The soil formation – one of the famous mechanisms in biosphere

Bakhnov V. K.

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Hydrosphere is the most ancient part of biosphere the further development of which is directed to the settling of aerial surroundings and lithosphere cover by organisms. This main track was assumed as a basis of partition of development history into three periods such as hydrozemic, atmozemic and lithozemic ones. Each period is accompanied by respective trend of soil formation, for example hydrozemic period corresponds with underwater soil formation and atmozemic and lithozemic ones to swamp and land respectively. Soil formation influenced on the development of biota by double means, in other words through the change of outer conditions which happened as a result of soil formation, and indirectly through the soil as a habitat

Keywords: Biosphier, soil formation, marsh, evolution.

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Issue: 4, 2008

Rubric: Theoretical Problems of Bog and Peat Studies

Pages: 11 — 14

Downloads: 997