The evolutionary history of the biosphere is characterized by aromorphosis: biological evolution by a general increase in the degree of organization without developing high degrees of specialization [1]. Four major stages of the evolutionary transformation of life (mega-aromorphoses) can be established in the recorded succession of the Neoproterozoic (Ediacaran)-Phanerozoic aromorphoses reflecting changes of the dominant groups. They are defined by the appearance of archetypes ensuring the possibilities of a prolonged and diverse rise of the level of their organization leading to significant increase in the activity of living organisms and their emerging independence from the environment. A successive series of developmental stages exploiting of the aquatic environment of the Neoproterozoic (Ediacaran)-Phanerozoic biosphere can be established based on their dominant groups: the biospheres of protozoans, proto-metazoans, protobilaterals, fishes and amphibians.
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