Open access peer-reviewed chapter

Oxygen: From Toxic Waste to Optimal (Toxic) Fuel of Life

Written By

Mónica Rosas‐Lemus, Cristina Uribe‐Alvarez, Martha Contreras‐ Zentella, Luis Alberto Luévano‐Martínez, Natalia Chiquete‐Félix, Norma Lilia Morales‐García, Emilio Espinosa Simón, Adriana Muhlia‐ Almazán, Edgardo Escamilla‐Marván and Salvador Uribe‐Carvajal

Reviewed: April 13th, 2016 Published: October 26th, 2016

DOI: 10.5772/63667

Chapter metrics overview

1,822 Chapter Downloads

View Full Metrics


Some 2.5 billion years ago, the great oxygenation event (GOE) led to a 105‐fold rise in atmospheric oxygen [O2], killing most species on Earth. In spite of the tendency to produce toxic reactive oxygen species (ROS), the highly exergonic reduction of O2 made it the ideal biological electron acceptor. During aerobic metabolism, O2 is reduced to water liberating energy, which is coupled to adenosine triphosphate (ATP) synthesis. Today, all organisms either aerobic or not need to deal with O2 toxicity. O2‐permeant organisms need to seek adequate [O2], for example, aquatic crustaceans bury themselves in the sea bottom where O2 is scarce. Also, the intestinal lumen and cytoplasm of eukaryotes is a microaerobic environment where many facultative bacteria or intracellular symbionts hide from oxygen. Organisms such as plants, fish, reptiles and mammals developed O2‐impermeable epithelia, plus specialized external respiratory systems in combination with O2‐binding proteins such as hemoglobin or leg‐hemoglobin control [O2] in tissues. Inside the cell, ROS production is prevented by rapid O2 consumption during the oxidative phosphorylation (OxPhos) of ATP. When ATP is in excess, OxPhos becomes uncoupled in an effort to continue eliminating O2. Branched respiratory chains, unspecific pores and uncoupling proteins (UCPs) uncouple OxPhos. One last line of resistance against ROS is deactivation by enzymes such as super oxide dismutase and catalase. Aerobic organisms profit from the high energy released by the reduction of O2, while at the same time they need to avoid the toxicity of ROS.


  • oxygen
  • ROS
  • oxidative stress
  • oxyconformers
  • oxyregulators
  • adaptative metabolism

1. At the beginning, all life was anaerobic

The early Earth atmosphere contained high [H2], [NH3] and [CH4], while [O2] was less than 10-5 the present atmospheric level (PAL) [1, 2]. All life forms were anaerobic [3, 4]. Early redox reactions involved electron donors such as H2, CO2 or HS [5, 6], while electron acceptors were sulfur and NO3 [7]. Eukaryotes were present before O2 rose [8, 9] and contained anaerobic mitochondrion‐like organelles [10, 11].


2. The massive increase in [O2] and the need to counteract its toxicity

Approximately 2.5 billion years ago, the great oxygenation event (GOE) was precipitated by both geological processes [12] and by the photosynthetic activity of cyanobacteria [13, 14]. Today, O2 is the preferred electron acceptor used by facultative microorganisms and the only one used by aerobes. The highly exergonic reduction of O2 provided the energy needed for the development of multicellular organisms. In addition, the high energy of activation required for O2 reduction ensures that this reaction occurs mostly through catalyzed reactions. For instance, oxidases bind their substrate tightly, preventing the liberation of reactive oxygen species (ROS) [15]. At low concentrations, ROS are useful as signaling molecules, while at higher concentrations ROS damage and kill cells. Cells need much less [O2] than what is found in the atmosphere and thus, to prevent ROS production internal O2 is kept at a low level [16]. Cells have developed two mechanisms to deal with surplus O2: (1) avoiding it and (2) rapidly reducing it. Furthermore, cellular O2 is found mostly bound to proteins such as hemoglobin, leg‐hemoglobin and myoglobin. Early oxy‐conformer organisms are permanent to O2, and thus, at different stages in their life cycle, they have to migrate to microaerobic or anaerobic spaces (Table 1) to cope with variations in O2. More evolved oxyregulator organisms from fish to mammals enveloped themselves in an O2‐impermeable epithelium, while at the same time developing highly specialized systems that control tissue [O2] (Figure 1). Oxyconformers and oxyregulators display different strategies to manage O2‐by‐product toxicity (Figure 1).

In oxyconformers, all cells are exposed to environmental [O2]. O2‐permeable organisms do have O2 transport proteins and intracellular O2‐binding proteins, but in addition, they need to implement diverse strategies to deal with changing O2. These include searching for microaerophilic or anaerobic environments. Arthropoda, the most abundant and widely distributed phylum on Earth, are oxyconformers [17]; it comprises subphyla Chelicerata (spiders), Myriapoda (centi‐ and millipedes), Hexapoda (Insects) and Crustacea, all of them protected by an exoskeleton. Nonaquatic insects possess a hard waterproof cuticle and branched invaginated tubules forming a specialized respiratory structure that works well at constant [O2]. Aquatic organisms, including most of the crustacea, are exposed to highly variant [O2], which may be 26 times lower than in the atmosphere [18, 19]. In water, [O2] varies with temperature, depth, mechanical aeration and tidal movements. Only few invertebrates (Plathelmynthes, Nematoda, Molluska, Anellida and Sypuncula) have been thoroughly studied in regard to their mechanisms to deal with fluctuating [O2] [20, 21]. Remarkably, very few studies on Crustacea are available.

