Sy. Smith et Ra. Stockey, A new species of Pityostrobus from the lower Cretaceous of California and its bearing on the evolution of Pinaceae, INT J PL SC, 162(3), 2001, pp. 669-681
A single cylindrical, abraded cone specimen has been found associated with
ammonites of the Lower Cretaceous Budden Canyon Formation near Ono, Califor
nia. The specimen was embedded in bioplastic and sectioned using the cellul
ose acetate peel technique. The pith is composed of parenchyma and scattere
d sclereids and is bounded by a ring of resin canals. The secondary xylem o
f the cone axis, with a ring of small-diameter resin canals, is continuous.
The cortex is composed primarily of parenchyma with an outer sclerotic zon
e 10-16 cells thick and has 27-30 dilating resin canals. Vascular traces to
the ovuliferous scale and bract diverge separately from the vascular cylin
der and are accompanied by a single resin canal from the pith that is posit
ioned between the arms of the horseshoe-shaped ovuliferous scale trace. The
bract trace is terete, accompanied by two lateral resin canals from the co
rtical axial system, and enters the free part of the bract. The ovuliferous
scale is almost completely sclerotic, with resin canals both abaxial and a
daxial to the vascular strands. A large interseminal ridge is present betwe
en the two winged seeds on each scale. This cone represents a new species o
f Pityostrobus and is described as Pityostrobus californiensis sp. nov. A p
hylogenetic analysis using morphological data from the ovulate cones of all
the extant and fossil taxa of Pinaceae, as well as those of Cryptomeria ja
ponica, Sciadopitys verticillata, and Pararaucaria patagonica, was done. Re
lationships of the fossil species of Pityostrobus, Obirastrobus, and Pseudo
araucaria to the living taxa of Pinaceae were assessed. The idea that Pityo
strobus represents an artificial assemblage of pinaceous taxa is supported
by the analyses. The genus Obirastrobus cannot be distinguished from Pityos
trobus species, while Pseudoaraucaria species appear as a clade. The diffic
ulty of basing fossil taxa purely on cone characteristics is discussed in l
ight of the analyses.