R. Martens et F. Zadrazil, SCREENING OF WHITE-ROT FUNGI FOR THEIR ABILITY TO MINERALIZE POLYCYCLIC AROMATIC-HYDROCARBONS IN SOIL, Folia microbiologica, 43(1), 1998, pp. 97-103
Soil samples from an agricultural field contaminated with 10 ppm C-14-
benz(a)anthracene in glass tubes were brought into contact with cultur
es of wood-rotting fungi, precultivated on wheat straw substrate. Fort
y-five strains of white-rot fungi and four brown-rot fungi were tested
for their ability to colonize the soil and to mineralize C-14-benz(a)
anthracene to (CO2)-C-14 within a 20-week incubation time. Twenty-two
white-rot fungi and all brown-rot fungi were unable to colonize the so
il. Twenty-three strains of white-rot fungi, all belonging to the genu
s Pleurotus, colonized the soil. During the experiment the noncolonizi
ng fungi and their substrate disintegrated more and more to a nonstruc
tured pulp From which water diffused into the soil. The same phenomeno
n was observed in the control which contained only straw without fungu
s and contaminated soil. In samples with colonizing fungi the substrat
e as well as the mycelia in the soil remained visibly unchanged during
the entire experiment. Surprisingly, most samples with fungi not colo
nizing the soil and the control without fungus liberated between 40 an
d 58 % of the applied radioactivity as (CO2)-C-14 whereas the samples
with the colonizing fungi respired only 15-25 % as (CO2)-C-14. This wa
s 3-5 times more (CO2)-C-14 than that liberated from the control (4.9
%) which contained only contaminated soil without straw and fungus. A
similar result was obtained with selected colonizing and noncolonizing
fungi and soil contaminated with 10 ppm C-14-pyrene. However, in pure
culture studies in which C-14-pyrene was added to the straw substrate
, Pleurotus sp. (P2), as a representative of the colonizing fungi, min
eralized 40.3 % of the added radioactivity to (CO2)-C-14 The noncoloni
zing fungi Dichomitus squalens and Flammulina velutipes liberated only
17.2 or 1.7 %, respectively, as (CO2)-C-14 These results lead to the
hypothesis that the native soil microflora stimulated by the formed pr
oducts of straw lysis is responsible for high degradation rates found
with noncolonizing fungi.