Environment O2 concentration (μM) References
Atmosphere 1000m ASL 256.0
Sea level 1028.0
Alveoles 143.0 [89]
Arteries 123.0
Hb bound 120.5
Not bound 2.5
Capillaries 130.0 [89]
Interstitial fluid 55.0 [89]
Tissue cells 31.0 [89]
Veins 59.0 [89]
Mitochondria Minimal for coupling 0.1
Minimal reported 20.0
Distilled water 223.0 [92]
Sea water Surface 198‐397.0
MOZ < 20.0
Estuaries Surface 375.0
Bottom 62.5

Table 1.

Oxygen concentrations in different environments.

Oxygen concentrations reported were modified from partial pressures to micromolar concentration (μM) using Henry's law at 310.15K ASL (above sea level).

In order to control the release of ROS oxyconformers reduce aerobic activity during hypoxia/ anoxia cycles, marine crustaceans display different responses to hypoxia/anoxia. To avoid hyperoxygenated or anoxic waters, crustaceans migrate between open sea and coastal lagoons (Figure 2), or migrate vertically through the water column to flee the O2‐minimum zone (OMZ) and into [O2] compatible with their metabolic needs [22, 23]. Some shrimp species, such as the burrowing thalassinids Upogebia major and Callianasa japonica, which commonly inhabit the extremely hypoxic or even anoxic intertidal flats, can reduce their respiratory rate in dugout burrows, surviving up to 5 h of anoxia for U. major and 19 h for C. japonica [24]. Artemia franciscana is well known for its high tolerance to anoxia; the embryos of this species survive without O2 for years through the complete depression of their metabolic rates [25, 26]. Metabolic rate depression is also observed in ectotherms, which lower their mitochondrial activity in function of temperature adjusting their O2 consumption machinery accordingly [27]. However, it is not clear how mitochondria from oxyconformers respond to hypoxia, how respiratory activity adapts to reduced metabolic rates and how the cellular redox balance and energetic homeostasis are preserved [28, 29].

Figure 1.

Oxygen management strategies in different organisms. Organisms need to adapt to the O2 concentration in the environment. Therefore, either they move to environments with adequate O2 or they engineer different mechanisms to process O2 at varying rates (electron transport chain (ETC) activity, mitochondrial unspecific channels (MUC), uncoupling proteins (UCPs). Additionally, oxyregulators have developed O2‐excluding mechanisms such as impermeable epithelia, external respiratory systems (lungs, gills, stomas) and O2‐transporting proteins (hemoglobin, myoglobin).

Figure 2.

Migration of shrimp during their life cycle. Shrimp spend most of their life in the open sea, where they mate and lay eggs which hatch and undergo different larval stages (Nauplius, Protozoa, Mysis). Once in the postlarval stage, they travel to estuaries where they mature reaching the juvenile stage, and burying themselves in the sand for long periods. Once maturity is reached, they begin the cycle again returning to the open sea. This migration pattern takes shrimp to waters with widely different O2 concentrations.

Among unicellular organisms, diverse yeast species can survive at almost any [O2]. Saccharomyces cerevisiae can thrive at very low [O2] through fermentation, although it does possess a facultative aerobic metabolism. The anaerobic metabolism of S. cerevisiae, D. hansenii and other yeast species is the basis for the fermentation industry of bread, wine and cheese. For example, during wine fermentation, S. cerevisiae produces large amounts of ethanol, while D. hansenii produces volatile products conferring the characteristic aroma of wine [30]. Also, S. cerevisiae participates in cheese fermentation, whereas D. hansenii protects against other filamentous fungi during ripening [31, 32]. Yeast and other organisms have developed diverse systems to detoxify oxygen through physiological uncoupling and these are discussed later.

Figure 3.

Diversity of bacterial respiratory chains at different [O2]. A. The respiratory chain from Escherichia coli during aerobiosis, micro‐aerobiosis and anaerobiosis. Modified from [35, 36]. Ubiquinone is expressed at high [O2] and NADH DH type II is overexpressed as compared to the NADH DH type I, which in turn is expressed at low [O2]. The major final oxidase is cytochrome bo. During anaerobiosis, the respiratory chain in Escherichia coli succinate dehydrogenase is not expressed, whereas fumarate reductase or nitrate reductase may be the final electron acceptors. B. Hypothetical respiratory chain of Wolbachia pipientis constructed from BLAST and genome sequences reported in [76, 77]. At high [O2] cytochrome, bc1 and different cytochrome oxidases are expressed. Under microaerobic conditions, cytochrome bd is expressed. Then, under anaerobiosis, nitrate reductase is expressed.

Many bacteria are facultative. Among these, Escherichia coli is a very illustrative representative that may thrive both in microaerobic environments such as the intestinal lumen and in the external environment in a wide range of [O2]. Bacteria respond to environmental [O2] variations or other conditions such as the need to fixate N2 [33, 34] by varying the composition of their branched respiratory chains (Figure 3A), which vectorially transport from 0 to 10 protons, as many as those in orthodox respiratory chains [35, 36]. Still, when motile, bacteria will swim toward environments containing the ideal [O2].

Obligate endosymbionts, such as R. prowazekii, Wolbachia sp. or Sodalis, live in cytoplasmic vacuoles of multicellular organisms. The cytoplasm is a microaerophilic environment equipped with O2‐consuming organelles and ROS‐detoxifying enzymes. Remarkably, most endosymbionts contain a respiratory chain that at least in the case of Wolbachia seems to aid host mitochondria to deplete intracellular O2 (Figure 3B).

Many parasites exhibit various life‐cycle stages, which have different sensitivities to ROS engineered to endure attacks from macrophages. Leishmania sp. undergoes a relatively simple life cycle with two stages: the flagellated mobile promastigote living in the gut of the sand fly vector and the intracellular amastigote within phagolysosomal vesicles of the vertebrate host macrophage [37]. Promastigotes contain respiratory complexes I, II, III and IV, while it is not clear whether amastigotes possess an oxidative phosphorylation (OxPhos) machinery. Strikingly, amastigotes exhibit a succinate‐dependent, uncoupler‐sensitive transmembrane potential. Differences in sensitivity to oxidants are also observed between them, in vitro, promastigotes are more resistant to H2O2 than amastigotes [38].

