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...
Published in: | Geological Magazine |
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Main Author: | |
Format: | Text |
Language: | unknown |
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BearWorks
1988
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Online Access: | https://bearworks.missouristate.edu/articles-cnas/3553 https://doi.org/10.1017/S0016756800013029 |