Brief Summary

Read full entry


 Primary thallus: squamulose, persistent; squamules: up to 6 mm long and 4 mm wide, unevenly dentate to crenate-lobate or sinuate, coarsely sorediate (especially under margins), sometimes breaking into masses of soredia; podetia: 6-30 (-40) mm tall, 1-2 mm wide, green to whitish gray, unbranched, with trumpet-shaped cups forming at apices; cups: 2-6 mm wide; margins: entire or minutely dentate; surface: ecorticate or persistently corticated at the base (sometimes cortex extending up to cup bases); soredia: abundant, farinose, sometimes enlarging, later disintegrating and exposing the white medulla; Apothecia: uncommon, brown, up to 1.5 mm diam; ascospores: oblong, 8-14 x 3-4.4 micro meter; Pycnidia: at cup margins, subglobose, with hyaline gelatin; conidia: 7-8 x 1.5-2.5 micro meter; Spot tests: K- or K+ dingy yellow to dingy brown, C-, KC-, P+ brick red, UV-; Secondary metabolite: fumarprotocetraric acid.; Habitat and ecology: on wood, tree trunks, soil or mosses over rocks, usually in deep shade; mainly temperate-boreal; World distribution: on all continents; Sonoran distribution: Arizona, southern California, Baja California and Chihuahua.; Notes: This species is widespread in Arizona but rare elsewhere in the Sonoran Region. Earlier reports from southern California belong either to Cladonia subfimbriata, which has narrower, dentate cups (sometimes cups are missing) and more elongate, whitish podetia, or C. nashii, which has very short podetia with wide cups, like those in C. humilis (see discussion under that species). Cladonia fimbriata is characterized by the green (grayish when exposed so sun), thick, persistent layer of very fine soredia on podetia. The cups are generally symmetrical and often bear fimbriate proliferations on the margin. 


Creative Commons Attribution Non Commercial Share Alike 3.0 (CC BY-NC-SA 3.0)

© Lichen Unlimited: Arizona State University, Tempe.

Source: Lichen Flora of the Greater Sonoran Desert Region

Belongs to 0 communities

This taxon hasn't been featured in any communities yet.

Learn more about Communities


EOL content is automatically assembled from many different content providers. As a result, from time to time you may find pages on EOL that are confusing.

To request an improvement, please leave a comment on the page. Thank you!