Celtis
publication ID |
https://doi.org/ 10.37520/fi.2023.004 |
persistent identifier |
https://treatment.plazi.org/id/4D2487A3-EF4D-8277-FBB8-FA966E79FB4F |
treatment provided by |
Felipe |
scientific name |
Celtis |
status |
|
Genus Celtis View in CoL L.
Text-fig. 7j, k View Text-fig
M a t e r i a l. UF 19652-86483, 19652-86484, 19652-
86485, 19652-86486, 19652-86487, 19652-86488.
L o c a l i t y. M3.
D e s c r i p t i o n. Endocarp calcareous, ovoid, 4.7 mm long, 3.5 mm wide, with reticulate surface ridging, areoles of the reticulum square; endocarp 7 squares wide and about 8 squares tall.
R e m a r k s. A calcified endocarp with reticulate sculpture enables us to place this fossil in Celtis . Such endocarps are commonly known from Eocene deposits ( Manchester 1989, 1994).
Family Juglandaceae DC. ex PERLEB
Genus Palaeocarya SAPORTA
Text-fig. 8i View Text-fig
M a t e r i a l. USNM PAL 622690.
L o c a l i t y. Disbrow Creek.
D e s c r i p t i o n. Winged fruit incomplete, 2.1 cm long and 1.7 cm wide; main wing trilobed; lobes lanceolate diverging at 46.4°, middle lobe 7.0 mm wide and lateral lobes 5.4–5.8 mm wide; wing lobes possessing three main veins, each with the midvein being the thickest; lateral ascending veins dissipate into loops distally, epimedial veins mostly perpendicular, exmedial veins branching apically, veins visible up to third order. Prophyllum ca. 0.8 cm long and 0.6 cm wide with straight, unbranched trichomes below the wing measuring between and 1.7 to 3.7 mm long.
R e m a r k s. Palaeocarya is a fossil genus that accommodates fruits with trilobed wings, similar to those of the extant genera, Engelhardia LESCH. ex BLUME of Asia and Oreomunnea of Central America. Distinctions between species of the extant genera and in Palaeocarya can be made in part by wing venation patterns ( Manchester 1987). Only the basal portions of the wings are seen in this specimen. Palaeocarya clarnensis MANCHESTER and P. uintaensis (MACGINITIE) MANCHESTER both appear to have three main veins in the basal portion of their wings, however, the lateral veins of P. uintaensis become secondary loops more apically ( Manchester 1987) whereas P. clarnensis has a pubescent nutlet base ( Manchester 1987) like this fossil. Because this fossil shares features of both species and P. uintaensis is known from only one specimen, this fossil is not being assigned to a species. More specimens may help resolve its taxonomic affinity. P. clarnensis has been observed in collections from the Green River Formation (Little Mountain, Wyoming) as well as from the Clarno Formation (West Branch Creek and Gosner Road, Oregon), with the Clarno localities being a similar age to the Kishenehn Formation ( Manchester 1987). P. uintaensis is known only from the Green River Formation (Rainbow, Utah) ( MacGinitie 1969, Manchester 1987).
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