Selenium is a rare and dispersed element; its content in the
earth’s crust (clarke) is 5 X 10–6 percent by weight. The history of selenium in the earth’s crust is closely linked to that of sulfur. Selenium displays a tendency toward concentration and, despite its low clarke, forms 38 minerals of its own, including selenides, selenites, and selenates. Isomor-phous admixtures of selenium are characteristic in sulfides and native sulfur.
Selenium undergoes active migration in the biosphere. Igneous rocks, volcanic gases, and volcanic hot springs are sources of selenium accumulations in organisms. For this reason, the soils and sedimentary rocks in active and dormant volcanic regions are often enriched with selenium. Here, the average content in clays and shales is 6 × 10–5 percent.
Distribution in nature.