Cones from the Early Cretaceous of southeastern Victoria, and Middle J
urassic of southeastern Queensland are described and illustrated. They
are compared with Palissya bartrumi from the Jurassic of New Zealand
and the Palissya type material, P. sphenolepis, from the Liassic of Sw
eden and Germany. Cones from Australia and New Zealand share the same
basic structure. They are composed of stalked sporophylls arranged hel
ically on a central axis, with paired, cup-shaped processes attached a
daxially to the sporophyll blade. These processes surround indentation
s in the sporophyll surface that are probably the sites where seeds we
re once attached. Morphological differences, the number of adaxial pro
cesses pet sporophyll, and geographical and chronological separation,
are the basis for describing the Victorian and Queensland specimens as
several new species.