significantly elevated (P less than 0.001) at 51.7 +/- 18.0, 70.8 +/- 14.2, and 22.7 +/- 3.0 ng/dl, respectively; in the other group, corticosterone and 18-OHDOC were normal at 363.6 +/- 76.0 and 7.8 +/- 1.1 ng/dl, respectively. No significant increases in response to upright posture were observed in DOC, 18-OHB, or aldosterone. After a 1-h Cortrosyn stimulation test, the already elevated levels of DOC, 18-OHB, and aldosterone showed slight additional increases, but the normal levels of corticosterone and 18-OHDOC changed little within the normal unstimulated range. In these patients certain mineralocorticoid hormone patterns permit the identification of the zonal origins of steroids. The normal and fixed levels of 18-OHDOC and corticosterone, zona fasciculata steroids, are similar to those of cortisol and imply deficiency of formation and of their precursor, zona fasciculata DOC, a 21-hydroxylated steroid. Both the mineralocorticoid and glucocorticoid pathways distal to 21-hydroxylation are impaired in the zona fasciculata. However, the elevated and partially responsive levels of DOC, 18-OHB, and aldosterone imply that there is greater activation of 21-hydroxylation in the zona glomerulosa than in the zona fasciculata, with its normal fixed steroid levels, and that the elevated level of DOC is primarily from this zone.