Radiolarians recovered from three sites in the early Llandoverian Cher
ry Spring chert, north-central Nevada, provide the first Early Siluria
n radiolarian data from the conterminous United States. Two assemblage
s were recovered that contain abundant pylomate sphaerellarians, rotas
phaerids, inaniguttids, and possible palaeoactinosphaerids. The pyloma
te taxa have an intermediate spine morphology with Cessipylorum and Ac
iferopylorum, bringing into question the present criteria for distingu
ishing these two genera. Rotasphaerids include both species of Rotasph
aera and Secuicollacta, that have five primary rods per spine unit, si
milar to those present in Ordovician assemblages (Caradocian-Ashgillia
n) reported from Nevada and Australia. Oriundogutta is another common
component shared between the Cherry Spring and Caradocian-Ashgillian a
ge faunas. To a lesser extent. the Cherry Spring fauna resembles late
Early-Late Silurian (Wenlockian-Ludlovian) assemblages that contain ab
undant inaniguttids and rotasphaerids. None of the younger species of
inaniguttids have been recognized, however, and younger species of rot
asphaerids differ in that they have six primary rods per spine unit an
d a more diverse spine morphology. These preliminary data indicate a s
tronger similarity between Late Ordovician and early Llandoverian asse
mblages than between early Llandoverian and Wenlockian-Ludlovian assem
blages. The Cherry Spring chert faunas contain several distinct forms,
such as Cessipylorum(?) sp. A and B, that may prove useful for biostr
atigraphic correlation.