Ra. Stockey et al., PERMINERALIZED FRUITS OF DIPLOPANAX (CORNACEAE, MASTIXIOIDEAE) FROM THE MIDDLE EOCENE PRINCETON CHERT OF BRITISH-COLUMBIA, Review of palaeobotany and palynology, 103(3-4), 1998, pp. 223-234
Over 80 specimens of a permineralized fruit referable to the Cornaceae
(Mastixioideae) have been recovered from the middle Eocene Princeton
chert (Allenby Formation) of British Columbia, Canada. Specimens were
studied using a modified cellulose acetate peel technique using hydrof
luoric acid. Diplopanax eydei Stockey, LePage et Pigg sp. nov has frui
ts with endocarps up to 11 mm long and 10 mm in diameter that have a s
mooth stone surface, a single locule that is U-shaped in cross section
, and a germination valve that extends nearly the full length of the f
ruit. An epicarp (exocarp + mesocarp) composed of thin-walled parenchy
matous cells, 1.2-1.5 mm thick, is preserved on one specimen. Remnants
of an apical disc with possible perianth scars are seen in three spec
imens. The endocarp is composed of interlocking fibers with scattered
resin ducts and vascular tissue that parallels the edges of the valve.
Seed integuments consist of a single external layer of large cells wi
th brown contents and an inner zone of two to four thin-walled cells o
f smaller diameter lacking contents. Numerous septate fungal hyphae ar
e usually present in the integumentary layers. These fruits represent
the first reported fossils of the genus Diplopanax Handel-Mazzetti, an
d the northernmost known mastixioids in North America. The fruits are
compared to those of other living and fossil mastixioids including Mas
tixicarpum Chandler and add to our knowledge of the diversity and dist
ribution of the North American mastixioids during the Tertiary. (C) 19
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