Ra. Stockey et al., Permineralized ferns from the middle Eocene Princeton chert. I. Makotopteris princetonensis gen. et sp nov (Athyriaceae), INT J PL SC, 160(5), 1999, pp. 1047-1055
The occurrence of numerous anatomically preserved specimens of an extinct f
ilicalean fern in the middle Eocene Princeton chert from southern British C
olumbia, Canada, provides the basis for characterizing a new genus and spec
ies of the Athyriaceae. Fossils include narrow horizontal rhizomes with a r
adial amphiphloic dictyostele and internodes up to 1.5 cm long. Fronds are
monomorphic. Adventitious roots are diarch and display a parenchymatous cor
tex. Stipes diverge in a radial fashion and display two hippocampiform bund
les at the base. Distally, the bundles unite into a single trace, and pinnu
les are produced in an opposite to subopposite arrangement. The stipe, rach
is, and pinnules display a continuous U-shaped groove on the adaxial surfac
e. Sori of annulate sporangia are borne below veins on swollen receptacles.
The sporangia are characterized by a vertical annulus and a narrow, elonga
ted stalk. Spores are monolete and ellipsoidal, with a psilate exine and a
distinctly spiny perispore, Makotopteris princetonensis gen. et sp. nov. si
gnificantly increases our knowledge of the fossil record for the Athyriacea
e and documents that essentially modern athyrioids were present in the flor
a of North America by the early Tertiary.