AN OVERLOOKED PERMIAN UNIT IN THE CRAIG QUADRANGLE, ALEXANDER TERRANE, SE ALASKA
In our reconnaissance of the coastal Permian section, we found that the unit strikes approximately parallel to the shoreline and dips steeply to the southwest. It is dominated by rhythmically bedded carbonates that contain lenses of skeletal debris often deposited in cross-bedding. We observed large, abundant brachiopods in one heavily silicified shell bed which included Horridonia, Waagenoconcha, Linoproductus, Meekella, Rhynchonopora, Cleiothyridina, Neospirifer, Timaniella (or Fasciculatia), Spiriferellina, and Dielasma. Together these brachiopods suggest a Middle Permian age. A bryozoan, Tabulipora aff. T. colvillensis indicates a Wordian (Middle Permian) age. Samples processed for conodonts were barren and yielded only a few dermal scutes. Our limited collection appears to be a different fauna than the fossiliferous Permian beds (Halleck and Pybus Formations) on Kuiu Island. This unnamed unit is lithologically distinct from the other Permian formations in the Alexander Terrane.
Southeastern Alaska is not known as an oil-producing area, but the upper Paleozoic conodonts indicate low thermal alteration, and the limestones produce an oil slick when etched in acid. Oil slicks are also noted from the acidization of Middle Devonian limestones in the San Alberto Islands north of Craig.