Byproducts of normal mitochondrial metabolism and homeostasis include the buildup of potentially damaging levels of reactive oxygen species (ROS), Ca2+, etc., which must be normalized. Evidence suggests that brief mitochondrial permeability transition pore (mPTP) openings play an important physiological role maintaining healthy mitochondria homeostasis. Adaptive and maladaptive responses to redox stress may involve mitochondrial channels such as mPTP and inner membrane anion channel (IMAC). Their activation causes intra- and intermitochondrial redox-environment changes leading to ROS release. This regenerative cycle of mitochondrial ROS formation and release was named ROS-induced ROS release (RIRR). Brief, reversible mPTP opening-associated ROS release apparently constitutes an adaptive housekeeping function by the timely release from mitochondria of accumulated potentially toxic levels of ROS (and Ca2+). At higher ROS levels, longer mPTP openings may release a ROS burst leading to destruction of mitochondria, and if propagated from mitochondrion to mitochondrion, of the cell itself. The destructive function of RIRR may serve a physiological role by removal of unwanted cells or damaged mitochondria, or cause the pathological elimination of vital and essential mitochondria and cells. The adaptive release of sufficient ROS into the vicinity of mitochondria may also activate local pools of redox-sensitive enzymes involved in protective signaling pathways that limit ischemic damage to mitochondria and cells in that area. Maladaptive mPTP- or IMAC-related RIRR may also be playing a role in aging. Because the mechanism of mitochondrial RIRR highlights the central role of mitochondria-formed ROS, we discuss all of the known ROS-producing sites (shown in vitro) and their relevance to the mitochondrial ROS production in vivo.

Mitochondrial Reactive Oxygen Species (ROS) and ROS-Induced ROS Release

Majors topics addressed in this review on zinc physiology are ; 1) chemistry and biochemistry; 2) interface of biochemistry and physiology of zinc; 3) physiology and cell and molecular biology; 4) pathology

The biochemical basis of zinc physiology

Virtually all nonequilibrium electron transfers on Earth are driven by a set of nanobiological machines composed largely of multimeric protein complexes associated with a small number of prosthetic groups. These machines evolved exclusively in microbes early in our planet's history yet, despite their antiquity, are highly conserved. Hence, although there is enormous genetic diversity in nature, there remains a relatively stable set of core genes coding for the major redox reactions essential for life and biogeochemical cycles. These genes created and coevolved with biogeochemical cycles and were passed from microbe to microbe primarily by horizontal gene transfer. A major challenge in the coming decades is to understand how these machines evolved, how they work, and the processes that control their activity on both molecular and planetary scales.

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The Microbial Engines That Drive Earth's Biogeochemical Cycles

For present purposes, a protein-bound metal site consists of one or more metal ions and all protein side chain and exogenous bridging and terminal ligands that define the first coordination sphere of each metal ion. Such sites can be classified into five basic types with the indicated functions: (1) structural -- configuration (in part) of protein tertiary and/or quaternary structure; (2) storage -- uptake, binding, and release of metals in soluble form: (3) electron transfer -- uptake, release, and storage of electrons; (4) dioxygen binding -- metal-O{sub 2} coordination and decoordination; and (5) catalytic -- substrate binding, activation, and turnover. The authors present here a classification and structure/function analysis of native metal sites based on these functions, where 5 is an extensive class subdivided by the type of reaction catalyzed. Within this purview, coverage of the various site types is extensive, but not exhaustive. The purpose of this exposition is to present examples of all types of sites and to relate, insofar as is currently feasible, the structure and function of selected types. The authors largely confine their considerations to the sites themselves, with due recognition that these site features are coupled to protein structure at all levels. In themore » next section, the coordination chemistry of metalloprotein sites and the unique properties of a protein as a ligand are briefly summarized. Structure/function relationships are systematically explored and tabulations of structurally defined sites presented. Finally, future directions in bioinorganic research in the context of metal site chemistry are considered. 620 refs.« less

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Structural and Functional Aspects of Metal Sites in Biology

▪ Abstract Proton-coupled electron transfer (PCET) is an important mechanism for charge transfer in a wide variety of systems including biology- and materials-oriented venues. We review several are...

/pdf/proton-coupled-electron-transfer-3oyvp0w9qd.pdf

Proton-Coupled Electron Transfer

Part 1 The chemical and physical factors controlling the elements of life: the chemical elements in biology the principles of the chemical uptake and speciation of the elements in biology physical separation of the elements - compartments and zones in biology kinetic considerations of element reactions energy in biological systems and hydrogen biochemistry the functional value of the chemical elements in biological systems. Part 2 The roles of individual elements in biology: the role of biological macromolecules and polymers sodium and potassium - osmotic control, electrolyte equilibria and currents magnesium - primary metabolism and polynucleotide structures calcium - controls and triggers zinc - Lewis acid catalysis and regulation non-haem iron redox reactions and controls haem iron - coupled redox reactions manganese copper - extracellular redox reactions and matrix formation nickel and cobalt - primitive hydrogen and organmetallic biochemistry molybdenum and vanadium - nitrogen fixation and extracellular oxygen transfer phosphorus and silicon - condensation reactions of non-metals redox non-metals - sulphur, selenium and halogens. Part 3 The co-operative interaction of elements in living systems: biomineralization and shape homeostasis and morphogenesis man's interference in element distribution - medicines and pollutants.

The Biological Chemistry of the Elements: The Inorganic Chemistry of Life

/pdf/the-biological-chemistry-of-the-elements-4yc4q018cx.pdf

The Biological Chemistry of the Elements

https://www.pnas.org/content/pnas/59/2/498.full.pdf

Metalloenzymes: the entatic nature of their active sites

Possible functions of chains of catalysts

Evolution is treated here in a novel way. DNA or any other code is considered to be conservative and therefore, once life began, it would prevent change. Change was imposed upon the DNA code as a stress resulting in vulnerability to 'advantageous' DNA damage and mutation. In this respect it is the stress, the changing environment, that opened up a possibility of evolution once an early life form had optimised itself in primitive circumstances. Here I examine the initial slow-coming-to-terms with the environment of primitive life, and then its evolution as the environment forced the DNA into novel development by introducing chemical elements in new forms. The situation today is no different. Environmental change is hostile to present day life and will lead to further evolution.

R. J. P. Williams

Papers

The Biological Chemistry of the Elements: The Inorganic Chemistry of Life

The Biological Chemistry of the Elements

Metalloenzymes: the entatic nature of their active sites

Possible functions of chains of catalysts

The Natural Selection of the Chemical Elements