In the bloodstream, Trypanosoma cruzi trypomastigotes contain high complex II and III activities. Interestingly, cytochrome c oxidase (COX) activity decreases creating an “electron bottleneck” that favors an increase in electron leakage, thus overproducing ROS. The oxidative preconditioning provided by this mechanism confers protection to bloodstream trypomastigotes against ROS liberated by the host immune system. These changes in mitochondrial activity, during the T. cruzi life cycle, are probably a key metabolic adaptation for survival in different hosts [39].

Malarial parasites are vulnerable to oxidative stress during their intraerythrocyte life stages. They contain the canonical respiratory chain (complex I, II, III and IV) plus an alternative electron transport pathway. Moreover, malarial mitochondria coordinate the biosynthesis of pyrimidine, heme and coenzyme Q [40]. Plasmodium falciparum possesses genes for two different superoxide dismutases (SOD), a cytosolic, Fe2+‐dependent, (SOD‐1) expressed throughout the intraerythrocytic life of the parasite. The second, SOD‐2, is mitochondrial and possesses a reminiscent apicoplast‐targeting sequence. The host immune response to malaria involves phagocytosis and the production of nitric oxide and ROS that end up contributing to the pathology of the disease [41].

Regardless the organism studied, cytoplasmic [O2] can vary widely, so damage control is needed at two levels. Either O2 is reduced independently of adenosine triphosphate (ATP) production in a process known as physiological uncoupling, or the ROS‐handling enzymes are activated. We shall briefly describe only physiological uncoupling as many reviews on ROS‐handling enzymes, such as superoxide dismutase and catalase are found elsewhere [42, 43].


3. Physiological uncoupling as an O2‐depleting mechanism and prevents ROS production

Both in oxyconformers and in oxyregulators, once O2 enters the cell it has to be reduced at a high rate. When ATP is needed the respiratory chain rapidly catalyzes this reduction. When there is energy surplus, O2 consumption has to be uncoupled from ATP synthesis with the aim of preventing ROS overproduction [44]. A review on the physiological uncoupling mechanisms observed in mitochondria from different species of yeasts has been published recently [45]. Yeast mitochondrial uncoupling mechanisms may be (a) proton sinks, such as the mitochondrial unspecific channels [4648] and the uncoupling protein (UCP) [49, 50], or (b) nonpumping redox alternative enzymes found in branched respiratory chains [5155].

(a). Proton sinks: The opening of the mitochondrial permeability transition pore (MPTP) leads to mitochondrial uncoupling and to the activation of signaling events leading to apoptosis [56], which was first detected in mammalian mitochondria as a response to the disruption of intracellular calcium homeostasis. In crustaceans subjected to hypoxia, mitochondrial functions are downregulated [57, 58, 20] and there is an anoxia‐triggered intracellular increase in both calcium and phosphate, while ATP production is inhibited, probably as a result of the opening of a MPTP. In Artemia franciscana [26] and in the ghost shrimp Lepidophthalmus louisianensis [59], the proteins needed to form the MPTP are present. However, whether these crustaceans possess MPTPs is to be defined. Both in crustacean mitochondria and in other known hypoxia‐tolerant invertebrates (mussels, oysters, and cnidarians among others), the role of a putative MPTP is an interesting question.

(b). Branched respiratory chains: Bacteria do not exhibit a permeability transition. This seems to be a mitochondrial trait. Instead, bacteria (and many mitochondria) exhibit branched respiratory chains. Indeed, different species of mitochondria may exhibit from none to three alternative enzymes. In contrast, bacteria may contain as much as twenty electron entry ports and as many exits. Thus, in most prokaryotes, branched respiratory chains seem to be the mechanism of choice to maintain a high rate of O2 consumption, while adjusting ATP production to the energy requirements of the cell. In this regard, the bioenergetic efficiency for each entry point is defined as the stoichiometry of H+ pumped per e traveling through the respiratory chain [60]. In addition, terminal oxidases are remarkably varied and their active site orientation, to the cytoplasm or to the periplasm determines their pumping efficiency [36].

Alternative oxidoreductases is the term designating all components of the respiratory chain different to the usual complexes I through IV. Most alternative oxidoreductases lack proton‐pumping activity and may coexist with, or substitute for the respiratory proton‐pumping complexes. Alternative enzymes catalyze the rapid, uncoupled flow of electrons towards O2. Alternative NADH dehydrogenases may either substitute for (S. cerevisiae) or coexist with (bacteria, plants and diverse fungi) complex I [61, 62].

Alternative oxidases (AOXs) catalyze the oxidation of ubiquinol to quinone and the reduction of O2 to H2O in the absence of proton translocation [53]. Although highly represented among plants, fungi and protist species, animal AOXs have been predicted to exist only in Molluska, Nematoda and Chordata [63]. Recently, the number of phyla that probably possess AOX has increased including Placozoa, Porifera, Cnidaria, Annelida, Echinodermata, Hemichordata and Chordata. In some marine vertebrates, such as sipunculids, annelids (Nereis pelagica, and Arenicola marina) and in bivalves (Arctica islandica), AOX has been detected [6466]. However, there are no confirmed reports for AOX in mitochondria from crustaceans [51]. In different plant and animal species, cells lacking AOX show an increased susceptibility to death due to H2O2, hypoxia and pathogens [67]. The ultimate decoupling of electron flow occurs when NADH dehydrogenases act in concert with alternative oxidases. The yeast Yarrowia lipolytica is a strict aerobic organism for which several biotechnological applications have been developed, such as in the cheese fermentation, obtention of extracellular enzymes [68], production of organic acids [69] and interconversion of fatty acids and alkenes [70]. In Y. lipolytica, metabolism occurs in a complex network between compartments, such as peroxisomes, endoplasmic reticulum, lipid bodies and mitochondria [69]. Mitochondria play an important role in ATP production, as well as in the maintenance of the NADH/NAD+ redox ratio [71]. The respiratory chain is composed of the classic complexes: I, II, III and IV, one alternative NADH dehydrogenase external (NADH2) [72] and two isoforms of AOX [73]. During the logarithmic growth phase, NADH2 interacts with supercomplexes III–IV channeling the electrons to oxygen, while pumping protons at both complex III and IV [74]. In contrast, during the stationary growth phase, electrons are directly transferred from alternative NDH2 to AOX, thus uncoupling oxidative phosphorylation and decreasing the production of ROS [54, 55]. This is a very illustrative example, which suggests that physiological uncoupling systems are present in all living organisms. Furthermore, in Y. lipolytica, both proton sinks and branched chains are observed [50, 54].

