Abstract

A small collection of Upper Devonian conodonts from Cottonwood Canyon on the W. side of the Bighorn Mountains, Wyoming, is described. The majority of the species are the same as those reported from the Darby formation in the Wind River Mountains in western Wyoming. General correlation with the Saverton of Missouri and part of the Clymenia-Stufe of Europe is indicated.

You do not currently have access to this article.