Alnus sp.
publication ID |
https://doi.org/ 10.37520/fi.2023.004 |
persistent identifier |
https://treatment.plazi.org/id/4D2487A3-EF4B-8276-FBCF-FBC66D21FF39 |
treatment provided by |
Felipe |
scientific name |
Alnus sp. |
status |
|
Alnus sp. L1
Text-fig. 8a–c View Text-fig
M a t e r i a l. DMNH L6933, DMNH EPI.48136a&b,
DMNH EPI.48179.
L o c a l i t y. Dishbrow Creek.
D e s c r i p t i o n. Leaves simple, elliptical, 5.5–9.2 cm long, 0.7–2.2 mm wide; base and apex acute; petioles 1.6– 2.2 cm long, 0.8–1.1 mm wide; venation pinnate, secondaries arising decurrently, arising at 51° craspedodromous, entering sinuses of large teeth; 0.84 secondaries/cm; tertiaries veins percurrent, opposite and alternate; higher venation not visible; teeth compound, with one large and or two small teeth; large teeth with retroflexed proximal flank, rounded apex and straight distal flank; smaller teeth with concave proximal and distal flanks with acute or rounded apices; 2.68 teeth per cm.
R e m a r k s. Alnus is a microthermal taxon that can be found in riparian areas ( Wing 1987). Fossils of Alnus are known from the early Eocene McAbee, Quilchena and Falkner floras of British Columbia ( Lowe et al. 2018, Mathewes et al. 2016, Smith et al. 2012), Republic flora of Washington ( Pigg et al. 2011), Yellowstone flora of Wyoming ( Wing 1987), the Golden Valley Formation of North Dakota ( Hickey 1977, Wing 1987), mid-Eocene Thunder Mountain flora of Idaho ( Axelrod 1998), White Cliffs flora of the Clarno Formation of Oregon ( Liu et al. 2014), late Eocene Copper Basin flora of Nevada ( Wing 1987), Bull Run flora of Nevada ( Wing 1987), Whitecap Knoll flora of the John Day Formation, Oregon ( Manchester 2000) and Oligocene Ruby Basin of Montana ( Becker 1959) .
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