“what they do in forest systems is take all the leaf litter and any of the decaying organic matter that drops down [onto the forest floor] and very quickly pull it down into the soil, where it’s mobilized and converted into more accessible carbon,” smith says. “as a result, instead of having a soft, spongy forest floor that intercepts water, any rainfall that comes down quickly is going to tend to run off.”
in addition to runoff, earthworm activity changes the soil’s ph balance, reduces fertility, damages intricate root networks, throws the carbon-to-nitrogen ratio out of whack and leaves the soil surface bare, making it more susceptible to erosion, drought and temperature fluctuations. and there’s more.
“you don’t have a buffer—the insulation that leaf litter would normally provide—and so you see exposed tree roots, or tree roots that are higher out of the ground than normal, and they are more likely to suffer from severe cold, especially during spring and fall, when the thaw really impacts plants,” smith says. “so you lose insulation, you lose the sponge that slows water movement down, and yet the processes of nutrient cycling get speeded up.”
the result is decreasing forest productivity, increasing risk of invasion by foreign species, and declining plant and wildlife diversity. that decline extends down to the creatures that normally reside in the diminished layers of organic matter, including soil microbes.