Plerandreoxylon oskolskii, Wheeler & Manchester & Baas, 2023

Wheeler, Elisabeth A., Manchester, Steven R. & Baas, Pieter, 2023, A late Eocene wood assemblage from the Crooked River Basin, Oregon, USA, PaleoBios 40 (14), pp. 1-55 : 40-42

PLERANDREOXYLON OSKOLSKII SP. NOV.

FIG. 19A–G

Diagnosis— Growth rings distinct, marked by radially flattened latewood fibers, and differences in vessel diameter between latewood and earlywood of subsequent rings.

Semi-ring-porous to ring-porous. Vessels solitary and in radial multiples, small clusters in the latewood. Earlywood with multiple rows of vessels, latewood vessels arranged in a tangential to diagonal pattern in narrower rings. Perforation plates simple, intervessel pits alternate, medium to large; vessel-ray parenchyma pits with reduced borders to simple, oval to slightly horizontally elongate. Tyloses present.

Fibers with simple to minutely bordered pits; thin to thick-walled; septate.

Axial parenchyma extremely rare.

Rays predominantly multiseriate, sheath cells occasional, average ray height <1 mm. Rays homocellular, composed of procumbent body cells, or heterocellular with a single marginal row of square cells and weakly procumbent cells. Rays per mm few.

Holotype — UF 278-84872 , estimated maximum diameter 8–9 cm.

Paratype — UF 278-84905 .

Occurrence— Dietz Hill, UF 278.

Etymology— Named for our good colleague and friend Alexei Oskolski who has studied Araliaceae wood and done much to further the field of wood anatomy in general.

Description— Growth rings distinct, marked by radially flattened latewood fibers. Ring-porous to semi-ring-porous. Vessels solitary and in short radial multiples, small clusters in the latewood. Earlywood with multiple rows of vessels; latewood vessels arranged in a tangential to diagonal pattern in narrower rings, mostly in radial multiples, solitary vessels not common ( Fig. 19A, B .). Earlywood vessels 97 (SD=22) µm, range 48–137 µm. Vessel element lengths commonly 350–500 µm. Perforation plates simple ( Fig. 19C ). Intervessel pits alternate, 8–10 µm in horizontal diameter, tending to be angular in outline ( Fig. 19D ); vessel-ray parenchyma pits with reduced borders and oval to slightly horizontally elongate ( Fig. 19E ). Tyloses present ( Fig. 19C, E, G ).

Fibers with simple to minutely bordered pits, septate ( Fig. 19F ), thin to thick-walled.

Axial parenchyma extremely rare.

Rays homocellular, composed of procumbent body cells, or heterocellular with a single marginal row of square cells and barely procumbent cells; sheath cells occasional; 3–7 cells wide, mostly 5–6 cells ( Fig. 19F, G ). Ray height averages 449 (126) µm, range 126–728 µm; 3–4 rays per mm.

Crystals, oil/mucilage cells, storied structure, and radial canals absent.

Comparisons to extant and fossil woods— We searched the InsideWood database multiple times. One search used: distinct growth ring boundaries (1p); wood ring-porous to semi-ring porous (5a, not diffuse-porous); vessels in wavy tangential bands (6p);simple perforation plates (13p); intervessel pits alternate and not minute (22p 24a); vessel-ray parenchyma pits rounded with much reduced borders (30a, 31p); septate fibers (65p); axial parenchyma rare (75p); rays more than 4-seriate, <1 mm high and with one row of square marginal cells (98p 102a 106p); storied structure, oil/mucilage cells, and radial canals absent (118a 120a 124a 125a 126a 130a). The IW matches only included Araliaceae (order Apiales ): two modern ( Aralia elata var. ryukyuensis J.Wen (1994) and Kalopanax septemlobus (Thunb.) Koidz. (1925) , both East Asian) and two fossil woods ( Plerandreoxylon oregonensis Wheeler and Manchester, 2002 , and Aralinium excellens Platen, 1908 ), both from the Eocene of the USA. These two Dietz Hill woods' absence of uniseriate rays and the occasional occurrence of sheath cells are additional features that are consistent with the Araliaceae . Unfortunately, Platen’s Aralinium excellens cannot be placed with certainty in the Araliaceae and reasonably compared with this Dietz Hill (UF 278) wood because its description lacks details on ray cellular composition and height and whether fibers are septate or non-septate ( Platen 1908). Moreover, it was described as having crystals in enlarged cells, a feature not reported for the Araliaceae .

