“…The use of the A = 101 isobar in combination with other isotopic markers has been key for developing an understanding of geological transformations and geochemical behaviours of different isotopes and radioisotopes that were formed in the Oklo natural fission reactor in Gabon. For example, one study on the micro-metallic and ε-phase aggregates, including the fission-derived elements Ru, Rh, Pd, Te, Pb, As, S, and Bi, were collected and the isotopic ratios of different isotopic systems, i.e., 235 U/ 238 U, 90 Zr/ 91 Zr, 95 Mo/ 97 Mo, and 99 Ru/ 101 Ru, were analysed 128 . Whereas the 90 Zr/ 91 Zr and 95 Mo/ 97 Mo ratios in the metallic aggregates varied little in composition, likely due to constant separate mixing of fissiogenic and non-fissiogenic components, the 99 Ru/ 101 Ru ratios exhibited large variations, which could not be described by such processes.…”