- •It is recommended for publishing as a study aid by the Editorial Board of Tomsk Polytechnic University
- •Соntents
- •Introduction
- •1. History of knowledge development about biosphere chemical composition and scale of its transformations
- •Global emission of chemical elements (thous.T/year) (according to V.V. Yermakov, 2003)
- •2. Key approachers to classification of chemical elements
- •Fig. 1 Classification of elements in human organism in terms of abundance and use (Underwood e., 1962)
- •Vital elements in composition of organisms (according to а. Lenindger)
- •Content of some elements in plants, animal and human organisms, mg/kg
- •Concentration of cations in marine water and organisms liquids of some mammals and birds, mg/kg (Bgatov а.V., 1999, with recalculations of Ignatova т.N., 2009)
- •Biogenetic classification of elements
- •3. Factors and processes element composition formation of living matter
- •4. Regional aspects of biogeochemistry
- •4.1. Conditions of the Natural Environment Components According to Ecological-Geochemical Monitoring and Population Health Data (Tomsk Region)
- •Geochemical specific characteristics in districts of Tomsk region to maximum element concentration in pathologically changed thyroid glands (relative to regional monitoring)
- •Different diseases of separate thyroid gland pathology types in districts of Tomsk region per 1000 persons (during 5 years)
- •4.2. Element composition of human organs and tissues
- •Contemporary estimation of the environmental pathology (wt. %) and trace elements (mg/kg) in a human body (From Ulf Lindh, 2005 with changes)
- •Comparative estimation of element analysis results obtained by inaa method with published data of domestic and international standards
- •4.3. Biogeochemistry of uranium and thorium
- •Thorium content in the plants of the Large Vasyugan marsh, mg/kg (dm) (“Geochemistry…”, 2002)
- •4.4. Rare earth element in human organs and tissues
- •4.5. Element content in children hair samples
- •Comparative analysis of evaluation level of the chemical element concentration in human hair (mg/kg, dry weight)
- •Comparative data of children hair composition (mg/kg, dry weight) from different regions of Russia, Belorussia and Kazakhstan
- •Geochemical specification of population hair in Tomsk oblast and other regions (n – number of samples)
- •Conclusion
- •References
- •Geochemistry of living organisms
- •Published in author’s version
- •Printed in the tpu Publishing House in full accordance with the quality of the given make up page
Content of some elements in plants, animal and human organisms, mg/kg
Element |
Plants |
Animals |
Human organism |
Hydrogen |
55000 |
70000 |
99900 |
Lithium |
0,098 |
0,021 |
|
Boron |
50,9 |
0,506 |
0,28 |
Carbon |
454000 |
465000 |
228000 |
Nitrogen |
30002 |
100002 |
25700 |
Oxygen |
410000 |
186000 |
0,61 |
Fluorine |
0,49-40 |
150-499,7 |
37,13 |
Sodium |
1196 |
4002 |
1430 |
Magnesium |
3168 |
984 |
270 |
Aluminum |
494 |
3,9-96,2 |
0,87 |
Silicon |
196-5012 |
112-5992 |
|
Phosphorous |
2294 |
16988-45440 |
11000 |
Sulfur |
3392 |
4992 |
1900 |
Chlorine |
2023,5 |
2804,5 |
1,35*103 |
Potassium |
14040 |
7410 |
1,9*103 |
Calcium |
18000 |
200-8500 |
14300 |
Titanium |
0,96 |
0,192 |
|
Vanadium |
1,53 |
0,153 |
|
Chromium |
0,228 |
0,073 |
9,4*10-2 |
Manganese |
629,7 |
0,22 |
0,17 |
Iron |
140 |
162,4 |
59,9 |
Cobalt |
0,472 |
0,0295 |
21,4*10-3 |
Nickel |
43,2 |
0,82 |
0,14 |
Copper |
14 |
2,54 |
1,03 |
Zinc |
99,4 |
159 |
32,8 |
Gallium |
0,056 |
0,0055 |
|
Rubidium |
19,5 |
17 |
9,7 |
Strontium |
26,4 |
14,08 |
4,5 |
Zirconium |
0,64 |
0,27 |
|
Barium |
13,7 |
0,685 |
0,31 |
Lead |
2,7 |
2,07 |
1,7 |
Uranium |
|
|
1,28*10-3 |
Actually, the first four elements could form the whole row of organic molecules such as elementary hydrocarbons, aldehydes, spirits and a number of amino acids. Academician А.I. Oparin showed this in his model experiments simulating the natural conditions, assumingly existed about 3 bill. years ago. The same elements are the frame of any organic molecule.
To the four elements mentioned, above undoubtedly predominated in the ancient atmosphere and hydrosphere, and surely included in before-cellular forms of life it necessary to add two more – phosphorous and sulfur.
Indeed, life is impossible to imagine without two things – transmission of hereditary information and energy. Phosphorous forms the basis of hereditary molecules – DNA and RNA as well as a molecule generating energy – АТP. A commonly accepted F. Engels’s definition: "Life as a way of existence of protein bodies..." – is not correct in its sense as some "living" viruses do without protein presenting only a chain of DNA or RNA capable of autonomous existence.
As for sulfur this element forms the composition of two out of 20 basic amino acids – methionine and cysteine, units constituting proteins of all higher organisms, in this case the composition includes sulfur forming disulfide bridges produces tertiary, globular protein structure.
Both phosphorous and sulfur are products of volcanic emissions. Among the elements of similar origin they are one of the lightest and capable of reactions. Their concentration in ancient ocean, apparently, reached the level necessary for the primary life forms early enough (in evolutionary sense.
All the elements considered above have in common the fact that they are abundant in all cells, organs, and tissues of both plant and animal organisms due to the properties mentioned above, i.e. they are evolutionarily "through", though the latter two occupy a comparatively small place with respect to weight as compared to the former four.
In the process of complication of living organisms their functions extended and specialized. For instance, with formation of skeleton the latter two elements were found in composition of bone structure, but with formation of blood system – in composition of sulfate and phosphate buffers of blood.
Those six elements, from the standpoint of biogenic classification, should be referred to the elements of the first group or the primary elements.
Cellular level of life and macroelements
Combination of six elements considered above could support before-cellular life level. Monocellular organisms are assumed to appear on the Earth in the littoral zones of the ancient ocean about 3 bill. years ago. Their appearance was the beginning of development of the first internal mineral homeostasis system: living matter gained the possibility to border from the external environment by means of developed cellular membrane, having its inner self being. For this purpose the development of buffer system was required that could be provided by cations, the concentration of which reached the optimum in the process of leaching at the earlier stages of mineral hydrosphere evolution – potassium, sodium, calcium and magnesium, as well as anions of volcanic activity in addition to already used phosphorous and sulfur – chlorine.
The following aspect should be paid special attention. Most researchers dealing with chemistry of human body compare its mineral composition with that of contemporary land, whereas 90% of living organism evolution took place in the Ocean. In Table 3 the mineral composition of contemporary Ocean with mineral composition of some animal’s blood is compared. The Table presents the data obtained by different scientists. Apparently, on the basis of these data one can judge about the formation process of sodium-potassium pumping system in living cells.
Table 3
