Crust fungi (also called corticioid fungi) are of great ecological importance as well as morphological and evolutionary diversity. You can find them almost anywhere where there is wood, growing on the underside of a stick or log, on the bark of living trees, or even on the bottom of leaves, duff, and rocks. They make their living as saprotrophs, eating dead organic matter; or biotrophs, gaining nutrition from a living host. In the latter case, they can be mutualistic, resulting in reciprocal growth and survival benefits for the plant host and the fungus; or pathogenic, thriving at the expense of the plant. While mushroom hunters often scoff at crusts, fungal ecologists increasingly appreciate their importance for forest health and ecosystem functioning (Rosenthal et al. 2017). Saprotrophic crusts are essential recyclers of nutrients in forest ecosystems and mycorrhizal crusts are often the dominant soil symbionts in coniferous forests. Some crusts even form mycorrhizal associations with orchids, meaning we wouldn't have these awe-inspiring flowers without humble crust fungi.
I'll be the first to admit that these aren't the flashiest of organisms. They are usually small and indiscrete, some nothing more than a sheen or different hue on the bottom of a decaying branch. And no, they are not edible. However, some crusts take on wild textures and colors whose evolutionary purpose defies explanation. If one dares to travel to the microscopic realms, they are greeted by truly bizarre structures like swollen oily cells, crystal-shrouded lances, and spiky clubs. To look into the microscope at a crust is to touch down on an extraterrestrial world with fractal geography and ornate constructions. In the study of crusts, you will broaden yourself as a mycologist and become acquainted with the taxonomic and microscpic nuances of almost all of Agaricomycotina.
While crusts often speak for themselves, mycologists do have a technical definition for what constitutes a corticioid fungus. According to Larsson (2007), corticioid fungi are basidiomycetes with effused, resupinate basidiomata; a smooth, merulioid, or hydnoid hymenophore; and holobasidia. However, I prefer the more expansive definition of Gorjón (2020), who defines crust fungi simply as "basidiomycete fungi in which basidiomes are generally resupinate". This means that the fungus belongs to the phylum Basidiomycota (the group of fungi that produce sexual spores on club-like structures called basidia) and generally grows flat along the bottom of a substrate. Beyond that, the spore-bearing surface (hymenium) can be smooth or take on any number of configurations to increase surface area (bumps, folds, pores, or teeth); the fungus can be entirely flat or produce shelf-like caps; or be thin and whispy, thick and rubbery, or whatever it likes. This broad definition naturally butts up against what mycologists refer to as stereoid fungi, a term that refers to fungi with a primarily smooth hymenium and that produce caps, whether or not they also have some resupinate growth (resembling Stereum spp.); it also sometimes results in overlap with other form groups typically treated on their own such as polypores and hydnoid fungi (but never agarics, or gilled fungi).
Despite their apparent simplicity, a precise definition of crust fungi is difficult to formulate because they are a form group (defined by a vaguely similar morphology) rather than a monophyletic group (defined by a shared evolutionary history). In the past, all crust fungi were thought of as closely related species and were placed together in the family Corticiaceae — hence the name corticioid fungus, signifiying an affinity to fungi in the family Corticiaceae. Nowadays, we can sequence an organism's DNA to more accurately determine its relatedness to other species and this has drastically changed corticioid taxonomy. Crust fungi are actually distributed across most of the orders in the the class Agaricomycetes, intermixed with more popular mushrooms such as agarics, polypores, boletes, puffballs, and chanterelles (Hibbett et al. 2014). Related to each of these very different types of mushrooms are crusts that, while looking very similar to each other, are actually only distantly related. This is shown below in Figure 1.
All Agaricomycetes, in fact, may be derived from a crust-like ancestor (Hibbett et al. 2014). Over hundreds of millions of years, fungi have evolved extraordinary shapes, colors, and mechanisms of spore dispersal, but many have retained the crust form, and many others have converged upon this simple morphology. Crusts come and go again and again over evolutionary time like the kneading of dough. As a result, scientists recognize a very large number of crusts (thousands of species) spread across more than 400 genera (Gorjón 2020) and 40 families (Larsson 2007). About 1000 species of crust fungi are known to occur in Canada and the United States alone (Ginns 1998). Given the fact that we have documented less than 10% of all fungi and that relatively little attention has been devoted to crusts, especially in the tropics, the number of species of crust fungi is most definitely far greater.
