Permian and Early(?) Triassic radiolarian faunas from the Grindstone terrane, central Oregon

Moderately well preserved Permian (late Wolfcampian, Leonardian, Guadalupian, and Djulfian) and Early(?) Triassic radiolarian faunas from sedimentary mélange cherts of the Grindstone terrane in central Oregon are nearly identical to coeval chert faunas in Japan. These Permian faunas are similar to those used in constructing the radiolarian zonations for Japan and the Tethyan regions. Although several Oregon taxa have been reported from limestone sequences in the central United States, most of the Oregon forms have only been found in cherty rocks and nearly half have not previously been reported from North America. Forty-two taxa belonging to 19 genera (AlbaillellaDeflandre,DeflandrellaDe Wever and Caridroit,EntactiniaForeman,EntactinosphaeraForeman,FollicucullusOrmiston and Babcock,HaplentactiniaForeman,HegleriaNazarov and Ormiston,IshigaumDe Wever and Caridroit,KashiwaraSashida and Tonishi,LatentibifistulaNazarov and Ormiston,LatentifistulaNazarov and Ormiston,NazarovellaDe Wever and Caridroit,NeoalbaillellaTakemura and Nakaseko,ParentactiniaDumitrica,PraedeflandrellaKozur and Mostler,PseudoalbaillellaHoldsworth and Jones,PseudotormentusDe Wever and Caridroit,QuinqueremisNazarov and Ormiston, andTriplanospongosSashida and Tonishi) are systematically treated. Co-occurrences of some species in Oregon indicate that their ranges in North America may differ from those in Japan. This paper also contains the first illustrated record of Early(?) Triassic radiolarians from North America.