Mollic epipedons are created by long-term addition of organic materials derived from plant roots and typically have soft, granular soil structure.Mollisols typically occur in savannahs and mountain valleys (such as Central Asia, and the North American Great Plains).Though most other soil orders known today were formed at the beginning of the Carboniferous Ice Age 280 million years ago, Mollisols are best known from the paleopedological record as early as the Eocene.Soils which are mostly similar to Mollisols but contain either continuous or discontinuous permafrost, consequently affected by cryoturbation are common in high mountain plateaus of Tibet and the Andean altiplano.These soils are especially common in parts of South America in the Paraná River basin receiving abundant but erratic rainfall and extensive deposition of clay-rich minerals from the Andes.
Mollisols are generally associated with the
steppe
biome