Abundant and morphologically fairly diverse siliceous sponge spicules of Da
rriwilian (Middle Ordovician) age were collected from the Table Cove Format
ion of Port au Port Peninsula, western Newfoundland. Without co-occurrence
of appropriate sponge body fossils, it is difficult to refer these disartic
ulated sponge spicules to existing or to new taxa. However, representatives
of demosponges and hexactinellids are recognized. While marked differences
are noted between older and younger lithistid dendroclones, for example, s
picule form in these Middle Ordovician specimens is similar overall to prev
iously known assemblages of various ages, demonstrating the morphologically
conservative nature of the spicular skeleton.