AXSMITH, BRIAN1* and MICHAEL KRINGS2. 1Department of Biological Sciences, LSCB 124, University of South Alabama, Mobile, Alabama, 36688; 2Department of Ecology and Evolutionary Biology, University of Kansas, Lawrence, Kansas, 66045. - An alternative reconstruction of the cheirolepidiaceous conifer Pseudofrenelopsis parceramosa.
Leafy shoots of the cheirolepidiaceous conifer Pseudofrenelopsis
parceramosa are a common and widespread component of many Lower
Cretaceous floras in North America and Europe. Based on material from
Great Britain, Alvin and colleagues have reconstructed the source
plant of these shoots as a large tree with whorled lower order
branches and spirally arranged ultimate shoots and leaves. Although
such phyllotactic shifts are otherwise unknown among extant and fossil
conifers, this reconstruction is, nevertheless, based on convincing
association and anatomical evidence. We have undertaken an alternative
reconstruction of the Pseudofrenelopsis parceramosa source
plant based on new material from a locality in southwestern Arkansas
originally described by Stanley and Delevoryas. Unfortunately, much of
the earlier collection has been lost. The new fossils were recovered
by screening clay collected along a stream bank exposure of the Holly
Creek Formation. Although the gross morphological and cuticular
features of the ultimate leafy shoots examined to date essentially
conform to the British specimens, all of the branches, including the
largest specimens representing lower branch orders, exhibit a spiral
arrangement. Furthermore, the pollen cones, which are known from
specimens attached to the leafy shoots, differ from those associated
with the British specimens in several aspects of microsporophyll
morphology, including the shape and the presence of long hairs on the
microsporophyll lamina margin. It is becoming increasing likely that
the fossils from Arkansas and the British material represent two
distinct species of conifer with generally similar ultimate shoots.
This finding may, at least in part, explain the persistent
controversies surrounding the paleoecology of “P. parceramosa,”
and underscores the importance of accurate reconstructions in
elucidating the structure, diversity, paleoecology, and
paleobiogeography of fossil plants. Preliminary information on the
associated, intact ovulate cones and newly discovered fusainized wood
will also be presented.
Key words: Cheirolepidiaceae, conifer, Cretaceous, Mesozoic, Pseudofrenelopsis