Numerous anatomically preserved fragments of the Middle Pennsylvanian age f
ilicalean fern, Botryopteris tridentata, occur in coal balls collected at t
he Pittsburgh and Midway Coal Company mine near Baxter Springs, Kansas. Inc
luded are the first fertile specimens of the species, evidence of complete
vegetative frond architecture, and fronds that are specialized for vegetati
ve propagation. Rhizomes are erect and unbranched, have helical phyllotaxis
and short internodes, and typically display an ectophloic solenostele. Fro
nds are tripinnately compound with lobed pinnules that have open, dichotomo
us venation. Fertile pinnae or individual pinnules are interspersed among v
egetative frond segments and produce sori of annulate sporangia beneath vei
ns on the abaxial pinnule surface. Fertile pinnule lobes are rolled toward
the abaxial surface to enclose the sori. Sporangia have a horizontally elon
gated biseriate annulus located near the short broad stark and produce tetr
ahedral-shaped trilete spores with coarse spines. Epiphyllous branches dive
rge from the stipe or rachis, and some fronds produce only branches. This f
ern is reconstructed as having short stems. Helically arranged fronds are e
ither pinnately dissected with lobed vegetative pinnules and abaxially roll
ed fertile pinnules or are specialized for vegetative propagation. The latt
er functioned as the foliar equivalent of stolons. While some characters of
the B, tridentata plant are similar to those of Botryopteris forensis, gen
eritype of the Botryopteridaceae, others are more comparable to those of Ps
alixochlaena cylindrica, generitype of Psalixochlaenaceae, suggesting the n
eed for reevaluation of systematic relationships among species of the Botry
opteridaceae and Psalixochlaenaceae.