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Bromus briziformis

Species of grass


Summary

Species of grass

Bromus briziformis is a species of brome grass known by the common name rattlesnake brome. The specific epithet briziformis comes from the resemblance of the grass to grasses of the genus Briza, particularly Briza maxima. The common name is derived from the resemblance of the spikelets to the rattles of rattlesnakes. The grass has a diploid number of 14.

Description

Bromus briziformis is an annual grass, with erect or ascending culms growing 20-80 cm tall. The leaf sheaths are shaggy and ligules, measuring 0.5-2 mm long, are densely hairy. The leaf blades are 3-13 cm long and 2-4 mm wide, and are lightly hairy to glabrous on both sides. The lax and secund panicles have long spreading or drooping branches that bear solitary terminal spikelets. The panicles are 5-15 cm long and 3-7 cm wide, and the branches are typically longer than the spikelets. The flat spikelets are 15-27 mm long and 0.8-1.3 cm broad. The glumes are smooth or slightly scabrous. The lower glumes are three to five-veined and 5-6 mm long, and the upper glumes are seven to nine-veined and 6-8 mm long. The lemmas are ovate or slightly rhombic, have broad translucent margins, and are awnless. The anthers are 0.7-1 mm long. The caryopses are as long or shorter than the paleas, and are flat or slightly rolled inwards.

Habitat and distribution

Bromus briziformis grows in waste areas, disturbed areas, and road verges, on dry soils. It is native to southwest Eurasia, but naturalized throughout North America from New Mexico up to southern British Columbia, and scattered throughout the eastern United States.

References

References

  1. Merrit Lyndon Fernald. (1970). "Gray's Manual of Botany". D. Van Nostrand Company.
  2. Flora of North America Editorial Committee. (1993). "Flora of North America: North of Mexico". Oxford University Press.
Wikipedia Source

This article was imported from Wikipedia and is available under the Creative Commons Attribution-ShareAlike 4.0 License. Content has been adapted to SurfDoc format. Original contributors can be found on the article history page.

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