Filamentous fossils dated to 2.4 Ga were found in basalt samples from the Ongeluk Formation, which were suggested to be fossils of fungi-like organisms.[3][4]
^Gumsley, A.P., Chamberlain, K.R., Bleeker, W., Söderlund, U., de Kock, M.O., Larsson, E.R., Bekker, A., 2017, "Timing and tempo of the Great Oxidation Event", Proceedings of the National Academy of Sciences of the U.S.A., vol. 114, pp. 1811–1816.