Sr. Manchester et al., An extinct genus with affinities to extant Davidia and Camptotheca (Cornales) from the Paleocene of North America and eastern Asia, INT J PL SC, 160(1), 1999, pp. 188-207
A new genus of Cornales is recognized based on infructescences and foliage
from the Paleocene of Wyoming, Montana, and North Dakota in the United Stat
es; southern Alberta, Canada; Heilongjiang, northeastern China; and Kamchat
ka and the Koryak Upland, northeastern Russia. Amersinia obtrullata gen. et
sp. nov. has globose to ellipsoid infructescences with four or five basal
deciduous bracts and numerous obtrullate, trilocular fruits with epigynous
calyces. Each locule bears one seed and has a dorsal germination valve near
the apex. The infructescences and fruits show many similarities to those o
f extant Camptotheca, but the extant genus is distinguished by only one or
two locules and the absence of infructescence bracts. Fossil leaves previou
sly assigned to "Viburnum" cupanioides (Newberry) Brown, Viburnum kingiensi
s Chelebaeva, and Viburnum pseudoantiquum Golovneva are transferred to the
extinct foliage genus Beringiaphyllun gen, nov. They are distinguished from
Viburnum by their long petioles and compare favorably to the leaves of ext
ant Davidia. The fossil leaves are elliptical to ovate with pinnate seconda
ry veins, percurrent tertiary veins, and obtuse teeth. Beringinaphyllum lea
ves and Amersinia fruits are considered likely to represent a single extinc
t genus because of their shared cornalean affinity and co-occurrence at num
erous sites both in North America and Asia. Although the leaves share more
characters with Davidia, the Amersinia fruits share more characters with Ca
mptotheca. The existence of Amersinia and Beringiaphyllum both in Asia and
North America, together with their absence or rarity in the Paleogene of Eu
rope, indicates that this plant probably dispersed across Beringia in the l
ate Cretaceous or early Tertiary.