Soil organic carbon (SOC) can be divided into plant-derived and microbial-derived carbon. Studying the latitudinal variation of these two sources and their controlling factors is critical to understanding SOC persistence and stabilization.
Study reveals latitude patterns, controlling factors of microbial residues and lignin phenol accumulation in forest soil retrieved 4 July 2024 from https://phys.org/news/2024-07-reveals-latitude-patterns-factors-microbial.html
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