The previously mentioned relations and regularities are required for such a systematic analysis.

Conclusion on Chapter 3.

The width of annual tree-rings is the important indicator that helps evaluate cosmic energies. Thus, it is crucial to understand that the relation between the width of tree-rings and the Earth’s rotational velocity will be different depending on the region.

Chapter 4. From concentration of isotopes contained in annual growth rings to analysis of cosmic energies’ dynamics and development of the society

4.1 Lack of sustained relations between the width of annual growth rings and concentration of isotopes contained in them in a 40-year prospective

The intensity of isotopes’ formation in every period of time is connected with the uneven infiltration of isotopes from the atmosphere into the soil and then into the roots and into tree’s trunk.

The concentration of the isotopes in soil differs depending on the soil depth (see Brian M. Fagan, Christopher R. DeKors, Archeology, Moscow, 2007).

Due to the different concentration in soil layers, the isotopes permeate a tree unevenly.

Different studies show that even during the Maunder Minimum period, the concentration of the isotopes contained in annual rings was unstable and constantly changing.

M.G. Ogurtsov, 2007 http://naukarus.com/kosmogennye-izotopy-i-ih-rol-v-sovremennoy-paleoastrofizike-solntsa

However, it should be noted that it only concerns short-term fluctuations. After 50 years the concentration of the isotopes contained in annual rings of a tree accurately correlates with the historical events.

There are two aspects which explain why more attention should be paid to the data about concentration of the isotopes contained in annual rings that are more than 40 years old.

Firstly, the data on concentration of the isotopes contained in annual rings in a particular region helps to understand the dynamics of magnetic and gravitational field strength in this region because it is reasonable to suppose that they influence transportation of the isotopes through the roots and trunk of a tree. (Cholmansky et al)

Secondly, changes in the concentration of the isotopes of different substances contained in annual rings and changes in ice cores of hundreds of years old take place at one historical period. Moreover, these changes are connected with the significant historic events which are important not only for the history of biome’s development but also for the history of mankind. When taking this into consideration, it becomes possible to understand history deeper and look at it from the new perspective.

In the 40-years prospective isotopes concentration of different substances in the air in fast-expanding biome area is connected with the Earth’s rotational velocity. However, this connection has the aligned index. Rapid changes in the Earth’s rotational velocity (during several years) and peaks in isotopes’ formation are smoothed inside the annual rings with the process of isotopes’ probability distribution of different substances through the whole planet, through biome. In comparison, the Earth’s rotational velocity may be considered as a mean within the span from 20 to 40 years.

The local data on concentration of the isotopes of different substances in annual rings, mushrooms and berries may be correlated with the Earth’s rotational velocity and with the time period of one year. It may be proved even considering nuclear weapons testing and release of radioactive material and the isotopes into the environment after catastrophic nuclear accidents (Chernobyl and Fukushima Daiichi disasters e.g).