Bacterial cytochrome‐containing oxidases are many. These enzymes are differentially expressed in response to different oxygen concentrations and on whether an organism is an obligate aerobic or a facultative species. In addition, oxidases may coexist depending on the species under study and they may play different roles in the cell [75]. In E. coli, different oxidases are expressed depending on [O2]. At high O2, bo3 is expressed, while at low O2, bd cytochromes are observed. Furthermore, E. coli is capable of growth under anaerobiosis, using respiratory chains reminiscent of the early Earth that use ubiquinone, menaquinone or demethylmenaquinone to donate electrons to enzymes that use terminal acceptors different to O2 (Figure 3A) [35, 36]. Branched respiratory chains provide the possibility of consuming O2 without producing ATP. In the yeast Y. lipolytica, in the bacterium E. coli and probably in the Rickettsial Wolbachia sp., the arrangement of the respiratory chain varies such that when [O2] is high, or ATP is needed, high proton pumping efficiency is observed. In contrast, factors such as arrival to the stationary phase or microaerophilic conditions probably trigger overexpression of the alternative NADH dehydrogenase and/or the AOX leading to the futile reduction of O2 [61]. A possible arrangement of the respiratory chain of Wolbachia sp is illustrated (Figure 3B) where a large number of possible electron‐donating enzymes reduce menaquinone or ubiquinone that in turn reduce final electron‐accepting enzymes that are expressed according to the presence of O2 in the cytoplasm of the host [76, 77].


4. N‐fixating bacteria are a special case

Nitrogen‐fixating bacteria may be facultative as Klebsiella pneumonia or strict aerobics as Azotobacter vinelandii or Gluconobacter diazotrophicus. As they contain fragile, oxygen‐sensitive nitrogen‐fixating enzymes that need to be protected, these bacteria have developed many strategies to detoxify [O2]. Thus, in N‐fixating bacteria, both N‐reductases and different oxidases are expressed: A. vinelandii contains a highly active respiratory chain and is able to adjust the expression of its three oxidases to a wide range of [O2]. Among these, cytochrome bd has high O2 affinity (KmO2= 5 μM) and becomes active during N fixation [15, 7880]. Indeed, during N fixation the H+/O index is low, at 1 [81]. In Ga. diazotrophicus different periplasmic membrane enzymes such as glucose‐, acetaldehyde‐ or ethanol-dehydrogenase reduce a quinone, which in turn donates its electrons to two different oxidases, ba which is coupled to ATP synthesis and bb3 which is not coupled, but its role is to deplete O2 in the vicinity of nitrogen reductases [82].


5. ROS detoxification

In spite of the production‐prevention mechanisms outlined earlier, ROS may reach high concentrations, for example, during ischemia‐reperfusion. The last line of defense is detoxification. Enzymes such as superoxide dismutases (SODs) and catalases deactivate ROS. SODs have been grouped on the basis of the metal cofactor, which can be Fe, Mn, Ni or Cu/Zn [83]. The Fe‐SODs are mostly found in microaerophiles and anaerobes. Microorganisms in aerobic environments prefer Mn‐SOD [84]. Catalase dismutates hydrogen peroxide to water plus O2 [85]. Several genes capable of H2O2 dismutation evolved from ancestral genomes. The most abundant was heme‐containing enzymes spread among bacteria, Archaea and Eukarya [86].

In Clostridium acetobutylicum, a strict anaerobic that survives little time when exposed to O2, no catalases are found [87], and a function has yet to be found for the annotated SODs.


6. Conclusion

During the early paleoproterozoic period, a massive death toll resulted from a 105 times rise in atmospheric O2. In order to survive, organisms had to learn to cope with O2 toxicity while profiting from the large energy release coupled to its reduction. Several O2‐management strategies are revised here. Among these is hiding away from O2, moving to adequate O2 concentrations or excluding O2 with impermeable epithelia. Once O2 enters the cell, other mechanisms are designed to handle it. Its reactivity is controlled by O2‐quenching proteins or by rapidly reducing it with specific oxidases. In order to avoid side reactions, the rate of reduction had to be kept at optimal pace, independently of ATP production and thus several mechanisms of physiological uncoupling of oxidative phosphorylation evolved. Physiological uncoupling was achieved either by opening proton sinks or by using O2 independently of the proton gradient. Today, these mechanisms are expressed in many cells. Proton sinks include unspecific channels and uncoupling proteins, while proton gradient‐independent consumption of O2 involved alternative oxido‐reductases found in the branched respiratory chains of fungi, plants and arthropods. In spite of the function of all these O2‐management machines, O2 can still react unspecifically to form ROS, which destroy the cell through processes such as aging, apoptosis or necrosis. Once formed, ROS may still be eliminated by enzymes such as SOD and catalase, which are reviewed elsewhere [43] O2 is a great source of energy for the cell, but its high toxicity has to be dealt with, through mechanisms that we are only beginning to understand.



Authors thank Ramón Méndez‐Franco for technical assistance. Partially funded by the PAPIIT program and DGAPA/UNAM (grant IN202612). MRL, NLMG and CUA are CONACYT fellows enrolled in the Biochemistry Graduate Program at UNAM.

Declaration of Interest. The authors do not have any interests to disclose.


  1. 1. Lane N. Oxygen the molecule that made the world. Oxford: Oxford University Press; 2002. p. 384.
  2. 2. Sessions AL, Doughty DM, Welander PV, Summons RE, Newman DK. The continuing puzzle of the great oxidation event. Current Biology. 2009;19(14):R567–74.
  3. 3. Pavlov AA, Kasting JF. Mass‐independent fractionation of sulfur isotopes in Archean sediments: strong evidence for an anoxic Archean atmosphere. Astrobiology. 2002;2(1):27–41.
  4. 4. Martin W, Rotte C, Hoffmeister M, Theissen U, Gelius‐Dietrich G, Ahr S, et al. Early cell evolution, eukaryotes, anoxia, sulfide, oxygen, fungi first (?), and a tree of genomes revisited. IUBMB Life. 2003;55(4–5):193–204.
  5. 5. Nisbet EG, Sleep NH. The habitat and nature of early life. Nature. 2001;409(6823):1083–91.
  6. 6. Martin W, Muller M. The hydrogen hypothesis for the first eukaryote. Nature. 1998;392(6671):37–41.
  7. 7. Castresana J, Saraste M. Evolution of energetic metabolism: the respiration‐early hypothesis. Trends in Biochemical Sciences. 1995;20(11):443–8.
  8. 8. Gray MW. Evolution of organellar genomes. Current Opinion in Genetics & Development. 1999;9(6):678–87.
  9. 9. Kurland CG, Andersson SG. Origin and evolution of the mitochondrial proteome. Microbiology and Molecular Biology Reviews. 2000;64(4):786–820.
  10. 10. Hellemond JJv, Klei Avd, Weelden SHv, Tielens AGM. Biochemical and evolutionary aspects of anaerobically functioning mitochondria. Philosophical Transactions of the Royal Society of London Series B: Biological Sciences. 2003;358(1429):205–15.
  11. 11. Mentel M, Martin W. Energy metabolism among eukaryotic anaerobes in light of Proterozoic ocean chemistry. Philosophical Transactions of the Royal Society of London Series B, Biological Sciences. 2008;363(1504):2717–29.
  12. 12. Hayes JM, Waldbauer JR. The carbon cycle and associated redox processes through time. Philosophical Transactions of the Royal Society B: Biological Sciences. 2006;361(1470):931–50.
  13. 13. Holland HD. The oxygenation of the atmosphere and oceans. Philosophical Transactions of the Royal Society of London Series B, Biological Sciences. 2006;361(1470):903–15.
  14. 14. Golblatt C, Lenton TM, Watson AJ. Bistability of atmospheric oxygen and the Great Oxidation. Nature. 2006;443(7112):683–6.
  15. 15. Poole RK, D’Mello R, Hill S, Ioannidis N, Leung D, Wu G. The oxygen reactivity of bacterial respiratory haemoproteins: oxidases and globins. Biochimica et Biophysica Acta. 1994;1187(2):226–31.
  16. 16. Hinton HE. Respiratory systems of insect egg shells. Annual review of entomology. 1969;14:343–68.
  17. 17. Hochachka PW, Somero GN. Biochemical adaptation: mechanism and process in physiological evolution. United States Of America: Oxford University Press; 2002. 467 p.
  18. 18. Hill RW, Wyse GA, Anderson M. Animal physiology. MA, USA: Sinauer Associates Inc. Publishers; 3rd Ed., 2012, P.799.
  19. 19. Abele D. Toxic oxygen: the radical life‐giver. Nature. 2002;420(6911):27.
  20. 20. Martinez‐Cruz O, Calderon de la Barca AM, Uribe‐Carvajal S, Muhlia‐Almazan A. The function of mitochondrial F(O)F(1) ATP‐synthase from the whiteleg shrimp Litopenaeus vannamei muscle during hypoxia. Comparative Biochemistry and Physiology Part B, Biochemistry & Molecular Biology. 162(4):107–12.
  21. 21. Müller M, Mentel M, van Hellemond JJ, Henze K, Woehle C, Gould SB, et al. Biochemistry and evolution of anaerobic energy metabolism in eukaryotes. Microbiology and Molecular Biology Reviews. 2012;76(2):444–95.
  22. 22. Dall W, Hill BJ, Rothlisberg PC, Sharples DJ. The biology of the Penaeidae. Advances in Marine Biology; 1990. pp 489, 27. CSIRO Marine Laboratories, P.O. Box 120, Cleveland, Qld. 4163, Australia 1990.
  23. 23. Ekau W, Auel H, Pörtner HO, Gilbert D. Impacts of hypoxia on the structure and processes in pelagic communities (zooplankton, macro‐invertebrates and fish). Biogeosciences. 2010;7(5):1669–99.
  24. 24. Mukai H, Koike I. Behavior and respiration of the Burrowing Shrimps Upogebia major (de Haan) and Callianassa japonica (de Haan). Journal of Crustacean Biology. 1984;4(2):191–200.
  25. 25. Clegg J. Embryos of Artemia franciscana survive four years of continuous anoxia: the case for complete metabolic rate depression. Journal of Experimental Biology. 1997;200(3):467–75.
  26. 26. Menze MA, Hutchinson K, Laborde SM, Hand SC. Mitochondrial permeability transition in the crustacean Artemia franciscana: absence of a calcium‐regulated pore in the face of profound calcium storage. American Journal of Physiology – Regulatory, Integrative and Comparative Physiology. 2005;289(1):R68–76.
  27. 27. Galli GJ, Richards J. Mitochondria from anoxia‐tolerant animals reveal common strategies to survive without oxygen. Journal of Comparative Physiology B. 2014;184(3):285–302.
  28. 28. Strahl J, Dringen R, Schmidt MM, Hardenberg S, Abele D. Metabolic and physiological responses in tissues of the long‐lived bivalve Arctica islandica to oxygen deficiency. Comparative Biochemistry and Physiology Part A, Molecular & Integrative Physiology. 2011;158(4):513–9.
  29. 29. Buttemer WA, Abele D, Costantini D. From bivalves to birds: oxidative stress and longevity. Functional Ecology. 2010;24(5):971–83.
  30. 30. Rosi I, Vinella M, Domizio P. Characterization of beta‐glucosidase activity in yeasts of oenological origin. The Journal of Applied Bacteriology. 1994;77(5):519–27.
  31. 31. Roostita R, Fleet GH. Growth of yeasts in milk and associated changes to milk composition. International Journal of Food Microbiology. 1996;31(1–3):205–19.
  32. 32. Eliskases‐Lechner F, Ginzinger W, Rohm H, Tschager E. Raw milk flora affects composition and quality of Bergkäse. 1. Microbiology and fermentation compounds. Lait. 1999;79(4):385–96.
  33. 33. Baracchini O, Sherris JC. The chemotactic effect of oxygen on bacteria. The Journal of Pathology and Bacteriology. 1959;77(2):565–74.
  34. 34. Ulloa O, Canfield DE, DeLong EF, Letelier RM, Stewart FJ. Microbial oceanography of anoxic oxygen minimum zones. Proceedings of the National Academy of Sciences of the United States of America. 2012;109(40):15996–6003.
  35. 35. Ingledew WJ, Poole RK. The respiratory chains of Escherichia coli. Microbiological Reviews. 1984;48(3):222–71.
  36. 36. Unden G, Bongaerts J. Alternative respiratory pathways of Escherichia coli: energetics and transcriptional regulation in response to electron acceptors. Biochimica et Biophysica Acta. 1997;1320(3):217–34.
  37. 37. Chakraborty B, Biswas S, Mondal S, Bera T. Stage specific developmental changes in the mitochondrial and surface membrane associated redox systems of Leishmania donovani promastigote and amastigote. Biochemistry Biokhimiia. 2010;75(4):494–518.
  38. 38. Van Assche T, Deschacht M, da Luz RA, Maes L, Cos P. Leishmania‐macrophage interactions: insights into the redox biology. Free Radical Biology & Medicine. 2011;51(2):337–51.
  39. 39. Gonçalves RL, Barreto RF, Polycarpo CR, Gadelha FR, Castro SL, Oliveira MF. A comparative assessment of mitochondrial function in epimastigotes and bloodstream trypomastigotes of Trypanosoma cruzi. Journal of Bioenergetics and Biomembranes. 2011;43(6):651–61.
  40. 40. Krungkrai J. The multiple roles of the mitochondrion of the malarial parasite. Parasitology. 2004;129(Pt 5):511–24.
  41. 41. Muller S. Redox and antioxidant systems of the malaria parasite Plasmodium falciparum. Molecular Microbiology. 2004;53(5):1291–305.
  42. 42. McCord JM, Keele BB, Jr., Fridovich I. An enzyme‐based theory of obligate anaerobiosis: the physiological function of superoxide dismutase. Proceedings of the National Academy of Sciences of the United States of America. 1971;68(5):1024–7.
  43. 43. D’Autreaux B, Toledano MB. ROS as signalling molecules: mechanisms that generate specificity in ROS homeostasis. Nature Reviews Molecular Cell Biology. 2007;8(10):813–24.
  44. 44. Kadenbach B. Intrinsic and extrinsic uncoupling of oxidative phosphorylation. Biochimica et Biophysica Acta. 2003;1604(2):77–94.
  45. 45. Guerrero‐Castillo S, Araiza‐Olivera D, Cabrera‐Orefice A, Espinasa‐Jaramillo J, Gutierrez‐Aguilar M, Luevano‐Martinez LA, et al. Physiological uncoupling of mitochondrial oxidative phosphorylation. Studies in different yeast species. Journal of Bioenergetics and Biomembranes. 2011;43(3):323–31.
  46. 46. Manon S, Roucou X, Guerin M, Rigoulet M, Guerin B. Characterization of the yeast mitochondria unselective channel: a counterpart to the mammalian permeability transition pore? Journal of Bioenergetics Biomembranes. 1998;30(5):419–29.
  47. 47. Bernardi P. The mitochondrial permeability transition pore: a mystery solved? Frontiers in Physiology. 2013;4:95.
  48. 48. Uribe‐Carvajal S, Luevano‐Martinez LA, Guerrero‐Castillo S, Cabrera‐Orefice A, Corona‐de‐la‐Pena NA, Gutierrez‐Aguilar M. Mitochondrial unselective channels throughout the eukaryotic domain. Mitochondrion. 2011;11(3):382–90.
  49. 49. Nicholls DG, Rial E. A history of the first uncoupling protein, UCP1. Journal of Bioenergetics and Biomembranes. 1999;31(5):399–406.
  50. 50. Luevano‐Martinez LA, Moyano E, de Lacoba MG, Rial E, Uribe‐Carvajal S. Identification of the mitochondrial carrier that provides Yarrowia lipolytica with a fatty acid‐induced and nucleotide‐sensitive uncoupling protein‐like activity. Biochimica et Biophysica Acta. 2010;1797(1):81–8.
  51. 51. McDonald AE, Vanlerberghe GC, Staples JF. Alternative oxidase in animals: unique characteristics and taxonomic distribution. Journal of Experimental Biology. 2009;212(Pt 16):2627–34.
