Fraxinus sp.

Kovar-Eder, Johanna, Kvaček, Zlatko, Teodoridis, Vasilis, Mazouch, Petr & Collinson, Margaret E., 2022, Floristic, Vegetation And Climate Assessment Of The Early / Middle Miocene Parschlug Flora Indicates A Distinctly Seasonal Climate, Fossil Imprint 78 (1), pp. 80-144 : 95

publication ID

https://doi.org/ 10.37520/fi.2022.005

persistent identifier

https://treatment.plazi.org/id/6E40384F-924C-CE5A-5A5B-D96AA9CF4ADA

treatment provided by

Felipe

scientific name

Fraxinus sp.
status

 

Fraxinus sp.

Pl. 7, Figs 6–8

M a t e r i a l. IBUG 1580, 1617, 1946.

D e s c r i p t i o n. Leaflets sessile; lamina oblong to narrow elliptic or ovate, mostly asymmetrical, occasionally symmetrical, l × w = 43– ~77 × 11–22 mm, ratio l/w = 2.3–3.9, base convex to cuneate, apex acute; margin more or less regularly serrate, teeth tiny, indistinct, not dense; midvein slightly bent; secondaries semicraspedodromous to eucamptodromous, regularly, rather densely spaced, originating at wide to almost right angles; simple intersecondaries rather regularly positioned, tertiaries reticulate, indistinct.

Differing from Ailanthus pythii , Dicotylophyllum sp. 5 , H, W, CC, FF, and GG see those taxa.

Differing from leaflets of Juglans sp. by smaller leaflet size, wider angles of secondaries, more numerous intersecondaries and no indication of percurrent tertiaries.

Kingdom

Plantae

Phylum

Tracheophyta

Class

Magnoliopsida

Order

Lamiales

Family

Oleaceae

Genus

Fraxinus

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