Fig. 2 in Ostracods and facies of the Early and Middle Frasnian at Devils Gate in Nevada: Relationship to the Alamo Event

Fig. 2. Lithology of the lower member of the type Devils Gate Limestone showing positions of ostracod, conodont, and sedimentological samples. Ostracod samples numbered DVG are from Sandberg et al. (1988, 2003). Other columns indicate conodont zones revised herein by Sandberg, paleoenvironmental interpretation, and microfacies evolution. Abbreviation: Pa., Palmatolepis.