Betula sp.

Smith, MacKenzie A., Greenwalt, Dale E. & Manchester, Steven R., 2023, Diverse Fruits And Seeds Of The Mid-Eocene Kishenehn Formation, Northwestern Montana, Usa, And Their Implications For Biogeography, Fossil Imprint 79 (1), pp. 37-88 : 58

publication ID

https://doi.org/ 10.37520/fi.2023.004

persistent identifier

https://treatment.plazi.org/id/4D2487A3-EF4A-8276-FEFE-FEA86DD8FC30

treatment provided by

Felipe

scientific name

Betula sp.
status

 

Betula sp.

Text-fig. 8g View Text-fig

M a t e r i a l. USNM PAL 624925.

L o c a l i t y. Dakin.

D e s c r i p t i o n. Samara obovate 4.0 mm long, 2.2 mm wide; seed body in center of wing, fusiform 3.0 mm long, 0.8 mm wide; style splits near margin of wing 1.3 mm long, curled; wing 0.6 mm wide and tapers at base.

R e m a r k s. The thin wing that is differentiated from the seed body and long styles of the seed distinguish this specimen as Betula and can be contrasted with the nondifferentiated wing and short styles in Alnus . Betula fossils are known from the early Eocene McAbee, One Mile Creek, Quilchena and Falkland floras of British Columbia ( Crane and Stockey 1987, Lowe et al. 2018, Mathewes et al. 2016, Smith et al. 2012), Republic flora of Washington ( Wolfe and Wehr 1987, Pigg et al. 2011) and late Eocene Bull Run flora of Nevada ( Wing 1987). Alnus appears to be more common in Paleogene deposits compared to Betula , which may be due to temperature or its proximity to the water (pers. obs.).

Kingdom

Plantae

Phylum

Tracheophyta

Class

Magnoliopsida

Order

Fagales

Family

Betulaceae

Genus

Betula

Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF