The
phylogenetic relationships among superoxide dismutases (SODs) are one of many genetic components that have been used to help reconstruct an early timeline of events and predict the evolutionary descent of species, individuals, or genes from a common ancestor over time. Around the period of Earth's transition from
anaerobic to
aerobic conditions about 2.4 billion years ago (bya), the evolution of SOD enzymes crucially allowed organisms to overcome the effects of
oxidative stress following the surge of molecular oxygen (O2) in the atmosphere (Miller 2012). However, evidence suggests that the origination of
reactive oxygen species (ROS) took place as early as 4.1 to 3.5 bya (Inupakutika
et al. 2016). For the first aerobic organisms, survival depended largely on their ability to defend against ROS. For this reason, it is relevant to understand the environmental constraints that allowed such protective defense enzymes to evolve.
The Great Oxidation Event Atmospheric and oceanic compositions have drastically changed since the formation of early Earth. One significant event,
the Great Oxidation Event (GOE), marked the period of time in which oxygen became a major component of Earth's atmosphere and surface ocean. However, the physical or biochemical drivers responsible for the transition from a reducing to oxidizing environment remains up for debate (Olejarz
et al. 2021). To date, the evolution of
cyanobacteria and cyanobacterial photosynthesis is commonly accepted as the primary driver of oxygen production, alongside several physical events behaving as proximal drivers of environmental state change (Kasting 2013; Inupakutika
et al. 2016).
Selective Pressure and Enzyme Evolution The atmospheric accumulation of highly reactive O2 likely exercised a strong selective pressure against anaerobic organisms, and led to the adaptive evolution of oxygen utilization in metabolism (Boden
et al. 2021). The process of
oxidative phosphorylation and aerobic respiration permitted a 400-fold increase in energy extraction efficiency per mole glucose as compared to anaerobic respiration. Although the increased yield of
adenosine triphosphate (ATP), a common form of cellular energy currency, was metabolically beneficial, the tradeoff between efficiency and risk to the metabolic machinery grew more prominent. Behaving as the terminal
electron acceptor during
cellular respiration, the high rate of O2 electron flux is accompanied by an increased risk of ROS formation, which can induce irreversible damage to cellular organelles and their processes (Case 2017). In response to the accumulation of the hazardous metabolic byproducts of aerobic respiration, biological systems evolved various strategies to counteract
O2 toxicity. The Rise of Antioxidants During the transition from aerobic to anaerobic conditions, phylogenetic investigations suggest that SODs are ancient molecules, which were likely selected for before the GOE. While it is intuitively assumed that antioxidants emerged during the GOE to defend against O2 reactivity and toxicity caused by the accelerated oxygenation of the atmosphere,
sequencing and phylogenetic analyses of antioxidant systems from ancient organisms suggests that antioxidant enzymes including SODs may have originated long before the surge of atmospheric and oceanic O2 (Wolfe-Simon
et al. 2005; Inupakutika
et al. 2016).
Necessity of ROS-Defense Mechanisms The oxidizing capacity of O2 makes it a highly efficient final electron acceptor for several biological processes, producing more energy per mole substrate relative to other available electron acceptors during aerobic respiration (Boden
et al. 2021). On the other hand, its high reactivity also contributes to the uncontrolled removal of electrons, which underlies pathological cell damage through the propagation of highly reactive oxygen-containing molecules.
Superoxide (O2•−) is the most common reactive free-radical formed by the univalent reduction of O2. While they are known to exhibit beneficial roles in some cellular processes, superoxide free radicals also possess the ability to initiate a cascade of ROS and free-radical species formation in biological systems. As a consequence, the unrestrained and potentially lethal accumulation of ROS threatens to damage many biomolecules: lipids, proteins, DNA, and host cells. Additionally, oxidative stress in excess is understood to participate in the dysregulation of cellular processes and disease development (Zewen
et al. 2018). To maintain a balance of intracellular superoxide, organisms have developed strategies to protect against overexposure. One such mechanism functions to catalyze the dismutation of superoxide radicals into hydrogen peroxide and oxygen, which is accomplished by SOD enzymes.
Independent Evolution of SOD Families Studies examining the phylogenetic distribution of SODs support the proposal that the major
physiological function of SOD is to act as a protective mechanism among oxygen-metabolizing organisms against the formation of superoxide free radicals (McCord
et al. 1971). Although the enzyme is functionally limited to the conversion of superoxide radicals into less toxic oxygen-containing molecules, methodological approaches utilizing phylogenetic and structural protein analysis suggest that three SOD
isoforms have evolved independently to combat superoxide accumulation. Each enzyme family is characterized by a distinct 3D structure, amino acid sequence, and with regard to the metal-binding
cofactor(s) used to support its structural stability and
catalytic activity (Case 2017): either manganese (MnSOD), nickel (NiSOD), or both copper and zinc (Miller 2012). An additional family utilizing an iron cofactor (FeSOD) has also been identified, which is evolutionarily related to MnSOD (Wolfe-Simon
et al. 2005). The evolution of metalliform diversity can likely be explained by changes in heavy metal bioavailability that took place during large compositional changes of the earth's early atmosphere and oceans.
Fe/MnSODs SODs containing Fe (FeSOD), Mn (MnSOD), or may contain either (Fe/MnSOD) are believed to have been the earliest SOD isoforms among life on early earth. During this time, Fe and Mn would have been highly bioavailable. The differences between the
oxidation and reduction potentials of each metal is thought to have been advantageous to organism survival, allowing them to exist in environments with varying O2 concentration and metal availability.
CuZnSODs The most modern SOD family is believed to utilize both Cu and Zn ions (CuZnSOD). The absence of CuZnSODs from
archaeal and
protist genomes coupled with the post-GOE increased bioavailability of Cu and Zn suggests that the development of this isoform took place at a later period in evolutionary time (Banci
et al. 2005; Wilkinson
et al. 2006).
NiSODs The family of Ni-containing SODs (NiSOD) is less understood. Evidence suggests that these isoforms are largely distributed among
marine bacteria and
algae (Wolfe-Simon
et al. 2005; Dupont
et al. 2008). The evolution of NiSOD is currently predicted to have occurred around the time of the GOE when a decrease in aquatic bioavailability of Fe took place. == Stability and folding mechanism ==