SIMS, HALLIE J. Department of Geophysical Sciences, University of Chicago, Chicago, IL 60637. - Contrasting evolutionary trends in seed (ovule) size and megaspore volume during the late Paleozoic.
Seed size reflects a compromise among several factors, including
amount of nutritive tissue supporting the plant’s initial development,
amount of parental investment in individual offspring, and dispersal
mechanism. The late Paleozoic is a key interval to investigate
evolutionary patterns in seed size because it records a major
transition in the structure and composition of terrestrial ecosystems
with the origin of seed plants and increasing prevalence of herbivory.
Although previous works have focused on overall seed size, megaspore
volume is a more accurate estimate of nutritive resources in
propagules and provides a useful alternative to compare with overall
size. Results from a compilation of 650+ Paleozoic seed species
indicate that mean overall size increased steadily through the
Carboniferous and early Permian, reflecting an increase in maximum
size while the smallest sizes were maintained. Because previous
analyses of Cenozoic seed floras indicated a potential latitudinal
gradient to seed size, sampling was restricted to a paleolatitudinal
band (30oN to 30oS). A steep increase in
variance was driven by diversification of genera with large seeds in
several groups of seed plants. This suggests that the earliest were
near a structural or functional boundary at the lower limit and that
open “evolutionary space” lay only toward larger sizes. Although the
overall size distribution moves from positively skewed to more
symmetrical through the late Paleozoic, higher groups (e.g.,
medullosans, cordaites) do not show parallel changes in skewness.
Preliminary analysis of megaspore data indicates that there is also an
increase in mean megaspore volume during the Carboniferous, but that
patterns within groups are not consistent with overall size. The
contrasting large-scale evolutionary trends indicated by these results
suggest that there may have been different mechanisms affecting
overall seed size and megaspore volume during the radiation of seed
plants.
Key words: megaspore, paleoecology, Paleozoic, seed size, seeds, trends