Melanized pseudosclerotial plates, commonly referred to as zone lines,
form at colony boundaries of Phellinus weirii and other white-rot fun
gi in response to various stimuli. Pseudosclerotial plates of P. weiri
i produced in the laboratory can sequester metal ions from contact wit
h soil in concentrations up to fifteen times greater than found in the
soil. Phellinus weirii accumulated greater ion concentrations for 11
of 13 elements assayed than did Fomitopsis pinicola, a brown rot fungu
s that produces thick mycelial mats but does not produce melanized pse
udosclerotial plates. Ion concentrations for 10 of 13 elements were si
gnificantly greater in soil-treated pseudosclerotial plates of P. weir
ii than in controls. Aluminum and iron concentrations for soil-treated
pseudosclerotial plates of P. weirii were 152 and 117 times greater,
respectively, than that of controls. Ion concentration for untreated m
ats of P. weirii and F. pinicola were not significantly different in 1
2 of 13 elements assayed. The metal ion-rich outer layer of the pseudo
sclerotial plates of P. weirii may help in protecting the fungus from
combative antagonistic organisms and enhance long-term saprophytic sur
vival of this fungus.