The ratio of stable carbon isotopes is very sensitive to 1,1,1-TCA degradation.
Biotic FeS formation mediated abiotic degradation of 1,1,1-TCA.
CSIA enabled verification of abiotic degradation by a different pathway than RD.
Field data suggest that abiotic degradation of 1,1,1-TCA is a relevant process also at the field site.