An extinct genus with affinities to extant Davidia and Camptotheca (Cornales) from the Paleocene of North America and eastern Asia

Citation
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
Citations number
41
Categorie Soggetti
Plant Sciences
Journal title
INTERNATIONAL JOURNAL OF PLANT SCIENCES
ISSN journal
10585893 → ACNP
Volume
160
Issue
1
Year of publication
1999
Pages
188 - 207
Database
ISI
SICI code
1058-5893(199901)160:1<188:AEGWAT>2.0.ZU;2-1
Abstract
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.