Figure 1. Boletales, Polyporales, and Russulales are taxonomic orders that we typically associate with non-corticioid mushrooms (boletes, polypores, and agarics, respectively) but actually contain corticioid fungi. This shows that crust fungi are sometimes only distantly related, even if they have a similar morphology.
Why do I collect crusts and why should you? As a mycologist, I am curious about all the members of the Queendom Fungi. When you start foraging, you invariably run into crusts, and start to wonder, "who are you and what are you doing hiding under that log"? Not much accessible yet scientifically detailed information exists on the internet about crusts. I hope that CrustFungi.Com fills this niche so that interested individuals may better understand corticioid fungi. However, given that crusts are sadly understudied and underexplored, it will inevitably fall short. If you are intersted in discovering new species or having a large contribution to the documentation of the biogeography and ecology of fungi, whether as a community scientist or professional mycologist, crusts certainly have a lot to offer.
Unlike the meditative wanderings of mushroom hunters, crusts are most easily discovered by meticulously searching a single area with lots of fallen branches. While crust fungi might be visible on the tops of the branches, you'll find the greatest diversity by picking the branches up and scanning their undersides. Log rolling is another fruitful method — you will be delighted by all the different organisms that grow and live on and under a large log, even when it is cold out. Success is maximized by looking under woody debris of multiple tree species, sizes, and stages of decay, as different crusts have different ecological and successional preferences, with newly fallen wood being the least interesting. The bark and dead branches of standing trees and shrubs are great places to find hardy species that don't mind drying out. More elusive species, like ectomycorrhizal crusts, often grow on the bottom of leaf debris and conifer duff, and are suprisingly prevalent on the underside of rocks (scree or lapidicolous fungi). Wooden debris in wet areas like bogs, marshes, riverbeds, and sea shores (yes, there are marine crusts!) sometimes harbor very unique species. Other specialty crusts can be found on diverse substrates such as lichens, herbaceous debris, and dead ferns, which are particulary small, delicate, and understudied. Finally, human constructions such as wooden fences, posts, railings, and bridges apparently also harbor small and rarely collected species (Hjortstam et al. 1973).
Many crusts are impossible to identify to species without microscopic study or DNA sequencing. I assume you have access to a compound microscope (one with up to 1000x magnification) in my comments below. If you do not have access to a microscope, some charismatic crusts can be identified by their macromorphology alone; check out the synoptic key or browse the photos on the species page to see if any are a good match. Regardless, succesful identification begins with close inspection of the crust and careful notetaking of its traits that are discernable by the naked eye. First, when and where did you find it? What is the substrate, the type of associated rot if a wood-decay fungus (only a few genera produce brown rot, which makes identification of brown-rot crusts easier), and nearby trees? If it is not a "typical" crust growing on the underside of a branch or log, this is important to note.
Then, what can you observe about the growth of the crust (open up the glossary in a new tab to read more about these and following terms)? Note the colors of the fruiting body, the hymenophore configuration, and its consistency. Make sure to also note what is going on along the expanding edge of the crust. Is the margin a distinct color from the rest of the fruiting body? How are the hyphae growing? Observation of these features is aided by a small hand lens or jeweler's loupe.
Once you have observed all these traits and photographed the crust in situ, collect a sample for further study. A good knife is usually sufficient, but a small axe or saw may be necessary to handle hard wood. In whatever container you carry the specimen (plastic tackleboxes with adjustable walls work really well), try to place it in the same orientation that it was growing. Basidiomycete fungi will often reorient themselves so that their spores fall in the same direction as gravity. This is most noticeable with gilled mushrooms, which, if placed horizontally over a few hours, will completely bend over so that their gills are facing down. In the case of crust fungi, if placed upside down, the hyphae may start to grow into the spore-bearing surface resulting in a fuzzy appearance and challenging microscopy.
Back at home, you can try to get a spore print by putting the crust hymenium-side down on a piece of aluminum foil or a glass slide and placing a wet paper towel or cloth on top over night. The next morning, you may find a cloudy deposit of spores. Most crust fungi produce white spore prints, but you may collect some with spore prints that are brown, orange, or other colors. A spore print serves multiple purposes. For one, measuring spores will be a breeze: rather than tediously searching for spores in a squash mount, you have thousands that can be quickly scraped onto a slide and viewed and measured under the microscope. Second, the crust can be cultured from the spores for further study in the lab or to sequence its genome. Third, some mycologists toss crusts that do not produce spore prints because these are likely to be infertile (without basidia or basidiospores), making identification challenging to impossible. Crusts should be dried at room temperature or in a dehydrator at low temperature (approximately 95 ˚F) as soon as possible after collection and acquiring a spore print. The specimens should be totally dried before storage, but should not be exposed to extreme temperatures in the dehydration process as this will modify or damage the microscopic structures.
