lowermost of two divisions of the Lower Triassic Series, representing those rocks deposited worldwide during Induan time (from 251 million to 249.7 million years ago) in the Triassic Period. The stage name is derived from the Indus River in the Salt Range of Pakistan. The stratotype for the Induan, as originally defined, is the strata above the Chhideru beds and below the Upper Ceratite Limestone of the Salt Range. The Induan stage is subdivided into two substages, which in ascending order are the Griesbachian and Dienerian. Induan marine strata are correlated worldwide by six biozones (biozone) containing ammonoid cephalopod index fossils. Five of these biozones have designated type localities in North America. These zones cannot be used for nonmarine rocks, however. The Induan Stage underlies the Olenekian Stage of the Lower Triassic Series and overlies the Changhsingian Stage of the Permian Series.