Triassic conodonts have been found in limestone sections from the Wasatch Mountains of N.-central Utah to ranges in E.-central Nevada. Although the largest concentrations of conodonts are in the Meekoceras ammonoid zone, certain species range several hundred feet above and below this time marker. Two new genera, Parachirognathus and Furnishius, and new species of Gondolella, Prioniodina, and Hindeodella ar described.