Abstract
Ten samples from a 160m section through the lower Whittaker Formation yielded Red River Province conodonts as well as a shelly macrofossil assemblage representing the "Arctic Ordovician fauna.' Both the microfossils and macrofossils have strong affinites with taxa represented in strata of Cincinnatian age in the western Midcontinent Province of North America. Conodont-based graphic correlation of section W-1 with a Composite Standard Section developed for midcontinental United States indicates that the lower Whittaker Formation on the east flank of the Redstone Arch represents nearly the entire Cincinnatian Series. -from Authors
| Original language | English |
|---|---|
| Pages (from-to) | 74-87 |
| Number of pages | 14 |
| Journal | Canadian Journal of Earth Sciences |
| Volume | 26 |
| Issue number | 1 |
| DOIs | |
| State | Published - 1989 |
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