Equisetum 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 : 40

publication ID

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

persistent identifier

https://treatment.plazi.org/id/4D2487A3-EF5C-8260-FED7-FBC56D4DF8BA

treatment provided by

Felipe

scientific name

Equisetum sp.
status

 

Equisetum sp.

Text-fig. 2a View Text-fig

M a t e r i a l. USNM PAL 620616.

L o c a l i t y. Park.

D e s c r i p t i o n. Stem 20.8 mm long and 2.2 mm wide; 3 nodes, 2 internodes; 5–6 leaves visible per node (estimate fully 10–12 leaves per node); basal leaves 2.9 mm long, 0.5 mm wide at base, apical leaves 5.1 mm long, 0.5 mm wide at base; sheath (excluding leaves) 4.0 mm long.

R e m a r k s. Equisetum commonly grow in wet areas next to streams and ponds and is commonly preserved in the fossil record. The single specimen that we studied is noteworthy in the relatively elongate triangular leaves. Similar species include Equisetum limosum ? L. which has longer internodes ( Lesquereux 1878) and E. winchesteri BROWN from the Green River Formation of Wyoming and Colorado, but E. winchesteri is larger in width and has more leaves ( Brown 1929). Equisetum is also recognized from the early Eocene Okanagan floras of British Columbia ( Smith et al. 2012, Greenwood et al. 2016) and middle Eocene Thunder Mountain flora of Idaho ( Axelrod 1998).

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