What sets this region apart from much of Canada and even the lower portions of the Yukon Territory is that it escaped glaciation in the last ice age. Dawson City actually has topsoil, which holds not only fungal spores but also mammoth bones and all sorts of curiosities from the Pleistocene era.
I use the field guides for the Northwest Pacific American States as I find the mushrooms in our region key-out most closely — not exactly, but pretty darn close — to the winter species listed there. I use a combination of fruiting body appearance with spore prints and, because I geek out on this sort of thing, microscopic spore examination.
The remnants of the mammoths have long since stopped adapting to the local environment but our mushrooms have continued their own path of adaptation over the intervening tens of thousands of years since those glaciers scraped off all the topsoil between the Tintina Trench and Spokane.
But this year has been a bust. I cannot recall a year so devoid of mushrooms in my time living up north. Not even the usually prolific, hardy and poisonous Cortinarius has appeared. Yesterday I found a portion of a deer mushroom (Pluteus cervinus) which a nervous squirrel dropped as I walked by on a trail. After a good rainfall over the last couple days a pathetic cluster of maggoty puffballs (Bovista plumbea) appeared beyond my doorstep. A week ago I found a couple mummified Lactarius deliciosus or delicious milk cap (not always delicious but always pretty).
And that has been it. My hunch is that it has been too dry this summer to promote decay of the substrates (dead wood, forest floor duff) along with the growth of the fungal mycelia which are the “roots” of a mushroom but actually the largest component of the organism that live for days to hundreds of years. Perhaps if we get more rain and some warm days, we could still see a decent crop of mushrooms. Fingers crossed!
Arora, David. (1991) All that the Rain Promises and More… Berkley, California: Ten Speed Press
Ward, Brent & D. Bond, Jeffrey & Gosse, John. (2007). Evidence for a 55–50 ka (early Wisconsin) glaciation of the Cordilleran ice sheet, Yukon Territory, Canada. Quaternary Research. 68. 141-150. 10.1016/j.yqres.2007.04.002. (Specifically reference to the diagram)