  52. 52. McDonald AE, Vanlerberghe GC. Alternative oxidase and plastoquinol terminal oxidase in marine prokaryotes of the Sargasso Sea. Gene. 2005;349:15–24.
  53. 53. Vanlerberghe GC, McIntosh L. Alternative oxydase: from gene to function. Annual Review of Plant Physiology and Plant Molecular Biology. 1997;48:703–34.
  54. 54. Guerrero‐Castillo S, Cabrera‐Orefice A, Vazquez‐Acevedo M, Gonzalez‐Halphen D, Uribe‐Carvajal S. During the stationary growth phase, Yarrowia lipolytica prevents the overproduction of reactive oxygen species by activating an uncoupled mitochondrial respiratory pathway. Biochimica et Biophysica Acta. 2012;1817(2):353–62.
  55. 55. Cabrera‐Orefice A, Chiquete‐Felix N, Espinasa‐Jaramillo J, Rosas‐Lemus M, Guerrero‐Castillo S, Pena A, et al. The branched mitochondrial respiratory chain from Debaryomyces hansenii: components and supramolecular organization. Biochimica et Biophysica Acta. 2013;1837(1):73–84.
  56. 56. Bernardi P. Mitochondrial transport of cations: channels, exchangers, and permeability transition. Physiological Reviews. 1999;79(4):1127–55.
  57. 57. Kwast KE, Hand SC. Acute depression of mitochondrial protein synthesis during anoxia: contributions of oxygen sensing, matrix acidification, and redox state. The Journal of Biological Chemistry. 1996;271(13):7313–9.
  58. 58. Eads BD, Hand SC. Mitochondrial mRNA stability and polyadenylation during anoxia‐induced quiescence in the brine shrimp Artemia franciscana. The Journal of Experimental Biology. 2003;206(Pt 20):3681–92.
  59. 59. Holman JD, Hand SC. Metabolic depression is delayed and mitochondrial impairment averted during prolonged anoxia in the ghost shrimp, Lepidophthalmus louisianensis (Schmitt, 1935). Journal of Experimental Marine Biology and Ecology. 2009;376(2):85–93.
  60. 60. Borisov VB, Murali R, Verkhovskaya ML, Bloch DA, Han H, Gennis RB, et al. Aerobic respiratory chain of Escherichia coli is not allowed to work in fully uncoupled mode. Proceedings of the National Academy of Sciences. 2011;108(42):17320–4.
  61. 61. Kerscher SJ. Diversity and origin of alternative NADH:ubiquinone oxidoreductases. Biochimica et Biophysica Acta (BBA) ‐ Bioenergetics. 2000;1459(2–3):274–83.
  62. 62. Büschges R, Bahrenberg G, Zimmermann M, Wolf K. Nadh: Ubiquinone oxidoreductase in obligate aerobic yeasts. Yeast. 1994;10(4):475–9.
  63. 63. McDonald A, Vanlerberghe G. Branched mitochondrial electron transport in the Animalia: presence of alternative oxidase in several animal phyla. IUBMB Life. 2004;56(6):333–41.
  64. 64. Tschischka K, Abele D, Portner HO. Mitochondrial oxyconformity and cold adaptation in the polychaete Nereis pelagica and the bivalve Arctica islandica from the Baltic and White Seas. The Journal of Experimental Biology. 2000;203(Pt 21):3355–68.
  65. 65. Buchner T, Abele D, Portner HO. Oxyconformity in the intertidal worm Sipunculus nudus: the mitochondrial background and energetic consequences. Comparative Biochemistry and Physiology Part B, Biochemistry & Molecular Biology. 2001;129(1):109–20.
  66. 66. Hildebrandt TM, Grieshaber MK. Three enzymatic activities catalyze the oxidation of sulfide to thiosulfate in mammalian and invertebrate mitochondria. FEBS Journal. 2008;275(13):3352–61.
  67. 67. Vanlerberghe GC, Robson CA, Yip JY. Induction of mitochondrial alternative oxidase in response to a cell signal pathway down‐regulating the cytochrome pathway prevents programmed cell death. Plant Physiology. 2002;129(4):1829–42.
  68. 68. Beckerich JM, Boisrame‐Baudevin A, Gaillardin C. Yarrowia lipolytica: a model organism for protein secretion studies. International Microbiology: The Official Journal of the Spanish Society for Microbiology. 1998;1(2):123–30.
  69. 69. Otto C, Holz M, Barth G. Production of Organic Acids by Yarrowia lipolytica. In: Barth G, editor. Yarrowia lipolytica: Biotechnological Applications. Berlin, Heidelberg: Springer Berlin Heidelberg; 2013. p. 137–49.
  70. 70. Darvishi Harzevili F. Yarrowia lipolytica: An Overview. Chapter 1, Biotechnological Applications of the Yeast Yarrowia lipolytica. SpringerBriefs in Microbiology, Springer International Publishing; 2014. p. 1–16.
  71. 71. Kerscher S, Dröse S, Zwicker K, Zickermann V, Brandt U. Yarrowia lipolytica, a yeast genetic system to study mitochondrial complex I. Biochimica et Biophysica Acta (BBA) – Bioenergetics. 2002;1555(1–3):83–91.
  72. 72. Kerscher SJ, Okun JG, Brandt U. A single external enzyme confers alternative NADH:ubiquinone oxidoreductase activity in Yarrowia lipolytica. Journal of Cell Science. 1999;112(Pt 14):2347–54.
  73. 73. Medentsev AG, Arinbasarova AY, Golovchenko NP, Akimenko VK. Involvement of the alternative oxidase in respiration of Yarrowia lipolytica mitochondria is controlled by the activity of the cytochrome pathway. FEMS Yeast Research. 2002;2(4):519–24.
