Conodonts as biostratigraphic tools for redefinition and correlation of the Cambrian-Ordovician Boundary

The Cambrian-Ordovician Boundary is recognized at different horizons on various continents by utilizing several fossil groups. Conodonts are abundant, diverse, and less provincial and facies-controlled than other fossils in this interval; many species are widespread and some are cosmopolitan. Strata...

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Bibliographic Details
Published in:Geological Magazine
Main Author: Miller, James F.
Format: Text
Language:unknown
Published: BearWorks 1988
Subjects:
Online Access:https://bearworks.missouristate.edu/articles-cnas/3553
https://doi.org/10.1017/S0016756800013029