Trifoliolate leaves of Platanus bella (Heer) comb. n. from the Paleocene of North America, Greenland, and Asia and their relationships among extinct and extant Platanaceae
Z. Kvacek et al., Trifoliolate leaves of Platanus bella (Heer) comb. n. from the Paleocene of North America, Greenland, and Asia and their relationships among extinct and extant Platanaceae, INT J PL SC, 162(2), 2001, pp. 441-458
Trifoliolate leaves of Platanus bella (Heer) comb. n., a species previously
known only from the Paleocene of western Greenland, are newly recognized f
rom the Paleocene of northern Wyoming, U.S.A., and Altai of Xinjiang Provin
ce, northwestern China, indicating that the species was circumboreal in the
early Tertiary. Epidermal anatomy preserved in specimens from all three ar
eas confirms that these compound leaves belong to the Platanaceae. Platanus
bella (Heer) comb. n. differs from modern species of Platanus but resemble
s the European Tertiary species Platanus fraxinifolia (Johnson & Gilmore) W
alther and Platanus neptuni (Ettingshausen) Buzek, Holy & Z. Kvacek, in the
presence of large peltate glandular trichomes. We erect a new subgenus, Gl
andulosa, to accommodate P. bella, P. fraxinifolia, and P. neptuni. Each of
these species possesses similar leaf epidermal structure, with the charact
eristic platanaceous stomatal apparatus and compound hair bases. In additio
n, the fossils bear peltate glandular trichomes on the epidermal surfaces t
hat are not known among extant Platanus species. Reproductive structures li
nked to P. neptuni indicate that subgenus Glandulosa is properly placed in
the Platanaceae but that it is a distinct clade from those of the extant su
bgenera Platanus and Castaneophyllum Leroy. We also review the status of th
e fossil genera Debeya and Dewalquea, to which some Cretaceous and Tertiary
leaves of similar morphology have been placed, and reject the use of eithe
r of these names to accommodate leaves of subgenus Glandulosa.