  74. 74. Guerrero‐Castillo S, Vazquez‐Acevedo M, Gonzalez‐Halphen D, Uribe‐Carvajal S. In Yarrowia lipolytica mitochondria, the alternative NADH dehydrogenase interacts specifically with the cytochrome complexes of the classic respiratory pathway. Biochimica et Biophysica Acta. 2009;1787(2):75–85.
  75. 75. Cook GM, Poole RK. Oxidase and periplasmic cytochrome assembly in Escherichia coli K‐12: CydDC and CcmAB are not required for haem‐membrane association. Microbiology. 2000;146(Pt 2):527–36.
  76. 76. Wu M, Sun LV, Vamathevan J, Riegler M, Deboy R, Brownlie JC, et al. Phylogenomics of the reproductive parasite Wolbachia pipientis wMel: a streamlined genome overrun by mobile genetic elements. PLoS Biology. 2004;2(3):E69.
  77. 77. Klasson L, Walker T, Sebaihia M, Sanders MJ, Quail MA, Lord A, et al. Genome evolution of Wolbachia strain wPip from the Culex pipiens group. Molecular Biology and Evolution. 2008;25(9):1877–87.
  78. 78. Haddock BA, Jones CW. Bacterial respiration. Bacteriological Reviews. 1977;41(1):47–99.
  79. 79. Jones K. Acetilene reduction by mats of blue‐green algae in sub‐tropical grassland: possible contribution by other micro‐organisms. New Phytologist. 1977;78(2):437–40.
  80. 80. Ng TCN, Laheri AN, Maier RJ. Cloning, sequencing, and mutagenesis of the cytochrome c4 gene from Azotobacter vinelandii: characterization of the mutant strain and a proposed new branch in the respiratory chain. Biochimica et Biophysica Acta (BBA) – Bioenergetics. 1995;1230(3):119–29.
  81. 81. Bertsova YV, Bogachev AV, Skulachev VP. Two NADH:ubiquinone oxidoreductases of Azotobacter vinelandii and their role in the respiratory protection. Biochimica et Biophysica Acta. 1998;1363(2):125–33.
  82. 82. González PJ, Correia C, Moura I, Brondino CD, Moura JJG. Bacterial nitrate reductases: molecular and biological aspects of nitrate reduction. Journal of Inorganic Biochemistry. 2006;100(5–6):1015–23.
  83. 83. Whittaker MM, Whittaker JW. A glutamate bridge is essential for dimer stability and metal selectivity in manganese superoxide dismutase. The Journal of Biological Chemistry. 1998;273(35):22188–93.
  84. 84. Cannio R, Fiorentino G, Morana A, Rossi M, Bartolucci S. Oxygen: friend or foe? Archaeal superoxide dismutases in the protection of intra‐ and extracellular oxidative stress. Frontiers in Bioscience: A Journal and Virtual Library. 2000;5:D768–79.
  85. 85. Klotz MG, Loewen PC. The molecular evolution of catalatic hydroperoxidases: evidence for multiple lateral transfer of genes between prokaryota and from bacteria into eukaryota. Molecular Biology and Evolution. 2003;20(7):1098–112.
  86. 86. Zamocky M, Furtmuller PG, Obinger C. Evolution of catalases from bacteria to humans. Antioxidants & Redox Signaling. 2008;10(9):1527–48.
  87. 87. Nölling J, Breton G, Omelchenko MV, Makarova KS, Zeng Q, Gibson R, et al. Genome sequence and comparative analysis of the solvent‐producing bacterium Clostridium acetobutylicum. Journal of Bacteriology. 2001;183(16):4823–38.
  88. 88. Peacock AJ. ABC of oxygen: oxygen at high altitude. British Medical Journal. 1998;317(7165):1063–6.
  89. 89. Hall JE, Guyton AC. Unit VII Respiration. In: Hall J, editor. Textbook of Medical Physiology. 12. Philadelphia, PA, USA: Elsevier; 2012.
  90. 90. Popel AS. Theory of oxygen transport to tissue. Critical Reviews in Biomedical Engineering. 1989;17(3):257–321.
  91. 91. Wilson DF, Rumsey WL, Green TJ, Vanderkooi JM. The oxygen dependence of mitochondrial oxidative phosphorylation measured by a new optical method for measuring oxygen concentration. The Journal of Biological Chemistry. 1988;263(6):2712–8.
  92. 92. Geng M, Duan Z. Prediction of oxygen solubility in pure water and brines up to high temperatures and pressures. Geochimica et Cosmochimica Acta. 2010;74(19):5631–40.
  93. 93. Chapelle G, Peck LS. Amphipod crustacean size spectra: new insights in the relationship between size and oxygen. Oikos. 2004;106(1):167–75.
  94. 94. Beman JM, Carolan MT. Deoxygenation alters bacterial diversity and community composition in the ocean's largest oxygen minimum zone. Nature Communications. 2013;4:2705.
  95. 95. Borsuk ME, Stow CA, Luettich Jr RA, Paerl HW, Pinckney JL. Modelling oxygen dynamics in an intermittently stratified estuary: estimation of process rates using field data. Estuarine, Coastal and Shelf Science. 2001;52(1):33–49.
  96. 96. Engle V, Summers JK. Refinement, validation, and application of a benthic condition index for Northern Gulf of Mexico estuaries. Estuaries. 1999;22(3):624–35.

Written By

Mónica Rosas‐Lemus, Cristina Uribe‐Alvarez, Martha Contreras‐ Zentella, Luis Alberto Luévano‐Martínez, Natalia Chiquete‐Félix, Norma Lilia Morales‐García, Emilio Espinosa Simón, Adriana Muhlia‐ Almazán, Edgardo Escamilla‐Marván and Salvador Uribe‐Carvajal

Reviewed: April 13th, 2016 Published: October 26th, 2016