“…All kinds of microbes, including prokaryotes and eukaryotes and their symbiotic associations with each other and higher organisms, can contribute actively to geological phenomena, and central to many such geomicrobial processes are transformations of metals and minerals. Indeed a diverse Proterozoic-Phanerozoic sedimentary stratigraphic rocks in Mongolia record and faunal, floral, and also bacterial localities (Mitrofanov et al, 1981;Bat-Ireedui, 1991, Bosak et al, 2011a, b;Barsbold and Byamba, 2012;Byamba, 2012;Dorjnamjaa, 2016;Dorjnamjaa et al, 2016;Dorjnamjaa, 2017;Anderson et al, 2017aAnderson et al, , b, 2018. In Mongolia the oldest microorganisms from the Paleoproterozoic were found in the iron-bearing quartzite.…”