“No… not exactly.” While many oaks have died and more can be expected to die, we are not witnessing any particularly menacing or threatening disease. The causes of oak mortality are variable and often complex. Investigations over several years, however, have revealed some common causes in Florida.

In certain cases, root disease fungi such as Armillaria, Ganoderma, andPhytophthora are involved, singularly or in combination. And in most cases, environmental influences play a major role.Armillaria and Ganoderma are naturally occurring, mushroom-forming fungi that colonize and decay tree stumps and roots. They frequently enter roots of living trees when roots are cut or damaged during construction or site disturbance activities, when trees are subjected to natural environmental stresses (severe droughts, floods, defoliation by insects, etc.), or when the roots of living trees come in contact with decaying stumps or roots. Phytophthora species are microscopic soilborne fungi that feed on and destroy the roots of many plants and trees, especially in poorly drained or waterlogged soils. Over time (often years), infected root systems are progressively debilitated by these and sometimes other root-infecting fungi. Eventually, infected root systems are debilitated to a point beyond which they are incapable of supplying adequate moisture and nutrients to their trees’ crowns, and tree death occurs.

Tree death may occur slowly over months or years with dying trees exhibiting progressive dieback and crown thinning, etc. Or tree death may occur “suddenly”, or at least appear to do so. This latter mode of demise is commonly observed in the summer months of July and August because hot summer air temperatures and fully foliated tree crowns increase trees’ transpirational water loss to the atmosphere, and debilitated root systems simply cannot supply the water “demanded” by actively transpiring crowns.

Root disease scenarios are often compounded in Florida by the state’s variable and unpredictable rainfall. Droughts clearly add to tree stress, especially if root systems are debilitated by root diseases. Additionally, however, excessive rainfall resulting in water impoundment and/or saturated soils is often the “straw that breaks the camel’s back”. Water-saturated soil conditions result in reduced soil oxygen levels and the buildup of carbon dioxide and an array of chemicals not found or scarce in well aerated soils. Such anaerobic conditions are directly toxic to tree roots and cause physiological damage to roots in direct proportion to the severity and duration of the conditions. When trees with pre-existing root diseases are subjected to anaerobic soil conditions the deleterious effects are additive, and tree death is often unavoidable and rapid.

Dead turkey oaks – brown dead foliage indicates “rapid” death – typical of turkey oaks killed by Armillariaand/or Phytophthora in rain saturated soils.

Another compounding and often poorly understood factor in the death of oaks in Florida is the presence of one or more species of Hypoxylon on dying trees.Hypoxylon species are opportunistic, secondary fungal pathogens that are common on a variety of hardwood species, especially on oaks. Research has demonstrated that certain species ofHypoxylon actually reside in the bark of healthy oaks. Only after severe physiological stress, when a tree’s water content drops below a certain threshold, do these fungi penetrate into the xylem (wood) of host trees; “finishing them off”, so to speak. Stresses sufficient to initiate lethal infections are typically related to drought, but may include mechanical injury, flooding, and even root diseases. For all intents and purposes, Hypoxylonspecies are indicators more than they are causes of death. Hypoxylon species are usually recognized as small to large, irregularly shaped sheets or patches of black or silver-gray crust-like fruiting structures appearing on infected stems or branches as the bark sloughs off the ailing tree(s). At certain stages of fungus development, Hypoxylon species often appear as irregular sheets of brownish powder (asexual spores) prior to the occurrence of the crust-like sexual fruiting structures.