Snow mold
Sclerotinia borealis
Sclerotinia borealis is a highly specialized fungal pathogen from the Sclerotiniaceae family, known as the primary cause of snow mold in various winter crops.
What the section contains
Snow mold
This psychrophilic organism belongs to the Ascomycota division and has evolved to thrive in cold, moist environments beneath the snow cover.
The fungus survives in the soil and on crop residues as small, black sclerotia, which act as persistent resting structures capable of surviving severe winters for several years.
Its mycelium is highly active at temperatures near 0°C, allowing it to colonize host tissues throughout the winter season when other pathogens remain dormant.
The pathogen is strictly adapted to northern climates, where consistent and deep snow cover provides a stable, protected microclimate for its vegetative expansion.
The main hosts of Sclerotinia borealis include winter wheat, winter rye, winter barley, and various perennial grasses used for forage.
The fungus causes severe damage to the crown area and leaf tissues, often leading to the complete death of the plant before the arrival of spring.
Severe infestations can result in significant stand reduction, requiring replanting of large areas and causing major economic losses for farmers.
Plants that survive infection typically exhibit delayed development and reduced photosynthetic capacity due to the destruction of the tiller base.
Indirect damage occurs as the infected areas become prone to colonization by opportunistic weeds, further reducing the overall productivity of the field.
The infection process starts in late autumn when soil temperatures drop below 5°C, providing the necessary thermal conditions for the pathogen's growth.
The peak activity of the fungus occurs during late winter and early spring, specifically during the period of snowmelt when moisture levels remain high.
Spread is primarily achieved through mycelial growth from infected tissues to healthy neighbors, often resulting in circular or irregular patches of dead plants.
Extended, cool springs with persistent high humidity are ideal for the pathogen, as rapid temperature fluctuations or drought are detrimental to its growth.
Once the soil surface warms up and dries out completely, the fungal mycelium loses its viability, and the pathogen enters its resting phase.
The most diagnostic sign is a fluffy, white to grayish mycelial mat covering the surface of leaves and crowns immediately after the snow melts.
Tissues affected by the fungus appear water-soaked, turn brownish, and rapidly decay into a soft, rotten mass under the influence of fungal enzymes.
Small, black, hard sclerotia are often visible on the decaying plant debris, providing confirmation of the presence of Sclerotinia borealis.
Infected plants are easily detached from the soil because the root system and the base of the tiller are usually consumed by the infection.
Fields exhibit localized, irregular patches of dead or dying plants that appear stunted and chlorotic compared to the healthy sections of the crop.
Crop rotation remains the most effective long-term management strategy, ideally involving non-host crops to starve the fungus in the soil.
Selecting resistant or cold-hardy cultivars is essential for areas with a high history of snow mold pressure and long winter periods.
Proper agronomic practices, such as deep plowing to bury plant debris and avoid excessive accumulation of biomass in autumn, can help reduce inoculum levels.
Balanced fertilization, particularly with potassium, improves the winter hardiness of the crop and its internal resistance to fungal colonization.
When environmental conditions favor high infection rates, prophylactic application of systemic fungicides in late autumn can effectively protect the plants throughout the winter.