1.Biosphere and its stability
a) Fundamentals of biological organization
b) Nutrients
c) Resources of the biosphere
d) Structure of the biosphere
e) Evolution of the Biosphere
2. Concept of living matter
3. Global biogeochemical cycles
4.Conclusion
5.Literature
The biosphere is the global sum of all ecosystems. It can also be termed the zone of life on Earth, a closed system (apart from solar and cosmic radiation and heat from the interior of the Earth), and largely selfregulating. By the most general biophysiological definition, the biosphere is the global ecological system integrating all living beings and their relationships, including their interaction with the elements of the lithosphere, geosphere, hydrosphere, and atmosphere. The biosphere is postulated to have evolved, beginning with a process of biopoesis (life created naturally from non-living matter such as simple organic compounds) or biogenesis (life created from living matter), at least some 3.5 billion years ago.The earliest evidence for life on Earth includes biogenic graphite found in 3.7 billion-year-old metasedimentary rocks from Western Greenland and
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Subsequent investigation of the "Man - Economy - Biota Wednesday" should start with her ancestors and foundations wildlife oioty. The main attention should be paid to the quantitative characteristics of the system in the sequence of "organism population - ecosystem - biosphere" that determine their interaction with a doy and which, when oditsya consider when solving applied problems of ecology.
All of these fundamental properties of living systems to some extent already been realized at the cellular level. However, the completeness of all natural phenomena of life is presented only in the last two - ecosystem levels (or even only on the biosphere), since no cell or one organism, any form can exist without a plurality of other cells, organisms, species and conditions they create environment.
Competence Ecology begins with the