It is important to mention that you do not need to do microscopy on crusts when they are fresh (so-called vital taxonomy). In fact, crust species are described after being dried and therefore it is possible identification will be thrown off by unaccounted-for differences of the fungus in the fresh state. Depending on the thickness or hardness of the crust, a vertical section or scraping can be made. For more robust crusts, cut as thin of a section of the crust as possible with a single-edge razor blade, ideally under a dissection microscope. A good section will be so thin that it curls like a pencil shaving and include all layers of the fruiting body, from the substrate to the hymenium. Transfer the section to a drop of mounting medium on a glass slide, place a cover slip on top, and gently tap with a pencil eraser. For thin or otherwise insubstantial crusts, a scraping can be made by first dipping the razor blade in the mounting medium and then touching the razor blade to the crust to wet a small area. Scrape or cut a small amount of tissue and transfer to the drop on the slide. Various mounting media and stains can be used, and each is good for its own purposes (check out the glossary). If the section or scraping is thoroughly crushed by putting pressure on the cover slip, this is referred to as a squash mount.
Now that you have prepared a slide, observe the thickness and makeup of the different layers of the crust. This is best accomplished with a very thin, full section of the fruiting body that has not been crushed. Following that, make notes and measurements of the following traits, which are crucial for identification (and often easier to observe after thoroughly squashing the tissue): hyphal system and clamp connections; number of sterigmata on the basidia and basidia shape and size; basidiospore shape, size, ornamentation, and chemical reactions; and sterile structures such as cystidia. Often times multiple slides will have to be prepared from different parts of the crust to observe all these different features. It is also usually necessary to observe these traits in different media. For example, KOH stained with phloxine B is my default mounting medium, but Melzer's reagent is necessary to observe amyloidy of spores or other structures, and water may be necessary to accurately observe traits that dissolve in KOH (like halocystidia).
The first true compendium of crust fungi was Hyménomycètes de France by Bourdot and Galzin, published in 1928. Around 50 years later, The Corticiaceae of Europe in eight volumes (1973-1988) by Eriksson, Ryvarden, and colleagues became the new standard for corticiology. Today, Fungi Europaei, Volume 12: Corticiaceae s.l. (2010) by Bernicchia and Gorjón is the most useful reference available. While general treatments of North American crusts are relatively scarce, The Resupinate Non-poroid Aphyllophorales of the Temperate Northern Hemisphere (1980) by Jülich and Stalpers contains some good information and Stereoid Fungi of America (2010) by Ryvarden discusses many crusty fungi as well.
For assistance in identification, general questions related to crust fungi, and community support, I recommend you join the group Crust Fungi and Polypores on Facebook. With over 3000 members across the world, it is an amazing forum to share and learn about crusts. Other useful online resources related to crust fungi include MushroomExpert.Com, Gary Lincoff's website with a gallery of 21 common crusts, Danny Miller's pictoral key to Pacific Northwest crusts, and the very excellent website Crusts and Jells.
Ginns, J. (1998). How many species are there? Folia Cryptogamica Estonica, 33, 29–33.
Gorjón, S. P. (2020). Genera of corticioid fungi: Keys, nomenclature and taxonomy. Studies in Fungi, 5(1), 125–309. DOI
Hibbett, D. S., Bauer, R., Binder, M., Giachini, A. J., Hosaka, K., Justo, A., … Thorn, R. G. (2014). Agaricomycetes. In D. J. McLaughlin & J. W. Spatafora (Eds.), Systematics and Evolution: Part A: Second Edition (pp. 379–429). DOI
Hjortstam, K., K.-H. Larsson, & L. Ryvarden (1988). The Corticiaceae of North Europe, Volume 1. Fungiflora, Oslo, Norway.
Larsson, K.-H. (2007). Re-thinking the classification of corticioid fungi. Mycological Research, 111(9), 1040–1063. DOI
Rosenthal, L. M., Larsson, K.-H., Branco, S., Chung, J. A., Glassman, S. I., Liao, H.-L., … Bruns, T. D. (2017). Survey of corticioid fungi in North American pinaceous forests reveals hyperdiversity, underpopulated sequence databases, and species that are potentially ectomycorrhizal. Mycologia, 109(1), 115–127. DOI