Deviacer, Manchester, 1994
publication ID |
https://doi.org/ 10.37520/fi.2023.004 |
persistent identifier |
https://treatment.plazi.org/id/4D2487A3-EF4F-8273-FC67-FC7A6A81F86D |
treatment provided by |
Felipe |
scientific name |
Deviacer |
status |
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Deviacer wolfei MANCHESTER
Text-fig. 7c View Text-fig
M a t e r i a l. USNM PAL 717328.
L o c a l i t y. Disbrow Creek.
Description. Samara 2.1 cm long, 0.7 cm wide at widest point of wing; nutlet elliptical 0.5 cm long and 0.3 cm wide; peduncle persistent, small projection pointing distally along the dorsal side of the wing near the apex of the nutlet; dorsal side of wing slightly convex; ventral side of wing becomes wider just past the nutlet apex and reaches full width ⅔ of the way to the distal end; veins originate near the nutlet apex and curve down to the ventral side of the wing, generally dichotomizing, occasionally anastomosing and cross veins with proximal veins more likely to anastomose.
R e m a r k s. Fruits of Deviacer wolfei are known from the similarly aged Nut Beds of the Clarno Formation of central Oregon; they are samaras with elliptical nutlets, persistent styles, dorsal projections and fall within the same size range and ratios ( Manchester 1994, Chen and Manchester 2015). Deviacer fruits that appear similar but are unassigned to a species are also known from the early Eocene Republic flora of eastern Washington ( Pigg et al. 2008) and early Eocene Falkland flora of British Columbia ( Smith et al. 2012). Late Paleocene fossil fruits with this morphology from Almont, North Dakota with anatomical preservation were named Paleosecuridaca PIGG, DEVORE et M.F. WOJC. ( Pigg et al. 2008) . According to those authors, similarities suggest that at least some of these fruits are assignable to Polygalaceae .
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