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hosil boʻlishгенезис

evolution of the alive nature depending on no environmental conditions, driven and regulated by the internal (non-material) factors. The theory of A. g. is analogous to a vitalizm. In ecology this concept is usually applied to communities and ecosystems.

process of formation of organic compounds by living organisms. A theory of B. denies a concept of origin of life on the Earth as a result of generation of living things from a lifeless matter. A basic idea of B. lays in opposing of the living things from the lifeless substance and idea of eternity of life.

atmosfera, gidrosfera va tirik modda taʼsirida yer qobigʻining yuqori qismlaridagi hamda uning yuzidagi togʻ jinslari va maʼdanlarning fizik va kimyoviy oʻzgarish jarayonlarining jami.

process (assumed) of origin of life with gradual evolution of matters into more complicated forms of inorganic nature and originating of biopolymers (nucleon acids, protein, etc.) which are characterized by the basic properties of living things and, first and foremost, by capacities to metabolism, as an indispensable condition of their existence.

individual development of an organism, all complex of its transformations from origin up to the end of its life.

all processes of physical chemical transformation of rocks and minerals in top horizons of the earth crust and on its surface under the influence of atmosphere, hydrosphere and living matters.

historical development of living organisms as a whole, and of separate taxonomic groups. The term Ph. was introduced by E.Hekkel in 1866.

an endogenic development of a territorial collection of ecosystems as a result of originating and forming of new species and loss of existing ones.

a process of forming and development of vegetative communities.

processes of an internal genesis caused by internal reasons (e.g., disintegration of radio-isotopes, earthquake, volcanism).