|
|
| H, He, Li, Be, B, C, N, O, F, Ne, Na, Mg, Al, Si, P, S, Cl, Ar, K, Ca, Sc, Ti, V, Cr, Mn, Fe, Co, Ni, Cu, Zn, Ga, Ge, As, Se, Br, Kr, Rb, Sr, Y, Zr, Nb, Mo, Tc, Ru, Rh, Pd, Ag, Cd, In, Sn, Sb, Te, I, Xe, Cs, Ba, Lanthanides, Hf, Ta, W, Re, Os, Ir, Pt, Au, Hg, Tl, Pb, Bi, Po, At, Rn, Fr, Ra, Actinides | | Figure 3–1 Elements essential to animal life and health. Bulk elements (shaded orange) are structural components of cells and tissues and are required in the diet in gram quantities daily. For trace elements (shaded yellow), the requirements are much smaller: for humans, a few milligrams per day of Fe, Cu, and Zn, even less of the others. The elemental requirements for plants and microorganisms are very similar to those shown here. | |
| | Only about 30 of the more than 90 naturally occurring chemical elements are essential to living organisms. Most of the elements in living matter have relatively low atomic numbers; only five have atomic numbers above that of selenium, 34 (Fig. 3–1). The four most abundant elements in living organisms, in terms of the percentage of the total number of atoms, are hydrogen, oxygen, nitrogen, and carbon, which together make up over 99% of the mass of most cells. They are the lightest elements capable of forming one, two, three, and four bonds, respectively (Fig. 3–2). In general, the lightest elements form the strongest bonds. Six of the eight most abundant elements in the | | Atom, Number of unpaired electrons (in red), Number of electrons in complete outer shell, Dihydrogen, Water, Ammonia, Methane, Sulfur dioxide, Phosphoric acid | | Figure 3–2 Covalent bonding. Two atoms with unpaired electrons in their outer shells can form covalent bonds with each other by sharing electron pairs. Atoms participating in covalent bonding tend to fill their outer electron shells. | |
| | human body are also among the nine most abundant elements in seawater (Table 3–1), and several of the elements abundant in humans are components of the atmosphere and were probably present in the atmosphere before the appearance of life on earth. Primitive seawater was most likely the liquid medium in which living organisms first arose, and the primitive atmosphere was probably a source of methane, ammonia, water, and hydrogen, the starting materials for the evolution of life. The trace elements (Fig. 3–1) represent a miniscule fraction of the weight of the human body, but all are absolutely essential to life, usually because they are essential to the function of specific enzymes (Table 3–2). | | Table 3–1, Table 3–2 Elemental abundance in seawater, the human body, and the earth’s crust* / Seawater (%), Human body (%), Earth’s crust (%) / H, 66, H, 63, O, 47 / O, 33, O, 25.5, Si, 28 / Cl, 0.33, C, 9.5, Al, 7.9 / Na, 0.28, N, 1.4, Fe, 4.5 / Mg, 0.033, Ca, 0.31, Ca, 3.5 / S, 0.017, P, 0.22, Na, 2.5 / Ca, 0.0062, Cl, 0.08, K, 2.5 / K, 0.0060, K, 0.06, Mg, 2.2 / C, 0.0014 / * Values are given as percentage of total number of atoms.The biological functions of some trace elements / Element, Example of biological function / Fe, Electron carrier in oxidation–reduction reactions / Cu, Component of mitochondrial oxidase / Mn, Cofactor of the enzyme arginase and other enzymes / Zn, Cofactor of dehydrogenases / Co, Component of vitamin B12 / Mo, Component of N2-fixing enzyme / Se, Component of the enzyme glutathione peroxidase / V, Cofactor of the enzyme nitrate reductase / Ni, Cofactor of the enzyme urease / I, Component of thyroid hormone / Mg, Cofactor in photosynthesis | |
|
|
|
|
|