We report the discovery of anomalies in the xenon isotopic composition of A
rchean cherts belonging to the metasedimentary sequences of Pilbara Craton,
Western Australia. The cherts show contemporary excesses of Xe and Xe131-1
36, compared to atmospheric Xe. The Xe-129 excesses are comparable to those
observed in mantle-derived samples, U-238 fissiogenic-produced such as MOR
Bs, xenoliths, diamonds and CO2-rich well gases and correlate with excesses
of Xe-136. close to the mantle ratio. However, isotope Xe-131 is in excess
of U-238 fissiogenic-Xe production. The Xe-129/Xe-131 ratio ranges from 0.
7 to 3.2 and it is consistent with production of these two isotopes by neut
ron-capture reactions with tellurium. These anomalies are analogous to thos
e measured in metamorphic rocks (gneisses and amphibolites) in the KTB bore
hole in Germany and probably were produced by reactions with Te. (C) 2001 E
lsevier Science B.V. All rights reserved.