Thermophilic anaerobic biodegradation of tetrachloroethene (PCE) was invest
igated with various inocula from geothermal and nongeothermal areas. Only p
olluted harbor sediment resulted in a stable enrichment culture that Conver
ted PCE via trichloroethene to cis-1,2-dichloroethene at the optimum temper
ature of 60 to 65 degrees C. after several transfers, methanogens were elim
inated from the culture. Dechlorination was supported by lactate, pyruvate,
fructose,fumarate; and malate as electron donor but not by H-2, formate, o
r acetate. Fumarate and L-malate led to the highest dechlorination rate. In
the absence of PCE, fumarate was fermented to acetate, H-2, CO2, and succi
nate. With PCE, less H-2 was formed, suggesting that PCE competed for the r
educing equivalents leading to H-2. PCE dechlorination, apparently, was not
outcompeted by fumarate as electron acceptor. At the optimum dissolved PCE
concentration of similar to 60 mu M, a high dechlorination rate of 1.1 mu
mol h(-1) mg(-1) (dry weight) was found, which indicates that the dechlorin
ation is not a cometabolic activity. Microscopic analysis of the fumarate-g
rown culture showed the dominance of a long thin rod. Molecular analysis, h
owever, indicated the presence of two dominant species, both belonging to t
he low-G+C gram positives. The highest similarity was found with the genus
Dehalobacter (90%), represented by the halorespiring organism Dehalobacter
restrictus, and with the genus Desulfotomaculum (86%).