H. Sandermann et al., A NEW INTERMEDIATE IN THE MINERALIZATION OF 3,4-DICHLOROANILINE BY THE WHITE-ROT FUNGUS PHANEROCHAETE-CHRYSOSPORIUM, Applied and environmental microbiology, 64(9), 1998, pp. 3305-3312
Phanerochaete chrysosporium ATCC 34541 has been reported to be unable
to mineralize 3,4-dichloroaniline (DCA), However, high mineralization
is now shown to occur when a fermentation temperature of 37 degrees an
d gassing with oxygen are used, Mineralization did not correlate with
lignin peroxidase activity. The latter was high under C limitation and
low under N limitation, whereas the reverse was true for mineralizati
on. The kinetics of DCA metabolism was studied in low N and low-C and
C- and N-rich culture media by metabolite analysis and (CO2)-C-14 dete
rmination. In all cases, DCA disappeared within 2 days, and a novel hi
ghly polar conjugate termed DCAX accumulated in the growth medium. Thi
s metabolite was a dead-end product under C and N enrichment, In oxyge
nated low-C medium and in much higher yield in oxygenated low-N medium
, DCAX was converted to DCA-succinimide and then mineralized. DCAX was
purified by high-performance liquid chromatography and identified as
3,4-dichlorophenyl)-alpha-ketoglutaryl-delta-amide by high-performance
liquid chromatography and mass spectroscopy, gas chromatography and m
ass spectroscopy, and nuclear magnetic resonance spectroscopy. The for
mation of conjugate intermediates is proposed to facilitate mineraliza
tion because the sensitive amino group of DCA needs protection so that
ring cleavage rather than oligomerization can occur.