Abstract
Upper Devonian conodonts in the black shales of the Woodford Formation in the Permian Basin are dominated by species of Palmatolpis indicative of the Upper/Uppermost crepida, Lower/Middle marginifera, and Middle expansa zones. Accumulation of these strata corresponds to eustatic deepening pulses and similar depositional settings in the central and eastern North American epicontinental basins.
| Original language | English |
|---|---|
| Pages (from-to) | 271-279 |
| Number of pages | 9 |
| Journal | Stratigraphy |
| Volume | 8 |
| Issue number | 4 |
| State | Published - 2011 |
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