Jk. Rigby et Wl. Manger, MORROWAN LITHISTID DEOSPONGES AND HEXACTINELLIDS FROM THE OZARK MOUNTAINS OF NORTHWESTERN ARKANSAS, Journal of paleontology, 68(4), 1994, pp. 734-746
Silicified and well-preserved specimens of the new orchocladine anthas
pidellid genus and species, Virgaspongia ichnata, the rhizomorine hapl
istiid, Haplistion sphaericum Finks, 1960, and various root tufts, and
the new hexactinellid species Steioderma hadra are reported from the
Brentwood Member of the Morrowan Bloyd Formation from the Sulphur City
quadrangle, in the Ozark Mountains of northwestern Arkansas. Virgaspo
ngia is a subcylindrical branched or unbranched sponge that lacks a sp
ongocoel and has a dendroclone-based skeleton in which trabs diverge u
pward and outward from an axial region. It is abundant here but is one
of only a few anthaspidellid genera known from the Pennsylvanian. Thi
s is the first record of Haplistion from Pennsylvanian rocks of Arkans
as, although the genus is widespread in upper Paleozoic rocks. The new
hexactinellid species, Stioderma hadra, also documents the first occu
rrence of that genus from Arkansas and in Morrowan rocks. Only fragmen
ts were recovered but the swollen grotesque spicules, of several sizes
, that make the fused dermal layer and outer sponge wall are distincti
ve, particularly where combined with an inner layer(?) or root tuft of
monaxons of various sizes. Two different root tufts and one demospong
e wall fragment(?) also occur in the collection.