Fagus (Fagaceae) Fruits, Foliage, and Pollen from the Middle Eocene of Pacific Northwestern North America

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Fagus (Fagaceae) Fruits, Foliage, and Pollen from the Middle Eocene of Pacific Northwestern North America 1509 Fagus (Fagaceae) fruits, foliage, and pollen from the Middle Eocene of Pacific Northwestern North America Steven R. Manchester and Richard M. Dillhoff Abstract: Fruits and leaves from the Middle Eocene of McAbee, British Columbia, and Republic, Washington, provide an earlier record for the genus Fagus than previously accepted for this member of the Fagaceae. The fruits are trigonal nuts borne within spiny four-valved cupules on long peduncles. The leaves are borne alternately on the twigs and are ovate to elliptic with craspedodromous secondary veins and simple teeth distributed one per secondary vein. The shale preserving these megafossils also contains dispersed pollen with morphology and ornamentation diagnostic of Fagus. Previously, the oldest Fagus occurrences confirmed by fruits were early Oligocene (ca. 32 Ma). The recognition of Middle Eocene (ca. 50 Ma) representatives helps to reduce the disparity between molecular evidence favoring Fagus as a primitive genus within Fagaceae, and fossil evidence, which had indicated older occurrences of Castanea and Quercus than Fagus. Key words: Eocene, Fagus, fossil, foliage, fruits, British Columbia. Résumé : Des fruits et des feuilles de l’Éocène moyen provenant de McAbee en Colombie-Britannique, et de Republic dans l’État de Washington, constituent une mention antérieure pour le genre Fagus, par rapport à ce qui est générale- ment accepté pour cette entité des Fagaceae. Les fruits sont des noix à trois côtés, développées dans des cupules à quatre valves portées sur de longs pédoncules. Les feuilles se forment en alternance sur les rameaux; ils sont ovés à el- liptiques avec des veines secondaires craspédodromes et des dents distribuées à raison d’une par veine secondaire. Le schiste préservant ces méga-fossiles contient également des pollens dispersés, avec une morphologie et une ornementa- tion caractéristiques des Fagus. Auparavant, la mention la plus ancienne des Fagus, confirmée par des fruits, provenait du début de l’Oligocène (ca 32 Ma). La reconnaissance de représentants de l’Éocène moyen (ca 50 Ma) aide à réduire la disparité entre les preuves moléculaires favorisant les Fagus comme genre primitif des Fagaceae, avec les preuves fossiles, qui indiquait une préséance des Castanea et des Quercus, par rapport aux Fagus. Mots clés : Éocène, Fagus, fossile, feuillage, fruits, Colombie-Britannique. [Traduit par la Rédaction] Manchester and Dillhoff 1517 Introduction years the earliest fruit records of other extant genera includ- ing Castanea (Middle Eocene of Tennessee; Crepet and Beech trees have an extensive fossil record in the North- Daghlian 1980; personal observations) and both Castanopsis ern Hemisphere based on foliage and fruits of the genus and Quercus (Middle Eocene of Oregon; Manchester 1994). Fagus. The fossil occurrences have been reviewed in system- The relatively late occurrence of Fagus compared with other atic treatments of this genus in the European (Kva ek and extant and fossil genera of the family seemed paradoxical in Walther 1991a, 1991b; Denk and Meller 2001) and Asian view of molecular data suggesting a basal divergence of (Tanai 1974, 1995; Iljinskaya 1982; Liu et al. 1996; Uemura Fagus from other Fagaceae species (Manos et al. 2001; Li et 1980) Tertiary. al. 2004). Cupules of Fagus are similar in appearance to Fagus pacifica Chaney from the early Oligocene Bridge those of the Southern Hemisphere genus Nothofagus, which Creek flora of Oregon (Chaney 1927; Meyer and Manchester formerly was also included in the Fagaceae; however, that 1997; Denk and Meller 2001) has been regarded as the old- genus differs substantially from Fagus and other genera of est occurrence of this genus based on both fruits and leaves. the family in pollen morphology, leaf architecture, and chro- However, the Oligocene age of about 32 Ma indicated for mosome number, supporting its recognition as a separate the Bridge Creek flora postdates by more than 22 million family, Nothofagaceae (Nixon 1989). Leaves resembling Fagus were previously recognized Received 19 March 2004. Published on the NRC Research Press Web site at http://canjbot.nrc.ca on 9 November 2004. from the Middle Eocene of Republic Washington, One Mile Creek, British Columbia (Gandolfo 1996), and sites in China S.R. Manchester.1 Florida Museum of Natural History, (Liu et al. 1996), but until recently, the lack of convincing Gainesville, FL 32611, USA. reproductive structures caused us to regard the identification R.M. Dillhoff. Evolving Earth Foundation, P.O. Box 2090, of the leaves as Fagus as tentative. Recently, the fossil re- Issaquah, WA 98027, USA. cord of Fagus has been extended back to the Middle Eocene 1Corresponding author (e-mail: [email protected]). based on cupule and nut impressions mentioned and figured Can. J. Bot. 82: 1509–1517 (2004) doi: 10.1139/B04-112 © 2004 NRC Canada 1510 Can. J. Bot. Vol. 82, 2004 by Pigg and Wehr (2002) from the Middle Eocene of Wash- ETYMOLOGY: This species is named to honor David Langevin ington, USA, and British Columbia, Canada. In the present whose love of the McAbee site has lead to the discovery and paper, we formally describe this new species, based on co- conservation of numerous important fossil specimens. occurring reproductive organs and leaves from the Middle Eocene lacustrine shales of McAbee, western British Colum- DIAGNOSIS: Pedunculate cupules. Cupule ovate, composed of bia. four ovate valves fully enclosing two trigonal nuts. External surface with spiny appendages occasionally bifurcate near tip. Peduncle long (up to 2.5 times as long as the cupule), Materials and methods thickened near junction with cupule. Nuts triangular in cross This investigation was based on specimens from three lo- section, ovate, elliptical, to obovate in face view, with a nar- calities of similar Middle Eocene age. Most of the speci- row wing or flange developed along the three angles of the mens of leaves and fruits were collected from the McAbee nut. Sepals arising from apex of nut and surrounding the locality, situated at N50°47.818′ W121°08.568′ near the town three styles. of Cache Creek, British Columbia. Additional leaves (e.g., Gandolfo 1996, Fig. 5) and a few nuts (e.g., Pigg and Wehr DESCRIPTION: Cupule (Figs. 1A–1I) ovate, 10–14 mm in 2002, Fig. 15) were observed in collections from Republic, length and 8–13 mm wide, composed of four ovate valves, Washington. Rare leaves of the same kind were also ob- fully enclosing two trigonal nuts. Appendages spiny, up to served from the One Mile Creek site, near Princeton, British 1.2 mm long, and occasionally bifurcate near tip (Fig. 1F), Columbia (e.g., Gandolfo 1996, Fig. 6). This analysis was often lacking basally (by abrasion). Peduncle long (up to based primarily on specimens deposited at the Burke Mu- 2.5 times the cupule length), up to 29 mm long and 1.9 mm seum (UWBM), Seattle, Washington, University College of thick, thickened near junction with base of cupule (Fig. 1C). the Cariboo, Kamloops, British Columbia, Canada (UCC), Nuts (Figs. 1J–1M) triangular in cross section, ovate, ellipti- and the Florida Museum of Natural History (UF), Gaines- cal, to obovate in face view, length 7.0–10.5 mm, width 4.5– ville, Florida. 7.5mm, a thin wing or flange developed along the three an- To determine whether Fagus pollen was deposited along gles of the nut (or apparently absent; see discussion). Sepals with the fruit and leaf remains, a small piece of shale bear- up to 1.3 mm long, arising from apex of nut and surrounding ing a Fagus leaf impression from McAbee was crushed and the three styles, which are 1.3–2.5 mm long (Fig. 1M). processed for dispersed pollen. The sample was digested in Leaves alternate, subtending enlarged, rounded, non- hydrofluoric acid and then washed in water. The organic res- stipitate, axillary buds. Petiole slender (0.8–1 mm thick), idue was extracted using heavy liquid (a saturated solution 7−13 mm long. Lamina ovate to elliptic, 52–193 mm long, of ZnCl). The resulting residue contains cuticle fragments as 27–74 mm wide, average L:W ratio 2.1:1, symmetrical well as pollen and spores. Attempts at further processing (Figs. 2B–2D) to asymmetrical (Figs. 2A, 2F, and 4B) at the (such as the standard treatment in Schultze’s solution fol- base; basal angle acute (Fig. 2C) to rarely obtuse (Fig. 2D), lowed by KOH) resulted in selective destruction of the more basal flanks typically convex, occasionally cuneate or decur- fragile palynomorphs including Fagus. Therefore, the un- rent; apex angle acute, with typically convex flanks. Margin macerated residue was simply washed in water and mounted serrate (Figs. 2A and 2B) to subtly crenate (Figs. 2C, 3A, for study by light and scanning electron microscopy (SEM). and 3B). Venation pinnate, craspedodromous. Primary vein A drop of the residue was evaporated onto a circular glass moderately thick, straight, not sinuous. Secondary veins 9– coverslip, which was temporarily mounted face-up on an 17 pairs, (mean 11), arising decurrently from the primary at aluminum stub for SEM. After locating and imaging Fagus angles of 40–60° (decreasing apically), markedly parallel grains by SEM, the coverslip was removed from the stub, and uniform, straight to slightly concave. Intersecondaries, and mounted face-down with a drop of glycerine jelly on a agrophic and fimbrial veins absent. Tertiary veins percurrent, glass microscope slide for light microscopy of the same pol- mostly opposite, occasionally alternate, straight to sinuous, len grains. spaced 1.4–3.5 mm apart (3 to 7 per cm) at angles of 135– 150° near base and 105–130° apically; increasing basally. Quaternary veins alternate percurrent to regular polygonal Systematics reticulate, 4th and 5th order veins forming an orthogonal Family Fagaceae reticulum, areolation well developed (Fig. 3E) consisting of Genus Fagus L.
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