Another search used absence of vessel-ray parenchyma pits similar to intervessel pits (30a) rather than 31p and absence of obvious axial parenchyma features (77a, 79–86a) rather than 75p. This search returned an additional two modern woods ( Aralia spinosa L., 1753; Gamblea ciliata C.B. Clarke, 1879 ; Araliaceae ) and an additional fossil wood ( Evodia gadjirian Gregory, 1976 , from an unspecified Eocene site in the vicinity of Post, Oregon, USA). Unfortunately, the description of the putative Evodia Forst. and Forst. (1775) lacked information on intervessel and vessel-ray parenchyma pitting and ray cellular composition; the accompanying images were at too low of a magnification to determine those details. Whether or not this wood truly is Evodia ( Rutaceae ) or might be Araliaceae is impossible to determine because the location of Gregory’s material is unknown and so it cannot be reexamined.

Alternative searches, e.g., 1p, 4p, 9a, 10a, 13p, 26p, 30a, 31p, 56p, 61p, 65p, 98p, 106p, in addition to Araliaceae , also retrieved two extant species of Toricellia DC (1830) ( Toricelliaceae Hu 1934 ), also in the Apiales . Adams (1949, p. 239) remarked “[the] overall character of the wood is suggestive of araliaceaeous affinities.” Toricellia differs from the fossil in having helical vessel wall thickenings, taller rays (to 1.8 mm), slightly more rays per mm, scanty paratracheal parenchyma more obvious, and conspicuous tyloses ( Noshiro and Baas 1998). Toricellia DC , is known by fruits from the Clarno Nut Beds ( Manchester et al. 2017) but is not known from any Post locality.

There are araliaceous fruits ( Paleopanax oregonensis Manchester, 1994) and two species of fossil wood, Plerandreoxylon nutbedensis Wheeler and Manchester (2002) and Pl. oregonensis Wheeler and Manchester (2002) , known from the middle Eocene Clarno Formation. This Dietz Hill wood agrees with the diagnosis of Plerandreoxylon , aside from “rays usually less than 4-seriate” and so we have emended the diagnosis to rays less than 10-seriate. Plerandreoxylon nutbedensis differs in having some scalariform perforation plates, some scalariform intervessel pitting, with uniseriate rays more common; Pl. oregonensis has mostly non-septate fibers and some scalariform intervessel pitting ( Wheeler and Manchester 2002). We consider these differences sufficient to warrant assigning this wood to a new species of Plerandreoxylon .

Figures

Figure 19. Araliaceae. Plerandreoxylon oskolski sp. nov., UF 278-84906. A. Semi-ring-porous wood with latewood vessels arranged in wavy tangential bands/diagonal arrangement, vessel clusters in latest latewood, axial parenchyma rare, T.S. B. Semi-ring-porous wood, vessels solitary and in short radial multiples, axial parenchyma rare, TS. C. Simple perforation plates, rays with procumbent body cells, RLS. D. Crowded alternate intervessel pitting, TLS. E. Vessel-ray parenchyma pits with reduced borders, oval to slightly horizontally elongate in outline, tyloses, RLS. F. Rays 5-6 cells wide, septate fibers, TLS. G. Rays predominantly multiseriate, TLS. Scale bars: 200 µm in A, B, G; 100 µm in C, F. 50 µm in E; 20 µm in D.