Soil and Nutrient Cycling

The cold climate and short growing season in coniferous forests lead to slow decomposition rates, resulting in the accumulation of organic material known as the "duff layer." This layer is nutrient-rich and supports the growth of plants like mosses and lichens. The process contributes to nutrient enrichment, creating an ecosystem where plants adapted to cold, nutrient-poor conditions thrive. Additionally, the slow decomposition leads to acidic soils due to the buildup of organic acids. This unique cycle of decomposition and nutrient dynamics shapes the distinct characteristics of coniferous forest ecosystems.