Histosols are organic-rich soils found in wetlands like bogs and peat marshes, characterized by high water retention and low decomposition rates, leading to the accumulation of organic matter. In contrast, Aridisols are dry, mineral-rich soils prevalent in deserts and arid regions, where limited moisture inhibits organic matter accumulation and promotes soil salinity. While Histosols support diverse wetland ecosystems, Aridisols are typically less fertile and support sparse vegetation adapted to extreme dryness. Both soil types reflect their respective ecosystems' hydrological conditions and biological activity.
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