The Structure of the Biosphere from the Point of View of the Concept of the Biogeome

The authors propose considering the structure and evolutionary changes in the biosphere from the standpoint of a biogeomics approach. It is necessary to study biogeomes as systems of ecosystems that are similar in their structural and functional organization. Biogeomes are structural units of the biosphere and elements of biospheromerons. Based on an analysis of the concept of the “biome”, it is concluded that its primary use is limited, since it is only based on the phytocenotic approach; however, it should be noted that it is this aspect that is currently developing most successfully. The authors note that A. Tansley (1935), critically examining the concept of the biome, essentially introduced the concept of the biogeome, which is broader than the concept of the “ecosystem”. The authors consider the characteristics of five main terrestrial and atmobiontic biogeomes (hylea, grass biogeome, tundra, and desert biogeome), as well as seven hydrosphere biogeomes (shelf, pelagic ocean biogeome, bathyal–abyssal bottom, hydrothermal, bioherm, limnobiogeome, and rheobiogeome). They are grouped, based on the physiognomic approach and an analysis of the “biogeomic formulas”, into the following three types: biotic (the appearance of ecosystems is determined by the biome), oligobiotic (the appearance of ecosystems is determined by both the biome and abiotic elements, as well as the geome), and nanobiotic, where the general appearance of ecosystems is determined by the elements of the geome. The biogeomic approach allows us to consider the organization of terrestrial and hydrosphere ecosystems in a general way and to introduce important elements into the structure of the Earth’s biosphere, which has gone through complex and lengthy stages during its evolution.