A late Frasnian (Late Devonian) radiolarian, sponge spicule, and conodont fauna from the Slaven Chert, northern Shoshone Range, Roberts Mountains allochthon, Nevada
Sq. Boundy-sanders et al., A late Frasnian (Late Devonian) radiolarian, sponge spicule, and conodont fauna from the Slaven Chert, northern Shoshone Range, Roberts Mountains allochthon, Nevada, MICROPALEON, 45(1), 1999, pp. 62-68
Co-occuring conodonts, radiolarians, and sponge spicules from the type loca
lity of the Slaven Chert, northern Shoshone Range, Nevada, indicate that th
e radiolarian and sponge spicule assemblage described herein correlates wit
h the Late rhenana conodont Zone (late Frasnian). The moderately well prese
rved radiolarians are the first Frasnian-age fauna described from the Weste
rn Hemisphere. They include spumellarians, Ceratoikiscum, and Paleoscenidiu
m, and a radiolarian which we have assigned to a new genus, Durahelenifore
Boundy-Sanders and Murchey, with its type species, Durahelenifore robustum
Boundy-Sanders and Murchey. Sponge spicules include umbellate microscleres
of the Subclass Amphidiscophora, Order Hemidiscosa, previously documented o
nly in Pennsylvanian and younger rocks.