Life on earth emerged in an anoxic environment. The earliest prokaryotes that inhabited our planet for hundreds of million years relied on H 2 , H 2 S, and CH 4 as potential electron donors and were perfectly adapted to live in the absence of what is today an essential element of the biosphere, i.e., O 2 . Oxygen began to accumulate in oceans and then in the atmosphere about 2.2 billion years ago, following the emergence of oxygenic photosynthetic microorganisms, which were able to split water and release molecular O 2 . This event is rightly considered a major step in the evolution of the biosphere, for a series of important reasons. (1) The introduction of O 2 in an anaerobic environment acted as a cataclysm on the preexisting biosphere, given the unprotected vulnerability of life forms to oxygen-derived reactive species. (2) The ensuing strong selection pressure precipitated the development of novel enzymes and new pathways, in order to cope with the bio-toxicity of O 2 derivatives [ 151 ]. (3) Evidence indicates that rising concentrations of O 2 also caused the reshuffl ing of integral biochemical pathways, with many enzymatic reactions that were central to anoxic metabolism being effectively replaced in aerobic organisms [ 148 ]. (4) The availability of molecular oxygen also made possible a highly exergonic respiratory chain based on O 2 as a terminal electron acceptor, an event that is considered as crucial for the evolution of eukaryotes and complex multicellular life species [ 46 , 48 ] and possibly for the colonization of terrestrial environments. Thus, both the quality and the quantity of existing biochemical networks were heavily impacted upon by the appearance of molecular oxygen [ 54 , 149 ]. Using model systems, it has been